﻿nullJ	Hoem, FS; van den Broek, K; López-Quirós, A; van de Lagemaat, SHA; Bohaty, SM; Hillenbrand, CD; Larter, RD; van Peer, TE; Brinkhuis, H; Sangiorgi, F; Bijl, PK				Hoem, Frida S.; van den Broek, Karlijn; Lopez-Quiros, Adrian; van de Lagemaat, Suzanna H. A.; Bohaty, Steve M.; Hillenbrand, Claus-Dieter; Larter, Robert D.; van Peer, Tim E.; Brinkhuis, Henk; Sangiorgi, Francesca; Bijl, Peter K.			Stepwise Oligocene-Miocene breakdown of subpolar gyres and strengthening of the Antarctic Circumpolar Current	JOURNAL OF MICROPALAEONTOLOGY			English	Article							WALLED DINOFLAGELLATE CYSTS; OFFSHORE WILKES LAND; ICE-SHEET SENSITIVITY; DRAKE PASSAGE; EOCENE-OLIGOCENE; ATLANTIC SECTOR; STRATIGRAPHIC CALIBRATION; SOUTHERN-HEMISPHERE; KERGUELEN PLATEAU; SUBTROPICAL FRONT	Through the Cenozoic (66-0 Ma), the dominant mode of ocean surface circulation in the Southern Ocean transitioned from two large subpolar gyres to circumpolar circulation with a strong Antarctic Circumpolar Current (ACC) and complex ocean frontal system. Recent investigations in the southern Indian and Pacific oceans show warm Oligocene surface water conditions with weak frontal systems that started to strengthen and migrate northwards during the late Oligocene. However, due to the paucity of sedimentary records and regional challenges with traditional proxy methods, questions remain about the southern Atlantic oceanographic transition from gyral to circumpolar circulation, with associated development of frontal systems and sea ice cover in the Weddell Sea. Our ability to reconstruct past Southern Ocean surface circulation and the dynamic latitudinal positions of the frontal systems has improved over the past decade. Specifically, increased understanding of the modern ecologic affinity of organic-walled dinoflagellate cyst (dinocyst) assemblages from the Southern Ocean has improved reconstructions of distinct past oceanographic conditions (sea surface temperature, salinity, nutrients, and sea ice) using downcore assemblages from marine sediment records. Here we present new late Oligocene to latest Miocene (similar to 26-5 Ma) dinocyst assemblage data from marine sediment cores in the southwestern Atlantic Ocean (International Ocean Discovery Program (IODP) Site U1536, Ocean Drilling Program (ODP) Site 696 and piston cores from Maurice Ewing Bank). We compare these to previously published latest Eocene-latest Miocene (similar to 37-5 Ma) dinocyst assemblage records and sea surface temperature (SST) reconstructions available from the SW Atlantic Ocean in order to reveal oceanographic changes as the Southern Ocean gateways widen and deepen. The observed dinocyst assemblage changes across the latitudes suggest a progressive retraction of the subpolar gyre and southward migration of the subtropical gyre in the Oligocene-early Miocene, with strengthening of frontal systems and progressive cooling since the middle Miocene (similar to 14 Ma). Our data are in line with the timing of the removal of bathymetric and geographic obstructions in the Drake Passage and Tasmanian Gateway regions, which enhanced deep-water throughflow that broke down gyral circulation into the Antarctic circumpolar flow. Although the geographic and temporal coverage of the data is relatively limited, they provide a first insight into the surface oceanographic evolution of the late Cenozoic southern Atlantic Ocean.	[Hoem, Frida S.; van den Broek, Karlijn; van de Lagemaat, Suzanna H. A.; Brinkhuis, Henk; Sangiorgi, Francesca; Bijl, Peter K.] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Lopez-Quiros, Adrian] Univ Granada, Dept Stratig & Paleontol, Granada, Spain; [Bohaty, Steve M.; van Peer, Tim E.] Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton, England; [Hillenbrand, Claus-Dieter; Larter, Robert D.] British Antarctic Survey, Cambridge, England; [van Peer, Tim E.] UCL, Dept Earth Sci, London, England; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, Dept Ocean Syst Res, Texel, Netherlands; [Hoem, Frida S.] Univ Bergen, Dept Earth Sci, Bergen, Norway; [Bohaty, Steve M.] Heidelberg Univ, Inst Educ Sci, Heidelberg, Germany; [van Peer, Tim E.] Univ Leicester, Sch Geog Geol & Environm, Leicester, England	Utrecht University; University of Granada; NERC National Oceanography Centre; University of Southampton; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of London; University College London; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bergen; Ruprecht Karls University Heidelberg; University of Leicester	Hoem, FS (通讯作者)，Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands.; Hoem, FS (通讯作者)，Univ Bergen, Dept Earth Sci, Bergen, Norway.	frida.hoem@uib.no	Brinkhuis, Henk/IUO-8165-2023; van Peer, Tim/R-8157-2016; Lopez Quiros, Adrian/K-6513-2017	Brinkhuis, Henk/0000-0003-0253-6610; van Peer, Tim/0000-0003-3516-4198; Larter, Robert/0000-0002-8414-7389; Lopez Quiros, Adrian/0000-0002-7522-2834; Hoem, Frida/0000-0002-8834-6799	Dutch Research Council (Nederlandse Organisatie voor Wetenschappelijk Onderzoek, NWO) polar programme [ALW.2016.001]; European Research Council [802835]	Dutch Research Council (Nederlandse Organisatie voor Wetenschappelijk Onderzoek, NWO) polar programme; European Research Council(European Research Council (ERC))	This research has been supported by the Dutch Research Council (Nederlandse Organisatie voor Wetenschappelijk Onderzoek, NWO) polar programme (grant no.ALW.2016.001), and the European Research Council H2020 programme (grant no. 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J	Lorente, MA; Noto, C; Flaig, P				Lorente, Maria Antonieta; Noto, Christopher; Flaig, Peter			A glimpse into the Late Cretaceous (Cenomanian) palynology of the Arlington Archosaur Site, Texas, USA	PALYNOLOGY			English	Article; Early Access						Cenomanian; biostratigraphy; palaeoclimate; Arlington; Texas; USA	WESTERN INTERIOR SEAWAY; ANOXIC EVENT; DINOFLAGELLATE CYSTS; ORGANIC-MATTER; STRATIGRAPHY; BASIN; PALYNOSTRATIGRAPHY; WOODBINE; RIVER; NORTH	The Arlington Archosaur Site between Dallas and Fort Worth, Texas, USA, is known as a rich fossiliferous section. The age of these rocks is generally considered to be Middle Cenomanian, but conflicting evidence suggests they may be as young as the Late Cenomanian-Early Turonian. To address the issue, a palynological study was designed and conducted based on close sampling of the four lithofacies associations, labelled A to D, in ascending order. The study was quantitative and focused on palynological associations to determine the palaeoenvironment, palaeoclimate, biostratigraphy and age of the exposure. The rich palynological assemblages comprise spores from seedless plants, gymnosperms, angiosperms, fungi, freshwater algae, acritarchs and dinoflagellate cysts. Bryophyte spores were abundant mainly in Facies A and B, with Zlivisporis cenomanianus taking over the habitat of bryophytes in Facies D. Lycophytes abundant in the alluvial and coastal plains are considered to have been transported. Conifer pollen represent the predominant group of gymnosperms, mainly transported into the section. Freshwater algal remains include Schizophacus laevigatus/Ovoidites parvus, Schizosporis reticulatus, Botryococcus sp. and Pediastrum sp. The overall terrestrial vegetation represented in the palynological assemblages indicates tropical to subtropical palaeoclimatic conditions. In addition, the assemblage richness and abundance peaks of dinoflagellate cysts are interpreted as increased marine influence and possible flooding surfaces. The results support the alternation of marine incursions within deltaic and floodplain sequences related to short-term climate oscillations that affected the vegetation on the upland and lowland drainage areas. Key palynological markers point to an early Late Cenomanian age whereas the Cyclonephelium compactum-membraniphorum (Ccm morphological plexus) presence signals the incursion of boreal waters during the Plenus Cold Event of the Ocean Anoxic Event 2 reaching the southern coast of Appalachia.	[Lorente, Maria Antonieta] Cent Univ Venezuela, Dept Geol, Caracas, Venezuela; [Lorente, Maria Antonieta] Ellington Geol Serv LLC, Houston, TX USA; [Noto, Christopher] Univ Wisconsin Parkside, Dept Biol Sci, Kenosha, WI USA; [Flaig, Peter] Univ Texas Austin, Jackson Sch Geosci, BEG, Austin, TX USA	University of Central Venezuela; University of Wisconsin System; University of Wisconsin Parkside; University of Texas System; University of Texas Austin	Lorente, MA (通讯作者)，Cent Univ Venezuela, Dept Geol, Caracas, Venezuela.	lorente.maria.antonieta@gmail.com			State of Texas Advanced Resource Recovery Program at the Bureau of Economic Geology, University of Texas at Austin; Biological Sciences Department, University of Wisconsin-Parkside; Ellington Geological Services	State of Texas Advanced Resource Recovery Program at the Bureau of Economic Geology, University of Texas at Austin; Biological Sciences Department, University of Wisconsin-Parkside; Ellington Geological Services	The co authors was funded by the State of Texas Advanced Resource Recovery Program at the Bureau of Economic Geology, University of Texas at Austin; the Biological Sciences Department, University of Wisconsin-Parkside; and Ellington Geological Services.	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J	Jiang, Y; Ramanan, R; Yoon, S; Lee, BM; Kang, YH; Li, Z				Jiang, Yue; Ramanan, Rishiram; Yoon, Sungae; Lee, Bo-Mi; Kang, Yoon-Ho; Li, Zhun			Toxin production in bloom-forming, harmful alga<i> Alexandrium</i><i> pacificum</i> (Group IV) is regulated by cyst formation-promoting bacteria<i> Jannaschia</i><i> cystaugens</i> NBRC 100362T	WATER RESEARCH			English	Article						Cyst formation; Paralytic shellfish toxins; Saxitoxin biosynthesis; Bacteria interactions; Co-cultivation	PARALYTIC SHELLFISH TOXINS; BAYESIAN PHYLOGENETIC INFERENCE; HIROSHIMA BAY; MASAN BAY; DINOFLAGELLATE; TAMARENSE; DINOPHYCEAE; GROWTH; SAXITOXIN; TOXICITY	Harmful algal blooms (HABs) caused by dinoflagellates like Alexandrium pacificum pose significant ecological and public health risks due to their production of paralytic shellfish toxins (PSTs). Bacterial populations, particularly Alexandrium cyst formation-promoting bacteria (Alex-CFPB), are known to significantly influence growth, encystment, toxin synthesis, the composition of toxic components, and bloom dynamics of these dinoflagellates. However, the role of Alex-CFPB in Alexandrium toxin synthesis and the mechanisms thereof are still unclear. Here, we show that co-culturing A. pacificum with cyst formation-promoting bacteria Jannaschia cystaugens significantly increases total intracellular PSTs content in the late stationary phase (including more cysts and less vegetable cells compared with axenic group). Our results demonstrate that the presence of J. cystaugens alters metabolic pathways in A. pacificum by upregulating key paralytic shellfish toxins synthesis genes and inducing downregulation of sulfotransferase sxtN (related to PSTs sulfation) which decreases sulfated PSTs components (low-toxicity), leading to an increase in high-toxicity PSTs content at a single-cell level. Furthermore, bacterial oxidative stress signals, nutrient competition, and quorum sensing contribute to increased toxin synthesis. These results provide insights into the major role of bacteria in modulating growth, physiology, and toxin production in bloom-forming algae, and the complex regulatory mechanisms therein. This study thus defines the critical function of microbial associations in bloom formation and toxin production with implications for managing HABs and mitigating their impacts.	[Jiang, Yue; Li, Zhun] Korea Res Inst Biosci & Biotechnol, Biol Resource Ctr, Korean Collect Type Cultures KCTC, Jeongeup 56212, South Korea; [Jiang, Yue] Chonnam Natl Univ, Dept Integrat Food Biosci & Biotechnol, Gwangju 61186, South Korea; [Ramanan, Rishiram] Cent Univ Kerala, Dept Environm Sci, Sustainable Resources Lab, Kasaragod 671316, Kerala, India; [Yoon, Sungae; Lee, Bo-Mi; Kang, Yoon-Ho] Natl Inst Environm Res, Water Environm Res Dept, Incheon 22689, South Korea; [Li, Zhun] Univ Sci & Technol UST, KRIBB Sch Biotechnol, Dept Environm Biotechnol, Daejeon 34113, South Korea	Korea Research Institute of Bioscience & Biotechnology (KRIBB); Chonnam National University; Central University of Kerala; National Institute of Environmental Research (NIER), Republic of Korea; University of Science & Technology (UST)	Li, Z (通讯作者)，Korea Res Inst Biosci & Biotechnol, Biol Resource Ctr, Korean Collect Type Cultures KCTC, Jeongeup 56212, South Korea.; Kang, YH (通讯作者)，Natl Inst Environm Res, Water Environm Res Dept, Incheon 22689, South Korea.	korea1975@korea.kr; lizhun@kribb.re.kr	Li, Zhun/IUQ-5309-2023; Ramanan, Rishiram/AAW-7916-2020	LI, ZHUN/0000-0001-8961-9966; Jiang, Yue/0000-0001-6654-1609	Korea Research Institute of Bioscience and Biotechnology Research Initiative Program [KGM5232423]; Grant "Advancement of Central Microbial Resource Center of the Ministry of Science and ICT" from National Research Foundation of Korea (NRF) [NRF-2021M3H9A1030164, NRF-2021R1C1C1008377]; National Institute of Environmental Research (NIER) - Ministry of Environment (ME) of the Republic of Korea [NIER-2024- 01-01-034]	Korea Research Institute of Bioscience and Biotechnology Research Initiative Program; Grant "Advancement of Central Microbial Resource Center of the Ministry of Science and ICT" from National Research Foundation of Korea (NRF); National Institute of Environmental Research (NIER) - Ministry of Environment (ME) of the Republic of Korea(Ministry of Environment (ME), Republic of KoreaNational Institute of Environmental Research (NIER), Republic of Korea)	This work was supported by the Korea Research Institute of Bioscience and Biotechnology Research Initiative Program (KGM5232423) , the grant "Advancement of Central Microbial Resource Center of the Ministry of Science and ICT" from National Research Foundation of Korea (NRF) (No. NRF-2021M3H9A1030164 and NRF-2021R1C1C1008377) and a grant from the National Institute of Environmental Research (NIER) funded by the Ministry of Environment (ME) of the Republic of Korea (NIER-2024- 01-01-034) .	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MAR 15	2025	272								122930	10.1016/j.watres.2024.122930	http://dx.doi.org/10.1016/j.watres.2024.122930		DEC 2024	16	Engineering, Environmental; Environmental Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Water Resources	Q9T9D	39674136	hybrid			2025-03-11	WOS:001388019500001
J	Niechwedowicz, M; Voigt, S; Desmares, D; Jurkowska, A; Martinez, M				Niechwedowicz, Mariusz; Voigt, Silke; Desmares, Delphine; Jurkowska, Agata; Martinez, Mathieu			Organic-walled dinoflagellate cyst record across the Campanian-Maastrichtian (Upper Cretaceous) boundary stratotype section (Tercis-les-Bains, SW France)	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cysts; Biostratigraphy; Paleoenvironment; Campanian-Maastrichtian boundary; Stratotype section; Tercis; France	VISTULA RIVER SECTION; CARBON-ISOTOPE STRATIGRAPHY; OUTER WESTERN CARPATHIANS; SILESIAN UNIT; BIOSTRATIGRAPHY; ZONATION; BASIN; SUCCESSION; SEDIMENTS; DEPOSITS	The Global Boundary Stratotype Section and Point (GSSP) for the base of the Maastrichtian Stage (Tercis-lesBains, SW France) was formally approved in 2001, but over the years the boundary definition gave rise to serious doubts about the utility of some of the macro- and microfossil events chosen to approximate the position of the boundary. To address the issue, the Subcommission on Cretaceous Stratigraphy appointed a new Maastrichtian Working Group, whose members recently revisited Tercis section. Re-sampling of the GSSP locality revealed relatively rich and diverse dinoflagellate cyst assemblages. The stratigraphic succession of the highest (HOs) and lowest (LOs) occurrences of particular cyst taxa is compared with the dinoflagellate cyst record previously reported from the site and elsewhere. We noticed that among the dinoflagellate cyst events included in the definition of the Campanian-Maastrichtian boundary, only the HOs of Raetiaedinium evittigratia, and of R. truncigerum can be used as good boundary markers. Other formal cyst bioevents either had a restricted biogeographical distribution (Corradinisphaeridium horridum), or disappear distinctly above the Maastrichtian GSSP level (Samlandia carnarvonensis, S. mayi). The HOs of Coronifera oceanica, Gillinia hymenophora, Odontochitina costata, Xenascus ceratioides, and the LOs of Cladopyxidium paucireticulatum, C. saeptum, C. verrucosum, Glaphyrocysta expansa, and of G. pala, can probably also be used to approximate the Campanian-Maastrichtian transition. The actual utility of the above-mentioned bioevents seems promising, but requires further studies. First preliminary paleoenvironmental data were acquired based on the composition of the entire dinoflagellate cyst assemblage from Tercis.	[Niechwedowicz, Mariusz] UNIV WARSAW, Fac Geol, Ul Zwirki & Wigury 93, PL-02089 Warsaw, Poland; [Voigt, Silke] Goethe Univ Frankfurt, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany; [Desmares, Delphine] Sorbonne Univ, CR2P Ctr Rech Paleontol Paris, MNHN, UMR 7207,CNRS, 4 Pl Jussieu, F-75005 Paris, France; [Jurkowska, Agata] AGH Univ Krakow, Fac Geol Geophys & Environm Protect, Mickiewicza 30, PL-30059 Krakow, Poland; [Martinez, Mathieu] Univ Rennes, Geosci Rennes, UMR 6118, CNRS, F-35000 Rennes, France	University of Warsaw; Goethe University Frankfurt; Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); AGH University of Krakow; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Rennes	Niechwedowicz, M (通讯作者)，UNIV WARSAW, Fac Geol, Ul Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	niechwedowicz.m@uw.edu.pl	Jurkowska, Agata/A-9734-2016; Voigt, Silke/G-7270-2017; Niechwedowicz, Mariusz/LJL-9003-2024; Martinez, Mathieu/N-9746-2015		University of Warsaw internal grant program IDUB [PSP 501-D113-20-0004316]	University of Warsaw internal grant program IDUB	We are deeply grateful to Alain Rousset, the president of the Conseil Regional Nouvelle-Aquitaine, for permission to access the Tercis quarry and collect samples. Yves Gilly, Cyrille Greaume, Jeannette Le Breton, and Marie Lo Cascio (Reserve Naturelle Regionale Geologique des carrieres de Tercis-les-Bains) kindly prepared the outcrop by cleaning it of soil, and provided logistic support during the fieldwork. Our warm thanks are also offered to Micha l Durlej for his invaluable help during the sampling. Sample shipment was assisted by the SCS. We thank the reviewers (Peter Bijl and an anonymous referee) for their constructive comments that improved the manuscript. This study was supported by University of Warsaw internal grant program IDUB (grant no. PSP 501-D113-20-0004316) to MN.	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Pet. Geol.	MAR	2025	173								107249	10.1016/j.marpetgeo.2024.107249	http://dx.doi.org/10.1016/j.marpetgeo.2024.107249		DEC 2024	14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	Q6T9X					2025-03-11	WOS:001385990000001
J	Noga, PMB; de Vernal, A; da Silva, DML; Gomes, DF				Noga, Pietro Martins Barbosa; de Vernal, Anne; da Silva, Daniela Mariano Lopes; Gomes, Doriedson Ferreira			Non-pollen palynomorphs as indicators of local environmental conditions in a Neotropical Estuary (Northeast Brazil)	MARINE MICROPALEONTOLOGY			English	Article						Surface sediment; Benthic assemblages; Micropaleontology; Biogeochemistry	WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; MARINE-SEDIMENTS; MICROFORAMINIFERAL LININGS; WATER; FAUNA; PALEOECOLOGY; PRESERVATION; ASSEMBLAGES; PALYNOLOGY	Non-pollen palynomorphs (NPPs) are organic-walled microfossils derived from diverse aquatic and terrestrial organisms, frequently observed in palynological studies. This study documents the distribution of NPPs in surface sediment samples from the two main rivers of Camamu Bay (Northeast Brazil), analyzed to explore their response to estuarine environmental and nutritional gradients. Using standard palynological techniques, 69 NPP taxa were identified, spanning 40 divisions, including dinoflagellates, foraminiferal linings, chlorophytes, cyanobacteria, ciliates, amoebozoans, scolecodonts, zoological fragments, and fungal spores. Assemblages were dominated by fungal spores across most stations. Distinct environmental gradients were reflected in NPP distribution, for instance upstream stations with low salinity (3 psu) and high nutrient ratios favored chlorophytes, while downstream stations with higher salinity (up to 35 psu) and lower N:P ratios (<40 mu M) were dominated by foraminiferal linings. Multivariate statistic analyses revealed that salinity and nutrient stoichiometry were significant drivers of assemblage composition. These findings highlight the utility of NPPs as indicators of environmental and biogeochemical conditions, particularly in low-latitude estuarine systems, and underscore their potential applications in paleoecological reconstruction.	[Noga, Pietro Martins Barbosa; Gomes, Doriedson Ferreira] Univ Fed Bahia, Lab Ecol & Paleoecol Aquat Environm ECOPALEO, Lab Geoquim Marinha, Rua Barao Jeremoabo S-N, BR-40170115 Salvador, BA, Brazil; [de Vernal, Anne] Univ Quebec Montreal, Geotop Res Ctr Dynam Syst Earth, Succursale Ctr Ville, CP 8888, Montreal, PQ H3C 3P8, Canada; [da Silva, Daniela Mariano Lopes] Univ Estadual Santa Cruz, Dept Ciencias Biol, Rod Jorge Amado Km 16, BR-45562900 Ilheus, BA, Brazil	Universidade Federal da Bahia; University of Quebec; University of Quebec Montreal; Universidade Estadual de Santa Cruz	Noga, PMB (通讯作者)，Univ Fed Bahia, Lab Ecol & Paleoecol Aquat Environm ECOPALEO, Lab Geoquim Marinha, Rua Barao Jeremoabo S-N, BR-40170115 Salvador, BA, Brazil.	p.noga@pasb.com.br	Martins Barbosa Noga, Pietro/K-2776-2016; Gomes, Doriedson/F-8228-2013		Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [88887.814723/2023-00]; Fundacao de Apoio a Pesquisa do Estado da Bahia-FAPESB [RED0026/2014]; University of Quebec in Montreal through the Centre de recherche sur la dynamique du systeme Terre (Geotop)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Apoio a Pesquisa do Estado da Bahia-FAPESB(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); University of Quebec in Montreal through the Centre de recherche sur la dynamique du systeme Terre (Geotop)	The authors wish to thank the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) for the scholarship to PMBN (process number 88887.814723/2023-00) and Fundacao de Apoio a Pesquisa do Estado da Bahia-FAPESB for the sampling under project RED0026/2014. Also the scholarship to PMBN provided by the University of Quebec in Montreal through the Centre de recherche sur la dynamique du systeme Terre (Geotop) is gratefully acknowledged. A special thank to the sampling crew, Amana Almeida and Loreane Dias and Angelica Cardozo for her contribution with the algae identification. The authors also thank the valuable and accurate contributions of the anonymous peer reviewers of this article.	Allen SE., 1974, CHEM ANAL ECOLOGICAL; Amorim F.N., 2005, Caracterizacao oceanografica da Baia de Camamu e adjacencias e mapeamento das areas de risco a derrames de oleo; [Anonymous], 2017, J. 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J	Badylak, S; Phlips, EJ; Milbrandt, EC; Morrison, ES; Stelling, BD; Lee, SA; Frankovich, TA; Kaplan, D				Badylak, Susan; Phlips, Edward J.; Milbrandt, Eric C.; Morrison, Elise S.; Stelling, Benjamin D.; Lee, Shin-Ah; Frankovich, Thomas A.; Kaplan, David			Influence of regulated water discharges on phytoplankton composition and biomass in a subtropical canal	JOURNAL OF ENVIRONMENTAL MANAGEMENT			English	Article							HARMFUL ALGAL BLOOMS; DURINSKIA-BALTICA DINOPHYCEAE; LAKE LAKE OKEECHOBEE; CALOOSAHATCHEE ESTUARY; DINOFLAGELLATE CYSTS; VERTICAL MIGRATION; CELL-VOLUME; FLORIDA; GROWTH; MANAGEMENT	Phytoplankton composition and biomass were investigated in the C-43 Canal in southwest Florida during a period of shifting discharges from water control structures. The canal receives regulated discharges from eutrophic Lake Okeechobee via the S77 structure. During periods of high S77 discharge in spring and early summer, cyanobacteria biomass dominated the phytoplankton community, including blooms of the harmful algal bloom (HAB) species Raphidiopsis raciborskii, Limnothrix redekei and Microcystis aeruginosa. During periods of low discharges from the lake, in mid-summer and autumn, water inputs to the canal came primarily from tributaries in the watershed surrounding the C-43. Phytoplankton biomass decreased, but the relative importance of dinoflagellates increased, including a bloom in July. The dinoflagellate community included Ceratium, Durinskia baltica, Glochidinium penardiforme, Gymnodinium fuscum, Parvodinium goslaviense, Parvodinium umbonatum/inconspicuum complex, Peridiniopsis quadridens, Woloszynskia reticulata, and an unidentified thecate and athecate species. D. baltica and P. goslaviense were recorded for the first time in Florida. Data was also obtained on water temperature, conductivity, fluorescent dissolved organic matter, chlorophyll a , total nitrogen, dissolved inorganic nitrogen, total phosphorus, PO4, discharge rates from water control structures, and water residence times. Results show that temporal shifts in the sources and rates of water inputs to the C-43 influence the character of environmental conditions that define phytoplankton composition and biomass in the canal. This suggests that management of discharges can play a role in mitigating HABs in the canal and downstream coastal environments receiving water from the canal.	[Badylak, Susan; Phlips, Edward J.; Stelling, Benjamin D.] Univ Florida, Sch Forestry Fisheries & Geomatics Sci, 7922 NW 71st St, Gainesville, FL 32653 USA; [Milbrandt, Eric C.] Sanibel Capt Conservat Fdn, 900A Tarpon Bay Rd, Sanibel, FL 33957 USA; [Morrison, Elise S.; Lee, Shin-Ah; Kaplan, David] Univ Florida, Engn Sch Sustainable Infrastructure & Environm, 365 Weil Hall, Gainesville, FL 32611 USA; [Frankovich, Thomas A.] Florida Int Univ, Southeast Environm Res Ctr, 98630 Overseas Highway, Key Largo, FL 33037 USA	State University System of Florida; University of Florida; State University System of Florida; University of Florida; State University System of Florida; Florida International University	Phlips, EJ (通讯作者)，Univ Florida, Sch Forestry Fisheries & Geomatics Sci, 7922 NW 71st St, Gainesville, FL 32653 USA.	phlips@ufl.edu	Kaplan, David/G-5951-2010; Lee, Shin-Ah/AAE-2322-2020		U.S. Army Corps of Engineers ERDC [W912HZ-21-2-0057]; USDA, National Institute of Food and Agriculture, Hatch Project [1017098]	U.S. Army Corps of Engineers ERDC(United States Department of DefenseUnited States Army); USDA, National Institute of Food and Agriculture, Hatch Project	We thank Susan Carty for reviewing our manuscript and providing valuable insights into the dinoflagellates observed in this study. We also thank Karen Kelley of the ICBR Electron Microscopy and Bioimaging Lab (University of Florida) for the scanning microscopy images. The research presented in this paper was in part funded by a grant from U.S. Army Corps of Engineers ERDC, W912HZ-21-2-0057. Edward Phlips, Susan Badylak and Ben Stelling are supported by the USDA, National Institute of Food and Agriculture, Hatch Project 1017098.	Aguilera A, 2018, PHYCOLOGIA, V57, P130, DOI 10.2216/17-2.1; AGUSTI S, 1992, LIMNOL OCEANOGR, V37, P434, DOI 10.4319/lo.1992.37.2.0434; AHLGREN G, 1983, ARCH HYDROBIOL, V98, P489; Anderson DM, 2021, HARMFUL ALGAE, V102, DOI 10.1016/j.hal.2021.101975; [Anonymous], 1958, Mitt. Int. Ver. Theor. Angew. 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J	Garvang, ES; Eliassen, LK; Titelman, J; Andersen, T				Garvang, Even Sletteng; Eliassen, Lasse Kroger; Titelman, Josefin; Andersen, Tom			Outbreak conditions and impacts of parasites in copepod populations	ECOSPHERE			English	Article						<italic>Blastodinium</italic>; copepods; disease modeling; parasitism; pelagic ecology; zooplankton	VERTICAL-DISTRIBUTION; CALANUS-FINMARCHICUS; BLASTODINIUM SPP.; HOST; DYNAMICS; DINOFLAGELLATE; ECOSYSTEMS; MORTALITY; GROWTH; SEA	Although parasitism is vital for ecosystem dynamics and food webs, the population effects of parasitism in the marine pelagic have received little attention. Pelagic copepods link primary producers and higher consumers in marine food webs and host numerous parasites that may affect reproduction, behavior, and survival. We present a simple model consisting of uninfected hosts, infected hosts, and the free-living parasite stage and use it to investigate population dynamics and outbreak conditions of this host-parasite system. The host population growth is limited by a carrying capacity determined by resource availability and stoichiometric constraints. We parameterized the model for 10 copepod species with different traits but with the same Blastodinium-like parasite. We derived a threshold ratio R0$$ {R}_0 $$ for establishing infection, which showed that the parasite could invade and persist in all hosts. The ability of parasites to invade host populations largely depended on traits of free-living spores and host density. From numerical analysis, we found that the parasite typically induced oscillations in the host population. Host traits were important for infection dynamics: High host growth rates mitigated some of the consequences of infection, and larger copepods were more susceptible to infection than smaller ones. The model implies that parasitism can impact the functional role of the copepod population in the ecosystem, and the system as a whole.	[Garvang, Even Sletteng; Eliassen, Lasse Kroger; Titelman, Josefin; Andersen, Tom] Univ Oslo, Dept Biosci, Oslo, Norway	University of Oslo	Garvang, ES (通讯作者)，Univ Oslo, Dept Biosci, Oslo, Norway.	evengar@uio.no	; Titelman, Josefin/B-4450-2009	Garvang, Even Sletteng/0009-0005-6188-8861; Titelman, Josefin/0000-0002-1550-9497	The Research Council of Norway [315892]; Research Council of Norway; University of Oslo	The Research Council of Norway(Research Council of Norway); Research Council of Norway(Research Council of Norway); University of Oslo	This is a contribution to the POICE project financed by The Research Council of Norway (RCN number 315892 to Josefin Titelman and Tom Andersen). Even Sletteng Garvang was funded by a PhD fellowship from POICE and Lasse Kr & oslash;ger Eliassen by a PhD fellowship from the University of Oslo.	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J	Vasilyeva, ON				Vasilyeva, O. N.			Evolutionary Lineages of Peridinioid Dinoflagellate Cysts (Class Dinophyceae Pascher, 1914) in the Middle Eocene of the Lower Volga Region	PALEONTOLOGICAL JOURNAL			English	Article						Middle Eocene; dinoflagellate cysts; peridinioids; taxonomy; evolutionary lines; Lower Volga region; Russia	BIOSTRATIGRAPHY; PALEOGENE	The sequential evolutionary appearance of closely related species of peridinioid dinoflagellate cysts has been established in the Middle Eocene deposits of the Lower Volga region (Ravninnaya R-43 borehole, Volgograd region, Russia). Two new species of dinoflagellate cysts, Wilsonidium imperfectum sp. nov. and Wilsonidium michouxi sp. nov., are described from the Keresta Formation in the Volga region. Evolutionary morphological changes of species from the genera Phthanoperidinium Drugg et Loeblich Jr., 1967 and Wilsonidium Lentin et Williams, 1976 are considered. Analysis of the stratigraphic and geographical distribution of taxa indicates that the species studied have a high correlation potential on the Russian Platform.	[Vasilyeva, O. N.] Russian Acad Sci, Zavaritsky Inst Geol & Geochem, Ural Branch, Ekaterinburg 620110, Russia	Russian Academy of Sciences	Vasilyeva, ON (通讯作者)，Russian Acad Sci, Zavaritsky Inst Geol & Geochem, Ural Branch, Ekaterinburg 620110, Russia.	vasilyeva@igg.uran.ru			Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences [123011800010-5, FUMZ-2023-0009]	Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences(Russian Academy of SciencesChinese Academy of Sciences)	This work was performed as part of State Assignment 123011800010-5 (topic FUMZ-2023-0009) to the Zavaritsky Institute of Geology and Geochemistry, Ural Branch, Russian Academy of Sciences. No additional grants were received to conduct or direct this specific study.	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J	Vishnevskaya, VS				Vishnevskaya, V. S.			Gilianelles (Microproblematics) from Late Cretaceous Deposits of Mount Polyus (Crimean Peninsula)	PALEONTOLOGICAL JOURNAL			English	Article						Gilianelles; calcareous microproblematics; Campanian Stage; Crimea; Russia	CALCAREOUS DINOFLAGELLATE CYST	Gilianelles, calcareous microproblematics, representatives of the Late Campanian group of microfossils, were found for the first time in the Upper Cretaceous deposits of the interfluve of the Kacha and Belbek rivers in the Crimean Mountains. They come from deposits of the Polyus section, previously dated as Turonian-Santonian. It is proposed that the 50-m thick "calcisphere" limestones along the dirt road on the western slope of Mount Polyus to its summit (outcrop 3177) can be dated as Campanian.	[Vishnevskaya, V. S.] Russian Acad Sci, Geol Inst, Moscow 119017, Russia	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences	Vishnevskaya, VS (通讯作者)，Russian Acad Sci, Geol Inst, Moscow 119017, Russia.	valentina.vishnaa@mail.ru						Alekseev A.S, 1989, GEOLOGICHESKOE STROE, P123; Arkadiev V.V., 1997, Atlas of the Cretaceous Fauna of South-Western Crimea; Baraboshkin EY, 2024, STRATIGR GEO CORREL+, V32, P89, DOI 10.1134/S0869593824020023; Bison KM, 2004, J MICROPALAEONTOL, V23, P127, DOI 10.1144/jm.23.2.127; Bragina L.G., 2007, Radiolarians in the Upper Cretaceous (TuronianConiacian) deposits of the Belbek River basin (Southwestern Crimea), Paleontolohichni doslidzhennya v Ukrayini: istoriya, suchasnyy stan ta perspektyvy: Zb.Nauk. Prats IGN NAN of Ukrainy (Paleontological Research in Ukraine: History; Burnett J.A., 1998, Calcareous Nannofossil Biostratigraphy; Golubev V.K., 2023, PALEOSTRAT 2023, P16; Guzhikov A.Yu., 2024, Anomalous features of the geomagnetic field regime at the end of the Cretaceous superchron of normal polarity according to the results of studies of the TuronianSantonian of the southwestern Crimea, DOI [10.1134/S1069351324700150, DOI 10.1134/S1069351324700150]; Klikushin V.G., 1985, Byulleten' Moskovskogo Obshchestva Ispytatelei Prirody Otdel Geologicheskii, V60, P69; Kopaevich L, 2016, PALAEOGEOGR PALAEOCL, V441, P493, DOI 10.1016/j.palaeo.2015.09.024; Krasheninnikov V.A., 1983, Leg 71; Odin G.S., 2001, Developments in Palaeontology and Stratigraphy, V19; Odin G.S., 2006, Notebooks on Geology, V05, P1; Odin G.S., 2008, Mem, V01, P1; Odin GS, 2008, CR PALEVOL, V7, P195, DOI 10.1016/j.crpv.2008.03.004; Odin GS, 2007, CR PALEVOL, V6, P181, DOI 10.1016/j.crpv.2006.10.001; Odin GS, 2011, PALAEONTOLOGY, V54, P133, DOI 10.1111/j.1475-4983.2010.01012.x; Odin Gilles Serge, 2009, Revue de Paleobiologie, V28, P175; Versteegh GJM, 2009, PALAEONTOLOGY, V52, P343, DOI 10.1111/j.1475-4983.2009.00854.x; Vishnevskaya V.S., 2023, T 14 VSER MIKR SOV F, P393; Vishnevskaya V.S., 2023, The first discovery of gilianellids (calcareous microproblematics) in the Late Cretaceous deposits of Crimea; Vishnevskaya V.S., 2023, EKZOLIT 2023 NOVATOR, P46; Wendler J, 2004, REV PALAEOBOT PALYNO, V129, P133, DOI 10.1016/j.revpalbo.2003.12.011; Willems H., 1990, Lethaea, V70, P239	24	0	0	0	0	PLEIADES PUBLISHING INC	NEW YORK	PLEIADES HOUSE, 7 W 54 ST, NEW YORK,  NY, UNITED STATES	0031-0301	1555-6174		PALEONTOL J+	Paleontol. J.	DEC	2024	58	8					968	975		10.1134/S0031030124600604	http://dx.doi.org/10.1134/S0031030124600604			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	O4R6R					2025-03-11	WOS:001371022700002
J	Matul, AG; Novichkova, EA; Klyuvitkina, TS; Chekhovskaya, MP; Lozinskaia, LA; Iakimova, KS; Kazarina, GK; Melnikova, AA				Matul, A. G.; Novichkova, E. A.; Klyuvitkina, T. S.; Chekhovskaya, M. P.; Lozinskaia, L. A.; Iakimova, K. S.; Kazarina, G. Kh.; Melnikova, A. A.			Paleoceanology of the Norwegian-Greenland Basin in the Middle-Late Holocene Based on the Microfossil Distribution	PALEONTOLOGICAL JOURNAL			English	Article						Holocene; Norwegian-Greenland Basin; micropaleontology; paleotemperature reconstruction	NORTH-ATLANTIC HOLOCENE; EVOLUTION; TEMPERATURE; CLIMATE; WATER	Micropaleontological analysis of the assemblages of planktic and benthic foraminifers, dinoflagellate cysts, and diatoms in a sediment core AMK-6142 MK from the southwestern part of the Lofoten Basin of the Norwegian Sea provides new data on regional paleoceanology in the Middle-Late Holocene. Reconstructions of the summer sea surface (based on dinocysts) and subsurface (based on planktic foraminifers) temperatures show possible short, time-transgressive (in different areas) intervals of rapid movement of the Arctic Front to the east/southeast in the Norwegian-Greenland Basin during Neoglaciation in the last 5000-6000 years.	[Matul, A. G.; Novichkova, E. A.; Chekhovskaya, M. P.; Lozinskaia, L. A.; Iakimova, K. S.; Kazarina, G. Kh.; Melnikova, A. A.] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia; [Klyuvitkina, T. S.] Moscow State Univ, Moscow 119991, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; Lomonosov Moscow State University	Matul, AG (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia.	amatul@mail.ru	K, Tatiana/GZL-4850-2022		Ministry of Education and Science, Shirshov Institute of Oceanology, Russian Academy of Sciences [FMWE-2024-0020]; Ministry of Education and Science, Moscow State University [121051100135-0]; Russian Science Foundation for the Shirshov Institute of Oceanology, Russian Academy of Sciences [21-17-00235]	Ministry of Education and Science, Shirshov Institute of Oceanology, Russian Academy of Sciences; Ministry of Education and Science, Moscow State University; Russian Science Foundation for the Shirshov Institute of Oceanology, Russian Academy of Sciences	This study was performed according to State Assignment no. FMWE-2024-0020 of the Ministry of Education and Science, Shirshov Institute of Oceanology, Russian Academy of Sciences, and State Assignment no. 121051100135-0 of the Ministry of Education and Science, Moscow State University, and supported by grant no. 21-17-00235 (https://rscf.ru/project/21-17-00235)from the Russian Science Foundation for the Shirshov Institute of Oceanology, Russian Academy of Sciences. No additional grants were received to conduct or direct this specific study.	Aagaard-Sorensen S, 2014, MAR GEOL, V355, P15, DOI 10.1016/j.margeo.2014.05.009; Andersen C, 2004, QUATERNARY SCI REV, V23, P2155, DOI 10.1016/j.quascirev.2004.08.004; Andersson Carin, 2013, PANGAEA, DOI 10.1594/PANGAEA.820583; Berben SMP, 2014, CLIM PAST, V10, P181, DOI 10.5194/cp-10-181-2014; Blindheim J, 2005, GEOPH MONOG SERIES, V158, P11; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; Boyer T.P., 2018, World Ocean Atlas 2018. 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J	Rogov, MA; Zakharov, VA; Pestchevitskaya, EB; Vishenvskaya, VS; Zverkov, NG; Baraboshkin, EY				Rogov, M. A.; Zakharov, V. A.; Pestchevitskaya, E. B.; Vishenvskaya, V. S.; Zverkov, N. G.; Baraboshkin, E. Yu.			Upper Jurassic Volgian Stage and Lower Cretaceous Ryazanian Stage of the Panboreal Biogeographic Superrealm	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						biostratigraphy; Upper Jurassic; Lower Cretaceous; stage; mollusks; dinocysts; radiolarians; marine reptiles	HIGH-RESOLUTION STRATIGRAPHY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; BOREAL-TETHYAN CORRELATION; MAROUA LE SAIX; AGARDHFJELLET FORMATION; NORDVIK PENINSULA; CENTRAL SPITSBERGEN; RUSSIAN PLATFORM; BOUNDARY STRATA; EAST SIBERIA	The history of study of the Upper Jurassic Volgian Stage and Lower Cretaceous Ryazanian Stage, their geographic occurrence, and use in world practice, subdivision, and correlation are considered. The data on the occurrence of various groups of macro- and microfossils (ammonites, bivalves, radiolarians, dinocysts, and marine vertebrates) in the Volgian and Ryazanian are reviewed. In spite of significantly different lifestyle of all these groups, the Volgian and Ryazanian assemblages are highly similar in the entire Panboreal Superrealm, on one hand, and significantly different from coeval Tethyan fauna, on the other hand. The biostratigraphic scales of these stages based on successions of ammonites, bivalves, radiolarians, and dinocysts are analyzed. It is shown that the substage boundaries of the Volgian are reliably traced along the entire Panboreal Superrealm. None of the boundaries, except for the base of the Volgian, corresponds even to a zonal boundary of the Tethys-Pantalassa Superrealm. A similar situation is also observed in the Ryazanian: its lower boundary, as well as the Lower-Upper Ryazanian boundary, does not coincide with any well-traced boundary in the Tethys-Pantalassa Superrealm. The necessity of using the Volgian and Ryazanian in geological studies is substantiated for all Russian regions with abundant Boreal deposits, as well as inclusion of these stages to the General Stratigraphic Scale in parallel with the Tithonian and Berriasian. We suggest the cancellation of the Decree of the Interdepartmental Stratigraphic Committee of Russia about the transition of the Volgian into regional stratigraphic subdivisions, as well as the reconsideration of the correlation scheme of the Volgian and Ryazanian accepted in the same decree.	[Rogov, M. A.; Zakharov, V. A.; Vishenvskaya, V. S.; Zverkov, N. G.; Baraboshkin, E. Yu.] Russian Acad Sci, Geol Inst, Moscow 119017, Russia; [Pestchevitskaya, E. B.] Russian Acad Sci, Siberian Branch, Trofimuk Inst Petr Geol & Geophys, Novosibirsk 630090, Russia; [Baraboshkin, E. Yu.] Moscow MV Lomonosov State Univ, Moscow 119991, Russia	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Lomonosov Moscow State University	Rogov, MA (通讯作者)，Russian Acad Sci, Geol Inst, Moscow 119017, Russia.	rogov@ginras.ru			Geological Institute, Russian Academy of Sciences (Moscow, Russia) [FMMG-2021-003]; Russian Science Foundation [22-17-00054, FWZZ-2022-0004]	Geological Institute, Russian Academy of Sciences (Moscow, Russia); Russian Science Foundation(Russian Science Foundation (RSF))	he summarizing the materials on ammonites, bivalves, and radiolarians was supported by state contract no. FMMG-2021-003 of the Geological Institute, Russian Academy of Sciences (Moscow, Russia). 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J	Bruno, AC; Helenes, J				Bruno, Alessandro-Cesare; Helenes, Javier			Eocene to Early Miocene dinoflagellate cysts from the southern Gulf of Mexico	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cyst assemblages; DSDP Site 94; Palaeoecology; Biostratigraphy; New species	SURFACE SEDIMENTS; HISTORICAL BIOGEOGRAPHY; UPWELLING SYSTEM; PALEOCENE; OLIGOCENE; TRANSITION; BASIN; BIOSTRATIGRAPHY	This paper documents the Eocene to Miocene dinoflagellate cyst assemblages found at Site 94 in the southern part of the Gulf of Mexico. Four unique dinoflagellate cyst assemblages representing depositional periods from the Early Eocene to the Early Miocene are defined in this study. The Early to Middle Eocene assemblage presents the highest average concentrations of dinoflagellate cysts, is dominated by Operculodinium, and contains few heterotrophic taxa. The Early Oligocene assemblage has medium concentration and is dominated by Deflandrea. The Late Oligocene also has high average concentrations of dinoflagellate cysts, is dominated by Homotryblium, and contains few heterotrophic taxa. The Early Miocene assemblage has lower average concentrations of dinoflagellate cysts, is dominated by Pyxidinopsis, and lacks heterotrophic taxa. Our palynological data is related to significant regional paleogeographic and paleoceanographic changes. Namely, the Early to Middle Eocene free flow of tropical water masses from the south and the Late Eocene restriction of this flow by a land bridge connecting northern South America to Cuba in the north. The Oligocene gradual return of the tropical water masses and finally, the Early Miocene emergence of the Florida Platform when the Gulf of Mexico reached modern oceanographic conditions. The stratigraphic ranges of selected dinoflagellate cysts fit in age with previous microfossil data from the site and allowed us to define the Early Oligocene - Late Oligocene transition. The presence of well-preserved dinoflagellate cysts allowed the identification of 60 species and the discovery of three new species: Achomosphaera psilata sp. nov., Carpatella reticulata sp. nov., and Hystrichosphaeropsis gulficum sp. nov.	[Bruno, Alessandro-Cesare; Helenes, Javier] CICESE Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico		Bruno, AC (通讯作者)，CICESE Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico.	bruno@cicese.edu.mx; jhelenes@cicese.mx			CONACYT-CICESE Mexico scholarship	CONACYT-CICESE Mexico scholarship	The authors thank the International Ocean Discovery Program for providing site 94 samples. Thanks to the CONACYT-CICESE Mexico scholarship for funding the first author ' s study. Thanks to Lic. Luis-Carlos Gradilla-Martinez for technical support in SEM analysis and Ocean. Edna Collins-Ramirez for assistance in palynological prepara-tion. Special thanks to Dr. James B. Riding and Dr. Manuel Vieira for their valuable feedback, and to Dr. Shijun Jiang for his insightful com-ments. We also extend our gratitude to Dr. Xavier Crosta and the two anonymous reviewers for their careful review of the manuscript.	Antolinez-Delgado H, 2007, PALYNOLOGY, V31, P53, DOI 10.2113/gspalynol.31.1.53; Askin RA., 2003, Encyclopedia of Physical Science and Technology, P563, DOI [10.1016/B0-12-227410-5/00930-3, DOI 10.1016/B0-12-227410-5/00930-3]; Awad WK, 2018, J AFR EARTH SCI, V140, P267, DOI 10.1016/j.jafrearsci.2018.01.014; Barron A, 2017, GEOL SOC AM BULL, V129, P218, DOI 10.1130/B31559.1; BENNINGHOFF W. 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DEC	2024	193								102422	10.1016/j.marmicro.2024.102422	http://dx.doi.org/10.1016/j.marmicro.2024.102422		NOV 2024	17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	O5G4E					2025-03-11	WOS:001371406200001
J	Dodsworth, P; Black, RD				Dodsworth, Paul; Black, Roderick D.			Two areoligeracean dinoflagellate cysts from the Carstone Formation (Lower Cretaceous) at Middlegate Quarry, North Lincolnshire, UK	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							BOUNDARY STRATOTYPE SECTION; WALLED MARINE MICROPLANKTON; WESTERN INTERIOR; PRE-GUITTARD; POINT GSSP; SEA REGION; BASE; STAGE; BIOSTRATIGRAPHY; STRATIGRAPHY	Five Lower Albian (Lower Cretaceous) areoligeracean dinoflagellate cyst species are present in the Carstone Formation at Middlegate Quarry, North Lincolnshire, UK: Canninginopsis monile, Circulodinium deflandrei, Cyclonephelium compactum, Cyclonephelium intonsum and Cyclonephelium longispinatum. The taxonomy of Circulodinium deflandrei is reviewed with respect to 20 measured Carstone specimens. The taxonomy of Cyclonephelium longispinatum is reviewed with respect to 70 measured Carstone specimens and a study of 40 measured specimens from its type material in Site 361, Deep Sea Drilling Project Leg 40, offshore southwestern Africa. Circulodinium deflandrei and Cyclonephelium longispinatum have recently been considered by other workers to be junior synonyms, respectively, of Circulodinium hirtellum and Tenua anaphrissa. However, following detailed study of their morphologies, the synonymies are formally rejected here. An emended diagnosis is given for C. longispinatum. A re-assessment of the stratigraphical ranges of taxa co-occurring with the type material of C. longispinatum is consistent with a Late Albian to Early Turonian age range in Site 361.	[Dodsworth, Paul] StrataSolve Ltd, 15 Francis Rd, Stockton Heath WA4 6EB, England; [Black, Roderick D.] 22 Holtermann St, Crows Nest 2065, Australia		Dodsworth, P (通讯作者)，StrataSolve Ltd, 15 Francis Rd, Stockton Heath WA4 6EB, England.	dodsworth@stratasolve.com; rod.black1@outlook.com			University of Sheffield, UK; Keyworth, UK	University of Sheffield, UK; Keyworth, UK	We thank Stan Duxbury (Chester, UK), Robert A. Fensome (Geological Survey of Canada (Atlantic), Nova Scotia, Canada) and Martin A. Pearce (Evolution Applied Ltd, Sherborne, UK) for advice and feedback on dinoflagellate cyst taxonomy. Paul N. Hildreth kindly provided the digital photographs of Middlegate Quarry. Charles H. Wellman assisted with the loan of Carstone Formation microscope slides from the University of Sheffield, UK. Simon Harris, Louise Neep and Paul Shepherd assisted with the loan of type material microscope slides from the British Geological Survey, Keyworth, UK. James B. Riding (referee) and Paul B. Wignall (editor) suggested improvements to the manuscript.	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F., 1968, Proceedings of the Yorkshire Geological Society, V36, P513; Pearce MA, 2003, MAR MICROPALEONTOL, V47, P271, DOI 10.1016/S0377-8398(02)00132-9; Pearce MA, 2020, REV PALAEOBOT PALYNO, V278, DOI 10.1016/j.revpalbo.2020.104188; Prauss M.L., 2000, The Oceanographic and Climatic Interpretation of Marine Palynomorph Phytoplankton Distribution from Mesozoic, Cenozoic and Recent Sections, V76; Prssl KF., 1990, PALAEONTOGR ABT B, V218, P93; Riding J.B., 1992, P7; Smart J.G.O., 1976, Proceedings of the Yorkshire Geological Society, V40, P586, DOI [10.1144/pygs.40.4.581, DOI 10.1144/PYGS.40.4.581]; van Helmond NAGM, 2016, BIOGEOSCIENCES, V13, P2859, DOI 10.5194/bg-13-2859-2016; Versey H.C., 1926, Proceedings of the Yorkshire Geological Society, V20, P349, DOI [10.1144/pygs.20.3.349, DOI 10.1144/PYGS.20.3.349]; Whitham F., 1992, Humberside Geologist, V10, P4; Williams G.L., 1985, P847	50	0	0	0	0	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0044-0604	2041-4811		P YORKS GEOL SOC	Proc. Yorks. Geol. Soc.	NOV 29	2024	65	1-2							pygs2024004	10.1144/pygs2024-004	http://dx.doi.org/10.1144/pygs2024-004			11	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	F5H2F					2025-03-11	WOS:001310119700001
J	Huang, SN; Mertens, KN; Derrien, A; David, O; Shin, HH; Li, Z; Cao, XY; Cabrini, M; Klisarova, D; Gu, HF				Huang, Shuning; Mertens, Kenneth Neil; Derrien, Amelie; David, Ophelie; Shin, Hyeon Ho; Li, Zhun; Cao, Xiuyun; Cabrini, Marina; Klisarova, Daniela; Gu, Haifeng			<i>Gonyaulax</i><i> montresoriae</i> sp. nov. (Dinophyceae) from the Adriatic Sea produces predominantly yessotoxin	HARMFUL ALGAE			English	Article						Cysts; Dinoflagellate; Harmful algal bloom; Mediterranean Sea; Spiniferites	IZMIR BAY; DINOFLAGELLATE; SPINIFERITES; TEMPERATURE; SALINITY; MUSSELS; ANALOG	Yessotoxin is one of the shellfish toxins leading to mussel farm closures in the Adriatic Sea of Italy. Two putative Gonyaulax spinifera strains GSA0501 and GSA0602 are known as yessotoxins producers, but their identities have remained elusive since 2005. To address this gap, we established five Gonyaulax strains by incubating sediments from the Adriatic Sea and subsequently isolating single cells. Both cyst and theca morphology were examined using light and scanning electron microscopy. In addition, LSU and/or SSU rRNA gene sequences were obtained for all strains. Two strains produce cysts resembling Spiniferites mirabilis and one strain was related to S. scabratus. The other two strains are described as Gonyaulax montresoriae sp. nov., characterized by a high cingular displacement and overhang, along with two unequal antapical spines. Cysts of G. montresoriae are pear-shaped, showing a smooth surface and exclusively gonal processes with perforations at the base, the latter similar to S. lazus. LSU rRNA gene sequence comparison suggests that the G. spinifera strain GSA0501 isolated from the Adriatic Sea in 2005 should also be identified as G. montresoriae. Maximum likelihood and Bayesian inference analyses based on LSU and SSU rRNA gene sequences reveal that G. montresoriae is monophyletic, and close to several toxic strains of presumable Gonyaulax spinifera from the Adriatic Sea and New Zealand, whose taxonomic positions are uncertain. One strain of G. montresoriae was examined for yessotoxin production using LC-MS/MS, and found to produce predominantly yessotoxin at a concentration of 3.0 pg cell-1 . Our results highlight the rich diversity and risks associated with Gonyaulax species in the Mediterranean Sea.	[Huang, Shuning] Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China; [Huang, Shuning; Gu, Haifeng] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil; Derrien, Amelie; David, Ophelie] IFREMER, COAST, F-29900 Concarneau, France; [David, Ophelie] Univ Brest, IFREMER, CNRS, UMR 6538,Geoocean, F-29280 Plouzane, France; [Shin, Hyeon Ho] Pukyong Natl Univ, Div Fisheries Life Sci, Busan 48574, South Korea; [Li, Zhun] Korea Res Inst Biosci & Biotechnol, Biol Resource Ctr, KCTC, Jeongeup 56212, South Korea; [Cao, Xiuyun] Chinese Acad Sci, Inst Hydrobiol, Wuhan 430072, Peoples R China; [Cabrini, Marina] Natl Inst Oceanog & Expt Geophys, Sgonico, Italy; [Klisarova, Daniela] Med Univ Pleven, Fac Med, Dept Anat Histol Cytol & Biol, Pleven, Bulgaria; [Klisarova, Daniela] Agricultural Acad, Inst Fish Resources, Varna 9000, Bulgaria	Nanjing University of Information Science & Technology; Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; Ifremer; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ifremer; Universite de Bretagne Occidentale; Pukyong National University; Korea Research Institute of Bioscience & Biotechnology (KRIBB); Chinese Academy of Sciences; Institute of Hydrobiology, CAS; Medical University Pleven; Agricultural Academy - Bulgaria	Gu, HF (通讯作者)，Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Li, Zhun/IUQ-5309-2023; Mertens, Kenneth/C-3386-2015	David, Ophelie/0009-0009-8006-4349; Mertens, Kenneth/0000-0003-2005-9483; Shin, Hyeon Ho/0000-0002-9711-6717; huang, shuning/0009-0005-7441-119X; LI, ZHUN/0000-0001-8961-9966; Derrien, Amelie/0000-0001-9656-7850	National Natural Science Foundation of China [42076085]; French National Research Agency (ANR) [ANR-20-CE02-0025]; Project ORDINAR [ANR-22-CE01-0010];  [42030404]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); French National Research Agency (ANR)(Agence Nationale de la Recherche (ANR)Norwegian Agency for Development Cooperation - NORAD); Project ORDINAR; 	This work was supported by the National Natural Science Foundation of China (42076085, 42030404) . KNM and OD was financially supported by the French National Research Agency (ANR) PhenoMap project, ANR-20-CE02-0025 and the project ORDINAR (ANR-22-CE01-0010) .	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J	Omietimi, EJ; Lenhardt, N; Yang, RC; Goetz, AE; Edegbai, AJ; Bumby, AJ				Omietimi, Erepamo J.; Lenhardt, Nils; Yang, Renchao; Goetz, Annette E.; Edegbai, Aitalokhai J.; Bumby, Adam J.			Multi-Parameter Investigation of Cretaceous to Palaeocene Sedimentary Sequences in the Anambra and Niger Delta Basins, Nigeria: Organic Matter Characterisation, Palynofacies and Implications for Palaeoclimate and Sea-Level Changes	GEOLOGICAL JOURNAL			English	Article						black shale; marginal marine environment; palaeobathymetry; sea-level changes; subsurface interpretations; Upper Cretaceous	TRIASSIC YANCHANG FORMATION; GEOCHEMICAL CHARACTERISTICS; BENUE TROUGH; RARE-EARTH; DEPOSITIONAL ENVIRONMENT; TRACE-ELEMENTS; INLAND BASINS; SOURCE-ROCK; OIL-SHALE; PALEOENVIRONMENT	The Anambra Basin of Nigeria, part of the larger West and Central African Rift System (WCARS) across Africa, contains primarily Cretaceous to Palaeocene shallow to marginal marine and freshwater sedimentary deposits. The organic-rich deposits of the Cretaceous Nkporo and Mamu formations within the Anambra Basin and the Palaeocene Imo Formation of the Niger Delta Basin constitute important conventional source rocks. Despite its economic significance, research on organic matter characterisation, palynofacies, sea-level fluctuations, palaeoclimate, hydrogeography, basin restriction, palaeobathymetry and the factors controlling organic matter preservation remains largely undocumented. The here presented new inorganic and organic geochemical and organic petrography data of the Cretaceous to Palaeocene deposits serve to refine the regional interpretation at a basinal scale and within the supra-regional context of the WCARS. Geochemical palaeotemperature proxies suggest a warm and humid tropical palaeoclimate during the Late Cretaceous within the study area. Furthermore, the measured TOC values indicate poor to very good organic content. Palynofacies analysis revealed high abundances of opaque and translucent phytoclasts and low amounts of palynomorphs with negligible amorphous organic matter (AOM) in the studied mudrocks. Two palynofacies groups suggest shallow-marine conditions in a proximal shelf setting and a heterolithic oxic basin. The palynofacies of the upper Imo Formation reveal higher percentages of dinoflagellate cysts during the early highstand phase, with equidimensional, opaque phytoclasts representing the maximum flooding phase, accompanied by warmer conditions. Additionally, abundant terrestrial phytoclasts, Deltoidospora spp., Classopollis spp. and geochemical indicators collectively indicate warm tropical climatic conditions consistent with geochemical interpretations. The palaeobathymetry reconstructions suggest a shallow seaway during the Upper Cretaceous in the Anambra Basin.	[Omietimi, Erepamo J.; Lenhardt, Nils; Edegbai, Aitalokhai J.; Bumby, Adam J.] Univ Pretoria, Dept Geol, Pretoria, South Africa; [Omietimi, Erepamo J.] Niger Delta Univ, Dept Geol, Amassoma, Yenagoa, Nigeria; [Yang, Renchao] Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao, Peoples R China; [Yang, Renchao] Qingdao Marine Sci & Technol Ctr, Lab Marine Mineral Resources, Qingdao, Peoples R China; [Goetz, Annette E.] Georg August Univ Gottingen, Dept Struct Geol & Geodynam, Gottingen, Germany; [Edegbai, Aitalokhai J.] Univ Benin, Dept Geol, Benin, Nigeria	University of Pretoria; Shandong University of Science & Technology; University of Gottingen; University of Benin	Lenhardt, N (通讯作者)，Univ Pretoria, Dept Geol, Pretoria, South Africa.	nils.lenhardt@up.ac.za	Omietimi, Erepamo/IWD-7777-2023; Götz, Annette/AAJ-5873-2020; Lenhardt, Nils/F-4773-2010; Edegbai, Aitalokhai/AAX-1356-2021	Lenhardt, Nils/0000-0002-7239-9634; Gotz, Annette E./0000-0002-7467-3617; Omietimi, Erepamo/0000-0002-3214-0740; Edegbai, Aitalokhai/0000-0003-0089-5126	National Natural Science Foundation of China; University of Pretoria [12120100500017001]; Nigerian Geological Survey Agency;  [41972146]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); University of Pretoria; Nigerian Geological Survey Agency; 	E. J. O. and N. L. thank the University of Pretoria for their financial support. R. Y. thanks the China-ASEAN Maritime Cooperation Fund Project (Grant 12120100500017001) and the National Natural Science Foundation of China (Grant 41972146) for financial support. Reuben Okoliko of the Nigerian Geological Survey Agency is acknowledged for his support in providing the ditch/core samples. We want to express our gratitude to Dr. Tim Moore for his constructive feedback and suggestions that greatly improved the quality of the manuscript. Additionally, we sincerely appreciate the valuable feedback of the anonymous reviewer, which significantly contributed to presenting the results of our work. Finally, we also thank the Editor-in-Chief, Prof. Ian D. Somerville, for his valuable corrections and handling of our manuscript.	Abubakar M.B., 2014, Nat. 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J	Li, ZC; Zhuang, JY; Cao, JZ; Han, Q; Luo, Z; Wang, BT; Wang, HB; Dong, CF; Li, AX				Li, Zhicheng; Zhuang, Jingyu; Cao, Jizhen; Han, Qing; Luo, Zhi; Wang, Baotun; Wang, Hebing; Dong, Chuanfu; Li, Anxing			Fine structural features of the free-living stages of <i>Amyloodinium ocellatum</i> (Dinoflagellata, Thoracosphaeraceae): A marine fish ectoparasite	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						<italic>Amyloodinium ocellatum</italic>; organelle; parasitic dinoflagellate; ultrastructure	MILKFISH CHANOS-CHANOS; CYST WALL; CRYPTOCARYON-IRRITANS; DICENTRARCHUS-LABRAX; STANDARDIZED METHOD; BROWN 1931; CILIATE; ULTRASTRUCTURE; EXTRUSOMES; PHYLOGENY	Amyloodinium ocellatum is a protozoan parasite that causes amyloodiniosis in marine and brackish water fish, threatening global aquaculture. The present study investigates the morphology and ultrastructure of the free-living stages of A. ocellatum (tomont and dinospore) using light microscopy (LM), scanning electron microscopy (SEM), and transmission electron microscopy (TEM). Dinospores measured 13.03-19.66 mu m in length, 12.32-18.71 mu m in width, and were laterally flattened. Dinospores had a transverse flagellum for propulsion and a longitudinal flagellum for direction control. The cyst wall had three distinct layers and included cellulose. The outer wall was coated with numerous bacteria. The orange-red speckled eyespot was observed all tomont developmental stages and in the dinospore of A. ocellatum. Tomonts proliferation required successive nuclear division, the formation of new cyst walls, and cytoplasmic segregation. The cytoplasm comprises mainly the matrix, organelles, and inclusions. The matrix was grainy and evenly distributed. In addition to organelles, including mitochondria with tubular cristae, Golgi apparatus, and endoplasmic reticulum, the cytoplasm had starch grains and lipid droplets as inclusions. The A. ocellatum cells lacked chloroplasts. This study provides the first ultrastructural view of the cytoplasmic structure of the free-living stages of A. ocellatum.	[Li, Zhicheng; Zhuang, Jingyu; Cao, Jizhen; Han, Qing; Luo, Zhi; Wang, Baotun; Wang, Hebing; Dong, Chuanfu; Li, Anxing] Sun Yat Sen Univ, State Key Lab Biocontrol, Guangdong Prov Key Lab Improved Variety Reprod Aqu, Sch Life Sci, 135 Xingang West St, Guangzhou 510275, Guangdong, Peoples R China; [Li, Zhicheng; Zhuang, Jingyu; Cao, Jizhen; Han, Qing; Luo, Zhi; Wang, Baotun; Wang, Hebing; Dong, Chuanfu; Li, Anxing] Sun Yat Sen Univ, Inst Aquat Econ Anim, Sch Life Sci, 135 Xingang West St, Guangzhou 510275, Guangdong, Peoples R China	Sun Yat Sen University; Sun Yat Sen University	Li, AX (通讯作者)，Sun Yat Sen Univ, State Key Lab Biocontrol, Guangdong Prov Key Lab Improved Variety Reprod Aqu, Sch Life Sci, 135 Xingang West St, Guangzhou 510275, Guangdong, Peoples R China.; Li, AX (通讯作者)，Sun Yat Sen Univ, Inst Aquat Econ Anim, Sch Life Sci, 135 Xingang West St, Guangzhou 510275, Guangdong, Peoples R China.	lianxing@mail.sysu.edu.cn	Luo, Zhi/GRY-1871-2022		Marine Economic Development in Guangdong Province	Marine Economic Development in Guangdong Province	We wish to cordially acknowledge Hongmei Li, Yingying Li, Dong Chen, Jiabiao Yang, and Jiamin Zhang from the electron microscope chamber of the State Key Laboratory of Biocontrol. 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J	Tulatz, S; Krock, B; Tillmann, U; Meunier, CL				Tulatz, Simon; Krock, Bernd; Tillmann, Urban; Meunier, Cedric Leo			Effects of temperature, salinity and CO<sub>2</sub> concentration on growth and toxin production of the harmful algal bloom species <i>Alexandrium pseudogonyaulax</i> (Dinophyceae) from the Danish Limfjord	HARMFUL ALGAE			English	Article						Autecology; Goniodomin A; Biogeography; Northern Europe	PHYTOPLANKTON COMMUNITIES; OSTENFELDII DINOPHYCEAE; SPIROLIDE PRODUCTION; INORGANIC NITROGEN; CYST PRODUCTION; COASTAL WATERS; LIFE-HISTORY; TOXICITY; DYNAMICS; EXCYSTMENT	The marine dinoflagellate Alexandrium pseudogonyaulax is a widely distributed Harmful Algal Bloom (HAB) species that produces the macrocyclic polyketide goniodomin A (GDA). Occurrences in northern European waters are increasing and a spreading of the species along a salinity gradient into the Baltic Sea has been observed. As GDA is suspected to lead to invertebrate mortality, the spreading is of concern for the environment and possibly human health. In order to assess the potential of A. pseudogonyaulax to adapt to the environmental conditions in the Baltic Sea and the risk of future harmful blooms of that species, we quantified the influence of bottom-up factors on the growth and toxin content of three strains of A. pseudogonyaulax from the Danish Limfjord. Specifically, we exposed these strains to salinities ranging from 5 to 50, temperatures in the range of 10 - 30 degrees C and to three different CO2 concentrations of 250, 400 and 1000 mu atm. All strains tolerated a broad range of salinities and temperatures, resulting in positive growth rates ranging from 0.06 to 0.33 d-1 between temperatures of 12 and 27 degrees C and between salinities of 10 and 40. The highest cell quotas of GDA were measured at low temperatures. For two strains, GDA amounts were almost unaffected by salinity, while the cell quota of the third strain decreased about 20-fold when salinity increased above 30. Different CO2 concentrations had no effect on growth or GDA production. In summary, these findings show a high ecological tolerance towards a wide range of temperatures and salinities of the Limfjord population of A. pseudogonyaulax, together with distinct intraspecific physiological differences within the population. Our results also suggest that a further spreading into the Baltic Sea might be possible.	[Tulatz, Simon; Krock, Bernd; Tillmann, Urban] Alfred Wegener Inst Helmholtz Zentrum Polar & Meer, Handelshafen 12, D-27570 Bremerhaven, Germany; [Meunier, Cedric Leo] Alfred Wegener Inst Helmholtz Zentrum Polar & Meer, Biolog Anstalt Helgoland, D-27483 Helgoland, Germany		Tulatz, S (通讯作者)，Alfred Wegener Inst Helmholtz Zentrum Polar & Meer, Handelshafen 12, D-27570 Bremerhaven, Germany.	simon.tulatz@awi.de	Krock, Bernd/ABB-7541-2020; Meunier, Cedric/K-2792-2015					Abdullah N, 2023, HARMFUL ALGAE, V127, DOI 10.1016/j.hal.2023.102475; Aguilera-Belmonte A, 2011, HARMFUL ALGAE, V12, P105, DOI 10.1016/j.hal.2011.09.006; Andersson A, 2015, AMBIO, V44, pS345, DOI 10.1007/s13280-015-0654-8; Back O., 2019, Product Information Document (PIDoc), DOI [10.13155/61815, DOI 10.13155/61815]; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Beuzenberg V, 2012, J APPL PHYCOL, V24, P1023, DOI 10.1007/s10811-011-9726-8; Biecheler B., 1952, Bull. Biol. Fr. 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J	Tao, Z; Liu, XH; Song, XY; Deng, YY; Shang, LX; Chai, ZY; Hu, ZX; Liu, YY; Tang, YZ				Tao, Zhe; Liu, Xiaohan; Song, Xiaoying; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Hu, Zhangxi; Liu, Yuyang; Tang, Ying Zhong			Species and genetic diversity of notorious dinoflagellates<i> Pfiesteria</i><i> piscicida,</i><i> Luciella</i><i> masanensis,</i> and relatives in marine sediments of China	HARMFUL ALGAE			English	Article						Dinoflagellate; Resting cysts; Pfiesteria; Luciella masanensis; Fluorescence in situ hybridization (FISH); Single-cyst sequencing	TOXIC PFIESTERIA COMPLEX; DINOFLAGELLATE PFIESTERIA; GEOGRAPHIC-DISTRIBUTION; COASTAL WATERS; SP-NOV; GREEN AUTOFLUORESCENCE; PISCICIDA DINOPHYCEAE; APHANOMYCES-INVADANS; GONYAULAX-TAMARENSIS; ATLANTIC MENHADEN	The dinoflagellate genus Pfiesteria, encompassing Pfiesteria piscicida and P. shumwayae, became a hot topic in HABs research in the early 2000s due to numerous but controversial reports regarding life cycle and toxicity. While Pfiesteria presence has been reported from all continents, surprisingly, there has been no documented presence in China to date. Here, we report our findings on the presence, species, and genetic diversity of Pfiesteria and its phylogenetic relatives (particularly Luciella masanensis) using a combined approach. First, we demonstrated the presence of P. piscicida and L. masanensis using metabarcoding analysis of >320 sediment samples. Pfiesteria piscicida was identified in 32 sampling sites across all four seas of China, with rDNA sequences exhibiting considerable differences from the type strain (up to 3.83 %), while Luciella masanensis presented in 212 sites from all four seas and included only ribotypes 1 and 3 among the four known ribotypes. Second, based on the metabarcoding detections, our application of FISH with species-specific probes and subsequent single-cyst PCR sequencing to the "positive" sediments confirmed, both morphologically and molecularly, the existence of P. piscicida and L. masanensis cysts in the sediments. Finally, individual cysts were isolated using the sodium polytungstate protocol and sequenced targeting 28S rDNA D1-D6 domains. Phylogenetic analysis revealed that 35 resting cysts were relatives of Pfiesteria, likely belonging to either new species or novel genera and family because they formed at least two distinct clades in the phylogenetic tree. Pfiesteria shumwayae was not detected from any sample, suggesting its absence in Chinese waters. We believe this work provides important factual basis for the global biogeography of these species and future HABs monitoring of in China.	[Tao, Zhe; Liu, Xiaohan; Song, Xiaoying; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Liu, Yuyang; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Liu, Yuyang; Tang, Ying Zhong] Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Tao, Zhe; Liu, Xiaohan; Song, Xiaoying] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Hu, Zhangxi] Guangdong Ocean Univ, Coll Fisheries, Dept Aquaculture, Zhanjiang 524088, Peoples R China; [Liu, Yuyang] Shandong Univ Sci & Technol, Coll Safety & Environm Engn, Qingdao 266590, Shandong, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Guangdong Ocean University; Shandong University of Science & Technology	Liu, YY; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Liu, YY; Tang, YZ (通讯作者)，Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.	yuyangliu@sdust.edu.cn; yingzhong.tang@qdio.ac.cn	Tao, Zhe/LIG-2380-2024; ZHANG, hui jie/HTN-1690-2023; Chai, Zhaoyang/F-7485-2017; Li, Yang/KFB-5350-2024	Hu, Zhangxi/0000-0002-4742-4973	Science and Technology Innovation Project of Laoshan Laboratory [LSKJ202203700]; Science & Technology Basic Resources Investigation Program of China [2018FY100200]; National Science Foundation of China [42106199]	Science and Technology Innovation Project of Laoshan Laboratory; Science & Technology Basic Resources Investigation Program of China; National Science Foundation of China(National Natural Science Foundation of China (NSFC))	We are extremely grateful to the members of the research team who diligently collected the sediment samples used in the study. This work was financially supported by the Science and Technology Innovation Project of Laoshan Laboratory (Grant No. LSKJ202203700), the Science & Technology Basic Resources Investigation Program of China (Grant No. 2018FY100200), and the National Science Foundation of China (Grant No. 42106199) . We are also grateful to Dr. Po Teen Lim from the University of Malaya for the help in editing the manuscript and to two anonymous reviewers for their highly constructive comments.	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J	Iakovleva, AI				Iakovleva, Alina I.			Organic walled dinoflagellate cyst biostratigraphy of the Bartonian/ Priabonian GSSP Alano di Piave section, NE Italy	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Eocene; Organic walled dinoflagellate cysts; Biostratigraphy; GSSP Bartonian-Priabonian; Italy	EOCENE-OLIGOCENE TRANSITION; MIDDLE EOCENE; RESEARCH BOREHOLE; SEA; STRATIGRAPHY; ZONATION; CLIMATE; RECORD	The present paper augments the multidisciplinary stratigraphic analysis of the Global Stratotype Section and Point (GSSP) Bartonian-Priabonian boundary Alano di Piave section (NE Italy). Twenty-seven stratigraphically signficant organic walled dinoflagellate cyst events, calibrated against the magnetostratigraphic polarity timescale, and earlier established zonations based on calcareous microfossils are recognized. Among these events the first occurrence (FO) of Oligokolpoma agniniae sp. nov. (-8 m below the GSSP boundary), and the FO of Reticulatosphaera actinocoronata (-8 m above the GSSP boundary) may be considered as additional stratigraphic indicators for the Bartonian-Priabonian boundary. Six new potentially stratigraphically significant species Heteraulacacysta alanoensis sp. nov., Heteraulacacysta reticulata sp. nov., Impagidinium bellunoensis sp. nov., Impagidinium veneziaense sp. nov., Lophocysta domenicorioi sp. nov., and Oligokolpoma agniniae sp. nov. are formally described.	[Iakovleva, Alina I.] Russian Acad Sci, Geol Inst, Pyzhevsky Pereulok 7, Moscow 119017, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Iakovleva, AI (通讯作者)，Russian Acad Sci, Geol Inst, Pyzhevsky Pereulok 7, Moscow 119017, Russia.	alina.iakovleva@gmail.com			State program of the Geological Institute of Russian Academy of Sciences	State program of the Geological Institute of Russian Academy of Sciences	Dr. Claudia Agnini and co-workers are thanked for providing the samples from Alano di Piave. The technicians of the laboratories of the UU Geolab are thanked for sample processing. I am extremely grateful to my colleagues Henk Brinkhuis (NIOZ and Utrecht University, The Netherlands) and Sander Houben (Geological Survey, TNO, The Netherlands) for our joint efforts on this material, our regular and fruitful discussions, and very useful advices. Manuel Vieira is thanked for his careful review. The present research was supported by the State program of the Geological Institute of Russian Academy of Sciences.	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J	Lazarev, S; Alcicek, MC; Rausch, L; Stoica, M; Kuiper, K; Neubauer, TA; Abels, HA; Hoyle, TM; van Baak, CGC; Foubert, A; Bista, D; Sangiorgi, F; Wesselingh, FP; Krijgsman, W				Lazarev, Sergei; Alcicek, Mehmet Cihat; Rausch, Lea; Stoica, Marius; Kuiper, Klaudia; Neubauer, Thomas A.; Abels, Hemmo A.; Hoyle, Thomas M.; van Baak, Christiaan G. C.; Foubert, Anneleen; Bista, Diksha; Sangiorgi, Francesca; Wesselingh, Frank P.; Krijgsman, Wout			Early Pleistocene invasion of Pontocaspian Fauna into the Denizli Basin (SW Anatolia): New stratigraphic constraints and implications for Aegean-Pontocaspian hydrological exchange	QUATERNARY SCIENCE REVIEWS			English	Article						Early Pleistocene; Denizli basin; Pontocaspian fauna; Ecological turnover	LATE MIOCENE; DACIAN BASIN; TECTONOSEDIMENTARY EVOLUTION; PALEOENVIRONMENTAL EVOLUTION; DEPOSITIONAL-ENVIRONMENTS; DINOFLAGELLATE CYSTS; SEDIMENTARY FACIES; CLIMATE CHANGES; LATE PLIOCENE; TURKEY	Aquatic biodiversity hotspots often emerge in regions with active tectonism, diverse climate conditions and complex basin configurations enabling episodic biotic isolation and exchange. The Anatolian microcontinent, located between the Mediterranean and Pontocaspian regions, has been considered a cradle of biodiversity for continental aquatic organisms. The Denizli Basin succession of SW Anatolia contains a " Didacna " mollusc fauna that could be the precursor of the modern Pontocaspian mollusc faunas of the Black Sea-Caspian Sea regions. However, the appearance of Pontocaspian faunas in the Denizli Basin and constraints upon their ages and dispersal pathways remain enigmatic. Moreover, the emergence of the Pontocaspian biota far into the Anatolian continental interior raises questions regarding the connectivity history and tectonic evolution of the Anatolian, Aegean and Pontocaspian realms. Here, we present an integrated stratigraphy of the 1 km thick succession of the Kolankaya Formation of the Denizli Basin, previously assigned to the Late Miocene. To date the first occurrence of Pontocaspian fauna in the Denizli Basin and to characterise accompanying palaeoenvironmental/ palaeohydrological changes, we focus on three sets of approaches: dating (magnetostratigraphy and 40 Ar/ 39 Ar), biotic record (molluscs, ostracods and dinoflagellates) and hydrological connectivity (O- and C-isotopes and 87 Sr/ 86 Sr). We date the studied section as Early Pleistocene, spanning a time range of 2.6 Ma to 0.7 Ma. During that time, the Denizli Basin hosted an isolated to partially hydrologically open oligo-to mesohaline lake. The biotic record shows a drastic turnover of mollusc fauna from endemic Aegean-Anatolian and Pannonian/Paratethyan to Pontocaspian affinity at 1.8 Ma. The palaeogeographic evolution of the region, along with the geographically limited appearance of the Pontocaspian faunas, suggests a dispersal pathway from the Black Sea Basin via the Aegean Basin. Subsequently, a short incursion into the Denizli Basin may have occurred via a series of graben-type basins: either via the So<spacing diaeresis>ke-Milet Basin - B & uuml;y & uuml;k Menderes Graben or via Izmir Bay - Gediz Graben. Our study shows that the Denizli Basin was not a cradle but rather a sink of the Pontocaspian biota during the Early Pleistocene. The new Early Pleistocene age assignment for the Pontocaspian fauna and the Kolankaya Formation in Denizli calls for a major reappraisal of models for the tectonic and stratigraphic evolution of SW Anatolia, including the regional interbasinal connectivity history.	[Lazarev, Sergei; Hoyle, Thomas M.; van Baak, Christiaan G. C.; Sangiorgi, Francesca; Wesselingh, Frank P.; Krijgsman, Wout] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Lazarev, Sergei; Foubert, Anneleen] Univ Fribourg, Dept Geosci, Fribourg, Switzerland; [Lazarev, Sergei] Jurass Museum, Porrentruy, Switzerland; [Alcicek, Mehmet Cihat] Pamukkale Univ, Dept Geol, Denizli, Turkiye; [Rausch, Lea; Stoica, Marius] Univ Bucharest, Dept Geol Palaeontol & Mineral, Bucharest, Romania; [Rausch, Lea] Petrostrat Ltd, Tan Y Graig Parc Caer Seion, Conwy, Wales; [Kuiper, Klaudia] Vrije Univ Amsterdam, Dept Earth Sci, Amsterdam, Netherlands; [Neubauer, Thomas A.] SNSB, Bavarian State Collect Palaeontol & Geol, Munich, Germany; [Neubauer, Thomas A.; Wesselingh, Frank P.] Nat Biodivers Ctr, Leiden, Netherlands; [Abels, Hemmo A.] Delft Univ Technol, Dept Geosci & Engn, Delft, Netherlands; [Hoyle, Thomas M.] Broadcast Engn Syst, Liskeard, Cornwall, England; [Bista, Diksha] British Geol Survey, Keyworth, England	Utrecht University; University of Fribourg; Ministry of Energy & Natural Resources - Turkey; Pamukkale University; University of Bucharest; Vrije Universiteit Amsterdam; Naturalis Biodiversity Center; Delft University of Technology; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Lazarev, S (通讯作者)，Univ Fribourg, Dept Geosci, Fribourg, Switzerland.	s.lazarev@uu.nl	Neubauer, Thomas/I-1889-2019; Lazarev, Sergei/AAP-2723-2021	Lazarev, Sergei/0000-0003-3735-1296; Neubauer, Thomas A./0000-0002-1398-9941; van Baak, Christiaan/0000-0002-2044-2872; Abels, Hemmo/0000-0001-7648-3369	European Union [642973]	European Union(European Union (EU))	Our research was part of the PRIDE project (Drivers of Pontocaspian Biodiversity Rise and Demise) , funded by the European Union's Horizon 2020 research and innovation program under the Marie Sklodowska-Curie Action (grant agreement No 642973) . We would like to thank Sabrina van de Velde (University of Delft) and Guelcin Ayguen for organising the fieldwork and Andres Rueggeberg for helping with isotopic data acquisition. We are also thankful to two anonymous reviewers for improvements of the manuscript.	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Sci. Rev.	DEC 15	2024	346								109050	10.1016/j.quascirev.2024.109050	http://dx.doi.org/10.1016/j.quascirev.2024.109050		NOV 2024	17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	M5X8A		hybrid			2025-03-11	WOS:001358271300001
J	Sluijs, A; Brinkhuis, H				Sluijs, Appy; Brinkhuis, Henk			High Arctic late Paleocene and early Eocene dinoflagellate cysts	JOURNAL OF MICROPALAEONTOLOGY			English	Article							BIOMARKER PALEOTHERMOMETRY; ENVIRONMENTAL-CHANGE; NORTH-SEA; CLIMATE; MARINE; BASIN; BIOSTRATIGRAPHY; RECONSTRUCTIONS; ASSEMBLAGES; TEMPERATURE	Palynomorphs, notably sporomorphs and organic-walled dinoflagellate cysts, or "dinocysts", are the only abundant microfossils consistently present in the sole available central Arctic upper Paleocene to lower Eocene sedimentary succession recovered at the central Lomonosov Ridge by the Integrated Ocean Drilling Program (IODP) Expedition 302 (or the Arctic Coring Expedition, ACEX) in 2004, close to the North Pole. While the analysis and interpretation of a part of these assemblages have so far guided many major stratigraphic, climatological, and paleoenvironmental findings from ACEX, intrinsic details, notably of the dinocyst taxa and assemblages, have not yet been addressed. Here, we present new ACEX dinocyst data for the interval spanning the latest Paleocene to the earliest Eocene (similar to 56.5-53.8 Ma; cores 32X-27X) and integrate these with previous results. We develop a pragmatic taxonomic framework, document critical biostratigraphic events, and propose two new genera (Guersteinia and Sangiorgia) and seven new species (Batiacasphaera obohikuenobeae, Chaenosphaerula sliwinskae, Heterolaucacysta pramparoae, Pyxidinopsis iakovlevae, Sangiorgia pospelovae, Sangiorgia marretiae, and Spiniferella crouchiae). In addition, we interpret trends and aberrations in dinocyst assemblages in terms of variability in regional temperature, hydrology, and tectonism across the long-term and the Paleocene-Eocene Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM2) global warming phases.	[Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CB Utrecht, Netherlands; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, Dept Ocean Syst OCS, POB 1790, NL-1790 AB Den Burg, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Sluijs, A (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CB Utrecht, Netherlands.	a.sluijs@uu.nl	Sluijs, Appy/B-3726-2009; Brinkhuis, Henk/IUO-8165-2023	Brinkhuis, Henk/0000-0003-0253-6610	H2020 European Research Council; Arctic Coring Expedition	H2020 European Research Council(Horizon 2020European Research Council (ERC)); Arctic Coring Expedition	We thank the International Ocean Discovery Program and predecessors for samples and data and the science party of the Arctic Coring Expedition (2004) for their scientific and collaborative efforts. We thank Natasja Welters and Giovanni Dammers (Geolab, Utrecht University) for palynological processing and Gea Zijlstra (Utrecht University) for advice regarding the nomenclature of the newly described taxa. We also thank Ian Harding and an anonymous reviewer for their constructive and detailed analysis of the originally submitted version of this work.	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J	Everaert, S; Deckers, J; Bosselaers, M; Schiltz, M; Louwye, S				Everaert, Stijn; Deckers, Jef; Bosselaers, Mark; Schiltz, Marco; Louwye, Stephen			A Neogene succession in the city centre of Antwerp (Belgium): stratigraphy, palaeontology and geotechnics of the Rubenshuis temporary outcrop	GEOLOGICA BELGICA			English	Article						Kiel Member; Antwerpen Member; Kattendijk Formation; molluscs; dinoflagellate cysts; Miocene; Pliocene; Cone Penetration Tests	DINOFLAGELLATE CYST STRATIGRAPHY; MEMBER BERCHEM FORMATION; NORTHERN BELGIUM; MIOCENE; PLIOCENE; BASIN; SEQUENCE; PALEOECOLOGY; POLYCHAETA; DEPOSITS	A temporary outcrop near the "Rubenshuis" in the centre of Antwerp (northern Belgium) facilitated the study of the Neogene glauconitic sand of the Berchem and Kattendijk formations, west and south of their respective stratotype sections. In contrast to the latter sections, the exposed Kiel Member of the Berchem Formation contains a relatively silty interval in its upper part, which is also reflected in Cone Penetration Tests. This silty interval is rich in molluscs, including the subspecies Glossus lunulatus cf. lunulatus and Ennucula haesendoncki haesendoncki, previously unknown from this member. Dinoflagellate cysts indicate that the main body of the Kiel Member was deposited during the middle Burdigalian, while only the upper part was deposited during the late Burdigalian. The Kiel Member is covered by the shell-rich, silty sand of the Langhian Antwerpen Member (Berchem Formation). Both members display soft-sediment deformation structures, probably caused by differences in silt content between and within these units. The Antwerpen Member is incised by the Lower Pliocene Kattendijk Formation, which reduced the thickness of the former to only 1.1 m, compared to 7 m in northeastern Antwerp. As a result, the basal gravel of the Kattendijk Formation contains many fossils reworked from the Antwerpen Member, in addition to autochthonous molluscs and Ditrupa. The Zanclean fauna resembles associations known from the highest part of the Kattendijk Formation in the former Oosterweel outcrop north of Antwerp, while it differs from the fauna of the lowermost Kattendijk Formation near Doel and Kallo. Hence, the palaeontological observations corroborate the regional depositional model of this unit, suggesting that only the youngest gully sequence of the Kattendijk Formation was deposited across the city of Antwerp.	[Everaert, Stijn; Bosselaers, Mark] Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium; [Deckers, Jef] VITO, Boeretang 200, B-2400 Mol, Belgium; [Bosselaers, Mark] Koninklijk Zeeuwsch Genootschap Wetenschappen, POB 378, NL-4330 AJ Middelburg, Netherlands; [Schiltz, Marco] Samsuffit BVBA, Eggelstr 8, B-2530 Boechout, Belgium; [Louwye, Stephen] Univ Ghent, Dept Geol, Paleontol & Paleoenvironm, Krijgslaan 281, B-9000 Ghent, Belgium	Royal Belgian Institute of Natural Sciences; VITO; Ghent University	Everaert, S (通讯作者)，Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium.	stijn.everaert1@gmail.com; jef.deckers@vito.be; mark.bosselaers@telenet.be; marco@samsuffit.be; stephen.louwye@ugent.be	Louwye, Stephen/D-3856-2012; Everaert, Stijn/JBJ-5025-2023	Everaert, Stijn/0000-0001-9551-9275	Bureau for Environment and Spatial Development - Flanders	Bureau for Environment and Spatial Development - Flanders	We would like to thank several people who contributed to this study. Dimitri De Clerck and Kris Huyghe (both BAM Interbuild) provided access to the Rubenshuis outcrop. We thank the Bureau for Environment and Spatial Development - Flanders, VPO, for financial support. Roel De Koninck (VITO, Mol) assisted in the field. Frank Wesselingh (NBC, Leiden), Ronald Pouwer (NBC, Leiden), Peter Moerdijk (Middelburg) and Aad Bastemeijer (The Hague) helped with the identification ofPliocene molluscs. Frank and Ronald also helped with photographing shells. Kristiaan Hoedemakers (RBINS, Brussels) identified teleost otoliths, and drew our attention to the profile of the Van Ertbornstraat outcrop (June 1996). We thank Rik Houthuys (Halle) for the discussion on the sedimentology. Alfred Uchinan (Jagiellonian University, Poland) provided information about ichnofossils. Ray Perreault (Jarreau Scientific, USA) and Alberto Collareta (Universita di Pisa, Italy) re-identified the barnacles. Pieter De Schutter (RBINS, Brussels) photographed sediment samples. Katleen Van Baelen (VITO, Mol) did the excellent graphic work for the figures. Annelise Folie (RBINS, Brussels) stored the collected fossils in the RBINS collection. Stijn Goolaerts (RBINS, Brussels) shared his insights on the Kattendijk Formation. Finally, we want to thank the reviewers: Noel Vandenberghe (KU Leuven) and Frank Wesselingh (NBC, Leiden). Their constructive suggestions improved our paper significantly.	Bosch J., 2006, CAINOZOIC RES, V4, P109; COGELS P., 1874, Annales de la Societe Malacologique de Belgique, V9, P7; de Heinzelin de Braucourt J., 1950, Stratigraphie pliocene et quaternaire observee au Kruisschans. I. Analyse stratigraphique & II. Conclusions, V26/40-41, P1; de Heinzelin de Braucourt J., 1955, Deuxieme serie d'observations stratigraphiques au Kruisschans. Coupes de l'ecluse Baudoin. I. Analyse stratigraphique & II. 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Belg.		2024	27	1-2					47	70		10.20341/gb.2024.005	http://dx.doi.org/10.20341/gb.2024.005		NOV 2024	24	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	P1F5B					2025-03-11	WOS:001350300700001
J	Ezat, MM; Fahl, K; Rasmussen, TL				Ezat, Mohamed M.; Fahl, Kirsten; Rasmussen, Tine L.			Arctic freshwater outflow suppressed Nordic Seas overturning and oceanic heat transport during the Last Interglacial	NATURE COMMUNICATIONS			English	Article							SOUTHERN NORWEGIAN SEA; NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYSTS; CLIMATE RECORDS; ICE COVER; SURFACE; GREENLAND; MARINE; RECONSTRUCTION	The Last Interglacial period (LIG) was characterized by a long-term Arctic atmospheric warming above the preindustrial level. The LIG thus provides a case study of Arctic feedback mechanisms of the cryosphere-ocean circulation-climate system under warm climatic conditions. Previous studies suggested a delay in the LIG peak warming in the North Atlantic compared to the Southern Ocean and evoked the possibility of southward extension of Arctic sea ice to the southern Norwegian Sea during the early LIG. Here we compile new and published proxy data on past changes in sea ice distribution, sea surface temperature and salinity, deep ocean convection, and meltwater sources based on well-dated records from the Norwegian Sea. Our data suggest that southward outflow of Arctic freshwater supressed Nordic Seas deep-water formation and northward oceanic heat transport during the early LIG. These findings showcase the complex feedback interactions between a warming climate, sea ice, ocean circulation and regional climate.	[Ezat, Mohamed M.] Arctic Univ Norway, Ctr Ice Cryosphere Carbon & Climate iC3, Dept Geosci, UiT, Tromso, Norway; [Fahl, Kirsten] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Handelshafen 12, Bremerhaven, Germany; [Rasmussen, Tine L.] Arctic Univ Norway, Dept Geosci, UiT, Tromso, Norway	UiT The Arctic University of Tromso; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; UiT The Arctic University of Tromso	Ezat, MM (通讯作者)，Arctic Univ Norway, Ctr Ice Cryosphere Carbon & Climate iC3, Dept Geosci, UiT, Tromso, Norway.	mohamed.ezat@uit.no		Ezat, Mohamed/0000-0002-9475-0974; Fahl, Dr., Kirsten/0000-0001-9317-4656	Norges Forskningsrd (Research Council of Norway) [A31720]; Troms Forskningsstiftelse; Research Council of Norway [274429, 332635]; International Programmes (COFUND)-Marie Sklstrok;odowska-Curie Actions under the EU [101118519]; ERC synergy project i2B	Norges Forskningsrd (Research Council of Norway)(Research Council of Norway); Troms Forskningsstiftelse; Research Council of Norway(Research Council of Norway); International Programmes (COFUND)-Marie Sklstrok;odowska-Curie Actions under the EU; ERC synergy project i2B	We thank M. Lindgren, N. El bani Altuna, T. Dahl, I. Hald, K. Monsen, B. Honish, J. Ruprecht, L. Pena, K. Esswein, and W. Luttmer for laboratory support. We also thank E. Capron for sharing data from sediment core MD95-2009. This study is financed by a starting grant from the Troms & oslash; Forskningsstiftelse to M.M.E., project number A31720. The research also received support from the Research Council of Norway and the Co-funding of Regional, National, and International Programmes (COFUND)-Marie Sk & lstrok;odowska-Curie Actions under the EU Seventh Framework Programme (FP7), project number 274429. M.M.E. is also part of the Centre of Excellence iC3, grant number 332635 and the ERC synergy project i2B, grant number 101118519.	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Commun.	OCT 27	2024	15	1							8998	10.1038/s41467-024-53401-3	http://dx.doi.org/10.1038/s41467-024-53401-3			9	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	K4P1D	39465242	gold			2025-03-11	WOS:001343700600004
J	Mazur-Marzec, H; Andersson, AF; Blaszczyk, A; Dabek, P; Górecka, E; Grabski, M; Jankowska, K; Jurczak-Kurek, A; Kaczorowska, AK; Kaczorowski, T; Karlson, B; Katarzyte, M; Kobos, J; Kotlarska, E; Krawczyk, B; Luczkiewicz, A; Piwosz, K; Rybak, B; Rychert, K; Sjöqvist, C; Surosz, W; Szymczycha, B; Torunska-Sitarz, A; Wegrzyn, G; Witkowski, A; Wegrzyn, A				Mazur-Marzec, Hanna; Andersson, Anders F.; Blaszczyk, Agata; Dabek, Przemyslaw; Gorecka, Ewa; Grabski, Michal; Jankowska, Katarzyna; Jurczak-Kurek, Agata; Kaczorowska, Anna K.; Kaczorowski, Tadeusz; Karlson, Bengt; Katarzyte, Marija; Kobos, Justyna; Kotlarska, Ewa; Krawczyk, Beata; Luczkiewicz, Aneta; Piwosz, Kasia; Rybak, Bartosz; Rychert, Krzysztof; Sjoqvist, Conny; Surosz, Waldemar; Szymczycha, Beata; Torunska-Sitarz, Anna; Wegrzyn, Grzegorz; Witkowski, Andrzej; Wegrzyn, Alicja			Biodiversity of microorganisms in the Baltic Sea: the power of novel methods in the identification of marine microbes	FEMS MICROBIOLOGY REVIEWS			English	Review						Baltic Sea; marine ecosystem; diversity of microorganisms; molecular methods; prokaryotic and eukaryotic microorganisms; marine viruses	DINOFLAGELLATE RESTING CYSTS; RESISTANT ESCHERICHIA-COLI; AREA KIEL-BIGHT; ANTIBIOTIC-RESISTANCE; COASTAL WATERS; ANTIMICROBIAL RESISTANCE; COMMUNITY STRUCTURE; SEASONAL DYNAMICS; WASTE-WATER; BEACH SAND	Until recently, the data on the diversity of the entire microbial community from the Baltic Sea were relatively rare and very scarce. However, modern molecular methods have provided new insights into this field with interesting results. They can be summarized as follows. (i) Although low salinity causes a reduction in the biodiversity of multicellular species relative to the populations of the North-East Atlantic, no such reduction occurs in bacterial diversity. (ii) Among cyanobacteria, the picocyanobacterial group dominates when considering gene abundance, while filamentous cyanobacteria dominate in means of biomass. (iii) The diversity of diatoms and dinoflagellates is significantly larger than described a few decades ago; however, molecular studies on these groups are still scarce. (iv) Knowledge gaps in other protistan communities are evident. (v) Salinity is the main limiting parameter of pelagic fungal community composition, while the benthic fungal diversity is shaped by water depth, salinity, and sediment C and N availability. (vi) Bacteriophages are the predominant group of viruses, while among viruses infecting eukaryotic hosts, Phycodnaviridae are the most abundant; the Baltic Sea virome is contaminated with viruses originating from urban and/or industrial habitats. These features make the Baltic Sea microbiome specific and unique among other marine environments.	[Mazur-Marzec, Hanna; Blaszczyk, Agata; Kobos, Justyna; Surosz, Waldemar; Torunska-Sitarz, Anna] Univ Gdansk, Dept Marine Biol & Biotechnol, Al Pilsudskiego 46, PL-81378 Gdynia, Poland; [Andersson, Anders F.] KTH Royal Inst Technol, Dept Gene Technol, Sci Life Lab, Tomtebodavagen 23A, SE-17165 Stockholm, Sweden; [Dabek, Przemyslaw; Gorecka, Ewa; Witkowski, Andrzej] Univ Szczecin, Inst Marine & Environm Sci, Mickiewicza 16A, PL-70383 Szczecin, Poland; [Grabski, Michal] Univ Gdansk, Int Ctr Canc Vaccine Sci, Kladki 24, PL-80822 Gdansk, Poland; [Jankowska, Katarzyna] Gdansk Univ Technol, Dept Environm Engn Technol, Narutowicza 11-12, PL-80233 Gdansk, Poland; [Jurczak-Kurek, Agata] Univ Gdansk, Dept Evolutionary Genet & Biosystemat, Wita Stwosza 59, PL-80308 Gdansk, Poland; [Kaczorowska, Anna K.] Univ Gdansk, Collect Plasmids & Microorganisms, Wita Stwosza 59, PL-80308 Gdansk, Poland; [Kaczorowski, Tadeusz] Univ Gdansk, Dept Microbiol, Lab Extremophiles Biol, Wita Stwosza 59, PL-80308 Gdansk, Poland; [Karlson, Bengt] Swedish Meteorol & Hydrol Inst, Res & Dev, Oceanog, Goteborgseskaderns Plats 3, SE-42671 Vastra Frolunda, Sweden; [Katarzyte, Marija] Klaipeda Univ, Marine Res Inst, Univ Ave 17, LT-92294 Klaipeda, Lithuania; [Kotlarska, Ewa; Szymczycha, Beata] Polish Acad Sci, Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland; [Krawczyk, Beata] Gdansk Univ Technol, Dept Biotechnol & Microbiol, Narutowicza 11-12, PL-80233 Gdansk, Poland; [Piwosz, Kasia] Natl Marine Fisheries Res Inst, Kollataja 1, PL-81332 Gdynia, Poland; [Rybak, Bartosz] Med Univ Gdansk, Fac Hlth Sci, Dept Environm Toxicol, Inst Maritime & Trop Med, Debowa 23A, PL-80204 Gdansk, Poland; [Rychert, Krzysztof] Pomeranian Univ Slupsk, Arciszewskiego 22a, PL-76200 Slupsk, Poland; [Sjoqvist, Conny] Abo Akad Univ, Environm & Marine Biol, Henriksgatan 2, FI-20500 Turku, Finland; [Wegrzyn, Grzegorz] Univ Gdansk, Dept Mol Biol, Wita Stwosza 59, PL-80308 Gdansk, Poland; [Wegrzyn, Alicja] Univ Gdansk, Univ Ctr Appl & Interdisciplinary Res, Kladki 24, PL-80822 Gdansk, Poland	Fahrenheit Universities; University of Gdansk; Royal Institute of Technology; University of Szczecin; Fahrenheit Universities; University of Gdansk; Fahrenheit Universities; Gdansk University of Technology; Fahrenheit Universities; University of Gdansk; Fahrenheit Universities; University of Gdansk; Fahrenheit Universities; University of Gdansk; Swedish Meteorological & Hydrological Institute; Klaipeda University; Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; Fahrenheit Universities; Gdansk University of Technology; National Marine Fisheries Research Institute; Fahrenheit Universities; Medical University Gdansk; Abo Akademi University; Fahrenheit Universities; University of Gdansk; Fahrenheit Universities; University of Gdansk	Wegrzyn, A (通讯作者)，Univ Gdansk, Univ Ctr Appl & Interdisciplinary Res, Kladki 24, PL-80822 Gdansk, Poland.	alicja.wegrzyn@ug.edu.pl	Szymczycha, Beata/ACC-7693-2022; Kaczorowska, Anna-Karina/HNS-7190-2023; Piwosz, Kasia/B-1131-2010; Kotlarska, Ewa/AFO-7236-2022; Krawczyk, Beata/ABG-4358-2020; Mazur-Marzec, Hanna/J-8511-2017; Wegrzyn, Grzegorz/AAL-1179-2020; Sjöqvist, Conny/AAL-1053-2020; Rychert, Krzysztof/G-9703-2011; Andersson, Anders/J-9310-2019; Rybak, Bartosz/N-4801-2019; Luczkiewicz, Aneta/HGU-3312-2022; Kotlarska, Ewa/D-6875-2014; Szymczycha, Beata/T-9029-2018	Torunska-Sitarz, Anna/0000-0003-1274-2688; Kotlarska, Ewa/0000-0002-3122-7772; Szymczycha, Beata/0000-0002-5815-215X; Sjoqvist, Conny/0000-0003-2562-0217; Grabski, Michal/0000-0002-2574-5688	National Science Centre; Commission of Marine Biology and Biotechnology of the Gdansk Branch of the Polish Academy of Sciences	National Science Centre(National Science Centre, Poland); Commission of Marine Biology and Biotechnology of the Gdansk Branch of the Polish Academy of Sciences	The authors acknowledge that the idea of preparing a review article on the biodiversity of Baltic microorganisms appeared during the activity of the Commission of Marine Biology and Biotechnology of the Gdansk Branch of the Polish Academy of Sciences. The authors thank Joanna Bart for professional language corrections.	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Rev.	OCT 24	2024	48	5							fuae024	10.1093/femsre/fuae024	http://dx.doi.org/10.1093/femsre/fuae024			42	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	K0M1N	39366767	hybrid			2025-03-11	WOS:001340902700001
J	Kaga, S; Ito, M; Watanabe, S; Tada, Y; Saido, T; Ito, K				Kaga, Shinnosuke; Ito, Mana; Watanabe, Shiho; Tada, Yumiko; Saido, Takahiro; Ito, Katsutoshi			Effect of the macrobenthic organisms <i>Theora lata</i> (Mollusca), <i>Thyasira tokunagai</i> (Mollusca), and Maldanidae sp. (Annelida) on the germination and abundance of ellipsoidal <i>Alexandrium</i> cysts (Dinophyceae) in Ofunato Bay	FISHERIES SCIENCE			English	Article						Ellipsoidal Alexandrium cysts; Ingestion experiments; Macrobenthic organisms; Theora lata; Maldanidae	RESTING CYSTS; FECAL PELLETS; TIDAL FLAT; DINOFLAGELLATE	One way to resolve the paralytic shellfish poisoning problem is to reduce the number of causative plankton cysts through dredging. However, due to the long-term survival capabilities of Alexandrium cysts, suppressing germination remains a challenge, particularly in areas where these cysts are buried deep within sediments. This challenge could be mitigated by utilizing macrobenthic organisms, specifically deposit feeders, which are capable of ingesting ellipsoidal Alexandrium cysts. In this study, we examined whether three macrobenthic organisms collected from Ofunato Bay, along the Pacific coast of northern Japan, influence the abundance and germination of ellipsoidal Alexandrium cysts through ingestion experiments. The cyst counts in the sediments from ingestion experiments with Thyasira tokunagai (Mollusca) and Maldanidae sp. (Annelida) remained unchanged compared to the control, whereas a significant reduction was observed in the sediments from ingestion experiments with Theora lata (Mollusca). The digestion rate of ellipsoidal Alexandrium cysts by T. lata amounted to 375 cysts per individual per day. Moreover, the germination percentage in the presence of all three macrobenthic organisms declined compared to the control. These findings suggest that T. lata, which are highly concentrated in Ofunato Bay, are effective at removing ellipsoidal Alexandrium cysts and suppressing their germination.	[Kaga, Shinnosuke; Watanabe, Shiho; Tada, Yumiko; Saido, Takahiro] Iwate Fisheries Technol Ctr, 3 75 3 Heita, Kamaishi, Iwate 0260001, Japan; [Ito, Mana; Ito, Katsutoshi] Japan Fisheries Res & Educ Agcy, Fisheries Technol Inst, Environm Conservat Div, 2 17 5 Maruishi, Hatsukaichi, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Kaga, S (通讯作者)，Iwate Fisheries Technol Ctr, 3 75 3 Heita, Kamaishi, Iwate 0260001, Japan.	s-kaga@pref.iwate.jp; ito_mana40@fra.go.jp; shiho@pref.iwate.jp; yumiko-tada@pref.iwate.jp; t-saido@pref.iwate.jp; ito_katsutoshi15@fra.go.jp		Kaga, Shinnosuke/0000-0001-7066-4142				Antonio ES, 2010, ESTUAR COAST SHELF S, V86, P401, DOI 10.1016/j.ecss.2009.05.010; HUGHES RN, 1969, J MAR BIOL ASSOC UK, V49, P805, DOI 10.1017/S0025315400037309; Ichimi K, 2001, FISHERIES SCI, V67, P1178, DOI 10.1046/j.1444-2906.2001.00378.x; Ishihi Y, 2003, MAR ECOL PROG SER, V255, P303, DOI 10.3354/meps255303; Ito K, 2011, MAR BIOL, V158, P1211, DOI 10.1007/s00227-011-1641-7; Kawaida S, 2013, J EXP MAR BIOL ECOL, V449, P93, DOI 10.1016/j.jembe.2013.09.003; Kikuchi T., 1981, B COASTAL OCEANOGRAP, V18, P67; Kremp A, 2003, MAR ECOL PROG SER, V263, P65, DOI 10.3354/meps263065; Liu Wen, 2014, Plankton & Benthos Research, V9, P156; Matsuoka K, 2018, MAR ENVIRON RES, V135, P123, DOI 10.1016/j.marenvres.2018.01.001; Mine H, 2016, 2016 JPN FISHERIES E, P47; Miyazono A, 2012, HARMFUL ALGAE, V16, P81, DOI 10.1016/j.hal.2012.02.001; Niiyama T, 2011, FISHERIES SCI, V77, P649, DOI 10.1007/s12562-011-0361-8; Ogata T., 2016, Nippon Suisan Gakkaishi, V82, P155, DOI 10.2331/suisan.WA2247-21; Okumura Y., 2022, 10 YEAR GREAT E JAPA, P53; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Persson A, 2008, MALACOLOGIA, V50, P341, DOI 10.4002/0076-2997-50.1-2.341; Persson A, 2023, REV FISH SCI AQUAC, DOI 10.1080/23308249.2023.2268715; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Persson A, 2009, AQUAT BIOL, V6, P227, DOI 10.3354/ab00129; Rhoads D.C., 1974, Oceanography mar Biol, V12, P263; Sakamoto K, 2007, FISHERIES SCI, V73, P675, DOI 10.1111/j.1444-2906.2007.01381.x; Shin HH, 2014, HARMFUL ALGAE, V37, P47, DOI 10.1016/j.hal.2014.05.005; Tsujino M, 2004, J EXP MAR BIOL ECOL, V303, P1, DOI 10.1016/j.jembe.2003.10.018; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; Tsujino Mutsumi, 2005, Benthos Research, V60, P45; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	27	0	0	4	4	SPRINGER JAPAN KK	TOKYO	SHIROYAMA TRUST TOWER 5F, 4-3-1 TORANOMON, MINATO-KU, TOKYO, 105-6005, JAPAN	0919-9268	1444-2906		FISHERIES SCI	Fish. Sci.	JAN	2025	91	1					157	164		10.1007/s12562-024-01829-3	http://dx.doi.org/10.1007/s12562-024-01829-3		OCT 2024	8	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	R7Y4I					2025-03-11	WOS:001340511700001
J	Blumenberg, M; Scheeder, G; Stoepke, FL; Pierau, R; Erbacher, J				Blumenberg, Martin; Scheeder, Georg; Stoepke, Fritz-Lukas; Pierau, Roberto; Erbacher, Jochen			Rapidly changing environmental conditions in a coastal setting during the Berriasian ("German Wealden", lower Cretaceous): evidence from biomarker and bulk geochemical data	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						Biomarkers; Berriasian; Buckeberg group; German Wealden; Dinosteranes; Dinoflagellates; KB-Rehburg 2 core; Lower Saxony Basin (LSB)	LOWER SAXONY BASIN; ORGANIC GEOCHEMISTRY; NORTHERN GERMANY; SOURCE ROCKS; SEDIMENTS; 2-METHYLHOPANOIDS; IDENTIFICATION; PETROGRAPHY; PATTERNS; FACIES	During the Middle to Late Berriasian (so called "German Wealden") a large lake system developed in the Lower Saxony Basin (LSB; in northwestern Germany) of which the eastern part is characterized by varying fluvial and lacustrine influences. The changeable situation through the earliest Cretaceous, particularly in the eastern LSB, is relatively understudied and a recently drilled well (KB-Rehburg 2; R-2) can help shedding light on these variations. R-2 covers the Berriasian ostracod zones Wealden 1 to 4 (Wd1 to Wd4), and palynomorphs presented in another study record stages with fluctuating predominantly terrigenous or aquatic organic matter. Short-term marine ingressions (MI) and more extensive transgressive events (TE) during that time interval have been reported, but some remained questionable. We here present novel organic geochemical data (including Rock-Eval and biomarkers) from R-2 showing a low maturity in terms of organic geochemical stress (Rock-Eval T-max similar to 435 to 445 degrees C) and bulk geochemical and biomarker data support the fluctuation in the sources of the predominating organic matter. In addition to the recently published marine influx events recorded in R-2, a significant decrease in pristane/phytane and increase in dinosterane index biomarker ratios demonstrate the previously unclear TE2 at the beginning of zone Wd4. While dinoflagellate cysts during that stage were reported to occur only sporadic, the dinoflagellate-specific dinosterane biomarker became highly abundant ["dinosterane/(regular steranes + dinosteranes)" ratio up to 0.15]. It demonstrates that dinoflagellates also flourished at R-2 during zone Wd4. This palynomorph/biomarker mismatch may be explained by the prevalence of non-cyst forming, or less likely, non-preservation of cells of dinoflagellates. Our data from R-2 also points at a likely widespread and general complication for palaeoreconstructions because we observed a slight lag between first records of palynomorphs used for TE and MI event identification compared to changing biomarker ratios and bulk organic geochemistry. We hypothesize that while the first likely demonstrate first occurrences of pioneer organisms, which mark events best, organic geochemical data appear to be more integrating and record changes only after establishment of a palaeoenvironment.	[Blumenberg, Martin; Scheeder, Georg] Fed Inst Geosci & Nat Resources BGR, Stilleweg 2, D-30655 Hannover, Germany; [Stoepke, Fritz-Lukas] Leibniz Univ Hannover, Inst Geol, Callin str 30, D-30167 Hannover, Germany; [Pierau, Roberto; Erbacher, Jochen] State Off Min Energy & Geol LBEG, Stilleweg 2, D-30655 Hannover, Germany	Leibniz University Hannover	Blumenberg, M (通讯作者)，Fed Inst Geosci & Nat Resources BGR, Stilleweg 2, D-30655 Hannover, Germany.	martin.blumenberg@bgr.de			Bundesanstalt fr Geowissenschaften und Rohstoffe (BGR) (4230) [PSP A-0104006]	Bundesanstalt fr Geowissenschaften und Rohstoffe (BGR) (4230)	We thank Petra Adam, Annelie Freiberg, Sabrina Koopmann, Yannick Meve, and Ina Sosnitza, for laboratory assistance. This is a contribution within the BGR project PSP A-0104006.A. We also thank Jolanta Kus, Ulrich Heimhofer and Christian Ostertag-Henning for discussion. Furthermore, we thank the associate editor, Armelle Riboulleau and one anonymous reviewer for their comments, which helped improving the manuscript.	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J. Earth Sci.	FEB	2025	114	1					99	111		10.1007/s00531-024-02470-2	http://dx.doi.org/10.1007/s00531-024-02470-2		OCT 2024	13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	U0V6L		hybrid			2025-03-11	WOS:001338099100001
J	Mudie, PJ; Aksu, AE; Hiscott, RN				Mudie, Petra J.; Aksu, Ali E.; Hiscott, Richard N.			Late Pleistocene-Holocene palynology and paleoceanography of I<SUP>•</SUP>mralı <SUP>•</SUP> mralı Basin, Marmara Sea: Pollen-spore, dinoflagellate cyst and other NPP zonations	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Paleoclimate; Paleoceanography; Last 30 cal ka; CONISS; Zonation	LATE QUATERNARY CORES; WESTERN BLACK-SEA; SURFACE SEDIMENTS; AEGEAN SEA; SPINIFERITES-CRUCIFORMIS; ENVIRONMENTAL-CHANGES; MEDITERRANEAN REGION; THECA RELATIONSHIP; GONYAULAX-BALTICA; SAPROPELIC LAYERS	The Marmara Sea is the oceanographic gateway that links the hypersaline Eastern Mediterranean Sea with the hyposaline Black Sea via Straits of Dardanelles and Bosphorus, respectively, and also occupies a transitional vegetation and climatic regime between the Mediterranean and Euxinic phytogeographic ecosystems. Recent palynological studies of long cores from the shallow I(center dot)mral & imath; (center dot) mral & imath; Basin perched on the southeastern slope of the Marmara Sea reveal that major paleoecological changes accompanied the isolation and reconnection of the Marmara Sea during the last two Pleistocene glacial-interglacial cycles. Here, we use data primarily from two I(center dot)mral & imath; (center dot) mral & imath; Basin cores to determine new quantitative zonations for the pollen-spore, dinoflagellate cyst (dinocyst) and other non-pollen palynomorph (NPP) assemblages in sediments representing the last 30 cal ka. A gap in one core is closed using data from three short gravity cores. Twenty-four radiocarbon ages and 20 correlation-ties for sapropel and ash layers from these five cores provide an essentially complete record for the past 30 cal ka. Use of a full suite of palynomorph data (pollen and spores, fungal spores, dinocysts and other phytoplankton, aquatic parasites/saprophytes, zoo-planktonic and zoo-benthic NPPs) shows for the first time that fluctuations in aquatic palynoassemblages during the glacial periods are more complex than simple salinity or temperature responses. The changes involve food web-level turnovers in trait- and size-based food web components in which potential parasites/saprophytes appear critically important. Pollen stratigraphies reveal a significant loss of Euxinic tree taxa by MIS 3c, with only partial recovery in MIS 1. The Euxinic forest elements are replaced by cultivars and other indicators of anthropogenic influences during the MIS 1 that is also marked by a dry interval and corresponding in part with the 4.2 cal ka Eastern Mediterranean Drought Event. The dinocyst zones for the last 30 cal ka show a clear turnover from assemblages dominated by brackish Ponto-Caspian taxa to marine assemblages at 11.7 cal ka. This phytoplanktonic signal lags slightly behind (a) the vegetation and shift in the other NPP commencing 13.2 cal ka, the initial marine incursion at 13.8 cal ka, and the arrival of coccolithophores at 13 cal ka. Comparison to published MIS 6 and 5 data reveals higher MIS 2-1 species diversity, reappearance of the MIS 6 marker Impagidinium inaequalis, and the emergences of Pyxidinopsis psilata f. quadrata, cf. Boreadinium breve, , and Peridinium spp. of Brenner 2005. The pre- reconnection microbiota is dominated by the unicellular alga Sigmopollis, , spikes of colonial Pediastrum algae, the saprophytes/parasites cf. Multiplicisphaeridium and Chytridiomycota. This microbiota is displaced by the post- reconnection assemblage dominated by Botryococcus coenobia, various Platyhelminth egg capsules and ostracod lining-types that persist through the Holocene. A distinctive transitional microbiota with Discocotyle-- type turbellarian egg capsules marks the B & oslash;lling-Aller & oslash;d & oslash; lling-Aller & oslash; d warming, followed at 13.3 ka by a marine assemblage with micro-foraminiferal linings and crustacean eggs. The interglacial marine phase of MIS 1 in I(center dot)mral & imath; (center dot) mral & imath; Basin has much higher dinocyst species diversity than MIS 5e, reflecting Neolithic impacts (agriculture, land clearance) and expanded shipping trade. Initial marine flooding in the Marmara Sea during both interglacials are marked by sapropel deposition but variations of ravinement surface erosion, and marine deep water residence time in a stratified Marmara Sea are potentially important factors underlying hypoxia/anoxia and sapropel deposition.	[Mudie, Petra J.] Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Aksu, Ali E.; Hiscott, Richard N.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland	Mudie, PJ (通讯作者)，Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada.	pmudie@nrcan.gc.ca; aaksu@mun.ca; rhiscott@mun.ca			Natural Sciences and Engineering Research Council of Canada; NSERC	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors thank Suzanne Leroy (LAMPEA, Aix-Marseilles University) , Andre Rochon (UQAR) and David Wall (WHOI, retired) for providing helpful information on dinoflagellate morphology. AEA and RNH acknowledge research and shiptime funding from the Natural Sciences and Engineering Research Council of Canada, NSERC, and thank the officers and crew of the RV Koca Piri Reis for their assistance during the 1995, 1997, 1998, 2002 and 2014 geophysical and coring operations. This project began with the MSc palynological study of Kathryn Roberts, who provided the first glimpse of the potential for a high-resolution investigation using Memorial University of Newfoundland cores.	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Palynology	DEC	2024	331								105179	10.1016/j.revpalbo.2024.105179	http://dx.doi.org/10.1016/j.revpalbo.2024.105179		OCT 2024	78	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	J7Q0Q					2025-03-11	WOS:001338959700001
J	Sorbino, CM; Castro-Parada, A; Cartelle, V; Martínez-Carreño, N; Delgado, C; Cazás, N; Lázaro, I; García-Gil, S				Sorbino, C. Munoz; Castro-Parada, A.; Cartelle, V.; Martinez-Carreno, N.; Delgado, C.; Cazas, N.; Lazaro, I.; Garcia-Gil, S.			Sediment recycling during the Holocene marine transgression in Ria de Vigo (NW Iberia): multiproxy evidence and environmental implications	QUATERNARY SCIENCE REVIEWS			English	Article						High system tract; Sea level; Postglacial; Coastal wetlands; Coastal hydrology; Pinewoods; Reworked pollen	LAST 3 MILLENNIA; SAN SIMON BAY; CIES ISLANDS; DINOFLAGELLATE CYST; REDEPOSITED POLLEN; SURFACE SEDIMENTS; NORTHWEST IBERIA; SW EUROPE; SEA; EVOLUTION	A new multiproxy study of a 155-cm sediment core located in Ria de Vigo (NW Iberia) recording the transgressive and highstand system tract of the Holocene sea-level rise is presented. New data described include grain size, geochemical analyses, high-resolution qualitative/quantitative analyses of pollen, non-pollen palynomorphs and dinoflagellate cysts content, the qualitative evaluation of diatoms at different key levels and the reconsideration of some seismic interpretations. Besides, 14 radiocarbon dates were obtained from shells and pollen extracts. This new evidence revealed that notable changes in the sedimentation rates and the relative abundance of the different types of palynomorphs occurred during the Holocene. The sediment core studied shows anomalous pollen successions, including unexpected Pinus pollen peaks, during the Early and Middle-Holocene. Differential dating revealed that those anomalous successions correspond to conspicuously aged sediment that has inverted pollen chronologies. Thus, these facies may constitute evidence of redeposition of ancient upland sediments, formed above the ancient coastline at different intervals comprised between the end of the Last Glacial Maximum and the early stages of the Lateglacial, which were rich in very resistant pollen types ( Pinus ). Dinoflagellate cyst records in combination with the non-reworked pollen evidence reveal a reliable climatic seesaw during the Holocene, includingwet stormy periods of prevailing mixed waters, with strong development of Lingulodinium and high accumulation rates in dinoflagellate cysts, which alternate with other sparsely stormy and drier phases, characterised by the coastal upwelling intensification, well-stratified waters, and increases in Bitectatodinium and Spiniferites spp. but low accumulation rates in dinoflagellate cysts. These climatic dynamics, including a millennial drier cool period that occurred just after the Thermal Optimum are consistent with previous evidence obtained in other limnetic systems in the Iberian Peninsula. Furthermore, there is a delay between the two phases with the highest marine contribution to sediment (ca. 11.0-8.2 and ca. 4.0-3.0 cal ka BP) and the subsequent warm stages when the relative sea level stabilises: the Thermal Optimum (8.0-6.0 ka BP) and the 2.50.5 ka BP interval, respectively. Changes in Pinus pollen concentrations and grain size recorded in the postglacial sediments suggest that some upland ancient (Lateglacial) pollen evidence might be remobilised, especially during stages of upwelling intensification, and then resedimented in the seabed. Further studies will be needed to determine if the significant differences existing between the Pinus pollen grain sizes respond to climatic variations affecting the region or have been the result of any replacement of pine species in the area. Nonetheless, Pinus pollen evidence almost disappeared with the first signs of anthropisation in the area, and only recovered after the modern repopulations. Our findings open up new possibilities to further our understanding of sediment reworking and recycling mechanisms through the integration of multiproxy studies encompassing pollen, seismic and sedimentary data.	[Sorbino, C. Munoz; Castro-Parada, A.; Cazas, N.; Lazaro, I.; Garcia-Gil, S.] Univ Vigo, Ctr Invest Marina, Vigo, Spain; [Sorbino, C. Munoz; Castro-Parada, A.; Cazas, N.] Univ Vigo, Dept Biol Vexetal & Ciencias Solo, Fac Ciencias, E-36210 Vigo, Spain; [Cartelle, V.] Flanders Marine Inst VLIZ, InnovOcean Campus,Jacobsenstr 1, B-8400 Oostende, Belgium; [Martinez-Carreno, N.] CSIC, Ctr Oceanog Vigo, Spanish Inst Oceanog IEO, Vigo 36390, Spain; [Delgado, C.] Univ Vigo, Dept Ecoloxia & Biol Anim, Fac Ciencias, E-36210 Vigo, Spain; [Lazaro, I.; Garcia-Gil, S.] Univ Vigo, Dept Xeociencias Marinas, Fac Ciencias, E-36210 Vigo, Spain	Universidade de Vigo; CIM UVIGO; Universidade de Vigo; Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); Universidade de Vigo; Universidade de Vigo	Sorbino, CM (通讯作者)，Univ Vigo, Ctr Invest Marina, Vigo, Spain.	bvcastor@uvigo.es	Cartelle Álvarez, Víctor/AFR-6659-2022; Munoz Sobrino, Castor/H-2948-2015	Cazas Fraga, Nerea/0000-0002-8854-9211; Cartelle, Victor/0000-0002-8894-7172; Munoz Sobrino, Castor/0000-0001-8191-3001	Spanish Ministry of Education and Science [CGL2012-33584]; ERDF funds) , Spanish Min-istry of Science Innovation and Universities [PID2023-147147OB-I00]; ERDF; Spanish Ministry of Science and Innovation the European NextGeneration EU Funds [TED2021-131141B-I00]; Xunta de Galicia GRC [2015/020, ED431C 2019/28]	Spanish Ministry of Education and Science(Spanish Government); ERDF funds) , Spanish Min-istry of Science Innovation and Universities; ERDF(European Union (EU)); Spanish Ministry of Science and Innovation the European NextGeneration EU Funds; Xunta de Galicia GRC	This work was funded by the Spanish Ministry of Education and Science CGL2012-33584 (co-financed with ERDF funds) , Spanish Min-istry of Science Innovation and Universities PID2023-147147OB-I00 (co-financed with ERDF funds) and Spanish Ministry of Science and Innovation the European NextGeneration EU Funds TED2021-131141B-I00; the Xunta de Galicia GRC 2015/020 and ED431C 2019/28 projects; and the Axudas Propias a Investigacio<acute accent>n <acute accent> n da Universidade de Vigo 2024.	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Sci. Rev.	NOV 15	2024	344								109006	10.1016/j.quascirev.2024.109006	http://dx.doi.org/10.1016/j.quascirev.2024.109006		OCT 2024	22	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	J7L7M		hybrid			2025-03-11	WOS:001338846800001
J	Vallejo, JD; de Gusmao, RB; Carvalho, MD; Fallgatter, C; Piovesan, EK				Vallejo, Juan David; de Gusmao, Regina Buarque; Carvalho, Marcelo de Araujo; Fallgatter, Claus; Piovesan, Enelise Katia			Sedimentary organic matter and paleoenvironmental reconstruction of the Santana Group (Lower Cretaceous), Araripe Basin, Northeast Brazil	CRETACEOUS RESEARCH			English	Article						Palynofacies; Late Aptian; Post-rift I sequence; Biozone	SEQUENCE STRATIGRAPHY; SOUTH ATLANTIC; SUCCESSION; BIOSTRATIGRAPHY; PALYNOFACIES; MEMBER	Depositional controls of the Santana Group in the Araripe Basin are still being debated. The main controversial subject is their marine influence and paleoenvironmental evolution. In this study, palynofacies analysis was performed on 59 samples from one core drilled at S & iacute;tio Romualdo in the Araripe Basin to investigate sedimentary organic matter. Three palynofacies associations (structureless, continental particles, and aquatic & thorn; opaque) were identified. The Santana Group consist of Barbalha, Crato, Ipubi and Romualdo formations. Based on palynofacies associations we conclude that the depositional setting of the Barbalha Formation reflects a fluvially-fed lacustrine system under oxic conditions. The Crato Formation, associated with tidal flats, coastal lakes, and lagoons within an open bay environment, represents a bayhead delta system. The Ipubi Formation corresponds to a coastal plain typical of sabkha paleoenvironments, characterized by low energy under reducing conditions, during drier climate conditions. The Romualdo Formation records mainly an estuarine paleoenvironment characterized by dysoxic to anoxic conditions. The presence of palynomorph groups typifies a late Aptian age for the Santana Group, which is based on the range of guide species marked mainly by the presence of Sergipea variverrucata biozone (P-270), as well as the occurrence of Complicatisaccus cearensis and Equisetosporites maculosus. The identification of marine palynomorphs (dinoflagellate cysts Subtilisphaera and foraminiferal test linings) are indicative of several, local marine incursions. (c) 2024 Elsevier Ltd. All rights are reserved, including those for text and data mining, AI training, and similar technologies.	[Vallejo, Juan David; de Gusmao, Regina Buarque; Fallgatter, Claus; Piovesan, Enelise Katia] Univ Fed Pernambuco, Dept Geol, Appl Micropaleontol Lab LAGESE LITPEG, Ave Arquitetura S-N, BR-50740540 Recife, PE, Brazil; [Vallejo, Juan David; de Gusmao, Regina Buarque; Fallgatter, Claus; Piovesan, Enelise Katia] Univ Fed Pernambuco, Technol & Geosci Ctr, Grad Program Geosci, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Carvalho, Marcelo de Araujo] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Plant Paleoecol Lab LAPAV, Natl Museum, Rio De Janeiro, RJ, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal do Rio de Janeiro	Vallejo, JD (通讯作者)，Univ Fed Pernambuco, Dept Geol, Appl Micropaleontol Lab LAGESE LITPEG, Ave Arquitetura S-N, BR-50740540 Recife, PE, Brazil.; Vallejo, JD (通讯作者)，Univ Fed Pernambuco, Technol & Geosci Ctr, Grad Program Geosci, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	juandavidv85@gmail.com	Piovesan, Enelise/Q-2953-2017	VALLEJO RAMIREZ, JUAN DAVID/0000-0002-2335-7008; PIOVESAN, ENELISE/0000-0002-0433-0395; Fallgatter, Claus/0009-0009-3051-3732; BUARQUE DE GUSMAO, REGINA/0009-0004-6784-7705				Appi, 1990, C BRAS GEOL NAT, V1, P211; Arai M, 2000, CRETACEOUS RES, V21, P351, DOI 10.1006/cres.2000.0211; Arai M., 2001, S BAC AR BAC INT NOR, P1; Arai M., 2009, Boletim de Geociencias da Petrobras, Rio de Janeiro, V2, P331; Arai M., 2006, GEOCIENCIAS, V25, P7; Arai M, 2020, CRETACEOUS RES, V116, DOI 10.1016/j.cretres.2020.104610; Arai M, 2014, BRAZ J GEOL, V44, P339, DOI 10.5327/Z2317-4889201400020012; Araripe RC, 2022, J S AM EARTH SCI, V116, DOI 10.1016/j.jsames.2022.103814; Araripe RC, 2021, CRETACEOUS RES, V122, DOI 10.1016/j.cretres.2021.104766; Asmus H., 1973, OCEAN BASIN MARGIN, P87, DOI [DOI 10.1007/978-1-4684-3030-1_3, 10.1007/978-1-4684-3030-1_3]; Assine M.L., 2007, B GEOCI NCIAS PETROB, V15, P371; Assine M.L., 1992, Revista Brasileira de Geociencias, V22, P289, DOI [10.25249/0375-7536.1992289300, DOI 10.25249/0375-7536.1992289300]; Batten D., 1996, Palynology: principles and applications, P1011; Beurlen G., 1987, Boletim de Geociencias da Petrobras, V1, P135; Bobco F.E.R., 2017, PESQUI GEOCIENC, V44, P431, DOI 10.22456/1807-9806.83267; Bom MHH, 2023, PALEOCEANOGR PALEOCL, V38, DOI 10.1029/2023PA004736; Brito Ignacio Machado, 1995, Anais da Academia Brasileira de Ciencias, V67, P493; Gonzalez LDC, 2020, INT J COAL GEOL, V225, DOI 10.1016/j.coal.2020.103482; Carvalho MD, 2022, SCI REP-UK, V12, DOI 10.1038/s41598-022-16580-x; 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; Carvalho MD, 2019, CRETACEOUS RES, V100, P172, DOI 10.1016/j.cretres.2019.03.021; Carvalho MD, 2017, PALAEOGEOGR PALAEOCL, V485, P543, DOI 10.1016/j.palaeo.2017.07.011; Chagas D.B., 2007, Geocie^ncias UNESP, V26, P313; Coimbra JC, 2002, GEOBIOS-LYON, V35, P687; Coimbra JC, 2021, REV BRAS PALEONTOLOG, V24, P37, DOI 10.4072/rbp.2021.1.03; COOPER MR, 1977, PALAEOGEOGR PALAEOCL, V22, P1, DOI 10.1016/0031-0182(77)90032-3; Custódio MA, 2017, SEDIMENT GEOL, V359, P1, DOI 10.1016/j.sedgeo.2017.07.010; Dino R., 1992, PhD thesis, P300; DINO R., 1994, Boletim de Geociencias da Petrobras, V8, P257; Scherer CM, 2014, J S AM EARTH SCI, V49, P106, DOI 10.1016/j.jsames.2013.10.007; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; Fabin CE, 2018, AN ACAD BRAS CIENC, V90, P2049, DOI 10.1590/0001-3765201820170526; Fambrini G.L., 2020, GEOL USP SER CIENT, V20, P169, DOI DOI 10.11606/issn.2316-9095.v20-163467; Fambrini G.L., 2019, GEOL SOC SPEC PUBL, V488, P119, DOI [10.1144/SP488-2017-275, DOI 10.1144/SP488-2017-275, 10.1144/SP488-2017-275,488(1., DOI 10.1144/SP488-2017-275,488(1]; Fambrini G.L., 2011, Geologia USP. 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FEB	2025	166								106016	10.1016/j.cretres.2024.106016	http://dx.doi.org/10.1016/j.cretres.2024.106016		OCT 2024	12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	J4G4S					2025-03-11	WOS:001336663400001
J	Monedero-Contreras, RD; Martínez-Ruiz, F; Rodríguez-Tovar, FJ; Mesa-Fernandez, JM; Sangiorgi, F				Monedero-Contreras, Ricardo D.; Martinez-Ruiz, Francisca; Rodriguez-Tovar, Francisco J.; Mesa-Fernandez, Jose M.; Sangiorgi, Francesca			Tracking orbital and suborbital climate variability in the westernmost Mediterranean over the past 13,000 years: New insights from paleoperspectives on marine productivity responses	QUATERNARY SCIENCE REVIEWS			English	Article						Paleoproductivity; Dinoflagellates; Mediterranean sea; Barite; Marine geochemistry	NORTH-ATLANTIC OSCILLATION; SEA-SURFACE TEMPERATURE; LAST GLACIAL MAXIMUM; WALLED DINOFLAGELLATE CYSTS; EASTERN ALBORAN-SEA; PARTICLE FLUXES; SEDIMENTARY RECORD; SIERRA-NEVADA; LATE HOLOCENE; DEEP-SEA	This study presents a comprehensive analysis of a sediment record from the Western Alboran Basin (core GP04PC), utilizing palynological and geochemical tools to investigate marine productivity responses to orbital and suborbital climate variability over the past 13,000 years. High productivity during the Younger Dryas humid phase (similar to 12.4-11.7 ka) and the Holocene humidity optimum (similar to 10.5-8.5 ka) was driven by increased local river discharges resulting from rapid mountain glaciers melting and enhanced regional precipitation. During the late Holocene, frequent flood events linked to negative North Atlantic Oscillation (NAO) incursions potentially led to multicentennial-scale productivity increases. The findings indicate that periods characterized by wet regional conditions and increased river run-off, influenced by orbital (e.g., insolation cycles) and suborbital factors (e.g., NAO and Atlantic Meridional Overturning Circulation changes), consistently enhanced marine productivity in the Western Alboran Basin. The study also reveals that the current high productivity and carbon export in the Western Alboran Basin are maintained by active upwelling and downwelling systems driven by a persistent positive NAO phase following the southward migration of the Intertropical Convergence Zone (ITCZ) that occurred around 6.5 ka. Furthermore, geochemical proxies support a strong detrital influence on trace metal concentrations, including barium (Ba), in deep Western Alboran sediments during the Holocene. This limits the use of Ba/Al ratios for accurately reconstructing productivity changes and highlights the importance of dinocyst analysis as a complementary tool for robust marine productivity reconstructions in this region. These observations provide valuable paleoperspectives on marine ecosystem responses to climate variability, contributing to the development of robust long-term productivity models essential for adapting to ongoing environmental changes in the region, and demonstrating the strong influence of North Atlantic climate and ocean dynamics on centennial-scale productivity oscillations in this region.	[Monedero-Contreras, Ricardo D.; Martinez-Ruiz, Francisca] CSIC, Inst Andaluz Ciencias Tierra, Armilla, Spain; [Rodriguez-Tovar, Francisco J.; Mesa-Fernandez, Jose M.] Univ Granada, Dept Estratig & Paleontol, Granada, Spain; [Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); University of Granada; Utrecht University	Monedero-Contreras, RD (通讯作者)，CSIC, Inst Andaluz Ciencias Tierra, Armilla, Spain.	ricardo.monedero@csic.es	Monedero-Contreras, Ricardo/ADL-8874-2022; Rodríguez-Tovar, Francisco/AAA-9041-2020; Martinez-Ruiz, Francisca/C-5908-2014	Monedero Contreras, Ricardo David/0000-0003-3921-4631; Martinez-Ruiz, Francisca/0000-0002-8301-4453; Rodriguez-Tovar, Francisco/0000-0002-1400-2715	MCIN/AEI [PID2019-104624RB-I00, PID2019-104625RB-100, TED2021-131697B-C22]; Grants FEDER/Junta de Andalucia [P18-RT-3804, P18-RT- 4074]; Junta de Andalucia [RNM-179, RNM-178]	MCIN/AEI; Grants FEDER/Junta de Andalucia; Junta de Andalucia(Junta de Andalucia)	This study has been funded by Grants PID2019-104624RB-I00, PID2019-104625RB-100, and TED2021-131697B-C22 funded by MCIN/AEI/10.13039/501100011033, Grants FEDER/Junta de Andalucia P18-RT-3804 and P18-RT- 4074, and by Research Groups RNM-179 and RNM-178 funded by the Junta de Andalucia. We thank the GeoLab staff from Utrecht University, more precisely the Organic Geochemistry Lab, Stable Isotope Lab and Palynology Lab, for their valuable contributions to organic matter analyses and their assistance in preparing palynomorph slides. We are also grateful to the Center for Scientific Instrumentation (CIC, University of Granada) and the XRF Unit of the Instituto Andaluz de Ciencias de la Tierra (CSIC) for ICP and XRF analyses, respectively. Lastly, we thank editor Dr. Antje Voelker and the two anonymous reviewers for their insightful feedback, which has significantly improved the quality of this study.	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J	Rodríguez-Villegas, C; Pérez-Santos, I; Díaz, PA; Baldrich, AM; Lee, MR; Saldías, GS; Mancilla-Gutiérrez, G; Urrutia, C; Navarro, CR; Varela, DA; Ross, L; Figueroa, RI				Rodriguez-Villegas, Camilo; Perez-Santos, Ivan; Diaz, Patricio A.; Baldrich, angela M.; Lee, Matthew R.; Saldias, Gonzalo S.; Mancilla-Gutierrez, Guido; Urrutia, Cynthia; Navarro, Claudio R.; Varela, Daniel A.; Ross, Lauren; Figueroa, Rosa I.			Deep Turbulence as a Novel Main Driver for Multi-Specific Toxic Algal Blooms: The Case of an Anoxic and Heavy Metal-Polluted Submarine Canyon That Harbors Toxic Dinoflagellate Resting Cysts	MICROORGANISMS			English	Article						microalgae toxins; submarine canyon; sediment anoxia; dinoflagellate resting cyst; encystment; excystment process	ALEXANDRIUM-CATENELLA DINOPHYCEAE; HUMBOLDT CURRENT; ABUNDANCE; OXYGEN; ENCYSTMENT; DYNAMICS; HISTORY; FUTURE; MODEL; OCEAN	Over the recent decades, an apparent worldwide rise in Harmful Algae Blooms (HABs) has been observed due to the growing exploitation of the coastal environment, the exponential growth of monitoring programs, and growing global maritime transport. HAB species like Alexandrium catenella-responsible for paralytic shellfish poisoning (PSP)-Protoceratium reticulatum, and Lingulaulax polyedra (yessotoxin producers) are a major public concern due to their negative socioeconomic impacts. The significant northward geographical expansion of A. catenella into more oceanic-influenced waters from the fjords where it is usually observed needs to be studied. Currently, their northern boundary reaches the 36 degrees S in the Biobio region where sparse vegetative cells were recently observed in the water column. Here, we describe the environment of the Biobio submarine canyon using sediment and water column variables and propose how toxic resting cyst abundance and excystment are coupled with deep-water turbulence (10-7 Watt/kg) and intense diapycnal eddy diffusivity (10-4 m2 s-1) processes, which could trigger a mono or multi-specific harmful event. The presence of resting cysts may not constitute an imminent risk, with these resting cysts being subject to resuspension processes, but may represent a potent indicator of the adaptation of HAB species to new environments like the anoxic Biobio canyon.	[Rodriguez-Villegas, Camilo; Perez-Santos, Ivan; Diaz, Patricio A.; Baldrich, angela M.; Lee, Matthew R.; Mancilla-Gutierrez, Guido; Varela, Daniel A.] Univ Lagos, Ctr imar, Casilla 557, Puerto Montt 5480000, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Baldrich, angela M.] Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt 5480000, Chile; [Perez-Santos, Ivan; Saldias, Gonzalo S.] Univ Concepcion, Ctr Invest Oceanograf COPAS COASTAL, Concepcion 4070386, Chile; [Perez-Santos, Ivan] Ctr Invest Ecosistemas Patagonia CIEP, Coyhaique 5950000, Chile; [Saldias, Gonzalo S.] Univ Bio Bio, Fac Ciencias, Dept Fis, Coyhaique 4081112, Chile; [Urrutia, Cynthia; Navarro, Claudio R.] Univ Los Lagos, Dept Recursos Nat & Medio Ambiente, Chinquihue Km 6, Puerto Montt 5480000, Chile; [Urrutia, Cynthia] Univ La Frontera, Sci & Technol Bioresource Nucleus BIOREN, Ave Francisco Salazar 01145, Temuco 4811230, Chile; [Ross, Lauren] Univ Maine, Dept Civil & Environm Engn, Orono, ME 04469 USA; [Figueroa, Rosa I.] CSIC, Inst Espanol Oceanog IEO, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain	Universidad de Los Lagos; Universidad de Los Lagos; Universidad de Concepcion; Universidad del Bio-Bio; Universidad de Los Lagos; Universidad de La Frontera; University of Maine System; University of Maine Orono; Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC)	Rodríguez-Villegas, C (通讯作者)，Univ Lagos, Ctr imar, Casilla 557, Puerto Montt 5480000, Chile.; Rodríguez-Villegas, C (通讯作者)，Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt 5480000, Chile.; Figueroa, RI (通讯作者)，CSIC, Inst Espanol Oceanog IEO, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain.	camilo.rodriguez@ulagos.cl; ivan.perez@ulagos.cl; patricio.diaz@ulagos.cl; angela.baldrich@ulagos.cl; matthew.lee@ulagos.cl; gsaldias@ubiobio.cl; guido.mancilla@ulagos.cl; cynthia.urrutia@ulagos.cl; claudio.navarro@ulagos.cl; daniel.varela@ulagos.cl; lauren.ross1@maine.edu; rosa.figueroa@ieo.csic.es	Varela, Daniel/D-9484-2013; Perez, Ivan/B-9321-2018; Saldias, Gonzalo/C-3577-2016; Diaz, Patricio/B-8128-2018; Varela, Daniel/D-7908-2013; Baldrich, Angela M./AAC-8054-2022; Lee, Matthew/B-6360-2008; Rodriguez Villegas, Camilo/AAB-8563-2022; Figueroa, Rosa/M-7598-2015	Saldias, Gonzalo/0000-0003-3462-464X; Diaz, Patricio/0000-0002-9403-8151; Varela, Daniel/0000-0003-4603-4970; Baldrich, Angela M./0000-0002-2624-7357; Lee, Matthew/0000-0001-9675-9908; Rodriguez Villegas, Camilo/0000-0002-1429-2775; Navarro Oyarzo, Claudio Rene/0009-0002-0417-8992; Ross, Lauren/0000-0001-8542-2875; Urrutia Molina, Cynthia/0009-0006-3729-4825; Figueroa, Rosa/0000-0001-9944-7993	ANID AUB2200011 [AUB2200011]; ANID [3240110]; FONDECYT Posdoctorado (ANID) [ANID-PIA FB0001]; Centre of Biotechnology and Bioengineering (CeBiB) [COASTAL ANID FB210021, CIEP R20F00, FONDECYT 1211037]; Universidad de Los Lagos - COPAS [FB210021, FONDECYT 1220167]; COPAS Coastal ANID; Fulbright U.S. Scholar grant	ANID AUB2200011; ANID; FONDECYT Posdoctorado (ANID); Centre of Biotechnology and Bioengineering (CeBiB); Universidad de Los Lagos - COPAS; COPAS Coastal ANID; Fulbright U.S. Scholar grant	This work was funded by ANID AUB2200011. C.R.-V. was funded by FONDECYT Posdoctorado (ANID, 3240110) and by the Centre of Biotechnology and Bioengineering (CeBiB ANID-PIA FB0001), Universidad de Los Lagos. I.P.-S. was funded by COPAS COASTAL ANID FB210021, CIEP R20F00, and FONDECYT 1211037. G.S. has been partially funded by COPAS Coastal ANID FB210021 and FONDECYT 1220167. L.R. received a Fulbright U.S. Scholar grant during the research that led to this publication.	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J	Aboutofail, S; Slimani, H				Aboutofail, Salma; Slimani, Hamid			The Paleocene-Eocene Thermal Maximum (PETM) interval in the southwestern Mediterranean Tethys at Morocco: New data from a high-resolution study of dinoflagellate cysts and palynofacies in the Rif Chain	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paleocene-Eocene transition; Sekada section; Palynostratigraphy; Palynofacies; Paleoenvironnements; Paleoclimate; PETM	CRETACEOUS-PALEOGENE BOUNDARY; WESTERN EXTERNAL RIF; DOMAIN EASTERN CARPATHIANS; SEA-SURFACE TEMPERATURE; OULED HADDOU; TERTIARY BOUNDARY; CALCAREOUS NANNOFOSSIL; SEQUENCE STRATIGRAPHY; ORGANIC-MATTER; EL-KEF	Palynological research, carried out in the Paleocene-Eocene transition of the Sekada section, Tangier Unit (western External Rif, northwestern Morocco), revealed the presence of a palynological content composed essentially of dinoflagellate cysts (dinocysts), phytoclasts and amorphous organic matter (AOM). Their qualitative and quantitative analyses allowed a detailed biostratigraphic interpretation, a reconstruction of the paleoenvironment and paleoclimate and identification of the Paleocene-Eocene Thermal Maximum (PETM) interval in the Sekada section. Thanetian and Ypresian ages, previously assigned respectively to the grey-brown marls and the marly limestones in the studied section are here revised based on several marker dinocyst events. Acmes of the subtropical dinocyst Apectodinium spp. (in particular, Apectodinium homomorphum), recorded along the analyzed interval, represent a response to the global warming of the PETM, and therefore support the assignment of this interval to the Paleocene-Eocene transition. Quantitative analyses of the main constituents of kerogen (dinocysts, phtoclasts, AOM) and selected dinocyst groups, which are previously considered in the literature as environmental markers, generally suggest a proximal (coastal eutrophic) depositional environment. Furthermore, quantitative fluctuations in the heterotrophic dinocyst Apectodinium and open marine autotrophic dinocysts versus total dinocysts, and in phytoclasts, AOM and palynomorphs versus total kerogen appear to be controlled by fluctuations in terrestrial inputs, which are most likely related to climate changes.	[Aboutofail, Salma; Slimani, Hamid] Mohammed V Univ Rabat, Sci Inst, Res Ctr GEOPAC, Geophys Nat Patrimony & Green Chem,Geobiodivers &, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco	Mohammed V University in Rabat	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Sci Inst, Res Ctr GEOPAC, Geophys Nat Patrimony & Green Chem,Geobiodivers &, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	hamid.slimani@is.um5.ac.ma	Slimani, Hamid/AAL-4055-2020					AFNOR, 1996, Determination of the Carbonate Content-Calcimeter Method, P94; [Anonymous], 1988, Geol. 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J	Baraboshkin, EY; Arkadiev, VV; Guzhikov, AY; Savelieva, YN; Shurekova, OV; Platonov, ES; Ustinova, MA				Baraboshkin, E. Yu; Arkadiev, V. V.; Guzhikov, A. Yu.; Savelieva, Yu. N.; Shurekova, O. V.; Platonov, E. S.; Ustinova, M. A.			Developments in the Cretaceous Stratigraphy of Crimea. Part 1. Introduction and the Lower Cretaceous	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Early Cretaceous; ammonites; organic-walled dinoflagellate cysts; ostracods; nannoplankton; calpionellids; magnetostratigraphy	JURASSIC/CRETACEOUS BOUNDARY; CALCAREOUS NANNOFOSSILS; THEODOSIA AREA; BIOSTRATIGRAPHY; SOUTHWESTERN; MAGNETOSTRATIGRAPHY; SEDIMENTS; GENUS; OSTRACODS; DEPOSITS	This paper summarizes the state of knowledge of the Cretaceous stratigraphy of the Mountainous Crimea and selected biostratigraphic groups and magnetostratigraphy. The first part of the paper discusses the Early Cretaceous, its stratigraphy, selected fossil groups and magnetostratigraphy of the Mountainous Crimea. The data on the figured reference sections were updated in terms of biostratigraphic zonation. Selected fossil groups represented in the paper include ammonites, organic-walled dinoflagellate cysts, ostracods, calpionellids and nannoplankton. The description of each group contains an information on the main publications, types of biostratigraphic units and their distribution, fossil assemplages, images of the most important fossils, and brief discussion on the correlation. Some of the ammonite index fossils are figured for the first time. The magnetostratigraphy summarizes latest data published mostly in Russian for the whole Early Cretaceous succession of the Mountainous Crimea.	[Baraboshkin, E. Yu] Moscow MV Lomonosov State Univ, Geol Fac, Moscow 119234, Russia; [Arkadiev, V. V.] St Petersburg State Univ, Inst Earth Sci, St Petersburg 199034, Russia; [Guzhikov, A. Yu.] Saratov NG Chernyshevskii State Univ, Geol Fac, Saratov 410012, Russia; [Savelieva, Yu. N.] All Russian Res Geol Oil Inst, Aprelevka Branch, Aprelevka Town 143360, Moskow Region, Russia; [Shurekova, O. V.] Russian Geol Res Inst, Dept Stratig & Paleontol, St Petersburg 199106, Russia; [Platonov, E. S.] All Russian Res Geol Oil Inst, St Petersburg Branch, St Petersburg 192019, Russia; [Baraboshkin, E. Yu; Ustinova, M. A.] Russian Acad Sci, Geol Inst, Dept Stratig, Moscow 119017, Russia	Lomonosov Moscow State University; Saint Petersburg State University; Saratov State University; A.P. Karpinsky Russian Geological Research Institute (VSEGEI); Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Baraboshkin, EY (通讯作者)，Moscow MV Lomonosov State Univ, Geol Fac, Moscow 119234, Russia.; Baraboshkin, EY (通讯作者)，Russian Acad Sci, Geol Inst, Dept Stratig, Moscow 119017, Russia.	EJBaraboshkin@mail.ru			Russian Science Foundation [22-17-00091]	Russian Science Foundation(Russian Science Foundation (RSF))	The study was supported by the Russian Science Foundation Grant No. 22-17-00091, https://rscf.ru/project/22-17-00091/.	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J	Sousa, R; Laizé, V; Lourenco-Marques, C; Barata, M; Pousao-Ferreira, P; Soares, F				Sousa, Rui; Laize, Vincent; Lourenco-Marques, Catia; Barata, Marisa; Pousao-Ferreira, Pedro; Soares, Florbela			Inactivation in vitro of the marine parasite Amyloodinium ocellatum	DISEASES OF AQUATIC ORGANISMS			English	Article						Aquaculture; Fish parasite; Amyloodiniosis; Treatment; Prevention	MILKFISH CHANOS-CHANOS; SPOTTED SEA-TROUT; RED SNAPPER; SAPROLEGNIA-PARASITICA; DICENTRARCHUS-LABRAX; CYNOSCION-NEBULOSUS; BROWN 1931; TOXICITY; FISH; DINOFLAGELLIDA	The ectoparasite Amyloodinium ocellatum is a dinoflagellate that causes severe morbidity and mortality in both brackish and marine warmwater aquaculture fishes worldwide. A. ocellatum has a triphasic life cycle based on a free-living flagellate (the dinospore), a parasitic stage (the trophont) and a resting and reproductive cyst (the tomont). Current chemical treatments have shown some efficacy in eliminating dinospores but fail to inactivate the tomonts. Here we evaluated the efficacy of alternative treatments in vitro through sporulation tests and the quantification of dinospore production and motility. Hydrogen peroxide and peracetic acid efficiently decreased dinospore production at low concentrations, but total inactivation of tomonts was only achieved with higher dosages. Tomont inactivation was also observed with disinfectants such as sodium hypochlorite and Virkon S. This work provides insights into effective and environmentally friendly alternatives for the elimination of resistant forms of the marine parasite A. ocellatum.	[Sousa, Rui; Laize, Vincent; Lourenco-Marques, Catia; Pousao-Ferreira, Pedro; Soares, Florbela] Assoc Sustainable & Smart Aquaculture, S2AQUA Collaborat Lab, Ave Parque Nat Ria Formosa S-N, P-8700194 Olhao, Portugal; [Laize, Vincent] Univ Algarve, CCMAR Ctr Marine Sci, Campus Gambelas, P-8005139 Faro, Portugal; [Lourenco-Marques, Catia; Barata, Marisa; Pousao-Ferreira, Pedro; Soares, Florbela] IPMA Portuguese Inst Ocean & Atmosphere, EPPO Aquaculture Res Stn, Ave Parque Nat Ria Formosa S-N, P-8700194 Olhao, Portugal	Universidade do Algarve; Instituto Portugues do Mar e da Atmosfera	Soares, F (通讯作者)，Assoc Sustainable & Smart Aquaculture, S2AQUA Collaborat Lab, Ave Parque Nat Ria Formosa S-N, P-8700194 Olhao, Portugal.; Soares, F (通讯作者)，IPMA Portuguese Inst Ocean & Atmosphere, EPPO Aquaculture Res Stn, Ave Parque Nat Ria Formosa S-N, P-8700194 Olhao, Portugal.	fsoares@ipma.pt	Soares, Florbela/K-1184-2012; Pousão-Ferreira, Pedro/H-3689-2014; Lourenco Marques, Catia/E-5037-2013	Lourenco Marques, Catia/0000-0003-0093-747X; Barata, Marisa/0000-0001-6965-0958; Couto de Sousa, Rui Manuel/0000-0002-7683-3821	Project SAUDEAQUA [MAR-0205.01-FEAPMP-0009]; Project AQUA-RAS4 [MAR-02.01.02-FEAMP-0223]	Project SAUDEAQUA; Project AQUA-RAS4	This research was supported by projects SAUDE&AQUA (MAR-0205.01-FEAPMP-0009) and AQUA-RAS (MAR-02.01.02-FEAMP-0223). 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J	Penaud, A; Fersi, W; Toucanne, S; Goñi, MFS; Rossignol, L; Naughton, F; Wary, M; Eynaud, F				Penaud, Aurelie; Fersi, Wiem; Toucanne, Samuel; Goni, Maria Fernanda Sanchez; Rossignol, Linda; Naughton, Filipa; Wary, Melanie; Eynaud, Frederique			Environmental changes in the Fleuve Manche paleoriver drainage system (Western Europe) linked to North Atlantic sub-millennial climate variability across Heinrich Stadial 1: Palynological evidence from the Bay of Biscay	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Heinrich Stadial 1; Northern Bay of Biscay; Paleoriver runoff-discharge; Pollen and dinocysts; Land-sea approach	LAST GLACIAL MAXIMUM; ICE-SHEET; DINOFLAGELLATE CYSTS; VEGETATION; DEGLACIATION; IMPACTS; HISTORY; EVENTS; RIVERS; TERMINOLOGY	Marine microfossils (dinoflagellate cysts and planktonic foraminifera) and geochemical (XRF-Ti/Ca)-based matic records from a core (MD13-3438) located off the Fleuve Manche (FM) paleo-mouth have revealed sustained warm summer sea surface temperatures (SSTs) during sub-millennial climate changes within (similar to 18-14.7 ka) may have played a key role in the FM regime related to the European Ice Sheet (EIS) melting In this study, we have analyzed the MD13-3438 pollen content over the HS1 at a mean resolution of similar to 50 years test whether vegetation-based air temperatures were coupled to SSTs face to this rapid climate variability. our results highlight two major phases of pollen sources at site MD13-3438, preventing the pollen record interpreted as a continuous record of the evolution of vegetation and climate occupying a single watershed HS1. The first phase, i.e. the HS1-a interval (similar to 18-16.8 ka), is marked by strong occurrences of boreal pollen (especially Picea-Abies). Considering their spatial distribution and the coalescence of the British and Scandinavian ice sheets into the North Sea during the Last Glacial Maximum, these taxa probably originated from North European Plain, i.e., eastern FM tributaries (east of the Rhine River), where cool-humid conditions generally prevailed. Then, the second phase, i.e. the HS1-b interval (similar to 16.8-14.7 ka BP), is characterized deceleration of the EIS retreat and the drop of boreal pollen values at site MD13-3438 further signing influence of the upstream FM drainage system and thus a better characterization of pollen sources related western FM tributaries. Superimposed to these two HS1 main phases, pollen fluctuations are concomitant sub-millennial variability in the EIS deglaciation intensity. During the early HS1 (HS1-a), we discuss two short-term increases in the ratio between deciduous trees (Quercus-Corylus-Alnus) and herbaceous plants (Plantago-Amaranthaceae-Artemisia). These events are coeval with phases of increasing dinocyst-based SST seasonality through summer SST amplification). We associate these events with lower contribution of the upstream catchment as well as, possibly, atmospheric warming and regional sea-level positive oscillations. The HS1-b composed of three main phases that appear more influenced by the downstream FM drainage system. HS1-b1 (16.8-16.3 ka BP) corresponds to the driest and coldest conditions west of the Rhine River. HS1-b2 (16.3-15.5 ka BP) is coeval with large arrivals of iceberg from the Hudson strait in the Bay of Biscay and likely to a major sea-level positive oscillation associated with a phase of FM valley reworking. HS1-b3 (15.5-14.7 ka BP) corresponds to persistent arid conditions that preceded the subsequent more humid tions recorded from 14.7 ka BP at the start of the Bolling-Allerod.	[Penaud, Aurelie; Fersi, Wiem; Toucanne, Samuel] Univ Brest, CNRS, Geoocean, UMR6538,Ifremer, F-29280 Plouzane, France; [Goni, Maria Fernanda Sanchez; Rossignol, Linda; Wary, Melanie; Eynaud, Frederique] Univ Bordeaux, CNRS, Environm & Paleoenvironnements Ocean & Continentau, UMR 5805, F-33615 Pessac, France; [Goni, Maria Fernanda Sanchez] PSL, Ecole Prat Hautes Etud EPHE, F-75014 Paris, France; [Naughton, Filipa] Portuguese Inst Sea & Atmosphere IPMA, Rua Alfredo Magalhaes Ramalho 6, P-1495006 Lisbon, Portugal; [Naughton, Filipa] Algarve Univ, Ctr Marine Sci CCMAR, Campus Gambelas, P-8005139 Faro, Portugal	Ifremer; Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Instituto Portugues do Mar e da Atmosfera; Universidade do Algarve	Penaud, A (通讯作者)，Univ Brest, CNRS, Geoocean, UMR6538,Ifremer, F-29280 Plouzane, France.	aurelie.penaud@univ-brest.fr	Naughton, Filipa/AAA-1589-2019; Wary, Mélanie/S-1121-2018; Toucanne, Samuel/H-3437-2011; Sanchez Goñi, Maria Fernanda/R-3699-2019	Toucanne, Samuel/0000-0002-4858-8953	EPOC oratory (Bordeaux University); LOCEAN (Paris); EPOC laboratories; ISblue project, Interdisciplinary graduate school for the blue planet [ANR-17-EURE-0015]; French government under program "Investissements d'Avenir" [PTDC/CTA-CLI/4297/2021]	EPOC oratory (Bordeaux University); LOCEAN (Paris); EPOC laboratories; ISblue project, Interdisciplinary graduate school for the blue planet; French government under program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR))	This work was supported by the French projects: ANR IDEGLACE, INSU RISCC, INSU ICE-BIO-RAM and ERC ACCLIMATE. This project includes regional, national and international collaborations, between Geo-Ocean laboratory (Brest University, Ifremer, Plouzane), EPOC laboratory (Bordeaux University, Pessac) and LOCEAN (Paris). We received funding from the CG29 ( Conseil General du Finistere, 29) and financial support from Geo-Ocean and EPOC laboratories. We thank Muriel Georget (EPOC; Bordeaux University) for the helpful support for laboratory assistance. This work was supported by the ISblue project, Interdisciplinary graduate school for the blue planet (ANR-17-EURE- 0015), co-funded by a grant from the French government under the program "Investissements d'Avenir" as well as the project Hydroshifts (PTDC/CTA-CLI/4297/2021).	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Paleoclimatol. Paleoecol.	DEC 1	2024	655								112512	10.1016/j.palaeo.2024.112512	http://dx.doi.org/10.1016/j.palaeo.2024.112512		SEP 2024	14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	H1V8G					2025-03-11	WOS:001321393000001
J	Gu, HF; Tian, QR; Mertens, KN; Derrien, A; Chomérat, N; Wang, N; He, HS; Uttayarnmanee, P				Gu, Haifeng; Tian, Qirui; Mertens, Kenneth Neil; Derrien, Amelie; Chomerat, Nicolas; Wang, Na; He, Haisong; Uttayarnmanee, Praderm			Biodiversity study of the genus <i>Bysmatrum</i> from the South China Sea and France reveals a new benthic dinoflagellate, <i>Bysmatrum ingrilense sp. nov</i>. (Peridiniales, Dinophyceae)	PHYCOLOGIA			English	Article						Biogeography; Bysmatrum granulosum; Bysmatrum subsalsum; Cysts; Peridinium sociale	RDNA-BASED PHYLOGENY; SUBSALSUM DINOPHYCEAE; 1ST REPORT; ULTRASTRUCTURE; MORPHOLOGY	The dinoflagellate genus Bysmatrum is an unusual member of the Peridiniales and cannot be attributed to any known family. Bysmatrum differs from typical peridinialean genera in that the second and third anterior intercalary plates are separated and both antapical plates are asymmetrical. Currently, Bysmatrum encompasses six epibenthic or tide-pool species, but information on their genetic diversity and biogeography remains limited. In the present study, we obtained five strains of Bysmatrum from the South China Sea by isolating single cells and three strains from Ingril, a French Mediterranean lagoon by incubating sediments. Strains from Ingril Lagoon displayed the plate formula Po, cp, X, 4 ', 3a, 7 '', 6C, 4S, 5 ''', 2 ''''. They also exhibited an elongated nucleus in the hypocone and a type B eyespot. Smooth and spherical cysts were produced in culture. Small and/or partially large subunit ribosomal DNA sequences were obtained for all eight strains. Molecular phylogeny was inferred using these concatenated sequences through maximum likelihood and Bayesian inference methods. Bysmatrum granulosum and B. subsalsum were identified from Thailand and China for the first time, each of them comprising of two ribotypes. Bysmatrum ingrilense sp. nov. was monophyletic and closest to B. subsalsum ribotype B. Pinnatoxin and related toxins were examined in two strains of Bysmatrum ingrilense by LC-MS/MS, but none were detected. Our results highlight that the diversity of Bysmatrum might be underestimated.	[Gu, Haifeng; Tian, Qirui] Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China; [Gu, Haifeng; Tian, Qirui; Wang, Na; He, Haisong] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Mertens, Kenneth Neil; Derrien, Amelie; Chomerat, Nicolas] LITTORAL, Ifremer, F-29900 Concarneau, France; [Uttayarnmanee, Praderm] Marine & Coastal Resources Res & Dev Ctr, Dept Marine & Coastal Resources, Cent Gulf Thailand, Chumphon 86000, Thailand	Nanjing University of Information Science & Technology; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources; Ifremer	Gu, HF (通讯作者)，Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China.; Gu, HF (通讯作者)，Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Chomerat, Nicolas/0000-0001-9691-6344; Mertens, Kenneth/0000-0003-2005-9483; Derrien, Amelie/0000-0001-9656-7850	National Natural Science Foundation of China [42030404, 42076085]; China's Asian Cooperation Fund Project "Development of Indonesia-China Center for Ocean Climate"; China-ASEAN Maritime Cooperation Fund; French National Research Agency (ANR) PhenoMap project [ANR-20-CE02-0025]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); China's Asian Cooperation Fund Project "Development of Indonesia-China Center for Ocean Climate"; China-ASEAN Maritime Cooperation Fund; French National Research Agency (ANR) PhenoMap project(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco)	This work was supported by the National Natural Science Foundation of China [42030404, 42076085], China's Asian Cooperation Fund Project "Development of Indonesia-China Center for Ocean & Climate" and China-ASEAN Maritime Cooperation Fund. KNM, NC and AD were financially supported by the French National Research Agency (ANR) PhenoMap project, ANR-20-CE02-0025.	Adl SM, 2005, J EUKARYOT MICROBIOL, V52, P399, DOI 10.1111/j.1550-7408.2005.00053.x; Almazán-Becerril A, 2015, BOT MAR, V58, P115, DOI 10.1515/bot-2014-0093; Anglès S, 2017, J PHYCOL, V53, P833, DOI 10.1111/jpy.12546; Aráoz R, 2020, HARMFUL ALGAE, V98, DOI 10.1016/j.hal.2020.101887; Balech E., 1964, HYDROBIOLOGIA, V4, P179; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. Mexico, V7, P57; Biecheler B., 1952, Bull. Biol. Fr. 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H., 1908, WISSENSCHAFTLICHE ER, V8, P123; Park JS, 2021, J MAR SCI ENG, V9, DOI 10.3390/jmse9060649; Pascher A., 1914, Berlin Ber D bot Ges, V32; Posada D, 2008, MOL BIOL EVOL, V25, P1253, DOI 10.1093/molbev/msn083; Reñé A, 2024, EUR J PHYCOL, V59, P196, DOI 10.1080/09670262.2023.2279547; Satta CT, 2013, HARMFUL ALGAE, V24, P65, DOI 10.1016/j.hal.2013.01.007; SPURR AR, 1969, J ULTRA MOL STRUCT R, V26, P31, DOI 10.1016/S0022-5320(69)90033-1; Stamatakis A, 2006, BIOINFORMATICS, V22, P2688, DOI 10.1093/bioinformatics/btl446; 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; Tillmann U, 2012, PROTIST, V163, P701, DOI 10.1016/j.protis.2011.10.005; Zeng N, 2012, NEW ZEAL J MAR FRESH, V46, P511, DOI 10.1080/00288330.2012.719911	54	0	0	5	5	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	SEP 2	2024	63	5					490	501		10.1080/00318884.2024.2400043	http://dx.doi.org/10.1080/00318884.2024.2400043		SEP 2024	12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	J9W0H					2025-03-11	WOS:001317612700001
J	Deckers, J; Munsterman, D; Rombaut, B; Kruisselbrink, A				Deckers, Jef; Munsterman, Dirk; Rombaut, Bernd; Kruisselbrink, Andreas			A latest Eocene depocenter in between uplifted masses (SW Netherlands and NW Belgium)	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						Subsidence; Inversion; Priabonian; Biostratigraphy; Vertical surface movements	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; NORTH-SEA; BASIN INVERSION; PALEOGENE; EVOLUTION	Under Priabonian (latest Eocene) far-field compression, the major Jurassic graben systems and their proximal areas experienced domal uplift in the Netherlands and northeastern Belgium. It has been proposed that this flexural uplift was simultaneous with flexural subsidence of the surrounding areas. This hypothesis is, however, only based on the correlation of few widely spaced boreholes without supporting biostratigraphic or seismic data. For this study, a seismic line and cross-boundary borehole log correlation panel, comprising three biostratigraphically analyzed boreholes, were used to critically examine the abovementioned hypothesis. The seismic line and correlation panel run from the southern flank of the uplifted West Netherlands Basin, also known as the Voorne Trough, towards the south. They both show a gradual thickening of the Priabonian sequences towards the Voorne Trough, confirming the flexural subsidence hypothesis. The underlying Bartonian and overlying lowermost Rupelian units do not share the abovementioned thickness trend, which highlights the particularity of Priabonian basin dynamics. Within the Priabonian depocenter, plenty of reworked organic material was deposited, mostly of Bartonian age, providing further evidence of the simultaneity of subsidence and uplift in nearby regions. We consider it very likely that subsidence and uplift were part of the same vertical surface deformation process. The results of this study are consistent with the mechanism of lithospheric folding under far-field compression by the convergence between Africa and Europe. A Priabonian N-S compressional stress-field would also be consistent with fault, joint and vein analyses performed at the British Isles west of the study area. As the regional stress-field changed around the Eocene-Oligocene boundary, the vertical surface movements of the study area also changed.	[Deckers, Jef; Rombaut, Bernd] Flemish Inst Technol Res, VITO, Boeretang 200, Mol, Belgium; [Munsterman, Dirk; Kruisselbrink, Andreas] TNO Geol Survey Netherlands GSN, POB 80015, NL-3508 TA Utrecht, Netherlands	VITO	Deckers, J (通讯作者)，Flemish Inst Technol Res, VITO, Boeretang 200, Mol, Belgium.	jef.deckers@vito.be; dirk.munsterman@tno.nl; bernd.rombaut@vito.be; andreas.kruisselbrink@tno.nl		Munsterman, Dirk/0000-0003-1774-4615; Deckers, Jef/0000-0002-5373-8733	Flemish Bureau for Environment and Spatial Development; Flanders Environment Agency (VMM); Province of Noord-Brabant, drinking water company Brabant Water; GSN; GSB	Flemish Bureau for Environment and Spatial Development; Flanders Environment Agency (VMM); Province of Noord-Brabant, drinking water company Brabant Water; GSN; GSB	This article is largely based on interpretations and insights acquired during execution of the H3O-De Voorkempen project by Vernes et al. (2023). The H3O-De Voorkempen project delivered a seamless, cross-border 3D (hydro)geological model of the Noorderkempen (Flanders) and the western part of Noord-Brabant (The Netherlands); it was carried out by a partnership between TNO-Geological Survey of the Netherlands (GSN), VITO and RBINS-Geological Survey of Belgium (GSB), with financial support from the Flemish Bureau for Environment and Spatial Development (VPO), Flanders Environment Agency (VMM), the Province of Noord-Brabant, drinking water company Brabant Water, GSN and GSB. We are grateful to the H3O project team and steering committee for the fruitful collaboration and discussions that helped improve our understanding of the Cenozoic geology of this cross-border area. A special thanks to Katleen van Baelen (VITO) for her excellent work on the figures. We thank ONDRAF-NIRAS for allowing to visualize the confidential wireline logs of the Doel-2b and ON-Essen-1 boreholes. Reviews by Jan de Jager and Noel Vandenberghe led to significant improvements in the article.	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J. Earth Sci.	OCT	2024	113	7					1643	1656		10.1007/s00531-024-02461-3	http://dx.doi.org/10.1007/s00531-024-02461-3		SEP 2024	14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	L6E2P					2025-03-11	WOS:001314816300001
J	Zou, SM; Yu, XK; Sun, TT; Wei, LA; Wu, XM				Zou, Shanmei; Yu, Xinke; Sun, Tiantian; Wei, Lina; Wu, Xuemin			Unveiling bacterial communities linked with<i> Alexandrium</i><i> catenella,</i> , their impact and influential mechanism on paralytic shellfish toxin production	ALGAL RESEARCH-BIOMASS BIOFUELS AND BIOPRODUCTS			English	Article						Alexandrium catenella; Associated bacteria; PSTs; Toxin physiological process; Molecular regulation	HARMFUL ALGAL BLOOMS; POISONING TOXINS; GENETIC-MARKERS; RESTING CYSTS; DINOFLAGELLATE; FUNDYENSE; GROWTH; DINOPHYCEAE; TAMARENSE; TOXICITY	Alexandrium causes serious food safety and human death due to paralytic shellfish toxins (PSTs) production. The associated bacteria can affect PSTs production of Alexandrium. However, the influencing mechanism is still unclear. Here we firstly screened functional associated bacteria for affecting PSTs production of Alexandrium catenella in Yangtze Estuary and further studied their influence on physiological process and molecular regulation of A. catenella. Thirteen bacteria strains for affecting PSTs production of A. catenella were selected. The A. catenella strains co-cultured with different functional associated bacteria all produced more PSTs than axenic strain with antibiotic treatment. Compared with axenic A. catenella, the non-axenic A. catenella produced more algal cells, soluble sugar, soluble protein and neutral lipid. By RNA-seq, it was found that non-axenic A. catenella produced more upregulated functional genes than axenic A. catenella. The biosynthesis of cofactors and spliceosome were the dominant different pathways between axenic and non-axenic A. catenella strains. The sxtA expression was closely related with Arginine and proline metabolism, Arginine biosynthesis, Fatty acid biosynthesis, TCA cycle and Glutathione metabolism, which were all downregulated in axenic A. catenella. Meantime, the non-axenic A. catenella under nitrogen deprivation produced less PSTs and functional genes than non-axenic strain under common culture condition, indicating the nitrogen significance for PSTs production. The detailed signal molecular released by associated bacteria for regulating PSTs of A. catenella needs to be further studied.	[Zou, Shanmei; Yu, Xinke; Sun, Tiantian; Wei, Lina; Wu, Xuemin] Nanjing Agr Univ, Coll Resources & Environm Sci, Nanjing 210095, Peoples R China	Nanjing Agricultural University	Zou, SM (通讯作者)，Nanjing Agr Univ, Coll Resources & Environm Sci, Nanjing 210095, Peoples R China.	zousm912@njau.edu.cn	wu, xue/LVS-0478-2024		National Natural Science Foundation of China [31600294]; Bioinformatics Center of Nanjing Agricultural University	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Bioinformatics Center of Nanjing Agricultural University	This study was supported by a grant from "National Natural Science Foundation of China (31600294) ". The bioinformatics analysis of the project was supported by the Bioinformatics Center of Nanjing Agricultural University.	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OCT	2024	83								103698	10.1016/j.algal.2024.103698	http://dx.doi.org/10.1016/j.algal.2024.103698		SEP 2024	12	Biotechnology & Applied Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology	G5Y6D					2025-03-11	WOS:001317392900001
J	Li, J; Yang, SX; Liu, J; Mei, X; Guo, XW; Zhang, XH; Liu, JX; Gu, F; Zheng, Z				Li, Jie; Yang, Shixiong; Liu, Jian; Mei, Xi; Guo, Xingwei; Zhang, Xunhua; Liu, Jianxing; Gu, Fang; Zheng, Zhuo			Pollen evidence of enhanced Yellow River provenance into the South Yellow Sea after the Middle Pleistocene Transition	QUATERNARY SCIENCE REVIEWS			English	Article						Pollen analysis; Provenance shift; The Middle Pleistocene Transition; South Yellow Sea	CHINA SEA; LEVEL CHANGES; BOHAI SEA; SEDIMENTARY EVOLUTION; SURFACE SEDIMENTS; MARINE-SEDIMENTS; BASIN; HISTORY; VEGETATION; SUBSIDENCE	Quaternary sediment of the South Yellow Sea (SYS) is usually assumed to record climatic changes, tectonic activities and major river evolutions. However, as an important terrigenous indicator, a long sequence of pollen proxy in the SYS lacks for studies of river provenance and climate changes. In this study, we focused on a 150-m pollen record in the SYS that covered most of the Quaternary period over the past 1.7 Ma. The most significant changes of pollen assemblage were caused by river provenance, that high pollen percentages of broadleaved trees such as Castanea/Castanopsis reflect a dominant provenance of the Yangtze River since ca. 1.8 Ma, with a decline trend during the Middle Pleistocene Transition (MPT) mainly between 1.1 and 0.8 Ma. The sharp increase in coniferous pollen, particularly Picea, originated from the Yellow River drainage areas, suggesting a major alteration in terrigenous pollen source from the Yangtze River to the Yellow River at similar to 0.8 Ma, which agrees well with the timing of the final integration of the modern Yellow River. The high pollen quantities of Artemisia and Ephedra also shows the enhanced Yellow River provenance where most landscape was covered by semi-arid open vegetation (e.g. steppe). The alternate appearances of marine foraminifera and dinoflagellate cysts, and freshwater wetland plants (Cyperaceae, Poaceae) through the interglacial intervals from MIS 19/21 demonstrate different estuary sedimentary environments and diverse salinity, associated with the sea-level fluctuations. The pollen concentration suggests an increase in terrigenous materials towards the interglacial MIS 11 and the preliminary delta formation of the Yellow River. We propose that the terrigenous input from the Yellow River accelerated after the MPT, and combined effects of tectonic movement drove the evolution of the river delta plains in eastern China. Our data also reveal some secondary periodic changes in evergreen broadleaved forest during the past 1.8 Ma and cold-tolerant coniferous forest after particularly the MPT, which are generally linked with the 400-ka long eccentricity cycle and the variability of monsoon climate.	[Li, Jie; Yang, Shixiong; Liu, Jian; Mei, Xi; Guo, Xingwei; Zhang, Xunhua] Qingdao Inst Marine Geol, Northern Observat & Res Stn Coastal Salt Marshes, MNR, Qingdao 266237, Peoples R China; [Yang, Shixiong; Liu, Jian] Qingdao Marine Sci & Technol Ctr, Lab Marine Geol, Qingdao 266237, Peoples R China; [Guo, Xingwei; Zhang, Xunhua] Shandong Univ, Inst Marine Sci & Technol, Qingdao 266237, Peoples R China; [Liu, Jianxing] Minist Nat Resources MNR, Inst Oceanog 1, Key Lab Marine Geol & Metallogeny, Qingdao 266061, Peoples R China; [Gu, Fang] China Univ Geosci, Sch Ocean Sci, Beijing 100083, Peoples R China; [Zheng, Zhuo] Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Key Lab Geodynam & Geohazards, Zhuhai 519082, Peoples R China	China Geological Survey; Qingdao Institute of Marine Geology (QIMG); Shandong University; Ministry of Natural Resources of the People's Republic of China; First Institute of Oceanography, Ministry of Natural Resources; China University of Geosciences; Sun Yat Sen University	Yang, SX (通讯作者)，Qingdao Inst Marine Geol, Northern Observat & Res Stn Coastal Salt Marshes, MNR, Qingdao 266237, Peoples R China.; Zheng, Z (通讯作者)，Sun Yat Sen Univ, Sch Earth Sci & Engn, Guangdong Key Lab Geodynam & Geohazards, Zhuhai 519082, Peoples R China.	yshixiong@mail.cgs.gov.cn; eeszzhuo@mail.sysu.edu.cn	Yang, Shixiong/KWT-8752-2024; Zheng, Zhuo/AAL-7564-2020; guo, xingwei/G-8641-2013		National Natural Science Foundation of China, China [U20A20116, U22A20558, 41876057]; China Geological Survey, China projects [DD20221775, DD20189503]; China-ASEAN Maritime Cooperation Fund, China [121201005000151110]; Ocean Negative Carbon Emissions Program	National Natural Science Foundation of China, China(National Natural Science Foundation of China (NSFC)); China Geological Survey, China projects; China-ASEAN Maritime Cooperation Fund, China; Ocean Negative Carbon Emissions Program	The authors are very thankful to Dr. Zhen Li from Geological Survey of Canada Pacific and Dr. James B. 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J	Simard, N; Weise, AM; Rochon, A; Briski, E; Macisaac, HJ; Mckindsey, CW				Simard, Nathalie; Weise, Andrea M.; Rochon, Andre; Briski, Elizabeta; Macisaac, Hugh J.; Mckindsey, Christopher W.			Discharge of ballast residual sediments during de-ballasting procedures: A more realistic estimate of propagule pressure	MARINE POLLUTION BULLETIN			English	Article						Invasive species; Ballast sediment; Dinoflagellate cyst; Invertebrate resting stage; Propagule pressure	DINOFLAGELLATE CYSTS; TANK SEDIMENTS; RESTING EGGS; GREAT-LAKES; EAST-COAST; WATER; TRANSPORT; EFFICACY; MARINE; INVERTEBRATES	Ship ballast residual sediments are an important vector of introduction for non-indigenous species. We evaluated the proportion of residual sediments and associated organisms released during de-ballasting operations of a commercial bulk carrier and estimated a total residual sediment accumulation of similar to 13 t, with accumulations of up to 20 cm in some tank areas that had accumulated over 11 years. We observed interior hull-fouling (anemones, hydrozoans, and bryozoans) and high abundances of viable invertebrate resting stages and dinoflagellate cysts in sediments. Although we determined that <1 % of residual sediments and associated resting stages were resuspended and released into the environment during individual de-ballasting events, this represents a substantial inoculum of 21 x 10(7) viable dinoflagellate cysts and 7.5 x 10(5) invertebrate resting stages with many taxa being nonindigenous, cryptogenic, or toxic/harmful species. The methods used and results will help estimate propagule pressure associated with this pathway and will be relevant for residual sediments and nonindigenous species management.	[Simard, Nathalie; Weise, Andrea M.; Mckindsey, Christopher W.] Fisheries & Oceans Canada, Maurice Lamontagne Inst, 850 Route Mer, Mont Joli, PQ G5H 3Z4, Canada; [Rochon, Andre] Univ Quebec Rimouski, Inst Sci Mer, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [Briski, Elizabeta] GEOMAR Helmholtz Ctr Ocean Res Kiel, Wischhofstr 1-3, D-24148 Kiel, Germany; [Macisaac, Hugh J.] Univ Windsor, Great Lakes Inst Environm Res, Windsor, ON, Canada	Fisheries & Oceans Canada; University of Quebec; Universite du Quebec a Rimouski; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Windsor	Mckindsey, CW (通讯作者)，Fisheries & Oceans Canada, Maurice Lamontagne Inst, 850 Route Mer, Mont Joli, PQ G5H 3Z4, Canada.	Chris.McKindsey@dfo-mpo.gc.ca	Briski, Elizabeta/P-4108-2019		Fisheries and Oceans Canada (Aquatic Invasive Species Program); Canadian Aquatic Invasive Species Network (CAISN); NSERC Discovery grants; Canada Research Chair; Institut des Sciences de la Mer (ISMER) of the Universite du Quebec a Rimouski	Fisheries and Oceans Canada (Aquatic Invasive Species Program); Canadian Aquatic Invasive Species Network (CAISN); NSERC Discovery grants(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canada Research Chair(Natural Resources CanadaCanadian Forest ServiceCanada Research Chairs); Institut des Sciences de la Mer (ISMER) of the Universite du Quebec a Rimouski	This work was supported by Fisheries and Oceans Canada (Aquatic Invasive Species Program), the Canadian Aquatic Invasive Species Network (CAISN), NSERC Discovery grants (HJM, AR), Canada Research Chair (HJM), and the Institut des Sciences de la Mer (ISMER) of the Universite du Quebec a Rimouski.	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J	Liu, XH; Tao, Z; Liu, YY; Hu, ZX; Deng, YY; Shang, LX; Lim, PT; Chai, ZY; Tang, YZ				Liu, Xiaohan; Tao, Zhe; Liu, Yuyang; Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Lim, Po-Teen; Chai, Zhaoyang; Tang, Ying-Zhong			Resting Cysts of the Toxic Dinoflagellate <i>Gymnodinium catenatum</i> (Dinophyceae) Ubiquitously Distribute along the Entire Coast of China, with Higher Abundance in Bloom-Prone Areas	JOURNAL OF MARINE SCIENCE AND ENGINEERING			English	Article						harmful algal blooms (HABs); Gymnodinium catenatum; resting cyst; geographic distribution; quantitative PCR	HARMFUL ALGAL BLOOMS; RED TIDE; GONYAULAX-TAMARENSIS; GRAHAM; PROFILE; PHYLOGENY; HEALTH; UNIQUE; GULF	Blooms of Gymnodinium catenatum have occurred occasionally in different areas of China and caused tremendous economic loss and even threatened human health. Not only is G. catenatum an important harmful-algal-bloom (HAB)-causing species, but also the only gymnodinioid dinoflagellate known to produce paralytic shellfish poisoning toxins (PSTs). Due to the germination of resting cysts, which often initiates blooms, the distribution and abundance of cysts in sediments and particularly the confirmation of cyst beds are important information for understanding and predicting dinoflagellate blooms. In this research, 199 sediment samples were collected from China's coastal seas, ranging from the Beidaihe in the Bohai Sea (BS) to the southernmost sample from the Nansha Islands of the South China Sea (SCS). TaqMan quantitative PCR (qPCR) assays with species-specific primers and probes were developed to specifically detect the distribution and abundance of cysts in the 199 samples. The detection revealed that G. catenatum cysts were widely present in the sediments (126 of the 199 samples), with 93.55%, 74.65%, 42.37%, and 50% of the samples detected positively from the BS, YS, ECS and SCS, respectively, and covering the vast sea area from Nansha Islands to the Beidaihe area. The single-cyst morpho-molecular identification in the samples from Beidaihe confirmed the existence of G. catenatum cysts in the BS, and the positive detections of G. catenatum cysts using the qPCR methods. While G. catenatum cysts were widely distributed in all four seas of China, the average abundance was relatively low (1.0 cyst per gram of wet sediment). Three samples from the East China Sea (ECS), however, contained G. catenatum cysts at a relatively higher level (23 cysts g(-1) wet sediment) than other sea areas, suggesting a pertinence of cyst abundance to the frequent occurrences of G. catenatum blooms in the area during recent years. Collectively, for G. catenatum being such an important toxic and HAB-causing species globally, the ubiquitous distribution of its cysts along the coastal waters of China and higher abundance in the bloom-prone areas warns us of a risk that cyst beds, although currently low in abundance, may seed HABs in any and many sea areas of China at any forthcoming year, and particularly those areas with records of frequent HABs outbreaks in the past.	[Liu, Xiaohan; Tao, Zhe; Liu, Yuyang; Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying-Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying-Zhong] Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying-Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Liu, Xiaohan] Natl Marine Environm Monitoring Ctr, Dalian 116023, Peoples R China; [Tao, Zhe] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Hu, Zhangxi] Guangdong Ocean Univ, Coll Fisheries, Dept Aquaculture, Zhanjiang 524088, Peoples R China; [Lim, Po-Teen] Univ Malaya, Inst Ocean & Earth Sci, Bachok 16310, Kelantan, Malaysia	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; National Marine Environmental Monitoring Center; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Guangdong Ocean University; Universiti Malaya	Chai, ZY; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Chai, ZY; Tang, YZ (通讯作者)，Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Chai, ZY; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	zhaoyangchai@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	Tao, Zhe/LIG-2380-2024; Li, Yang/KFB-5350-2024; ZHANG, hui jie/HTN-1690-2023; Chai, Zhaoyang/F-7485-2017; Lim, Po Teen/C-9758-2013	Deng, Yunyan/0000-0001-5967-3611; Liu, Yuyang/0000-0003-0418-4989; Lim, Po Teen/0000-0003-2823-0564; Chai, Zhaoyang/0000-0003-0526-8930; Hu, Zhangxi/0000-0002-4742-4973	National Key Research and Development Program of China; Science and Technology Innovation Project of Laoshan Laboratory [LSKJ202203700]; Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science [KFJ-SW-YW047]; Science and Technology Basic Resources Investigation Program of China [2018FY100200];  [2022YFC3105201]	National Key Research and Development Program of China(National Key Research & Development Program of China); Science and Technology Innovation Project of Laoshan Laboratory; Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science; Science and Technology Basic Resources Investigation Program of China; 	This research was funded by the National Key Research and Development Program of China (grant No. 2022YFC3105201), the Science and Technology Innovation Project of Laoshan Laboratory (grant No. LSKJ202203700), the Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science (grant No. KFJ-SW-YW047), and the Science and Technology Basic Resources Investigation Program of China (2018FY100200).	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J	Rubino, F; Denti, G; Belmonte, M; Belmonte, G				Rubino, Fernando; Denti, Giuseppe; Belmonte, Manuela; Belmonte, Genuario			Plankton Resting Stages Distribution in Bottom Sediments along the Confinement Gradient of the Taranto Sea System (Ionian Sea, Southern Italy)	JOURNAL OF MARINE SCIENCE AND ENGINEERING			English	Article						resting stages; cyst bank; confined coastal areas; Dinophyta; Copepoda; plankton; resurrection ecology; Taranto Sea System; Mediterranean Sea	MAR PICCOLO; DINOFLAGELLATE CYSTS; BODY-SIZE; ZOOPLANKTON; ASSEMBLAGES	The abundance distribution and species richness of encysted plankton have been investigated in the bottom sediments of the Taranto Marine System (southern Italy) for contributing to the understanding of plankton dynamics in a confined coastal area. This confined area is characterized by four contiguous basins with different degrees of confinement. The investigation was carried out in the fall season with the aim to intercept a period of rich cyst production from the plankton before overwintering. From the analysis of a total of 36 sediment samples, from 12 sample sites, the highest abundance of cysts and species richness were registered in the confined part of the system. A total of 103 cyst morphotypes have been recognized in the whole area, with highest abundances and taxa richness in the most confined stations. These results, suggesting a benthic-pelagic exchange of living matter, more intense in confined environments than in the open sea, highlight the necessity of (i) including the analysis of sediment cyst banks in studies of plankton dynamics, and (ii) to consider the role of confined areas, where the variability of environmental conditions favours a higher planktonic biodiversity in the sediments than in the water column.	[Rubino, Fernando; Denti, Giuseppe; Belmonte, Manuela] CNR Water Res Inst IRSA, I-74100 Taranto, Italy; [Belmonte, Genuario] Univ Salento, Dept Biol & Environm Sci & Technol, I-73100 Lecce, Italy	Consiglio Nazionale delle Ricerche (CNR); Istituto di Ricerca sulle Acque (IRSA-CNR); University of Salento	Belmonte, G (通讯作者)，Univ Salento, Dept Biol & Environm Sci & Technol, I-73100 Lecce, Italy.	fernando.rubino@irsa.cnr.it; giuseppe.denti@irsa.cnr.it; manuela.belmonte@vicodecarolis.edu.it; genuario.belmonte@unisalento.it	Rubino, Fernando/GOP-0332-2022; Denti, Giuseppe/LIG-9854-2024; BELMONTE, GENUARIO/AAG-4029-2020	Denti, Giuseppe/0000-0003-0204-5942; belmonte, genuario/0000-0002-7473-116X; Rubino, Fernando/0000-0003-2552-2510	Italian Ministry of University and Research; CNR IRSA of Taranto [3138, 3175]; National Recovery and Resilience Plan [CN_00000033, 1034, CUP D33C22000960007]; European Union NextGenerationEU	Italian Ministry of University and Research(Ministry of Education, Universities and Research (MIUR)); CNR IRSA of Taranto; National Recovery and Resilience Plan; European Union NextGenerationEU(European Union (EU))	The study did not receive direct funding. It, however, was carried out in the framework of the Project CyDiTSe (Cyst Distribution in Taranto Seas), funded by CNR IRSA of Taranto, and it was also indirectly sustained by the National Recovery and Resilience Plan (NRRP), Mission 4 Component 2 Investment 1.4-Call for tender n. 3138 of 16 December 2021, rectified by Decree n. 3175 of 18 December 2021 of Italian Ministry of University and Research funded by the European Union NextGenerationEU; Award Number: Project code CN_00000033, Concession Decree No. 1034 of 17 June 2022 adopted by the Italian Ministry of University and Research, CUP D33C22000960007, Project title "National Biodiversity Future Center-NBFC".	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J	Lebedeva, NK				Lebedeva, N. K.			Biogeography and Paleogeography of Taxonomic Diversity of Coniacian-Santonian Dinocysts of the Northern Hemisphere	RUSSIAN GEOLOGY AND GEOPHYSICS			English	Article						dinoflagellate cysts; Coniacian; Santonian; biogeography; paleogeography; correlation	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; UPPER CRETACEOUS DEPOSITS; PALYNOSTRATIGRAPHY; BASIN; SEDIMENTARY; BOREHOLE; SOUTH	-Dinocyst assemblages are subjected to taxonomic typification based on a qualitative and quantitative assessment of their generic composition for the Northern Hemisphere during the Coniacian-Santonian time in order to identify correlation taxa. The typification is carried out using a cluster analysis according to the Jacquard calculation model (BioDiversity Professional, 1997). Three types of dinocyst assemblages have been identified in the Coniacian. As compared to the Turonian, the relatively cold-water West Siberian basin is characterized by a decrease in the number of cosmopolitan taxa and an increase in species endemism. The only taxa identified at present are those allowing for intrabasin correlations. Three types of dinocyst assemblages have also been established for the Santonian. Free interbasin connections in the Northern Hemisphere contribute to the equalization of the generic composition between the three identified types and to the identification of characteristic taxa that allow for interregional correlation.	[Lebedeva, N. K.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Lebedeva, NK (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia.	LebedevaNK@ipgg.sbras.ru			Russian Ministry of Science and Higher Education [FWZZ-2022-0004]	Russian Ministry of Science and Higher Education	This work was financially supported by the Russian Ministry of Science and Higher Education within the framework of a state task (Project No. FWZZ-2022-0004).	Aleksandrova GN, 2012, STRATIGR GEO CORREL+, V20, P426, DOI 10.1134/S0869593812050024; Amon E.O., 1998, Radiolarians of the Urals and Their Stratigraphic Significance; Amon E.O., 1985, Sov. Geol. Geophys, V2, P112; Amon E.O., 2001, Russ. Geol. Geophys, V42, P459; AMON EO, 1990, NATO ADV SCI I C-MAT, V327, P923; Antonescu E., 1974, DariSeama Sedintelor LX(4), Stratigraphie, P25; Aurisano R., 1977, Developments in Palaeontology and Stratigraphy, V6, P369; Aurisano R.W., 1989, Palynology, V13, P143; Barss M.S., 1979, Geol. Surv. 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J	Zorzi, C; de Vernal, A				Zorzi, C.; de Vernal, A.			Evolution of West-East Contrast in the Subarctic Pacific Gyre During the Plio-Pleistocene Based on Palynological Evidence at ODP Sites 882 and 887	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						North Pacific Ocean; Pliocene; dinocysts; pollen grains; biozonation; sea surface reconstructions	WALLED DINOFLAGELLATE CYSTS; NORTH PACIFIC; LATE PLIOCENE; PRIMARY PRODUCTIVITY; MIDDLE PLEISTOCENE; SURFACE SEDIMENTS; BERING-SEA; OCEAN; GULF; BIOSTRATIGRAPHY	Fragmentary and contradictory evidence prevents a clear understanding of the possible role of the North Pacific Ocean surface on the ice-sheet evolution. New palynological data encompassing the Pliocene and Pleistocene at Ocean Drilling Program Site 882 in the northwest Pacific document sea-surface conditions from dinoflagellate cysts in addition to atmospheric trajectories from pollen grains and spores. The comparison of the Site 882 record with that of Site 887 from the northeast Pacific also permits documenting West to East contrasts across the subarctic North Pacific. The dinocyst assemblages at the two sites indicate strong temperature contrasts until 4.2 Ma, with much warmer conditions in the East. From 4.2 to 3.6 Ma, dinocyst assemblages of both sites are characterized by alternated dominance of the extinct taxa Habibacysta tectata and Impagidinium detroitense suggesting homogenous and cool conditions across the subarctic Pacific gyre. A major transition is recorded in the palynological assemblages at Site 882 around 2.7 Ma. It is marked by the highest occurrence of Habibacysta tectata and high percentages of Filisphaera microornata additionally to thermophilic taxa. Dinocyst record indicates high seasonality and warmer surface conditions due to reinforced stratification, which support the hypothesis of high evaporation at the origin of atmospheric moisture supply to high latitudes. During the last 1.2 Ma, the increase of Operculodinium centrocarpum relative to Nematosphaeropsis labyrinthus is tentatively interpreted as a reinforced influence of the subtropical waters. Hence, we suggest that the warm surface ocean fostered the inception and growth of northwestern North American ice-sheets during the Pliocene and Pleistocene. Dinocyst assemblages in the subarctic Pacific record changes in temperature and productivity through the Plio-Pleistocene The major transitions reflect halocline onset at 2.7 Ma and a major cooling at 1.7 Ma Subarctic ocean temperature and Westerlies migration may have affected northward moisture supply and ice-sheet growth over North America	[Zorzi, C.; de Vernal, A.] Univ Quebec Montreal, GEOTOP, Montreal, PQ, Canada; [Zorzi, C.] Univ Algarve, Ctr Marine Sci CCMAR CIMAR LA, Campus Gambelas, Faro, Portugal; [Zorzi, C.] Inst Portugues Mar & Atmosfera IPMA, Ave Alfredo Magalhaes Ramalho 6, Lisbon, Portugal	University of Quebec; University of Quebec Montreal; Universidade do Algarve; Instituto Portugues do Mar e da Atmosfera	Zorzi, C (通讯作者)，Univ Quebec Montreal, GEOTOP, Montreal, PQ, Canada.; Zorzi, C (通讯作者)，Univ Algarve, Ctr Marine Sci CCMAR CIMAR LA, Campus Gambelas, Faro, Portugal.; Zorzi, C (通讯作者)，Inst Portugues Mar & Atmosfera IPMA, Ave Alfredo Magalhaes Ramalho 6, Lisbon, Portugal.	coraliezorzi@gmail.com	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Zorzi, Coralie/0000-0002-4910-5255	Natural Sciences and Engineering Research Council (NSERC) of Canada; FCT-Foundation for Science and Technology [UIDB/04326/2020, UIDP/04326/2020, LA/P/0101/2020]	Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); FCT-Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT))	This study is an ArcTrain contribution. We acknowledge the support provided by the Natural Sciences and Engineering Research Council (NSERC) of Canada through the Collaborative Research and Training Experience (CREATE) program and Discovery Grants to AdV. This study received Portuguese national funds from FCT-Foundation for Science and Technology through projects UIDB/04326/2020 (https://doi.org/10.54499/UIDB/04326/2020), UIDP/04326/2020 (https://doi.org/10.54499/UIDP/04326/2020) and LA/P/0101/2020 (https://doi.org/10.54499/LA/P/0101/2020 ) and through CZ's contract (https://doi.org/10.54499/2022.03976.CEECIND/CP1729/CT0001). The authors thank the scientific party, technical staff and crews of ODP Leg 145 for their efforts in providing the data and samples used in this research. 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Paleoclimatology	SEP	2024	39	9							e2024PA004873	10.1029/2024PA004873	http://dx.doi.org/10.1029/2024PA004873			17	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	E4L3C		hybrid			2025-03-11	WOS:001302730400001
J	Premaor, E; Ferreira, EP; Guerstein, GR; Souza, PA				Premaor, Eduardo; Ferreira, Elizabete P.; Guerstein, G. Raquel; Souza, Paulo A.			Eocene paleoceanographic and paleoclimatic events recognized by assemblages of dinoflagellate cysts in the Southwest Atlantic Ocean( vol 130 , 104587 , 2023)	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Correction												eduardopremaor@gmail.com						Aubry M.P., 2003, CAUSES CONSEQUENCES, V369, P551; Schmitz B, 2001, PALAEOGEOGR PALAEOCL, V165, P299, DOI 10.1016/S0031-0182(00)00167-X	2	0	0	0	0	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	OCT 15	2024	146								105021	10.1016/j.jsames.2024.105021	http://dx.doi.org/10.1016/j.jsames.2024.105021		AUG 2024	1	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	G5S7X					2025-03-11	WOS:001317239400001
J	Nag, D; Sangode, SJ; Singh, SP; Uddandam, PR; Choudhuri, A; Phartiyal, B; Prasad, V				Nag, Debarati; Sangode, Satish J.; Singh, Sarvendra P.; Uddandam, Prem R.; Choudhuri, Adrita; Phartiyal, Binita; Prasad, Vandana			Magnetostratigraphy and rock magnetic studies on the Cretaceous-Paleogene transition strata along the Um Sohryngkew River, Therriaghat, Meghalaya, India	GEOLOGICAL JOURNAL			English	Article						aerosol; akagan & eacute;ite; bollide impact; Deccan volcanism; K-Pg boundary; magnetic susceptibility; Meghalaya	TERTIARY BOUNDARY; DECCAN VOLCANISM; DINOFLAGELLATE CYST; IRIDIUM ENRICHMENT; KHASI HILLS; SECTION; SUSCEPTIBILITY; IMPACT; SUCCESSION; SEDIMENTS	A combination of magnetic polarity and rock magnetic analysis on the well-documented section of the Um Sohryngkew River (USR) in the south Shillong Plateau, NE India, produced a sharp reversal marking the C29r-C29n geomagnetic polarity transition at approximately 65.688 Ma. The rock magnetic studies indicate ferrimagnetic dominant mineralogy with abundance of SSD grains, with an anomalous peak in susceptibility coinciding with Ir-rich limonitic layer. The magnetic reversal occurs precisely 61 m above the Ir-rich distinct in situ limonitic layer, indicating that the C29r-C29n geomagnetic reversal post-dates the widely accepted Ir-anomaly based K-Pg boundary by approximately 355 Ka. Furthermore, the rock magnetic studies indicate its frequency dependence coinciding with the Ir-rich limonitic layer suggesting a possible dust/aerosol source, while akagan & eacute;ite is reported from the interval approximately 1 m below peak susceptibility, indicating signature of Deccan volcanism. This study infers the completeness of the USR section with a high rate of sedimentation of approximately 17 cm/ka among the marine K-Pg boundary sections in the world. The first magnetostratigraphic record from the Um Sohryngkew River section of Meghalaya produced a sharp reversal marking the C29r-C29n geomagnetic polarity transition. Further mineralogical and rock magnetic analyses reveal signature of Deccan volcanism from the studied sedimentary sequence and the potential of the section to identify relative position of impact and Deccan Phase 2. image	[Nag, Debarati; Sangode, Satish J.] Savitribai Phule Pune Univ, Dept Geol, Ganeshkhind Rd, Pune 411007, India; [Singh, Sarvendra P.; Uddandam, Prem R.; Choudhuri, Adrita; Phartiyal, Binita; Prasad, Vandana] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, India	Savitribai Phule Pune University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Nag, D (通讯作者)，Savitribai Phule Pune Univ, Dept Geol, Ganeshkhind Rd, Pune 411007, India.; Prasad, V (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, India.	debarati_nag@yahoo.co.in; prasad.van@gmail.com	Sangode, Satish/MBG-5274-2025	Phartiyal, Binita/0000-0003-3086-8735	BSIP	BSIP	The authors are thankful to the Head, Department of Geology, Savitribai Phule Pune University for encouragement and support permission to avail Rock Magnetic Lab. The authors are also grateful to the Director, Birbal Sahni Institute of Palaeosciences, Lucknow, India for support and using SAIF facility of BSIP for the research work. Debarati Nag is thankful to the Director BSIP for providing BSRA fellowship. Dr. Sabyasachi Mandal (Scientist B, BSIP) is acknowledged for his fruitful discussions during the field work.	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NOV	2024	59	11					3048	3067		10.1002/gj.5046	http://dx.doi.org/10.1002/gj.5046		AUG 2024	20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	L1H1J		Bronze			2025-03-11	WOS:001297680800001
J	Wang, R; Cheng, Y; Wan, QQ; Cao, RH; Cai, J; Huang, TL; Wen, G				Wang, Ru; Cheng, Ya; Wan, Qiqi; Cao, Ruihua; Cai, Jie; Huang, Tinglin; Wen, Gang			Emergency control of dinoflagellate bloom in freshwater with chlorine enhanced by solar radiation: Efficiency and mechanism	WATER RESEARCH			English	Article						Peridinium umbonatum; Solar/chlorine; Enhanced; Influencing factors; Apoptosis mechanism	MICROCYSTIS-AERUGINOSA; VERTICAL MIGRATION; CELL INTEGRITY; BALLAST WATER; DISINFECTION; DEGRADATION; INACTIVATION; PHOTOLYSIS; PHOTOSYNTHESIS; IDENTIFICATION	Dinoflagellate requires a lower temperature and blooms frequently in the spring and autumn compared to regular cyanobacteria. The outbreak of dinoflagellate bloom will also lead to the death of some aquatic organisms. However, research on freshwater dinoflagellates is still lacking due to the challenges posed by classification and culture in laboratory. The removal effect and mechanism of Peridinium umbonatum (P. umbonatum, a typical dinoflagellate) were investigated using solar/chlorine in this study. The effect of simulated solar alone on the removal of algae was negligible, and chlorine alone had only a slight effect in removing algae. However, solar/ chlorine showed a better removal efficiency with shoulder length reduction factor and kmax enhancement factor of 2.80 and 3.8, respectively, indicating a shorter latency period and faster inactivation rate for solar/chlorine compared to solar and chlorine alone. The removal efficiency of algae gradually increased with the chlorine dosage, but it dropped as the cell density grew. When the experimental temperature was raised to 30 degrees C, algal removal efficiency significantly increased, as the temperature was unsuitable for the survival of P. umbonatum. Attacks on cell membranes by chlorine and hydroxyl radicals (center dot OH) produced by solar/chlorine led to a decrease in cell membrane integrity, leading to a rise in intracellular reactive oxygen species and an inhibition of photosynthetic and antioxidant systems. Cell regeneration was not observed in either the chlorine or solar/ chlorine systems due to severe cell damage or cysts formation. In addition, natural solar radiation was demonstrated to have the same enhancing effect as simulated solar radiation. However, the algal removal efficiency of solar/chlorine in real water was reduced compared to 119 medium, mainly due to background material in the real water substrate that consumed the oxidant or acted as shading agents.	[Wang, Ru; Cheng, Ya; Wan, Qiqi; Cao, Ruihua; Cai, Jie; Huang, Tinglin; Wen, Gang] Xian Univ Architecture & Technol, Res Stn Water Qual Qinling Mt, Shaanxi Prov Field Sci Observat, Xian 710055, Peoples R China; [Wang, Ru; Cheng, Ya; Wan, Qiqi; Cao, Ruihua; Cai, Jie; Huang, Tinglin; Wen, Gang] Xian Univ Architecture & Technol, Shaanxi Key Lab Environm Engn, Xian 710055, Peoples R China; [Huang, Tinglin; Wen, Gang] Xian Univ Architecture & Technol, Collaborat Innovat Ctr Water Pollut Control & Wate, Xian 710055, Peoples R China	Xi'an University of Architecture & Technology; Xi'an University of Architecture & Technology; Xi'an University of Architecture & Technology	Wen, G (通讯作者)，Xian Univ Architecture & Technol, Res Stn Water Qual Qinling Mt, Shaanxi Prov Field Sci Observat, Xian 710055, Peoples R China.; Wen, G (通讯作者)，Xian Univ Architecture & Technol, Shaanxi Key Lab Environm Engn, Xian 710055, Peoples R China.; Wen, G (通讯作者)，Xian Univ Architecture & Technol, Collaborat Innovat Ctr Water Pollut Control & Wate, Xian 710055, Peoples R China.	hitwengang@163.com	Cai, Jie/ABB-4771-2020		Natural Science Foundation of China [52370018, 52300010]; Shaanxi Provincial Key Scientific and Technological Innovation Team [2023-CX-TD-32]; China Postdoctoral Science Foundation [2023MD734208]; Research Program of Youth Innovation Team (Shaanxi Provincial Department of Education) [23JP077]; Technology Innovation Leading Program of Shaanxi [2023GXLH-058]	Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Shaanxi Provincial Key Scientific and Technological Innovation Team; China Postdoctoral Science Foundation(China Postdoctoral Science Foundation); Research Program of Youth Innovation Team (Shaanxi Provincial Department of Education); Technology Innovation Leading Program of Shaanxi	This research was funded by the Natural Science Foundation of China (Grant No. 52370018, 52300010) , Shaanxi Provincial Key Scientific and Technological Innovation Team (2023-CX-TD-32) , China Postdoctoral Science Foundation (No. 2023MD734208) , Research Program of Youth Innovation Team (Shaanxi Provincial Department of Education, No. 23JP077) , and Technology Innovation Leading Program of Shaanxi (No.2023GXLH-058) .	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NOV 1	2024	265								122275	10.1016/j.watres.2024.122275	http://dx.doi.org/10.1016/j.watres.2024.122275		AUG 2024	11	Engineering, Environmental; Environmental Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Water Resources	D9I1E	39163711				2025-03-11	WOS:001299235300001
J	Jaydawi, S; Hssaida, T; Yousfi, MZ; Maatouf, W; Chakir, S; Talih, A; Chafai, K; Khaffou, H; Benmlih, A				Jaydawi, Soukaina; Hssaida, Touria; Yousfi, Mohamed Zakaria; Maatouf, Wafaa; Chakir, Sara; Talih, Amine; Chafai, Khaoula; Khaffou, Hanane; Benmlih, Abdelouahed			Callovian- Kimmeridgian palynology and palaeobiogeography of the Essaouira- Agadir Basin (Moroccan Atlantic Margin)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						North-west Africa; Jurassic; Callovian; Oxfordian; Kimmeridgian; Dinoflagellate cysts; Correlation; Palaeobiogeography	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEQUENCE STRATIGRAPHY; ALGARVE BASIN; TIMOR SEA; MIDDLE; NORTH; ASSEMBLAGES; BOUNDARY; AMMONITE; FRANCE	The Jurassic formations within the Essaouira-Agadir Basin are of considerable interest for petroleum exploration, owing to their reservoir facies and hydrocarbon potentiality. These formations exhibit a scarcity of macrofossils, and their age is determined through lithological correlation. The Agadir-Essaouira Basin is a Mesozoic-Cenozoic sedimentary basin, part of the Tethyan Realm, precisely belonging to the Central Atlantic province which extends the Tethys westward. The material studied originates from five boreholes (GTE-1, MKL-110, NDK-2, NDK-3 and ESS-1) located at the center the basin along an East-West axis. The organic residue of the studied samples revealed a diverse dinoflagellate cyst assemblage with specific associations incorporating globally recognized marker taxa. The Early Callovian is distinguished by species such as: Ctenidodinium combazii, Ctenidodinium continuum, Ctenidodinium cornigerum, Dichadogonyaulax sellwoodii, and Impletosphaeridium varispinosum. The Late Callovian is characterized by the presence of marker cysts including: Compositosphaeridium polonicum, Endoscrinium galeritum Gonyaulacysta centriconnata, Liesbergia liesbergensis, Wanaea thysanota. The Early Oxfordian is marked by the association of species including: Gonyaulacysta jurassica subsp. jurassica, Rhynchodiniopsis cladophora, Scriniodinium crystallinum, Systematophora areolata, Systematophora penicillata, and Trichodinium scarburghense. The Late Oxfordian to basal Kimmeridgian is characterized by an association of dinoflagellate cysts including: Cribroperidinium globatum, Dichadogonyaulax? panneum, Downiesphaeridium polytrichum, Egmontodinium polyplacophorum, Endoscrinium galeritum, Gochteodinia mutabilis, Perisseiasphaeridium pannosum, Prolixosphaeridium anasillum, Scriniodinium crystallinum, Systematophora areolata, Systematophora penicillata, Surculosphaeridium vestitum, Systematophora? daveyi, and Wallodinium krutzschii. Our associations have been correlated with those in contemporary basins within other paleogeographic realms, contributing to the formulation of a global paleobiogeographic pattern. This pattern complements previous research on the distribution of dinoflagellate cysts during the Callovian-Early Kimmeridgian time interval.	[Jaydawi, Soukaina; Talih, Amine; Benmlih, Abdelouahed] Mohammed V Univ Rabat, Fac Sci, Dept Geol, Geosci Water & Environm Lab, Ave Ibn Batouta,BP 1014, Rabat, Morocco; [Hssaida, Touria; Chafai, Khaoula; Khaffou, Hanane] Hassan II Univ Casablanca, Fac Sci Ben Msick, Geosci & Applicat Lab, Casablanca, Morocco; [Yousfi, Mohamed Zakaria; Maatouf, Wafaa] Natl Off Hydrocarbons & Min, Dept Petr Lab, 34 Ave Fadila, Rabat, Morocco; [Chakir, Sara] Sidi Mohamed Ben Abdellah Univ, Fac Sci Dhar El Mahraz, Dept Geol, Fes, Morocco	Mohammed V University in Rabat; Hassan II University of Casablanca; Sidi Mohamed Ben Abdellah University of Fez	Jaydawi, S (通讯作者)，Mohammed V Univ Rabat, Fac Sci, Dept Geol, Geosci Water & Environm Lab, Ave Ibn Batouta,BP 1014, Rabat, Morocco.	soukaina.jaydawi@fsr.um5.ac.ma			National office of hydrocarbons and Mining (ONHYM)	National office of hydrocarbons and Mining (ONHYM)	The authors would like to thank the skills of the National office of hydrocarbons and Mining (ONHYM) for the material and scientific assistance, without which this work would not have been possible. The journal Editor-in-chief Prof. Dr. Henk Brinkhuis and the two anonymous reviewers are kindly thanked for their positive and constructive com-ments which improved the quality of the manuscript. This study is led by Touria HSSAIDA.	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Palaeobot. Palynology	OCT	2024	329								105154	10.1016/j.revpalbo.2024.105154	http://dx.doi.org/10.1016/j.revpalbo.2024.105154		AUG 2024	20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	D2Y4J					2025-03-11	WOS:001294891700001
J	Durugbo, EU; Fajemila, OT; Olayiwola, MA; Ogbahon, OA; Bamford, MK				Durugbo, Ernest U.; Fajemila, Olugbenga T.; Olayiwola, Moshood A.; Ogbahon, Osazuwa A.; Bamford, Marion K.			Organic walled dinoflagellate cyst biostratigraphy of the middle-late Miocene western Niger Delta, Nigeria	REVUE DE MICROPALEONTOLOGIE			English	Article						Dinoflagellate cysts; Niger Delta; Biostratigraphy; Assemblage zones; Middle Miocene	TERTIARY PALYNOLOGY; EOCENE; PALEOCENE; BASIN; OLIGOCENE; ASSEMBLAGES; SEDIMENTS; PALYNOSTRATIGRAPHY; BIOZONATION; INDICATORS	Palynological analysis of 200 ditch cuttings of wells M6 and M7 from the western Niger Delta yield a diverse assemblage of pollen, spores, freshwater algae, foraminiferal wall linings and dinoflagellate cysts. Based on pollen and spore marker species, the wells date middle - late Miocene (P720-P860). The regular occurrence of dinoflagellate cysts enhances the subdivision of the sequences into eight and seven tentative dinoflagellate cysts assemblage zones for the M6 and M7 wells respectively. The proposed Niger Delta Dinoflagellate Cysts (C-I) zones are viz: the Lingulodinium machaerophorum Assemblage zone; Homotryblium spp./Sumatradinium spp. Assemblage zone; Operculodinium centrocarpum Assemblage zone; Nematosphaeropsis labyrinthus Assemblage zone; and the Protoperidinium spp./Selenopemphix spp. Assemblage zone. The boundaries are marked by remarkable dinocysts events such as first downhole occurrences or highest stratigraphic occurrences, supplemented with last down- hole occurrences or lowest stratigraphic occurrences as the samples were ditch cuttings. The common presence of dinoflagellate cysts and the dominance of Nematosphaeropsis labyrinthus and Impagidinium spp. indicate open marine conditions during the deposition of the studied section.	[Durugbo, Ernest U.] Redeemers Univ, Dept Biol Sci, PMB 230, Ede, Osun State, Nigeria; [Fajemila, Olugbenga T.] Osun State Univ, Dept Geol Sci, Osogbo, Osun State, Nigeria; [Olayiwola, Moshood A.] Obafemi Awolowo Univ, Nat Hist Museum, Ife, Osun State, Nigeria; [Ogbahon, Osazuwa A.] Fed Univ Technol Akure, Dept Appl Geol, Akure, Ondo State, Nigeria; [Bamford, Marion K.] Univ Witwatersrand, Evolutionary Studies Inst, Johannesburg, South Africa	Redeemers University; Obafemi Awolowo University; University of Witwatersrand	Fajemila, OT (通讯作者)，Osun State Univ, Dept Geol Sci, Osogbo, Osun State, Nigeria.	olugbenga.fajemila@uniosun.edu.ng	Durugbo, Ernest/A-9056-2017; Olayiwola, Moshood/JPK-8915-2023; Fajemila, Olugbenga/AAT-7453-2021	Fajemila, Olugbenga Temitope/0000-0002-9949-0091	Palaeontological Sci-entific Trust (PAST) , Johannesburg, South Africa	Palaeontological Sci-entific Trust (PAST) , Johannesburg, South Africa	This study was supported by grant from The Palaeontological Sci-entific Trust (PAST) , Johannesburg, South Africa (to Durugbo Ernest Uzodimma) for the Dinoflagellate Biostratigraphy of the Tertiary Niger Delta " in March 2017.	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OCT	2024	84								100787	10.1016/j.revmic.2024.100787	http://dx.doi.org/10.1016/j.revmic.2024.100787		AUG 2024	10	Paleontology	Emerging Sources Citation Index (ESCI)	Paleontology	D2U3M					2025-03-11	WOS:001294784400001
J	Ouyang, H; Chen, JZ; Lin, LP; Zheng, H; Xie, CL; Wang, CF; Wang, ZH				Ouyang, Hong; Chen, Jiazhuo; Lin, Lanping; Zheng, Hu; Xie, Changliang; Wang, Chaofan; Wang, Zhaohui			Metabarcoding and co-occurrence network reveal significant effects of mariculture on benthic eukaryotic microalgal community: A case study in Daya Bay of the South China Sea	MARINE POLLUTION BULLETIN			English	Article						Eukaryotic microalgae; Resting stages; Surface sediments; Metabarcoding; Biogenic elements; Co-occurrence network	HARMFUL ALGAL BLOOMS; SURFACE SEDIMENTS; BIOGENIC ELEMENTS; RESTING CYSTS; ENVIRONMENTAL-CHANGES; SPATIAL-DISTRIBUTION; YELLOW SEA; DINOFLAGELLATE; PHYTOPLANKTON; PATTERNS	Benthic eukaryotic microalgae were analyzed by metabarcoding the partial 18S rRNA gene in Daya Bay bimonthly in 2021. Altogether 941 eukaryotic microalgal OTUs were detected, belonging to 27 classes of 8 phyla. Dinophyta and Chlorophyta were the dominant phyla. Microalgal community in the mariculture zone differed significantly from those in non-mariculture zone, reflected by low alpha diversity indexes and increasing abundance and richness of chlorophytes and correspondingly decreasing of dinoflagellates. The abundant occurrences of the pico- and nano-sized taxa such as the chlorophyte Picochlorum in the mariculture zone suggested that nutrient enrichment might result in the miniaturization of the benthic eukaryotic microalgae. The cooccurrence network suggested more negative interactions between taxa in the mariculture zone. A total of 41 algal bloom and/or harmful algal bloom (HAB) species were detected in this study, suggesting a high potential risk of HABs in Daya Bay, especially for the recurrent bloom species Scrippsiella acuminata.	[Ouyang, Hong; Chen, Jiazhuo; Lin, Lanping; Zheng, Hu; Xie, Changliang; Wang, Chaofan; Wang, Zhaohui] Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Peoples R China	Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Coll Life Sci & Technol, Guangzhou 510632, Peoples R China.	twzh@jnu.edu.cn	Wang, Zhaohui/C-9795-2016		National Key Research and Development Program of China [2022YFE0122100]; National Natural Science Foundation of China [42076141]	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))	This work was supported by the National Key Research and Development Program of China (No. 2022YFE0122100) , and the National Natural Science Foundation of China (No. 42076141) .	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Pollut. Bull.	OCT	2024	207								116832	10.1016/j.marpolbul.2024.116832	http://dx.doi.org/10.1016/j.marpolbul.2024.116832		AUG 2024	13	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	D2M5T	39128232				2025-03-11	WOS:001294581200001
J	Yang, Q; Ying, QE; Li, LQ; Zhang, J; Gong, FH; Sun, SL; Wang, HS; Tan, X; Liang, F				Yang, Qun; Ying, Qiaoer; Li, Liqin; Zhang, Jian; Gong, Fanhao; Sun, Shouliang; Wang, Hongshan; Tan, Xiao; Liang, Fei			Palynological evidence for the Late Cretaceous lake transgression event in the Songliao Basin, NE China	CRETACEOUS RESEARCH			English	Article						Upper Cretaceous; Santonian; LTE; SEG; Palynology	GEOCHRONOLOGICAL CONSTRAINTS; NENJIANG FORMATION; CYCLOSTRATIGRAPHY; STRATIGRAPHY; ACCUMULATION; ECOLOGY; FERNS	The lake transgression event (LTE) associated with a lake anoxic event (LAE) has been reported previously from the Cretaceous Nenjiang Formation in the Songliao Basin, NE China. Detailed studies based on sedimentology, dinoflagellates, ostracods, and biomarkers have provided important evidence for this LTE in Member 1 of the Nenjiang Formation (K2n1). 2 n 1 ). However, the related floristic record has not received enough attention. In this paper, palynological data of borehole Ji Tao Di-1 (JTD-1) from the western slope of the Songliao Basin were analyzed to investigate vegetation and climate changes associated with this Cretaceous LTE. Three palynological sub-assemblages reflect significant paleovegetation and paleoclimate changes through this LTE and reveal ecosystem fluctuations related to the global Cretaceous oceanic anoxic event (OAE3). A significant increase in the relative abundance of Schizaeoisporites and Cyathidites spores may represent the LTE in the Nenjiang Formation. Principal Components Analysis (PCA) and Sporomorph EcoGroup (SEG) model indicate that climate changed from cool and humid subtropical before the LTE, to relatively warm temperate during the LTE and temperate after the LTE in this area. The relatively warmer and drier climate during the later period of the LTE may be influenced by the contemporaneous OAE3. After the LTE, the highland mixed forests were dominant, and a large number of angiosperms (i.e., members of the Proteaceae) occupied the ecological niches of the middle canopy, indicating that the flourishing of angiosperms in the late Santonian may be closely related to environmental disturbances resulted from the LTE and OAE. (c) 2024 Elsevier Ltd. All rights are reserved, including those for text and data mining, AI training, and similar technologies.	[Yang, Qun; Ying, Qiaoer; Tan, Xiao; Liang, Fei] Shenyang Normal Univ, Coll Paleontol, Shenyang 110034, Peoples R China; [Yang, Qun; Ying, Qiaoer; Tan, Xiao; Liang, Fei] Minist Nat Resources, Key Lab Evolut Life NE Asia, Shenyang 110034, Peoples R China; [Li, Liqin] Zhejiang Inst Geosci, Zhejiang Inst Geol & Mineral Resources, Hangzhou 310007, Peoples R China; [Zhang, Jian; Gong, Fanhao; Sun, Shouliang] China Geol Survey, Shenyang Ctr Geol Survey, Shenyang 110034, Liaoning, Peoples R China; [Wang, Hongshan] Univ Florida, Florida Museum Nat Hist, Gainesville, FL 32611 USA	Shenyang Normal University; Ministry of Natural Resources of the People's Republic of China; China Geological Survey; State University System of Florida; University of Florida	Liang, F (通讯作者)，Shenyang Normal Univ, Coll Paleontol, Shenyang 110034, Peoples R China.; Gong, FH (通讯作者)，China Geol Survey, Shenyang Ctr Geol Survey, Shenyang 110034, Liaoning, Peoples R China.	gongfanhao@qq.com; liangfei5777@163.com			National Natural Science Foundation of China [42172017, 42072009]; China Geological Survey projects [DD20242686, DD20242217]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); China Geological Survey projects(China Geological Survey)	The research was supported by the National Natural Science Foundation of China (42172017, 42072009) and China Geological Survey projects (Grant Nos. DD20242686, DD20242217). Heartfelt thanks to Eugenia Bugdaevad and Valentina Markevich, Federal Scientific Center of East Asia Terrestrial Biodiversity, and Abdul Rahman Ashraf of Bonn University, for their help in palynomorphs identification and experimentation. Thanks are also extended to the faculty and students of Paleontology College of Shenyang Normal University for their assistance in the field work, and to the editor, Maria Rose Petrizzo, and the two reviewers, Mihai Emilian Popa and Jennifer Galloway, for their kind suggestions and comments on the manuscript.	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Q., 2002, CRETACEOUS OSTRACODE, P11; Yu ZQ, 2019, CRETACEOUS RES, V102, P160, DOI 10.1016/j.cretres.2019.05.006; Zhang LM, 2018, GEOLOGY, V46, P271, DOI 10.1130/G39992.1; Zhang M.M., 1977, Vertebrata Palasiatica, V15, P194; Zhao J, 2014, SCI CHINA EARTH SCI, V57, P2985, DOI 10.1007/s11430-014-4975-4	57	0	0	11	11	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JAN	2025	165								105971	10.1016/j.cretres.2024.105971	http://dx.doi.org/10.1016/j.cretres.2024.105971		AUG 2024	10	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	C8Z7Y					2025-03-11	WOS:001292199700001
J	Ando, T; Zonneveld, K; Versteegh, GJM; Ishigaki, M; Yamamoto, T; Matsuoka, K				Ando, Takuto; Zonneveld, Karin; Versteegh, Gerard J. M.; Ishigaki, Mika; Yamamoto, Tatsuyuki; Matsuoka, Kazumi			Why cysts of<i> Alexandrium</i><i> catenella</i> and/or<i> A.</i><i> pacificum</i> (Gonyaulacales, Dinophyceae) do not remain in sediments as fossils?	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Alexandrium catenella; Cyst wall; Fourier Transform infrared Spectroscopy (FTIR); Lingulodinium machaerophorum; Raman spectroscopy	DINOFLAGELLATE CYSTS; BAY; EXCAVATA; WALL	The dinoflagellate genus Alexandrium contains a number of species that produce paralytic shellfish toxins and have been the focus of attention as toxic plankton for harmless algal studies. Among Alexandrium species, A. catenella and A. pacificum form ellipsoidal-shaped resting cysts, which are preserved in marine sediments, and have attracted attention as potential seeds for future proliferation after favorable environmental conditions environmental improvement. However, although these cysts are preserved in surface of marine sediments, there is no record of their occurrence from solidified sediments as fossils. In order to clarify the reason for this, we investigated the differences in the chemical composition of cyst walls between colorless cyst of Alexandrium catenella/pacificum and Lingulodinium machaerophorum, Polysphaeridium zoharyi, Spiniferites spp. by measuring the thickness of cyst walls and using Fourier Transform Infrared Spectroscopy (FTIR) and Raman Spectroscopy. The results showed that the cyst wall of A. catenella/pacificum and L. machaerophorum were all composed of cellulosic organic matter. However, A. catenella/pacificum have the higher percentage of alpha- /beta-glucosidic linkages and that the thickness of their cyst walls is about one-third of that of L. machaerophorum. Therefore, these are reasons for the cysts of A. catenella/pacificum being more easily degraded in the sediment.	[Ando, Takuto] Akita Univ, Grad Sch Int Resource Sci, Akita, Japan; [Ando, Takuto] Shimane Univ, Estuary Res Ctr, Matsue, Japan; [Zonneveld, Karin] Univ Bremen, Ctr Marine Environm Sci, MARUM, Leobener Str 8, D-28359 Bremen, Germany; [Zonneveld, Karin; Versteegh, Gerard J. M.] Constructor Univ Bremen, Dept Phys & Earth Sci, Campus Ring 1, D-28759 Bremen, Germany; [Ishigaki, Mika] Shimane Univ, Ctr Promot Project Res, Matsue, Japan; [Yamamoto, Tatsuyuki] Shimane Univ, Fac Life & Environm Sci, Matsue, Japan; [Matsuoka, Kazumi] Nagasaki Univ, Inst East China Sea Res, Nagasaki, Japan; [Matsuoka, Kazumi] Osaka Museum Nat Hist, Osaka, Japan	Akita University; Shimane University; University of Bremen; Shimane University; Shimane University; Nagasaki University	Ando, T (通讯作者)，Akita Univ, Grad Sch Int Resource Sci, Akita, Japan.; Ando, T (通讯作者)，Shimane Univ, Estuary Res Ctr, Matsue, Japan.; Matsuoka, K (通讯作者)，Nagasaki Univ, Inst East China Sea Res, Nagasaki, Japan.; Matsuoka, K (通讯作者)，Osaka Museum Nat Hist, Osaka, Japan.	tact@gipc.akita-u.ac.jp; kzonneveld@marum.de; ishigaki@life.shimane-u.ac.jp; tyamamot@life.shimane-u.ac.jp; kazu-mtk@nagasaki-u.ac.jp			FY2019 program - Arctic Challenge for Sustainability (ArCS); JSPS KAKENHI [19K23448, 20K14591, 20K04089]	FY2019 program - Arctic Challenge for Sustainability (ArCS); 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))	This work is supported by FY2019 program for overseas visits by young researchers funded by Arctic Challenge for Sustainability (ArCS) (T.A.), and JSPS KAKENHI Grant Number 19K23448 (T.A.), 20K14591 (T.A.) and 20K04089 (K.M).	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Palaeobot. Palynology	OCT	2024	329								105161	10.1016/j.revpalbo.2024.105161	http://dx.doi.org/10.1016/j.revpalbo.2024.105161		AUG 2024	11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	C3V5W					2025-03-11	WOS:001288673500001
J	Rodrigues, C; Mendes, M; Pereira, Z; Nsungani, PC; Fernandes, P; Duarte, LV; Chitangueleca, B; Sebastia, L; Aida, B; Degli Esposti, D; Freitas, D				Rodrigues, Cristina; Mendes, Marcia; Pereira, Zelia; Nsungani, Pedro Claude; Fernandes, Paulo; Duarte, Luis Vitor; Chitangueleca, Belarmino; Sebastia, Lumen; Aida, Benedito; Degli Esposti, Davide; Freitas, Domingos			Palynology of the Albian-Turonian sediments from the Sumbe region, Kwanza Basin (Angola): Implications for paleoenvironment, paleoclimate, and paleogeography	CRETACEOUS RESEARCH			English	Article						Albian-Turonian; Dinoflagellate cysts; Sporomorphs; South atlantic; Gondwana breakup	OCEANIC ANOXIC EVENT; ELATER-BEARING POLLEN; NORTH-WESTERN DESERT; SOUTH-ATLANTIC; SERGIPE BASIN; PALYNOFACIES; DINOFLAGELLATE; TEMPERATURE; BRAZIL; BIOSTRATIGRAPHY	Palynological investigations in the Sumbe region of the Kwanza Basin, Angola, have identified Albian to Turonian assemblages in four sections of the Quissonde Facies of the Mucanzo, Cabo Ledo, and Itombe formations. These studies aimed to determine their biostratigraphic ages and infer paleoenvironmental, paleoclimatic, and paleogeographic models. The presence of Odontochitina costata, Palaeohystrichophora infusorioides, and Xiphophoridium alatum cysts supports an upper Albian to lower Cenomanian age for the Mucanzo Formation. Litosphaeridium siphoniphorum cyst and the Elateroplicites africaensis pollen found In the Cabo Ledo Formation suggest a Cenomanian age, while Conosphaeridium striatoconum, Heterosphaeridium difficile, and Dinogymnium acuminatum supports a Turonian age for the lower part of the Itombe Formation. All samples predominantly contain fluorescent amorphous organic matter (AOM) derived from phytoplankton degradation, with increasing AOM in the uppermost units, indicating inner neritic marine deposition under dysoxic-anoxic conditions. During the Lower to mid-Cretaceous, the Gondwana breakup caused significant changes, with the palynological indicating a Tethyan affinity with some high-latitude taxa, suggesting a cosmopolitan distribution. The subtropical to tropical nature of the assemblages, along with high-latitude species, indicates a mid-Cretaceous water connection between the Central Atlantic and the South Atlantic oceans, extending to the Kwanza Basin. (c) 2024 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).	[Rodrigues, Cristina] Univ Fernando Pessoa, FP ENAS, Praca 9 Abril 349, P-4249004 Porto, Portugal; [Rodrigues, Cristina] MARE Ctr Ciencia Mar & Ambiente URI Coimbra, Coimbra, Portugal; [Mendes, Marcia; Pereira, Zelia] LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Nsungani, Pedro Claude] Univ Agostinho Neto, Fac Ciencias, Dept Geol, Ave 4 Fevereiro 71, Luanda, Angola; [Fernandes, Paulo] Univ Algarve, Ctr Marine & Environm Res, CIMA, ARNET Infrastructure Network Aquat Res, Campus Gambelas, P-8000139 Faro, Portugal; [Duarte, Luis Vitor] Univ Coimbra, ARNET, MARE, Coimbra, Portugal; [Duarte, Luis Vitor] Dept Ciencias Terra, Coimbra, Portugal; [Chitangueleca, Belarmino; Sebastia, Lumen; Aida, Benedito] Agencia Nacl Petr Gas & Biocombustiveis ANPG, Explorat Div DEX, Luanda, Angola; [Degli Esposti, Davide] PGS Geophys Angola, Luanda, Angola; [Freitas, Domingos] Victory Oil & Energy VOE, Geosci Div, Luanda, Angola	Universidade Fernando Pessoa; Laboratorio Nacional de Energia e Geologia IP (LNEG); University Agostinho Neto; Universidade do Algarve; Universidade de Coimbra	Mendes, M (通讯作者)，LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal.	cfrodrig@gmail.com; marcia.mendes@lneg.pt; zelia.pereira@lneg.pt; pedroclaudensungani@yahoo.combr; pfernandes@ualg.pt; belarmino.Chitangueleca@anpg.co.ao; Lumen.Sebastiao@anpg.co.ao; benedito.aida@anpg.co.ao; davide.Degli.Esposti@pgs.com; dgmanager@victoryoe.com	Duarte, Luis/F-5282-2013; Rodrigues, Cristina/S-6536-2017; Fernandes, Paulo/J-6577-2014; Pereira, Zelia/B-2740-2017; Mendes, Marcia/E-2897-2019	Fernandes, Paulo/0000-0003-4888-0230; Pereira, Zelia/0000-0003-3056-6219; Rodrigues, Cristina Fernanda Alves/0000-0002-7616-6985; Mendes, Marcia/0000-0003-2290-891X			suggestions, which significantly contributed to the enhancement of the manuscript's quality. Their input is sincerely acknowledged.	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Res.	DEC	2024	164								105953	10.1016/j.cretres.2024.105953	http://dx.doi.org/10.1016/j.cretres.2024.105953		AUG 2024	15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	C3H0Z		hybrid			2025-03-11	WOS:001288284200001
J	Vallerand, J; de Vernal, A; Roy, N				Vallerand, Joan; de Vernal, Anne; Roy, Natasha			Climate variations in eastern Hudson bay over the past 3000 years	QUATERNARY SCIENCE REVIEWS			English	Article						Late holocene; Hudson bay; Palynology; Dinocysts; Pollen and spores; Sea-surface temperature; Salinity; Sea-ice; Paleoclimate	NORTHERN NORTH-ATLANTIC; SEA-ICE COVER; DINOFLAGELLATE CYSTS; ATMOSPHERIC CIRCULATION; NORTHWESTERN QUEBEC; BOREAL-FOREST; LAKE LEVELS; TREE-LINE; HOLOCENE; VEGETATION	Palynological analyses of the marine sediment core AMD0509-20 collected north of WhapmagoostuiKuujjuarapik in Nunavik were performed to investigate past changes in climate and sea-surface conditions based on pollen and spores and dinoflagellate cysts, respectively. Our results show relatively warm sea-surface temperatures before 2600 BP, about 2 degrees C higher than at present in summer, in addition to higher salinity suggesting relatively low freshwater inputs, thus low precipitation over the watershed. After 2400 years BP, an abrupt drop in sea-surface temperatures was recorded, followed by a decrease in salinity particularly pronounced until similar to 2000 years BP. After 1600 years BP, summer sea-surface temperatures and salinity stabilized around current values. The changes recorded in surface waters during the late Holocene can be associated with a regional shift in the hydroclimatic regime that led to a gradual decline of spruce (Picea) in pollen assemblages.	[Roy, Natasha] Univ Quebec Montreal, Geotop, CP 8888, Montreal, PQ H3C 3P8, Canada; Univ Quebec Montreal, Dept Sci Terre & Atmosphere, CP 8888, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal; University of Quebec; University of Quebec Montreal	Roy, N (通讯作者)，Univ Quebec Montreal, Geotop, CP 8888, Montreal, PQ H3C 3P8, Canada.	roy.natasha@uqam.ca	de Vernal, Anne/D-5602-2013		Fonds de recherche du Que <acute accent> bec-Nature et Technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada	Fonds de recherche du Que <acute accent> bec-Nature et Technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	<BOLD>I, the author, declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest. The data used was all collected during my master's degree and belongs to me. </BOLD> This study has received support from the Fonds de recherche du Que <acute accent> bec-Nature et Technologies (FRQNT) through support to the Geotop Research Center as a regroupement strate <acute accent> gique and a graduate scholarship to J. Vallerand. Support from the Natural Sciences and Engineering Research Council (NSERC) of Canada through research support to Anne de Vernal is also acknowledged. We are grateful to Bianca Fre <acute accent> chette for her help in the interpretation of pollen data. We also thank the anony-mous reviewers of the journal for their constructive comments.	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J	Nohr-Hansen, H				Nohr-Hansen, Henrik			The Cretaceous to Eocene: a biostratigraphical review and a new detailed palynostratigraphy of Greenland and adjacent areas	PALYNOLOGY			English	Article						Arctic biostratigraphy; Cretaceous-Eocene; detailed palynozonation; dinoflagellate cysts; Greenland	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; WESTERN INTERIOR SEAWAY; TERTIARY BOUNDARY; NUUSSUAQ BASIN; DAVIS STRAIT; SEQUENCE STRATIGRAPHY; LOWER PALEOGENE; VOLCANIC-ROCKS; WOLLASTON FORLAND; ATANE FORMATION	This paper compiles and correlates for the first time Cretaceous to Eocene palynostratigraphies across the Arctic. It focuses on Greenland and adjacent areas, including the Labrador-Baffin Seaway, onshore Nuussuaq Basin in central West Greenland, onshore southern East Greenland, central East Greenland, North-East Greenland, eastern North Greenland and the Danmarkshavn Basin, but also extends to the Canadian Arctic Archipelago and the Barents Sea region offshore Norway. The paper compiles data from more than three decades of detailed Arctic palynological analyses, based mainly on dinoflagellate cysts. It gives a historical overview of the Cretaceous to Paleogene palaeontological studies of Greenland and presents an overview of 85 palynological intervals and numerous bioevents. The palynological assemblages from the Labrador-Baffin Seaway, Nuussuaq Basin and north-east Baffin Bay reflect the opening of the Labrador-Baffin Seaway, from a brackish to freshwater environment in a large embayment in the Early Cretaceous to an open marine seaway in the Late Cretaceous. Assemblages reveal dinoflagellate cyst provincialism between the opening stages of the Labrador-Baffin Seaway and the already opened Greenland-Norwegian-Barents seaway. The Upper Cretaceous global Oceanic Anoxic Event 2 (OAE2) spanning the Cenomanian/Turonian boundary is recognised from Arctic Canada, north-east Baffin Bay, Nuussuaq Basin in central West Greenland, and North-East Greenland, and is mapped and correlated based on dinoflagellate cyst stratigraphy and carbon isotope (delta 13Corg) curves. The dinoflagellate cyst assemblages of the Cretaceous/Paleogene boundary are correlated from the Labrador Sea across to the Nuussuaq Basin in central West Greenland; in both areas the earliest Danian palynological assemblage is represented by incoming warm-water species. The presence of the global Paleocene-Eocene Thermal Maximum (PETM) in the Paleogene successions in North-East Greenland and in exploration wells in the Labrador-Baffin Seaway is indicated by the incoming of the warm-water dinoflagellate cyst species Axiodinium augustum.	[Nohr-Hansen, Henrik] Geol Survey Denmark & Greenland GEUS, Dept Geoenergy & Storage, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Nohr-Hansen, H (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Geoenergy & Storage, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	hnh@geus.dk					The present work is based on fieldwork and sample collections by myself and several of my GGU/GEUS colleagues during field seasons in southern East, central East, North-East, north-eastern, and central West Greenland. In particular, Peter Alsen, Morten Bjerager, JOrgen Bojesen-Koefoed, John Boserup, Flemming Getreuer Christiansen, Gregers Dam, Michael B.W. Fyhn, Jussi Hovikoski, Jon Ineson, Lotte Melchior Larsen, Lars Henrik Nielsen, Gunver Kraup Pedersen, Stefan Piasecki, Lars Stemmerik, Martin SOnderholm, Henrik Vosgerau, Michael Larsen (INEOS Oil and Gas Denmark) and Asger Ken Pedersen (Natural History Museum of Denmark) are thanked for their collection of samples and good company in the field. A special thanks goes to Yvonne Desezar, Charlotte Olsen, Annette Ryge, Dorthe Salomonsen and Kim Villadsen for prosessing and preparing high-quality slides of numerous palynological samples. Jette Halskov did the fantastic artwork. A special acknowledgement to the colleagues who helped and encouraged me in the initial and final phase of the project: Peter Alsen, Flemming Getreuer Christiansen, Lars Henrik Nielsen, and Stefan Piasecki. A special thank you goes to my wife, Bente Meldgaard Clausen, who helped and supported me during the preparation of this work. I thank the Carlsberg Foundation for financial support (1987-1989) during my PhD studies on Lower Cretaceous palynology from North-East Greenland and for financial support for a field excursion to the K/T boundary locality at Nuussuaq central West Greenland (1995). The Danish Ministry of Environment and Energy is thanked for financing my work on the project 'Bassin modellering VestgrOnland' (Grant No. EFP 1313/91-0014) and on the project 'Pal ae ogen sydlig VestgrOnland' (Grant No. EFP 1313/99-0025). The companies of the Sindri Group are gratefully acknowledged for their generous support of my work on material from the Kangerlussuaq Basin southern East Greenland. The licensees of the Sindri Group during the project were: Agip Denmark BV, Amerada Hess (Faroes) Ltd., Anadarko Faroes Company, P/F Atlantic Petroleum, BP Amoco Exploration Faroes Ltd., British Gas International BV, DONG FOroyar P/F, Enterprise Oil Exploration Ltd., FOroya Kolvetni P/F, Petro-Canada Faroes GmbH, Phillips Petroleum Europe Exploration Ltd., Shell (UK) Ltd., and Statoil F ae rOyene AS. Two institutions, the Geological Survey of Denmark and Greenland (GEUS) and the Geological Survey of Canada (Atlantic), (GSCA), part of Natural Resources Canada, are thanked for their support of my Labrador-Baffin Seaway studies. The reviewer Robert A. Fensome, an anonymous reviewer and the editor James B. Riding are thanked for their many constructive comments and suggestions that contributed significantly in improving the paper.	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J	Mansour, A; Wang, J; Fu, XG; Tahoun, SS; Ruebsam, W				Mansour, Ahmed; Wang, Jian; Fu, Xiugen; Tahoun, Sameh S.; Ruebsam, Wolfgang			Regional to global correlation of Cenomanian-early Turonian sea-level evolution and related dynamics: New perspectives	EARTH-SCIENCE REVIEWS			English	Article						Biostratigraphy; Dinoflagellate cysts; Palynology; Sea-level dynamics; Early late Cenomanian transgression; Early Turonian sea-level maximum; Short-term sea-level change	WESTERN INTERIOR SEAWAY; BOUNDARY STRATOTYPE SECTION; UPPER CRETACEOUS SEQUENCES; OCEANIC ANOXIC EVENT; CARBON ISOTOPES; OIL-FIELD; FORAMINIFERAL BIOSTRATIGRAPHY; TEMPERATURE EVOLUTION; ENVIRONMENTAL-CHANGES; AMMONITE FAUNAS	Major sea-level cycles occurred in the Cenomanian-early Turonian greenhouse world and impacted depositional conditions and ecosystems across the paleo-shelf seas. These sea-level cycles have been interpreted from various paleogeographic settings around the globe, such as the Western Interior Seaway (North America), the ProtoNorth Atlantic, Western Europe, and eastern Tethys (SE India). However, their drivers remain poorly understood and may include glacio-, aquifer-, thermo-, and/or tectono-eustasy. Uncertainties also persist regarding the timing, synchronicity, and magnitude of Cenomanian-early Turonian eustatic cycles. By combining palynological data from northern Africa (Gindi Basin, Egypt) with data available in the literature, a detailed synthesis of Cenomanian palynostratigraphy and sea-level dynamics is presented. Age-diagnostic spores, pollen, and organic walled dinoflagellate cysts (dinocysts) are correlated to global marine biozonation schemes, which provide a comprehensive biostratigraphic framework for the Cenomanian-early Turonian. Additionally, palynological data enable the identification of an early late Cenomanian Dinopterygium bio-event marked by the highest abundances of dinocysts. This bio-event can be correlated to the Neolobites ammonite bio-event and the Jukes-Browne Carbon Isotope Event. The bio-events stratigraphically constrain with a major transgression, which occurred in the early late Cenomanian, slightly preceding Oceanic Anoxic Event 2 (OAE2). Another major transgression spans the late Cenomanian-early Turonian, referred to the Plenus transgression bio-event, and consistent with the onset of the OAE2. Regional to global correlations indicate that these transgressive events reflect eustatic sea-level rises that can be recognized throughout the Tethys, Proto-North Atlantic, Europe, Western Interior Seaway, and India. These transgressions occurred within <1.0 Myr with modest magnitudes of 10-60 m. Rates of sea-level change has commonly been attributed to glacio-eustasy, which is however difficult to reconcile with a probably ice-free Cenomanian-early Turonian greenhouse world. Both transgressions coincide with phases of rising temperatures, whereby warming was most pronounced during the early late Cenomanian transgression. However, we can only speculate whether rising temperatures indicate the demise of polar glaciations. Eustatic processes, including tectono-eustasy, and to some extent aquifer- and thermo-eustasy, likely played a role in the sea-level rise during the early late Cenomanian and early Turonian. Environmental changes associated with the early late Cenomanian transgression may have triggered the onset of OAE2 possibly exacerbated by sluggish ocean circulation in a warming greenhouse world where sea ice formation was limited.	[Mansour, Ahmed; Wang, Jian; Fu, Xiugen] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed; Wang, Jian; Fu, Xiugen] Southwest Petr Univ, Qiangtang Inst Sedimentary Basin, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Menia 61519, Egypt; [Tahoun, Sameh S.] Cairo Univ, Fac Sci, Geol Dept, Giza 12613, Egypt; [Ruebsam, Wolfgang] Univ Kiel, Inst Geosci, Dept Organ & Isotope Geochem, Kiel, Germany	Southwest Petroleum University; Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; Egyptian Knowledge Bank (EKB); Cairo University; University of Kiel	Wang, J; Fu, XG (通讯作者)，Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China.	ahmedmans48@mu.edu.eg; w1962jian@163.com; fuxiugen@126.com; stahoun@cu.edu.eg; wolfgang.ruebsam@ifg.uni-kiel.de	Ruebsam, Wolfgang/AGG-2315-2022; Mansour, Ahmed/AAR-4969-2020		National Natural Science Foundation of China [42241202, 42241203]	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 (grant numbers: 42241202 and 42241203) . We thank the editor Christopher Fielding as well as Emad Nagm and three anonymous reviewers for their suggestions and constructive comments, which improved the manuscript.	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Rev.	SEP	2024	256								104863	10.1016/j.earscirev.2024.104863	http://dx.doi.org/10.1016/j.earscirev.2024.104863		JUL 2024	33	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	A1M7E					2025-03-11	WOS:001280249600001
J	Deng, YY; Li, FT; Shang, LX; Hu, ZX; Yue, CX; Tang, YZ				Deng, Yunyan; Li, Fengting; Shang, Lixia; Hu, Zhangxi; Yue, Caixia; Tang, Ying Zhong			The resting cyst of dinoflagellate <i>Scrippsiella acuminata</i> host bacterial microbiomes with more diverse trophic strategies under conditions typically observed in marine sediments	FRONTIERS IN MICROBIOLOGY			English	Article						acetogenic bacteria (acetogen); ammonium-oxidizing (anammox) bacteria; anaerobic respiration; chemotrophic bacteria; dinoflagellate resting cysts; nitrate-reducing bacteria (NRB); selective preservation; sulfate-reducing bacteria (SRB)	ALEXANDRIUM DINOPHYCEAE; HIROSHIMA BAY; TROCHOIDEA CYSTS; ORGANIC-MATTER; DEGRADATION; VIABILITY; GROWTH; LINGULODINIUM; ENVIRONMENTS; PHAEOBACTER	Variation in the condition of marine sediments provides selective preservation milieus, which act as a key determinant for the abundance and distribution of dinoflagellate resting cysts in natural sediments. Microbial degradation is an understudied biological factor of potential importance in the processes. However, gaps remain in our knowledge about the fundamental information of the bacterial consortia associated with dinoflagellate resting cysts both in laboratory cultures and in the field. Here we used Scrippsiella acuminata as a representative of cyst-producing dinoflagellates to delineate the diversity and composition of bacterial microbiomes co-existing with the laboratory-cultured resting cysts, and to explore possible impacts of low temperature, darkness, and anoxia (the mock conditions commonly observed in marine sediments) on the associated bacterial consortia. Bacterial microbiome with high diversity were revealed associated with S. acuminata at resting stage. The mock conditions could significantly shift bacterial community structure and exert notably inhibitory effects on growth-promoting bacteria. Resting cysts under conditions typically observed in marine sediments fostered bacterial microbiomes with more diverse trophic strategies, characteristic of prominently enriched anaerobic chemotrophic bacteria generating energy via respiration with several different terminal electron acceptors, which yielded more acidic milieu unfavorable for the preservation of calcareous resting cysts. Our findings suggest that there is complex and dynamic interaction between dinoflagellates resting cysts and the associated bacterial consortia in natural sediments. This intrinsic interaction may influence the maintenance and/or accumulation of dinoflagellate resting cysts with potential of germination and initiation blooms in the field.	[Deng, Yunyan; Li, Fengting; Shang, Lixia; Hu, Zhangxi; Yue, Caixia; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Deng, Yunyan; Li, Fengting; Shang, Lixia; Tang, Ying Zhong] Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Deng, Yunyan; Li, Fengting; Shang, Lixia; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China; [Hu, Zhangxi] Guangdong Ocean Univ, Coll Fisheries, Zhanjiang, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Guangdong Ocean University	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 Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023		National Science Foundation of China [42176207]; Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Sciences [COMS2019Q09]; Qingdao Postdoctoral Applied Research Project [QDBSH20220202137]	National Science Foundation of China(National Natural Science Foundation of China (NSFC)); Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Sciences; Qingdao Postdoctoral Applied Research Project	The author(s) declare that financial support was received for the research, authorship, and/or publication of this article. This research was financially supported by the National Science Foundation of China (Grant No. 42176207), the Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Sciences (Grant No. COMS2019Q09), and the Qingdao Postdoctoral Applied Research Project (No. QDBSH20220202137).	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JUL 22	2024	15								1407459	10.3389/fmicb.2024.1407459	http://dx.doi.org/10.3389/fmicb.2024.1407459			11	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	A7Q2J	39104580	Green Published, gold			2025-03-11	WOS:001284439000001
J	Savannah, M; Eelco, R; Timme, D; Katharine, G; Jörg, K; Gianluca, M; Francesca, S; Francesca, C; Caterina, M; Anna, S; Alessandra, N				Savannah, Myers; Eelco, Rohling; Timme, Donders; Katharine, Grant; Joerg, Keller; Gianluca, Marino; Francesca, Sangiorgi; Francesca, Caridi; Caterina, Morigi; Anna, Sabbatini; Alessandra, Negri			The "glacial" sapropel S6 (172 ka; MIS 6): A multiproxy approach to solve a Mediterranean "cold case"	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Sapropel S6; Multiproxy approach; Meltwater; Monsoon; Mediterranean Sea; Pleistocene	ICE-SHEET DYNAMICS; MILLENNIAL-SCALE; CLIMATE VARIABILITY; CALCAREOUS NANNOPLANKTON; PLANKTONIC-FORAMINIFERA; LATE PLEISTOCENE; AFRICAN MONSOON; QUATERNARY SAPROPELS; DINOFLAGELLATE CYSTS; ISOTOPIC COMPOSITION	Sequences of dark, organic-rich sediment layers (sapropels) exist throughout the Neogene of the Mediterranean Sea sedimentary record. While the mechanisms behind their cyclical deposition are not entirely understood, they have been found to correspond with precession minima (Northern Hemisphere [NH] insolation maxima). This causes NH summer monsoon to shift northward and intensify, which increases precipitation over North Africa and alters Mediterranean freshwater budget, leading to restricted bottom-water ventilation and anoxia. Most Mediterranean sapropels were deposited during interglacial periods, but sapropel S6 formed during the penultimate glaciation of Marine Isotopic Stage 6 (MIS 6; 190-130 ka), during which the Eurasian ice sheet extended to its maximum size of the Quaternary. Eurasian ice-sheet melting may have provided an additional input of freshwater to the Mediterranean during S6 deposition. To test this hypothesis, we present a multiproxy paleoecological (planktic foraminifera, calcareous nannofossils, pollen, dinocysts) and geochemical (foraminiferal delta 18O) study of S6 from the Ionian Sea. We confirm that S6 deposition resulted from an interaction of two different mechanisms of freshwater input to the Mediterranean, in which: (1) local ice-sheet meltwater discharge preconditioned the basin for stratification; and (2) increased monsoon activity over North Africa caused intense precipitation and river runoff that exacerbated water-column stratification. Our results provide new evidence for the prevalence of mild/temperate and humid conditions during S6 deposition, dispelling the notion that this "glacial" sapropel formed under cold and dry conditions and we document signals of warm (interstadial) and cold (stadial) conditions within S6 in the eastern Mediterranean basin.	[Savannah, Myers; Francesca, Caridi; Anna, Sabbatini; Alessandra, Negri] Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, Ancona, Italy; [Eelco, Rohling; Katharine, Grant] Australian Natl Univ, Res Sch Earth Sci, 142 Mills Rd, Canberra, Australia; [Timme, Donders] Univ Utrecht, Dept Phys Geog, Princetonlaan 8a, Utrecht, Netherlands; [Joerg, Keller] Albert Ludwigs Univ Freiburg, Inst Geo & Umweltnaturwissensch Mineral & Petrol, Albertstr 23b, D-79104 Freiburg, Germany; [Gianluca, Marino] Univ Vigo, Ctr Invest Marina, Palaeoclimatol Lab, GEOMA, Vigo 3610, Spain; [Francesca, Sangiorgi] Univ Utrecht, Dept Earth Sci, Princetonlaan 8a, Utrecht, Netherlands; [Caterina, Morigi] Univ Pisa, Dipartimento Sci Terra, Via Santa Maria 53, Pisa, Italy; [Eelco, Rohling] Univ Southampton, Natl Oceanog Ctr, Ocean & Earth Sci, Southampton SO14 3ZH, England	Marche Polytechnic University; Australian National University; Utrecht University; University of Freiburg; Universidade de Vigo; Utrecht University; University of Pisa; University of Southampton; NERC National Oceanography Centre	Alessandra, N (通讯作者)，Univ Politecn Marche, Dipartimento Sci Vita & Ambiente, Via Brecce Bianche, Ancona, Italy.	s.myers@pm.univpm.it; eelco.rohling@anu.edu.au; t.h.donders@uu.nl; katharine.grant@anu.edu.au; Joerg.Keller@minpet.uni-freiburg.de; gianluca.marino@uvigo.es; f.sangiorgi@uu.nl; f.caridi@staff.univpm.it; caterina.morigi@unipi.it; a.sabbatini@staff.univpm.it; a.negri@staff.univpm.it	Marino, Gianluca/AAN-3969-2020; Negri, Alessandra/D-4085-2011; Morigi, Caterina/L-3883-2016	Morigi, Caterina/0000-0003-1340-9932; Marino, Gianluca/0000-0001-9795-5337; Negri, Alessandra/0000-0002-8133-3936			The research benefited from the DISVA Department funds 2023 to Alessandra Negri. It is part of the PhD Fellowship awarded to Savannah Myers. We are deeply indebted to Laura Aiudi and Michelle de Groot for the nannofossil and palynomorphs data obtained in their Master thesis. We are grateful to the reviewers for their useful comments that helped us to improve the manuscript.	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Paleoclimatol. Paleoecol.	SEP 15	2024	650								112384	10.1016/j.palaeo.2024.112384	http://dx.doi.org/10.1016/j.palaeo.2024.112384		JUL 2024	16	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	ZK6J1		hybrid, Green Published			2025-03-11	WOS:001275228300001
J	Agüero, LS; Martínez, MA; Olivera, DE; Villa, RD; Zavala, C				Aguero, Luis S.; Martinez, Marcelo A.; Olivera, Daniela E.; Villa, Rocio D.; Zavala, Carlos			New dinoflagellate cyst records from the uppermost part of the Vaca Muerta Formation (uppermost Jurassic) in the Picun Leufu area, Neuquen Basin, Patagonia, Argentina	CRETACEOUS RESEARCH			English	Article						Upper Tithonian; Dino flagellate cysts; Vaca Muerta Formation; Neuquen Basin; Patagonia; Argentina	SEQUENCE STRATIGRAPHY; JURASSIC/CRETACEOUS BOUNDARY; ANTARCTIC PENINSULA; TENDAGURU BEDS; VOLGA BASIN; BIOSTRATIGRAPHY; PALYNOFACIES; PALYNOLOGY; PALYNOSTRATIGRAPHY; DINOCYSTS	This contribution presents a new palynological record from the uppermost Vaca Muerta Formation in the Picun Leufu area, Neuquen Basin, Argentina. A 76 m section was measured, and seven mudstone samples from the top of the Vaca Muerta Formation and the base of the Picun Leufu Formation were collected. Seventy-three palynomorph species were recognised and specimens of the dinoflagellate cyst genera Dingodinium, Gochteodinia, Ambonosphaera, Diacanthum, Systematophora, Tubotuberella, Wrevittia and Canningia were described and illustrated. The following taxa are mentioned for the first time: Tubotuberella in the Vaca Muerta Formation; Gochteodinia in Argentina; and Wrevittia in the Jurassic of Argentina. The dinoflagellate cyst content, integrated with previous studies, constrain the top of the Vaca Muerta Formation in the southern part of the basin, to the lower upper Tithonian. This study extends the basal limit of Pseudoceratium notiale to the lower upper Tithonian and Cribroperidinium reticulatum to the Tithonian. From a paleobiogeographic perspective, the presence of Thalassiphora robusta could provide evidence of its migration from the Volga Basin. Besides, taxa shared with the Tithonian of southeast Tanzania could be reflecting the connection between the Neuquen and the Mandawa basins via the Mozambique Corridor. The dinoflagellate cyst content of the uppermost Vaca Muerta Formation shows a relative decrease in previously reported species for this unit approaching the formational contact, alongside an increase in those species previously documented for the Picun Leufu Formation. The distribution of Pseudoceratium notiale, Dichadogonyaulax culmula and Pilosidinium cactosum was extended to the uppermost Vaca Muerta Formation. (c) 2024 Elsevier Ltd. All rights are reserved, including those for text and data mining, AI training, and similar technologies.	[Aguero, Luis S.; Martinez, Marcelo A.; Olivera, Daniela E.] Univ Nacl, Inst Geol INGEOSUR, CONICET, Ave Alem 1253,Cuerpo B0, RA-B8000ICN Bahia Blanca, Buenos Aires, Argentina; [Martinez, Marcelo A.; Olivera, Daniela E.; Villa, Rocio D.; Zavala, Carlos] Univ Nacl UNS, Dept Geol, CONICET, Avda Alem 1253,Cuerpo B0 2 Piso, RA-B8000ICN Bahia Blanca, Buenos Aires, Argentina; [Zavala, Carlos] Argentina SRL, Geol Cuencas Sedimentarias GCS, Molina Campos 150, RA-B8002CYD Bahia Blanca, Buenos Aires, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Agüero, LS (通讯作者)，Univ Nacl, Inst Geol INGEOSUR, CONICET, Ave Alem 1253,Cuerpo B0, RA-B8000ICN Bahia Blanca, Buenos Aires, Argentina.	luisaguero@ingeosur-conicet.gob.ar	Zavala, Carlos/AAT-6026-2021	Martinez, Marcelo/0000-0003-0538-4739; ZAVALA, CARLOS/0000-0001-9362-4282	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) [PIP 514CO]; Secretaria General de Ciencia y Tecnologia of Universidad Nacional del Sur (SEGCyT) [PGI 24/H156]	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Secretaria General de Ciencia y Tecnologia of Universidad Nacional del Sur (SEGCyT)	This work was supported by the Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) [grant number PIP 514CO] ; and the Secretaria General de Ciencia y Tecnologia of Universidad Nacional del Sur (SEGCyT) [grant number PGI 24/H156] .	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Res.	NOV	2024	163								105956	10.1016/j.cretres.2024.105956	http://dx.doi.org/10.1016/j.cretres.2024.105956		JUL 2024	18	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	ZA9F9					2025-03-11	WOS:001272680700001
J	Aydin, H; Uzar, S; Cingöz, EE; Kücüksezgin, F; Pospelova, V				Aydin, Hilal; Uzar, Serdar; Cingoz, Emine Erdem; Kucuksezgin, Filiz; Pospelova, Vera			Environmental factors influencing the abundance and spatial distribution of modern dinoflagellate cysts in Izmir Bay (Eastern Mediterranean)	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Lingulodinium machaerophorum; Eutrophication; Water quality; Izmir Bay; Environmental conditions	RECENT MARINE-SEDIMENTS; SURFACE SEDIMENTS; AEGEAN SEA; TOKYO-BAY; INDUSTRIAL-POLLUTION; COASTAL WATERS; YOKOHAMA-PORT; RESTING CYSTS; BLACK-SEA; ASSEMBLAGES	We analyzed surface sediments from 12 stations located in Izmir Bay to determine the impact of anthropogenic pollution on dinoflagellate cysts. Forty-three dinoflagellate cyst taxa and two cyst assemblage zones were identified. Zone 1 is characterized by the dominance of cysts of Gymnodinium nolleri, , Selenopemphix nephroides, and Operculodinium centrocarpum from the oligotrophic part of Izmir Bay. Zone 2 is in the highly productive inner part of the bay and is characterized by the high abundances of Lingulodinium machaerophorum, , Spiniferites ramosus, , cysts of Scrippsiella spp., cysts of Polykrikos spp. and Quinquecuspis concreta. . We used multivariate statistical analysis (DCA and CCA) on dinoflagellate cysts and environmental variables to support the identification of Zones 1 and 2. Our analyses also revealed that summer and winter chlorophyll-a a as well as elevated nitrate and nitrite concentrations are significant parameters in controlling dinoflagellate cyst distribution in Izmir Bay.	[Aydin, Hilal; Uzar, Serdar; Cingoz, Emine Erdem] Manisa Celal Bayar Univ, Fac Sci & Arts, Biol Dept, TR-45140 Manisa, Turkiye; [Kucuksezgin, Filiz] Dokuz Eylul Univ, Inst Marine Sci, Technol Inst Marine Sci & Technol, TR-35340 Izmir, Turkiye; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA	Celal Bayar University; Dokuz Eylul University; University of Minnesota System; University of Minnesota Twin Cities	Aydin, H (通讯作者)，Manisa Celal Bayar Univ, Fac Sci & Arts, Biol Dept, TR-45140 Manisa, Turkiye.	hilalaydin66@gmail.com	Pospelova, Vera/IXD-6686-2023; Uzar, Serdar/G-9956-2014	Pospelova, Vera/0000-0003-4049-8133	Scientific and Technical Research Council of Turkey (TUBITAK) [113Y006]	Scientific and Technical Research Council of Turkey (TUBITAK)(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK))	This study was supported by Scientific and Technical Research Council of Turkey (TUBITAK) (Project No. 113Y006) . This study con-tains a part of PhD dissertation prepared by Serdar Uzar in Manisa Celal Bayar University. The authors are grateful to marine chemistry labora-tory of Dokuz Eylul University Institute of Marine Science and Tech-nology performing chemical analysis. The authors also thank to crew of R/VK. Piri Reis for their assistance during fieldwork. Two anonymous reviewers and the associate editor are acknowledged for constructive comments that improved the manuscript.	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Pollut. Bull.	AUG	2024	205								116612	10.1016/j.marpolbul.2024.116612	http://dx.doi.org/10.1016/j.marpolbul.2024.116612		JUL 2024	14	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	I8B5H	38991358				2025-03-11	WOS:001332456400001
J	Fachon, E; Pickart, RS; Sheffield, G; Pate, E; Pathare, M; Brosnahan, ML; Muhlbach, E; Horn, K; Spada, NN; Rajagopalan, A; Lin, PG; McRaven, LT; Lago, LS; Huang, J; Bahr, F; Stockwell, DA; Hubbard, KA; Farrugia, TJ; Lefebvre, KA; Anderson, DM				Fachon, Evangeline; Pickart, Robert S.; Sheffield, Gay; Pate, Emma; Pathare, Mrunmayee; Brosnahan, Michael L.; Muhlbach, Eric; Horn, Kali; Spada, Nathaniel N.; Rajagopalan, Anushka; Lin, Peigen; McRaven, Leah T.; Lago, Loreley S.; Huang, Jie; Bahr, Frank; Stockwell, Dean A.; Hubbard, Katherine A.; Farrugia, Thomas J.; Lefebvre, Kathi A.; Anderson, Donald M.			Tracking a large-scale and highly toxic Arctic algal bloom: Rapid detection and risk communication	LIMNOLOGY AND OCEANOGRAPHY LETTERS			English	Letter							DINOFLAGELLATE ALEXANDRIUM-FUNDYENSE; CHUKCHI SEA; RESTING CYSTS; GEORGES BANK; WEST-COAST; MAINE; ABUNDANCE; GULF; PROFILES; BAY	In recent years, blooms of the neurotoxic dinoflagellate Alexandrium catenella have been documented in Pacific Arctic waters, and the paralytic shellfish toxins (PSTs) that this species produces have been detected throughout the food web. These observations have raised significant concerns about the role that harmful algal blooms (HABs) will play in a rapidly changing Arctic. During a research cruise in summer 2022, a massive bloom of A. catenella was detected in real time as it was advected through the Bering Strait region. The bloom was exceptional in both spatial scale and density, extending > 600 km latitudinally, reaching concentrations > 174,000 cells L-1, and producing high-potency PST congeners. Throughout the event, coastal stakeholders in the region were engaged and a multi-faceted community response was mobilized. This unprecedented bloom highlighted the urgent need for response capabilities to ensure safe utilization of critical marine resources in a region that has little experience with HABs.	[Fachon, Evangeline; Pathare, Mrunmayee; Brosnahan, Michael L.; Horn, Kali; Spada, Nathaniel N.; Rajagopalan, Anushka; Anderson, Donald M.] Woods Hole Oceanog Inst, Biol Dept, Woods Hole, MA 02543 USA; [Fachon, Evangeline] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA; [Pickart, Robert S.; Lin, Peigen; McRaven, Leah T.; Lago, Loreley S.; Huang, Jie; Bahr, Frank] Woods Hole Oceanog Inst, Phys Oceanog Dept, Woods Hole, MA USA; [Sheffield, Gay] Univ Alaska Fairbanks, Marine Advisory Program, Alaska Sea Grant, Nome, AK USA; [Pate, Emma] Norton Sound Hlth Corp, Off Environm Hlth, Nome, AK USA; [Muhlbach, Eric; Hubbard, Katherine A.] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, St Petersburg, FL USA; [Rajagopalan, Anushka] Northeastern Univ, Coll Sci, Boston, MA USA; [Lin, Peigen] Shanghai Jiao Tong Univ, Sch Oceanog, Shanghai, Peoples R China; [Stockwell, Dean A.] Univ Alaska Fairbanks, Coll Fisheries & Ocean Sci, Fairbanks, AK USA; [Farrugia, Thomas J.] Alaska Ocean Observing Syst, Anchorage, AK USA; [Lefebvre, Kathi A.] NOAA, Environm & Fisheries Sci Div, Northwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA USA	Woods Hole Oceanographic Institution; Massachusetts Institute of Technology (MIT); Woods Hole Oceanographic Institution; University of Alaska System; University of Alaska Fairbanks; Florida Fish & Wildlife Conservation Commission; Northeastern University; Shanghai Jiao Tong University; University of Alaska System; University of Alaska Fairbanks; National Oceanic Atmospheric Admin (NOAA) - USA	Fachon, E (通讯作者)，Woods Hole Oceanog Inst, Biol Dept, Woods Hole, MA 02543 USA.; Fachon, E (通讯作者)，MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA.	efachon@whoi.edu	Huang, Jie/KCX-8283-2024	Brosnahan, Michael/0000-0002-2620-7638; Huang, Jie/0000-0003-1134-5752; Fachon, Evangeline/0000-0003-2933-7283	NSF Office of Polar Programs [OPP-1823002]; NOAA's Arctic Research program [NA14OAR4320158, NA19OAR4320074]; NOAA Centers for Coastal and Ocean Science (NCCOS) Competitive Research Program [NA20NOS4780195]; NCCOS HAB Event Response Program; Woods Hole Center for Oceans and Human Health (National Science Foundation) [OCE-1840381]; Woods Hole Center for Oceans and Human Health (National Institutes of Health) [NIEHS-1P01-ES028938-01]; National Science Foundation Graduate Research Fellowship [2141064]; North Pacific Research Board Graduate Student Research Award; National Natural Science Foundation of China [42306251]; Shanghai Pujiang Program [22PJ1406400]	NSF Office of Polar Programs(National Science Foundation (NSF)); NOAA's Arctic Research program; NOAA Centers for Coastal and Ocean Science (NCCOS) Competitive Research Program; NCCOS HAB Event Response Program; Woods Hole Center for Oceans and Human Health (National Science Foundation); Woods Hole Center for Oceans and Human Health (National Institutes of Health)(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH Division of Research Services (DRS)); National Science Foundation Graduate Research Fellowship(National Science Foundation (NSF)); North Pacific Research Board Graduate Student Research Award; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Shanghai Pujiang Program(Shanghai Pujiang Program)	We acknowledge the crew and science personnel of the R/V Norseman II cruises. We also thank coastal community leadership as well as community clinicians throughout the Bering Strait region, Northwest Arctic Borough, and North Slope Borough. This work was supported by the NSF Office of Polar Programs (OPP-1823002); NOAA's Arctic Research program (through the Cooperative Institute for the North Atlantic Region [NA14OAR4320158 and NA19OAR4320074]); NOAA Centers for Coastal and Ocean Science (NCCOS) Competitive Research Program (NA20NOS4780195); NCCOS HAB Event Response Program; the Woods Hole Center for Oceans and Human Health (National Science Foundation grant OCE-1840381 and National Institutes of Health grant NIEHS-1P01-ES028938-01). EF received support from National Science Foundation Graduate Research Fellowship Grant No. 2141064; North Pacific Research Board Graduate Student Research Award. PL was supported by the National Natural Science Foundation of China (42306251); Shanghai Pujiang Program (22PJ1406400). The contents of this publication are solely the responsibility of the authors and do not necessarily represent the official views of any funding agency. This is ECOHAB publication number ECO1107.	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J	Soliman, A; Riding, JB; Smelror, M; El Atfy, H				Soliman, Ali; Riding, James B.; Smelror, Morten; El Atfy, Haytham			A review of the Mesozoic<i>-</i>Cenozoic acritarch genus <i>Cyclopsiella</i> Drugg & Loeblich Jr. 1967 emend. nov.	PALYNOLOGY			English	Article						Acritarchs; biostratigraphy; Cyclopsiella; geographical distributions; Mesozoic-Cenozoic; palaeoecology; review; taxonomy	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; NORTHERN BELGIUM; REFERENCE SECTION; UTSIRA FORMATION; LOWER OLIGOCENE; UPPER MIOCENE; UPPER EOCENE; SEA; PLIOCENE; AREA	The acritarch genus Cyclopsiella is extant and ranges back to the Middle Jurassic. This genus cannot be assigned to any of the established acritarch subgroups and has a relatively simple morphology; species are often referred to using open nomenclature. This study provides a comprehensive analysis of Cyclopsiella and its different morphotypes and species, outlining their characteristics and similarities. Through an extensive literature review, this study identifies previous sources of taxonomic confusion, reevaluates the characteristics and stratigraphical utility of this genus, and discusses the significance of the constituent species for Mesozoic and Cenozoic biostratigraphy. A series of synonymies and emendations are proposed, and 10 species of Cyclopsiella are maintained. One new species, Cyclopsiella reticulata sp. nov., is described. This robust morphological investigation strengthens the biostratigraphical and palaeoecological potential of Cyclopsiella.	[Soliman, Ali] Tanta Univ, Geol Dept, Tanta, Egypt; [Riding, James B.] British Geol Survey, Nottingham, England; [Smelror, Morten] Geol Survey Norway, Trondheim, Norway; [El Atfy, Haytham] Univ Munster, Inst Geol & Palaeontol, Palaeobotany Grp, Munster, Germany; [El Atfy, Haytham] Mansoura Univ, Geol Dept, Mansoura, Egypt	Egyptian Knowledge Bank (EKB); Tanta University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Geological Survey of Norway; University of Munster; Egyptian Knowledge Bank (EKB); Mansoura University	Soliman, A (通讯作者)，Tanta Univ, Geol Dept, Tanta, Egypt.	ali.soliman@science.tanta.edu.eg	Atfy, Haytham/AAT-2276-2021; Soliman, Ali/R-1583-2018	El Atfy, Haytham/0000-0003-1618-7220; Smelror, Morten/0000-0002-9593-648X; Soliman, Ali/0000-0001-7366-4607	Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences	Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences(Chinese Academy of Sciences)	We thank Hong-He Xu of the Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, for the translation of the description of taxa described in Chinese to English. Ali Soliman thanks W.E. Piller (Graz, Austria) for the Miocene samples, laboratory, and SEM facilities; R. Sachsenhofer (Leoben, Austria) for the Oligocene samples; and T. Suttner (Appalachian State University) for the Campanian samples. James B. Riding publishes with the approval of the Director, British Geological Survey (NERC). We would like to thank all the copyright holders for permission to use the images reproduced in Plates 1 and 2. Stefan Piasecki and Peter Bijl are thanked for their excellent reviews of the original submission, which helped us to substantially improve the paper. We thank Vera Korasidis, Assistant Editor, for her professional handling of the manuscript.	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J	Sixto, M; Riobó, P; Rodriguez, F; Díaz, PA; Figueroa, RI				Sixto, Marta; Riobo, Pilar; Rodriguez, Francisco; Diaz, Patricio A.; Figueroa, Rosa I.			Climate Change Stressors, Phosphate Limitation, and High Irradiation Interact to Increase <i>Alexandrium minutum</i> Toxicity and Modulate Encystment Rates	MICROORGANISMS			English	Article						Alexandrium minutum; light; paralytic shellfish poisoning; harmful algal blooms; pulse amplitude modulation; encystment	TOXIN PRODUCTION; PHOSPHORUS; GROWTH; TEMPERATURE; DINOPHYCEAE; SALINITY; PROFILES; DYNAMICS; BLOOMS; LIGHT	The changes in the cell physiology (growth rate, cell size, and cell DNA content), photosynthetic efficiency, toxicity, and sexuality under variable light and nutrient (phosphates) conditions were evaluated in cultures of the dinoflagellate Alexandrium minutum obtained from a red tide in the Ria de Vigo (NW Spain). The cells were grown at low (40 and 150 mu E m(-2) s(-1)), moderate (400 mu E m(-2) s(-1)), and high (800 mu E m(-2) s(-1)) light intensities in a medium with phosphate (P+) and without (P-). Cultures were acclimated to the irradiance conditions for one week, and the experiment was run for similar to 1 month. The cell size and DNA content were monitored via flow cytometry. Two different clonal strains were employed as a monoculture (in a P- or P+ medium) or, to foster sexuality and resting cyst formation, as a mixed culture (only in a P- medium). A. minutum growth was favored by increasing light intensities until 400 mu E m(-2) s(-1). The DNA content analyses indicated the accumulation of S-phase cells at the highest light intensities (400 and 800 mu E m(-2) s(-1)) and therefore the negative effects on cell cycle progression. Only when the cells were grown in a P- medium did higher light intensities trigger dose-dependent, significantly higher toxicities in all the A. minutum cultures. This result suggests that the toxicity level is responsive to the combined effects of (high) light and (low) P stress. The cell size was not significantly affected by the light intensity or P conditions. The optimal light intensity for resting cyst formation was 150 mu E m(-2) s(-1), with higher irradiances reducing the total encystment yield. Encystment was not observed at the lowest light intensity tested, indicative of the key role of low-level irradiance in gamete and/or zygote formation, in contrast to the stressor effect of excessive irradiance on planozygote formation and/or encystment.	[Sixto, Marta; Rodriguez, Francisco; Figueroa, Rosa I.] Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro 50-52, Vigo 36390, Spain; [Sixto, Marta] Univ Vigo, Fac Ciencias Mar, Campus Mar, Vigo 36311, Spain; [Riobo, Pilar] Consejo Super Invest Cient IIM CSIC, Inst Invest Marinas, Eduardo Cabello 6, Vigo 36208, Spain; [Diaz, Patricio A.] Univ Lagos, Ctr imar, Casilla 557, Puerto Montt 5480000, Chile; [Diaz, Patricio A.] Univ Lagos, CeBiB, Casilla 557, Puerto Montt 5480000, Chile	Spanish Institute of Oceanography; Universidade de Vigo; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Universidad de Los Lagos; Universidad de Los Lagos	Sixto, M; Figueroa, RI (通讯作者)，Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro 50-52, Vigo 36390, Spain.; Sixto, M (通讯作者)，Univ Vigo, Fac Ciencias Mar, Campus Mar, Vigo 36311, Spain.	sixto.marta@gmail.com; pilarriobo@iim.csic.es; francisco.rodriguez@ieo.csic.es; patricio.diaz@ulagos.cl; rosa.figueroa@ieo.csic.es	; Figueroa, Rosa/M-7598-2015; Rodriguez, Francisco/A-5934-2019; Riobo, Pilar/K-1945-2017; Diaz, Patricio/B-8128-2018	Sixto, Marta/0000-0002-7028-7647; Figueroa, Rosa/0000-0001-9944-7993; Rodriguez, Francisco/0000-0002-6918-4771; Riobo, Pilar/0000-0002-1921-6229; Diaz, Patricio/0000-0002-9403-8151	Spanish project BIOTOX [PID2021-125643OB-C22]; EU-INTERREG Atlantic Area project PRIMROSE [EAPA 182/2016]; GAIN grant GRC-VGOHAB from the Innovation Agency (Xunta de Galicia) [IN607A-2019/04]; CCVIEO culture collection of microalgae (IEO Vigo); Spanish project DIANAS under the RETOS Programme (MINECO) [CTM2017-86066-R]; ANID-FONDECYT [1231220]; Centre for Biotechnology and Bioengineering (CeBiB) (ANID, Chile) [FB0001]	Spanish project BIOTOX; EU-INTERREG Atlantic Area project PRIMROSE(Interreg Europe); GAIN grant GRC-VGOHAB from the Innovation Agency (Xunta de Galicia); CCVIEO culture collection of microalgae (IEO Vigo); Spanish project DIANAS under the RETOS Programme (MINECO); ANID-FONDECYT; Centre for Biotechnology and Bioengineering (CeBiB) (ANID, Chile)	This research was funded by the Spanish project BIOTOX (PID2021-125643OB-C22), the EU-INTERREG Atlantic Area project PRIMROSE (EAPA 182/2016), the GAIN grant GRC-VGOHAB IN607A-2019/04 for the Galician Networks of Excellence from the Innovation Agency (Xunta de Galicia), and the CCVIEO culture collection of microalgae (IEO Vigo). Marta Sixto acknowledges the pre-doctoral contract granted by the Spanish project DIANAS (CTM2017-86066-R) under the RETOS Programme (MINECO). Patricio A. Diaz was funded by the ANID-FONDECYT 1231220 and by the Centre for Biotechnology and Bioengineering (CeBiB) (PIA project FB0001, ANID, Chile).	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J	Siebels, A; ten Veen, J; Munsterman, D; Deckers, J; Kasse, C; van Balen, R				Siebels, Alexandra; ten Veen, Johan; Munsterman, Dirk; Deckers, Jef; Kasse, Cornelis; van Balen, Ronald			Miocene sequences and depocentres in the Roer Valley Rift System	BASIN RESEARCH			English	Article							LOWER RHINE BASIN; NORTH-SEA BASIN; DIEST FORMATION; DINOFLAGELLATE CYST; SHORELINE TRAJECTORIES; SEDIMENTARY; EVOLUTION; TERTIARY; BELGIUM; MIDDLE	The Miocene sequence in the Roer Valley Rift System consists of alternating open-to-shallow marine, coastal and fluvio-deltaic deposits. In this study, well logs, bio-chronostratigraphy and seismostratigraphy are used to characterize major units and their bounding unconformities and to infer sediment dispersal patterns. Three major unconformities occur in the sequence: the early, middle and late Miocene unconformities (EMU, MMU and LMU). The EMU formed due to tectonic motions related to the Savian phase. After formation of the EMU, a broad depocentre developed in the south-eastern part of the Roer Valley Graben (RVG). Sediment accumulation increased during this period and peaked in the middle Langhian, after which it diminished again to a low level during the late Serravallian. The decrease in sediment accumulation coincided with a period of tectonic subsidence along the major bounding fault zones (i.e. the Peel Boundary Fault System, the Feldbiss Fault System and the Veldhoven Fault System). The resulting transgression caused sediment starvation in the central RVG. Subsequently, global sea-level fall during the early Tortonian caused large-scale erosion, and formation of incised valleys on the highs adjacent to the RVG (Peel Block and Campine Block), as well as the south-eastern RVG, forming the MMU. However, sedimentation continued during this period in the central part of the RVG where no erosional hiatus developed. From the Tortonian onwards, accumulation rates increased again. The depocentre shifted towards the north-west and clinoforms developed in the RVG. During the latest Miocene, the depocentre was concentrated along the south-western margin of the RVG. Meanwhile, the depositional environment of the entire RVRS gradually shallowed as the LMU was formed. This research presents new insights into the evolution of the Miocene depocentres in the Roer Valley Rift System. A multi-scale approach was used to establish a subdivision of the late Miocene sequence that can be regionally correlated, and further characterize the implications of the 'Mid-Miocene Unconformity'.image	[Siebels, Alexandra; Kasse, Cornelis; van Balen, Ronald] Vrije Univ Amsterdam, Amsterdam, Netherlands; [Siebels, Alexandra; ten Veen, Johan; Munsterman, Dirk] TNO Geol Survey Netherlands, Utrecht, Netherlands; [Deckers, Jef] VITO Flemish Inst Technol Res, Mol, Netherlands	Vrije Universiteit Amsterdam; Netherlands Organization Applied Science Research	Siebels, A (通讯作者)，Vrije Univ Amsterdam, Amsterdam, Netherlands.	alexandra_siebels@hotmail.com	Van Balen, Ronald/A-4275-2010	Van Balen, Ronald/0000-0002-8019-7426; Siebels, Alexandra/0009-0004-8883-8015; Kasse, Cornelis/0000-0002-1466-1016	Geological Survey of the Netherlands (TNO- GDN)	Geological Survey of the Netherlands (TNO- GDN)	Geological Survey of the Netherlands (TNO- GDN)	Adriaens R., 2020, Geologica Belgica, V23, P365; Böhme M, 2012, PLOS ONE, V7, DOI 10.1371/journal.pone.0036817; Boenigk W, 2006, QUATERNARY SCI REV, V25, P550, DOI 10.1016/j.quascirev.2005.01.018; Böhme M, 2003, PALAEOGEOGR PALAEOCL, V195, P389, DOI 10.1016/S0031-0182(03)00367-5; Boogaert H.A. 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JUL	2024	36	4							e12886	10.1111/bre.12886	http://dx.doi.org/10.1111/bre.12886			33	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	YT9B0		hybrid			2025-03-11	WOS:001270844100001
J	Atkinson, M; Normandeau, A; Van Nieuwenhove, N; de Vernal, A; Saunders, M; Woollett, J; Limoges, A				Atkinson, M.; Normandeau, A.; Van Nieuwenhove, N.; de Vernal, A.; Saunders, M.; Woollett, J.; Limoges, A.			Labrador Coastal Current and productivity variations offshore Nain (Nunatsiavut) during the late Holocene	QUATERNARY SCIENCE REVIEWS			English	Article						Paleoceanography; North Atlantic; Labrador sea; Shelf sediments; Sortable silt; Micropaleontology; Dinocysts; Bulk sediment geochemistry	NORTH-ATLANTIC OSCILLATION; SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYSTS; RECENT SEDIMENTS; ORGANIC-CARBON; WATER; PRESERVATION; VARIABILITY; CIRCULATION; RECONSTRUCTION	The Labrador Coastal Current (LCC) transports cold and fresh waters of Arctic origin towards the North Atlantic and has a strong influence on the coastal ecosystems and climate of eastern Canada. Here, we present a multidecadally resolved record of changes in sea -surface and near -bottom conditions of the LCC during the last 3000 years based on the analysis of biogenic tracers (organic -walled dinoflagellate cysts, carbon, and nitrogen geochemistry) and sedimentary content (sortable silt, magnetic susceptibility, elemental ratios) in the upper 2 m of sediments in a core retrieved offshore Nain, Nunatsiavut. Our data reveal multi -centennial bottom flow strength variability in the LCC, with strong linkages to changes in regional ocean circulation patterns. At about 2100- and 550 -years BP, the sedimentological and biogenic tracer data suggest changes in the LCC bottom current intensity (decline and strengthening, respectively) that coincide with shifts in the persistent mode of the North Atlantic Oscillation. Our proxy data suggests increased biological production during the last 500 years compared to the preceding 2500 years, possibly reflecting a gradual decrease length of the sea -ice season. The data show a decline in the LCC strength during periods of increased polar water influence identified in previous palaeoceanographic studies conducted further north, which may be attributed to the trapping of freshwater in sea ice during these periods. Our results highlight the dynamical oceanographic and atmospheric factors that influence the LCC and the coastal ecosystems along its path and confirm that the processes in Baffin Bay impact the Labrador Shelf oceanography.	[Atkinson, M.; Van Nieuwenhove, N.; Limoges, A.] Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB, Canada; [Normandeau, A.] Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [de Vernal, A.] Univ Quebec, Ctr GEOTOP, 201 Ave President Kennedy, Montreal, PQ, Canada; [Saunders, M.] Nunatsiavut Govt, Lands & Nat Resources, Nain, NF, Canada; [Woollett, J.] Univ Laval, Dept Sci Hist, Ctr Etud Nord, Quebec City, PQ, Canada	University of New Brunswick; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; University of Quebec; University of Quebec Montreal; Laval University	Atkinson, M; Limoges, A (通讯作者)，Univ New Brunswick, Dept Earth Sci, 2 Bailey Dr, Fredericton, NB, Canada.	m.atkinson@unb.ca; alimoges@unb.ca	de Vernal, Anne/D-5602-2013	Limoges, Audrey/0000-0002-4587-3417; Atkinson, Margaret/0009-0003-3528-308X	Sentinel North and Institut Nordique du Quebec (Nunat-siavut Coastal Interactions Project); Natural Sciences and Engineering Research Council of Canada (NSERC) [2018-03984]; Marine Geoscience for Marine Spatial Planning of the Geological Survey of Canada; Crown-Indigenous Relations and Northern Affairs Canada (CIRNAC); ArcticNet, a Network of Centres of Excellence in Canada; Canada Foundation for Innovation; NSERC; Swedish Research Council [2018-03984] Funding Source: Swedish Research Council	Sentinel North and Institut Nordique du Quebec (Nunat-siavut Coastal Interactions Project); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Marine Geoscience for Marine Spatial Planning of the Geological Survey of Canada; Crown-Indigenous Relations and Northern Affairs Canada (CIRNAC); ArcticNet, a Network of Centres of Excellence in Canada; Canada Foundation for Innovation(Canada Foundation for InnovationCGIARSpanish Government); NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Swedish Research Council(Swedish Research Council)	We would like to acknowledge the Nunatsiavut Government, the Nunatsiavut Research Centre and the Labrador Inuit of Nain for their guidance on research conducted in traditional Inuit lands. This work was supported by Sentinel North and Institut Nordique du Quebec (Nunatsiavut Coastal Interactions Project) ; Natural Sciences and Engineering Research Council of Canada (NSERC; grant number 2018-03984) ; the Marine Geoscience for Marine Spatial Planning of the Geological Survey of Canada; Crown-Indigenous Relations and Northern Affairs Canada (CIRNAC) and ArcticNet, a Network of Centres of Excellence in Canada. We thank Amundsen Science which is supported by the Canada Foundation for Innovation and NSERC. We thank officers, crew members and scientists for their assistance in the collection of core 2021805-005PC during the 2021 Amundsen Leg 2.	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J	Chafai, K; Hssaida, T; Maatouf, W; Slimani, H; Rjimati, EC; Afenzar, A; Louaya, A; Jaydawi, S; Chakir, S; Khaffou, H				Chafai, Khaoula; Hssaida, Touria; Maatouf, Wafaa; Slimani, Hamid; Rjimati, Ech-charqui; Afenzar, Abdelkrim; Louaya, Abdelkarim; Jaydawi, Soukaina; Chakir, Sara; Khaffou, Hanane			Palynostratigraphy and paleoenvironment of Upper Cretaceous sedimentary deposits from the Tarfaya-Laayoune-Boujdour-Dakhla Basin, southwestern Morocco	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Tarfaya-Laayoune-Boujdour-Dakhla Basin; Lower Turonian; Upper Campanian; lowermost Maastrichtian; Dinoflagellate cyst; Biostratigraphy; Paleoenvironment	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; OCEANIC ANOXIC EVENT; TURONIAN BOUNDARY EVENT; WESTERN EXTERNAL RIF; SEA-LEVEL CHANGE; TERTIARY BOUNDARY; CALCAREOUS NANNOFOSSIL; NORTHERN APENNINES; PALEOGENE BOUNDARY; CHICXULUB IMPACT	Palynological investigations were carried out on Upper Cretaceous sediments from the three onshore sections, Tah, Amma Fatma and Oum Dbaa of the Tarfaya-Laayoune-Boujdour-Dakhla Basin, southwestern Morocco. 64 samples were collected for this palynological study, which yielded a very rich, diverse and well-preserved palynological content, including sporomorphs, prasinophytes, acritarchs, foraminiferal test linings and colonial fresh-water algae, dominated by dinoflagellate cysts comprising 141 species. The dinoflagellate cyst stratigraphic marker events used for the biostratigraphic interpretations include the first and last occurrences of stratigraphic marker species. The dinoflagellate cyst biostratigraphy allowed to assign the Amma Fatma section to the lower Turonian and the Tah section to the upper Campanian. The Oum Dbaa section is revised in detail and re-assigned to the upper Campanian-lowermost Maastrichtian. Analyses of the relative abundances of marine palynomorphs (mainly dinoflagellate cysts), as well as those of the palynofacies (amorphous organic matter, phytoclasts and palynomorphs) indicate two depositional settings alternating between a proximal inner shelf under suboxic-anoxic conditions and an outer neritic environment under dysoxic-anoxic conditions.	[Chafai, Khaoula; Hssaida, Touria; Khaffou, Hanane] Hassan II Univ Casablanca, Fac Sci Ben Msik, Geosci & Applicat Lab, Casablanca, Morocco; [Maatouf, Wafaa] Off Natl Hydrocarbures & Mines, Dept Petr Lab, Rabat, Morocco; [Slimani, Hamid] Mohammed V Univ Rabat, Sci Inst, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Geobiodivers & Nat Patrimony Lab GEOBIO, Rabat, Morocco; [Rjimati, Ech-charqui] Minist Energy Mines Water & Environm, Rabat, Morocco; [Afenzar, Abdelkrim; Louaya, Abdelkarim; Chakir, Sara] Sidi Mohamed Ben Abdellah Univ, Fac Sci Dhar El Mahraz, Geosci Environm & Associated Resources Lab, Fes, Morocco; [Jaydawi, Soukaina] Mohammed V Univ, Geosci Water & Environm Lab, Fac Sci, Rabat, Morocco	Hassan II University of Casablanca; Mohammed V University in Rabat; Sidi Mohamed Ben Abdellah University of Fez; Mohammed V University in Rabat	Chafai, K (通讯作者)，Hassan II Univ Casablanca, Fac Sci Ben Msik, Geosci & Applicat Lab, Casablanca, Morocco.	chafai.khaoula12@gmail.com	Slimani, Hamid/AAL-4055-2020	Abdelkrim, Afenzar/0000-0002-0833-3112			The authors thank the staffs of the Laboratory of Geosciences and Applications (Faculty of Sciences, Ben M ' sik, Casablanca) for their technical assistance. The authors are grateful to the Review of Palae- obotany and Palynology Editor -in -Chief and Associate Editor for handling our manuscript. The authors are also indebted to the reviewers for critical reviews and constructive suggestions which have signifi- cantly improved the manuscript.	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J	Deckers, J; Munsterman, D; DE Koninck, R; Schiltz, M				Deckers, Jef; Munsterman, Dirk; DE Koninck, Roel; Schiltz, Marco			Facies variability of the Lower Miocene Houthalen Member in the southern Genk municipality (northeastern Belgium)	GEOLOGICA BELGICA			English	Article						Bolderberg Formation; Cone Penetration Tests; boreholes; correlations; Eigenbilzen Formation; Albert Canal	BIOSTRATIGRAPHY	The Oligocene Eigenbilzen Formation and Miocene Bolderberg Formation were studied along the Albert Canal in the southern Genk municipality, eastern Belgium. Previous studies have subdivided the Eigenbilzen Formation into geophysical subunits based on borehole logs. Correlations of borehole logs with a deep Cone Penetration Test reveal that this subdivision is also geotechnically distinct. The Eigenbilzen Formation is unconformably overlain by the Houthalen Member (lower Bolderberg Formation), which holds a late Burdigalian age according to the dinoflagellate cyst analyses on borehole samples by this study. The average glauconite, organic and carbonate content of the Houthalen Member in the study area is 8.2%, 0.5% and 3%. Within the Houthalen Member, we distinguished two different geotechnical CPT and lithological facies, herein referred to as clayey and sandy facies. Granulometric analyses indicate that both facies are dominated by fine sands, however, with the sandy facies having an average 5.1% fine fraction (<63 <mu>m), and the clayey facies 18.8%. The clayey facies is very distinct, whereas the sandy facies is geotechnically and granulometrically similar to the superjacent Genk Member (upper Bolderberg Formation). Besides carbonate content, the main difference between the sandy Houthalen Member and the Genk Member is the larger glauconite content of the first. As the glauconite content decreases upwards in the sandy Houthalen Member, it transitions into the Genk Member. Along the 3.6 km long correlation panel, the clayey Houthalen Member thins from over six meters in the southeast towards less than one meter in the northwest, which highlights the sedimentological complexity within the unit.	[Deckers, Jef; DE Koninck, Roel] Flemish Inst Technol Res, VITO, Boeretang 200, Mol, Belgium; [Munsterman, Dirk] TNO Geol Survey Netherlands GSN, POB 80015, NL-3508 TA Utrecht, Netherlands; [Schiltz, Marco] Samsuffit Bv, Eggelstr 8, B-2530 Boechout, Belgium	VITO	Deckers, J (通讯作者)，Flemish Inst Technol Res, VITO, Boeretang 200, Mol, Belgium.	jef.deckers@vito.be; dirk.munsterman@tno.nl; roel.dekoninck@vito.be; marco@samsuffit.be		Munsterman, Dirk/0000-0003-1774-4615; Deckers, Jef/0000-0002-5373-8733; De Koninck, Roel/0000-0001-8795-8016				Adriaens R., 2015, THESIS KU LEUVEN LEU; De Man E, 2010, EPISODES, V33, P3; Deckers J, 2022, GEOL BELG, DOI 10.20341/gb.2022.002; Deckers J, 2022, GEOL J, V57, P2129, DOI 10.1002/gj.4384; Deckers J, 2020, GEOL BELG, V23, P323, DOI 10.20341/gb.2020.017; Deckers J, 2019, GEOL MAG, V156, P525, DOI 10.1017/S0016756817000991; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Everaert S, 2020, GEOL BELG, V23, P167, DOI 10.20341/gb.2020.025; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Halet F., 1936, Bulletin de la Societe belge de Geologie, de Paleontologie et dHydrologie, V46, P194; Halet P., 1935, BOREHOLE DESCRIPTION; Halet P., 1936, BOREHOLE DESCRIPTION; Janssen N, 2008, SAMPLE PROCESSING PR; Köthe A, 2007, Z DTSCH GES GEOWISS, V158, P287, DOI 10.1127/1860-1804/2007/0158-0287; Kothe A., 2003, REV PALEOBIOL, V22, P895; Lengkeek HJ, 2022, CONE PENETRATION TES, P503, DOI [10.1201/9781003308829-71, DOI 10.1201/9781003308829-71]; Louwye S, 2005, GEOL J, V40, P441, DOI 10.1002/gj.1021; Louwye S, 2020, GEOL BELG, V23, P137, DOI 10.20341/gb.2020.010; Louwye S, 2010, GEOL BELG, V13, P269; Matthijs J., 1999, TOELICHTINGEN BIJ GE; Munsterman DK, 2024, NETH J GEOSCI, V103, DOI 10.1017/njg.2024.10; Munsterman DK, 2022, NETH J GEOSCI, V101, DOI 10.1017/njg.2022.3; Munsterman DK, 2020, GEOL BELG, V23, P127, DOI 10.20341/gb.2020.007; Munsterman DK, 2019, NETH J GEOSCI, V98, DOI 10.1017/njg.2019.10; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; Ogg JG, 2016, CONCISE GEOLOGIC TIME SCALE 2016, P1; Powell A.J., 1992, P155; Robertson K.P., 2010, 2nd International Symposium on Cone Penetration Testing, V2, P2; ROBERTSON PK, 1990, CAN GEOTECH J, V27, P151, DOI 10.1139/t90-014; Schiltz M, 2020, GEOL BELG, V23, DOI 10.20341/gb.2020.019; Van Adrichem Boogaert A.H., 1993, MEDEDELINGEN RIJKS G, V50; Van Simaeys S, 2005, REV PALAEOBOT PALYNO, V134, P105, DOI 10.1016/j.revpalbo.2004.12.003; Vandenberghe N., 2001, AARDKUNDIGE MEDEDELI, V11, P69; Vandenberghe N., 2023, Lithostratigraphic Information Sheets Rupel Group; Vandenberghe N., 2020, GEOL BELG, V23; Vandenberghe N., 1978, KLASSE WETENSCHAPPEN, V40/147	36	0	0	0	0	Geologica Belgica Luxemburga Scientia & Professionis	BRUSSELS	JENNER STREET 13, BRUSSELS, BELGIUM	1374-8505	2034-1954		GEOL BELG	Geol. Belg.		2024	27	1-2					33	46		10.20341/gb.2024.003	http://dx.doi.org/10.20341/gb.2024.003		JUN 2024	14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	WO0R9		gold			2025-03-11	WOS:001253221100001
J	García-Moreiras, I; Amorim, A; Zonneveld, K				Garcia-Moreiras, Iria; Amorim, Ana; Zonneveld, Karin			Transport and preservation of calcareous and organic-walled dinoflagellate cysts off Cape Blanc (NW africa) in relation to nepheloid layers	MARINE ENVIRONMENTAL RESEARCH			English	Article						Dinoflagellate cysts; Organic-walled cysts; Calcareous cysts; Nepheloid layers; Advection; Offshore environments; NW African upwelling	SURFACE SEDIMENTS; GYMNODINIUM-CATENATUM; UPWELLING SYSTEM; PARTICLE DISTRIBUTION; ENVIRONMENTAL-CHANGE; MARINE-SEDIMENTS; ATLANTIC-OCEAN; RESTING STAGES; ARABIAN SEA; DINOPHYCEAE	Our understanding of dinoflagellates' present-day and past ecology is limited due to the scarcity of data on the transport of dinoflagellate cysts in oceanic environments. Previous studies have shown that lateral transport affects the source-to-sink trajectory of cysts in the very productive region off Cape Blanc (NW Africa). Unsolved questions remain, such as: how far these cysts can be advected, whether the cyst sources vary over time and whether lateral transport is a permanent feature or restricted to individual events. To fill these gaps and assess the role of nepheloid layers on the lateral transport and preservation of dinoflagellate cysts, new data on dinoflagellate cyst distributions in the water column and sediments along a land-sea transect were obtained. Samples were collected in November 2018 along a shelf break-offshore transect during intense upwelling, notably, within and between the nepheloid layers. The composition and abundance of cysts with organic walls in the water column and surface sediments were studied. Moreover, the distribution of calcareous cysts was also analysed in the water samples, using non-destructive acid-free preparation methods. The records were dominated by empty cysts, but no clear indications that these originated from local resuspension of older sediments were observed. Clustering, principal component analysis and redundant discriminant analysis were used to compare cyst assemblages in the water column and surface sediments, and environmental conditions in the upper water column. The strong similarity in species composition of water samples collected in the active upwelling region to those collected from the more onshore parts of the Benthic Nepheloid Layer (BNL), upper Intermediate Nepheloid Layer (INL) (similar to 1000 m depth) and lower INL (similar to 2200 m depth) indicated that lateral transport of cysts within these NLs occurred until about similar to 110 km from the shelf break. Cyst assemblages from above and below these NLs showed significantly different taxa composition reinforcing the role of NLs in the lateral advection of cysts. In the more offshore stations, vertically similar cyst assemblages were observed in the same station, independent of the sample depth, within or between the NLs, which supported that at these stations vertical transport was the dominant process influencing cyst assemblages. Consequently, the cyst signal in sediments off Cape Blanc may be affected both by horizontal transport of allochthonous cysts and vertical deposition of locally-produced cysts, particularly in the more offshore stations (>2000 m depth). Despite lateral transport and possible species-specific preservation effects, horizontal distributions of most cyst taxa in the water column and the surface sediments could be explained to a great extent by the main environmental gradients in the upper water column. This agrees with observations made in other regions, and reinforces that dinoflagellate cysts as good proxies to reconstruct past environmental conditions in offshore environments. New data on dinoflagellate cyst distribution, transport and accumulation patterns in deep environments off Cape Blanc may be useful for interpreting past environmental signals in the region. This is particularly relevant regarding calcareous cysts, as information on their distribution and ecology is very scarce. The present work contributes to a better understanding of the dispersal patterns of dinoflagellate cysts in the deep ocean, highlighting the significant role played by nepheloid layers in this process and thus on the dinoflagellate cyst signature in deep-sea sediments.	[Garcia-Moreiras, Iria] Univ Vigo, Ctr Invest Marina CIM, Fac Ciencias, Campus As Lagas Marcosende, Vigo 36310, Spain; [Garcia-Moreiras, Iria] Univ Vigo, Dept Biol Vexetal & Ciencias Solo, Vigo 36310, Spain; [Amorim, Ana] Univ Lisbon, Fac Ciencias, Ctr Ciencias Mar & Ambiente MARE, Aquat Res Network ARNET, P-1749016 Lisbon, Portugal; [Amorim, Ana] Univ Lisbon, Fac Ciencias, Dept Biol Vegetal, P-1749016 Lisbon, Portugal; [Zonneveld, Karin] Zentrum Marine Umweltwissensch Univ Bremen MARUM, Leobener Str 8, D-28359 Bremen, Germany; [Zonneveld, Karin] Univ Bremen, Geosci Dept, Klagenfurter Str, D-28359 Bremen, Germany	Universidade de Vigo; Universidade de Vigo; Universidade de Lisboa; Universidade de Lisboa; University of Bremen	García-Moreiras, I (通讯作者)，Univ Vigo, Ctr Invest Marina CIM, Fac Ciencias, Campus As Lagas Marcosende, Vigo 36310, Spain.	iriagamo@uvigo.es	GARCIA-MOREIRAS, IRIA/H-4627-2015	GARCIA-MOREIRAS, IRIA/0000-0001-8713-0374	Deutsche Forschungsgemeinschaft, Germany [Mer/Met: 17-87]; Xunta de Galicia, Spain [ED481B-2019-074]; FCT: Fundacao para a Ciencia e a Tecnologia (Portugal) [UIDB/04292/2020, UIDP/04292/2020, LA/P/0069/2020]; Universidade de Vigo/CISUG, Spain	Deutsche Forschungsgemeinschaft, Germany(German Research Foundation (DFG)); Xunta de Galicia, Spain(Xunta de Galicia); FCT: Fundacao para a Ciencia e a Tecnologia (Portugal)(Fundacao para a Ciencia e a Tecnologia (FCT)); Universidade de Vigo/CISUG, Spain	This work was a contribution to the project: Marine carbon pro- duction, export, relocation and degradation under varying ocean redox conditions off NW Africa (MACPEI), funded by the Deutsche Forschungsgemeinschaft [Mer/Met: 17-87] , Germany. Iria Garcia-Moreiras was supported by a postdoctoral fellowship from Xunta de Galicia (ED481B-2019-074, 2019), Spain. Ana Amorim was supported by FCT: Fundacao para a Ciencia e a Tecnologia (Portugal) through the strategic projects UIDB/04292/2020 and UIDP/04292/2020 awarded to MARE and through project LA/P/0069/2020 granted to the Associate Laboratory ARNET". Funding for open access charge was provided by Universidade de Vigo/CISUG, Spain. We would also like to thank the two anonymous reviewers for their insightful comments and suggestions.	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JUL	2024	199								106577	10.1016/j.marenvres.2024.106577	http://dx.doi.org/10.1016/j.marenvres.2024.106577		JUN 2024	23	Environmental Sciences; Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Toxicology	WL8P6	38878348	hybrid			2025-03-11	WOS:001255119300001
J	Hansen, G; Tolstrup, L; Petersen, G; Maguet, R; Madsen, T				Hansen, Gert; Tolstrup, Lea; Petersen, Gitte; Maguet, Remi; Madsen, Torben			Viability assessed with the most probable number dilution culture method after chemical treatment of ballast water reveals the presence of false negatives from an approved vital stain method	MARINE POLLUTION BULLETIN			English	Article						Ballast water; Chlorination; BWMS; CMFDA/FDA; MPN; Vital stain	EXAMINE DNA CONCENTRATION; CELL-PROLIFERATION ASSAY; VIABLE PHYTOPLANKTON; APPLICABILITY; UV; ORGANISMS; TRANSPORT; CYSTS	The present study compares the CMFDA/FDA + motility- and the Most Probable Number (MPN) Dilution Culture + Motility methods for testing the viability of >= 10-<50 mu m organisms in chlorine treated ballast water. The results of both methods were within the regulatory compliance criterion <10 organisms/mL, but the MPNmethod revealed that growth-outs did occur. While the CMFDA/FDA method showed <0.5 organisms/mL, the MPN-method gave approx. 6 organisms/mL. This demonstrated that false negatives, i.e. living but not stained organisms, may occur when using the CMFDA/FDA-method for compliance testing of chemical treated ballast water. Organisms surviving the treatment were primarily the dinoflagellate Scrippsiella sp. and various coccoid chlorophytes present in a brackish- and freshwater test, respectively. It is suggested that their resilience to the chemical treatment is the ability to transform into a temporary cyst (Scrippsiella sp.) or the presence of a chemical resistant cell wall (certain chlorophytes).	[Hansen, Gert; Tolstrup, Lea; Petersen, Gitte; Madsen, Torben] DHI, Agern Alle 5, DK-2970 Horsholm, Denmark; [Hansen, Gert] Univ Copenhagen, Dept Biol, Marine Biol Sect, Univ Pk 4, DK-2100 Copenhagen O, Denmark	Danish Hydraulic Institute (DHI); University of Copenhagen	Hansen, G (通讯作者)，DHI, Agern Alle 5, DK-2970 Horsholm, Denmark.	geha@dhigroup.com						[Anonymous], 2012, Federal Register, V77; [Anonymous], 2004, International Convention for the Control and Management of Ships' Ballast Water and Sediments; Batista WR, 2017, ENVIRONMENTS, V4, DOI 10.3390/environments4030054; Beddow D.G., 1966, Master Thesis; BENTLEYMOWAT JA, 1982, BOT MAR, V25, P203; Blatchley ER, 2018, ENVIRON SCI TECHNOL, V52, P8075, DOI 10.1021/acs.est.8b00341; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Casas-Monroy O, 2016, J APPL PHYCOL, V28, P2821, DOI 10.1007/s10811-016-0798-3; Cullen J.J., 2019, Zenodo, DOI [10.5281/zenodo.2656597, DOI 10.5281/ZENODO.2656597]; Cullen JJ, 2018, SCI TOTAL ENVIRON, V627, P1602, DOI 10.1016/j.scitotenv.2018.01.302; Cullen JJ, 2016, J APPL PHYCOL, V28, P279, DOI 10.1007/s10811-015-0601-x; Dang K., 2004, GloBallast Monograph Series, V15, P103; EPA, 2010, EPA600R10146 NSF INT; Fistarol GO, 2004, ENVIRON MICROBIOL, V6, P791, DOI 10.1111/j.1462-2920.2004.00609.x; Frazier M, 2013, ECOL APPL, V23, P339, DOI 10.1890/11-1639.1; Garvey M, 2007, MAR ECOL PROG SER, V352, P17, DOI 10.3354/meps07134; Gregg Matthew, 2009, Aquatic Invasions, V4, P521, DOI 10.3391/ai.2009.4.3.14; Guney Ceren Bilgin, 2022, Marine Science and Technology Bulletin, V11, P397, DOI 10.33714/masteb.1162688; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hansen G., 2018, SUSSWASSERFLORA MITT, VXII, P39; Hansen G., 2023, Mar. 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Pollut. Bull.	AUG	2024	205								116586	10.1016/j.marpolbul.2024.116586	http://dx.doi.org/10.1016/j.marpolbul.2024.116586		JUN 2024	7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	WM0Z5	38878418				2025-03-11	WOS:001255181800001
J	Zheng, XM; Lin, L; Xue, MY; Wang, Q; Wang, J; Wu, HX				Zheng, Xuming; Lin, Ling; Xue, Muyang; Wang, Qiong; Wang, Jian; Wu, Huixian			Study on the diversity and germination of dinoflagellate cysts in the sediments of foreign ships in Shanghai Port	MARINE POLLUTION BULLETIN			English	Article						Ballast water; Dinoflagellate cyst; Germination; Shanghai Port; Sediments in ports	BALLAST WATER; RESTING CYSTS; TRANSPORT; VIABILITY; VESSELS; COAST	The dinoflagellate cysts present in the ballast water sediment of foreign ships in Shanghai Port have not been previously studied. Therefore, sediment samples were collected from the ballast water of 16 foreign ships in Shanghai Port, and the types of dinoflagellate cysts were identified and their abundance was calculated, with a specific focus on the analysis of toxic and harmful dinoflagellates. Moreover, simulations of temperature and salinity conditions throughout the year in the Shanghai port waters were conducted to carry out dinoflagellate cyst germination experiments, with analyze and compare the germinated dinoflagellate cysts under different conditions. Dinoflagellate cysts were found in 100 % of the ship sediment samples, including a total of 9 species of toxic and harmful dinoflagellate cysts. In the germination experiment, 15 degrees C was found to be the optimal temperature for the germination of dinoflagellate cysts in ballast water sediment, and high salinity is more favorable for cyst germination.	[Zheng, Xuming; Lin, Ling; Wang, Qiong; Wu, Huixian] Shanghai Ocean Univ, Coll Oceanog & Ecol Sci, 999th Huchenghuan Rd, Shanghai 201306, Peoples R China; [Xue, Muyang; Wu, Huixian] Hong Kong Univ Sci & Technol, Kowloon, Clear Water Bay, Hong Kong 999077, Peoples R China; [Lin, Ling; Wang, Jian] Cosco Shipping Heavy Ind Technol Weihai Co Ltd, Weihai 264203, Peoples R China	Shanghai Ocean University; Hong Kong University of Science & Technology	Wu, HX (通讯作者)，Shanghai Ocean Univ, Coll Oceanog & Ecol Sci, 999th Huchenghuan Rd, Shanghai 201306, Peoples R China.	hxwu@shou.edu.cn	Wu, Huixian/N-6353-2014					Bailey SA, 2003, LIMNOL OCEANOGR, V48, P1701, DOI 10.4319/lo.2003.48.4.1701; Casas-Monroy O, 2011, AQUAT INVASIONS, V6, P231, DOI 10.3391/ai.2011.6.3.01; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Hofmann EE, 2021, HARMFUL ALGAE, V107, DOI 10.1016/j.hal.2021.102064; Hulsmann N., 2002, Protists-A Dominant Component of the BallastTransported Biota, DOI [10.1007/978-94-015-9956-63, DOI 10.1007/978-94-015-9956-63]; Karlson B, 2021, HARMFUL ALGAE, V102, DOI 10.1016/j.hal.2021.101989; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Li Dacheng, 2019, Fisheries Science (Liaoning), V38, P545; Li DR, 2023, OCEAN COAST MANAGE, V234, DOI 10.1016/j.ocecoaman.2022.106474; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Pertola S, 2006, MAR POLLUT BULL, V52, P900, DOI 10.1016/j.marpolbul.2005.11.028; Ricciardi A, 2000, TRENDS ECOL EVOL, V15, P62, DOI 10.1016/S0169-5347(99)01745-0; Ruiz GM, 2000, NATURE, V408, P49, DOI 10.1038/35040695; Shen Renjie, 2017, China Manag. Inform., V20, P115; Su Yuping, 2015, Acta Ecol. Sin., V36, P2875, DOI [10.13671/j.hjkxxb.2014.1082, DOI 10.13671/J.HJKXXB.2014.1082]; Wang Dou, 2019, Mar. Econ., V9, P29, DOI [10.19426/j.cnki.cn12-1424/p.2019.01.004, DOI 10.19426/J.CNKI.CN12-1424/P.2019.01.004]; Xiang JY, 2023, MANAG BIOL INVASION, V14, P178, DOI 10.3391/mbi.2023.14.1.10	19	0	0	6	11	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	AUG	2024	205								116566	10.1016/j.marpolbul.2024.116566	http://dx.doi.org/10.1016/j.marpolbul.2024.116566		JUN 2024	10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	WT0I3	38875971				2025-03-11	WOS:001257003200001
J	Li, RX; Deng, YY; Shang, LX; Liu, YY; Tao, Z; Chai, ZY; Tang, YZ				Li, Ruoxi; Deng, Yunyan; Shang, Lixia; Liu, Yuyang; Tao, Zhe; Chai, Zhaoyang; Tang, Ying Zhong			Evidence for the production of asexual resting cysts in a free-living species of Symbiodiniaceae (Dinophyceae)	HARMFUL ALGAE			English	Article						Asexual resting cyst; Effrenium voratum; Fluorescence in situ hybridization (fish); Life cycle; Single -cyst PCR sequencing	ALEXANDRIUM DINOPHYCEAE; PHYLOGENETIC ANALYSIS; GONYAULAX-TAMARENSIS; CORAL-REEFS; LIFE-CYCLE; DINOFLAGELLATE; IDENTIFICATION; ZOOXANTHELLAE; MORPHOLOGY; CARBON	Coral reef ecosystems are the most productive and biodiverse marine ecosystems, with their productivity levels highly dependent on the symbiotic dinoflagellates belonging to the family Symbiodiniaceae. As a unique life history strategy, resting cyst production is of great significance in the ecology of many dinoflagellate species, those HABs-causing species in particular, however, there has been no confirmative evidence for the resting cyst production in any species of the family Symbiodiniaceae. Based on morphological and life history observations of cultures in the laboratory and morpho-molecular detections of cysts from the marine sediments via fluorescence in situ hybridization (FISH), cyst photography, and subsequent singe -cyst PCR sequencing, here we provide evidences for the asexual production of resting cysts by Effrenium voratum , the free-living, red tide -forming, and the type species of the genus Effrenium in Symbiodiniaceae. The evidences from the marine sediments were obtained through a sequential detections: Firstly, E. voratum amplicon sequence variants (ASVs) were detected in the cyst assemblages that were concentrated with the sodium polytungstate (SPT) method from the sediments collected from different regions of China Seas by high -throughput next generation sequencing (NGS); Secondly, the presence of E. voratum in the sediments was detected by PCR using the species -specific primers for the DNA directly extracted from sediment; Thirdly, E. voratum cysts were confirmed by a combined approach of FISH using the species -specific probes, light microscopic (LM) photography of the FISH -positive cysts, and a subsequent single -cyst PCR sequencing for the FISH -positive and photographed cysts. The evidences from the laboratory -reared clonal cultures of E. voratum include that: 1) numerous cysts formed in the two clonal cultures and exhibited a spherical shape, a smooth surface, absence of ornaments, and a large red accumulation body; 2) cysts could maintain morphologically intact for a storage of two weeks to six months at 4 degrees C in darkness and of which 76 -92 % successfully germinated through an internal development processes within a time period of 3 -21 days after being transferred back to the normal culturing conditions; 3) two or four germlings were released from each cyst through the cryptopylic archeopyle in all cysts with continuous observations of germination processes; and 4) while neither sexual mating of gametes nor planozygote (cells with two longitudinal flagella) were observed, the haploidy of cysts was proven with flow cytometric measurements and direct LM measurements of fluorescence from cells stained with either propidium iodide (PI) or DAPI, which together suggest that the cysts were formed asexually. All evidences led to a conclusion that E. voratum is capable of producing asexual resting cysts, although its sexuality cannot be completely excluded, which guarantees a more intensive investigation. This work fills a gap in the knowledge about the life cycle, particularly the potential of resting cyst formation, of the species in Symbiodiniaceae, a group of dinoflagellates having unique life forms and vital significance in the ecology of coral reefs, and may provide novel insights into understanding the recovery mechanisms of coral reefs destructed by the global climate change and suggest various forms of resting cysts in the cyst assemblages of dinoflagellates observed in the field sediments, including HABs-causing species.	[Li, Ruoxi; Deng, Yunyan; Shang, Lixia; Liu, Yuyang; Tao, Zhe; Chai, Zhaoyang; Tang, Ying Zhong] Chinese Acad Sci Qingdao, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Deng, Yunyan; Shang, Lixia; Tang, Ying Zhong] Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266237, Shandong, Peoples R China; [Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Li, Ruoxi; Tao, Zhe] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Chai, ZY; Tang, YZ (通讯作者)，Chinese Acad Sci Qingdao, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266237, Shandong, Peoples R China.; Chai, ZY; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	zhaoyangchai@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	Tao, Zhe/LIG-2380-2024; Chai, Zhaoyang/F-7485-2017; Li, Ruoxi/GWN-1740-2022; Li, Yang/KFB-5350-2024		Field Stations of the Chinese Academy of Science [KFJ-SW-YW047]	Field Stations of the Chinese Academy of Science	We are grateful of Dr. Zhangxi Hu for the collection of sediment samples, Professor Ning Xu from Jinan University, Guangzhou, China, for the provision of the culture SJNU, and the two anonymous re-viewers' constructive comments and suggestions for our work. This research was supported by the Science and Technology Innovation Project of Laoshan Laboratory (Grant No. LSKJ202203700) , the Science & Technology Basic Resources Investigation Program of China (Grant No. 2018FY100200) , and the Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science (Grant No. KFJ-SW-YW047) .r Field Stations of the Chinese Academy of Science (Grant No. KFJ-SW-YW047) .	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J	Holdgate, GR; Sluiter, IRK; Clowes, CD; Reichgelt, T; Frieling, J				Holdgate, Guy R.; Sluiter, Ian R. K.; Clowes, Chris D.; Reichgelt, Tammo; Frieling, Joost			The Paleocene- Eocene mangroves of southeastern Australia: spatial and temporal occurrences across four geological basins	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						SE Australia; PETM; Palynology; Mangroves; Paleocene-Eocene palaeoclimates	THERMAL MAXIMUM PETM; TEMPERATURE EVOLUTION; OCEAN ACIDIFICATION; SOUTHWEST PACIFIC; CLIMATE; RECONSTRUCTIONS; ASSEMBLAGES; TRANSITION; VEGETATION; BOUNDARY	The advent of the Paleocene-Eocene Thermal Maximum (PETM), a similar to 200 kyr period of global warming ca. 56 Ma, caused sea-levels to rise, transgressing near-coastal environments in southeastern (SE) Australia over >55,000 km(2). During the PETM, warming tropical climates may have extended south to >= 60 S-degrees paleolatitude. The PETM in SE Australia is corroborated primarily by stable carbon isotope chemostratigraphy and detailed palynology records in four geological basins. Previous work showed that, in addition to the globally recognised carbon isotope excursion, the PETM interval in coastal SE Australia can be identified using the dual occurrence of the tropical mangrove Nypa palm pollen ( Spinizonocolpites prominatus ) accompanied by thermophilic marine dinoflagellate cysts (mainly Apectodinium hyperacanthum ). We here document a total of twenty-six Gippsland Basin wells that record this Nypa - A.hyperacanthum association in the earliest Eocene Kingfish Formation (Lower Malvacipollis diversus Zone). In the Bass Basin, eight wells record Nypa-A.hyperacanthum association within the Eastern View Group basal Koorkah Formation, or lower part of the Lower M. diversus Zone (earliest Eocene). In the Bass Basin a further thirteen wells with Nypa occurrences near the top of the Cormorant Formation are found, which might be associated with the longer -term warmth of the Early Eocene Climatic Optimum (EECO, similar to 53-49 Ma). Government bores and petroleum wells across the Otway Basin record the Nypa-A. hyperacanthum PETM association within the Pember Mudstone Lower M. diversus Zone in twenty-one bores. Nine horizons with Nypa occurrences occur within the Burrungule Member (EECO) at the top of the Dilwyn Formation. In western Tasmania, Nypa occurs in the Sorell Basin and Macquarie Harbour area within the Lower M. diversus Zone. Together, these observations show the remarkable extent of the mangrove-coasts that were established across the mid-high paleolatitudes in SE Australia during the warmest intervals of the Cenozoic, the PETM and EECO.	[Holdgate, Guy R.] Geotrack Int P L, 11 Tullamarine Pk Rd, Tullamarine, Vic, Australia; [Sluiter, Ian R. 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J	Premathilake, R; Herath, J				Premathilake, Rathnasiri; Herath, Jayani			A record of late Holocene sea level and human impacts from the southeastern Coast of Sri Lanka	PALYNOLOGY			English	Article						Holocene; lagoon; mangrove; pollen; sea level; sediment; Sri Lanka	INDIAN-OCEAN TSUNAMI; MEKONG RIVER DELTA; ENVIRONMENTAL-CHANGES; SOUTHWEST COAST; MANGROVE ECOSYSTEM; WESTERN INDIA; SHELL-MIDDEN; EAST-COAST; CLIMATE; VEGETATION	AMS radiocarbon-dated palynological evidence from Embilikala Lagoon in Bundala National Park (one of the Ramsar wetland sites) on the southeast coast of Sri Lanka indicates palaeoenvironmental changes during the last 2,700 years. The persistence of fewer mangroves (eg Rhizophoraceae taxa) suggests that sea level low stands occurred between 2,700 and 1750 cal yr BP. From the later age, the relative sea level rose, and reached the present sea level at 950 cal yr BP as indicated by the mangrove maximum. At 2,250, 700-400 and 200-150 cal yr BP, the sudden increase in marine dinoflagellate cysts (eg Spiniferites mirabilis) and foraminifera (Globigerinoides ruber) suggests increased marine influence. This is consistent with a decrease in mangrove habitats. Between 2,700 and 950 cal yr BP, severely degraded dry monsoon forests and minimal levels mangrove suggest human and marine influences were the critical drivers for changing the major vegetation types along the southeastern coast. Vegetation changes have been drastic over the last millennia.	[Premathilake, Rathnasiri] Univ Kelaniya, Postgrad Inst Archaeol, 407 Bauddhaloka Mawatha, Colombo 7, Sri Lanka; [Herath, Jayani] Univ Sri Jayewardenepura, Dept Geog, Nugegoda, Sri Lanka; [Herath, Jayani] Queensland Univ Technol, Sch Architecture & Built Environm, Brisbane, Australia	University Kelaniya; Postgraduate Institute of Archaeology (PGIA); University Sri Jayewardenepura; Queensland University of Technology (QUT)	Premathilake, R (通讯作者)，Univ Kelaniya, Postgrad Inst Archaeol, 407 Bauddhaloka Mawatha, Colombo 7, Sri Lanka.	premathilake@hotmail.com			Faculty of Graduate Studies and the Chairperson of the Research Council of the University of Sri Jayewardenepura [ASP/01/RE/HSS/2019/05]	Faculty of Graduate Studies and the Chairperson of the Research Council of the University of Sri Jayewardenepura	This study was funded by Faculty of Graduate Studies and the Chairperson of the Research Council of the University of Sri Jayewardenepura (Research Grant No ASP/01/RE/HSS/2019/05)	Adikaram A. 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J	Dzhembekova, N; Zlateva, I; Rubino, F; Belmonte, M; Doncheva, V; Popov, I; Moncheva, S				Dzhembekova, Nina; Zlateva, Ivelina; Rubino, Fernando; Belmonte, Manuela; Doncheva, Valentina; Popov, Ivan; Moncheva, Snejana			Spatial distribution models and biodiversity of phytoplankton cysts in the Black Sea	NATURE CONSERVATION-BULGARIA			English	Article						Black Sea; cyst assemblages; habitat suitability; harmful algal blooms; MaxEnt; potentially toxic phytoplankton	SURFACE SEDIMENTS; DINOFLAGELLATE CYSTS; MAXIMUM-ENTROPY; ENVIRONMENTAL-FACTORS; SPECIES DISTRIBUTION; RESTING STAGES; WEST-COAST; BAY; ALEXANDRIUM; ASSEMBLAGES	The current study employed diverse statistical and machine learning techniques to investigate the biodiversity and spatial distribution of phytoplankton cysts in the Black Sea. The MaxEnt distribution modeling technique was used to forecast the habitat suitability for the cysts of three potentially toxic microalgal taxa (Lingulodinium polyedra, Polykrikos hartmannii, and Alexandrium spp.). The key variables controlling the habitat suitability of Alexandrium spp. and L. polyedra were nitrates and temperature, while for the P. hartmannii cysts, nitrates and salinity. The region with the highest likelihood of L. polyedra cyst occurrence appears to be in the western coastal and shelf waters, which coincides with the areas where L. polyedra red tides have been documented. The projected habitat suitability of the examined species partially overlapped, perhaps as a result of their cohabitation within the phytoplankton community and shared preferences for specific environmental conditions, demonstrating similar survival strategies. The nor th-western region of the Black Sea was found to be the most suitable environment for the studied potentially toxic species, presumably posing a greater risk for the onset of blooming events. Two distinct aspects of cysts' ecology and settlement were observed: the dispersal of cysts concerns their movement within the water column from one place to another prior to settling, while habitat suitability pertains to the particular environment required for their survival, growth, and germination. Therefore, it is crucial to validate the model in order to accurately determine a suitable habitat as well as understand the transportation patterns linked to the particular hydrodynamic properties of the water column and the distinct features of the local environment.	[Dzhembekova, Nina; Zlateva, Ivelina; Doncheva, Valentina; Popov, Ivan; Moncheva, Snejana] Bulgarian Acad Sci, Inst Oceanol Fridtjof Nansen, Parvi May 40, Varna, Bulgaria; [Rubino, Fernando; Belmonte, Manuela] Natl Res Council CNR IRSA, Water Res Inst, Via Roma 3, I-74123 Taranto, Italy	Bulgarian Academy of Sciences; Consiglio Nazionale delle Ricerche (CNR); Istituto di Ricerca sulle Acque (IRSA-CNR)	Zlateva, I (通讯作者)，Bulgarian Acad Sci, Inst Oceanol Fridtjof Nansen, Parvi May 40, Varna, Bulgaria.	ibikarska@yahoo.com	BELMONTE, MANUEL/LOR-8246-2024; Rubino, Fernando/GOP-0332-2022; Popov, Ivan/AFR-1234-2022; Dzhembekova, Nina/HTN-3019-2023; Belmonte, Manuel/H-1845-2015	Popov, Ivan/0000-0002-2012-3628; Dzhembekova, Nina/0000-0001-9620-6422; Rubino, Fernando/0000-0003-2552-2510; Belmonte, Manuel/0000-0001-6668-6920	National Science Fund, Ministry of Education and Science (MES), Bulgaria [DN01/8]; Ministry of Education and Sciences of Bulgaria through the National Roadmap for Scientific Infrastructure [D01-164/28.07.2022]	National Science Fund, Ministry of Education and Science (MES), Bulgaria; Ministry of Education and Sciences of Bulgaria through the National Roadmap for Scientific Infrastructure	This study was supported by the National Science Fund, Ministry of Education and Science (MES), Bulgaria, under the project "Phytoplankton cysts: an intricacy between a "memory" or a "potential" for Black Sea biodiversity and algal blooms" (Grant number DN01/8, 16.12.2016) and by the Contract No D01-164/28.07.2022 (project "National Geoinformation Center (NGIC) " financed by the Ministry of Education and Sciences of Bulgaria through the National Roadmap for Scientific Infrastructure 2020-2027.	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Conserv.-Bulgaria	JUN 4	2024		55					269	296		10.3897/natureconservation.55.121181	http://dx.doi.org/10.3897/natureconservation.55.121181			28	Biodiversity Conservation	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation	XJ2S6		gold			2025-03-11	WOS:001261257300001
J	Marret, F; de Vernal, A				Marret, Fabienne; de Vernal, Anne			Dinoflagellate cysts as proxies of environmental, ocean and climate changes in the Atlantic realm during the quaternary	FRONTIERS IN ECOLOGY AND EVOLUTION			English	Review						sea-surface conditions; palaeoproductivity; biostratigraphy; palaeoecology; palaeoceanography	SEA-SURFACE CONDITIONS; LAST GLACIAL MAXIMUM; NORTHERN NORTH-ATLANTIC; WATER CONDITIONS; ARCTIC-OCEAN; ACRITARCH BIOSTRATIGRAPHY; PALYNOMORPH DISTRIBUTION; DINOCYST ASSEMBLAGES; PRIMARY PRODUCTIVITY; EQUATORIAL ATLANTIC	Over the last four decades, organic-walled dinoflagellate cysts have shown high potential as tracers of past sea-surface conditions during the Quaternary. These microfossils relate to the pelagic productivity of both phototrophic and heterotrophic protist organisms and are recovered in high numbers in almost all marine environment settings from the nearshore and estuarine systems to the distal continental margin. In polar environments, where other conventional proxies are rare or absent, dinoflagellate cysts showed a relatively high diversity of species and a close relationship with sea-ice cover duration, winter and summer temperature, and salinity, enabling quantitative reconstructions of several oceanic variables over time. From the temperate to the tropical latitudes of the Atlantic Ocean, their modern distribution highlights a response to primary productivity and seasonal contrasts in surface temperature. They also have proven that they could be used as tracers of eutrophication in stratified systems and can also highlight human impact on their distribution. In this paper, we present an overview of dinoflagellate cysts as ecological tracers in recent and past sediments of the Atlantic Ocean, from the Arctic to the Antarctic. We provide examples of their use as proxies in paleoclimatic-palaeoceanographic studies at glacial to interglacial time scales, with emphasis on the last ice age to recent (last 25 kyr), the northern North Atlantic and western-eastern tropic North Atlantic. We also discuss their potential as tracers of anthropogenic stress in coastal environments.	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JUN 4	2024	12								1378931	10.3389/fevo.2024.1378931	http://dx.doi.org/10.3389/fevo.2024.1378931			22	Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	UN7J8		gold			2025-03-11	WOS:001248801500001
J	Shang, XM; Yang, S; Sun, J				Shang, Xiaomei; Yang, Shuang; Sun, Jun			Succession of phytoplankton communities from macro-scale to micro-scale in coastal waters of Qinhuangdao, China	FRONTIERS IN MARINE SCIENCE			English	Article						scallop farming; phytoplankton community; cryptophytes; dinoflagellate cysts; 18S rRNA	ALEXANDRIUM-MINUTUM DINOPHYCEAE; DINOFLAGELLATE CYST; RECENT SEDIMENTS; RIVER ESTUARY; ALGAL BLOOMS; RED TIDES; CRYPTOPHYCEAE; ABUNDANCE; NUTRIENTS; GROWTH	The coastal area of Qinhuangdao, particularly the Changli Gold Coast Nature Reserve, is experiencing ecological degradation and frequent Harmful Algal Blooms (HABs). This study focuses on the changing phytoplankton communities in these coastal waters, examining them from both a macroscopic and microscopic perspective. Utilizing microscopy, molecular techniques, and pigment analysis, seasonal shifts were observed, with diatoms predominating in June and July, and dinoflagellates in August. Our morphological examination enabled the classification of 89 species into four distinct groups. The species Paralia sulcata and Pseudo-nitzschia pungens were most abundant in early summer, while Tripos furca, a dinoflagellate, dominated in August. This indicates a shift in phytoplankton communities due to environmental factors such as phosphate deficiency and high nitrogen/phosphorus ratios. Additionally, the study notes the impact of reduced river runoff and reintroduction of scallop farming contributing to nitrogen-rich eutrophication in August. Molecular analysis revealed a disparity between microscopic observations and the prevalence of Teleaulax blooms during early summer. Elevated concentrations of TN and DOC, coupled with limited water exchange, emerged as primary factors contributing to their occurrence. Sediment analysis revealed a high diversity but low abundance of dinoflagellates in August, with a significant presence of harmful species. The study highlights the shift from diatoms to harmful dinoflagellate populations, exacerbated by eutrophication and pollution, leading to HABs. These findings provide a theoretical basis for understanding toxic algal blooms and are crucial for environmental agencies in developing strategies to protect and sustainably develop offshore environments.	[Shang, Xiaomei; Yang, Shuang; Sun, Jun] Tianjin Univ Sci & Technol, Res Ctr Indian Ocean Ecosyst, Tianjin, Peoples R China; [Sun, Jun] China Univ Geosci Wuhan, Coll Marine Sci & Technol, Wuhan, Hubei, Peoples R China	Tianjin University Science & Technology; China University of Geosciences	Sun, J (通讯作者)，Tianjin Univ Sci & Technol, Res Ctr Indian Ocean Ecosyst, Tianjin, Peoples R China.; Sun, J (通讯作者)，China Univ Geosci Wuhan, Coll Marine Sci & Technol, Wuhan, Hubei, Peoples R China.	phytoplankton@163.com	Sun, Jun/A-5254-2009		Natural Science Foundation of China [42206087, 41676112]; Changjiang Scholar Program of Chinese Ministry of Education [T2014253]	Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Changjiang Scholar Program of Chinese Ministry of Education	This work was supported by the Natural Science Foundation of China (No. 42206087, 41676112) and the Changjiang Scholar Program of Chinese Ministry of Education (T2014253) to JS. We also thank our colleagues from Dr. Guicheng Zhang and Dr. Dai Jia at Tianjin University of Science and Technology who provided helps on water sampling.	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Mar. Sci.	JUN 4	2024	11								1371196	10.3389/fmars.2024.1371196	http://dx.doi.org/10.3389/fmars.2024.1371196			10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	UM4K6		gold			2025-03-11	WOS:001248462500001
J	Prego, R; Bao, R; Varela, M; Carballeira, R				Prego, Ricardo; Bao, Roberto; Varela, Manuel; Carballeira, Rafael			Naturally and Anthropogenically Induced <i>Lingulodinium polyedra</i> Dinoflagellate Red Tides in the Galician Rias (NW Iberian Peninsula)	TOXINS			English	Article						harmful algal bloom; oceanography; bottom-up regulation; cysts; dinoflagellates; human impact; dredging; Galicia	HARMFUL ALGAL BLOOMS; SEASONAL-VARIATIONS; SHELF NW; A-CORUNA; PHYTOPLANKTON; CYSTS; HYDROGRAPHY; DINOPHYCEAE; VARIABILITY; ENCYSTMENT	Despite the fact that the first red tide reported on the coasts of the Iberian Peninsula was due to Lingulodinium polyedra, knowledge about their frequency and, particularly, about the environmental conditions contributing to bloom initiation is still scarce. For this reason, L. polyedra bloom episodes were observed and studied in three Galician rias during the summer season based on the 1993-2008 record database period; additionally, samples were collected in summer 2008. Proliferations of L. polyedra occurred in the rias of Ares and Barqueiro in June and August, respectively, while in the Ria of Coru & ntilde;a, they persisted from the end of June to early September. Red tides developed when the surface temperature reached 17 degrees C, with "seasonal thermal window" conditions, and when salinities were >= 30, i.e., an "optimal salinity window"; when these parameters were lower than these thresholds, cyst germination decreased. A cyst transport mechanism from sediments to the surface must also exist; this mechanism was found to be natural (tidal currents) in the ria of Barqueiro or anthropogenic (dredging) in the rias of Ares and Coru & ntilde;a. Surface temperatures during summer were usually favorable for cyst germination (85 to 100%) during the 1993-2008 period; however, water temperatures below 10 m depth only rarely reached the 17 degrees C threshold (2 to 18%). During this 16-year period, dredging activities could explain 71% (Coru & ntilde;a) and 44% (Ares) of the recorded bloom events. When a bloom episode developed in early summer, favorable conditions did not lead to a new red tide, probably due to the lag period required by cysts for germination. Moreover, blooms did not develop when high densities of diatoms (>1,000,000 cells<middle dot>L-1) remained in the water column as a result of summer upwelling pulses occurring in specific years. The temperature-sediment disturbance pattern found in this study provides a useful tool for the prevention of eventual risks resulting from red tides of this dinoflagellate.	[Prego, Ricardo] CSIC, Inst Invest Marinas IIM, Eduardo Cabello 6, Vigo 36208, Spain; [Bao, Roberto] Univ A Coruna, Ctr Interdisciplinar Quim & Biol CICA, GRICA Grp, Rua Carballeiras, La Coruna 15071, Spain; [Varela, Manuel] Inst Espanol Oceanog, Ctr Oceanog A Coruna, Apdo 130, E-15080 La Coruna, Spain; [Carballeira, Rafael] Univ Valencia, Inst Cavanilles Biodiversitat & Biol Evolut ICBiBE, C Catedrat Jose Beltran 2, Paterna 46980, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Universidade da Coruna; Centro interdisciplinar de Quimica e Bioloxia CICA; Spanish Institute of Oceanography; University of Valencia	Carballeira, R (通讯作者)，Univ Valencia, Inst Cavanilles Biodiversitat & Biol Evolut ICBiBE, C Catedrat Jose Beltran 2, Paterna 46980, Spain.	prego@iim.csic.es; roberto.bao@udc.es; manuel.varela@co.ieo.es; rafael.carballeira@uv.es	Prego, Ricardo/H-4169-2012; Bao, Roberto/D-4092-2009; Carballeira, Rafael/CAJ-1467-2022	Prego, Ricardo/0000-0001-8922-6775; Bao, Roberto/0000-0002-2928-2836; Carballeira, Rafael/0000-0002-2807-6942	INTERESANTE project of the Comision Interministerial de Ciencia y Tecnologia (CICYT) of the Spanish Government [CTM2007-62546-C03/MAR]	INTERESANTE project of the Comision Interministerial de Ciencia y Tecnologia (CICYT) of the Spanish Government	This research was funded by the INTERESANTE project of the Comision Interministerial de Ciencia y Tecnologia (CICYT) of the Spanish Government, grant number CTM2007-62546-C03/MAR.	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J	Manic, DC; Redil, RD; Rodriguez, IB				Manic, Dolly C.; Redil, Richard D.; Rodriguez, Irene B.			Trace Metals in Phytoplankton: Requirements, Function, and Composition in Harmful Algal Blooms	SUSTAINABILITY			English	Review						metal bioavailability; toxin production; nutrient limitation; harmful algal bloom dynamics; metal contamination; metal-phytoplankton feedback interaction	DOMOIC ACID PRODUCTION; DINOFLAGELLATE ALEXANDRIUM-CATENELLA; PSEUDO-NITZSCHIA-MULTISERIES; DISSOLVED ORGANIC-MATTER; DIATOM SYNEDRA-ACUS; SAN-FRANCISCO BAY; C-N-P; MICROCYSTIS-AERUGINOSA; NORTH-ATLANTIC; MARINE-PHYTOPLANKTON	In a constantly changing environment brought about by the climate crisis and escalated anthropogenic perturbations driven by the growing population, harmful algal bloom dynamics and their impacts are expected to shift, necessitating adaptive management strategies and comprehensive research efforts. Similar to primary productivity, HABs have been thought to be driven primarily by major nutrients such as N, P, and Si. However, recent investigations on the role and importance of micronutrients as limiting factors in aquatic environments have been highlighted. This paper provides a review of metal and phytoplankton interactions, with a specific emphasis on pertinent information on the influence of trace nutrients on growth, toxin production, and other underlying mechanisms related to the dynamics of HABs. Low to near-depleted levels of essential nutrients, including Fe, Cu, Zn, Se, Mn, Co, and Mo, negatively impact cell growth and proliferation of various marine and freshwater HAB species. However, evidence shows that at elevated levels, these trace elements, along with other non-essential ones, could still cause toxic effects to certain HAB species manifested by decreased photosynthetic activities, oxidative stress, ultrastructure damage, and cyst formation. Interestingly, while elevated levels of these metals mostly result in increased toxin production, Co (i.e., yessotoxins, gymnodimine, and palytoxins) and Mn (i.e., isodomoic acid, okadaic and diol esters) enrichments revealed otherwise. In addition to toxin production, releasing dissolved organic matter (DOM), including dissolved organic carbon (DOC) and humic substances, was observed as an adaptation strategy, since these organic compounds have been proven to chelate metals in the water column, thereby reducing metal-induced toxicity. Whilst current research centers on free metal toxicity of specific essential elements such as Cu and Zn, a comprehensive account of how trace metals contribute to the growth, toxin production, and other metabolic processes under conditions reflective of in situ scenarios of HAB-prone areas would yield new perspectives on the roles of trace metals in HABs. With the growing demands of the global population for food security and sustainability, substantial pressure is exerted on the agriculture and aquaculture sector, highlighting the need for effective communication of information regarding the interactions of macro- and micronutrients with HABs to improve existing policies and practices.	[Manic, Dolly C.; Redil, Richard D.; Rodriguez, Irene B.] Univ Philippines, Marine Sci Inst, Coll Sci, Quezon City 1101, Philippines	University of the Philippines System; University of the Philippines Diliman	Rodriguez, IB (通讯作者)，Univ Philippines, Marine Sci Inst, Coll Sci, Quezon City 1101, Philippines.	dmanic@msi.upd.edu.ph; ibrodriguez@msi.upd.edu.ph	Rodríguez, Irene/ISA-8218-2023	Manic, Dolly/0000-0002-9961-5499; Rodriguez, Irene/0000-0001-9848-9526; Redil, Richard/0009-0004-8996-9404	University of the Philippines System; Marine Science Institute, Department of Science and Technology (DOST), Philippine Council for Agriculture Aquatic and Natural Resource Research and Development (DOST-PCAARD); RVA-Marine Microalgal Culture Collection (RVA-MMCC)	University of the Philippines System; Marine Science Institute, Department of Science and Technology (DOST), Philippine Council for Agriculture Aquatic and Natural Resource Research and Development (DOST-PCAARD); RVA-Marine Microalgal Culture Collection (RVA-MMCC)	We express our gratitude to the University of the Philippines System, the Marine Science Institute, Department of Science and Technology (DOST), Philippine Council for Agriculture Aquatic and Natural Resource Research and Development (DOST-PCAARD), and the RVA-Marine Microalgal Culture Collection (RVA-MMCC) for their support to our research group.	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J	Majaneva, M; Jääskeläinen, S; Autio, R; Blomster, J; Rintala, JM				Majaneva, Markus; Jaaskelainen, Sara; Autio, Riitta; Blomster, Jaanika; Rintala, Janne-Markus			Dynamics of cold-water dinoflagellates in the northern Baltic Sea based on 18S rRNA gene metabarcoding	MARINE BIODIVERSITY			English	Article						Succession; Sea ice; Phytoplankton; Niche; Habitat preference	ICE; PATTERNS; BLOOM; PHYLOGENY; CATENATA	Cold-water dinoflagellates contribute significantly to spring blooms in temperate coastal waters. In the northern Baltic Sea, Peridiniella catenata, Apocalathium malmogiense, Gymnodinium corollarium, and Biecheleria baltica predominate the dinoflagellate spring blooms. Spring dynamics of cold-water dinoflagellates have been previously studied using cyst sedimentation data. Here, we utilize time-series data based on amplicons of the V4 region of the 18S rRNA gene spanning from autumn 2012 to spring 2013 and describe dynamics and habitat preferences of the relatively most abundant dinoflagellates in the northern Baltic Sea. Our results indicate that these species preferred either sea ice, under-ice water, or deeper water columns during the ice-covered season and that they shifted in temporal dominance during our sampling period.	[Majaneva, Markus] Norwegian Inst Nat Res NINA, Trondheim, Norway; [Majaneva, Markus; Jaaskelainen, Sara; Rintala, Janne-Markus] Univ Helsinki, Tvarminne Zool Stn, Hango, Finland; [Jaaskelainen, Sara; Blomster, Jaanika] Univ Helsinki, Fac Biol & Environm Sci, Helsinki, Finland; [Autio, Riitta] Finnish Environm Inst, Res Infrastruct Unit, Helsinki, Finland; [Rintala, Janne-Markus] Univ Helsinki, Inst Atmospher & Earth Syst Res INAR, Fac Sci, Helsinki, Finland	Norwegian Institute Nature Research; University of Helsinki; University of Helsinki; Finnish Environment Institute; University of Helsinki	Majaneva, M (通讯作者)，Norwegian Inst Nat Res NINA, Trondheim, Norway.; Majaneva, M (通讯作者)，Univ Helsinki, Tvarminne Zool Stn, Hango, Finland.	markus.majaneva@nina.no		Majaneva, Markus/0000-0003-3884-2548; Blomster, Jaanika/0000-0003-1347-7919; Rintala, Janne-Markus/0000-0002-3514-6582	Norwegian institute for nature research; Walter and Andree de Nottbeck Foundation; University of Helsinki 3 year research	Norwegian institute for nature research(Bioforsk); Walter and Andree de Nottbeck Foundation; University of Helsinki 3 year research	Open access funding provided by Norwegian institute for nature research. Walter and Andree de Nottbeck Foundation and University of Helsinki 3 year research grants provided funding to carry out the field and laboratory analysis within the Winter Ecology Research Project in 2013-2016, led by JMR.	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Biodivers.	JUN	2024	54	3							51	10.1007/s12526-024-01443-7	http://dx.doi.org/10.1007/s12526-024-01443-7			8	Biodiversity Conservation; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Marine & Freshwater Biology	SI9L6		hybrid			2025-03-11	WOS:001233942200001
J	Rukminasari, N; Andriyono, S; Hidayani, AA				Rukminasari, Nita; Andriyono, Sapto; Hidayani, Andi Aliyah			Dinoflagellate Cyst Assemblage, Abundance and Distribution in Three Estuaries in Bone Bay, South Sulawesi, Indonesia	OCEAN SCIENCE JOURNAL			English	Article						Dinoflagellate cyst; Distribution and assemblages; Bone Bay; Indonesia	NORTHERN NORTH-ATLANTIC; SURFACE SEDIMENTS; SPATIAL-DISTRIBUTION; RESTING CYSTS; ENVIRONMENTAL-FACTORS; KOLJO FJORD; MARINE; SEA; PRODUCTIVITY; INDICATORS	Dinoflagellates are the main group of primary producers in freshwater and marine ecosystems. Some of these species can produce toxins (only 10% from the total species) and cause the occurrence of harmful-algal-blooms (HABs) worldwide. The purpose of this study was to examine the species assemblages, distribution, diversity, species richness, and abundance of dinoflagellate cysts in three estuaries around Bone Bay, Sulawesi, Indonesia. Thirty-six surface sediment samples were collected from the Teko, Tangka and Panyula estuaries, and dinoflagellates cysts were counted and identified. Multivariate analyses were conducted to examine species assemblages, diversity and richness. Eighteen dinoflagellate taxa from 11 genera and 8 families were identified. The three most abundant dinoflagellate species were Alexandrium minutum, Pentapharsodinium tyrrhenicum, and Scrippsiella lachrymosa. Species assemblages varied between sampling sites, there was no shifting from autotroph to heterotroph dinoflagellate cysts, and based on species richness and diversity, Bone Bay was categorized as oligotrophic. These findings indicate that cyst species could be good indicators for eutrophication and industrial pollution, even though eutrophication was not detected at the sites in Bone Bay during the research period.	[Rukminasari, Nita; Hidayani, Andi Aliyah] Hasanuddin Univ, Fac Marine Sci & Fisheries, Sulawesi Selatan 90245, Indonesia; [Andriyono, Sapto] Airlangga Univ, Fac Fisheries & Marine, Surabaya 60115, Jawa Timur, Indonesia	Universitas Hasanuddin; Airlangga University	Rukminasari, N (通讯作者)，Hasanuddin Univ, Fac Marine Sci & Fisheries, Sulawesi Selatan 90245, Indonesia.	nita.r@unhas.ac.id	Andriyono, Sapto/AAB-7229-2021; Rukminasari, Nita/M-2410-2014; Hidayani, Andi Aliah/H-8117-2017	Rukminasari, Nita/0000-0003-2943-9538; Hidayani, Andi Aliah/0000-0002-4541-5539	Ministry of Eduction, Culture, Research and Higher Degree, Republic of Indonesia [1377/UN4.22/PT.01.03/2022]; Directorate Research and Community Service, Ministry of Education and Culture, Republic of Indonesia	Ministry of Eduction, Culture, Research and Higher Degree, Republic of Indonesia; Directorate Research and Community Service, Ministry of Education and Culture, Republic of Indonesia	We thanks to Director of Center of Excellent and Innovation of Seaweed Development and Utilization who has provided us with room and facilities for analyzing our samples. Also, thanks to Head of Bulukumba, Sinjai and Maros Regency who have given a permission for conducting sampling in their areas. This research was funded by Directorate Research and Community Service, Ministry of Education and Culture, Republic of Indonesia and Universitas Hasanuddin, under research scheme of Indonesian Research Collaboration (A Scheme) with the contract number: 1377/UN4.22/PT.01.03/2022. Author also want to thank to our students (Nur Inda Sari, Andi Widya Anugrah, Delfira, Umi Rintin, Nurul Kiswa and Rizky Amalia Ramadhani) who helping us in sampling and processing our samples.	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J.	JUN	2024	59	2							19	10.1007/s12601-024-00142-5	http://dx.doi.org/10.1007/s12601-024-00142-5			13	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	MX8U1					2025-03-11	WOS:001197034800001
J	Danesh, DC; McCarthy, FMG; Sangiorgi, F; Cumming, BF				Danesh, Donya C.; McCarthy, Francine M. G.; Sangiorgi, Francesca; Cumming, Brian F.			The utility of freshwater dinoflagellate cyst assemblages as a paleoecological proxy: An assessment from boreal lakes (northwest Ontario, Canada)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Freshwater dinoflagellate cysts; Palaeoecological proxies; Palaeoecology; Modern calibration set; Non -pollen palynomorphs (NPPs); Experimental Lakes Area	NON-POLLEN PALYNOMORPHS; CULTURAL EUTROPHICATION; PREINDUSTRIAL TIMES; DIATOM ASSEMBLAGES; UMBONATUM GROUP; ABUNDANCE; NOV; PERIDINIALES; PHYLOGENY; SEDIMENTS	Aquatic palynomorphs have the potential to provide valuable insights into past environments but little has been done to assess the utility of freshwater dinoflagellate cysts as palaeoecological proxies of lacustrine environments. This study is the first to compare the distribution of freshwater dinoflagellate cysts found in surface sediments from 32 boreal lakes with varying physical and chemical characteristics. Cysts of Fusiperidinium wisconsinense, Parvodinium umbonatum, and Peridinium willei were nearly ubiquitous, but of the remaining cyst taxa, only Parvodinium inconspicuum, Peridinium limbatum, and Peridinium volzii were abundant but present in a smaller number of lakes. Assemblage composition broadly clustered into three groups: 1) an assemblage (primarily Peridinium spp.) associated with relatively shallow, mesotrophic lakes; 2) an assemblage dominated by F. wisconsinense in mesotrophic lakes with intermediate depth and relatively high pH and alkalinity; and 3) an assemblage dominated by P. umbonatum in deeper oligotrophic lakes. Moreover, changes in dinoflagellate cyst assemblage were assessed in a sediment core spanning the Holocene from nearby Gall Lake and interpreted alongside other previously published paleoecological proxies from this core. High abundances of many dinoflagellate cysts including P. limbatum, P. willei, F. wisconsinense, and P. inconspicuum were observed when lake production was high at a time when lake-levels were low and climate was more arid than today. This study suggests that dinoflagellate cysts in lacustrine sediments are, when abundant, promising both in modern and core samples, and the relationships between assemblages today and in the past can contribution additional information in understanding past ecological conditions.	[Danesh, Donya C.; Cumming, Brian F.] Queens Univ, Dept Biol, Paleoecol Environm Assessment & Res Lab PEARL, Kingston, ON K7L 3J9, Canada; [Danesh, Donya C.] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam IBED, Dept Ecosyst & Landscape Dynam, NL-1090 GE Amsterdam, Netherlands; [Danesh, Donya C.; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, NL-3584 CB Utrecht, Netherlands; [McCarthy, Francine M. G.] Brock Univ, Earth Sci Dept, St Catharines, ON L2S 3A1, Canada	Queens University - Canada; University of Amsterdam; Utrecht University; Brock University	Danesh, DC (通讯作者)，Queens Univ, Dept Biol, Paleoecol Environm Assessment & Res Lab PEARL, Kingston, ON K7L 3J9, Canada.; Danesh, DC (通讯作者)，Univ Amsterdam, Inst Biodivers & Ecosyst Dynam IBED, Dept Ecosyst & Landscape Dynam, NL-1090 GE Amsterdam, Netherlands.; Danesh, DC (通讯作者)，Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, NL-3584 CB Utrecht, Netherlands.	d.c.danesh@uva.nl			Natural Sciences and Engineering Research Council (NSERC) [RGPIN-2016-04347, RGPIN-2018-03924]; Ontario Graduate Scholarship in Science and Technology (OGSST)	Natural Sciences and Engineering Research Council (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Ontario Graduate Scholarship in Science and Technology (OGSST)	This project was funded by Natural Sciences and Engineering Research Council (NSERC) Discovery grants to BF Cumming (grant number: RGPIN-2016-04347) and FMG McCarthy (RGPIN-2018-03924) and Ontario Graduate Scholarship in Science and Technology (OGSST) to DC Danesh.	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Palaeobot. Palynology	JUL	2024	326								105128	10.1016/j.revpalbo.2024.105128	http://dx.doi.org/10.1016/j.revpalbo.2024.105128		MAY 2024	14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	UJ4J8		Green Published			2025-03-11	WOS:001247674400001
J	Singh, YR; Devi, AB; Singh, NS; Abbott, MB; Arnold, TE; Singh, WA; Devi, MS; Singh, SP; Devi, OV				Singh, Y. Raghumani; Devi, A. Bijayalaxmi; Singh, Nithoujam Surdas; Abbott, Mark B.; Arnold, T. Elliot; Singh, W. Ajoykumar; Devi, M. Sapana; Singh, Sh. Priyokumar; Devi, O. Victory			Dinoflagellate cysts from the Shillong Plateau, Meghalaya (India): Palynological signature during the late Palaeocene-early Eocene Transition	TERRA NOVA			English	Article						Apectodinium; carbon stable isotope; Lakadong sandstone; Meghalaya; Palaeocene-Eocene transition; palynology	THERMAL MAXIMUM; ISOTOPE STRATIGRAPHY; APECTODINIUM ACME; BIGHORN BASIN; CLIMATE; CARBON; CIRCULATION; PALEOGENE; SECTION; OCEAN	The paper presents a new section of the late Palaeocene-early Eocene, palynological assemblages and stable carbon isotopes from the Lakadong sandstone member of the East Khasi Hills of Meghalaya (India). The Palaeocene-Eocene transition (PET) is marked by stratigraphic markers of dinoflagellate cysts (taxa of Apectodinium augustum, now Axiodinium augustum) and negative carbon isotope excursion. The palynofloral assemblage indicates the sequence represents warm, humid tropical to subtropical conditions with heavy rainfall. The depositional environment of the Lakadong Sandstone Member is interpreted to be neritic. The new insights of this study in this section suggest the PET with the occurrence of Apectodinium acme consisting of A. augustum at CS5-15a.	[Singh, Y. Raghumani; Devi, A. Bijayalaxmi; Singh, W. Ajoykumar; Devi, M. Sapana; Singh, Sh. Priyokumar; Devi, O. Victory] Manipur Univ, Dept Earth Sci, Imphal 795003, India; [Devi, A. Bijayalaxmi] Pravabati Coll, Dept Geol, Mayang Imphal, India; [Singh, Nithoujam Surdas] Geol Survey India, Northeastern Reg, Shillong, India; [Abbott, Mark B.; Arnold, T. Elliot] Univ Pittsburgh, Dept Geol & Environm Sci, Pittsburgh, PA USA	Manipur University; Geological Survey India; Pennsylvania Commonwealth System of Higher Education (PCSHE); University of Pittsburgh	Singh, YR (通讯作者)，Manipur Univ, Dept Earth Sci, Imphal 795003, India.	yengmani@gmail.com		Arnold, Thomas Elliott/0000-0003-4192-7980	Science and Engineering Research Board (SERB), Government of India [EEQ/2022/000263, CRG/2023/004591]; Oil India Limited, Centre of Excellence for Studies, Guwahati [6209163]	Science and Engineering Research Board (SERB), Government of India; Oil India Limited, Centre of Excellence for Studies, Guwahati	The author (YRS) acknowledges the authority of Manipur University to provide a geological field to publish the present research work. The author (YRS) is grateful to the Science and Engineering Research Board (SERB), Government of India (Grant No. EEQ/2022/000263; CRG/2023/004591) and Oil India Limited, Centre of Excellence for Studies, Guwahati (Contract no. 6209163) for supporting this work. YRS sincerely thanks Dr. Alina I. Iakovleva, Geological Institute of Russian Academy of Sciences, Russia, and Dr. Robert A. Fensome of Natural Resources Canada, Geological Survey of Canada, for helping to identify palynomorphs. We also are thankful to Venus Guruaribam, and T. Nganthoi Chanu for their assistance during the sample analysis.	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Nova	DEC	2024	36	6					425	436		10.1111/ter.12725	http://dx.doi.org/10.1111/ter.12725		MAY 2024	12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	M2G9V					2025-03-11	WOS:001230687400001
J	Filipova-Marinova, M; Pavlov, D; Slavova, K				Filipova-Marinova, Mariana; Pavlov, Danail; Slavova, Krasimira			Paleoclimate changes and ecosystem responses of the Bulgarian Black Sea zone during the last 26000 years	NATURE CONSERVATION-BULGARIA			English	Article						Dinoflagellate cyst; non-pollen palynomorphs; radiocarbon dating; spore-pol- len analysis	HOLOCENE VEGETATION HISTORY; DINOFLAGELLATE CYST RECORD; HIGH-RESOLUTION POLLEN; ABRUPT CLIMATE-CHANGE; CORYLUS-AVELLANA L.; MARMARA SEA; MEDITERRANEAN SEA; ENVIRONMENTAL-CHANGE; HYDROLOGICAL CHANGES; SURFACE SALINITY	Multi-proxy analysis (spore-pollen, dinoflagellate cysts, other non-pollen palynomorphs (NPPs), radiocarbon dating and lithology) was performed on marine sediments from three new cores retrieved during the two cruise expeditions on board the Research Vessel "Akademik" in 2009 and 2011. The Varna transect comprises three cores extending from the outer shelf, continental slope and deep-water zone. The record spans the last 26000 years (all ages obtained in this study are given in calendar years BP (cal. yrs BP)). The pollen record reveals the spreading of steppe vegetation dominated by Artemisia and Chenopodiaceae, suggesting cold and dry environments during the Late Pleniglacial - Oldest Dryas (25903-15612 cal. yrs BP). Stands of Pinus and Quercus reflect warming/humidity increase during the melting pulses (19.2-14.5 cal. ka BP) and the Late Glacial interstadials B & oslash;lling and Aller & oslash;d. The Younger Dryas (13257-11788 cal. yrs BP) coldest and driest environments are clearly demonstrated by the maximum relative abundance of Artemisia and Chenopodiaceae. During the Early Holocene (Preboreal and Boreal chronozones, 11788-8004 cal. yrs BP), Quercus appeared as a pioneer species and, along with other temperate deciduous arboreal taxa, formed open deciduous forests as a response to the increased temperature. The rapid expansion of these taxa indicates that they survived in Glacial refugia in the coastal mountains. During the Atlantic chronozone (8004-5483 cal. yrs BP), optimal climate conditions (high humidity and increased mean annual temperatures) stimulated the establishment of species-rich mixed temperate deciduous forests. During the Subboreal chronozone (5483-2837 cal. yrs BP), Carpinus betulus and Fagus expanded simultaneously and became more important components of mixed oak forests and probably also formed separate communities. During the Subatlantic chronozone (2837 cal. yrs BP to pre-industrial time), climate-driven changes (an increase of humidity and a cooling of the climate) appear to be the main drivers of the specific vegetation succession expressed by increased abundance of Alnus, , Fraxinus excelsior and Salix along with lianas, suggesting formation of flooded riparian forests (so called 'Longoz') lining the river valleys along the Black Sea coast. The first indicators of farming and other human activities have been recorded since 7074 cal. yrs BP. The dinoflagellate cyst (dinocyst) assemblages have been analysed to assess the changes in the Black Sea environment over the last 26000 years in terms of fluctuation in paleoproduction and surface water conditions related to changes in climate, freshwater input and Mediterranean water intrusion. Two major dinocyst assemblages were distinguished: one dominated by stenohaline freshwater/ brackish-water species and a successive one dominated by euryhaline marine species.The changes in the composition of the assemblages occurred at 7668 cal. yrs BP. The abrupt decrease of stenohaline freshwater/brackish-water species Pyxidinopsis psilata and Spiniferites cruciformis was followed upwards by a gradual increase in euryhaline marine species, such as Lingulodinium machaerophorum, , Spiniferites belerius, , S. bentorii and acritarch Cymatiosphaera globulosa. . The first occurrence of euryhaline marine species took place synchronously with the onset of sapropel deposition. Modern marine conditions were established after 6417 cal yrs BP when an abundance of Mediterranean-related species, such as Operculodinium centrocarpum and Spiniferites mirabilis, , along with other heterotrophic species, occurred. After the stable cold and dry environment during the Last Glacial Maximum, the phytoplankton record of core AKAD 11-17 shows that Pediastrum boryanum var. boryanum has a cyclical abundance associated with the deposition of four red-brown clay layers between 19.2 and 14.5 cal. ka BP. This event is associated with the major melting phase of European Ice drained by the Danube and Dnieper Rivers in response to climate warming observed after the end of the Last Glacial Maximum. During the Early Holocene, P. psilata, , characterised by a preference to warmer temperatures, demonstrates its ecological optimum for growth concerning SST reaching maximum relative abundance of 94% between 11072 and 8638 cal. yrs BP. This maximum was interrupted by an abrupt significant short-term decrease in the relative abundance of P. psilata centred between 8500 and 8300 cal. yrs BP reflecting cold conditions similar to those of Younger Dryas. This finding, also confirmed by the rapid significant decrease of arboreal pollen, particularly of Quercus in the same studied core, is considered a regional expression of the well-known '8.2 ka cold event' which is commonly linked to a meltwater-related perturbation of the Atlantic Meridional Overturning Circulation (AMOC) and associated collapse of oceanic northward heat transport. Our fossil pollen and dinocyst data confirm that the high amplitude temperature anomaly associated with 'the 8.2 ka cold event' may have also occurred in south-eastern Europe, at lower latitudes of the western Black Sea coastal area, most probably due to atmospheric transition and/or river discharge.	[Filipova-Marinova, Mariana] Museum Nat Hist, 41 Maria Louisa Blvd, Varna, Bulgaria; [Pavlov, Danail] Med Univ Varna, Varna, Bulgaria; [Slavova, Krasimira] Bulgarian Acad Sci, Inst Oceanol, Varna, Bulgaria	Medical University Varna; Bulgarian Academy of Sciences	Filipova-Marinova, M (通讯作者)，Museum Nat Hist, 41 Maria Louisa Blvd, Varna, Bulgaria.	marianafilipova@yahoo.com	Pavlov, Danail/N-7815-2013	Filipova-Marinova, Mariana/0000-0002-0786-9476; Pavlov, Danail/0000-0001-7382-2054	Bulgarian National Science Fund [Akad 09-15]; Ministry of Education and Science [DO 02-337]	Bulgarian National Science Fund(National Science Fund of Bulgaria); Ministry of Education and Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT))	The studied gravity cores Akad 09-10, Akad 09-15 and Akad 11-17 were collected by an international scientific team during both expeditions, with financial support by the Bul-garian National Science Fund within the Project DO 02-337, led by Prof. Petko Dimitrov. The study was partly supported by the Project "Upgrading of distributed scientific infra-structure - Bulgarian Network for Long-Term Ecosystem Research" (LTER-BG) , (agree-ment with Ministry of Education and Science, DO1-163/28.07.2022) .	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Conserv.-Bulgaria	MAY 21	2024		55					201	248		10.3897/natureconservation.55.121842	http://dx.doi.org/10.3897/natureconservation.55.121842			48	Biodiversity Conservation	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation	YH0Z2		gold			2025-03-11	WOS:001267492500001
J	Wang, SL; Mansour, A; Li, C; Su, PD; Meng, LJ; Ahmed, MS				Wang, Shilin; Mansour, Ahmed; Li, Cong; Su, Peidong; Meng, Lingjian; Ahmed, Mohamed S.			Source rock assessment and organic matter characterization of the Oligocene upper Shahejie and Dongying formations in the Nanpu depression of the saline lacustrine Bohai Bay basin, China: Geochemical, palynological, and mineralogical perspectives	MARINE AND PETROLEUM GEOLOGY			English	Article						Paleoredox conditions; Palynology; Organic carbon drivers; Thermal maturity; Kerogen types; Petroleum generation; Organic matter preservation	EVAL PYROLYSIS; 1ST MEMBER; RAOYANG SAG; CARBON; ACCUMULATION; PRESERVATION; SUBSIDENCE; SEDIMENTS; DILUTION; KEROGEN	The Bohai Bay Basin, located in eastern China, is a significant petroliferous, non -marine rift basin, underwent intricate tectonic activities throughout the Cenozoic. The Nanpu Depression in the Huanghua sub -basin in the northern part of the basin was controlled by Paleogene rifting and increased subsidence. These geological processes resulted in the deposition of the Shahejie and Dongying formations, which exhibited varying quantities and qualities of organic matter. Eighty drill cuttings samples of the Paleogene First Member (Es 1 ) and the overlying Third (Ed 3 ) and Second (Ed 2 ) members of the Shahejie and Dongying formations, respectively, were investigated. An integrated approach including organic and inorganic geochemistry, palynology, and mineralogy was employed to assess the paleoredox and marine incursion conditions, source rock quality and levels of thermal maturity, and factors that governed organic matter accumulation. Results indicated that the Es1 Member was deposited under anoxic conditions, resulting in the accumulation of organic matter -rich mudstones in the Nanpu Depression. Abundant pollen grains and acritarchs were found in the Es1 Member yielded along with minor occurrences of dinoflagellate cysts, freshwater algae, and spores. Terrestrial palynomorph composition provided evidence of increased terrestrial runoff, while the high abundance of acritarchs, accompanied by some dinoflagellate cysts, confirmed episodes of marine incursion and deposition under hypersaline conditions in the lacustrine Bohai Bay Basin. The Ed 2 Member exhibited poor to fair amounts of organic matter and a limited potential of hydrocarbon generation with a variety of kerogen Types, including IV, III, II/III, and II. The Ed 3 Member shows fair to good organic matter richness and hydrocarbon potential of kerogen Types III, II/III, and II. The Es 1 Member emerged as the most promising source rock within the studied interval, boasting good to excellent organic matter richness, and fair to good hydrocarbon generation potential of kerogen Types III and II/ III. Evaluating the thermal maturity of organic matter, based on T max and VRo-Eq% and related cross -plots, revealed that the Shahejie and Dongying formations are still in the immature to the early stage of the oil window. The mineralogical composition of the Es 1 Member primarily consists of clay and quartz with some carbonate and accessory minerals, such as epigenetic halite, dolomite, and plagioclase. Weak correlations observed between the total organic carbon (TOC) and mineral components indicated that the availability of organic matter was primarily controlled by enhanced production and preservation rather than limited dilution under saline lacustrine, oxygen -deprived, and well -stratified water column conditions. Regional investigations of the Es 1 Member confirmed the widespread anoxia and deposition of organic -rich source rocks in the Bohai Bay Basin during the Oligocene.	[Wang, Shilin; Mansour, Ahmed; Su, Peidong] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Li, Cong; Meng, Lingjian] PetroChina, Jidong Oilfield Co, Explorat & Dev Res Inst, Tangshan 063000, Hebei, Peoples R China; [Ahmed, Mohamed S.] King Saud Univ, Coll Sci, Geol & Geophys Dept, Riyadh 11451, Saudi Arabia	Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; Sinopec; China National Petroleum Corporation; King Saud University	Wang, SL; Mansour, A (通讯作者)，Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China.	ybybwsl@163.com; ahmedmans48@mu.edu.eg; ls_licong@petrolchina.com.cn; spdong@126.com; barbarity@163.com; mohahmed@ksu.edu.sa	Su, Peidong/ABC-2136-2021; Ahmed, Mohamed/GQP-1116-2022; Mansour, Ahmed/AAR-4969-2020	Mansour, Ahmed/0000-0003-2466-7494	King Saud University, Riyadh, Saudi Arabia [RSP2024R455]	King Saud University, Riyadh, Saudi Arabia(King Saud University)	We thank the Jidong Oilfield Company of PetroChina, Tangshan, Hebei, China for their permissions to obtain the samples and data of the four studied wells. This work was partially funded by Researchers Supporting project number (RSP2024R455) , King Saud University, Riyadh, Saudi Arabia. Special thanks to the editor -in -chief Massimo Zecchin and the section editor Thomas Gentzis as well as two anony- mous reviewers for their valuable comments and suggestions, which improved the manuscript.	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J	Peryt, D; Gedl, PL; Jurek, K; Wieclaw, D; Worobiec, E; Worobiec, G; Peryt, TM				Peryt, Danuta; Gedl, Przemys law; Jurek, Krzysztof; Wieclaw, Dariusz; Worobiec, Elzbieta; Worobiec, Grzegorz; Peryt, Tadeusz Marek			Environmental perturbations around the Badenian/Sarmatian (Middle Miocene) boundary in the Central Paratethys: Micropalaeontological and organic geochemical records	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paratethys; Middle Miocene; Micropalaeontology; Biostratigraphy; Organic geochemistry; Inorganic geochemistry; Extinction; Palaeoenvironments; Anoxic events; Badenian; Sarmatian	BUSKO MLYNY PIG-1; CARPATHIAN FOREDEEP BASIN; ROMANIA PALEOGEOGRAPHIC CHANGES; SARMATIAN EXTINCTION EVENT; BADENIAN SALINITY CRISIS; POSIDONIA BLACK SHALE; DINOFLAGELLATE CYSTS; SOURCE ROCKS; PLANT BIOMARKERS; STABLE-ISOTOPE	The boundary between the two regional Middle Miocene stages (the Badenian and Sarmatian) of the Central Paratethys is associated with the largest faunal turnover event in the Paratethys realm. A recent study performed in the northern Polish Carpathian Foredeep revealed that the Badenian/Sarmatian boundary is coeval with a major change in benthic and planktonic foraminiferal assemblages that occurs a few metres below the beginning of the Anomalinoides dividens Interval Zone in our section. The lowermost Sarmatian biozone is the Elphidium angulatum Partial Range Zone, and its lower boundary corresponds to the disappearance of almost all Badenian foraminiferal species. Detailed analysis of a fully cored borehole in southern Poland using micropalaeontological tools (foraminifera and palynology) and a range of (inorganic and organic) geochemical methods indicated that during the late Badenian and almost the entire profile of Anomalinoides dividens Zone, oxic or suboxic sedimentary conditions prevailed. In the Elphidium angulatum Zone and the lowest part of the subsequent Anomalinoides dividens Zone, suboxic and anoxic conditions dominated the sea bottom. This research indicated that the sudden disappearance of marine Badenian species in the Polish Carpathian Foredeep was caused by a rapid change in basin chemistry although not necessarily it implies open marine conditions changing to brackish water environments.	[Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland; [Gedl, Przemys law] Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland; [Jurek, Krzysztof; Wieclaw, Dariusz] AGH Univ Krakow, Fac Geol Geophys & Environm Protect, Al A Mickiewicza 30, PL-30059 Krakow, Poland; [Worobiec, Elzbieta; Worobiec, Grzegorz] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland; [Peryt, Tadeusz Marek] Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland	Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; AGH University of Krakow; Polish Academy of Sciences; W. Szafer Institute of Botany of the Polish Academy of Sciences; Polish Geological Institute - National Research Institute	Peryt, TM (通讯作者)，Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland.	tadeusz.peryt@pgi.gov.pl	Wieclaw, Dariusz/JAX-3392-2023; Jurek, Krzysztof/HNC-5618-2023; Wieclaw, Dariusz/A-4722-2016; Peryt, Tadeusz/F-9289-2019	Worobiec, Elzbieta/0000-0001-5997-9602; Wieclaw, Dariusz/0000-0001-6925-1586; Peryt, Tadeusz/0000-0002-8017-1701; Jurek, Krzysztof/0000-0002-3206-678X	National Science Centre, Poland [UMO-2017/27/B/ST10/01129]; PGI-NRI [62.9012.2414.00.0]	National Science Centre, Poland(National Science Centre, Poland); PGI-NRI	This study was financed by the National Science Centre, Poland, grant No. UMO-2017/27/B/ST10/01129. Special thanks to Dr. Dan V. Palcu, two anonymous reviewers and the editor Prof. Lucia Angiolini for thorough reviews of the paper. TMP acknowledges the PGI-NRI grant no. 62.9012.2414.00.0.	Alexandrowicz S.W., 1982, Geol. 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J	Francescangeli, F; Ferraro, L; Frontalini, F; Da Prato, S; Rubino, F				Francescangeli, F.; Ferraro, L.; Frontalini, F.; Da Prato, S.; Rubino, F.			Exploring the underwater life in transitional environments: Benthic foraminifera, ostracods, and dinoflagellate cysts - Biotic trends and EcoQS assessment in the Mar Piccolo of Taranto (Ionian sea, southern Italy)	MARINE ENVIRONMENTAL RESEARCH			English	Article							ECOLOGICAL QUALITY; SEDIMENTARY RECORD; HEAVY-METALS; SW FRANCE; POLLUTION; WATER; ECOSYSTEM; INDEX; BAY; ASSEMBLAGES	Coastal areas have historically thrived as centers of human activities due to their resources, economic opportunities, and natural allure. The rapid growth of coastal populations has however brought forth a multitude of challenges to tackle, with pollution emerging as a significant and far-reaching issue. Our study focuses on the Mar Piccolo of Taranto (Ionian Sea, Southern Italy), a lagoon -like coastal basin (separated in two sub -basins) that, since decades, has been heavily affected by human activities and aquaculture, leading to environmental deterioration. Although past studies have looked at environmental conditions in the Mar Piccolo from a chemical perspective, the biological component (e.g., biological indicators) has been mostly neglected. In this study, we firstly aim to examine the distribution and diversity of foraminifera, ostracods, and dinoflagellate cysts in December 2016 and compare our findings with data collected in December 2011. Foraminiferal and ostracod communities exhibit similar patterns in the two sampling campaigns, while the communities of encysted dinoflagellates show differences concerning both densities and diversity. Then, we evaluate the Ecological Quality Status (EcoQS) using ecological indices. While the indices in the inner basin appear to reflect an actual ecological degradation, they yield conflicting results in the outer basin. In the outer basin, indeed, the indices overestimate the EcoQS. This study highlights the potential of these indices for characterizing the EcoQS but emphasizes the need for improvements in their reliability. This research also contributes to a more holistic understanding of environmental condition in the Mar Piccolo and underscores the importance of integrating biological quality elements into ecosystem management and remediation strategies.	[Francescangeli, F.] Univ Fribourg, Dept Geosci, Chemin Musee 6, CH-1700 Fribourg Freiburg, Switzerland; [Ferraro, L.] CNR Calata Porta Massa, Inst Marine Sci, I-80133 Naples, Italy; [Frontalini, F.] Urbino Univ, Dept Pure & Appl Sci, I-61029 Urbino, Italy; [Da Prato, S.] CNR, Inst Geosci & Earth Resources, Via Moruzzi 1, I-56124 Pisa, Italy; [Rubino, F.] CNR, Inst Water Res, via Roma 3, I-74123 Taranto, Italy	Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); University of Urbino; Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); Consiglio Nazionale delle Ricerche (CNR)	Ferraro, L (通讯作者)，CNR Calata Porta Massa, Inst Marine Sci, I-80133 Naples, Italy.	fabio.francescangeli@unifr.ch	Francescangeli, Fabio/AAS-1693-2020; Ferraro, Luciana/AAX-6983-2020; Rubino, Fernando/GOP-0332-2022	Francescangeli, Fabio/0000-0002-8309-3315; Ferraro, Luciana/0000-0002-6491-2274	CNR-IRSA of Taranto	CNR-IRSA of Taranto	The field work was financially supported by the CNR-IRSA of Taranto. Special thanks are owed to the crew of the m/b Attilio Cerruti and its Captain Mr. Cosimo Macrip ` o. Giovanni Fanelli (CNR-IRSA Taranto) is acknowledged for his help during the SCUBA dive sampling activities.	Al-Enezi E, 2022, SCI TOTAL ENVIRON, V833, DOI 10.1016/j.scitotenv.2022.155093; Alve E, 2016, MAR MICROPALEONTOL, V122, P1, DOI 10.1016/j.marmicro.2015.11.001; Martins MVA, 2016, ESTUAR COAST SHELF S, V182, P211, DOI 10.1016/j.ecss.2016.10.011; Martins MVA, 2015, PLOS ONE, V10, DOI 10.1371/journal.pone.0118077; Anadon P., 2002, Quat. Res., V131, P227; Annicchiarico C, 2007, ECOTOXICOLOGY, V16, P239, DOI 10.1007/s10646-006-0123-z; [Anonymous], 1998, Serie generale, P291; [Anonymous], 2016, dplyr: A Grammar of Data Manipulation. 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Environ. Res.	JUN	2024	198								106545	10.1016/j.marenvres.2024.106545	http://dx.doi.org/10.1016/j.marenvres.2024.106545		MAY 2024	12	Environmental Sciences; Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Toxicology	TP0G4	38749196	hybrid			2025-03-11	WOS:001242340500001
J	Munsterman, DK; Deckers, J				Munsterman, Dirk K.; Deckers, Jef			Cross-border correlations showing diachronous lithostratigraphic units in the southeastern North Sea Basin during the Early Oligocene (middle-late Rupelian)	NETHERLANDS JOURNAL OF GEOSCIENCES			English	Article						Dinoflagellate cyst analysis; geophysical logs; Boom and Steensel members (NL); Boom and Eigenbilzen formations (B); Oligocene	MIOCENE; EOCENE	Wireline log correlation panels of palynologically analysed boreholes illustrate lateral facies transitions within Rupelian age strata of the Dutch Rupel Formation across the southeastern North Sea Basin. The middle to upper part of the Rupel Formation consists of clays and silts of the Boom Member and the overlying sandier Steensel Member. In the Mill and Goirle boreholes in the Dutch Province of North Brabant, the Boom Member is thickly developed and represents the middle to upper Rupelian (biozones NSO3 to NSO5a), while the Steensel Member is rather thinly developed and only comprises the uppermost Rupelian (biozone NSO5a). Borehole log correlations show that towards the south (or more proximal to the palaeo-continent) the Rupel Formation becomes sandier and the clayey Boom Member thins in favour of the sandy superjacent Steensel Member. Palynological analyses confirm that the Boom Member is restricted to the middle Rupelian (biozone NSO3) age here, and that the superjacent Steensel Member is of middle to upper Rupelian age (biozones NSO3 to NSO5a). Geological models constructed for northern Belgium propose that this facies transition occurs rather sharply, along a WSW-ENE oriented zone parallel to the presumed shoreline at that time. The results of this study support this interpretation and extend the trend towards the Netherlands.	[Munsterman, Dirk K.] Geol Survey Netherlands, Utrecht, Netherlands; [Deckers, Jef] VITO, Mol, Belgium	VITO	Munsterman, DK (通讯作者)，Geol Survey Netherlands, Utrecht, Netherlands.	dirk.munsterman@tno.nl		Munsterman, Dirk/0000-0003-1774-4615; Deckers, Jef/0000-0002-5373-8733				Bogemans F, 2018, GEOLOGISCH HYDROGEOL; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; De Man E, 2010, EPISODES, V33, P3; Deckers J., 2019, VITO, Mol, VITO-rapport 2018/RMA/R/1569; Deckers J., 2014, Geologisch en hydrogeologisch 3D model van het Cenozoicum van de Roerdalslenk in Zuidoost-Nederland en Vlaanderen (H3O-Roerdalslenk), P200; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Fensome RA., 2019, AM ASS STRATIGRAPHIC, V50, P1173; Halet F., 1936, Bulletin de la Societe belge de Geologie, de Paleontologie et dHydrologie, V46, P194; Heilmann-Clausen C, 2005, PALYNOLOGY, V29, P143, DOI 10.2113/29.1.143; Kothe A., 2003, REV PALEOBIOL, V22, P895; Laenen B., 1998, Aardkundige Mededelingen, V9, P61; Louwye S, 2005, GEOL J, V40, P441, DOI 10.1002/gj.1021; Louwye S, 2020, GEOL BELG, V23, P137, DOI 10.20341/gb.2020.010; Matthijs J., 1999, Belgische Geologische Dienst en Ministerie van de Vlaamse Gemeenschap, P104; Munsterman D.K., 2022, De resultaten van de palynologische studie naar de ouderdom van boring Mill, B46C0478, interval: 10-481 m (Peelhorst), P22; Munsterman D.K., 1998, TNO rapport NITG 98-224-B; Munsterman DK, 2022, NETH J GEOSCI, V101, DOI 10.1017/njg.2022.3; Munsterman DK, 2020, GEOL BELG, V23, P127, DOI 10.20341/gb.2020.007; Munsterman DK, 2019, NETH J GEOSCI, V98, DOI 10.1017/njg.2019.10; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; Ogg JG, 2016, CONCISE GEOLOGIC TIME SCALE 2016, P1; Powell A.J., 1992, P155; RGD, 1980, Verhandelingen KNGMG, V32, P77; Sliwinska KK, 2019, J MICROPALAEONTOL, V38, P143, DOI 10.5194/jm-38-143-2019; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; TNO-GDN, 2023, Stratigrafische Nomenclator van Nederland; Van Adrichem Boogaert A.H., 1993, Stratigraphic Nomenclature of the Netherlands, revision and update by RGD and NOGEPA, P39; Van Simaeys S, 2005, REV PALAEOBOT PALYNO, V134, P105, DOI 10.1016/j.revpalbo.2004.12.003; Vandenberghe N., 2014, Memoirs of the Geological Survey of Belgium, V60; Vandenberghe N., 2023, Lithostratigraphic Information Sheets Rupel Group; Vandenberghe N., 2001, The Netherlands, Aardkundige Mededelingen, V11; Vandenberghe N, 2014, GEOL BELG, V17, P161; Vandenberghe N, 2013, NEWSL STRATIGR, V46, P319, DOI 10.1127/0078-0421/2013/0034; Vernes R.W., 2023, Geologisch en hydrogeologisch 3D model van het Cenozoicum van de Belgisch-Nederlandse grensstreek van De Noorderkempen/West-Brabant (H3O-De Voorkempen), P156; Vis GJ, 2016, NETH J GEOSCI, V95, P221, DOI 10.1017/njg.2016.25	35	1	1	0	0	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	0016-7746	1573-9708		NETH J GEOSCI	Neth. J. Geosci.	MAY 13	2024	103								e11	10.1017/njg.2024.10	http://dx.doi.org/10.1017/njg.2024.10			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QE9T9		gold			2025-03-11	WOS:001219327500001
J	Rodríguez-Barreiro, I; Santos, AA; Villanueva-Amadoz, U; Louwye, S; Robinson, SA; Diez, JB				Rodriguez-Barreiro, Ivan; Santos, Artai A.; Villanueva-Amadoz, Uxue; Louwye, Stephen; Robinson, Stuart A.; Diez, Jose B.			Lead-up and manifestation of the Oceanic Anoxic Event 2 at the DSDP Site 398 (Vigo Seamount, NW Iberian offshore): Palynological and geochemical insights	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paleopalynology; Cenomanian-Turonian Boundary Event; Bonarelli Event; Black shales; Hatteras Formation; Mid-Cretaceous	DINOFLAGELLATE CYST ASSEMBLAGES; ATMOSPHERIC CARBON-DIOXIDE; TURONIAN BOUNDARY EVENT; PALEOENVIRONMENTAL ANALYSIS; STRATOTYPE SECTION; INTERIOR BASIN; RECORD; NORMAPOLLES; DINOCYST; PHYTOPLANKTON	Extreme climatic conditions, volcanism, and paleogeographical distribution presumably led to the Oceanic Anoxic Event 2 (OAE 2), one of the most disruptive events for Cretaceous ecosystems. Although the terrestrial response to this issue is barely studied, a turnover within the plant communities seems to be linked to the OAE 2, besides the well-known extinction of several marine groups. In this study, palynological and 813Corg analyses were combined to research the sediments from DSDP Site 398 (Vigo Seamount) cores 398D-58 to 398D-56 (upper Albian to lower Turonian). The 813Corg curve exhibits a Carbon Isotopic Excursion (CIE) observed between the interval 948,60 and 947,77 m below seafloor (mbsf), corresponding to the OAE 2. Four palynological assemblages were differentiated, ranging from the uppermost Albian to the lower Turonian. These assemblages comprised diverse marine and terrestrial communities with generally excellent preservation. In addition to previous biostratigraphic works, we present a more detailed chronostratigraphy of DSDP Hole 398D based on palynomorphs. The paleoecological reconstruction reveals the significant changes during the OAE 2 period: a decrease in the diversity and abundance of dinoflagellate cysts and a shift to angiosperm-dominated terrestrial communities (i.e., Normapolles) which, unlike other sites, occurs prior to the maximum values of 813C.	[Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo, Ctr Invest Marinas, BASAN, Vigo 36310, Spain; [Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo, Dept Xeociencias Marinas & Ordenac Terr, Vigo 36310, Spain; [Santos, Artai A.] Swedish Museum Nat Hist, Dept Palaeobiol, SE-10405 Stockholm, Sweden; [Villanueva-Amadoz, Uxue] UNAM, Inst Geol, Estn Reg Noroeste ERNO, Hermosillo 83000, Mexico; [Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Robinson, Stuart A.] Univ Oxford, Dept Earth Sci, Oxford, England; [Rodriguez-Barreiro, Ivan] Univ Vigo, Ctr Invest Marina, BASAN, Vigo 36310, Spain	Universidade de Vigo; Universidade de Vigo; Swedish Museum of Natural History; Universidad Nacional Autonoma de Mexico; Ghent University; University of Oxford; Universidade de Vigo; CIM UVIGO	Rodríguez-Barreiro, I (通讯作者)，Univ Vigo, Ctr Invest Marinas, BASAN, Vigo 36310, Spain.; Rodríguez-Barreiro, I (通讯作者)，Univ Vigo, Ctr Invest Marina, BASAN, Vigo 36310, Spain.	ivan.rodriguez.barreiro@uvigo.gal	Louwye, Stephen/D-3856-2012; Villanueva-Amadoz, Uxue/G-9899-2015; Santos, Artai/AAM-4202-2021; Robinson, Stuart/C-4808-2011	Rodriguez-Barreiro, Ivan/0000-0002-0938-662X; Villanueva Amadoz, Uxue/0000-0002-5189-5911	Xunta de Galicia (Spain) [EDC431C-2019/28]; European Social Fund -European Union [ED481A-2020/175]; Swedish Research Council [VR 2022-03920]; Universidade de Vigo/CISUG	Xunta de Galicia (Spain)(Xunta de Galicia); European Social Fund -European Union; Swedish Research Council(Swedish Research Council); Universidade de Vigo/CISUG	The authors are grateful to the Bremen Core Repository for providing the sample material used to carry out this study. We also appreciate the services provided by the CACTI for Scanning Electron Microscopy and IRMS analysis. Funding for this research was provided by the Xunta de Galicia (Spain) , through project EDC431C-2019/28. IRB was supported by a predoctoral fellowship from the Xunta de Galicia (Spain) and the European Social Fund -European Union (ref.: ED481A-2020/175) . AAS was supported by a postdoctoral fellowship from the Swedish Research Council Grant (VR 2022-03920) managed by Dr. Stephen McLoughlin. We gratefully acknowledge the constructive suggestions of the editor Dr. Bing Shen, as well as Dr. Elke Schneebeli and other three anonymous reviewers. Funding for open access charge: Universidade de Vigo/CISUG.	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J	Shang, LX; Hu, ZX; Deng, YY; Li, J; Liu, YY; Song, XY; Zhai, XY; Zhan, ZF; Tian, W; Xu, JX; Han, YC; Shen, H; Ding, H; Tang, YZ				Shang, Lixia; Hu, Zhangxi; Deng, Yunyan; Li, Jing; Liu, Yuyang; Song, Xiaoying; Zhai, Xinyu; Zhan, Zifeng; Tian, Wen; Xu, Jinxiang; Han, Yangchun; Shen, Hao; Ding, Hua; Tang, Ying Zhong			Transoceanic ships as a source of alien dinoflagellate invasions of inland freshwater ecosystems	HARMFUL ALGAE			English	Article						Harmful algal blooms (HABs); Ballast water; Ballast tank sediments; Dinoflagellate resting cyst; Invasion; Intraspecific variation	BALLAST TANK SEDIMENTS; HARMFUL ALGAL BLOOMS; SP-NOV DINOPHYCEAE; CYST-THECA RELATIONSHIP; ALEXANDRIUM-OSTENFELDII DINOPHYCEAE; MULTIPLE SEQUENCE ALIGNMENT; PERIDINIUM-ACICULIFERUM; BIOLOGICAL INVASIONS; COASTAL WATERS; MOLECULAR CHARACTERIZATION	Ships' ballast water and sediments have long been linked to the global transport and expansion of invasive species and thus have become a hot research topic and administrative challenge in the past decades. The relevant concerns, however, have been mainly about the ocean-to-ocean invasion and sampling practices have been almost exclusively conducted onboard. We examined and compared the dinoflagellate cysts assemblages in 49 sediment samples collected from ballast tanks of international and domestic routes ships, washing basins associated with a ship-repair yard, Jiangyin Port (PS), and the nearby area of Yangtze River (YR) during 2017-2018. A total of 43 dinoflagellates were fully identified to species level by metabarcoding, single-cyst PCR-based sequencing, cyst germination and phylogenetic analyses, including 12 species never reported from waters of China, 14 HABs-causing, 9 toxic, and 10 not strictly marine species. Our metabarcoding and single-cyst sequencing also detected many OTUs and cysts of dinoflagellates that could not be fully identified, indicating ballast tank sediments being a risky repository of currently unrecognizable invasive species. Particularly important, 10 brackish and fresh water species of dinoflagellate cysts (such as Tyrannodinium edax) were detected from the transoceanic ships, indicating these species may function as alien species potentially invading the inland rivers and adjacent lakes if these ships conduct deballast and other practices in fresh waterbodies. Significantly higher numbers of reads and OTUs of dinoflagellates in the ballast tanks and washing basins than that in PS and YR indicate a risk of releasing cysts by ships and the associated ship-repair yards to the surrounding waters. Phylogenetic analyses revealed high intra-species genetic diversity for multiple cyst species from different ballast tanks. Our work provides novel insights into the risk of bio-invasion to fresh waters conveyed in ship's ballast tank sediments and washing basins of shipyards.	[Shang, Lixia; Hu, Zhangxi; Deng, Yunyan; Liu, Yuyang; Song, Xiaoying; Zhai, Xinyu; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Shang, Lixia; Hu, Zhangxi; Deng, Yunyan; Liu, Yuyang; Tang, Ying Zhong] Qingdao Marine Sci & Technol Ctr, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Shang, Lixia; Hu, Zhangxi; Deng, Yunyan; Liu, Yuyang; Song, Xiaoying; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Li, Jing; Tian, Wen; Xu, Jinxiang; Han, Yangchun; Shen, Hao; Ding, Hua] Comprehens Tech Serv Ctr Jiangyin Customs, State Key Lab Ballast Water Res, Jiangyin 214431, Peoples R China; [Song, Xiaoying; Zhai, Xinyu] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Zhan, Zifeng] Chinese Acad Sci, Lab Marine Organism Taxon & Phylogeny, Qingdao Key Lab Marine Biodivers & Conservat, Shandong Prov Key Lab Expt Marine Biol,Inst Oceano, Qingdao 266071, Peoples R China; [Li, Jing] Quanzhou Normal Univ, Sch Oceanol & Food Sci, Quanzhou 362000, Peoples R China; [Tian, Wen] Anim Plant & Food Inspect Ctr Nanjing Customs, Nanjing 210000, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Chinese Academy of Sciences; Quanzhou Normal University	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023; Zhang, Xing/ACQ-5035-2022; Li, Yang/KFB-5350-2024	Hu, Zhangxi/0000-0002-4742-4973	National Natural Science Foundation of China [41976134, 42106199]; Science and Technology Innovation Project of Laoshan Laboratory [LSKJ202203700]; Nanjing Custom Research Project [2021KJ42]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Science and Technology Innovation Project of Laoshan Laboratory; Nanjing Custom Research Project	This work was supported by the National Natural Science Foundation of China (Grant No. 41976134), the Science and Technology Innovation Project of Laoshan Laboratory (Grant No. LSKJ202203700), the National Natural Science Foundation of China (Grant No. 42106199), and the Nanjing Custom Research Project (Grant No. 2021KJ42) .	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J	Telesinski, MM; Kucharska, M; Lacka, M; Zajaczkowski, M				Telesinski, Maciej M.; Kucharska, Malgorzata; Lacka, Magdalena; Zajaczkowski, Marek			A late response of the sea-ice cover to Neoglacial cooling in the western Barents Sea	HOLOCENE			English	Article						dinoflagellate cysts; Echinidinium karaense; Islandinium minutum; Late-Holocene; Operculodinium centrocarpum s.l.; PIP25; Storfjordrenna; Svalbard; XRF	NORTHERN NORTH-ATLANTIC; CYST-THECA RELATIONSHIP; DINOFLAGELLATE CYSTS; HOLOCENE CLIMATE; ESTUARINE SEDIMENTS; OXYGEN-ISOTOPE; NORDIC SEAS; WATER-FLOW; KA BP; VARIABILITY	In high northern latitudes, the Middle to Late-Holocene was a time of orbitally-induced atmospheric cooling. This led to increased sea-ice production in the Arctic Ocean and its export southward, a decrease in sea surface temperatures (SST), and glacier advances at least since 5-4 ka BP. However, the response of the ocean-climate system to decreasing insolation was not uniform. Our research shows that the sea-ice cover in the northwestern Barents Sea experienced a late response to Neoglacial cooling. We analyzed dinoflagellate cyst assemblages from a sediment core from Storfjordrenna, south of Svalbard. We found that the area experienced ice-free conditions throughout most of the Mid- and Late-Holocene. It was only after 2.3 ka BP that the study site became covered with winter drift ice and primary productivity decreased subsequently. Other regional data support the decrease in SST, the expansion of the sea-ice cover, and the deterioration of the environmental conditions around that time. Our findings indicate that the sea-ice cover in the northwestern Barents Sea required a significant amount of time to respond to the general cooling trend in the region. These results have important implications for present-day environmental changes. Even if the current warming trend is revoked in the future, the observed sea-ice loss in the Barents Sea may be incredibly challenging to reverse.	[Telesinski, Maciej M.; Kucharska, Malgorzata; Lacka, Magdalena; Zajaczkowski, Marek] Polish Acad Sci, Inst Oceanol, Sopot, Poland; [Telesinski, Maciej M.] Polish Acad Sci, Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland	Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences	Telesinski, MM (通讯作者)，Polish Acad Sci, Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland.	mtelesinski@iopan.pl	Łącka, Magdalena/P-2071-2019; Telesiński, Maciej Mateusz/K-1717-2017; Telesinski, Maciej Mateusz/I-6527-2015	Telesinski, Maciej Mateusz/0000-0002-5765-2849	National Science Centre, Poland [2020/39/B/ST10/01698]	National Science Centre, Poland(National Science Centre, Poland)	The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This study was supported by grant no. 2020/39/B/ST10/01698 funded by the National Science Centre, Poland.	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J	Wubben, E; Spiering, BR; Veenstra, T; Bos, R; Wang, ZY; van Dijk, J; Raffi, I; Witkowski, J; Hilgen, FJ; Peterse, F; Sangiorgi, F; Sluijs, A				Wubben, Evi; Spiering, Bianca R.; Veenstra, Tjerk; Bos, Remco; Wang, Zongyi; van Dijk, Joost; Raffi, Isabella; Witkowski, Jakub; Hilgen, Frederik J.; Peterse, Francien; Sangiorgi, Francesca; Sluijs, Appy			Tropical Warming and Intensification of the West African Monsoon During the Miocene Climatic Optimum	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						Miocene Climatic Optimum; tropical sea surface temperature warming; West African Monsoon; dinoflagellate cysts; orbital climate variability	SEA-SURFACE TEMPERATURE; ISOPRENOID TETRAETHER LIPIDS; WALLED DINOFLAGELLATE CYSTS; MIDDLE MIOCENE; EQUATORIAL ATLANTIC; WATER-COLUMN; ISOTOPE STRATIGRAPHY; PARTICULATE MATTER; MARINE-SEDIMENTS; MEMBRANE-LIPIDS	Studying monsoon dynamics during past warm time periods such as the Miocene Climatic Optimum (MCO; similar to 16.9-14.5 Ma) could greatly aid in better projecting monsoon intensity, in the context of future greenhouse warming. However, studies on regional MCO temperature change and its effect on the monsoons during this time period are lacking. Here, we present the first high-resolution, low-latitude record of sea surface temperature (SST) and paleoceanographic change covering the Miocene Climatic Optimum, in the eastern equatorial Atlantic, at Ocean Drilling Program Site 959, based on TEX86 paleothermometry. SSTs were similar to 1.5 degrees C warmer at the onset of the MCO (16.9 Ma) relative to the pre-MCO (similar to 18.3-17.7 Ma). This warming was accompanied by a transient increase in %total organic carbon. Prior to the MCO, sediment composition, geochemical proxy data as well as dinoflagellate cyst assemblages imply a productive surface ocean at Site 959. Immediately following the MCO onset (similar to 16.9-16.5 Ma), we record an intensification of the West African Monsoon (WAM) characterized by higher amplitude variability in all proxy records on precession to obliquity timescales. We interpret increased orbital-scale SST, biogenic Ba and dinocyst assemblage variability to represent intensification of equatorial upwelling, forced by the WAM strength. Furthermore, higher SSTs during eccentricity maxima correlate to increased relative abundances of the warm and stratification-favoring dinocyst Polysphaeridium zoharyi, during periods of low WAM intensity. Finally, while long-term SSTs decline toward the middle Miocene, maximum SSTs and Polysphaeridium zoharyi abundances occur during MCO peak warming at similar to 15.6 Ma. The global climate during the Miocene Climatic Optimum (MCO) (similar to 16.9-14.5 Ma) was warm, perhaps similar to the future. Better understanding the climate system during this time period could aid in predicting future climate change. Tropical climates are the engine of global climate because they transport heat and moisture to higher latitudes with winds and ocean currents. Monsoons are an important feature of tropical climates. Importantly, continuous sea surface temperature reconstructions covering the MCO from the tropics are lacking. Here, we present an unprecedented resolution novel sea surface temperature record using sediments recovered in the eastern equatorial Atlantic Ocean which cover the MCO. Surface ocean temperatures rose by similar to 1.5 degrees C between the Early Miocene (similar to 18.3-17.7 Ma) and the onset of the MCO. Concomitantly, we record an increase in wind strength, surface ocean mixing and biological growth in the ocean, caused by a stronger West African Monsoon in this warmer climate. The monsoon strength is also strongly determined by variations in solar insolation, through periodic variations in the Earth's orbit. The recorded monsoon intensification with warming is consistent with projections of future monsoons under modern global warming. The first high-resolution tropical sea surface temperature record shows that the Miocene Climatic Optimum was similar to 1.5 degrees C warmer than the Early Miocene in the eastern equatorial Atlantic The West African Monsoon intensified following warming at similar to 17 Ma, resulting in variable surface ocean conditions forced by orbital cycles Intensification of the monsoon system caused increased dust supply and strong upwelling alternating with hyperstratification	[Wubben, Evi; Spiering, Bianca R.; Veenstra, Tjerk; Bos, Remco; Wang, Zongyi; van Dijk, Joost; Hilgen, Frederik J.; Peterse, Francien; Sangiorgi, Francesca; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands; [Raffi, Isabella] Univ GD Annunzio Chieti, Int Res Sch Planetary Sci IRSPS, Pescara, Italy; [Witkowski, Jakub] Univ Szczecin, Inst Marine & Environm Sci, Szczecin, Poland	Utrecht University; G d'Annunzio University of Chieti-Pescara; University of Szczecin	Wubben, E (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands.	e.wubben@uu.nl	Raffi, Isabella/AAY-5505-2020; Sluijs, Appy/B-3726-2009; Witkowski, Jakub/HMD-6743-2023; Peterse, Francien/AAY-1473-2021; Peterse, Francien/H-5627-2011	Peterse, Francien/0000-0001-8781-2826; Bos, Remco/0000-0002-3664-3265; Wubben, Evi/0000-0002-2478-0748; Spiering, Bianca/0009-0007-8561-0922	European Research Council [771497]; Horizon 2020 program; European Research Council (ERC) [771497] Funding Source: European Research Council (ERC)	European Research Council(European Research Council (ERC)); Horizon 2020 program; European Research Council (ERC)(European Research Council (ERC))	This research used samples and data from the International Ocean Discovery Program (IODP) and its predecessors (Ocean Drilling Program; ODP) and we are grateful to H. Kuhlmann and A. Wuelbers at the Bremen Core Repository for facilitating the intensive sampling of the core. This work is funded by the European Research Council Consolidator Grant 771497, funded by the Horizon 2020 program to A. Sluijs. We thank Antoinette van den Dikkenberg, Joost van Dijk, Harvey de Graaff, Desmond Eefting, Coen Mulder and Natasja Welters for laboratory assistance and technical support. We thank Henk Brinkhuis for discussions on dinoflagellate cyst taxonomy and an anonymous reviewer and Prof. dr. Sarah Feakins for constructive reviews.	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Paleoclimatology	MAY	2024	39	5							e2023PA004767	10.1029/2023PA004767	http://dx.doi.org/10.1029/2023PA004767			27	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	PP8Z1		Green Submitted, hybrid			2025-03-11	WOS:001215387300001
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J	Ghasemi-Nejad, E; Esmaili, P; Majidifard, MR; Sharifi, M				Ghasemi-Nejad, Ebrahim; Esmaili, Parvin; Majidifard, Mahmoud Reza; Sharifi, Mohammad			Biostratigraphy of Bajocian-Oxfordian strata based on dinoflagellate cysts and ammonites from the Dalichai Formation, northeastern Iran	PALAEOWORLD			English	Article						Middle Jurassic; northern Tethyan Realm; Binalud Mountains; biostratigraphy; dinoflagellate cysts; ammonites	JURASSIC SYSTEM; SHEMSHAK GROUP; MIDDLE; NORTH; ALBORZ; PALEOBIOGEOGRAPHY; TECTONICS; EVOLUTION; RADIATION; ORIGIN	The Bajocian-Oxfordian Dalichai Formation of the Binalud Mountains (northeastern Iran) consists of marls, marly limestones and limestones that were sampled and studied in detail for their palynomorph and ammonite contents. Palynological studies enabled differentiation of three marine biozones (Cribroperidinium crispum, Dichadogonyaulax sellwoodii, and Ctenidodinium continuum) within the lower interval of the formation. The palynofacies analysis shows a gradual sea-level rise during the depositional period of the rock unit, while terrestrial palynomorphs (spores and pollen grains) revealed a predominantly tropical climate for the time interval. Furthermore, a large number of ammonites were recovered from the formation, based on which 12 families, 22 genera, 30 species and 12 biozones (Zigzag, Aurigerus, Retrocostatum, Discus, Bullatus, Gracilis, Anceps, Coronatum, Athleta, Transversarium, Bifurcatus, and Bimammatum) were differentiated. When comparing the dinoflagellate cyst zones with the ammonite zones, the Dichadogonyaulax sellwoodii dinoflagellate cyst zone was correlated with the ammonite zones of Zigzag, Aurigerus, Retrocostatum, Discus, Bullatus, and Gracilis and the Ctenidodinium continuum dinocyst zone was correlated with the Gracilis and Anceps ammonite zones. The dinocyst and ammonite assemblages of the Binalud Mountains are similar to assemblages described from northern and northeastern Iran (Alborz and Koppeh-Dagh basins) as well as Northwest Europe. This suggests marine connections between these sedimentary basins during the Bajocian-Oxfordian. Consequently, the integrated dinocyst and ammonite zonation established here can be utilized also in other parts of the northern Tethyan Realm. The diachroneity of the upper boundary of the Dichadogonyaulax sellwoodii Zone between the Binalud Mountains and Northwest Europe is however revealed by comparison with the ammonite zones. (c) 2023 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.	[Ghasemi-Nejad, Ebrahim] Univ Tehran, Coll Sci, Dept Geol, Tehran, Iran; [Esmaili, Parvin; Majidifard, Mahmoud Reza] Geol Survey Iran, Res Inst Earth Sci, Tehran, Iran; [Sharifi, Mohammad] Univ Kurdistan, Fac Sci, Dept Earth Sci, Sanandaj, Iran	University of Tehran; University of Kurdistan	Sharifi, M (通讯作者)，Univ Kurdistan, Fac Sci, Dept Earth Sci, Sanandaj, Iran.	m.sharifi@uok.ac.ir	Sharifi, Mohammad/KZV-0123-2024	Sharifi, Mohammad/0000-0003-2351-7670	Geological Survey of Iran (GSI); University of Tehran; University of Kurdistan	Geological Survey of Iran (GSI)(Geological Survey & Mineral Exploration of Iran); University of Tehran(University of Tehran); University of Kurdistan(University of Kurdistan)	The authors express their sincere gratitude to the Geological Survey of Iran (GSI) and the universities of Tehran and Kurdistan for their support. Prof. Niels E. Poulsen, Prof. Franz Fuersich, an anonymous reviewer and the jour- nal's editors are greatly thanked for reviewing the manuscript and giving many insightful comments that improved the paper. This paper is dedicated to the late Prof. Ebrahim Ghasemi-Nejad who passed away during the course of this study.	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J	Iakovleva, AI; Zakrevskaya, EY; Shcherbinina, EA				Iakovleva, Alina I.; Zakrevskaya, Elena Y.; Shcherbinina, Ekaterina A.			Middle Eocene to earliest Oligocene dinoflagellate cysts from southern Armenia: biostratigraphy and palaeoecology	PALYNOLOGY			English	Article						Middle Eocene-earliest Oligocene; dinoflagellate cysts; palynomorphs; biostratigraphy; palaeosettings; Armenia	RESEARCH BOREHOLE; SECTION; PALEOCENE; STRATIGRAPHY; NANNOFOSSILS; TRANSITION; ZONATION	The results of a palynological study of the middle Eocene-lowermost Oligocene strata of the Shagap and Landzhar outcrop sections (southern Armenia) are presented. A series of stratigraphically important dinoflagellate cyst events were recognized in the uppermost Lutetian-lowermost Rupelian parts of the sections, including the lowermost occurrences of the key-species Rhombodinium draco, Schematophora speciosa, Hemiplacophora semilunifera, Hapsocysta kysingensis, Thalassiphora? cf. rota, Rhombodinium porosum, Glaphyrocysta semitecta, Reticulatosphaera actinocoronata, Stoveracysta ornata-group and Wetzeliella gochtii. Based on the first-order calibrations with calcareous nannoplankton and foraminifers, R. draco first occurs at the Lutetian-Bartonian transition, while the lowermost occurrence of R. actinocoronata is very close to the Bartonian-Priabonian boundary. The analysis of the ratios of palynogroups and dinoflagellate eco-groups permits to interpret the environmental conditions during the accumulation of regional formations: (1) a major marine transgression started at the beginning of the Lutetian and the gradual deepening of the marine basin occurred during the middle-late Lutetian (Arpa Formation); (2) the marine transgression, accompanied by deepening, continued during the early Bartonian, but towards the end of the Bartonian slightly shallower depositional conditions were established (Azatek Formation); (3) the sea continued to gradually become shallower during the Priabonian (Urtsadzor Formation) and, finally, the maximum of regression was observed at the Eocene-Oligocene transition, ending with the establishment of brackish environments at the beginning of Rupelian (Shagap Formation).	[Iakovleva, Alina I.; Shcherbinina, Ekaterina A.] Russian Acad Sci, Geol Inst, Moscow, Russia; [Zakrevskaya, Elena Y.] Russian Acad Sci, Sci Dept, Vernadsky State Geol Museum, Moscow, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences	Iakovleva, AI (通讯作者)，Russian Acad Sci, Geol Inst, Moscow, Russia.	alina.iakovleva@gmail.com			Russian Foundation for Basic Research [15-55-05102, 18-55-05017]; State Committee for Science of the Republic of Armenia [SCS 18RF-090]; Russian State program of the Geological Institute of Russian Academy of Sciences [1021061009468-8-1.5.1]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); State Committee for Science of the Republic of Armenia; Russian State program of the Geological Institute of Russian Academy of Sciences	We are grateful to our Armenian colleagues F.A. Hayrapetyan, L.G. Sahakyan, T.E. Grigoryan and K.B. Meliksetyan from the Institute of Geological Sciences of the Armenian National Academy of Sciences for the organization of the fieldwork in 2013-2019. G.N. Aleksandrova (GIN RAS) is thanked for the chemical preparation of palynological samples. Thanks to Henk Brinkhuis (Utrecht University) for fruitful discussions on the Eocene dinoflagellate cysts. Claus Heilmann-Clausen, Peter Bijl and an anonymous reviewer are thanked for their careful and very constructive reviews, which improved the paper. We also thank James Riding for his very helpful editorial suggestions. The fieldwork in southern Armenia was funded by the Russian Foundation for Basic Research (RFFI project No. 15-55-05102 and 18-55-05017) and the State Committee for Science of the Republic of Armenia (project SCS 18RF-090). The research of A.I. Iakovleva and E. A. Shcherbinina was supported by the Russian State program of the Geological Institute of Russian Academy of Sciences. The research of E.Y. Zakrevskaya was carried out within the framework of the state assignment to SGM RAS 1021061009468-8-1.5.1 (Vernadsky State Geological Museum).	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J	Roza, SEV; Versteegh, GJM; Pospelova, V; Zonneveld, KAF				Roza, Surya Eldo V.; Versteegh, Gerard J. M.; Pospelova, Vera; Zonneveld, Karin A. F.			Environmental control of interannual and seasonal variability in dinoflagellate cyst export flux over 18 years in the Cape Blanc upwelling region (Mauritania)	FRONTIERS IN MARINE SCIENCE			English	Article						dinoflagellate cysts; ecology; coastal upwelling; Saharan dust; interannual variability; ecosystem change	SEA-SURFACE TEMPERATURE; AFRICAN DUST TRANSPORT; SEDIMENT TRAP; GYMNODINIUM-CATENATUM; NORTHWEST AFRICA; ECOLOGICAL ROLES; COASTAL; OCEAN; DINOPHYCEAE; BASIN	The increasing threat of anthropogenic environment and climate change amplifies the urgency to investigate the effect of these changes on marine ecosystems. We provide information about the export flux of organic-walled dinoflagellate cysts between 2003 and 2020 in the upwelling ecosystem off Cape Blanc (Mauritania), one of the world's most productive regions. We compared the cyst export flux with variability in environmental parameters, such as wind speed, wind direction, dust emission, sea surface temperature (SST), SST difference between trap location and open ocean (SSTa), and chlorophyll-a concentration. This information is valuable to determine the ecological signal of dinoflagellate cysts that could be applied in recent and paleo records. The total export production of dinoflagellate cysts fluctuated between 0 - 1.18 x 105 cysts m-2 d-1 for the heterotrophs and 0 - 1.06 x 104 cysts m-2 d-1 for the photo-/mixotrophs. The export productions of both groups were in line with changes in upwelling intensity, which in most years, intensified in spring - summer. Dinoflagellate cyst association was dominated by heterotrophic taxa that formed an average of 94% of the association throughout the sediment trap record. A strong interannual variation in the cyst export fluxes, as well as the association composition was observed in the record. We identified five groups that showed comparable variability in export production with changes in environmental conditions: (1) maximal upwelling; Echinidinium delicatum/granulatum, E. transparantum/zonneveldiae, Echinidinium spp., Trinovantedinium spp., and Protoperidinium latidorsale, (2) combined maximal upwelling and dust input; Archaeperidinium spp., P. americanum, P. stellatum, and P. subinerme, (3) upwelling relaxation; Gymnodinium spp. and L. polyedra, (4) warm surface waters; Bitectatodinium spongium and Protoceratium reticulatum, (5) species with no specific relationship to the studied environmental variables; Brigantedinium spp., E. aculeatum, Impagidinium aculeatum, P. conicum, P. monospinum, Pentapharsodinium dalei, and Spiniferites spp. The sediment trap record documented a gradual shift in the cyst taxa association that co-occurred with the gradual increase of Saharan dust input to the region, notably after 2008. The cyst association contained five photo-/mixotrophic taxa that were formed by potentially toxic dinoflagellates. The latter could cause threats to the socio-economy of coastal communities.	[Roza, Surya Eldo V.; Zonneveld, Karin A. F.] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Versteegh, Gerard J. M.; Zonneveld, Karin A. F.] Univ Bremen, Dept Geosci, Bremen, Germany; [Versteegh, Gerard J. M.] Constructor Univ, Dept Phys & Earth Sci, Bremen, Germany; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN USA	University of Bremen; University of Bremen; University of Minnesota System; University of Minnesota Twin Cities	Roza, SEV (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany.	eroza@marum.de		Roza, Surya Eldo Virma/0009-0000-6586-8722; Pospelova, Vera/0000-0003-4049-8133	German Research Foundation (DFG) through MARUM Excellence Cluster "The Ocean in the Earth System"	German Research Foundation (DFG) through MARUM Excellence Cluster "The Ocean in the Earth System"(German Research Foundation (DFG))	The authors thank the captains and crew members of RV Poseidon, RV METEOR, and RV Maria S. Merian, the MARUM sediment trap team for deploying and recovering the sediment trap, and all institutions and individuals who have participated and contributed throughout this research. The authors are also thankful of the support from German, Moroccan, and Mauritanian authorities. The work was supported by the Hanse-Wissenschaftskolleg (HWK) senior research fellowship in marine and climate research to Dr. Pospelova during her 2016 sabbatical at the Institute for Advanced Study (Germany) with Prof. Zonneveld group at the University of Bremen.r The author(s) declare financial support was received for the research, authorship, and/or publication of this article. This comprehensive research is supported by the funding from German Research Foundation (DFG) through MARUM Excellence Cluster "The Ocean in the Earth System".	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Mar. Sci.	APR 15	2024	11								1284425	10.3389/fmars.2024.1284425	http://dx.doi.org/10.3389/fmars.2024.1284425			22	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	OT0L9		gold			2025-03-11	WOS:001209412000001
J	Strack, T; Jonkers, L; Rillo, MC; Baumann, KH; Hillebrand, H; Kucera, M				Strack, T.; Jonkers, L.; Rillo, M. C.; Baumann, K. -H.; Hillebrand, H.; Kucera, M.			Coherent response of zoo-and phytoplankton assemblages to global warming since the Last Glacial Maximum	GLOBAL ECOLOGY AND BIOGEOGRAPHY			English	Article						biodiversity; coccolithophores; dinoflagellate cysts; last deglaciation; microfossils; planktonic foraminifera	WALLED DINOFLAGELLATE CYSTS; SURFACE TEMPERATURES; MARINE BIODIVERSITY; SOUTHERN-OCEAN; CLIMATE-CHANGE; PRESERVATION; RECONSTRUCTION; DIVERSITY; EVOLUTION; ABUNDANCE	Aim: We are using the fossil record of different marine plankton groups to determine how their biodiversity has changed during past climate warming comparable to projected future warming. Location: North Atlantic Ocean and adjacent seas. Time series cover a latitudinal range from 75 degrees N to 6 degrees S. Time period: Past 24,000 years, from the Last Glacial Maximum (LGM) to the current warm period covering the last deglaciation. Major taxa studied: Planktonic foraminifera, dinoflagellates and coccolithophores. Methods: We analyse time series of fossil plankton communities using principal component analysis and generalized additive models to estimate the overall trend of temporal compositional change in each plankton group and to identify periods of significant change. We further analyse local biodiversity change by analysing species richness, species gains and losses, and the effective number of species in each sample, and compare alpha diversity to the LGM mean. Results: All plankton groups show remarkably similar trends in the rates and spatio-temporal dynamics of local biodiversity change and a pronounced non-linearity with climate change in the current warm period. Assemblages of planktonic foraminifera and dinoflagellates started to change significantly with the onset of global warming around 15,500 to 17,000 years ago and continued to change at the same rate during the current warm period until at least 5000 years ago, while coccolithophore assemblages changed at a constant rate throughout the past 24,000 years, seemingly irrespective of the prevailing temperature change. Main conclusions: Climate change during the transition from the LGM to the current warm period led to a long-lasting reshuffling of zoo-and phytoplankton assemblages, likely associated with the emergence of new ecological interactions and possibly a shift in the dominant drivers of plankton assemblage change from more abiotic-dominated causes during the last deglaciation to more biotic-dominated causes with the onset of the Holocene.	[Strack, T.; Jonkers, L.; Baumann, K. -H.; Kucera, M.] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Rillo, M. C.; Hillebrand, H.] Inst Chem & Biol Marine Environments ICBM, Wilhelmshaven, Germany; [Baumann, K. -H.] Univ Bremen, Dept Geosci, Bremen, Germany; [Hillebrand, H.] Carl von Ossietzky Univ Oldenburg, Helmholtz Inst Funct Marine Biodivers HIFMB, Oldenburg, Germany; [Hillebrand, H.] Alfred Wegener Inst AWI, Helmholtz Ctr Polar & Marine Res, Bremerhaven, Germany	University of Bremen; University of Bremen; Carl von Ossietzky Universitat Oldenburg; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Strack, T (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany.	strack@marum.de	Kucera, Michal/ABH-6065-2020; Costa Rillo, Marina/GYJ-6389-2022; Jonkers, Lukas/H-6314-2011; Kucera, Michal/B-9277-2009; Hillebrand, Helmut/I-1717-2014	Costa Rillo, Marina/0000-0002-2471-0002; Strack, Tonke/0000-0003-4748-528X; Jonkers, Lukas/0000-0002-0253-2639; Kucera, Michal/0000-0002-7817-9018; Hillebrand, Helmut/0000-0001-7449-1613	Bundesministerium fur Bildung und Forschung (PALMOD); 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Ecol. Biogeogr.	JUN	2024	33	6							e13841	10.1111/geb.13841	http://dx.doi.org/10.1111/geb.13841		APR 2024	18	Ecology; Geography, Physical	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography	QU2O4		Green Published			2025-03-11	WOS:001197321000001
J	Cardenas, D; Rodríguez, G; Pinzón, D; Vargas, MC; Parra, FD; Louwye, S				Cardenas, Damian; Rodriguez, Guillermo; Pinzon, Diego; Vargas, Maria Carolina; Parra, Felipe de la; Louwye, Stephen			The Neogene record of the dinoflagellate cyst genus Trinovantedinium Reid 1977 in the tropical Americas	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Miocene; Pliocene; Peridinioid dinoflagellate cysts; Biostratigraphy; Caribbean; Eastern equatorial Pacific	PALEOECOLOGY; PACIFIC; MIOCENE; STRATIGRAPHY	The genus Trinovantedinium Reid 1977 comprises eleven Neogene-Quaternary and one Paleogene dinoflagellate cyst taxa that have been successfully used for biostratigraphy. Combining new and published records of Trinovantedinium species in the Neogene of the tropical Americas, we report preliminary stratigraphic ranges for T. applanatum (Aquitanian-Recent), T. ferugnomatum (Burdigalian-Zanclean), T. glorianum (Burdigalian-Messinian), T. papula (Aquitanian-Zanclean), T. uitpensis (Aquitanian-Tortonian), T. variabile (Aquitanian-Recent) and T.? xylochoporum (Aquitanian-Messinian) in the region. Although the stratigraphic ranges of T. applanatum, T. variabile and T.? xylochoporum in the tropical Americas seem to be coetaneous with previous records elsewhere, the first appearance datums of T. ferugnomatum, T. glorianum and T. papula seem to be at least similar to 2-3 Myr. older in the tropical Americas. In contrast, only the last appearance datum of T. glorianum seems to be similar to 4 Myr. younger in the Northern Hemisphere. Our results demonstrate that the Cenozoic marine palynological record of the tropical Americas is therefore key to discriminate dinoflagellate cyst stratigraphic ranges across latitudes.	[Cardenas, Damian] Univ Nacl Colombia, Dept Geosci, Bogota, Colombia; [Rodriguez, Guillermo; Vargas, Maria Carolina; Parra, Felipe de la] Inst Colombiano Petr, Biostratig Team, Ecopetrol, Bogota, Santander, Colombia; [Pinzon, Diego] Consejo Nacl Invest Cient & Tecn, Inst Argentino Nivol Glaciol & Ciencias Ambiental, Mendoza, Argentina; [Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium	Universidad Nacional de Colombia; Ecopetrol; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Ghent University	Cardenas, D (通讯作者)，Univ Nacl Colombia, Dept Geosci, Bogota, Colombia.	dcardenasl@unal.edu.co	Rodriguez, Guillermo/JPA-4743-2023; Louwye, Stephen/D-3856-2012; Cardenas, Damian/AAB-3440-2020	Cardenas, Damian/0000-0002-9823-6470				Bijl PK, 2022, EARTH SYST SCI DATA, V14, P579, DOI 10.5194/essd-14-579-2022; Boyd JL, 2018, EARTH-SCI REV, V177, P366, DOI 10.1016/j.earscirev.2017.11.018; Bringué M, 2019, PROG OCEANOGR, V171, P175, DOI 10.1016/j.pocean.2018.12.007; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Cárdenas D, 2021, REV PALAEOBOT PALYNO, V290, DOI 10.1016/j.revpalbo.2021.104427; Cárdenas D, 2020, PALAEOGEOGR PALAEOCL, V558, DOI 10.1016/j.palaeo.2020.109955; Correa E, 2021, MAR MICROPALEONTOL, V167, DOI 10.1016/j.marmicro.2021.102024; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; De Verteuil L., 1996, P OCEAN DRILLING PRO, V150, P439; De Verteuil L., 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs, P391; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Duffield S.L., 1986, Papers from the First Symposium on Neogene Dinoflagellate Cyst Biostratigraphy. vol, V17, P27; Duque-Herrera AF, 2018, MAR MICROPALEONTOL, V141, P42, DOI 10.1016/j.marmicro.2018.05.002; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; HEAD MJ, 1993, J PALEONTOL, V67, P1; Helenes Javier, 2003, Palynology, V27, P5, DOI 10.2113/27.1.5; Jaramillo C, 2020, PALEOCEANOGR PALEOCL, V35, DOI 10.1029/2020PA003933; Jaramillo C, 2017, SCI ADV, V3, DOI 10.1126/sciadv.1601693; Leandro LM, 2020, MAR MICROPALEONTOL, V160, DOI 10.1016/j.marmicro.2020.101898; Louwye S, 2008, GEOL MAG, V145, P321, DOI 10.1017/S0016756807004244; Matsuoka K., 1987, Bull. 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Palaeobot. Palynology	JUN	2024	325								105100	10.1016/j.revpalbo.2024.105100	http://dx.doi.org/10.1016/j.revpalbo.2024.105100		APR 2024	8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	RA8P8					2025-03-11	WOS:001225046600001
J	Shevchuk, O; Vajda, V				Shevchuk, Olena; Vajda, Vivi			Cretaceous (Albian-Coniacian) dinoflagellate biostratigraphy of the Vomb Trough, southern Sweden	GFF			English	Article						Dinoflagellate cysts; Albian; Cenomanian; Turonian; Coniacian; biostratigraphy; southern Sweden	RECORD; BOUNDARY; IMPACT; DISTRIBUTIONS; STRATIGRAPHY; GEOLOGY; BASIN; PART	We document diverse and well-preserved dinoflagellate cyst assemblages from Cretaceous successions in the Kullemolla 1 drill core (640.0 m-590.0 m), Vomb Trough, southern Sweden. Palynology reveals a nearshore marine environment. Dinoflagellate index taxa indicate an Albian to Coniacian age, thus spanning the Early-Late Cretaceous boundary. The lower part of the core is Albian, based on the presence of the index dinocyst taxa Pareodinia and Callaiosphaeridium asymmetricum. The First Appearance Datum (FAD) of Oligosphaeridium prolixispinosum, together with the presence of Achomosphaera ramulifera, Heterosphaeridium difficile and Oligosphaeridium pulcherrimum, reveals a Cenomanian age for the interval 635- m-617 m. The Turonian interval is characterized by an increase in the dinocysts Chatangiella spectabilis and Florentinia spp., in combination with the FAD of Senoniasphaera rotundata, whereas the youngest samples are dated to the Coniacian as defined by the appearance of Glaphyrocysta sp.We show that Cenomanian and Turonian strata are indeed represented by a relatively condensed section between 635 m and 612 m in the Kullemolla 1 core showing that the apparent hiatus recorded by calcareous microfossils elsewhere is likely a result of post-depositional dissolution of calcareous tests and limestone, a process that did not affect the organic-walled plankton. This is further supported by the presence of hardgrounds and dissolution features.This updated, detailed biostratigraphical assessment based on dinoflagellates provides a framework for correlation with zonations based on other marine fossil groups, useful, for e.g., correlating aquifers in subsurface successions and, further, provides opportunities for linking marine and continental biotas.	[Shevchuk, Olena; Vajda, Vivi] Swedish Museum Nat Hist, Dept Palaeobiol, Stockholm, Sweden; [Shevchuk, Olena] Inst Geol Sci, NAS Ukraine, Kiev, Ukraine; [Vajda, Vivi] Swedish Museum Nat Hist, Dept Palaeobiol, S-E10405 Stockholm, Sweden	Swedish Museum of Natural History; National Academy of Sciences Ukraine; Institute of Geological Sciences, National Academy of Sciences of Ukraine; Swedish Museum of Natural History	Vajda, V (通讯作者)，Swedish Museum Nat Hist, Dept Palaeobiol, S-E10405 Stockholm, Sweden.	vivi.vajda@nrm.se	Vajda, Vivi/N-7693-2018; Shevchuk, Olena/AAD-6231-2020	Vajda, Vivi/0000-0003-2987-5559; Shevchuk, Olena/0000-0001-7221-4540	Swedish Foundation for Strategic Research, grants for Ukrainian scientists 2022 [UKR22-0020]; Swedish Foundation for Strategic Research [2020.0145]; Knut & Alice Wallenberg Foundation KAW [2019-4061]; Swedish Research Council VR; Swedish Government; Swedish Museum of Natural History; Russian invasion of Ukraine	Swedish Foundation for Strategic Research, grants for Ukrainian scientists 2022(Swedish Foundation for Strategic Research); Swedish Foundation for Strategic Research(Swedish Foundation for Strategic Research); Knut & Alice Wallenberg Foundation KAW(Knut & Alice Wallenberg Foundation); Swedish Research Council VR(Swedish Research Council); Swedish Government; Swedish Museum of Natural History; Russian invasion of Ukraine	Funding is acknowledged from the Swedish Foundation for Strategic Research, grant UKR22-0020 (O. Shevchuk). We are further thankful to the Knut & Alice Wallenberg Foundation KAW 2020.0145 (V. Vajda), and the Swedish Research Council VR grants 2019-4061 (V. Vajda). Olena Shevchuk wishes to thank the Swedish Government, the Swedish Museum of Natural History, and Stockholm University for hosting her under the Temporary Protection Directive, following the Russian invasion of Ukraine. We thank the reviewers for their constructive comments.	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P., 2020, Volumina Jurassica, V18, P121, DOI 10.7306/VJ.18.7; Wimbledon William A. P., 2020, Volumina Jurassica, V18, P53, DOI 10.7306/VJ.18.5	65	0	0	1	4	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	1103-5897	2000-0863		GFF	GFF	OCT 2	2023	145	3-4					165	176		10.1080/11035897.2024.2312575	http://dx.doi.org/10.1080/11035897.2024.2312575		APR 2024	12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	J5Q3T		hybrid			2025-03-11	WOS:001195692100001
J	Plata-Torresa, A; Pardo-Trujillo, A; Flores, JA				Plata-Torresa, Angelo; Pardo-Trujillo, Andres; Flores, Jose Abel			A contribution to the knowledge of Cretaceous to Neogene Palynology in the Colombian Caribbean.	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Maastrichtian; Paleogene; Neogene; Colombian Caribbean	SAN JACINTO BASIN; MIOCENE; BIOSTRATIGRAPHY; STRATIGRAPHY; OLIGOCENE; EVOLUTION; MIDDLE	The palynological study of a composite section of 14 cores drilled from the Sinu-San Jacinto Basin in the Colombian Caribbean (NW South America) provides for the first time a Cenozoic palynostratigraphic zonation scheme for this region. In addition, the study of calcareous nannofossils and planktonic foraminifera allowed an independent calibration of the palynomorph assemblages to the international chronostratigraphic chart. The palynological results were compared with other studies for the northern part of South America and Colombia. Twelve Late Paleocene-Pliocene palynological zones are proposed for the Caribbean, some of which differ from those proposed for the Llanos and Llanos Foothills basins. A Paleocene palynological assemblage is reported for this part of the basin. Variations in the biostratigraphic ranges of some palynomorphs and new species with stratigraphic value are described. High diversity and abundance of dinoflagellate cysts in some stratigraphic intervals require more detailed study. Evidence of reworking in some stratigraphic intervals (e.g., Cretaceous and Oligocene in Miocene sediments), makes it necessary to be careful about the last appearance record of microfossils in exploration and geologic mapping.	[Plata-Torresa, Angelo; Flores, Jose Abel] Univ Salamanca, Salamanca 340007, Spain; [Plata-Torresa, Angelo; Pardo-Trujillo, Andres] Univ Caldas, Inst Invest Estratig IIES, Calle 65 26-10,Edificio Orlando Sierra,2 Piso, Manizales, Colombia	University of Salamanca; Universidad de Caldas	Plata-Torresa, A (通讯作者)，Univ Salamanca, Salamanca 340007, Spain.; Plata-Torresa, A (通讯作者)，Univ Caldas, Inst Invest Estratig IIES, Calle 65 26-10,Edificio Orlando Sierra,2 Piso, Manizales, Colombia.	angelo.plata@ucaldas.edu.co; andres.pardo@ucaldas.edu.co; flores@usal.es		Plata-Torres, Angelo/0000-0001-8509-0567	Agencia Nacional de Hidrocarburos (ANH) [1300916, FP44842-494-2017]; Minciencias; Universidad de Caldas (Vicerrectoria de Investigaciones y Posgrados -VIP)	Agencia Nacional de Hidrocarburos (ANH); Minciencias; Universidad de Caldas (Vicerrectoria de Investigaciones y Posgrados -VIP)	We thank the Agencia Nacional de Hidrocarburos (ANH) for allowing us to use the data generated in 2016 and 2018 (projects 1300916 and FP44842-494-2017) , which involve Agencia Nacional de Hidrocarburos-ANH, Minciencias, Universidad de Caldas (Vicerrectoria de Investigaciones y Posgrados -VIP) . Thanks to the Instituto de Investigaciones en Estratigrafia-IIES, Universidad de Caldas, and overall, to the palynology and stratigraphy teams in 2018 to L. Contreras, F. Car- vajal, A. Diaz, J. Martinez, V. Ramirez, E. Ramirez, J.D. Vallejo, D. Rios, F. Gallego, F.J. Cardona, and the administrative and support team V. Vargas, M.D. Marin S. Gutierrez and J.P. Betancourt. Thanks to Mauricio Reyes for his invaluable help in the preparation of the palynological slides.	Mora JA, 2018, MAR PETROL GEOL, V97, P288, DOI 10.1016/j.marpetgeo.2018.06.032; ANH U., 2009, en la cuenca del Sinu, V1; ANH - Universidad de Caldas, 2017, Estratigrafia del Cretacico Superior - Paleogeno del sector Sinu - San Jacinto. Aporte al conocimiento de su evolucion geologica y sistemas petroliferos; ANH - Universidad de Caldas, 2020, Certificacion de estratigrafia fisica y edad de los nucleos de perforacion recuperados por la ANH Cuencas Sinu San Jacinto (SSJ) y Cordillera Oriental. 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Palaeobot. Palynology	JUN	2024	325								105098	10.1016/j.revpalbo.2024.105098	http://dx.doi.org/10.1016/j.revpalbo.2024.105098		APR 2024	25	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	QW0A4					2025-03-11	WOS:001223776700001
J	Maleki, S				Maleki, Saeed			The Middle Jurassic (Bajocian-Bathonian) flora of the Tabas Block, central Iran	GEOLOGOS			English	Article						Sporomorph EcoGroup; Plant EcoGroup; palynology; palaeobotany; Hojedk Formation	HOJEDK FORMATION; ATMOSPHERIC CO2; REVISED MODEL; CARBON-CYCLE; BASIN; VEGETATION; KERMAN; RECONSTRUCTION; STRATIGRAPHY; PERTURBATION	The present study discusses the outcome of palynlogical and palaeobotanocal investigations of Middle Jurassic strata of the Tabas Block. The most commonly identified spore type is a trilete spore, Klukisporites, which accounts for 30 per cent, and the genus Ischyosporites which makes up 12 per cent of the spore collection. Plant fossils recovered from the borehole studied are indicative of a varied assemblage, starting with a diverse range of ferns and followed by Cycadophytes, Ginkgophytes and Coniferophytes. The predominance of the Lowland group in the Tabas Block during the Bajocian-Bathonian, as indicated by the Sporomorph EcoGroup (SEG) and Plant EcoGroup (PEG) models, suggests that the strata studied were laid down mainly in a lowland environment. Dinoflagellate cysts were found in locations that correspond to river and coastal ecogroups, hinting at marine influence.	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J	Azanza, RV; Yñiguez, AT; Onda, DF; Benico, GA; Lim, PT; Leaw, CP; Iwataki, M				Azanza, Rhodora V.; Yniguez, Aletta T.; Onda, Deo Florence; Benico, Garry A.; Lim, Po Teen; Leaw, Chui Pin; Iwataki, Mitsunori			Expansion of Toxic Algal Blooms in Coastal and Marine Areas in the Philippines and Malaysia: Is It Climate Change Related?	SUSTAINABILITY			English	Review						Pyrodinium; toxic algal blooms; marine food systems; climate change; paralytic shellfish poisoning (PSP); Ciguatera fish poisoning (CFP)	ALEXANDRIUM-TAMIYAVANICHII; EUTROPHIC CONDITIONS; PYRODINIUM BLOOMS; PLASTIC DEBRIS; FISH KILL; DINOPHYCEAE; BOLINAO; DYNAMICS; COMMUNITIES; MARICULTURE	This paper provides a review of toxic algal blooms in the Philippine and Malaysian coastal and marine systems, considering relevant available knowledge, including climate change dimension/s in the assessment of their recorded recent expansion. The first record of human toxicity in the Philippines associated with HABs/toxic algal blooms specifically was during the bloom of Pyrodinium bahamense in the Sorsogon, Samar, and Leyte waters in 1983. Since then, the species has been identified to occur and cause blooms in about 44 sites/areas in the country. Recent government reports, i.e., 2021, 2022, and 2023, have also identified other paralytic shellfish poisoning (PSP) causative organisms (Gymnodinium catenatum, Alexandrium spp.) in the country. New records indicate that the presence of PSP causative species has been reported almost year-round in the Philippines. In Malaysia, PSP caused by P. bahamense was initially confined in 1981 to the state of Sabah, Malaysia Borneo, but since then, blooms of this species have been reported almost annually at different scales across the coastal waters of Sabah. P. bahamense and other cyst-forming dinoflagellates could be transported naturally or through human activities. Other eco-physiological and environment factors from the field and the laboratory have been used to study the bloom dynamics and transport of PSP causative species in several areas in the Philippines and Malaysia. More recently, plastics and other marine litter have been considered potential vectors of invasion/transport or expansion of dinoflagellates with other microorganisms. ENSO events have been observed to be stronger since 1950 compared with those recorded from 1850 to 1950. The extreme phases of the ENSO phenomenon have a strong modulating effect based on seasonal rainfall in the Philippines, with extreme ENSO warm events (El Nino) often associated with drought and stresses on water resources and agriculture/aquaculture. In contrast, cold events (La Nina) often result in excessive rainfall. The La Nina Advisories from 2021 to 2023 (18 advisories) showed the persistence of this part of ENSO, particularly in regions with recurrent and new records of HABs/toxic algal blooms. More studies and monitoring of another type of toxic algal bloom, Ciguatera Fish Poisoning (CFP), are recommended in tropical countries such as the Philippines and Malaysia, which have extensive reef areas that harvest and culture marine fish for local and export purposes, as accelerating reports of this type of poisoning have apparently increased and causative organisms have been identified in several areas. There is an urgent need to enhance HAB/toxic algal bloom research and monitoring, particularly those related to climate change, which has apparently impacted these blooms/occurrences directly or indirectly. Local researchers and managers should be made aware of the knowledge and tools already available for their utilization and enhancement to meet local conditions and challenges for potential recurrence and expansion of HABs/toxic algal blooms. Regional and international HAB research and collaboration should be further advanced for the protection of public health and marine resources.	[Azanza, Rhodora V.; Yniguez, Aletta T.; Onda, Deo Florence] Univ Philippines, Marine Sci Inst, Quezon City 1101, Philippines; [Benico, Garry A.] Cent Luzon State Univ, Coll Sci, Dept Biol Sci, Sci City Munoz 3120, Philippines; [Lim, Po Teen; Leaw, Chui Pin] Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia; [Iwataki, Mitsunori] Univ Tokyo, Grad Sch Agr & Life Sci, 1-1-1 Yayoi, Tokyo 1138657, Japan	University of the Philippines System; University of the Philippines Diliman; Central Luzon State University; Universiti Malaya; University of Tokyo	Azanza, RV (通讯作者)，Univ Philippines, Marine Sci Inst, Quezon City 1101, Philippines.	rvazanza@up.edu.ph; atyniguez@msi.upd.edu.ph	Benico, Garry/S-6313-2019; Lim, Po Teen/C-9758-2013; Iwataki, Mitsunori/H-9640-2019; Leaw, Chui Pin/F-5220-2012	Lim, Po Teen/0000-0003-2823-0564; Iwataki, Mitsunori/0000-0002-5844-2800; Benico, Garry/0000-0002-2617-0222; Leaw, Chui Pin/0000-0003-3336-1438; Onda, Deo Florence/0000-0003-4670-2051	Philippines was funded by the Department of Science and Technology-Philippine Council for Agriculture and Aquatic Resources Research and Development (DOST-PCAARRD); Marine Science Institute, University of the Philippines	Philippines was funded by the Department of Science and Technology-Philippine Council for Agriculture and Aquatic Resources Research and Development (DOST-PCAARRD); Marine Science Institute, University of the Philippines	We gratefully acknowledge the varied kinds of assistance provided by the Marine Science Institute, University of the Philippines, Diliman. We also wish to acknowledge our Philippine, Malaysian, ASEAN, and other international collaborators and co-workers in the laboratory and the field who have helped or influenced our research. Positive recommendations from the editor/s and reviewers enhanced this paper.	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J	Munsterman, DK; van den Bosch, M; Wesselingh, FP; Helwerda, M; Busschers, FS				Munsterman, Dirk K.; Van den Bosch, Maarten; Wesselingh, Frank P.; Helwerda, Marian; Busschers, Freek S.			A proposal for an updated and revised stratigraphical framework of the Miocene in the Achterhoek (eastern Netherlands)	NETHERLANDS JOURNAL OF GEOSCIENCES			English	Article						Dinoflagellate cysts; lithostratigraphy; Neogene; southern North Sea Basin; Stratigraphic Nomenclature NL	NORTH-SEA BASIN; DINOFLAGELLATE CYST; BELGIUM; BIOSTRATIGRAPHY; ATLANTIC; PLIOCENE; AREA	The comprehensive overview of Neogene lithostratigraphy in the eastern Netherlands dates back to the mid-1970s. In the present study, continuous gamma-ray logs and in situ sediment core samples from six boreholes in the area allowed palynological and mollusc analyses and wireline log-based correlation. These investigations were aimed at updating and revising the existing Neogene lithostratigraphy within the Stratigraphic Nomenclature of the Netherlands by integrating litho-, bio-, and sequence-stratigraphic approaches. The analytical results yielded the establishment of new holo- and lectostratotype sections, together with cross-border interregional correlation. The lithostratigraphic revision resulted in the modified definition of the Aalten, Eibergen and Delden members and the definition of two new proposed members: the Dale and Doetinchem members. The Ticheloven bed, removed in earlier studies, is proposed to be reinstated, and the Stemerdink Bed is upgraded in its hierarchical status to the Stemerdink member. All lithostratigraphic units are included in the present Miocene subdivision of the Groote Heide and Diessen formations, which include three recognisable unconformities: the Early-Miocene Unconformity (EMU), Mid-Miocene Unconformity (MMU) and Late-Miocene Unconformity (LMU). The new, revised, reintroduced and existing local lithostratigraphic units and sequences are discussed with their counterparts in the south and southeast of the Netherlands, in Germany and Belgium, and from this a regionally consistent framework has emerged of the regional Neogene lithostratigraphy.	[Munsterman, Dirk K.; Busschers, Freek S.] TNO Geol Survey Netherlands, Subsurface Modelling, Utrecht, Netherlands; [Van den Bosch, Maarten] Geol Veldlaboratorium Winterswijk, Winterswijk, Netherlands; [Wesselingh, Frank P.; Helwerda, Marian] Nat Biodivers Ctr, Leiden, Netherlands; [Wesselingh, Frank P.] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands	Netherlands Organization Applied Science Research; Naturalis Biodiversity Center; Utrecht University	Munsterman, DK (通讯作者)，TNO Geol Survey Netherlands, Subsurface Modelling, Utrecht, Netherlands.	dirk.munsterman@tno.nl	Busschers, Freek/HLQ-6717-2023; Wesselingh, Frank/C-1367-2018	Munsterman, Dirk/0000-0003-1774-4615; Busschers, Freek/0000-0003-1495-1766; Wesselingh, Frank/0000-0003-3655-0701	Arie Janssen; Miocene of the region; Jef Deckers (Flemish Institute for Technical Research); Jasper Verhaegen (Department of Environment of the Flemish Government)	Arie Janssen; Miocene of the region; Jef Deckers (Flemish Institute for Technical Research); Jasper Verhaegen (Department of Environment of the Flemish Government)	The authors specially thank Nico Janssen (TNO) and Malcolm Jones (ex-PLS- UK) for the palynological sample preparation. Susan Kerstholt-Boegehold (ex-TNO) is acknowledged for her share of the dinoflagellate cyst analysis over the years. We are indebted to Mr. J. van der Voort (Ostercappeln, Germany) for updating the nomenclature and critical reading of molluscan sections of this manuscript. Johan ten Veen (TNO) is appreciated for his lithostratigraphic discussion and his seismic study of the eastern Netherlands. The members of the Dutch Stratigraphical Commission are thanked for discussion and for embracing the proposal of update and revision of the lithostratigraphy in the eastern part of the country in 2022. We wish to express our extraordinary gratitude to Ed F. de Vogel and Arie W. Janssen, both of whom died in 2021. Arie Janssen was the main driver of the Miste excavations and the expert on the molluscan faunas from the Miocene of the region, whilst Ed De Vogel made very important early studies of the successions and biostratigraphy zonation of the Miocene successions. He was deeply involved in this study. Nik Trabucho (TNO) is gratefully recognised for his help in composing and improving the figures. We also express our gratitude to Jef Deckers (Flemish Institute for Technical Research), Jasper Verhaegen (Department of Environment of the Flemish Government) and an anonymous reviewer who improved the manuscript. Jef Deckers is also much appreciated for his cooperation in the updating of the schematic cross-section graphics, in part of the Antwerp area (Figure 18). Phil Gibbard (University of Cambridge) is highly appreciated for improving (the English in) the final manuscript. Rick Donselaar (University of Delft) is acknowledged for his help on parts of the text and his assistance as an associate editor of the Netherlands Journal of Geosciences.	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J	Baraboshkin, EY; Guzhikov, AY; Aleksandrova, GN; Akinin, VV; Ryabov, IP; Ustinova, MA; Rtischev, NA; Vishnevskaya, VS				Baraboshkin, E. Yu.; Guzhikov, A. Yu.; Aleksandrova, G. N.; Akinin, V. V.; Ryabov, I. P.; Ustinova, M. A.; Rtischev, N. A.; Vishnevskaya, V. S.			Reference Section of the Campanian Stage of the Southwestern Crimea: Problems of Substage Subdivision and Global Correlation	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Kudrino; Upper Cretaceous; stratigraphy; belemnites; ammonites; inoceramids; foraminifers; nannoplankton; dynocysts; gilianelles; magnetostratigraphy; Chron 33r; stable isotopes	CARBON-ISOTOPE STRATIGRAPHY; BOUNDARY STRATOTYPE SECTION; UPPER CRETACEOUS DEPOSITS; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; DINOCYST BIOSTRATIGRAPHY; MAASTRICHTIAN BOUNDARY; POINT GSSP; PART 2; CHALK; SEA	Stratigraphy of Campanian deposits in the stratotype of the Kudrinskaya Formation in the Southwestern Crimea is revised. For the first time, integrated sedimentological, biostratigraphic (ichnofossils, cephalopods, inoceramids, foraminifers, dinocysts, nannoplankton, gilianelles), isotope-geochemical, paleo- and petromagnetic characteristics of the section were obtained. The boundary of the lower and upper Campanian is substantiated and confirmed by U-Pb dating of zircons from the well-known bentonite (kil) clay bed in the interval of 77-80 Ma. It is proposed to accept the Campanian Substage boundary of the General Stratigraphic Chart (for bipartite stage subdivision) at the top of the Chron C33r, located near the delta C-13 isotopic excursion "MCaE" - Mid-Campanian Event, near the first occurrence of the benthic foraminifer Brotzenella monterelensis and a number of other traditional biomarkers.	[Baraboshkin, E. Yu.; Aleksandrova, G. N.; Ustinova, M. A.; Rtischev, N. A.] Moscow MV Lomonosov State Univ, Moscow 119991, Russia; [Guzhikov, A. Yu.] Saratov NG Chernyshevskii State Univ, Saratov 410012, Russia; [Baraboshkin, E. Yu.; Aleksandrova, G. N.; Ryabov, I. P.; Ustinova, M. A.; Rtischev, N. A.; Vishnevskaya, V. S.] Russian Acad Sci, Geol Inst, Moscow 119017, Russia; [Akinin, V. V.] Russian Acad Sci, Far Eastern Branch, Shilo North East Interdisciplinary Sci Res Inst, Magadan 685000, Russia	Lomonosov Moscow State University; Saratov State University; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Baraboshkin, EY (通讯作者)，Moscow MV Lomonosov State Univ, Moscow 119991, Russia.; Baraboshkin, EY (通讯作者)，Russian Acad Sci, Geol Inst, Moscow 119017, Russia.	barabosh@geol.msu.ru	Akinin, Viacheslav/ABE-4687-2020; Akinin, Vyacheslav/A-5937-2016	Akinin, Vyacheslav/0000-0001-9984-2571; Rtishchev, Nikolay/0000-0001-7592-7650	Russian Science Foundation [22-17-00091]	Russian Science Foundation(Russian Science Foundation (RSF))	The study was supported by the Russian Science Foundation, grant no. 22-17-00091, https://rscf.ru/project/22-17 - 0 0 0 91 / .	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J	Nosova, N; Fedyaevskiy, A; Lyubarova, A				Nosova, Natalya; Fedyaevskiy, Andrey; Lyubarova, Anna			New findings of gymnosperms in the Middle Jurassic of the East European platform	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Czekanowskia; Pseudotorellia; Podozamites; Belgorod Region; Kursk Region; Belarus	KRAKOW-SILESIA HOMOCLINE; LOCALITY KURSK REGION; ORE-BEARING CLAYS; PSEUDOTORELLIA FLORIN; NOV GYMNOSPERMAE; GENUS; SYSTEMATICS; PHYLOGENY; DEPOSITS; GNASZYN	The plant-bearing layers in the Stoilensky open mine (Belgorod Region, Russia) are dated to the middle Bathonian-early Callovian based on the dinoflagellate cysts and spore-pollen assemblages, and in the Mikhailovsky open mine (Kursk Region, Russia) - to the middle-late Bathonian based on palynological data. Representatives of Pseudotorellia are recorded in the Middle Jurassic of the Belgorod and Kursk regions for the first time. A new species, Pseudotorellia oskolica, is described from the Stoilensky open mine based on the unique morphological and epidermal features. Leaves of this species are very narrow, they are characterized by the presence of stomata on the adaxial leaf surface. The type material of Czekanowskia europea from the Middle Jurassic of the Pripyat depression in Belarus was restudied. The diagnosis for C. europea is provided, since only a description of this species was given in the original publication. Czekanowskia leaves are recorded from the Belgorod and Kursk regions for the first time. They are determined as C. europea based on the similar epidermal features as in the type leaves. A shoot of Pagiophyllum sp. and numerous leaf fragments of Podozamites sp. were found in association with C. europea in the Pripyat depression. These genera are recorded in Belarus for the first time. Findings of Pseudotorellia, Czekanowskia and Podozamites leaves in the Middle Jurassic floras of the East European platform are discussed.	[Nosova, Natalya; Lyubarova, Anna] Russian Acad Sci, Komarov Bot Inst, St Petersburg, Russia; [Fedyaevskiy, Andrey] Palynol & Stratig Lab PalyStrat LLP, Alma Ata, Kazakhstan	Russian Academy of Sciences; Komarov Botanical Institute, Russian Academy of Sciences	Nosova, N (通讯作者)，Russian Acad Sci, Komarov Bot Inst, St Petersburg, Russia.	nnosova@binran.ru	Fedyaevskiy, Andrey/IQU-1631-2023	Fedyaevskiy, Andrey/0000-0001-8739-0416	Russian Science Foundation [23-24-00105]	Russian Science Foundation(Russian Science Foundation (RSF))	We are sincerely grateful to Dr. Tatiana Alekseeva and Dr. Andrey Alekseev (Institute of Physicochemical and Biological Problems in Soil Science of RAS) for the organization of joint fieldworks in the Stoilensky and Mikhailovsky open mines. 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J	Anschütz, AA; Maselli, M; Traboni, C; Boon, AR; Stolte, W				Anschuetz, Anna-Adriana; Maselli, Maira; Traboni, Claudia; Boon, Arjen R.; Stolte, Willem			Importance of integrating mixoplankton into marine ecosystem policy and management-Examples from the Marine Strategy Framework Directive	INTEGRATED ENVIRONMENTAL ASSESSMENT AND MANAGEMENT			English	Review						Coastal and marine management; HAB risk assessment; Marine Strategy Framework Directive; Mixoplankton; Plankton monitoring guidelines	HARMFUL ALGAL BLOOMS; MIXOTROPHIC DINOFLAGELLATE; ENVIRONMENTAL STATUS; RESTING CYSTS; PHYTOPLANKTON; PLANKTON; INDICATORS; DINOPHYSIS; GROWTH; FOOD	Marine plankton capable of photosynthesis and predation ("mixoplankton") comprise up to 50% of protist plankton and include many harmful species. However, marine environmental management policies, including the European Union Marine Strategy Framework Directive (MSFD) and the USEPA, assume a strict dichotomy between autotrophic phytoplankton and heterotrophic zooplankton. Mixoplankton often differ significantly from these two categories in their response to environmental pressures and affect the marine environment in ways we are only beginning to understand. While the management policies may conceptually provide scope for incorporating mixoplankton, such action is rarely implemented. We suggest that the effectiveness of monitoring and management programs could benefit from explicit implementations regarding the ecological roles and impact of mixoplankton. Taking the MSFD as an example of marine management guidelines, we propose appropriate methods to explicitly include mixoplankton in monitoring and marine management. Integr Environ Assess Manag 2024;00:1-18. (c) 2024 The Authors. Integrated Environmental Assessment and Management published by Wiley Periodicals LLC on behalf of Society of Environmental Toxicology & Chemistry (SETAC). Mixoplankton (capable of photo- and heterotrophy) are a broad trophic group that is currently not considered by marine environmental management, while they often display different responses to environmental changes than strict phytoplankton or zooplankton due to their unique physiology. Many harmful algal species that are currently being monitored due to their impact on public health and the economy are mixoplankton, and effective forecasting systems may be challenging to establish by not considering their unique trophic mode. We showcase where the current omission of mixoplankton from marine management can misinform on the environmental status of marine ecosystems and how existing management and monitoring programs can benefit from including mixoplankton. Using the European Marine Strategy Framework Directive as an example, we show how mixoplankton can be integrated into existing management programs and where research gaps still exist.	[Anschuetz, Anna-Adriana] Leibniz Inst Balt Sea Res Warnemunde, Rostock, Germany; [Anschuetz, Anna-Adriana] Cardiff Univ, Sch Earth & Environm Sci, Cardiff, Wales; [Anschuetz, Anna-Adriana; Traboni, Claudia] Univ Libre Bruxelles, Lab Ecol Syst Aquat, Brussels, Belgium; [Maselli, Maira] Univ Copenhagen, Marine Biol Sect, Helsingor, Denmark; [Maselli, Maira] Stn Zool Anton Dohrn, Naples, Italy; [Traboni, Claudia] CSIC, Inst Ciencies Mar, Barcelona, Spain; [Boon, Arjen R.] Avans Univ Appl Sci, Breda, Netherlands; [Stolte, Willem] Deltares, Delft, Netherlands	Leibniz Institut fur Ostseeforschung Warnemunde; Cardiff University; Universite Libre de Bruxelles; University of Copenhagen; Stazione Zoologica Anton Dohrn; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Deltares	Anschütz, AA (通讯作者)，Leibniz Inst Balt Sea Res Warnemunde, Rostock, Germany.; Anschütz, AA (通讯作者)，Cardiff Univ, Sch Earth & Environm Sci, Cardiff, Wales.; Anschütz, AA (通讯作者)，Univ Libre Bruxelles, Lab Ecol Syst Aquat, Brussels, Belgium.	anna.a.anschuetz@gmail.com	Boon, Arjen/A-7257-2010; Maselli, Maira/IXN-4018-2023; Boon, Arjen/MAH-1959-2025; Traboni, Claudia/O-6684-2018	Anschutz, Anna-Adriana/0000-0002-1583-9613; Boon, Arjen/0000-0003-2614-5024; Traboni, Claudia/0000-0003-0380-2888	European Union [766327]; European Union's Horizon 2020 Research and Innovation Program Project "MixITiN" under Marie Sklstrok;odowska-Curie; Leibniz Institute for Baltic Sea Research Warnemunde (IOW); Projekt DEAL	European Union(European Union (EU)); European Union's Horizon 2020 Research and Innovation Program Project "MixITiN" under Marie Sklstrok;odowska-Curie; Leibniz Institute for Baltic Sea Research Warnemunde (IOW); Projekt DEAL	The authors thank colleagues in the MixITiN project () for discussions that have improved this work. This project received funding from the European Union's Horizon 2020 Research and Innovation Program Project "MixITiN" under Marie Sklodowska-Curie grant agreement No. 766327 and the Leibniz Institute for Baltic Sea Research Warnemunde (IOW). Open Access funding enabled and organized by Projekt DEAL.	Abad D, 2016, MAR BIOL, V163, DOI 10.1007/s00227-016-2920-0; Adolf JE, 2009, J PHYCOL, V45, P176, DOI 10.1111/j.1529-8817.2008.00641.x; Anderson D. 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Environ. Assess. Manag.	SEP	2024	20	5					1366	1383		10.1002/ieam.4914	http://dx.doi.org/10.1002/ieam.4914		MAR 2024	18	Environmental Sciences; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Toxicology	D6F2G	38546146	hybrid			2025-03-11	WOS:001192233600001
J	Ajuaba, S; Sachsenhofer, RF; Galasso, F; Garlichs, TU; Gross, D; Schneebeli-Hermann, E; Misch, D; Oriabure, JE				Ajuaba, Stephen; Sachsenhofer, Reinhard F.; Galasso, Francesca; Garlichs, Thorsten U.; Gross, Doris; Schneebeli-Hermann, Elke; Misch, David; Oriabure, Jonathan E.			The Toarcian Posidonia Shale at Salem (North Alpine Foreland Basin; South Germany): hydrocarbon potential and paleogeography	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						Biomarkers; Stable carbon isotopes; Palynology; Toarcian oceanic anoxic event; Carbon isotope excursion; Lower Jurassic	OCEANIC ANOXIC EVENT; EARLY JURASSIC EXTINCTION; CARBON-ISOTOPE RECORD; LOWER SAXONY BASIN; IN-SOURCE ROCKS; BLACK SHALE; SW-GERMANY; ORGANIC FACIES; SEA-LEVEL; DEPOSITIONAL ENVIRONMENT	The Posidonia Shale in the basement of the North Alpine Foreland Basin of southwestern Germany represents an important archive for environmental changes during the Toarcian oceanic anoxic event and the associated carbon isotope excursion (T-CIE). It is also an important hydrocarbon source rock. In the Salem borehole, the Posidonia Shale is similar to 10 m thick. The lower 7.5 m (1763.5-1756.0 m) of the Posidonian Shale and the uppermost part of the underlying Amaltheenton Formation were cored and studied using a total of 62 samples. Rock-Eval, palynological, maceral, biomarker and carbon isotope data were collected to assess variations in environmental conditions and to quantify the source rock potential. In contrast to most other Toarcian sections in southwest Germany, TOC contents are high in sediments deposited during the T-CIE, but reach a peak in post-CIE sediments. Biomarker ratios suggest that this reflects strong oxygen-depletion during the T-CIE (elegantulum to lower elegans subzones), but also during the falciferum Subzone, which is also reflected by a prolonged dinoflagellate cyst blackout. While sediments of the tenuicostatum Zone to the elegans Subzone are thinner than in neighbouring sections (e.g., Dotternhausen), sediments of the falciferum Subzone are unusually thick, suggesting that increased subsidence might have contributed to anoxia. The T-CIE interval is very thin (0.75 m). delta C-13 values of n-alkanes show that the maximum negative isotope shift predates the strongest basin restriction during the T-CIE and that the carbon isotope shift is recorded earlier for aquatic than for terrigenous organisms. In Salem, the Posidonia Shale is thermally mature and highly oil-prone. The residual source petroleum potential is about 0.8 tHC/m(2).	[Ajuaba, Stephen; Sachsenhofer, Reinhard F.; Gross, Doris; Misch, David; Oriabure, Jonathan E.] Montan Univ Leoben, Chair Energy Geosci, Peter Tunner Str 5, A-8700 Leoben, Austria; [Galasso, Francesca; Schneebeli-Hermann, Elke] Univ Zurich, Palaontol Inst & Museum, Karl Schmid Str 4, CH-8001 Zurich, Switzerland; [Galasso, Francesca] Senckenberg Forschungsinst & Naturmuseum Frankfurt, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Gross, Doris] Sandv Min & Construct Gm b H, Alpinestr 1, A-8740 Zeltweg, Austria; [Garlichs, Thorsten U.] Wintershall Dea Norge AS, Jattaflaten 27, N-4020 Stavanger, Norway; [Garlichs, Thorsten U.] Wintershall Dea Norge, POB 230 Sentrum, N-4001 Stavanger, Norway	University of Leoben; University of Zurich	Ajuaba, S (通讯作者)，Montan Univ Leoben, Chair Energy Geosci, Peter Tunner Str 5, A-8700 Leoben, Austria.	stephen.ajuaba@unileoben.ac.at	Ajuaba, Stephen/LNR-5273-2024; Galasso, Francesca/AAH-4005-2021; Sachsenhofer, Reinhard/KFA-6113-2024; Schneebeli, Elke/F-4873-2011	Ajuaba, Stephen/0000-0001-5748-7284; Schneebeli, Elke/0000-0002-1552-4785; Sachsenhofer, Reinhard/0000-0002-6616-5583; Gross, Doris/0000-0001-7442-5093; Galasso, Francesca/0000-0001-5391-7902	Wintershall Dea	Wintershall Dea	The authors thank Wintershall Dea for providing access to the core and for the permission to publish the data. The authors thank Boris Jammernegg for scanning the core. The paper benefited from the constructive comments of an anonymous reviewer and Ksenija Stojanovic (Belgrade).	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J. Earth Sci.	NOV	2024	113	8			SI		2093	2130		10.1007/s00531-024-02392-z	http://dx.doi.org/10.1007/s00531-024-02392-z		MAR 2024	38	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	P3T8T		Green Published, hybrid			2025-03-11	WOS:001194855600001
J	Li, JG; Rao, X; Mu, L; Cui, XH; Li, X; Luo, H; Liu, PX				Li, Jianguo; Rao, Xin; Mu, Lin; Cui, Xiaohui; Li, Xin; Luo, Hui; Liu, Peixue			Jurassic integrative stratigraphy, biotas, and paleogeographical evolution of the Qinghai-Tibetan Plateau and its surrounding areas	SCIENCE CHINA-EARTH SCIENCES			English	Review						Biostratigraphy; Chronostratigraphy; Correlation; Yarlung Zangbo suture; Bangong Co-Nujiang suture; Tethys	NUJIANG SUTURE ZONE; EARLY CRETACEOUS PALYNOFLORAS; SOUTHERN XIZANG TIBET; VOLCANIC-ROCKS; NORTHERN TIBET; TECTONIC EVOLUTION; QIANGTANG BASIN; RADIOLARIAN ASSEMBLAGES; DONGQIAO OPHIOLITE; TETHYAN HIMALAYA	The Qinghai-Tibetan Plateau experienced a unique geological evolution during the Jurassic, driven by the termination of the Palaeotethys and the reduction of the Neotethys. The Indian Plate separated from the northern margin of Gondwana and drifted northward from the Southern Hemisphere. Given that the timing of strata serves as the basis for reconstructing geological history, the present work aimed to develop a new multiple stratigraphic and chronologic framework for the Jurassic strata of the Qinghai-Tibetan Plateau region via a synthesis of the material on lithostratigraphy, palaeontology, iso-radiometric dating, magnetostratigraphy, and other techniques with an emphasis on recent progress and findings. The new framework included the Jurassic System from the four major subdivisions of the plateau: the Baryan Har, Qiangtang, Lhasa-Gandise, and Southern Xizang (Himalaya). Ultimately, a more complete, refined biostratigraphic sequence was proposed, comprising the most common fossils in the plateau and those that are stratigraphically significant for the Jurassic stratigraphy, including ammonites, bivalves, brachiopods, foraminifera, radiolarians, and dinoflagellate cysts for the marine strata, and pollen and spores, and charophytes for the terrestrial sediments. This biostratigraphic framework was correlated with the Jurassic international standard zonation of the Geological Time Scale 2020 via standard or representative species or genera of ammonites. Based on this framework, we constructed a lateral correlation of the Jurassic strata between different basins of the plateau. The palaeontologic correlation in the present work shows that the Lhasa-Gandise Block had a closer relationship with the Qiangtang Block than with the Southern Xizang Himalaya during the Jurassic Period. Meanwhile, the Lhasa-Gandise Block and Qiangtang Block shared similar marine fauna features of the north marginal East Tethys. This contrasts the opinion suggesting that the Yarlung Zangbo Tethys was a small back-arc basin. A combination of stratigraphical, palaeontological, and sedimentological analyses implies that the Bangong Co-Nujiang Tethys may have begun rifting in the Late Triassic, evolving to the birth at the late Early Jurassic with the formation of ocean crust. However, this resulted in failure after it grew into the climax at the end of the Middle Jurassic when the Qiangtang Block began subducting under the Lhasa-Gandise Block. In the Early Cretaceous, the two blocks finally merged.	[Li, Jianguo; Rao, Xin; Mu, Lin; Cui, Xiaohui; Li, Xin; Luo, Hui] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China; [Li, Jianguo; Liu, Peixue] Univ Chinese Acad Sci, Nanjing Coll, Nanjing 211135, Peoples R China	Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Li, JG (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Ctr Excellence Life & Paleoenvironm, Nanjing 210008, Peoples R China.; Li, JG (通讯作者)，Univ Chinese Acad Sci, Nanjing Coll, Nanjing 211135, Peoples R China.	jgli@nigpas.ac.cn	刘, 培学/F-7582-2016		Second Tibetan Plateau Scientific Expedition and Research [2019QZKK0706]; National Natural Science Foundation of China [42372019, 41888101, 41872004, 42272027, 42288201, 42172028]; Strategic Priority Research Program of the Chinese Academy of Sciences [XDB26000000, XDA2007020203]	Second Tibetan Plateau Scientific Expedition and Research; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Strategic Priority Research Program of the Chinese Academy of Sciences(Chinese Academy of Sciences)	Special thanks are given to Professor Shuzhong SHEN, Jiarui YIN, and the reviewers for their helpful comments. This work was supported by the Second Tibetan Plateau Scientific Expedition and Research (Grant No. 2019QZKK0706), the National Natural Science Foundation of China (Grant Nos. 42372019, 41888101, 41872004, 42272027, 42288201, 42172028), and the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant Nos. XDB26000000, XDA2007020203).	[Anonymous], 2010, Geol. Bull. 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J	Souza, T; Helenes, J; Carvalho, MA; Barreto, CF; Neto, JAB				Souza, Taisa; Helenes, Javier; Carvalho, Marcelo Araujo; Barreto, Cintia Ferreira; Neto, Jose Antonio Baptista			Climatic variation of the last 29.000 years BP in the northern Santos basin (Rio de Janeiro Shelf) inferred by an alternation of cysts<i> Tuberculodinium</i> vancampoae and Operculodinium centrocarpum	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dinoflagellate cysts; Santos basin; Sea-surface changes; Pleistocene-holocene temperature; Last glacial maximum	SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYSTS; UPWELLING SYSTEM; LATE QUATERNARY; HIGH-LATITUDES; SOUTHEASTERN; ASSEMBLAGES; TEMPERATURE; ATLANTIC; RECORD	During the transition from the Pleistocene to the Holocene, significant changes occurred on the Brazilian continental shelf. In this study, we investigated the environmental changes that occurred during this period through the quantification and classification of cosmopolitan dinoflagellate cysts. We used three cores collected in the northern part of the Santos Basin and analyzed a total of 42 samples. The results showed a predominance of cysts of O. centrocarpum, L. machaerophorum and T. vancampoae, whose occurrence was influenced by sea-level fluctuations during the Pleistocene-Holocene transition and by changes in ocean currents due to temperature variations. Oligotrophic species were established during the Late Pleistocene, followed by mixotrophic species from the Holocene. Analysis of the dinocysts showed the presence of colder waters due to upwelling and the entry of waters with lower salinity due to the formation of transitional estuarine systems. These environmental changes have contributed to the configuration of the current Brazilian coastal scenario.	[Souza, Taisa; Barreto, Cintia Ferreira; Neto, Jose Antonio Baptista] Univ Fed Fluminense, Inst Geociencias, Dept Geol & Geofis Marinha, Ave Gen Milton Tavares Souza s-n, BR-24210346 Niteroi, RJ, Brazil; [Carvalho, Marcelo Araujo] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Lab Paleoecol Vegetal, Museu Nacl, BR-22040040 Rio De Janeiro, RJ, Brazil; [Helenes, Javier] Ctr Invest Cient & Educ Super Ensenada CICESE, Dept Geol, Carretera Ensenada Tijuana 3918,Fraccionamiento Pl, Ensenada 22860, Baja California, Mexico	Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Souza, T (通讯作者)，Univ Fed Fluminense, Inst Geociencias, Dept Geol & Geofis Marinha, Ave Gen Milton Tavares Souza s-n, BR-24210346 Niteroi, RJ, Brazil.	taisasouza@id.uff.br						AKSU AE, 1992, PALAEOGEOGR PALAEOCL, V92, P121, DOI 10.1016/0031-0182(92)90138-U; Albuquerque AL, 2016, PALAEOGEOGR PALAEOCL, V445, P72, DOI 10.1016/j.palaeo.2016.01.006; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Angulo RJ, 2007, RADIOCARBON, V49, P1255, DOI 10.1017/S0033822200043162; Artusi L., 2004, Geologia, geomorfologia e sismoestratigrafia rasa da plataforma continental ao largo da Laguna de Araruama RJ; Bonnet S, 2012, MAR MICROPALEONTOL, V84-85, P87, DOI 10.1016/j.marmicro.2011.11.006; Bravo Isabel, 2014, Microorganisms, V2, P11; Castro B.M. de, 1987, Bol. do Inst. 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JUN	2024	138								104878	10.1016/j.jsames.2024.104878	http://dx.doi.org/10.1016/j.jsames.2024.104878		MAR 2024	9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	C7D1V					2025-03-11	WOS:001290930200001
J	Bijl, PK				Bijl, Peter K.			DINOSTRAT version 2.1-GTS2020	EARTH SYSTEM SCIENCE DATA			English	Article							DATABASE	DINOSTRAT version 2.1-GTS2020 is now available (10.5281/zenodo.10506652, Bijl et al., 2024b). This version updates DINOSTRAT to the Geologic Time Scale 2020, and new publications are added into the database. The resulting database now contains over 9450 entries from 209 sites. This update has not led to major and profound changes in the conclusions made previously. DINOSTRAT allows full presentation of the first and last stratigraphic occurrences of dinoflagellate cyst subfamilies and families, as well as the evolutionary turnover throughout geologic history, as a reliable representation of dinoflagellate evolution. Although the picture of dinoflagellate evolution from DINOSTRAT is broadly consistent with that in previous publications, with DINOSTRAT the underlying data are openly available, reproducible and up to date. This release of DINOSTRAT allows calibration of stratigraphic records to the Geologic Time Scale 2020 using dinoflagellate cysts as a biostratigraphic tool.	[Bijl, Peter K.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonlaan 8A, NL-3584 CB Utrecht, Netherlands	Utrecht University	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonlaan 8A, NL-3584 CB Utrecht, Netherlands.	p.k.bijl@uu.nl		Bijl, Peter/0000-0002-1710-4012	LPP Foundation; Department of Earth Sciences of Utrecht University	LPP Foundation; Department of Earth Sciences of Utrecht University	The author thanks the LPP Foundation and the department of Earth Sciences of Utrecht University for supporting this work. Thanks go to Appy Sluijs, Henk Brinkhuis, Francesca Sangiorgi, Denise Kulhanek, Jeremy Young and Paul Bown for fruitful discussions. I thank the editor Giuseppe Manzella for helpful comments on this paper. Jan Hennissen, Rob Fensome and the anonymous reviewer are thanked for their constructive review of the paper.	Bijl P. K., DINOSTRAT Version2.1-GTS2020(2.1), Zenodo, DOI [10.5281/zenodo.10506652,2024b, DOI 10.5281/ZENODO.10506652,2024B]; Bijl PK, 2022, EARTH SYST SCI DATA, V14, P579, DOI 10.5194/essd-14-579-2022; Bijl PK, 2024, Zenodo, DOI 10.5281/ZENODO.10501273; Bravo Isabel, 2014, Microorganisms, V2, P11; Bujak J, 2022, ATL GEOL, V58, P55, DOI 10.4138/atlgeo.2022.003; Copestake P., 2023, Geological Society, London, Memoirs, V59, P387, DOI [10.1144/M59-2022-61, DOI 10.1144/M59-2022-61]; Crouch EM, 2024, NEW ZEAL J GEOL GEOP, V67, P20, DOI 10.1080/00288306.2022.2090386; Fensome R. A., 1993, Special Paper; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Estebenet MSG, 2021, REV PALAEOBOT PALYNO, V285, DOI 10.1016/j.revpalbo.2020.104342; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1, DOI 10.1016/B978-0-444-59425-9.00001-9; Gradstein F.M., 2020, GEOLOGIC TIME SCALE, DOI [10.1016/B978-0-12-824360-2.00032-2, DOI 10.1016/B978-0-12-824360-2.00032-2]; Guerrero-Murcia LA, 2022, J S AM EARTH SCI, V115, DOI 10.1016/j.jsames.2022.103730; Jarvis I, 2021, CRETACEOUS RES, V123, DOI 10.1016/j.cretres.2021.104782; Pearce MA, 2022, CR GEOSCI, V354, P45, DOI 10.5802/crgeos.118; Pearce MA, 2020, REV PALAEOBOT PALYNO, V278, DOI 10.1016/j.revpalbo.2020.104188; Rochon A, 2009, REV PALAEOBOT PALYNO, V155, P52, DOI 10.1016/j.revpalbo.2008.12.017; Thöle LM, 2023, J MICROPALAEONTOL, V42, P35, DOI 10.5194/jm-42-35-2023; Torricelli S, 2022, J AFR EARTH SCI, V192, DOI 10.1016/j.jafrearsci.2022.104536; Vaes B, 2023, EARTH-SCI REV, V245, DOI 10.1016/j.earscirev.2023.104547; Vasilyeva ON, 2023, PALAEOWORLD, V32, P523, DOI 10.1016/j.palwor.2022.11.006; Vieira M, 2022, PALYNOLOGY, V46, DOI 10.1080/01916122.2021.2006817; Vieira M, 2020, MAR PETROL GEOL, V117, DOI 10.1016/j.marpetgeo.2020.104400; Wickham H., 2016, GGPLOT2 ELEGANT GRAP, V1	24	0	0	1	1	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	1866-3508	1866-3516		EARTH SYST SCI DATA	Earth Syst. Sci. Data	MAR 15	2024	16	3					1447	1452		10.5194/essd-16-1447-2024	http://dx.doi.org/10.5194/essd-16-1447-2024			6	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	ME2F4		gold, Green Submitted			2025-03-11	WOS:001191877500001
J	Barreto, CF; Freitas, ADD; Souza, TCSD; Toledo, MBD; Portilho-Ramos, RD; Reis, ATD; Silva, CGD				Barreto, Cintia Ferreira; Freitas, Alex da Silva de; Souza, Taisa Camila Silveira de; Toledo, Mauro Bevilacqua de; Portilho-Ramos, Rodrigo da Costa; Reis, Antonio Tadeu dos; Silva, Cleverson Guizan da			A late Quaternary palynological record from the southeastern margin of Brazil: Implications for the evolution of palaeoceanography, palaeoclimates and vegetation over the last 109 kyr	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late quaternary; Pollen; Dinoflagellate cysts; South Atlantic Ocean; Palaeovegetation; Palaeoclimate; Palaeoceanography	SEA-LEVEL; DINOFLAGELLATE CYSTS; CLIMATE DYNAMICS; CONTINENTAL-MARGIN; MARINE-SEDIMENTS; LATE PLEISTOCENE; SOUTHERN BRAZIL; CORE; VARIABILITY; OFFSHORE	Integration of late Quaternary continental and marine proxies allows improved reconstruction of palaeoenvironment and palaeoclimates models for the south-eastern coast of Brazil. In this paper, we analyse pollen, fern spores, and dinoflagellate cysts in a marine sediment core (GL74) over the last -109 kyr. Results showed that, between 109 and 89.5 kyr, low sea levels promoted the expansion of herbaceous taxa across open areas while climatic conditions were relatively warm and humid, as indicated by the high frequency of Atlantic rainforest Ombrophilous forest pollen types and abundant of fern spores. Between -79-49 kyr, higher concentrations of palynomorphs were recorded, which were likely related to the low relative sea level during the last glacial period. During this interval, there was a decrease in tree pollen grains and an increase in shrub and herbaceous pollen grains, indicating cold and relatively dry weather conditions. In the Holocene period, the low deposition of palynomorphs may have been influenced by the gradual submergence of the central part of the Brazilian coast. This process was associated with warm and humid climatic conditions, as suggested by the expansion of rainforests and the presence of hygrophyte/aquatic taxa and fern spores, as well as the retraction of grassland pollen types. Dinocyst assemblages suggest that nutrient -rich waters and/or the presence of upwelling cells were dominant between -109-88 kyr, but gradually reduced between 88 and 65 kyr (and/or - 88-20 kyr) under the influence of subtropical fronts. The study culminated in the dominance of unproductive warm water in the upper column between 65 and 0.5 kyr.	[Barreto, Cintia Ferreira; Freitas, Alex da Silva de; Souza, Taisa Camila Silveira de; Silva, Cleverson Guizan da] Univ Fed Fluminense, Dept Geol & Geofis Marinha, LAGEMAR, Inst Geociencias, BR-24210340 Niteroi, RJ, Brazil; [Toledo, Mauro Bevilacqua de] Global Inst Water Secur, Saskatoon, SK, Canada; [Portilho-Ramos, Rodrigo da Costa] MARUM, Ctr Marine Environm Sci, Bremen, Germany; [Reis, Antonio Tadeu dos] Univ Estado Rio De Janeiro, Fac Oceanog, Dept Oceanog Geol, GEOMARGEM, BR-20550900 Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense; University of Saskatchewan; Global Institute for Water Security; University of Bremen; Universidade do Estado do Rio de Janeiro	Barreto, CF; Souza, TCSD (通讯作者)，Univ Fed Fluminense, Dept Geol & Geofis Marinha, LAGEMAR, Inst Geociencias, BR-24210340 Niteroi, RJ, Brazil.	cintiapalino@yahoo.com.br; alexsf@id.uff.br	Silva, Cleverson/G-2518-2012		Petrobras S.A.; Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)	Petrobras S.A.(PetrobrasFundacao de Amparo a Pesquisa do Amapa (FAPEAP)); Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was sponsored by the Petrobras S.A., Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) , Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) .	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J	Skupien, P; Bubík, M; Reháková, D; Svábenická, L; Elbra, T; Kosták, M; Svobodová, A; Rybová, P; Mikulás, R; Pruner, P; Schnabl, P; Kdyr, S; Vanková, L; Trubac, J; Mazuch, M				Skupien, Petr; Bubik, Miroslav; Rehakova, Daniela; Svabenicka, Lilian; Elbra, Tiiu; Kostak, Martin; Svobodova, Andrea; Rybova, Pavlina; Mikulas, Radek; Pruner, Petr; Schnabl, Petr; Kdyr, Simon; Vankova, Lucie; Trubac, Jakub; Mazuch, Martin			The Jurassic-Cretaceous boundary on the northern Tethyan margin: Karpentna and Ropice sections (Outer Western Carpathians, Czech Republic)	CRETACEOUS RESEARCH			English	Article						Carpathians; Biostratigraphy; Tithonian; Berriasian; Palynology; Dino flagellata; Calpionellids; Calcareous nannofossils; Foraminifera; Magnetic properties; Stable isotopes	JURASSIC/CRETACEOUS BOUNDARY; KUROVICE SECTION; J/K BOUNDARY; BIOSTRATIGRAPHY; INTERVAL; MAGNETO; RECORD; MAGNETOSTRATIGRAPHY; CRASSICOLLARIA; CALPIONELLIDS	Microfacies and high-resolution studies at the Silesian Unit (Outer Western Carpathians, Czech Republic) on calpionellids, calcareous and non-calcareous dinoflagellate cysts, foraminifers and calcareous nannofossils, aligned with paleomagnetism, delta C-13(carb) and delta C-18(carb), allow construction of a detailed stratigraphy and palaeoenvironmental interpretations across the Jurassic-Cretaceous (J/K) boundary. Two studied sections consist of allodapic and biomicritic limestones and marlstones. Ropice section spans the stratigraphic range from the upper Tithonian calpionellid Chitinoidella Zone, nannoplankton zone NJT16 to the lower Berriasian calpionellid Alpina Subzone of the Calpionella Zone, nannoplankton NC1 Zone. The J/K boundary is marked by the dominance of small forms of Calpionella alpina, rare occurrence of Nannoconus wintereri, and the first occurrence of organic-walled dinoflagellate cysts Dichadogonyaulax bensonii and Muderongia longicorna. A negative shift in the delta C-13(carb) values corresponds to the Tithonian/ Berriasian boundary, the base of the Calpionella Zone (Alpina Subzone). Karpentna section is represented by upper Tithonian calpionellid Chitinoidella to Crassicollaria zones. Remagnetization was documented in both sections. (c) 2024 Elsevier Ltd. All rights reserved.	[Skupien, Petr; Rybova, Pavlina] VSB Tech Univ Ostrava, Dept Geol Engn, 17 listopadu 15, CZ-70833 Ostrava, Czech Republic; [Bubik, Miroslav] Czech Geol Survey, Leitnerova 22, Brno 65869, Czech Republic; [Rehakova, Daniela] Comenius Univ, Fac Nat Sci, Dept Geol & Palaeontol, Ilkovicaova 6, Bratislava 84215, Slovakia; [Svabenicka, Lilian] Czech Geol Survey, Klarov 131-3, Prague 11821, Czech Republic; [Elbra, Tiiu; Svobodova, Andrea; Pruner, Petr; Schnabl, Petr; Kdyr, Simon; Vankova, Lucie] Inst Geol, Czech Acad Sci, Rozvojova 269, Prague 16500, Czech Republic; [Vankova, Lucie; Mazuch, Martin] Charles Univ Prague, Inst Geol & Paleontol, Fac Sci, Albertov 6, Prague 2, Czech Republic; [Kdyr, Simon; Trubac, Jakub] Charles Univ Prague, Fac Sci, Inst Geochem Mineral & Mineral Resources, Albertov 6, Prague 12800 2, Czech Republic	Technical University of Ostrava; Czech Geological Survey; Comenius University Bratislava; Czech Geological Survey; Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Charles University Prague; Charles University Prague	Skupien, P (通讯作者)，VSB Tech Univ Ostrava, Dept Geol Engn, 17 listopadu 15, CZ-70833 Ostrava, Czech Republic.	petr.skupien@vsb.cz; miroslav.bubik@geology.cz; rehakova@nic.fns.uniba.sk; lilian.svabenicka@geology.cz; elbra@gli.cas.cz; martin.kostak@natur.cuni.cz; asvobodova@gli.cas.cz; pruner@gli.cas.cz; schnabl@gli.cas.cz; kdyr@gli.cas.cz; lucie.vankova@natur.cuni.cz; jakub.trubac@natur.cuni.cz; martin.mazuch@natur.cuni.cz	Mikulas, Radek/F-4136-2010; Reháková, Daniela/Z-1300-2019; Vaňková, Lucie/AAD-3273-2019; Schnabl, Petr/I-7125-2012; Elbra, Tiiu/F-6859-2012; Mazuch, Martin/I-5964-2017; Skupien, Petr/G-8767-2019; Trubac, Jakub/J-5890-2012; Kostak, Martin/I-6006-2017	Mazuch, Martin/0000-0002-1697-3742; Vankova, Lucie/0000-0002-4363-2003; Skupien, Petr/0000-0001-9158-466X; Trubac, Jakub/0000-0002-9470-1304; Kdyr, Simon/0000-0003-2759-899X; Kostak, Martin/0000-0002-0818-3505; Mikulas, Radek/0000-0002-9827-2367; Elbra, Tiiu/0000-0001-6115-0588	Czech Science Foundation [20-10035S]; Projects of the Slovak Research and Development Agency [APVV-20-0079, APVV-21-0281]; Ministry of Education Science Research and Sport of the Slovak Republic [VEGA 2/0012/24, VEGA 1/0435/21]; COOPERATIO(Faculty of Science, Charles University) [UNCE/SCI/006]; Czech Geological Survey [311430]	Czech Science Foundation(Grant Agency of the Czech Republic); Projects of the Slovak Research and Development Agency; Ministry of Education Science Research and Sport of the Slovak Republic; COOPERATIO(Faculty of Science, Charles University); Czech Geological Survey	The research was supported by Czech Science Foundation project no. 20-10035S. Microfacies, calpionellid and calcareous dinocyst research was supported by the projects of the Slovak Research and Development Agency - APVV-20-0079, APVV-21-0281, and by projects of the Ministry of Education Science Research and Sport of the Slovak Republic VEGA 2/0012/24, VEGA 1/0435/21.Stable isotope analyses were supported by project COOPERATIO(Faculty of Science, Charles University) and project UNCE/SCI/006.The research is in accordance with research plan no. RVO67985831,and with main aims of Berriasian Working Group and IGCP 679 project. Foraminifer and nannofossil study is a contribution to the Project No. 311430 within the Research Plan DRKVO 2023e2027 of the Czech Geological Survey. Authors would like to thank K.Bachova, J. Petracek, L. Kouklikova and J. Geist for their help during fieldwork, sample preparation and magnetic analyses. Authors are grateful for editors and anonymous reviewers for their comments, which helped to improve the paper. The research is contribution to work to work of Berriasian Working Group and IGCP 679 project.	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JUL	2024	159								105868	10.1016/j.cretres.2024.105868	http://dx.doi.org/10.1016/j.cretres.2024.105868		MAR 2024	24	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	OR1T1					2025-03-11	WOS:001208915900001
J	Aggarwal, N; Goswami, S				Aggarwal, Neha; Goswami, Shreerup			Tectonic inferences from palynology of Permian sequences of the Godavari Valley Coalfield, Southern India	PALYNOLOGY			English	Article						palynology; Lower Gondwana; Permian; Triassic; interrupted sequences; reworked palynomorphs; Godavari Valley Coalfield; stratigraphy; Southern India	DINOFLAGELLATE CYSTS; SP-NOV; MOLECULAR PHYLOGENY; BRITISH-COLUMBIA; DINOPHYCEAE; PROTOPERIDINIUM; PERIDINIALES; PRODUCTIVITY; SEDIMENTS; WATERS	Core samples from four boreholes (SAV-1, SAV-117, SAV-124, SAV-125) within the Vaddugudem block of the Godavari Valley Coalfield, Southern India have been palynologically investigated to understand the stratigraphic setting of that area. Only 60 out of the 172 samples yielded identifiable palynoassemblages. From the observed palynofloral composition, five distinct palynoassemblages (Scheuringipollenites Assemblage: PA-I, Striatopodocarpites + Faunipollenites Assemblage: PA-II, Striates + Striasulcites Assemblage: PA-III, Striates + Guttulapollenites Assemblage: PA-IV, Lundbladispora + Verrucosisporites Assemblage: PA-V) were identified. Furthermore, five distinct palynozones (Scheuringipollenites barakarensis Zone = PZ-1, Striatopodocarpites + Faunipollenites Zone = PZ-2, Gondisporites raniganjensis Zone = PZ-3, Guttulapollenites gondwanensis-Striatopodocatpites tiwarii Zone = PZ-4 and Playfordiaspora cancellosa Zone = PZ-5) were identified. These correspond to the Artinskian (PZ-1), Wordian-Capitanian (PZ-2 and PZ-3), Wuchiapingian-Changhsingian (PZ-4) and Induan-Olenekian (PZ-5), respectively. The study site is situated within a geologically active region within the basin, primarily attributed to the exposure of elevated basement rocks on the eastern side of the borehole locations. Notably, the palynozones appear as relatively narrow layers in the boreholes investigated within this tectonically disturbed basin. The repetition of palynoassemblages and palynozones at small intervals suggests that the boreholes are located in a fault zone with multiple fault planes and that palynomorphs were reworked along these fault planes. Fault slices of different lithological units containing palynoassemblages may have intersected the boreholes. Specifically, the recurrence of thin marker palynoassemblages and palynozones, which show similarities in age to the Barakar and Lower Kamthi/Raniganj formations, is likely attributable to tectonic disturbances, such as faulting. This disturbance may have induced the reworking or migration of palynomorphs along the fault plane. As a result, it is concluded that variations in the stratigraphic abundance of these reworked palynomorphs can serve as indicators of tectonic settings, even when these settings are not readily discernible in the geological record.	[Aggarwal, Neha] Birbal Sahni Inst Palaeosci, Lucknow, Uttar Pradesh, India; [Goswami, Shreerup] Utkal Univ, Dept Geol, Bhubaneswar 751004, Odisha, India; [Aggarwal, Neha] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Utkal University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Aggarwal, N (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	neha_264840@yahoo.co.in	Goswami, Shreerup/AAN-8798-2020					Aggarwal N., 2015, Journal Indian Geological Congress, V7, P5; Aggarwal N, 2022, J PALAEOGEOG-ENGLISH, V11, P123, DOI 10.1016/j.jop.2021.07.001; Aggarwal N, 2019, INT J COAL GEOL, V214, DOI 10.1016/j.coal.2019.103285; Aggarwal N, 2019, J PALEOLIMNOL, V61, P329, DOI 10.1007/s10933-018-0062-8; Aggarwal N, 2017, J PALAEONTOL SOC IND, V62, P175; Aggarwal N, 2013, J ASIAN EARTH SCI, V64, P38, DOI 10.1016/j.jseaes.2012.11.041; BACKHOUSE J, 1991, REV PALAEOBOT PALYNO, V67, P237, DOI 10.1016/0034-6667(91)90046-6; Chakrabarthi SK., 1994, GONDW 9 9 INT GONDW, V2, P599; Goswami S, 2007, J GEOL SOC INDIA, V70, P131; Helby R.J., 1987, MEM ASSOC AUSTRALASI, V4, P1; Jha N, 1996, GONDWANA NINE - NINTH INTERNATIONAL GONDWANA SYMPOSIUM, VOLS 1 AND 2, P355; Jha Neerja, 2006, Journal of the Palaeontological Society of India, V51, P43; Jha N, 2018, J ASIAN EARTH SCI, V163, P1, DOI 10.1016/j.jseaes.2018.05.014; Jha N, 2012, J EARTH SYST SCI, V121, P1257, DOI 10.1007/s12040-012-0224-4; Jha N, 2011, J EARTH SYST SCI, V120, P663, DOI 10.1007/s12040-011-0095-0; Jha Neerja, 2008, Journal of the Palaeontological Society of India, V53, P159; KEMP E M, 1977, BMR (Bureau of Mineral Resources) Journal of Australian Geology and Geophysics, V2, P177; King W., 1881, Memoir of Geological Survey of India, V18, P116; Kutty T.S., 1988, Palaeobotanist (Lucknow), V36, P214; Laurie JR, 2016, AUST J EARTH SCI, V63, P701, DOI 10.1080/08120099.2016.1233456; Medlicott HB., 1879, A manual of the geology of India (part I: Peninsular Area); MISHRA DC, 1987, J GEOL SOC INDIA, V30, P469; MISHRA DC, 1989, EARTH PLANET SC LETT, V94, P344, DOI 10.1016/0012-821X(89)90151-9; Mukhopadhyay G, 2010, J GEOL SOC INDIA, V76, P251, DOI 10.1007/s12594-010-0097-6; Murty BVR, 1996, GONDWANA NINE - NINTH INTERNATIONAL GONDWANA SYMPOSIUM, VOLS 1 AND 2, P67; Prasad B., 1995, Geoscience Journal, V16, P155; Prasad B, 2017, J GEOL SOC INDIA, V90, P405, DOI 10.1007/s12594-017-0735-3; QURESHY MN, 1968, GEOL SOC AM BULL, V79, P1221, DOI 10.1130/0016-7606(1968)79[1221:GAATGR]2.0.CO;2; Raja Rao CS., 1982, Geological Survey of India Bulletin, Series A, V45, P9; Ramanamurty BV., 1979, Geological Survey of India Miscellaneous Publication, V45, P89; Ravn RL., 1988, Palynology, V12, p):179; Singh YR, 2016, HIMAL GEOL, V37, P35; Srinivasarao K., 1977, P 4 INT GONDW S CALC, VII, P889; Srivastava SC., 1992, Geophytology, V20, P83; Srivastava SC., 1996, Palaeobotanist, V46, P88; Thiergart F., 1962, Indien. Berichte der Deutschen Botanischen Gesellschaft, V75, P71; Tiwari RS., 1991, Journal of Palaeosciences, V40, P194; Traverse A., 2007, Topics in Geobiology Series, American Association of Stratigraphic Palynologists Foundation, V28, P1; Van de Laar JGM., 1989, Mededelingen Rijks Geologische Dienst, V43, P35	39	3	3	3	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	JUL 2	2024	48	3								10.1080/01916122.2024.2323730	http://dx.doi.org/10.1080/01916122.2024.2323730		MAR 2024	18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ZG1P8					2025-03-11	WOS:001199371000001
J	Mansour, A; Ruebsam, W; Tahoun, SS; Wang, J; Ahmed, MS; Fu, XG				Mansour, Ahmed; Ruebsam, Wolfgang; Tahoun, Sameh S.; Wang, Jian; Ahmed, Mohamed S.; Fu, Xiugen			Palynological sequence stratigraphic development and eustatic sea-level controls during the Late Albian-Cenomanian from fluvio-deltaic to the shallow platform settings at the northern paleo-Gondwana margin (Egypt)	MARINE AND PETROLEUM GEOLOGY			English	Article						Third -order sequence; Eustatic sea -level; Dinoflagellate cysts; Glacio-eustasy; Gindi basin; North Africa	UPPER CRETACEOUS SEQUENCES; DINOFLAGELLATE CYSTS; BAHARIYA FORMATION; WESTERN DESERT; OIL-FIELD; SYSTEMS; RECORD; BASIN; HISTORY; ROCKS	The late Albian-Cenomanian (mid -Cretaceous) greenhouse world was characterized by major eustatic sea -level variations and environmental change. However, little is known about the drivers of Cenomanian sea -level change. This work discusses stratigraphic trends in the palynofacies and palynomorph composition for upper Albian-Cenomanian strata from the North Qarun-1x well in the Gindi Basin (Egypt). These new data were combined with previously published data and embedded into a sequence stratigraphic framework. Results reveal four third -order (ca. 1.2 Myr) transgressive -regressive sequences for the upper Albian-middle Cenomanian upper Kharita and Bahariya formations and two sequences for the upper Cenomanian Abu Roash G Member. The increasing content of dinoflagellate cysts, mainly chorate and skolochorate forms, along with microforaminiferal test linings (FTLs) and an increase in the palynological marine index (PMI) compared to decreasing trends of spores and pollen grains are indicative for the deepening of the depositional setting upon sea -level rise and vice versa. Chorate and skolochorate dinoflagellate forms, such as Dinopterygium, Florentinia, Coronifera, Spiniferites groups, usually occur in transgressive systems tracts (TST), compared to marginal marine forms, such as Subtilisphaera and Aptea?, which are recorded in regressive systems tract (RST) sediments. Trans -regional correlation between the upper Albian-Cenomanian stratigraphic sequences from the Gindi and Abu Gharadig basins in the North Western Desert and Gulf of Suez indicates synchronous major marine transgression during the Cenomanian. Trans -regional correlation with other coeval third -order sequences from Morocco, Algeria, and Germany provide evidence for a regional to global eustatic control of sea -level changes at the northern Gondwana paleo-margin at this time. The magnitudes and timing of the late Albian-Cenomanian sea -level cycles were modest (about 35 m), pointing to glacio-eustasy as a potential driver.	[Mansour, Ahmed; Wang, Jian; Fu, Xiugen] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed; Wang, Jian; Fu, Xiugen] Southwest Petr Univ, Qiangtang Inst Sedimentary Basin, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Ruebsam, Wolfgang] Univ Kiel, Inst Geosci, Dept Organ & Isotope Geochem, Kiel, Germany; [Tahoun, Sameh S.] Cairo Univ, Fac Sci, Geol Dept, Giza 12613, Egypt; [Ahmed, Mohamed S.] King Saud Univ, Coll Sci, Dept Geol & Geophys, POB 2455, Riyadh 11451, Saudi Arabia	Southwest Petroleum University; Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; University of Kiel; Egyptian Knowledge Bank (EKB); Cairo University; King Saud University	Mansour, A (通讯作者)，Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China.	ahmedmans48@mu.edu.eg	Ruebsam, Wolfgang/AGG-2315-2022; Mansour, Ahmed/AAR-4969-2020; Ahmed, Mohamed/GQP-1116-2022	Mansour, Ahmed/0000-0003-2466-7494	National Natural Science Foundation of China [42241202, 42241203]; King Saud University, Riyadh, Saudi Arabia [RSP 2024R455]; Egyptian General Petroleum Corporation	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); King Saud University, Riyadh, Saudi Arabia(King Saud University); Egyptian General Petroleum Corporation	This study was supported by the National Natural Science Foundation of China (grant numbers: 42241202 and 42241203) and Researchers Supporting project number (RSP 2024R455) , King Saud University, Riyadh, Saudi Arabia. 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Pet. Geol.	MAR	2024	163								106781	10.1016/j.marpetgeo.2024.106781	http://dx.doi.org/10.1016/j.marpetgeo.2024.106781		MAR 2024	18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OE9Q3					2025-03-11	WOS:001205711300001
J	Peryt, D; Gedl, P; Worobiec, E; Worobiec, G; Peryt, TM				Peryt, Danuta; Gedl, Przemyslaw; Worobiec, Elzbieta; Worobiec, Grzegorz; Peryt, Tadeusz Marek			Foraminiferal and Palynological Records of an Abrupt Environmental Change at the Badenian/Sarmatian Boundary (Middle Miocene): A Case Study in Northeastern Central Paratethys	GEOSCIENCES			English	Article						foraminifera; palynofacies; dinocysts; pollen; spores; Miocene; Central Paratethys; Carpathian Foredeep; Poland	CARPATHIAN FOREDEEP BASIN; ROMANIA PALEOGEOGRAPHIC CHANGES; SARMATIAN EXTINCTION EVENT; BADENIAN SALINITY CRISIS; PALCU ET-AL.; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; GLOBIGERINA-BULLOIDES; OXYGEN INDEX; ASH LAYER	The Badenian/Sarmatian boundary in the Central Paratethyan basins is characterised by a change from open marine conditions during the late Badenian to the assumed brackish conditions during the early Sarmatian. The foraminiferal and palynological results of the Badenian/Sarmatian boundary interval in the Babczyn 2 borehole (in SE Poland) showed that the studied interval accumulated under variable, unstable sedimentary conditions. The Badenian/Sarmatian boundary, as correlated with a sudden extinction of stenohaline foraminifera, is interpreted as being due to the shallowing of the basin. The lack of foraminifera and marine palynomorphs just above the Badenian/Sarmatian boundary can reflect short-term anoxia. The composition of the euryhaline assemblages, characteristic for the lower Sarmatian part of the studied succession, indicates from marine to hypersaline conditions.	[Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland; [Worobiec, Elzbieta; Worobiec, Grzegorz] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland; [Peryt, Tadeusz Marek] Polish Geol Inst, Natl Res Inst, Rakowiecka 4, PL-00975 Warsaw, Poland	Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; W. 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J	Shinzato, C; Yoshioka, Y				Shinzato, Chuya; Yoshioka, Yuki			Genomic Data Reveal Diverse Biological Characteristics of Scleractinian Corals and Promote Effective Coral Reef Conservation	GENOME BIOLOGY AND EVOLUTION			English	Review						scleractinian corals; genome sequencing; evolution; conservation; diversity	GREAT-BARRIER-REEF; GENETIC DIVERSITY; WILD POPULATIONS; ACROPORA-TENUIS; BIOSYNTHESIS; RESPONSES; SYMBIOSIS	Reef-building corals (Scleractinia, Anthozoa, Cnidaria) are the keystone organisms of coral reefs, which constitute the most diverse marine ecosystems. Since the first decoded coral genome reported in 2011, about 40 reference genomes are registered as of 2023. Comparative genomic analyses of coral genomes have revealed genomic characters that may underlie unique biological characteristics and coral diversification. These include existence of genes for biosynthesis of mycosporine-like amino acids, loss of an enzyme necessary for cysteine biosynthesis in family Acroporidae, and lineage-specific gene expansions of DMSP lyase-like genes in the genus Acropora. While symbiosis with endosymbiotic photosynthetic dinoflagellates is a common biological feature among reef-building corals, genes associated with the intricate symbiotic relationship encompass not only those shared by many coral species, but also genes that were uniquely duplicated in each coral lineage, suggesting diversified molecular mechanisms of coral-algal symbiosis. Coral genomic data have also enabled detection of hidden, complex population structures of corals, indicating the need for species-specific, local-scale, carefully considered conservation policies for effective maintenance of corals. Consequently, accumulating coral genomic data from a wide range of taxa and from individuals of a species not only promotes deeper understanding of coral reef biodiversity, but also promotes appropriate and effective coral reef conservation. Considering the diverse biological traits of different coral species and accurately understanding population structure and genetic diversity revealed by coral genomic analyses during coral reef restoration planning could enable us to "archive" coral reef environments that are nearly identical to natural coral reefs.	[Shinzato, Chuya] Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba 2778564, Japan; [Yoshioka, Yuki] Okinawa Inst Sci & Technol Grad Univ, Marine Genom Unit, Okinawa 9040412, Japan	University of Tokyo; Okinawa Institute of Science & Technology Graduate University	Shinzato, C (通讯作者)，Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba 2778564, Japan.	c.shinzato@aori.u-tokyo.ac.jp	Yoshioka, Yuki/AAO-5382-2020; Shinzato, Chuya/G-2958-2015	Shinzato, Chuya/0000-0001-7843-3381; Yoshioka, Yuki/0000-0001-6348-4629	Japan Society for the Promotion of Science (JSPS) KAKENHI [20H03235, 20K21860]; JSPS [20J21301, 23KJ2129]; Grants-in-Aid for Scientific Research [23KJ2129, 20H03235, 20K21860] Funding Source: KAKEN	Japan Society for the Promotion of Science (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)); 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))	Preparation of the manuscript was partially supported by Japan Society for the Promotion of Science (JSPS) KAKENHI grants (20H03235 and 20K21860 for C.S.) and Grant-in-Aid for JSPS Fellows to Y.Y. (20J21301 and 23KJ2129).	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J	Mout, JM; Sarmah, RK				Mout, Joya Moni; Sarmah, Ranjan Kumar			Palynological Study of the Eocene Kopili Shale, Assam-Arakan Basin, India	PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS			English	Article						Palynology; Late Eocene; Kopili Shale; North Cachar Hills; Assam Arakan Basin	NORTH CACHAR HILLS; DINOFLAGELLATE CYSTS; PALYNOFOSSILS; GUJARAT; AREA	Palynological investigation was conducted to reconstruct the palaeodepositional and palaeoclimatic conditions of the late Eocene Kopili Shale of Assam-Arakan Basin (AAB), India. The palynoassemblage (PA) comprises particulate organic matters (POMs), dinoflagellate cysts (DCs), pteridophytic spores (PSs), angiospermous pollen (APs), acritarchs, fungal remains (FRs) and foraminiferal linings (FLs). Amorphous organic matter (AOM), making up 55 to 97 % of the PA, is the predominant form of organic matter (OM) among the POMs. The palynoflora is dominated by DCs comprising 5 genera (Cordosphaeridium, Hystrichosphaeridium, Heteraulacacysta, Glaphyrocysta and Thalassiphora) and 22 referable species. The PSs are assigned to 3 families (Polypodiaceae, Matoniaceae and Osmundaceae) and 8 referable species. The APs are characterised by 3 families (Arecaceae, Fabaceae and Gunneraceae) and 9 pollen species. The palynological data reveal that the Kopili Shale was deposited in a marginal-marine to shallow marine environment under suboxic-anoxic basin condition having influx of coastal elements into the depositional basin. The palaeoclimatic condition during the deposition of the Kopili Shale was tropical-subtropical and warm-humid.	[Mout, Joya Moni; Sarmah, Ranjan Kumar] Dibrugarh Univ, Dept Appl Geol, Dibrugarh 786004, Assam, India	Dibrugarh University	Mout, JM (通讯作者)，Dibrugarh Univ, Dept Appl Geol, Dibrugarh 786004, Assam, India.	joya.mout1990@gmail.com			Regional Geoscience Laboratories (RGL)	Regional Geoscience Laboratories (RGL)	The authors thank the Regional Geoscience Laboratories (RGL), ONGCL, Sivasagar, Assam for providing laboratory facilities to carry out this work. The authors acknowledge Mr. Lusuchu Phor's assistance in identifying the fossils. The authors also thank the Editors of PBPE, Torsten Utescher and anonymous reviewers for their constructive comments and suggestions, which improved the final version of this manuscript.	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J	Hedberg, P; Olsson, M; Höglander, H; Brüchert, V; Winder, M				Hedberg, Per; Olsson, Markus; Hoglander, Helena; Bruchert, Volker; Winder, Monika			Climate change effects on plankton recruitment from coastal sediments	JOURNAL OF PLANKTON RESEARCH			English	Article						resting stage; recruitment; emergence; phytoplankton; zooplankton; dinoflagellate; cyanobacteria; diatoms; copepods	FILAMENTOUS CYANOBACTERIA; SEASONAL OCCURRENCE; COMMUNITY ECOLOGY; CALANOID COPEPODS; RESTING STAGES; LIFE-HISTORY; BALTIC SEA; PHYTOPLANKTON; BLOOMS; EGGS	In highly seasonal systems, the emergence of planktonic resting stages from the sediment is a key driver for bloom timing and plankton community composition. The termination of the resting phase is often linked to environmental cues, but the extent to which recruitment of resting stages is affected by climate change remains largely unknown for coastal environments. Here we investigate phyto- and zooplankton recruitment from oxic sediments in the Baltic Sea in a controlled experiment under proposed temperature and light increase during the spring and summer. We find that emergence of resting stage differs between seasons and the abiotic environment. Phytoplankton recruitment from resting stages were high in spring with significantly higher emergence rates at increased temperature and light levels for dinoflagellate and cyanobacteria than for diatoms, which had highest emergence under cold and dark conditions. In comparison, hatching of copepod nauplii was not affected by increased temperature and light levels. These results show that activation of plankton resting stages are affected to different degrees by increasing temperature and light levels, indicating that climate change affects plankton dynamics through processes related to resting stage termination with potential consequences for bloom timing, community composition and trophic mismatch.	[Hedberg, Per; Olsson, Markus; Hoglander, Helena; Winder, Monika] Stockholm Univ, Dept Ecol Environm & Plant Sci, Stockholm, Sweden; [Bruchert, Volker] Stockholm Univ, Dept Geol Sci, Stockholm, Sweden; [Bruchert, Volker; Winder, Monika] Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden; [Hedberg, Per] Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland	Stockholm University; Stockholm University; University of Helsinki	Winder, M (通讯作者)，Stockholm Univ, Dept Ecol Environm & Plant Sci, Stockholm, Sweden.; Winder, M (通讯作者)，Stockholm Univ, Bolin Ctr Climate Res, Stockholm, Sweden.	per.hedberg@helsinki.fi; markus.olsson@su.se; helena.hoglander@su.se; volker.bruchert@geo.su.se; monika.winder@su.se	Winder, Monika/F-5318-2016	Olsson, Markus/0009-0004-5622-1723; Winder, Monika/0000-0001-9467-3035; Bruchert, Volker/0000-0002-8956-3840; Hedberg, Per/0000-0001-9809-5439	Swedish Research Council Formas [2015-1320]	Swedish Research Council Formas(Swedish Research Council Formas)	We are grateful for the support by the staff at the Asko field station, Nellie Stjarnkvist and Sebastian Strandgaard in sample collection. We also acknowledge constructive feedback from reviewers. This project was funded by the Swedish Research Council Formas (Grant 2015-1320).	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Plankton Res.	FEB 15	2024	46	2					117	125		10.1093/plankt/fbad060	http://dx.doi.org/10.1093/plankt/fbad060		FEB 2024	9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	YP2D5	38572122	Green Published, hybrid			2025-03-11	WOS:001166202500001
J	Elbra, T; Skupien, P; Bubík, M; Kosták, M; Matejová, MM; Pruner, P; Reháková, D; Svábenická, L; Vañková, L; Cígler, V; Geist, J; Kdyr, S; Lukeneder, A; Rybová, P; Mazuch, M; Schnabl, P; Svobodová, A; Trubac, J; Ucar, H				Elbra, T.; Skupien, P.; Bubik, M.; Kostak, M.; Matejova, M. Molcan; Pruner, P.; Rehakova, D.; Svabenicka, L.; Vankova, L.; Cigler, V.; Geist, J.; Kdyr, S.; Lukeneder, A.; Rybova, P.; Mazuch, M.; Schnabl, P.; Svobodova, A.; Trubac, J.; Ucar, H.			Integrated stratigraphy across the Jurassic-Cretaceous boundary in the Rettenbacher section (Northern Calcareous Alps, Salzburg, Austria)	CRETACEOUS RESEARCH			English	Article						Northern Calcareous Alps; Jurassic-Cretaceous boundary; Biostratigraphy; Magnetic properties; C -O stable isotopes	OXYGEN-ISOTOPE; JURASSIC/CRETACEOUS BOUNDARY; WESTERN CARPATHIANS; KUROVICE SECTION; LEUBE QUARRY; BIOSTRATIGRAPHY; EVOLUTION; CARBON; TETHYAN; RECONSTRUCTION	Rettenbacher Quarry carbonate sequence in the Northern Calcareous Alps represents highly dynamic pelagic carbonate sedimentation in the lower slope environment. The section spans from upper Tithonian Crassicollaria colomi Subzone to middle Berriasian Calpionella elliptica Subzone. Radiolarian samples belong to Pseudodictyomitra carpatica Zone. Considerable redeposition of calpionellids, organic walled dinoflagellate cysts, calcareous nannofossils and foraminifera in the allodapic layers, as well as extensive normal polarity remagnetisation event with substantial clockwise rotation is documented. Quantitative predominance of genera Watznaueria and Cyclagelosphaera indicate strong nannofossil modification during diagenesis. The almost straight trend in the 313C with some slight carbon-isotope perturbations is recorded at Rettenbacher. Three significant and stratigraphically important negative excursions of the 313Ccarb values were identified - including tentative indication of a new "Negative peak 4" in the upper part of the Elliptica Subzone - and correlated with other sections confirming stability, respectively isochronity within carbon chemostratigraphy.	[Elbra, T.; Pruner, P.; Vankova, L.; Kdyr, S.; Schnabl, P.; Svobodova, A.; Ucar, H.] Czech Acad Sci, Inst Geol, Rozvojova 269, CZ-16500 Prague, Czech Republic; [Skupien, P.; Rybova, P.] VSB Tech Univ Ostrava, Dept Geol Engn, 17 Listopadu 15, Poruba Ostrava 70833, Czech Republic; [Bubik, M.; Cigler, V.] Czech Geol Survey, Leitnerova 22, Brno 60200, Czech Republic; [Kostak, M.; Vankova, L.; Geist, J.; Mazuch, M.] Charles Univ Prague, Inst Geol & Palaeontol, Fac Sci, Albertov 6, Prague 2, Czech Republic; [Matejova, M. Molcan; Rehakova, D.] Comenius Univ, Dept Geol & Palaeontol, Ilkovicova 6, SK-84215 Bratislava, Slovakia; [Svabenicka, L.] Czech Geol Survey, Klarov 131-3, Prague CZ-11821, Czech Republic; [Kdyr, S.; Trubac, J.] Charles Univ Prague, Fac Sci, Inst Geochem Mineral & Mineral Resources, Albertov 6, Prague 2, Czech Republic; [Lukeneder, A.] Nat Hist Museum Vienna, Geol & Palaeontol Dept, Burgring 7, A-1010 Vienna, Austria; [Ucar, H.] Charles Univ Prague, Fac Sci, Inst Hydrogeol Engn Geol & Appl Geophys, Albertov 6, Prague 2, Czech Republic	Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Technical University of Ostrava; Czech Geological Survey; Charles University Prague; Comenius University Bratislava; Czech Geological Survey; Charles University Prague; Charles University Prague	Elbra, T (通讯作者)，Czech Acad Sci, Inst Geol, Rozvojova 269, CZ-16500 Prague, Czech Republic.	elbra@gli.cas.cz; petr.skupien@vsb.cz; miroslav.bubik@geology.cz; martin.kostak@natur.cuni.cz; marina.matejova@uniba.sk; pruner@gli.cas.cz; daniela.rehakova@uniba.sk; lilian.svabenicka@geology.cz; lucie.vankova@natur.cuni.cz; vojtech.cigler@geology.cz; jan.geist@natur.cuni.cz; kdyr@gli.cas.cz; alexander.lukeneder@nhm-wien.ac.at; pavlina.rybova@vsb.cz; martin.mazuch@natur.cuni.cz; schnabl@gli.cas.cz; asvobodova@gli.cas.cz; jakub.trubac@natur.cuni.czr.cuni.cz; ucar@gli.cas.cz	Ucar, Hakan/ACZ-2429-2022; Vaňková, Lucie/AAD-3273-2019; Reháková, Daniela/Z-1300-2019; Geist, Jan/KGM-6370-2024; Elbra, Tiiu/F-6859-2012; Molcan Matejova, Marina/MCY-5588-2025; Mazuch, Martin/I-5964-2017; Trubac, Jakub/J-5890-2012; Kostak, Martin/I-6006-2017; Skupien, Petr/G-8767-2019	Vankova, Lucie/0000-0002-4363-2003; Lukeneder, Alexander/0000-0002-8384-3366; Mazuch, Martin/0000-0002-1697-3742; Elbra, Tiiu/0000-0001-6115-0588; Trubac, Jakub/0000-0002-9470-1304; Ucar, Hakan/0000-0002-6979-8941; Ucar, Hakan/0000-0002-2844-0118; Kostak, Martin/0000-0002-0818-3505; Molcan Matejova, Marina/0000-0002-5581-279X; Skupien, Petr/0000-0001-9158-466X; Kdyr, Simon/0000-0003-2759-899X; Cigler, Vojtech/0000-0002-9787-9650; Geist, Jan/0000-0003-2909-7427	Czech Science Foundation [20-10 035S]; Slovak Research and Development Agency [2/0012/24]; VEGA [RVO67985831]; IGCP; Research Plan DRKVO 2023-2027 of the Czech Geological Survey [APVV-20-0079]; COOPERATIO (Faculty of Science, Charles University) [679];  [APVV-21- 0281];  [311430];  [UNCE/SCI/006];  [1/0435/21]	Czech Science Foundation(Grant Agency of the Czech Republic); Slovak Research and Development Agency(Slovak Research and Development Agency); VEGA(Vedecka grantova agentura MSVVaS SR a SAV (VEGA)); IGCP; Research Plan DRKVO 2023-2027 of the Czech Geological Survey; COOPERATIO (Faculty of Science, Charles University); ; ; ; 	The research was supported by Czech Science Foundation project no. 20-10 035S. Microfacies, calpionellid and calcareous dinocyst research was supported by the projects of the Slovak Research and Development Agency-APVV-20-0079, APVV-21- 0281, and by VEGA 2/0012/24, VEGA 1/0435/21. The research is in accordance with research plan no. RVO67985831, and with main aims of Berriasian Working Group and IGCP 679 project. Foraminifer and nannofossil study is a contribution to the Project No. 311430 within the Research Plan DRKVO 2023-2027 of the Czech Geological Survey. Authors thank also to project COOPERATIO (Faculty of Science, Charles University) and project UNCE/SCI/006. Authors are especially grateful to the Rettenbacher family for allowing research in their quarry. Many thanks to K. Bachova, J. Petracek, and L. Kouklikova for assistance during fieldwork, sample preparation and magnetic analyses. Authors would like to thank editors, and Justyna Kowal-Kasprzyk and anonymous reviewer for their helpful reviews and improvements.	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P., 2020, Volumina Jurassica, V18, P121, DOI 10.7306/VJ.18.7; Wimbledon William A. P., 2020, Volumina Jurassica, V18, P53, DOI 10.7306/VJ.18.5; Wimbledon WAP, 2020, GEOL CARPATH, V71, P24, DOI 10.31577/GeolCarp.71.1.3; Young J.R., 2018, NANNOTAX3 WEBSITE; Zák K, 2011, PALAEOGEOGR PALAEOCL, V299, P83, DOI 10.1016/j.palaeo.2010.10.038	101	1	1	2	3	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JUN	2024	158								105854	10.1016/j.cretres.2024.105854	http://dx.doi.org/10.1016/j.cretres.2024.105854		FEB 2024	23	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	LP6I4					2025-03-11	WOS:001188040700001
J	Raafat, A; Zakaria, A				Raafat, Aya; Zakaria, Ahmed			Upper Cretaceous (Cenomanian) palynostratigraphy and palynofacies of the Shushan Basin, North Egypt	PALYNOLOGY			English	Article						Cenomanian (Upper Cretaceous); biozonation; paleoenvironment; Shushan Basin; Western Desert; Egypt	SEQUENCE STRATIGRAPHY; WESTERN DESERT; EASTERN DESERT; FORAMINIFERAL BIOSTRATIGRAPHY; TURONIAN SUCCESSION; PALYNOLOGY; SEDIMENTS; POLLEN; SINAI; BOREHOLE	This study provides an updated quantitative analysis and prospective paleoenvironment reconstruction of the Tut oilfield, Shushan Basin, North Egypt to evaluate the hydrocarbon reservoirs in space and times for further development plans and modeling in the Tethyan region. Two sporomorph interval zones (Classopollis brasiliensis and Afropollis jardinus), and one total foraminiferal Range Zone (Thomasinella punica) are proposed. Three palynofacies assemblages are differentiated using cluster analysis of the different palynofacies parameters. The paleoenvironmental conditions during the Cenomanian were reconstructed. Palynofacies assemblage I of the Baharyia Formation suggests a marginally dysoxic-oxic basin environment with a common occurrence of ostracods and terrestrial organic matter, while palynofacies assemblage II reflects the high abundance of dinoflagellate cysts, suggesting a suboxic-anoxic middle neritic environment. Palynofacies assemblage III of the upper part of the Abu Roash G Member represents a relatively deep water inner-middle neritic environment. Three 3rd order significant sequences separated by two hiatus surfaces (Ce3 and Ce4) are described and correlated with the global eustatic sea-level. The hydrocarbon evaluation results show that the samples from the Abu Roash G Member contain oil-prone material of kerogen type II, while the samples of the Baharyia Formation are characterized by kerogen type III (gas-prone). Spore coloration analysis reveals that the samples from the studied units are too immature to produce gas or oil and are ineffective as sources of hydrocarbons.	[Raafat, Aya; Zakaria, Ahmed] Cairo Univ, Fac Sci, Geol Dept, Giza, Egypt	Egyptian Knowledge Bank (EKB); Cairo University	Raafat, A (通讯作者)，Cairo Univ, Fac Sci, Geol Dept, Giza, Egypt.	ayar@sci.cu.edu.eg	Raafat, Aya/AHE-3464-2022					ABDALLAH H, 1995, CRETACEOUS RES, V16, P487, DOI 10.1006/cres.1995.1034; ANDREU B, 1993, GEOBIOS-LYON, V26, P69, DOI 10.1016/S0016-6995(93)80009-G; [Anonymous], 1992, Western Desert, oil and gas fields (A comprehensive overview), P431; Arai M., 1992, B S CRETACEO BRASIL, V2, P27; Bassiouni M.A.A., 2002, Neue Palaeontologische Abhandlungen, V5, P1; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Batten D. 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J	Bubik, M; Cigler, V; Mikulas, R; Rabrenovic, D; Rehakova, D; Skupien, P; Svabenicka, L; Svobodova, A; Svobodova, M				Bubik, Miroslav; Cigler, Vojtech; Mikulas, Radek; Rabrenovic, Dragoman; Rehakova, Daniela; Skupien, Petr; Svabenicka, Lilian; Svobodova, Andrea; Svobodova, Marcela			The integrated biostratigraphy and palaeoenvironments across the Jurassic-Cretaceous boundary in the Dedina section (eastern Serbian Carpathians)	CRETACEOUS RESEARCH			English	Article						Serbian Carpathians; Tithonian; Berriasian; Calpionellids; Calcareous nannofossils; Foraminifera	OUTER WESTERN CARPATHIANS; JURASSIC/CRETACEOUS BOUNDARY; CALPIONELLID BIOSTRATIGRAPHY; CALCAREOUS DINOFLAGELLATE; KUROVICE SECTION; SYSTEM; CRASSICOLLARIA; NANNOFOSSILS; MICROFACIES; TRANSITION	Upper Tithonian to lower Berriasian carbonate sequence of the Getic Nappe System was studied near Golubac using an integrated biostratigraphy approach based on calpionellid, calcareous dinoflagellate, nannofossil, foraminifer, and palynomorph record. Calpionellids allowed subdivision of the section to standard calpionellid zones including the Colomi and Alpina subzones on the Tithonian-Berriasian transition. Nannofossil Nannoconus wintereri proves the presence of the NC0 Zone. Foraminifer fauna on the Tithonian-Berriasian transition contain zonal marker Globospirillina neocomiana and some other potential stratigraphic markers, whose range and taxonomy have to be fixed yet. Poor palynomorph spectra consist of long-ranging Lower-Cretaceous spores and pollen, and a few dinoflagellate cysts known from the Berriasian. Integrated biostratigraphy of the Tithonian-Berriasian oligotrophic openmarine carbonate facies of the Dedina section contributes to the stratigraphic framework necessary for the definition of the Berriasian Global Boundary Stratotype Section and Point. (c) 2024 Elsevier Ltd. All rights reserved.	[Bubik, Miroslav; Cigler, Vojtech; Svobodova, Andrea; Svobodova, Marcela] Czech Geol Survey, Leitnerova 22, Brno 65869, Czech Republic; [Mikulas, Radek; Svobodova, Andrea; Svobodova, Marcela] Czech Acad Sci, Inst Geol, Rozvojova 269, Prague 16500, Czech Republic; [Rabrenovic, Dragoman] Geol Survey Serbia, Rovinjska 12, Belgrade 11000, Serbia; [Rehakova, Daniela] Comenius Univ, Fac Nat Sci, Dept Geol & Palaeontol, Ilkovicova 6, Bratislava 84215, Slovakia; [Skupien, Petr] VSB Tech Univ Ostrava, Dept Geol Engn, 17 Listopadu 15, Ostrava 70833, Czech Republic; [Svabenicka, Lilian] Czech Geol Survey, Klarov 131-3, Prague 11821, Czech Republic	Czech Geological Survey; Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Comenius University Bratislava; Technical University of Ostrava; Czech Geological Survey	Bubík, M (通讯作者)，Czech Geol Survey, Leitnerova 22, Brno 65869, Czech Republic.	miroslav.bubik@geology.cz; vojtech.cigler@geology.cz; mikulas@gli.cas.cz; dragoman.rabrenovic@gzs.gov.rs; daniela.rehakova@uniba.sk; petr.skupien@vsb.cz; lilian.svabenicka@geology.cz; asvobodova@gli.cas.cz; msvobodova@gli.cas.cz	Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X	Institute of Geology of the Czech Academy of Sciences [RVO67985831, 311430, DKRVO 2023-2027]; Slovak Research and Development Agency [APVV-20-0079, 2/0013/20]; VEGA agency	Institute of Geology of the Czech Academy of Sciences(Czech Academy of Sciences); Slovak Research and Development Agency(Slovak Research and Development Agency); VEGA agency(Vedecka grantova agentura MSVVaS SR a SAV (VEGA))	The research is supported by Czech Science Foundation project No. 20-10035S and co-financed by institutional support of theInstitute of Geology of the Czech Academy of Sciences, project RVO67985831. It is a contribution to the project No. 311430 within the Research Plan DKRVO 2023-2027 of the Czech Geological Survey. Microfacies, calpionellid and dinocyst investigations were supported by the Slovak Research and Development Agency project No. APVV-20-0079 and by the project No. 2/0013/20 of the VEGA agency. Many thanks to Silviya Petrova and Barbara Radulovic for careful reading of the munuscript and reviewer Stefan Jozsa for interesting discussion.r Institute of Geology of the Czech Academy of Sciences, project RVO67985831. It is a contribution to the project No. 311430 within the Research Plan DKRVO 2023-2027 of the Czech Geological Survey. Microfacies, calpionellid and dinocyst investigations were supported by the Slovak Research and Development Agency project No. APVV-20-0079 and by the project No. 2/0013/20 of the VEGA agency. Many thanks to Silviya Petrova and Barbara Radulovicy for careful reading of the munuscript and reviewer Sytefan Jyozsa for interesting discussion.	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P., 2020, Volumina Jurassica, V18, P121, DOI 10.7306/VJ.18.7; Wimbledon William A. P., 2020, Volumina Jurassica, V18, P53, DOI 10.7306/VJ.18.5; Wimbledon WAP, 2020, GEOL CARPATH, V71, P24, DOI 10.31577/GeolCarp.71.1.3; Wimbledon WAP, 2013, GEOL CARPATH, V64, P437, DOI 10.2478/geoca-2013-0030; Young J.R., 2018, NANNOTAX3 WEBSITE	54	3	3	1	4	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JUN	2024	158								105817	10.1016/j.cretres.2023.105817	http://dx.doi.org/10.1016/j.cretres.2023.105817		FEB 2024	26	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	KI1G8					2025-03-11	WOS:001179233800001
J	Wang, RR; Li, YC; Zhang, SR; Xu, QH; Ge, YW; Li, B; Fan, BS; Zhang, Z; Li, CE; Wang, Y; You, HF; Cao, YH; Li, Y				Wang, Rongrong; Li, Yuecong; Zhang, Shengrui; Xu, Qinghai; Ge, Yawen; Li, Bing; Fan, Baoshuo; Zhang, Zhen; Li, Cange; Wang, Ying; You, Hanfei; Cao, Yihang; Li, Yue			Response of late Holocene vegetation to abrupt climatic events on the northwestern coast of the Bay of Bohai, China	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Coastal wetland; Summer monsoon weakening; Climate change; 2.8 ka event; Sea level change	WALLED DINOFLAGELLATE CYSTS; ASIAN MONSOON RECORD; TROPICAL MAAR LAKE; HIGH-RESOLUTION; ICE-AGE; VARIABILITY; SEA; ENSO; SUMMER; POLLEN	Coastal wetlands provide valuable ecosystem services and understanding their response to past climatic changes may help predict their possible future responses. In this paper, we obtained records of pollen, algae, sediment grain-size, and other environmental proxies, from a late Holocene sediment core (CFD-E) from the Caofeidian area, on the northwest coast of the Bay of Bohai, China. Our results indicate three major stages of environmental change. During Stage I (3500-2800 cal yr BP), arboreal pollen content was high (mostly >60%), especially for Pinus and Quercus, and the PCA sample scores on Axis 1 were negative indicating that regional vegetation was temperate broadleaved forest and the climate was wet. During Stage II (2800-2350 cal yr BP), the arboreal pollen content decreased substantially (mostly <40%), and the PCA Axis 1 sample scores were positive indicating a decrease in forest vegetation, grassland expansion, and a drier climate. During Stage III (2350-1400 cal yr BP), the arboreal pollen content increased again (mostly >40%), although it remained lower than during Stage I, indicating that forests expanded under a relatively humid climate while the wetland area decreased slightly. Our results also record the 2.8 ka and 2.4 ka events of monsoon weakening, which were characterized by increases in herbaceous pollen (indicating grassland expansion) and the drying of the regional climate. There are several differences in the regional expression of these two climatic events. During the 2.4 ka event, Chenopodiaceae pollen increased substantially (average of 42.0%), indicating the expansion of halophytes; whereas during the 2.8 ka event, an increase in Artemisia indicates the occurrence of a dry climate throughout the region. We suggest that the aridity during the 2.8 ka event was triggered by decreased solar activity and the resulting changes in the El Nin similar to o-Southern Oscillation, which weakened the East Asian summer monsoon. However, we suggest that the 2.4 ka event was driven by the weakening of the Atlantic Meridional Overturning Circulation.	[Wang, Rongrong; Li, Yuecong; Zhang, Shengrui; Xu, Qinghai; Ge, Yawen; Li, Bing; Fan, Baoshuo; Li, Cange; Wang, Ying; You, Hanfei; Cao, Yihang; Li, Yue] Hebei Normal Univ, Coll Geog Sci, Shijiazhuang 050024, Hebei, Peoples R China; [Wang, Rongrong; Li, Yuecong; Zhang, Shengrui; Xu, Qinghai; Ge, Yawen; Li, Bing; Fan, Baoshuo; Li, Cange; Wang, Ying; You, Hanfei; Cao, Yihang; Li, Yue] Hebei Key Lab Environm Change & Ecol Construct, Shijiazhuang 050024, Hebei, Peoples R China; [Wang, Rongrong; Li, Yuecong; Zhang, Shengrui; Xu, Qinghai; Ge, Yawen; Li, Bing; Fan, Baoshuo; Li, Cange; Wang, Ying; You, Hanfei; Cao, Yihang; Li, Yue] Hebei Technol Innovat Ctr Remote Sensing Identific, Shijiazhuang 050024, Hebei, Peoples R China; [Zhang, Zhen] Hebei Geo Univ, Coll Earth Sci, Shijiazhuang 050031, Hebei, Peoples R China	Hebei Normal University; Hebei GEO University	Li, YC; Zhang, SR (通讯作者)，Hebei Normal Univ, Coll Geog Sci, Shijiazhuang 050024, Hebei, Peoples R China.; Li, YC; Zhang, SR (通讯作者)，Hebei Key Lab Environm Change & Ecol Construct, Shijiazhuang 050024, Hebei, Peoples R China.	lyczhli@aliyun.com; srzhang@hebtu.edu.cn	Zhang, Shengrui/P-1390-2019; Xu, Qinghai/HDO-8345-2022; Fan, Baoshuo/ACW-4046-2022; Ge, Yawen/LQJ-4950-2024		National Natural Science Foundation of China [U20A20116, 41877433]; Hebei Normal University [XCXZZSS202304]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Hebei Normal University	This research was supported by the National Natural Science Foundation of China (U20A20116, 41877433) and Hebei Normal University (XCXZZSS202304) . We thank the management of Caofeidian Wetland Nature Reserve in Hebei Province for their support during the field work. We thank senior engineer Qinmian Xu from the Tianjin Center, China Geological Survey, and Prof. Chunhai Li from the Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, for their assistance in sediment. We thank Dr. Jan Bloemendal for improving the English language.	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APR 1	2024	639								112062	10.1016/j.palaeo.2024.112062	http://dx.doi.org/10.1016/j.palaeo.2024.112062		FEB 2024	11	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	KG5O3					2025-03-11	WOS:001178820100001
J	Mitta, VV; Glinskikh, LA; Savelieva, YN; Shurekova, OV				Mitta, V. V.; Glinskikh, L. A.; Savelieva, Yu. N.; Shurekova, O. V.			Microfauna, Palynomorphs, and Biostratigraphy of the Upper Bajocian Strenoceras niortense Zone (Middle Jurassic) of the Kuban River Basin, Northern Caucasus	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Upper Bajocian; biostratigraphy; ammonites; foraminifers; ostracods; dinocysts; spores; pollen; Northern Caucasus	BOLSHOI ZELENCHUK RIVER; AMMONOIDEA STEPHANOCERATIDAE; PLANKTONIC-FORAMINIFERA; STRATIGRAPHY; PART; PERISPHINCTIDAE	Microfossils of the Strenoceras niortense Zone of the Upper Bajocian of the Karachay-Cherkessian Republic are studied. The zone is represented mainly by dark gray silty-sandy clays, with scattered nodules often arranged in interbeds, and belongs to the lower part of the upper subformation of the Djangura Formation. The taxonomic composition and distribution of foraminifera, ostracods, dinoflagellate cysts, and miospores in the section has been identified. The ranges of biostratigraphic units based on foraminifera, ostracods, and dinocysts are emended and these units are correlated with the ammonite scale. The distribution of benthic foraminifers indicates that these are Beds with Ophthalmidium caucasicum, comparable with the entire Niortense Zone and most of the Garantiana Zone. The Beds with Globuligerina dagestanica established using planktonic foraminifera are correlated with the entire studied interval from the Niortense Zone to the Lower Bathonian, inclusive. In the middle-upper part of the Niortense Zone (Rostovtsevi and Baculatum Subzones), the Beds with ostracods Palaeocytheridea (Malzevia) subtilis were recognized for the first time. The beds with dinocysts Carpathodinium predae, Rhynchodiniopsis? regalis, Meiourogonyaulax valensii are correlated with the range of the Niortense and Garantiana Zones and the lower part of the Parkinsoni Zone, inclusive. Characteristic taxa of microfauna and dinocysts are illustrated.	[Mitta, V. V.] Russian Acad Sci, Borissiak Paleontol Inst, Moscow 117647, Russia; [Glinskikh, L. A.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia; [Savelieva, Yu. N.] All Russian Geol Oil Inst, Aprelevka Branch, Aprelevka 143362, Moscow Oblast, Russia; [Shurekova, O. V.] Karpinsky Russian Geol Res Inst VSEGEI, St Petersburg 199106, Russia; [Mitta, V. V.] Cherepovets State Univ, Cherepovets 162600, Russia	Russian Academy of Sciences; Paleontological Institute of the Russian Academy of Sciences; Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences; A.P. Karpinsky Russian Geological Research Institute (VSEGEI); Cherepovets State University	Mitta, VV (通讯作者)，Russian Acad Sci, Borissiak Paleontol Inst, Moscow 117647, Russia.; Mitta, VV (通讯作者)，Cherepovets State Univ, Cherepovets 162600, Russia.	mitta@paleo.ru	Mitta, Vasily/O-2682-2018	Mitta, Vasily/0000-0001-7041-2295	Russian Ministry of Education and Science [FWZZ-2022-0005]	Russian Ministry of Education and Science(Ministry of Education and Science, Russian Federation)	The work was carried out under the project FWZZ-2022-0005 of the Russian Ministry of Education and Science (state assignment) (L.A. Glinskikh, Trofimuk Instituteof Petroleum Geology and Geophysics, Russian Academyof Sciences, Siberian Branch).	Antonova Z.A., 1958, T VNIGNI PROC ALL RU, V12, P213; Antonova Z.A., PROC KRASNODAR BR AL, VXVII, P41; Azbel A.A., 1991, Practical Guide on the Microfauna of the USSP. Vol. 5. Mesozoic Foraminifers; Beher Elke, 2010, Palaeodiversity, P43; Besnosov N.V., 1998, Bull. Collect. 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B, V75, P527; Yaroshenko O.P., 1965, Spores and pollen characteristic of Jurassic and Lower Cretaceous sediments of North Caucasus and their stratigraphy significance; Zatvornitsky A.Ya., 1914, Izv. Geol. Kom, V33, P525	48	0	0	0	1	PLEIADES PUBLISHING INC	NEW YORK	PLEIADES HOUSE, 7 W 54 ST, NEW YORK,  NY, UNITED STATES	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	FEB	2024	32	1					43	63		10.1134/S0869593824020060	http://dx.doi.org/10.1134/S0869593824020060			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	LZ4R4					2025-03-11	WOS:001190628300003
J	Chai, ZY; Liu, YY; Jia, SY; Li, FT; Hu, ZX; Deng, YY; Yue, CX; Tang, YZ				Chai, Zhaoyang; Liu, Yuyang; Jia, Siyang; Li, Fengting; Hu, Zhangxi; Deng, Yunyan; Yue, Caixia; Tang, Ying-Zhong			DNA and RNA Stability of Marine Microalgae in Cold-Stored Sediments and Its Implications in Metabarcoding Analyses	INTERNATIONAL JOURNAL OF MOLECULAR SCIENCES			English	Article						microalgae; DNA/RNA stability; resting cysts; sediments; metabarcoding; quantitative real-time PCR	POLYMERASE-CHAIN-REACTION; HARMFUL ALGAL BLOOMS; 16S RIBOSOMAL-RNA; REAL-TIME PCR; PROPIDIUM MONOAZIDE; BACTERIAL COMMUNITIES; EXTRACELLULAR DNA; GONYAULAX-TAMARENSIS; SP-NOV; CELLS	The ever-increasing applications of metabarcoding analyses for environmental samples demand a well-designed assessment of the stability of DNA and RNA contained in cells that are deposited or buried in marine sediments. We thus conducted a qPCR quantification of the DNA and RNA in the vegetative cells of three microalgae entrapped in facsimile marine sediments and found that >90% of DNA and up to 99% of RNA for all microalgal species were degraded within 60 days at 4 degrees C. A further examination of the potential interference of the relic DNA of the vegetative cells with resting cyst detection in sediments was performed via a metabarcoding analysis in artificial marine sediments spiked with the vegetative cells of two Kareniaceae dinoflagellates and the resting cysts of another three dinoflagellates. The results demonstrated a dramatic decrease in the relative abundances of the two Kareniaceae dinoflagellates in 120 days, while those of the three resting cysts increased dramatically. Together, our results suggest that a positive detection of microalgae via metabarcoding analysis in DNA or RNA extracted from marine sediments strongly indicates the presence of intact or viable cysts or spores due to the rapid decay of relic DNA/RNA. This study provides a solid basis for the data interpretation of metabarcoding surveys, particularly in resting cyst detection.	[Chai, Zhaoyang; Liu, Yuyang; Li, Fengting; Hu, Zhangxi; Deng, Yunyan; Yue, Caixia; Tang, Ying-Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Chai, Zhaoyang; Liu, Yuyang; Li, Fengting; Hu, Zhangxi; Deng, Yunyan; Tang, Ying-Zhong] Laoshan Lab, Qingdao 266237, Peoples R China; [Chai, Zhaoyang; Liu, Yuyang; Li, Fengting; Hu, Zhangxi; Deng, Yunyan; Tang, Ying-Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Jia, Siyang] Chinese Acad Sci, Inst Oceanol, Yellow Sea & East Sea Buoy Observat Stn, Qingdao 266071, Peoples R China; [Yue, Caixia] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Tang, YZ (通讯作者)，Laoshan Lab, Qingdao 266237, Peoples R China.; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	zhaoyangchai@qdio.ac.cn; lyy9303130@163.com; jiasy@qdio.ac.cn; lifengting111@126.com; huzx@gdou.edu.cn; yunyandeng@qdio.ac.cn; yuecaixia@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	Chai, Zhaoyang/F-7485-2017; ZHANG, hui jie/HTN-1690-2023; Li, Yang/KFB-5350-2024	Liu, Yuyang/0000-0003-0418-4989; Deng, Yunyan/0000-0001-5967-3611; Hu, Zhangxi/0000-0002-4742-4973; Chai, Zhaoyang/0000-0003-0526-8930; Tang, Ying-Zhong/0000-0003-0446-3128	Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science	Key Research Infrastructures in the CAS Field Stations of the Chinese Academy of Science	We would like to express our sincere gratitude to the four anonymous reviewers for their critical review and constructive comments.	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FEB	2024	25	3							1724	10.3390/ijms25031724	http://dx.doi.org/10.3390/ijms25031724			17	Biochemistry & Molecular Biology; Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Chemistry	HQ8I3	38339002	gold, Green Published			2025-03-11	WOS:001161059700001
J	Bertini, A; Niccolini, G; Gennari, R; Lozar, F; Menichetti, E; Natalicchio, M; Dela Pierre, F				Bertini, Adele; Niccolini, Gabriele; Gennari, Rocco; Lozar, Francesca; Menichetti, Elena; Natalicchio, Marcello; Dela Pierre, Francesco			Terrestrial and marine dynamics on the brink of the Messinian salinity crisis: A wet scenario from the northern Mediterranean	GLOBAL AND PLANETARY CHANGE			English	Article						Pollen; Organic -walled dinoflagellate cysts; Calcareous plankton; Paleoclimate; Late Miocene; Piedmont basin	FRESH-WATER BUDGET; DINOFLAGELLATE RESTING CYSTS; LATE MIOCENE; PIEDMONT BASIN; CLIMATE-CHANGE; PALEOENVIRONMENTAL EVOLUTION; BRAARUDOSPHAERA-BIGELOWII; SPATIAL-DISTRIBUTION; SAPROPEL SEQUENCES; TRIPOLI FORMATION	The ongoing debate on the causes and modalities of the Messinian Salinity Crisis (MSC) from 5.971 Ma needs to be implemented by an in-depth knowledge of the events and changes, on a global to regional scale, that have preceded its onset. Here we use palynological (pollen and dinocysts) and micropaleontological (foraminifers and calcareous nannoplankton) quantitative analyses from the Govone sedimentary succession (Northern Italy, western Mediterranean) to reconstruct the cyclical changes in atmosphere, surface, and deep -water hydrographic conditions during the Late Miocene, prior to the onset of the MSC (from ca 6.6 Ma) and across it (up to 5.96 Ma). On land, plant communities were dominated by arboreal life forms typical of warm and humid conditions. However, mid- to high altitude coniferous taxa attest to a sequence of cold to cool conditions, some coinciding with glacial obliquity -controlled phases, notably those across the MSC onset (i.e. TG34 and TG32). Dominant trees were Taxodioideae, especially in freshwater swamps, during warm and humid phases. The latter alternate with relatively less warm, and less humid phases characterised by the reduction of Taxodioideae, according to the precession -controlled sedimentary cyclicity (sapropel-marl couplets). The absence of any significant expansion in the herbaceous cover is evidence of no substantial increases in aridity at insolation minima. In the marine realm, the precession -controlled cycles correspond to prevalent alternations between warm water, oligotrophic (sapropel, insolation maxima) and cool water, eutrophic (marls, insolation minima) conditions. The progressive decrease of oceanic/outer neritic dinocyst taxa, along with a more continuous occurrence of the inner neritic ones, confirm the progressive restriction of Mediterranean and Atlantic connections, despite oceanic influxes, the latest at 6.14 Ma and 6.05 Ma. On the other hand, the occurrence of freshwater episodes, according to dinocysts, does not exclude possible connections with Paratethys, at 6.18 Ma and 6.07 Ma. All calcareous nannoplankton and foraminifera apparently disappear from the sedimentary record before the onset of the MSC, at ca 6.02 Ma; however, dinocysts allow the documentation of the history of pre-evaporitic conditions up to the beginning of the MSC onset, when lagoons, marked by frequent salinity changes, expanded in the inner neritic zone of the Govone intermediate depth basin, during ca 60 kyrs. Plant assemblages attest a long-lasting increase of seasonality (from 6.2 Ma) as well as a peculiar inversion in the dominant vegetal patterns of the sapropel-marl couplets, between ca 6.02 Ma and 5.96 Ma, corresponding to the uppermost four cycles. The significant restriction of the marine environment, after 6.02 Ma, possibly promoted atmospheric changes marked by reduced vs enhanced activity of the Mediterranean storm -track in phase with precession. This, in turn, regulated the amounts of runoff in the Northern Italian sectors from the Alps.	[Bertini, Adele; Niccolini, Gabriele; Menichetti, Elena] Univ Firenze, Dipartimento Sci Terra, Via G Pira 4, I-50121 Florence, Italy; [Gennari, Rocco; Lozar, Francesca; Natalicchio, Marcello; Dela Pierre, Francesco] Univ Torino, Dipartimento Sci Terra, Via Valperga Caluso 35, I-10125 Turin, Italy	University of Florence; University of Turin	Bertini, A (通讯作者)，Univ Firenze, Dipartimento Sci Terra, Via G Pira 4, I-50121 Florence, Italy.	adele.bertini@unifi.it; rocco.gennari@unito.it; francesca.lozar@unito.it; marcello.natalicchio@unito.it; francesco.delapierre@unito.it	Gennari, Rocco/S-4631-2019					[Anonymous], 2001, Baltica; Artoni A., 2004, GEOACTA-BOLOGNA, V3, P107; Bahr A., 2022, GEO SOC LONDON SPEC, V523, DOI [10.1144/SP523-2021-54, DOI 10.1144/SP523-2021-54]; Bartol M, 2008, PALAEOGEOGR PALAEOCL, V267, P77, DOI 10.1016/j.palaeo.2008.06.005; Baumann Karl-Heinz, 2016, Revue de Micropaleontologie, V59, P239, DOI 10.1016/j.revmic.2016.03.001; Beerling D, 2009, AM J SCI, V309, P97, DOI 10.2475/02.2009.01; 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Planet. Change	FEB	2024	233								104362	10.1016/j.gloplacha.2024.104362	http://dx.doi.org/10.1016/j.gloplacha.2024.104362		JAN 2024	20	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	JL2Z9		hybrid, Green Published			2025-03-11	WOS:001173269800001
J	Zonneveld, KAF; Harper, K; Kluegel, A; Chen, L; De Lange, G; Versteegh, GJM				Zonneveld, Karin A. F.; Harper, Kyle; Kluegel, Andreas; Chen, Liang; De Lange, Gert; Versteegh, Gerard J. M.			Climate change, society, and pandemic disease in Roman Italy between 200 BCE and 600 CE	SCIENCE ADVANCES			English	Article							WESTERN MEDITERRANEAN SEA; SURFACE TEMPERATURE VARIABILITY; LAST 2700 YEARS; PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYSTS; MULTI-PROXY; GULF; SEDIMENTS; RECORDS; TARANTO	Records of past societies confronted with natural climate change can illuminate social responses to environmental stress and environment-disease connections, especially when locally constrained high-temporal resolution paleoclimate reconstructions are available. We present a temperature and precipitation reconstruction for similar to 200 BCE to similar to 600 CE, from a southern Italian marine sedimentary archive-the first high-resolution (similar to 3 years) climate record from the heartland of the Roman Empire, stretching from the so-called Roman Climate Optimum to the Late Antique Little Ice Age. We document phases of instability and cooling from similar to 100 CE onward but more notably after similar to 130 CE. Pronounced cold phases between similar to 160 to 180 CE, similar to 245 to 275 CE, and after similar to 530 CE associate with pandemic disease, suggesting that climate stress interacted with social and biological variables. The importance of environment-disease dynamics in past civilizations underscores the need to incorporate health in risk assessments of climate change.	[Zonneveld, Karin A. F.; Versteegh, Gerard J. M.] Univ Bremen, Ctr Marine Environm Sci, MARUM, Leobener Str 8, D-28359 Bremen, Germany; [Zonneveld, Karin A. F.; Kluegel, Andreas; Chen, Liang] Univ Bremen, Geosci Dept, Klagenfurter Str, D-28359 Bremen, Germany; [Harper, Kyle] Univ Oklahoma, Dept Class & Letters, 650 Parrington Oval,CARN 110, Norman, OK 73019 USA; [Harper, Kyle] Santa Fe Inst, 1399 Hyde Pk Rd, Santa Fe, NM 87501 USA; [De Lange, Gert] Univ Utrecht, Fac Geosci, Dept Earth Sci, Geochem, Princetonpl 9, NL-3584 CC Utrecht, Netherlands; [Versteegh, Gerard J. M.] Constructor Univ Bremen, Dept Phys & Earth Sci, Campus Ring 1, D-28759 Bremen, Germany	University of Bremen; University of Bremen; University of Oklahoma System; University of Oklahoma - Norman; The Santa Fe Institute; Utrecht University	Zonneveld, KAF (通讯作者)，Univ Bremen, Ctr Marine Environm Sci, MARUM, Leobener Str 8, D-28359 Bremen, Germany.; Zonneveld, KAF (通讯作者)，Univ Bremen, Geosci Dept, Klagenfurter Str, D-28359 Bremen, Germany.	kzonneveld@marum.de	De Lange, Gert/B-9639-2014	De Lange, Gert/0000-0002-9420-3022; Harper, Kyle/0000-0001-9313-0725; Zonneveld, Karin/0000-0002-3390-1572	Geoscience Department at the University of Bremen; Department of Classics and Letters, University of Oklahoma; German Research Foundation [ZO114/15- 1]; German Science Foundation, grant DFG Cluster of Excellence (EXC); German Science Foundation Heisenberg [VE86/2, 3, 4]; ESF, EUROMARC [ZO114/2- 1, VE486/1]	Geoscience Department at the University of Bremen; Department of Classics and Letters, University of Oklahoma; German Research Foundation(German Research Foundation (DFG)); German Science Foundation, grant DFG Cluster of Excellence (EXC)(German Research Foundation (DFG)); German Science Foundation Heisenberg; ESF, EUROMARC	We acknowledge financial support by the Geoscience Department at the University of Bremen (K.A.F.Z. and A.K.); Department of Classics and Letters, University of Oklahoma (K.H.); German Research Foundation, grant ZO114/15- 1 (dating); German Science Foundation, grant DFG Cluster of Excellence (EXC): "The Ocean Floor - Earths Uncharted Interface" 2019-2025, RECEIVER Unit 3 (G.J.M.V.); German Science Foundation Heisenberg, grant VE86/2, 3, 4 (G.J.M.V.); and ESF, EUROMARC grants ZO114/2- 1 and VE486/1 (G.J.M.V. and L.C.).	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J	Fanberg, LM; Nagel, MA; Polkinghorne, CN; Teneyck, MC				Fanberg, Lana M.; Nagel, Michael A.; Polkinghorne, Christine N.; Teneyck, Matthew C.			Presence of zooplankton, eggs, and resting stages in ballast water samples from the Laurentian Great Lakes	JOURNAL OF GREAT LAKES RESEARCH			English	Article						Ballast water management; Dormancy; Invasion risk	INVERTEBRATE DIAPAUSING EGGS; RESIDUAL BALLAST; DINOFLAGELLATE CYSTS; BIOLOGICAL INVASIONS; EAST-COAST; SHIPS; SEDIMENTS; DORMANCY; RISK; INTRODUCTIONS	To minimize the introduction and spread of aquatic nuisance species, the United States Coast Guard (USCG) and the International Maritime Organization (IMO) regulate the allowed microbe, protist, and zooplankton densities present in ballast water discharged from commercial ships. However, the density of eggs and resting stages in ballast discharge are not routinely assessed when determining the effectiveness of ballast water treatment systems. While the density of eggs and resting stages found in residual sediment has been examined by various researchers, the density in ballast water uptake and discharge samples was previously unexamined. Untreated uptake and discharge ballast water samples from 2017, 2022, and 2023, collected on ships within the Laurentian Great Lakes from August through January, were analyzed for eggs and resting stages. The samples contained a total density of 325-140,859 eggs and resting stages per cubic meter. These results demonstrate that uncounted eggs and resting stages are present in ballast water, contributing to the risk of spreading aquatic nuisance species within the Great Lakes.	[Fanberg, Lana M.; Nagel, Michael A.; Polkinghorne, Christine N.; Teneyck, Matthew C.] Univ Wisconsin, Lake Superior Res Inst, POB 2000, Superior, WI 54880 USA	University of Wisconsin System	Fanberg, LM (通讯作者)，Univ Wisconsin, Lake Superior Res Inst, POB 2000, Superior, WI 54880 USA.	lfanberg@uwsuper.edu		Fanberg, Lana/0009-0007-1874-2490	U.S. Department of Transportation Maritime Administration [693JF72250002]	U.S. Department of Transportation Maritime Administration	<BOLD>Acknowledgements</BOLD> This material is based on work supported by the U.S. Department of Transportation Maritime Administration under Agreement No. 693JF72250002. The views and conclusions contained in this document are those of the authors and should not be interpreted as representing the opinions, policies, or endorsements of the U.S. Government. Mention of trade names or commercial products does not constitute their endorsement by the U.S. Government. We would like to thank Dr. Mary Balcer and Dr. Euan Reavie for their assistance with eggs and resting stages identification and Dr. Anne Kruchten, Dr. Jennifer Maki, Kelsey Prihoda, Heidi Schaefer, and Dr. Kurt Schmude for their help with this manuscript and discussions on this topic.	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Gt. Lakes Res.	FEB	2024	50	1							102275	10.1016/j.jglr.2023.102275	http://dx.doi.org/10.1016/j.jglr.2023.102275		JAN 2024	7	Environmental Sciences; Limnology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	IT8P0					2025-03-11	WOS:001168681400001
J	van Vliet, HJ; Bosselaers, MEJ; Munsterman, DK; Dijkshoorn, ML; de Groen, JJ; Post, K				van Vliet, Henk Jan; Bosselaers, Mark E. J.; Munsterman, Dirk K.; Dijkshoorn, Marcel L.; de Groen, Jeffrey Joel; Post, Klaas			A vertebra of a small species of<i> Pachycetus</i> from the North Sea and its inner structure and vascularity compared with other basilosaurid vertebrae from the same site	PEERJ			English	Article						Basilosaurids; Vertebral architecture; Dinoflagellate cysts; Maldegem Formation; Middle Eocene; Europe; Vascularity	MIDDLE EOCENE; ARCHAEOCETE WHALE; EOCETUS-WARDII; 1ST RECORD; CETACEA; MAMMALIA; BASIN; MODEL	In the Western Scheldt Estuary near the Belgian -Dutch border, middle to late Eocene strata crop out at the current seafloor. Most vertebrae of large Eocene basilosaurid taxa from this area were previously described in several papers. They represent three morphotypes: elongated vertebrae of a large species of Pachycetus (Morphotype 1b), a not -elongated vertebra of a large 'dorudontid' basilosaurid (Morphotype 2) and 'shortened' vertebrae of a new, unnamed taxon (Morphotype 3). This article deals with a still undescribed, smaller vertebra, NMR-16642, from this site. Our first aim was to date it by dinoflagellate cysts in adhering sediments. Yielding an age of about 38 Ma, it is one of the very few remains of basilosaurids from Europe, of which the age could be assessed with reasonable certainty. The vertebra, Morphotype 1a, is assigned to a small species of Pachycetus. High -quality CT scans are used to differentiate between NMR-16642, Morphotype 1a, and the large species of Pachycetus, Morphotype 1b. Another aim of this paper is to investigate the inner structure and vascularity of the study vertebra and that of the other morphotypes (1b, 2, 3) from this area by using high -quality CT scans. Notwithstanding differences in size, shape and compactness, the vertebral inner structure with a multi -layered cortex of periosteal bone, surrounding two cones of endosteal bone appears to be basically similar in all morphotypes. Apparently, this inner structure reflects the ontogenetic vertebral growth. An attempt to reconstruct the vascularity of the vertebrae reveals a remarkable pattern of interconnected vascular systems. From the dorsal and, if present, ventral foramina, vascular canals are running to a central vascular node. From this node a system of vascular canals goes to the epiphyseal ends, giving rise to separate systems for cortex and cones. It is the first time that the vascularity of vertebrae of archaeocetes is investigated.	[van Vliet, Henk Jan] Altrecht, Utrecht, Netherlands; [Bosselaers, Mark E. J.] Koninklijk Belg Inst Natuurwetenschappen, Brussels, Belgium; [Bosselaers, Mark E. J.] Koninklijk Zeeuwsch Genootschap Wetenschappen, Middelburg, Netherlands; [Munsterman, Dirk K.] Geol Survey Netherlands, Netherlands Org Appl Sci Res TNO, Utrecht, Netherlands; [Dijkshoorn, Marcel L.; de Groen, Jeffrey Joel] Erasmus Universitair Med Ctr Rotterdam, Rotterdam, Netherlands; [Post, Klaas] Nat Hist Museum Rotterdam, Natuurhist, Rotterdam, Netherlands	Netherlands Organization Applied Science Research	van Vliet, HJ (通讯作者)，Altrecht, Utrecht, Netherlands.	henkjanvanvliet@yahoo.com						Brandt J., 1873, M MOIRES LACAD MIE I, V20, P1, DOI 10.5962/bhl.title.39524; Brisson M., 1762, REGNUM ANIMALE CLASS, P1, DOI [10.5962/bhl.title.40361, DOI 10.5962/BHL.TITLE.40361]; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Cope E.D., 1867, Proceedings of the Academy of Natural Sciences of Philadelphia, V19, P138; Davydenko S, 2023, FRONT EARTH SC-SWITZ, V11, DOI 10.3389/feart.2023.1168681; de Buffrenil V., 1990, Journal of Vertebrate Paleontology, V10, P455; de Buffrénil V, 2010, J MAMM EVOL, V17, P101, DOI 10.1007/s10914-010-9130-1; De Smet D, 1997, project nummer TGO 94/47; Du Four I, 2006, VLIZ Special Publication, P16; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Fensome RA., 2019, AM ASS STRATIGRAPHIC, V50, P1173; Gingerich PD, 2022, PLOS ONE, V17, DOI 10.1371/journal.pone.0276110; Gingerich PD, 2015, J AFR EARTH SCI, V111, P273, DOI 10.1016/j.jafrearsci.2015.08.006; Girondot M, 2003, J VERTEBR PALEONTOL, V23, P458, DOI 10.1671/0272-4634(2003)023[0458:BPATTQ]2.0.CO;2; Gol'din P, 2013, J PALEONTOL, V87, P254, DOI 10.1666/12-080R.1; Gradstein F.M., 2020, GEOLOGIC TIME SCALE; Gray NM, 2007, ANAT REC, V290, P638, DOI 10.1002/ar.20533; Houssaye A, 2015, PLOS ONE, V10, DOI 10.1371/journal.pone.0118409; Kellogg R, 1936, A review of the Archaeoceti, P366; Le Bot S, 2003, Tertiary and quaternary geology of the Belgian Continental Shelf, P75; Martínez-Cáceres M, 2017, GEODIVERSITAS, V39, P7, DOI 10.5252/g2017n1a1; Muller J., 1849, On the fossil remains of the zeuglodonts of North America, with consideration on the European remains from this family, P38; Munsterman DK, 2004, TNO-NITG 04-016-B. 14; Munsterman DK, 2003, TNO-NITG 03-061-B. 20; Pilleri G, 1989, Contributions to the Paleontology of some Tethyan Cetacea and Sirenia (Mammalia), P27; Post K, 2017, Cranium, V34, P46; Post K, 2016, Deinsea, V16, P1; Post Klaas, 2007, Cranium, V24, P31; Powell A.J., 1992, P155; Schouten S, 2011, Cranium, V28, P17; Steurbaut E, 2015, GEOL BELG, V18, P147; Uhen M.D., 2001, Southeastern Geology, V40, P135; Uhen MD, 2008, J VERTEBR PALEONTOL, V28, P589, DOI 10.1671/0272-4634(2008)28[589:NPWFAA]2.0.CO;2; Uhen MD, 2008, FOSS REC, V11, P57, DOI 10.1002/mmng.200800001; Uhen MD, 1999, J PALEONTOL, V73, P512, DOI 10.1017/S002233600002802X; Van Benden P. J., 1883, B LACADEMIE SCI LETT, V6, P27; van Vliet Henk Jan, 2023, Deinsea (Rotterdam), P1; van Vliet Henk Jan, 2022, Deinsea (Rotterdam), P1; van Vliet Henk Jan, 2020, Cainozoic Research, V20, P121; Vandenberghe N, 2004, NETH J GEOSCI, V83, P155, DOI 10.1017/S0016774600020229; Weems RE, 2011, J PALEONTOL, V85, P271, DOI 10.1666/10-083.1	41	1	1	0	0	PEERJ INC	LONDON	341-345 OLD ST, THIRD FLR, LONDON, EC1V 9LL, ENGLAND	2167-8359			PEERJ	PeerJ	JAN 25	2024	12								e16541	10.7717/peerj.16541	http://dx.doi.org/10.7717/peerj.16541			27	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	GL7B9	38774542	Green Published, gold			2025-03-11	WOS:001152878300004
J	Soliman, A; Slimani, H; Said, S				Soliman, Ali; Slimani, Hamid; Said, Somia			Two new ceratioid cornucavate dinoflagellate cysts from the Upper Cretaceous, Gulf of Suez, Egypt	MARINE MICROPALEONTOLOGY			English	Article						Santonian; Matulla Formation; Ceratiaceae; Corniform gonyaulacoid; Odontochitina	PALEOENVIRONMENTAL ANALYSIS; BOREHOLE; POLLEN; BASIN; ASSEMBLAGES; SPORES; POLAND	Diverse and well-preserved assemblages of organic-walled dinoflagellate cysts have been recovered from the Matulla Formation (Coniacian - Santonian), Gulf of Suez, Egypt. Among the abundant dinoflagellate cyst assemblages, the new species Odontochitina elbeialyi sp. nov. and Odontochitina ornata sp. nov. (Family Ceratiaceae) are described. The two new species are unique by having a granulate periphragm and three prominent horns. The horns are truncated distally and devoid of striae, ridges and perforations. Odontochitina elbeialyi sp. nov. is characterized by a weakly expressed tabulation on the pericyst indicated by the occasional presence of sutural lines or low ridges indicating the cingulum (two transverse ridges), at plate boundaries. Odontochitina ornata sp. nov. differs from the former, particularly by its clear tabulation, which is corniform gonyaulacoid and more strongly expressed by sutural ridges, and by rare short (rudimentary) sutural (mostly gonal) nipple-like, to truncated processes. Based on the current material, Odontochitina elbeialyi sp. nov. and Odontochitina ornata sp. nov. have short stratigraphic ranges and may therefore be considered as stratigraphic markers for the late Santonian (Late Cretaceous). Their comparison with all formally published species of the genus Odontochitina is presented and discussed, and the associated relevant dinoflagellate cyst taxa are also indicated. The paleoenvironmental significance of the Odontochitina elbeialyi sp. nov. and Odontochitina ornata sp. nov. is discussed.	[Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Slimani, Hamid] Univ Mohammed V Rabat, Sci Inst, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Geobiodivers & Nat Patrimony Lab GEOBIO, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Said, Somia] Gen Petr Co, Explorat Dept, Nasr City 11759, Egypt	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	Slimani, Hamid/AAL-4055-2020					Alberti G., 1961, Palaeontographica, V116, P1; Barreda V.D., 1999, Revista Espanola de Micropaleontologia, V31, P53; BINT A N, 1986, Palynology, V10, P135; Boukhamsin H, 2022, CRETACEOUS RES, V129, DOI 10.1016/j.cretres.2021.104995; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; COOKSON ISABEL C., 1956, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V7, P183; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; Deflandre G., 1935, Bulletin Biologique de la France et de la Belgique, V69, P213; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; El Atfy H, 2023, J AFR EARTH SCI, V205, DOI 10.1016/j.jafrearsci.2023.105006; El Atfy H, 2017, PALZ, V91, P273, DOI 10.1007/s12542-017-0338-8; El-Mehdawi AD, 1998, J MICROPALAEONTOL, V17, P173, DOI 10.1144/jm.17.2.173; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Harris AJ, 2003, MAR MICROPALEONTOL, V48, P127, DOI 10.1016/S0377-8398(03)00002-1; He C., 1991, LATE CRETACEOUS EARL, P1; Herngreen GF., 1996, Palynology: Principles and Applications, V3, P1157; LISTER J K, 1988, Palaeontographica Abteilung B Palaeophytologie, V210, P9; MacRae RA, 1996, CAN J BOT, V74, P1687, DOI 10.1139/b96-205; Mahmoud MS, 2007, RIV ITAL PALEONTOL S, V113, P203, DOI 10.13130/2039-4942/5871; Mahmoudi Magdy S., 2007, Revue de Paleobiologie, V26, P593; Marshall N.G., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P195; McCarthy FMG, 1998, PALAEOGEOGR PALAEOCL, V138, P187, DOI 10.1016/S0031-0182(97)00135-1; MORGAN R., 1980, GEOLOGICAL SURVEY NE, V18, P1; Niechwedowicz M, 2022, NEWSL STRATIGR, V55, P21, DOI 10.1127/nos/2021/0639; Niechwedowicz M, 2019, PALYNOLOGY, V43, P423, DOI 10.1080/01916122.2018.1458754; Núñez-Betelu K, 1998, CAN J EARTH SCI, V35, P923, DOI 10.1139/e98-044; Pearce MA, 2003, MAR MICROPALEONTOL, V47, P271, DOI 10.1016/S0377-8398(02)00132-9; Pearce MA, 2010, J MICROPALAEONTOL, V29, P51, DOI 10.1144/jm.29.1.51; Peyrot D, 2011, CRETACEOUS RES, V32, P504, DOI 10.1016/j.cretres.2011.03.006; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Said R., 1990, GEOLOGY EGYPT, P439; Said S.G., 2022, Delta J. 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MAR	2024	187								102338	10.1016/j.marmicro.2024.102338	http://dx.doi.org/10.1016/j.marmicro.2024.102338		JAN 2024	13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	JC3H7					2025-03-11	WOS:001170912900001
J	Mertens, KN; Meyvisch, P; Gurdebeke, P; Pospelova, V; Matsuoka, K; Bilien, G; Gu, HF; Yamaguchi, A				Mertens, Kenneth Neil; Meyvisch, Pjotr; Gurdebeke, Pieter; Pospelova, Vera; Matsuoka, Kazumi; Bilien, Gwenael; Gu, Haifeng; Yamaguchi, Aika			New investigation of the cyst-motile relationship for <i>Votadinium spinosum</i> reveals a <i>Protoperidinium claudicans</i> species complex (Dinophyceae, Peridiniales)	PALYNOLOGY			English	Article						cysts; cordate; dinoflagellate; spinose; heterotrophic; Protoperidinium carriae; LSU rDNA; molecular phylogenetics; species complex	DINOFLAGELLATE CYSTS; SP-NOV; MOLECULAR PHYLOGENY; BRITISH-COLUMBIA; PRODUCTIVITY; SEDIMENTS; WATERS; GENUS	Protoperidinium claudicans is a planktonic, heterotrophic, bioluminescent dinoflagellate species commonly found in neritic waters. It has long been considered to display phenotypic variation in its second anterior intercalary plate, which could vary between quadra, penta and hexa. The equivalent spinose, cordate cyst goes under the name of Votadinium spinosum. Here we perform incubation experiments with cysts from France, Canada, China and Japan, which demonstrate that P. claudicans forms a species complex, with at least two ribotypes with a penta configuration (P. claudicans) and one with a quadra configuration (P. carriae sp. nov.). A fossil-based cyst, V. multispinosum sp. nov., is described as the equivalent of P. carriae. Molecular phylogenetics using large subunit ribosomal DNA supports these observations. The cyst-theca relationships for Votadinium psilodora and another, undescribed, cordate, spineless Votadinium species are also reported from China. Macromolecular analyses of the cyst wall of V. multispinosum reveal it is comprised of a protein-rich carbohydrate compound. We show that this compound is not uncommon in dinoflagellate and ciliate cysts and that it is unlikely to preserve very well upon sedimentation and burial.	[Mertens, Kenneth Neil; Bilien, Gwenael] Ifremer, LITTORAL, Concarneau, France; [Meyvisch, Pjotr; Gurdebeke, Pieter] Univ Ghent, Dept Geol, Ghent, Belgium; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN USA; [Matsuoka, Kazumi] Inst East China Sea Res, Nagasaki, Japan; [Gu, Haifeng] Minist Nat Resources, Dept Marine Biol & Ecol, Inst Oceanog 3, Xiamen, Peoples R China; [Yamaguchi, Aika] Hokkaido Univ, Fac Sci, Sapporo, Japan	Ifremer; Ghent University; University of Minnesota System; University of Minnesota Twin Cities; Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; Hokkaido University	Mertens, KN (通讯作者)，Ifremer, LITTORAL, Concarneau, France.	kenneth.mertens@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Meyvisch, Pjotr/ABB-1527-2021; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483	French National Research Agency (ANR) PhenoMap project [ANR-20-CE02-0025]; Grants-in-Aid for Scientific Research [20KK0141, 20K04089, 22KJ0037] Funding Source: KAKEN; Agence Nationale de la Recherche (ANR) [ANR-20-CE02-0025] Funding Source: Agence Nationale de la Recherche (ANR)	French National Research Agency (ANR) PhenoMap project(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco); 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)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	KNM and GB were financially supported by the French National Research Agency (ANR) PhenoMap project, ANR-20-CE02-0025.	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J	Carvajal-Landinez, FM; Helenes, J; Murcia, LAG				Carvajal-Landinez, Francy Milena; Helenes, Javier; Murcia, Luis-Andres Guerrero			Quantitative biostratigraphy and paleoecology of Neogene tropical dinoflagellate cysts	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dinoflagellate cyst bioevents; Ranking and scaling; Gulf of Mexico; Miocene; Pliocene	GULF-OF-MEXICO; CENTRAL-AMERICAN SEAWAY; MIDDLE MIOCENE; STRATIGRAPHY; EVOLUTION; CALIBRATION; OLIGOCENE; SEDIMENTS; RANKING; CLIMATE	Understanding the biostratigraphy of tropical areas during the Neogene period can be improved by studying dinoflagellate cyst events. These events have traditionally been identified through qualitative analysis. Nevertheless, to obtain consistent data on this subject, we used quantitative and probabilistic analysis of palynological data from the Southern Gulf of Mexico to identify dinoflagellate cyst events in the Neogene era. We analyzed a database of six wells, including 1,005 core and cuttings samples, a change from past qualitative analysis methods. With this quantitative approach with the RASC program, we obtained the Ranking Optimum Sequence (ROS) and compared it with ten published databases from Neogene tropical sites. The ROS identified eleven dinoflagellate species as age markers, we propose a most likely sequence of dinoflagellate cysts bioevents and define three assemblages: "Cantharellus"(Oligocene to early Miocene), "Hyalina"(Miocene), and "Patulum"(middle Miocene to Pleistocene), that can help recognize most Neogene stratigraphic stages in tropical areas. The comparison with the previous databases shows that the Gulf of Mexico and the tropical sites share 60% of the species, which enables age calibration of the optimal sequence and allows us to infer a possible provincial affinity. Additionally, we found a predominance of autotrophic dinocysts during the Neogene in tropical oceans. This trend mirrors the current abundance of gonyaulacoid cysts in tropical and subtropical areas, which has persisted since the Jurassic era.	[Carvajal-Landinez, Francy Milena; Helenes, Javier; Murcia, Luis-Andres Guerrero] Ctr Invest Cient & Educ Super Ensenada CICESE, Geol Dept, Ensenada, Mexico; [Carvajal-Landinez, Francy Milena] Ctr Invest Cient & Educ Super Ensenada CICESE, Geol Dept, Carretera Ensenada Tijuana 3918 Zona Playitas, Ensenada 22860, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Carvajal-Landinez, FM (通讯作者)，Ctr Invest Cient & Educ Super Ensenada CICESE, Geol Dept, Carretera Ensenada Tijuana 3918 Zona Playitas, Ensenada 22860, Baja California, Mexico.	fcarvajal@cicese.edu.mx		GUERRERO, LUIS/0000-0003-1751-0341	CONAHCYT - CICESE [992867]	CONAHCYT - CICESE	Thanks to CONAHCYT-CICESE for financial support to the first author throughout this study with the Ph.D. scholarship 992867.	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FEB	2024	134								104776	10.1016/j.jsames.2023.104776	http://dx.doi.org/10.1016/j.jsames.2023.104776		JAN 2024	14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	IC7T4					2025-03-11	WOS:001164198000001
J	Head, MJ; Mertens, KN; Fensome, RA				Head, Martin J.; Mertens, Kenneth N.; Fensome, Robert A.			Dual nomenclature in organic-walled dinoflagellate cysts II: <i>Spiniferites elongatus</i> and <i>S. membranaceus</i>, and their equivalent non-fossil species <i>Gonyaulax ovum</i> comb. nov. and <i>G. lewisiae</i> sp. nov.	PALYNOLOGY			English	Article						Dinocyst; taxonomy; dual nomenclature; Gonyaulax ovum; Gonyaulax lewisiae; Spiniferites elongatus; Spiniferites membranaceus	MANTELL 1850; CLASSIFICATION; DINOPHYCEAE; PROPOSALS	The cyst-defined extant Spiniferites elongatus Reid 1974 and Spiniferites membranaceus (Rossignol 1964) Sarjeant 1970 are environmentally significant fossil-species of the Quaternary, the former often dominating polar and subpolar assemblages. Following cyst incubation experiments and the establishment of cultures, these species were emended to incorporate information on their motile stages, and transferred to the non-fossil genus Gonyaulax Diesing 1866, as Gonyaulax elongata (Reid 1974) Ellegaard et al. 2003 and Gonyaulax membranacea (Rossignol 1964) Ellegaard et al. 2003. This unified approach to dinoflagellate nomenclature severs an important link with the fossil-genus Spiniferites Mantell 1850. We have applied dual nomenclature, as sanctioned by the International Code of Nomenclature for algae, fungi and plants, in returning these species to their previous assignments as Spiniferites elongatus and Spiniferites membranaceus, and we propose Gonyaulax ovum (Gaarder 1954) comb. nov., emend. and Gonyaulax lewisiae sp. nov., respectively, as their equivalent non-fossil species. A distinctive morphotype initially described as Rottnestia amphicavata var. amphicavata Dobell & Norris in Harland et al. 1980 is proposed as Spiniferites elongatus forma amphicavata stat. nov.	[Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON, Canada; [Mertens, Kenneth N.] Ifremer, LITTORAL, Concarneau, France; [Fensome, Robert A.] Geol Survey Canada Atlantic, Bedford Inst Oceanog, Nat Resources Canada, Dartmouth, NS, Canada; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University; Ifremer; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Brock University	Head, MJ (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	mjhead@brocku.ca	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Mertens, Kenneth/0000-0003-2005-9483	Natural Sciences and Engineering Research Council of Canada Discovery Grant; French National Research Agency (ANR) PhenoMap project [ANR-20-CE02-0025]; Natural Resources Canada (Geological Survey of Canada); Agence Nationale de la Recherche (ANR) [ANR-20-CE02-0025] Funding Source: Agence Nationale de la Recherche (ANR)	Natural Sciences and Engineering Research Council of Canada Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); French National Research Agency (ANR) PhenoMap project(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco); Natural Resources Canada (Geological Survey of Canada)(Natural Resources Canada); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	We are most grateful to N. Van Nieuwenhove for providing photos of Spiniferites elongatus (Plate 1, figs. 1-4), and to M. Bringue as NRCan internal reviewer and three journal reviewers for their constructive comments. MJH acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. KNM was financially supported by the French National Research Agency (ANR) PhenoMap project, ANR-20-CE02-0025. RAF acknowledges the support of Natural Resources Canada (Geological Survey of Canada); this is NRCan contribution number 2023098. We dedicate this article to the memory of Professor Geoffrey Norris (1937-2023), a highly respected palynologist and outstanding mentor.	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J	Rodríguez-Barreiro, I; Santos, AA; Villanueva-Amadoz, U; Gasulla, JM; Escaso, F; Ortega, F; Gee, CT; Diez, JB				Rodriguez-Barreiro, Ivan; Santos, Artai A.; Villanueva-Amadoz, Uxue; Gasulla, Jose Miguel; Escaso, Fernando; Ortega, Francisco; Gee, Carole T.; Diez, Jose B.			Palynological reconstruction of the habitat and diet of<i> Iguanodon</i><i> bernissartensis</i> in the Lower Cretaceous Morella Formation, NE Iberian Peninsula	CRETACEOUS RESEARCH			English	Article						Cretaceous paleobotany; Herbivorous dinosaur diet; Iguanodontian diet; Iguanodontian habitat reconstruction; Palau-3 site; Upper Barremianpalynoflora	STRONTIUM-ISOTOPE STRATIGRAPHY; FORMATION WEALDEN GROUP; BASIN; PALEOECOLOGY; WESTERN; POLLEN; RECORDS; DINOSAURS; SAUERLAND; EVOLUTION	The recent discovery of iguanodontid remains from the new Palau -3 site in the Lower Cretaceous Morella Formation is the most complete non-articulated skeleton of Iguanodon bernissartensis on the NE Iberian Peninsula. To elucidate the paleoenvironment of the Palau -3 site, a palynological analysis was carried out on matrix samples collected from around the skeleton. The palynological assemblage is found to correspond to an upper Barremian age. While the assemblage is composed of bryophytes, pteridophytes, gymnosperms, freshwater algae, dinoflagellate cysts and fungal spores, the palynoflora is mostly dominated by the Cheirolepidiaceae conifer (Classopollis) and Anemiaceae fern (mainly Cicatricosisporites) families. The absence of angiosperm pollen in this flora is also noteworthy, as angiosperm remains have been recorded previously elsewhere in the Morella Formation. At the Palau -3 site, the fronds of Cyatheaceae and Anemiaceae ferns, as well as the foliage of the Cheirolepidiaceae conifers, may have been the major sources of nutrition of I. bernissartensis and other herbivorous iguanodontians. The paleobotany of the four major localities bearing I. bernissartensis remains in western Europe was surveyed to determine the habitat and feeding preferences of this styracosternan dinosaur. These localities are Bernissart (Belgium), Isle of Wight (England), Nehden (Germany), and Morella (Spain). In accordance to this survey, the habitat preferences of I. bernissartensis and association with specific plant communities show that this ornithopod species was adapted to a wide variety of paleoenvironments. (c) 2023 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).	[Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo, Ctr Invest Marina, BASAN, Vigo 36310, Spain; [Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo, Dept Xeociencias Marinas Ordenac Terr, Vigo 36310, Spain; [Santos, Artai A.] Swedish Museum Nat Hist, Dept Palaeobiol, SE-10405 Stockholm, Sweden; [Santos, Artai A.; Villanueva-Amadoz, Uxue] UNAM, Inst Geol, Estn Reg Noroeste ERNO, Hermosillo 83000, Mexico; [Gasulla, Jose Miguel; Escaso, Fernando; Ortega, Francisco] Univ Nacl Educ Distancia UNED, Fac Ciencias, Grp Biol Evolut, Avda Esparta S-N, Las Rozas De Madrid 28232, Spain; [Gee, Carole T.] Univ Bonn, Inst Geowissensch, Abt Palaontol, D-53115 Bonn, Germany	Universidade de Vigo; CIM UVIGO; Universidade de Vigo; Swedish Museum of Natural History; Universidad Nacional Autonoma de Mexico; Universidad Nacional de Educacion a Distancia (UNED); University of Bonn	Rodríguez-Barreiro, I (通讯作者)，Univ Vigo, Ctr Invest Marina, BASAN, Vigo 36310, Spain.; Rodríguez-Barreiro, I (通讯作者)，Univ Vigo, Dept Xeociencias Marinas Ordenac Terr, Vigo 36310, Spain.	ivan.rodriguez.barreiro@uvigo.gal	Villanueva-Amadoz, Uxue/G-9899-2015; Ortega, Francisco/K-3255-2015; Santos, Artai/AAM-4202-2021; Escaso, Fernando/H-9782-2015	Escaso, Fernando/0000-0001-7642-1555; Rodriguez-Barreiro, Ivan/0000-0002-0938-662X; Santos Lopez, Artai Anton/0000-0002-2399-8825; Villanueva Amadoz, Uxue/0000-0002-5189-5911	Xunta de Galicia (Spain) [UNAM-DGAPA 2023-2024]; European Social Fund-European Union [ED481A-2020/175]; UNAM (Mexico); Swedish Research Council [ED431C-2019/28]; Universidade de Vigo/CISUG;  [VR 2022-03920]	Xunta de Galicia (Spain)(Xunta de Galicia); European Social Fund-European Union; UNAM (Mexico)(Universidad Nacional Autonoma de Mexico); Swedish Research Council(Swedish Research Council); Universidade de Vigo/CISUG; 	The authors would like to thank the Editor-in-Chief of Cretaceous Research, Eduardo Koutsoukos, and an anonymous reviewer for their constructive suggestions which improved the quality of this paper. We also would like to thank the Vega del Moll S.A.com pany for their participation, cooperation, and financing of the fieldwork at the Palau-3 site, as well as the Morella City Council for their collaboration. Funding for this research was provided by the Xunta de Galicia (Spain), through project ED431C-2019/28). IRB is supported by a predoctoral fellowship from the Xunta de Galicia (Spain) and the European Social Fund-European Union (ref.: ED481A-2020/175). AAS is supported by a postdoctoral fellowship from the UNAM (Mexico, ref.: UNAM-DGAPA 2023-2024) and a subsequent fellowship funded by the Swedish Research Council Grant VR 2022-03920 managed by Dr. Stephen Mcloughlin. Funding for open access charge: Universidade de Vigo/CISUG.	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Res.	APR	2024	156								105804	10.1016/j.cretres.2023.105804	http://dx.doi.org/10.1016/j.cretres.2023.105804		JAN 2024	16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	GS1H8		hybrid			2025-03-11	WOS:001154566400001
J	Piasecki, S				Piasecki, Stefan			The<i> Scriniodinium</i><i> crystallinum</i> dinoflagellate cyst zone in the Middle-Upper Oxfordian, Upper Jurassic, Ilimananngip Nunaa (Milne Land), East Greenland	GEUS BULLETIN			English	Article						stratigraphy; Upper Jurassic; Oxfordian-Kimmeridgian; East Greenland	SUCCESSION	The biostratigraphy of the Jurassic in East Greenland is historically based on macroscopic fossils. Stratigraphy based on palynomorphs (spores, pollen and dinoflagellate cysts) has progressed more slowly and sporadically. The Scriniodinium crystallinum dinoflagellate cyst Zone is identified in middle - upper Oxfordian strata of Ilimananngip Nunaa (Milne Land), central East Greenland. The lower boundary is defined by the last occurrence of Trichodinium scarburghense in the Cardioceras tenuiserratum ammonite Zone. The upper boundary is defined by the last occurrence of S. crystallinum in the uppermost Amoeboceras rosenkrantzi ammonite Zone. However, the subzonal division of the S. crystallinum Zone recorded in North-West Europe is not identified in Greenland. Eighteen characteristic dinoflagellate cyst events are considered stratigraphically significant and useful in East Greenland. Fifteen of these events provide an informal, detailed stratigraphical subdivision of the S. crystallinum Zone into 10 subunits. Identification of the zone is an addition to the previously defined upper Bathonian - middle Oxfordian zonation, where the uppermost palynostratigraphical event was recorded to be the last occurrence of T. scarburghense. With this study, the correlation of dinoflagellate cyst and ammonite stratigraphy in the lower and middle Oxfordian is slightly modified. The S. crystallinum Zone documented here, in combination with the zonation used forthe stratigraphy of the Blokelv-1, R & oslash;dryggen-1 and Brorson Halv & oslash;-1 cores of the Upper Jurassic to Lower Cretaceous, completes the dinoflagellate cyst stratigraphy ofthe marine Jurassic in East Greenland. Together with previous studies of spores and pollen in less marine units, the first complete palynological Jurassic stratigraphy is thus established forthe Jurassic succession in East Greenland.	[Piasecki, Stefan] Univ Copenhagen, Globe Inst, Sect Geobiol, Copenhagen, Denmark; [Piasecki, Stefan] Geol Survey Denmark & Greenland GEUS, Dept Geophys & Sedimentary Basins, Copenhagen, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland	Piasecki, S (通讯作者)，Univ Copenhagen, Globe Inst, Sect Geobiol, Copenhagen, Denmark.; Piasecki, S (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Geophys & Sedimentary Basins, Copenhagen, Denmark.	stefan.piasecki@sund.ku.dk			Danish Natu-ral Science Research Foundation [1977-1980]	Danish Natu-ral Science Research Foundation(Danish Natural Science Research Council)	Funding statement The original fieldwork and office studies were financed by Danish Natu-ral Science Research Foundation grants in 1977-1980.	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J	Duxbury, S				Duxbury, Stan			Palynology of the Late Berriasian to Early Hauterivian of the Tethyan Realm in SE France: biostratigraphy and taxonomy of the Vergol (Montbrun-les-Bains) and La Charce (Serre de l'Acirc;ne) sections, Vocontian Basin	MICROPALEONTOLOGY			English	Article						Palynology; taxonomy; biozonation; dinocysts; miospores; Berriasian; Valanginian; Hauterivian; Vocontian Basin; Vergol; La Charce	DINOFLAGELLATE CYSTS; ATLANTIC	Quantitative palynofloral analysis of late Berriasian to early Hauterivian aged sediments from the Vocontian Basin of southeast France has involved fifty-four outcrop samples from Vergol (Montbrun-les-Bains) and twenty-seven from La Charce (Serre de l'Acirc;ne). All samples were marls except for two from the early Valanginian Barrande layers, thin black layers rich in organic carbon. Sampling was focused particularly on the Berriasian/Valanginian, early/late Valanginian and Valanginian/Hauterivian boundaries with two of these particularly important as La Charce is the GSSP for base Hauterivian and Vergol is a GSSP candidate for base Valanginian. Although little has been previously published on the palynology of the Vocontian Basin, this study has benefitted from many previous multi-disciplinary studies in the area; the numerous palynofloral events recorded are tied closely to the standard ammonite zonation. Analyses were mainly focused on the dinocysts, but miospores have also been considered in terms of their palaeoenvironmental response, allowing broad assessment of relative sea level changes. Some linkage between peaks in coastal/lowland ratios, the delta 13C curve through the Weissert carbon isotope excursion (CIE) and the Muderongia group (possible reduced salinity) have been shown. A new dinocyst zonation scheme is proposed, involving twelve zones, eight of which cover the Valanginian; previous schemes are briefly discussed. Two genera, twenty-three species and five subspecies of stratigraphically-significant dinoflagellate cysts are described as new, two genera have been emended and thirteen new combinations have been proposed. The diagnosis of one acritarch genus has been emended and two new combinations effected.	[Duxbury, Stan] Church Lane, Chester CH2 1DJ, England		Duxbury, S (通讯作者)，Church Lane, Chester CH2 1DJ, England.	duxburydsc@aol.com						Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; Agelopoulos J., 1964, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V11, P673; Alberti G., 1961, Palaeontographica, V116, P1; ALBERTI G., 1959, Zur Kenntnis der Gattung Deflandrea Eisenack (Dinoflag.) in der Kreide und im Alttertiar Nordund Mitteldeutschlands; [Anonymous], 1998, LPP Contributions Series; [Anonymous], 1980, Bulletin de la Societe Geologique de France (serie 7); [Anonymous], Neues Jahrbuch fur Geologie und Palaontologie, Monatshefte, V3, P137; ANTONESCU E., 1980, ANNUAIRE I GEOLOGIE, V56, P4; ARHUS N, 1992, GRANA, V31, P305, DOI 10.1080/00173139209429453; Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; Bailey D., 1987, Journal of Micropalaeontology, V6, P89; Bailey D.A., 1991, Journal of Micropalaeontology, V9, P245; Batten D.J., 1979, INIT REPS DSDP, V48, P579; BEJU D., 1971, Annales Instituti Geologici Publici Hungarici, V54, P275; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BELOW R, 1982, Revista Espanola de Micropaleontologia, V14, P23; BENEDEK P N, 1981, Palaeontographica Abteilung B Palaeophytologie, V180, P39; Benson D.G. 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C., 1958, Proceedings of the Royal Society of Victoria N S, V70, P19; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; COTILLON P, 1984, INITIAL REP DEEP SEA, V77, P339; Courtinat B, 1998, MICROPALEONTOLOGY, V44, P435, DOI 10.2307/1486043; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; Palliani RB, 1997, REV PALAEOBOT PALYNO, V96, P99, DOI 10.1016/S0034-6667(96)00019-X	51	1	1	0	0	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2024	70	6					543	677		10.47894/mpal.70.6.01	http://dx.doi.org/10.47894/mpal.70.6.01			135	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	P6N5T					2025-03-11	WOS:001379054200001
J	Mahmoud, MS; Deaf, AS; El Hussieny, MAT				Mahmoud, Magdy s.; Deaf, Amr s.; El Hussieny, Mennat-Allah T.			Neogene-Quaternary paleoenvironments and kerogen assessment of the NDO B-1 well, offshore Nile Delta, Egypt, Eastern Mediterranean: palynological evidence	ACTA GEOLOGICA POLONICA			English	Article						Palynofacies; Palynomorphs; Kerogen; Offshore Egypt.	WALLED DINOFLAGELLATE CYSTS; ORGANIC-MATTER; BASIN; PALYNOFACIES; STRATIGRAPHY; PRESERVATION; MIOCENE; SUBSURFACE; EVOLUTION; CALABRIA	Palynofacies and palynological investigations conducted on the Neogene-Quaternary succession from the NDO B-1 well, located in the offshore Nile Delta, Egypt, in the Eastern Mediterranean, suggest generally shallow marine (neritic) conditions. These environments are manifested by the overall palynofacies composition and the occurrence of dinoflagellate cysts (e.g., Spiniferites spp., Lingulodinium spp., Hystrichokolpoma spp., Homotryblium spp. and Selenopemphix spp.). Neritic environments are suggested for the lower and middle Miocene Sidi Salim, and the Pliocene to Pleistocene upper Kafr El Sheikh, El Wastani and Mit Ghamr formations, while shallower, coastal to inner neritic settings were interpreted for the late Miocene (Qawasim and Rosetta formations) and early Pliocene (Abu Madi and lower Kafr El Sheikh formations). Anoxic conditions existed during the deposition of the studied well succession, which can be seen from the occurrence of imprints of pyrite crystals and some types of oxygen-sensitive dinoflagellate cysts. The palynofacies fluctuated repeatedly between Amorphous Organic Matter (AOM)-dominated and phytoclast-dominated intervals, of kerogen types II and III, respectively. The spore coloration index (SCI) of indigenous thin-walled palynomorphs confirms thermally mature sediments, generative of dry gas and wet gas/condensates. Reworking during the deposition of the upper Sidi Salim, Qawasim and Rosetta formations is inferred from the occurrence of Cretaceous dinoflagellate cysts and pollen.	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Pol.		2024	74	3							e21	10.24425/agp.2024.151751	http://dx.doi.org/10.24425/agp.2024.151751			21	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	P1D8T		gold			2025-03-11	WOS:001375413300004
C	Ben Moktar, N; Mannaï-Tayech, B		Lucci, F; Doronzo, DM; Knight, J; Trave, A; Grab, S; Kallel, A; Panda, S; Chamine, HI; Rodrigo-Comino, S; Khomsi, S; Banerjee, S; Merkel, B; Chenchouni, H		Ben Moktar, Nadia; Mannai-Tayech, Beya			Lithofacies and Palynofacies of the Miocene Deposits in the Paralic Basin of Tunisia (Basin of the Cap Bon and Basin of Saouaf): Reconstruction of Palaeoenvironments	SELECTED STUDIES IN GEOMORPHOLOGY, SEDIMENTOLOGY, AND GEOCHEMISTRY, CAJG-3 2020	Advances in Science Technology and Innovation		English	Proceedings Paper	3rd Conference of the Arabian-Journal-of-Geosciences (CAJG)	NOV 02-05, 2020	ELECTR NETWORK	Arabian Journal Geosciences		Lithofacies; Palynofacies; Palaeoenvironment; Miocene; Tunisia	SERIES	The Miocene micro-basins of north-east Tunisia are filled with molasse and fluvio-deltaic siliciclastic deposits, including organic matter-rich phytogenic deposits. A multidisciplinary study including sedimentological, palynofacies and palynological analyses was carried out in the Cap Bon and Saouaf basins. The study of palynofacies variation in correspondence with different facies associations allows us to evaluate the paleoenvironment of deposition. Our data set indicates an offshore-type environment during the Lower Burdigalian-Langhian. In the middle and upper Langhian, a shoreface environment evolved into a dominantly marine environment. The Langhian is known to be a phase of transgression in the Mediterranean. For palynofacies, sea level rise results in exceptional abundance of dinoflagellate cysts (Impagidinium, Cordosphaeridium inodes minimus, Cleistosphareridium, Spiniferites and others) and chitinous tests of foraminifera as well as dominance of amorphous organic matter. The base of the Serravallian is defined by a gradual change from a shallow submarine channel environment towards a coastal and, eventually, a deltaic plain. This change is followed by a regressive sequence that led to a decrease in amorphous organic matter in favour of non-oxidized and oxidized organic matter. Subsequently, a new transgression led to changes from lagoonal to a foreshore environment. These marine incursions are attested by an increase in amorphic organic matter, dinocysts and by the presence of foraminifera with chitinous tests. Finally, a deltaic deposit with a confined lagoon corresponds to the last regressive sequence. The environment is paralic in character (with twelve levels of lignite) and dominated by non-oxidized and oxidized organic matter. This is the last transgressive/regressive cycle of the Serravallian-Tortonian.	[Ben Moktar, Nadia] Univ Gabes, Gabes 6072, Tunisia; [Mannai-Tayech, Beya] Univ Tunis El Manar, Tunis 2092, Tunisia	Universite de Gabes; Universite de Tunis-El-Manar	Ben Moktar, N (通讯作者)，Univ Gabes, Gabes 6072, Tunisia.	nadiabenrhit34@gmail.com						Abbes C., 1983, Thesis, Fac. Sc., P121; Bedir M., 1995, Ph.D. Thesis, P416; Ben Moktar N, 2014, ARAB J GEOSCI, V7, P385, DOI 10.1007/s12517-012-0808-y; Ben Moktar N, 2012, GEODIVERSITAS, V34, P445, DOI 10.5252/g2012n2a11; Ben Salem H., 1992, Contribution to the knowledge of the geology of Cap Bon: Stratigraphy, tectonics and sedimentology; BISMUTH H, 1994, B CENT RECH EXPL, V18, P489; Bismuth H., 1984, Social Science, P2; Blondel T., 1991, Thesis, P487; Boujamaoui M., 2000, Univ. Tunis II; Burollet P.F., 1956, Ann. Min. Geol. (Tun), P350; Castany G., 1951, Ph.D Thesis, P151; Devolvet J.J., 1974, Thesis, P154; Jauzein A., 1959, Notes from the Geological Survey, V18; Mannaï-Tayech B, 2006, GEOBIOS-LYON, V39, P71, DOI 10.1016/j.geobios.2004.08.003; Mannai-Tayech B., 2004, EARTH WAT P, P4; Meddeb N., 1984, report, P47; Saadi M., 1997, THESIS U TUNIS MANAR, P348; Salaj J., 1970, NOTES SERVICE GEOLOG, V3, P79; Solignac M., 1927, Etude geologique de la Tunisie septentrionale, P1; Tayech B., 1984, THESIS U C BERNARD L, P121; Turki M.M., 1985, These Doct, V7, P252; Yaich C., 1997, THESIS U TUNIS MANAR, P479	22	0	0	0	0	SPRINGER INTERNATIONAL PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2522-8714	2522-8722	978-3-031-43746-5; 978-3-031-43744-1; 978-3-031-43743-4	ADV SCI TECHNOL INN	Adv. Sci. Technol. Innov.		2024							139	142		10.1007/978-3-031-43744-1_28	http://dx.doi.org/10.1007/978-3-031-43744-1_28			4	Geochemistry & Geophysics; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geochemistry & Geophysics; Geology	BX5MQ					2025-03-11	WOS:001300500000028
C	Domenico, G; Kurita, H		Lucci, F; Doronzo, DM; Knight, J; Trave, A; Grab, S; Kallel, A; Panda, S; Chamine, HI; Rodrigo-Comino, S; Khomsi, S; Banerjee, S; Merkel, B; Chenchouni, H		Domenico, Gilamichael; Kurita, Hiroshi			The Role of Eustasy and Local Tectonics in Jurassic Carbonate Sedimentation in the Blue Nile and Northwest Ogaden Basins of Ethiopia	SELECTED STUDIES IN GEOMORPHOLOGY, SEDIMENTOLOGY, AND GEOCHEMISTRY, CAJG-3 2020	Advances in Science Technology and Innovation		English	Proceedings Paper	3rd Conference of the Arabian-Journal-of-Geosciences (CAJG)	NOV 02-05, 2020	ELECTR NETWORK	Arabian Journal Geosciences		Jurassic; Carbonates; Ethiopia; Local tectonics; Eustasy		Microscopic, paleontologic and field studies were undertaken on the Middle to Upper Jurassic Antalo Limestone exposed in the Blue Nile and the northwest Ogaden basins of Ethiopia to determine the age, depositional environment and discuss their evolution. The study also explained the timing and formation of Mesozoic carbonate platforms in Ethiopia in detail for the first time. For the Blue Nile Basin, this work used a new age scheme by recent studies on Callovian-Oxfordian dinoflagellate cyst records, benthic foraminifers and green algae from the Antalo Limestone Formation. These allowed us to date the entire carbonate succession in the basin as Callovian to Early Kimmeridgian. A detailed facies analysis of the Antalo Limestone (ca. 550 m thick) in both basins reveals nearshore tidal flat (inner ramp), shelf (subtidal), open marine and barrier (shoal) facies associations. The second-order depositional sequence identified from the Blue Nile is characterized by more open marine facies and marked by a maximum flooding zone (MFZ) of Oxfordian age. In northwest Ogaden, the MFZ is represented by cherty and ammonoid-bearing spicular mudstones of Early Kimmeridgian age. Both local tectonics and eustasy are responsible for the evolution of the sediments. Differential subsidence formed a sub-basin in the Blue Nile area, whereas the northwest Ogaden could represent a paleohigh. Marine flooding could be at the peak stage during Late Oxfordian to Early Kimmeridgian, and this can be attributed to eustatic conditions during the opening of the Indian Ocean.	[Domenico, Gilamichael] East Los Angeles Coll, 1301 Ave Cesar Chavez, Monterey Pk, CA 91754 USA; [Kurita, Hiroshi] Niigata Univ, Fac Sci, Niigata 9502181, Japan	Niigata University	Domenico, G (通讯作者)，East Los Angeles Coll, 1301 Ave Cesar Chavez, Monterey Pk, CA 91754 USA.	domenigk@elac.edu	Kurita, Hiroshi/KIC-0968-2024	Kidanemariam Domenico, Gilamichael/0000-0001-6850-9282				Al-Thour KA, 1997, MAR PETROL GEOL, V14, P643, DOI 10.1016/S0264-8172(97)00030-5; Bosellini A., 1989, Memorie di Science Geologiche, Universita di Padova, V41, P373; Domenico G., 2010, Ph.D. thesis; Domenico G., 2006, 113 ANN M GEOL SOC J, P80; Dunham R.J., 1962, Classification of Carbonate Rocks; Fl?gel E, 2010, MICROFACIES CARBONAT; Hallam A, 2001, PALAEOGEOGR PALAEOCL, V167, P23, DOI 10.1016/S0031-0182(00)00229-7; Kurita H., 2009, 2009 ANN M PAL SOC J; Russo A., 1994, Neues Jahrbuch Fur Geologie Und Palaontologie-Monatshefte, P291, DOI [10.1127/njgpm/1994/1994/291, DOI 10.1127/NJGPM/1994/1994/291]; Van Wagoner J.C., 1988, SEPM, P39, DOI DOI 10.2110/PEC.88.01.0039; Ziegler M.A., 2001, GEOARABIA, V6, P445, DOI DOI 10.2113/GEOARABIA0603445	11	0	0	0	0	SPRINGER INTERNATIONAL PUBLISHING AG	CHAM	GEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND	2522-8714	2522-8722	978-3-031-43746-5; 978-3-031-43744-1; 978-3-031-43743-4	ADV SCI TECHNOL INN	Adv. Sci. Technol. Innov.		2024							147	150		10.1007/978-3-031-43744-1_30	http://dx.doi.org/10.1007/978-3-031-43744-1_30			4	Geochemistry & Geophysics; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geochemistry & Geophysics; Geology	BX5MQ					2025-03-11	WOS:001300500000030
J	Sremac, J; Bosnjak, M; Firi, KF; Simicevic, A; Ascic, S				Sremac, Jasenka; Bosnjak, Marija; Firi, Karmen Fio; Simicevic, Ana; Ascic, Simun			Marine microfossils: Tiny archives of ocean changes through deep time	AIMS MICROBIOLOGY			English	Review						microbiota; fossilization; biostratigraphy; paleoenvironment; raw materials	MIDDLE MIOCENE; CENTRAL PARATETHYS; BENTHIC FORAMINIFERA; ISOTOPIC COMPOSITION; MT. CROATIA; SHALLOW; BASIN; DEPOSITS; SEA; BIOSTRATIGRAPHY	Microorganisms have inhabited the oceans since the dawn of Earth. Some of them have organic walls and some produce mineral tests that are usually composed of carbonate minerals or silica. They can therefore be preserved with original parts during sedimentary deposition or fossilized through permineralization or carbonization processes. The most common marine fossil groups studied by micropaleontologists are cyanobacteria, coccolithophores, dinoflagellates, diatoms, silicoflagellates, radiolarians, foraminifers, red and green algae, ostracods, and pteropods. Dormant or reproductive cysts can also be used for determinations of the fossil microbiota. Microfossils can be studied in petrographic slides prepared from rocks or separated from loosely consolidated rocks by disaggregation or dissolution and wet sieving. Their presence is sometimes recognized by biomarkers. Transmitted light microscopy and reflected light stereomicroscopy are necessary for micropaleontological studies whereas scanning electronic microscopy (SEM) aids research on the tiniest fossils and reveals fine skeletal details. Microorganisms have influenced the oxygenation of water and the atmosphere, as well as Earth's carbon cycle and have contributed to the formation of sedimentary rocks. By studying microfossils, paleontologists depict the age of the rock and identify depositional environments. Such studies help us recognize periods of stress in Earth's history and understand their influence on living organisms. Biogenic rocks, made of microfossils, can be used as raw materials, such as fossil fuels, building stone, or additives for the food industry, agricultural, or cosmetic purposes.	[Sremac, Jasenka; Firi, Karmen Fio; Ascic, Simun] Univ Zagreb, Fac Sci, Dept Geol, Horvatovac 102b, HR-10000 Zagreb, Croatia; [Bosnjak, Marija] Croatian Nat Hist Museum, Demetrova 1, Zagreb 10000, Croatia; [Simicevic, Ana] Franka Lisice 4, Zadar 23000, Croatia	University of Zagreb	Sremac, J (通讯作者)，Univ Zagreb, Fac Sci, Dept Geol, Horvatovac 102b, HR-10000 Zagreb, Croatia.	jsremac@geol.pmf.hr	Sremac, Jasenka/J-9364-2014; Bošnjak, Marija/ABG-2197-2020				Results of our research were partly obtained through the Croatian Science Foundation Project "Sedimentary paleobasins, water corridors and biota migrations" (IP-2019-04-7042) ,-2019-04-7042) , led by Marijan Kovai (University of Zagreb, Faculty of Science) . We are grateful to Kristina Pikelj (University of Zagreb, Faculty of Science) for providing diatom and silicoflagellate remains, and Duje Kuko (Croatian Geological Survey) for radiolarian images. Authors would like to thank the reviewers and editors for their constructive and helpful comments, which have significantly improved the quality of this paper.	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J	Lipsewers, T				Lipsewers, Tobias			Consistent separation of resting stages and vegetative cells of spring bloom dinoflagellates in the Baltic Sea benefits coherent data acquisition	BOREAL ENVIRONMENT RESEARCH			English	Editorial Material									[Lipsewers, Tobias] Gartenstr 73, D-33397 Rietberg, Germany		Lipsewers, T (通讯作者)，Gartenstr 73, D-33397 Rietberg, Germany.	tobias.lipsewers@gmail.com			Academy of Finland [259164, 263862]; Onni Talas Foundation; University of Helsinki; Academy of Finland (AKA) [263862] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Onni Talas Foundation; University of Helsinki; Academy of Finland (AKA)(Research Council of Finland)	The following people and institutions are acknowledged: Dr. Harri Kuosa (Marine and freshwater solutions, Finnish Environment Institute, Helsinki (SYKE) ) for his helpful feedback on the manuscript; Dr. Anke Kremp (Leibniz-Institute for Baltic Sea Research, Warnemunde, Germany) for making me aware of the resting stages of Gymnodinium corollarium ; Johanna Oja (SYKE) for carrying out part of the "Lugol-microscopy", which was essential for the planning of the subsequent epifluorescence microscopy and different analyses; SYKE for the opportunity to work in the C-FluxII-project and to participate in the cruises; and the crew of R/V Aranda for great technical support and fabulous catering. During a large part of the practical work, funding was available from the Academy of Finland (decision numbers 259164 and 263862) for the C-fluxII-project and personal grants were awarded to Tobias Lipsewers by the Onni Talas Foundation and the University of Helsinki. This study utilised SYKE's marine research infrastructure as a part of the national FINMARI consortium.r different analyses; SYKE for the opportunity to work in the C-FluxII-project and to participate in the cruises; and the crew of R/V Aranda for great technical support and fabulous catering. During a large part of the practical work, funding was available from the Academy of Finland (decision num-bers 259164 and 263862) for the C-fluxII-project and per-sonal grants were awarded to Tobias Lipsewers by the Onni Talas Foundation and the University of Helsinki. This study utilised SYKE's marine research infrastructure as a part of the national FINMARI consortium.	Lipsewers T, 2023, BOREAL ENVIRON RES, V28, P195; Lipsewers T, 2018, BOREAL ENVIRON RES, V23, P127; Spilling K, 2019, LIMNOL OCEANOGR, V64, P1779, DOI 10.1002/lno.11150; Sundström AM, 2009, J PHYCOL, V45, P938, DOI 10.1111/j.1529-8817.2009.00712.x; Tamminen T, 2007, MAR ECOL PROG SER, V340, P121, DOI 10.3354/meps340121; Wasmund N, 2017, FRONT MAR SCI, V4, DOI 10.3389/fmars.2017.00022	6	0	0	1	1	FINNISH ENVIRONMENT INST	HELSINKI	P O BOX 140, FIN-00251 HELSINKI, FINLAND	1239-6095	1797-2469		BOREAL ENVIRON RES	Boreal Environ. Res.		2024	29						127	129						3	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	YX4K1					2025-03-11	WOS:001271769300001
J	Mahmoud, M; Temraz, A; Moawad, AR; Khalaf, M				Mahmoud, Magdy; Temraz, Amal; Moawad, Abdel-Rahim; Khalaf, Miran			Application of palynomorphs and palynofacies in Early Cretaceous paleoenvironmental reconstruction; Shushan Basin, Egypt	ACTA GEOLOGICA POLONICA			English	Article						Cretaceous; Paleoenvironment; Palynomorphs; Palynofacies; Egypt	SEDIMENTARY ORGANIC-MATTER; NORTHERN WESTERN-DESERT; SERGIPE BASIN; 3 BOREHOLES; WELL; PALEOECOLOGY; STRATIGRAPHY; PALYNOLOGY; CARBONATES; POLLEN	An integration of palynomorph and palynofacies data from the Shushan-1X well is used to infer the paleoenvironmental conditions of the Valanginian to Middle Cenomanian (Cretaceous) section of the western Shushan Basin, northern Egypt. The data obtained contribute significantly to the depositional history of the basin. The low diversity of dinoflagellate cyst assemblages, along with the dominance of land-derived spores and pollen, suggest restricted (marginal) marine environments, in contrast to their coeval representatives from the Tethyan Realm. Open marine (inner shelf) environments developed at a few horizons in the Dahab and Bahariya formations, partly contemporary with the global Aptian and Cenomanian eustatic cycles. These environments were relatively more offshore than those described in the eastern and southeastern parts of the basin. The study of total palynological organic matter (TPOM) has contributed largely to these established environmental settings. It has also allowed the recognition of redox (suboxic to anoxic) conditions and the impact of a large magnitude of terrigenous influence.	[Mahmoud, Magdy] Assiut Univ, Fac Sci, Geol Dept, Assiut 71516, Egypt; [Temraz, Amal; Moawad, Abdel-Rahim] South Valley Univ, Fac Sci, Geol Dept, Qena 83523, Egypt; [Khalaf, Miran] Sohag Univ, Fac Sci, Geol Dept, Sohag 82524, Egypt	Egyptian Knowledge Bank (EKB); Assiut University; Egyptian Knowledge Bank (EKB); South Valley University Egypt; Egyptian Knowledge Bank (EKB); Sohag University	Khalaf, M (通讯作者)，Sohag Univ, Fac Sci, Geol Dept, Sohag 82524, Egypt.	magdysm@aun.edu.eg; amalatemraz@yahoo.com; abdelrahimmoawad@gmail.com; miran_kha2@yahoo.com	Khalaf, Miran/JWO-5876-2024	Khalaf, Miran/0000-0002-9561-6873			Thanks are due to the Egyptian General Petroleum Corpo-ration (E.G.P.C.) , for providing the material for the present study. We are deeply indebted to Anna yliska (Editor) , Przemysaw Gedl (Polish Academy of Science, Krakow, Poland) and an anonymous reviewer for critical remarks and improvement of the manuscript.	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Pol.		2024	74	2							e13	10.24425/agp.2024.150004	http://dx.doi.org/10.24425/agp.2024.150004			26	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	YB8J7		gold			2025-03-11	WOS:001266114400008
J	Peryt, D; Gedl, P; Jasionowski, M; Peryt, TM; Poberezhskyy, A				Peryt, Danuta; Gedl, Przemyslaw; Jasionowski, Marek; Peryt, Tadeusz Marek; Poberezhskyy, Andriy, V			The Badenian/Sarmatian (Middle Miocene) boundary in the Central Paratethys (Kreminna, western Ukraine): foraminiferal and palynological evidence	GEOLOGICAL QUARTERLY			English	Article						Middle Miocene; Carpathian Foredeep Basin; foraminifers; palynofacies; palaeoenvironments	CARPATHIAN FOREDEEP BASIN; BADENIAN SALINITY CRISIS; ROMANIA PALEOGEOGRAPHIC CHANGES; SARMATIAN EXTINCTION EVENT; DINOFLAGELLATE CYST; OXYGEN INDEX; RECORDS; CLIMATE; MARINE; POLAND	The Badenian/Sarmatian boundary in the Paratethys basin, that marks the transition from normal marine to restricted semi-marine conditions due to isolation of the basin from the world ocean at the onset of Sarmatian time, is still far from being fully under stood. The Kreminna section is located at the northeastern margin of the Carpathian Foreland Basin (Central Paratethys) in the Medobory Hills region. The Miocene deposits that overlie here the Upper Cretaceous substratum comprise the >1 m thick upper Badenian marls and clays passing up wards into similar to 4 m thick Sarmatian marly limestones with intercalations of marls, clays and limestones, and >2 m thick limestones in the uppermost part of the expo sure. Fifty-three species of benthic foraminifera and four species of plank tonic foraminifera have been recorded. Six benthic foraminiferal assemblages are composed almost exclusively of calcareous forms; agglutinated taxa are practically lacking. Elphidium spp., miliolids, Lobatula lobatula and Ammonia spp. are the most common calcareous benthic foraminifera in the material studied. Planktonic foraminifera are represented only by species of Globigerina and occur rarely in the lowermost part of the section. A characteristic feature of palynofacies is the very low proportion of land-derived elements - sporomorphs and cuticles, which suggests a sedimentary setting without terrestrial influx, and taxonomical impoverishment of dinoflagellate cyst assemblages, which are either monospecific or consist mainly of two to three species: in a majority of samples, assemblages with Polysphaeridium zoharyi and P. subtile occur. Most delta O-18 values range from -1.5 to similar to+0.5 parts per thousand VPDB and most delta C-13 values are between 0 and +2 parts per thousand VPDB. In general, the delta C-13 curve mirrors the delta O-18 changes in the section. The Badenian/Sarmatian boundary is placed at the level where the Cibicidoides ungerianus Assemblage is re placed by the Elphidium fichtelianum Assemblage. At the boundary, planktonic foraminifers and most abundant stenohaline benthic foraminifera disappeared. Bottom waters were well-oxygenated both in the latest Badenian and earliest Sarmatian in the Kreminna location.	[Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland; [Jasionowski, Marek; Peryt, Tadeusz Marek] Polish Geol Inst, Natl Re search Inst, Rakowiecka 4, PL-00975 Warsaw, Poland; [Poberezhskyy, Andriy, V] Natl Acad Sci Ukraine, Inst Geol & Geo Chem, Naukova 3a, UA-79060 Lvov, Ukraine	Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Geological Institute - National Research Institute; National Academy of Sciences Ukraine	Peryt, D (通讯作者)，Polish Acad Sci, Inst Paleobiol, Twarda 51-55, PL-00818 Warsaw, Poland.	d.peryt@twarda.pan.pl	Poberezhskyy, Andriy/GZA-4384-2022; Jasionowski, Marek/Z-2956-2019; Peryt, Tadeusz/F-9289-2019	Jasionowski, Marek/0000-0003-3825-7859; Peryt, Tadeusz/0000-0002-8017-1701	National Science Centre, Poland [UMO-2017/27/B/ST 10/01129]; Ministry of Sciences and Higher Education [307 113635]	National Science Centre, Poland(National Science Centre, Poland); Ministry of Sciences and Higher Education	This study was financed by the National Science Centre, Poland, grant No. UMO-2017/27/B/ST 10/01129 to D.P., and the pi lot study was sup ported by the Ministry of Sciences and Higher Education, grant N 307 113635 to M.J. 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Q.		2024	68	1							7	10.7306/gq.1731	http://dx.doi.org/10.7306/gq.1731			23	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QS0T6		gold			2025-03-11	WOS:001222749100008
J	Dvoretsky, AG; Dvoretsky, VG				Dvoretsky, Alexander G.; Dvoretsky, Vladimir G.			Filling knowledge gaps in Arctic marine biodiversity: Environment, plankton, and benthos of Franz Josef Land, Barents Sea	OCEAN & COASTAL MANAGEMENT			English	Review						Barents sea; Oceanography; Climate; Pelagic organisms; Zoobenthos; Diversity	CLIMATE-CHANGE; INTERANNUAL DYNAMICS; COMMUNITY STRUCTURE; ISLAND; OCEAN; BIOMASS; FAUNA; MESOZOOPLANKTON; ZOOPLANKTON; DIVERSITY	Franz Josef Land (FJL) is a remote archipelago that has become more accessible for large-scale studies due to recent warming. This paper summarizes recent survey findings on oceanography, climate, plankton, and benthic communities conducted in FJL. Cold Arctic waters predominantly affect FJL, but an increased inflow of warmer Atlantic water has been observed in recent decades. The bacterioplankton in FJL is mainly comprised of ultra-small bacterial cells, which make up to 60% of the biomass. Phytoplankton are predominantly composed of cells smaller than 20 mu m, with the greatest concentrations found above the pycnocline. The population of larger microalgae ranges from 4.5 to 1250 thousand cells L-1, with dinoflagellates occupying the euphotic zone, Dinobryon being the most abundant species in the thermocline, and spore-bearing cells of Chaetoceros diatoms dominating in the deepest region. Summer zooplankton comprise large Calanus copepods, smaller copepods, and meroplankton, with an average dry biomass of 114-391 mg m(-3). The community structure varies mainly based on water temperature and phytoplankton density, with greater biomasses found in colder offshore waters. August represents the breeding season for plankton populations. The local benthic fauna is diverse and displays high species abundance (3370 ind. m(-2)) and wet biomass (428 g m(-2)). There is a distinct vertical stratification in the benthic community structure, evidenced by a consistent decline in both abundance and biomass with increasing depth. The trophic structure is predominantly influenced by food availability, sediments, and currents. The trend of borealization in the Barents Sea biota is supported by recent distribution records of certain boreal benthic species and increased abundances of typical Atlantic zooplankton species. The results of our study establish a foundational dataset to aid in ongoing scientific inquiry, preservation efforts, and strategic decision-making with regards to the natural resources of the FJL region.	[Dvoretsky, Alexander G.; Dvoretsky, Vladimir G.] RAS, MMBI, Murmansk, Russia	Russian Academy of Sciences	Dvoretsky, AG (通讯作者)，RAS, MMBI, Murmansk, Russia.	dvoretskiya@mmbi.info	Dvoretsky, Alexander/AAP-6435-2021		Ministry of Science and Higher Education of the Russian Federation	Ministry of Science and Higher Education of the Russian Federation	This study was funded by the Ministry of Science and Higher Education of the Russian Federation. We thank three anonymous reviewers for their constructive feedback.	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J	Mathewes, RW; Clague, JJ; Hughes, JF				Mathewes, Rolf W.; Clague, John J.; Hughes, Jonathan F.			Paleoecology of vegetation changes associated with a prehistoric earthquake at Serpentine Fen, southwestern British Columbia, Canada	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palynology; Wetland plant succession; Paleo-earthquake; Estuarine marsh	LATE HOLOCENE EARTHQUAKE; TIDAL MARSH; COSEISMIC SUBSIDENCE; VANCOUVER-ISLAND; VASCULAR PLANTS; WEST-COAST; FORAMINIFERA; CASCADIA; OREGON	A sedimentary exposure near the mouth of Serpentine River, about 25 km southeast of Vancouver, British Columbia, records evidence of a large earthquake that happened about 2000 years ago. The evidence includes sand dykes injected into late Holocene peat and mud. Vegetation changes based on pollen analysis and radiocarbon-dated wood match sedimentary changes at the Serpentine Fen site. A shift from herbaceous to woody peat is matched by a dramatic peak (similar to 45%) in pollen of Myrica shrubs, indicating uplift and a vegetation shift to drier shrubland from fen, also incorporating detrital spruce wood (Picea). At the top of the woody peat, Myrica pollen disappears and intertidal mud with Triglochin-type pollen increases, indicating subsidence and establishment of an intertidal environment. The section above the woody peat shows increasing amounts of halophyte pollen, especially Chenopodiaceae (or Amaranthaceae) which reaches values up to 60%, and scattered dinoflagellate cysts, indicative of a continued tidal influence. The combined evidence of uplift and subsidence over a short interval is rare at most sites in south-coastal British Columbia.	[Mathewes, Rolf W.] Simon Fraser Univ, Dept Biol Sci, 8888 Univ Dr, Burnaby, BC V5A1S6, Canada; [Clague, John J.] Simon Fraser Univ, Dept Earth Sci, 8888 Univ Dr, Burnaby, BC V5A1S6, Canada; [Hughes, Jonathan F.] Univ Fraser Valley, Dept Geosci, 33844 King Rd, Abbotsford, BC V2S 2R9, Canada	Simon Fraser University; Simon Fraser University; University of Fraser Valley	Mathewes, RW (通讯作者)，Simon Fraser Univ, Dept Biol Sci, 8888 Univ Dr, Burnaby, BC V5A1S6, Canada.	mathewes@sfu.ca			Natural Science and Engineering Research Council of Canada [A3835]	Natural Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	<STRONG>We thank S.B. Archibald for assistance with drafting figures. Funding was provided by a Natural Science and Engineering Research Council of Canada grant to R.W.M. (individual Discovery Grant A3835). </STRONG>	Atwater B.F., 1997, GEOL SURV PROF PAPER, V1576, P1; Atwater BF, 2004, DEV QUA SCI, V1, P331; Benson BE, 2001, QUATERNARY RES, V56, P139, DOI 10.1006/qres.2001.2251; Clague J.J., 1998, Geological Survey of Canada Bulletin, V525, P177; Faegri K., 1975, Textbook of pollen analysis.; Grimm E., 2011, TILIA: A Pollen Program for Analysis and Display; GUILBAULT JP, 1995, PALAEOGEOGR PALAEOCL, V118, P49, DOI 10.1016/0031-0182(94)00135-U; Guilbault JP, 1996, QUATERNARY SCI REV, V15, P913, DOI 10.1016/S0277-3791(96)00058-3; HEMPHILLHALEY E, 1995, GEOL SOC AM BULL, V107, P367, DOI 10.1130/0016-7606(1995)107<0367:DEFEIS>2.3.CO;2; Hughes JF, 2003, HOLOCENE, V13, P877, DOI 10.1191/0959683603hl670rp; Hughes JF, 2002, PALAEOGEOGR PALAEOCL, V185, P145, DOI 10.1016/S0031-0182(02)00283-3; Hutchinson I., 1998, GEOL SURV CAN BULL, V525, P161; Kelsey HM, 2012, J GEOPHYS RES-SOL EA, V117, DOI 10.1029/2011JB008816; Klinka K., 1989, INDICATOR PLANTS COA; Krajina V.J. K. Klinka., 1982, Distribution and Ecological Characteristics of Trees and Shrubs of British Columbia; MacKenzie WilliamH., 2004, Wetlands of British Columbia: a guide to identification; MATHEWES RW, 1994, SCIENCE, V264, P688, DOI 10.1126/science.264.5159.688; Moore P.D., 1991, POLLEN ANAL; NELSON AR, 1993, J COASTAL RES, V9, P673; NORTH MEA, 1984, SYESIS, V17, P47; Palmer A.J.M., 1991, Paper 91-1E, P109; POJAR J., 1994, PLANTS COASTAL BRIT; Shennan I, 1998, QUATERNARY SCI REV, V17, P365, DOI 10.1016/S0277-3791(97)00055-3; Sherrod BL, 2013, GEOSPHERE, V9, P827, DOI 10.1130/GES00880.1; WILLIAMS HFL, 1991, PALAEOGEOGR PALAEOCL, V86, P297, DOI 10.1016/0031-0182(91)90087-8; Yamaguchi DK, 1997, NATURE, V389, P922, DOI 10.1038/40048	26	0	0	2	2	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	FEB	2024	321								105040	10.1016/j.revpalbo.2023.105040	http://dx.doi.org/10.1016/j.revpalbo.2023.105040		DEC 2023	5	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	GP8C4					2025-03-11	WOS:001153953300001
J	Geddada, D; Narsimha, K				Geddada, Divya; Narsimha, Kanchi			Record of Early Cretaceous dinoflagellate cysts from well JM-A, Dhansiri Valley of Upper Assam Shelf, India	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Dinoflagellate cysts; Bamangaon; Early cretaceous; Dhansiri calley; Upper Assam Shelf; India		A palynological study on subsurface Early Cretaceous sediments (1550-1860 m) in well JM-A located in Dhansiri Valley, Upper Assam Shelf has been carried out for determination of age and depositional environment. The palynological investigations resulted into the identification of the characteristic and diversified occurrence of Early Cretaceous dinoflagellate cysts comprising Batioladinium micropodum, Achomosphaera? neptuni, Batiacasphaera asperata, Lagenorhytis sp. cf. L. delicatula, Mendicodinium caperatum and Canningia sp. along with associated dinoflagellate cysts. The significant assemblage of spore-pollen assemblage represented by Cicatricosisporites australiensis, Ceratosporites equalis, Gleicheniidites circinidites, Contignisporites cooksonii, Microcachryidites antarcticus, Podosporites tripakshii and Callialasporites trilobatus has also been recorded. The Early Cretaceous sediments are regarded as Bamangaon Formation in Dhansiri Valley. The occurrence of dinoflagellate cysts suggests marginal marine environment for Bamangaon Formation deposited during the Early Cretaceous period corresponding to the Rift Phase. The Formation overlies the Metamorphic Basement Complex, and it is unconformably overlain by the sediments of Tura Formation of Ypresian (Early Eocene) age, deposited under subtidal to inner shelf environment during the Passive Margin Tectonic Phase.	[Geddada, Divya] Oil & Nat Gas Corp Ltd, Reg Geosci Labs, 14 Pk Rd, Chennai, Tamil Nadu, India; [Narsimha, Kanchi] Oil & Nat Gas Corp Superannuated ONGC, Geol Labs, RGL, Jorhat, Assam, India	Oil & Natural Gas Corporation	Geddada, D (通讯作者)，Oil & Nat Gas Corp Ltd, Reg Geosci Labs, 14 Pk Rd, Chennai, Tamil Nadu, India.	geddada_divya@ongc.co.in			ONGC, New Delhi [Convener 28th ICMS-2022]	ONGC, New Delhi	The authors wish to express their sincere gratitude to Smt Sushma Rawat, Director (Exploration), ONGC, New Delhi, for granting permission to publish this work. The authors are thankful to Shri Gour Mohan Das, Executive Director-Chief Labs, Mumbai for motivation and constant support. The authors are grateful to Shri Vishal Shastri, Executive Director-Basin Manager, Assam and Assam Arakan Basin, Jorhat for assigning the project, motivation and support. The authors are grateful to Sri K. Karvannan, Chief General Manager-Basin Manager, Krishna Godavari-Pranhita Godavari Basin, Rajahmundry for constant support and guidance. The authors are obliged to Dr Rajani Panchang, UGC FRP Assistant Professor, Department of Environmental Science, Convener 28th ICMS-2022, SPPU, Pune and Guest Editor, Special Issue JPSI for consideration of the paper for publication in Special Issue, JPSI. The authors are thankful to Dr R.K. Saxena, Ex CGM, ONGC and another anonymous reviewer, for reviewing the paper and improving the manuscript with their valuable suggestions.	[Anonymous], 1987, Palaeobotanist; Basavaraju MH, 2007, J GEOL SOC INDIA, V70, P158; Deshpande S. V., 1993, ONGC DOC X ASSAM ARA, V1 2; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Jansonius J., 1976, Genera file of fossil spores; Khanna S.N., 1973, WELL COMPLETION REPO; Lal NK, 2009, J GEOL SOC INDIA, V73, P249, DOI 10.1007/s12594-009-0081-1; Mathur K., 1991, STANDARD LAB TECHNIQ, P83; Mehrotra N. C., 2022, PALYNOLOGY HYDROCA 3, V7; Mehrotra N. C., 2005, PALYNOLOGY HYDROCA 2, V61, P1; Mehrotra N. C., 2002, PALYNOLOGY HYDROCARB, V48, P1; Narsimha K., 2023, J PALAEONTOL SOC IND; Prasad B., 1985, GEOSCI J, V16, P155; Singh C., 1971, LOWER CRETACEOUS MIC, V28; Stover L. E., 1978, ANALYSES PREPLIESTOC; Thanikaimoni G., 1984, SELECTED TERTIARY AN; Williams G.L., 1985, P847; Williams G. L., 1993, MORPHOLOGY STRATIGRA, P137; Wilson G.G., 1980, Canadian Forestry Service Forest Pest Management Institute Information Report FPM-X, P1	19	0	0	0	1	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	DEC	2023	68	2			SI		199	206		10.1177/05529360231219329	http://dx.doi.org/10.1177/05529360231219329		DEC 2023	8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	IC2G0		hybrid			2025-03-11	WOS:001142076400001
J	Ling, CH; Xue, B; Yao, SC; Zhang, WC; Pan, DD; Tang, LY				Ling, Chaohao; Xue, Bin; Yao, Shuchun; Zhang, Wenchao; Pan, Dadong; Tang, Lingyu			High-resolution sea-level fluctuations during the Mid-Holocene in the Ningshao Coastal Plain region, eastern China	FRONTIERS IN ECOLOGY AND EVOLUTION			English	Article						Holocene; sea-level fluctuations; pollen; dinoflagellate cysts; foraminiferal organic linings; Ningshao coastal plain	WALLED DINOFLAGELLATE CYSTS; YANGTZE DELTA; HOLOCENE VEGETATION; SEDIMENTARY RECORD; YAOJIANG VALLEY; HANGZHOU BAY; MIDDLE; RISE; RICE; CLIMATE	Sea level changes during the Mid-Holocene directly influenced the Neolithic culture in the Yangtze River Delta region (YRD). However, the high-resolution sea level change characteristics for this period remain unclear. In this study, we performed a high-resolution palynological analysis, including pollen, Dinoflagellate cysts, and Foraminiferal organic linings, using a high-resolution sediment core from Shanglin Lake, in the North of Ningshao Plain (the south of Hangzhou Bay). 11 accelerator mass spectrometry 14C(AMS) datings indicate the age of the sediments range from 8 cal ka B.P. to 5.6 cal ka B.P. The results show that during the Mid-Holocene, Shanglin Lake evolved from an estuary - subtidal lagoon - semi-enclosed bay - semi-enclosed lagoon - semi-enclosed bay - enclosed lagoon to a modern freshwater lake. There was a period of no, or minimal, eustatic sea-level rise between 7733 and 7585 cal yr B.P. The Mid-Holocene high sea level comes in 7253-7082 cal yr BP. Between 7000 cal yr BP and 5502 cal yr BP, the sea level is close to modern value. The sea level change during this period had a significant impact on the local Neolithic human activity.	[Ling, Chaohao; Pan, Dadong] Minnan Normal Univ, Sch Hist & Geog, Zhangzhou, Peoples R China; [Ling, Chaohao; Xue, Bin; Yao, Shuchun] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing, Peoples R China; [Zhang, Wenchao] China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing, Peoples R China; [Tang, Lingyu] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing, Peoples R China	MinNan Normal University; Chinese Academy of Sciences; Nanjing Institute of Geography & Limnology, CAS; China University of Geosciences; Chinese Academy of Sciences	Xue, B (通讯作者)，Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing, Peoples R China.	Bxue@niglas.ac.cn		Ling, Chaohao/0000-0002-9851-5920	Natural Science Foundation of Fujian Province [2022J05178]; Natural Science Foundation of Hunan Province [2021JJ30555]	Natural Science Foundation of Fujian Province(Natural Science Foundation of Fujian Province); Natural Science Foundation of Hunan Province(Natural Science Foundation of Hunan Province)	We are very grateful to Prof. Baohua Li (Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences) for his help in the identification of foraminifera fossils. Jingkui Tao and Wei Wang from Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences are thanked for their hard work during the field campaign.r This research has been supported by, the Natural Science Foundation of Fujian Province (grant no. 2022J05178) and the Natural Science Foundation of Hunan Province (grant no. 2021JJ30555).	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Ecol. Evol.	DEC 21	2023	11								1218658	10.3389/fevo.2023.1218658	http://dx.doi.org/10.3389/fevo.2023.1218658			14	Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	EG7T4		gold			2025-03-11	WOS:001137841300001
J	Gu, HF; Zheng, J; Huang, SN; Morquecho, L; Krock, B; Shin, HH; Li, Z; Derrien, A; Mertens, KN				Gu, Haifeng; Zheng, Jing; Huang, Shuning; Morquecho, Lourdes; Krock, Bernd; Shin, Hyeon Ho; Li, Zhun; Derrien, Amelie; Mertens, Kenneth Neil			A new dinoflagellate Gonyaulax pospelovana with resting cysts resembling Spiniferites delicatu<i>s</i> and its biogeography and ecology revealed by DNA metabarcoding	PHYCOLOGIA			English	Article						Cyst-theca relationship; Gonyaulax spinifera; 18S V4; Tara Oceans; Yessotoxin	GULF-OF-CALIFORNIA; SP-NOV; PROTOCERATIUM RETICULATUM; DINOPHYCEAE; WATER; SEQUENCES; SEDIMENTS; LAGOON; BLOOM; BASIN	Extant species of the dinoflagellate genus Gonyaulax are capable of producing resting cysts morphologically similar to different cyst-based genera, and their cyst-theca relationships are far from resolved. Here we have carried out germination experiments on several living cysts that resemble Spiniferites delicatus from the subtropical regions of China and Mexico. Both cyst and theca morphology were examined by light and scanning electron microscopy. A new species, Gonyaulax pospelovana, is described, characterized by a cingulum displacement and an overhang of twice its width, and two short antapical spines. The cysts of G. pospelovana had a granular surface and gonal processes with petaloid tips. Maximum likelihood and Bayesian inference analyses based on LSU and SSU rRNA gene sequences revealed that strains identified as G. pospelovana were monophyletic, forming a sister clade to Gonyaulax ellegaardiae and several presumable strains of Gonyaulax spinifera. One Chinese strain and two Mexican strains of G. pospelovana were examined for yessotoxin production using LC-MS/MS, but were not found to produce a detectable amount of toxins. Metabarcoding targeting the 18S V4 rRNA gene was performed on monthly collected samples in Xiamen Bay, China. A ZOTU (zero-radius operational taxonomic units) was detected that was consistent with G. pospelovana. Its maximum abundance was recorded in summer. Additionally, an OTU was identified as G. pospelovana from the Tara Oceans metabarcoding data, which occurred in the Indian and Pacific oceans at temperatures ranging from 28(degrees)C to 31(degrees)C, suggesting that it is a warm water species.	[Gu, Haifeng; Zheng, Jing; Huang, Shuning] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Morquecho, Lourdes] Ctr Invest Biol Noroeste CIBNOR, Av IPN 195, La Paz 23096, Baja California, Mexico; [Krock, Bernd] Alfred Wegener Inst Polar & Marine Res, Handelshafen 12, D-27570 Bremerhaven, Germany; [Shin, Hyeon Ho] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea; [Li, Zhun] Korea Res Inst Biosci & Biotechnol, Biol Resource Ctr, Korean Collect Type Cultures KCTC, Jeongeup 56212, South Korea; [Derrien, Amelie; Mertens, Kenneth Neil] Ifremer, LITTORAL, F-29900 Concarneau, France	Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Korea Institute of Ocean Science & Technology (KIOST); Korea Research Institute of Bioscience & Biotechnology (KRIBB); Ifremer	Gu, HF (通讯作者)，Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China.; Mertens, KN (通讯作者)，Ifremer, LITTORAL, F-29900 Concarneau, France.	guhaifeng@tio.org.cn; kenneth.mertens@ifremer.fr	Krock, Bernd/ABB-7541-2020; Mertens, Kenneth/AAO-9566-2020; Morquecho, Lourdes/JPY-0626-2023; Gu, Haifeng/ADN-4528-2022; Mertens, Kenneth/C-3386-2015	Gu, Haifeng/0000-0002-2350-9171; Derrien, Amelie/0000-0001-9656-7850; Mertens, Kenneth/0000-0003-2005-9483; Shin, Hyeon Ho/0000-0002-9711-6717	National Key Research and Development Program of China; National Key Research and Development Program of China [2019YFE0124700]; National Natural Science Foundation of China [42076085]; Korean Culture Collection of Microalgae and Collaboration Center [NRF- 2022M3H9A1083416]; Regional Council of Brittany; General Council of Finistere; Urban Community of Concarneau-Cornouaille- Agglomeration; Collection of Marine Dinoflagellates (CODIMAR)	National Key Research and Development Program of China(National Key Research & Development Program of China); 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)); Korean Culture Collection of Microalgae and Collaboration Center; Regional Council of Brittany(Region Bretagne); General Council of Finistere(Region Bretagne); Urban Community of Concarneau-Cornouaille- Agglomeration; Collection of Marine Dinoflagellates (CODIMAR)	This work was supported by the the National Key Research and Development Program of China (2019YFE0124700), National Natural Science Foundation of China (42076085), and the Korean Culture Collection of Microalgae and Collaboration Center (NRF- 2022M3H9A1083416). The Sigma 300 FE-SEM used in this study was funded by The Regional Council of Brittany, the General Council of Finistere and the Urban Community of Concarneau-Cornouaille- Agglomeration. The isolation and maintenance in perpetuity of the strains from Mexico is supported by the Collection of Marine Dinoflagellates (CODIMAR) belonging to CIBNOR.	Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; Alvarez G, 2016, HARMFUL ALGAE, V58, P8, DOI 10.1016/j.hal.2016.07.006; AMADI I, 1992, BOT MAR, V35, P451, DOI 10.1515/botm.1992.35.5.451; Andersen R. A., 2005, Algal culturing techniques, P83; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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L., 2017, Am. Assoc. Stratigraphic Palynologist Data Ser.; Zhang Q, 2011, EUR J PROTISTOL, V47, P149, DOI 10.1016/j.ejop.2011.03.001; Zhang W, 2020, PHYCOLOGIA, V59, P246, DOI 10.1080/00318884.2020.1735926; Zonneveld KAF, 2013, REV PALAEOBOT PALYNO, V191, P1, DOI 10.1016/j.revpalbo.2012.08.003	65	2	2	3	10	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	JAN 2	2024	63	1					74	88		10.1080/00318884.2023.2293311	http://dx.doi.org/10.1080/00318884.2023.2293311		DEC 2023	15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	HB0J9					2025-03-11	WOS:001130254300001
J	Bijl, PK; Brinkhuis, H				Bijl, Peter K.; Brinkhuis, Henk			Palsys.org: an open-access taxonomic and stratigraphic database of organic-walled dinoflagellate cysts	JOURNAL OF MICROPALAEONTOLOGY			English	Review								It is with great pleasure that we introduce palsys.org (https://palsys.org/genus/, last access: 8 December 2023), a fully open-access taxonomic, stratigraphic and image database of organic-walled dinoflagellate cysts. Palsys.org started as the in-house database of the Laboratory of Palaeobotany and Palynology (LPP) Foundation over 30 years ago. It is now owned by Utrecht University and has been expanded and transformed into a public online platform for use in research and education. Palsys.org includes the taxonomic descriptions of genera and species of organic walled dinoflagellate cysts, from the (often translated) literature, and emendations and synonymy, mainly following Williams et al. (2017) and the stratigraphic calibrations from DINOSTRAT (Bijl, 2022), and has around 25 000 images of species. Here, in this launch paper, we explain the history of the database, present its current functionalities and explain our set-up of the data quality control. We call upon the community to help us keep palsys.org up to date and complete by, for example, by sending additional information, imagery and feedback in general through the platform. Palsys.org brings dinoflagellate micropaleontology in line with the open-science principles of modern academia.	[Bijl, Peter K.; Brinkhuis, Henk] Univ Utrecht, Fac Geosci Marine Palynol & Paleoceanog, Dept Earth Sci, VMA Bldg,Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands; [Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst Res OCS, POB 59, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci Marine Palynol & Paleoceanog, Dept Earth Sci, VMA Bldg,Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/IUO-8165-2023	Bijl, Peter/0000-0002-1710-4012; Brinkhuis, Henk/0000-0003-0253-6610	LPP Foundation; American Association of Stratigraphic Palynologists (AASP); Micropaleontological Society (TMS)	LPP Foundation; American Association of Stratigraphic Palynologists (AASP); Micropaleontological Society (TMS)	Funding for the development of PALSYS had been provided by the LPP Foundation from the 1990s until 2000and from 2012 until 2019. From 2000 until 2012, TNO gave in-kind contributions to the database content of PALSYS. Several institutes 15 have contributed since 2012 to the transformation of PALSYS to palsys.org. These include the Department of Earth Sciences and Physical Geography of Utrecht University, Heidelberg University, GNS Science in Aotearoa/New Zealand, the Geological Survey of Denmark and Greenland (GEUS) and the Dutch Geological Sur20vey. Financial contributions by the American Association of Strati-graphic Palynologists (AASP) and the Micropaleontological Society (TMS) made it possible to make palsys.org open access.	Bijl PK, 2022, EARTH SYST SCI DATA, V14, P579, DOI 10.5194/essd-14-579-2022; Evitt W.R., 1985, pi; Fensome R. A., 1993, Special Paper; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; Williams G. L., 2017, Data Ser., V2	5	1	1	0	1	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	DEC 19	2023	42	2					309	314		10.5194/jm-42-309-2023	http://dx.doi.org/10.5194/jm-42-309-2023			6	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	IU5C0		gold, Green Submitted			2025-03-11	WOS:001168853100001
J	Head, MJ; Mertens, KN; Fensome, RA				Head, Martin J.; Mertens, Kenneth N.; Fensome, Robert A.			Dual nomenclature in organic-walled dinoflagellate cysts I: concepts, methods and applications	PALYNOLOGY			English	Article						Dinocyst; taxonomy; dual nomenclature; hybridised names; Lingulodinium; Lingulaulax	SP-NOV DINOPHYCEAE; THECA RELATIONSHIP; SPATIAL-DISTRIBUTION; GONYAULAX-BALTICA; RECENT SEDIMENTS; LIVING FOSSILS; SEA; PROPOSALS; TAXONOMY; NORTH	Dual nomenclature in dinoflagellates is supported under the current nomenclatural code for algae, fungi and plants and allows a fossil-defined (usually cyst) species to bear a name other than that of its equivalent non-fossil species, as established for example by incubation experiments. Two names can then apply to the same cyst morphotype, reflecting the separate but overlapping concepts and criteria used for fossil- and non-fossil taxa. Fossil-species are normally and logically assigned to fossil-genera and non-fossil species to non-fossil genera, a practice that facilitates dual nomenclature. Inconsistencies and ambiguities arise when binomials combine the names of fossil- with non-fossil taxa. Examples of this hybridised nomenclature and its consequences are examined, with problems identified and potential solutions discussed. Accordingly, a new non-fossil genus Lingulaulax is proposed with Lingulaulax polyedra (von Stein 1883) comb. nov. as its type and equivalent to the fossil-species Lingulodinium machaerophorum (Deflandre & Cookson 1955) Wall 1967, along with the new combination Lingulaulax milneri (Murray & Whitting 1899); the genus Lingulodinium Wall 1967 is retained in its exclusively fossil status. The non-fossil name Gonyaulax ellegaardiae Mertens et al. 2015 is validly published herein.	[Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Mertens, Kenneth N.] Ifremer, LITTORAL, Concarneau, France; [Fensome, Robert A.] Nat Resources Canada, Bedford Inst Oceanog, Geol Survey Canada Atlantic, Dartmouth, NS, Canada	Brock University; Ifremer; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Head, MJ (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	mjhead@brocku.ca	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Head, Martin/0000-0003-3026-5483; Mertens, Kenneth/0000-0003-2005-9483	Natural Sciences and Engineering Research Council of Canada Discovery Grant; French National Research Agency (ANR) PhenoMap project [ANR-20-CE02-0025]; Natural Resources Canada [20230058]; Agence Nationale de la Recherche (ANR) [ANR-20-CE02-0025] Funding Source: Agence Nationale de la Recherche (ANR)	Natural Sciences and Engineering Research Council of Canada Discovery Grant(Natural Sciences and Engineering Research Council of Canada (NSERC)); French National Research Agency (ANR) PhenoMap project(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco); Natural Resources Canada(Natural Resources CanadaCanadian Forest Service); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	Haifeng Gu is thanked for providing the basis for Figure 4. MJH acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. KNM was financially supported by the French National Research Agency (ANR) PhenoMap project, ANR-20-CE02-0025. RAF acknowledges the support of Natural Resources Canada; this is NRCan contribution number 20230058. We are most grateful to P.J. Mudie and the four journal reviewers, including V. Pospelova, all of whom provided helpful comments.	Abe T. 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J	Huang, D; Cheng, CQ; Qiu, JB; Huang, Y; Zhang, HY; Xu, ZH; Wu, SW; Huang, YT; Chen, J; Zou, LG; Yang, WD; Zheng, XF; Li, HY; Li, DW				Huang, Dan; Cheng, Cai-Qin; Qiu, Jiang-Bing; Huang, Yun; Zhang, Hao-Yun; Xu, Zhen-Hao; Wu, Si-Wei; Huang, Yi-Tong; Chen, Jian; Zou, Li-Gong; Yang, Wei-Dong; Zheng, Xiao-Fei; Li, Hong-Ye; Li, Da-Wei			Mechanistic insights into the effects of diuron exposure on Alexandrium pacificum	WATER RESEARCH			English	Article						(DCMU); Pollutant removal; Bioremediation; Alexandrium pacificum; Paralytic shellfish toxins; Cell growth; N-(3,4-dichlorophenyl)-N,N-dimethylurea	COASTAL WATERS; REMOVAL; CONTAMINATION; SEDIMENTS; TOXICITY; SEAWATER; IRGAROL; SEA; BIOSYNTHESIS; PESTICIDES	Diuron (N-(3,4-dichlorophenyl)-N,N-dimethylurea, DCMU), a ureic herbicide, is extensively used in agriculture to boost crop productivity; however, its extensive application culminates in notable environmental pollution, especially in aquatic habitats. Therefore, the present study investigated the effect of diuron on the dinoflagellate Alexandrium pacificum, which is known to induce harmful algal blooms (HAB), and its potential to biodegrade DCMU. Following a four-day DCMU exposure, our results revealed that A. pacificum proficiently assimilated DCMU at concentrations of 0.05 mg/L and 0.1 mg/L in seawater, attaining a complete reduction (100 % efficiency) after 96 h for both concentrations. Moreover, evaluations of paralytic shellfish toxins content indicated that cells subjected to higher DCMU concentrations (0.1 mg/L) exhibited reductions of 73.4 %, 86.7 %, and 75 % in GTX1, GTX4, and NEO, respectively. Exposure to DCMU led to a notable decrease in A. pacificum's photosynthetic efficacy, accompanied by increased levels of reactive oxygen species (ROS) and suppressed cell growth, with a growth inhibition rate of 41.1 % at 72 h. Proteomic investigations pinpointed the diminished expression levels of specific proteins like SxtV and SxtW, linked to paralytic shellfish toxins (PSTs) synthesis, as well as key proteins associated with Photosystem II, namely PsbA, PsbD, PsbO, and PsbU. Conversely, proteins central to the cysteine biosynthesis pathways exhibited enhanced expression. In summary, our results preliminarily resolved the molecular mechanisms underlying the response of A. pacificum to DCMU and revealed that DCMU affected the synthesis of PSTs. Meanwhile, our data suggested that A. pacificum has great potential in scavenging DCMU.	[Huang, Dan; Cheng, Cai-Qin; Huang, Yun; Zhang, Hao-Yun; Xu, Zhen-Hao; Huang, Yi-Tong; Zou, Li-Gong; Yang, Wei-Dong; Zheng, Xiao-Fei; Li, Hong-Ye; Li, Da-Wei] Jinan Univ, Affiliated Hosp 1, Dept Sports Med,Guangzhou Key Lab Precis Orthoped, Guangdong Prov Key Lab Speed Capabil, Guangzhou 510630, Peoples R China; [Wu, Si-Wei] Jinan Univ, Guangdong Higher Educ Inst, Coll Life Sci & Technol, Key Lab Eutrophicat & Red Tide Prevent, Guangzhou 510632, Peoples R China; [Qiu, Jiang-Bing] Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Peoples R China; [Chen, Jian] Zhuhai Int Travel Healthcare Ctr, State Key Lab Med Vector Surveillance, Zhuhai 519020, Guangdong, Peoples R China	Jinan University; Jinan University; Ocean University of China	Li, DW (通讯作者)，Jinan Univ, Affiliated Hosp 1, Dept Sports Med,Guangzhou Key Lab Precis Orthoped, Guangdong Prov Key Lab Speed Capabil, Guangzhou 510630, Peoples R China.	daweili@jnu.edu.cn	Huang, Yitong/HZI-4904-2023; Yang, Weidong/ABA-5036-2021; J, Qiu/AAY-2929-2020; 孙, 笑川/GWN-2355-2022; zheng, xiaofei/IUN-8791-2023; zhang, hao/KXQ-8149-2024	Da-Wei, Li/0000-0002-1452-0264; Huang, Dan/0000-0001-7853-502X	Natural Science Foundation of China [31870027, 51908244, 32100080]; Guangdong Natural Science Foundation [2019A1515110390, 2021A1515011486]; Fundamental Research Funds for the Central Universities [21620337]	Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Guangdong Natural Science Foundation(National Natural Science Foundation of Guangdong Province); Fundamental Research Funds for the Central Universities(Fundamental Research Funds for the Central Universities)	DWL is thankful to the Natural Science Foundation of China (32100080) , Guangdong Natural Science Foundation (2019A1515110390, 2021A1515011486) and the Fundamental Research Funds for the Central Universities for the research funding (21620337) . HYL acknowledges the Natural Science Foundation of China (31870027, 51908244) for the research grant. We would like to thank Editage ( www.editage.cn) for English language editing.	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FEB 15	2024	250								120987	10.1016/j.watres.2023.120987	http://dx.doi.org/10.1016/j.watres.2023.120987		DEC 2023	10	Engineering, Environmental; Environmental Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Water Resources	ER7S9	38113594				2025-03-11	WOS:001140722300001
J	Kietzmann, DA				Kietzmann, Diego A.			New Tithonian-Berriasian morphospecies of the genus <i>Stomiosphaera</i> Wanner (calcareous dinoflagellate cysts) from the Vaca Muerta Formation, Neuquen Basin, Argentina	CRETACEOUS RESEARCH			English	Article						Calcareous dinofagellate cysts; Vaca Muerta Formation; Upper Jurassic; Lower Cretaceous	MAGNETOSTRATIGRAPHY; BOUNDARY; AMMONITE	Five new morphospecies of calcareous dinoflagellate cysts belonging to the genus Stomiosphaera Wanner, are described from the Tithonian-Berriasian Vaca Muerta Formation, in the Neuquen Basin, Western Argentina: Stomiosphaera triangulata sp. nov., Stomiosphaera quadrata sp. nov., Stomiosphaera subechinata sp. nov., Stomiosphaera subspinosa sp. nov., and Stomiosphaera gracilis sp. nov. Their stratigraphic distribution is discussed, particularly that of Stomiosphaera subechinata sp. nov. (Tithonian - lower Berriasian), which was previously assigned to Stomiosphaera echinata Nowak, a species that in the Tethys domain appears for the first time in the upper Valanginian. Likewise, possible assignments to the genera defined from three-dimensional observations are proposed, and eutrophic neritic conditions are interpreted for the time in which these species appear in the Neuquen Basin. (c) 2023 Elsevier Ltd. All rights reserved.	[Kietzmann, Diego A.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol UBA FCEN, Pabellon 2,Intendente Guiraldes 2160,C1428EHA, Buenos Aires, DF, Argentina; [Kietzmann, Diego A.] Consejo Nacl Invest Cient & Tecn CONICET, Inst Geociencias Bas Ambientales & Aplicadas Bueno, Pabellon 2,Intendente Guiraldes 2160,C1428EHA, Buenos Aires, DF, Argentina	University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Kietzmann, DA (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol UBA FCEN, Pabellon 2,Intendente Guiraldes 2160,C1428EHA, Buenos Aires, DF, Argentina.; Kietzmann, DA (通讯作者)，Consejo Nacl Invest Cient & Tecn CONICET, Inst Geociencias Bas Ambientales & Aplicadas Bueno, Pabellon 2,Intendente Guiraldes 2160,C1428EHA, Buenos Aires, DF, Argentina.	diegokietzmann@gl.fcen.uba.ar	Kietzmann, Diego/S-4549-2019	Kietzmann, Diego Alejandro/0000-0003-1222-7811	Agencia Nacional de Promocion Cientifica y Tecnologica [PICT2018-02492]	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government)	This research was supported by the Agencia Nacional de Promocion Cientifica y Tecnologica, Proyecto PICT2018-02492. I would like to acknowledge Mohamed Benzaggagh, an anonymous reviewer, and the editor Eduardo Koutsoukos for their valuable comments and corrections, which contributed significantly to improve this paper.	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Res.	MAR	2024	155								105786	10.1016/j.cretres.2023.105786	http://dx.doi.org/10.1016/j.cretres.2023.105786		DEC 2023	13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	EH3V6					2025-03-11	WOS:001138001000001
J	Okeke, KK; Slimani, H; Jbari, H; Ukpabi, N; Asadu, AN				Okeke, Kachikwulu Kingsley; Slimani, Hamid; Jbari, Hassan; Ukpabi, Ndubuisi; Asadu, Anthonia Nwaneze			Palynostratigraphy and palaeoenvironment of the Danian sediments from the Nsukka Formation of the Anambra Basin at the vicinity of Ikpankwu, southeastern Nigeria	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynostratigraphy; Palaeoenvironment; Ikpankwu; Microflora; Nsukka Formation	CRETACEOUS-TERTIARY BOUNDARY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; PALEOGENE K/PG BOUNDARY; WESTERN EXTERNAL RIF; SEA-LEVEL; OULED HADDOU; CALCAREOUS NANNOFOSSIL; PLANKTIC FORAMINIFERA; PALEOCENE SUCCESSION; EASTERN CARPATHIANS	Detailed investigations of biostratigraphy of the Nsukka Formation in the Ikpankwu area are paramount due to the fluctuation of depositional environment, fossil flora abundance and diversity interchange, and lateral facies change dynamics from the southern to northern sections of this formation. The microflora assemblages, chronostratigraphic age and depositional paleoenvironment of index palynomorphs suggest a Danian age for the studied strata, based on global dinoflagellate cyst events. The persistent abundance of monocolpate assemblages and the biostratigraphic resolution attained, suggest that the studied sediment interval is continuous. The marker species of terrestrial microflora (Constructipollenites ineffectus, Echitriporites trianguliformis, Foveotriletes margaritae, Longapertites group, Proxapertites group, Retidiporites magdalenensis, Scabratriporites annellus, Spinizonocolpites group, Syncolporites marginatus) and dinocysts (Carpatella cornuta, Danea californica, Fibrocysta licia, Kenleyia pachycerata, Spiniferella cornuta subsp. kasira), compared with several reference sections from the tropical to subtropical province, engineered a refined geologic age and paleoenvironment of deposition of the sediments. These dinocysts taxa are global Danian index fossils which are valuable in the identification of earliest Palaeocene sequence of the formation. The depositional paleoenvironment alternately fluctuates from continental setting to marginal marine inner neritic and outer neritic conditions, based on the presence of land-derived miospores and dinocysts. These macroenvironments are the products of effective vacillating depositional environment systems between the lower and upper deltaic plains, oscillating from tidal flat, lagoon, tidal bar to nearshore open marine influenced settings. Lycopodiaceae-Zlivisporis blanensis fern spore with fragile perispore substantiate the autochtonous vegetation and least transport and palynomorph hydrodynamic system inherent in the predominant pollen and spore species and close proximity to fresh water settings visible in medium to coarse grained sandstone units of the middle section. These microenvironment syntheses of the Nsukka Formation revealed a confirmed and pronounced transgressive systems tract (TST), articulated in the shale sample from the Ikpankwu section of the Nsukka Formation, Anambra Basin. The palaeoenvironments and palynostratigraphic dynamics illustrate that overall progradation was trailed by sporadic retrogradation of the delta with a high biostratigraphic resolution system indicative of continuous biological imprints of the terrestrial and marine microflora of the Nsukka Formation during the Danian.	[Okeke, Kachikwulu Kingsley] Univ Nigeria, Dept Geol, Nsukka, Nigeria; [Slimani, Hamid; Jbari, Hassan] Mohammed V Univ Rabat, Geobiodivers & Nat Patrimony Lab GEOBIO,Geophys, Nat Patrimony & Green Chem Res Ctr GEOPAC, Dept Geol & Remote Sensing,Sci Inst, Rabat, Morocco; [Ukpabi, Ndubuisi] Univ Port Harcourt, Geol Dept, Port Harcourt, Nigeria; [Asadu, Anthonia Nwaneze] Fed Univ Petr Resources, Effurun, Delta State, Nigeria	University of Nigeria; Mohammed V University in Rabat; University of Port Harcourt	Okeke, KK (通讯作者)，Univ Nigeria, Dept Geol, Nsukka, Nigeria.	kachikwulu.okeke@unn.edu.ng	Slimani, Hamid/AAL-4055-2020	Ukpabi, Ndubuisi/0000-0002-8535-9041; Hassan, Jbari/0000-0001-9781-1843				Açikalin S, 2015, CRETACEOUS RES, V52, P251, DOI 10.1016/j.cretres.2014.07.011; Adebayo O. F., 2004, Pakistan Journal of Scientific and Industrial Research, V47, P417; Adebayo O.F, 2006, Global J. Geol. 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A., 1966, Leidse Geologische Mededelingen	148	0	0	0	0	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1464-343X	1879-1956		J AFR EARTH SCI	J. Afr. Earth Sci.	FEB	2024	210								105133	10.1016/j.jafrearsci.2023.105133	http://dx.doi.org/10.1016/j.jafrearsci.2023.105133		DEC 2023	15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	EK1V2					2025-03-11	WOS:001138736600001
J	Narsimha, K; Phor, L; Ghosh, TK; Panda, S; Geddada, D; Patra, BP				Narsimha, Kanchi; Phor, Lusuchu; Ghosh, Tushar Kanti; Panda, Sudeshna; Geddada, Divya; Patra, Biswa Prakash			Palynostratigraphy and depositional environment of Tura and Pre-Tura sedimentary successions in Dhansiri Valley of Upper Assam Shelf, Assam & Assam-Arakan Basin, Assam, India	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Tura; Moabund; Bamangaon; Dergaon; Dhansiri Valley; dinoflagellate cysts		Detailed palynological investigations have been carried out to reconstruct stratigraphy and interpretation of depositional environment of Tura and Pre-Tura sedimentary sections in Dhansiri Valley of Upper Assam Shelf, Assam & Assam-Arakan Basin. Sediments of the Tura Formation dated as Early Eocene and interpreted to be deposited under subtidal to inner shelf environment. Pre-Tura sediments, developed in studied wells, led to the identification of Dergaon, Bamangaon and Moabund formations with intervening unconformities, having different tectonic history and distinct palynofossil assemblages. Early Permian sediments of the Dergaon Formation (=Talchir Formation), the oldest in the basin are deposited under the intracratonic phase, overlie the metamorphic basement complex. The sediments of the Dergaon Formation are unconformably overlain by the Bamangaon Formation deposited during the Early Cretaceous, whereas, in well DR-A, the sediments of the Dergaon Formation are directly overlain by the Moabund Formation corresponding to the Late Maastrichtian age. The sediments of the Tura Formation overlie the Maobund Formation in well DR-A, and they overlie the Bamangaon Formation in the rest of the wells in Dhansiri Valley.	[Narsimha, Kanchi; Phor, Lusuchu; Ghosh, Tushar Kanti] Oil & Nat Gas Corp Superannuated ONGC, Geol Labs, RGL, Jorhat, Assam, India; [Panda, Sudeshna; Patra, Biswa Prakash] ONGC, WOB, NBP Green Hts, BKC, Mumbai, Maharashtra, India; [Geddada, Divya] ONGC, RGL, 14 Pk Rd, Chennai, India		Narsimha, K (通讯作者)，Oil & Nat Gas Corp Superannuated ONGC, Geol Labs, RGL, Jorhat, Assam, India.	narasimha_kanchi@yahoo.co.in			ONGC, New Delhi	ONGC, New Delhi	The authors wish to express their sincere gratitude to Smt Sushma Rawat, Director (Exploration), ONGC, New Delhi, for granting permission to publish this work, constant encouragement and valuable suggestions. The authors are thankful to Sri Gour Mohan Das, ED-Chief Labs, Mumbai for motivation and constant support. The authors are thankful to Shri Vishal Shastry, ED-Basin Manager, A&AA Basin, Jorhat for assigning the project, motivation and support. The authors are grateful to Sri K. Karvannan, CGM-Basin Manager, KG-PG Basin, Rajahmundry for constant support and guidance. Dr Naresh Mehrotra and Dr Anju Saxena are thanked for their valuable reviews that helped improve the manuscript.	[Anonymous], 1978, Analyses of pre-Pleistocene organic walled dinoflagellates; [Anonymous], 1987, Palaeobotanist; Basavaraju MH, 2007, J GEOL SOC INDIA, V70, P158; Bharadwaj D. C., 1978, PALEOBOTANIST, V25, P62; Chandra A., 1980, P 4 INT PAL C, V2, P117; Deshpande S.V., 1993, Lithostratigraphy of Indian Petroliferous Basins; Fox C. S., 1937, DIRECTORS GEN REPORT, V72, P85; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Jansonius J., 1976, Genera file of fossil spores; Khanna S.N., 1973, WELL COMPLETION REPO; Madan Mohan, 1973, FORAMINIFERAL REPORT; Mathur K., 1991, STANDARD LAB TECHNIQ, P83; Mehrotra N. C., 2022, PALYNOLOGY HYDROCARB, V7, P1; Mehrotra N. C., 2005, PALYNOLOGY HYDROCA 2, V61, P1; Mehrotra N. C., 2002, PALYNOLOGY HYDROCARB, V48, P1; Nautiyal D. D., 2000, P 16 ICMS ONGC B, V37, P113; Prasad B., 1985, GEOSCI J, V16, P155; Sharma K. D., 1986, B OIL NAT GAS COMM, V23, P101; Singh H.P., 1988, J. Palaeosci., V36, P168; Srivastava S. C., 1984, PALEOBOTANIST, V32, P26; Stover, 1993, MORPHOLOGY STRATIGRA; Thanikaimoni G., 1984, Selected Tertiary Angiosperm Pollen from India and Their Relationship with African Tertiary Pollen, V19, P1; Tiwari R. S., 1992, PALAEOBOTONIST, V49, P195; Williams G.L., 1985, P847; Wilson G.G., 1980, Canadian Forestry Service Forest Pest Management Institute Information Report FPM-X, P1	25	0	0	1	1	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	DEC	2023	68	2			SI		173	187		10.1177/05529360231216337	http://dx.doi.org/10.1177/05529360231216337		DEC 2023	15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	IC2G0		hybrid			2025-03-11	WOS:001142095500001
J	Usman, MB; Jolley, DW; Brasier, AT; Boyce, AJ				Usman, Musa B.; Jolley, David W.; Brasier, Alexander T.; Boyce, Adrian J.			Sequence stratigraphical and palaeoenvironmental implications of Cenomanian-Santonian dinocyst assemblages from the Trans-Sahara epicontinental seaway: a multivariate statistical approach	DEPOSITIONAL RECORD			English	Article						Benue Trough; dinocysts; Late Cretaceous; oceanic anoxic event 2; palaeoecology	DINOFLAGELLATE CYST ASSEMBLAGES; WESTERN INTERIOR SEAWAY; BENUE TROUGH; BASIN; STRATIFICATION; PALEOGEOGRAPHY; PHYTOPLANKTON; EVOLUTION; FRAMEWORK; HUMMOCKY	The Cretaceous was punctuated by episodic flooding of continental margins forming epicontinental seas. The Trans-Sahara Seaway was one of these epicontinental seas, connecting the Gulf of Guinea with the Tethys Ocean. In this study, data including microplankton abundances, stable carbon isotopes of organic material and elemental geochemistry were integrated with traditional sedimentological analyses from the Trans-Sahara Seaway. The carbon isotopic data provide the first evidence that oceanic anoxic event 2 was present in the Trans-Sahara Seaway, and palynology shows it was associated with an increase in peridinioid dinocyst abundance. A combined study of microplankton assemblages and sedimentology reveals palaeoenvironmental trends linked to sea-level change. Lowstand system tracts were characterised by increased siliciclastic grain size, low microplankton diversity, and were dominated by Chlorophyceae. Transgressive system tracts were associated with diversity increases during rising sea level, with open marine gonyaulacoid dinocysts dominating the assemblages. Maximum flooding surfaces were recognised by the highest increase in biological diversity in argillaceous deposits. As sea level started to fall, the peridinioid dinocysts became dominant, with decreased microplankton diversity during highstand systems tracts. This combination of sedimentology and interpretation of dinocyst assemblages allows the identification of shallow to deeper marine depositional sequences of Cenomanian-Santonian strata within the Yola Sub-basin. This approach could be used to delineate marine depositional sequences where using conventional sedimentological methods alone is very challenging. image	[Usman, Musa B.; Jolley, David W.; Brasier, Alexander T.] Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen, Scotland; [Usman, Musa B.] Gombe State Univ, Fac Sci, Dept Geol, Gombe, Nigeria; [Boyce, Adrian J.] Scottish Univ Environm Res Ctr, East Kilbride, Scotland; [Usman, Musa B.] Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen AB24 3UE, Scotland	University of Aberdeen; University of Aberdeen	Usman, MB (通讯作者)，Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen AB24 3UE, Scotland.	musausman51@gmail.com	Boyce, Adrian/D-2263-2010; Brasier, Alexander/E-7412-2010	Usman, Musa Bappah/0000-0001-9989-6115; Brasier, Alexander/0000-0001-6103-2848; Jolley, David/0000-0003-0909-2952	Petroleum Technology Development Fund (PTDF) Nigeria; Petroleum Technology Development Fund (PTDF)	Petroleum Technology Development Fund (PTDF) Nigeria; Petroleum Technology Development Fund (PTDF)	M.B. 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Min. Geol., V36, P153	71	1	1	0	0	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA		2055-4877		DEPOS REC	Depos. Rec.	FEB	2024	10	1					91	123		10.1002/dep2.260	http://dx.doi.org/10.1002/dep2.260		DEC 2023	33	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	IR7W8		Green Published, gold			2025-03-11	WOS:001121336800001
J	García-Moreiras, I; Hatherly, M; Zonneveld, K; Dubert, J; Nolasco, R; Santos, AI; Oliveira, A; Moita, T; Oliveira, PB; Magalhaes, JM; Amorim, A				Garcia-Moreiras, Iria; Hatherly, Melissa; Zonneveld, Karin; Dubert, Jesus; Nolasco, Rita; Santos, Ana Isabel; Oliveira, Anabela; Moita, Teresa; Oliveira, Paulo B.; Magalhaes, Jorge M.; Amorim, Ana			New physical and biological evidence of lateral transport affecting dinoflagellate cyst distribution in the benthic nepheloid layer along a land-sea transect off Figueira da Foz (Atlantic Iberian margin)	FRONTIERS IN MARINE SCIENCE			English	Article						benthic nepheloid layer; dinoflagellate cysts; cyst reservoir; advection; coastal ecosystems; Portuguese margin	HARMFUL ALGAL BLOOMS; GYMNODINIUM-CATENATUM; ALEXANDRIUM-CATENELLA; RECENT SEDIMENTS; LINGULODINIUM-POLYEDRUM; VERTICAL MIGRATION; SHELLFISH TOXICITY; UPWELLING SYSTEMS; RIVER PLUMES; RIAS-BAIXAS	Introduction The production of resting cysts is a key dispersal and survival strategy of many dinoflagellate species. However, little is known about the role of suspended cysts in the benthic nepheloid layer (BNL) in the initiation and decline of planktonic populations.Methods In September 2019, sampling of the dinoflagellate cyst community at different water depths in the water column and in the bottom sediments, and studies of spatio-temporal changes in physical properties (temperature, salinity, density and suspended sediment concentration), were carried out along a land-sea transect off Figueira da Foz (NW Portugal) to investigate the dinoflagellate cyst distribution and the factors (physical and biological) affecting it. A clustering analysis was used to compare the BNL and sediment cyst records with the cyst rain recorded by a sediment trap at a fixed station. Furthermore, Lagrangian particle experiments enabled simulating cyst trajectories in the BNL 5 and 10 days before sampling and assessing cross-shore, vertical and alongshore transport within the studied region.Results A well-developed BNL was present during the survey, which covered a change from active (14th of September) to relaxed (19th of September) upwelling conditions. Organic-walled dinoflagellate cysts were dominant in all samples, although calcareous dinoflagellate cysts consistently occurred (at low abundances). High proportions of full cysts were observed in the BNL, of which a significant portion was viable as shown by excystment experiments. Moreover, BNL cyst records collected on the 19th of September along the land-sea transect were similar to the sediment trap cyst record but greatly differed from sediment cyst records. The heterotrophic small spiny brown cysts (SBC) and cysts of the autotrophic yessotoxin-producer Protoceratium reticulatum notably increased during the survey, in the BNL and in the water column above.Discussion The comparison of the BNL, surface sediment and sediment trap cyst records supported that the main origin of cysts in the BNL was the recent production in the water column. The spatial coincidences in the distribution of cysts and vegetative cells of Protoceratium reticulatum also supported that full cysts in the water column were being produced in surface waters. New data evidenced the presence of a significant reservoir of viable cysts in the BNL that have the potential to seed new planktonic blooms. Furthermore, back-track particle modelling evidenced that alongshore advection was the main physical mechanism controlling cyst dynamics in the BNL during most part of the survey period, being particularly intense in coastal stations (<100 m depth). Consequently, the sediment cyst signal is a mixture of locally and regionally produced cysts. We provide multi-disciplinary data evidencing that cysts recently formed in the photic zone can be laterally advected within the studied region through the BNL, contributing to a better understanding of the role of the BNL in cyst dynamics and tracing the seed sources of the new blooms.	[Garcia-Moreiras, Iria] Univ Vigo, CIM Ctr Invest Marina, Vigo, Spain; [Garcia-Moreiras, Iria] Univ Vigo, Dept Biol Vexetal Ciencias Solo, Fac Ciencias, Vigo, Spain; [Hatherly, Melissa; Amorim, Ana] Univ Lisbon, MARE Marine & Environm Sci Ctr, Fac Ciencias, ARNET Aquat Res Network, Lisbon, Portugal; [Hatherly, Melissa; Amorim, Ana] Univ Lisbon, Fac Ciencias, Dept Biol Vegetal, Lisbon, Portugal; [Zonneveld, Karin] Univ Bremen, Ctr Marine Environm Sci, MARUM, Bremen, Germany; [Zonneveld, Karin] Univ Bremen, Geosci Dept, Bremen, Germany; [Dubert, Jesus; Nolasco, Rita] Univ Aveiro, Ctr Environm Marine Studies CESAM, Dept Fis, Aveiro, Portugal; [Dubert, Jesus; Nolasco, Rita] Univ Aveiro, Ctr Estudos Ambiente & Do Mar, Aveiro, Portugal; [Dubert, Jesus; Nolasco, Rita] CSIC, Inst Invest Marinas, CSIC, IIM, Vigo, Spain; [Santos, Ana Isabel; Oliveira, Anabela] Inst Hidrog IH, Marine Geol Div, Lisbon, Portugal; [Oliveira, Anabela] Univ Lisbon, Fac Ciencias, Inst Dom Luiz, Lisbon, Portugal; [Moita, Teresa] Univ Algarve, CCMAR Ctr Ciencias Mar, Faro, Portugal; [Oliveira, Paulo B.] IPMA Inst Portugues Mar & Atmosfera, Alges, Portugal; [Magalhaes, Jorge M.] Univ Porto, Interdisciplinary Ctr Marine & Environm Res, CIIMAR, Porto, Portugal; [Magalhaes, Jorge M.] Univ Porto, Fac Sci, Dept Geosci Environm & Spatial Planning DGAOT, Porto, Portugal	Universidade de Vigo; Universidade de Vigo; Universidade de Lisboa; Universidade de Lisboa; University of Bremen; University of Bremen; Universidade de Aveiro; Universidade de Aveiro; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Universidade de Lisboa; Universidade do Algarve; Instituto Portugues do Mar e da Atmosfera; Universidade do Porto; Universidade do Porto	García-Moreiras, I (通讯作者)，Univ Vigo, CIM Ctr Invest Marina, Vigo, Spain.; García-Moreiras, I (通讯作者)，Univ Vigo, Dept Biol Vexetal Ciencias Solo, Fac Ciencias, Vigo, Spain.; Amorim, A (通讯作者)，Univ Lisbon, MARE Marine & Environm Sci Ctr, Fac Ciencias, ARNET Aquat Res Network, Lisbon, Portugal.; Amorim, A (通讯作者)，Univ Lisbon, Fac Ciencias, Dept Biol Vegetal, Lisbon, Portugal.	iriagamo@uvigo.es; aaferreira@ciencias.ulisboa.pt	Magalhaes, Jorge/AAS-1999-2020; Oliveira, Anabela/L-8373-2013; Dubert, Jesus/B-7517-2008; GARCIA-MOREIRAS, IRIA/H-4627-2015; Amorim, Ana/AAA-2615-2020; Calixto de Jesus Moita Garnel, Maria Teresa/M-4039-2013	Oliveira, Anabela/0000-0001-5098-3939; GARCIA-MOREIRAS, IRIA/0000-0001-8713-0374; Dubert, Jesus/0000-0002-3338-6777; Amorim, Ana/0000-0002-9612-4280; Oliveira, Paulo/0000-0001-6838-7377; Calixto de Jesus Moita Garnel, Maria Teresa/0000-0002-8995-7516	EU ERDF funds; Fundaco para a Ciencia e Tecnologia, I.P.(FCT, I.P.); CESAM by FCT/MCTES [UIDP/04423/2020, LISBOA-01-0145-FEDER-031265]; Xunta de Galicia, Spain [UIDB/04292/2020]; Fundaco para a Ciencia e Tecnologia [UIDP/04292/2020, UIDP/50017/2020+UIDB/50017/2020+LA/P/0094/2020]; HABWAVE project; AQUIMAR project MAR2020; FCT through the strategic projects; The project MIWAVES;  [LA/P/0069/2020];  [UIDB/04326/2020];  [ED481B-2019-074];  [UIDB/04423/2020];  [MAR-02.01.01-FEAMP-017]	EU ERDF funds; Fundaco para a Ciencia e Tecnologia, I.P.(FCT, I.P.); CESAM by FCT/MCTES(Fundacao para a Ciencia e a Tecnologia (FCT)); Xunta de Galicia, Spain(Xunta de Galicia); Fundaco para a Ciencia e Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT)); HABWAVE project; AQUIMAR project MAR2020; FCT through the strategic projects; The project MIWAVES; ; ; ; ; 	The author(s) declare financial support was received for the research, authorship, and/or publication of this article. This work is a contribution to HABWAVE project LISBOA-01-0145-FEDER-031265, co-funded by EU ERDF funds, within the PT2020 Partnership Agreement and Compete 2020, and national funds through Fundac & atilde;o para a Ciencia e Tecnologia, I.P.(FCT, I.P.) also to AQUIMAR project MAR2020; MAR-02.01.01-FEAMP-017. This study had the support of FCT through the strategic projects UIDB/04292/2020 and UIDP/04292/2020 awarded to MARE and through project LA/P/0069/2020 granted to the Associate Laboratory ARNET, the strategic project UIDB/04326/2020 awarded to CCMAR. Thanks are also due for the financial support to CESAM by FCT/MCTES (UIDP/50017/2020+UIDB/50017/2020+LA/P/0094/2020), Partnership Agreement and Compete 2020. IG-M was supported by a postdoctoral fellowship from Xunta de Galicia, Spain (ref. ED481B-2019-074, 2019). 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DEC 8	2023	10								1270343	10.3389/fmars.2023.1270343	http://dx.doi.org/10.3389/fmars.2023.1270343			30	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	DV8M9		Green Published, gold			2025-03-11	WOS:001134948900001
J	Suc, JP; Fauquette, S; Warny, S; Jiménez-Moreno, G; Do Couto, D				Suc, Jean-Pierre; Fauquette, Severine; Warny, Sophie; Jimenez-Moreno, Gonzalo; Do Couto, Damien			Climate and Atlantic sea-level recorded in Southwestern Spain from 6.3 to 5.2 Ma. Inferences on the Messinian Crisis in the Mediterranean.	BSGF-EARTH SCIENCES BULLETIN			English	Article						Stratigraphy; palynology; climate; climatostratigraphic relationships; sea-level changes; two steps of the Messinian Crisis; Stratigraphie; palynologie; climat; correlations climatostratigraphiques; variations du niveau oceanique; deux stades de la Crise messinienne	SALINITY CRISIS; LATE MIOCENE; LAGO MARE; ALBORAN SEA; GUADALQUIVIR BASIN; APENNINE FOREDEEP; EROSIONAL SURFACE; RIFIAN CORRIDOR; EVOLUTION; INSIGHTS	The Mio-Pliocene succession of Andalusia on the Atlantic coast (Guadalquivir Basin) is known as one of the former stratotype candidate for the Andalusian Stage, proposed during the seventies as the last stage of the Miocene. Its type section is located in Carmona, east of Seville. Our investigation includes the drilling of three cored boreholes, which provide bio- and magnetic-stratigraphic data in complement to pre-existing industrial information, and a high-resolution palynological analysis (pollen grains, spores and dinoflagellate cysts). The pollen flora and its climatic quantification provide the mean to correlate the section to the oxygen isotope curve from the Montemayor-1 borehole, located about 80 km to the West of Carmona. The variations in the ratio between dinoflagellate cysts and pollen grains are used to identify high and low oceanic levels, consistently with a recent paleobathymetric reconstruction based on foraminifera: the two lowest levels being successively marked by the deposit of a littoral calcarenite (the Calizza Tosca Formation) then by a subaerial erosive episode. Based on the correlation with the Montemayor-1 regional drilling, the two major lowerings in oceanic level observed at Carmona are linked with the two episodes of the Messinian Crisis. The interlocking position of the high-energy sandstone deposits inscribed in the Messinian valley leads to an assessment of a drop in the global oceanic level of about 114 m at the beginning of the paroxysm of the Messinian Crisis, amplitude to be moderated with respect to the potential effect of isostatic readjustements due to the Messinian Crisis. Comparisons are discussed with the amplitude of the Messinian Erosional Surface in the West-Alboran Basin which potentially remained suspended and fed with Atlantic waters during the height of the crisis and isolated from the rest of the almost totally dried Mediterranean Basin. The quantified climate constructed from the pollen records confirms that dry conditions existed before the Messinian Crisis in Southern Mediterranean latitudes including the Atlantic side, making the Mediterranean Sea climatically predisposed to desiccation. Atlantic sea-level variations observed in the Guadalquivir region and measured at Carmona suggest that global glacio-eustatism somewhat facilitated the onset and completion of the Messinian Crisis in the Mediterranean Basin. At last, this work allows to discriminate two regional erosive events: the first one, dated at 5.60 Ma, of fluvial origin in relation with global eustasy; the second one, submarine, occurred just before 5.33 Ma, and referred to the strain exerted by the Guadalquivir olistostrome. La succession mio-pliocene d'Andalousie atlantique (bassin du Guadalquivir) est connue comme ancienne candidate pour le stratotype de l'Andalousien, propose comme dernier etage du Miocene dans les annees 70. Sa coupe-type est situee a Carmona, a l'est de Seville. Nos travaux comprennent notamment la realisation de trois forages carottes ou furent acquises des donnees bio- et magneto-stratigraphiques complementaires aux informations connues des recherches industrielles et, surtout, une analyse palynologique (grains de pollen et kystes de dinoflagelles) a haute resolution. La flore pollinique et la quantification climatique autorisent des correlations climatostratigraphiques avec la courbe delta 18O du forage Montemayor-1 implante pres de Huelva. Les variations du rapport entre kystes de dinoflagelles et grains de pollen permettent d'identifier les hauts et bas niveaux oceaniques en accord avec une recente estimation paleobathymetrique basee sur les foraminiferes, les deux plus bas niveaux etant successivement marques par le depot d'une calcarenite littorale (Formation de la Caliza Tosca) puis par un episode erosif subaerien. Apres correlation avec le forage Montemayor-1, ces deux baisses du niveau oceanique sont respectivement mises en correspondance avec les deux temps de la Crise messinienne. L'emboitement des depots greseux a haute energie inscrits dans la vallee messinienne conduit a evaluer une chute du niveau atlantique d'environ 114 m lors du paroxysme de la Crise messinienne, amplitude a moderer toutefois compte tenu du possible effet des rebonds isostatiques lies a la Crise messinienne. Des comparaisons sont discutees avec l'ampleur de l'erosion messinienne dans le bassin ouest-Alboran potentiellement reste suspendu et alimente en eaux atlantiques pendant le paroxysme de la crise et isole du reste du bassin mediterraneen quasi-totalement asseche. Les restitutions quantifiees du climat comparees entre la province atlantique et le domaine mediterraneen confirment les conditions xeriques des latitudes sud-mediterraneennes s.l. et ainsi la predisposition climatique de la Mediterranee a la dessiccation. Les variations du niveau atlantique observees dans la region du Guadalquivir et mesurees a Carmona suggerent que le glacio-eustatisme global a quelque peu contribue au declenchement et a l'achevement de la Crise messinienne en Mediterranee. Ce travail permet enfin de discriminer deux evenements erosifs regionaux : le premier a 5,60 Ma, d'origine fluviatile en relation avec l'eustatisme global, le second intervenu peu avant 5,33 Ma, sous-marin, lie aux contraintes exercees par l'olistostrome du Guadalquivir.	[Suc, Jean-Pierre; Do Couto, Damien] Sorbonne Univ, Inst Sci Terre, CNRS INSU, ISTeP UMR 7193, F-75005 Paris, France; [Fauquette, Severine] Univ Montpellier, ISEM, CNRS, IRD,EPHE, Montpellier, France; [Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA USA; [Jimenez-Moreno, Gonzalo] Univ Granada, Dept Estratig & Paleontol, Ave Fuentenueva S-N, Granada 18002, Spain	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Louisiana State University System; Louisiana State University; University of Granada	Suc, JP (通讯作者)，Sorbonne Univ, Inst Sci Terre, CNRS INSU, ISTeP UMR 7193, F-75005 Paris, France.	jeanpierre.suc@gmail.com	Fauquette, Severine/M-3686-2019; DO COUTO, Damien/HGT-7175-2022; Warny, Sophie/A-8226-2013; Jimenez-Moreno, Gonzalo/K-6753-2017; DO COUTO, Damien/W-9543-2018	Fauquette, Severine/0000-0003-0516-7734; Jimenez-Moreno, Gonzalo/0000-0001-7185-8686; DO COUTO, Damien/0000-0003-0589-208X; Suc, Jean-Pierre/0000-0002-5207-8622	CNRS-INSU; Total company; Elf-Aquitaine company	CNRS-INSU(Centre National de la Recherche Scientifique (CNRS)); Total company(Total SA); Elf-Aquitaine company	The late G. Clauzon actively contributed to two field trips, particularly in evidencing the valley fill including the Nested Sandstone Formation. E.J. Mayoral guided us on the field. P. Guenet handled the coring process. The late F. Gautier contributed to the coring campaign, especially in paleomagnetic logging and measurements in Grenoble. J. Pocachard and T. Thomas (LETI-CEA, Grenoble) contributed in providing the paleomagnetism logging material used in situ and access to the measurement bed in Grenoble. Some additional information on foraminifera and paleomagnetism were provided by F.J. Sierro and W. Krijgsman, respectively. The coring campaign was financially supported by CNRS-INSU, Total and Elf-Aquitaine companies. We particularly appreciated the comments and suggestions addressed by the two referees, P. Sternai and G. Booth-Rea.	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J	Quattrocchio, ME; Diaz, PE; Agüero, LS				Quattrocchio, Mirta E.; Diaz, Pablo E.; Aguero, Luis S.			The late Paleocene-Eocene interval of the Magallanes-Austral Basin (Chile-Argentina): Palynostratigraphy, paleoclimate and geochemical data	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Paleocene-eocene transition; Magallanes -austral basin; Palynostratigraphy; Paleoenvironment; Geochemistry	DINOFLAGELLATE CYST ASSEMBLAGES; TIERRA-DEL-FUEGO; THERMAL MAXIMUM; ENVIRONMENTAL-CHANGE; CHORRILLO CHICO; BOUNDARY EVENT; FORELAND BASIN; PUNTA PRAT; SEA-LEVEL; PATAGONIA	The Magallanes-Austral Foreland Basin preserves an important record of orogenesis and landscape evolution in the Patagonian Andes of Chile and Argentina. This paper evaluates the comparison between the thick Paleogene sequences in the Chilean Peninsula Brunswick (Chorrillo Chico and Agua Fresca formations) and the reduced Paleogene sequence (La Barca Formation) in the Punta Ainol locality, Argentina, by taking account of palynological and geochemical analyses. Warm and humid subtropical conditions (Subtropical Gondwanic Paleoflora) are inferred for the late Paleocene-Eocene interval studied. A new record of Lactoridaceae in the La Barca Formation expanded the known fossil range of this family in Patagonia. During the late Paleocene the Chorrillo Chico and La Barca formations would have been deposited mainly from hyperpycnal flows and this accumulation process continued until the Lutenian in the La Barca Formation. A relative rise in the sea level in the early Eocene would be recognized in both sections. In the middle Eocene a relative fall in the sea level would have occurred with increased terrigenous influx. The rate of sedimentation was similar in both sections during the Thanetian and Ypresian intervals according to the ages assigned by biostratigraphy, suggesting that the sedimentation rate would have been controlled mainly by relative changes in sea level during the Paleocene-Eocene transition. Paleoenvironmental changes during the Paleocene-Eocene transition were characterized at the La Barca Formation of the Punta Ainol section, considering the new geochemical and palynological data provided in this contribution.	[Quattrocchio, Mirta E.] Univ Nacl Sur, Dept Geol, Blanca, Argentina; [Diaz, Pablo E.; Aguero, Luis S.] Univ Nacl Sur, Inst Geol INGEOSUR, CONICET, Ave Alem 1253 Cuerpo B,B8000ICN, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Quattrocchio, ME (通讯作者)，Univ Nacl Sur, Dept Geol, Blanca, Argentina.	mquattro@criba.edu.ar			Secretary of Science and Technology at the National University of the South (SEGCyT) [PGI-24/H156.]	Secretary of Science and Technology at the National University of the South (SEGCyT)	Special thanks to Dr. Eduardo Olivero for the outcrops samples of the La Barca Formation. The author would like to thank the handling editor Dr. Francisco J. Vega, and reviewers Dr. Carlos Jaramillo, Dr. Andres Folguera and anonymous reviewer for their careful reading of our manuscript and their many insightful comments and suggestions, which significantly improved this paper. The Authors also thank to Gast on Otegui and Raul Guanco from the Geochemical Laboratory of Y-TEC (YPF Tecnologia) for geochemistry analysis. This work was supported by the Secretary of Science and Technology at the National University of the South (SEGCyT) under Grant [PGI-24/H156.-M.A. Martinez] .	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J	Zeng, YY; Sun, CH				Zeng, Yong-Yao; Sun, Chong-Hui			Magnetostratigraphy and Biostratigraphy of the Jurassic sedimentary sequences, Qiangtang Basin, revealed the initial time of the Lhasa-Qiangtang collision	APPLIED GEOPHYSICS			English	Article						Paleomagnetic ages; Biostratigraphy; Qiangtang Basin; Lhasa-Qiangtang collision	TIBETAN PLATEAU; NORTHERN TIBET; PALEOMAGNETIC INCLINATIONS; DINOFLAGELLATE CYSTS; TECTONIC EVOLUTION; SHALLOW BIAS; CONSTRAINTS; GEOCHRONOLOGY; GEOCHEMISTRY; INSIGHTS	The Qiangtang Basin, located in the Tibetan Plateau, is an appropriate area to verify the Lhasa-Qiangtang collision, which was recorded by the middle-upper part of the Yanshiping Group (the Xiali and Suowa Fms) in the basin. However, the chronology of the Xiali and Suowa Fms is HYPERLINK "javascript:;" controversial, which limits comprehending the timing of the Lhasa-Qiangtang collision. More importantly, HYPERLINK "javascript:;" oil HYPERLINK "javascript:;" shale and salt springs were exposed in the Xiali and Suowa Fms in the basin. 544 paleomagnetic samples were collected from the Yanshiping section in the basin in order to reveal the timing of the Lhasa-Qiangtang collision from the view of paleomagnetic ages of the two formations. However, we did not give credible magnetostratigraphic ages of the two formations because of ammonite fossils, a global primary standard for the Jurassic strata correlation, without being found in the last study. Yin (2016) revised the long-term HYPERLINK "javascript:;" controversial paleontological age of the Suowa Fm. from a Tithonian age of the Late Jurassic or a Berriasian age of the Early Cretaceous, to a Middle Bathonian-Middle Callovian age of the Middle Jurassic based on new ammonite fossils. Considering ammonite fossils as a powerful tool and a global primary standard for the Jurassic strata correlation, we attempted to correlate the last magnetostratigraphy with the GPTS 2012 again. Magnetostratigraphic ages of 164.0-160.2 Ma and 160.2-156.8 Ma for the Xiali and Suowa Fms are suggested, respectively. The timing of the Lhasa-Qiangtang collision (156.8-154.9 Ma) is revealed from the magnetostratigraphic ages and the zircon U-Pb age of the Xueshan Fm, 154.9 (+6.8/-1.6) Ma, overlying the Suowa Fm in the Yanshiping section.	[Zeng, Yong-Yao] Lanzhou Resources & Environm Voc Tech Univ, Lanzhou 730000, Peoples R China; [Sun, Chong-Hui] Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pro, Lanzhou 730000, Peoples R China	Lanzhou Resources & Environment Voc-Tech University; Lanzhou University	Zeng, YY (通讯作者)，Lanzhou Resources & Environm Voc Tech Univ, Lanzhou 730000, Peoples R China.	ruoshuizeng@126.com			National Basic Research Program of China [2011CB403003]	National Basic Research Program of China(National Basic Research Program of China)	This study was supported by the National Basic Research Program of China (Grant No. 2011CB403003). Professors Shuang Dai and Defei Yan from Lanzhou University are thanked for their constructive suggestions for magnetostratigraphic correlations and for identifying a biostratigraphical framework. We are grateful to the reviewer for their constructive and thoughtful comments. And Gang Niu, Song Wu, Jiaqiu Pan and Jiwei Yang are thanked for laboratory and fieldwork assistance.	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Geophys.	DEC	2023	20	4					572	591		10.1007/s11770-023-1046-7	http://dx.doi.org/10.1007/s11770-023-1046-7			20	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	MA8V9					2025-03-11	WOS:001191004100007
J	Vologina, EG; Sturm, M; Kulagina, NV; Astakhov, AS				Vologina, E. G.; Sturm, M.; Kulagina, N. V.; Astakhov, A. S.			Impact of Natural and Anthropogenic Factors on Late Holocene Sedimentation in the Chukchi Sea	IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS			English	Article						Chukchi Sea; bottom sediments; Cs-137 activity; modern sedimentation rates; grain size distribution; light and heavy minerals; magnetic susceptibility; pollen	BOTTOM SEDIMENTS; DIATOM; RECONSTRUCTION; GEOCHEMISTRY; DISPERSION; TRANSPORT; ACCIDENT; OCEAN; CORE	Late Holocene sediments have been recovered in a core from the central Chukchi Sea to reconstruct their accumulation conditions. The sediments consist mainly of terrigenous and just partly of biogenic material. Fine sand is dominated by up to 99.8% light fraction minerals, whereas heavy minerals account for not more than 1.4%. Results of magnetic susceptibility, related to the sand and heavy mineral content, decrease from the bottom to the top of the core. The species composition of pollen spectra varies insignificantly throughout the core and, on the whole, reflects the modern vegetation of the Chukchi Sea coast. The increased number of cysts of dinoflagellates and other aquatic palynomorphs, as well as some increased content of coarse-grained material at the upper part of the sediment core, is presumably caused by recent climate warming conditions. Two peaks of Cs-137 activity at the 7.5 and 1.5 cm in the core are related to radioactive fallout, caused by the accidents at the Chernobyl nuclear power plant in 1986 and the Fukushima nuclear power plant in 2011. The resulting sedimentation rates of 2.5-3 mm/yr correspond well to rates of sedimentation determined by 210Pb dating (2.0 mm/yr).	[Vologina, E. G.; Kulagina, N. V.] Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664033, Russia; [Sturm, M.] Swiss Fed Inst Aquat Sci & Technol, CH-8600 Dubendorf, Switzerland; [Astakhov, A. S.] Russian Acad Sci, Ilichev Pacific Oceanol Inst, Far East Branch, Vladivostok 690041, Russia	Russian Academy of Sciences; Irkutsk Science Centre of the Russian Academy of Sciences; Institute of Earth's Crust of Siberian Branch of the Russian Academy of Sciences; Swiss Federal Institutes of Technology Domain; Swiss Federal Institute of Aquatic Science & Technology (EAWAG); Russian Academy of Sciences	Vologina, EG (通讯作者)，Russian Acad Sci, Inst Earths Crust, Siberian Branch, Irkutsk 664033, Russia.	vologina@crust.irk.ru	Kulagina, Natalya/O-4667-2014		Russian Science Foundation [21-17-00081]; Russian Ministry of Higher Education and Science [121021700342-9];  [2018SD-KJ0104-3]	Russian Science Foundation(Russian Science Foundation (RSF)); Russian Ministry of Higher Education and Science; 	The study was supported by the Russian Science Foundation (project no. 21-17-00081). Expeditionary studies were supported by the Russian Ministry of Higher Education and Science (project no. 121021700342-9) and a grant from Shandong Province to the Qingdao National Laboratory of Marine Science and Technology (grant no. 2018SD-KJ0104-3). The study partially involved equipment of theCollective Use Center "Geodynamics and Geochronol-ogy" of the Institute of the Earth's Crust, Siberian Branch,Russian Academy of Sciences.	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Atmos. Ocean. Phys.	DEC	2023	59	12					1698	1708		10.1134/S0001433823110087	http://dx.doi.org/10.1134/S0001433823110087			11	Meteorology & Atmospheric Sciences; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Meteorology & Atmospheric Sciences; Oceanography	LN4F1					2025-03-11	WOS:001187462500006
J	Dehbozorgi, A; Maleki, S				Dehbozorgi, Afsaneh; Maleki, Saeed			Palynostratigraphy and Foraminiferal Stratigraphy of the Early Miocene Qom Formation in the Northeastern Margin of the Tethyan Seaway	PALEONTOLOGICAL JOURNAL			English	Article						benthic foraminifera; dinoflagellate cyst; palynology; Aquitanian; Burdigalian	FORE-ARC BASIN; CENTRAL IRAN; BENTHIC FORAMINIFERA; EARLY OLIGOCENE; BIOSTRATIGRAPHY; DEPOSITS; PALEOECOLOGY; NORTH; AREA; BOUNDARY	Lower Miocene strata are exposed in the northwest of Ashtian, in the Central Iran Zone. Biostratigraphy of the Qom Formation was investigated using dinoflagellate cyst and benthic foraminifera. The stratigraphic distribution of the dinocysts lead to the identification of two distinctive stratigraphically non-continuous palynozones viz., Caligodinium amiculum (late Aquitanian) and Cordosphaeridium cantharellus (early Burdigalian) zones. This biozonation is equivalent to that recognized in Northwest Europe. Moreover, the presence of such stratigraphically distinctive taxa as Borelis melo curdica, Meandropsina iranica, Elphidium sp. 14, and Miogypsina sp. enabled the identification of the two consecutive biozones: the Elphidium sp. 14-Miogypsina Assemblage Subzone and the Borelis melo group Meandropsina iranica Assemblage Zone. The late Aquitanian-Burdigalian age is collectively attributed, therefore, to the studied section. This age assignment is based on the dinocysts and foraminifer species compared with other stratigraphic sections. The close resemblance of the dinoflagellate cyst assemblages of the Qom Basin with Northwest Europe and the northwestern Tethys during the Oligocene-early Miocene indicates a marine connection and faunal exchange between the two regions.	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DEC	2023	57	7					833	847		10.1134/S0031030123070031	http://dx.doi.org/10.1134/S0031030123070031			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	Z2WO6					2025-03-11	WOS:001110732400005
J	Maleki, S				Maleki, Saeed			The life and scientific work of Ebrahim Ghasemi-Nejad (1960-2020)	PALYNOLOGY			English	Biographical-Item							KOPPEH-DAGH BASIN; PETROLEUM POTENTIAL EVALUATION; GURPI FORMATION; INTEGRATED BIOSTRATIGRAPHY; PLANKTONIC-FORAMINIFERA; SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; ABDERAZ FORMATION; ZAGROS MOUNTAINS; NE IRAN		[Maleki, Saeed] Museum Natl Hist Nat, UMR Hist Nat Homme Prehist 7194, Paris, France	Museum National d'Histoire Naturelle (MNHN)	Maleki, S (通讯作者)，Museum Natl Hist Nat, UMR Hist Nat Homme Prehist 7194, Paris, France.	saeed.maleki@edu.mnhn.fr	Maleki, Saeed/HNQ-7316-2023	Maleki, Saeed/0000-0003-2345-6652	Support Foundation of the University of Tehran	Support Foundation of the University of Tehran	During the writing of this obituary, the author had the honor of conducting several interviews with Dr. Sholeh Mansouri, the wife of the late Professor Ebrahim Ghasemi-Nejad. The author expresses gratitude for Dr. Mansouri's warm hospitality and generosity as well as her willingness to share her memories and insights about Professor Ghasemi-Nejad. Her patience and tolerance in answering my questions were invaluable in capturing a personal and insightful perspective on his life and legacy. The Support Foundation of the University of Tehran is also acknowledged for providing information about his donations and scholarship. The author expresses gratitude for the helpful comments provided by Dr. Haytham El Atfy to enhance this obituary. Dr. James Riding is also acknowledged for his assistance in publishing this work.	Allameh M, 2016, ARAB J GEOSCI, V9, DOI 10.1007/s12517-015-2111-1; [Anonymous], 1984, Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen; ASSERETO R, 1968, Rivista Italiana di Paleontologia e Stratigrafia, V74, P1; ASSERETO RICCARDO, 1966, RIV ITAL PALEONTOL STRATIGR, V72, P1133; Beiranvand B, 2013, GEOPERSIA, V3, P11; Beiranvand B, 2014, CR PALEVOL, V13, P235, DOI 10.1016/j.crpv.2013.10.003; Beiranvand B, 2013, REV BRAS PALEONTOLOG, V16, P5, DOI 10.4072/rbp.2013.1.01; Davtalab E, 2018, STRATIGRAPHY, V15, P47, DOI 10.29041/strat.15.1.47-66; Davtalab E, 2017, GEOPERSIA, V7, P153, DOI 10.22059/geope.2017.231253.648316; Farmani T, 2020, IRAN J EARTH SCI, V12, P54; Ghasemi-Nejad E., 1999, SCHWEIZERISCHE PAL O, V119, p130p; Ghasemi-Nejad E, 2024, PALAEOWORLD, V33, P374, DOI 10.1016/j.palwor.2023.04.003; Ghasemi-Nejad E, 2010, PALAEOGEOGR PALAEOCL, V291, P338, DOI 10.1016/j.palaeo.2010.03.005; Ghasemi-Nejad E, 2008, J MICROPALAEONTOL, V27, P125, DOI 10.1144/jm.27.2.125; Ghasemi-Nejad E, 2009, MAR PETROL GEOL, V26, P805, DOI 10.1016/j.marpetgeo.2008.05.005; Ghasemi-Nezhad E., 2021, AVAYE ZAMFIR, P150; Ghourchaei S, 2015, ARAB J GEOSCI, V8, P2153, DOI 10.1007/s12517-014-1276-3; Kimyai A., 1975, Geoscience and Man, V11, P117; Kimyai A., 1977, P 2 GEOL S IR, P191; Kimyai A., 1974, Jurassic plant microfossils from Iran, V3, P1; Mafi A, 2014, ARAB J GEOSCI, V7, P3683, DOI 10.1007/s12517-013-0976-4; Mazaheri-Johari M, 2022, PALAEOGEOGR PALAEOCL, V586, DOI 10.1016/j.palaeo.2021.110777; Mazaheri-Johari M, 2021, RIV ITAL PALEONTOL S, V127, P189, DOI 10.13130/2039-4942/15646; Mirzaloo M, 2012, GEOPERSIA, V2, P27; Mohammad S, 2019, ACTA GEOL SIN-ENGL, V93, P1885, DOI 10.1111/1755-6724.13823; Moshirfar Y, 2015, ARAB J GEOSCI, V8, P867, DOI 10.1007/s12517-013-1184-y; Nafarieh E, 2019, J FORAMIN RES, V49, P275, DOI 10.2113/gsjfr.49.3.275; Rabbani J, 2015, ARAB J GEOSCI, V8, P827, DOI 10.1007/s12517-013-1164-2; Rostami Masoud Asgharian, 2013, Open Journal of Geology, V3, P33; Sabbaghiyan H, 2020, REV PALAEOBOT PALYNO, V282, DOI 10.1016/j.revpalbo.2020.104308; Sarfi M, 2015, ARAB J GEOSCI, V8, P7245, DOI 10.1007/s12517-014-1712-4; Seyed-Emami K., 1971, GEOLOGICAL SURVEY IR, V19, P1; Sharfi M, 2024, CRETACEOUS RES, V153, DOI 10.1016/j.cretres.2023.105696; Wheeler J.W., 1990, Modern Geology, V14, P267; Yazdi-Moghadam M., 2021, CRETACEOUS RES, V126, P104885; Zarei E, 2015, ARAB J GEOSCI, V8, P4011, DOI 10.1007/s12517-014-1443-6; Zarei E, 2014, ARAB J GEOSCI, V7, P4265, DOI 10.1007/s12517-013-0993-3	38	0	0	0	0	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	APR 2	2024	48	2								10.1080/01916122.2023.2289575	http://dx.doi.org/10.1080/01916122.2023.2289575		DEC 2023	5	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	NG6Z7		Bronze			2025-03-11	WOS:001130246400001
J	Kuzmina, OB; Iakovleva, AI; Mychko, EV				Kuzmina, O. B.; Iakovleva, A. I.; Mychko, E. V.			The Age and Depositional Settings of the Upper Paleogene-Lower Neogene Kurshskaya Formation in its Stratotype Section (Kaliningrad Oblast) based on Palynological Data	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						pollen and spores; dinoflagellate cysts; latest Eocene; Oligocene; Miocene; Kaliningrad Oblast	DINOFLAGELLATE CYSTS; MIDDLE EOCENE; BELAYA RIVER; OLIGOCENE; MIOCENE; SUCCESSION; BOREHOLE; POLLEN; SPORE	The results of the palynological study of the Kurshskaya Formation stratotype (Primorsky quarry, Kaliningrad Oblast) are presented. The lower part of the Kurshskaya Formation (Member of "chocolate" clays) contains an assemblage of latest Eocene dinoflagellate cysts Areosphaeridium diktyoplokum, Glaphyrocysta semitecta, and Cordosphaeridium funiculatum. The formation is characterized by four spore-pollen assemblages: (1) latest Eocene Pinuspollenites-Inaperturopollenites-Sciadopityspollenites assemblage in the "chocolate" clays and in the lower part of brown sands; (2) early Oligocene Sequoiapollenites-Betulaepollenites betuloides assemblage in the lower part of the brown sands member; (3) early Oligocene Boehlensipollis hohli-Carpinipites carpinoides in the middle part of brown sands member; (4) late Oligocene-early Miocene Alnipollenites-Corylopollis assemblage in the upper part of the brown sands of the Kurshskaya Formation. In total, the Kurshskaya Formation is terminal Eocene-early Miocene in age. The lower part of the Zamland Formation, which overlies the Kurshskaya Formation, contains the presumably middle Miocene Pinuspollenites-Tricolporopollenites pseudocingulum-T. euphorii assemblage. Based on the obtained palynological data, the depositional settings at the end of the Eocene-Oligocene-early Miocene in the South Baltic region are reconstructed. The regression of the marine basin began as early as the end of the Priabonian, the climate was still quite warm and humid, close to subtropical. Mesophytic mixed coniferous-broad-leaved forests grew along the shores of the strait, lowlands were occupied by marsh vegetation. Cooling at the Eocene/Oligocene boundary resulted in the appearance of hemlock in plant communities and increase in the proportion of catkins (alder, birch, hornbeam). Presumably, in the late Oligocene-early Miocene, the proportion of small-leaved trees, especially alder and hazel, sharply increased in mesophytic forests, while the number of pine trees decreased. Wetter and warmer climatic conditions are assumed for the early Miocene: this time is characterized by an increase in the number of walnut, cypress, and Cyrillaceae. In the middle Miocene, the climate was still quite warm, but drier, and such moisture-loving species as Podocarpus, spruce, Glyptostrobus, and swamp cypress disappeared from plant communities.	[Kuzmina, O. B.] Russian Acad Sci, Siberian Branch, Trofimuk Inst Petr Geol & Geophys, Novosibirsk 630090, Russia; [Iakovleva, A. I.] Russian Acad Sci, Geol Inst, Moscow 119017, Russia; [Mychko, E. V.] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117218, Russia; [Mychko, E. V.] Immanuel Kant Balt Fed Univ, Sci & Educ Ctr Geoecol & Marine Resource Managemen, Kaliningrad 236041, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Shirshov Institute of Oceanology; Immanuel Kant Baltic Federal University	Kuzmina, OB (通讯作者)，Russian Acad Sci, Siberian Branch, Trofimuk Inst Petr Geol & Geophys, Novosibirsk 630090, Russia.	KuzminaOB@ipgg.sbras.ru	Kuzmina, Olga/I-9547-2018; Mychko, Eduard/V-1121-2017		The authors express their gratitude to M.I. Zatsepin, the General Director of the Federal State Unitary Enterprise "Yantarny Combine" for access to the Primorsky quarry, as well as to A.E. Korkin, the chief geologist of the "Yantarny Combine" and V.I. Alek	The authors express their gratitude to M.I. Zatsepin, the General Director of the Federal State Unitary Enterprise "Yantarny Combine" for access to the Primorsky quarry, as well as to A.E. Korkin, the chief geologist of the "Yantarny Combine" and V.I. Alek	The authors express their gratitude to M.I. Zatsepin, the General Director of the Federal State Unitary Enterprise "Yantarny Combine" for access to the Primorsky quarry, as well as to A.E. Korkin, the chief geologist of the "Yantarny Combine" and V.I. Alekseev, the researcher of the Institute of Oceanology, Russian Academy of Sciences (Kaliningrad) for assistance in sampling. The authors are grateful to L.F. Bobkova and E.V. Tupitsina (IPGG SB RAS) for the chemical treatment of palynological samples, as well as to reviewers N.K. Lebedeva, O.V. Shurekova, and M.E. Bylinskaya for valuable remarks and comments that improved the quality of the paper.	Akhmet'ev MA, 2001, STRATIGR GEO CORREL+, V9, P373; Akhmetiev M.A., 1978, Trans. USSR Geol. 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Ukraine, V8, P68	41	4	4	1	3	PLEIADES PUBLISHING INC	NEW YORK	PLEIADES HOUSE, 7 W 54 ST, NEW YORK,  NY, UNITED STATES	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	DEC	2023	31	6					657	675		10.1134/S0869593823060072	http://dx.doi.org/10.1134/S0869593823060072			19	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	Y3ZG5					2025-03-11	WOS:001104675300010
J	Rohozin, Y; Ljung, K				Rohozin, Yevhenii; Ljung, Karl			Palaeoenvironmental changes in eastern Crimea over the last 7600 years inferred from a multi-proxy study of a sediment archive from Lake Chokrak	HOLOCENE			English	Article						coastal processes; Holocene; human impact; hypersaline lake; organic geochemistry; palaeoclimate; palynology; vegetation history; XRF	NON-POLLEN PALYNOMORPHS; WESTERN BLACK-SEA; DINOFLAGELLATE CYSTS; ENVIRONMENTAL-CHANGE; MEDITERRANEAN SEA; HOLOCENE CLIMATE; VEGETATION; MARINE; HISTORY; REGION	The study presents a multi-proxy archive from hypersaline coastal Lake Chokrak in eastern Crimea, a steppe region which is particularly susceptible to moisture fluctuations. XRF, organic carbon and nitrogen, and palynological analyses are used to reconstruct the evolution of the lake and landscape development around it and to provide information about the driving forces behind those changes, such as climate and human impact. The findings show that the basin was an open marine bay between 7640 and 5500 cal. yr BP. After 5500 cal. yr BP, the low rates of sea-level rise led to gradual infilling of the basin. The prevalence of mesic herb-grass steppe around the site, as well as the expansion of broad-leaved trees in the Crimean mountains, indicate relatively warm and humid climate conditions during the Mid-Holocene. Elemental proxies and marine NPPs point to a transition to lagoonal conditions from 4270 cal. yr BP. The progressive shallowing of the basin was accompanied by the spread of more xeric Artemisia-grass steppe, which suggests a shift to arid conditions. The occurrence of cereal pollen from 3660 cal. yr BP may indicate the first signs of cultivation in the study area. The active build-up of a sand barrier from 3000 cal. yr BP led to a gradual separation of the basin from the sea. By 900 cal. yr BP, the fully-formed sand barrier resulted in a transformation of the lagoon into a hypersaline lake. The closing of the lagoon was accompanied by an expansion of halophytic communities around the site. Human-induced vegetation changes became more pronounced with the development of agrarian and pastoral activities around the site from ca. 750 cal. yr BP.	[Rohozin, Yevhenii] Taras Shevchenko Natl Univ Kyiv, Fac Geog, Kiev, Ukraine; [Rohozin, Yevhenii; Ljung, Karl] Lund Univ, Dept Geol, Lund, Sweden; [Rohozin, Yevhenii] Taras Shevchenko Natl Univ Kyiv, Fac Geog, Volodymyrska St 64-13, UA-01601 Kiev, Ukraine	Ministry of Education & Science of Ukraine; Taras Shevchenko National University of Kyiv; Lund University; Ministry of Education & Science of Ukraine; Taras Shevchenko National University of Kyiv	Rohozin, Y (通讯作者)，Taras Shevchenko Natl Univ Kyiv, Fac Geog, Volodymyrska St 64-13, UA-01601 Kiev, Ukraine.	yevhenii.rohozin@knu.ua	Rohozin, Yevhenii/L-7861-2018	Ljung, Karl/0000-0002-4290-7933; Rohozin, Yevhenii/0000-0001-6288-4655	Swedish Institute (SI)	Swedish Institute (SI)	The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This study was funded by a Visby Scholarship for PhD and postdoctoral studies by the Swedish Institute (SI).	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J	Yedema, YW; Donders, T; Peterse, F; Sangiorgi, F				Yedema, Yord W.; Donders, Timme; Peterse, Francien; Sangiorgi, Francesca			Dinoflagellate cyst and pollen assemblages as tracers for marine productivity and river input in the northern Gulf of Mexico	JOURNAL OF MICROPALAEONTOLOGY			English	Article							SOUTH CHINA SEA; SURFACE SEDIMENTS; ORGANIC-MATTER; CONTINENTAL-MARGIN; COASTAL WATERS; TOKYO-BAY; BLACK-SEA; TRANSPORT; HOLOCENE; EUTROPHICATION	Both marine dinoflagellate cysts and terrestrially derived pollen and spores are abundant in coastal sediments close to river mouths, making sediment records from such settings ideal to simultaneously study land-ocean climate interactions, marine productivity patterns and freshwater input over time. However, few studies consider the combined calibration of these palynological proxies in modern coastal sediments offshore from rivers, which is needed to strengthen the interpretation of paleoreconstructions. Here, we analyze the palynological content of marine surface sediments along land-sea transects off the Mississippi and Atchafalaya river mouths in the northern Gulf of Mexico (GoM) and test three palynological indices which are often employed in the paleo-domain: (i) the abundance of cysts of heterotrophic and autotrophic dinoflagellates (dinocysts) as a tracer for primary productivity ( H / A ratio) and (ii) the ratio between non-bisaccate pollen and bisaccates ( P / B ) as well as (iii) the ratio between pollen (excluding bisaccates) and dinocysts ( P / D ), which are both tracers for river input and distance to the coast.Our results show that dinoflagellate cysts are most abundant on the shelf, where heterotrophic dinocyst species dominate coastal assemblages in reach of the river plume, while autotrophic taxa are more present in the oligotrophic open ocean. This is clearly reflected in decreasing H / A values further offshore. Individual dinocyst taxa also seem to inhabit specific niches along an onshore-offshore transect, linked to nutrient availability and proximity to the turbid river plume. The highest pollen concentrations are found close to the Mississippi river mouth and mostly represent a mixture of local coastal and upstream vegetation, whereas bisaccate pollen was most abundant further offshore of the Mississippi river. Multivariate redundancy analysis (RDA) performed on both pollen and dinocyst assemblages, a set of environmental parameters, and the three palynological ratios showed that net primary productivity was the most important variable influencing the dinocyst assemblages, likely as the result of nutrient input. Additionally, the RDA confirmed that the H / A ratio indeed seems to track primary productivity, while the P / B ratio results in a robust indicator for distance to the coast, and the P / D ratio better reflects river input. Together, our data confirm and further specify the suitability of these three palynological ratios in river-dominated coastal margins as proxies for (past) marine productivity and distance to the coast and river.	[Yedema, Yord W.; Peterse, Francien; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands; [Donders, Timme] Univ Utrecht, Dept Phys Geog, NL-3584 CB Utrecht, Netherlands	Utrecht University; Utrecht University	Yedema, YW (通讯作者)，Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands.	y.w.ijedema@uu.nl	Peterse, Francien/AAY-1473-2021; Peterse, Francien/H-5627-2011	Yedema, Yord/0000-0001-7852-6799; Peterse, Francien/0000-0001-8781-2826; Sangiorgi, Francesca/0000-0003-4233-6154	Netherlands Earth System Science Centre; Netherlands Earth System Science Centre (NESSC)	Netherlands Earth System Science Centre; Netherlands Earth System Science Centre (NESSC)	We thank the editor, Debra Willard, and one anonymous reviewer for their comments and feedback, which improved the manuscript. This work was carried out under the program of the Netherlands Earth System Science Centre (NESSC). We thank the scientists and crew aboard the R/V Pelagia cruise 64PE467. 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J	Frieling, J; van Roij, L; Kleij, I; Reichart, GJ; Sluijs, A				Frieling, Joost; van Roij, Linda; Kleij, Iris; Reichart, Gert-Jan; Sluijs, Appy			Single-species dinoflagellate cyst carbon isotope fractionation in core-top sediments: environmental controls, CO<sub>2</sub> dependency and proxy potential	BIOGEOSCIENCES			English	Article							HARMFUL ALGAL BLOOMS; CONCENTRATING MECHANISMS; ORGANIC-MATTER; DISCRIMINATION; PHYTOPLANKTON; TEMPERATURE; DIOXIDE; DEGRADATION; DELTA-C-13; PALEOCENE	Sedimentary bulk organic matter and various molecular organic components exhibit strong CO2-dependent carbon isotope fractionation relative to dissolved inorganic carbon sources. This fractionation (epsilon(p)) has been employed as a proxy for paleo-pCO(2). Yet, culture experiments indicate that CO2-dependent epsilon(p) is highly specific at genus and even species level, potentially hampering the use of bulk organic matter and non-species-specific organic compounds. In recent years, significant progress has been made towards a CO2 proxy using controlled growth experiments with dinoflagellate species, also showing highly species-specific epsilon(p) values. These values were, however, based on motile specimens, and it remains unknown whether these relations also hold for the organic-walled resting cysts (dinocysts) produced by these dinoflagellate species in their natural environment. We here analyze dinocysts isolated from core tops from the Atlantic Ocean and Mediterranean Sea, representing several species (Spiniferites elongatus, S. (cf.) ramosus, S. mirabilis, Operculodinium centrocarpum sensu Wall and Dale (1966) (hereafter referred to as O. centrocarpum) and Impagidinium aculeatum) using laser ablation-nano-combustion-gas-chromatography-isotope ratio mass spectrometry (LA/nC/GC-IRMS). We find that the dinocysts produced in the natural environment are all appreciably more C-13-depleted compared to the cultured motile dinoflagellate cells, implying higher overall epsilon(p) values, and, moreover, exhibit large isotope variability. Where several species could be analyzed from a single location, we often record significant differences in isotopic variance and offsets in mean delta C-13 values between species, highlighting the importance of single-species carbon isotope analyses. The most geographically expanded dataset, based on O. centrocarpum, shows that epsilon(p) correlates significantly with various environmental parameters. Importantly, O. centrocarpum shows a CO2-dependent epsilon(p) above similar to 240 mu atm pCO(2). Similar to other marine autotrophs, relative insensitivity at low pCO(2) is in line with active carbon-concentrating mechanisms at low pCO(2), although we here cannot fully exclude that we partly underestimated epsilon(p) sensitivity at low pCO(2) values due to the relatively sparse sampling in that range. Finally, we use the relation between epsilon(p) and pCO(2) in O. centrocarpum to propose a first pCO(2) proxy based on a single dinocyst species.	[Frieling, Joost; van Roij, Linda; Kleij, Iris; Reichart, Gert-Jan; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonlaan 8, NL-3584CB Utrecht, Netherlands; [Reichart, Gert-Jan] NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst, Landsdiep 4, NL-1797SZ T Horntje, Texel, Netherlands; [Frieling, Joost] Univ Oxford, Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Oxford	Frieling, J (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonlaan 8, NL-3584CB Utrecht, Netherlands.; Frieling, J (通讯作者)，Univ Oxford, Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England.	joost.frieling@earth.ox.ac.uk	Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018	Frieling, Joost/0000-0002-5374-1625; Reichart, Gert-Jan/0000-0002-7256-2243	European Research Council; Netherlands Organisation for Scientific Research (NWO) [771497]; European Research Council (ERC); Netherlands Earth System Science Centre (NESSC); Dutch Ministry of Education, Culture and Science	European Research Council(European Research Council (ERC)); Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); European Research Council (ERC)(European Research Council (ERC)); Netherlands Earth System Science Centre (NESSC); Dutch Ministry of Education, Culture and Science	We thank Arnold van Dijk, Michiel Kienhuis and Helen de Waard (Utrecht University) for technical and analytical assistance. Appy Sluijs acknowledges funding from Netherlands Organisation for Scientific Research (NWO) no. ALWOP.223 and a European Research Council (ERC) Consolidator grant 771497 (SPANC). 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. We thank three anonymous reviewers for their insightful and highly constructive comments and Steven Bouillon for editorial handling.	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J	Nascimento, MC; Lima, M; Terra, GJS; Alves, MAO; Bruno, MDR				Nascimento, Maria Caroline; Lima Filho, Mario; Terra, Gerson J. S.; Alves, Marcella A. O.; Bruno, Mauro D. R.			Microfacies analysis and paleoenvironmental interpretation of the late Aptian-Albian (Early Cretaceous) carbonates of the Riachuelo Formation in the Sergipe Sub-basin, northeastern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Aptian carbonates; Sergipe-Alagoas basin; Riachuelo formation; Microbialites	BASIN; ATLANTIC; CLIMATE; STRATIGRAPHY; EVOLUTION; PALEOCEANOGRAPHY; BIOSTRATIGRAPHY; PALEOGEOGRAPHY; PRECIPITATION; BIOGEOGRAPHY	The beginning of the drift phase, in the Aptian-Albian transition, marked the development of marine conditions in the South Atlantic Ocean, characterized by the deposition of evaporites, followed by the development of carbonate platforms. The carbonate rocks of this interval were deposited in a passive margin context as part of the Riachuelo Formation in the Sergipe-Alagoas Basin, northeastern Brazil. The objective of present study was to analyze the microfacies of the Aptian-Albian interval in the northern portion of Sergipe State, near the city of Pacatuba. The mainly carbonates of two cores were investigated and five carbonate microfacies were identified: oncoidal rudstone, bioclastic rudstone, oncoidal packstone, peloidal packstone/wackestone, and mudstone with planktonic bioelements that suggest the paleoenvironments were relatively shallow marine. The microfacies were dominated by oncoids in almost every sample, which occurred in association with stromatolites. The biostratigraphic results were based on palynomorphs and calcareous nannofossils. The palynomorphs assemblages indicated a late Aptian age. Paleoecological results of these fossil groups show paleoenvironmental conditions of the shallow waters with proximal characteristics, with the predominance of pollens and spores associated with rare dinoflagellates and ascidians. A striking feature was the presence of authigenic glauconite which filled skeletal cavities and partially replaced the oncoids and their nuclei, mostly in the oncoidal packstone facies. Together, these findings suggest that the samples formed at the basal portion of the Riachuelo Formation in a transgressive systems tract, corresponding to the first depositional stage of the Riachuelo Formation.	[Nascimento, Maria Caroline] Univ Fed Pernambuco UFPE, Ctr Tecnol & Geociencias, Lab Geol Sedimentar & Ambiental, Programa Posgrad Geociencias, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Lima Filho, Mario] Univ Fed Pernambuco UFPE, Ctr Tecnol & Geociencias, Dept Geol, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Terra, Gerson J. S.] Observ Nacl ON, Rio De Janeiro, RJ, Brazil; [Alves, Marcella A. O.] Univ Fed Pernambuco UFPE, Dept Geol, Lab Micropaleontol Aplicada LAGESE LITPEG, Recife, PE, Brazil; [Bruno, Mauro D. R.] Unisinos Univ, Univ Vale do Rio dos Sinos, Inst Tecnolo Paleoceanog & Mudancas Climat Itt Oce, Sao Leopoldo, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade do Vale do Rio dos Sinos (Unisinos)	Nascimento, MC (通讯作者)，Univ Fed Pernambuco UFPE, Ctr Tecnol & Geociencias, Lab Geol Sedimentar & Ambiental, Programa Posgrad Geociencias, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	mariacaroline@gmail.com	Bruno, Mauro/HGC-0717-2022; Nascimento, Mariá/A-5707-2012	Rodrigues Bruno, Mauro Daniel/0000-0001-5290-9855	UFPE/ANP/FINEP (Brazil) Human Resources Program [PRH 47]; Federal University of Pernambuco, (UFPE), Brazil [PRH 47]; Laboratory of Sedimentary and Environmental Geology (LAGESE)	UFPE/ANP/FINEP (Brazil) Human Resources Program; Federal University of Pernambuco, (UFPE), Brazil; Laboratory of Sedimentary and Environmental Geology (LAGESE)	To the UFPE/ANP/FINEP (Brazil) Human Resources Program (PRH 47) for granting the master's scholarship to Maria Caroline do Nascimento. The authors also thank PRH 47, the Federal University of Pernambuco, (UFPE), Brazil and the Laboratory of Sedimentary and Environmental Geology (LAGESE) for the logistical and financial support to carry out this work, as well as the reviewers for the pertinent and constructive corrections. We would like to thank Enelise Katia Piovesan, coordinator of the LMA-UFPE Micropaleontology Laboratory, for providing the entire structure for analyzes with palynomorphs, as well as for allowing the use of SEM, in which the microbial features were considered under the supervision of Robbyson Melo. The authors also thank Gerson Fauth for providing the necessary structure to carry out analyzes with calcareous nannofossils at itt Oceaneon - Technological Institute of Paleoceanography and Climate Change - UNISINOS. We thank the owners of the drill sites, Mizu Cimentos - Pacatuba (Sergipe State), for all their support and for kindly contributing to the project. We also thank researchers Fernanda Luft-Souza (UNISINOS), Edilma de Jesus Andrade (UFS), Sonia Agostino (UFPE), Osvaldo Correia (UFPE), Rick Souza de Oliveira (UFOPA), Virginio Henrique de Miranda Lopes Neumann (UFPE), and Zenilda Batista (UFAL) for their constructive comments, discussions, and suggestions. This manuscript has benefited from the constructive comments of two anonymous reviewers, as well as the editor Francisco J. Vega.	AMOROSI A, 1995, J SEDIMENT RES B, V65, P419; Antonietto L.S., 2015, Tese de Doutorado; Asmus H., 1973, OCEAN BASIN MARGIN, P87, DOI [DOI 10.1007/978-1-4684-3030-1_3, 10.1007/978-1-4684-3030-1_3]; Azevedo RLM., 2004, B GEOCI NCIAS PETROB, V12, P231; Baldermann A, 2013, CLAY CLAY MINER, V61, P258, DOI 10.1346/CCMN.2013.0610307; Bandeira Jr A.N, 1978, Petrobras. 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South Am. Earth Sci.	JAN	2024	133								104688	10.1016/j.jsames.2023.104688	http://dx.doi.org/10.1016/j.jsames.2023.104688		NOV 2023	19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	CH3K7					2025-03-11	WOS:001124322100001
J	Regaudie-de-Gioux, A; Latorre, L; Basterretxea, G				Regaudie-de-Gioux, A.; Latorre, L.; Basterretxea, G.			Phytoplankton metabolism in a stratified nearshore ecosystem with recurrent harmful algal blooms (HABs)	JOURNAL OF PLANKTON RESEARCH			English	Article						HABs; primary production; respiration; nearshore waters; Mediterranean Sea	TIME-SERIES; ALEXANDRIUM-MINUTUM; RECENT SEDIMENTS; CLIMATE-CHANGE; RESTING CYSTS; GROWTH-RATES; COASTAL; VARIABILITY; NITROGEN; MICROZOOPLANKTON	The coastal ocean is experiencing changes in its physical and chemical properties that strongly affect planktonic metabolism assemblages and, in some cases, favor the occurrence of harmful algal blooms (HABs). Here we analyze the variations in phytoplankton biomass, gross and net primary production (NCP) as well as community respiration (CR) at two nearshore sampling sites (P1 and P2) located at a Mediterranean beach where high biomass HABs are recurrent. At P1, the most exposed site, phytoplankton chlorophyll was generally low, whereas dinoflagellates outbreaks of the genus Gymnodinium and Alexandrium were recurrent during summer at P2 spanning for 10-20 days. During bloom episodes, NCP increased up to 10-fold (>80 mmol O2 m(-3) day(-1)). Contrastingly, variation in CR only reached an average of 1.8-fold the rates of non-bloom conditions. Remarkably, although the enhanced NCP:CR ratio suggests net autotrophic population growth, production per unit biomass at P1 and P2 was not significantly different. Our results indicate that although summer conditions favor the necessary primary production enhancement leading to HAB occurrences, the short-term dynamics driving high biomass episodes are not driven by metabolic variations but instead are governed by subtle accumulative processes of some flagellate species in the nutrient-rich nearshore environment.	[Regaudie-de-Gioux, A.] Ifremer Dyneco Pelagos, FRench Inst Sea Res, 1625 Route Sainte Anne, F-29280 Plouzane, France; [Latorre, L.; Basterretxea, G.] CSIC, UIB, Imedea, Dept Marine Ecol, Miquel Marques 21, Esporles 07190, Balearic Island, Spain	Ifremer; Consejo Superior de Investigaciones Cientificas (CSIC); ATTITUS Educacao; Universitat de les Illes Balears	Regaudie-de-Gioux, A (通讯作者)，Ifremer Dyneco Pelagos, FRench Inst Sea Res, 1625 Route Sainte Anne, F-29280 Plouzane, France.	aregaudi@ifremer.fr; llatorreconservation@gmail.com; gotzon@imedea.uib-csic.es	Regaudie-de-Gioux, Aurore/AAC-1816-2022; Basterretxea, Gotzon/D-2314-2011; Regaudie-de-Gioux, Aurore/G-8116-2014	Basterretxea, Gotzon/0000-0001-7466-1360; Regaudie-de-Gioux, Aurore/0000-0001-9015-8589	HYDROALGAL [RTC -2016-4812-5]; Incorporacion de personal investigador -Ministry of Innovation, Research and Tourism of the Balearic Island Government	HYDROALGAL; Incorporacion de personal investigador -Ministry of Innovation, Research and Tourism of the Balearic Island Government	This research was financed by HYDROALGAL (RTC -2016-4812-5) project and partially carried out within the framework of the activities of the Spanish Government through the "Maria de Maeztu Centre of Excellence" accreditation to IMEDEA (CSIC-UIB) (CEX2021-001198-M). A.R-de-G. was supported by a post-doctoral fellowship "Incorporacion de personal investigador" funded by the Ministry of Innovation, Research and Tourism of the Balearic Island Government.	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Plankton Res.	DEC 8	2023	45	6					785	793		10.1093/plankt/fbad039	http://dx.doi.org/10.1093/plankt/fbad039		NOV 2023	9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	AC5B8					2025-03-11	WOS:001109217800001
J	de Espronceda, PM; Rodríguez-Barreiro, I; Pérez-Barreiro, M; Bádenas, B; Canudo, I; Puértolas-Pascual, E; Santos, AA; Diez, JB				de Espronceda, P. Martinez; Rodriguez-Barreiro, I.; Perez-Barreiro, M.; Badenas, B.; Canudo, I.; Puertolas-Pascual, E.; Santos, A. A.; Diez, J. B.			Palynostratigraphical review of the K-Pg boundary from the Ibero-Armorican Island: New data from the Maastrichtian dinosaur outcrop Veracruz 1 (Pyrenees, NE Iberian Peninsula)	CRETACEOUS RESEARCH			English	Review						Palynology; K-T boundary; K-Pg biostratigraphy; Palynological dating; Paleoecological reconstruction; SW Europe	SOUTH-CENTRAL PYRENEES; CRETACEOUS-TERTIARY BOUNDARY; MASS EXTINCTION; TREMP FORMATION; FOSSIL RECORD; SPAIN; BASIN; CATALONIA; NORTH; CLIMATE	The palynostratigraphy of the K-Pg boundary interval in SW Europe has been a subject of ongoing debate, despite numerous palynological studies in the region. To address this, we review previous publications and conduct analysis of new deposits to establish a palynostratigraphical chart. A total of 40 palynological studies within the Normapolles palynological province were reexamined to elucidate key taxa restricted to the Cretaceous (K-taxa), to the Maastrichtian-Danian interval (KPg-taxa) and those restricted to the Paleogene (Pg-taxa). Eventually, we propose 18 key taxa to differentiate a Maastrichtian from a Danian palynological assemblage within the Normapolles Province. Afterward, a palynostratigraphical analysis was carried out in Veracruz 1 (Aragonese Pyrenees), one of the more modern dinosaur bearing sites of Europe. The palynological assemblage corresponded to an upper Maastrichtian age and was composed by pteridophyte spores, gymnosperms, angiosperms, dinoflagellate cysts, algae, and fungal spores. It was predominated by angiosperm pollen (Liliaceae, post-Normapolles, and triporate pollen). The plant communities in Veracruz 1 seem to be characterized by plants from an open coastal forest prevailed by Liliaceae flowering herbs and Juglandaceae/Myricaceae dicotyledonous trees and shrubs thriving in temperate-warm paleoclimate. The Gondwanan botanical influence was also supported by the presence of Bacumorphomonocolpites sp., as this taxon was previously recorded in other upper Maastrichtian deposits from Europe.(c) 2023 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY-NC license (http://creativecommons.org/licenses/by-nc/4.0/).	[de Espronceda, P. Martinez; Rodriguez-Barreiro, I.; Diez, J. B.] Univ Vigo, Dept Xeociencias Marinas & Ordenac Terr, Vigo 36310, Spain; [de Espronceda, P. Martinez; Perez-Barreiro, M.; Badenas, B.; Canudo, I.; Puertolas-Pascual, E.] Univ Zaragoza, Fac Ciencias, Grp Aragosaurus IUCA, C Pedro Cerbuna 12, Zaragoza 50009, Aragon, Spain; [Rodriguez-Barreiro, I.; Diez, J. B.] Univ Vigo, Ctr Invest Marina, BASAN, Vigo 36310, Spain; [Santos, A. A.] Swedish Museum Nat Hist, Dept Palaeobiol, SE-10405 Stockholm, Sweden; [Santos, A. A.] UNAM, Inst Geol, Estn Reg Noroeste ERNO, Hermosillo 83000, Mexico	Universidade de Vigo; University of Zaragoza; Universidade de Vigo; CIM UVIGO; Swedish Museum of Natural History; Universidad Nacional Autonoma de Mexico	Rodríguez-Barreiro, I (通讯作者)，Univ Vigo, Dept Xeociencias Marinas & Ordenac Terr, Vigo 36310, Spain.		Bádenas, Beatriz/Q-2955-2019; Santos, Artai/AAM-4202-2021; Puertolas Pascual, Eduardo/A-3309-2012	Canudo Sanagustin, Jose Ignacio/0000-0003-1732-9155; Santos Lopez, Artai Anton/0000-0002-2399-8825; Puertolas Pascual, Eduardo/0000-0003-0759-7105; Badenas Lago, Beatriz Maria/0000-0003-1112-524X; Rodriguez-Barreiro, Ivan/0000-0002-0938-662X	Spanish Ministry of Science and Innovation [PID2021-122612OB-I00]; Aragon Regional Government (DGA) [E18_23R]; Xunta de Galicia (Spain) [ED431C-2019/28]; European Social Fund- European Union [ED481A-2020/175]; UNAM (Mexico) [UNAM- DGAPA 2023-2024]; Swedish Research Council [VR 2022-03920]; Universidade de Vigo/CISUG; Swedish Research Council [2022-03920] Funding Source: Swedish Research Council	Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); Aragon Regional Government (DGA); Xunta de Galicia (Spain)(Xunta de Galicia); European Social Fund- European Union; UNAM (Mexico)(Universidad Nacional Autonoma de Mexico); Swedish Research Council(Swedish Research Council); Universidade de Vigo/CISUG; Swedish Research Council(Swedish Research Council)	The authors would like to thank the handling editor (Eduardo Koutsoukos) and two anonymous reviewers because of their constructive suggestions, which improved the quality of this paper. In addition, we are grateful to Luis Miguel Sender for his collaboration during the sampling process. Funding for this research was provided by the Spanish Ministry of Science and Innovation (project PID2021-122612OB-I00) , the Aragon Regional Government (DGA) (E18_23R Aragosaurus: Recursos Geologicos y Paleo-ambientales) , and the Xunta de Galicia (Spain) through project ED431C-2019/28. IRB was supported by a predoctoral fellowship from the Xunta de Galicia (Spain) and the European Social Fund- European Union (ref.: ED481A-2020/175) . AAS is supported by a postdoctoral fellowship from the UNAM (Mexico, ref.: UNAM- DGAPA 2023-2024) and a subsequent fellowship funded from the Swedish Research Council (ref.: VR 2022-03920) . 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Res.	FEB	2024	154								105757	10.1016/j.cretres.2023.105757	http://dx.doi.org/10.1016/j.cretres.2023.105757		NOV 2023	16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	AO1Y4		Green Published, hybrid			2025-03-11	WOS:001119327200001
J	Curren, E; Leong, SCY				Curren, Emily; Leong, Sandric Chee Yew			Plankton assemblages from microplastics of tropical coastal environments reveal high diversity and evidence of toxic species	MARINE ENVIRONMENTAL RESEARCH			English	Article						Transport; Vector; Microplastics; Community; Singapore; Sustainability	CYANOBACTERIUM LYNGBYA-MAJUSCULA; HARMFUL ALGAL BLOOMS; DOCOSAHEXAENOIC-ACID; PLASTIC DEBRIS; BACTERIAL ASSEMBLAGES; MICROBIAL COMMUNITIES; RED-TIDE; MARINE; ALEXANDRIUM; SHELLFISH	Microplastics are a major constituent of plastic waste and are of an increasing global concern. Although microplastics are prevalent in marine ecosystems, the characterisation of plankton communities has been largely neglected in this aspect, especially in tropical ecosystems. To better understand the role of microplastics as a carrier of harmful plankton in marine ecosystems, epiplastic plankton communities in tropical marine ecosystems were studied from beach sediments along the Johor and Singapore Straits. Complementary analysis of microscopy and high throughput sequencing of the 16S rRNA (V3-V4) and 18S (V4) rRNA regions provided evidence that the plastisphere provided an appropriate environment to host a wide range of planktonic organisms. An average of 781 OTUs were identified across the three sampling sites. The structures of plankton communities were distinct across the sampling sites and were generally dominated by dinoflagellates, fungi and chlorophytes. We demonstrate that marine microplastics serve as microhabitats that are a host to harmful phytoplankton species, including viable resting cysts of dinoflagellates. Furthermore, plastics isolated from the location with the greatest anthropogenic influence demonstrated the greatest plankton diversity. This study presents evidence of diverse toxic plankton species present on the plastisphere and highlights its importance as a vector of the transport of harmful opportunistic species in relation to anthropogenic influence, in the marine environment.	[Curren, Emily; Leong, Sandric Chee Yew] Natl Univ Singapore, Trop Marine Sci Inst, St Johns Isl Natl Marine Lab, 18 Kent Ridge Rd, Singapore 119227, Singapore	National University of Singapore	Curren, E (通讯作者)，Natl Univ Singapore, Trop Marine Sci Inst, St Johns Isl Natl Marine Lab, 18 Kent Ridge Rd, Singapore 119227, Singapore.	e0013223@u.nus.edu	Leong, Sandric/F-5304-2013		National University of Singapore	National University of Singapore(National University of Singapore)	This work was partially supported by funds awarded to Dr. Sandric Leong through the National University of Singapore and was made possible because of the support of members of Team HABs.	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Environ. Res.	JAN	2024	193								106251	10.1016/j.marenvres.2023.106251	http://dx.doi.org/10.1016/j.marenvres.2023.106251		NOV 2023	10	Environmental Sciences; Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Toxicology	Z5UH4	37952304				2025-03-11	WOS:001112717600001
J	Suzuki, KW; Dinh, HT				Suzuki, Keita W.; Dinh, Hanh T.			Bottom-up effects of variable winter weather conditions on phytoplankton dynamics in an enclosed bay: implications for ecological responses to climate change	JOURNAL OF PLANKTON RESEARCH			English	Article						diatom bloom; grazing pressure; nutrient supply; snowmelt; wind mixing	COASTAL PLANKTONIC DIATOMS; RESTING-STAGE CELLS; MAIZURU BAY; SKELETONEMA BACILLARIOPHYCEAE; SPECIES COMPOSITION; FOOD CONCENTRATION; NERITIC COPEPODS; ACARTIA-OMORII; FEEDING RATES; SPRING BLOOM	To investigate phytoplankton dynamics in response to variable winter weather conditions along the Sea of Japan, we conducted daily sampling in enclosed Maizuru Bay in five winters and found distinctive differences between 2016/2017 and 2018/2019. A clear diatom bloom occurred through the water column in moderately cold/snowy 2016/2017, whereas in exceptionally warm/snow-free 2018/2019 a small peak of dinoflagellates occurred only in the subsurface. Nutrient concentrations changed drastically depending on freshwater discharge and diatom growth in 2016/2017, showing a contrast with constant nutrient concentrations in 2018/2019. Copepod densities were similar to 10 times higher in 2016/2017 than in 2018/2019, indicating bottom-up effects in 2016/2017. As the absence of a diatom bloom from 2018/2019 can be attributed neither to nutrient limitation nor to grazing pressure, we hypothesize that wind mixing is a key factor triggering a diatom bloom. Within the five winters, clear diatom blooms were found only after strong winds and heavy precipitation including snowfall. Wind mixing would possibly promote the germination/rejuvenation of viable resting stage cells as inocula for a diatom bloom, while the growth and maintenance are supported by nutrient supply through freshwater discharge. In Maizuru Bay, winter production is likely activated by harsh weather conditions characteristic of this region.	[Suzuki, Keita W.] Kyoto Univ, Field Sci Educ & Res Ctr, Maizuru Fisheries Res Stn, Maizuru 6250086, Japan; [Suzuki, Keita W.; Dinh, Hanh T.] Kyoto Univ, Grad Sch Global Environm Studies, Lab Ecosyst Linkages & Human Soc, Oiwake Cho,Sakyo Ku, Kyoto 6068502, Japan	Kyoto University; Kyoto University	Suzuki, KW (通讯作者)，Kyoto Univ, Field Sci Educ & Res Ctr, Maizuru Fisheries Res Stn, Maizuru 6250086, Japan.; Suzuki, KW (通讯作者)，Kyoto Univ, Grad Sch Global Environm Studies, Lab Ecosyst Linkages & Human Soc, Oiwake Cho,Sakyo Ku, Kyoto 6068502, Japan.	suzuki.keita.3r@kyoto-u.ac.jp; dthanh@ria1.org			We express our gratitude to the present and former staff and students of Maizuru Fisheries Research Station of Kyoto University for their assistance with field sampling and laboratory analysis. Monitoring data of temperature and salinity were kindly provid; Kyoto Fishery Cooperative Association; Fuji SLI Chlorophyll Laboratory; Grants-in-Aid for Scientific Research [20K06206] Funding Source: KAKEN	We express our gratitude to the present and former staff and students of Maizuru Fisheries Research Station of Kyoto University for their assistance with field sampling and laboratory analysis. Monitoring data of temperature and salinity were kindly provid; Kyoto Fishery Cooperative Association; Fuji SLI Chlorophyll Laboratory; 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 our gratitude to the present and former staff and students of Maizuru Fisheries Research Station of Kyoto University for their assistance with field sampling and laboratory analysis. Monitoring data of temperature and salinity were kindly provided by Kyoto Fishery Cooperative Association. High-purity chlorophyll a was generously offered as an analytical standard by Fuji SLI Chlorophyll Laboratory.	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Plankton Res.	DEC 8	2023	45	6					815	831	fbad046	10.1093/plankt/fbad046	http://dx.doi.org/10.1093/plankt/fbad046		NOV 2023	17	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	AC5B8		Green Submitted			2025-03-11	WOS:001103529000001
J	Hou, SN; Stap, LB; Paul, R; Nelissen, M; Hoem, FS; Ziegler, M; Sluijs, A; Sangiorgi, F; Bijl, PK				Hou, Suning; Stap, Lennert B.; Paul, Ryan; Nelissen, Mei; Hoem, Frida S.; Ziegler, Martin; Sluijs, Appy; Sangiorgi, Francesca; Bijl, Peter K.			Reconciling Southern Ocean fronts equatorward migration with minor Antarctic ice volume change during Miocene cooling	NATURE COMMUNICATIONS			English	Article							OFFSHORE WILKES LAND; SEA-LEVEL; SHEET SENSITIVITY; SUBTROPICAL FRONT; TEMPERATURE; CLIMATE; MIDDLE; EVOLUTION; VARIABILITY; INSIGHTS	Gradual climate cooling and CO2 decline in the Miocene were recently shown not to be associated with major ice volume expansion, challenging a fundamental paradigm in the functioning of the Antarctic cryosphere. Here, we explore Miocene ice-ocean-climate interactions by presenting a multi-proxy reconstruction of subtropical front migration, bottom water temperature and global ice volume change, using dinoflagellate cyst biogeography, benthic foraminiferal clumped isotopes from offshore Tasmania. We report an equatorward frontal migration and strengthening, concurrent with surface and deep ocean cooling but absence of ice volume change in the mid-late-Miocene. To reconcile these counterintuitive findings, we argue based on new ice sheet modelling that the Antarctic ice sheet progressively lowered in height while expanding seawards, to maintain a stable volume. This can be achieved with rigorous intervention in model precipitation regimes on Antarctica and ice-induced ocean cooling and requires rethinking the interactions between ice, ocean and climate. Hou et al. propose, based on dinocysts, clumped isotopes and ice sheet modelling, that during Miocene cooling, the Antarctic ice sheet progressively lowered in height while expanding seawards, to maintain a relatively stable volume.	[Hou, Suning; Paul, Ryan; Hoem, Frida S.; Ziegler, Martin; Sluijs, Appy; Sangiorgi, Francesca; Bijl, Peter K.] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Stap, Lennert B.] Univ Utrecht, Inst Marine & Atmospher Res Utrecht, Utrecht, Netherlands; [Nelissen, Mei] NIOZ Royal Netherlands Inst Sea Res, Texel, Netherlands	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Hou, SN (通讯作者)，Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands.	s.hou@uu.nl	Ziegler, Martin/N-9699-2013; Sluijs, Appy/B-3726-2009	Hou, Suning/0000-0002-8902-6367; Bijl, Peter/0000-0002-1710-4012; Nelissen, Mei/0009-0002-6802-2495; Sangiorgi, Francesca/0000-0003-4233-6154; Stap, Lennert/0000-0002-2108-3533; Ziegler, Martin/0000-0003-3198-6434; Hoem, Frida/0000-0002-8834-6799	ERC Starting Grant [802835]	ERC Starting Grant(European Research Council (ERC))	We thank Mariska Hoorweg, Natasja Welters, Giovanni Dammers, Desmond Eefting and Arnold van Dijk of the GeoLab for laboratory assistance. We thank IODP and scientists of ODP Leg 189, and technicians at KCC in Kochi, Japan for the help with sampling. We are grateful to Tobias Agterhuis, Ilja Kocken and Elena Dominguez Valdes for insightful discussion regarding clumped isotopes. This research is funded by ERC Starting Grant 802835 to Peter K. Bijl.	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Commun.	NOV 9	2023	14	1							7230	10.1038/s41467-023-43106-4	http://dx.doi.org/10.1038/s41467-023-43106-4			12	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	Y1QK3	37945579	Green Published, gold			2025-03-11	WOS:001103080000029
J	Santiago, G; Carvalho, MD; Ramos, RRC; Scheffler, SM				Santiago, Gustavo; Carvalho, Marcelo de Araujo; Ramos, Renato Rodriguez Cabral; Scheffler, Sandro Marcelo			Paleoenvironmental changes recorded in the Santa Marta Formation (Santonian-Campanian, Upper Cretaceous), James Ross Island, Antarctica, inferred from palynofacies analyses	CRETACEOUS RESEARCH			English	Article						Palynofacies; Santonian-Campanian; Antarctic Peninsula; Paleoenvironments	SEDIMENTARY ORGANIC-MATTER; LARSEN-BASIN; STRATIGRAPHY; CARBONATES; EVOLUTION; RECONSTRUCTION; LITHOFACIES; ASSEMBLAGES; SUCCESSION; PENINSULA	The Santa Marta Formation (Santonian-Campanian; James Ross Island, Antarctic Peninsula) is part of one of the most complete sedimentary sequences in the Southern Hemisphere. Paleoenvironmental changes recorded in the formation are reflected in the stratigraphic distribution of sedimentary organic matter in the Lachman Crags and Herbert Sound members. Fifty-three samples from the Lachman Crags section and ten samples from the Herbert Sound section were prepared using standard non-oxidative methods for palynofacies. Analyses were performed using transmitted white light and fluorescence microscopy to identify the groups and subgroups of sedimentary organic matter: non-opaque non-biostructured and biostructured opaque particles, membrane fragments, degraded and non-degraded cuticles, spores, pollen grains, fungal spores, Botryococcus, Palambages, dinoflagellates cysts, amorphous organic matter, pseudoamorphous (product of disintegration of macrophyte tissues) and resins. Three palynofacies associations are distinguished: terrestrial, opaque, and marine palynomorphs. Based on stratigraphically restricted cluster analysis (CONISS), three intervals have been identified: Interval 1, at the base of the Lachman Crags section, conspicuously dominated by the terrestrial palynofacies association. Interval 2, the middle portion of the Lachman Crags section, is marked by alternating terrestrial and opaque palynofacies associations. Interval 3, which coincides with the Herbert Sound section, is distinguished by an abrupt increase in marine elements. The composite section shows progressive transgression, accompanied by a decrease in continental elements, culminating in an open marine environment towards the top of the section.(c) 2023 Elsevier Ltd. All rights reserved.	[Santiago, Gustavo; Carvalho, Marcelo de Araujo] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Lab Paleoecol Vegetal LAPAV, Museu Nacl, BR-20940040 Rio De Janeiro, Brazil; [Ramos, Renato Rodriguez Cabral] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Museu Nacl, Setor Estratigra fia, Rio De Janeiro, Brazil; [Scheffler, Sandro Marcelo] Univ Fed Rio deJaneiro, Dept Geol & Paleontol, Lab Paleoinvertebrados LAPIN, Museu Nacl, BR-20940040 Rio De Janeiro, Brazil; [Santiago, Gustavo; Carvalho, Marcelo de Araujo; Ramos, Renato Rodriguez Cabral; Scheffler, Sandro Marcelo] CNPq PROANTAR, FLORANTAR, Projeto Paleoflora Peninsula Antartica, Brasilia, DF, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Santiago, G (通讯作者)，Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Lab Paleoecol Vegetal LAPAV, Museu Nacl, BR-20940040 Rio De Janeiro, Brazil.	gustavo.santiago@ymail.com	Scheffler, Sandro/S-3869-2019; Carvalho, Marcelo/G-8463-2015	Rodriguez Cabral Ramos, Renato/0000-0003-4023-6301	Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq]) [557347/2005-0, 442765/2018-5]	Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq])(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This project was primarily funded by the Brazilian National Council for Scientific and Technological Development (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq] grant nos. 557347/2005-0 and 442765/2018-5) . We wish to thank the Brazilian Navy for logistical and technical support during the expedition to Antarctica. The authors thank the anonymous reviewer and Editor for helpful suggestions.	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Res.	FEB	2024	154								105718	10.1016/j.cretres.2023.105718	http://dx.doi.org/10.1016/j.cretres.2023.105718		NOV 2023	13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	Z3ZE3					2025-03-11	WOS:001111485200001
J	Kim, JH; Park, BS; Kim, JH				Kim, Joo-Hwan; Park, Bum Soo; Kim, Jin Ho			Comprehensive understanding of the life history of harmful raphidophyte <i>Heterosigma akashiwo</i>: Integrating <i>in situ </i>and <i>in vitro</i> observations	HARMFUL ALGAE			English	Article						Heterosigma akashiwo; Harmful alga; Raphidophyceae; Life history; Life cycle; Sexual reproduction; Hologamete; Homothallism; Zygote (large cell); Multiple cells; Cell cluster; Cyst cluster	RED TIDE FLAGELLATE; CHATTONELLA-MARINA RAPHIDOPHYCEAE; DINOFLAGELLATE COCHLODINIUM-POLYKRIKOIDES; MARGALEF DINOPHYCEAE; OVATA RAPHIDOPHYCEAE; MOLECULAR PHYLOGENY; PIGMENT COMPOSITION; CYST FORMATION; GEN.-NOV.; MORPHOLOGY	Heterosigma akashiwo (Raphidophyceae) is widely recognized as a species responsible for harmful algal blooms worldwide. The species has long been speculated to possess a more complex life history, attributed to the diverse morphological variations observed during cell cultivation. However, the understanding of its life history has remained insufficient due to limitations in observing transitions between life cycle stages in vitro and challenges associated with in situ investigations. In this study, a combination of in vitro (laboratory-based) and in situ (field -based) observations was employed to define the life cycle stages of H. akashiwo and elucidate the pathways of transition between these stages. Notably, novel homothallic sexual reproduction processes involving the fusion of hologametes and the subsequent formation of zygotes were observed for the first time in vitro. These zygotes were found to either divide into vegetative cells (Pathway I) or undergo enlargement, resulting in the formation of multiple cells with multiple nuclei (Pathway II). Furthermore, this study provides the first documentation of large cells and cell clusters in situ , including intermediate stages referred to as large cells with ongoing cyto-plasmic division that serve as a bridge between these two cell types. The observed zygotes in vitro exhibited a large size (21.9-51.8 mu m) and multinucleated characteristics, similar to the large cells (38.2-45.8 mu m) and cell clusters observed in situ. This finding suggests that the large cells observed in situ were zygotes undergoing cell division to form cell clusters (Pathway III). Moreover, based on the striking similarities in cell morphology and nuclear size between the cells comprising the cell cluster (2.7-4.4 mu m) and the cyst clusters of this species, along with the synchronized germination characteristics of cyst clusters, it is proposed that the cell cluster serves as a precursor to cysts. By integrating the in situ and in vitro observations, this study provides a comprehensive un-derstanding of the previously poorly understood life history of H. akashiwo.	[Kim, Joo-Hwan; Park, Bum Soo] Hanyang Univ, Coll Nat Sci, Dept Life Sci, Seoul 04763, South Korea; [Kim, Joo-Hwan] Minist Environm, Govt Complex Sejong, Sejong 30103, South Korea; [Park, Bum Soo] Hanyang Univ, Hanyang Inst Biosci & Biotechnol, Seoul 04763, South Korea; [Park, Bum Soo] Hanyang Univ, Res Inst Convergence Basic Sci, Seoul 04763, South Korea; [Kim, Jin Ho] Hanyang Univ, Hanyang Inst Adv BioConvergence, Seoul 04763, South Korea; [Kim, Jin Ho] Jeju Natl Univ, Coll Ocean Sci, Dept Earth & Marine Sci, Jeju 63243, South Korea	Hanyang University; Hanyang University; Hanyang University; Hanyang University; Jeju National University	Park, BS (通讯作者)，Hanyang Univ, Coll Nat Sci, Dept Life Sci, Seoul 04763, South Korea.; Kim, JH (通讯作者)，Jeju Natl Univ, Coll Ocean Sci, Dept Earth & Marine Sci, Jeju 63243, South Korea.	parkbs@hanyang.ac.kr; kimj@jejunu.ac.kr	Kim, Se Young/GSE-5296-2022; PARK, Bum Soo/W-3178-2017	Kim, Joo-Hwan/0000-0002-2172-9357; PARK, Bum Soo/0000-0002-5441-6779	National Research Foundation of Korea (NRF) - Korea Government (MSIT) [2022R1C1C1003582, RS -2023-00209356]; Marine Biotics - Ministry of Ocean and Fisheries, Korea [20210469]; Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) - Ministry of Education [2019R1A6A1A10072987]; Korea Institute of Marine Science & Technology (KIMST) - Ministry of Oceans and Fisheries [RS -2023-00256330]	National Research Foundation of Korea (NRF) - Korea Government (MSIT)(National Research Foundation of KoreaMinistry of Science, ICT & Future Planning, Republic of KoreaMinistry of Science & ICT (MSIT), Republic of Korea); Marine Biotics - Ministry of Ocean and Fisheries, Korea; Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) - Ministry of Education(Ministry of Education (MOE), Republic of KoreaNational Research Foundation of Korea); Korea Institute of Marine Science & Technology (KIMST) - Ministry of Oceans and Fisheries(Korea Institute of Marine Science & Technology Promotion (KIMST))	From the outset of this research, we extend our profound respect and heartfelt gratitude to Dr. Myung-Soo Han, who consistently provided valuable insights and imparted invaluable inspiration. This research was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea Government (MSIT) (No. 2022R1C1C1003582 and RS -2023-00209356) , the Marine Biotics project (20210469) funded by the Ministry of Ocean and Fisheries, Korea, the Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) funded by the Ministry of Education (2019R1A6A1A10072987) , and the Korea Institute of Marine Science & Technology (KIMST) funded by the Ministry of Oceans and Fisheries (RS -2023-00256330, Development of risk managing technology tackling ocean and fisheries crisis around Korean Peninsula by Kuroshio Current) .	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J	Hohmann, S; Kucera, M; de Vernal, A				Hohmann, Sabrina; Kucera, Michal; de Vernal, Anne			Disentangling environmental drivers of subarctic dinocyst assemblage compositional change during the Holocene	CLIMATE OF THE PAST			English	Article							SEA-SURFACE CONDITIONS; WALLED DINOFLAGELLATE CYSTS; ZOOPLANKTON FECAL PELLETS; NORTHERN NORTH-ATLANTIC; DISKO BUGT AREA; WEST GREENLAND; LABRADOR SEA; BAFFIN-BAY; FORAMINIFERAL ASSEMBLAGES; PALEOCEANOGRAPHIC CHANGES	Analysis of compositional changes in fossil organic-walled dinoflagellate cyst (dinocysts) assemblages is a widely used tool for the quantitative reconstruction of past environmental parameters. This approach assumes that the assemblage composition is significantly related to the reconstructed environmental parameter, which requires an independent correlation between the assemblage and the variable, meaning that the variable explains a dimension of the assemblage variance that is not also explained by other parameters. Theoretically, dinocyst assemblages can be used to reconstruct multiple environmental variables. However, there is evidence that primary and subordinate drivers for assemblage compositions regionally differ, and it remains unclear whether a significant relationship to specific parameters in the present ocean always implies that this relationship is significant in fossil assemblages, questioning if past changes in these multiple parameters can be reconstructed simultaneously from fossil assemblages. Here, we analysed a local subset of the Northern Hemisphere dinocyst calibration dataset (n = 1968), including samples from the Baffin Bay area (n = 421), and evaluated the benefits of a local versus a more regional or global calibration for the environmental reconstruction of Baffin Bay oceanography during the Holocene. We determined the dimensionality of the dinocyst ecological response and identified environmental drivers in the Baffin Bay area for the modern dataset. We analysed four existing Holocene records along a north-south transect in the area and evaluated the statistical significance of downcore reconstructions by applying the local and global datasets with different techniques: the modern analogue technique (MAT), the weighted average partial least square (WA-PLS) and maximum likelihood (ML). We evaluated reconstructions tested as significant in light of the existing state of knowledge about West Greenland's Holocene palaeoceanography. Our analyses imply that present-day and Holocene dinocyst assemblages in the Baffin Bay area are primarily driven by salinity changes; other parameters were less important in driving assemblage compositions, and their contribution differed among the studied records. We show that the objectively occurring and temporally coherent shifts in dinocyst assemblages in the Holocene of Baffin Bay can be robustly interpreted only by transfer functions that are locally calibrated. Transfer functions based on the broad Northern Hemisphere calibration yielded many insignificant environmental reconstructions. At the same time, we show that even in the local calibration, not all parameters that appear to significantly affect dinocyst assemblages in the calibration dataset can be meaningfully reconstructed in the fossil record. A thorough evaluation of the calibration dataset and the significance of downcore applications is necessary to reveal the region-specific information contained in dinocyst assemblage composition.	[Hohmann, Sabrina; Kucera, Michal] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [de Vernal, Anne] Univ Quebec Montreal, Ctr Geotop, CP 8888, Montreal, PQ H3C 3P8, Canada	University of Bremen; University of Quebec; University of Quebec Montreal	Hohmann, S (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany.	hohmannlls@gmail.de	Kucera, Michal/ABH-6065-2020; de Vernal, Anne/D-5602-2013; Kucera, Michal/B-9277-2009	Kucera, Michal/0000-0002-7817-9018	Deutsche Forschungsgemeinschaft [IRTG 1904]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	This research has been supported by the Deutsche Forschungsgemeinschaft (grant no. IRTG 1904). The article processing charges for this open-access publication were covered by the University of Bremen.	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OCT 26	2023	19	10					2027	2051		10.5194/cp-19-2027-2023	http://dx.doi.org/10.5194/cp-19-2027-2023			25	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	LU4A8		Green Submitted, gold			2025-03-11	WOS:001189289300001
J	Paine, B; Armbrecht, L; Bolch, C; Mcminn, A; Hallegraeff, GM				Paine, Bradley; Armbrecht, Linda; Bolch, Christopher; Mcminn, Andrew; Hallegraeff, Gustaaf M.			Dinoflagellate cyst distribution over the past 9 kyrs BP from offshore east Tasmania, southeast Australia	PALYNOLOGY			English	Article						palaeoclimate; ocean currents; sea level rise; dinoflagellate cysts; trophic dynamics; Tasmania; Australia	SURFACE SEDIMENTS; GYMNODINIUM-CATENATUM; MARINE-SEDIMENTS; RESTING CYSTS; SEASONAL VARIABILITY; GENUS ALEXANDRIUM; FALKLAND TROUGH; COASTAL WATERS; BALLAST WATER; TOKYO-BAY	Southeastern Australia's marine waters are notably warming, surpassing global averages. This region has emerged as a strategic location for researching planktic microfossils, particularly dinoflagellate cysts, in modern and Late Quaternary sediments, offering crucial insights into the biophysical properties of mid-latitude waters. This study examined cyst distribution in marine sediment cores near Maria Island, Tasmania, southeastern Australia, up to 9000 years before present (kyrs BP). Dominant cysts included Protoceratium reticulatum, Protoperidinium spp. (P. avellana, P. conicum, P. oblongum, P. subinerme, P. shanghaiense), and Spiniferites spp. (S. bulloideus, S. hyperacanthus, S. membranaceus, S. mirabilis, S. pachydermus, and S. ramosus). Inshore, Spiniferites spp. constituted a higher proportion (up to 61%), while offshore was dominated by P. reticulatum (up to 80%). Impagidinium spp. and Nematosphaeropsis labyrinthus were exclusively found offshore and displayed increased abundance from similar to 6 kyrs BP, suggesting a shift from a shallow to a deep-water habitat. Alexandrium tamarense species complex cysts were present over 140 years inshore and approaching 9 kyrs BP offshore, indicating a longstanding endemic presence. Gymnodinium catenatum cysts were detected exclusively inshore from similar to 50 years ago, indicating a relatively recent bloom phenomenon. The East Australian Current's limited southward reach is suggested by the absence of the warm-water cyst-producing taxon Lingulodinium polyedra. Similarly, the non-detection of the cold-water species Spiniferites antarctica and Impagidinium pallidum reflects Subtropical Front boundaries against subantarctic incursions from the south. In contrast to coccolithophores in the same core, no noticeable shift from cold to warm-water dinoflagellate cyst species was observed. This documentation of dinoflagellate cysts aids in predicting environmental impacts on local communities and beyond.	[Paine, Bradley; Armbrecht, Linda; Bolch, Christopher; Mcminn, Andrew; Hallegraeff, Gustaaf M.] Univ Tasmania UTAS, Inst Marine & Antarctic Studies, Battery Point, Tas, Australia; [Armbrecht, Linda] Australian Ctr Excellence Antarctic Sci ACEAS, Battery Point, Tas, Australia; [Paine, Bradley] Univ Tasmania UTAS, Inst Marine & Antarctic Studies, 20 Castray Esplanade, Battery Point, Tas 7004, Australia	University of Tasmania; University of Tasmania	Paine, B (通讯作者)，Univ Tasmania UTAS, Inst Marine & Antarctic Studies, 20 Castray Esplanade, Battery Point, Tas 7004, Australia.	bradley.paine@utas.edu.au		Paine, Bradley/0000-0003-3908-9877	Australian Research Council [H0025318]; Australian Research Council (ARC Discovery Project) [DP170102261]; Australian Research Council (ARC) Discovery Early Career Researcher Award (DECRA) Fellowship [DE210100929]	Australian Research Council(Australian Research Council); Australian Research Council (ARC Discovery Project)(Australian Research Council); Australian Research Council (ARC) Discovery Early Career Researcher Award (DECRA) Fellowship(Australian Research Council)	The authors wish to thank the crew and the on-ship scientific team of RV Investigator voyage IN2018_T02 during core collection (2018 MNF Grant H0025318). In addition, we thank Prof. Henk Heijnis (ANSTO) for contributions to funding and logistical support for this project, Dr Craig Woodward for guiding sediment dating analysis and palynology slide preparation, and Dr Sandrin Feig at UTAS Central Science Laboratory for access and assistance with SEM facilities. This study was funded through the Australian Research Council (ARC Discovery Project DP170102261). L.A. was supported by an Australian Research Council (ARC) Discovery Early Career Researcher Award (DECRA) Fellowship (DE210100929). Finally, the authors would like to thank the reviewers of the initial manuscript submission for their valuable and informative feedback that has led to the much-improved final version presented here.	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J	Soliman, A; El Atfy, H				Soliman, Ali; El Atfy, Haytham			The history of palynology in Egypt	PALYNOLOGY			English	Article						palynology; Egypt; history; annotated bibliography	NORTHERN WESTERN-DESERT; TUNIS 1X BOREHOLE; ANGIOSPERM POLLEN; CRETACEOUS PALYNOSTRATIGRAPHY; EASTERN DESERT; DAKHLA OASIS; NILE DELTA; BIOSTRATIGRAPHY; PALYNOMORPHS; PALEOENVIRONMENT	This contribution marks the achievements made in the past decades by a group of mainly Egyptian palynologists. The data generated covers a long-time span from the Precambrian to the Holocene of Egypt. Previously published results are devoted primarily to the study of many exploration wells and outcrop sections. Comprehensive studies were carried out on a range of palynomorph groups including spores and pollen, algae and prasinophytes, dinoflagellate cysts, acritarchs, scolecodonts, chitinozoans, and other miscellaneous forms as well as palynofacies. Particular attention is given to the history of palaeopalynology. This study has identified three main phases. The results of the first phase were limited, as the knowledge of palynology in Egypt was poorly known from 1959 until 1979. Between 1980 and 2000, which represents the second or shaping phase, an intensive study of surface and subsurface material was carried out. The third phase (2000 until now) provides the academic and commercial expansion of palynological research in Egypt, where palynology can have immediate application in petroleum exploration studies. In the first phase, the application of palynology was seriously hampered by the limited extent of the published data. Only 27 works emerged by the end of 1979. A considerable acceleration was noted in the second phase when palynological research was established in many national institutions and started to play a considerable role in petroleum exploration. Beyond academia, some of the operating oil companies started to set up palynological laboratories and staff as part of biostratigraphy teams. These included, for example, GPC, Khalda Petroleum Company with a focus on the north Western Desert, and GUPCO with a focus on the Gulf of Suez, and most of the results obtained were incorporated with the internal data on the well files. During the period 2000-2009, especially when palynofacies studies were incorporated, the progress and the direction of palynological research changed. This allowed for a more accurate reconstruction of the depositional process and eventually a palaeobiogeographical history mainly for the Cretaceous, which is an important target for hydrocarbon exploration in Egypt. From 2010 onwards, the number of publications has clearly grown and reached 23 publications in 2020. Such a high pace of development seems to have been at the expense of basic research comprising taxonomy and biostratigraphy, something that might negatively impact the quality of research and also researchers, especially early career researchers. The change brought about through this phase by integrating organic geochemistry, sedimentology, and other disciplines may, however, have left a positive impact, principally in terms of international collaborations and expansion of palynological applications beyond the standard academic cluster. Important highlights and outputs, and prospective forthcoming developments and recommendations pertaining to Egyptian palynology generally (and in each phase) are discussed.	[Soliman, Ali] Tanta Univ, Fac Sci, Geol Dept, Tanta, Egypt; [El Atfy, Haytham] Univ Munster, Inst Geol & Palaeontol, Palaeobotany Grp, Munster, Germany; [El Atfy, Haytham] Mansoura Univ, Fac Sci, Geol Dept, Mansoura, Egypt; [El Atfy, Haytham] Univ Munster, Inst Geol & Palaeontol Palaeobotany, Heisenbergstr 2, D-48149 Munster, Germany	Egyptian Knowledge Bank (EKB); Tanta University; University of Munster; Egyptian Knowledge Bank (EKB); Mansoura University; University of Munster	El Atfy, H (通讯作者)，Univ Munster, Inst Geol & Palaeontol Palaeobotany, Heisenbergstr 2, D-48149 Munster, Germany.	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J	Luostarinen, T; Ribeiro, S; Zimmermann, HH; Kvorning, AB; Heikkilä, M				Luostarinen, Tiia; Ribeiro, Sofia; Zimmermann, Heike H.; Kvorning, Anna B.; Heikkilae, Maija			Single-cell DNA from West Greenland marine sediments suggests presence of <i>Protoperidinium tricingulatum</i> in the Arctic	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Arctic sea-ice proxies; dinoflagellate cysts; Islandinium; LSU rDNA; phylogenetic analyses; Protoperidinium	CYST-THECA RELATIONSHIP; WALLED DINOFLAGELLATE CYST; MOTILE STAGE RELATIONSHIPS; SEA-SURFACE CONDITIONS; SP-NOV; PHYLOGENETIC POSITIONS; NORTHERN-HEMISPHERE; HIGH-LATITUDES; SP. NOV.; DINOPHYCEAE	Spiny brown dinoflagellate cysts are commonly used as sea-ice indicators in the Arctic, but their biological affinities are not well known. We present the first indication of hitherto temperate Protoperidinium tricingulatum in the Arctic based on single-cell LSU rDNA sequencing from sediments of the Disko Bay-Vaigat Sound, West Greenland. The morphological similarity of the sequenced cyst morphotype to the sea-ice indicator Islandinium? cezare morphotype 1 (Journal of Quaternary Science, 16, 2001 and 621) is striking. The morphology of the isolated cysts, as well as those observed in the total cyst assemblage following standard palynological preparation, both resemble either I.? cezare morphotype 1 or P. tricingulatum, suggesting that the specimens may in fact be close morphological variants of the same species. In addition, nine LSU rDNA sequences were obtained from morphological variants assigned to Islandinium minutum s.l.: including both subspecies minutum and subspecies barbatum. The two subspecies could not be differentiated based on partial LSU rDNA sequencing. Overall, Arctic spiny brown dinoflagellate cyst species may be morphologically more diverse and taxonomically more complex than shown earlier and further genetic and morphological studies are needed. Importantly, the value of cysts as palaeoecological indicators depends on a sound understanding of their biological affinity and taxonomy.	[Luostarinen, Tiia; Heikkilae, Maija] Univ Helsinki, Fac Biol & Environm Sci, Ecosyst & Environm Res Program, Environm Change Res Unit ECRU, Helsinki, Finland; [Luostarinen, Tiia; Heikkilae, Maija] Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, Helsinki, Finland; [Ribeiro, Sofia; Zimmermann, Heike H.; Kvorning, Anna B.] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Copenhagen, Denmark; [Luostarinen, Tiia] Univ Helsinki, Fac Biol & Environm Sci, Ecosyst & Environm Res Programme, Environm Change Res Unit ECRU, POB 65, Viikinkaari 1, Helsinki 00014, Finland	University of Helsinki; University of Helsinki; Geological Survey Of Denmark & Greenland; University of Helsinki	Luostarinen, T (通讯作者)，Univ Helsinki, Fac Biol & Environm Sci, Ecosyst & Environm Res Programme, Environm Change Res Unit ECRU, POB 65, Viikinkaari 1, Helsinki 00014, Finland.	tiia.luostarinen@helsinki.fi	Ribeiro, Sofia/AAZ-2782-2021; Zimmermann, Heike/AAC-8404-2022; Luostarinen, Tiia/HKV-0993-2023; Heikkila, Maija/N-7659-2013; Ribeiro, Sofia/G-9213-2018	Heikkila, Maija/0000-0003-3885-8670; Bang Kvorning, Anna/0000-0003-4030-9080; Luostarinen, Tiia/0000-0002-2368-237X; Ribeiro, Sofia/0000-0003-0672-9161	This study was funded by the Academy of Finland (grant nos. 1296895, 1307282, and 1328540), the Alfred Kordelin Foundation, and the Danish Independent Research Fund (grant no. 9064-00039B to SR). The authors would like to acknowledge Matthew Owen, Tove Nie [1296895, 1307282, 1328540]; Academy of Finland [1296895, 1307282, 1328540]; Alfred Kordelinin Saatio; Danmarks Frie Forskningsfond [9064-00039B]; Alfred Kordelin Foundation; Danish Independent Research Fund [9064-00039B]	This study was funded by the Academy of Finland (grant nos. 1296895, 1307282, and 1328540), the Alfred Kordelin Foundation, and the Danish Independent Research Fund (grant no. 9064-00039B to SR). The authors would like to acknowledge Matthew Owen, Tove Nie; Academy of Finland(Research Council of Finland); Alfred Kordelinin Saatio; Danmarks Frie Forskningsfond; Alfred Kordelin Foundation; Danish Independent Research Fund	Academy of Finland, Grant/Award Number: 1296895, 1307282 and 1328540; Alfred Kordelinin Saatio; Danmarks Frie Forskningsfond, Grant/Award Number: 9064-00039B This study was funded by the Academy of Finland (grant nos. 1296895, 1307282, and 1328540), the Alfred Kordelin Foundation, and the Danish Independent Research Fund (grant no. 9064-00039B to SR). The authors would like to acknowledge Matthew Owen, Tove Nielsen, John Boserup, and the entire crew on board the Vaigat cruise with RV Sanna 2019 for their valuable help and patience during surface sediment sampling. 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Eukaryot. Microbiol.	JAN	2024	71	1								10.1111/jeu.13005	http://dx.doi.org/10.1111/jeu.13005		OCT 2023	15	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	JS5A0	37877451	hybrid			2025-03-11	WOS:001090379300001
J	Vasilyeva, ON				Vasilyeva, Olga N.			New dinoflagellate cyst species from the Middle Eocene of the Volgograd-Volga region, south-west Russia	PALYNOLOGY			English	Article						dinoflagellate cysts; Middle Eocene; Lutetian; south-west Russia; Volgograd-Volga region; taxonomy	BIOSTRATIGRAPHY; SEDIMENTS; PALEOGENE	The Keresta Formation, located in the Volgograd-Volga region (the Volga-Caspian subregion of south-west Russia) has been dated as Middle Eocene, Lutetian, based on dinoflagellate cysts of the Enneadocysta arcuata Zone and nannofossils from the Lutetian subzones CP13c-CP14a. Within this interval, four new species of dinoflagellate cysts are described: Spiniferella grigorovichiae sp. nov., Impagidinium tuberculatum sp. nov., Hystrichostrogylon crassitunicatum sp. nov. and Hystrichosphaeropsis tenerum sp. nov. The new species present a high correlation potential for Middle Eocene stratigraphy over the southern part of the Russian Platform. Also, the assemblage of organic-walled microphytoplankton from the Keresta Formation indicates warm-water marine environments within the marginal part of the Paratethys Basin.	[Vasilyeva, Olga N.] Russian Acad Sci, Inst Geol & Geochem, Ural Branch, 15 Vonsovskogo St, Ekaterinburg 620110, Russia	Russian Academy of Sciences	Vasilyeva, ON (通讯作者)，Russian Acad Sci, Inst Geol & Geochem, Ural Branch, 15 Vonsovskogo St, Ekaterinburg 620110, Russia.	vasilyeva@igg.uran.ru		Vasil'eva, Olga/0000-0002-0584-9201	The author is grateful to the authorities of the 'EuroChem-VolgaKaliy' company for granting permission to work with core materials and publish results; V.V. Savin (chief hydrogeologist of company) and V.A. Musatov (Lower Volga Institute of Geology and Geop [FUMZ-2023-0009]; state assignment 123011800010-5; Institute of Geology and Geochemistry of the Ural Branch, Russian Academy of Sciences	The author is grateful to the authorities of the 'EuroChem-VolgaKaliy' company for granting permission to work with core materials and publish results; V.V. Savin (chief hydrogeologist of company) and V.A. Musatov (Lower Volga Institute of Geology and Geop; state assignment 123011800010-5; Institute of Geology and Geochemistry of the Ural Branch, Russian Academy of Sciences	The author is grateful to the authorities of the 'EuroChem-VolgaKaliy' company for granting permission to work with core materials and publish results; V.V. Savin (chief hydrogeologist of company) and V.A. Musatov (Lower Volga Institute of Geology and Geophysics) are acknowledged for their cooperation. The author expresses deep gratitude to Manuel Vieira and an anonymous reviewer for their constructive and kind review of the manuscript. The author would like to thank Przemys & lstrok;aw Gedl for editing the manuscript. Editor-in-chief James B. Riding (Nottingham, UK) is thanked for valuable ideas and publishing support. The research was conducted within the framework of the theme FUMZ-2023-0009, state assignment 123011800010-5, with budget financing by the Institute of Geology and Geochemistry of the Ural Branch, Russian Academy of Sciences.	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J	Lambert, O; Bosselaers, M; Louwye, S				Lambert, Olivier; Bosselaers, Mark; Louwye, Stephen			Past beaked whale diversity in the North Sea: reappraisal through a new Miocene record and biostratigraphic analyses	GEOLOGICA BELGICA			English	Article						Cetacea; Ziphiidae; fossil; palynology; Serravallian; Tortonian; radiation	DINOFLAGELLATE CYST STRATIGRAPHY; MIDDLE MIOCENE; DEEP-SEA; CETACEA; ODONTOCETI; BELGIUM; ZIPHIIDAE; PLIOCENE; NEOGENE; MESSAPICETUS	Extant beaked whales (family Ziphiidae) are deep diving suction feeders and none of them can be considered as a permanent resident of the shallow southern North Sea. The rich fossil record of ziphiids from Neogene deposits of this area is thus surprising. However, chronostratigraphic intervals of most recorded taxa remain poorly constrained, preventing from assessing the evolution of their local diversity. In this work, we describe a new ziphiid cranium from the Neogene of Antwerp (north of Belgium), which is attributed to Caviziphius aff. C. altirostris. Sediment samples were extracted from 15 fossil ziphiid cranial remains from this area (including the one described herein), referred to eight species. The samples were analysed for their palynological content, leading to improved chronostratigraphic ranges for several species. Seven to eight ziphiid species from the southern North Sea, all from the Messapicetus clade, are proposed to originate from a Serravallian to Tortonian (late Middle to early Late Miocene) interval, and three to six more precisely from the mid-to late Tortonian. Added to the fossil record of other regions, these results point to a Late Miocene radiation of members of the Messapicetus clade, possibly related to the synchronous worldwide decline of several hyper-longirostrine dolphin clades.	[Lambert, Olivier; Bosselaers, Mark] Inst Royal Sci Nat Belgique, DO Terre & Hist Vie, Rue Vautier 29, B-1000 Brussels, Belgium; [Bosselaers, Mark] Koninklijk Zeeuwsch Genooschap Wetenschappen, Koudsteensedijk 7, NL-4331 Middelburg, Netherlands; [Louwye, Stephen] Univ Ghent, Dept Geog, Krijgslaan 281-S8, B-9000 Ghent, 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.	olambert@naturalsciences.be.ddddddddddddddd	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Lambert, Olivier/0000-0003-0740-5791; Bosselaers, Mark E. 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Belg.		2023	26	3-4					117	126		10.20341/gb.2023.009	http://dx.doi.org/10.20341/gb.2023.009		OCT 2023	10	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	DK6V8		Green Published, gold			2025-03-11	WOS:001087174600001
J	Persson, A; Smith, BC; Alix, JH; Wikfors, GH				Persson, Agneta; Smith, Barry C.; Alix, Jennifer H.; Wikfors, Gary H.			Properties and Behavior of Sexual Life Stages Underlying Dinoflagellate HAB Events of Cyst-Producing Species That Disrupt Fisheries and Aquaculture	REVIEWS IN FISHERIES SCIENCE & AQUACULTURE			English	Editorial Material; Early Access						Dinoflagellate; gamete; HAB; life cycle; resting cyst; zygote	ALEXANDRIUM-FUNDYENSE; GYMNODINIUM-CATENATUM; MARINE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; RED TIDE; VERTICAL MIGRATION; KARENIA-BREVIS; RESTING CYSTS; CYCLE STAGES; C2 TOXIN	Harmful algal blooms (HAB) are natural environmental occurrences that can disrupt ecosystem function that supports fisheries and aquaculture, as well as rendering harvested seafood, especially shellfish, unsafe for consumption by humans or wildlife species. Many dinoflagellates that cause HAB have a life cycle with a sexually produced resting stage called the resting cyst. The resting cyst enables the species to persist in an area where conditions for growth vary seasonally. These species often are found as vegetative stages only during a short period of the year. Most of the time is spent dormant or quiescent as thick-walled resting cysts with very low metabolic activity. By summarizing findings from an iterative series of research projects investigating different parts of the sexual life cycle, a more complete picture of the role of the sexual stages emerges, illuminating the consequences of life cycle within the environmental context. Gametes, the sexual stages, are formed at the end of the growing season in response to environmental signals which remain largely unknown. Gametes have lower cell-specific density and different swimming behavior compared to vegetative cells. Specifically, vegetative cells perform daily vertical migrations; whereas, gametes accumulate in patterns influenced by lower cell-specific density, changed swimming behavior, and attraction to each other. The patterns and patches of accumulated gametes (sexually induced cells) aggregate into larger and larger patterns. Together with large-scale hydrographic water movements, such as upwelling, water stratification, and fronts, cells originating from a low vegetative cell density background distribution assemble and become concentrated within a constricted space, thus forming a dense "bloom." This process is distinctly different from the paradigm of blooms resulting from simple, vegetative cell divisions. Undisturbed blooms of cyst-producing dinoflagellate gametes end with gamete fusion into diploid zygotes that transform into resting cysts. The resting cysts sink according to shape and cell-specific density into the silt fraction of the sediment. Cyst preservation depends upon the oxygenation level of the sediment and the presence of fauna. Hypoxic/anoxic conditions lower cyst mortality from benthic grazers. The reestablishment of motile, vegetative cells occurs under seasonally favorable conditions, and successful population growth depends upon environmental conditions, such as weather and nutrient availability. Factors that increase HAB risks of resting cyst-producing dinoflagellates are eutrophication leading to high cell numbers and high cyst preservation in hypoxic benthic zones. Hydrographic factors causing increased cell accumulation also are important, and intensified water stratification can amplify encystment success. These insights underscore mechanisms by which climate change is affecting HAB ecology and subsequent effects upon marine and coastal fisheries and aquaculture.	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Fish. Sci. Aquac..	2023 OCT 9	2023										10.1080/23308249.2023.2268715	http://dx.doi.org/10.1080/23308249.2023.2268715		OCT 2023	18	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	W4XD2					2025-03-11	WOS:001091661000001
J	Ciurej, A; Dubicka, Z; Poberezhskyy, A				Ciurej, Agnieszka; Dubicka, Zofia; Poberezhskyy, Andriy			Calcareous dinoflagellate blooms during the Late Cretaceous 'greenhouse' world- a case study from western Ukraine	PEERJ			English	Article						Upper Turonian; Late Cretaceous; Calcareous dinocysts; Pithonellids; Nutrient crisis; Sea-level fluctuations; Central European Basin	STABLE-ISOTOPE RECORDS; SEA-LEVEL; ATLANTIC-OCEAN; SURFACE SEDIMENTS; CYSTS; CARBON; BASIN; STRATIGRAPHY; BOUNDARY; PALEOECOLOGY	The Late Cretaceous was a unique period in the history of the Earth characterized by elevated sea levels, reduced land area, and significantly high concentrations of atmospheric CO2 resulting in increased temperatures across the globe-a 'Greenhouse World'. During this period, calcareous dinoflagellate cysts (c-dinocysts) flourished and became a ubiquitous constituent of calcifying plankton around the world. An acme in calcareous dinocysts during the Albian to the Turonian coincided with the highest recorded seawater surface temperatures and was possibly linked to conditions that favored calcification and a highly oligotrophic system in European shelf seas. This study examines the potential applicability of c-dinocysts as a proxy for paleoenvironmental conditions based on their assemblage changes plotted against foraminiferal occurrences and microfacies analysis. The material was extracted from the upper Turonian chalk of the Dubivtsi region in western Ukraine. An inverse correlation was observed between species diversity and the number of c-dinocyst specimens. Nutrient availability gradients apparently determined important changes in the calcareous dinocysts distribution. These trophic changes were likely caused by the interplay of eustatic sealevel fluctuations and Subhercynian tectonic activity leading to changeable nutrient inputs from the nearby land.	[Ciurej, Agnieszka] Pedag Univ Krakow, Inst Biol & Earth Sci, Dept Geol & Palaeontol, Krakow, Poland; [Dubicka, Zofia] Univ Warsaw, Fac Geol, Warsaw, Poland; [Dubicka, Zofia] GFZ German Res Ctr Geosci, Potsdam, Germany; [Poberezhskyy, Andriy] NAS Ukraine, Inst Geol & Geochem Combustible Minerals, Lvov, Ukraine	University of the National Education Commission; University of Warsaw; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; National Academy of Sciences Ukraine; Institute of Cell Biology of NASU; Institute of Geology & Geochemistry of Combustible Minerals, NAS of Ukraine	Ciurej, A (通讯作者)，Pedag Univ Krakow, Inst Biol & Earth Sci, Dept Geol & Palaeontol, Krakow, Poland.	agnieszka.ciurej@up.krakow.pl	Ciurej, Agnieszka/HNS-7682-2023; Poberezhskyy, Andriy/GZA-4384-2022; Dubicka, Zofia/ABB-3388-2020	Dubicka, Zofia/0000-0003-1105-4111	Faculty of Exact and Natural Sciences, Pedagogical University of Krakow, Poland, Statutory Funds [WPBU/2022/04/00194]; National Science Centre, Poland [2017/27/B/ST10/00687]	Faculty of Exact and Natural Sciences, Pedagogical University of Krakow, Poland, Statutory Funds; National Science Centre, Poland(National Science Centre, Poland)	This work was supported by the Faculty of Exact and Natural Sciences, Pedagogical University of Krakow, Poland, Statutory Funds, Project no. WPBU/2022/04/00194 and the National Science Centre, Poland, grant no. 2017/27/B/ST10/00687. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. Grant Disclosures The following grant information was disclosed by the authors: Faculty of Exact and Natural Sciences, Pedagogical University of Krakow, Poland, Statutory Funds: WPBU/2022/04/00194. National Science Centre, Poland: 2017/27/B/ST10/00687.	Andryuschenko AI, 1975, Byulletin' Moskovskogo Obshchestva Ispytateliy Prirody ot'del Geologii, V5, P105; Be A.W.H., 1977, P1; BE ALLAN W. 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J	Ragab, MO; Bassiouni, MEA; Boukhary, M; Makled, WA; Mostafa, TF				Ragab, Muhammad Omar; Bassiouni, Mohamed El Amin Ahmed; Boukhary, Mohamed; Makled, Walid Ahmed; Mostafa, Tarek Fouad			Organic petrography and palynofacies of the Upper Cretaceous (Campanian-Maastrichtian) organic rich strata of the Quseir-Safaga Region, Eastern Egypt	MARINE AND PETROLEUM GEOLOGY			English	Article						Upper cretaceous; Duwi formation; Dakhla formation; Palynofacies; Organic petrography; Environmental analysis	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SOURCE-ROCK EVALUATION; WESTERN EXTERNAL RIF; MARINE BLACK SHALES; TERTIARY BOUNDARY; PALEOGENE BOUNDARY; CALCAREOUS NANNOFOSSIL; NORTHERN APENNINES; OULED HADDOU; RED-SEA	The Campanian-Maastrichtian organic-rich rocks in the Quseir - Safaga Region in the Eastern Desert of Egypt have growing economic importance. This economic importance is discussed in many of previous studies by many of different geological tools that lacked the petrographic examination of organic matter occurrence modes. The organic petrography provides the essential tools for microscopic analysis to study the organic matter that are applied for the first time in the present study. The palynofacies and organic petrography are used in the present study to investigate the nature of the organic matter and the paleoenvironmental settings that controlled their distribution in the Duwi and Dakhla formations in the Younis and Mohamed Rabah areas (Egypt). The study of dinoflagellate cysts allowed the identification of the biostratigraphically characteristic assemblages of the Campanian - Maastrichtian in the Eastern Desert including Assemblage II/I (in Duwi Formation) and Assemblage III (in Dakhla Formation) that were identified in Egyptian oil shales of this time range. The identified assemblages are correlated with local and regional studies to delineating the formal biozonation. The organic matter in the Duwi Formation comprises rich fluorescent amorphous organic matter, prasinophytes, sporomorphs, dinocysts as well as a minor terrigenous component of phytoclasts. In the Dakhla Formation, the fluorescent AOM is found to be highly mixed with Botryococcus in addition to prasinophytes and marine palynomorphs. The paleoenvironmental analysis indicates deposition in distal anoxic to proximal suboxic marine conditions with high paleoproductivity. The results are confirmed with the inorganic geochemical composition of redox sensitive elements. The analysis reveals that the Younis section is differentiated into two palynofacies types (proximal, suboxic high productivity in the Duwi Formation and distal anoxic in the Dakhla Formation). The Mohamed Rabah section, one palynofacies type is recognized that is proximal, suboxic high productivity. The principal component analysis is used to interpret the distribution of organic matter abundances. The kerogen types are distinguished based on the area percentages of the fluorescent organic matter and application of kerogen plots. The samples of both formations fall within oil prone kerogen type II. The spore coloration and measured vitrinite reflectance indicate immature kerogen in the studied sections. The organic matter in the studied rocks comprises hydrogen rich compounds that can be treated for direct composition or retorted to extract shale oil. The heavy metals concentrations are significant and present technology will increase its economic value.	[Ragab, Muhammad Omar; Makled, Walid Ahmed; Mostafa, Tarek Fouad] Egyptian Petr Res Inst EPRI, Explorat Dept, 1 Ahmed El Zomor St, Cairo 11727, Egypt; [Bassiouni, Mohamed El Amin Ahmed; Boukhary, Mohamed] Ain Shams Univ, Dept Geol, Fac Sci, Cairo 11566, Egypt	Egyptian Knowledge Bank (EKB); Egyptian Petroleum Research Institute (EPRI); Egyptian Knowledge Bank (EKB); Ain Shams University	Makled, WA (通讯作者)，Egyptian Petr Res Inst EPRI, Explorat Dept, 1 Ahmed El Zomor St, Cairo 11727, Egypt.	walidmakled@epri.sci.eg	Makled, Walid/K-1454-2019	Makled, Walid/0000-0002-2209-885X				Abdel Razik T.M., 1972, 8 AR PETR C ALG, P23; Abou El-Anwar E, 2021, MINERALS-BASEL, V11, DOI 10.3390/min11121416; Abu-Ali R., 2023, Advances in Petroleum Source Rock Characterizations: Integrated Methods and Case Studies, Advances in Science, Technology & Innovation, DOI [10.1007/978-3-031-16396-8_7, DOI 10.1007/978-3-031-16396-8_7]; Akash BA, 2003, ENERG SOURCE, V25, P1171, DOI 10.1080/00908310390233612; Algeo TJ, 2004, CHEM GEOL, V206, P289, DOI 10.1016/j.chemgeo.2003.12.009; [Anonymous], 1957, Bulletin de I'Institut du desert d'Egypte, V1, P35; [Anonymous], 1984, Pollen/spore color 'standard'; [Anonymous], 2015, Annu. 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J	Matsuda, R; Makabe, R; Sano, M; Takao, S; Moteki, M; Kurosawa, N				Matsuda, R.; Makabe, R.; Sano, M.; Takao, S.; Moteki, M.; Kurosawa, N.			Fecal Pellet-Like <i>Gyrodinium</i> Species in Sinking Particles: Newly Found Potential Contributors for Carbon Export in the Antarctic Seasonal Ice Zone	JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES			English	Article						Southern Ocean; biological pump; Gyrodinium; drifting sediment trap	COMB. NOV. DINOPHYCEAE; HETEROTROPHIC DINOFLAGELLATE; BIOLOGICAL PUMP; SOUTHERN-OCEAN; MARINE SNOW; ZOOPLANKTON; COPEPOD; FLUX; SEA; ULTRASTRUCTURE	Fecal pellets (FPs) are generated by various species and have gained attention as contributors to the biological carbon pump. Metazoans and protozoans are known as FP and minipellet-producers, respectively. Herein, we discovered fecal pellet-like dinoflagellates (FLDs) in the seasonal sea ice zone in the Southern Ocean. The size and form of these FLDs were similar to those of zooplankton oval FPs. However, due to their appearance, they have been misclassified as FPs rather than dinoflagellates, leading to potential oversight of their role in the carbon cycle. Thus, we aimed to identify FLD cells at the species level and examine the impact of FLDs on flux estimation of particulate organic carbon (POC). Our findings are as follows: first, FLD cells were identified as Gyrodinium rubrum and Gyrodinium heterogrammum through 18S rRNA gene sequencing. Second, FLDs can potentially excrete larger FPs than minipellets. Third, the sinking rate of FLDs is higher than that of other protozoa and dinoflagellate cysts. Finally, a maximum of 12 mgC m(-2) day(-1) of the POC flux can be attributed to FLDs (representing 32% of POC flux). These results suggest that FLDs are important drivers not only for the microbial loop but also for the biological carbon pump. In future projections of carbon sequestration, the contribution of metazoans to carbon export must be considered, but not that of FLDs. Their unknown physiological and ecological characteristics, especially including the responses to climate changes, must be urgently investigated for future projections of carbon sequestration in the Southern Ocean. Plain Language Summary Zooplankton feed on phytoplankton cells and excrete fecal pellets (FPs). FPs have gained attention as carbon carriers from the surface to the deep ocean because of their high carbon contents and sinking rate. Previous studies have sampled FPs using sediment traps and estimated carbon fluxes through microscopic observations to better understand the ocean carbon cycle. Here, we report the discovery of a dinoflagellate that closely resembles FP and was captured using a drifting sediment trap. This dinoflagellate has been named "fecal-pellet-like dinoflagellate (FLD)." It is believed that FLD cells have been misclassified as FPs given their appearance. Our findings indicated that a maximum of 12 mgC m(-2) day(-1) (representing 32% of the particulate organic carbon flux at 50 m depths during the summer productive season) may be attributed to FLD carbon flux. This result suggests that FLD cells serve as potential contributors for carbon export, contrary to the knowledge that heterotrophic dinoflagellates had been known as one of the dominant microbial loop components. Studies on FLDs are essential to understand the Southern Ocean carbon cycle.	[Matsuda, R.; Kurosawa, N.] Soka Univ, Grad Sch Sci & Engn, Dept Environm Engn Symbiosis, Tokyo, Japan; [Makabe, R.; Sano, M.; Moteki, M.] Natl Inst Polar Res, Tokyo, Japan; [Makabe, R.; Moteki, M.] Tokyo Univ Marine Sci & Technol, Dept Ocean Sci, Tokyo, Japan; [Makabe, R.] Grad Univ Adv Studies SOKENDAI, Dept Polar Sci, Tokyo, Japan; [Sano, M.] Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Japan; [Takao, S.] Natl Inst Environm Studies, Ibaraki, Japan	Soka University; Research Organization of Information & Systems (ROIS); National Institute of Polar Research (NIPR) - Japan; Tokyo University of Marine Science & Technology; Graduate University for Advanced Studies - Japan; University of Tokyo; National Institute for Environmental Studies - Japan	Matsuda, R (通讯作者)，Soka Univ, Grad Sch Sci & Engn, Dept Environm Engn Symbiosis, Tokyo, Japan.	ryomatsuda@soka.gr.jp	Takao, Shintaro/M-8269-2019	Sano, Masayoshi/0000-0001-7264-9528; Kurosawa, Norio/0000-0001-5095-2104; Takao, Shintaro/0000-0002-0118-6447; Matsuda, Ryo/0000-0001-9312-2231	We would like to express our gratitude to the late Dr. T. Odate from the National Institute of Polar Research, who passed away in February 2021, for providing us with the opportunity to conduct our observations. We also extend our thanks to the captain and [17H06319, 17K07579, 20H04313, 23KJ2057]; Japan Society for the Promotion of Science KAKENHI [KP-308]; Research Project Funds of the National Institute of Polar Research [AP-0939]; Japanese Antarctic Research Expedition [2021-4085]; Sasakawa Scientific Research; Japan Science Society [JPMJSP2143]; Japan Science and Technology Society (Support for Pioneering Research Initiated by the Next Generation [SPRING]); Grants-in-Aid for Scientific Research [20H04313, 23KJ2057] Funding Source: KAKEN	We would like to express our gratitude to the late Dr. T. Odate from the National Institute of Polar Research, who passed away in February 2021, for providing us with the opportunity to conduct our observations. We also extend our thanks to the captain and; Japan Society for the Promotion of Science KAKENHI(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Research Project Funds of the National Institute of Polar Research; Japanese Antarctic Research Expedition; Sasakawa Scientific Research; Japan Science Society; Japan Science and Technology Society (Support for Pioneering Research Initiated by the Next Generation [SPRING]); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We would like to express our gratitude to the late Dr. T. Odate from the National Institute of Polar Research, who passed away in February 2021, for providing us with the opportunity to conduct our observations. We also extend our thanks to the captain and crew of the icebreaker <ITALIC>Shirase</ITALIC> and the TV <ITALIC>Umitaka-maru</ITALIC> for their support during the cruises. Special thanks are offered to Dr. M. Yamamoto-Kawai for her valuable comments on the study results. We would also like to acknowledge A. Kagesawa, S. Okano, and J. Han for their technical assistance during the experiments. This work was supported by the Japan Society for the Promotion of Science KAKENHI (Grants 17H06319 to M. Moteki, 17K07579 and 20H04313 to R. Makabe, and 23KJ2057 to R. Matsuda), the Research Project Funds of the National Institute of Polar Research (Grant KP-308 to T. Odate), the Japanese Antarctic Research Expedition (Grant AP-0939 to M. Moteki), the Sasakawa Scientific Research (Grant 2021-4085 to R. Matsuda) from the Japan Science Society, and the Japan Science and Technology Society (Support for Pioneering Research Initiated by the Next Generation [SPRING]; Grant JPMJSP2143).	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Geophys. Res.-Biogeosci.	OCT	2023	128	10							e2023JG007705	10.1029/2023JG007705	http://dx.doi.org/10.1029/2023JG007705			16	Environmental Sciences; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	T0NW4		hybrid			2025-03-11	WOS:001075050900001
J	Klyuvitkina, TS; Novichkova, EA; Matul, AG; Kravchishina, MD				Klyuvitkina, T. S.; Novichkova, E. A.; Matul, A. G.; Kravchishina, M. D.			The Holocene Environment of the Norwegian Sea Based on Fossil Microalgae Assemblages	DOKLADY EARTH SCIENCES			English	Article						North Atlantic; paleoreconstructions; dinoflagellate cysts; Arctic Front	NORDIC SEAS	Detailed micropaleontological analysis was performed on the sediment core AMK-6142 collected in the deep southwestern part of the Lofoten Basin in the Norwegian Sea. Summer sea-surface temperature for the 7 cal. ka BP was reconstructed from dinocyst assemblages using the modern analogue technique (MAT). Sea-surface reconstruction and dinocysts species composition indicate repeated changes in environmental conditions in the surface water layer during the Middle and Late Holocene. Episodes of cooling and probable displacement of the Arctic Front to the southwestern part of the Lofoten Basin were recorded for 5-7, 1.6-2.1, and 0.1-1.0 cal. ka BP.	[Klyuvitkina, T. S.] Moscow State Pedag Univ, Moscow 119991, Russia; [Novichkova, E. A.; Matul, A. G.; Kravchishina, M. D.] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia	Moscow State University of Education; Russian Academy of Sciences; Shirshov Institute of Oceanology	Klyuvitkina, TS (通讯作者)，Moscow State Pedag Univ, Moscow 119991, Russia.	t.klyuvitkina@mail.ru	K, Tatiana/GZL-4850-2022; Kravchishina, Marina/B-3741-2017; Novichkova, Ekaterina/B-5807-2017	Novichkova, Ekaterina/0000-0001-5687-1719	The authors are grateful to the crew of the R/V <italic>Akademik Mstislav Keldysh</italic>, G.V. Malafeev, S.M. Isachenko, and D.F. Budko for their help in collecting sediment samples; to A.A. Klyuvitkin for comprehensive assistance; and to E.A. Agafonova	The authors are grateful to the crew of the R/V <italic>Akademik Mstislav Keldysh</italic>, G.V. Malafeev, S.M. Isachenko, and D.F. Budko for their help in collecting sediment samples; to A.A. Klyuvitkin for comprehensive assistance; and to E.A. Agafonova	The authors are grateful to the crew of the R/V <ITALIC>Akademik Mstislav Keldysh</ITALIC>, G.V. Malafeev, S.M. Isachenko, and D.F. Budko for their help in collecting sediment samples; to A.A. Klyuvitkin for comprehensive assistance; and to E.A. Agafonova for laboratory processing of samples. We would like to thank Professor Liping Zhou for his work on dating the core sediments.	Bauch HA, 2001, QUATERNARY SCI REV, V20, P659, DOI 10.1016/S0277-3791(00)00098-6; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Blindheim J, 2004, ICES J MAR SCI, V61, P846, DOI 10.1016/j.icesjms.2004.05.003; de Vernal A., 2020, MAR MICROPALEONTOL, V159, P101796, DOI [10.1016/j.marmicro.2019.101796, DOI 10.1016/J.MARMICRO.2019.101796]; de Vernal A, 2013, QUATERNARY SCI REV, V79, P111, DOI 10.1016/j.quascirev.2013.07.006; de Vernal A, 2013, QUATERNARY SCI REV, V79, P122, DOI 10.1016/j.quascirev.2013.06.022; Grosfjeld K, 2009, NORW J GEOL, V89, P121; Guiot J, 2007, DEV MARINE GEOL, V1, P523, DOI 10.1016/S1572-5480(07)01018-4; Henry M., 2010, Notes Prepared for Students of Course SCT, V8245; Klyuvitkin AA, 2020, OCEANOLOGY+, V60, P421, DOI 10.1134/S0001437020030030; Lappo S. S., 1984, OCEAN ATMOSPHERE INT; Locarnini R.A., 2013, World Ocean Atlas 2013, Volume, P40; Reimer PJ, 2020, RADIOCARBON, V62, P725, DOI 10.1017/RDC.2020.41; Rochon A., 1999, American Association of Stratigraphic Palynologists Contributions Series, V35, P1, DOI DOI 10.1016/0377-8398(94)00016-G; STUIVER M, 1993, RADIOCARBON, V35, P215, DOI 10.1017/S0033822200013904; Van Nieuwenhove N, 2020, MAR MICROPALEONTOL, V159, DOI 10.1016/j.marmicro.2019.101814; Van Nieuwenhove N, 2016, HOLOCENE, V26, P722, DOI 10.1177/0959683615618258; Vorren TO, 1998, QUATERNARY SCI REV, V17, P273, DOI 10.1016/S0277-3791(97)00072-3; 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	20	2	2	0	3	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1028-334X	1531-8354		DOKL EARTH SCI	Dokl. Earth Sci.	DEC	2023	513	2					1361	1365		10.1134/S1028334X23601943	http://dx.doi.org/10.1134/S1028334X23601943		SEP 2023	5	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	IY1Q3					2025-03-11	WOS:001075320200001
J	Guerstein, GR; Amenábar, CR; Fensome, RA; Daners, G; Palma, ED				Guerstein, G. Raquel; Amenabar, Cecilia R.; Fensome, Robert A.; Daners, Gloria; Palma, Elbio D.			Turbiosphaera archangelskyi sp. nov. and a morphological complex from the late Middle to Late Eocene of southern high latitudes: Biostratigraphic, palaeoenvironmental and palaeoceanographic implications	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Polymorphism; Morphological species complex; Palaeocology; Drake Passage opening; Patagonia	TIERRA-DEL-FUEGO; DINOFLAGELLATE CYSTS; PALEOGENE; ARGENTINA; PATAGONIA; STRATIGRAPHY; ESTUARINE; BASIN	We record a morphological complex of species of the dinoflagellate-cyst genus Turbiosphaera from the uppermost Rio Turbio Formation, considered to be of late Priabonian age, and from equivalent units of the AustralMagallanes Basin, southern Argentina and southern Chile. Previously, specimens now assigned to Turbiosphaera archangelskyi sp. nov and Turbiosphaera sarrisii were assigned to the cosmopolitan latest Maastrichtian to Middle Eocene species Turbiosphaera filosa. We now identify three species in our Turbiosphaera archangelskyi species complex, which excludes Turbiosphaera filosa. At one end of the complex is Turbiosphaera sarrisii with incipient processes, and at the other end, with well-developed individual processes, is Turbiosphaera sagena. The new species, Turbiosphaera archangelskyi, represents the intermediate stage and is the most abundant form. These three species have only been recorded together in the Austral-Magallanes Basin; their earliest occurrences are slightly asynchronous: Turbiosphaera sarrisii and Turbiosphaera archangelskyi have earliest occurrences in the late Bartonian, but that of Turbiosphaera sarrisii is slightly older. The earliest occurrence of Turbiosphaera sagena is recorded in the middle Priabonian. Our results highlight the biostratigraphic value of these species and their limited palaeogeographical distribution. The morphological variability exhibited by the Turbiosphaera archangelskyi species complex in the latest Eocene may be environmentally influenced, perhaps reflecting the deepening of the Drake Passage and the consequent influx of low-salinity water from the shelf and nearshore regions of the southeastern Pacific onto the Patagonian Shelf.	[Guerstein, G. Raquel] Univ Nacl Sur, Dept Geol, Inst Geol Sur, CONICET, Ave Alem 1253, RA-8000 Bahia Blanca, BA, Argentina; [Amenabar, Cecilia R.] Univ Buenos Aires FCEN UBA, Inst Estudios Andinos Don Pablo Groeber, Consejo Nacl Invest Cient & Tecn IDEAN CONICET, Dept Ciencias Geol,Fac Ciencias Exactas & Nat,Lab, Ciudad Univ,Intendente Guiraldes 2160,CP 1428 EGA, Buenos Aires, Argentina; [Amenabar, Cecilia R.] Inst Antartico Argentino, Dept Paleontol, Area Ciencias Tierra, 25 Mayo 1143, RA-1650 San Martin, Buenos Aires, Argentina; [Fensome, Robert A.] Bedford Inst Oceanog, Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Daners, Gloria] Univ Republ UDELAR, Fac Ciencias, Igua 4225, Montevideo 11400, Uruguay; [Palma, Elbio D.] Univ Nacl, Dept Fis, Avda Alem 1253, RA-8000 Bahia Blanca, Argentina; [Palma, Elbio D.] Consejo Nacl Invest Cient & Tecn, Inst Argentino Oceanog IADO, Avda Alem 1253, RA-8000 Bahia Blanca, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); University of Buenos Aires; Instituto Antartico Argentino; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; Universidad de la Republica, Uruguay; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, Inst Geol Sur, CONICET, Ave Alem 1253, RA-8000 Bahia Blanca, BA, Argentina.	raquel.guerstein@uns.edu.ar; amenabar@gl.fcen.uba.ar; rob.fensome@nrcan-rncan.gc.ca; lagluar@gmail.com; uspalma@criba.edu.ar		AMENABAR, CECILIA R./0000-0003-1280-3903	Universidad Nacional del Sur [PGI 24/F079]; Agencia Nacional de Promocion Cientifica y Tecnologica; Natural Resources Canada; Geological Survey of Canada;  [PICT 2018-00917]	Universidad Nacional del Sur; Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Natural Resources Canada(Natural Resources CanadaCanadian Forest Service); Geological Survey of Canada(Natural Resources Canada); 	We thank G. del Fueyo, M.C. Zamaloa and A. Gandolfo for inviting us to participate in the special volume dedicated to Sergio Archangelsky. We also thank E. Olivero (CADIC-CONICET, Argentina) who shared the samples of the Leticia Formation collected at Cabo Campo del Medio (Tierra del Fuego) . O. Cardenas (MACN, Argentina) is especially acknowledged for the palynological technical assistance in processing the samples from the CA-1 Core. The work carried out by P. Diaz (INGEOSUR - CONICET) in the physico-chemical extraction of palyno-logical samples from the Loreto Formation and the preparation of the palynological residues for SEM study is highly appreciated. We also thank C. Gutierrez Ayesta from the Microscopy Laboratory CCT-BB/CONICET. The valuable comments of detailed critical readings of G. Williams (Geological Survey of Canada, Natural Resources Canada) and A. Iakovleva (Geological Institute, Russian Academy of Science) improved a previous version of the manuscript. The contributions of A. Soliman (Geology Department, Faculty of Science, Tanta University, Egypt) and an anonymous reviewer along with the editors'suggestions were very helpful and are very much acknowledged. Financial support was provided by the Universidad Nacional del Sur (PGI 24/F079) and the Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 2018-00917) . This work is a contribution to the Instituto Antartico Argentino (IAA) and the Instituto de Estudios Andinos 'Don Pablo Groeber' (contribution number R-466) . RAF acknowledges support from Natural Resources Canada, Geological Survey of Canada; this is NRCan contribution no. 20230174.	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Palaeobot. Palynology	DEC	2023	319								104991	10.1016/j.revpalbo.2023.104991	http://dx.doi.org/10.1016/j.revpalbo.2023.104991		SEP 2023	18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	HH9N1					2025-03-11	WOS:001158721600001
J	Sharfi, M; Yazdi-Moghadam, M; Ghasemi-Nejad, E; Sarfi, M; Foroughi, F				Sharfi, Mohammad; Yazdi-Moghadam, Mohsen; Ghasemi-Nejad, Ebrahim; Sarfi, Mehdi; Foroughi, Fariba			Integrated biostratigraphy (orbitolinids, calcareous nannofossils, and palynomorphs) of the Lower Cretaceous Sarcheshmeh Formation, western Koppeh-Dagh Basin, NE Iran	CRETACEOUS RESEARCH			English	Article						Aptian; Orbitolinids; Calcareous nannofossils; Dinoflagellate cysts; Biostratigraphy; Koppeh-Dagh Basin	ONTONG JAVA PLATEAU; DINOFLAGELLATE CYST; PLANKTONIC-FORAMINIFERA; BLACK SHALES; STRATIGRAPHY; ASSEMBLAGES; TETHYAN; PALYNOSTRATIGRAPHY; PALEOENVIRONMENTS; PALEOBIOGEOGRAPHY	An integrated biostratigraphy using orbitolinids, calcareous nannofossils, and dinoflagellate cysts was conducted on the Lower Cretaceous Sarcheshmeh Formation in two stratigraphic sections from the western Koppeh-Dagh Basin (NE Iran). The analyzed successions consist mainly of deep-marine shales and marlstones with intercalations of thin-bedded orbitolinid-bearing limestones. These strata yielded common to abundant and fairly well to well-preserved calcareous nannofossil assemblages. The afore-mentioned assemblages led to the identification of parts of the NC6 and NC7a biozones that can be correlated with parts of the CC7a and CC7b zones. The organic-walled dinoflagellate cysts also show well-preserved and relatively diverse assemblages in the studied sections that corresponded to the Odontochitina operculata Zone. Additionally, within the limestone intercalations of the Sarcheshmeh Formation, two index species of orbitolinids, Praeorbitolina cormyi Schroeder, and P. wienandsi Schroeder, were recorded, indicating the presence of the Praeorbitolina cormyi Zone. According to the literature, these recognized biozones are compatible with the ammonite zones of Deshayesites forbesi, Deshayesites deshayesi, and Dufrenoyia furcata, as well as the Globigerinelloides blowi and Leupoldina cabri planktonic foraminiferal zones. By the compilation of all acquired data, an age of late early Aptian (late Bedoulian) is deduced for the Sarcheshmeh Formation in the studied sections.(c) 2023 Elsevier Ltd. All rights reserved.	[Sharfi, Mohammad] Univ Kurdistan, Fac Sci, Dept Earth Sci, Sanandaj, Iran; [Yazdi-Moghadam, Mohsen] Natl Iranian Oil Co Explorat Directorate, Sheikh Bahaie Sq, Tehran, Iran; [Ghasemi-Nejad, Ebrahim; Foroughi, Fariba] Univ Tehran, Coll Sci, Dept Geol, Tehran, Iran; [Yazdi-Moghadam, Mohsen; Sarfi, Mehdi] Damghan Univ, Sch Earth Sci, Damghan, Iran	University of Kurdistan; National Iranian Oil Company (NIOC); University of Tehran; Damghan University	Sharfi, M (通讯作者)，Univ Kurdistan, Fac Sci, Dept Earth Sci, Sanandaj, Iran.	m.sharifi@uok.ac.ir	Moghadam, Mohsen/GSP-6543-2022; Sharifi, Mohammad/AAG-7084-2019; Foroughi, Fariba/HIK-1236-2022	Sharifi, Mohammad/0000-0003-2351-7670				Afshar-Harb A., 1994, TREATISE GEOLOGY IRA; Aguado R, 2014, CRETACEOUS RES, V51, P153, DOI 10.1016/j.cretres.2014.06.002; Allen MB, 2003, TECTONOPHYSICS, V366, P223, DOI 10.1016/S0040-1951(03)00098-2; Ando A, 2008, PALAEOGEOGR PALAEOCL, V260, P463, DOI 10.1016/j.palaeo.2007.12.007; Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; Barrier E., 2008, Paleotectonic Maps of the Middle East: Atlas of 14 Maps: Commission De La Carte Geologique; Bellanca A, 2002, PALAEOGEOGR PALAEOCL, V185, P175, DOI 10.1016/S0031-0182(02)00299-7; Bottini C, 2015, CLIM PAST, V11, P383, DOI 10.5194/cp-11-383-2015; Bottini C, 2012, NEWSL STRATIGR, V45, P115, DOI 10.1127/0078-0421/2012/0017; Bown P.R., 1998, P86; Bown P.R., 1998, P16; Bralower T.J., 1993, American Geophysical Union Schlanger Memorial Volume, V73, P5; Bralower T.J., 1995, Geochronology Time Scales and Global Stratigraphic Correlation, P65; BRALOWER TJ, 1987, MAR MICROPALEONTOL, V11, P293, DOI 10.1016/0377-8398(87)90003-X; Bucur Ioan I., 2019, Acta Palaeontologica Romaniae, V15, P13; Carevic I, 2013, CRETACEOUS RES, V40, P110, DOI 10.1016/j.cretres.2012.06.003; Cherchi A, 2013, CRETACEOUS RES, V39, P70, DOI 10.1016/j.cretres.2012.02.018; Coccioni R, 2006, PALAEOGEOGR PALAEOCL, V235, P66, DOI 10.1016/j.palaeo.2005.09.024; Costa L.I., 1992, P99; Davey R.J., 1974, Palaeontology, V17, P91; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; El Atfy H, 2016, MAR PETROL GEOL, V76, P362, DOI 10.1016/j.marpetgeo.2016.05.032; Ela NMA, 2020, PALYNOLOGY, V44, P94, DOI 10.1080/01916122.2018.1510858; Erba E, 2004, MAR MICROPALEONTOL, V52, P85, DOI 10.1016/j.marmicro.2004.04.007; Erba E, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2003PA000884; ERBA E, 1994, PALEOCEANOGRAPHY, V9, P483, DOI 10.1029/94PA00258; Erba E, 2015, GEOL SOC AM SPEC PAP, V511, P271, DOI 10.1130/2015.2511(15); 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; Föllmi KB, 2012, CRETACEOUS RES, V35, P230, DOI 10.1016/j.cretres.2011.12.005; Gard G, 2016, CRETACEOUS RES, V61, P180, DOI 10.1016/j.cretres.2016.01.001; Garzanti E, 2002, SEDIMENT GEOL, V151, P67, DOI 10.1016/S0037-0738(01)00231-7; Glennie, 2000, SEPM SPECIAL PUBLICA, V69, P9, DOI DOI 10.2110/PEC.00.69.0009; Godet A, 2014, CRETACEOUS RES, V48, P110, DOI 10.1016/j.cretres.2013.12.006; Golonka J, 2004, TECTONOPHYSICS, V381, P235, DOI 10.1016/j.tecto.2002.06.004; Haq BU, 2014, GLOBAL PLANET CHANGE, V113, P44, DOI 10.1016/j.gloplacha.2013.12.007; Hardas P, 2007, MAR MICROPALEONTOL, V66, P52, DOI 10.1016/j.marmicro.2007.07.007; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; Hathway B, 2001, ANTARCT SCI, V13, P67, DOI 10.1017/S0954102001000104; HEILMANN-CLAUSEN C., 1987, DANMARKS GEOLOGISKE, V17, P1; Heimhofer U, 2006, PALAEOGEOGR PALAEOCL, V235, P93, DOI 10.1016/j.palaeo.2005.09.025; Helby R., 2004, Updated Jurassic and Early Cretaceous dinocyst zonation NWS Australia; Helby R., 1992, Proceedings of the Ocean Drilling Program, Scientific Results, V123; Helby R.J., 1987, MEM ASSOC AUSTRALASI, V4, P1; Herrle JO, 2003, CRETACEOUS RES, V24, P1, DOI 10.1016/S0195-6671(03)00023-5; HOEDEMAEKER PJ, 1995, CRETACEOUS RES, V16, P195, DOI 10.1006/cres.1995.1016; Hubber H., 1976, Geological map of Iran, 1: 1,000,000 scale; Ibrahim MIA, 2002, NEUES JAHRB GEOL P-A, V224, P255; JAFFREZO M, 1972, CR ACAD SCI D NAT, V274, P802; Jaffre⠂zo M., 1971, Stratigraphie de l'Aptien (s. l.) du massiv de la Clape (Aude). 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Res.	JAN	2024	153								105696	10.1016/j.cretres.2023.105696	http://dx.doi.org/10.1016/j.cretres.2023.105696		SEP 2023	14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	U5RY1					2025-03-11	WOS:001085386200001
J	Chukwuka, AV; Jerome, FC; Hassan, A; Ebonwu, B; Adeogun, AO				Chukwuka, Azubuike Victor; Jerome, Fisayo C.; Hassan, Adesola; Ebonwu, Benjamin; Adeogun, Aina O.			Redox-active metals and oxidative stress-mediated myopathies in <i>Callinectes amnicola</i>, blue crab populations from impacted sites of the Lagos Lagoon: inferences for adverse ecological outcomes	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Muscle atrophy; Reactive oxygen species	LOBSTER NEPHROPS-NORVEGICUS; SKELETAL-MUSCLE; NORWAY LOBSTER; DINOFLAGELLATE INFECTION; HISTOPATHOLOGICAL SURVEY; CARCINUS-MAENAS; PATHOLOGY; NECROSIS; DECAPOD; L.	While oxidative stress pathways are associated with a wide variety of tissue pathologies, its applications for evaluating and discerning ecological risks are limited. This study seeks to associate trends of lipid peroxidation and oxidative stress to risks of muscle pathologies in blue crabs inhabiting regions of the Lagos Lagoon. Crab samples (n = 520) were selected from pollution-impacted sites of the lagoon at Iddo, Ajah, Okobaba, Makoko, and the mid-lagoon area (control site). Antioxidant enzyme capacity, i.e., superoxide dismutase, catalase, glutathione peroxidase (GPx), and glutathione-S-transferase, and lipid peroxidation were evaluated in the muscle tissue of the blue crabs. The study findings showed distinct patterns of metal uptake in muscle, with redox-active metals (Cu and Zn) and redox-inactive metals (Pb and Cd) exhibiting site-specific differences. Additionally, there were changes in antioxidant modulation, lipid peroxidation, and the presence of associated myopathies. Blue crabs from sites (Makoko and Ajah) with greater uptake of redox-active metals (Cu and Zn) in muscle tissue showed higher trends of lipid peroxidation and the most prevalence of severe regression-type myopathies. Sites with lower uptake of redox-active metals showed the predominance of circulatory-type myopathies. This study also provides evidence of severe necrosis and myositis associated with digenean parasite cysts in crab muscle. Pathological evidence of severe skeletal muscle deterioration in the presence of greater lipid peroxidation could have implications for motor-neuron activity and reduced force-generating capacity necessary for adaptive responses in the wild. We conclude that elevated uptake of redox metals could aggravate the onset of myopathies in wild populations.	[Chukwuka, Azubuike Victor] Natl Environm Stand & Regulat Enforcement Agcy NES, Environm Qual Control Dept, Conservat Unit, Osogbo, Osun, Nigeria; [Jerome, Fisayo C.] Nigerian Inst Oceanog & Marine Res, Fisheries Resources Dept, Marine Biol Sect, Lagos, Nigeria; [Jerome, Fisayo C.; Hassan, Adesola; Adeogun, Aina O.] Univ Ibadan, Dept Zool, Ibadan, Nigeria; [Ebonwu, Benjamin] Nigerian Inst Oceanog & Marine Res, Fisheries Resources Dept, Aquaculture Sect, Lagos, Nigeria	University of Ibadan	Chukwuka, AV (通讯作者)，Natl Environm Stand & Regulat Enforcement Agcy NES, Environm Qual Control Dept, Conservat Unit, Osogbo, Osun, Nigeria.	zubbydoo@gmail.com						Achudume Albert, 2010, Journal of Water Resource and Protection, V2, P751, DOI 10.4236/jwarp.2010.28087; Adeogun AO, 2020, COMP BIOCHEM PHYS C, V229, DOI 10.1016/j.cbpc.2019.108676; AJAO EA, 1990, OIL CHEM POLLUT, V7, P85, DOI 10.1016/S0269-8579(05)80017-6; Al-Mayahi Basim, 2021, Iraqi Journal of Veterinary Sciences, V35, P245, DOI 10.33899/ijvs.2020.126748.1368; 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Sci. Pollut. Res.	OCT	2023	30	50					108565	108581		10.1007/s11356-023-29912-9	http://dx.doi.org/10.1007/s11356-023-29912-9		SEP 2023	17	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	W3QS0	37752391				2025-03-11	WOS:001074324400005
J	Wang, SY; Li, YC; Fan, BS; Cao, YH; You, HF; Wang, RR; Ge, YW; Da, S; She, ZJ; Zhang, Z; Zhang, SR; Li, CG				Wang, Siyu; Li, Yuecong; Fan, Baoshuo; Cao, Yihang; You, Hanfei; Wang, Rongrong; Ge, Yawen; Da, Shuoqiang; She, Zijing; Zhang, Zhen; Zhang, Shengrui; Li, Cange			Middle to late Holocene environmental evolution and sea level change on the west coast of Bohai Bay	QUATERNARY INTERNATIONAL			English	Article						Coastal wetland; Middle to Late Holocene; Geochemical elements; Sedimentary environment; Relative sea level change	ASIAN MONSOON; EAST; LAKE; CLIMATE; POLLEN; RISE; DEGLACIATION; HIGHSTAND; SEDIMENTS; DEPOSITS	Bohai Bay is a typical area of global change research in East Asia, due to its unique geographical location and shallow water environment. In this paper, we present the results of a study of grain-size, geochemistry, pollen and algae of a middle to late Holocene sediment core from Haixing wetland, which located on the west coast of Bohai Bay. The results show that: 1) Prior to 6700 cal a B.P., the content of Cl, Sr/Ca ratio were the highest, endmember analysis of grain size suggested EM2 were dominant, which is characteristic of marine sediment and the concentrations of Pediastrum and Typha (indicating a freshwater environment) pollen were lowest, overall indicating the maximum of relative sea level; 2) During 6700-5000 cal a B.P., and the Ti and K contents, EM1 (lacustrine sedimentary component) increased substantially, EM2 decreased, and EM3 (fluvial sedimentary component) began to appear. The concentrations of Pediastrum, Dinophyceae and Typha pollen began to increase. All these indicating that the relative sea level began to fall and the study area became a lagoon environment; 3) During 5000-3500 cal a B.P. the Ti and K content increased further; EM1 was dominant, EM2 was rare, indicating that the relative sea level decreased further and the lagoon gradually became enclosed; 4) After 3500 cal a B.P., the Ti content reached its maximum and the Cl content and Sr/Ca ratio decreased to their lowest levels. EM1 was dominant and EM2 was virtually absent; dinoflagellate cysts almost disappeared and there was large increase of Typha pollen, indicating the complete exclusion of a marine influence during most of this period. However, during 2500-2000 cal a B.P. the Cl and the Sr/Ca ratio increased slightly once again, indicating a transient transgression.	[Wang, Siyu; Li, Yuecong; Fan, Baoshuo; Cao, Yihang; You, Hanfei; Wang, Rongrong; Ge, Yawen; Da, Shuoqiang; Zhang, Shengrui; Li, Cange] Hebei Normal Univ, Coll Geog Sci, Shijiazhuang 050024, Hebei, Peoples R China; [Wang, Siyu; Li, Yuecong; Fan, Baoshuo; Cao, Yihang; You, Hanfei; Wang, Rongrong; Ge, Yawen; Da, Shuoqiang; Zhang, Shengrui; Li, Cange] Hebei Key Lab Environm Change & Ecol Construct, Shijiazhuang 050024, Hebei, Peoples R China; [Wang, Siyu; Li, Yuecong; Fan, Baoshuo; Cao, Yihang; You, Hanfei; Wang, Rongrong; Ge, Yawen; Da, Shuoqiang; Zhang, Shengrui; Li, Cange] Hebei Technol Innovat Ctr Remote Sensing Identific, Shijiazhuang 050024, Hebei, Peoples R China; [She, Zijing] Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Jiangsu, Peoples R China; [Zhang, Zhen] Hebei GEO Univ, Coll Earth Sci, Shijiazhuang 050031, Hebei, Peoples R China	Hebei Normal University; Nanjing University; Hebei GEO University	Li, YC; Fan, BS (通讯作者)，Hebei Normal Univ, Coll Geog Sci, Shijiazhuang 050024, Hebei, Peoples R China.	lyczhli@aliyun.com; fanbaoshuo2018@163.com	Zhang, Shengrui/P-1390-2019; Fan, Baoshuo/ACW-4046-2022; Ge, Yawen/LQJ-4950-2024		National Natural Science Foundation of China [CXZZBS2023088, U20A20116, 41877433, 42007404]; Graduate Innovation Grant Program of Hebei Province [CXZZBS2023088]; management of Haixing Wetland Nature Reserve in Hebei Province	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Graduate Innovation Grant Program of Hebei Province; management of Haixing Wetland Nature Reserve in Hebei Province	This research was supported by the National Natural Science Foundation of China (U20A20116, 41877433, & 42007404) , and the Graduate Innovation Grant Program of Hebei Province (CXZZBS2023088) . We would like to thank the management of Haixing Wetland Nature Reserve in Hebei Province for their support in the field work. We thank Prof. Weiming Gao from Hebei Normal University, Prof. Chunhai Li from Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, and Dr. Jiaxing Yang from Lanzhou University for their assistance in the sampling process. We thank Dr. Jan Bloemendal for correcting the English language.	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J	Woltz, CR; Anderson, RP; Tosca, NJ; Porter, SM				Woltz, C. R.; Anderson, R. P.; Tosca, N. J.; Porter, S. M.			The role of clay minerals in the preservation of Precambrian organic-walled microfossils	GEOBIOLOGY			English	Article						clay minerals; mineralogy; organic-walled microfossils; paleontology; Precambrian; preservation	SOFT-TISSUE PRESERVATION; ORDOVICIAN SOOM SHALE; SOUTH CHINA SEA; BURGESS-SHALE; MATTER PRESERVATION; FOSSIL PRESERVATION; EXCEPTIONAL PRESERVATION; DINOFLAGELLATE CYSTS; CELL-WALL; EXAMPLE	Precambrian organic-walled microfossils (OWMs) are primarily preserved in mudstones and shales that are low in total organic carbon (TOC). Recent work suggests that high TOC may hinder OWM preservation, perhaps because it interferes with chemical interactions involving certain clay minerals that inhibit the decay of microorganisms. To test if clay mineralogy controls OWM preservation, and if TOC moderates the effect of clay minerals, we compared OWM preservational quality (measured by pitting on fossil surfaces and the deterioration of wall margins) to TOC, total clay, and specific clay mineral concentrations in 78 shale samples from 11 lithologic units ranging in age from ca. 1650 to 650 million years ago. We found that the probability of finding well-preserved microfossils positively correlates with total clay concentrations and confirmed that it negatively correlates with TOC concentrations. However, we found no evidence that TOC influences the effect of clay mineral concentrations on OWM preservation, supporting an independent role of both factors on preservation. Within the total clay fraction, well-preserved microfossils are more likely to occur in shales with high illite concentrations and low berthierine/chamosite concentrations; however, the magnitude of their effect on preservation is small. Therefore, there is little evidence that bulk clay chemistry is important in OWM preservation. Instead, we propose that OWM preservation is largely regulated by physical properties that isolate organic remains from microbial degradation such as food scarcity (low TOC) and low sediment permeability (high total clay content): low TOC increases the diffusive distances between potential carbon sources and heterotrophic microbes (or their degradative enzymes), while high clay concentrations reduce sediment pore space, thereby limiting the diffusion of oxidants and degradative enzymes to the sites of decay.	[Woltz, C. R.; Porter, S. M.] Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA; [Woltz, C. R.] Stanford Univ, Dept Earth & Planetary Sci, Stanford, CA USA; [Anderson, R. P.] Univ Oxford, All Souls Coll, Oxford, England; [Anderson, R. P.] Univ Oxford, Dept Earth Sci, Oxford, England; [Tosca, N. J.] Univ Cambridge, Dept Earth Sci, Cambridge, England	University of California System; University of California Santa Barbara; Stanford University; University of Oxford; University of Oxford; University of Cambridge	Woltz, CR (通讯作者)，Univ Calif Santa Barbara, Dept Earth Sci, Santa Barbara, CA 93106 USA.; Woltz, CR (通讯作者)，Stanford Univ, Dept Earth & Planetary Sci, Stanford, CA 94305 USA.	cwoltz@stanford.edu	Tosca, Nicholas/MBH-4246-2025	Woltz, Christina/0000-0001-9364-2341; Anderson, Ross/0000-0002-0558-7563; Tosca, Nicholas/0000-0003-4415-4231; Porter, Susannah/0000-0002-4707-9428	All Souls College, University of Oxford; Clay Mineral Society; Geological Society of America; National Science Foundation; Royal Society; Simons Foundation	All Souls College, University of Oxford; Clay Mineral Society; Geological Society of America; National Science Foundation(National Science Foundation (NSF)); Royal Society(Royal Society); Simons Foundation	All Souls College, University of Oxford; Clay Mineral Society; Geological Society of America; National Science Foundation; Royal Society; Simons Foundation	Agic H., 2021, GEOLOGICAL SOC SPECI, V511, pG; Agic H, 2017, PRECAMBRIAN RES, V297, P101, DOI 10.1016/j.precamres.2017.04.042; Allison P., 1991, TAPHONOMY RELEASING, P25, DOI [10.1007/978-1-4899-5034-5_2, DOI 10.1007/978-1-4899-5034-5_2]; ALLISON PA, 1993, GEOLOGY, V21, P527, DOI 10.1130/0091-7613(1993)021<0527:EFRDOS>2.3.CO;2; Anderson EP, 2011, GEOLOGY, V39, P643, DOI 10.1130/G31969.1; Anderson RP, 2023, TRENDS ECOL EVOL, V38, P1060, DOI 10.1016/j.tree.2023.05.014; Anderson RP, 2021, GEOLOGY, V49, P355, DOI 10.1130/G48067.1; Anderson RP, 2020, INTERFACE FOCUS, V10, DOI 10.1098/rsfs.2020.0011; Anderson RP, 2018, GEOLOGY, V46, P347, DOI 10.1130/G39941.1; Arouri KR, 2000, ORG GEOCHEM, V31, P75, DOI 10.1016/S0146-6380(99)00145-X; Bartley JK, 1996, PALAIOS, V11, P571, DOI 10.2307/3515192; Baruch ET, 2015, AAPG BULL, V99, P1745, DOI 10.1306/04061514181; Becker-Kerber B, 2022, GEOL SOC AM BULL, V134, P1334, DOI 10.1130/B36033.1; Beghin J, 2017, PRECAMBRIAN RES, V299, P1, DOI 10.1016/j.precamres.2017.07.016; BJORKUM PA, 1988, J SEDIMENT PETROL, V58, P506; Briggs DEG, 2003, ANNU REV EARTH PL SC, V31, P275, DOI 10.1146/annurev.earth.31.100901.144746; BRIGGS DEG, 1993, PALEOBIOLOGY, V19, P107, DOI 10.1017/S0094837300012343; Briggs DEG, 2014, BIOESSAYS, V36, P482, DOI 10.1002/bies.201400010; Butler AD, 2015, P ROY SOC B-BIOL SCI, V282, DOI 10.1098/rspb.2015.0476; Butterfield NJ, 2012, GEOLOGY, V40, P71, DOI 10.1130/G32580.1; Butterfield N. 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J	Magohe, SP; Houben, AJP; Mtelela, C; Verreussel, RMCH; Janssen, NMM				Magohe, Stephen P.; Houben, Alexander JP.; Mtelela, Cassy; Verreussel, Roel MCH.; Janssen, Nico MM.			The first record of Permo-Triassic palynomorphs and palynological change across the Triassic-Jurassic transition in the onshore Ruvu Basin, Tanzania	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynology; Ruvu basin; Permo-Triassic; Triassic-Jurassic transition	LATE CRETACEOUS PALYNOFLORAS; SOUTHERN COASTAL TANZANIA; EAST-AFRICA; KAROO BASIN; GONDWANA; STRATIGRAPHY; EVOLUTION; BOUNDARY; HISTORY; BREAKUP	The Ruvu Basin in northeastern coastal Tanzania is one of the least studied basins in the country. It likely contains a record of the pre-and post-breakup sequences of the Gondwana supercontinent. In this study, the first comprehensive palynological investigation on drill-cuttings samples from the Makarawe-1 well in the Ruvu Basin was conducted. In the lower section of this well, four distinct palynologic intervals are recorded: Aratrisporites spp.-Klausipollenites schaubergeri interval (Upper Permian); Reduviasporonites spp. interval (Permo-Triassic transition); Extinction Interval (Permo-Triassic extinction) and Alisporites-Falcisporites Interval (Upper Triassic). This implies that the Ruvu Basin heralds a succession across the Permian-Triassic boundary and its associated extinction. We also record substantial palynological change across the transition to the upper portion of the Makarawe-1 well, where marine dinoflagellate cysts and abundant Classopollis pollen dominate the assemblage. Based on the ranges of dinoflagellate cysts supplemented by pollen-spore ranges, two main palynological intervals (the Classopollis-Nannoceratopsis interval and the Wanaea clathrata interval) are here established. These intervals are of late Middle Jurassic and Late Jurassic (Bajocian - Kimmeridgian) age. This suggests possible correlations with the Lugoba, Msata, Msolwa, Magindu and Malivundo formations of the Ruvu Basin. The findings presented herein suggest a downhole extension of the Wanaea clathrata interval (Oxfordian-Kimmeridgian) sensu [Msaky 2007] to 1215-1235 m. In addition, the Nannoceratopsis-dominated assemblage is indicative of an Early Jurassic association that developed during immediate post-break-up phase, with low-salinities and basinal restriction. With similarity to the Ngerengere dinocyst assemblage reported in previous studies, these results further suggest that the Ngerengere beds are not a so-called Karoo equivalent, but rather a syn- or postbreakup sequence. The recorded intervals are highly similar to other palynostratigraphic units of Africa, Australia, Europe and South America. The data collected in this study add important insights for the general stratigraphic framework within this poorly constrained coastal basin, while also providing a perspective on more distant correlations using palynology.	[Magohe, Stephen P.; Mtelela, Cassy] Univ Dar es Salaam, Dept Geosci, POB 35052, Dar Es Salaam, Tanzania; [Magohe, Stephen P.] Univ Calgary, Dept Earth Energy & Environm, 2500 Univ Dr NW, Calgary, AB T2N 1N4, Canada; [Houben, Alexander JP.; Verreussel, Roel MCH.; Janssen, Nico MM.] TNO Geol Survey Netherlands, POB 80015NL, NL-3508 TA Utrecht, Netherlands	University of Dar es Salaam; University of Calgary; Netherlands Organization Applied Science Research	Magohe, SP (通讯作者)，Univ Dar es Salaam, Dept Geosci, POB 35052, Dar Es Salaam, Tanzania.	stephen.magohe@ucalgary.ca; alexander.houben@tno.nl; cassymtelela@gmail.com; roel.verreussel@tno.nl; nico.janssen@tno.nl		Magohe, Stephen/0000-0002-0945-1655				Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; Ainsworth N.R., 1989, Northwest European Micropaleontology and Palynology, P1; ALVIN KL, 1982, REV PALAEOBOT PALYNO, V37, P71, DOI 10.1016/0034-6667(82)90038-0; BALDUZZI A, 1992, J AFR EARTH SCI, V15, P405, DOI 10.1016/0899-5362(92)90025-8; Bally A.W., 1981, Am. 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Afr. Earth Sci.	NOV	2023	207								105070	10.1016/j.jafrearsci.2023.105070	http://dx.doi.org/10.1016/j.jafrearsci.2023.105070		SEP 2023	22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	T7QI5					2025-03-11	WOS:001079888000001
J	Premaor, E; Ferreira, EP; Guerstein, GR; Souza, PA				Premaor, Eduardo; Ferreira, Elizabete P.; Guerstein, G. Raquel; Souza, Paulo A.			Eocene paleoceanographic and paleoclimatic events recognized by assemblages of dinoflagellate cysts in the Southwest Atlantic Ocean	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Palynology; Paleogene; Microplankton; Apectodinium homomorphum Enneadocysta; dictyostila; Antarctic species	THERMAL MAXIMUM; PELOTAS BASIN; DRAKE PASSAGE; ENVIRONMENTAL-CHANGES; APECTODINIUM ACME; NEOGENE SECTION; EARLIEST EOCENE; CLIMATE-CHANGE; SEA-LEVEL; PALEOCENE	Variations in the relative frequencies between cosmopolitan dinoflagellate cysts and Antarctic assemblage species indicate temperature changes and variations of ocean currents during the Paleogene. This study is based on the analysis of 23 samples from two stratigraphic intervals from the Well BP-01 (Imbe ' Formation), drilled by in the Pelotas Basin offshore. We identified 66 dinoflagellate cyst taxa, 47 of them belong to the Order Gonyaulacales and 19 to the Order Peridiniales. The relative abundance data highlight two different dinoflagellate ecogroups represented by Apectodinium and Enneadocysta in the intervals A and B, respectively. The level with the highest percentages of Apectodinium recorded in the Calcareous Nannofossil Zone N-410 (Ypresian), suggest that the Apectodinium maximum represents the Early Eocene Maximum Thermal Event (EMT-2). Enneadocysta Acmes registered near the Bartonian/Priabonian boundary, can be correlated with a drop in sea surface temperature that occurred after the Mid-Eocene Climatic Optimum. Dinoflagellate occurrences suggest deposition in open sea conditions during the transgressive phase. The P/G ratio does not reach significant values in the analyzed intervals, indicating low dissolved nutrient concentrations.	[Premaor, Eduardo] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Lab Palinol Marleni Marques Toigo, Programa Posgrad Geociencias,Inst Geociencias, Av Bento Goncalves 9500 Campus Vale, BR-91540000 Porto Alegre, RS, Brazil; [Ferreira, Elizabete P.] Petrobras Cenpes, Av Horacio Macedo 950,Predio 32, BR-21941915 Rio De Janeiro, RJ, Brazil; [Guerstein, G. Raquel] Univ Nacl Sur, Dept Geol, Inst Geol Sur, CONICET, Av Alem 1253, RA-8000 Bahia Blanca, BA, Argentina	Universidade Federal do Rio Grande do Sul; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Premaor, E (通讯作者)，Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Lab Palinol Marleni Marques Toigo, Programa Posgrad Geociencias,Inst Geociencias, Av Bento Goncalves 9500 Campus Vale, BR-91540000 Porto Alegre, RS, Brazil.	eduardopremaor@gmail.com; elizabete@petrobras.com.br; raquel.guerstein@uns.edu.ar; paulo.alves.souza@ufrgs.br						Agnini C, 2007, MAR MICROPALEONTOL, V64, P215, DOI 10.1016/j.marmicro.2007.05.003; Agnini C, 2011, GEOL SOC AM BULL, V123, P841, DOI 10.1130/B30158.1; Aleksandrova GN, 2011, STRATIGR GEO CORREL+, V19, P424, DOI 10.1134/S0869593811040022; Alroy J, 2000, PALEOBIOLOGY, V26, P259, DOI 10.1666/0094-8373(2000)26[259:GCCANA]2.0.CO;2; Amenábar CR, 2022, PALAEONTOLOGY, V65, DOI 10.1111/pala.12601; Amenábar CR, 2020, GEOL MAG, V157, P351, DOI 10.1017/S0016756819000591; Anjos-Zerfass G.S., 2008, Rev. 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South Am. Earth Sci.	OCT	2023	130								104587	10.1016/j.jsames.2023.104587	http://dx.doi.org/10.1016/j.jsames.2023.104587		SEP 2023	20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	T3YJ6					2025-03-11	WOS:001077372900001
J	Rodríguez-Villegas, C; Figueroa, RI; Baldrich, AM; Pérez-Santos, I; Díaz, M; Tomasetti, SJ; Seguel, M; Alvarez, G; Salgado, P; Díaz, PA				Rodriguez-Villegas, Camilo; Figueroa, Rosa I.; Baldrich, Angela M.; Perez-Santos, Ivan; Diaz, Manuel; Tomasetti, Stephen J.; Seguel, Miriam; Alvarez, Gonzalo; Salgado, Pablo; Diaz, Patricio A.			Small and patchy is enough: An example about how toxic HAB events can spread through low resting cyst loads	HARMFUL ALGAE			English	Article						Alexandrium catenella; Strain sexual compatibility; Resting cysts; Ecoregion; Chilean Patagonia; Paralytic Shellfish Poisoning	ALEXANDRIUM-CATENELLA WHEDON; KOFOID BALECH 1985; SOUTHERN CHILE; SURFACE SEDIMENTS; DINOFLAGELLATE BLOOMS; PATAGONIA; ABUNDANCE; DINOPHYCEAE; POPULATION; SALINITY	The frequency of harmful algal blooms (HABs) has increased over the last two decades, a phenomenon enhanced by global climate change. However, the effects of climate change will not be distributed equally, and Chile has emerged as one important, vulnerable area. The Chilean Patagonian region (41-56 degrees S) hosts two marine ecor-egions that support robust blue economies via wild fisheries, aquaculture, and tourism. However, the harmful algal bloom-forming dinoflagellate Alexandrium catenella, a causative agent of paralytic shellfish poisoning outbreaks, threatens the viability of blue industries in this region and others worldwide. Despite the proliferation of A. catenella blooms over the last few decades, the role of sedimentary resting cysts in the recurrence of harmful algal blooms and the species' northward expansion across Chilean Patagonia is not well understood. As a resting cyst-producing species, the sediment-cyst dynamics of A. catenella likely contribute to the geographical expansion and bloom recurrence of this species. For this purpose, we analyzed a decade of A. catenella surface sediment cyst records across the two ecoregions of the Chilean Patagonian System that were further stratified into five sub -regions based on water temperature, salinity, dissolved oxygen, and nutrient characteristics. We also analyzed spatio-temporal cyst dynamics in a pre-, during-, and post-bloom scenario of the Chiloense ecoregion (more northern) of the Magellanic province. Our results indicated highly variable A. catenella resting cyst abundances, with a maximum of 221 cysts cm-3 recorded in 2002 after an intense bloom. Generalized linear mixed models and linear mixed models found that sampling season, subregion, and Total Organic Matter (%) explained resting cyst presence and density. The results also demonstrated the presence of A. catenella cysts in northern subregions, evidencing the northward geographical expansion observed during the last few decades. The risks of A. catenella bloom recurrence from small, patchy resting cyst distributions across broad geographical areas and under changing environmental conditions are discussed.	[Rodriguez-Villegas, Camilo] Univ Las Lagos, Programa Doctorado Ciencias, Menc Conservac & Manejo Recursos Nat, Camino Chinquihue Km 6, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Baldrich, Angela M.; Perez-Santos, Ivan; Diaz, Patricio A.] Univ Los Lagos, Ctr i mar, Casilla 557, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Baldrich, Angela M.; Diaz, Patricio A.] Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt, Chile; [Figueroa, Rosa I.] CSIC, Ctr Oceanog Vigo, Inst Espanol Oceanog IEO, Subida Radio Faro 50, Vigo 36390, Spain; [Perez-Santos, Ivan] Univ Concepcion, Ctr Invest Oceanog COPAS COASTAL, Concepcion, Chile; [Diaz, Manuel] Univ Austral Chile, Programa Invest Pesquera, Inst Acuicultura, Puerto Montt, Chile; [Tomasetti, Stephen J.] Univ Maryland Eastern Shore, Dept Nat Sci, Princess Anne, MD USA; [Seguel, Miriam] Univ Austral Chile, Ctr Reg Anal Recursos & Medio Ambiente CERAM, Los Pinos S-N, Balneario Pelluco, Puerto Montt, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Dept Acuicultura, Larrondo 1281, Coquimbo 1781421, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Ctr Invest & Desarrollo Tecnol Algas CIDTA, Larrondo 1281, Coquimbo, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Ctr Ecol & Sustainable Management Ocean Isl ESMOI, Dept Biol Marina, Coquimbo, Chile; [Salgado, Pablo] Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Enr Abello 0552, Punta Arenas, Chile; [Perez-Santos, Ivan] Ctr Invest Ecosistemas Patagonia CIEP, Coyha, Chile	Universidad de Los Lagos; Universidad de Los Lagos; Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); Universidad de Concepcion; Universidad Austral de Chile; University System of Maryland; University of Maryland Eastern Shore; Universidad Austral de Chile; Universidad Catolica del Norte; Universidad Catolica del Norte; Universidad Catolica del Norte; Instituto de Fomento Pesquero (Valparaiso)	Rodríguez-Villegas, C (通讯作者)，Univ Las Lagos, Programa Doctorado Ciencias, Menc Conservac & Manejo Recursos Nat, Camino Chinquihue Km 6, Puerto Montt, Chile.; Rodríguez-Villegas, C (通讯作者)，Univ Los Lagos, Ctr i mar, Casilla 557, Puerto Montt, Chile.	camilo.rodriguez@ulagos.cl	Alvarez, Gonzalo/W-1262-2017; Díaz, Manuel/AAM-6225-2021; Salgado, Pablo/KMA-0636-2024; Díaz, Patricio/B-8128-2018; Perez, Ivan/B-9321-2018; Baldrich, Angela M./AAC-8054-2022; Figueroa, Rosa/M-7598-2015; Rodriguez Villegas, Camilo/AAB-8563-2022	Baldrich, Angela M./0000-0002-2624-7357; Alvarez Vergara, Gonzalo/0000-0001-5812-1559; Tomasetti, Stephen/0000-0001-6947-5141; Salgado, Pablo/0000-0002-4168-3675; Figueroa, Rosa/0000-0001-9944-7993; Rodriguez Villegas, Camilo/0000-0002-1429-2775	Comite Oceanografico Nacional (CONA) [CF-07, CF-10, CF-11, CF-12, CF-13, CF-14, CF-15, CF-16, FB210021, R20F002]; Centro de Biotecnologia y Bioingenieria (CeBiB) (PIA project, ANID, Chile) [FB0001]; COPAS COASTAL [CF-10, CF-11, BIOTOX PID2021-1256430B-C22]; CIEP; Spanish Ministry of Science and Innovation; European Community, European Regional Development Fund (ERDF);  [CF-08];  [CF-09]	Comite Oceanografico Nacional (CONA); Centro de Biotecnologia y Bioingenieria (CeBiB) (PIA project, ANID, Chile); COPAS COASTAL; CIEP(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT Regional/CIEP); Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); European Community, European Regional Development Fund (ERDF); ; 	This work was funded by Comite Oceanografico Nacional (CONA, CF-07 to CF-16 projects), Centro de Biotecnologia y Bioingenieria (CeBiB) (PIA project FB0001, ANID, Chile), and by COPAS COASTAL FB210021, and CIEP R20F002. Rosa I. Figueroa was funded by a national project from the Spanish Ministry of Science and Innovation and the European Community, European Regional Development Fund (ERDF; Project BIOTOX PID2021-1256430B-C22). The authors also acknowledge the AGS-61 "Cabo de Hornos" crew and their commandants of the Chilean Navy for the human and technical support of the oceanographic campaigns. The work aboard the Servicio Hidrografico y Oceanografico of the Chilean Navy (SHOA) is also recognized.	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J	Guerrero-Murcia, LA; Helenes, J				Guerrero-Murcia, Luis-Andres; Helenes, Javier			Upper Cretaceous dinoflagellate cysts events from the sub-tropical northern hemisphere	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Fossil dinoflagellates; Upper cretaceous; Sub-tropical localities; Quantitative biostratigraphy	EASTERN EQUATORIAL PACIFIC; SEQUENCE STRATIGRAPHY; SURFACE SEDIMENTS; BAJA-CALIFORNIA; WESTERN DESERT; BIOSTRATIGRAPHY; PALYNOLOGY; BASIN; BOREHOLE; RANKING	Recognizing the ranking optime sequence of fossil dinoflagellate cysts can be a challenge for qualitative biostratigraphy. For this reason, we present the result of a quantitative stratigraphic study through probabilistic analysis of six wells from Baja California (Mexico) and six from the Gulf of Suez and the Mediterranean Sea (Egypt), which allows us to recognize 22 species of dinoflagellate cysts in an optimal sequence with 95% probability for the Upper Cretaceous in subtropical areas of the Northern Hemisphere. Photoautotrophic species represent the largest number in the database (159 species), indicating that they are the main producers, while heterotrophic species are in the minority (74 species). Spiniferites and Florentinia are the most abundant and diverse taxa, which, together with the absence of the genus Impagidinium, indicates a shallow marine depositional environment. The quantitative analysis estimates an optimal classified succession that allows the Upper Cretaceous to be divided into five groups (G1 to G5) of species communities with similar ages. The greatest species diversity is found in group G4, associated with the Maastrichtian, and the least in group G1, associated with the early Cenomanian to early Turonian. These results and comparison with previous studies using the same method of quantitative biostratigraphy suggest a similarity of paleoenvironmental conditions in subtropical regions of the Northern Hemisphere and tropical regions during the Upper Cretaceous.	[Guerrero-Murcia, Luis-Andres; Helenes, Javier] Ctr Estudios Cient & Educ Super Ensenada, Dept Geol, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico		Guerrero-Murcia, LA (通讯作者)，POB 434843, San Diego, CA 92143 USA.	lguerrero@cicese.mx; jhelenes@cicese.mx		GUERRERO, LUIS/0000-0003-1751-0341				Agterberg FP, 2013, COMPUT GEOSCI-UK, V54, P279, DOI 10.1016/j.cageo.2013.01.002; Agterberg FP, 1999, EARTH-SCI REV, V46, P1, DOI 10.1016/S0012-8252(99)00007-0; Al-Ameri TK, 2001, CRETACEOUS RES, V22, P735, DOI 10.1006/cres.2001.0288; Alsharhan AS, 2003, AAPG BULL, V87, P143; Arai M., 1994, Simposio sobre o Cretaceo do Brasil, V3, P59; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BERTHOU PY, 1990, REV PALAEOBOT PALYNO, V66, P313, DOI 10.1016/0034-6667(90)90045-K; BINT A N, 1986, Palynology, V10, P135; Bouimetarhan I, 2009, QUATERNARY RES, V72, P188, DOI 10.1016/j.yqres.2009.05.003; Boyd JL, 2018, EARTH-SCI REV, V177, P366, DOI 10.1016/j.earscirev.2017.11.018; 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J	Ineson, JR; Bowman, VC; Crame, JA; Whittle, RJ; Francis, JE				Ineson, Jon R.; Bowman, Vanessa C.; Crame, J. Alistair; Whittle, Rowan J.; Francis, Jane E.			Sequence stratigraphy of a wave-dominated, tidally influenced delta in the Danian of Seymour Island, Antarctica: An integrated sedimentological-palaeoecological approach	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Antarctic Peninsula; James Ross Basin; Sobral Formation; Paleocene; Palynology; Invertebrate macrofauna	INCLINED HETEROLITHIC STRATIFICATION; CHORATE DINOFLAGELLATE CYSTS; BACK-ARC BASIN; CRETACEOUS STRATIGRAPHY; MARAMBIO GROUP; NEW-JERSEY; PALEOCENE; DEPOSITS; EVOLUTION; BOUNDARY	Lower Paleocene marine siliciclastics of the Sobral Formation (Seymour Island, Antarctica) form an important component of a key southern high latitude reference section for the Maastrichtian-Eocene. The formation comprises a coarsening-upward, regressive succession (270 m thick), shallowing from prodeltaic, mud-rich to sandy nearshore sediments. Sedimentary facies analysis, integrated with macrofaunal and microfloral palaeoecological studies, indicate a wave-dominated, tidally influenced deltaic environment. Four depositional sequences (1-4) record the role of relative sea-level changes in controlling the stepwise progradation of the system. Prodeltaic and distal delta-front deposits (Sequences 1, 2), comprise coarsening-upward parasequences of mudrich heteroliths and bioturbated fine-grained muddy sands displaying draped slump scars. The overlying erosional sequence boundary is marked by incised valleys filled with fluvio-estuarine sediments; succeeding sand-rich facies (Sequences 3, 4) represent the proximal delta front and delta platform. The macro-invertebrate and palynological datasets display contrasting responses to the regressive history of the formation. The macrofaunal record in the distal deltaic sediments reflects the marine influence, though a stratigraphic increase in diversity was controlled both by ecological factors and biotic recovery following the K-Pg event. The associated palynological assemblage also displays a strong marine signal and includes typical outer neritic - oceanic dinoflagellate cyst taxa. A sharp decline in macrofossil diversity and abundance in Sequences 3, 4 is compatible with ecological stress in shallow-water, restricted inshore settings. Though the palynological record at this level is terrestrially dominated, the marine component reflects the cosmopolitan nature of dinoflagellates, displaying the highest diversities in the formation. The regressive Sobral Formation ended a protracted c. 60 Myr history of regional subsidence and marine sedimentation; although amplified by two Danian sea-level falls of probable eustatic origin, the regressive trend heralded mid-Paleocene basin inversion potentially linked to the onset of regional tectonic reorganization that ultimately led to opening of the Scotia Sea.	[Ineson, Jon R.] Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Bowman, Vanessa C.; Crame, J. Alistair; Whittle, Rowan J.; Francis, Jane E.] British Antarctic Survey, Madingley Rd, Cambridge CB3 OET, England; [Bowman, Vanessa C.] Jesus Coll, Jesus Lane, Cambridge CB5 8BL, England	Geological Survey Of Denmark & Greenland; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of Cambridge	Ineson, JR (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	ji@geus.dk; jacr@bas.ac.uk; roit@bas.ac.uk; janefr@bas.ac.uk			Carlsberg Foundation [2009/01/0702]; GEUS (Geological Survey of Denmark); British Antarctic Survey Polar Science for Planet Earth Programme; NERC (UK) [NE/I005803/1, NE/I00582X/1]	Carlsberg Foundation(Carlsberg Foundation); GEUS (Geological Survey of Denmark); British Antarctic Survey Polar Science for Planet Earth Programme; NERC (UK)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The professional logistic support of the British Antarctic Survey during the 2009-10 field season is gratefully acknowledged, as is the generous hospitality of the personnel at the Argentinian Marambio base on Seymour Island. We also thank the following: Tom Weston for his patient and highly competent field assistance, Peter Bucktrout (BAS) for photographic support, and Teal Riley (BAS) for discussion of the regional tectonic context. Jette Halskov and Jacob Lind Bendtsen (both GEUS) produced the figures. We thank three anonymous reviewers for their constructive and insightful comments and suggestions. JI's field participation was supported financially by the Carlsberg Foundation (grant 2009/01/0702) , and subsequent participation in the Paleopolar project by GEUS (Geological Survey of Denmark and Greenland) ; publication by this author is by permission of GEUS. The Paleopolar project, funded by NERC (UK) grants NE/I005803/1 and NE/I00582X/1, is a part of the British Antarctic Survey Polar Science for Planet Earth Programme.	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Paleoclimatol. Paleoecol.	NOV 1	2023	629								111789	10.1016/j.palaeo.2023.111789	http://dx.doi.org/10.1016/j.palaeo.2023.111789		SEP 2023	22	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	T5SK1					2025-03-11	WOS:001078583800001
J	Lindström, S				Lindstrom, Sofie			Valvaeodinium hymenosynypha (Morbey) comb. nov., a dinoflagellate cyst from the uppermost Triassic and lowermost Jurassic (Rhaetian and Hettangian) of Europe	PALYNOLOGY			English	Article						Europe; Jurassic (Hettangian) morphology; taxonomy; Triassic (Rhaetian)		Cymatiosphaera hymenosynypha Morbey 1975, previously recorded from the Rhaetian Westbury Formation in the United Kingdom, occurs in Triassic-Jurassic boundary strata from Denmark. From the present study it is clear that this small, finely reticulate, ellipsoidal, two-layered palynomorph is not a prasinophyte, but a dinoflagellate cyst with a combination apical/intercalary archaeopyle (type tAtI) which involves three apical plates plus one intercalary plate. This cavate cyst is morphologically similar but not identical to Valvaeodinium hanneae Piasecki 2001 from the uppermost Bathonian to lower Callovian of East Greenland, and it is therefore here transferred to Valvaeodinium, as Valvaeodinium hymenosynypha (Morbey) Lindstrom comb. nov. The appearance of Valvaeodinium hymenosynypha in Rhaetian strata in the Danish Basin suggests that the lineage of cavate Valvaeodinium cysts originated in the Late Triassic alongside a chorate species of the genus. Valvaeodinium hymenosynypha seems to have survived just barely past the end-Triassic mass extinction as it is also present in the earliest Hettangian.	[Lindstrom, Sofie] Dept Geosci & Nat Resource Management, Copenhagen, Denmark; [Lindstrom, Sofie] GEUS Geol Survey Denmark & Greenland, Copenhagen, Denmark; [Lindstrom, Sofie] Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Lindstrom, Sofie] GEUS Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland; Geological Survey Of Denmark & Greenland	Lindström, S (通讯作者)，Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.; Lindström, S (通讯作者)，GEUS Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	msl@ign.ku.dk	Lindström, Sofie/G-5481-2018	Lindstrom, Malin Sofie/0000-0001-8278-1055	Daniel Mantle and one anonymous reviewer, as well as the editor Jim Riding, are gratefully acknowledged for their comments and helpful suggestions that improved the manuscript.	Daniel Mantle and one anonymous reviewer, as well as the editor Jim Riding, are gratefully acknowledged for their comments and helpful suggestions that improved the manuscript.	Daniel Mantle and one anonymous reviewer, as well as the editor Jim Riding, are gratefully acknowledged for their comments and helpful suggestions that improved the manuscript.	Adl SM, 2005, J EUKARYOT MICROBIOL, V52, P399, DOI 10.1111/j.1550-7408.2005.00053.x; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; Bijl PK, 2022, EARTH SYST SCI DATA, V14, P579, DOI 10.5194/essd-14-579-2022; Butschli O., 1885, DR HG BRONNS KLASSEN; Davies E.H., 1983, Geological Survey of Canada Bulletin, P1; Dorhofer G., 1980, MISCELLANEOUS PUBLIC, P91; Fensome R.A., 1993, CLASSIFICATION FOSSI; Habib D., 1972, DEEP SEA DRILLING PR, V11, P367; Lentin JK., 1993, CONTRIBUTIONS SERIES, V28; Lindström S, 2023, PALYNOLOGY, V47, DOI 10.1080/01916122.2023.2241068; Mangerud G, 2019, REV PALAEOBOT PALYNO, V261, P53, DOI 10.1016/j.revpalbo.2018.11.010; Mantle DJ, 2020, REV PALAEOBOT PALYNO, V281, DOI 10.1016/j.revpalbo.2020.104254; Mantle DJ, 2012, REV PALAEOBOT PALYNO, V180, P41, DOI 10.1016/j.revpalbo.2012.03.005; Morbey J., 1975, Palaeontographica B, V152, P1; MORBEY SJ, 1974, REV PALAEOBOT PALYNO, V17, P161, DOI 10.1016/0034-6667(74)90097-9; Morgenroth P., 1970, Neues Jb. Geol. Palaont. Abh., V136, P345; Palliani RB, 1997, REV PALAEOBOT PALYNO, V96, P99, DOI 10.1016/S0034-6667(96)00019-X; Pascher A., 1914, Berlin Ber D bot Ges, V32; Piasecki S, 2001, NEUES JAHRB GEOL P-A, V219, P15, DOI 10.1127/njgpa/219/2001/15; Poulsen N.E., 1990, Danmarks Geologiske Undersogelse Serie C, V10, P1; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Riding JB, 2021, PALYNOLOGY, V45, P1, DOI 10.1080/01916122.2021.1878305; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; Smelror M., 1991, Journal of Micropalaeontology, V10, P175; Vozzhennikova TF., 1979, DOKL AKAD NAUK, V422, P1	26	0	0	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	SEP 13	2023	47	4								10.1080/01916122.2023.2252482	http://dx.doi.org/10.1080/01916122.2023.2252482		SEP 2023	8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	X3LR6					2025-03-11	WOS:001070308900001
J	Sharman, GR; Szymanski, E; Hackworth, RA; Kahn, ACM; Febo, LA; Oefinger, J; Gregory, GM				Sharman, Glenn R.; Szymanski, Eugene; Hackworth, Rebecca A.; Kahn, Alicia C. M.; Febo, Lawrence A.; Oefinger, Jordan; Gregory, Gunnar M.			Carbon isotope chemostratigraphy, geochemistry, and biostratigraphy of the Paleocene-Eocene Thermal Maximum, deepwater Wilcox Group, Gulf of Mexico (USA)	CLIMATE OF THE PAST			English	Article							SEA-LEVEL; ENVIRONMENTAL-CHANGES; DRAINAGE REORGANIZATION; EASTERN MEXICO; CLIMATE-CHANGE; SEDIMENT FLUX; BASIN; EVOLUTION; HISTORY; MARINE	The Paleocene-Eocene Thermal Maximum (PETM) represents the most pronounced hyperthermal of the Cenozoic era and is hypothesized to have resulted in an intensification of the paleohydrologic cycle, including enhanced seasonality and increased sediment discharge to the coastal ocean. Although the PETM has been widely documented, there are few records from deposits that form the distal, deepwater components of large sediment-routing systems. This study presents new constraints on the stratigraphic placement of the PETM in the deepwater Gulf of Mexico basin through analysis of geochemical, carbon isotopic, and biostratigraphic data within a similar to 124 m cored interval of the Wilcox Group. Biostratigraphic and carbon isotopic data indicate that the PETM extends over similar to 13 m based on acmes in the dinoflagellate Apectodinium homomorphum and calcareous nannoplankton Rhomboaster cuspis as well as a similar to - 2 parts per thousand shift in bulk organic delta 13 C values. A decrease in bioturbation and benthic foraminifera suggests that a reduction in oxygen of Gulf of Mexico bottom waters and/or an increase in sedimentation rates were coincident with the onset of the PETM. A similar to 2 m lag in the depositional record separates the onset of the PETM negative carbon isotope excursion (CIE) and deposition of a 5.7 m thick interval of organic-lean claystone and marlstone that reflects a shut-off of the supply of sand, silt, and terrestrial palynomorphs to the basin.We interpret deposits of the PETM in the deepwater Gulf of Mexico to reflect the combined effects of increased erosional denudation and rising sea level that resulted in sequestration of sand and silt near the coastline but that allowed delivery of terrigenous mud to the deep sea. The similarity of oceanographic changes observed in the Gulf of Mexico and Atlantic Ocean during the PETM supports the inference that these water masses were connected during latest Paleocene-earliest Eocene times. Although deposition of typical Wilcox Group facies resumed during and after the PETM recovery, an increased influx of terrestrial detritus (i.e., pollen, spores, terrestrial organic debris) relative to marine dinoflagellates is suggestive of long-lasting effects of the PETM. This study illustrates the profound and prolonged effects of climatic warming on even the most distal reaches of large ( >= 1 x 10 6 km 2 ) sediment-routing systems.	[Sharman, Glenn R.; Szymanski, Eugene; Oefinger, Jordan; Gregory, Gunnar M.] Univ Arkansas, Dept Geosci, Fayetteville, AR 72701 USA; [Szymanski, Eugene] Utah Geol Survey, 1594 W North Temple,Suite 3110, Salt Lake City, UT 84116 USA; [Hackworth, Rebecca A.; Kahn, Alicia C. M.; Febo, Lawrence A.] Chevron Technol Ctr, 1500 Louisiana St, Houston, TX 77002 USA	University of Arkansas System; University of Arkansas Fayetteville	Sharman, GR (通讯作者)，Univ Arkansas, Dept Geosci, Fayetteville, AR 72701 USA.	gsharman@uark.edu			Chevron Gulf of Mexico Business Unit	Chevron Gulf of Mexico Business Unit	We thank the Chevron Gulf of Mexico Business Unit and the Chevron Technology Center for access to core, scientific conversations, and the approval to publish these data. Erin Meyers and Ellen Reat Wersan provided useful reviews of early manuscripts. Erik Pollock at the University of Arkansas Stable Isotope Laboratory (UASIL) assisted with laboratory analyses. We thank Mac McGilvery for helpful discussions of Wilcox Group depositional facies.	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Past.	SEP 5	2023	19	9					1743	1775		10.5194/cp-19-1743-2023	http://dx.doi.org/10.5194/cp-19-1743-2023			33	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	HT7M3		gold, Green Submitted			2025-03-11	WOS:001161823800001
J	Telesinski, MM; Pospelova, V; Mertens, KN; Kucharska, M; Zajaczkowski, M				Telesinski, Maciej M.; Pospelova, Vera; Mertens, Kenneth Neil; Kucharska, Malgorzata; Zajaczkowski, Marek			Dinoflagellate cysts and benthic foraminifera from surface sediments of Svalbard fjords and shelves as paleoenvironmental indicators	OCEANOLOGIA			English	Article						North Atlantic; Nordic Seas; Sea ice; Primary productivity; Fjords; Sediments; Chlorophyll-a	NORTHERN NORTH-ATLANTIC; PALAEO SEA-ICE; ARCTIC FJORD; FRESH-WATER; DISTRIBUTION PATTERNS; ESTUARINE SEDIMENTS; BRINE PRODUCTION; BARENTS SEA; ASSEMBLAGES; ADVENTFJORDEN	Due to the Arctic amplification effect, the Svalbard archipelago is an important area for studying ongoing environmental changes. However, its marine ecosystem is extremely complex. In this study, we analyze modern assemblages of dinoflagellate cysts (dinocysts) and benthic foraminifera from surface sediment samples around Svalbard. We use multivariate statistical analyses to examine relationships between environmental conditions (summer and winter sea surface temperature and salinity, sea-ice cover, etc.) and both microfossil groups to evaluate their use as proxies for reconstructions of the marine environment in the region. Our results show that the most important factor controlling the environment around Svalbard is the Atlantic Water which mostly impacts the western coast, but its influence reaches as far as the eastern coast of Nordaustlandet. However, on a local scale, such factors as the sea-ice cover, the presence of tidewater glaciers, or even the morphology and hydrology of fjords become increasingly important. We found that two dinocyst species, cysts of Polarella glacialis and Echinidinium karaense, can be considered regional winter drift ice indicators. The relationships between environmental parameters and benthic foraminiferal assemblages are much more difficult to interpret. Although statistical analysis shows a correlation of benthic foraminiferal species with various environmental parameters, this correlation might be some what coincidental and caused by other factors not analyzed in this study. Nevertheless, the use of two complementary microfossil groups as (paleo)environmental indicators can provide a more comprehensive picture of the environmental conditions.(c) 2023 Institute of Oceanology of the Polish Academy of Sciences. Production and hosting by Elsevier B.V.This is an open access article under the CC BY-NC-ND license ( http://creativecommons.org/licenses/by-nc-nd/4.0/ ).	[Telesinski, Maciej M.; Kucharska, Malgorzata; Zajaczkowski, Marek] Polish Acad Sci, Inst Oceanol, Sopot, Poland; [Pospelova, Vera] Univ Minnesota, Coll Sci & Engn, Dept Earth & Environm Sci, Minneapolis, MN USA; [Mertens, Kenneth Neil] Ifremer, LITTORAL, Concarneau, France; [Telesinski, Maciej M.] Polish Acad Sci, Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland	Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; University of Minnesota System; University of Minnesota Twin Cities; Ifremer; Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences	Telesinski, MM (通讯作者)，Polish Acad Sci, Inst Oceanol, Powstancow Warszawy 55, PL-81712 Sopot, Poland.	mtelesinski@iopan.pl	Mertens, Kenneth/AAO-9566-2020; Telesiński, Maciej Mateusz/K-1717-2017; Mertens, Kenneth/C-3386-2015; Telesinski, Maciej Mateusz/I-6527-2015	Mertens, Kenneth/0000-0003-2005-9483; Zajaczkowski, Marek/0000-0002-3823-7359; Pospelova, Vera/0000-0003-4049-8133; Telesinski, Maciej Mateusz/0000-0002-5765-2849	National Science Centre, Poland - Norwegian Financial Mechanism [2014/15/N/ST10/05115]; National Science Centre, Poland [2019/34/H/ST10/00682, 2020/39/B/ST10/01698]	National Science Centre, Poland - Norwegian Financial Mechanism; National Science Centre, Poland(National Science Centre, Poland)	Study design and data collection (dinocyst analyses) have been supported by grant no. 2014/15/N/ST10/05115 funded by the National Science Centre, Poland . Data collection (foraminiferal analyses) and statistical analysis have been funded by Norwegian Financial Mechanism for 2014-2021, project no. 2019/34/H/ST10/00682. Data interpretation and manuscript preparation have been supported by grant no. 2020/39/B/ST10/01698 funded by the National Science Centre, Poland .	AAGAARD K, 1987, J GEOPHYS RES-OCEANS, V92, P3778, DOI 10.1029/JC092iC04p03778; Ahrens MJ, 1997, J MARINE SYST, V10, P445, DOI 10.1016/S0924-7963(96)00052-8; Akimova A, 2011, DEEP-SEA RES PT I, V58, P403, DOI 10.1016/j.dsr.2011.02.001; Ambrose WG, 2006, GLOBAL CHANGE BIOL, V12, P1595, DOI 10.1111/j.1365-2486.2006.01181.x; [Anonymous], 1990, Pol. 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J	Liu, YY; Hu, ZX; Gu, HF; Tao, Z; Deng, YY; Shang, LX; Chai, ZY; Tang, YZ				Liu, Yuyang; Hu, Zhangxi; Gu, Haifeng; Tao, Zhe; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying Zhong			<i>Biecheleria donggangensis sp. nov</i>. (Suessiaceae, Dinophyceae), a new marine woloszynskioid species germinated from coastal sediment of the Yellow Sea, China	PHYCOLOGIA			English	Article						Amphiesmal vesicle (AV); Dinoflagellates; Genetic distance; Nucleus-encoded rDNA; Phylogeny	ELECTRON-MICROSCOPY; RDNA SEQUENCES; LAKE TOVEL; COMB. NOV; GEN. NOV.; DINOFLAGELLATE; ULTRASTRUCTURE; PHYLOGENY; CINCTA; APPROXIMATION	A new marine woloszynskioid dinoflagellate, Biecheleria donggangensis sp. nov., germinated from the sediments of Rizhao coastal area, China, was examined by light and scanning electron microscopy. Its phylogenetic position was inferred from nuclear rDNA (partial LSU, SSU and ITS1-5.8S-ITS2) sequences. Cells were spherical to ellipsoidal (8.5-19.2 mu m long and 5.9-11.5 mu m wide) with numerous small and discoid chloroplasts, and a centrally located nucleus. Scanning electron microscopy showed an apical furrow area consisting of a single elongated apical vesicle (EAV) with 20 to 34 small globular knobs at the top of the epicone, and 13-15 latitudinal series of amphiesmal vesicles (AVs). Biecheleria donggangensis can be distinguished from other congeneric species by the configuration of the AVs bordering the EAV, the number of latitudinal AVs, and the trichocyst pore (TP) structures around the EAV. Thick-walled and spherical (or oval) cysts were 16.1-23.5 mu m in diameter and decorated with needle-like processes, each with a distal swelling. Molecular phylogenies using maximum likelihood (ML) were examined by three statistical methods (bootstrap, approximate Bayes and the Shimodaira-Hasegawa-like approximate likelihood-ratio test), which clearly demonstrated that the isolate belonged to the genus Biecheleria but formed a clade distinct from all previously described species. Genetic distance analyses justified describing the isolate as a new species rather than a new ribotype of B. cincta.	[Liu, Yuyang; Hu, Zhangxi; Tao, Zhe; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Liu, Yuyang; Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying Zhong] Laoshan Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Liu, Yuyang; Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Tao, Zhe] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Gu, Haifeng] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Hu, Zhangxi] Guangdong Ocean Univ, Coll Fisheries, Dept Aquaculture, Zhanjiang 524088, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; Guangdong Ocean University	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)，Laoshan 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	Chai, Zhaoyang/F-7485-2017; Li, Yang/KFB-5350-2024; ZHANG, hui jie/HTN-1690-2023; Tao, Zhe/LIG-2380-2024; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	National Science Foundation of China [42106199]; Science & Technology Basic Resources Investigation Program of China [2018FY100204]; Science and Technology Innovation Project of Laoshan Laboratory [LSKJ202203700]	National Science Foundation of China(National Natural Science Foundation of China (NSFC)); Science & Technology Basic Resources Investigation Program of China; Science and Technology Innovation Project of Laoshan Laboratory	This work was financially supported by the National Science Foundation of China (No. 42106199), the Science & Technology Basic Resources Investigation Program of China (2018FY100204) and the Science and Technology Innovation Project of Laoshan Laboratory (LSKJ202203700).	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J	Estebenet, MSG; Guler, MV				Gonzalez Estebenet, M. Sol; Guler, M. Veronica			<i>TRITHYRODINIUM VERRUCOSUM</i> (HEISECKE, 1970) COMB. NOV., EMEND: AN EARLY PALEOGENE (DANIAN) DINOFLAGELLATE CYST SPECIES FROM THE NORTH OF PATAGONIA, ARGENTINA. REGIONAL STRATIGRAPHIC AND PALEOENVIRONMENTAL RELEVANCE	AMEGHINIANA			English	Article						Danian; Dinoflagellate cysts; Patagonia; Argentina; Trithyrodinium	CRETACEOUS-TERTIARY BOUNDARY; SEA-LEVEL CHANGES; PALEOCENE; BIOSTRATIGRAPHY; BASIN; TRANSGRESSION; ENVIRONMENTS; FORAMINIFERA; CLIMATE; OROGENY	Trithyrodinium verrucosum comb. nov., emend. was originally described as Scriniodinium verrucosum in Danian deposits of the Roca Formation (Neuquen Basin, west Argentina) by Heisecke (1970). Well-preserved specimens recovered from the YPF.Ch.PV.es-1 borehole (Valdes Basin, east Argentina) and the re-examination of the original material allowed in this paper the emendation of the species, including recognition of an archeopyle type 3I, one of the diagnostic feature that led us to transfer the species to the genus Trithyrodinium. Based on the dinoflagellate cyst assemblages as well as the calcareous foraminifera and nannofossils content recovered from the stratigraphical interval containing Trithyrodinium verrucosum, we suggest the age of the Highest Common Occurrence (HCO) of this species not younger than middle Danian, and linked to the nannofossil Zone NP3. Hence, Trithyrodinium verrucosum may be a biostratigraphical marker for the Danian in the north of Patagonia, and the HCO is potentially useful for regional (inter-basinal) correlation of early Paleocene chronostratigraphical units from the south Atlantic basins. Also, the peak abundance of Trithyrodinium verrucosum in association with warm-water taxa ( e.g., Trithyrodinium evittii) might have occurred during globally warming episodes in the Danian.	[Gonzalez Estebenet, M. Sol; Guler, M. Veronica] Univ Nacl Sur UNS, Inst Geol Sur INGEOSUR, Consejo Nacl Invest Cient & Tecn CONICET, San Juan 670, RA-8000 Bahia Blanca, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South	Estebenet, MSG (通讯作者)，Univ Nacl Sur UNS, Inst Geol Sur INGEOSUR, Consejo Nacl Invest Cient & Tecn CONICET, San Juan 670, RA-8000 Bahia Blanca, Argentina.	sol.gonzalezestebenet@uns.edu.ar; vguler@criba.edu.ar			UNS (Universidad Nacional del Sur) [PGI 24/H157]; Fondo para la Investigacion Cientifica y Tecnologica [PICT-2020-SERIE A-01212-FONCyT]	UNS (Universidad Nacional del Sur); Fondo para la Investigacion Cientifica y Tecnologica	The authors thank P. Diaz for the palynological preparation of the samples studied. 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J	Gale, A; Batenburg, S; Coccioni, R; Dubicka, Z; Erba, E; Falzoni, F; Haggart, J; Hasegawa, T; Ifrim, C; Jarvis, I; Jenkyns, H; Jurowska, A; Kennedy, J; Maron, M; Muttoni, G; Pearce, M; Petrizzo, MR; Premoli-Silva, I; Thibault, N; Voigt, S; Wagreich, M; Walaszczyk, I				Gale, Andy; Batenburg, Sietske; Coccioni, Rodolfo; Dubicka, Zofia; Erba, Elisabetta; Falzoni, Francesca; Haggart, Jim; Hasegawa, Takishi; Ifrim, Christina; Jarvis, Ian; Jenkyns, Hugh; Jurowska, Agata; Kennedy, Jim; Maron, Matteo; Muttoni, Giovanni; Pearce, Martin; Petrizzo, Maria Rose; Premoli-Silva, Isabella; Thibault, Nicolas; Voigt, Silke; Wagreich, Michael; Walaszczyk, Irek			The Global Boundary Stratotype Section and Point (GSSP) of the Campanian Stage at Bottaccione (Gubbio, Italy) and its Auxiliary Sections: Seaford Head (UK), Bocieniec (Poland), Postalm (Austria), Smoky Hill, Kansas (USA), Tepayac (Mexico)	EPISODES			English	Article							CARBON-ISOTOPE STRATIGRAPHY; PALEOCENE MAGNETIC STRATIGRAPHY; WESTERN INTERIOR BASIN; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CRETACEOUS NANAIMO GROUP; GEOMAGNETIC POLARITY; PLANKTONIC-FORAMINIFERA; BENTHIC FORAMINIFERA; BRITISH-COLUMBIA	Following the unanimous vote of the Executive Com-mittee of International Union of Geological Sciences in October 2022, the Global boundary Stratotype Section and Point for the base of the Campanian Stage is con-firmed as the magnetic polarity reversal from Chron 34n (top of the Long Cretaceous Normal Polarity-Chron) to Chron C33r at the 221.53 m level in the Bottaccione Gorge section at Gubbio, Umbria-Marche Basin, Italy. This event has been widely identified in oceanic settings and in wide-spread onshore outcrops. Sedimentation across the San-tonian-Campanian boundary interval in the proposed GSSP appears to be continuous, supported by evidence from the carbon isotope record and complete micro- and nannofossil biostratigraphy. The succession comprises deep-water cherty limestones (mudstones and foraminiferal wackestones) which provide a detailed record of calcareous nannofossils and planktonic foraminifera and yields an excellent palaeomagnetic record. The high-resolution carbon isotope record, derived from bulk sediment, provides an important additional means of correlation to other regions.	[Gale, Andy] Univ Portsmouth, Sch Environm Geog & Geol Sci, Burnaby Bldg,Burnaby Rd, Portsmouth PO1 3QL, Hampshire, England; [Gale, Andy; Pearce, Martin] Nat Hist Museum, Dept Earth Sci, Cromwell Rd, London SW1 5BD, England; [Batenburg, Sietske] Univ Barcelona, Dept Dinam Terra & Ocea, Fac Ciencies Terra, Marti i Franques S-N, E-08028 Barcelona, Spain; [Coccioni, Rodolfo] Univ Urbino Carlo Bo, Dipartimento Sci Terra Vita & Ambiente, Campus Sci E Mattei, I-61029 Urbino, Italy; [Dubicka, Zofia; Walaszczyk, Irek] Univ Warsaw, Fac Geol, Al Zwirki & Wigury 93, PL-02098 Warsaw, Poland; [Erba, Elisabetta; Falzoni, Francesca; Maron, Matteo; Muttoni, Giovanni; Petrizzo, Maria Rose; Premoli-Silva, Isabella] Univ Milan, Dipartimento Sci Terra A Desio, Via Mangiagalli 34, I-20133 I Milano, Italy; [Haggart, Jim] Geol Survey Canada, 1500-605 Robson St, Vancouver, BC V6B 5J3, Canada; [Hasegawa, Takishi] Kanazawa Univ, Fac Sci, Dept Earth Sci, Kakuma Machi, Kanazawa 9201192, Japan; [Ifrim, Christina] SNSB Jura Museum, Eichstatt, Germany; [Jarvis, Ian] Kingston Univ London, Dept Geog Geol & Environm, Kingston Upon Thames KT1 2EE, England; [Jenkyns, Hugh; Kennedy, Jim] Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England; [Jurowska, Agata] AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Mickiewicza 30, PL-30059 Krakow, Poland; [Kennedy, Jim] Oxford Univ Museum Nat Hist, Parks Rd, Oxford OX1 3PW, England; [Thibault, Nicolas] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Voigt, Silke] Goethe Univ Frankfurt, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany; [Wagreich, Michael] Univ Vienna, Dept Geol, Althanstr 14, A-1090 Vienna, Austria; [Maron, Matteo] Univ G Annunzio Chieti Pescara, Dipartimento Ingn & Geol, Via Vestini 31, I-66100 Chieti, Italy	University of Portsmouth; Natural History Museum London; University of Barcelona; University of Urbino; University of Warsaw; University of Milan; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Kanazawa University; Kingston University; AGH University of Krakow; University of Copenhagen; Goethe University Frankfurt; University of Vienna; G d'Annunzio University of Chieti-Pescara	Gale, A (通讯作者)，Univ Portsmouth, Sch Environm Geog & Geol Sci, Burnaby Bldg,Burnaby Rd, Portsmouth PO1 3QL, Hampshire, England.; Gale, A (通讯作者)，Nat Hist Museum, Dept Earth Sci, Cromwell Rd, London SW1 5BD, England.	andy.gale@port.ac.uk	Maron, Matteo/AAD-5853-2021; Walaszczyk, Ireneusz/ABE-7229-2021; Voigt, Silke/G-7270-2017; Petrizzo, Maria/M-8672-2013; Wagreich, Michael/D-2279-2013; Jurkowska, Agata/A-9734-2016; Thibault, Nicolas/B-1106-2013; Dubicka, Zofia/ABB-3388-2020; Jarvis, Ian/A-1637-2008	Jurkowska, Agata/0000-0001-5457-9968; Thibault, Nicolas/0000-0003-4147-5531; Ifrim, Christina/0000-0002-4465-3121; Dubicka, Zofia/0000-0003-1105-4111; Wagreich, Michael/0000-0002-8828-0857; Falzoni, Francesca/0000-0002-5694-9827; Jarvis, Ian/0000-0003-3184-3097; Pearce, Martin/0000-0001-7856-1076; Maron, Matteo/0000-0003-4335-2893	International Subcommission on Cretaceous Stratigraphy; Grants-in-Aid for Scientific Research [23K22615] Funding Source: KAKEN	International Subcommission on Cretaceous Stratigraphy; Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We would like to thank numerous colleagues for their comments and advice on Cretaceous stratigraphy. We thank the Mayor of Gubbio, Prof Filippo Mario Striati, for his help on conservation of the proposed Bottaccione GSSP and Dave Watkins for location of the Kansas sections. We thank an anonymous referee for invaluable comments. We thank the Voting Members of the International Sub-commission on Cretaceous Stratigraphy and of the International Commission on Stratigraphy for comments which helped to improve the final version of the proposal. Jin-Yong Lee, Episodes Editor-in-Chief, is thanked for comments on the final version of the manuscript. We acknowledge financial support by the International Subcommission on Cretaceous Stratigraphy (http://cretaceous.stratigraphy.org/) .	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J	Dai, WY; Han, L; Li, PF; Li, QD; Xie, LJ; Liu, CY; Kong, JR; Jia, R; Li, DY; Yang, GP				Dai, Wen-Ying; Han, Lu; Li, Pei-Feng; Li, Qin-Dao; Xie, Li-Jun; Liu, Chun-Ying; Kong, Jun-Ru; Jia, Ru; Li, Dan-Yang; Yang, Gui-Peng			The sulfate assimilation and reduction of marine microalgae and the regulation of illumination	MARINE ENVIRONMENTAL RESEARCH			English	Article						Sulfate assimilation and reduction; Light; Photon flux density; Phaeodactylum tricornutum; Amphidinium carterae	ADENOSINE 5'-PHOSPHOSULFATE SULFOTRANSFERASE; PHAEODACTYLUM-TRICORNUTUM BOHLIN; SULFUR ASSIMILATION; DIMETHYLSULFONIOPROPIONATE DMSP; OCEANIC PHYTOPLANKTON; ORGANIC SULFUR; LIGHT; TRANSPORT; GROWTH; METABOLISM	To examine the sulfate assimilation and reduction process and the regulation of illumination, diatom Phaeo-dactylum tricornutum and dinoflagellate Amphidinium carterae were selected for continuous simulation incubation under different photon flux densities (PFDs) (54, 108 and 162 & mu;mol photons m- 2 s- 1), and concentration var-iations of related sulfur compounds sulfate, dimethylsulfoniopropionate (DMSP), dimethylsulfide (DMS) and acrylic acid (AA) in the culture system were observed. The optimal PFD for the growth of two microalgae was 108 & mu;mol photons m- 2 s- 1. However, the maximum sulfate absorption occurred at 162 & mu;mol photons m- 2 s- 1 for P. tricornutum and at 54 & mu;mol photons m- 2 s- 1 for A. carterae. With the increase of PFD, the release of DMSP by P. tricornutum decreased while A. carterae increased. The largest release amount of DMS was 0.59 & PLUSMN; 0.05 fmol cells- 1 for P. tricornutum and 2.61 & PLUSMN; 0.89 fmol cells- 1 for A. carterae under their optimum growth light condition. The sulfate uptake of P. tricornutum was inhibited by the addition of amino acids, cysteine had a greater inhibitory effect than methionine, and the absorption process was controlled by light. The intermediate products of sulfur metabolism had an up-control effect on the sulfate uptake process of P. tricornutum. However, the addition of amino acids had no obvious effect on the sulfate absorption of A. carterae.	[Dai, Wen-Ying; Han, Lu; Li, Pei-Feng; Li, Qin-Dao; Xie, Li-Jun; Liu, Chun-Ying; Kong, Jun-Ru; Jia, Ru; Li, Dan-Yang; Yang, Gui-Peng] Ocean Univ China, Inst Adv Ocean Studies, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Key Lab Marine Chem Theory & Technol,Minist Educ, Qingdao 266100, Peoples R China; [Liu, Chun-Ying; Yang, Gui-Peng] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Liu, Chun-Ying] Ocean Univ China, Key Lab Marine Chem Theory & Technol, Minist Educ, 238 Songling Rd, Qingdao 266100, Peoples R China	Ocean University of China; Laoshan Laboratory; Ocean University of China	Liu, CY (通讯作者)，Ocean Univ China, Key Lab Marine Chem Theory & Technol, Minist Educ, 238 Songling Rd, Qingdao 266100, Peoples R China.	roseliu@ouc.edu.cn	Li, Peifeng/E-9421-2015; Xie, li/HGE-6052-2022; Yang, Gui-Peng/GZG-6468-2022; danyang, li/GLT-1067-2022	Liu, Chun-Ying/0000-0002-9052-2800	Natural Science Foun-dation of Shandong Province, China [ZR2021MD113]; National Key Research and Development Program of China [2016YFA0601301]	Natural Science Foun-dation of Shandong Province, China(Natural Science Foundation of Shandong Province); National Key Research and Development Program of China(National Key Research & Development Program of China)	This work was financially supported by the Natural Science Foun-dation of Shandong Province, China (ZR2021MD113) and the National Key Research and Development Program of China (No. 2016YFA0601301) .	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J	Biswas, S; Pandey, DK; Nair, N; Uddandam, PR				Biswas, Sanki; Pandey, Dhananjai K. K.; Nair, Nisha; Uddandam, Prem Raj			Stable δ<SUP>13</SUP>C and δ<SUP>15</SUP>N isotope and palynofacies study of the late Miocene to early Pliocene Nicobar Fan sediments, Indian Ocean: implication for organic matter provenance and depositional environment	GEO-MARINE LETTERS			English	Article							AYEYARWADY IRRAWADDY; HIMALAYAN FORELAND; CONTINENTAL-SHELF; SURFACE SEDIMENTS; EARLY DIAGENESIS; CLIMATE-CHANGE; NORTHERN BAY; C/N RATIOS; CARBON; NITROGEN	The sedimentary core (late Miocene to early Pliocene) retrieved from the Nicobar Fan (Site-U1480) was used to determine organic matter provenances, paleodeposition, and paleoclimate conditions on the hinterland. Total organic carbon (C-org), nitrogen (N-total), and C-org/ N-total vary from 0.11 to 0.58%, 0.01 to 0.08%, and 2.5 to 33.0, separately. High C-org/ N-total values (11.0 to 33.0) are observed between 367.53 and 718.05 mbsf depths, suggesting highly land-derived OM. The carbon (delta C-13(org): - 22.95 to - 27.58 parts per thousand) and nitrogen (delta N-15: + 0.40 to + 2.51 parts per thousand) isotope values suggest that OM was mostly derived from mixed terrestrial C-3 plants and freshwater- phytoplanktons, with some marine OM. Palynofacies analysis also indicates that during the late Miocene, majority of OM is of terrestrial origin with little of marine origin. The spore-pollens are represented by Pinus, Picea, Abies, and Cerdus pollen, as well as trilete, and monolete spores, transported through major rivers like Irrawaddy and Salween from the surrounding Himalayan regions. Two facies assemblages have been recognized. Assemblage I: similar to 100% opaque phytoclasts at depths of 718.05mbsf, 969.78mbsf, and 1291.77mbsf indicate an oxidizing environment and existence of wildfires in the hinterland, which further point towards increased aridity during the late Miocene period. Assemblage II: non-opaque phytoclasts (avg. similar to 66.68%) are dominant over opaque phytoclasts (avg. similar to 25.82%) with few palynomorphs, suggesting enhanced sediment supply into the Nicobar Fan region. The dinoflagellate cysts are low in abundance, mostly represented by Spiniferites spp. and Operculodinium spp. Their productivity is relatively high during the late Miocene and declines in early Pliocene period, indicating a shift in monsoon conditions.	[Biswas, Sanki; Pandey, Dhananjai K. K.; Nair, Nisha] Natl Ctr Polar & Ocean Res NCPOR, Earth Syst Sci Org, MoES, Vasco Da Gama 403804, Goa, India; [Biswas, Sanki] Univ Johannesburg, Dept Geol, Box 524, ZA-2006 Auckland Pk, South Africa; [Uddandam, Prem Raj] Birbal Sahni Inst Palaeosci BSIP, 53-Univ Rd, Lucknow 226007, India	Earth System Science Organization (ESSO); Ministry of Earth Sciences (MoES) - India; National Centre for Polar and Ocean Research (NCPOR); University of Johannesburg; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Pandey, DK (通讯作者)，Natl Ctr Polar & Ocean Res NCPOR, Earth Syst Sci Org, MoES, Vasco Da Gama 403804, Goa, India.	pandey@ncpor.res.in	Biswas, Sanki/ABG-3348-2021		Ministry of Earth Sciences (MoES), Govt. of India [MoES/PO(Seismo)/8(16)2020]	Ministry of Earth Sciences (MoES), Govt. of India(Ministry of Earth Sciences (MoES) - India)	This research is supported and funded (to DP and NN) by the Ministry of Earth Sciences (MoES), Govt. of India through research grant MoES/PO(Seismo)/8(16)2020.	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Lett.	SEP	2023	43	3							14	10.1007/s00367-023-00755-0	http://dx.doi.org/10.1007/s00367-023-00755-0			16	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	N4MY1					2025-03-11	WOS:001036784400001
J	Mayr, G; De Pietri, VL; Love, L; Mannering, A; Crouch, E; Reid, C; Scofield, RP				Mayr, Gerald; De Pietri, Vanesa L.; Love, Leigh; Mannering, Al; Crouch, Erica; Reid, Catherine; Scofield, R. Paul			Partial skeleton from the Paleocene of New Zealand illuminates the early evolutionary history of the Phaethontiformes (tropicbirds)	ALCHERINGA			English	Article						Aves; Clymenoptilon novaezealandicum; gen. et sp. nov.; evolution; fossil birds; phylogeny; Waipara Greensand	DINOFLAGELLATE CYST; LOWER EOCENE; AVES; BIRDS; PROPHAETHONTIDAE; MIOCENE	We describe a new stem group representative of the Phaethontiformes (tropicbirds) from the Paleocene Waipara Greensand in New Zealand. The fossil consists of a partial skeleton with a nearly complete skull and represents the first unambiguous record of the Phaethontiformes from the Paleocene of the Southern Hemisphere. Clymenoptilon novaezealandicum gen. et sp. nov. has a proportionally shorter pelvis than Prophaethon shrubsolei from the early Eocene London Clay and appears to have been less adapted to foraging in an aquatic environment at or below sea-level. It is furthermore distinguished from P. shrubsolei and Lithoptila abdounensis from the late Paleocene/early Eocene of Morocco in a proportionally smaller foramen magnum of the skull. Together with other plesiomorphic features, this suggests that C. novaezealandicum is the sister taxon of a clade including Lithoptila, Prophaethon and crown group Phaethontiformes, and as one of the oldest stem group phaethontiforms the new species may indicate a Southern Hemispheric centre of origin of tropicbirds. After a recently described bony-toothed bird, C. novaezealandicum is the second seabird species from the Waipara Greensand to show affinities to taxa from the early Paleogene of the Northern Hemisphere. The wide early Paleogene distribution of the Phaethontiformes stands in sharp contrast to the geographic restriction of coeval diving seabirds, and different factors appear to have limited the dispersal of aquatic and pelagic seabird taxa in the early Paleogene.	[Mayr, Gerald] Senckenberg Res Inst, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Mayr, Gerald] Nat Hist Museum Frankfurt, Ornithol Sect, Senckenberganlage 25, D-60325 Frankfurt, Germany; [De Pietri, Vanesa L.] Univ Canterbury, Sch Earth & Environm, Private Bag 4800, Christchurch 8140, New Zealand; [Mannering, Al] Canterbury Museum, Rolleston Ave, Christchurch 8050, New Zealand; [Love, Leigh] POB 49, Waipara 7483, New Zealand; [Crouch, Erica] GNS Sci, 1 Fairway Dr, Lower Hutt 5040, New Zealand; [Reid, Catherine] Univ Canterbury, Sch Earth & Environm, Christchurch 8140, New Zealand; [Scofield, R. Paul] Canterbury Museum, Rolleston Ave, Christchurch 8050, New Zealand; [Scofield, R. Paul] Univ Canterbury, Sch Earth & Environm, Private Bag 4800, Christchurch 8140, New Zealand	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Canterbury; GNS Science - New Zealand; University of Canterbury; University of Canterbury	Mayr, G (通讯作者)，Senckenberg Res Inst, Senckenberganlage 25, D-60325 Frankfurt, Germany.; Mayr, G (通讯作者)，Nat Hist Museum Frankfurt, Ornithol Sect, Senckenberganlage 25, D-60325 Frankfurt, Germany.	Gerald.Mayr@senckenberg.de; vanesa.depietri@canterbury.ac.nz; lvlove@xtra.co.nz; alman@slingshot.co.nz; e.crouch@gns.cri.nz; catherine.reid@canterbury.ac.nz; pscofield@canterburymuseum.com	Scofield, R./A-4271-2011		Marsden Fund Council;  [21-UOC-040]	Marsden Fund Council(Royal Society of New ZealandMarsden Fund (NZ)); 	This study was supported by a grant from the Marsden Fund Council from government funding managed by Royal Society Te Aparangi [21-UOC-040]	Andrews C. 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J	Liu, XY; Chen, HH; Mu, XS; Zhang, HG; Fan, JJ; Huang, YH; Zhao, K; Mansour, A; Gentzis, T; Ostadhassan, M				Liu, Xiuyan; Chen, Honghan; Mu, Xiaoshui; Zhang, Hongan; Fan, Junjia; Huang, Yahao; Zhao, Ke; Mansour, Ahmed; Gentzis, Thomas; Ostadhassan, Mehdi			Organic matter preservation conditions in the third member of the Shahejie Formation (Dongpu Depression, China)	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Paleoredox proxies; Peleoproductivity; Paleoenvironment; OM preservation; Trace elements; Stable isotopes; Shale; Palynology	BOHAI BAY BASIN; GEOCHEMICAL PROXIES; OCEANIC ANOXIA; SHALE; PRODUCTIVITY; EVOLUTION; SEDIMENTS; CARBON; PALEOENVIRONMENT; PALEOREDOX	The third member of the Paleogene Shahejie Formation (Es3) in the Dongpu Depression, China, was studied to interpret its paleoenvironment through a series of trace element proxies, to reveal paleosalinity conditions, to elucidate on the hydrological conditions of the paleolake using carbon and oxygen stable isotopes, and to investigate the effects of paleoredox conditions on organic matter preservation. Most of the redox-sensitive proxies, such as U/Th, V/Cr, Ni/Co, Uauth, (Cu + Mo)/Zn, Cu/Zn, Th/U, and V/Sc, indicate that the Es3 was deposited under predominantly oxic and oxic/suboxic conditions, while V/(V + Ni) and 8U and previous studies suggested that the formation was deposited under mainly anoxic conditions. Oxygen levels agreed with the trace element ratios and showed a decrease from the lower to the upper part of the Es3 and an increase in paleoproductivity in the same direction. Salt rocks interbedded within the formation were shown to have overall lower oxygen levels than their neighboring organic-rich layers, black shale, and mudstone intervals, thus have likely altered the paleoredox proxies to oxygen consumption. Although Sr/Ba values point to a saline lake environment, the relative fluctuations seen suggest that the above ratio is not an appropriate indicator of paleosalinity in saltbearing strata and that the variations in paleoredox conditions in the formation are not a function of paleosalinity. Based on the negative 813C and 818O stable isotopic values, it is inferred that the shales in the Es3 were deposited in a hydrologically open lake environment. However, the presence of palynomorphs such as dinoflagellate cysts that are typically found in middle to outer neritic and open marine environments reinforces the assumption of a sea level transgression and inundation of the lake basin and mixing with freshwater algae and rare terrigenous phytoclasts such as cuticles, wood fragments, and suberin. The higher paleoproductivity and lower oxygen levels in the upper Es3 have contributed to greater OM preservation conditions in the absence of any variations in salinity or freshwater influx. The study also demonstrates that many of the paleoredox proxies and thresholds established are not valid to properly characterize certain formations deposited in lacustrine lake paleoenvironments such as the Shahejie, thus their applicability in certain situations must be re-evaluated.	[Liu, Xiuyan; Chen, Honghan; Zhao, Ke] China Univ Geosci, Key Lab Tecton & Petr Resources, Educ Minist, Wuhan 430074, Peoples R China; [Mu, Xiaoshui; Zhang, Hongan] SINOPEC, Zhongyuan Oilfield Co, Puyang 457001, Peoples R China; [Fan, Junjia] China Natl Petr Corp, Res Inst Petr Explorat & Dev, Key Lab Basin Struct & Hydrocarbon Accumulat, RIPED, Beijing 100083, Peoples R China; [Huang, Yahao] Yangtze Univ, Coll Resources & Environm, Key Lab Explorat Technol Oil & Gas Resources, Minist Educ, Wuhan 430100, Peoples R China; [Mansour, Ahmed] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Southwest Petr Univ, Qiangtang Inst Sedimentary Basin, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610050, Peoples R China; [Gentzis, Thomas] Core Labs Inc, Reservoir Geol, 6316 Windfern Rd, Houston, TX 77040 USA; [Ostadhassan, Mehdi] Christian Albrechts Univ Kiel, Inst Geosci Marine & Land Geomech & Geotecton, D-24118 Kiel, Germany	China University of Geosciences; Sinopec; China National Petroleum Corporation; Yangtze University; Southwest Petroleum University; Southwest Petroleum University; Southwest Petroleum University; University of Kiel	Zhao, K (通讯作者)，China Univ Geosci, Key Lab Tecton & Petr Resources, Educ Minist, Wuhan 430074, Peoples R China.; Huang, YH (通讯作者)，Yangtze Univ, Coll Resources & Environm, Key Lab Explorat Technol Oil & Gas Resources, Minist Educ, Wuhan 430100, Peoples R China.; Ostadhassan, M (通讯作者)，Christian Albrechts Univ Kiel, Inst Geosci Marine & Land Geomech & Geotecton, D-24118 Kiel, Germany.	hyhtr08916@163.com; 158896398@qq.com; mehdi.ostadhassan@ifg.uni-kiel.de	Chen, Honghan/AFC-2891-2022; ostadhassan, mehdi/AAE-4941-2020; Song, Zezhang/ABC-6131-2020; Mansour, Ahmed/AAR-4969-2020		Corporation (CNPC) Scientific Research and Technology Development Project [2021DJ0303, 2021DJ0101, 2021DJ0105]; Petrochina Carbonate Reservoir Key Laboratory Foundation [RIPED-2022-JS-2382]	Corporation (CNPC) Scientific Research and Technology Development Project; Petrochina Carbonate Reservoir Key Laboratory Foundation	This study is funded by the International Cooperation Project of Petro China Research Institute of Petroleum Exploration & Development (RIPED, China) and the Centre National de la Recherche Scientifique (CNRS, France) (YGJ20190403) , the China National PetroleumCorporation (CNPC) Scientific Research and Technology Development Project (2021DJ0303, 2021DJ0101, 2021DJ0105) , and the Petrochina Carbonate Reservoir Key Laboratory Foundation (RIPED-2022-JS-2382) . Zhongrui Wu from China University of Geosciences (Wuhan, China) is greatly thanked for the knowledge sharing on trace elements. The authors would also like to thank Editor-in-Chief, Professor Deolinda Flores, for her efficient handling of the manuscript, and two anonymous reviewers for their constructive comments that helped improve the quality of the manuscript.r Corporation (CNPC) Scientific Research and Technology Development Project (2021DJ0303, 2021DJ0101, 2021DJ0105) , and the Petrochina Carbonate Reservoir Key Laboratory Foundation (RIPED-2022-JS-2382) . Zhongrui Wu from China University of Geosciences (Wuhan, China) is greatly thanked for the knowledge sharing on trace elements. The authors would also like to thank Editor-in-Chief, Professor Deolinda Flores, for her efficient handling of the manuscript, and two anonymous reviewers for their constructive comments that helped improve the quality of the manuscript.	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J. Coal Geol.	SEP 1	2023	277								104334	10.1016/j.coal.2023.104334	http://dx.doi.org/10.1016/j.coal.2023.104334		AUG 2023	20	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	T7VM4					2025-03-11	WOS:001080023400001
J	Meyvisch, P; Mertens, KN; Gurdebeke, PR; Sandt, C; Pospelova, V; Vrielinck, H; Borondics, F; Louwye, S				Meyvisch, Pjotr; Mertens, Kenneth Neil; Gurdebeke, Pieter Roger; Sandt, Christophe; Pospelova, Vera; Vrielinck, Henk; Borondics, Ferenc; Louwye, Stephen			Does dinocyst wall composition really reflect trophic affinity? New evidence from ATR micro-FTIR spectroscopy measurements	JOURNAL OF PHYCOLOGY			English	Article						attenuated total reflection micro-Fourier transform infrared spectroscopy; bleaching; dinosporin composition; optical photothermal infrared spectroscopy; organic-walled dinocysts; pigments; spectrochemical methods; sunscreen; synchrotron radiation; trophic affinity	AMINO-ACIDS MAAS; DINOFLAGELLATE CYSTS; ABSORBING COMPOUNDS; ULTRAVIOLET-RADIATION; CHEMICAL-COMPOSITION; MELANIN; PHYTOPLANKTON; AUTOFLUORESCENCE; PRESERVATION; PERSPECTIVE	Attenuated total reflection (ATR) microscope Fourier transform infrared (micro-FTIR) spectroscopy was used to investigate the dinosporin composition in the walls of modern, organic-walled dinoflagellate resting cysts (dinocysts). Variable cyst wall compositions were observed, which led to the erection of four spectrochemical groups, some with striking similarities to other resistant biomacromolecules such as sporopollenin and algaenan. Furthermore, possible proxies derivable from the spectrochemical composition of modern and fossil dinocysts were discussed. The color of the dinocyst walls was reflected in the spectral data. When comparing that color with a standard and the results of a series of bleaching experiments with oxidative agents, eumelanin was assigned as a likely pigment contributing to the observed color. Following this assignment, the role of eumelanin as an ultraviolet sunscreen in colored dinocysts was hypothesized, and its implications on the autofluorescence and morphological preservation of dinocysts were further discussed. Unlike what had previously been assumed, it was shown that micro-FTIR data from dinocysts cannot be used to unambiguously infer trophic affinities of their associated cells. Finally, using methods with high spatial resolutions (synchrotron transmission micro-FTIR and optical photothermal infrared spectroscopy), it was shown that dinocyst wall layers are chemically homogenous at the probed scales. This study fills a large knowledge gap in our understanding of the chemical nature of dinocyst walls and has nuanced certain assumptions and interpretations made in the past.	[Meyvisch, Pjotr; Gurdebeke, Pieter Roger; Louwye, Stephen] Univ Ghent, Dept Geol, Campus Sterre,Bldg S8,Krijgslaan 281, Ghent, Belgium; [Mertens, Kenneth Neil] Ifremer, LITTORAL, Paris, France; [Sandt, Christophe; Borondics, Ferenc] SOLEIL Synchrotron, SMIS Beamline, Paris, France; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN USA; [Vrielinck, Henk] Univ Ghent, Dept Solid State Sci, Ghent, Belgium	Ghent University; Ifremer; University of Minnesota System; University of Minnesota Twin Cities; Ghent University	Meyvisch, P (通讯作者)，Univ Ghent, Dept Geol, Campus Sterre,Bldg S8,Krijgslaan 281, Ghent, Belgium.	pjotr.meyvisch@ugent.be	Louwye, Stephen/D-3856-2012; Gurdebeke, Pieter/AAY-7059-2020; Vrielinck, Henk/M-8367-2016; Meyvisch, Pjotr/ABB-1527-2021; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Sandt, Christophe/M-9806-2014	Mertens, Kenneth/0000-0003-2005-9483; Vrielinck, Henk/0000-0003-4861-9630; Sandt, Christophe/0000-0002-6432-2004; Gurdebeke, Pieter R./0000-0003-1425-8515; 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Phycol.	OCT	2023	59	5					1064	1084		10.1111/jpy.13382	http://dx.doi.org/10.1111/jpy.13382		AUG 2023	21	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	X1LK7	37623312	Green Published			2025-03-11	WOS:001082624100001
J	Meunier, M; Danelian, T				Meunier, Mathias; Danelian, Taniel			No dramatic changes observed in subtropical radiolarian plankton assemblages during the Middle Eocene Climatic Optimum (MECO); evidence from the North Atlantic ODP Site 1051	MARINE MICROPALEONTOLOGY			English	Article						Middle eocene; Global warming; Middle Eocene Climatic Optimum; Blake nose; Radiolaria; Biodiversity	LATE PALEOCENE; DINOFLAGELLATE CYSTS; ALANO SECTION; OCEAN; RECORD; DIVERSITY; EVENT; MARINE; BIOSTRATIGRAPHY; EXTRAPOLATION	The Middle Eocene Climatic Optimum (MECO; ca. 40 Ma) was a prominent global warming event that lasted 400 kyr and was characterized by a 4-6 degrees C rise in high latitude surface and deep-water temperatures. As the radiolarian plankton response to this warming event is practically unknown, whole assemblage quantitative analyses were undertaken on well-preserved radiolarian assemblages from ODP Site 1051 (western North Atlantic). Although radiolarians have apparently benefited at this site from increase in oceanic fertility induced by the MECO, this event does not appear to have had a severe impact on subtropical radiolarian fauna. No prominent faunal turnover was found in the studied interval, suggesting that subtropical radiolarians are relatively resilient to transient warming events. Likewise, variations in radiolarian assemblage composition establish that ocean warming induced only a weak ecological response. One of the most striking faunal changes associated with the MECO is the clear increase in radiolarian diversity (taxic richness), as a result of the northward migration of warm tropical radiolarian species. Similarly, several typical middle Eocene tropical species are found to be more abundant in the warmest interval. In addition to these poleward migrations, we identified three radiolarian clusters composed of warm-water or cool-water species, as well as two abundant artostrobiid species which may represent nutrient opportunists.	[Meunier, Mathias; Danelian, Taniel] Univ Lille, CNRS, UMR 8198 Evo Ecopaleo, F-59000 Lille, France	Universite de Lille; Centre National de la Recherche Scientifique (CNRS)	Meunier, M (通讯作者)，Univ Lille, CNRS, UMR 8198 Evo Ecopaleo, F-59000 Lille, France.	mathias.meunier@univ-lille.fr	Danelian, Taniel/A-7067-2018					Alroy J, 2010, SCIENCE, V329, P1191, DOI 10.1126/science.1189910; Alroy J., 2010, Paleontol. Soc. 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Micropaleontol.	SEP	2023	184								102272	10.1016/j.marmicro.2023.102272	http://dx.doi.org/10.1016/j.marmicro.2023.102272		AUG 2023	14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	S1RC9		Bronze			2025-03-11	WOS:001069003900001
J	Rush, W; Self-Trail, J; Zhang, Y; Sluijs, A; Brinkhuis, H; Zachos, J; Ogg, JG; Robinson, M				Rush, William; Self-Trail, Jean; Zhang, Yang; Sluijs, Appy; Brinkhuis, Henk; Zachos, James; Ogg, James G.; Robinson, Marci			Assessing environmental change associated with early Eocene hyperthermals in the Atlantic Coastal Plain, USA	CLIMATE OF THE PAST			English	Article							ISOPRENOID TETRAETHER LIPIDS; THERMAL MAXIMUM EVIDENCE; LATE PALEOCENE; LATEST PALEOCENE; TERRESTRIAL RECORDS; PARTICULATE MATTER; CONTINENTAL-SHELF; BIGHORN BASIN; WATER-COLUMN; PROXY DATA	Eocene transient global warming events (hyperthermals) can provide insight into a future warmer world. While much research has focused on the Paleocene-Eocene Thermal Maximum (PETM), hyperthermals of a smaller magnitude can be used to characterize climatic responses over different magnitudes of forcing. This study identifies two events, namely the Eocene Thermal Maximum 2 (ETM2 and H2), in shallow marine sediments of the Eocene-aged Salisbury Embayment of Maryland, based on magnetostratigraphy, calcareous nannofossil, and dinocyst biostratigraphy, as well as the recognition of negative stable carbon isotope excursions (CIEs) in biogenic calcite. We assess local environmental change in the Salisbury Embayment, utilizing clay mineralogy, marine palynology, d(18)O of biogenic calcite, and biomarker paleothermometry (TEX86). Paleotemperature proxies show broad agreement between surface water and bottom water temperature changes. However, the timing of the warming does not correspond to the CIE of the ETM2 as expected from other records, and the highest values are observed during H2, suggesting factors in addition to pCO(2) forcing have influenced temperature changes in the region. The ETM2 interval exhibits a shift in clay mineralogy from smectite-dominated facies to illite-rich facies, suggesting hydroclimatic changes but with a rather dampened weathering response relative to that of the PETM in the same region. Organic walled dinoflagellate cyst assemblages show large fluctuations throughout the studied section, none of which seem systematically related to CIE warming. These observations are contrary to the typical tight correspondence between climate change and assemblages across the PETM, regionally and globally, and ETM2 in the Arctic Ocean. The data do indicate very warm and (seasonally) stratified conditions, likely salinity-driven, across H2. The absence of evidence for strong perturbations in local hydrology and nutrient supply during ETM2 and H2, compared to the PETM, is consistent with the less extreme forcing and the warmer pre-event baseline, as well as the non-linear response in hydroclimates to greenhouse forcing.	[Rush, William] Yale Univ, Dept Earth & Planetary Sci, 210 Whitney Ave, New Haven, CT 06511 USA; [Rush, William] Univ Colorado, Cooperat Inst Res Environm Sci, 216 UCB, Boulder, CO 80309 USA; [Self-Trail, Jean; Robinson, Marci] US Geol Survey, Florence Bascom Geosci Ctr, Reston, VA USA; [Zhang, Yang] Univ Bremen, Fac Geosci, Bremen, Germany; [Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands; [Brinkhuis, Henk] NIOZ Royal Netherlands Inst Sea Res, Dept Ocean Syst Res, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Zachos, James] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, 1156 High St, Santa Cruz, CA 95064 USA; [Ogg, James G.] Purdue Univ, Dept Earth Atmospher & Planetary Sci, 550 Stadium Mall Dr, W Lafayette, IN 47907 USA; [Ogg, James G.] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Sichuan, Peoples R China; [Ogg, James G.] Deep Time Digital Earth Res Ctr Excellence Suzhou, Int Union Geol Sci, 1699 Zuchongzhi South Rd, Kunshan, Jiangsu, Peoples R China	Yale University; University of Colorado System; University of Colorado Boulder; United States Department of the Interior; United States Geological Survey; University of Bremen; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of California System; University of California Santa Cruz; Purdue University System; Purdue University; Chengdu University of Technology	Rush, W (通讯作者)，Yale Univ, Dept Earth & Planetary Sci, 210 Whitney Ave, New Haven, CT 06511 USA.; Rush, W (通讯作者)，Univ Colorado, Cooperat Inst Res Environm Sci, 216 UCB, Boulder, CO 80309 USA.	william.rush@yale.edu	Sluijs, Appy/B-3726-2009; Zachos, James/A-7674-2008; ZHANG, Yang/AAK-4210-2020; Brinkhuis, Henk/IUO-8165-2023	Brinkhuis, Henk/0000-0003-0253-6610; Rush, William/0000-0002-8522-5684; Ogg, James/0000-0001-5716-3511; Zhang, Yang/0000-0002-6625-0913	NSF [OCE-1415958, OCE-1658017, OCE-2103513]; European Research Council [771497]; USGS Climate Research and Development Program; Geologic Timescale Foundation; USGS National Cooperative Geologic Mapping Program	NSF(National Science Foundation (NSF)); European Research Council(European Research Council (ERC)); USGS Climate Research and Development Program; Geologic Timescale Foundation; USGS National Cooperative Geologic Mapping Program	Funding for this project has been provided by NSF (grant nos.& nbsp;OCE-1415958, OCE-1658017, and OCE-2103513). We thank Antoinette & nbsp;van & nbsp;den & nbsp;Dikkenberg, Giovanni & nbsp;Dammers, and Natasja & nbsp;Welters (Utrecht University) for analytical and technical assistance. Appy & nbsp;Sluijs thanks the European Research Council for the Consolidator Grant (grant no.& nbsp;771497; SPANC). Core collection and Marci Robinson have been funded by the USGS Climate Research and Development Program. Jean & nbsp;Self-Trail has been funded by the USGS National Cooperative Geologic Mapping Program. Yang & nbsp;Zhang and the paleomagnetic work have been funded by the Geologic Timescale Foundation.	Abels HA, 2016, CLIM PAST, V12, P1151, DOI 10.5194/cp-12-1151-2016; Agnini C, 2014, NEWSL STRATIGR, V47, P131, DOI 10.1127/0078-0421/2014/0042; Babila TL, 2022, SCI ADV, V8, DOI 10.1126/sciadv.abg1025; Bijl P. 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Past.	AUG 17	2023	19	8					1677	1698		10.5194/cp-19-1677-2023	http://dx.doi.org/10.5194/cp-19-1677-2023			22	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	P3WE2		Green Submitted, Green Published, gold			2025-03-11	WOS:001049971500001
J	Biltekin, D; Eris, KK; Çagatay, MN; Henry, P; Yakupoglu, N				Biltekin, Demet; Eris, K. Kadir; Cagatay, M. Namik; Henry, Pierre; Yakupoglu, Nurettin			New records of vegetation and climate changes in the Sea of Marmara during the Marine Isotope Stages 3, 4 and 5 (a-c)	QUATERNARY INTERNATIONAL			English	Article						Pollen analysis; Palaeoclimatology; Palaeovegetation; Sea of Marmara	GLACIAL-HOLOCENE PALEOCEANOGRAPHY; NON-POLLEN PALYNOMORPHS; NORTH ANATOLIAN FAULT; LATE QUATERNARY CORES; BLACK-SEA; FUNGUS SPORES; DINOFLAGELLATE CYSTS; SAPROPELIC LAYERS; RESERVOIR AGES; LEVEL CHANGES	A giant piston core MRS-CS27 sedimentary sequence in the Sea of Marmara (SoM) was investigated by palynological analysis to evaluate the paleoenvironmental and climate changes, corresponding to the Marine Isotope Stages MIS-5 (c-a), MIS-4, MIS-3, and the earliest part of the MIS-2. During MIS-5c, the palynological analysis indicates a warm and humid climate in the SoM. The pollen assemblage is characterized by the presence of broad-leaved deciduous woody taxa, with a predominance of deciduous Quercus. Following MIS-5c, a relatively colder and drier climate is inferred during MIS-5b, as indicated by the herbaceous assemblages found in the sedimentary sequence. The presence of herbaceous plants in the pollen record suggests less favorable conditions for woody vegetation and a shift towards a cooler and drier climate compared to the previous phase. Within the MIS-5a interval, the palynological analysis reveals the presence of abundant mesophyllous woody taxa. This indicates a return to a warm and humid climate during this period, supporting the growth of diverse forest vegetation. Distinct changes in vegetation are observed during MIS-4, with the presence of abundant Cedrus pollen. This suggests the survival of montane trees in the region under a cooler climate compared to the previous stages. Relict plants such as Coaya, Tsuga, and Carya are identified during MIS-3 and MIS-4. Their presence can be attributed to the reworking of older sediments during these periods, indicating that these plants were not contemporary with the sediment but were preserved from earlier time periods.	[Biltekin, Demet] Istanbul Tech Univ, Eurasia Inst Earth Sci, Ayazaga Campus, TR-34469 Istanbul, Turkiye; [Eris, K. Kadir; Cagatay, M. Namik; Yakupoglu, Nurettin] Istanbul Tech Univ, EMCOL Res Ctr, TR-34469 Istanbul, Turkiye; [Eris, K. Kadir; Cagatay, M. Namik; Yakupoglu, Nurettin] Dept Geol Engn, TR-34469 Istanbul, Turkiye; [Eris, K. Kadir; Cagatay, M. Namik; Yakupoglu, Nurettin] EIES, TR-34469 Istanbul, Turkiye; [Henry, Pierre] Aix Marseille Univ, Coll France, CNRS, IRD,INRAE,CEREGE, Aix En Provence, France	Istanbul Technical University; Istanbul Technical University; Universite PSL; College de France; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; INRAE	Biltekin, D (通讯作者)，Istanbul Tech Univ, Eurasia Inst Earth Sci, Ayazaga Campus, TR-34469 Istanbul, Turkiye.	biltekin@itu.edu.tr	Henry, Pierre/A-4045-2011; yakupoğlu, nurettin/AAV-3693-2021; Biltekin, Demet/AAB-3460-2020		EC FP7 project MARSITE [308417]; "Laboratoire d'Excellence" LabexMER [ANR-10-LABX-19]; French government	EC FP7 project MARSITE; "Laboratoire d'Excellence" LabexMER; French government	We would like to thank the scientific team of Marsite cruise, and in particular the co-chiefs, Louis Geli and Livio Ruffine, and the captains and crews of RV Pourquoi pas. The Marsite cruise was co-granted by the EC FP7 project MARSITE (grant number: 308417) "Long-term monitoring experiment in geologically active regions of Europe prone to natural hazards: the Supersite concept" under the call ENV.2012.6.4-2 and by the "Laboratoire d'Excellence" LabexMER (ANR-10-LABX-19) through the projects called Micro-GaMa and MISS Marmara, and by a grant from the French government under the program "Investissements d'Avenir". We would like to thank Editors Jule Xiao and Jan-Berend W. Stuut, and two anonymous reviewers for their constructive comments and suggestions for improving this paper.	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J	Lacerda, JNL; do Nascimento, LRDL; Barreto, AMF				Lacerda, Josefa Nilmara Lopes; do Nascimento, Luiz Ricardo da Silva Lobo; Barreto, Alcina Magnolia Franca			Paleoecology and paleoenvironmental inferences based on palynomorphs from the Romualdo Formation (Lower Cretaceous) of the Araripe Basin, Serrol(a)over-capndia Mine, Pernambuco, northeastern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Lower cretaceous; Dinoflagellate cysts; Marine paleoenvironment; Sedimentary basins; Palynology	POLLEN; BIOSTRATIGRAPHY; ATLANTIC	The present study is based on a paleoecological and paleoclimatic analysis of the palynological associations found in the section of the Serrol (a) over cap ndia Mine in Ouricuri, Pernambuco, which contributes to the reconstruction of the paleoenvironment of the Lower Cretaceous Romualdo Formation of the Araripe Basin, in northeastern Brazil. A total of 19 samples were collected from this section, which has a total height of 17 m. Only seven of these samples contained palynomorphs, which were analyzed by counting 200 palynomorphs per sample, permitting the identification of a total of 64 taxa, most of which were continental in origin. These continental palynomorph taxa included 34 pollen grains of gymnosperms and four of angiosperms, as well as the 14 spores of ferns and lycophytes, two freshwater microalgae, and fungal spores. The marine palynomorphs were represented by eight dinoflagellate cysts taxa and foraminiferal linings. The most abundant taxa overall were Classopollis spp., Afropollis jardinus, Cycadopites spp., and Gnetaceaepollenites jansonii, whose presence indicates a warm (semiarid to arid) paleoclimate. A distribution and cluster analysis identified two groups, G1, representing the lower layers (3.5-4.2 m), and G2, at a higher level (4.4-6.0 m). The palynomorphs of G1 were 92% continental and 8% marine, being represented by the dinocysts Batiacasphaera sp. A, Cometodinium ? sp., and Odontochitina ? sp. This group represents a proximal marine paleoenvironment with a strong terrestrial influence, whereas in G2, there is a decrease in the influence of continental palynomorphs (79%) and a significant increase in the contribution of marine palynomorphs (21%), including foraminiferal linings and the dinocysts of Subtilisphaera sp., Spiniferites sp., Odontochitina ? sp., and Atopodinium sp., etc. These characteristics are consistent with the conclusion that G2 represents a distal marine paleoenvironment. These findings provide important insights into the paleoenvironment of the Romualdo Formation in the Araripe Basin of northeastern Brazil during the Early Cretaceous.	[Lacerda, Josefa Nilmara Lopes; do Nascimento, Luiz Ricardo da Silva Lobo; Barreto, Alcina Magnolia Franca] Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Lab Paleontol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil	Universidade Federal de Pernambuco	Lacerda, JNL (通讯作者)，Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Lab Paleontol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	nilmaralacerda@gmail.com; nilmaralacerda@gmail.com; alcina.franca@ufpe.br		Lopes Lacerda, Josefa Nilmara/0000-0002-2645-6087	PETROBRAS [2018/00305-0]; Vinnova [2018-00305] Funding Source: Vinnova	PETROBRAS(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Vinnova(Vinnova)	We are grateful to PETROBRAS for its financial support of the "Projeto Araripe: Analise Paleoecologica e Bioestratigrafica do Albiano-Aptiano da Bacia do Araripe baseado em microfosseis carbonaticos e palinomorfos" (grant no. 2018/00305-0), and for providing a research scholarship to Josefa Nilmara L. Lacerda. We would like to thank Dr. Mitsuru Arai from Universidade Estadual de Sao Paulo (UNESP) for his valuable contributions to the taxonomy of the dinoflagellate cysts, and the UFPE Paleontologia Lab (PALEOLAB) and all its members that contributed to the collection of samples in the field. We would also like to thank Stephen Ferrari for reviewing the English language of this manuscript. 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J	Mota, MAD; Jones, TD; Sulaiman, N; Edgar, KM; Yamaguchi, T; Leng, MJ; Adloff, M; Greene, SE; Norris, R; Warren, B; Duffy, G; Farrant, J; Murayama, M; Hall, J; Bendle, J				Mota, Marcelo A. De Lira A.; Jones, Tom Dunkley; Sulaiman, Nursufiah; Edgar, Kirsty M. M.; Yamaguchi, Tatsuhiko; Leng, Melanie J. J.; Adloff, Markus; Greene, Sarah E. E.; Norris, Richard; Warren, Bridget; Duffy, Grace; Farrant, Jennifer; Murayama, Masafumi; Hall, Jonathan; Bendle, James			Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition	NATURE COMMUNICATIONS			English	Article							WALLED DINOFLAGELLATE CYSTS; ANTARCTIC GLACIATION; MISSISSIPPI RIVER; VICKSBURG GROUPS; COASTAL-PLAIN; MIDDLE EOCENE; CLIMATE; RECORDS; GREENHOUSE; EVOLUTION	Sea level fall with the growth of the Antarctic Ice Sheet 34 million years ago, and the shift in nutrients and carbon from continental margins to the ocean, initially provided a negative feedback that slowed global cooling and ice sheet expansion. Continental-scale expansion of the East Antarctic Ice Sheet during the Eocene-Oligocene Transition (EOT) is one of the largest non-linear events in Earth's climate history. Declining atmospheric carbon dioxide concentrations and orbital variability triggered glacial expansion and strong feedbacks in the climate system. Prominent among these feedbacks was the repartitioning of biogeochemical cycles between the continental shelves and the deep ocean with falling sea level. Here we present multiple proxies from a shallow shelf location that identify a marked regression and an elevated flux of continental-derived organic matter at the earliest stage of the EOT, a time of deep ocean carbonate dissolution and the extinction of oligotrophic phytoplankton groups. We link these observations using an Earth System model, whereby this first regression delivers a pulse of organic carbon to the oceans that could drive the observed patterns of deep ocean dissolution and acts as a transient negative feedback to climate cooling.	[Mota, Marcelo A. De Lira A.; Jones, Tom Dunkley; Sulaiman, Nursufiah; Edgar, Kirsty M. M.; Greene, Sarah E. E.; Warren, Bridget; Duffy, Grace; Farrant, Jennifer; Hall, Jonathan; Bendle, James] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, England; [Mota, Marcelo A. De Lira A.] Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Sulaiman, Nursufiah] Univ Malaysia Kelantan, Fac Earth Sci, Jeli Campus, Locked Bag 100, Jeli 17600, Kelantan, Malaysia; [Yamaguchi, Tatsuhiko] Natl Museum Nat & Sci, 4-1-1 Amakubo, Tsukuba 3050005, Japan; [Yamaguchi, Tatsuhiko; Murayama, Masafumi] Kochi Univ, Ctr Adv Marine Core Res, 200 Monobe Otsu, Nanko Ku, Kochi 7838502, Japan; [Leng, Melanie J. J.] British Geol Survey, Nottingham NG12 5GG, England; [Leng, Melanie J. J.] Univ Nottingham, Ctr Environm Geochem, Sch Biosci, Nottingham LE12 5RD, England; [Adloff, Markus] Univ Bristol, Sch Geog Sci, Univ Rd, Bristol BS8 1SS, England; [Adloff, Markus] Univ Bern, Oeschger Ctr, Hochschulstr 6, CH-3012 Bern, Switzerland; [Norris, Richard] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [Murayama, Masafumi] Kochi Univ, Fac Agr & Marine Sci, B200 Monobe, Nanko Ku, Kochi 7838502, Japan	University of Birmingham; Universidade de Sao Paulo; Universiti Malaysia Kelantan; National Museum of Nature and Science; Kochi University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Nottingham; University of Bristol; University of Bern; University of California System; University of California San Diego; Scripps Institution of Oceanography; Kochi University	Mota, MAD (通讯作者)，Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, England.; Mota, MAD (通讯作者)，Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	marcelomota@usp.br	De Lira Mota, Marcelo/AAX-1671-2021; Sulaiman, Nursufiah/HQZ-0960-2023; Edgar, Kirsty/AAR-9052-2021; Dunkley Jones, Tom/A-8441-2008	Edgar, Kirsty/0000-0001-7587-9951; Yamaguchi, Tatsuhiko/0000-0001-8967-2564; Hall, Jonathan/0000-0002-3707-6709; Dunkley Jones, Tom/0000-0002-9518-8143; De Lira Mota, Marcelo Augusto/0000-0001-6436-0951; Sulaiman, Nursufiah/0000-0003-0419-8176; Greene, Sarah/0000-0002-3025-9043; Warren, Bridget/0000-0002-3931-7596	National Council for Scientific and Technological Development (CNPq/Brazil) [206218/2014-1]; Natural Environment Research Council (NERC/UK) [NE/P013112/1]; NERC/UK [NE/P01903X/1]; NERC [bgs06001, NE/P013112/1] Funding Source: UKRI	National Council for Scientific and Technological Development (CNPq/Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Natural Environment Research Council (NERC/UK)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC/UK(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We sincerely~thank D.~Dockery and the Mississippi Department of Environmental Quality for their help, hospitality and provision of access to the Mossy Grove core;~C. D'Apolito Junior for helpful suggestions on this work; R. Burgess for the initial pilot study revealing excellent palynomorph preservation; staff from Petrostrat Ltd (G. Smith, M. Polling, N. Campion, and P. Cornick) and the British Geological Survey (J. Lacey and C. Kendrick) for laboratory help; and Alexandra Hangsterfer for XRF core scanner operation. While working on this manuscript, M.A.D.L.M. was supported by National Council for Scientific and Technological Development (CNPq/Brazil) Grant 206218/2014-1, T.D.J. and K.M.E. were supported by Natural Environment Research Council (NERC/UK) Grant NE/P013112/1, and S.E.G. and M.A. were supported by NERC/UK Grant NE/P01903X/1.	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Commun.	AUG 8	2023	14	1								10.1038/s41467-023-39806-6	http://dx.doi.org/10.1038/s41467-023-39806-6			13	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	P1UD3	37553323	Green Published, gold, Green Accepted			2025-03-11	WOS:001048553800036
J	Andreasen, N; Jackson, R; Rudra, A; Nohr-Hansen, H; Sanei, H; Bojesen-Koefoed, J; Seidenkrantz, MS; Pearce, C; Thibault, N; Ribeiro, S				Andreasen, Nanna; Jackson, Rebecca; Rudra, Arka; Nohr-Hansen, Henrik; Sanei, Hamed; Bojesen-Koefoed, Jorgen; Seidenkrantz, Marit-Solveig; Pearce, Christof; Thibault, Nicolas; Ribeiro, Sofia			From land to sea: provenance, composition, and preservation of organic matter in a marine sediment record from the North-East Greenland shelf spanning the Younger Dryas-Holocene	BOREAS			English	Article							ARCTIC-OCEAN; ICE CONDITIONS; CARBON-SOURCE; FRAM STRAIT; WATER; VARIABILITY; PYROLYSIS; COALS; LAKE	The organic matter content of marine sediments is often used to infer past changes in ocean conditions. However, the organic carbon pool preserved in coastal sediments is a complex mixture derived from different sources and may not reflect in situ processes. In this study, we combine taxonomic identification of reworked palynomorphs with pyrolysis organic geochemistry and reflected-light organic petrographic microscopy to investigate the provenance, composition and preservation of organic matter in a marine sediment core retrieved from the NE Greenland shelf. Our study reveals continuous yet variable input of land-derived organic carbon to the marine environment throughout the late Younger Dryas-Holocene, with the highest input of inert carbon in the late Younger Dryas. Although the sediments contain some recent marine palynomorphs, there is no other evidence of fresh marine organic carbon. In contrast, our results indicate that these shelf sediments represent a significant sink of recycled organic carbon. The results of pyrolysis geochemistry revealed that similar to 90% of the total organic carbon in the sediments is inert. The organic petrography analyses revealed that >70-84% of the organic carbon in the sediment core is terrigenous. Reworked dinoflagellate cysts showed a continuous provenance of Cretaceous land-derived material, most likely from the nearby Clavering Island. Our study points to the importance of constraining the organic matter origin, composition and preservation in marine sediments to achieve more accurate palaeoenvironmental reconstructions based on organic proxies.	[Andreasen, Nanna; Jackson, Rebecca; Nohr-Hansen, Henrik; Bojesen-Koefoed, Jorgen; Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Andreasen, Nanna; Thibault, Nicolas] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Andreasen, Nanna] Univ Copenhagen, Niels Bohr Inst, Tagensvej16, DK-2200 Copenhagen N, Denmark; [Jackson, Rebecca; Ribeiro, Sofia] Univ Copenhagen, Globe Inst, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark; [Rudra, Arka; Sanei, Hamed] Aarhus Univ, Dept Geosci, Lithospher Organ Carbon LOC Lab, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Seidenkrantz, Marit-Solveig; Pearce, Christof] Aarhus Univ, Dept Geosci, Palaeoceanog & Palaeoclimate Grp, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Seidenkrantz, Marit-Solveig; Pearce, Christof] Aarhus Univ, Arctic Res Ctr, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Seidenkrantz, Marit-Solveig; Pearce, Christof] Aarhus Univ, iClimate Ctr, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark	Geological Survey Of Denmark & Greenland; University of Copenhagen; University of Copenhagen; Niels Bohr Institute; University of Copenhagen; Aarhus University; Aarhus University; Aarhus University; Aarhus University	Andreasen, N (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.; Andreasen, N (通讯作者)，Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.; Andreasen, N (通讯作者)，Univ Copenhagen, Niels Bohr Inst, Tagensvej16, DK-2200 Copenhagen N, Denmark.	nanna.andreasen@nbi.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Andreasen, Nanna/JQJ-2592-2023; Pearce, Christof/M-4852-2013; Sanei, Hamed/LEM-2435-2024; Jackson, Rebecca/G-5485-2018; Thibault, Nicolas/B-1106-2013; Seidenkrantz, Marit-Solveig/A-3451-2012; Ribeiro, Sofia/G-9213-2018	Thibault, Nicolas/0000-0003-4147-5531; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Jackson, Rebecca/0000-0002-0861-3173; Sanei, Hamed/0000-0002-2961-9654; Ribeiro, Sofia/0000-0003-0672-9161; Andreasen, Nanna/0000-0002-0134-4003; Rudra, Arka/0000-0001-9970-2544	European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie [846142]; GEOCENTER Denmark; Danish Council for Independent Research (DFF-Sapere Aude grant) [9064-00039B, 7014-00113B (G-Ice), 0135-00165B]; European Union [869383]; Danish Centre for Marine Research; Natural Science and Engineering Research Council of Canada; Marie Curie Actions (MSCA) [846142] Funding Source: Marie Curie Actions (MSCA)	European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie(Marie Curie Actions); GEOCENTER Denmark; Danish Council for Independent Research (DFF-Sapere Aude grant)(Det Frie Forskningsrad (DFF)); European Union(European Union (EU)); Danish Centre for Marine Research; Natural Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Marie Curie Actions (MSCA)(Marie Curie Actions)	This study received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement no. 846142. The project has also received support from GEOCENTER Denmark (project GreenShift). The project further received funding from the Danish Council for Independent Research (DFF-Sapere Aude grant no. 9064-00039B to SR, and grant nos 7014-00113B (G-Ice project) and 0135-00165B (GreenShelf), to M-SS). Additional funding was provided by the European Union's Horizon 2020 research and innovation programme under grant agreement no. 869383 (ECOTIP; AU/M-SS as partner). The NorthGreen17 expedition was funded by the Danish Centre for Marine Research and the Natural Science and Engineering Research Council of Canada. We are grateful to the captain, crew and scientific party of the NorthGreen2017 expedition on board RV Dana' and to Anne de Vernal (Universite du Quebec a Montreal), Principal Investigator of the Canadian grant that co-funded the NorthGreen2017 expedition. We warmly thank Charlotte Olsen and Annette Ryge for laboratory assistance during the preparation of samples for palynology. Furthermore, we thank the two reviewers J. Knies and K. Mertens for their valuable input and constructive suggestions, and thank Jan A. Piotrowski for editorial handling of the manuscript. The authors declare no conflict of interests.	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L., 2017, Am. Assoc. Stratigraphic Palynologist Data Ser.	64	1	2	5	16	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0300-9483	1502-3885		BOREAS	Boreas	OCT	2023	52	4					459	475		10.1111/bor.12630	http://dx.doi.org/10.1111/bor.12630		AUG 2023	17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	X1QR6		hybrid			2025-03-11	WOS:001043155200001
J	Lindström, S; Pedersen, GK; Vosgerau, H; Hovikoski, J; Dybkjaer, K; Nielsen, LH				Lindstrom, Sofie; Pedersen, Gunver Krarup; Vosgerau, Henrik; Hovikoski, Jussi; Dybkjaer, Karen; Nielsen, Lars Henrik			Palynology of the Triassic-Jurassic transition of the Danish Basin (Denmark): a palynostratigraphic zonation of the Gassum-lower Fjerritslev formations	PALYNOLOGY			English	Article						Rhaetian; Hettangian; Sinemurian; spores; pollen; Denmark; dinoflagellate cysts; palynomorphs; biostratigraphy	TERRESTRIAL ECOSYSTEM CHANGE; CARBON-ISOTOPE STRATIGRAPHY; ATLANTIC MAGMATIC PROVINCE; NORTHERN CALCAREOUS ALPS; ST-AUDRIES BAY; TRIASSIC/JURASSIC BOUNDARY; VEGETATION HISTORY; MASS-EXTINCTION; TECTONIC EVOLUTION; DIVERSITY PATTERNS	The Upper Triassic-Lower Jurassic succession in the Danish Basin is penetrated by many deep wells that were drilled during former hydrocarbon exploration campaigns, but it is today targeted for geothermal energy and storage of CO2. The Stenlille salt dome on Sj & UAELIG;lland sandstones of the Gassum Formation, sealed by the overlying Fjerritslev Formation mudstones, has been used for decades as a seasonal storage for natural gas. With its comprehensive dataset of seismics, geophysical well logs and conventional core data from 20 wells, the Stenlille succession serves as a model for other salt domes currently being evaluated as potential CO2 storage sites in the basin. Over the last decade the cored Triassic-Jurassic boundary succession has contributed to the understanding of environmental and palynological events during the end-Triassic mass extinction. Core, sidewall core and cutting samples from several of the closely situated Stenlille wells are here used to establish a high-resolution palynostratigraphic zonation scheme covering the entire Rhaetian to Sinemurian succession by integrating new analyses with previously published data. The palynological dataset has allowed the recognition of nine formally described spore-pollen zones, of which eight are new, while two previously described dinoflagellate cyst zones are subdivided into three informal subzones each. The palynological zonation is integrated with a sequence stratigraphic framework and will form the basis for the dating of future well sections in the Danish Basin and other basins and for correlation to outcrops. The large palynological dataset further shows that the vegetation around the Danish Basin was remarkably stable during the early to middle Rhaetian, but that events related to the emplacement of the Central Atlantic Magmatic Province accelerated ecosystem changes for c. 175 ky in the late Rhaetian and earliest Hettangian, including & SIM;25 ky of successional recovery before the terrestrial ecosystem had again stabilised.	[Lindstrom, Sofie] Dept Geosci & Nat Resource Management, Copenhagen, Denmark; [Lindstrom, Sofie; Pedersen, Gunver Krarup; Vosgerau, Henrik; Hovikoski, Jussi; Dybkjaer, Karen; Nielsen, Lars Henrik] GEUS Geol Survey Denmark & Greenland, Copenhagen, Denmark; [Lindstrom, Sofie] Appl Petr Technol AS, Oslo, Norway; [Hovikoski, Jussi] GTK Geol Survey Finland, Espoo, Finland	Geological Survey Of Denmark & Greenland; Geological Survey of Finland (GTK)	Lindström, S (通讯作者)，Dept Geosci & Nat Resource Management, Copenhagen, Denmark.	msl@ign.ku.dk	Dybkjær, Karen/G-5223-2018; Lindström, Sofie/G-5481-2018; Hovikoski, Jussi/H-3280-2018; Pedersen, Gunver Krarup/G-9411-2018	Hovikoski, Jussi/0000-0001-6330-8713; Pedersen, Gunver Krarup/0000-0002-0792-2257; Lindstrom, Malin Sofie/0000-0001-8278-1055	This study benefitted from Geocenter Denmark research grants 3-2010 and 6-2013 to SL, and from the CCUS2020 grant to GEUS that allocated time for the study. The authors are grateful for helpful reviews from two anonymous reviewers as well as helpful commen [6-2013, CCUS2020]; Geocenter Denmark;  [3-2010]	This study benefitted from Geocenter Denmark research grants 3-2010 and 6-2013 to SL, and from the CCUS2020 grant to GEUS that allocated time for the study. The authors are grateful for helpful reviews from two anonymous reviewers as well as helpful commen; Geocenter Denmark; 	This study benefitted from Geocenter Denmark research grants 3-2010 and 6-2013 to SL, and from the CCUS2020 grant to GEUS that allocated time for the study. The authors are grateful for helpful reviews from two anonymous reviewers as well as helpful comments from the editor Jim Riding.	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J	Kim, Y; Yi, S; Jun, CP; Saavedra-Pellitero, M; Lee, GS; Kim, GY				Kim, Yongmi; Yi, Sangheon; Jun, Chang-Pyo; Saavedra-Pellitero, Mariem; Lee, Gwang-Soo; Kim, Gil Young			Palynological implications for the paleoclimate and paleoceanographic reconstruction of the East Sea since the early Pleistocene at IODP site U1430	QUATERNARY SCIENCE REVIEWS			English	Article						East asian winter monsoon variation; East sea; Expedition 346; Mid-brunhes event; Mid-pleistocene transition; Palynological record; Tsushima warm current	CHANGJIANG DILUTED WATER; ASIAN MONSOON; ULLEUNG BASIN; DINOFLAGELLATE CYSTS; TIBETAN PLATEAU; POLLEN ANALYSIS; CLIMATE-CHANGE; JAPAN SEA; RECORD; VEGETATION	Palynomorphs, including pollen and dinoflagellate cysts from marine sediments, can provide a history of paleoclimate and paleoceanography. We present new palynological profiles based on a core from the Integrated Ocean Drilling Program Site U1430, which was drilled in the Ulleung Plateau East Sea. This core covers the past 2 Ma and spans the Mid-Pleistocene Transition (MPT, 1.2-0.8 Ma) and Mid-Brunhes Event (MBE, similar to 0.43 Ma). Terrestrial and marine palynomorph records indicate orbital-scale variations in paleoclimate and paleoceanography, reflecting changes in the interconnections between vegetation, climate, and the ocean. Before the MPT, the high pollen taxa ratio and abundant temperate pollen suggest a relatively warm temperature associated with astronomical forcing-induced insolation changes. At ca. 1.3 Ma, boreal coniferous pollen increased, suggesting intensification of the East Asian winter monsoon (EAWM). The long-term trend of boreal coniferous pollen concentration was similar to that of benthic delta O-18. This orbital scale boreal conifer pollen assemblage variation indicates Quaternary EAWM evolution controlled by changes in global ice volume and climatic cooling. The marine palynological data reflect the ocean circulation history of the study area, where sea level fluctuations and tectonic activity played important roles around the marginal sea. The abundance of warm-water dinoflagellate species after ca. 1.9 Ma, including Tuberculodinium vancampoae, indicates Tsushima Warm Current intrusion related to the expansion of the Korea (Tsushima) Strait. Nematosphaeropsis labyrinthus and other cold-water species increased markedly during the MPT, suggesting a low sea surface temperature and weakened vertical mixing of the East Sea due to the cooled climate and sea ice during the MPT. The marked sea level fluctuation associated with the glacial-interglacial cycling after the MBE resulted in an assemblage composition shift from cold to warm water species. Tsuga and Betula thrived during mild winters, primarily influenced by winter insolation. These genera were particularly prosperous in the early Pleistocene, coinciding with a strong intrusion of the Tsushima Warm Current (TWC). Our findings should be considered in developing a comprehensive understanding of the paleoclimate and paleoceanographic history of northern East Asia across the major climate transitions of the Pleistocene.	[Kim, Yongmi; Yi, Sangheon; Lee, Gwang-Soo; Kim, Gil Young] Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea; [Yi, Sangheon] Korea Univ Sci & Technol, Daejeon 34113, South Korea; [Jun, Chang-Pyo] Chonnam Natl Univ, Gwangju 61186, South Korea; [Saavedra-Pellitero, Mariem] Univ Portsmouth, Portsmouth, England	Korea Institute of Geoscience & Mineral Resources (KIGAM); University of Science & Technology (UST); Chonnam National University; University of Portsmouth	Yi, S (通讯作者)，Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea.	shyi@kigam.re.kr	; YI, Sangheon/D-4780-2011	Jun, Chang-Pyo/0000-0002-6626-7918; YI, Sangheon/0000-0002-2938-0380; Saavedra, Mariem/0000-0003-0621-7932	Ministry of Oceans and Fisheries, Korea; Ministry of Oceans and Fisheries, Korea [GP2020- 023]; Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Science and ICT [GP2022-006]; Basic Research Project of the Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Science and ICT;  [20110183];  [239851]	Ministry of Oceans and Fisheries, Korea; Ministry of Oceans and Fisheries, Korea; Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Science and ICT(Ministry of Science, ICT & Future Planning, Republic of Korea); Basic Research Project of the Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Science and ICT(Ministry of Science, ICT & Future Planning, Republic of Korea); ; 	This research was supported by "International Ocean Discovery Program (20110183) " and "Study on characterizations of submarine faults in the southwestern sea, Korea (23-9851) ," funded by the Ministry of Oceans and Fisheries, Korea, and a Basic Research Project (GP2020- 023 and GP2022-006) of the Korea Institute of Geoscience and Mineral Resources (KIGAM) funded by the Ministry of Science and ICT.	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J	Berndt, C; Planke, S; Zarikian, CAA; Frieling, J; Jones, MT; Millett, JM; Brinkhuis, H; Bünz, S; Svensen, HH; Longman, J; Scherer, RP; Karstens, J; Manton, B; Nelissen, M; Reed, B; Faleide, JI; Huismans, RS; Agarwal, A; Andrews, GDM; Betlem, P; Bhattacharya, J; Chatterjee, S; Christopoulou, M; Clementi, VJ; Ferré, EC; Filina, IY; Guo, PY; Harper, DT; Lambart, S; Mohn, G; Nakaoka, R; Tegner, C; Varela, N; Wang, MY; Xu, WM; Yager, SL				Berndt, Christian; Planke, Sverre; Zarikian, Carlos A. Alvarez A.; Frieling, Joost; Jones, Morgan T. T.; Millett, John M. M.; Brinkhuis, Henk; Bunz, Stefan; Svensen, Henrik H. H.; Longman, Jack; Scherer, Reed P. P.; Karstens, Jens; Manton, Ben; Nelissen, Mei; Reed, Brandon; Faleide, Jan Inge; Huismans, Ritske S. S.; Agarwal, Amar; Andrews, Graham D. M.; Betlem, Peter; Bhattacharya, Joyeeta; Chatterjee, Sayantani; Christopoulou, Marialena; Clementi, Vincent J. J.; Ferre, Eric C. C.; Filina, Irina Y. Y.; Guo, Pengyuan; Harper, Dustin T. T.; Lambart, Sarah; Mohn, Geoffroy; Nakaoka, Reina; Tegner, Christian; Varela, Natalia; Wang, Mengyuan; Xu, Weimu; Yager, Stacy L. L.			Shallow-water hydrothermal venting linked to the Palaeocene-Eocene Thermal Maximum	NATURE GEOSCIENCE			English	Article							NORTH-SEA; METHANE; RELEASE; CARBON; BASIN; COMPLEXES; CONSEQUENCES; EVOLUTION; ABUNDANCE; CLIMATE	Widespread shallow-water hydrothermal venting in the North Atlantic, probably a source of methane, coincided with the onset of the Palaeocene-Eocene Thermal Maximum, according to borehole proxy records and seismic imaging. The Palaeocene-Eocene Thermal Maximum (PETM) was a global warming event of 5-6 & DEG;C around 56 million years ago caused by input of carbon into the ocean and atmosphere. Hydrothermal venting of greenhouse gases produced in contact aureoles surrounding magmatic intrusions in the North Atlantic Igneous Province have been proposed to play a key role in the PETM carbon-cycle perturbation, but the precise timing, magnitude and climatic impact of such venting remains uncertain. Here we present seismic data and the results of a five-borehole transect sampling the crater of a hydrothermal vent complex in the Northeast Atlantic. Stable carbon isotope stratigraphy and dinoflagellate cyst biostratigraphy reveal a negative carbon isotope excursion coincident with the appearance of the index taxon Apectodinium augustum in the vent crater, firmly tying the infill to the PETM. The shape of the crater and stratified sediments suggests large-scale explosive gas release during the initial phase of vent formation followed by rapid, but largely undisturbed, diatomite-rich infill. Moreover, we show that these vents erupted in very shallow water across the North Atlantic Igneous Province, such that volatile emissions would have entered the atmosphere almost directly without oxidation to CO2 and at the onset of the PETM.	[Berndt, Christian; Karstens, Jens] GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany; [Planke, Sverre; Millett, John M. M.; Manton, Ben] Volcan Basin Energy Res AS, Oslo, Norway; [Planke, Sverre; Jones, Morgan T. T.; Svensen, Henrik H. H.; Faleide, Jan Inge; Betlem, Peter] Univ Oslo, Dept Geosci, Oslo, Norway; [Zarikian, Carlos A. Alvarez A.] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA; [Frieling, Joost] Univ Oxford, Dept Earth Sci, Oxford, England; [Millett, John M. M.] Univ Aberdeen, Kings Coll, Dept Geol & Geophys, Aberdeen, Scotland; [Brinkhuis, Henk; Nelissen, Mei] NIOZ Royal Netherlands Inst Sea Res, Den Burg, Texel, Netherlands; [Bunz, Stefan] UiT Arctic Univ Tromso, Dept Geol, Tromso, Norway; [Longman, Jack] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm ICBM, Marine Isotope Geochem, Oldenburg, Germany; [Longman, Jack] Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne, England; [Scherer, Reed P. P.; Reed, Brandon; Christopoulou, Marialena] Northern Illinois Univ, Dept Earth Atmosphere & Environm, De Kalb, IL USA; [Huismans, Ritske S. S.] Univ Bergen, Dept Earth Sci, Bergen, Norway; [Agarwal, Amar] Indian Inst Technol Kanpur, Dept Earth Sci, Appl Struct Geol, Kanpur, India; [Andrews, Graham D. M.] Univ Hull, Sch Environm Sci, Fac Sci & Engn, Kingston Upon Hull, England; [Betlem, Peter] Univ Ctr Svalbard, Dept Arctic Geol, Svalbard, Norway; [Bhattacharya, Joyeeta] Picarro Inc, Santa Clara, CA USA; [Chatterjee, Sayantani] Niigata Univ, Dept Geol, Niigata, Japan; [Chatterjee, Sayantani] Univ Tokyo, Earthquake Res Inst, Tokyo, Japan; [Clementi, Vincent J. J.] Rutgers State Univ, Dept Marine & Coastal Sci, New Brunswick, NJ USA; [Ferre, Eric C. C.] Univ Louisiana Lafayette, Sch Geosci, Lafayette, LA USA; [Filina, Irina Y. Y.] Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA; [Guo, Pengyuan] Chinese Acad Sci, Inst Oceanol, Qingdao, Peoples R China; [Harper, Dustin T. T.; Lambart, Sarah] Univ Utah, Dept Geol & Geophys, Salt Lake City, UT USA; [Mohn, Geoffroy] CY Cergy Paris Univ, Lab Geosci & Environm Cergy GEC, Neuville Sur Oise, France; [Nakaoka, Reina] Kobe Univ, Dept Planetol, Kobe, Japan; [Tegner, Christian] Aarhus Univ, Dept Geosci, Aarhus, Denmark; [Varela, Natalia] Virginia Tech, Dept Geosci, Blacksburg, VA USA; [Wang, Mengyuan] Sun Yat Sen Univ, Sch Marine Sci, Zhuhai, Peoples R China; [Xu, Weimu] Univ Coll Dublin, Sch Earth Sci, Dublin, Ireland; [Xu, Weimu] Univ Coll Dublin, SFI Res Ctr Appl Geosci iCRAG, Dublin, Ireland; [Yager, Stacy L. L.] Ball State Univ, Dept Environm Geol & Nat Resources, Muncie, IN USA	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Oslo; Texas A&M University System; Texas A&M University College Station; University of Oxford; University of Aberdeen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); UiT The Arctic University of Tromso; Carl von Ossietzky Universitat Oldenburg; Northumbria University; Northern Illinois University; University of Bergen; Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Kanpur; University of Hull; University Centre Svalbard (UNIS); Niigata University; University of Tokyo; Rutgers University System; Rutgers University New Brunswick; University of Louisiana Lafayette; University of Nebraska System; University of Nebraska Lincoln; Chinese Academy of Sciences; Institute of Oceanology, CAS; Utah System of Higher Education; University of Utah; CY Cergy Paris Universite; Kobe University; Aarhus University; Virginia Polytechnic Institute & State University; Sun Yat Sen University; University College Dublin; University College Dublin; Ball State University	Berndt, C (通讯作者)，GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany.	cberndt@geomar.de	Millett, John/AAH-9845-2019; Agarwal, Amar/AAL-7217-2020; Karstens, Jens/JQJ-1482-2023; Berndt, Christian/GVS-3279-2022; Tegner, Christian/A-5295-2012; Huismans, Ritske/C-3938-2013; Brinkhuis, Henk/IUO-8165-2023; Planke, Sverre/AAE-1721-2021; Harper, Dustin/H-1713-2018; Jones, Morgan/AAB-9916-2020; Lambart, Sarah/B-9719-2014	Longman, Jack/0000-0002-2725-2617; Berndt, Christian/0000-0001-5055-0180; Bunz, Stefan/0000-0002-9215-7325; Planke, Sverre/0000-0001-6128-2193; Millett, John/0000-0002-1275-6206; Varela, Natalia/0000-0002-9611-9393; Frieling, Joost/0000-0002-5374-1625; Yager, Stacy/0000-0003-2792-6164; Jones, Morgan/0000-0003-3047-0751; Tegner, Christian/0000-0003-1407-7298; Lambart, Sarah/0000-0002-3636-7950; Xu, Weimu/0000-0002-3239-0272; Brinkhuis, Henk/0000-0003-0253-6610; Karstens, Jens/0000-0002-9434-2479; Nelissen, Mei/0009-0002-6802-2495; Bhattacharya, Joyeeta/0000-0002-7662-4122	Integrated Ocean Drilling Program; Research Council of Norway [336293, 223272]; AkerBP (PDRILL project); IODP; Norwegian Petroleum Directorate; AkerBP (PDRILL project)	Integrated Ocean Drilling Program; Research Council of Norway(Research Council of Norway); AkerBP (PDRILL project); IODP; Norwegian Petroleum Directorate; AkerBP (PDRILL project)	The work was funded through the Integrated Ocean Drilling Program. We thank the master, crew and technical staff of D/S Joides Resolution on Expedition 396. Without their efforts, this work would not have been possible. S.P., M.T.J., H.H.S. and J.I.F. acknowledge the support of the Research Council of Norway through the PALMAR (no. 336293) and CEED (no. 223272) research projects. The other authors were funded through IODP for Expedition 396. We thank the Norwegian Petroleum Directorate and AkerBP (PDRILL project) for supporting site survey acquisition and data analyses, and TGS for access to seismic data.	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Geosci.	SEP	2023	16	9					803	+		10.1038/s41561-023-01246-8	http://dx.doi.org/10.1038/s41561-023-01246-8		AUG 2023	15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	Q8AK7		hybrid			2025-03-11	WOS:001045179900005
J	Wang, CY; Zheng, P; Gu, HF; Luo, ZH; Luo, ZH; Mao, LJ; Zhang, YZ				Wang, Changyou; Zheng, Ping; Gu, Haifeng; Luo, Zhaohe; Luo, Zhuhua; Mao, Longjiang; Zhang, Yuanzhi			Predicting Ecological Distribution of the Toxic Dinoflagellate <i>Alexandrium minutum</i> in China Sea Using Ecological Niche Modeling	JOURNAL OF OCEAN UNIVERSITY OF CHINA			English	Article						Alexandrium minutum; MaxEnt, habitat suitability; environmental variable; potential distributions	EAST-COAST; DINOPHYCEAE; BLOOMS; SEDIMENTS; MAXENT; GROWTH; CYSTS	Alexandrium minutum from the China Sea produces a range of toxins and causes damage to the local ecosystems and aquaculture. This is essential to understand environmental factors affecting potential distribution. Potential distributions of A. minutum in the China Sea were predicted based on maximum entropy modeling, and dominant environmental variables were studied through analyses of variable contributions and response curves. The results showed that highly suitable areas were mainly located in the southwest of the Yellow Sea, the Laizhou Bay, and north of Haizhou Bay. The coast of the South China Sea was predicted as a low-suitability area, and the coast of the East China Sea as an unsuitable area. Mean temperature of the coldest month (T_min) had the largest drop in permutation importance but a low percent contribution. The probability of presence of A. minutum increased with increasing concentration of nitrate (NO3-) and annual mean temperature (T_ann) over a wide range of them. The response curves decreased with increasing concentration of phosphate (PO43-) and ratio of NO3- to PO43- (N_P_ratio) when PO43- is above 0.049 mu mol L-1 and N_P_ratio above 4, indicating that low values of PO43- concentration and N_P_ratio favour the occurrence of A. minutum. As a predictor, the variance of annual temperature (T_Var) had the highest percent contribution and gains. PO43- was predicted to have much more information than the other variables, and exhibited the second largest drop in permutation importance and percent contribution. The T_Var and PO43- are the most important dominant predictor variables.	[Wang, Changyou; Zheng, Ping; Gu, Haifeng; Luo, Zhaohe; Luo, Zhuhua; Mao, Longjiang; Zhang, Yuanzhi] Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China; [Gu, Haifeng; Luo, Zhuhua] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Luo, Zhuhua] Minist Nat Resources, Inst Oceanog 3, Key Lab Marine Biogenet Resources, Xiamen 361005, Peoples R China	Nanjing University of Information Science & Technology; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources	Wang, CY (通讯作者)，Nanjing Univ Informat Sci & Technol, Sch Marine Sci, Nanjing 210044, Peoples R China.	chywang@nuist.edu.cn	Luo, Zhaohe/ITT-7163-2023; luo, zhuhua/ADX-8382-2022; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	This work was supported by the National Key Research and the Development Program of China (No. 2019YFE 0124700), the China National Key Research and Development Program (No. 2022YFC3106002), the National Natural Science Foundation of China (No. U1901215), [2019YFE 0124700]; National Key Research and the Development Program of China [2022YFC3106002]; China National Key Research and Development Program [U1901215]; National Natural Science Foundation of China [2020r028]; Startup Foundation for Introducing Talent of NUIST	This work was supported by the National Key Research and the Development Program of China (No. 2019YFE 0124700), the China National Key Research and Development Program (No. 2022YFC3106002), the National Natural Science Foundation of China (No. U1901215),(National Key Research & Development Program of China); National Key Research and the Development Program of China(National Key Research & Development Program of China); China National Key Research and Development Program(National Key Research & Development Program of China); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Startup Foundation for Introducing Talent of NUIST	This work was supported by the National Key Research and the Development Program of China (No. 2019YFE 0124700), the China National Key Research and Development Program (No. 2022YFC3106002), the National Natural Science Foundation of China (No. U1901215), and the Startup Foundation for Introducing Talent of NUIST (No. 2020r028).	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OCEAN UNIV.	AUG	2023	22	4					1119	1128		10.1007/s11802-023-5422-y	http://dx.doi.org/10.1007/s11802-023-5422-y			10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	U5MY1					2025-03-11	WOS:001085255300026
J	Singh, YP; Verma, P; Singh, A; Bali, R				Singh, Yogesh Pal; Verma, Poonam; Singh, Abha; Bali, Rameshwar			Early Miocene (Burdigalian) Dinoflagellate Cysts from the Kerala Basin, Southwest India: Indicators of Marine Ingression at the Onset of the Mid-Miocene Climate Optimum (MMCO) (vol 99, pg 357, 2023)	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Correction									[Singh, Yogesh Pal; Verma, Poonam; Singh, Abha] Birbal Sahni Inst Palaeosciences, 53 Univ Rd, Lucknow 226007, India; [Singh, Yogesh Pal; Bali, Rameshwar] Univ Lucknow, Ctr Adv study Geol, Lucknow 226007, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Lucknow University	Verma, P (通讯作者)，Birbal Sahni Inst Palaeosciences, 53 Univ Rd, Lucknow 226007, India.	verma.poonam07@gmail.com						Singh YP, 2023, J GEOL SOC INDIA, V99, P357, DOI 10.1007/s12594-023-2318-9	1	0	0	0	2	GEOLOGICAL SOC INDIA	BANGALORE	NO 63, 12TH CORSS, BASAPPA LAY OUT, GAVIPURAM PO, PO BOX 1922, BANGALORE, 560-019, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	AUG	2023	99	8							1183	10.1007/s12594-023-2448-0	http://dx.doi.org/10.1007/s12594-023-2448-0			1	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	P2TK4		Bronze			2025-03-11	WOS:001049213200019
J	Wu, XE; Lemay-Tougas, M; de Vernal, A; Garneau, M; Fréchette, B; Audet, T; Hillaire-Marcel, C				Wu, Xiner; Lemay-Tougas, Mathieu; de Vernal, Anne; Garneau, Michelle; Frechette, Bianca; Audet, Tiffany; Hillaire-Marcel, Claude			Multi-proxy reconstruction of climate changes in the Lower St. Lawrence Estuary, Canada, during the Middle and Late-Holocene	HOLOCENE			English	Article						benthic foraminifera; bottom-water conditions; dinoflagellate cysts; hydroclimate; mid-late-Holocene; pollen; sea-surface conditions; St. Lawrence Estuary	WATER MASS CHANGES; LABRADOR SEA; GASPE-PENINSULA; HEMLOCK DECLINE; LATE QUATERNARY; GULF; CIRCULATION; SURFACE; MARINE; OXYGEN	The micropaleontological and palynological content, and geochemical and isotopic composition of a marine sediment core collected off Pointe-des-Monts in eastern Quebec, Canada, reveal regional palaeoclimatic and paleoceanographic conditions in the Lower St. Lawrence Estuary over the last similar to 8200 years. The pollen and spore content allows comparison with the terrestrial palynostratigraphy, whereas dinoflagellate cysts and benthic foraminifera are used to reconstruct sea-surface conditions and bottom water properties, respectively. The dinocyst-based reconstructions indicate shifts between estuarine and oceanic conditions with important changes in sea-surface temperature, salinity, and primary productivity. Both the dinocyst assemblages and the quantitative sea-surface estimates highlight a distinct transition at ca. 4200 cal years BP. It is notably marked by a change towards higher salinity, which suggests reduced freshwater discharge, hence lower precipitation in the watershed, during the Late-Holocene. The isotopic composition (delta O-18 and delta C-13) and assemblages of the benthic foraminifera indicate centennial to millennial frequency variability of bottom water properties, over a general trend towards decreasing temperatures and increasing ventilation from the beginning of the Middle Holocene until the last century. Since then, reverse trends with abrupt warming and decreasing dissolved oxygen content in bottom water have been observed.	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J	Leroy, SAG; Henry, P; Marret, F; Pailles, C; Licari, L; Kende, J; Rostek, F; Bard, E				Leroy, S. A. G.; Henry, P.; Marret, F.; Pailles, C.; Licari, L.; Kende, J.; Rostek, F.; Bard, E.			Dinocyst assemblages and water surface conditions in the Sea of Marmara during MIS 6 and 5 from two long cores	QUATERNARY SCIENCE REVIEWS			English	Article						Dinocysts; MIS 6 and 5; Marmara sea; Connection; Sea level; Sapropel	BLACK-SEA; DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; LATE PLEISTOCENE; CASPIAN BASIN; SAPROPEL S1; AEGEAN SEA; HOLOCENE; EVOLUTION; SEDIMENTS	The Sea of Marmara is the connection between the vast Black Sea-Caspian Sea basin (Pontocaspian) and the Global Ocean via the Mediterranean Sea. Its water levels and water conditions has widely varied over times. Combining two cores in the Sea of Marmara (Turkey) and using organic-walled dinoflagellate cyst assemblages as the main proxy (combined with alkenones, diatoms and benthic foraminifera), allow qualitatively reconstructing water conditions during Marine Isotopic Stage (MIS) 6 and 5, such as salinity and oxygen level. A clear main marine phase is illustrated in MIS 5e. A minor marine incursion occurred during MIS 5c, mostly supported by alkenone data. The rest of the record indicates brackish Pontocaspian conditions, with more Spiniferites inaequalis in MIS 6 and more S. cruciformis in the non-marine parts of MIS 5.At the MIS 6/MIS 5 transition, an earlier initial marine flooding in the Sea of Marmara (dinocyst assemblages) in comparison to the Black Sea was highlighted. The marine reconnection occurred at different moments as seen in the terrestrial vegetation reconstructed from pollen analysis linking the two seas.The sapropels of the Sea of Marmara form when marine water penetrates at depth from the Aegean Sea beneath a layer of lower salinity water. Variations of the residence time of the marine deep water in a stratified Sea of Marmara are potentially an important factor underlying hypoxia/anoxia and sapropel deposition. When combining surface water proxies with benthic foraminifera (test assemblages and presence of inner organic lining), it appears that the successive MIS 5 sapropels formed under decreasing salinity and oxygen availability conditions as the marine inflow was increasingly restricted. Understanding the hydrologic evolution of the Sea of Marmara during MIS 5 implies taking into account that the Bosphorus and Dardanelle straits are hydrodynamically coupled and may not be simplified as on/off switches based on present day sill depths.	[Leroy, S. A. G.; Henry, P.; Pailles, C.; Licari, L.; Kende, J.; Rostek, F.; Bard, E.] Aix Marseille Univ, Coll France, CNRS, IRD,INRAE,CEREGE, Aix En Provence, France; [Leroy, S. A. G.] Aix Marseille Univ, Minist Culture & Com, CNRS, LAMPEA, F-13094 Aix En Provence, France; [Leroy, S. A. G.; Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, England	Centre National de la Recherche Scientifique (CNRS); Universite PSL; College de France; INRAE; Institut de Recherche pour le Developpement (IRD); Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; University of Liverpool	Leroy, SAG (通讯作者)，Aix Marseille Univ, Coll France, CNRS, IRD,INRAE,CEREGE, Aix En Provence, France.	suzleroy@hotmail.com; henry@cerege.fr; fmarret@liverpool.ac.uk; pailles@cerege.fr; licari@cerege.fr; jj.kende@gmail.com; rostek@cerege.fr; bard@cerege.fr	PAILLES, Christine/JQI-8924-2023; Henry, Pierre/A-4045-2011	Marret-Davies, Fabienne/0000-0003-4244-0437	MARSITE FP7 EU Project [308417]; Bilateral ANR/TUEBITAK collaborative research project MAREGAMI [ANR-16-CE03-0010-02]; Tubitak Project [116Y371]	MARSITE FP7 EU Project; Bilateral ANR/TUEBITAK collaborative research project MAREGAMI; Tubitak Project(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK))	We are grateful to Jennifer Bradley and Luke Glascott at the University of Liverpool (UK) and Dahvya Belkacem at IMBE (Aix-en-Provence, France) for palynological extraction in the pollen laboratories. Cores were taken during the MARSITECRUISE of Ifremer/Genavir R.V. Pourquoi Pas? within the framework of MARSITE FP7 EU Project (grant agreement no: 308417) . Thanks are due to N. Cagatay, K. Eris , and N. Yakupoglu from ITU (Turkey) who gave access to core CS18 for sampling and contributed to the improvement of this publication owing to intensive discussions over the years. Part of this work has been supported by Bilateral ANR/TUEBITAK collaborative research project MAREGAMI (ANR-16-CE03-0010-02) and Tubitak Project (116Y371) . We are grateful to the reviewers for their constructive comments.	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Zwiep KL, 2018, QUATERNARY SCI REV, V200, P178, DOI 10.1016/j.quascirev.2018.08.026	98	6	6	0	3	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0277-3791	1873-457X		QUATERNARY SCI REV	Quat. Sci. Rev.	AUG 15	2023	314								108229	10.1016/j.quascirev.2023.108229	http://dx.doi.org/10.1016/j.quascirev.2023.108229		JUL 2023	21	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	P4UH8		Green Submitted, Green Published, Bronze			2025-03-11	WOS:001050619900001
J	Semin, S; Tas, S; Dursun, F				Semin, Sebahat; Tas, Seyfettin; Dursun, Fuat			Spatial-temporal variability of phytoplankton community and potentially harmful species in the Golden Horn Estuary (Sea of Marmara, Turkiye)	JOURNAL OF THE MARINE BIOLOGICAL ASSOCIATION OF THE UNITED KINGDOM			English	Article						estuary; Golden Horn; HABs; oceanography; phytoplankton; toxic species	SKELETONEMA-COSTATUM; EUTROPHIC ESTUARY; CYST FORMATION; RED TIDE; RIVER; DINOPHYCEAE; DIVERSITY; SALINITY; BLOOMS; SEASONALITY	Spatial-temporal variability of phytoplankton community and potentially harmful species in the Golden Horn Estuary (Sea of Marmara) was investigated from October 2018 to September 2019 together with some environmental factors. A total of 148 phytoplankton taxa were identified during the study period. Among these, 134 taxa (90.5%) consisted of diatoms (71 taxa, 48%) and dinoflagellates (63 taxa, 42.5%), while 14 taxa (9.5%) were other groups. Seventeen species were recorded for the first time in the study area. Species richness was highest in October, while it was lowest in August. The species diversity (H') varied according to sampling stations. Cell abundances were higher especially in the middle and upper estuary in spring and summer than in autumn and winter. The abundance of diatoms and euglenophyceans was highest in spring, while the abundance of raphidophycean and cryptophycean was highest in summer. Temperature was correlated positively with total abundance (P < 0.01), but negatively with species diversity (H') (P < 0.01). Several dense algal blooms causing discolouration in surface water occurred in spring and summer. A total of 12 microalgae species known as potentially toxic were detected during this study period. Among these, dinoflagellates Alexandrium cf. tamarense and Dinophysis infundibulum were recorded for the first time in the study area. The increase in species diversity and richness in the upper estuary, and the decrease in frequency of bloom events compared with the previous years indicated the changes in environmental conditions in this study period. Findings showed that phytoplankton might be used as an indicator of the changing environmental conditions in such ecosystems.	[Semin, Sebahat; Tas, Seyfettin; Dursun, Fuat] Istanbul Univ, Inst Marine Sci & Management, TR-34134 Istanbul, Turkiye	Istanbul University	Semin, S (通讯作者)，Istanbul Univ, Inst Marine Sci & Management, TR-34134 Istanbul, Turkiye.	sebahat_semin@hotmail.com	Tas, Seyfettin/AAC-5594-2020; Dursun, Fuat/AAD-4351-2022	, Seyfettin/0000-0002-4660-3937				Ahel M, 1996, MAR ECOL PROG SER, V143, P289, DOI 10.3354/meps143289; Albayrak S, 2010, MEDITERR MAR SCI, V11, P295, DOI 10.12681/mms.78; AlgaeBase, US; Altenburger A, 2020, SCI ADV, V6, DOI 10.1126/sciadv.abb1611; Balzano S, 2011, J PLANKTON RES, V33, P937, DOI 10.1093/plankt/fbq150; Barbosa AB, 2010, ESTUAR COAST, V33, P324, DOI 10.1007/s12237-009-9200-x; BARLOW RG, 1993, DEEP-SEA RES PT II, V40, P459, DOI 10.1016/0967-0645(93)90027-K; Buric Z, 2007, MAR ECOL-EVOL PERSP, V28, P169, DOI 10.1111/j.1439-0485.2007.00180.x; Cerino F, 2006, EUR J PHYCOL, V41, P363, DOI 10.1080/09670260600839450; Cetinic I, 2006, HYDROBIOLOGIA, V555, P31, DOI 10.1007/s10750-005-1103-7; Clarke K.R., 2001, PRIMER V5 USER MANUA; CLOERN JE, 1987, CONT SHELF RES, V7, P1367, DOI 10.1016/0278-4343(87)90042-2; Cupp Easter E., 1943, BULL SCRIPPS INST OCEANOGR, V5, P1; Drebes G., 1974, MARINES PHYTOPLANKTO; Dursun F, 2021, J MAR BIOL ASSOC UK, V101, P649, DOI 10.1017/S0025315421000631; Dursun F, 2019, J MAR BIOL ASSOC UK, V99, P279, DOI 10.1017/S0025315418000073; Dursun F, 2017, TURK J FISH AQUAT SC, V17, P653, DOI 10.4194/1303-2712-v17_4_01; Dursun Fuat, 2016, Su Urunleri Dergisi, V33, P201, DOI 10.12714/egejfas.2016.33.3.03; Guiry M.D., 2020, AlgaeBase; Hevia-Orube J, 2016, DIATOM RES, V31, P185, DOI 10.1080/0269249X.2016.1228548; Hoppenrath M., 2009, MARINE PHYTOPLANKTON; Irvali N, 2009, GEO-MAR LETT, V29, P151, DOI 10.1007/s00367-008-0129-z; Jasprica N, 2012, NOVA HEDWIGIA, P405; KALELI A, 2021, AQUAT RES, V4, P88, DOI DOI 10.3153/AR21008; Koyuncu A., 2018, 3 MARM SEA S NOV 201, P155; Lassus P., 2016, Toxic and harmful microalgae of the world ocean; Legrand C, 1998, AQUAT MICROB ECOL, V15, P65, DOI 10.3354/ame015065; Lionard M, 2005, HYDROBIOLOGIA, V540, P105, DOI 10.1007/s10750-004-7123-x; Liu DY, 2005, MAR POLLUT BULL, V50, P91, DOI 10.1016/j.marpolbul.2004.11.016; Lundholm N., 2009, IOC UNESCO TAXONOMIC; Mallin MA, 1999, ESTUARIES, V22, P825, DOI 10.2307/1353064; MANTOURA RFC, 1983, ANAL CHIM ACTA, V151, P297, DOI 10.1016/S0003-2670(00)80092-6; marinespecies, WORMS; McLusky DS., 2004, ESTUARINE ECOSYSTEM; Okus E., 2001, GOLD HORN 2001 S IST, P145; Olli K, 2004, MAR BIOL, V145, P1, DOI 10.1007/s00227-004-1295-9; Olli K, 1996, J PLANKTON RES, V18, P1587, DOI 10.1093/plankt/18.9.1587; Paerl HW, 2007, ECOL APPL, V17, pS88, DOI 10.1890/05-0840.1; Rensel J.E., 2007, Fish kills from the harmful alga Heterosigma akashiwo in Puget Sound: Recent blooms and review; Rensel JEJ, 2010, HARMFUL ALGAE, V10, P98, DOI 10.1016/j.hal.2010.07.005; Sarno D, 2005, J PHYCOL, V41, P151, DOI 10.1111/j.1529-8817.2005.04067.x; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Sur HI, 2002, WATER SCI TECHNOL, V46, P29, DOI 10.2166/wst.2002.0138; Tas S, 2015, MEDITERR MAR SCI, V16, P621, DOI 10.12681/mms.1049; Tas S, 2015, MEDITERR MAR SCI, V16, P432, DOI 10.12681/mms.1042; Tas S., 2003, TURK J MAR SCI, V9, P163; Tas S, 2006, ESTUAR COAST SHELF S, V68, P593, DOI 10.1016/j.ecss.2006.02.025; Tas S, 2020, J MAR BIOL ASSOC UK, V100, P1053, DOI 10.1017/S0025315420001058; Tas S, 2019, BOT MAR, V62, P537, DOI 10.1515/bot-2019-0035; Tas S, 2016, TURK MAR RES FND PUB, V42, P768; Tas S, 2017, FUND APPL LIMNOL, V189, P153, DOI 10.1127/fal/2016/0957; Tas S, 2017, J MAR BIOL ASSOC UK, V97, P1483, DOI [10.1017/s0025315416000837, 10.1017/S0025315416000837]; Tas S, 2011, TURK J FISH AQUAT SC, V11, P673, DOI 10.4194/1303-2712-v11_4_03; Tas S, 2009, ESTUAR COAST, V32, P1205, DOI 10.1007/s12237-009-9207-3; Throndsen J., 1978, Preservation and storage, P69, DOI DOI 10.1111/J.0022-3646.1975.00142.X; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Uysal Zahit, 1996, Turkish Journal of Botany, V20, P519; Wang ZH, 2007, J PLANKTON RES, V29, P209, DOI 10.1093/plankt/fbm008	58	3	3	3	11	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	0025-3154	1469-7769		J MAR BIOL ASSOC UK	J. Mar. Biol. Assoc. U.K.	JUL 24	2023	103								e56	10.1017/S0025315423000449	http://dx.doi.org/10.1017/S0025315423000449			14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	M7IQ9					2025-03-11	WOS:001031920200001
J	Hartkopf-Fröder, C; Martini, E; Heilmann-Clausen, C; Neumann, FH; Schäfer, P; Wilkes, H; Böcker, J; Hottenrott, M				Hartkopf-Froeder, Christoph; Martini, Erlend; Heilmann-Clausen, Claus; Neumann, Frank H.; Schaefer, Peter; Wilkes, Heinz; Boecker, Johannes; Hottenrott, Martin			Eocene sediments and a fresh to brackish water biota from the early rifting stage of the Upper Rhine Graben (west of oil field Landau, southwest Germany): implications for biostratigraphy, palaeoecology and source rock potential	PALAEOBIODIVERSITY AND PALAEOENVIRONMENTS			English	Article						Calcareous nannoplankton; Palynomorphs; Microfossils; Vertebrate remains; Palaeoecology; Organic geochemistry; Paleogene	LONG-DISTANCE DISPERSAL; NORTH-SEA BASIN; MIDDLE EOCENE; DINOFLAGELLATE CYSTS; THERMAL MATURITY; MOLASSE BASIN; COASTAL SWAMP; OLIGOCENE; PALEOGENE; PALEOCENE	The Eocene biota from the pre-rifting stage of the Upper Rhine Graben (southwest Germany) is, with exception of the world-famous fossil sites Messel and Bouxwiller, poorly known. While from these localities exclusively terrestrial and freshwater fossils were recovered, here we present floral and faunal assemblages from the middle Upper Rhine Graben which clearly indicate a temporarily brackish water environment and consist of a diverse palynomorph association, calcareous nannoplankton, foraminifers, ostracods and some fish and reptile remains. Based on the occurrence of Trochastrites hohnensis, a Lutetian age is assumed. Organic-walled dinoflagellate cysts, in particular Phthanoperidinium comatum, Phthanoperidinium echinatum, Apectodinium homomorphum and Apectodinium quinquelatum, suggest a late Ypresian to Lutetian age. The pollen and spores assemblage includes typical mid Eocene species, such as Tegumentisporis villosoides, Tricolporopollenites crassostriatus and representatives of Bombacaceae, but a late Ypresian to Priabonian age cannot be excluded. Foraminifers and ostracods do not further refine the biostratigraphical assignment. Hence, a Lutetian age is most probable. The mass occurrence of Neocyprideis, various foraminifer taxa and an organic-walled dinoflagellate cyst assemblage of very low diversity are indicative of a brackish water environment. Disarticulated vertebrate remains include fish teeth of Lepisosteidae, turtle plates and alligatoroid teeth of Diplocynodon and Hassiacosuchus. The present palaeogeographical scenarios do not consider a connection from the Upper Rhine Graben to the North Sea Basin, Alpine Sea/Paratethys or Paris Basin during the mid Eocene. Provided that the middle Upper Rhine Graben was land-locked and definitely not reached by a marine ingression during this time interval, we tentatively suggest that the brackish water taxa may have been accidentally introduced into a brackish inland sea by wind (anemochory), rain, highly mobile insects or vertebrates such as fish, birds and mammals (endozoochory/ectozoochory). The presumably freshwater calcareous nannoplankton species Nannoserratolithus minutus Martini is newly described.	[Hartkopf-Froeder, Christoph] Univ Cologne, Inst Geol & Mineral, Zulpicher Str 49a, D-50674 Cologne, Germany; [Martini, Erlend] Parkstr 40, D-61476 Kronberg, Germany; [Heilmann-Clausen, Claus] Aarhus Univ, Dept Geosci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Neumann, Frank H.] North West Univ, Fac Nat & Agr Sci, Unit Environm Sci & Management, Potchefstroom, South Africa; [Neumann, Frank H.] Univ Munster, Inst Geol & Palaeontol Palaeobotany, Heisenbergstr 2, D-48149 Munster, Germany; [Schaefer, Peter] Bachmayerstr 12, D-65195 Wiesbaden, Germany; [Wilkes, Heinz] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm, Carl von Ossietzky Str 9-11, D-26129 Oldenburg, Germany; [Boecker, Johannes] Neptune Energy Holding Germany GmbH, Ahrensburger Str 1, D-30659 Hannover, Germany; [Hottenrott, Martin] Hessian Agcy Nat Conservat Environm & Geol, Rheingaustr 186, D-65203 Wiesbaden, Germany	University of Cologne; Aarhus University; North West University - South Africa; University of Munster; Carl von Ossietzky Universitat Oldenburg	Hartkopf-Fröder, C (通讯作者)，Univ Cologne, Inst Geol & Mineral, Zulpicher Str 49a, D-50674 Cologne, Germany.	hartkopf-froeder@gmx.de; claus.heilmann@geo.au.dk; frank.neumann@nwu.ac.za; heinz.wilkes@uni-oldenburg.de	Heilmann-Clausen, Claus/A-4848-2012; Hartkopf-Froder, Christoph/ACK-0770-2022	Heilmann-Clausen, Claus/0000-0002-5894-7139; Hartkopf-Froder, Christoph/0000-0002-1835-577X; Neumann, Frank H./0000-0002-3620-2742				Agha M, 2019, CONSERV PHYSIOL, V7, DOI 10.1093/conphys/coz054; Agha M, 2018, BIOL REV, V93, P1634, DOI 10.1111/brv.12410; Akkiraz MS, 2006, TURK J EARTH SCI, V15, P155; Allenbach RP, 2006, INT J EARTH SCI, V95, P803, DOI 10.1007/s00531-006-0071-0; [Anonymous], 1977, ARCH SCI GENEVE; [Anonymous], 1988, JAHRESBERICHTE MITTE, DOI [10.1127/jmogv/70/1988/399, DOI 10.1127/JMOGV/70/1988/399]; [Anonymous], 1981, B CENT RECH EXPL; Ashraf A.R., 1996, Neues Jb. 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J	Vasilyeva, ON; Musatov, VA				Vasilyeva, Olga N.; Musatov, Vladimir A.			Dinoflagellate cyst and nannoplankton assemblages from the Middle Eocene Kuma Formation of Crimean Peninsula -biostratigraphy and palynofacies	PALAEOWORLD			English	Article						dinocysts; nannoplankton; Lutetian; Bartonian; biostratigraphy; Crimean Peninsula	PALEOCENE; STRATIGRAPHY	The stratigraphic correlation of the Kuma Formation from the south of the Russian Platform and the Crimea-Caucasian region has been a matter of debate for decades. A bed-by-beds study of dinocysts and nannoplankton from the the Kuma Formation made it possible to recognize a sequence of biotic events, important for defining and correlating the biozones. At the Bakhchisarai limestone quarry, six dinoflagellate zones and six nannoplankton zonal units were recognized, assignable to the Middle Eocene Lutetian and Bartonian stages. Our paleoecological analyses of the organic-walled microphytoplankton assemblages and of the palynofacies indicate that the the Kuma Formation deposited in the inner shelf zone, probably of anoxic and eutrophic settings within the Pontic-Transcaucasian magmatic belt. Assemblages of organic-walled microphytoplankton comprise potentially toxic dinoflagellate species of Alexandrium. The Middle Eocene Climatic Optimum event is recorded in the upper part of the the Kuma Formation, presumably indicated by the Dracodinium rhomboideum dinoflagellate zone, which is characterized by an acme of Dracodinium laszczynskii Gedl and the lowest occurrence of nannofossils Reticulofenestra bisecta (Hay, Mohler and Wade) Roth. Two new species are described: Pentadinium rugosum Vasilyeva, n. sp. (dinocyst) and Corannulus tauricum Musatov, n. sp. (nannofossil). The bioevents and biozones established herein are significant for correlations of the Middle Eocene of the Crimean Peninsula and the south of the Russian Platform. & COPY; 2022 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights reserved.	[Vasilyeva, Olga N.] Russian Acad Sci, Inst Geol & Geochem, Ural Branch, 15 Akad Vonsovskogo St, Ekaterinburg 620110, Russia; [Musatov, Vladimir A.] Lower Volga Inst Geol & Geophys, 70 Moskovskaya St, Saratov 410012, Russia	Russian Academy of Sciences	Vasilyeva, ON (通讯作者)，Russian Acad Sci, Inst Geol & Geochem, Ural Branch, 15 Akad Vonsovskogo St, Ekaterinburg 620110, Russia.	vasilyeva@igg.uran.ru; dr.musatov@yandex.ru			Ural Branch, Russian Academy of Sciences [AAAA-A18-118052590025-8]	Ural Branch, Russian Academy of Sciences(Russian Academy of Sciences)	We express our deep gratitude to the authorities of the Bakhchisarai "Stroyindustriya" integrated works, to the chief surveyor Emiraly Mustafayev and to the head of the mining department A.G. Saitov for assistance and for providing the means to study the section within the quarry. We are also grateful to Przemyslaw Gedl, an anonymous reviewer and Qun Yang (Editor-in-Chief of Palaeoworld) for reviewing the manuscript with helpful comments and recommendations, and to our colleagues from the Institute of geological sciences at the Ukrainian NAS and the Lugansk University for participating in the team field work in 2005. The work has been made within the framework of the theme No. AAAA-A18-118052590025-8 of the state assignment for Institute of Geology and Geochemistry of the Ural Branch, Russian Academy of Sciences.	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J	Steinsland, K; Grant, DM; Ninnemann, US; Fahl, K; Stein, R; De Schepper, S				Steinsland, Kristine; Grant, Danielle M.; Ninnemann, Ulysses S.; Fahl, Kirsten; Stein, Ruediger; De Schepper, Stijn			Sea ice variability in the North Atlantic subpolar gyre throughout the Last Interglacial	QUATERNARY SCIENCE REVIEWS			English	Article						Sea ice; Labrador sea; Eirik drift; Ocean circulation; Dinoflagellate cysts; Biomarkers; IP25; MIS 5e	DINOFLAGELLATE CYST ASSEMBLAGES; ARCTIC-OCEAN; SOUTHERN GREENLAND; SURFACE CONDITIONS; GLACIAL INCEPTION; DEEP-WATER; BAFFIN-ISLAND; NORWEGIAN SEA; LABRADOR SEA; FRAM STRAIT	The Last Interglacial period, Marine Isotope Stage 5e (MIS 5e similar to 116-128 ka), is thought to have had a warmer, but less stable climate than the present interglacial. One key factor that has the potential to influence the ocean and climate is sea ice, but its presence and extent throughout MIS 5e is poorly constrained. Here we reconstruct the sea surface hydrography and sea ice variability in the Labrador Sea, a region influenced by the subpolar gyre (SPG) and where deep water formation occurs, in order to evaluate the potential of sea ice to drive or amplify ocean variability. We analysed biomarkers (highly branched isoprenoids, HBIs, and sterols), dinoflagellate cyst assemblages and stable oxygen isotopes from the late stages of MIS 6, throughout MIS 5e, into MIS 5d. Our results show that the late glacial MIS 6 was likely characterised by a thick multiyear sea ice cover. During the first phase of MIS 5e, the hydrography was highly variable. The initial 1500 years (128-126.5 ka) were characterised by the presence of a seasonal Marginal Ice Zone (MIZ) accompanied by subsurface warmth. As the sea ice retreated, cool, likely polar-sourced water dominated the surface and subsurface ocean (126.5-124 ka), until an abrupt surge of sea ice marked the final pulse of the remnants of the deglaciation. The second half of MIS 5e (124-116 ka) was characterised by a persistent inflow of warm water, only interrupted by incursions of cold water as summer insolation declined. Seasonal sea ice returned to the Eirik Drift during MIS 5d. We infer that sea ice variability throughout MIS 5e was coupled with the variability of the SPG. Especially the location of a proximal MIZ to the Labrador Sea convection region could have been important for SPG dynamics. In addition, the presence of sea ice at the transitions into and out of MIS 5e could point to its important role in modulating and enhancing the magnitude and coherence of climate signals at major climatic transitions. (c) 2023 Published by Elsevier Ltd.	[Steinsland, Kristine; Grant, Danielle M.; De Schepper, Stijn] NORCE Norwegian Res Ctr, NORCE Climate & Environm, Bergen, Norway; [Steinsland, Kristine; Grant, Danielle M.; De Schepper, Stijn] Bjerknes Ctr Climate Res, Bergen, Norway; [Ninnemann, Ulysses S.] Univ Bergen, Dept Earth Sci, Bergen, Norway; [Ninnemann, Ulysses S.] Bjerknes Ctr Climate Res, Bergen, Norway; [Fahl, Kirsten; Stein, Ruediger] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany; [Stein, Ruediger] Univ Bremen, Fac Geosci, Bremen, Germany; [Stein, Ruediger] Ctr Marine Environm Sci, Bremen, Germany; [Stein, Ruediger] Ocean Univ China, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Qingdao, Peoples R China; [Stein, Ruediger] Key Lab Marine Chem Theory & Technol, Qingdao, Peoples R China	Norwegian Research Centre (NORCE); Bjerknes Centre for Climate Research; University of Bergen; Bjerknes Centre for Climate Research; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Bremen; Ocean University of China	Steinsland, K (通讯作者)，NORCE Norwegian Res Ctr, NORCE Climate & Environm, Bergen, Norway.; Steinsland, K (通讯作者)，Bjerknes Ctr Climate Res, Bergen, Norway.	stei@norceresearch.no	Grant, Danielle/AAI-6908-2020; De Schepper, Stijn/A-2836-2011	Grant, Danielle Magann/0000-0003-4062-6481; Steinsland, Kristine/0000-0002-1276-0109	European Research Council (ERC) under the European Union; European Research Council under the European Union;  [818449];  [610055]	European Research Council (ERC) under the European Union(European Research Council (ERC)); European Research Council under the European Union(European Research Council (ERC)); ; 	This study is part of the AGENSI project, which is funded by the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement n degrees 818449) . We like to thank the researchers and crew on board RV G.O. Sars during the 2016 cruise of the Ice2Ice project, which was funded by the European Research Council under the European Union's Seventh Framework Programme (FP7/2007-2013, ERC grant agreement n degrees 610055) . We thank Walter Luttmer in the biomarker laboratory, Dag Inge Blindheim for technical support and Malcolm Jones at Palynological Laboratory Service Ltd.	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Sci. Rev.	AUG 1	2023	313								108198	10.1016/j.quascirev.2023.108198	http://dx.doi.org/10.1016/j.quascirev.2023.108198		JUL 2023	17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	N8RE4		Green Published, hybrid			2025-03-11	WOS:001039612800001
J	Koutsodendris, A; Brauer, A; Friedrich, O; Tjallingii, R; Putyrskaya, V; Hennrich, B; Kühn, R; Klemt, E; Pross, J				Koutsodendris, Andreas; Brauer, Achim; Friedrich, Oliver; Tjallingii, Rik; Putyrskaya, Victoria; Hennrich, Barbara; Kuehn, Robert; Klemt, Eckehard; Pross, Joerg			Natural and human-induced ecosystem change in SE Europe since AD 1700 derived from a partially varved sediment record from Lake Vouliagmeni (Greece)	HOLOCENE			English	Article						Eastern Mediterranean region; lacustrine turbidites; Little Ice Age; varve microfacies; vegetation dynamics; XRF core scanning	ENVIRONMENTAL-CHANGE; CLIMATE VARIABILITY; KORINTHIAKOS GULF; PINNA-NOBILIS; CORINTH; RECONSTRUCTION; HOLOCENE; ETOLIKO; STRAIN; LAGOON	To reconstruct naturally and anthropogenically induced environmental change in SE Europe since the Little Ice Age, we have examined five partially varved sediment cores from coastal Lake Vouliagmeni, Greece. Our reconstructions are based on a multi-proxy approach including microfacies analysis, X-ray fluorescence core scanning, radionuclide dating (Pb-210, Cs-137, and Am-241), and palynological analysis (pollen, spores, and dinoflagellate cysts). A 131 -cm-long composite record that encompasses the past c. 300 years reveals 181 varves of endogenic and mixed clastic-biogenic types. The formation of these varves was controlled by seasonal variability in clastic input and primary productivity. The non-varved intervals consist of homogenous lake sediments and turbidite deposits. Based on a chronology developed through radionuclide dating, varve counting and exclusion of turbidites from the sequence, we have compared our proxy data with meteorological data and historical records of earthquakes and human activities. Our results suggest that the surroundings of Lake Vouliagmeni experienced relatively wet conditions during the late solar Maunder Minimum (1645-1715 AD) and relatively dry conditions during the Dalton Minimum (1790-1830 AD), which highlights the hydroclimatic heterogeneity in SE Europe during the Little Ice Age. The evaluation of historical documentation suggests that the majority of the turbidites is related to lake-slope instabilities following earthquake shocks. Human impact on Lake Vouliagmeni includes (i) a change in aquatic biota following the artificial connection of the lake to the sea at c. 1880 AD, and (ii) expansion of agricultural areas and reduction of natural forests around the lake due to population growth over the past 300 years.	[Koutsodendris, Andreas; Friedrich, Oliver; Hennrich, Barbara; Kuehn, Robert; Pross, Joerg] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany; [Brauer, Achim; Tjallingii, Rik] German Res Ctr Geosci, Climate Dynam & Landscape Evolut, Potsdam, Germany; [Putyrskaya, Victoria; Klemt, Eckehard] Univ Appl Sci Ravensburg Weingarten, Weingarten, Germany; [Koutsodendris, Andreas] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany	Ruprecht Karls University Heidelberg; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; Ruprecht Karls University Heidelberg	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	Koutsodendris, Andreas/0000-0003-4236-7508				Ahmed M, 2013, NAT GEOSCI, V6, P339, DOI [10.1038/NGEO1797, 10.1038/ngeo1797]; Ambraseys NN, 1997, J EARTHQ ENG, V1, P433, DOI 10.1080/13632469708962374; AMBRASEYS NN, 1990, GEOPHYS J INT, V101, P663, DOI 10.1111/j.1365-246X.1990.tb05577.x; Anthony EJ, 2014, EARTH-SCI REV, V139, P336, DOI 10.1016/j.earscirev.2014.10.003; Appleby P.G., 2001, Tracking Environmental Change Using Lake Sediments, P171, DOI [DOI 10.1007/0-306-47669-X9, DOI 10.1007/0-306-47669-X_9]; Ariztegui D, 2010, GLOBAL PLANET CHANGE, V71, P183, DOI 10.1016/j.gloplacha.2009.11.016; BEHRE KE, 1990, MANS ROLE IN THE SHAPING OF THE EASTERN MEDITERRANEAN LANDSCAPE, P219; Ben Dor Y, 2019, QUATERNARY SCI REV, V215, P173, DOI 10.1016/j.quascirev.2019.04.011; Birks HH, 2006, VEG HIST ARCHAEOBOT, V15, P235, DOI 10.1007/s00334-006-0066-6; Botemma S., 1975, PALAEOHISTORIA, VXVII, P17; Brauer A, 2004, GKSS SCH ENVIRONM, P109; Brauer A, 2001, J PALEOLIMNOL, V25, P163, DOI 10.1023/A:1008136029735; Büntgen U, 2016, NAT GEOSCI, V9, P231, DOI 10.1038/NGEO2652; Büntgen U, 2011, SCIENCE, V331, P578, DOI 10.1126/science.1197175; Carleton TA, 2016, SCIENCE, V353, DOI 10.1126/science.aad9837; Carrión JS, 2002, QUATERNARY SCI REV, V21, P2047, DOI 10.1016/S0277-3791(02)00010-0; Chapman J, 2020, ANNU REV ANTHROPOL, V49, P123, DOI 10.1146/annurev-anthro-120219-014908; Cohen, 2003, PALEOLIMNOLOGY HIST; Collier REL, 1998, J GEOPHYS RES-SOL EA, V103, P30001, DOI 10.1029/98JB02643; Constantinidis T., 1997, THESIS U ATHENS GREE; Corella JP, 2014, QUATERNARY SCI REV, V93, P77, DOI 10.1016/j.quascirev.2014.03.020; Croudace IW, 2015, DEV PALEOENVIRON RES, V17, P1, DOI 10.1007/978-94-017-9849-5; Czymzik M, 2010, WATER RESOUR RES, V46, DOI 10.1029/2009WR008360; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Davies Siriol., 2007, Between Venice and Istanbul: Colonial Landscapes in Early Modern Greece; Degroot D, 2021, NATURE, V591, P539, DOI 10.1038/s41586-021-03190-2; Dimitrakopoulos AP, 2011, CLIMATIC CHANGE, V109, P331, DOI 10.1007/s10584-011-0026-8; Duffy OB, 2015, BASIN RES, V27, P473, DOI 10.1111/bre.12084; Emmanouilidis A, 2022, PALAEOGEOGR PALAEOCL, V595, DOI 10.1016/j.palaeo.2022.110964; Emmanouilidis A, 2020, APPL SCI-BASEL, V10, DOI 10.3390/app10228273; European U, COP LAND MON SERV 20; Faegri K., 1975, Textbook of pollen analysis.; Fick SE, 2017, INT J CLIMATOL, V37, P4302, DOI 10.1002/joc.5086; Finné M, 2011, J ARCHAEOL SCI, V38, P3153, DOI 10.1016/j.jas.2011.05.007; Galanidou N., 2020, ARCHAEOLOGY EUROPES, P371, DOI DOI 10.1007/978-3-030-37367-2_19; Gregory TimothyE., 2007, Between Venice and Istanbul: Colonial Landscapes in Early Modern Greece, P173; Haldon JohnF., 2009, The Social History of Byzantium; Heiri O, 2001, J PALEOLIMNOL, V25, P101, DOI 10.1023/A:1008119611481; Hellenic National Meteorological Service, 2016, MET DAT STAT KOR 195; Hu H., 2022, NAT COMMUN, V13, P1; Jenny JP, 2016, GLOBAL CHANGE BIOL, V22, P1481, DOI 10.1111/gcb.13193; Kaniewski D, 2013, SCI REP-UK, V3, DOI 10.1038/srep03540; Katsanevakis S., 2005, Endanger. 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J	Selina, MS; Efimova, KV; Morozova, TV; Hoppenrath, M				Selina, Marina S.; Efimova, Kseniya V.; Morozova, Tatiana V.; Hoppenrath, Mona			Morpho-molecular description of the new sand-dwelling dinoflagellate genus Aliferia gen. nov. (Dinophyceae) from the Sea of Japan, including two new species	PHYCOLOGIA			English	Article						Amphidiniopsis; Benthic; Diplopsalidoideae; Molecular phylogeny; Morphology; Peridiniales; Taxonomy	MULTIPLE SEQUENCE ALIGNMENT; CYST-THECA RELATIONSHIP; MARINE DINOFLAGELLATE; SP. NOV.; BENTHIC DINOFLAGELLATE; ELECTRON-MICROSCOPY; EMENDED DESCRIPTION; DIPLOPSALIS GROUP; COASTAL WATERS; COMB. NOV.	Two new marine sand-dwelling dinoflagellate species from subtidal sand collected in Peter the Great Bay, Sea of Japan, were described by morphological and molecular methods. Both species were slightly flattened dorsoventrally or laterally, roughly oval in shape, with small epitheca and large hypotheca, with ascending cingulum, and sulcus covered by a wide list of the first postcingular plate. The species differed in the thecal ornamentation, the number of epithecal plates, the shape of the left sulcal list and the shape of the fifth postcingular plate. Phylogenetic reconstructions based on LSU rDNA sequences of the two new species and their morphological characters confirmed their monophyly and justified the establishment of a new genus, Aliferia gen. nov., with Al. nikselinii sp. nov. and Al. kharlamenkoi sp. nov. The new genus was characterized by dorsoventrally or laterally flattened cells with small epitheca and large hypotheca, ascending cingulum, shifted or not shifted sulcus covered by a wide list on the left side, and with one or two ventral spines. Thecal tabulation: APC 3 ' 2a 6-7 '' 2 ? or 3c 5s 5 ''' 1 ''''. Distance-based analyses indicated Diplopsalidoideae as the closest phylogroup to Aliferia. Seven phylogroups of the Amphidiniopsis complex, Herdmania, the Protoperidinium complex, and Archaeperidinium (Clade ' Y ') were grouped with the highest support values, and Aliferia formed an independent branch basal to members of Clade ' Y '. The genus Aliferia showed morphological similarity to both sand-dwelling (Amphidiniopsis and Herdmania) and planktonic (Diplopsalidoideae) species. The morphology and phylogeny of Aliferia suggested complex taxonomic relationships between the planktonic and benthic genera.	[Selina, Marina S.; Efimova, Kseniya V.; Morozova, Tatiana V.] Russian Acad Sci, AV Zhirmunsky Natl Sci Ctr Marine Biol, Far Eastern Branch, Ul Palchevskogo 17, Vladivostok 690041, Russia; [Hoppenrath, Mona] German Ctr Marine Biodivers Res DZMB, Senckenberg Meer, Sudstrand 44, D-26382 Wilhelmshaven, Germany	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN)	Selina, MS (通讯作者)，Russian Acad Sci, AV Zhirmunsky Natl Sci Ctr Marine Biol, Far Eastern Branch, Ul Palchevskogo 17, Vladivostok 690041, Russia.	marinaselina2012@yandex.ru	Efimova, Kseniya/AAJ-2040-2020; Selina, Marina/AAM-6847-2021; Morozova, Tatiana/G-4468-2018		Electron microscopic examinations were carried out at the Far Eastern Center of Electron Microscopy, A.V. Zhirmunsky National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences. The authors are sincerely grateful to the st; Far Eastern Center of Electron Microscopy, A.V. Zhirmunsky National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences	Electron microscopic examinations were carried out at the Far Eastern Center of Electron Microscopy, A.V. Zhirmunsky National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences. The authors are sincerely grateful to the st; Far Eastern Center of Electron Microscopy, A.V. Zhirmunsky National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences	Electron microscopic examinations were carried out at the Far Eastern Center of Electron Microscopy, A.V. Zhirmunsky National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences. The authors are sincerely grateful to the staff of the Center for their assistance with electron microscopy. 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J	Wang, Q; Chen, XR; Lin, L; Yao, W; Wu, HX				Wang, Qiong; Chen, Xiaorong; Lin, Ling; Yao, Wei; Wu, Huixian			The dispersal of dinoflagellate cyst caused by international ships under repair conditions: a potential invasion risk to the Yangtze River Estuary, China	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Ballast water tank sediments; Harmful; toxic species; Shipyard	BALLAST TANK SEDIMENTS; SURFACE SEDIMENTS; RESTING CYSTS; BAY; ASSEMBLAGES; COAST; WATER; GERMINATION; TRANSPORT; IMPACT	The foreign dinoflagellate cysts in ships' ballast water tank sediments (BWTS) can be viable for a long time under hostile storage conditions. It is crucial to understand the detailed mechanisms of harmful biological invasions in estuary ecosystems. To study the relationship between the abundance of dinoflagellate cysts and environmental factors, cyst assemblages were analyzed in 7 sediment samples, collected from one international commercial ship that arrived in Shanghai in August 2020. Twenty-three dinoflagellate cyst taxa were identified in 5 groups, including autotrophic (9) and heterotrophic (14) species. Distribution of dinoflagellate cysts in the different ballast water tanks is heterogeneous. Dinoflagellate cysts in BWTS of the repaired ship were dominated by Scrippsiella acuminata, Protoperidinium leonis, Protoperidinium oblongum, Lingulodinium polyedra, Alexandrium tamarense/A. catenella, Protoperidinium pentagonum, and Protoperidinium subinerme. The abundance of the dinoflagellate cysts in each tank ranged from 80.69 to 330.85 cysts g(-1) DS (dry sediment). Multivariate statistical analyses revealed that the variation in cysts from different tanks had positive correlations with total nitrogen (TN), total phosphorus (TP), and pH and negative correlations with total organic carbon (TOC) except for sample TK5. For germination of dinoflagellate cysts in BWTS, 12 species were germinated in 40 days and cysts of potentially toxic dinoflagellate species were more abundant than those of non-toxic species. Results show that potentially viable and harmful/toxic dinoflagellate cysts are present in BWTS of ships arriving in Shanghai, China. Consequently, knowledge obtained in this study can be valuable for further managing of potential biological invasion of the Yangtze River Estuary.	[Wang, Qiong; Chen, Xiaorong; Lin, Ling; Wu, Huixian] Shanghai Ocean Univ, Coll Marine Ecol & Environm, Shanghai 201306, Peoples R China; [Wang, Qiong; Lin, Ling; Wu, Huixian] Shanghai Ocean Univ, Ballast Water Detecting Lab, Shanghai 201306, Peoples R China; [Wang, Qiong; Wu, Huixian] Natl Engn Res Ctr Special Equipment & Power Syst S, Shanghai 200031, Peoples R China; [Yao, Wei] Shanghai COSCO Shipping Heavy Ind Co Ltd, Shanghai 201913, Peoples R China	Shanghai Ocean University; Shanghai Ocean University	Wu, HX (通讯作者)，Shanghai Ocean Univ, Coll Marine Ecol & Environm, Shanghai 201306, Peoples R China.; Wu, HX (通讯作者)，Shanghai Ocean Univ, Ballast Water Detecting Lab, Shanghai 201306, Peoples R China.; Wu, HX (通讯作者)，Natl Engn Res Ctr Special Equipment & Power Syst S, Shanghai 200031, Peoples R China.	hxwu@shou.edu.cn	Wu, Huixian/N-6353-2014		National Key Research and Development Program of China [2022YFC2302800]	National Key Research and Development Program of China(National Key Research & Development Program of China)	We thank the anonymous reviewers for their constructive comments. This work was supported by the National Key Research and Development Program of China (No. 2022YFC2302800).	Aydin H, 2014, FRESEN ENVIRON BULL, V23, P1795; Bailey SA, 2020, DIVERS DISTRIB, V26, P1780, DOI 10.1111/ddi.13167; Balech E, 1987, DINOFLAGELADOS ATLAN, V1; BINDER BJ, 1987, J PHYCOL, V23, P99; Casas-Monroy O, 2013, AQUAT CONSERV, V23, P254, DOI 10.1002/aqc.2310; DiBacco C, 2012, ICES J MAR SCI, V69, P483, DOI 10.1093/icesjms/fsr133; Dong Y, 2021, J EXP MAR BIOL ECOL, V545, DOI 10.1016/j.jembe.2021.151627; Gao H, 2019, ACTA OCEANOL SIN, V38, P160, DOI 10.1007/s13131-019-1375-9; Gao YC, 2017, AQUAT ECOSYST HEALTH, V20, P413, DOI 10.1080/14634988.2017.1403269; Gollasch S, 2021, MAR POLLUT BULL, V164, DOI 10.1016/j.marpolbul.2021.112046; Gollasch S, 2019, MAR POLLUT BULL, V147, P8, DOI 10.1016/j.marpolbul.2018.08.054; Guillard R. R. 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Sci. Pollut. Res.	AUG	2023	30	36					86178	86188		10.1007/s11356-023-28485-x	http://dx.doi.org/10.1007/s11356-023-28485-x		JUL 2023	11	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	N9OS6	37402915				2025-03-11	WOS:001025092900006
J	El Atfy, H; Abeed, Q; Uhl, D				El Atfy, Haytham; Abeed, Qusay; Uhl, Dieter			Non-pollen palynomorph and palynofacies assemblages from the Lower Cretaceous of Iraq: A glimpse into palaeobiology and palaeoenvironment	GEODIVERSITAS			English	Article						Leiosphaeridia; Botryococcus; Palambages; dinoflagellates; Yamama Formation; Cretaceous; Iraq; non-pollen palynomorphs; microforaminiferal linings	DINOFLAGELLATE CYSTS; MICROFORAMINIFERAL LININGS; DEPOSITIONAL-ENVIRONMENTS; FRAMBOIDAL PYRITE; YAMAMA FORMATION; BASIN; SEDIMENTS; PALEOECOLOGY; CLIMATE; PALYNOSTRATIGRAPHY	The Lower Cretaceous Yamama Formation is well-known as one of the main carbonate oil reservoirs for many of the southern Iraq oilfields. However, its depositional environment has so far been poorly described using palynological techniques. Palynological assemblages from the Lower Cretaceous Yamama Formation in southern Iraq contain variable proportions of non-pollen palynomorphs (NPPs). Although this is the first record of such assemblages from the Cretaceous of Iraq, they appear very diverse and comprise microforaminiferal linings, arthropod cuticles, Botryococcus Kutzing, 1849, dinoflagellate cysts, fungal remains, Leiosphaeridia Eisenack, 1958, and Palambages Wetzel, 1961. Palynofacies analyses reveal that samples are generally dominated by AOM and most of them contain smaller quantities of translucent phytoclasts and charcoal. These records, in addition to previous studies, suggest that deposition of the studied strata of the Yamama Formation took place under anoxic conditions in the inner to outer neritic zone in a relatively near-shore setting, as shown by significant terrestrial input.	[El Atfy, Haytham] Univ Tubingen, Dept Geosci, D-72076 Tubingen, Germany; [El Atfy, Haytham] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [Abeed, Qusay] Halliburton, 97 Jubillee Ave,Milton Pk, Abingdon OX14 4RW, England; [Uhl, Dieter] Senckenberg Forschungsinst, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Uhl, Dieter] Nat Museum Frankfurt, Senckenberganlage 25, D-60325 Frankfurt, Germany	Eberhard Karls University of Tubingen; Egyptian Knowledge Bank (EKB); Mansoura University; Halliburton; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN)	El Atfy, H (通讯作者)，Univ Tubingen, Dept Geosci, D-72076 Tubingen, Germany.; El Atfy, H (通讯作者)，Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt.	el-atfy@daad-alumni.de; qusayabeed@googlemail.com; dieter.uhl@senckenberg.de	Atfy, Haytham/AAT-2276-2021		Alexander von Humboldt Foundation, Germany [EGY -1190326 - GF-P]	Alexander von Humboldt Foundation, Germany(Alexander von Humboldt Foundation)	The authors gratefully thank Tatiana Miranda (Senckenberg Tubingen) for technical assistance with SEM facilities. HE acknowledges the financial support from the Alexander von Humboldt Foundation, Germany (EGY -1190326 - GF-P). The authors wish to thank Dr Mitsuru Arai and the anonymous reviewers, as well as the Editor, Emmanuel Cotez, for their insightful comments and constructive criticism that helped to improve the manuscript. We appreciate the linguistic check carried out by Prof. Alan Lord.	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J	Wichern, NMA; de Winter, NJ; Johnson, ALA; Goolaerts, S; Wesselingh, F; Hamers, MF; Kaskes, P; Claeys, P; Ziegler, M				Wichern, Nina M. A.; de Winter, Niels J.; Johnson, Andrew L. A.; Goolaerts, Stijn; Wesselingh, Frank; Hamers, Maartje F.; Kaskes, Pim; Claeys, Philippe; Ziegler, Martin			The fossil bivalve <i>Angulus benedeni benedeni</i>: a potential seasonally resolved stable-isotope-basedclimate archive to investigate Pliocene temperatures in the southern NorthSea basin	BIOGEOSCIENCES			English	Article							DINOFLAGELLATE CYST STRATIGRAPHY; SEA BASIN; CARBONATE MINERALS; ARCTICA-ISLANDICA; MASS-SPECTROMETRY; C-13-O-18 BONDS; OXYGEN; SHELLS; GROWTH; DIAGENESIS	Bivalves record seasonal environmental changes in their shells, making them excellent climate archives. However, not every bivalve can be used for this end. The shells have to grow fast enough so that micrometre- to millimetre-sampling can resolve sub-annual changes. Here, we investigate whether the bivalve Angulus benedeni benedeni is suitable as a climate archive. For this, we use ca. 3-million-year-old specimens from the Piacenzian collected from a temporary outcrop in the Port of Antwerp area (Belgium). The subspecies is common in Pliocene North Sea basin deposits, but its lineage dates back to the late Oligocene and has therefore great potential as a high-resolution archive. A detailed assessment of the preservation of the shell material by micro-X-ray fluorescence, X-ray diffraction, and electron backscatter diffraction reveals that it is pristine and not affected by diagenetic processes. Oxygen isotope analysis and microscopy indicate that the species had a longevity of up to a decade or more and, importantly, that it grew fast and large enough so that seasonally resolved records across multiple years were obtainable from it. Clumped isotope analysis revealed a mean annual temperature of 13.5 +/- 3.8 degrees C. The subspecies likely experienced slower growth during winter and thus may not have recorded temperatures year-round. This reconstructed mean annual temperature is 3.5 degrees C warmer than the pre-industrial North Sea and in line with proxy and modelling data for this stratigraphic interval, further solidifying A. benedeni benedeni's use as a climate recorder. Our exploratory study thus reveals that Angulus benedeni benedeni fossils are indeed excellent climate archives, holding the potential to provide insight into the seasonality of several major climate events of the past similar to 25 million years in northwestern Europe.	[Wichern, Nina M. A.] Westfalische Wilhelms Univ, Inst Geol & Paleontol, D-48149 Munster, Germany; [de Winter, Niels J.] Vrije Univ, Fac Sci, Dept Earth Sci, NL-1081 HV Amsterdam, Netherlands; [de Winter, Niels J.; Wesselingh, Frank; Hamers, Maartje F.; Ziegler, Martin] Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands; [de Winter, Niels J.; Kaskes, Pim; Claeys, Philippe] Vrije Univ, Analyt Environm & Geochem, B-1050 Brussels, Belgium; [Johnson, Andrew L. A.] Univ Derby, Sch Built & Nat Environm, Derby DE22 1GB, England; [Goolaerts, Stijn] Royal Belgian Inst Nat Sci, Earth & Hist Life & Sci Serv Heritage, B-1000 Brussels, Belgium; [Wesselingh, Frank] Nat Biodivers Ctr, NL-2333 CR Leiden, Netherlands	University of Munster; Vrije Universiteit Amsterdam; Utrecht University; Vrije Universiteit Brussel; University of Derby; Royal Belgian Institute of Natural Sciences; Naturalis Biodiversity Center	Wichern, NMA (通讯作者)，Westfalische Wilhelms Univ, Inst Geol & Paleontol, D-48149 Munster, Germany.	nwichern@uni-muenster.de	Ziegler, Martin/N-9699-2013; Kaskes, Pim/LUA-0857-2024; Claeys, Philippe/B-4895-2008; Johnson, Andrew/ABC-1334-2021	Wichern, Nina/0000-0001-5872-8086; Kaskes, Pim/0000-0002-2605-6366; Hamers, Maartje/0000-0002-4236-0296; Claeys, Philippe/0000-0002-4585-7687; Ziegler, Martin/0000-0003-3198-6434; Johnson, Andrew/0000-0001-5727-1889; de Winter, Niels/0000-0002-1453-5407	Research Foundation Flanders (FWO) PhD Fellowship [11E6621N, RPG-2021-090]; Leverhulme Trust - Flemish Research Foundation (FWO) [12ZB220N]	Research Foundation Flanders (FWO) PhD Fellowship(FWO); Leverhulme Trust - Flemish Research Foundation (FWO)	The authors gratefully acknowledge the following people for their help with this work: Leonard Bik (Utrecht University) made the polished thin sections for microscopy and EBSD work. Desmond & nbsp;Eefting and Arnold & nbsp;van & nbsp;Dijk (Utrecht University) provided technical assistance during isotope analyses. Lucas & nbsp;Lourens (Utrecht University) proofread the original version of this manuscript. Maarten Zeylmans (Utrecht University) helped produce high-resolution scans of cross sections of the specimens. Pim & nbsp;Kaskes is supported by a Research Foundation Flanders (FWO) PhD Fellowship (11E6621N). Stijn Goolaerts is grateful to Ir Murielle Reyns, Roger Sieckelink, and Nouredine Ouifak of "Mobiliteit en Openbare Werken (MOW)" for granting access to the Deurganckdoksluis construction site (2012-2014) allowing the collection of the study material. Andrew L. A. Johnson was funded by award RPG-2021-090 from the Leverhulme Trust. This work is part of the UNBIAS project funded by a Flemish Research Foundation (FWO; 12ZB220N) post-doctoral fellowship (Niels & nbsp;J.& nbsp;de & nbsp;Winter). The manuscript was greatly improved by the insightful comments of two anonymous reviewers, as well as Paul Butler.	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J	Willard, DA; Ruppert, LF				Willard, Debra A.; Ruppert, Leslie F.			Broadening the perspectives of sedimentary organic matter analysis to understand Earth system response to change	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Palynology; Sedimentary organic matter; Pollen; Spores; Dinocysts; Paleoclimate; Fire history; Forensics; Water quality	WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; MICROFORAMINIFERAL LININGS; CHARCOAL ACCUMULATION; ENVIRONMENTAL-CHANGES; MICROSCOPIC CHARCOAL; BRITISH-COLUMBIA; FOREST MORTALITY; GREAT-BASIN; BALTIC SEA	This paper broadens the description of sedimentary organic matter from the conventional use of coal petrography to include palynological and geochemical sedimentary organic matter. Palynological sedimentary organic matter includes all chemically resistant organic microfossils, such as pollen and spores, dinocysts, microforaminifera (chitinoid-like linings of foraminifera), microscopic algae, charcoal, palynodebris, acritarchs, chitinozoans, and scolecodonts. Geochemical sedimentary organic matter includes organic biomarkers, lipids, and photosynthetic pigments. We provide examples of the use of palynological and geochemical analysis of sedimentary organic matter to understand patterns and impacts of changing climate, fire regimes, hydrologic extremes, water quality, and land change on terrestrial and marine systems through geologic time to provide a long-term perspective to evaluate anthropogenic impacts on the Earth as well as to support forensics investigations.	[Willard, Debra A.] Florence Bascom Geosci Ctr, US Geol Survey, Reston, VA USA; [Ruppert, Leslie F.] US Geol Survey Energy & Minerals Sci Ctr, Reston, VA USA; [Willard, Debra A.] US Geol Survey, 12201 Sunrise Valley Dr,MS 926A, Reston, VA 20192 USA	United States Department of the Interior; United States Geological Survey; United States Department of the Interior; United States Geological Survey	Willard, DA (通讯作者)，US Geol Survey, 12201 Sunrise Valley Dr,MS 926A, Reston, VA 20192 USA.	dwillard@usgs.gov			U.S. Geological Survey Land Change Science and Energy Resources Programs	U.S. Geological Survey Land Change Science and Energy Resources Programs	Thomas M. Cronin, G. Lynn Wingard, Cortland F. Eble, and an anonymous reviewer provided thoughtful review and comments of this manuscript. We gratefully acknowledge Natalie Kehrwald, Matthew Waters, and Palma Botterell for sharing their expertise on organic bio- markers and their use to interpret the history of fire and harmful algal blooms and their utility in petroleum systems. We thank Tim Moore and the Organizing Committee of the 2022 The Society for Organic Petrology Annual Meeting for inviting the first author to give a keynote talk on the topic. The research was supported by the U.S. Geological Survey Land Change Science and Energy Resources Programs.	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J. Coal Geol.	JUN 1	2023	274								104281	10.1016/j.coal.2023.104281	http://dx.doi.org/10.1016/j.coal.2023.104281		JUN 2023	18	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	U9UN3					2025-03-11	WOS:001088185500001
J	Pérez-Cano, J; Pereira, HJR; Mendes, M; Pereira, Z; Callapez, PM; Fernandes, P				Perez-Cano, Jordi; Pereira, Helder J. R.; Mendes, Marcia; Pereira, Zelia; Callapez, Pedro Miguel; Fernandes, Paulo			Upper Barremian-lower Aptian charophyte biostratigraphy from Arrifes section (Algarve Basin, Southern Portugal): correlation with dinoflagellate cyst biostratigraphy	CRETACEOUS RESEARCH			English	Article						Charophyta; Iberia; Cretaceous; Clavatoraceae; Continental-marine biochronology; Palynology	CRETACEOUS CHAROPHYTES; CLAVATORACEAE; DEPOSITS; STRATIGRAPHY; BIOGEOGRAPHY; EVOLUTION; WESTERN; FRANCE	The Arrifes section (Algarve Basin, Southern Portugal) has been studied from the viewpoint of char-ophyte biostratigraphy. The previous sedimentological studies in this section showed that it is built of the interbedding of continental and marine facies that contain both marine and continental palynomorphs (pollen, spores, and dinoflagellates), providing an excellent sedimentary context to perform direct cor-relations between marine and continental domains. In the present work, the identified charophyte biozones have been correlated with dinoflagellate biozones previously recognized in the Arrifes section, being the first time that these two biochronologies can be directly correlated. From the charophyte biostratigraphy viewpoint, two assemblages are distinguished. The older one is found between 65 and 135 m of the stratigraphic section, and it is composed of the species Echinochara lazarii, Atopochara trivolvis var. triquetra, A. trivolvis var. trivolvis, Clavator grovesii var. jiuquanensis, Clavator harrisii var. harrisii, C. harrisii var. reyi, and C. harrisii var. zavialensis. This assemblage belongs to the upper Barremian -lower Aptian Clavator grovesii var. jiuquanensis Eurasian biozone and also to the Ascidiella cruciata-Pseudoglobator paucibracteatus European biozone and it is described in beds with the dinoflagellate cyst Subtilisphaera scabrata (lower to lowermost upper Barremian) and Odontochitina operculata (from upper Barremian upwards). The younger charophyte assemblage is found between 135 and 155 m of the stratigraphic section, and it is composed of the species A. trivolvis var. trivolvis, Clavator grovesii var. corrugatus, Clavator harrisii var. harrisii, C. harrisii var. reyi, and C. harrisii var. zavialensis. This assemblage belongs to Clavator grovesii var. corrugatus biozone, previously assigned to upper Aptian (Clavator grovesii var. lusitanicus biozone). However, in the Arrifes section, this assemblage is found in beds assigned to the dinoflagellate cyst Odontochitina operculata (from upper Barremian-lower Aptian). The direct correlation of the base of the C. grovesii var. corrugatus biozone with the dinoflagellate cyst O. operculata, indicates that the base of the Clavator grovesii var. corrugatus biozone is in the upper lower Aptian, which is slightly older than was previously suggested, and it is extended until the middle Albian. & COPY; 2023 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).	[Perez-Cano, Jordi] Univ Autonoma Barcelona, Inst Catala Paleontol Miquel Crusafont, ICTA-ICP Bldg,C Columnes S-N,Campus UAB, E-08193 Cerdanyola Del Valles, Catalonia, Spain; [Perez-Cano, Jordi] Univ Barcelona UB, Dept Dinam Terra & Ocea, Fac Ciencies Terra, Barcelona 08028, Catalonia, Spain; [Perez-Cano, Jordi] Univ Barcelona UB, Inst Recerca Biodiversitat IRBio, Barcelona, Catalonia, Spain; [Perez-Cano, Jordi] Univ Barcelona UB, Dept Mineral Petrol & Geol Aplicada, Fac Ciencies Terra, Barcelona 08028, Catalonia, Spain; [Pereira, Helder J. R.; Callapez, Pedro Miguel] Univ Coimbra Polo II, Univ Coimbra, Fac Sci & Technol, Ctr Earth & Space Res,Earth Sciences Dept, Rua Silvio Lima, P-3030790 Coimbra, Portugal; [Pereira, Helder J. R.; Fernandes, Paulo] Univ Algarve, Ctr Marine & Environm Res, ARNET Infrastruct Network Aquat Res, Campus Gambelas, P-8000139 Faro, Portugal; [Pereira, Zelia] Natl Lab Energy & Geol, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Callapez, Pedro Miguel] Univ Alcala, Dept Geol & Geog, Grp Invest PaleoIber, Alcala De Henares 28871, Spain	Institut Catala de Paleontologia Miquel Crusafont (ICP); Autonomous University of Barcelona; University of Barcelona; University of Barcelona; University of Barcelona; Universidade de Coimbra; Universidade do Algarve; Universidad de Alcala	Pérez-Cano, J (通讯作者)，Univ Autonoma Barcelona, Inst Catala Paleontol Miquel Crusafont, ICTA-ICP Bldg,C Columnes S-N,Campus UAB, E-08193 Cerdanyola Del Valles, Catalonia, Spain.	jordi.perez@icp.cat	Perez Cano, Jordi/AAL-8771-2021; Callapez Tonicher, Pedro Miguel/L-7089-2014; Pereira, Zelia/B-2740-2017; Mendes, Marcia/E-2897-2019; Fernandes, Paulo/J-6577-2014	Callapez Tonicher, Pedro Miguel/0000-0002-6493-2208; Pereira, Helder/0000-0001-7664-7650; Pereira, Zelia/0000-0003-3056-6219; Perez Cano, Jordi/0000-0002-1782-5346; Mendes, Marcia/0000-0003-2290-891X; Fernandes, Paulo/0000-0003-4888-0230	MCIN/AEI [PID2020-113912GB-100]; European Regional Development Fund (ERDF); Fundacao para a Ciencia e Tecnologia (FCT) [UIDB/00611/2020, UIDP/00611/2020, LA/P/0069/2020, UID/00350/2020]; Ministerio de Universidades of Spain; Spanish Government; European Union	MCIN/AEI; European Regional Development Fund (ERDF)(European Union (EU)); Fundacao para a Ciencia e Tecnologia (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); Ministerio de Universidades of Spain; Spanish Government(Spanish Government); European Union(European Union (EU))	This study was partially funded by and is a contribution to the project IBERINSULA (PID2020-113912GB-100), funded by MCIN/AEI/10.13039/501100011033 and the European Regional Development Fund (ERDF). This study also had the financial support Fundacao para a Ciencia e Tecnologia (FCT), under the projects UIDB/00611/2020 and UIDP/00611/2020 CITEUC and LA/P/0069/2020 granted to the Associate Laboratory ARNET and UID/00350/2020 CIMA. JP-C Margarita Salas postdoctoral contract and research is supported by the Ministerio de Universidades of Spain, "Plan de recuperacion, transformacion y resiliencia" of Spanish Government and the Next Generation founds from the European Union. Dr. Alejandro Gallardo (technician of the Palaeontological Laboratory of the Departament de Dinamica de la Terra i de l'Ocea) is acknowledged for his assistance in preparing the samples studied here. The manuscript has been highly improved during the peer-review after the detailed revisions and suggestions of the editor, Dr. Eduardo Koutsoukos, and the reviewers, Dr. Carles Martin-Closas (University of Barcelona), Dr. Alba Vicente (Instituto Politecnico Nacional, La Paz, Mexico), and Dr. Khaled Trabelsi (University of Vienna). Dr. Carles Martin-Closas is also acknowledged for the productive discussions in the early stages of this work.	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OCT	2023	150								105575	10.1016/j.cretres.2023.105575	http://dx.doi.org/10.1016/j.cretres.2023.105575		JUN 2023	15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	L3OG9		Green Published, hybrid			2025-03-11	WOS:001022381200001
J	Uddandam, PR; Kapur, VV; Parmar, S; Bansal, M; Manoj, MC; Sharma, A; Prasad, V				Uddandam, Prem Raj; Kapur, Vivesh V.; Parmar, Shalini; Bansal, Mahi; Manoj, M. C.; Sharma, Anupam; Prasad, Vandana			Danian-Ypresian dinocyst biostratigraphy, fish fauna and depositional environment of the Akli Formation, Barmer Basin, western India	HISTORICAL BIOLOGY			English	Article						Apectodinium; Danian; palaeoenvironment; Gnathostomata; Sonari Lignite Mine; Ypresian	PALEOCENE-EARLIEST EOCENE; GIRAL LIGNITE MINE; DINOFLAGELLATE CYSTS; APECTODINIUM ACME; THERMAL MAXIMUM; SEA-LEVEL; EL-KEF; RAJASTHAN; TRANSITION; DISTRICT	Herein, we present a diverse record of dinoflagellate cysts from the lignite-associated sedimentary succession (belonging to the Akli Formation) at Sonari Lignite Mine, Barmer Basin, Rajasthan State, western India. The dinoflagellate cyst assemblage implies a Danian to Ypresian age for the investigated succession and argues that the deposition of lignitic sequences along India's western margin is not coeval. We also identify two vertebrate (dominantly fish-yielding) units within the studied Akli Formation succession. The Ypresian fish genera (mainly represented by dental remains) include Ginglymostoma, Jaekelotodus, Brachycarcharias, Pycnodus and Myliobatis while the Selandian-Thanetian fish dental remains include Dasyatis. A discontinuous distribution of fish fauna during the early Paleogene (based on the temporal and spatial data) within the lignite-associated sedimentary successions of western and north India allows us to infer the prevalence of separated realms with variably restricted palaeoenvironmental conditions. Overall, the faunal evidence is indicative of dominantly estuarine to shallow marine conditions with enhanced freshwater influence during the Thanetian as compared to the Danian. Our study also argues in favour of the earliest appearance of dinoflagellate cyst Apectodinium in the near-equatorial region of the Tethys Ocean during the early Paleocene. (within Danian).	[Uddandam, Prem Raj; Kapur, Vivesh V.; Parmar, Shalini; Bansal, Mahi; Manoj, M. C.; Sharma, Anupam; Prasad, Vandana] Birbal Sahni Inst Palaeosci, 53, Univ Rd, Lucknow, India; [Kapur, Vivesh V.] Birbal Sahni Inst Palaeosci, 53, Univ Rd, Lucknow 226007, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Kapur, VV (通讯作者)，Birbal Sahni Inst Palaeosci, 53, Univ Rd, Lucknow 226007, India.	viveshkapur@gmail.com	Kapur, Vivesh/AAO-4885-2021; Manoj, M/AAR-1882-2020; Kapur, Vivesh V/AAR-9262-2021	Kapur, Vivesh V/0000-0001-6542-5964	Department of Science and Technology (DST), New Delhi [3]	Department of Science and Technology (DST), New Delhi(Department of Science & Technology (India))	This work was supported by the Department of Science and Technology (DST), New Delhi in the form of a Birbal Sahni Institute of Palaeosciences In-House Project Grant No. 3: 2021-2025 [No. 3: 2021-2025].	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JUL 2	2024	36	7					1401	1414		10.1080/08912963.2023.2214585	http://dx.doi.org/10.1080/08912963.2023.2214585		JUN 2023	14	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	WT6G1					2025-03-11	WOS:001004958200001
J	Nguyen, NL; Devendra, D; Szymanska, N; Greco, M; Angeles, IB; Weiner, AKM; Ray, JL; Cordier, T; De Schepper, S; Pawlowski, J; Pawlowska, J				Nguyen, Ngoc-Loi; Devendra, Dhanushka; Szymanska, Natalia; Greco, Mattia; Angeles, Ines Barrenechea; Weiner, Agnes K. M.; Ray, Jessica Louise; Cordier, Tristan; De Schepper, Stijn; Pawlowski, Jan; Pawlowska, Joanna			Sedimentary ancient DNA: a new paleogenomic tool for reconstructing the history of marine ecosystems	FRONTIERS IN MARINE SCIENCE			English	Review						paleoceanography; sedaDNA; marine sediment; metabarcoding; metagenomics; marine biodiversity	PLANKTON COMMUNITY STRUCTURE; EXTRACELLULAR DNA; SINKING VELOCITY; DINOFLAGELLATE CYSTS; DEGRADATION RATES; SULFUR BACTERIA; NUCLEIC-ACIDS; PLEISTOCENE; OCEAN; PRESERVATION	Sedimentary ancient DNA (sedaDNA) offers a novel retrospective approach to reconstructing the history of marine ecosystems over geological timescales. Until now, the biological proxies used to reconstruct paleoceanographic and paleoecological conditions were limited to organisms whose remains are preserved in the fossil record. The development of ancient DNA analysis techniques substantially expands the range of studied taxa, providing a holistic overview of past biodiversity. Future development of marine sedaDNA research is expected to dramatically improve our understanding of how the marine biota responded to changing environmental conditions. However, as an emerging approach, marine sedaDNA holds many challenges, and its ability to recover reliable past biodiversity information needs to be carefully assessed. This review aims to highlight current advances in marine sedaDNA research and to discuss potential methodological pitfalls and limitations.	[Nguyen, Ngoc-Loi; Devendra, Dhanushka; Szymanska, Natalia; Greco, Mattia; Pawlowski, Jan; Pawlowska, Joanna] Polish Acad Sci, Dept Paleoceanog, Inst Oceanol, Sopot, Poland; [Angeles, Ines Barrenechea] Univ Tromso UiT Arctic Univ Norway, Dept Geosci, Tromso, Norway; [Weiner, Agnes K. M.; Ray, Jessica Louise; Cordier, Tristan; De Schepper, Stijn] NORCE Norwegian Res Ctr, NORCE Climate & Environm, Bergen, Norway; [Weiner, Agnes K. M.; Ray, Jessica Louise; Cordier, Tristan; De Schepper, Stijn] Bjerknes Ctr Climate Res, Bergen, Norway	Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences; UiT The Arctic University of Tromso; Norwegian Research Centre (NORCE); Bjerknes Centre for Climate Research	Nguyen, NL; Pawlowska, J (通讯作者)，Polish Acad Sci, Dept Paleoceanog, Inst Oceanol, Sopot, Poland.	loinguyen@iopan.pl; pawlowska@iopan.pl	Devendra, Dhanushka/AAZ-5385-2020; Pawlowski, Jan/JNS-6857-2023; Barrenechea Angeles, Ines/JAO-3559-2023; Pawłowska, Joanna/O-8616-2015; Cordier, Tristan/B-7836-2018; De Schepper, Stijn/A-2836-2011; Nguyen, Ngoc-Loi/AAG-6356-2019; Ray, Jessica Louise/D-2210-2018; Greco, Mattia/HOF-9207-2023	Cordier, Tristan/0000-0001-7398-4790; Ray, Jessica Louise/0000-0002-7305-5737; Pawlowska, Joanna/0000-0001-9383-9785; Devendra, Dhanushka/0000-0003-1005-1621; Greco, Mattia/0000-0003-2416-6235; Barrenechea Angeles, Ines/0000-0002-8051-4110; Nguyen, Ngoc-Loi/0000-0001-9452-4830	Norwegian Financial Mechanism [2019/34/H/ST10/00682]; Norwegian Petroleum Directorate [287869]	Norwegian Financial Mechanism; Norwegian Petroleum Directorate	Funding The research leading to these results has been funded by Norwegian Financial Mechanism for 2014-2021, project no. 2019/34/H/ST10/00682 in the frame of project "Sedimentary ancient DNA - a new proxy to investigate the impact of environmental change on past and present biodiversity in Nordic Seas". IBA was supported by the Norwegian Petroleum Directorate and the project AKMA, project no. 287869.	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Mar. Sci.	JUN 9	2023	10								1185435	10.3389/fmars.2023.1185435	http://dx.doi.org/10.3389/fmars.2023.1185435			12	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	J9ZL4		Green Published, gold			2025-03-11	WOS:001013133800001
J	Hassan, S; Tahoun, SS; Darwish, M; Bosworth, W; Radwan, AE				Hassan, Sahar; Tahoun, Sameh S.; Darwish, Mohamed; Bosworth, William; Radwan, Ahmed E.			The Albian-Cenomanian boundary on the southern Tethyan margin: Abu Gharadig Basin, Northern Western Desert, Egypt	MARINE AND PETROLEUM GEOLOGY			English	Article						Borehole image log (BHI); Electrofacies; Chrono-lithostratigraphy; Depositional sequences; Southern Tethys margin; Albian-Cenomanian boundary; Abu Gharadig basin	SEQUENCE STRATIGRAPHY; BOREHOLE IMAGE; DEPOSITIONAL FACIES; BAHARIYA FORMATION; SOURCE ROCKS; PALYNOLOGY; AFRICA; INVERSION; WELL; EVOLUTION	Lithostratigraphy and biostratigraphy sometimes provide contradictory interpretations, especially when trying to establish a chrono-lithological boundary between two reservoir formations from different paleoenvironments. One of these contradictions is the definition of the boundary between the Kharita and Bahariya formations and the Albian and Cenomanian Stages in the Abu Gharadig Basin of the Western Desert, Egypt. an integrated approach has been applied to this problem using borehole image logs, palynology, and conventional wireline logs. authors also calibrate the stratigraphic sections with global chronostratigraphic charts, using nannoplankton, planktonic foraminifera, and dinoflagellates to construct a better understanding of this basin. The abundances of pollen, spores, and dinoflagellates in the interpreted reservoir intervals suggest that hydrocarbons trapped in the Albian-Cenomanian reservoirs are composed of type II/III kerogen. The interpreted intervals are subdivided into seven depositional cycles: one in the Kharita Formation, five in the Bahariya Formation, and one in the Abu Roash Formation. The interpreted environments are, from bottom to top: I) fluvio-deltaic distributary channels, II) and III) intertidal to subtidal deposits, IV) offshore bar deposits, V) intertidal to subtidal deposits, VI) shoreface deposits, and VII) shallow marine carbonate deposits. Diagnostic palynomorphs reflect climatic change from arid to humid conditions and also enable changes in salinity to be determined.Much of the published work in the southern Tethyan margin, particularly in the Western Desert, is either related to stratigraphy, palynology, or reservoir evaluation with a focus on a narrow field. Tectonostratigraphic studies and analyses of petroleum system elements have often been very regional in nature. The work presented here is of an intermediate scale linking regional frameworks with local details to provide comprehensive information about the Albian-Cenomanian succession in the Northern Western Desert. The focus has been the Abu Gharadig basin but this integrated approach has implications for other basins in North Africa. A specific example is the similarity of Western Desert and Libyan Sirt basin Albian-Cenomanian key palynomorphs which would facilitate a similar integrated chrono-lithologic intepretation.	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Pet. Geol.	AUG	2023	154								106334	10.1016/j.marpetgeo.2023.106334	http://dx.doi.org/10.1016/j.marpetgeo.2023.106334		JUN 2023	22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	J9KN7					2025-03-11	WOS:001012743300001
J	Li, Z; Pospelova, V; Mertens, KN; Liu, LJ; Wu, YS; Li, C; Gu, HF				Li, Zhen; Pospelova, Vera; Mertens, Kenneth Neil; Liu, Lejun; Wu, Yongsheng; Li, Chao; Gu, Haifeng			Evaluation of organic-walled dinoflagellate cyst distributions in coastal surface sediments of the China Seas in relation with hydrographic conditions for paleoceanographic reconstruction	QUATERNARY INTERNATIONAL			English	Article						Marine palynology; Dinoflagellate cysts; Surface sediments; Hydrographic conditions; Paleoceanographic reconstruction; China Seas	NORTHERN NORTH-ATLANTIC; RECENT MARINE-SEDIMENTS; SPATIAL-DISTRIBUTION; YELLOW SEA; BRITISH-COLUMBIA; ALEXANDRIUM-FUNDYENSE; PRIMARY PRODUCTIVITY; ESTUARINE SEDIMENTS; RESTING CYSTS; DAYA BAY	Dinoflagellate cysts are commonly used to reconstruct past climatic, oceanographic and environmental conditions. Such applications are based on the relationship between modern dinoflagellate cysts and environmental parameters. To evaluate cyst diversity and driving factors of their distributions in sediments of the China Seas for paleoenvironmental reconstruction, dinoflagellate cysts were analyzed in 18 surface sediment samples from the Bohai Sea, the Yellow Sea (YS), the East China Sea and the South China Sea (SCS). A total of 59 dinoflagellate cyst taxa were identified with the greatest diversity reported in the SCS. The highest cyst concentrations were found in the YS, where Spiniferites ramosus, Spiniferites spp., and cysts of Pentapharsodinium spp. were predominant in the assemblages. The Yellow Sea Warm Current is likely creating the environment favoring the high numbers of Spiniferites ramosus in the YS. The highest Brigantedinium spp. abundances were observed near the Pearl River mouth and are positively correlated with sea-surface temperature (SST) in August. Spiniferites hyperacanthus, S. mirabilis, S. pacificus, and Lingulodinium spp. were most abundant in the SCS. In contrast, cysts of Protoperidinium spp. and Selenopemphix quanta were more common at the sites directly influenced by coastal upwelling rather than by river discharges. Redundancy Analysis results show that SST, sea-surface salinity (SSS) and nitrate concentration in water are statistically significant parameters influencing the cyst assemblages. We also examined the morphological characteristics of Spiniferites ramosus and recommend grouping S. bulloideus with S. ramosus in the northwest Pacific dataset for quantitatively reconstructing paleoceanographic conditions.	[Li, Zhen] Geol Survey Canada Pacific, Nat Resources Canada, 9860 W Saanich Rd, Sidney, BC V8L 4B2, Canada; [Li, Zhen; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, POB 1700 STN CSC, Victoria, BC V8W 2Y2, Canada; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, 116 Church St SE, Minneapolis, MN 55455 USA; [Mertens, Kenneth Neil] Ifremer, LITTORAL, F-29900 Concarneau, France; [Liu, Lejun] Minist Nat Resources China, Inst Oceanog 1, 6 Xianxialing Rd, Qingdao 266061, Shandong, Peoples R China; [Wu, Yongsheng] Fisheries & Oceans Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [Li, Chao] Xiamen Univ, Coll Ocean & Earth Sci, 422 Siming South Rd, Xiamen 361102, Fujian, Peoples R China; [Gu, Haifeng] Third Inst Oceanog, Minist Nat Resources, Xiamen 361005, Fujian, Peoples R China	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Victoria; University of Minnesota System; University of Minnesota Twin Cities; Ifremer; First Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China; Bedford Institute of Oceanography; Fisheries & Oceans Canada; Xiamen University; Third Institute of Oceanography, Ministry of Natural Resources; Ministry of Natural Resources of the People's Republic of China	Li, Z (通讯作者)，Geol Survey Canada Pacific, Nat Resources Canada, 9860 W Saanich Rd, Sidney, BC V8L 4B2, Canada.	Zhen.Li2@nrcan-rncan.gc.ca	Li, Zhen/G-7667-2012; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Gu, Haifeng/ADN-4528-2022	Li, Zhen/0000-0003-3989-7233; Mertens, Kenneth/0000-0003-2005-9483; Pospelova, Vera/0000-0003-4049-8133; Gu, Haifeng/0000-0002-2350-9171	Natural Sciences and Engineering Research Council of Canada (NSERC); National Program on Global Change and Air-Sea Interaction, NMR [GASI-GEOGE-05]; National Key R & D Program of China [2016YFB0501703]; NSERC CGS D3 Fellowship [CGSD3-475098-2015]; NSERC; Regional Council of Brittany; General Council of Finistere; urban community of Concarneau-Cornouaille-Agglomeration;  [PDF5161862018]	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); National Program on Global Change and Air-Sea Interaction, NMR; National Key R & D Program of China; NSERC CGS D3 Fellowship; NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Regional Council of Brittany(Region Bretagne); General Council of Finistere(Region Bretagne); urban community of Concarneau-Cornouaille-Agglomeration; 	This work was partially funded by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a Discovery grant to V. Pospelova. L. Liu was partially supported by the National Program on Global Change and Air-Sea Interaction, NMR (No. GASI-GEOGE-05) and National Key R & D Program of China (2016YFB0501703) in this work. NSERC CGS D3 Fellowship (CGSD3-475098-2015), NSERC for CGS-MSFSS and NSERC Postdoctoral Fellowship (PDF-516186-2018) provided funding for this research to Z. Li. 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. We also thank to Copernicus Programme of the European Union for providing the data of environmental parameters.	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Int.	JUL 10	2023	661						60	75		10.1016/j.quaint.2023.03.007	http://dx.doi.org/10.1016/j.quaint.2023.03.007		JUN 2023	16	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	J6WV0					2025-03-11	WOS:001011011800001
J	Thöle, LM; Nooteboom, PD; Hou, SN; Wang, RJ; Nie, SY; Michel, E; Sauermilch, I; Marret, F; Sangiorgi, F; Bijl, PK				Thole, Lena Mareike; Nooteboom, Peter Dirk; Hou, Suning; Wang, Rujian; Nie, Senyan; Michel, Elisabeth; Sauermilch, Isabel; Marret, Fabienne; Sangiorgi, Francesca; Bijl, Peter Kristian			An expanded database of Southern Hemisphere surface sediment dinoflagellatecyst assemblages and their oceanographic affinities	JOURNAL OF MICROPALAEONTOLOGY			English	Article							OFFSHORE WILKES LAND; ANTARCTIC ICE-SHEET; SOUTHWEST PACIFIC; SEA; CYSTS; RECONSTRUCTION; FRAMEWORK; HOLOCENE	Dinoflagellate cyst assemblages present a valuable proxy to infer paleoceanographic conditions, yet factors influencing geographic distributions of species remain largely unknown, especially in the Southern Ocean. Strong lateral transport, sea-ice dynamics, and a sparse and uneven geographic distribution of surface sediment samples have limited the use of dinocyst assemblages as a quantitative proxy for paleo-environmental conditions such as sea surface temperature (SST), nutrient concentrations, salinity, and sea ice (presence). In this study we present a new set of surface sediment samples (n=66) from around Antarctica, doubling the number of Antarctic-proximal samples to 100 (dataset wsi_100) and increasing the total number of Southern Hemisphere samples to 655 (dataset sh_655). Additionally, we use modelled ocean conditions and apply Lagrangian techniques to all Southern Hemisphere sample stations to quantify and evaluate the influence of lateral transport on the sinking trajectory of microplankton and, with that, to the inferred ocean conditions. k-means cluster analysis on the wsi_100 dataset demonstrates the strong affinity of Selenopemphix antarctica with sea-ice presence and of Islandinium spp. with low-salinity conditions. For the entire Southern Hemisphere, the k-means cluster analysis identifies nine clusters with a characteristic assemblage. In most clusters a single dinocyst species dominates the assemblage. These clusters correspond to well-defined oceanic conditions in specific Southern Ocean zones or along the ocean fronts. We find that, when lateral transport is predominantly zonal, the environmental parameters inferred from the sea floor assemblages mostly correspond to those of the overlying ocean surface. In this case, the transport factor can thus be neglected and will not represent a bias in the reconstructions. Yet, for some individual sites, e.g. deep-water sites or sites under strong-current regimes, lateral transport can play a large role. The results of our study further constrain environmental conditions represented by dinocyst assemblages and the location of Southern Ocean frontal systems.	[Thole, Lena Mareike; Hou, Suning; Sauermilch, Isabel; Sangiorgi, Francesca; Bijl, Peter Kristian] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Nooteboom, Peter Dirk] Univ Utrecht, Inst Marine & Atmospher Res Utrecht IMAU, Dept Phys, Utrecht, Netherlands; [Nooteboom, Peter Dirk] Univ Utrecht, Ctr Complex Syst Studies, Utrecht, Netherlands; [Wang, Rujian; Nie, Senyan] Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China; [Michel, Elisabeth] Univ Paris Saclay, Lab Sci Climat & Environm, LSCE IPSL, Gif sur Yvette, France; [Marret, Fabienne] Univ Liverpool, Sch Environm, Dept Geog & Planning, Liverpool, England	Utrecht University; Utrecht University; Utrecht University; Tongji University; Universite Paris Saclay; University of Liverpool	Bijl, PK (通讯作者)，Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/B-4223-2009	Bijl, Peter/0000-0002-1710-4012; Marret-Davies, Fabienne/0000-0003-4244-0437; Sangiorgi, Francesca/0000-0003-4233-6154; Thole, Lena/0000-0002-5405-3613; Hou, Suning/0000-0002-8902-6367	European Research Council (ERC) [802835]	European Research Council (ERC)(European Research Council (ERC))	This research has been supported by the seventh framework programme of the European Research Council (ERC Starting grant no. 802835, OceaNice to Peter Kristian Bijl).	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J	Wierzbowski, A; Barski, M; Coe, AL; Hounslow, MW; Matyja, BA; Price, GD; Wierzbowski, H; Wright, JK; Grabowski, J; Mattioli, E; Morton, N; Ogg, JG; Oloriz, F; Page, K; Parent, H; Przybylski, P; Schweigert, G; Villaseñor, AB				Wierzbowski, Andrzej; Barski, Marcin; Coe, Angela L.; Hounslow, Mark W.; Matyja, Bronislaw A.; Price, Gregory D.; Wierzbowski, Hubert; Wright, John K.; Grabowski, Jacek; Mattioli, Emanuela; Morton, Nicol; Ogg, James G.; Oloriz, Federico; Page, Kevin; Parent, Horacio; Przybylski, Piotr; Schweigert, Guenter; Villasenor, Anna Bertha		Contributions Francois Atrops	The Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System), at Flodigarry, Staffin Bay, Isle of Skye, Scotland, UK	EPISODES			English	Article							OXFORDIAN/KIMMERIDGIAN BOUNDARY BEDS; AMMONITE SUCCESSION; NEUQUEN BASIN; TIME-SCALE; ISOTOPE; MAGNETOSTRATIGRAPHY; BIOSTRATIGRAPHY; STRATIGRAPHY; CARBON; CYCLOSTRATIGRAPHY	Following voting by the Kimmeridgian Working Group, the International Subcommission on Jurassic Stratigraphy and the International Commission on Stratigraphy, the Global Stratotype Section and Point (GSSP) for the base of the Kimmeridgian Stage (Jurassic System) was ratified by the executive of the International Union of Geological Sciences. The boundary is placed in the upper part of Bed 35 of the Staffin Shale Formation, 1.25 +/- 0.01 m below the base of Bed 36 in block F6 in the foreshore at Flodigarry, Staffin Bay, Isle of Skye, Scotland. The coordinates for the middle part of the two adjacent sections (sections F6N and F6S) are 57 degrees 39'39.5 '''N, 6 degrees 14'43.9 '' W and 57 degrees 39'40.5 '' N, 6 degrees 14'45 '' W; UK National Grid Scheme NG 4687 7139 and NG 4687 7142 +/- 5 m. This stratigraphic point coincides with the appearance over a short stratigraphic interval of several new ammonite taxa that delineate the base of the Subboreal ammonite Baylei Zone, the base of the Densicostata Subzone marked by the base of the flodigarriensis horizon, and, independently, the base of the Boreal ammonite Bauhini Zone. The main advantages of this locality are: the presence of a dual ammonite zonation marked by two extensively studied, well-preserved and very abundant groups of ammonites, and their preservation within a continuous section of similar to 120 m of open marine, fossiliferous, thermally immature mudrocks with no evidence of condensation or stratigraphic gaps. Dinoflagellate cysts, magnetostratigraphy and stable isotope data from the same section provide secondary markers. The stratigraphic point is located 0.17-0.65 m below the boundary interval between the dinoflagellate cyst zones DSJ 26 and DSJ 27 (equivalent to the boundary between subzones c and d of the Scriniodinium crystallinum (=Scr) Zone). The point is located 0.02-0.24 m above the base of reversed magnetozone F3r. This magnetozone probably correlates with marine magnetic anomaly M26r but may correlate to the younger anomaly M25r. The point coincides with a well-marked broad minimum in delta C-13 values and a calculated low Sr-isotope value of 0.70687. The section has yielded nannofossils that show that the potential last occurrence of Octopodorhabdus decussatus that marks the lower part of the NJ15 zone occurs about 1.09 m below the boundary. The thermal immaturity and unweathered nature of the strata in the Flodigarry section has permitted a direct Re-Os radio-isotopic age of 154.1 +/- 2.2 Ma to be obtained from the mudrocks 0.05 m below the Kimmeridgian GSSP. Sequence stratigraphic analysis indicates that the GSSP lies within the lower part of a highstand system tract. The corresponding stratigraphic level in the Submediterranean-Mediterranean successions is close to the boundary between the Hypselum and Bimammatum ammonite zones. The change in ammonite groups noted at this level provides biostratigraphic markers for further global correlation.	[Wierzbowski, Andrzej; Barski, Marcin; Matyja, Bronislaw A.] Univ Warsaw, Fac Geol, Warsaw, Poland; [Coe, Angela L.] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England; [Hounslow, Mark W.] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England; [Hounslow, Mark W.] Univ Liverpool, Earth Ocean & Ecol Sci, Liverpool L69 3GP, Merseyside, England; [Price, Gregory D.] Univ Plymouth, Sch Geog, Earth & Environm Sci, Drake Circus, Plymouth PL4 8AA, Devon, England; [Wierzbowski, Hubert; Grabowski, Jacek] Polish Geol Inst Natl Res Inst, Warsaw, Poland; [Wright, John K.] Royal Holloway Univ London, Dept Earth Sci, Egham TW20 0EX, Surrey, England; [Contributions Francois Atrops] Univ Lyon, Lab Geol, F-69622 Villeurbanne, France; [Ogg, James G.] Purdue Univ, Dept Earth & Atmospher Sci, Indiana, PA USA; [Ogg, James G.] Chengdu Univ Technol, Inst Sedimentary Geol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Peoples R China; [Oloriz, Federico] Univ Granada, Fac Ciencias, Granada, Spain; [Page, Kevin] Univ Exeter, Camborne Sch Mines, Penryn TR10 9FE, Cornwall, England; [Parent, Horacio] Univ Nacl Rosario, Rosario, Argentina; [Przybylski, Piotr] BP America Inc Southern Performance Unit, Houston, TX USA; [Schweigert, Guenter] Staatliches Museum Naturkunde, Stuttgart, Germany; [Villasenor, Anna Bertha] Inst Geol, Dept Paleontol, Mexico City, DF, Mexico	University of Warsaw; Open University - UK; Lancaster University; University of Liverpool; University of Plymouth; Polish Geological Institute - National Research Institute; University of London; Royal Holloway University London; Purdue University System; Purdue University; Chengdu University of Technology; University of Granada; University of Exeter; National University of Rosario	Coe, AL (通讯作者)，Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England.	angela.coe@open.ac.uk	Price, Gregory/AAC-1801-2020; Wierzbowski, Hubert/AAA-4354-2019; Coe, Angela/AAA-2913-2021; Hounslow, mark/E-7873-2014; Mattioli, Emanuela/D-7951-2012; Grabowski, Jacek/F-3097-2011	VILLASENOR, ANA BERTHA/0000-0002-6033-5684; Grabowski, Jacek/0000-0001-6204-017X; Price, Gregory/0000-0002-2461-7465; Mattioli, Emanuela/0000-0003-0990-1641; Wierzbowski, Hubert/0000-0003-2682-2945; Coe, Angela/0000-0003-1416-5052	International Union of Geosciences through the International Commission on Stratigraphy	International Union of Geosciences through the International Commission on Stratigraphy	We are very grateful to Maria Ustinova and Mikhail Rogov, for their highly valued contributions to this project (see reference list for more details). The following other members of the Kimmeridgian Working Group provided comments: John Cope, Raymond Enay, Ewa Glowniak, Dmitry Kiselev, Dhirendra Kumar Pandey, Giulio Pavia, Armin Scherzinger, Ekaterina Tesakova, Victor Zakharov. We thank Stephen Hesselbo (Chair of the International Subcommission on Jurassic Stratigraphy 2012-2020) and the voting members of the International Subcommission on Jurassic Stratigraphy for their advice which helped to improve this manuscript considerably. Funding for workshops from International Union of Geosciences through the International Commission on Stratigraphy is gratefully acknowledged.	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J	Amenábar, CR; Guerstein, GR; Alperin, M; Daners, G; Casadío, S; Raising, MR				Rodriguez Amenabar, Cecilia; Raquel Guerstein, G.; Alperin, Marta; Daners, Gloria; Casadio, Silvio; Rodriguez Raising, Martin			CoRRELATIoN oF MIDDLE To UPPER EoCENE UNITS FRoM HIGH LATITUDE SoUTHWESTERN ATLANTIC SITES	AMEGHINIANA			English	Article						Dinoflagellate cysts; Paleogene; Drake Passage; Compositional Data Analysis; Biostratigraphy	TIERRA-DEL-FUEGO; DINOFLAGELLATE CYSTS; DRAKE PASSAGE; SEYMOUR ISLAND; AUSTRAL BASIN; PATAGONIA; STRATIGRAPHY; PENINSULA; OCEAN; SEDIMENTOLOGY	To understand the important significant climatic and paleoceanographic changes occurred in the Southern Hemisphere during the Paleogene, and especially those related to the opening of the Drake Passage, is essential to correlate the Eocene lithostratigraphic units in areas adjacent to this passage, such as those from the Austral-Magallanes and James Ross basins, to the north and to the south, respectively. For many years, there was no correlation between these units due to the absence of reliable chronostratigraphic and biostratigraphic information. Recently, other authors published U/ Pb data for the Austral-Magallanes Basin and introduced important modifications to the previous stratigraphic scheme. Subsequently, due to reinterpretating the available isotope data together with U/Pb ages, the chronostratigraphic model has modified again, also including the James Ross Basin. In light of an updated quantitative dinoflagellate cyst dataset from the units adjacent to the Drake Passage, we performed a Principal Component Analysis (PCA) to discuss the correlation between the studied sections. The PCA groups assemblages with a high contribution of Antarctic taxa (e. g., Enneadocysta dictyostila, Deflandrea antarctica) containing in the Upper Member of the Rio Turbio Formation (lower part), Man Aike, Leticia, and La Meseta formations, being Bartonian in age. The other group joined assemblages with younger ages, Priabonian, dominated by Antarctic species (Vozzhennikovia-Spinidinium) and cosmopolitan taxa, corresponding to the Upper Member of the Rio Turbio Formation (upper part). This study reinforces the most recent chronostratigraphic proposal and proves the biostratigraphic useful of some taxa for sites near the Drake Passage.	[Rodriguez Amenabar, Cecilia] Univ Buenos Aires, Fac Ciencias Exactas & Nat,Inst Estudios Andinos, Consejo Nacl Invest Cient Tecn IDEAN CONICET, Lab Bioestratig Alta Resoluc,Dept Ciencias Geol, Buenos Aires, DF, Argentina; [Rodriguez Amenabar, Cecilia] Inst Antartico Argentino, Area Ciencias Tierra, Dept Paleontol, 25 Mayo 1143,CP 1650, San Martin, Buenos Aires, Argentina; [Raquel Guerstein, G.] Univ Nacl Sul, INGEOSUR, CONICET, Dept Geol,Inst Geol Sur, Bahia Blanca, Buenos Aires, Argentina; [Alperin, Marta] Univ Nacl La Plata, Fac Ciencias Nat & Museo, Calle 64 S-N,Bv 120 & Diag 113,CP 1900, La Plata, Argentina; [Daners, Gloria] Univ La Republ UDELAR, Fac Ciencias, Montevideo, Uruguay; [Casadio, Silvio] Univ Nacl Rio Negro, Inst Invest Paleobiol & Geol, Ave Roca 1242, RA-8332 Roca, Rio Negro, Argentina; [Rodriguez Raising, Martin] Tucuman, RA-8300 San Miguel De Tucuman, Argentina	University of Buenos Aires; Instituto Antartico Argentino; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Universidad de la Republica, Uruguay	Amenábar, CR (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat,Inst Estudios Andinos, Consejo Nacl Invest Cient Tecn IDEAN CONICET, Lab Bioestratig Alta Resoluc,Dept Ciencias Geol, Buenos Aires, DF, Argentina.; Amenábar, CR (通讯作者)，Inst Antartico Argentino, Area Ciencias Tierra, Dept Paleontol, 25 Mayo 1143,CP 1650, San Martin, Buenos Aires, Argentina.	amenabar@gl.fcen.uba.ar; raquel.guerstein@uns.edu.ar; alperin@fcnym.unlp.edu.ar; lagluar@gmail.com; scasadio@unrn.edu.ar; martinrodriguezraising@hotmail.com		AMENABAR, CECILIA R./0000-0003-1280-3903	Universidad Nacional del Sur [PGI 24/F079]; Agencia Nacional de Promocion Cientifica y Tecnologica [PICT 2018-00917]	Universidad Nacional del Sur; Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government)	We thank Drs. A. Concheyro and E. Bernasconi for inviting us to participate in this Special Volume project. We would like to express our gratitude to the reviewers, Drs. A. Iakovleva, E. G. ottone, and N. Toledo for the effort and the time invested in providing detailed and comprehensive comments. We also appreciate the recommendations made by the Artwork Editor of Ameghiniana, P. Pineiro and the Editor-in-chief, Dr. D. G. Lazo. All the suggestions have significantly improved our manuscript. Financial support was provided by the Universidad Nacional del Sur (PGI 24/F079) and the Agencia Nacional de Promocion Cientifica y Tecnologica (PICT 2018-00917). This is a contribution to the Instituto Antartico Argentino (IAA) and the contribution R-457 to the Instituto de Estudios Andinos "Don Pablo Groeber" (IDEAN-CoNICET).	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J	Mansour, A; Tahoun, SS; Raafat, A; Ahmed, MS; Gentzis, T				Mansour, Ahmed; Tahoun, Sameh. S. S.; Raafat, Aya; Ahmed, Mohamed. S. S.; Gentzis, Thomas			Recurring Patterns of Sea Level Changes within a Palynological-Based Sequence Stratigraphy Framework of the Middle Jurassic Organic Matter-Rich Khatatba Formation, Egypt	MINERALS			English	Article						dinoflagellate cysts; transgression-regression cycles; Bajocian; Bathonian-Callovian; Dahab-Mireir Basin; north Western Desert	DINOFLAGELLATE CYSTS; BASIN; BIOSTRATIGRAPHY; DESERT; AREA	The Middle Jurassic was a time of marginal to shallow shelf settings dominated by organic matter-rich deposition in northern Egypt, southern Tethys. Paleoenvironmental and sequence stratigraphic reconstructions are of paramount significance for a better understanding of basin history and related reservoirs and source rock units. For this purpose, a detailed palynomorph and palynofacies analysis of the Middle Jurassic Khatatba Formation in the Dahab-Mireir Basin, north Western Desert, was conducted. A moderately to well-preserved, moderately diverse palynomorph assemblage of spores, pollen, and dinoflagellate cysts is identified. Marker dinoflagellate cysts, including Dichadogonyaulax sellwoodii, Escharisphaeridia pocokii, Gonyaulacysta adecta, Korystocysta gochtii, Pareodinia ceratophora, and Wanaea acollaris, defined a Bajocian to Callovian age. Palynofacies analysis of the Khatatba Formation revealed two assemblages, whereby PFA-1 is the most abundant in the study well and is comprised mainly of terrestrial phytoclasts deposited nearby fluvio-deltaic sources. The infrequently reported PFA-2 consists of moderate abundances of phytoclasts and AOM, deposited in an inner shelf environment. A more reliable paleoenvironmental interpretation was indicated based on three palynomorph assemblages. The spore-dominated assemblage indicated deposition in a deltaic environment, while the mixed palynomorph assemblage revealed fluvio-deltaic to marginal shallow marine conditions. The microplankton-dominated assemblage is represented by minor samples and reflects an offshore inner shelf condition. Furthermore, the Middle Jurassic relative sea level was reconstructed based on the quantitative variations in the terrestrial/marine (T:M) ratios and abundances of spores, pollen, and dinoflagellate cysts. This led to the subdivide of the Khatatba Formation into thirteen third-order transgressive-regressive sequences, which can be correlated with the global Jurassic short-term sea level changes. Active tectonics and accelerated drifting of the Eurasian Plate during the Middle Jurassic are suggested to control basin uplift/subsidence and, therefore, recurring patterns of relative sea level change.	[Mansour, Ahmed] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Southwest Petr Univ, Qiangtang Inst Sedimentary Basin, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610050, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Tahoun, Sameh. S. S.; Raafat, Aya] Cairo Univ, Fac Sci, Geol Dept, Giza 12613, Egypt; [Ahmed, Mohamed. S. S.] King Saud Univ, Coll Sci, Geol & Geophys Dept, POB 2455, Riyadh 11451, Saudi Arabia; [Gentzis, Thomas] Core Labs Inc, Houston, TX 77040 USA	Southwest Petroleum University; Southwest Petroleum University; Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; Egyptian Knowledge Bank (EKB); Cairo University; King Saud University	Gentzis, T (通讯作者)，Core Labs Inc, Houston, TX 77040 USA.	ahmedmans48@mu.edu.eg; tahoun@cu.edu.eg; ayar210@yahoo.com; mohahmed@ksu.edu.sa; thomas.gentzis@corelab.com	Raafat, Aya/AHE-3464-2022; Mansour, Ahmed/AAR-4969-2020; Ahmed, Mohamed/GQP-1116-2022	Mansour, Ahmed/0000-0003-2466-7494; Gentzis, Thomas/0000-0003-4592-9318; Ahmed, Mohamed/0000-0001-9249-6231	King Saud University, Riyadh, Saudi Arabia [RSP2023R455]	King Saud University, Riyadh, Saudi Arabia(King Saud University)	This work was funded by Researchers Supporting Project, King Saud University, Riyadh, Saudi Arabia, number (RSP2023R455).	Aboul Ela N. 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J	Lebedeva, NK				Lebedeva, N. K.			Taxonomic Diversity of Cenomanian-Turonian Dinocysts in the Northern Hemisphere: Some Aspects of Paleobiogeography and Paleoclimatology	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Upper Cretaceous; paleoalgology; biostratigraphy; correlation; paleobiogeography; paleogeography	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; UPPER CRETACEOUS DEPOSITS; BOUNDARY EVENT CTBE; WESTERN INTERIOR; STRATIGRAPHY; PALYNOSTRATIGRAPHY; SEDIMENTS; SOUTH; PALYNOLOGY; SECTIONS	The taxonomic typification of dinocyst assemblages was carried out on the basis of a qualitative and quantitative assessment of their generic composition for the Northern Hemisphere in the Cenomanian-Turonian time to identify correlation taxa. Three types of dinocyst assemblages were identified in the Cenomanian. Cenomanian dinocyst assemblages are poorly differentiated; a large number of cosmopolitan genera were identified, which is in good agreement with paleobotanical data indicating a very warm, humid climate. Three types of dinocyst assemblages were established for the Turonian. The number of cosmopolitan dinocyst genera decreases and species endemism sharply increases in some Turonian basins. The differentiation of assemblages increases and their correlation potential decreases. However, the identified common genera and species of dinocysts in different types of assemblages provide the possibility of interregional correlation of Upper Cretaceous deposits at the stage, substage, and, at some sections, even more detailed levels in different climatic zones.	[Lebedeva, N. K.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Lebedeva, NK (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia.	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Geol. Correl.	JUN	2023	31	3					186	199		10.1134/S0869593823020041	http://dx.doi.org/10.1134/S0869593823020041			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	H3IR4					2025-03-11	WOS:000994941400004
J	Kuzmina, OB; Iakovleva, AI				Kuzmina, O. B.; Iakovleva, A. I.			New Spore and Pollen Data from the Upper Eocene Deposits of the Sambian Peninsula, Kaliningrad Oblast	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						spore and pollen assemblages; dinocyst zones; Eocene; Priabonian; Kaliningrad oblast	PALYNOLOGICAL CHARACTERISTICS; PALEOGENE DEPOSITS; PALYNOFLORA; REGION; WEST	The article presents the results of the study of continental palynomorphs from the amber-bearing Upper Eocene deposits in the Primorsky quarry (Kaliningrad oblast, southeastern coast of the Baltic Sea). Three spore and pollen assemblages were identified and calibrated with the dinoflagellate cyst Rhombodinium perforatum and Thalassiphora reticulata zones. The "Blue Earth" Member of the Prussian Formation of the early Priabonian age is characterized by the Tricolporopollenites exactus-T. retiformis-Quercoidites microhenrici assemblage. The upper Priabonian "Upper Quicksand" and "White Wall" members of the Prussian Formation and the Palve Formation are characterized by the Platanipollis ipelensis-Castaneoideaepollis oviformis-Tricolpopollenites foraminatus assemblage. The Inaperturopollenites-Sciadopityspollenites-Sequoiapollenites assemblage was recognized in the uppermost Palve and lowermost Kurshskaya formations of the terminal Priabonian. During the Late Eocene, the climatic conditions on the territory of the modern southern Baltic area were quite warm and humid, close to subtropical ones. Mixed coniferous-broad-leaved forests grew along the shores of the marine paleostrait, while the open spaces were occupied by heat-loving evergreen and moderately heat-loving deciduous shrubs and low-lying land areas were swamped. Gradual regression of the sea basin, which began at the end of the Priabonian, led to an increase in swampy areas on land, while the climate was still quite warm and humid.	[Kuzmina, O. B.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia; [Iakovleva, A. I.] Russian Acad Sci, Geol Inst, Moscow, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Kuzmina, OB (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia.	KuzminaOB@ipgg.sbras.ru	Kuzmina, Olga/I-9547-2018					Aleksandrova GN, 2008, STRATIGR GEO CORREL+, V16, P528, DOI 10.1134/S0869593808050067; Aleksandrova GN, 2008, STRATIGR GEO CORREL+, V16, P295, DOI 10.1134/S0869593808030052; Alekseev P. 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A., 2001, STRATIGRAFIYA KALINI; Zaporozhets NI, 2017, STRATIGR GEO CORREL+, V25, P638, DOI 10.1134/S0869593817060089; Ziembinska-Tworzydlo M., 1994, ACTA PALAEOBOT, V1994, P1; Zosimovich V.Yu., 1992, THESIS I GEOL NAUK A	43	3	3	2	2	PLEIADES PUBLISHING INC	NEW YORK	PLEIADES HOUSE, 7 W 54 ST, NEW YORK,  NY, UNITED STATES	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	JUN	2023	31	3					200	214		10.1134/S086959382303005X	http://dx.doi.org/10.1134/S086959382303005X			15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	H3IR4					2025-03-11	WOS:000994941400005
J	Porthun, SD; Antonioli, L; Dino, R; Portela, HA; Soares, EAA				Porthun, Stella do Amaral; Antonioli, Luzia; Dino, Rodolfo; Portela, Helena Antunes; Soares, Emilio Alberto Amaral			Upper maastrichtian palynology and paleoenvironment of the Urucutuca Formation, Almada basin (BA), Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dinoflagellate cysts; Biostratigraphy; Palynofacies; Upper cretaceous; Total organic carbon	APTIAN-ALBIAN SUCCESSION; SERGIPE BASIN	Hydrocarbon exploration involving the Urucutuca Formation is taking place in several basins located mainly in the central segment of the eastern Brazilian margin, including the Almada Basin. Relatively rich accumulations of organic material and promising prospects, especially for gas, have been discovered. The Brazilian National Pe-troleum Agency (ANP) considers the Urucutuca Formation as a speculative play exploratory (Urucutuca-Uru-cutuca) in deep and ultra-deep areas of the Almada Basin, including others. The focus was on improving the understanding of the sediments of the Urucutuca Formation and establishing a palynostratigraphic outline for the upper cretaceous strata, which still need to be updated. Therefore, integrated palynological, palynofaciological, and organic-geochemical (total organic carbon-TOC) investigation methods were carried out. For this purpose, 250 m of well 1-SST-01, drilled in the onshore part of the Almada Basin in Bahia State, were analyzed using 26 core samples along the Urucutuca Formation.By typifying palynofaciological variations based on organic matter content in conjunction with palynological and geochemical data, it was possible to distinguish three palynofacies with different characteristics of the marine influence environment. Palynofacies 1, the amorphous organic matter (AOM) group, predominates with proportions up to 54.1 and a TOC of 0.75%. The high phytoclasts percentage (70%) and a TOC content of 1% characterize the Palynofacies 2. Palynofacies 3, on the other hand, has the highest content of marine paly-nomorphs (40%).The analysis of total organic carbon yielded values ranging from 0.04% to 1.85%, which were heterogeneously distributed throughout the borehole.The palynological succession showed a dominance of representatives of continental origin. However, marine elements (dinoflagellates and microforaminiferal inner tests) are present throughout the section.Two expressive occurrences of dinoflagellate cysts are evident throughout the section. In the basal and middle portions, quantity and diversity suggest transgressive events or at least sea-level fluctuations. Bio-stratigraphically, the unit could be placed in the Tricornites elongatus (P-470) Biozone of the Crassitricolporites brasiliensis (P-450) Superzone and assigned to the Eomaastrichtian. These biostratigraphic units are consistent with the proposed zonation for other basins of the Brazilian Atlantic margin. Palynofacies and palynological data allowed the observation of variations in a predominantly platform paleoenvironment, sometimes distal and sometimes more proximal, with possible transgressions.	[Porthun, Stella do Amaral; Antonioli, Luzia; Dino, Rodolfo; Portela, Helena Antunes] Univ Estado Rio De Janeiro, Fac Geol, Programa Posgrad Geociencias, Rio De Janeiro, Brazil; [Soares, Emilio Alberto Amaral] Univ Fed Amazonas, Programa Posgrad Geocie ncias, Manaus, Amazonas, Brazil; [Porthun, Stella do Amaral] 524 Sao Francisco Xavier St,2024-A Room, BR-20550013 Rio De Janeiro, RJ, Brazil	Universidade do Estado do Rio de Janeiro; Universidade Federal de Amazonas	Porthun, SD (通讯作者)，524 Sao Francisco Xavier St,2024-A Room, BR-20550013 Rio De Janeiro, RJ, Brazil.	stelladoamaralporthun@gmail.com; luantonioli7@gmail.com; dinouerj@gmail.com; helenaportela@gmail.com; easoares@ufam.edu.br	Soares, Emílio/Q-5208-2017					Alberti G., 1959, Mitteilungen aus dem Geologischen Staatsinstitut in Hamburg, V28, P93; Alberti G., 1961, Palaeontographica, V116, P1; Antonioli L., 2020, ANU INST GEOCIENC, V43, P339, DOI DOI 10.11137/2020_1_339_345; Azema C, 1974, PALEOBIOL CONTINET M, V5, P1; Boltenhagen E., 1975, REV MICROPALE ONTOLO, V18, P69; Brenner G.J., 1963, Mines and Water Resources, V27, P215; Bruhn C.H.L., 1989, B GEOCIE NCIAS PETRO, V3, P235; Caixeta J.M., 2007, B GEOCIENCIAS PETROB, V15, P2; Carvalho K.W.B., 1965, B TE CNICO PETROBRAS, V8, P5; Carvalho MD, 2006, MAR MICROPALEONTOL, V59, P56, DOI 10.1016/j.marmicro.2006.01.001; Chang H.K., 1987, REV BRAS GEOCIENCIAS, V17, P74; Chang H.L., 1991, ORIGEM EVOLUCAO BACI; CHANG YI-MAW, 1967, J PALEONTOL, V41, P500; Cookson I. 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JUL	2023	127								104410	10.1016/j.jsames.2023.104410	http://dx.doi.org/10.1016/j.jsames.2023.104410		MAY 2023	16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	J5SB4					2025-03-11	WOS:001010203200001
J	Fuentes, SN				Fuentes, Sabrina Natalia			Miocene dinoflagellate cyst biostratigraphy of the Peninsula Valdes, Patagonia, Argentina	PALYNOLOGY			English	Article						Argentina; biostratigraphy; dinoflagellate cysts; Miocene; Peninsula Valdes	PUERTO-MADRYN FORMATION; BASIN NORTHERN BELGIUM; MIDDLE MIOCENE; PLIOCENE-PLEISTOCENE; CALCAREOUS NANNOPLANKTON; NORTHEASTERN PATAGONIA; ACRITARCH EVENTS; COLORADO BASIN; SEA; ATLANTIC	The present work documents the stratigraphic distribution of dinoflagellate cysts from the upper part (60-585 m) of the YPF.Ch. PV. es-1 borehole, Peninsula Valdes, Argentina. The assemblages exhibit a relatively moderate to low diversity. Most samples are characterized by frequent to abundant taxa of the order Gonyaulacales, such as Spiniferites/Achomosphaera spp., Reticulatosphaera actinocoronata, Operculodinium centrocarpum, and Melitasphaeridium choanophorum. Furthermore, a continuous succession of Early Miocene-Late Miocene diagnostic dinoflagellate cyst events was recorded for the first time from the Peninsula Valdes region. Eight diagnostic events of highest occurrences (HOs) of dinoflagellate cyst taxa are identified. These bioevents allowed a subdivision of the sedimentary succession into two well-defined stratigraphic sections: Early to Middle Miocene (Burdigalian-Langhian/probably Serravalian, 430/425-330/325 m) based on the HOs of Emmetrocysta urnaformis, Cannosphaeropsis quattrocchiae, Cousteaudinium auybriae, and Cleistosphaeridium ancyreum, and Late Miocene (Tortonian-Messinian, between 175-170 and 80/85 m) based on the HOs of Labyrinthodinium truncatum subsp. truncatum, Operculodinium piaseckii, and Reticulatosphaera actinocoronata. The ranges of these taxa are compared with well-documented information on Neogene dinoflagellate cysts recorded from different sites across the North and South Atlantic Ocean and adjacent seas. In general, the dinoflagellate cyst assemblages, as well as the selected diagnostic taxa, exhibit a clear similarity to those of the Northern Hemisphere. The only exception is Hystrichokolpoma rigaudiae, which is asynchronous, possibly indicating local paleoenvironmental conditions.	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J	Kuhn, LA; Zonneveld, KAF; Souza, PA; Cancelli, RR				Kuhn, Lidia A.; Zonneveld, Karin A. F.; Souza, Paulo A.; Cancelli, Rodrigo R.			Late Quaternary palaeoenvironmental evolution and sea level oscillation ofSanta Catarina Island (southern Brazil)	BIOGEOSCIENCES			English	Article							SANTA-CATARINA; HOLOCENE SEDIMENTS; COASTAL-PLAIN; SOUTHEASTERN BRAZIL; PALYNOLOGICAL DATA; ANGIOSPERM POLLEN; VEGETATION; CLIMATE; DYNAMICS; HISTORY	Sea level oscillation during the Quaternary played amajor role in the geomorphology and vegetation dynamics of coastal areas insouthern Brazil, encompassing ecosystems that often have a uniquebiodiversity. Understanding the natural evolution of these areas isessential for decision making regarding land use regulations towards sustainabledevelopment, as well as to preserve the uniqueness of the coastal ecosystems.The southern Brazil coastal plain is formed by marine, transitional andcontinental Quaternary deposits controlled by past variations of the sealevel. These variations shaped the coastal landscape and influenced thedevelopment of different Atlantic rainforest formations, such as mangrovesand restingas. In particular, the restinga formation corresponds to aspecific ecosystem that covers sandy soils of marine and fluvial-marineorigin formed during the Quaternary on the Brazilian coastal plain. In thiscontribution, we present high-resolution palynological and stable isotopedata from a Holocene core retrieved from the coastal plain of SantaCatarina Island (southern Brazil). We were able to identify four differentenvironmental zones for the last 6520 yr BP. The first zone (6520-2920 cal yr BP) is characterized by a lagoon with large marine-water influence.Notably, the observed dinoflagellate cyst association suggests that marinewaters entering the region had their origin in the relatively warm and salineBrazil Current waters. During the second zone (2920-1520 cal yr BP), marine-water contribution to the lagoon decreased until it became disconnected fromthe sea. The third zone (1520-550 cal yr BP) was marked by the decrease ofthe water level until it dried out and led to the colonization of herbaceousvegetation over the palaeo-lagoon. The last zone (550 cal yr BP-recent) ischaracterized by the consolidation of the coastal-plain Atlantic rainforest(restinga vegetation). Our results form an example of the strong sensitivityof southern Brazilian ecosystem change caused by relative sea levelvariations. As such, this study might contribute to the debate about the potentialeffects of current climate change induced by global sea level variations.	[Kuhn, Lidia A.; Souza, Paulo A.; Cancelli, Rodrigo R.] Univ Fed Rio Grande do Sul, Inst Geociencias, Lab Palinol Marleni Marques Toigo, BR-91540000 Porto Alegre, Brazil; [Kuhn, Lidia A.; Zonneveld, Karin A. F.] Univ Bremen, Fac Geosci, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany	Universidade Federal do Rio Grande do Sul; University of Bremen	Kuhn, LA (通讯作者)，Univ Fed Rio Grande do Sul, Inst Geociencias, Lab Palinol Marleni Marques Toigo, BR-91540000 Porto Alegre, Brazil.; Kuhn, LA; Zonneveld, KAF (通讯作者)，Univ Bremen, Fac Geosci, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany.	lidiaak.lak@gmail.com; kzonneveld@marum.de		Kuhn, Lidia/0000-0003-2120-1824	CNPq-National Council for Scientific and Technological Development of Brazil [141324/2017]; CAPES-Brazilian Coordination of Higher Education Staff Improvement [88887.467306/2019-00]	CNPq-National Council for Scientific and Technological Development of Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES-Brazilian Coordination of Higher Education Staff Improvement	This research has been supported by the CNPq-National Council for Scientific and Technological Development of Brazil (grant no. 141324/2017) and CAPES-Brazilian Coordination of Higher Education Staff Improvement (grant no.88887.467306/2019-00)	Alvares CA, 2013, METEOROL Z, V22, P711, DOI 10.1127/0941-2948/2013/0507; Angulo R. 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Shelf Sci; Vilanova I, 2012, AMEGHINIANA, V49, P303, DOI 10.5710/AMGH.v49i3(499); Wilson GP, 2005, ESTUAR COAST SHELF S, V64, P685, DOI 10.1016/j.ecss.2005.04.003; Ybert JP, 2003, PALAEOGEOGR PALAEOCL, V189, P11, DOI 10.1016/S0031-0182(02)00590-4; Zazo C, 2013, GEOMORPHOLOGY, V196, P36, DOI 10.1016/j.geomorph.2012.10.020; 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	98	3	3	0	5	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	1726-4170	1726-4189		BIOGEOSCIENCES	Biogeosciences	MAY 23	2023	20	10					1843	1861		10.5194/bg-20-1843-2023	http://dx.doi.org/10.5194/bg-20-1843-2023			19	Ecology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	H0DO8		gold			2025-03-11	WOS:000992758500001
J	Rojas-Castillo, OA; Pereira, L; Buffon, P; Cardoso, LD				Rojas-Castillo, Oscar Alberto; Pereira, Leonel; Buffon, Patricia; Cardoso, Luciana de Souza			Drivers and ecology of Ceratium furcoides invasion of a Brazilian subtropical reservoir and its interaction with the phytoplankton community	LIMNOLOGICA			English	Article						Phytoplankton dynamics; Dinophyceae; Dinoflagellate; Artificial lake; Freshwater; Invasion	LEVANDER LANGHANS 1925; DINOFLAGELLATE CERATIUM; 1ST RECORD; LAKE; HIRUNDINELLA; BLOOM; DAM; BACILLARIOPHYCEAE; ASSOCIATIONS; SUCCESSION	We analyzed the phytoplankton interactions during a Ceratium furcoides invasion along with the environmental variables contributing to its dominance and blooms in Marrecas, a south-Brazilian reservoir. We monitored Marrecas weekly/monthly (n = 116) from 2014 to 2018. C. furcoides avoided summer and preferred spring, which displayed optimal temperatures for the species (15-23 degrees C), exhibiting in October 2014 the maximum density ever reported (15,865 ind. mL-1). It showed direct correlation with iron, manganese, and turbidity; evidencing dependency of a mixing regime which triggers cyst resuspension (interrupting cysts' dormancy). Cryptomonas spp., Komma caudata, Discostella stelligera and after 2016 also Chlamydomonas sp. were the only species present during C. furcoides blooms. Komma caudata, Cryptomonas sp., and Aulacoseira alpigena correlated positively with the invader, as all prefer turbulent waters. C. furcoides correlated negatively with Chlorophyta (mainly Chlamydomonas spp.) which is vulnerable to mixing, and Bacillariophyta (Urosolenia eriensis and Discostella stelligera) that prefers clear waters. It also showed a consistent negative correlation with Ochrophyta (Mallomonas spp.), Cyanobacteria (Microcystis), and Urosolenia eriensis; suggesting competition for resources. Furthermore, it correlated negatively with species richness. Notwithstanding, based on the decrease of blooms, the phytoplankton community appears to have reached a more stable state (homogeneous species representation). However, further monitoring is required for confirmation.	[Rojas-Castillo, Oscar Alberto; Pereira, Leonel] Univ Coimbra, MARE Marine & Environm Sci Ctr, Associate Lab ARNET, Dept Life Sci, P-3001456 Coimbra, Portugal; [Buffon, Patricia] Serv Autonomo Municipal Agua & Esgoto Samae, BR-95020170 Caxias Do Sul, RS, Brazil; [Cardoso, Luciana de Souza] Univ Fed Rio Grande do Sul, BR-91501970 Porto Alegre, RS, Brazil; [Rojas-Castillo, Oscar Alberto] Univ Copenhagen, Dept Biol, Freshwater Biol Sect, Univ Pk 4 3rd Floor, DK-2100 Copenhagen, Denmark	Universidade de Coimbra; Universidade Federal do Rio Grande do Sul; University of Copenhagen	Rojas-Castillo, OA (通讯作者)，Univ Coimbra, MARE Marine & Environm Sci Ctr, Associate Lab ARNET, Dept Life Sci, P-3001456 Coimbra, Portugal.	oscar.rojas.gua27@gmail.com	de S Cardoso, Luciana/D-9523-2013; Pereira, Leonel/M-3527-2013	Pereira, Leonel/0000-0002-6819-0619; Rojas Castillo, Oscar Alberto/0000-0002-0176-9685	Coordenagao de Aperfei-goamento de Pessoal de Nfvel Superior-Brasil [001]; Coordenagao de Aperfei-goamento de Pessoal de Nfvel Superior-Brasil (CAPES) [001]; European Commission through the program Erasmus Mundus Master Course-International Master in Applied Ecology (EMMC-IMAE) [FPA 2023-0224/532524-1-FR-2012-1-ERA MUNDUS-EMMC]; national funds through Fundagao para a Ciencia e Tecnologia (FCT) [LA/P/0069/2020]	Coordenagao de Aperfei-goamento de Pessoal de Nfvel Superior-Brasil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Coordenagao de Aperfei-goamento de Pessoal de Nfvel Superior-Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); European Commission through the program Erasmus Mundus Master Course-International Master in Applied Ecology (EMMC-IMAE); national funds through Fundagao para a Ciencia e Tecnologia (FCT)	This work was supported partially by the Coordenagao de Aperfeigoamento de Pessoal de Nfvel Superior-Brasil (CAPES) -Finance Code 001, by the European Commission through the program Erasmus Mundus Master Course-International Master in Applied Ecology (EMMC-IMAE) (FPA 2023-0224/532524-1-FR-2012-1-ERA MUNDUS-EMMC), and by national funds through Fundagao para a Ciencia e Tecnologia (FCT) , under the project LA/P/0069/2020 granted to the Associate Laboratory ARNET.	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J	Shin, HH; Son, MH; Park, BS; Han, KH; Youn, JY; Kwak, KY; Lee, JH; Shin, AY; Byun, E; Yoo, YD; Seo, MH; Shin, K; Li, Z				Shin, Hyeon Ho; Son, Moon Ho; Park, Bum Soo; Han, Kyung Ha; Youn, Joo Yeon; Kwak, Kyeong Yoon; Lee, Ji Hoon; Shin, A. -Young; Byun, Eunjung; Yoo, Yeong Du; Seo, Min Ho; Shin, Kyungsoon; Li, Zhun			Bloom development of toxic dinoflagellate<i> Alexandrium</i><i> catenella</i> (Group I) in Jinhae-Masan Bay, Korea: Germination strategy of resting cysts in relation to temperature and salinity	MARINE POLLUTION BULLETIN			English	Article						PSP; Ellipsoidal cyst; Seed population; Dormancy period; Adaptation	SPECIES COMPLEX DINOPHYCEAE; TAMARENSE DINOPHYCEAE; EXCYSTMENT; FUNDYENSE; MINUTUM; SEA	To better understand the role of resting cysts in the outbreak of paralytic shellfish poisoning and bloom dynamics in Jinhae-Masan Bay, Korea, this study investigated the germination features of ellipsoidal Alexandrium cysts isolated from sediments collected in winter and summer under different combinations of temperature and salinity. Morphology and phylogeny of germling cells revealed that the ellipsoidal Alexandrium cysts belong to Alexandrium catenella (Group I). The cysts could germinate across a wide range of temperature (5-25 degrees C) with germination success within 5 days, indicating that continuous seeding for the maintenance of vegetative cells in the water column may occur through the year without an endogenous clock to regulate germination timing. In addition, the cyst germination of A. catenella (Group I) was not controlled by seasonal salinity changes. Based on the results, this study provides a schematic scenario of the bloom development of A. catenella (Group I) in Jinhae-Masan Bay, Korea.	[Shin, Hyeon Ho; Han, Kyung Ha; Youn, Joo Yeon; Kwak, Kyeong Yoon] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea; [Son, Moon Ho] Natl Inst Fisheries Sci, Busan 619705, South Korea; [Park, Bum Soo; Han, Kyung Ha] Hanyang Univ, Dept Life Sci, 222 Wangsipriro, Seoul 04763, South Korea; [Lee, Ji Hoon; Shin, A. -Young; Byun, Eunjung] Korea Inst Ocean Sci & Technol, Marine Biotechnol Res Ctr, Busan 49111, South Korea; [Yoo, Yeong Du] Kunsan Natl Univ, Fac Marine Appl Biosci, Gunsan 54150, South Korea; [Seo, Min Ho] Marine Ecol Res Ctr, Yeosu 59697, South Korea; [Shin, Kyungsoon] Korea Inst Ocean Sci & Technol, Ballast Water Res Ctr, Geoje 53201, South Korea; [Li, Zhun] Korea Res Inst Biosci & Biotechnol, Korean Collect Type Cultures KCTC, Biol Resource Ctr, Jeongeup 56212, South Korea	Korea Institute of Ocean Science & Technology (KIOST); National Institute of Fisheries Science; Hanyang University; Korea Institute of Ocean Science & Technology (KIOST); Kunsan National University; Korea Institute of Ocean Science & Technology (KIOST); Korea Research Institute of Bioscience & Biotechnology (KRIBB)	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 53201, South Korea.; Li, Z (通讯作者)，Korea Res Inst Biosci & Biotechnol, Korean Collect Type Cultures KCTC, Biol Resource Ctr, Jeongeup 56212, South Korea.	shh961121@kiost.ac.kr; lizhun@kribb.re.kr	Li, Zhun/IUQ-5309-2023; Park, Bum/W-3178-2017	LI, ZHUN/0000-0001-8961-9966; Shin, Hyeon Ho/0000-0002-9711-6717	Marine Biotics project [20210469]; Ministry of Ocean and Fisheries; Korean Culture Collection of Microalgae and Collaboration Center [NRF- 2022M3H9A1083416]; Techniques for the Management and Evaluation of Biofouling on Ship Hulls [20210651]; NIFS [R2022069]; KIOST [PEA0121]; Korea Research Institute of Bioscience and Biotechnology (KRIBB) Research Initiative Program [KGM5232322]	Marine Biotics project; Ministry of Ocean and Fisheries; Korean Culture Collection of Microalgae and Collaboration Center; Techniques for the Management and Evaluation of Biofouling on Ship Hulls; NIFS; KIOST; Korea Research Institute of Bioscience and Biotechnology (KRIBB) Research Initiative Program	This work was supported by grants from the Marine Biotics project (20210469) funded by the Ministry of Ocean and Fisheries, the Korean Culture Collection of Microalgae and Collaboration Center (NRF- 2022M3H9A1083416), Techniques for the Management and Evaluation of Biofouling on Ship Hulls (20210651), the NIFS (R2022069) and KIOST (PEA0121) projects, and the Korea Research Institute of Bioscience and Biotechnology (KRIBB) Research Initiative Program (KGM5232322).	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Pollut. Bull.	JUN	2023	191								114995	10.1016/j.marpolbul.2023.114995	http://dx.doi.org/10.1016/j.marpolbul.2023.114995		MAY 2023	7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	I0OG8	37146546				2025-03-11	WOS:000999849000001
J	Everaert, S; Deckers, J; Munsterman, D; Wesselingh, FP				Everaert, Stijn; Deckers, Jef; Munsterman, Dirk; Wesselingh, Frank P.			The Pliocene-Pleistocene transition in the subsurface of the Dutch-Belgian border region: insights from borehole Huijbergen	GEOLOGICA BELGICA			English	Article						stratigraphy; Neogene; Quaternary; molluscs; dinoflagellate cysts; Merksplas Formation; Lillo Formation	NORTH-SEA BASIN; DINOFLAGELLATE CYST; STRATIGRAPHY; NEOGENE; QUATERNARY; SEDIMENTS; PALEOECOLOGY	Cross-border correlations of the Pliocene-Pleistocene successions in the southern Netherlands and northernmost Belgium are problematic, because biostratigraphic markers are often lacking. Correlation is further hampered by the poor age constraints of the Belgian Merksplas Formation. To address these issues, sedimentary, mollusc and dinoflagellate cyst analyses are combined to characterise the lithostratigraphic units in the Huijbergen borehole (The Netherlands) and to provide age estimates. Subsequently, the Huijbergen borehole was correlated with nearby boreholes in Essen and Kalmthout (Belgium). The Piacenzian intervals of the Dutch Oosterhout Formation can be correlated with the Belgian Lillo Formation, with the latter's threefold borehole log signature appearing virtually continuous across the border between both countries. The Dutch Maassluis and Waalre formations are correlated with the shell-bearing lower part and the unfossiliferous higher part of the Merksplas Formation respectively. Although dinocysts are not age-diagnostic for the Maassluis and Waalre formations in borehole Huijbergen, characteristic interglacial marine shells provide a Gelasian age assessment for the Maassluis Formation. By correlation, this age estimate can also be applied to the lower part of the Merksplas Formation, thereby elucidating the Pliocene- Pleistocene transition near the Dutch-Belgian border.	[Everaert, Stijn] Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium; [Deckers, Jef] VITO, Boeretang 200, B-2400 Mol, Belgium; [Munsterman, Dirk] TNO Geol Survey Netherlands GSN, POB 80015, NL-3508 TA Utrecht, Netherlands; [Wesselingh, Frank P.] Nat Biodivers Ctr, POB 9517, NL- 2300 RA Leiden, Netherlands; [Wesselingh, Frank P.] Univ Utrecht, Earth Sci, Utrecht, Netherlands	Royal Belgian Institute of Natural Sciences; VITO; Naturalis Biodiversity Center; Utrecht University	Everaert, S (通讯作者)，Royal Belgian Inst Nat Sci, OD Earth & Hist Life, Vautierstr 29, B-1000 Brussels, Belgium.	stijn.everaert1@gmail.com; jef.deckers@vito.be; dirk.munsterman@tno.nl; frank.wesselingh@naturalis.nl	Everaert, Stijn/JBJ-5025-2023; Wesselingh, Frank/C-1367-2018	Deckers, Jef/0000-0002-5373-8733; Munsterman, Dirk/0000-0003-1774-4615; Everaert, Stijn/0000-0001-9551-9275; Wesselingh, Frank/0000-0003-3655-0701				Al-Silwadi S., 2017, THESIS BROCK U ONTAR; Aleffi Floriana, 2000, Anali za Istrske in Mediteranske Studije, V21, P173; [Anonymous], 1988, GEOLOGISCHES JB A; BGD, 1980, BOORV BGD 006E0130; Boele Joop, 2001, Afzettingen Werkgroep voor Tertiaire en Kwartaire Geologie, V22, P34; Bogemans F., 2014, NEOGENE REVISED LITH; Buffel P., 2001, AARDKUNDIGE MEDEDELI, V11, P1; Crampton-Flood ED, 2020, CLIM PAST, V16, P523, DOI 10.5194/cp-16-523-2020; Crampton-Flood ED, 2018, EARTH PLANET SC LETT, V490, P193, DOI 10.1016/j.epsl.2018.03.030; de Heinzelin de Braucourt J., 1955, B I ROYAL SCI NATURE, V31/66-67, P1; de Heinzelin de Braucourt J., 1955, B SOC BELG GEOL, V64, P463; de HEINZELIN de BRAUCOURT JEAN, 1950, INST ROY SCI NAT BELGIQUE BULL, V26, P1; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Schepper S, 2008, STRATIGRAPHY, V5, P137; De Schepper S, 2015, NAT COMMUN, V6, DOI 10.1038/ncomms9659; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; Deckers J, 2020, GEOL BELG, V23, P333, DOI 10.20341/gb.2020.027; Doppert J.W. 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Belg.		2023	26	1-2					25	40		10.20341/gb.2023.001	http://dx.doi.org/10.20341/gb.2023.001		MAY 2023	16	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	J6YM7		gold			2025-03-11	WOS:000989170400001
J	Goryacheva, AA; Glinskikh, LA; Dzyuba, OS; Urman, OS; Shurygin, BN				Goryacheva, A. A.; Glinskikh, L. A.; Dzyuba, O. S.; Urman, O. S.; Shurygin, B. N.			The First Data on Middle Jurassic Dinoflagellate Cysts and Foraminifera of the Russian Far East	DOKLADY EARTH SCIENCES			English	Article						microphytofossils; foraminifera; Middle Jurassic; Far East	BASIN	The first records of dinocysts and foraminifers in the Middle Jurassic deposits of the Russian Far East and their taxonomic affiliation are reported. The use of foraminiferal and ostracod assemblages as a tool for biostratigraphic subdivision and correlation of the Middle Jurassic sections of this region is very difficult due to the poor preservation and limited occurrence of these microfossils. Findings of the dinocysts Endoscrinium galeritum,Tubotuberella cf. apatela,Wanaea fimbriata, and Meiourogonyaulax cf. caytonensis raise the question of correcting the stratigraphic range of the lithological formations recognized in the Middle Jurassic.	[Goryacheva, A. A.; Glinskikh, L. A.; Dzyuba, O. S.; Urman, O. S.; Shurygin, B. N.] 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	Goryacheva, AA (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia.	goryachevaaa@ipgg.sbras.ru	Dzyuba, Oksana/I-8639-2018; Anna, Goryacheva/T-5116-2017; Shurygin, Boris/I-8387-2018	Dzyuba, Oksana/0000-0003-1523-8153; Anna, Goryacheva/0000-0002-9012-7376; Shurygin, Boris/0000-0001-5512-7509				Anoikin V. I., 2003, SER BUREINSKAYA, V2nd; Dzyuba O. S., 2020, P 8 ALL RUSS M INT P, P59; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Glinskikh LA, 2018, PALEONTOL J+, V52, P221, DOI 10.1134/S0031030118030048; Goryacheva AA, 2017, STRATIGR GEO CORREL+, V25, P265, DOI 10.1134/S0869593817030042; Ilyina VI, 2005, MICROPAL SOC SPEC PU, P109; Kirillova GL, 2012, RUSS J PAC GEOL, V6, P294, DOI 10.1134/S1819714012040021; Kirillova G. L., 2012, BUREYA SEDIMENTARY B; Marinov VA, 2019, RUSS J PAC GEOL, V13, P390, DOI 10.1134/S1819714019040043; [Маринов Владимир Аркадьевич Marinov Vladimir Arkad''evich], 2005, [Тихоокеанская геология, Russian Journal of Pacific Geology, Tikhookeanskaya geologiya], V24, P95; Medvedeva SA, 2014, RUSS J PAC GEOL, V8, P300, DOI 10.1134/S1819714014040058; Petruk N. N., 2009, SER FAR E SHEET; Riding J.B., 1999, American Association of Stratigraphic Palynologists Contributions Series, V36, P1; Sei I. I., 2004, MESOZOIC FAUNA RUSSI; Sei I. I., 1980, BIOSTRATIGRAPHY LOWE; Sharovskaya N. V., 1958, COLLECTION SCI PAPER, P31; Sharueva L. I., 2016, SER FAR E SHEET; Vaskin A. F., 2009, SER FAR E SHEET	18	1	1	0	0	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1028-334X	1531-8354		DOKL EARTH SCI	Dokl. Earth Sci.	MAY	2023	510	1					293	297		10.1134/S1028334X23600147	http://dx.doi.org/10.1134/S1028334X23600147			5	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	G7QJ9					2025-03-11	WOS:000991057500010
J	Kietzmann, DA; Sturlesi, MA				Kietzmann, Diego A.; Sturlesi, Magli A.			Upper Valanginian-Hauterivian calcareous dinoflagellate cyst and calpionellid zones from the Agrio Formation (Neuqu′en Basin), Argentina	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Calcareous dinocysts; Calpionellids; Biostratigraphy; Lower cretaceous; Agrio	JURASSIC-CRETACEOUS TRANSITION; VACA MUERTA FORMATION; JURASSIC/CRETACEOUS BOUNDARY; TITHONIAN CHITINOIDELLIDS; PELAGIC CARBONATES; PILMATUE MEMBER; UPPER AUSTRIA; BIOSTRATIGRAPHY; MICROFACIES; CARPATHIANS	In this paper we describe for the first time the calcareous dinoflagellate cysts and calpionellid associations from upper Valanginian-Hauterivian orbital-driven rhythmic distal ramp deposits (Agrio Formation) in the Neuque ' n Basin, Argentina. Three stratigraphic sections from the northern Neuque ' n province (Loma La Torre and El Port ' on) and southern Mendoza province (Arroyo Loncoche) were studied. The Agrio Formation contains a low diverse association of these microfossils, among which ten calcareous dinoflagellate cyst species and five calpionellid species were recognized, all of them known from the Lower Cretaceous pelagic sediments of the Tethyan region. Two calcareous dinoflagellate cyst zones (Carpistomiosphaera valanginiana, and Stomiosphaera echinata), as well one calpionellid zone (Tintinnopsella), previously proposed for the Tethyan realm, are confirmed for the Agrio Formation. These zones are consistent to late Valanginian - Hauterivian age assignments previously established based on ammonites, nannofossils, and organic-walled dinoflagellate cysts.	[Kietzmann, Diego A.; Sturlesi, Magli A.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, RA-1428 Buenos Aires, Argentina; [Kietzmann, Diego A.; Sturlesi, Magli A.] Univ Buenos Aires, CONICET, Inst Geociencias Basicas Ambientales & Aplicadas, Buenos Aires, Argentina	University of Buenos Aires; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Kietzmann, DA (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, RA-1428 Buenos Aires, Argentina.	diegokietzmann@gl.fcen.uba.ar	Kietzmann, Diego/S-4549-2019	Kietzmann, Diego Alejandro/0000-0003-1222-7811	Agencia Nacional de Promoci ' on Cientifica y Tecnol ' ogica of Argentina [PICT 2018-02492]	Agencia Nacional de Promoci ' on Cientifica y Tecnol ' ogica of Argentina(ANPCyT)	We acknowledge the Agencia Nacional de Promoci ' on Cientifica y Tecnol ' ogica of Argentina for financing this research by means the PICT 2018-02492 project. We also thanks to Graciela S. Bressan, Sebastian Paulin, Sebastian Saavedra, Franco Palazzolo and Ricardo Grille for assistant during fieldwork. We appreciate the editorial handling of Dr. Francisco Vega and the comments of two anonymous reviewers that allowed to improve the original version of the manuscript.	Aguado R, 2000, CRETACEOUS RES, V21, P1, DOI 10.1006/cres.2000.0198; Aguirre-Urreta B, 2019, GONDWANA RES, V70, P104, DOI 10.1016/j.gr.2019.01.006; Aguirre-Urreta B, 2017, CRETACEOUS RES, V75, P193, DOI 10.1016/j.cretres.2017.03.027; Aguirre-Urreta B, 2015, GEOL MAG, V152, P557, DOI 10.1017/S001675681400082X; Aguirre-Urreta B, 2012, CRETACEOUS RES, V35, P208, DOI 10.1016/j.cretres.2012.01.001; Aguirre-Urreta M. 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J	Li, QD; Li, PF; Duan, SS; Liu, CY; Xie, LJ; Yang, GP				Li, Qin-Dao; Li, Pei-Feng; Duan, Shan-Shan; Liu, Chun-Ying; Xie, Li-Jun; Yang, Gui-Peng			Effects of elevated temperature and acidification on sulfate assimilation and reduction of microalgae	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Temperature; Acidification; Sulfate assimilation and reduction; Phaeodactylum tricornutum; Amphidinium carterae	DIATOM THALASSIOSIRA-PSEUDONANA; DIMETHYL SULFIDE; DIMETHYLSULFONIOPROPIONATE DMSP; PHOTOCHEMICAL TRANSFORMATION; OCEANIC PHYTOPLANKTON; PHAEOCYSTIS GLOBOSA; EMILIANIA-HUXLEYI; SULFUR; BIOSYNTHESIS; GROWTH	Increased temperature and acidification are two important environmental factors affecting algal growth in marine ecosystems with the increase of atmospheric CO2. The dinoflagellate Amphidinium carterae and the diatom Phaeodactylum tricornutum were chosen to study the effect of warming and acidification on their sulfate assimilation and reduction processes by continuous incubation at different temperatures (15, 20 and 25 degrees C) and pH(NBS) values (8.10, 7.80 and 7.60). Variations in associated sulfur compounds, namely sulfate, dimethylsulfoniopropionate (DMSP), dimethylsulfide (DMS) and acrylic acid (AA) were observed. The largest sulfate uptake was at 25 degrees C for A. carterae and at 20 degrees C for P. tricornutum, however, the optimal growth temperature for both microalgae was 20 degrees C. The release of DMSP and DMS decreased in A. carterae while they increased in P. tricornutum under the condition of increased temperature. Seawater acidification increased the uptake of sulfate and promoted the growth of the microalgae. Acidification also reduced the release of DMSP, dissolved DMSP (DMSPd), DMS and AA from A. carterae with mean values of 55%, 22%, 9% and 40%, respectively. However, acidification increased the release of DMSP and DMSPd by P. tricornutum with mean values of 44% and 186%, the release of DMS was inhibited (25%) and with no significant difference in the release of AA (2%). Amino acids were found to inhibit the uptake of sulfate by the two microalgae, and the inhibitory effect of cysteine was found to be stronger than that of methionine. The inhibitory effect of amino acids was temperature sensitive and relatively weak at 20 degrees C. Besides, acidification could enhance the inhibitory effect and was evident in A. carterae. The sulfur metabolism intermediates (cysteine and methionine) have a feedback regulation effect on the sulfate absorption process of algae.	[Li, Qin-Dao; Li, Pei-Feng; Duan, Shan-Shan; Liu, Chun-Ying; Xie, Li-Jun; Yang, Gui-Peng] Ocean Univ China, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Key Lab Marine Chem Theory & Technol, Minist Educ, 238 Songling Rd, Qingdao 266100, Peoples R China; [Li, Qin-Dao; Li, Pei-Feng; Duan, Shan-Shan; Liu, Chun-Ying; Xie, Li-Jun; Yang, Gui-Peng] Ocean Univ China, Coll Chem & Chem Engn, 238 Songling Rd, Qingdao 266100, Peoples R China; [Li, Qin-Dao; Liu, Chun-Ying; Xie, Li-Jun; Yang, Gui-Peng] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China	Ocean University of China; Ocean University of China; Laoshan Laboratory	Liu, CY (通讯作者)，Ocean Univ China, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Key Lab Marine Chem Theory & Technol, Minist Educ, 238 Songling Rd, Qingdao 266100, Peoples R China.; Liu, CY (通讯作者)，Ocean Univ China, Coll Chem & Chem Engn, 238 Songling Rd, Qingdao 266100, Peoples R China.; Liu, CY (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.	roseliu@ouc.edu.cn	Yang, Gui-Peng/GZG-6468-2022; Li, Peifeng/E-9421-2015; Xie, li/HGE-6052-2022		Natural Science Foundation of Shandong Province, China [ZR2021MD113]; National Key Research and Development Program of China [2016YFA0601301]; National Natural Science Foundation of China [41676065]	Natural Science Foundation of Shandong Province, China(Natural Science Foundation of Shandong Province); 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))	This work was financially supported by the Natural Science Foundation of Shandong Province, China (ZR2021MD113), the National Key Research and Development Program of China (No 2016YFA0601301) and the National Natural Science Foundation of China (No. 41676065)	Alcolombri U, 2015, SCIENCE, V348, P1466, DOI 10.1126/science.aab1586; ANDREAE MO, 1985, J GEOPHYS RES-ATMOS, V90, P2891, DOI 10.1029/JD090iD07p12891; Archer SD, 2009, MAR ECOL PROG SER, V394, P111, DOI 10.3354/meps08284; Bajt O, 1997, MAR CHEM, V58, P255, DOI 10.1016/S0304-4203(97)00052-2; Bell TG, 2010, GLOBAL BIOGEOCHEM CY, V24, DOI 10.1029/2009GB003617; Berge T, 2010, MAR ECOL PROG SER, V416, P79, DOI 10.3354/meps08780; BIEDLINGMAIER S, 1989, Z NATURFORSCH C, V44, P495; Bochenek M, 2013, NEW PHYTOL, V199, P650, DOI 10.1111/nph.12303; Boucher O, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2001GL014048; Bowler C, 2010, ANNU REV MAR SCI, V2, P333, DOI 10.1146/annurev-marine-120308-081051; Boyd PW, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0063091; BRETON A, 1977, J BACTERIOL, V132, P224, DOI 10.1128/JB.132.1.224-232.1977; Caldeira K, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002671; CHALLENGER F, 1948, J CHEM SOC, P1591, DOI 10.1039/jr9480001591; CHARLSON RJ, 1987, NATURE, V326, P655, DOI 10.1038/326655a0; Curson ARJ, 2018, NAT MICROBIOL, V3, P430, DOI 10.1038/s41564-018-0119-5; Curson ARJ, 2017, NAT MICROBIOL, V2, DOI 10.1038/nmicrobiol.2017.9; Curson ARJ, 2011, NAT REV MICROBIOL, V9, P849, DOI 10.1038/nrmicro2653; DACEY JWH, 1987, GEOPHYS RES LETT, V14, P1246, DOI 10.1029/GL014i012p01246; DACEY JWH, 1986, SCIENCE, V233, P1314, DOI 10.1126/science.233.4770.1314; DEANE EM, 1975, ARCH MICROBIOL, V105, P295, DOI 10.1007/BF00447149; Deng LiMing Deng LiMing, 2009, China Tropical Medicine, V9, P363; EPPLEY RW, 1972, FISH B-NOAA, V70, P1063; Evans C, 2006, LIMNOL OCEANOGR, V51, P2468, DOI 10.4319/lo.2006.51.5.2468; Galí M, 2015, GLOBAL BIOGEOCHEM CY, V29, P496, DOI 10.1002/2014GB004940; Galí M, 2015, REMOTE SENS ENVIRON, V171, P171, DOI 10.1016/j.rse.2015.10.012; Gárate-Lizárraga I, 2019, MAR POLLUT BULL, V146, P532, DOI 10.1016/j.marpolbul.2019.06.073; Garren M, 2014, ISME J, V8, P999, DOI 10.1038/ismej.2013.210; GIOVANELLI J, 1978, J BIOL CHEM, V253, P5665; Goldman JAL, 2017, PHOTOSYNTH RES, V132, P83, DOI 10.1007/s11120-016-0330-2; GREEN LS, 1988, J BACTERIOL, V170, P583, DOI 10.1128/jb.170.2.583-587.1988; GREENE RC, 1962, J BIOL CHEM, V237, P2251; Gross M, 2012, CURR BIOL, V22, pR581, DOI 10.1016/j.cub.2012.07.041; Guillard R. 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Appl. Phycol.	AUG	2023	35	4					1603	1619		10.1007/s10811-023-02972-7	http://dx.doi.org/10.1007/s10811-023-02972-7		APR 2023	17	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	M6VI8					2025-03-11	WOS:000980146300005
J	Coussin, V; Penaud, A; Combourieu-Nebout, N; Peyron, O; Sicre, MA; Tisnérat-Laborde, N; Cattaneo, A; Babonneau, N				Coussin, V; Penaud, A.; Combourieu-Nebout, N.; Peyron, O.; Sicre, M. A.; Tisnerat-Laborde, N.; Cattaneo, A.; Babonneau, N.			Land-sea linkages on the Algerian Margin over the last 14 kyrs BP: Climate variability at orbital to centennial timescales	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Holocene; Dinocysts; Pollen; Biomarkers; oy analysis; Algerian Current	WESTERN MEDITERRANEAN SEA; GLACIAL-INTERGLACIAL TRANSITION; WALLED DINOFLAGELLATE CYSTS; LEVANTINE INTERMEDIATE WATER; RECENT MARINE-SEDIMENTS; NORTH-ATLANTIC CLIMATE; HIGH-RESOLUTION RECORD; EASTERN ALBORAN-SEA; HOLOCENE CLIMATE; PLANKTONIC-FORAMINIFERA	Past and present environmental conditions over the Holocene along the Algerian coast involve complex atmosphere-hydrosphere-biosphere interactions and anthropogenic activities on adjacent watersheds. Atlantic Ocean surface waters entering the western Mediterranean Sea at the Gibraltar Strait create the Algerian Current, which flows along the North African coast in a succession of strong and large-scale eddies. Deep-water upwelling plumes are other recurrent hydrological features of the Algerian margin affecting regional environmental features. However, vegetation and paleohydrological changes that have occurred over the Holocene have not yet been described. To bridge this gap, a suite of paleoclimate proxies was analysed in marine core MD04-2801 (2067 m water depth) at a secular-scale resolution over the last 14 kyrs BP. Terrestrial (pollen grains) and marine (dinoflagellate cysts or dinocysts) palynological assemblages, as well as sedimentological (grain-size analysis and XRD-based quantitative analysis of clay minerals) and biomarkers (alkenones and n-alkanes), were determined to explore the links between past sea surface hydrological conditions and regional environmental changes on nearby watersheds.The over-representation of heterotrophic dinocyst taxa (Brigantedinium spp.) indicates strong planktonic productivity in the study area. Results shows that the links between dryness on land and surface hydrological conditions are expressed by: (i) recurrent upwelling cells during the relatively dry climate conditions of the Younger Dryas (12.7 to 11.7 ka BP), the Early Holocene (11.7 to 8.2 ka BP) and from 6 ka BP onwards, (ii) enhanced fluvial discharges between 8.2 and 6 ka BP during the African Humid Period concomitant with the colonization of coastal lands by Mediterranean forest. Middle to Late Holocene transition around 4.2 ka BP characterizes by the intense event reffered to here as the Algerian Mega Drought (4.3 to 3.9 ka BP).	[Coussin, V; Penaud, A.; Cattaneo, A.; Babonneau, N.] Univ Brest, CNRS, UMR 6538, Geoocean,Ifremer, F-29280 Plouzane, France; [Combourieu-Nebout, N.] Museum Hist Nat, HPNP, CNRS, UMR 7194,Dept Prehist, F-75013 Paris, France; [Peyron, O.] Univ Montpellier 2, Inst Sci Evolut Montpellier ISEM, UMR 5554, CNRS, F-34095 Montpellier 05, France; [Sicre, M. A.] Sorbonne Univ, LOCEAN, CNRS, Campus Pierre & Marie Curie, F-75005 Paris, France; [Tisnerat-Laborde, N.] UVSQ CNRS CEA, UMR 8212, LSCE IPSL, Lab Sci Climat & Environm, Ave Terrasse, F-91198 Gif Sur Yvette, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ifremer; Universite de Bretagne Occidentale; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CEA; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay	Coussin, V; Penaud, A (通讯作者)，Univ Brest, CNRS, UMR 6538, Geoocean,Ifremer, F-29280 Plouzane, France.	vincent.coussin@univ-brest.fr; aurelie.penaud@univ-brest.fr	Marie-Alexandrine, Sicre/AAR-1516-2020; Cattaneo, Antonio/A-7344-2010; Penaud, Aurelie/F-2485-2011	Cattaneo, Antonio/0000-0001-5247-9138; Sicre, Marie-Alexandrine/0000-0002-5015-1400; Penaud, Aurelie/0000-0003-3578-4549	Region Bretagne; UBO (Univ Brest); French national programme (CNRS) LEFE-EC2CO ("DATAPOL"); ISblue project [ANR-17-EURE-0015]; French government under the program "Investissements d'Avenir"; INSU-Mistrals Progam-PaleoMex part	Region Bretagne(Region Bretagne); UBO (Univ Brest); French national programme (CNRS) LEFE-EC2CO ("DATAPOL"); ISblue project; French government under the program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR)); INSU-Mistrals Progam-PaleoMex part	This work was part of a PhD thesis (V.C.) financed by the Region Bretagne and UBO (Univ Brest) . The work was supported by the French national programme (CNRS) LEFE-EC2CO ("DATAPOL") and by the ISblue project, Interdisciplinary graduate school for the blue planet (ANR-17-EURE-0015), co-funded by a grant from the French government under the program "Investissements d'Avenir". The work was also supported by the INSU-Mistrals Progam-PaleoMex part. We thank Yannick Miras for his help in Non Pollen Palynomorph determination and discussions on their ecological signature. Thanks also to ISEM for their contribution.	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JUL 1	2023	621								111562	10.1016/j.palaeo.2023.111562	http://dx.doi.org/10.1016/j.palaeo.2023.111562		APR 2023	25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	Q1KK1		Green Submitted			2025-03-11	WOS:001055172600001
J	Lloyd, JM; Ribeiro, S; Weckström, K; Callard, L; Cofaigh, C; Leng, MJ; Gulliver, P; Roberts, DH				Lloyd, J. M.; Ribeiro, S.; Weckstrom, K.; Callard, L.; Cofaigh, C.; Leng, M. J.; Gulliver, P.; Roberts, D. H.			Ice-ocean interactions at the Northeast Greenland Ice stream (NEGIS) over the past 11,000 years	QUATERNARY SCIENCE REVIEWS			English	Article						Holocene; Paleoceanography; Greenland; Foraminifera; Dinocysts; Sedimentology; Marine cores	PALAEO SEA-ICE; BENTHIC FORAMINIFERA; LATE QUATERNARY; WATER MASSES; ARCTIC-OCEAN; FRAM STRAIT; DISKO BUGT; ATLANTIC; HOLOCENE; SHELF	Recent observations have identified increased mass loss from Greenland marine-terminating outlet glaciers (MTOG) with implications for global sea-level rise and wider ocean circulation. The flow of Atlantic-sourced waters to the Greenland margin is thought to be a major control on MTOG behaviour. Investigation of longer-term records of the role of Atlantic-sourced waters on MOTG dynamics are needed to improve understanding of potential future trends in MTOG behaviour. Here we present a multi-proxy study (benthic and planktic foraminifera, dinoflagellate cysts, diatoms, stable isotopes, sea ice biomarkers and sedimentological analyses) from core PS100-198 on the northeast Greenland shelf to investigate the interaction between the Northeast Greenland Ice Stream (NEGIS) and ocean circulation through the Holocene. Proximal glaciomarine conditions at the base of the core indicate deglaciation before 10.9 ka cal BP with the relatively warm Atlantic Water present through advection of the Return Atlantic Current (RAC) across the shelf. The advection of RAC increased through the early Holocene reaching peak subsurface warmth from 8 to 9 ka cal BP. Surface conditions at this time were charac-terised by heavy sea-ice cover. During the mid-to late Holocene (c. 7e2 ka cal BP) advection of RAC weakened with cooler subsurface waters, but with an amelioration of surface conditions characterised by seasonal sea ice. From c. 2 ka cal BP, during the late Holocene, surface conditions continued to improve with continued seasonal sea-ice cover while subsurface proxies record an increase in RAC advection. The last c. 100 years represent the most ameliorated surface conditions through the Holocene and with subsurface conditions as warm as the early Holocene peak. This coincided with the final break up of ice within 79N fjord and retreat of NEGIS to the Holocene minimum position. Current conditions, therefore, suggest the present-day ice shelf within 79N fjord is most likely susceptible to collapse in the near future. This study highlights the critical influence of Atlantic-sourced waters on the dynamics of major Greenland MTOGs.(c) 2023 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).	[Lloyd, J. M.; Cofaigh, C.; Roberts, D. H.] Univ Durham, Dept Geog, Durham DH1 3LE, England; [Ribeiro, S.; Weckstrom, K.] Geol Survey Denmark & Greenland, Glaciol & Climate Dept, DK-1350 Copenhagen, Denmark; [Weckstrom, K.] Univ Helsinki, Fac Biol & Environm Sci, Ecosyst & Environm Res Programme ECRU, POB 65 Vikinkaari 1, Helsinki 00014, Finland; [Callard, L.] Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne NE1 7RJ, England; [Leng, M. J.] British Geol Survey, Natl Environm Isotope Facil, Keyworth NG12 5GG, England; [Leng, M. J.] Univ Nottingham, Sch Biosci, Loughborough LE12 5RD, England; [Gulliver, P.] NERC Radiocarbon Facil, East Kilbridge G75 0QF, England	Durham University; Geological Survey Of Denmark & Greenland; University of Helsinki; Newcastle University - UK; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Nottingham	Lloyd, JM (通讯作者)，Univ Durham, Dept Geog, Durham DH1 3LE, England.	J.M.Lloyd@durham.ac.uk	Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018	Ribeiro, Sofia/0000-0003-0672-9161; Weckstrom, Kaarina/0000-0002-3889-0788	AWI [AWI_PS100_01, AWI_PS109_03]; NERC Standard Grant [NE/N011228/1, IP-1816-0618]; NERC [NRCF010001]; Independent Research Council Denmark [9064-00 039B]; (University of Helsinki and Stockholm University); NERC [bgs06003, NE/N011228/1, NRCF010001] Funding Source: UKRI	AWI; NERC Standard Grant(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Independent Research Council Denmark; (University of Helsinki and Stockholm University); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We thank Captains Schwarze and Wunderlich and the crew of RV Polarstern (cruises PS100 and PS109) for excellent support and cooperation during both cruises. We thank Torsten Kanzow (Chief Scientist on cruises PS100 and PS109) for help and support during the both cruises. We thank AWI for support with radiocarbon dating of small samples using the AWI MICADAS system. We gratefully acknowledge support from AWI for ship time via grants AWI_PS100_01 and AWI_PS109_03. Guillaume Mass?e and Caroline Guilmette are kindly thanked for the IP25 data. This work was funded by NERC Standard Grant NE/N011228/1. Additional support was provided through the NERC National Environmental Isotope Facility for stable isotope analyses (grant IP-1816-0618, analyses performed by Hilary Sloane, BGS) and NERC Radiocarbon Facility NRCF010001 (allocation number 2113.0418) . We acknowledge expertise of Dr Xiaomei Xu performing measurements at the KECK Carbon Cycle AMS Facility, University of California. SR received financial support from the Independent Research Council Denmark (grant nr. 9064-00 039B) and KW from Arctic Avenue (spearheadresearch project between the University of Helsinki and Stockholm University) .	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Sci. Rev.	MAY 15	2023	308								108068	10.1016/j.quascirev.2023.108068	http://dx.doi.org/10.1016/j.quascirev.2023.108068		APR 2023	19	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	F9BG7		Green Published, Green Accepted, hybrid			2025-03-11	WOS:000985221200001
J	Peyrot, D; Ibilola, O; Martin, SK; Thomas, CM; Olierook, HKH; Mory, AJ				Peyrot, Daniel; Ibilola, Olaoluwa; Martin, Sarah K.; Thomas, Charmaine M.; Olierook, Hugo K. H.; Mory, Arthur J.			Valanginian-Hauterivian vegetation inferred from palynological successions from the southern Perth Basin, Western Australia	CRETACEOUS RESEARCH			English	Article						Lower cretaceous; Palynology; Vegetation; Araucariaceae; Podocarpaceae	NORTHERN CARNARVON BASIN; ALEXANDER-ISLAND; BREAKUP; ASSEMBLAGES; ANTARCTICA; DIVERSITY; GONDWANA; DIVERSIFICATION; EPIPHYTISM; CONIFERS	The stepwise fragmentation of Gondwana had a lasting impact on Southern Hemisphere ecosystems, but its consequences remain difficult to ascertain without detailed knowledge of the biota colonizing the supercontinent before and during breakup. This palynological study characterizes the Early Cretaceous vegetation of the southern Perth Basin, a key location during the separation of Greater India from Western Australia. The well-preserved palynological assemblages recorded here include marine and putative freshwater dinoflagellate cysts and diverse spore and pollen associations. The palynomorphs indicate lacustrine, fluvial and estuarine depositional settings in the southern Perth Basin between the Berriasian and Hauterivian. The estuarine assemblages are characterized by rare to common marine dinoflagellate cysts, which indicate the early stages of marine deposition, conditions that later prevailed across most of the basin. The Early Cretaceous vegetation of the study area, as inferred from spores and pollen, is interpreted to consist mainly of conifer forests dominated by Araucariaceae, Podocarpaceae and Cheirolepidiaceae with an understory of ferns (Osmundaceae, Schizaeaceae) and other spore-producers (clubmosses, mosses, liverworts and hornworts). Two vegetation-types are hypothesized for the region with their distribution related to substrate characteristics and water availability: a more mesic, struc-turally complex, riverine forest within paleovalleys and topographic lows, and a more open forest accross the hinterland. (c) 2023 Elsevier Ltd. All rights reserved.	[Peyrot, Daniel] Univ Western Australia, Sch Earth Sci, 35 Stirling Highway, Perth, WA 6009, Australia; [Ibilola, Olaoluwa] 12 Koeanig Way, Clarkson, WA 6030, Australia; [Martin, Sarah K.; Thomas, Charmaine M.; Mory, Arthur J.] Ind Regulat & Safety, Dept Mines, 100 Plain St, Perth, WA 6004, Australia; [Olierook, Hugo K. H.] Curtin Univ, Inst Geosci Res, Sch Earth & Planetary Sci, GPO Box U1987, Perth, WA 6845, Australia; [Olierook, Hugo K. 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AUG	2023	148								105504	10.1016/j.cretres.2023.105504	http://dx.doi.org/10.1016/j.cretres.2023.105504		APR 2023	17	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	F5DM6					2025-03-11	WOS:000982551900001
J	Mansour, A; Tahoun, SS; Raafat, A; Ahmed, MS; Oboh-Ikuenobe, F; Gentzis, T; Fu, XG				Mansour, Ahmed; Tahoun, Sameh S.; Raafat, Aya; Ahmed, Mohamed S.; Oboh-Ikuenobe, Francisca; Gentzis, Thomas; Fu, Xiugen			Organic Matter Assessment and Paleoenvironmental Changes of the Middle Jurassic Main Source Rocks (Khatatba Formation) in the North Western Desert, Egypt: Palynofacies and Palynomorph Perspectives	MINERALS			English	Article						organic matter characterization; kerogen types; palynomorph composition; Matruh Basin; Shushan Basin; Dahab-Mireir Basin	DINOFLAGELLATE CYSTS; SHUSHAN BASIN; ALGARVE BASIN; MATRUH BASIN; BIOSTRATIGRAPHY; SUCCESSION; EVOLUTION; INVERSION; AFRICA; SYSTEM	The Middle Jurassic in the north Western Desert, Egypt, was a time of complex tectonics and increased environmental perturbations attributed to the predominant sedimentation of organic carbon-rich fine siliciclastic and carbonate deposits of the Khatatba Formation. Although some studies have addressed the hydrocarbon potential and source rock characteristics of the Khatatba Formation, a regional-scale investigation of the prevalent paleoenvironmental conditions and organic matter characteristics is still necessary. In this study, the Khatatba Formation is investigated for detailed palynofacies analysis and palynomorph composition to assess organic matter kerogen types and reconstruct the depositional paleoenvironmental patterns on a regional scale. For this purpose, 116 drill cuttings were collected from five wells in the Matruh, Shushan, and Dahab-Mireir Basins. Moderately diverse assemblages of spores, pollen, and dinoflagellate cysts are reported. Age-diagnostic dinoflagellate cysts, including Adnatosphaeridium caulleryi, Dichadogonyaulax sellwoodii, Korystocysta gochtii, Wanaea acollaris, and Pareodinia ceratophora, along with occasional records of Systematophora areolate and Systematophora penicillate, defined a Bajocian-Callovian age. Based on particulate organic matter (POM) composition, four palynofacies assemblages (PFAs) are identified. PFA-1 is the most common within the Khatatba Formation in the five studied wells. It contains high proportions of phytoclast fragments versus low contents of amorphous organic matter (AOM) and palynomorphs and is defined by a gas-prone kerogen Type III. PFA-2 is comprised of moderate abundances of AOM and phytoclast characteristics of oil-prone kerogen Type II. PFA-3 is dominated by phytoclasts and moderate to low proportions of AOM and palynomorphs of kerogen Type III, whereas PFA-4 consists of AOM and palynomorphs defining kerogen Type II. PFA-1 indicates predominant deposition in proximal active fluvio-deltaic sources to marginal marine conditions with enhanced contributions of terrestrial/riverine influx. PFA-2 and PFA-3 reveal deposition under an enhanced dysoxic to anoxic proximal inner neritic shelf due to the abundant occurrences of spores and coastal to shallow marine dinoflagellate cysts. PFA-4 suggests deposition under enhanced suboxic to anoxic distal inner neritic conditions because of enhanced AOM and abundant proximate and some chorate dinoflagellate cysts. Thus, the Middle Jurassic experienced a predominantly marginal to shallow water column in this part of the southern margin of the Tethyan Ocean where the Matruh, Shushan, and Dahab-Mireir Basins were located.	[Mansour, Ahmed; Fu, Xiugen] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610500, Peoples R China; [Mansour, Ahmed; Fu, Xiugen] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Tahoun, Sameh S.; Raafat, Aya] Cairo Univ, Fac Sci, Geol Dept, Giza 12613, Egypt; [Ahmed, Mohamed S.] King Saud Univ, Coll Sci, Geol & Geophys Dept, Riyadh 11451, Saudi Arabia; [Oboh-Ikuenobe, Francisca] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA; [Gentzis, Thomas] Core Labs Inc, 6316 Windfern Rd, Houston, TX 77040 USA	Southwest Petroleum University; Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; Egyptian Knowledge Bank (EKB); Cairo University; King Saud University; University of Missouri System; Missouri University of Science & Technology	Gentzis, T (通讯作者)，Core Labs Inc, 6316 Windfern Rd, Houston, TX 77040 USA.	ahmedmans48@mu.edu.eg; stahoun@cu.edu.eg; ayar210@yahoo.com; mohahmed@ksu.edu.sa; ikuenobe@mst.edu; thomas.gentzis@corelab.com	Ahmed, Mohamed/GQP-1116-2022; Mansour, Ahmed/AAR-4969-2020; Raafat, Aya/AHE-3464-2022	Mansour, Ahmed/0000-0003-2466-7494; Oboh-Ikuenobe, Francisca/0000-0002-2223-9691; Ahmed, Mohamed/0000-0001-9249-6231; Gentzis, Thomas/0000-0003-4592-9318	King Saud University, Riyadh, Saudi Arabia [RSP2023R455]	King Saud University, Riyadh, Saudi Arabia(King Saud University)	This work was funded by Researchers Supporting project number (RSP2023R455), King Saud University, Riyadh, Saudi Arabia.	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J	Targhi, S; Barhoun, NB; Taoufiq, NB; Achab, M; Essamoud, R; Bahaj, H; Rahmouna, J; Berry, N				Targhi, Soukaina; Barhoun, Nadia B.; Taoufiq, Naima Bachiri; Achab, Mohamed; Essamoud, Rachid; Bahaj, Hanane; Rahmouna, Jihad; Berry, Naima			Late Miocene biostratigraphy and paleoenvironment New insights from the Moulay Yakoub area	CARNETS DE GEOLOGIE			English	Article						Late Miocene; Foraminifera; palynology; paleoenvironment; Sais Basin; southern Rifian; Morocco	RIFIAN CORRIDOR MOROCCO; SEA-SURFACE CONDITIONS; TORTONIAN-MESSINIAN BOUNDARY; DINOFLAGELLATE CYSTS; SALINITY CRISIS; GUERCIF BASIN; INTEGRATED STRATIGRAPHY; BETIC CORDILLERA; ATLANTIC; NORTH	During the Late Miocene, the Rifian Corridor was one of the two main corridors allowing ex-changes between the Atlantic and the Mediterranean Seas. Sedimentary records accumulated along this corridor and specifically, in the Sais Basin, constitute case-study material for understanding the impact of the South Rifian Corridor on the evolution of the fauna, phytoplankton and environment dur-ing the Late Miocene. In order to reconstruct the evolution of marine paleoenvironments in the Moulay Yakoub region and to compare this evolution with other areas of the Sais basin, we conducted an inte-grated biostratigraphic and palynological study of the Upper Miocene of borehole KA 102. High -resolu-tion biostratigraphy based on planktonic foraminifera revised and defined the chronostratigraphic framework of the Upper Miocene sedimentary series of the Moulay Yakoub region providing an age of 7.8 Ma to 6.52 Ma (Late Tortonian to Early Messinian). In the Late Tortonian, the planktonic foraminif-eral assemblages suggest an open and relatively deep marine environment. At the Tortonian/Messinian boundary, planktonic foraminiferal and dinoflagellate associations, as well as distal indices, suggest a relatively deep and neritic distal marine environment with a decrease in diversity and an increase in re-worked taxa. Surface waters are warm with a minor cooling trend observed just below this boundary. In comparison to previously studied sections in the Sais Basin, the Lower Messinian is characterized by a deeper and more distal marine environment. However, proximal trends and warm surface water con-ditions persisted in all studied areas from the basin during this period.	[Targhi, Soukaina; Barhoun, Nadia B.; Taoufiq, Naima Bachiri; Essamoud, Rachid; Bahaj, Hanane; Rahmouna, Jihad; Berry, Naima] Hassan II Univ, Fac Sci Ben Msick Casablanca, Lab Geosci & Applicat, BP 7955, Sidi Othmane, Casablanca, Morocco; [Achab, Mohamed] Univ Mohammed V Rabat, Sci Inst, Ave Ibn Batouta,BP 703, Rabat 10106, Morocco	Hassan II University of Casablanca; Mohammed V University in Rabat	Targhi, S; Barhoun, NB (通讯作者)，Hassan II Univ, Fac Sci Ben Msick Casablanca, Lab Geosci & Applicat, BP 7955, Sidi Othmane, Casablanca, Morocco.	targhi.sokaina@gmail.com; nadia.barhoun@univh2c.ma						ABDELKHALIKI L., 1997, THESIS U MOHAMMED 5; Achalhi M, 2016, PALAEOGEOGR PALAEOCL, V459, P131, DOI 10.1016/j.palaeo.2016.06.040; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; BACHIRI TAOUFIQ N., 2000, THESIS U HASSAN 2 MO; BARGACH K., 2011, THESIS U MOHAMMED 5; BARHOUN N., 2000, THESIS U HASSAN 2 MO; Barhoun N, 2008, GEODIVERSITAS, V30, P21; Barhoun Nadia, 1999, Revue de Paleobiologie, V18, P491; Be A. 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APR 1	2023	23	4					53	75		10.2110/carnets.2023.2303	http://dx.doi.org/10.2110/carnets.2023.2303			23	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	D4RV2					2025-03-11	WOS:000968629500001
J	Winantris; Rosana, MF; Sena, K				Winantris; Rosana, Mega Fatimah; Sena, Katon			Age and Depositional Environment of the Sandstone Unit of Ciletuh Formation in Ciletuh-Palabuhanratu Geopark	INDONESIAN JOURNAL OF GEOSCIENCE			English	Article						Ciletuh-Palabuhanratu Geopark; relative age; depositional environment; palynomorphs		Sandstones form part of the Cenozoic Ciletuh Formation which is widely exposed in The Ciletuh Palabuhanratu Geopark, Indonesia. This study aims to establish the age of these sandstone units, and to evaluate their depositional environment based on palynological data. Five samples from Ciletuh sandstones were collected for palynomorph analysis. Exposed sections were measured and sampled to determine the stratigraphic position, with palynomorphs being separated from the sediment using acetolysis. Cluster analysis was applied to the resultant palynomorph assemblages and interpreted using plant association model, which refered to the depositional environment of different taxa. Two distinct clusters were identified, characterized by different environmental markers. The first cluster is dominated by Proxapertites operculatus and Proxapertites cursus, , while the second cluster is dominated by Podocarpus pollen. While the Proxapertites cluster includes Dicolpopollis kalewensis, Palmaepollenites kutchensis, , foraminiferal test linings, dinoflagellates cysts, plant debris, deposited in the marine environment. The Podocarpus cluster consists of Podocarpus pollen, plant debris, foraminiferal test linings, and dinoflagellate cysts, that was deposited in a more distal marine environment. All samples were deposited during the end of Middle Eocene (E6-zone), as defined by the age markers of Proxapertites. cursus, P. operculatus, Restioniidites punctulatus, and Podocarpus pollen. .	[Winantris; Rosana, Mega Fatimah; Sena, Katon] Univ Padjadjaran, Dept Geol, Bandung, Indonesia	Universitas Padjadjaran	Winantris (通讯作者)，Univ Padjadjaran, Dept Geol, Bandung, Indonesia.	winantris@unpad.ac.id					Age and Depositional Environment of The Sandstone Unit of Ciletuh Formation in Ciletuh-Palabuhanratu Geopark (Winantris et al.) The authors would like to thank Universitas Pa-djadjaran, which has supported us by Academic Leadership Research Grant. Special thanks to our laboratory team: Ria Fitriyani and Mr. Dayat. The authors are also very grateful to Dr. Robert J. Morley, who helped extensively with issues concerning the identification and naming of palm pollen, with age interpretation, and also interpretation of depositional environments, and many other important matters to reach the high standard of journals.	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J	Mertens, KN; Retho, M; Manach, S; Zoffoli, ML; Doner, A; Schapira, M; Bilien, G; Séchet, V; Lacour, T; Robert, E; Duval, A; Terre-Terrillon, A; Derrien, A; Gernez, P				Mertens, Kenneth Neil; Retho, Michael; Manach, Soazig; Zoffoli, Maria Laura; Doner, Anne; Schapira, Mathilde; Bilien, Gwenael; Sechet, Veronique; Lacour, Thomas; Robert, Elise; Duval, Audrey; Terre-Terrillon, Aouregan; Derrien, Amelie; Gernez, Pierre			An unprecedented bloom of<i> Lingulodinium</i><i> polyedra</i> on the French Atlantic coast during summer 2021	HARMFUL ALGAE			English	Article						Seed bank; Yessotoxins; Vilaine Bay; Southern Brittany; Harmful algal blooms	DINOFLAGELLATE CYSTS; RED-TIDE; VILAINE BAY; SEASONAL-VARIATION; PHYTOPLANKTON; EUTROPHICATION; DINOPHYCEAE; BISCAY; BRITTANY; YESSOTOXINS	At the end of July 2021, a bloom of Lingulodinium polyedra developed along the French Atlantic coast and lasted six weeks. The REPHY monitoring network and the citizen participation project PHENOMER contributed to its observation. A maximum concentration of 3,600,000 cells/L was reached on the 6th of September, a level never recorded on French coastlines. Satellite observation confirmed that the bloom reached its highest abundance and spatial extension early September, covering about 3200 km2 on the 4th of September. Cultures were established, and morphology and ITS-LSU sequencing identified the species as L. polyedra. The thecae displayed the characteristic tabulation and sometimes a ventral pore. The pigment composition of the bloom was similar to that of cultured L. polyedra, confirming that phytoplankton biomass was dominated by this species. The bloom was preceded by Leptocylindrus sp., developed over Lepidodinium chlorophorum, and was succeeded by elevated Noctiluca scintillans concentrations. Afterwards, relatively high abundance of Alexandrium tamarense were observed in the embayment where the bloom started. Unusually high precipitation during mid-July increased river discharges from the Loire and Vilaine rivers, which likely fueled phytoplankton growth by providing nutrients. Water masses with high numbers of dinoflagellates were characterized by high sea surface temperature and thermohaline stratification. The wind was low during the bloom development, before drifting it offshore. Cysts were observed in the plankton towards the end of the bloom, with concentrations up to 30,000 cysts/L and relative abundances up to 99%. The bloom deposited a seed bank, with cyst concentrations up to 100,000 cysts/g dried sediment, particularly in fine-grained sediments. The bloom caused hypoxia events, and concentrations of yessotoxins up to 747 mu g/kg were recorded in mussels, below the safety threshold of 3,750 mu g/kg. Oysters, clams and cockles also were contaminated with yessotoxins, but at lower concentrations. The established cultures did not produce yessotoxins at detectable levels, although yessotoxins were detected in the sediment. The unusual environmental summertime conditions that triggered the bloom, as well as the establishment of considerable seed banks, provide important findings to understand future harmful algal blooms along the French coastline.	[Mertens, Kenneth Neil; Doner, Anne; Bilien, Gwenael; Duval, Audrey; Terre-Terrillon, Aouregan; Derrien, Amelie] Ifremer, LITTORAL, F-29900 Concarneau, France; [Retho, Michael; Manach, Soazig] Ifremer, LITTORAL, F-56100 Lorient, France; [Zoffoli, Maria Laura] CNR, Ist Sci Marine CNR ISMAR, I-00133 Rome, Italy; [Schapira, Mathilde] Ifremer, LITTORAL, F-44300 Nantes, France; [Sechet, Veronique; Lacour, Thomas] Ifremer, PHYTOX, Lab PHYSALG, F-44000 Nantes, France; [Robert, Elise] Ifremer, PHYTOX, Lab GENALG, F-44000 Nantes, France; [Gernez, Pierre] Nantes Univ, Inst Subst & Organismes Mer, ISOMer, UR 2160, F-44000 Nantes, France	Ifremer; Ifremer; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Ifremer; Ifremer; Ifremer; Nantes Universite	Mertens, KN (通讯作者)，Ifremer, LITTORAL, F-29900 Concarneau, France.	kenneth.mertens@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Lacour, Thomas/ISB-1473-2023; Gernez, Pierre/G-8922-2011; Mertens, Kenneth/C-3386-2015	gernez, pierre/0000-0003-2055-410X; Derrien, Amelie/0000-0001-9656-7850; Retho, Michael/0000-0002-7260-5477; sechet, veronique/0000-0002-7085-3215; Zoffoli, Maria Laura/0000-0003-1892-0051; Mertens, Kenneth/0000-0003-2005-9483; Anne, DONER/0000-0002-1006-8047; Schapira, Mathilde/0000-0002-0130-9398	Sigma 300 FE-SEM - Regional Council of Brittany; Regional Council of Brittany; General Council of Finistere and the Urban Community of Concarneau-Cornouaille-Agglomeration; Centre National d'Etudes Spatiales; Region Pays de la Loire [LEPIDO-PEN [06582 2019]]; Agence de l'Eau Loire Bretagne [EPICE [180408801]]; Agence Nationale de la Recherche for France 2030 [ANR-22-POCE-0006]; H2020 RISE project EMERTOX-Emergent Marine Toxins in the North Atlantic and Mediterranean [778069]; Marie Curie Actions (MSCA) [778069] Funding Source: Marie Curie Actions (MSCA)	Sigma 300 FE-SEM - Regional Council of Brittany; Regional Council of Brittany(Region Bretagne); General Council of Finistere and the Urban Community of Concarneau-Cornouaille-Agglomeration; Centre National d'Etudes Spatiales(Centre National D'etudes Spatiales); Region Pays de la Loire(Region Pays de la Loire); Agence de l'Eau Loire Bretagne; Agence Nationale de la Recherche for France 2030(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)); H2020 RISE project EMERTOX-Emergent Marine Toxins in the North Atlantic and Mediterranean; Marie Curie Actions (MSCA)(Marie Curie Actions)	We like to thank Sylvain Ballu (CEVA) for providing the aerial photographs. The Sigma 300 FE-SEM used in this study was funded by The Regional Council of Brittany, the General Council of Finistere and the Urban Community of Concarneau-Cornouaille-Agglomeration. The authors acknowledge EUTMESAT and ESA for the Sentinel -3 observations. Part of this research was supported by the Centre National d'Etudes Spatiales (TOSCA projects LASHA and OSYNICO) , Region Pays de la Loire (project LEPIDO-PEN [06582 2019] , Agence de l'Eau Loire Bretagne (project EPICE [180408801] ) . This work benefited from a national funding through the Agence Nationale de la Recherche for France 2030 under the reference ANR-22-POCE-0006. KNM and VS acknowledge the project H2020 RISE project EMERTOX-Emergent Marine Toxins in the North Atlantic and Mediterranean: New Approaches to Assess their Occurrence and Future Scenarios in the Framework of Global Environmental Changes -Grant Agreement No. 778069. 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J	Tabara, D; Slimani, H; Chelariu, C; Bindiu-Haitonic, R; Balc, R; Csiki-Sava, Z; Fabianska, JM; Misz-Kennan, M; Chelariu, M				Tabara, Daniel; Slimani, Hamid; Chelariu, Ciprian; Bindiu-Haitonic, Raluca; Balc, Ramona; Csiki-Sava, Zoltan; Fabianska, J. Monika; Misz-Kennan, Magdalena; Chelariu, Marian			Five million years of life history record in an uppermost Cretaceous northern Tethyan marine succession, Eastern Carpathians (Romania): Microfossil content and palaeoenvironmental assessment	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinocysts; Foraminifera; Calcareous nannoplankton; Hangu Formation; Eastern Carpathians	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; WESTERN EXTERNAL RIF; AGGLUTINATED FORAMINIFERA; PALEOGENE BOUNDARY; PALEOCENE SUCCESSION; SUBSILESIAN UNIT; BASIN; EOCENE; PALYNOFACIES	New biostratigraphic investigations based on palynomorphs (mainly dinoflagellate cysts), foraminifera and calcareous nannoplankton recovered from eight geological sections indicate that the Hangu Formation near the Pluton-Pipirig area (Tarcau Nappe, Eastern Carpathians, Romania), previously assigned to the Senonian- Paleocene interval, includes only uppermost Cretaceous deposits. The palynological assemblages are moderately rich, with a total of 167 well-preserved taxa. The marine palynomorphs - essentially consisting of dinoflagellate cysts (dinocysts) - are dominated by peridinioid taxa, mainly recorded in upper Upper Campanian-lower Maastrichtian deposits, and by a high-diversity assemblage of gonyaulacoid taxa during the late Maastrichtian. Marine algae and dinogymnioid dinocysts were less common. The terrestrial palynoflora is dominated by fern spores and angiosperm pollen, with subordinate gymnosperm pollen. The foraminiferal assemblages include an assortment of well-preserved agglutinated forms, present mainly in the upper Maastrichtian deposits, whereas calcareous benthics and planktonic foraminifera are rare and poorly preserved. Calcareous nannoplank-ton assemblages are also rare, often represented by two taxa (Micula staurophora and Watznaueria barnesiae); certain important biostratigraphic markers were found to be reworked in the analyzed deposits. Age assignments for the studied sections were mainly provided by dinocysts, through the identification of significant marker taxa and comparisons with well-calibrated Campanian-Maastrichtian dinocyst assemblages from well-dated sections and stratotypes, located mostly in the Northern Hemisphere.Indices such as particulate organic matter (POM) composition, the relative abundance of dinocyst eco-groups, as well as agglutinated foraminiferal morphogroups, were used to reconstruct the depositional environments of the Hangu Formation from the studied area. The upper Upper Campanian-lower Maastrichtian deposits from the Pluton-Pipirig sections were mainly deposited in neritic marine conditions, although occasional redeposition of the sediments transported by turbidity currents towards deeper water settings is not excluded, either. The depo-sitional environments evolve towards outer neritic to distal (bathyal) during the late Maastrichtian, as indicated by palynofacies constituents and by high frequencies of gonyaulacoid dinocysts and deep-water benthic foraminifera.(c) 2023 Elsevier B.V. All rights reserved.	[Tabara, Daniel; Chelariu, Ciprian; Chelariu, Marian] Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol I Blv, Iasi 700505, Romania; [Slimani, Hamid] Mohammed V Univ Rabat, Geobiodivers & Nat Patrimony Lab GEOBIO, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Dept Geol & Remote Sensing,Sci Inst, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco; [Bindiu-Haitonic, Raluca] Babes Bolyai Univ, Dept Geol, 1 Mihail Kogalniceanu St, Cluj Napoca 400084, Romania; [Bindiu-Haitonic, Raluca] Babes Bolyai Univ, Res Ctr Integrated Geol Studies, 1 Mihail Kogalniceanu St, Cluj Napoca 400084, Romania; [Balc, Ramona] Babes Bolyai Univ, Fac Environm Sci & Engn, 30 Fantanele St, Cluj Napoca 400294, Romania; [Balc, Ramona] Babes Bolyai Univ, Interdisciplinary Res Inst Bionanosci, Treboniu Laurian 42, Cluj Napoca 400271, Romania; [Csiki-Sava, Zoltan] Univ Bucharest, Dept Geol, 1 Nicolae Balcescu Ave, Bucharest 010041, Romania; [Balc, Ramona; Csiki-Sava, Zoltan] Univ Bucharest, Ctr Risk Studies Space Modeling & Dynam Terr & Co, 1 Nicolae Balcescu Ave, Bucharest 010041, Romania; [Fabianska, J. Monika; Misz-Kennan, Magdalena] Univ Silesia Katowice, Fac Nat Sci, Bedzinska 60, PL-41200 Sosnowiec, Poland	Alexandru Ioan Cuza University; Mohammed V University in Rabat; Babes Bolyai University from Cluj; Babes Bolyai University from Cluj; Babes Bolyai University from Cluj; Babes Bolyai University from Cluj; University of Bucharest; University of Bucharest; University of Silesia in Katowice	Tabara, D; Chelariu, C (通讯作者)，Alexandru Ioan Cuza Univ, Dept Geol, 20A Carol I Blv, Iasi 700505, Romania.	dan.tabara@yahoo.com; ciprian.chelariu@uaic.ro	Bindiu-Haitonic, Raluca/AAU-5269-2021; Csiki-Sava, Zoltan/E-8695-2011; Tabara, Daniel/C-6630-2015; Balc, Ramona/D-1437-2017; Slimani, Hamid/AAL-4055-2020; Misz-Kennan, Magdalena/AAK-1845-2021; Chelariu, Ciprian/Q-3245-2018	Misz-Kennan, Magdalena/0000-0003-0475-331X; Slimani, Hamid/0000-0001-6392-1913	Ministry of Research, Innovation and Digitization, CNCS/CCCDI-UEFISCDI within PNCDI III [PN-III-P4-ID-PCE-2020-2570]; University of Bucharest [10056/2022]	Ministry of Research, Innovation and Digitization, CNCS/CCCDI-UEFISCDI within PNCDI III; University of Bucharest	This study was supported by a grant of the Ministry of Research, Innovation and Digitization, CNCS/CCCDI-UEFISCDI, project number PN-III-P4-ID-PCE-2020-2570, within PNCDI III; fieldwork in the Pluton-Pipirig area was also supported by the University of Bucharest grant 10056/2022. The journal Editor-in-Chief Jose Carrion and the anonymous reviewer are kindly thanked for their comments and suggestions that enhanced the initial manuscript.	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Palaeobot. Palynology	JUN	2023	313								104878	10.1016/j.revpalbo.2023.104878	http://dx.doi.org/10.1016/j.revpalbo.2023.104878		MAR 2023	22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	D5EG0					2025-03-11	WOS:000968957500001
J	Luostarinen, T; Weckström, K; Ehn, J; Kamula, M; Burson, A; Diaz, A; Massé, G; McGowan, S; Kuzyk, ZZ; Heikkilä, M				Luostarinen, Tiia; Weckstrom, Kaarina; Ehn, Jens; Kamula, Michelle; Burson, Amanda; Diaz, Aura; Masse, Guillaume; McGowan, Suzanne; Kuzyk, Zou Zou; Heikkila, Maija			Seasonal and habitat-based variations in vertical export of biogenic sea-ice proxies in Hudson Bay	COMMUNICATIONS EARTH & ENVIRONMENT			English	Article							DINOFLAGELLATE CYSTS; MANITOUNUK SOUND; LATE QUATERNARY; NORTH-ATLANTIC; FRESH-WATER; DIATOMS; VARIABILITY; BIOMARKER; QUEBEC; CANADA	Sedimentary assemblages of biogenic sea-ice proxies incorporate limited representation of the diverse sea-ice connected communities, according to direct springtime observations in the Belcher Islands Archipelago, Hudson Bay, Canada. Despite their wide use in past sea-ice reconstructions, the seasonal, habitat and species-based sources of sedimentary sea-ice proxies are poorly understood. Here, we conduct direct observations of the community composition of diatoms, dinoflagellate cysts and highly branched isoprenoid lipids within the sea ice, water column, sediment traps and sediment surface in the Belcher Islands Archipelago, Hudson Bay throughout spring 2019. We find that Arctic diatom and dinoflagellate cysts species commonly used as sea-ice proxies appear to be only indirectly linked to sea-ice conditions, and that the sediment assemblages of these groups overrepresent summertime pelagic blooms. Species contributing to the diverse sea-ice diatom communities are rare in the sediment. Dinoflagellate cysts form a typical Arctic assemblage in the sediment, although they are virtually absent in the sea ice and water column in spring. We also find that certain highly branched isoprenoid lipids that were previously considered indicators of open water, can be produced in sea-ice. We conclude that contextual knowledge and a multiproxy approach are necessary in reconstruction, encouraging further studies on the sources and controls of sea-ice proxy production in different geographic areas.	[Luostarinen, Tiia; Weckstrom, Kaarina; Heikkila, Maija] Univ Helsinki, Environm Change Res Unit ECRU, Ecosyst & Environm Res Programme, Fac Biol & Environm Sci, Helsinki, Finland; [Luostarinen, Tiia; Weckstrom, Kaarina; Heikkila, Maija] Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, Helsinki, Finland; [Weckstrom, Kaarina] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Copenhagen, Denmark; [Ehn, Jens; Kamula, Michelle; Diaz, Aura; Kuzyk, Zou Zou] Univ Manitoba, Ctr Earth Observat Sci, Winnipeg, MB, Canada; [Burson, Amanda] British Antarctic Survey, Cambridge, England; [Burson, Amanda; McGowan, Suzanne] Univ Nottingham, Sch Geog, Nottingham, England; [Masse, Guillaume] Univ Laval, CNRS, UMI 3376 TAKUVIK, Quebec City, PQ, Canada; [Masse, Guillaume] Stn Marine Concarneau, UMR7159, LOCEAN, Concarneau, France; [McGowan, Suzanne] Netherlands Inst Ecol NIOO KNAW, Dept Aquat Ecol, Wageningen, Netherlands	University of Helsinki; University of Helsinki; Geological Survey Of Denmark & Greenland; University of Manitoba; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of Nottingham; Laval University; Sorbonne Universite; Museum National d'Histoire Naturelle (MNHN); Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW)	Luostarinen, T (通讯作者)，Univ Helsinki, Environm Change Res Unit ECRU, Ecosyst & Environm Res Programme, Fac Biol & Environm Sci, Helsinki, Finland.; Luostarinen, T (通讯作者)，Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, Helsinki, Finland.	tiia.luostarinen@helsinki.fi	Luostarinen, Tiia/HKV-0993-2023; Heikkila, Maija/N-7659-2013	Heikkila, Maija/0000-0003-3885-8670; Weckstrom, Kaarina/0000-0002-3889-0788; Luostarinen, Tiia/0000-0002-2368-237X; Burson, Amanda/0000-0003-0729-3793; Diaz, Aura/0000-0002-7362-619X	Academy of Finland [1296895, 1307282, 1328540]; Alfred Kordelin Foundation; ArcticNet Networks of Centres of Excellence (NCE); Natural Sciences and Engineering Research Council of Canada (NSERC); Polar Knowledge Canada; Arctic Avenue; Helsinki University Library	Academy of Finland(Research Council of Finland); Alfred Kordelin Foundation; ArcticNet Networks of Centres of Excellence (NCE); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Polar Knowledge Canada; Arctic Avenue; Helsinki University Library	This study was funded by the Academy of Finland (grants 1296895, 1307282 and 1328540), The Alfred Kordelin Foundation, ArcticNet Networks of Centres of Excellence (NCE), Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery Grant Programs, Polar Knowledge Canada and Arctic Avenue. Open access was funded by Helsinki University Library. We thank Joel Heath, Johnny Kudluarok, Puasi Ippak, Johnassie Inuktaluk, Johnny Ippak, Ronnie Ippak, Charlie Novalinga, Lucy Ann Novalinga, Lucassie Arragutainaq, Arctic Eider Society, Sanikiluaq Hunters and Trappers Association, Meeri Nappila, Heini Ali-Kovero, Caroline Guilmette, Alessia Guzzi, Emmelia Stainton and Linda Chow for their valuable help. We also kindly acknowledge the helpful comments of two anonymous reviewers.	Amiraux R, 2019, ELEMENTA-SCI ANTHROP, V7, DOI 10.1525/elementa.377; Andrews JT, 2009, HOLOCENE, V19, P71, DOI 10.1177/0959683608098953; Arrigo K. 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Earth Environ.	MAR 16	2023	4	1							78	10.1038/s43247-023-00719-3	http://dx.doi.org/10.1038/s43247-023-00719-3			13	Environmental Sciences; Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Meteorology & Atmospheric Sciences	A0HL1		Green Published, Green Accepted, gold			2025-03-11	WOS:000952023600003
J	Kalanat, B; Raou, A				Kalanat, Behnaz; Raou, Ahmad			Palynological evidence for the Middle Jurassic environmental evolution in the eastern part of the Alborz Mountains (northern Iran)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Bajocian-Bathonian; Dalichai Formation; Palynofacies; Sporomorph; Dinocysts	WALLED DINOFLAGELLATE CYSTS; DALICHAI FORMATION; BASIN; SOUTH; PALYNOFACIES; BOTRYOCOCCUS; AMMONITES; BAJOCIAN; SEDIMENTARY; MODEL	The palynological assemblages of the Dalichai Formation were studied to reconstruct the paleoenvironmental evolution of the Middle Jurassic interval in the eastern part of the Alborz Mountains (N Iran). Dinoflagellate cyst biozones, planktonic foraminifera, and ammonites suggest a Bajocian-Callovian age for the Dalichai Formation. The palynodebris, mostly of terrestrial origin, are dominated by black opaque phytoclasts. Dinocysts, spores, pollen grains, and amorphous organic matters (AOM) are minor components in most samples. Terrestrial palynoflora are mainly represented by coastal gymnosperms (Araucariaceae, Cheirolepidiaceae), lowland simple monosulcate pollen producers (Cycadales/Bennettitales), ferns, upland seed ferns and conifers (Corystospermales and other bisaccate pollen producers). These assemblages indicate a warm climate with seasonally-dry conditions. However, an increase in Cheirolepidiaceae (Classopollis) in Bathonian assemblages reflects higher temperature during this interval. The dominance of the land-derived phytoclasts and presence of brackish water Botryococcus colonies with cells arranged irregularly suggest a proximal setting with high terrestrial and freshwater input during the Bajocian. The palynofacies analysis suggests a sea-level rise during the Bathonian, reflected by higher abundance and diversity of dinocysts as well as the presence of degraded small phytoclasts. This transgression phase is related to the increased subsidence of the Alborz region due to ongoing Neotethys subduction and creation of a large extensional back arc basin in the Eurasian margin. The syn-rift deposits are characterized by ammonitico rosso facies as well as hemipelagic carbonates containing planktonic foraminifera and pelagic bivalves.	[Kalanat, Behnaz] Agr Res Educ & Extens Org AREEO, Res Inst Forests & Rangelands, Palaeobot Dept, Tehran, Iran; [Raou, Ahmad] Farhangian Univ, Daneshvar Ctr, Neyshabour, Iran		Kalanat, B (通讯作者)，Agr Res Educ & Extens Org AREEO, Res Inst Forests & Rangelands, Palaeobot Dept, Tehran, Iran.	Kalanat@rifr-ac.ir	Kalanat, Behnaz/AAB-7559-2020	Kalanat, Behnaz/0000-0002-4410-3453	Research Institute of Forests and Rangelands (RIFR) , Iran [2-09-09-020-990464]	Research Institute of Forests and Rangelands (RIFR) , Iran(Research Institute of Forests & Rangelands RIFR)	The authors are greatly indebted to Dr. F. Hashemi-Yazdi of the RIFR, who kindly collaborated during this project. Our thanks also go to Editors-in-Chief for their editorial helps and two anonymous reviewers for the constructive and helpful comments that have improved the quality of this manuscript. This project was supported by the Research Institute of Forests and Rangelands (RIFR) , Iran (grant number #2-09-09-020-990464) .	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J	Sobdjou, CK; Mfayakouo, BC; Ngueutchoua, G; Kenfack, RGN; Ngos, S				Sobdjou, C. K.; Mfayakouo, B. C.; Ngueutchoua, G.; Kenfack, R. G. N.; Ngos, S.			Palaeoenvironment of the Albian-Cenomanian Mundeck Formation in the Douala Basin (SW, Cameroon): Evidence from facies analysis and geochemistry	GEOLOGICAL JOURNAL			English	Article						Douala Basin; Facies analysis; Mundeck Formation; organic matter source; palaeoenvironment; palynofacies	TECTONIC SETTING DISCRIMINATION; ORGANIC-MATTER; SOUTH CAMEROON; SOURCE ROCKS; PROVENANCE; EVOLUTION; SEDIMENTS; PALYNOFACIES; PALEOREDOX; INTERIOR	The Lower Cretaceous syn-rift deposits of the Douala Basin (Mundeck Formation), located in the equatorial West African margin were investigated in order to determine the palaeoenvironment and organic matter source, redox conditions, palaeoclimate, and tectonic settings, based on facies, organic and inorganic geochemical analyses. The sediments consist of pebble, coarse, medium- to fine-grained sandstone, siltstone, and grey to black fossiliferous shales. The shales are characterized by an average total organic carbon (TOC) of 1.02%, fair to poor source generative potential with present-day hydrogen index values, which range from 31 to 350 mg HC/g TOC suggesting that the shale contains Type III kerogens with mainly gas generative potential. The organic particles are dominated by phytoclasts (40% on average) and non-fluorescent amorphous organic matter (34% on average). The palynomorphs represent about 26% on average with a large amount of pollen grain and a minor amount of dinoflagellate cysts and microforaminifera test linings. The inferred depositional environment of the studied sediments is an alluvial fan to fluvio-lacustrine with shallow marine incursion. This depositional environment received the contribution of aquatic algae and microorganisms with a large amount of terrestrial organic matter, evidenced by the presence of some dinoflagellate cysts and microforaminifera test linings, and relatively higher amounts of SiO2, Al2O3, and phytoclasts. The presence of trace elements such as Ba, Sr, V, Ni, Co and Cr in the analysed samples and their ratio, suggest suboxic to anoxic conditions of deposition with low salinity. The warm to cold and dry climatic conditions prevailed during the deposition of the Mundeck deposits and sediments from active continental margin setting during the lower Cretaceous periods in the Douala Basin as confirmed by inorganic geochemical data. This study sheds light on the early stage of the evolution of the Douala Basin which could be integrated into the context of a mid-Jurassic to lower Cretaceous regional evolution of the opening of a passive margin. This evolution is characterized by an alluvial fan, fluviatile, lacustrine, lagoon and marine depositional system. This depositional system is recognized as part of the petroleum system recognized within the syn-rift deposits in the others basins along the West African margin, where giant hydrocarbons have been discovered.	[Sobdjou, C. K.; Mfayakouo, B. C.; Ngos, S.] Univ Maroua, Fac Sci, Dept Earth Sci, Maroua, Cameroon; [Sobdjou, C. K.] Inst Geol & Min Res, Yaounde, Cameroon; [Ngueutchoua, G.; Ngos, S.] Univ Yaounde, Fac Sci, Dept Earth Sci, Yaounde, Cameroon; [Kenfack, R. G. N.] Univ Dschang, Fac Sci, Dept Earth Sci, Dschang, Cameroon; [Mfayakouo, B. C.] Univ Maroua, Fac Sci, Dept Earth Sci, POB 814, Maroua, Cameroon	University of Yaounde I; Universite de Dschang	Mfayakouo, BC (通讯作者)，Univ Maroua, Fac Sci, Dept Earth Sci, POB 814, Maroua, Cameroon.	bmfayakouo@gmail.com						Ackerman W. C., 1993, AAPG BULL, V77, P1604; Agyingi C. 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MAY	2023	58	5					2057	2077		10.1002/gj.4710	http://dx.doi.org/10.1002/gj.4710		MAR 2023	21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	E5QH7					2025-03-11	WOS:000947973900001
J	Salgado, P; Pizarro, G; Frangopulos, M; Pinto-Torres, M; Toro, C; Torres, R; Alarcon, E; Guzman, L; Manriquez, K; Raimapo, R; Cascales, E				Salgado, Pablo; Pizarro, Gemita; Frangopulos, Maximo; Pinto-Torres, Marco; Toro, Carolina; Torres, Rodrigo; Alarcon, Emilio; Guzman, Leonardo; Manriquez, Karen; Raimapo, Roberto; Cascales, Emma			Distribution of dinoflagellate cyst assemblages in surface sediments of Magellan fjords and channels (Patagonia, Chile) with a focus on harmful species: An overview on environmental scenario	PROGRESS IN OCEANOGRAPHY			English	Review						Alexandrium catenella; Cyst assemblages; Environmental parameters; Harmful dinoflagellates; Magellan fjords and channels	SOUTHERN CHILE; ALEXANDRIUM-CATENELLA; BLOOM DYNAMICS; RESTING CYSTS; FRESH-WATER; GYMNODINIUM-CATENATUM; SCRIPPSIELLA-HANGOEI; GENUS ALEXANDRIUM; ALGAL BLOOMS; SP-NOV	Several dinoflagellate species form benthic resting cysts in their life cycle. In order to study the composition, abundance and distribution of cyst assemblages, with a focus on harmful species, thirty-one surface sediment samples from the Magellan fjords and channels system were analysed. In situ (temperature, salinity, inorganic nutrients, dissolved oxygen, organic matter, and chlorophyll-a) and five-year (salinity, temperature, dissolved oxygen, and chlorophyll-a) measurement data were analysed to obtain an overview on environmental scenario. A total of 56 cyst morphotypes were recorded, some of which were identified for the first time for the Chilean coast (Dactylodinium cf. arachnoides, Impagidinium cf. velorum, Archaeperidinium sp., Protoperidinium haizhouense, Pro-toperidinium sinuosum, Protoperidinium tricingulatum, and Dubridinium cf. ulsterum). In vitro germination of cysts allowed the vegetative form of the species of the order Suessiales to be determined. Total cyst concentrations were highly variable, ranging from 145 to 5453 cysts mL-1 of wet sediment (mean 1246 +/- 1061 cysts mL-1), with the lowest cyst values in the area adjacent to the Southern Patagonian Ice Field. Pentapharsodinium dalei and Protoperidinium conicoides generally dominated (%) the cyst assemblages. The harmful species Alexandrium cat-enella and Alexandrium ostenfeldii were not abundant and sparsely distributed, while Protoceratium reticulatum was widespread and highly abundant with Gonyaulax spinifera in Inutil Bay (Magellan Strait). Cluster and nMDS analyses performed with cyst concentrations of the 56 taxa in the 31 stations formed seven cyst assemblage clusters, reflecting high environmental variability. Canonical correspondence analyses performed with cyst concentrations and in situ and long-term environmental data showed different ecological signals, demonstrating that in situ parameters must be used carefully when studying cysts in surface sediments.	[Salgado, Pablo; Pizarro, Gemita; Toro, Carolina; Raimapo, Roberto] Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Enrique Abello 0552, Punta Arenas, Chile; [Frangopulos, Maximo] Univ Magallanes, Ctr Invest GAIA Antartica CIGA, Av Bulnes 01855, Punta Arenas, Chile; [Frangopulos, Maximo] Univ Magallanes, Cape Horn Int Ctr CHIC, Puerto Williams, Chile; [Frangopulos, Maximo] Millennium Inst Biodivers Antarctic & Subantarctic, Las Palmeras 3425, Santiago, Chile; [Pinto-Torres, Marco] Univ Austral Chile, Escuela Grad, Programa Doctorado Ciencias Acuicultura, Puerto Montt, Chile; [Pinto-Torres, Marco; Torres, Rodrigo] Ctr Invest Dinam Ecosistemas Marinos Altas Latitud, Punta Arenas, Chile; [Torres, Rodrigo; Alarcon, Emilio] Ctr Invest Ecosistemas Patagonia CIEP, Jose de Moraleda 16, Coyhaique, Chile; [Guzman, Leonardo; Cascales, Emma] Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Padre Harter 574, Puerto Montt, Chile; [Manriquez, Karen] Univ Andres Bello UNAB, Fac Ciencias Vida, Dept Ecol & Biodivers, Republ 440, Santiago, Chile	Instituto de Fomento Pesquero (Valparaiso); Universidad de Magallanes; Universidad de Magallanes; Universidad Austral de Chile; Instituto de Fomento Pesquero (Valparaiso); Universidad Andres Bello	Salgado, P (通讯作者)，Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Enrique Abello 0552, Punta Arenas, Chile.	pablo.salgado@ifop.cl	Frangopulos, Maximo/ABC-8933-2020; Salgado, Pablo/KMA-0636-2024	Pinto Torres, Marco Antonio/0000-0002-5942-206X; pizarro, gemita/0000-0003-2974-2609; frangopulos, maximo/0000-0002-6857-273X; Torres, Rodrigo/0000-0003-0416-4291	Comite Oceanografico Nacional [CONA-C25F, 21160047]; "Concurso Nacional de Asignacion de Tiempo de Buque Oceanografico AGS-61 Cabo de Hornos 2019" - Associative Research Program PIA-CONICYT/ANID [CONA C25F 19-02]; Undersecretary of Economy and Smaller Companies and Undersecretary of Fisheries and Aquaculture; ANID - Millennium Science Initiative Program; ANID BASAL; Aquaculture Sciences at the Universidad Austral de Chile, Centro Fondap IDEAL; Doctorado Becas Chile;  [PROFAN AUB 1900003];  [ICN2021_002];  [FB210018];  [15150003]	Comite Oceanografico Nacional; "Concurso Nacional de Asignacion de Tiempo de Buque Oceanografico AGS-61 Cabo de Hornos 2019" - Associative Research Program PIA-CONICYT/ANID; Undersecretary of Economy and Smaller Companies and Undersecretary of Fisheries and Aquaculture; ANID - Millennium Science Initiative Program; ANID BASAL; Aquaculture Sciences at the Universidad Austral de Chile, Centro Fondap IDEAL; Doctorado Becas Chile; ; ; ; 	This work was funded by Comite Oceanografico Nacional (CONA-C25F, 2019) by the projects CONA C25F 19-02 (G. Pizarro) and PROFAN AUB 1900003 of the "Concurso Nacional de Asignacion de Tiempo de Buque Oceanografico AGS-61 Cabo de Hornos 2019" - Associative Research Program PIA-CONICYT/ANID. G. Pizarro and R. Raimapo participated in CIMAR-25 and P. Salgado and G. Pizarro in PROFAN supported by the Undersecretary of Economy and Smaller Companies and Undersecretary of Fisheries and Aquaculture, through the project "Programa de manejo y monitoreo de las mareas rojas en el sistema de fiordos y canales de Chile, etapa XIII 2019-2020" carried out by IFOP. Authors acknowledge the commander and the crew of the AGS-61 Cabo de Hornos of the Chilean Navy for their support during the oceanographic campaigns. The work of the Servicio Hidrografico y Oceanografico of the Chilean Navy (SHOA) is also recognized. M. Fragopulos also thanks ANID - Millennium Science Initiative Program - ICN2021_002 and ANID BASAL FB210018. M. Pinto-Torres thanks the doctoral program in Aquaculture Sciences at the Universidad Austral de Chile, Centro Fondap IDEAL 15150003 and to Doctorado Becas Chile - 2016 -Folio No 21160047 for the logistical and instrumental support, shipment and processing of the samples used here. We thank the two anonymous reviewers who helped to improve the manuscript with their constructive comments, and to the native reviewer who grammatically corrected the text.	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J	Smith, BC; Persson, A; Alix, JH				Smith, Barry C.; Persson, Agneta; Alix, Jennifer H.			Dinoflagellate cell density limits explored using <i>Scrippsiella lachrymosa</i> cultured in flow-through cages	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Culturing; Dinoflagellate; Gamete; Life stage; Red tide; Scrippsiella lachrymosa	HARMFUL ALGAL BLOOMS; LIFE-CYCLE STAGES; ALEXANDRIUM-FUNDYENSE; ACTIVATED CARBON; DRINKING-WATER; CYST FORMATION; RED TIDE; TOXICITY; DYNAMICS; PATTERNS	Dinoflagellates constitute one of the most important groups of primary producers and micro-zooplankton on earth, common in both marine and freshwater environments. Despite their prominent position among phytoplankton, they are difficult to grow into dense cultures in the laboratory. This discrepancy between field and laboratory indicates serious limitations caused by the laboratory culturing conditions. A difficult to study but important factor is the constraints of enclosure in a limited volume of water. We conducted an experiment wherein the dinoflagellate Scrippsiella lachrymosa was grown in "flow cells" - 100 cm(3) cylindrical cages constructed from plankton net, inserted in larger volumes of growth medium, allowing an exchange of medium without dilution of the culture. Cell numbers far exceeding the normal for culturing of this species and dinoflagellates in general were attained, even though the experiment was terminated before cultures reached stationary phase. A cell number ten times higher than under regular batch culturing was achieved (up to 340,000 cells mL(-1)). Pattern formation was distinct in cultures when cells were plentiful and water movements caused cell accumulation, not dispersion. High cell density concurrent with access to new growth medium promoted induction of the sexual cell cycle. The results indicate serious limitations to growth set by enclosure in a limited water volume in laboratory experiments; thus, maximum growth rates of dinoflagellates in favourable field conditions may be vastly underestimated. Cell accumulation behavior of dinoflagellates during the sexual life cycle may together with physical transport by larger forces in nature explain sudden bloom occurrences.	[Smith, Barry C.; Alix, Jennifer H.] NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT USA; [Persson, Agneta] Gothenburg Univ, Dept Biol & Environm Sci, Box 461, S-40530 Gothenburg, Sweden	National Oceanic Atmospheric Admin (NOAA) - USA; University of Gothenburg	Smith, BC (通讯作者)，NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT USA.	Barry.Smith@noaa.gov; agnetapersson77@gmail.com		Persson, Agneta/0000-0003-0202-6514	Signe and Olof Wallenius foundation; J. Gust. Richert's foundation	Signe and Olof Wallenius foundation; J. Gust. Richert's foundation	Financial support to Agneta Persson was provided by Signe and Olof Wallenius foundation and J. Gust. Richert's foundation.	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J	Barrón, E; Peyrot, D; Bueno-Cebollada, CA; Kvacek, J; Alvarez-Parra, S; Altolaguirre, Y; Meléndez, N				Barron, Eduardo; Peyrot, Daniel; Bueno-Cebollada, Carlos; Kvacek, Jiri; Alvarez-Parra, Sergio; Altolaguirre, Yul; Melendez, Nieves			Biodiversity of ecosystems in an arid setting: The late Albian plant communities and associated biota from eastern Iberia	PLOS ONE			English	Article							LOWER CRETACEOUS AMBER; ANGIOSPERM POLLEN; PSEUDOASTEROPHYLLITES-CRETACEUS; CHARENTE-MARITIME; GALVE SUBBASIN; HIGH-FREQUENCY; PALYNOLOGY; DEPOSITS; SPAIN; WESTERN	Deserts are stressful environments where the living beings must acquire different strategies to survive due to the water stress conditions. From the late Albian to the early Cenomanian, the northern and eastern parts of Iberia were the location of the desert system represented by deposits assigned to the Utrillas Group, which bear abundant amber with numerous bioinclusions, including diverse arthropods and vertebrate remains. In the Maestrazgo Basin (E Spain), the late Albian to early Cenomanian sedimentary succession represents the most distal part of the desert system (fore-erg) that was characterised by an alternation of aeolian and shallow marine sedimentary environments in the proximity of the Western Tethys palaeo-coast, with rare to frequent dinoflagellate cysts. The terrestrial ecosystems from this area were biodiverse, and comprised plant communities whose fossils are associated with sedimentological indicators of aridity. The palynoflora dominated by wind-transported conifer pollen is interpreted to reflect various types of xerophytic woodlands from the hinterlands and the coastal settings. Therefore, fern and angiosperm communities abundantly grew in wet interdunes and coastal wetlands (temporary to semi-permanent freshwater/salt marshes and water bodies). In addition, the occurrence of low-diversity megafloral assemblages reflects the existence of coastal salt-influenced settings. The palaeobotanical study carried out in this paper which is an integrative work on palynology and palaeobotany, does not only allow the reconstruction of the vegetation that developed in the mid-Cretaceous fore-erg from the eastern Iberia, in addition, provides new biostratigraphic and palaeogeographic data considering the context of angiosperm radiation as well as the biota inferred in the amber-bearing outcrops of San Just, Arroyo de la Pascueta and La Hoya (within Cortes de Arenoso succesion). Importantly, the studied assemblages include Afropollis, Dichastopollenites, Cretacaeiporites together with pollen produced by Ephedraceae (known for its tolerance to arid conditions). The presence of these pollen grains, typical for northern Gondwana, associates the Iberian ecosystems with those characterising the mentioned region.	[Barron, Eduardo; Bueno-Cebollada, Carlos] Museo Geominero, Ctr Nacl Inst Geol & Minero Espana CN IGME CSIC, Madrid, Spain; [Peyrot, Daniel] Univ Western Australia, Ctr Energy Geosci, Sch Earth & Environm, Crawley, WA, Australia; [Kvacek, Jiri] Natl Museum Prague, Prague, Czech Republic; [Alvarez-Parra, Sergio] Univ Barcelona, Dept Dinam Terra & Ocea, Fac Ciencies Terra, Barcelona, Spain; [Alvarez-Parra, Sergio] Univ Barcelona, Inst Recerca Biodiversitat IRBio, Barcelona, Spain; [Altolaguirre, Yul] Heidelberg Acad Sci, Senckenberg Res Inst, OCEEH Res Ctr role cultura early expans humans, Frankfurt, Germany; [Melendez, Nieves] Univ Complutense Madrid, Fac Ciencias Geol, Dept Geodinam Estratig & Paleontol, Madrid, Spain	University of Western Australia; National Museum; University of Barcelona; University of Barcelona; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Complutense University of Madrid	Barrón, E (通讯作者)，Museo Geominero, Ctr Nacl Inst Geol & Minero Espana CN IGME CSIC, Madrid, Spain.	e.barron@igme.es	Barrón, Eduardo/L-4726-2014; peyrot, Daniel/AAI-6091-2020; Kvacek, Jiri/A-1784-2014	Bueno Cebollada, Carlos Alberto/0000-0003-0367-4177; Kvacek, Jiri/0000-0003-2001-121X; Alvarez-Parra, Sergio/0000-0002-0232-1647; Altolaguirre Zancajo, Yul/0000-0002-2479-8788; peyrot, Daniel/0000-0002-3897-6733	Ministerio de Ciencia, Innovacion y Universidades (Spain) [CRE CGL2017-84419]; "Severo Ochoa" extraordinary grants for excellence IGME-CSIC (AECEX2021); Secretaria d'Universitats i Recerca de la Generalitat de Catalonia (Spain); European Social Fund [2021FI_B2 0003]	Ministerio de Ciencia, Innovacion y Universidades (Spain)(Spanish Government); "Severo Ochoa" extraordinary grants for excellence IGME-CSIC (AECEX2021); Secretaria d'Universitats i Recerca de la Generalitat de Catalonia (Spain); European Social Fund(European Social Fund (ESF))	This study is a contribution to the project CRE CGL2017-84419 AEI/FEDER, UE from the Ministerio de Ciencia, Innovacion y Universidades (Spain) and the "Severo Ochoa" extraordinary grants for excellence IGME-CSIC (AECEX2021). The coauthor S.A '.-P. thanks the support from the Secretaria d'Universitats i Recerca de la Generalitat de Catalonia (Spain) and the European Social Fund (2021FI_B2 0003). 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	Pei, Y; Blumenberg, M; Duda, JP; Höche, N; Peckmann, J; Birgel, D; Luo, JX; Kment, K; Reitner, J				Pei, Yu; Blumenberg, Martin; Duda, Jan-Peter; Hoeche, Nils; Peckmann, Joern; Birgel, Daniel; Luo, Jinxiong; Kment, Kurt; Reitner, Joachim			Ecosystem changes through the Permian-Triassic and Triassic-Jurassic critical intervals: Evidence from sedimentology, palaeontology and geochemistry	SEDIMENTOLOGY			English	Article						Calcispheres; dinoflagellates; haptophytes; lipid biomarkers; mass extinctions; microfacies; stable carbon isotopes	NORTHERN CALCAREOUS ALPS; PHOTIC ZONE EUXINIA; MASS EXTINCTION; SOUTH CHINA; OCEAN ACIDIFICATION; CARBON-CYCLE; POINT GSSP; BOUNDARY; BASIN; VOLCANISM	The Permian-Triassic and Triassic-Jurassic critical intervals are among the most significant ecological upheavals in the Phanerozoic. Both evolutionary junctures are characterized by environmental deterioration associated with a marked biodiversity decline. In this study, Permian-Triassic and Triassic-Jurassic boundary sections from South China and the Northern Calcareous Alps were investigated. In order to reconstruct the interplay between biotic and abiotic processes, a multifaceted approach that included optical microscopy, X-ray diffraction, Raman spectroscopy, stable carbon isotopes and lipid biomarkers was employed. The lower parts of these two sections are similar as both consist of limestone with abundant fossils of eukaryotic organisms. However, the Permian-Triassic record is dominated by dasyclad green algae and fusulinid foraminifera, while the Triassic-Jurassic record is typified by corals and coralline sponges. Moving upward, both sections consist mainly of micrite and marl. Concerning the Permian-Triassic section, it transits to volcanic ash intercalated by a distinct limestone bed with abundant calcispheres (tentatively attributed to ancestors of dinoflagellates). The Triassic-Jurassic section does not provide direct evidence for volcanic activity, but also becomes rich in calcisphere-type cysts towards the top. Additionally, the section preserves abundant 4-methyl sterenes (diagnostic for dinoflagellates) and C37-39 n-alkanes (indicative for haptophytes). Hence, both critical intervals were associated with marked blooms of (ancestral) dinoflagellates and haptophytes (for example, coccolithophorids). These blooms were followed by ecological lag-phases, as indicated by low carbonate contents and scarce fossils which only increased further up the sections. For both critical intervals, it is commonly assumed that the formation of voluminous volcanic provinces (Siberian Traps and Central Atlantic Magmatic Province, respectively), as well as associated processes (for example, burning of organic-rich sediments such as coal), resulted in ecological devastation. However, results suggest that volcanism also had a positive effect on certain planktonic primary producers such as dinoflagellates and haptophytes, perhaps by delivering essential nutrients.	[Pei, Yu; Duda, Jan-Peter] Eberhard Karls Univ Tubingen, Dept Geosci, Schnarrenbergstr 94-96, D-72076 Tubingen, Germany; [Pei, Yu; Duda, Jan-Peter; Reitner, Joachim] Gottingen Acad Sci & Humanities, Origin Life Group, Theater Str 7, D-37073 Gottingen, Germany; [Blumenberg, Martin; Kment, Kurt] Fed Inst Geosci & Nat Resources, Stilleweg 2, D-30655 Hannover, Germany; [Duda, Jan-Peter; Reitner, Joachim] Georg August Univ Gottingen, Geosci Ctr, Dept Geobiol, Goldschmidtstr 3, D-37077 Gottingen, Germany; [Hoeche, Nils] Johannes Gutenberg Univ Mainz, Inst Geosci, Johann Joachim Becher Weg 21, D-55118 Mainz, Germany; [Peckmann, Joern; Birgel, Daniel] Univ Hamburg, Inst Geol, Ctr Earth Syst Res & Sustainabil, Bundesstr 55, D-20146 Hamburg, Germany; [Luo, Jinxiong] Yangtze Univ, Sch Geosci, Coll Rd 111, Wuhan 430100, Peoples R China; [Kment, Kurt] Vogelau 20, D-83317 Teisendorf, Germany	Eberhard Karls University of Tubingen; University of Gottingen; Johannes Gutenberg University of Mainz; University of Hamburg; Yangtze University	Pei, Y (通讯作者)，Eberhard Karls Univ Tubingen, Dept Geosci, Schnarrenbergstr 94-96, D-72076 Tubingen, Germany.; Pei, Y; Reitner, J (通讯作者)，Gottingen Acad Sci & Humanities, Origin Life Group, Theater Str 7, D-37073 Gottingen, Germany.; Reitner, J (通讯作者)，Georg August Univ Gottingen, Geosci Ctr, Dept Geobiol, Goldschmidtstr 3, D-37077 Gottingen, Germany.	yu.pei@mnf.uni-tuebingen.de; jreitne@gwdg.de	Pei, Yu/GRI-9837-2022	Hoche, Nils/0000-0002-8850-3328; Peckmann, Jorn/0000-0002-8572-0060	China Council Scholarship (CSC); University of Tubingen (Germany); Forestry Department Oberammergau	China Council Scholarship (CSC); University of Tubingen (Germany); Forestry Department Oberammergau	We thank N. Sheldon, P. Suarez-Gonzalez and an anonymous reviewer for valuable comments and suggestions. Many thanks are given to A. Munnecke, A.L. Clau beta en, E. Jarochowska, G. Mathes, L.M. Baumann, M. Natalicchio, P. Suarez-Gonzalez and S. Kiel for helpful discussions. B. Feng, D. Grabow, E. Siedersbeck, G. Wu, H. Mei, Y. He and Z-Q. Chen are thanked for field assistance. A. Freiberg, A. Hackmann, A. Pack, A. Reimer, B. Roering, C. Conradt, D. Hause-Reitner, D. Kohl, G. Scheeder, J. Dyckmans, J. Schoenig, K. Luensdorf, K. Wemmer, P. Adam, T. Wasselin and W. Droese are acknowledged for lab. assistance. This study was financially supported by the China Council Scholarship (CSC) and a Teach@Tuebingen Fellowship by the University of Tuebingen (Germany). The Forestry Department Oberammergau (Bayerische Staatsforsten) gave permission to drive on closed forest roads. Open Access funding enabled and organized by Projekt DEAL.	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J	Frieling, J; Bohaty, SM; Cramwinckel, MJ; Gallagher, SJ; Holdgate, GR; Reichgelt, T; Peterse, F; Pross, J; Sluijs, A; Bijl, PK				Frieling, J.; Bohaty, S. M.; Cramwinckel, M. J.; Gallagher, S. J.; Holdgate, G. R.; Reichgelt, T.; Peterse, F.; Pross, J.; Sluijs, A.; Bijl, P. K.			Revisiting the Geographical Extent of Exceptional Warmth in the Early Paleogene Southern Ocean	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						Paleocene-Eocene Thermal Maximum; temperature reconstruction; multi-proxy; paleoceanography; SW Pacific; Australo-Antarctic Gulf	EOCENE THERMAL MAXIMUM; ISOPRENOID TETRAETHER LIPIDS; DIALKYL GLYCEROL TETRAETHERS; SUSPENDED PARTICULATE MATTER; SOUTHWEST PACIFIC-OCEAN; DINOFLAGELLATE CYSTS; MEMBRANE-LIPIDS; METHANE HYDRATE; BIOMARKER PALEOTHERMOMETRY; TEMPERATURE EVOLUTION	To assess zonal temperature and biogeographical patterns in the Southern Ocean during the Paleogene, we present new multi-proxy air-and sea-surface temperature data for the latest Paleocene (similar to 57-56 Ma) and the Paleocene-Eocene Thermal Maximum (PETM; similar to 56 Ma) from the northern margin of the Australo-Antarctic Gulf (AAG). The various proxy data sets document the well-known late Paleocene warming and, superimposed, two transient late Paleocene pre-cursor warming events, hundreds of kyr prior to the PETM. Remarkably, temperature reconstructions for the AAG and southwest Pacific during the latest Paleocene, PETM and Early Eocene Climatic Optimum (similar to 53-49 Ma) show similar trends as well as similar absolute temperatures east and west of the closed Tasmanian Gateway. Our data imply that the exceptional warmth as recorded by previous studies for the southwest Pacific extended westward into the AAG. This contrasts with modeling-derived circulation and temperature patterns. We suggest that simulations of ocean circulation underestimate heat transport in the southwest Pacific due to insufficient resolution, not allowing for mesoscale eddy-related heat transport. We argue for a systematic approach to tackle model and proxy biases that may occur in marginal marine settings and non-analog high-latitude climates to assess the temperature reconstructions.	[Frieling, J.; Cramwinckel, M. J.; Peterse, F.; Sluijs, A.; Bijl, P. K.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands; [Frieling, J.] Univ Oxford, Dept Earth Sci, Oxford, England; [Bohaty, S. M.] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany; [Gallagher, S. J.] Univ Melbourne, Sch Geog Earth & Atmospher Sci, Melbourne, Vic, Australia; [Holdgate, G. R.] Geotrack Int, Brunswick West, Vic, Australia; [Reichgelt, T.] Univ Connecticut, Dept Geosci, Storrs, CT USA	Utrecht University; University of Oxford; Ruprecht Karls University Heidelberg; University of Melbourne; University of Connecticut	Frieling, J; Bijl, PK (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands.; Frieling, J (通讯作者)，Univ Oxford, Dept Earth Sci, Oxford, England.	joost.frieling@earth.ox.ac.uk; p.k.bijl@uu.nl	Gallagher, Stephen/AFL-9448-2022; Peterse, Francien/AAY-1473-2021; Peterse, Francien/H-5627-2011	Peterse, Francien/0000-0001-8781-2826; Reichgelt, Tammo/0000-0001-8652-5489; Bijl, Peter/0000-0002-1710-4012; Gallagher, Stephen/0000-0002-5593-2740; Frieling, Joost/0000-0002-5374-1625	Australian Integrated Ocean Drilling Program office; German Research Foundation (DFG) [PR 651/24-1]; European Research Council [771497]; NWO Vernieuwingsimpuls Veni [863.13.002]	Australian Integrated Ocean Drilling Program office; German Research Foundation (DFG)(German Research Foundation (DFG)); European Research Council(European Research Council (ERC)); NWO Vernieuwingsimpuls Veni	We thank G. Dammers, E.P. Huurdeman, K. Nierop, C. Rem, and A. van Leeuwen for assistance in palynological processing and organic geochemical analyses. E. Hopmans is thanked for assistance and discussions on UHPLC-MS data. E.P. Huurdeman is acknowledged for work on the Latrobe-1 core as part of a Master's thesis. SJG was supported by the Australian Integrated Ocean Drilling Program office. JP acknowledges support by the German Research Foundation (DFG; Grant PR 651/24-1). AS thanks the European Research Council for consolidator Grant 771497. PKB acknowledges support from NWO Vernieuwingsimpuls Veni Grant 863.13.002. We are thankful for constructive reviews, suggestions and comments from the associate editor, an anonymous reviewer and Kate Littler that helped improve this manuscript. 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Paleoclimatology	MAR	2023	38	3							e2022PA004529	10.1029/2022PA004529	http://dx.doi.org/10.1029/2022PA004529			24	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	I1EL9		hybrid, Green Published			2025-03-11	WOS:001000274600005
J	Dale, B				Dale, Barrie			Paleontological Evidence for Dinoflagellates and Ciliates as Early Eukaryotes	JOURNAL OF MARINE SCIENCE AND ENGINEERING			English	Article						dinoflagellate cysts; acritarchs; eukaryote evolution; ciliates; fossil record; molecular trees	RESTING CYST; PHYLOGENY; MICROFOSSILS; AFFINITIES; QUATERNARY; MORPHOLOGY; EVOLUTION; TAXONOMY; KEY	Molecular trees and geochemical markers suggest the divergence of dinoflagellates as early eukaryotes (similar to 650 million years ago), but the traditional fossil record of cysts (dinocysts) starts during the Triassic (similar to 230 million years ago). A re-evaluation of the pre-Triassic record shows that many acritarchs (microfossils of uncertain affinities) are dinocysts representing "missing" fossil evidence. Traditional diagnostic criteria for dinocysts, based on morphologic comparisons with motile stages, are biased towards thecate species. The approach proposed here, based on the more natural comparison with living cysts, includes athecate species. Many living cysts of athecate species would be "acritarchs" if found as fossils, and many earlier acritarchs would be accepted as dinoflagellate cysts if found living. The earliest acritarchs represent an innovation with profound implications for evolution: a cell wall of sporopollenin-like material enabling survival from microbial attack, in a then microbial-dominated world. Related cell wall material most likely evolved as protection for crucial stages in sexual reproduction (e.g., cysts in ciliates and dinoflagellates, and spores and pollen in algae and plants). Ciliates and dinoflagellates may have evolved in response to extreme climatic conditions in the Cryogenian, where a robust resting cyst would be advantageous. Thecate dinoflagellates most likely evolved from athecate forms, possibly in response to predatory pressure.	[Dale, Barrie] Univ Oslo, Geosci Dept, N-0316 Oslo, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Geosci Dept, N-0316 Oslo, Norway.	barrie.dale@geo.uio.no						ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; Belmonte G, 2019, OCEANOGR MAR BIOL, V57, P1; Bhattacharya Debashish, 2009, P116; Bowman VC, 2013, PALYNOLOGY, V37, P151, DOI 10.1080/01916122.2012.750898; Butterfield NJ, 2015, PALAEONTOLOGY, V58, P5, DOI 10.1111/pala.12139; Butterfield NJ, 1998, GEOLOGY, V26, P963, DOI 10.1130/0091-7613(1998)026<0963:DOWFIP>2.3.CO;2; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; Dale B., 1983, P69; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B, 1978, Palynology, V2, P187; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B, 2021, PALYNOLOGY, V45, P165, DOI 10.1080/01916122.2020.1771623; Demoulin CF, 2019, FREE RADICAL BIO MED, V140, P206, DOI 10.1016/j.freeradbiomed.2019.05.007; Dodd MS, 2017, NATURE, V543, P60, DOI 10.1038/nature21377; Ellegaard M, 2001, PHYCOLOGIA, V40, P542, DOI 10.2216/i0031-8884-40-6-542.1; Evitt W. 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Mar. Sci. Eng.	MAR	2023	11	3							533	10.3390/jmse11030533	http://dx.doi.org/10.3390/jmse11030533			20	Engineering, Marine; Engineering, Ocean; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Oceanography	A9OA5		Green Published, gold			2025-03-11	WOS:000958327300001
J	Khaffou, H; Hssaida, T; Oukassou, M; Maatouf, W; Afenzar, A; Zafaty, O; Chakir, S; Jaydawi, S; Chafai, K; Charrière, A				Khaffou, Hanane; Hssaida, Touria; Oukassou, Mostafa; Maatouf, Wafaa; Afenzar, Abdelkrim; Zafaty, Omar; Chakir, Sara; Jaydawi, Soukaina; Chafai, Khaoula; Charriere, Andre			Bajocian-Bathonian dinoflagellate cyst assemblages from the Middle Atlas, Morocco: Palynostratigraphic and paleoenvironmental implications	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Biostratigraphy; Palynology; Dinoflagellate cysts; Bajocian-Bathonian; Middle Atlas; Morocco	NORTH-WEST SHELF; ORGANIC FACIES; EASTERN DESERT; BASIN; PALYNOLOGY; SEDIMENTS; AREA; PALYNOMORPHS; STRATOTYPE; SEQUENCE	The Bajocian-Bathonian transition has been identified for the first time in the Skoura syncline of the folded Mid-dle Atlas of Morocco based on dinoflagellate cyst and palynofacies analysis of the Ich Timellaline/Bou Akrabene Formation carbonates. This palynological study involved 109 samples of marls and limestones whose organic content yielded diverse and well-preserved dinoflagellate cyst assemblages comprising 68 taxa including strati -graphic marker taxa. Two association biozones have been defined for the late Bajocian-early Bathonian interval. The Cribroperidinium crispum-Ctenidodinium cornigerum (CC/CC) biozone is defined between the base of the Recifa Formation (Upper Bajocian) and the Ich-Timellaline / Bou Akrabene Formation (Upper Bajocian-Lower Bathonian). The second association biozone of Ctenidodinium combazii and Dichadogonyaulax sellwoodii (CC/ DS) corresponds to the upper interval of the FD section (top of the Ich-Timellaline / Bou Akrabene Formation and the base of the El Mers I Formation). These two biozones were correlated with the late Bajocian-early Bathonian biozones defined in the Sub-Boreal (northwest Europe), Tethyan, and Australian domains. Close sim-ilarity between the Moroccan Middle Atlas, the Tethyan, and the Sub-Boreal domain associations has been noted. Quantitative analysis of organic matter constituents has allowed the paleoenvironmental reconstruction of the late Bajocian-early Bathonian. The organic residues of the studied samples recorded an increased land-derived phytoclasts dominance compared to amorphous organic matter and palynomorphs, indicating a proximal oxic shelf depositional environment with high terrestrial and freshwater influx during the late Bajocian-early Bathonian. During the Late Bajocian, the depositional environment corresponds to a proximal continental shelf with fluctuations from a distal to a marginal/stagnant environment.Below the Upper Bajocian-Lower Bathonian boundary, a significant marine incursion, or rather a transgression, is recorded in the studied sediments attested by an important marine fraction and dinoflagellate cysts abundance, which probably corresponds to the last Bajocian Maximum flooding surface (MFS).During the early Bathonian, the depositional environment evolved towards a distal continental shelf with an in-creasing marine fraction including dinoflagellate cysts and high species diversity. This maybe related to the rising sea level which corresponds to the first Bathonian eustatic elevation. The proximal /marginal conditions are re-stored at the uppermost part of the section.(c) 2023 Elsevier B.V. All rights reserved.	[Khaffou, Hanane; Hssaida, Touria; Chafai, Khaoula] Hassan II Univ Casablanca, Fac Sci Ben Msick, Geosci & Applicat Lab, Casablanca, Morocco; [Oukassou, Mostafa; Zafaty, Omar] Hassan II Univ Casablanca, Fac Sci Ben Msick, Appl Geol Geoinformat & Environm Lab, Casablanca, Morocco; [Maatouf, Wafaa] Natl Off Hydrocarbons & Min ONHYM, Dept Petr Lab, Rabat, Morocco; [Afenzar, Abdelkrim; Chakir, Sara] Sidi Mohamed Ben Abdellah Univ, Fac Sci Dhar El Mahraz, Geosci Environm & Associated Resources Lab, Fes, Morocco; [Jaydawi, Soukaina] Mohammed V Univ, Fac Sci, Rabat, Morocco; [Charriere, Andre] Toulouse III Univ, Anduze, France	Hassan II University of Casablanca; Hassan II University of Casablanca; Sidi Mohamed Ben Abdellah University of Fez; Mohammed V University in Rabat	Oukassou, M (通讯作者)，Hassan II Univ Casablanca, Fac Sci Ben Msick, Appl Geol Geoinformat & Environm Lab, Casablanca, Morocco.	mostafa.oukassou@univh2c.ma	OUKASSOU, MOSTAFA/AAG-9198-2020	Abdelkrim, Afenzar/0000-0002-0833-3112; OUKASSOU, MOSTAFA/0000-0002-3388-4581; ZAFATY, Omar/0000-0001-7550-5634				Almeras Y., 2007, GEOBIOS-LYON, V40, P1; Bailey D., 1987, Journal of Micropalaeontology, V6, P89; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; Batten D.J., 1996, Palynology: principles and applications, V2, P795; Batten D. 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Palaeobot. Palynology	MAY	2023	312								104862	10.1016/j.revpalbo.2023.104862	http://dx.doi.org/10.1016/j.revpalbo.2023.104862		MAR 2023	29	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	A1RL9					2025-03-11	WOS:000952971900001
J	Pedersen, GK; Nohr-Hansen, H; Bojesen-Koefoed, JA; Grube, KB; Pedersen, SAS; Pedersen, AK; Sorensen, EV; Hopper, JR				Pedersen, Gunver Krarup; Nohr-Hansen, Henrik; Bojesen-Koefoed, Jorgen A.; Grube, Kristian Bloch; Pedersen, Stig A. Schack; Pedersen, Asger Ken; Sorensen, Erik Vest; Hopper, John R.			A new record of the Cenomanian-Turonian transgression preserved in the Ikorfat Fault zone, Nuussuaq Basin, West Greenland	CRETACEOUS RESEARCH			English	Article						Ikorfat Fault zone; Late Cenomanian-early Turonian&nbsp; transgression; OAE2; Itilli Formation; Biostratigraphy; Palynology; Sedimentology; Structural geology; Nuussuaq Basin; West Greenland	ATANE FORMATION; MANTLE PLUMES; STRATIGRAPHY; PALEOCENE; SEDIMENTARY; HISTORY; EVENT; KILEN; SUCCESSION; EVOLUTION	The Ikorfat Fault zone in northern Nuussuaq, Central West Greenland, has preserved a hitherto unknown succession of Upper Cretaceous marine mudstones referred to the Itilli Formation, which have been removed by erosion on the footwall block and buried deeply below sea-level on the hanging-wall block. Outcrops in the fault zone provide new data on sedimentology, palynology, stable carbon isotopes and organic geochemistry in the lower part of the Itilli Formation. A new, detailed geological map of the study area is based on digital photogrammetry. Marine organic walled dinoflagellate cysts (dinocysts) demonstrate a late Cenomanian-Turonian age, coeval with the Oceanic Anoxic Event 2 (OAE2) and link the Nuussuaq Basin with the Baffin Bay and Sverdrup Basins. The Ikorfat Fault zone is part of the eastern boundary fault of the Nuussuaq Basin. Lower Campanian listric faults truncate the footwall block. Sub-sidence along steep normal faults continued during deposition of the volcanic Vaigat Formation of Danian to Selandian age. The downthrow of the hanging-wall block was around 2.5 km.(c) 2023 Elsevier Ltd. All rights reserved.	[Pedersen, Gunver Krarup; Nohr-Hansen, Henrik; Bojesen-Koefoed, Jorgen A.; Pedersen, Stig A. Schack; Pedersen, Asger Ken; Sorensen, Erik Vest; Hopper, John R.] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Grube, Kristian Bloch] Minist Mineral Resources MMR, POB 930, Nuuk 3900, Greenland; [Grube, Kristian Bloch] COWI A S, Parallelvej 2, DK-2800 Kongens Lyngby, Denmark; [Pedersen, Asger Ken] Nat Sci Museum, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland; COWI A/S	Pedersen, GK (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	gkp@geus.dk	Bojesen-Koefoed, Jørgen/AAH-5501-2020; Pedersen, Gunver/G-9411-2018; Sorensen, Erik Vest/X-5830-2018; Hopper, John Robert/B-1710-2010	Pedersen, Stig A. Schack/0000-0002-7867-5118; Sorensen, Erik Vest/0000-0002-1827-2894; Hopper, John Robert/0000-0003-3188-7583	Ministry of Mineral Resources in Nuuk, Greenland	Ministry of Mineral Resources in Nuuk, Greenland	The field work and the study of the samples had not been possible without funding from the Ministry of Mineral Resources in Nuuk, Greenland. Jan Schulz Adolfssen and Thomas Bang Holm participated in the field work and contributed to the discussion of the observations. At GEUS important technical assistance was provided by Jette Halskov, Annette Ryge, Charlotte Olsen, and Carsten Guvad. The constructive comments from the referees are greatly appreciated. The authors direct their warm thanks to the persons and institutions mentioned. The manuscript is published with permission of the Geological Survey of Denmark and Greenland.	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Res.	MAY	2023	145								105481	10.1016/j.cretres.2023.105481	http://dx.doi.org/10.1016/j.cretres.2023.105481		MAR 2023	37	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	A2HU1					2025-03-11	WOS:000953401300001
J	Singh, YP; Verma, P; Singh, A; Bali, R				Singh, Yogesh Pal; Verma, Poonam; Singh, Abha; Bali, Rameshwar			Early Miocene (Burdigalian) Dinoflagellate Cysts from the Kerala Basin, Southwest India: Indicators of Marine Ingression at the Onset of the Mid-Miocene Climate Optimum (MMCO)	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article							DINOCYST STRATIGRAPHY; UPPERMOST OLIGOCENE; QUILON LIMESTONE; SEA; ASSEMBLAGES; SEDIMENTS; SEQUENCE; EOCENE; NORTH; PALEOENVIRONMENTS	In the present study, the assemblages of organic walled dinoflagellate cyst (dinocysts) and calcareous nannofossils from Quilon Formation, Kerala Basin, south-western India are analyzed for age interpretation and reconstruction of the depositional environment. The integrated biostratigraphy based on dinocysts and calcareous nannofossils from the same sediment samples indicates that the studied succession was deposited during the early Miocene (middle Burdigalian, similar to 19-17.5 Ma) time. The dinocyst assemblages contain abundant taxa (Cleistosphaeridium, Polysphaeridium, Lingulodinium, Homotryblium and Spiniferites) that range from shallow inner to outer neritic marine zone. The abundance of autotrophic, thermophilic taxa suggests relatively high surface water temperatures and high nutrient availability. The dinocyst assemblage in the lower part of the studied succession is dominated by Cleistosphaeridium spp., Polysphaeridium spp., Spiniferites spp., Homotryblium spp. and Lingulodinium spp. An increase in the relative abundances of outer neritic dinocyst taxa such as Spiniferites, Achomosphaera and Hystrichokolpoma in the upper part of the succession suggests a change towards more open marine conditions created during marine ingression. The interpreted marine ingression along the south-western Indian coast probably corresponds to the initial small pulses of transgression at the onset of the long-term global sea-level maximum related to the Mid-Miocene Climatic Optimum (MMCO).	[Singh, Yogesh Pal; Verma, Poonam; Singh, Abha] Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, India; [Singh, Yogesh Pal; Bali, Rameshwar] Univ Lucknow, Ctr Adv study Geol, Lucknow 226007, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Lucknow University	Verma, P (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, India.	verma.poonam07@gmail.com	Singh, Abha/KYQ-5677-2024; Singh, Yogesh/X-6849-2019		Department of Science and Technology (DST-SERB), New Delhi;  [EMR/2016/005983]	Department of Science and Technology (DST-SERB), New Delhi(Department of Science & Technology (India)Department of Science & Technology (DOST), Philippines); 	AcknowledgementsAll authors would like to thank the Director of the Birbal Sahni Institute of Palaeosciences (BSIP) for providing constant encouragement, infrastructural facilities, and the Research Development Co-ordination Cell, BSIP, Lucknow for the necessary permission for publication (Permission no. BSIP/RDCC/72/2021-22). All authors are also thankful to reviewer for his critical comments for improvement of manuscript. YPS is also thankful to Dr. Mayank Shekhar (BSIP) for his help in statistical analysis part. The authors also acknowledge financial support from the Department of Science and Technology (DST-SERB), New Delhi (Project no. EMR/2016/005983).	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Geol. Soc. India	MAR	2023	99	3					357	369		10.1007/s12594-023-2318-9	http://dx.doi.org/10.1007/s12594-023-2318-9			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	9W2YG					2025-03-11	WOS:000948944900009
J	Cuellar-Martinez, T; Morquecho, L; Alonso-Rodríguez, R; Ruiz-Fernández, AC; Sanchez-Cabeza, JA				Cuellar-Martinez, Tomasa; Morquecho, Lourdes; Alonso-Rodriguez, Rosalba; Ruiz-Fernandez, Ana Carolina; Sanchez-Cabeza, Joan-Albert			Germination of <i>Pyrodinium bahamense</i> Cysts from a Pristine Lagoon in San José Island, Gulf of California: Implications of Long-Term Survival	PHYCOLOGY			English	Article						coastal lagoons; dinoflagellate cysts; germination; harmful algal blooms; recent sediments; Mexico; Gulf of California; Baja California Sur	ALEXANDRIUM-FUNDYENSE; DINOFLAGELLATE CYSTS; RESTING CYSTS; EXCYSTMENT PATTERNS; DINOPHYCEAE; VIABILITY; CATENELLA; SEDIMENTS; DYNAMICS; PHYTOPLANKTON	The production of cysts by dinoflagellates can be part of the life cycle of some species, improving their survival under adverse environmental conditions; cyst germination may explain the recurrence of algal blooms in some cases. In order to evaluate the germination rates of Pyrodinium bahamense, its cysts were retrieved from surface sediments collected in San Jos & eacute; Lagoon, SW Gulf of California, and germination assays were carried out through the cysts incubation under two contrasting light and nutrient concentration conditions. Also, to evaluate cysts viability, we isolated P. bahamense cysts and other dinoflagellate species from different depth layers of a Pb-210-dated sediment core (similar to 100 years) to examine their germination for 20 days. Germination rates were higher under light (28-56%) than in darkness (23-34%); there were indications that the nutrient-enriched media was more effective in promoting germination than seawater. Furthermore, germination was observed in cysts isolated from all selected core depths, even those corresponding to similar to 100 years. These results demonstrate that cysts remain viable for long periods, and P. bahamense cysts germinate in any light and nutrient conditions. The results of this research provide relevant information to understand its physiology and complex population dynamics. This species should be closely monitored in the area in the context of climate change, as current natural conditions are likely to change.	[Cuellar-Martinez, Tomasa] Inst Mar Peru, Esquina Gamarra & Gen Valle S-N, Callao, Peru; [Morquecho, Lourdes] Ctr Invest Biol Noroeste CIBNOR, Ave IPN 195, La Paz 23096, Baja Calif Sur, Mexico; [Alonso-Rodriguez, Rosalba; Ruiz-Fernandez, Ana Carolina; Sanchez-Cabeza, Joan-Albert] Univ Nacl Autonoma Mexico, Unidad Acad Mazatlan, Inst Ciencias Mar & Limnol, Mazatlan 82040, Sinaloa, Mexico	Instituto del Mar del Peru; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Universidad Nacional Autonoma de Mexico	Alonso-Rodríguez, R (通讯作者)，Univ Nacl Autonoma Mexico, Unidad Acad Mazatlan, Inst Ciencias Mar & Limnol, Mazatlan 82040, Sinaloa, Mexico.		Morquecho, Lourdes/JPY-0626-2023; Sanchez-Cabeza, Joan-Albert/Q-2394-2016; Alonso-Rodriguez, Rosalba/U-9896-2017	Cuellar Martinez, Tomasa/0000-0002-0460-6275; Sanchez-Cabeza, Joan-Albert/0000-0002-3540-1168; Alonso-Rodriguez, Rosalba/0000-0001-7716-3869	CONACYT; PAPIIT-UNAM [IN112914, IN203313, CIBNOR-CODIMAR 20014, PROMEP/103.5/13/9335, IAEA-ARCAL RLA 7014, 7020, 7025, 307783];  [196813];  [153492]	CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); PAPIIT-UNAM(Programa de Apoyo a Proyectos de Investigacion e Innovacion Tecnologica (PAPIIT)Universidad Nacional Autonoma de Mexico); ; 	This research was funded by CONACYT 196813 and 153492, PAPIIT-UNAM IN112914 and IN203313, CIBNOR-CODIMAR 20014, PROMEP/103.5/13/9335, FONDECYT 05/2019/ and IAEA-ARCAL RLA 7014, 7020, and 7025. This work is a contribution of the Marine-Coastal Research Stressors Network for Latin America and the Caribbean (REMARCO, www.remarco.org, accessed on 30 January 2023). T. Cuellar was a recipient of a Ph. D. CONACYT fellowship (307783).	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J	Roux, P; Schapira, M; Mertens, KN; Andre, C; Terre-Terrillon, A; Schmitt, A; Manach, S; Collin, K; Serghine, J; Noel, C; Siano, R				Roux, Pauline; Schapira, Mathilde; Mertens, Kenneth Neil; Andre, Coralie; Terre-Terrillon, Aouregan; Schmitt, Anne; Manach, Soazig; Collin, Karine; Serghine, Joelle; Noel, Cyril; Siano, Raffaele			When phytoplankton do not bloom: the case of the dinoflagellate <i>Lepidodinium chlorophorum</i> in southern Brittany (France) assessed by environmental DNA	PROGRESS IN OCEANOGRAPHY			English	Review						HABs; Cysts; Sediment resuspension; eDNA; Metabarcoding; Ammonium	DISSOLVED ORGANIC NITROGEN; ALEXANDRIUM-CATENELLA; RESTING CYSTS; GYMNODINIUM-CHLOROPHORUM; MARINE-PHYTOPLANKTON; GREEN DINOFLAGELLATE; SEQUENCING REVEALS; DINOPHYCEAE; GULF; SEDIMENTS	Green seawater discolorations caused by the marine dinoflagellate Lepidodinium chlorophorum are frequently observed during summer along southern Brittany coasts (NE Atlantic, France). Here, the ecology of L. chlorophorum is studied during a non-bloom period using high-throughput sequencing metabarcoding of environmental DNA (eDNA) samples for the detection of this species at low concentrations. Sediment samples (for metabarcoding and cyst analyses) were collected in January-February 2019 and water samples from two stations were collected at three water depths in September-March 2019-2020 and 2020-2021 (for meta-barcoding and environmental parameters). The protistan community was dominated by dinoflagellates and was homogenous in the water column. Amplicon sequence variants (ASVs) associated with the genus Lepidodinium were detected in autumn-winter at low relative abundances (minimum: 0.01%). Increases in Lepidodinium abundance were positively correlated with pulses of ammonium re-suspended from bottom sediments. Although Lepidodinium eDNA (<1%) was detected in the sediments, no cyst morphotypes could be associated with Lepidodinium , and germination experiments revealed no Lepidodinium-like cells, leaving in doubt the existence of resting cysts of this species in the seed bank. It is hypothesised that temporary Lepidodinium cells remained present in the water column at low concentrations during the autumn-winter period, awaiting ammonium input from sediments to initiate growth, and that blooms develop when water column stratification and river input provide favourable environmental conditions for biomass increases.	[Roux, Pauline; Schapira, Mathilde; Schmitt, Anne; Collin, Karine] Ifremer, LITTORAL, F-44300 Nantes, France; [Mertens, Kenneth Neil; Andre, Coralie; Terre-Terrillon, Aouregan] Ifremer, LITTORAL, F-29900 Concarneau, France; [Manach, Soazig] Ifremer, LITTORAL, F-56100 Lorient, France; [Serghine, Joelle; Siano, Raffaele] Ifremer, DYNECO, F-29280 Plouzane, France; [Andre, Coralie; Noel, Cyril] Ifremer, Serv Bioinformat SeBiMER, IRSI, Plouzane, France	Ifremer; Ifremer; Ifremer; Ifremer; Ifremer	Siano, R (通讯作者)，Ifremer, DYNECO, F-29280 Plouzane, France.	raffaele.siano@ifremer.fr	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Noel, Cyril/0000-0002-7139-4073; Schapira, Mathilde/0000-0002-0130-9398; Collin, Karine/0000-0001-9601-9299; Mertens, Kenneth/0000-0003-2005-9483	Ifremer; Agence de l'Eau Loire Bretagne (project EPICE) [180408801]; Region Pays de la Loire (project LEPIDO-PEN) [06582 2019]; GDR PHYCOTOX, a CNRS/Ifremer network on Harmful Algal Blooms	Ifremer; Agence de l'Eau Loire Bretagne (project EPICE); Region Pays de la Loire (project LEPIDO-PEN); GDR PHYCOTOX, a CNRS/Ifremer network on Harmful Algal Blooms	This work was carried out in the frame of the PhD of Pauline Roux, financed by Ifremer, Agence de l'Eau Loire Bretagne (project EPICE [180408801]), Region Pays de la Loire (project LEPIDO-PEN [06582 2019]) and was supported by the GDR PHYCOTOX, a CNRS/Ifremer network on Harmful Algal Blooms (https://www.phycotox.fr/). The authors thank Ifremer-LER/MPL staff for their technical contributions and the Ifremer Plateforme d'Analyse Sedimentaire (PAS) for technical support during granulometry analyses. The authors wish to thank Julien Quere for his dedicated assistance in DNA extraction.	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Oceanogr.	MAR	2023	212								102999	10.1016/j.pocean.2023.102999	http://dx.doi.org/10.1016/j.pocean.2023.102999		FEB 2023	15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	A0YW5		Green Submitted			2025-03-11	WOS:000952484600001
J	Shehata, AA; Tahoun, SS; Kassem, AA; Abdelsamea, EG; Hassan, HF				Shehata, Amer A.; Tahoun, Sameh S.; Kassem, Ahmed A.; Abdelsamea, Ethar G.; Hassan, Hatem F.			Palynostratigraphy and paleoenvironmental inferences of the Jurassic successions, Darag Basin, Gulf of Suez, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynostratigraphy; Palynofacies; Paleoenvironments; Jurassic; Darag basin; Gulf of suez; Egypt	NORTH-WESTERN DESERT; EASTERN DESERT; DINOFLAGELLATE CYSTS; SEQUENCE; PALYNOFACIES; STRATIGRAPHY; PALYNOLOGY; BIOSTRATIGRAPHY; PETROLEUM; BOREHOLE	The present study shows the advantage of the palynostratigraphy and paleoenvironmental inferences concepts in subdividing and interpreting the depositional environment of the Jurassic rocks, depending on two sections in two boreholes drilled in the Darag Basin, Egypt. Six Jurassic rock units representing the mixed siliciclastic and carbonate sediments were recognized from top to base; the Tauriat, Arousiah, Kehailia, Safa, Shusha and Rajabiah formations. The palynomorph assemblage associated with moderately diversified dinoflagellate cysts and fewer sporomorphs, show poor to fair preservation. About 20 dinoflagellate cysts, 8 pollen, and 3 pter-idophytic spore species have been recorded. The Jurassic rocks are originated from the late Jurassic (early Oxfordian) and early (Toarcian -Aaleneian) based on the recovered marker taxa. The studied sections are differentiated into six biozones, Systematophora sp. (Callovian-Oxfordian), Gonyaulacysta jurassica (Callovian), Dichadogonyaulax sellwoodii (Late Bathonian), Sentusidinium sp. (Early Bathonian), Pareodinia ceratophora (Bajocian) and Psilate spores, Classopollis and Sphaeripollenites Acme Zone (Toarcian-Aalenian). According to the Particulate Organic Matter (POM) composition in the studied wells, the palynofacies as-semblages led to identifying three depositional settings, the palynofacies-1 (PFA-1), which is characterized by opaque phytoclasts and high volume of spores and pollen grains was deposited in a marginal shallow-marine environment during a relative sea-level fall. The PFA-2 is composed of brown phytoclasts, moderate Amor-phous Organic Matter (AOM) with pollen grains and dominated dinocysts. It was deposited during a slight sea level rise in a proximal inner neritic environment. Simultaneously, the PFA-3, which was dominated by AOM and dinoflagellate cysts with moderate brown phytoclast content, was deposited as a distal inner neritic environment during a relatively high relative sea level.	[Shehata, Amer A.; Abdelsamea, Ethar G.; Hassan, Hatem F.] Port Said Univ, Fac Sci, Geol Dept, Port Fuad 42522, Egypt; [Shehata, Amer A.] Texas A&M Univ, Coll Sci, Dept Phys & Environm Sci, 6300 Ocean Dr, Corpus Christi, TX 78412 USA; [Tahoun, Sameh S.] Cairo Univ, Fac Sci, Geol Dept, Giza, Egypt; [Kassem, Ahmed A.] Gulf Suez Petr Co, Explorat Dept, Cairo 11742, Egypt	Egyptian Knowledge Bank (EKB); Port Said University; Texas A&M University System; Egyptian Knowledge Bank (EKB); Cairo University	Shehata, AA (通讯作者)，Port Said Univ, Fac Sci, Geol Dept, Port Fuad 42522, Egypt.	amer_esmail@sci.psu.edu.eg	Hassan, Hatem/JAA-9497-2023; Kassem, Ahmed/AFN-3178-2022; Shehata, Amer/AGY-3678-2022	Shehata, Amer/0000-0002-2997-6088				Abdelhady AA, 2015, J PALAEOGEOG-ENGLISH, V4, P305, DOI 10.1016/j.jop.2015.08.008; Abioui M., 2021, NAT RESOUR RES, P1; Aboul Ela N. 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Afr. Earth Sci.	APR	2023	200								104890	10.1016/j.jafrearsci.2023.104890	http://dx.doi.org/10.1016/j.jafrearsci.2023.104890		FEB 2023	12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	9W1IV					2025-03-11	WOS:000948835200001
J	Liu, ML; Tillmann, U; Ding, GM; Wang, AJ; Gu, HF				Liu, Minlu; Tillmann, Urban; Ding, Guangmao; Wang, Aijun; Gu, Haifeng			Metabarcoding revealed a high diversity of Amphidomataceae (Dinophyceae) and the seasonal distribution of their toxigenic species in the Taiwan Strait	HARMFUL ALGAE			English	Article						Azadinium poporum; Azaspiracids; High -throughput sequencing; Quantitative pcr; Cyst	DINOFLAGELLATE GENUS AZADINIUM; SP-NOV; POPORUM DINOPHYCEAE; AZASPIRACID PROFILE; ARGENTINEAN SHELF; COASTAL WATERS; A.-POPORUM; DALIANENSE; MORPHOLOGY; PHYLOGENY	The dinophyte family Amphidomataceae includes the genera Azadinium and Amphidoma. Four of these species are known to produce azaspiracids, which are lipophilic phycotoxins accumulating in shellfish. The diversity and biogeography of Amphidomataceae is far from yet resolved. Here we performed a time series sampling of both water and sediments in the Taiwan Strait from Nov. 2018 to April 2021. Metabarcoding was performed to unveil the diversity of Amphidomataceae targeting internal transcribed spacer (ITS1) region and partial large subunit ribosomal DNA (LSU rDNA D1-D3), followed by quantitative PCR (qPCR) with modified primers for Az. poporum ribotypes. The diversity of Amphidomataceae was revealed from the water samples with the aid of ITS1 and LSU based molecular phylogeny. The LSU based approach detected only a few species. In contrast, ITS1 based dataset showed eight new Azadinium clades and several ZOTUs (zero-radius operational taxonomic units) grouping together with Am. languida. Moreover, eleven known Azadinium species including three ribotypes of Az. poporum and Az. dexteroporum, and two ribotypes of Az. spinosum, were detected. The latter two species have not been reported in China before. Among these toxigenic species, Az. poporum was relevantly abundant whereas others were rare. The maximum of 209 cells L-1 of Az. poporum ribotype A was estimated using qPCR nearby Quanzhou in Nov. 2018 and 172 cells L 1 of Az. poporum ribotype B was detected far off coast in Apr. 2021. Metabarcoding on sediment samples revealed Az. poporum ribotypes B and C, but strains obtained with sediment incubation experiments yielded only ribotype B. Using qPCR about 0.2 cysts g-1 of Az. poporum ribotype B were quantified in May 2019 but cysts of Az. poporum ribotype C were not detected. Our results suggest that metabarcoding targeting ITS1 region is powerful to uncover the diversity of harmful dinophytes. Our results also highlight the rich diversity of Amphidomataceae and risk potential of azaspiracids in the Taiwan Strait and surrounding waters.	[Liu, Minlu; Wang, Aijun; Gu, Haifeng] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Tillmann, Urban] Alfred Wegener Inst, Helmholtz Zent Polar & Meeresforschung, Handelshafen 12, D-27570 Bremerhaven, Germany; [Ding, Guangmao] Fishery Resources Monitoring Ctr Fujian Prov, Fuzhou 350003, Peoples R China; [Gu, Haifeng] Minist Nat Resources, Key Lab Marine Ecol Conservat & Restorat, Xiamen 361005, Peoples R China; [Gu, Haifeng] Fujian Prov Key Lab Marine Ecol Conservat & Restor, Xiamen 361005, Peoples R China; [Wang, Aijun] Fujian Prov Key Lab Marine Phys & Geol Proc, Xiamen 361005, Peoples R China	Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Ministry of Natural Resources of the People's Republic of China	Gu, HF (通讯作者)，Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China.; Gu, HF (通讯作者)，Minist Nat Resources, Key Lab Marine Ecol Conservat & Restorat, Xiamen 361005, Peoples R China.; Gu, HF (通讯作者)，Fujian Prov Key Lab Marine Ecol Conservat & Restor, Xiamen 361005, Peoples R China.	guhaifeng@tio.org.cn	Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	National Natural Science Foundation of China [42106140, 32072329]; Scientific Research Foundation of Third Institute of Oceanography [2020007]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Scientific Research Foundation of Third Institute of Oceanography	This project was supported by the National Natural Science Foundation of China (No. 42106140) , the Scientific Research Foundation of Third Institute of Oceanography, MNR (No. 2020007) and the National Natural Science Foundation of China (No. 32072329) . Two anonymous reviewers are thanked for constructive suggestions that improved the manuscript greatly.	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J	Semmani, N; Fournier, F; Suc, JP; Fauquette, S; Godeau, N; Guihou, A; Popescu, SM; Melinte-Dobrinescu, MC; Thomazo, C; Marié, L; Deschamps, P; Borgomano, J				Semmani, Nazim; Fournier, Francois; Suc, Jean-Pierre; Fauquette, Severine; Godeau, Nicolas; Guihou, Abel; Popescu, Speranta-Maria; Melinte-Dobrinescu, Mihaela Carmen; Thomazo, Christophe; Marie, Lionel; Deschamps, Pierre; Borgomano, Jean			The Paleogene continental basins from SE France: New geographic and climatic insights from an integrated approach	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Priabonian; Rupelian; Eocene -Oligocene transition; Pb dating; Pollens; Strontium and sulfur isotopes; Climatostratigraphy; Marine intrusion	ISOTOPE COMPOSITIONS; STRUCTURAL STYLE; ALPINE FORELAND; GEODYNAMIC EVOLUTION; STRONTIUM ISOTOPES; EASTERN PYRENEES; WESTERN GULF; SULFUR; EVAPORITES; RECONSTRUCTION	New insights into the geodynamic evolution, the paleogeographic framework and the paleoclimatic setting of the Upper Eocene-Oligocene lacustrine basins from South-East France have been provided by an integrative approach combining geochronology, micropaleontology and stable isotope analyses. U-Pb dating on calcite, pollen-based climatostratigraphy and strontium and sulfur isotope signatures of sulfates provided a robust chronostratigraphic framework for the Upper Eocene and Oligocene succession from the Vistrenque, Ale`s and Roussillon basins. The thick Priabonian- lower Rupelian lacustrine succession from the Vistrenque Basin is interpreted to be deposited in a strike-slip basin associated with the latest stages of pyrenean shortening. Floral assemblages are used to reconstruct the vegetation cover in the lacustrine systems and their neighbouring lowlands and highlands. Composition of saltwater inferred from strontium and sulfur isotope signatures of sulfates, the occurrence of calcareous nannofossils, dinoflagellate cysts and pollen grains of mangrove-related plants provided strong evidence for marine intrusions into the Ale`s Basin during the Priabonian and the Vistrenque Basin during the Rupelian and Chattian. Paleogeographic reconstructions of Southeast France during the Priabonian and late Rupelian strongly suggest marine incursions from the Alpine Sea via two potential pathways: upper Rho<SIC>ne Valley via the Crest Sill and lower Rho<SIC>ne Valley via the Haut-Var Pyrenean synclines. On the other hand, Upper Oligocene evaporite basins in the Camargue area have been subjected to marine intrusions from the Western Mediterranean Sea following the collapse of the eastern pyrenean relief during the Liguro-Provencal rifting stage. Finally, pollen analysis and Climate Amplitude Method revealed a brief but significant stage of cooling and aridification at the very base of the Rupelian which could represent the regional and terrestrial expression of the global climate cooling following the Eocene-Oligocene Transition.	[Semmani, Nazim; Fournier, Francois; Godeau, Nicolas; Guihou, Abel; Marie, Lionel; Deschamps, Pierre; Borgomano, Jean] Aix Marseille Univ, CNRS, IRD, Cerege, 34,3 Pl Victor Hugo Case 67, F-13331 Marseille 03, France; [Suc, Jean-Pierre; Godeau, Nicolas] Sorbonne Univ, Inst Sci Terre Paris, CNRS, ISTeP,UMR 7193,INSU, F-75005 Paris, France; [Fauquette, Severine] Univ Montpellier, ISEM, CNRS, IRD,EPHE, Montpellier, France; [Popescu, Speranta-Maria] GeoBioStratData Consulting, 385 Route Mas Rillier, F-69140 Rillieux La Pape, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, 23-25 Dimitrie Onciul St, Bucharest, Romania; [Thomazo, Christophe] Univ Bourgogne Franche Comte, UMR CNRS uB6282 Biogeosci, 6 Bd Gabriel, F-21000 Dijon, France	Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Universite de Bourgogne	Fournier, F (通讯作者)，Aix Marseille Univ, CNRS, IRD, Cerege, 34,3 Pl Victor Hugo Case 67, F-13331 Marseille 03, France.	fournier@cerege.fr	Fournier, Francois/M-3274-2015; Fauquette, Severine/M-3686-2019; Deschamps, Pierre/M-9632-2013	Fauquette, Severine/0000-0003-0516-7734; Semmani, Nazim/0009-0001-7884-4946; Deschamps, Pierre/0000-0003-1687-3765	France's Ministry of Higher Education and Research; CEREGE; Carbonate Chair; ANR PYRAMID'; Total E P;  [APIC 2018 RRH];  [FR00040451]	France's Ministry of Higher Education and Research; CEREGE; Carbonate Chair; ANR PYRAMID'(Agence Nationale de la Recherche (ANR)); Total E P(Total SA); ; 	This work was funded by the France's Ministry of Higher Education and Research and is part of the PhD of the first author (NS) . This work also benefited from the financial supports of CEREGE (APIC 2018 RRH) and Carbonate Chair and we thank them warmly for their support. Sampling and analyses on the Canet 1 borehole were carried out thanks to the financial support of the ANR PYRAMID', to which this paper is a contribution. This work benefited from internal documents provided by Total E & P (Contract of cooperation and data exchange TOTAL E & P-Aix- Marseille University FR00040451) . The authors would also thank Gilles Graffin (STC core library, Boussens) for giving access to samples on the Camargue wells cores. Alain Tonetto (head of PRATIM, Aix -Marseille University) is also thanked for his help to carry out confocal microscope analyses. Scanning electronic microscope observations benefited from the assistance of Omar Boudouma (Sorbonne University) . Christian Gorini, Michel Seranne, an anonymous reviewer and the Editor are greatly thanked for their very constructive contribution to improve this manuscript.	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J	da Silva, LC; Santos, A; Fauth, G; Manríquez, LM; Kochhann, KG; Guerra, RD; Horodyski, RS; Villegas-Martín, J; da Silva, RR				Ferreira da Silva, Luiza Carine; Santos, Alessandra; Fauth, Gerson; Elizabeth Manriquez, Leslie Marcela; Diemer Kochhann, Karlos Guilherme; Guerra, Rodrigo do Monte; Horodyski, Rodrigo Scalise; Villegas-Martin, Jorge; da Silva, Rafael Ribeiro			High-latitude Cretaceous-Paleogene transition: New paleoenvironmental and paleoclimatic insights from Seymour Island, Antarctica	MARINE MICROPALEONTOLOGY			English	Article						L ?opez de Bertodano Formation; K-Pg transition; Geochemistry; Palynology; X-ray fluorescence (XRF) analysis; Filo Negro Section	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; MASS EXTINCTION; CLIMATE-CHANGE; OULED HADDOU; BOUNDARY; ASSEMBLAGES; BASIN; PALEOCENE; EVOLUTION; MIOCENE	The Filo Negro Section, on Seymour Island (Antarctic Peninsula), is a fossiliferous section with great potential for Late Cretaceous-Paleogene studies, which also presents an iridium anomaly layer. However, it has not been thoroughly studied in terms of integrated high-resolution paleontological and multi-proxy records yet. Paly-nomorphs and geochemical proxies are used herein to assess paleoenvironmental and paleoclimatic changes recorded at this section during the Maastrichtian-Danian transition. In addition, statistical tests are applied to our numerical palynological data (cluster analysis, Mann Kendall Trend test and chi 2-test) in order to further support our interpretations. The P/G ratio (peridinioid/gonyaulacoid dinoflagellate cysts) was adopted as a paleoproductivity proxy, whereas the T/M ratio (terrestrial/marine palynomorphs) was used to infer proximal/ distal depositional settings. The sedimentary succession was divided into three intervals, based on a cluster analysis. We infer humid, relatively warm conditions for the latest Maastrichtian, and cool paleoclimates after the K-Pg transition. This is supported by the Fe/K ratio, which depicts a general trend toward drier climates in the early Danian. A marked increase in terrestrial palynomorphs, along with a general Ti/Al ratio increasing-upwards trend, implies more proximal settings above the maximum flooding surface, marked at 9.9 m. The P/ G and Ba/terrigenous elements ratios imply a marine paleoproductivity drop around the K-Pg transition, remaining low during the earliest Danian. We also refined the previous position of the K-Pg transition in this section, placing it within 9.5 to 9.6 m, based on dinoflagellate cysts biostratigraphical analysis and geochemical data (iridium anomaly and increase in siderophile elements).	[Ferreira da Silva, Luiza Carine; Fauth, Gerson; Elizabeth Manriquez, Leslie Marcela; Diemer Kochhann, Karlos Guilherme; Horodyski, Rodrigo Scalise; da Silva, Rafael Ribeiro] Univ Vale Rio dos Sinos, Programa Posgrad Geol, Ave Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Santos, Alessandra; Fauth, Gerson; Diemer Kochhann, Karlos Guilherme; Guerra, Rodrigo do Monte; Villegas-Martin, Jorge] Univ Vale Rio dos Sinos, Inst Tecnol Paleoceanog & Mudancas Climat Itt Oce, Ave Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Guerra, Rodrigo do Monte] Museu Itinerante Ciencias Nat, BR-95185000 Carlos Barbosa, RS, Brazil	Universidade do Vale do Rio dos Sinos (Unisinos); Universidade do Vale do Rio dos Sinos (Unisinos)	da Silva, LC (通讯作者)，Univ Vale Rio dos Sinos, Programa Posgrad Geol, Ave Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil.	luizasilva@edu.unisinos.br	Kochhann, Karlos/AAH-4636-2019; Fauth, Gerson/AAE-3353-2021; Guerra, Roberto M/JNS-9000-2023; Horodyski, Rodrigo/A-3605-2014	do Monte Guerra, Rodrigo/0000-0003-1688-3322	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [CNPq/CAPES/MCTI/PROANTAR] [88887.314454/2019-00, 21/2018 -CNPq/PROANTAR: 88887.372443/2019- 00]; CNPq/MCTIC/CAPES/FNDCT [N o 21/2018 -CNPq/PROANTAR: 88887.372443/2019- 00]; CNPq [308087/2019-4]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [CNPq/CAPES/MCTI/PROANTAR](Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq/MCTIC/CAPES/FNDCT; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We are thankful to Unisinos and itt Oceaneon, for the equipment and all the infrastructure. We are grateful to Marcelo de A. Carvalho, for generating the cluster and diversity/dominance indices, and to Luciana Duarte, for carefully preparing the palynological slides. We are also thankful to Marcelo Motta, for the enlightening ideas on possible pa- leoclimatic approaches in palynology, and to Simone B. Fauth and Marcelo de A. Carvalho for the suggestions about this research. We thank Lilian M. Leandro, Mauro D. R. Bruno and Rodrigo B. Fauth for logistics support. This research was funded by the Conselho Nacional de Desenvolvimento Cient?fico e Tecnol ? ogico (CNPq) and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) , as part of the project ?Paleocene-Miocene climate evolution: Connections between the Southern Ocean and the Antarctic Peninsula? [CNPq/CAPES/MCTI/PROANTAR: Process 88887.314454/2019-00 and CNPq/MCTIC/CAPES/FNDCT N o 21/2018 -CNPq/PROANTAR: 88887.372443/2019- 00] . GF thanks to CNPq grant (Process 308087/2019-4) .	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Micropaleontol.	APR	2023	180								102214	10.1016/j.marmicro.2023.102214	http://dx.doi.org/10.1016/j.marmicro.2023.102214		FEB 2023	12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	9P7FI					2025-03-11	WOS:000944446200001
J	Gomes, BT; Aguilera, O; Silva-Caminha, SAFD; 'Apolito, C; Cardenas, D; Hocking, EP; Lemes, KKB				Gomes, Bianca Tacoronte; Aguilera, Orangel; Silva-Caminha, Silane Aparecida Ferreira da; 'Apolito, Carlos; Cardenas, Damian; Hocking, Emma P.; Lemes, Karyen Ketly Batista			Biostratigraphy and Paleoenvironments of the Pirabas Formation (Neogene, Par acute accent a State-Brazil)	MARINE MICROPALEONTOLOGY			English	Article						South America Equatorial platform; Miocene; Palynomorphs; Carbonate-siliciclastic	AMAZON RIVER; LATE MIOCENE; EQUATORIAL; MANGROVE; BASIN; PALYNOLOGY; EVOLUTION; FREQUENCY; SEDIMENTS; ESTUARY	The Pirabas Formation (Neogene, eastern Brazilian Amazonia) is the only marine Miocene unit in Brazil that crops out on the edge of the equatorial shelf. The formation has a distinctive mixture of carbonate and siliciclastic sediments. The paleodiversity of the deposit includes assemblages of foraminifera, ostracods, decapod crusta-ceans, mollusks, bryozoans, corals, echinoderms, fish, and sirenids. Microfossils are abundant and palynological studies can contribute to accurate paleoenvironmental reconstructions and biostratigraphic descriptions of the Pirabas formation. Here, we present 17 samples from eight outcrops and one quarry belonging to the Pirabas Formation with a goal to understand their depositional environments and relative ages. We recorded 9 species of dinoflagellate cysts, 7 spore species morphotypes, 59 pollen species morphotypes, 17 species of diatoms, and one species of silicoflagellate. We clustered the samples into two depositional groups, with one group formed by the Capanema quarry, Ponta do Castelo and Fazenda outcrops, deposited in a mesotrophic, shallow, marine environment, with a late early-Miocene age. The second one, formed by Atalaia, Aricuru, Macarico, and Baunilha Grande outcrops, was deposited in a mesotrophic coastal environment with nearby mangroves; these samples may date to the late middle to late Miocene.	[Gomes, Bianca Tacoronte] Florida Inst Technol, Inst Global Ecol, 150, Univ Blvd, Melbourne, FL 32901 USA; [Aguilera, Orangel] Fluminense Fed Univ, Rua Marcos Waldemar Freitas Reis, BR-24210201 Niteroi, RJ, Brazil; [Silva-Caminha, Silane Aparecida Ferreira da; Lemes, Karyen Ketly Batista] Univ Fed Mato Grosso, Geosci Fac, Fernando Correa Costa Ave,2367,, BR-78060090 Cuiaba, MT, Brazil; ['Apolito, Carlos] Univ Fed Acre, Ctr Ciencias Biolo g & Nat Estacionamento, Dist Ind, CEP, BR 364,km 4, BR-69920900 Rio Branco, AC, Brazil; [Cardenas, Damian] Univ Nacl Colombia, Dept Geosci, Bogota, Colombia; [Hocking, Emma P.] Northumbria Univ, Dept Geog & Environm Sci, Newcastle Upon Tyne, Northumberland, England	Florida Institute of Technology; Universidade Federal Fluminense; Universidade Federal de Mato Grosso; Universidad Nacional de Colombia; Northumbria University	Gomes, BT (通讯作者)，Florida Inst Technol, Inst Global Ecol, 150, Univ Blvd, Melbourne, FL 32901 USA.	bgomes2022@my.fit.edu; orangelaguilera@id.uff.br; silane.caminha@ufmt.br; carlos.dapolito@ufac.br; dcardenasl@unal.edu.co; emma.hocking@northumbria.ac.uk	Aguilera, Orangel/D-5055-2013; Hocking, Emma/Q-6241-2019; Hocking, Emma/K-8292-2013; Cardenas, Damian/AAB-3440-2020	Hocking, Emma/0000-0002-8925-1695; Cardenas, Damian/0000-0002-9823-6470	Brazilian Council of Science and Technological Development -CNPq [404937/2018-7, 305269/2017-8, 304693/2021-9]; FAPERJ [E-26/201.035/2021]	Brazilian Council of Science and Technological Development -CNPq; FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	The authors would like to thank the National Mining Agency of Brazil (ANM-COPAL) for the authorization to collect samples at the Pirabas Formation. The authors are very grateful to Ana Paula Linhares from the Paraense Museum Emilio Goeldi (MPEG), Dayana Alvarado from the Para Federal University (UFPA), Karen Bencomo and Daniel Lima from the Fluminense Federal University (UFF), Brazil, for collaboration and support during the field trips. Special thanks are due to Rafael Costa from the Brazilian Geological Service (CPRM) for providing the samples from the Colonia Pedro Teixeira. We also thank Ricardo Lopes from the Federal University of Rio de Janeiro (UFRJ) and Christiano Ng from CENPES-PETROBRAS for the incentive concerning the Pirabas Formation research. Last but not least, we warmly thank Vinicius Kutter (UFPA) for the academic support of the project. Thanks, are also to Ana Paula Linares (MPEG) and Marcelo Cohen (UFPA) for their valuable comments that greatly contributed to improving the present manuscript. 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J	Yedema, YW; Sangiorgi, F; Sluijs, A; Damsté, JSS; Peterse, F				Yedema, Yord W.; Sangiorgi, Francesca; Sluijs, Appy; Sinninghe Damste, Jaap S.; Peterse, Francien			The dispersal of fluvially discharged and marine, shelf-produced particulate organic matter in the northern Gulf of Mexico	BIOGEOSCIENCES			English	Article							DIALKYL GLYCEROL TETRAETHERS; LOWER MISSISSIPPI RIVER; CHAIN ALKYL DIOLS; SURFACE SEDIMENTS; CONTINENTAL-MARGIN; DINOFLAGELLATE CYSTS; STEROL COMPOSITION; POLLEN TRANSPORT; CARBON; LIPIDS	Rivers play a key role in the global carbon cycle by transporting terrestrial organic matter (TerrOM) from land to the ocean. Upon burial in marine sediments, this TerrOM may be a significant long-term carbon sink, depending on its composition and properties. However, much remains unknown about the dispersal of different types of TerrOM in the marine realm upon fluvial discharge since the commonly used bulk organic matter (OM) parameters do not reach the required level of source- and process-specific information. Here, we analyzed bulk OM properties, lipid biomarkers (long-chain n-alkanes, sterols, long-chain diols, alkenones, branched and isoprenoid glycerol dialkyl glycerol tetraethers (brGDGTs and isoGDGTs)), pollen, and dinoflagellate cysts in marine surface sediments along two transects offshore the Mississippi-Atchafalaya River (MAR) system, as well as one along the 20m isobath in the direction of the river plume. We use these biomarkers and palynological proxies to identify the dispersal patterns of soil-microbial organic matter (SMOM), fluvial, higher plant, and marine-produced OM in the coastal sediments of the northern Gulf of Mexico (GoM). The Branched and Isoprenoid Tetraether (BIT) index and the relative abundance of C-32 1,15-diols indicative for freshwater production show high contributions of SMOM and fluvial OM near the Mississippi River (MR) mouth (BIT D 0.6, FC32 1;15 > 50 %), which rapidly decrease further away from the river mouth (BIT < 0.1, FC32 1;15 < 20 %). In contrast, concentrations of long-chain n-alkanes and pollen grains do not show this stark decrease along the path of transport, and especially n-alkanes are also found in sediments in deeper waters. Proxy indicators show that marine productivity is highest close to shore and reveal that marine producers (di-atoms, dinoflagellates, coccolithophores) have different spatial distributions, indicating their preferred niches. Close to the coast, where food supply is high and waters are turbid, cysts of heterotrophic dinoflagellates dominate the assemblages. The dominance of heterotrophic taxa in shelf waters in combination with the rapid decrease in the relative contribution of TerrOM towards the deeper ocean suggest that TerrOM input may trigger a priming effect that results in its rapid decomposition upon discharge. In the open ocean far away from the river plume, autotrophic dinoflagellates dominate the assemblages, indicating more oligotrophic conditions. Our combined lipid biomarker and palynology approach reveals that different types of TerrOM have distinct dispersal patterns, suggesting that the initial composition of this particulate OM influences the burial efficiency of TerrOM on the continental margin.	[Yedema, Yord W.; Sangiorgi, Francesca; Sluijs, Appy; Sinninghe Damste, Jaap S.; Peterse, Francien] Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands; [Sinninghe Damste, Jaap S.] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, NL-1790 AB Den Burg, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Yedema, YW (通讯作者)，Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands.	y.w.ijedema@uu.nl	Peterse, Francien/AAY-1473-2021; Sluijs, Appy/B-3726-2009; Damste, Jaap/F-6128-2011; Peterse, Francien/H-5627-2011	Yedema, Yord/0000-0001-7852-6799; Peterse, Francien/0000-0001-8781-2826; Sangiorgi, Francesca/0000-0003-4233-6154	Netherlands Earth System Science Centre [024.002.001]	Netherlands Earth System Science Centre	This research has been supported by the Netherlands Earth System Science Centre (grant no. 024.002.001).	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J	Kim, JH; Ajani, PA; Murray, SA; Kang, SM; Kim, SH; Lim, HC; Teng, ST; Lim, PT; Park, BS				Kim, Jin Ho; Ajani, Penelope A.; Murray, Shauna A.; Kang, Su-Min; Kim, Sae-Hee; Lim, Hong Chang; Teng, Sing Tung; Lim, Po Teen; Park, Bum Soo			Abiotic and biotic factors controlling sexual reproduction in populations of Pseudo-nitzschia pungens (Bacillariophyceae)	HARMFUL ALGAE			English	Article						Pseudo-nitzschia pungens; Sexual reproduction; Mating rate; Potential cell activity	DINOFLAGELLATE GONYAULAX-TAMARENSIS; SIZE-REDUCTION; DOMOIC ACID; PERIDINIUM-CINCTUM; CYST FORMATION; LIFE-CYCLE; CELL-SIZE; DIATOM; ENCYSTMENT; GROWTH	Pseudo-nitzschia pungens is a widely distributed marine pennate diatom. Hybrid zones, regions in which two different genotypes may interbreed, are important areas for speciation and ecology, and have been reported across the globe for this species. However, sexual reproduction between differing clades in the natural envi-ronment is yet to be observed and is difficult to predict. Here we carried out experiments using two mono-clonal cultures of P. pungens from different genotypes to measure the frequency and timing of sexual reproduction across varying biotic (growth phases and cell activity potential) and abiotic conditions (nutrients, light, turbu-lence). We found the mating rates and number of zygotes gradually decreased from exponential to late stationary growth phases. The maximum zygote abundance observed was 1,390 cells mL-1 and the maximum mating rate was 7.1%, both which occurred during the exponential growth phase. Conversely, only 9 cells mL-1 and a maximum mating rate of 0.1% was observed during the late stationary phase. We also found the higher the relative potential cell activity (rPCA) in parent cells, as determined by the concentration of chlorophyll a per cell and the ratio of colony formation during parent cultivations, revealed higher mating rates. Furthermore, sexual events were reduced under nutrient enrichment conditions, and mating pairs and zygotes were not formed under aphotic (dark) or shaking culture conditions (150 rpm). In order to understand the sexual reproduction of Pseudo-nitzschia in the natural environment, our results highlight that it is most likely the combination of both biotic (growth phase, Chl. a content) and abiotic factors (nutrients, light, turbulence) that will determine the successful union of intraspecific populations of P. pungens in any given region.	[Kim, Jin Ho; Kang, Su-Min] Jeju Natl Univ, Coll Ocean Sci, Dept Earth & Marine Sci, Jeju 63243, South Korea; [Kim, Jin Ho; Ajani, Penelope A.; Murray, Shauna A.] Univ Technol Sydney, Sch Life Sci, POB 123, Sydney, NSW 2007, Australia; [Kim, Sae-Hee; Park, Bum Soo] Hanyang Univ, Coll Nat Sci, Dept Life Sci, Seoul 04763, South Korea; [Lim, Hong Chang] Tunku Abdul Rahman Univ Coll, Dept Appl Sci, Johor Branch Campus, Johor Baharu 53300, Malaysia; [Teng, Sing Tung] Univ Malaysia Sarawak, Fac Res Sci & Technol, Kota Samarahan 94300, Malaysia; [Lim, Po Teen] Univ Malaya, Inst Ocean & Earth Sci, Bachok Marine Res Stn, Bachok 16310, Kelantan, Malaysia; [Park, Bum Soo] Hanyang Univ, Hanyang Inst Biosci & Biotechnol, Seoul 04763, South Korea; [Park, Bum Soo] Hanyang Univ, Res Inst Nat Sci, Seoul 04763, South Korea	Jeju National University; University of Technology Sydney; Hanyang University; Tunku Abdul Rahman University College (TAR UC); University of Malaysia Sarawak; Universiti Malaya; Hanyang University; Hanyang University	Kim, JH (通讯作者)，Jeju Natl Univ, Coll Ocean Sci, Dept Earth & Marine Sci, Jeju 63243, South Korea.; Kim, JH (通讯作者)，Univ Technol Sydney, Sch Life Sci, POB 123, Sydney, NSW 2007, Australia.; Park, BS (通讯作者)，Hanyang Univ, Coll Nat Sci, Dept Life Sci, Seoul 04763, South Korea.; Park, BS (通讯作者)，Hanyang Univ, Hanyang Inst Biosci & Biotechnol, Seoul 04763, South Korea.; Park, BS (通讯作者)，Hanyang Univ, Res Inst Nat Sci, Seoul 04763, South Korea.	diatomist.jin@gmail.com; parkbs@hanyang.ac.kr	Lim, Hong/J-8761-2012; Teng, SingTung/E-8281-2015; Murray, Shauna/JAN-6668-2023; Ajani, Penelope/K-9987-2019; Lim, Po Teen/C-9758-2013; Murray, Shauna A/K-5781-2015; PARK, Bum Soo/W-3178-2017	Ajani, Penelope/0000-0001-5364-9936; Lim, Po Teen/0000-0003-2823-0564; Murray, Shauna A/0000-0001-7096-1307; PARK, Bum Soo/0000-0002-5441-6779	Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) - Ministry of Education [2019R1A6A1A10072987]; National Research Foundation of Korea (NRF) - Korea Gov- ernment (MSIT) [2022R1C1C1003582]; Research Fund of Hanyang University [HY-202200000003109]	Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) - Ministry of Education(Ministry of Education (MOE), Republic of KoreaNational Research Foundation of Korea); National Research Foundation of Korea (NRF) - Korea Gov- ernment (MSIT)(National Research Foundation of KoreaMinistry of Science, ICT & Future Planning, Republic of KoreaMinistry of Science & ICT (MSIT), Republic of Korea); Research Fund of Hanyang University	This research was supported by Basic Science Research Program to Research Institute for Basic Sciences (RIBS) of Jeju National University through the National Research Foundation of Korea (NRF) funded by the Ministry of Education (2019R1A6A1A10072987) , the National Research Foundation of Korea (NRF) grant funded by the Korea Gov- ernment (MSIT) (No. 2022R1C1C1003582) , and the Research Fund of Hanyang University (HY-202200000003109) .	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J	García-Moreiras, I; Costas, SV; García-Gil, S; Sobrino, CM				Garcia-Moreiras, Iria; Vila Costas, Sarai; Garcia-Gil, Soledad; Munoz Sobrino, Castor			Organic-walled dinoflagellate cyst assemblages in surface sediments of the Ria de Vigo (Atlantic margin of NW Iberia) in relation to environmental gradients	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Modern distribution; Lingulodinium polyedra; Coastal environments; Redundant discriminant analysis; Atlantic Iberian margin	ESTUARINE UPWELLING ECOSYSTEM; HARMFUL ALGAL BLOOMS; RED-TIDE; DEEP-SEA; LINGULODINIUM-POLYEDRUM; SPATIAL-DISTRIBUTION; COMMUNITY STRUCTURE; POLLEN TRANSPORT; MARINE-SEDIMENTS; WEST-COAST	Organic-walled dinoflagellate cyst assemblages were analysed in 31 surface sediment samples from the Ria de Vigo (NW Iberia) to obtain supporting evidence for the interpretation of past environmental signals from sediment cores. Complementarily, the totals of pollen (and pollen from riparian taxa), foraminiferal linings and freshwater algae were also considered to test their value as (palaeo)environmental indicators in fluvio-marine sedimentary environments. Abundances of foraminiferal linings gradually increased towards the ria's mouth, which supports its use as a proxy to infer the degree of marine influence in the sediment record. The ratio of dinoflagellate cysts to pollen and spores (D/P) increased with distance to the main river's mouth (and water depth) in the inner (< 7 m water depth) and the outer (> 20 m) parts of the ria. Total pollen concentrations decreased with water depth in the outer part but did not show any clear trend in the rest of the ria. No clear pattern in the distributions of pollen from riparian plants and spores from freshwater microalgae was detected. Multivariate analyses (clustering and RDA) performed on dinoflagellate cyst records and environmental data reflected a marked inshore-offshore distribution pattern mainly controlled by a fluvio-marine environmental gradient. Increasing abundances of cysts of Gymnodinium species and heterotrophic cysts as well as higher cyst diversity characterised the deeper environments of the outer ria. These observations suggest a relationship with increased shelf influence and are compatible with the heterotroph upwelling signal described in previous works. A very different cyst association with a predominance of autotrophic cysts characterised the intermediate and inner parts of ria, where exceptionally high cyst abundances of Lingulodinium polyedra (similar to 56-99% and similar to 200-114,000 cysts.g(-1)) were reported. Abundances of cysts of L. polyedra positively correlated with shallower and higher river-influenced environments characterised by higher sea-surface temperature. Our results agree with previous studies and reinforce the value of this species as an indicator of warmer and stratified conditions. Moreover, cysts of L. polyedra positively correlated with winter sea-surface nitrate contents, which is compatible with the nutrient enrichment signal (natural or anthropogenic) that has already been described in other deep and stratified estuarine environments and is consistent with historical cyst records obtained in the Ria de Vigo. However, further research is needed to disentangle the nutrient enrichment signal from the influence of other environmental factors.	[Garcia-Moreiras, Iria; Garcia-Gil, Soledad; Munoz Sobrino, Castor] Univ Vigo, BASAN, Ctr Invest Marina CIM, Edificio Ciencias Experimentais,Campus Vigo, Vigo 36310, Spain; [Garcia-Moreiras, Iria; Vila Costas, Sarai; Munoz Sobrino, Castor] Univ Vigo, Dept Biol Vexetal & Ciencias Solo, Vigo 36310, Spain; [Garcia-Gil, Soledad] Univ Vigo, Dept Xeociencias Marinas & Ordenac Terr, Campus Vigo, Vigo 36310, Spain	Universidade de Vigo; Universidade de Vigo; Universidade de Vigo	García-Moreiras, I (通讯作者)，Univ Vigo, Dept Biol Vegetal & Ciencias Solo, Fac Biol, Lab Palinoloxia, Campus Lagoas Marcosende S-N, Vigo 36310, Spain.	iriagamo@uvigo.es	Sobrino, Castor/N-6281-2019; GARCIA-MOREIRAS, IRIA/H-4627-2015; Munoz Sobrino, Castor/H-2948-2015	GARCIA-MOREIRAS, IRIA/0000-0001-8713-0374; Munoz Sobrino, Castor/0000-0001-8191-3001	Spanish Ministry of Education and Science [CGL2012-33584]; Xunta de Galicia GRC [GRC 2015/020, ED431C 2019/28]; Xunta de Galicia [ED481B-2019-074]; Universidade de Vigo/CISUG	Spanish Ministry of Education and Science(Spanish Government); Xunta de Galicia GRC; Xunta de Galicia(Xunta de Galicia); Universidade de Vigo/CISUG	This work was funded by the Spanish Ministry of Education and Science CGL2012-33584 (co-financed with ERDF funds) and the Xunta de Galicia GRC 2015/020 projects and ED431C 2019/28. Iria Garcda-Moreiras was supported by a postdoctoral fellowship from Xunta de Galicia (ED481B-2019-074, 2019). <STRONG>Funding</STRONG> for open access charge was provided by Universidade de Vigo/CISUG. Dr. Ana Amorim from MARE-Centro de Ciencias do Mar e do Ambiente (Sciences faculty from the University of Lisbon, Portugal) is greatly acknowledged for providing lab facilities to analyse some palynological samples. We also thank Dr. Jorge Iglesias Crespo for his valuable help in sampling the surface sediments in San Simon Bay, and Dr. Natalia Martdnez-Carreno for geophysical data acquisition and her support in sampling the sediment cores. Spetial thanks go for the two anonymous reviewers for their constructive comments that helped to improve our manuscript.	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Micropaleontol.	APR	2023	180								102217	10.1016/j.marmicro.2023.102217	http://dx.doi.org/10.1016/j.marmicro.2023.102217		FEB 2023	22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	9N6MK		Green Published, hybrid			2025-03-11	WOS:000943026400001
J	Polyakova, Y; Agafonova, E; Novichkova, E; de Vernal, A				Polyakova, Yelena; Agafonova, Elizaveta; Novichkova, Ekaterina; de Vernal, Anne			Holocene Paleoenvironmental Implications of Diatom, Non-Pollen Palynomorph, and Organic Carbon Records from the Kandalaksha Bay of the White Sea (European Arctic)	GEOSCIENCES			English	Article						the European Arctic; the White Sea; diatoms; dinocysts; Holocene; paleoenvironments	DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; LAST GLACIAL MAXIMUM; BARENTS SEA; DINOCYST ASSEMBLAGES; SURFACE CONDITIONS; MARGINAL FILTERS; BOTTOM SEDIMENTS; KARELIAN COAST; CENTRAL PART	Variations in sea surface conditions and sea level through the Holocene in the Kandalaksha Bay, the White Sea, were reconstructed based on the study of core sediments from the outer Kandalaksha Bay, using the modern analog technique applied to dinocysts in addition to diatoms, TOC, delta C-13(org), CaCO3, and grain size data. The chronostratigraphy of the core sediments was defined from accelerator mass spectrometry C-14 dates on mollusk shells. The results indicated an increase in water depth in the outer Kandalaksha Bay and in the central Dvina Bay until the late Holocene. From about 9.5 to 7.5 cal kyr BP, the data suggested a general trend of increasing sea surface temperatures (up to 14 degrees C), at least in areas with inflow of Atlantic waters. The last 2.5 kyr were characterized by increased freshwater runoff to the White Sea.	[Polyakova, Yelena] Lomonosov Moscow State Univ, Geog Fac, Moscow 119991, Russia; [Agafonova, Elizaveta; Novichkova, Ekaterina] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 119991, Russia; [de Vernal, Anne] Univ Quebec Montreal, Geotop Res Ctr Earth Syst Dynam, Montreal, PQ H3C 3P8, Canada	Lomonosov Moscow State University; Russian Academy of Sciences; Shirshov Institute of Oceanology; University of Quebec; University of Quebec Montreal	Agafonova, E (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol, Moscow 119991, Russia.	agafonovaelizaveta@mail.ru	Agafonova, Elizaveta/KCK-0835-2024; de Vernal, Anne/D-5602-2013; Novichkova, Ekaterina/B-5807-2017	de Vernal, Anne/0000-0001-5656-724X; Novichkova, Ekaterina/0000-0001-5687-1719; Agafonova, Elizaveta/0000-0001-5451-9586	Russian Science Foundation [21-17-00235]; Natural Sciences and Engineering Council of Canada	Russian Science Foundation(Russian Science Foundation (RSF)); Natural Sciences and Engineering Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	The sedimentological and micropaleontological study was supported by the Russian Science Foundation (project No 21-17-00235). The diatom researches of the Dvina Bay sediments were carried out within the framework of the State Assignments of Ministry of Science and High Education, Russia (Lomonosov Moscow State University, theme no. 121051100135-0). The studies by A. de V are supported by the Natural Sciences and Engineering Council of Canada.	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J	Kwok, ACM; Chan, WS; Wong, JTY				Kwok, Alvin Chun Man; Chan, Wai Sun; Wong, Joseph Tin Yum			Dinoflagellate Amphiesmal Dynamics: Cell Wall Deposition with Ecdysis and Cellular Growth	MARINE DRUGS			English	Review						cell wall; harmful algal blooms; cyst; dinoflagellates; amphiesma; cellulose; zooxanthellae	SYMBIODINIUM-MICROADRIATICUM FREUDENTHAL; MARINE ARMORED DINOFLAGELLATE; RED TIDE DINOFLAGELLATE; FINE-STRUCTURE; GONYAULAX-POLYEDRA; THECAL PLATES; ELECTRON-MICROSCOPE; LIFE-CYCLE; LINGULODINIUM-POLYEDRUM; PERIDINIUM-TROCHOIDEUM	Dinoflagellates are a major aquatic protist group with amphiesma, multiple cortical membranous "cell wall" layers that contain large circum-cortical alveolar sacs (AVs). AVs undergo extensive remodeling during cell- and life-cycle transitions, including ecdysal cysts (ECs) and resting cysts that are important in some harmful algal bloom initiation-termination. AVs are large cortical vesicular compartments, within which are elaborate cellulosic thecal plates (CTPs), in thecate species, and the pellicular layer (PL). AV-CTPs provide cellular mechanical protection and are targets of vesicular transport that are replaced during EC-swarmer cell transition, or with increased deposition during the cellular growth cycle. AV-PL exhibits dynamical-replacement with vesicular trafficking that are orchestrated with amphiesmal chlortetracycline-labeled Ca2+ stores signaling, integrating cellular growth with different modes of cell division cycle/progression. We reviewed the dynamics of amphiesma during different cell division cycle modes and life cycle stages, and its multifaceted regulations, focusing on the regulatory and functional readouts, including the coral-zooxanthellae interactions.	[Kwok, Alvin Chun Man; Chan, Wai Sun; Wong, Joseph Tin Yum] Hong Kong Univ Sci & Technol, Div Life Sci, Clear Water Bay, Hong Kong, Peoples R China	Hong Kong University of Science & Technology	Kwok, ACM; Wong, JTY (通讯作者)，Hong Kong Univ Sci & Technol, Div Life Sci, Clear Water Bay, Hong Kong, Peoples R China.	alvink@ust.hk; botin@ust.hk		KWOK, Alvin, Chun Man/0000-0002-5611-4512				Abidi W, 2022, FEMS MICROBIOL REV, V46, DOI 10.1093/femsre/fuab051; ADAMICH M, 1976, PLANTA, V130, P1, DOI 10.1007/BF00390837; Aktan Y., 2008, Harmful Algae News, V36, P1; Alldredge AL, 1998, J PLANKTON RES, V20, P393, DOI 10.1093/plankt/20.3.393; ANDERSON DM, 1984, ACS SYM SER, V262, P125; Barott KL, 2015, P NATL ACAD SCI USA, V112, P607, DOI 10.1073/pnas.1413483112; BERDALET E, 1992, J PHYCOL, V28, P267, DOI 10.1111/j.0022-3646.1992.00267.x; Berdalet E., 1991, TOXIC PHYTOPLANKTON, V3, P737; Berdieva Mariia, 2019, Protistology, V13, P57, DOI 10.21685/1680-0826-2019-13-2-2; Bibby B.T., 1972, British phycol J, V7, P85; Biquand E, 2017, ISME J, V11, P1702, DOI 10.1038/ismej.2017.17; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blossom HE, 2012, HARMFUL ALGAE, V17, P40, DOI 10.1016/j.hal.2012.02.010; Bogus K, 2014, J PHYCOL, V50, P254, DOI 10.1111/jpy.12170; Bravo Isabel, 2014, Microorganisms, V2, P11; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Brett CL, 2005, MOL BIOL CELL, V16, P1396, DOI 10.1091/mbc.E04-11-0999; BRICHEUX G, 1992, PROTOPLASMA, V168, P159, DOI 10.1007/BF01666262; Buhmann MT, 2016, J PHYCOL, V52, P463, DOI 10.1111/jpy.12409; Calado AJ, 1999, EUR J PHYCOL, V34, P179, DOI 10.1080/09670269910001736232; CARNELL L, 1994, J CELL BIOL, V127, P693, DOI 10.1083/jcb.127.3.693; Castillo-Medina RE, 2011, LIMNOL OCEANOGR-METH, V9, P460, DOI 10.4319/lom.2011.9.460; Cavalier-Smith T, 2004, EUR J PROTISTOL, V40, P185, DOI 10.1016/j.ejop.2004.01.002; CAVALIERSMITH T, 1991, SYST ASSOC SPEC VOL, V45, P113; Chan WS, 2019, FRONT MICROBIOL, V10, DOI 10.3389/fmicb.2019.00546; CHANAT E, 1991, J CELL BIOL, V115, P1505, DOI 10.1083/jcb.115.6.1505; CHANDLER DE, 1978, J CELL BIOL, V76, P371, DOI 10.1083/jcb.76.2.371; Chen HK, 2015, PLOS ONE, V10, DOI 10.1371/journal.pone.0132519; Cho T, 2017, GENES CELLS, V22, P94, DOI 10.1111/gtc.12458; DEANE EM, 1978, BRIT PHYCOL J, V13, P189, DOI 10.1080/00071617800650241; Deng YY, 2017, FRONT MICROBIOL, V8, DOI 10.3389/fmicb.2017.02450; DODGE J D, 1970, Botanical Journal of the Linnean Society, V63, P53, DOI 10.1111/j.1095-8339.1970.tb02302.x; Dodge J. 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Drugs	FEB	2023	21	2							70	10.3390/md21020070	http://dx.doi.org/10.3390/md21020070			26	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	9K3QN	36827111	gold, Green Published			2025-03-11	WOS:000940785800001
J	El Atfy, H; Coiffard, C; El Beialy, SY; Uhl, D				El Atfy, Haytham; Coiffard, Clement; El Beialy, Salah Y. Y.; Uhl, Dieter			Vegetation and climate change at the southern margin of the Neo-Tethys during the Cenomanian (Late Cretaceous): Evidence from Egypt	PLOS ONE			English	Article							NORTHERN WESTERN-DESERT; ABU GHARADIG BASIN; OIL-FIELD; DINOFLAGELLATE STRATIGRAPHY; SEQUENCE STRATIGRAPHY; BAHARIYA FORMATION; POLLEN GRAINS; FOSSIL LEAVES; PALYNOLOGY; OASIS	Changes in terrestrial vegetation during the mid-Cretaceous and their link to climate and environmental change are poorly understood. In this study, we use plant macrofossils and analysis of fossil pollen and spores from the Western Desert, Egypt, to assess temporal changes in plant communities during the Cenomanian. The investigated strata have relatively diverse sporomorph assemblages, which reflect the nature of parent vegetation. Specifically, the palynofloras represent ferns, conifers, monosulcate pollen producers, Gnetales, and a diverse group of angiosperms. Comparisons of both, dispersed palynoflora and plant macrofossils reveal different characteristics of the palaeoflora owing to a plethora of taphonomical and ecological biases including the depositional environment, production levels, and discrepancies between different plant organs. A combination of detailed records of sporomorphs, leaves, and charcoal from the studied successions provide new understandings of the palaeoclimate and palaeogeography during the Cenomanian and Albian-Cenomanian transition in Egypt. The mixed composition of the palynofloral assemblages reflects the presence of different depositional situations with a weak marine influence, as evidenced by a minor dinoflagellate cysts component. The local vegetation comprised various categories including herbaceous groups including ferns and eudicots, fluvial, open environments, and xeric arboreal communities dominated by Cheirolepidiaceae and perhaps including drought- and/or salt-tolerating ferns (Anemiaceae) and other gymnosperms (Araucariaceae, Ginkgoales, Cycadales, and Gnetales) as well as angiosperms. The presence of riparian and freshwater wetland communities favouring aquatic and/or hygrophilous ferns (of Salviniaceae and Marsileaceae), is noted. The wide variation of depositional settings derived from the palynological data may be attributed to a prevalent occurrence of producers in local vegetation during the early Cenomanian of Egypt. For the purpose of this work on the studied Bahariya Formation and its equivalent rock units, where iconic dinosaurs and other fossil fauna roamed, we attempt to improve the understanding of Egypt's Cenomanian climate, which is reconstructed as generally warm and humid punctuated by phases of considerably drier conditions of varying duration.	[El Atfy, Haytham] Univ Tubingen, Dept Geosci, Tubingen, Germany; [El Atfy, Haytham; El Beialy, Salah Y. Y.] Mansoura Univ, Fac Sci, Geol Dept, Mansoura, Egypt; [Coiffard, Clement] Free Univ Berlin, Inst Biol, Struct & Funct Plant Divers Grp, Berlin, Germany; [Uhl, Dieter] Senckenberg Forschungsinstitut & Nat Museum Frankf, Frankfurt, Germany	Eberhard Karls University of Tubingen; Egyptian Knowledge Bank (EKB); Mansoura University; Free University of Berlin	El Atfy, H (通讯作者)，Univ Tubingen, Dept Geosci, Tubingen, Germany.; El Atfy, H (通讯作者)，Mansoura Univ, Fac Sci, Geol Dept, Mansoura, Egypt.	El-Atfy@daad-alumni.de	Atfy, Haytham/AAT-2276-2021; Coiffard, Clément/C-8405-2012	Coiffard, Clement/0000-0003-4309-074X	Alexander von Humboldt Foundation [EGY - 1190326]	Alexander von Humboldt Foundation(Alexander von Humboldt Foundation)	The authors are indebted to the Egyptian General Petroleum Corporation (EGPC) for providing the samples and well logs for the studied boreholes. H.E. thanks Ahmed Mohamed (Mansoura University) for his help in the fieldwork, Thomas Lechner (The University of Tubingen, Germany) for helping to edit the mega-plant plates, Mohamed Zobaa (The University of Texas Permian Basin, USA), and Amr Deaf (Assiut University, Egypt) for giving access to some of their published illustrations. The authors wish to thank Ludwig Luthardt (Museum fur Naturkunde Berlin, Germany) for updating the curating data of megaflora specimens and also three anonymous reviewers, as well as the Editor, for their insightful comments and constructive criticism that helped to improve the manuscript.	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J	Fatourou, E; Kafetzidou, A; Marret, F; Panagiotopoulos, K; Kouli, K				Fatourou, Eugenia; Kafetzidou, Aikaterini; Marret, Fabienne; Panagiotopoulos, Konstantinos; Kouli, Katerina			Late Quaternary Ponto-Caspian dinoflagellate cyst assemblages from the Gulf of Corinth, Central Greece (eastern Mediterranean Sea)	MARINE MICROPALEONTOLOGY			English	Article						Glacial; interglacial cycles; Sea-level change; Dinoflagellate cyst assemblages; Sea-surface salinity; Northeastern Mediterranean Sea	LAST INTERGLACIAL COMPLEX; NORTH-ATLANTIC OCEAN; BLACK-SEA; TENAGHI PHILIPPON; MARMARA SEA; CLIMATE VARIABILITY; SPINIFERITES-CRUCIFORMIS; SEQUENCE STRATIGRAPHY; SURFACE SEDIMENTS; MARINE-SEDIMENTS	We present here the first long Quaternary record of organic-walled dinoflagellate cyst assemblages analysed from sediment cores retrieved during the International Ocean Discovery Program (IODP) Expedition 381 in the Gulf of Corinth. Site M0078A is located in the central part of the Gulf of Corinth (GoC), a semi-isolated marine basin that was repeatedly isolated and reconnected to the Mediterranean Sea during the Quaternary glacial/interglacial cycles. Our results show that dinoflagellate cysts are sorted in two major ecogroups, each group alternating between marine and isolated/brackish conditions. The marine intervals are characterised by high dinocyst di-versity whereas the isolated intervals are dominated by taxa thriving in low-salinity conditions such as Spiniferites cruciformis and Pyxidinopsis psilata. In several of these assemblages, S. cruciformis is so prevalent that it forms almost monospecific assemblages. The low salinity dinocyst assemblages are reported for the first time outside the Ponto-Caspian region and they show a close affinity to modern assemblages from the Black Sea, Caspian Sea and Marmara Sea. The alternations between marine and brackish conditions recorded in the Gulf of Corinth reflect changes in surface water salinity (SSS) and temperature (SST), in response to the Quaternary glacial-interglacial cycles. These seem to be in good agreement with regional and global marine isotope and sea-level records. Our findings suggest that the study region sensitively responds to climate forcing at orbital time scales and that local factors most likely drive shifts in dinoflagellate species composition and diversity.	[Fatourou, Eugenia; Kafetzidou, Aikaterini; Panagiotopoulos, Konstantinos; Kouli, Katerina] Natl & Kapodistrian Univ Athens, Nat Sci Geol & Geoenvironm, Athens, Greece; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool, England; [Panagiotopoulos, Konstantinos] Univ Cologne, Inst Geol & Mineral, Cologne, Germany	National & Kapodistrian University of Athens; University of Liverpool; University of Cologne	Kouli, K (通讯作者)，Natl & Kapodistrian Univ Athens, Nat Sci Geol & Geoenvironm, Athens, Greece.	efatourou@geol.uoa.gr; F.Marret@liverpool.ac.uk; panagiotopoulos.k@uni-koeln.de; akouli@geol.uoa.gr	Panagiotopoulos, Konstantinos/P-3823-2019; Kouli, Katerina/M-8243-2013	Fatourou, Eugenia/0000-0002-8147-3365; Marret-Davies, Fabienne/0000-0003-4244-0437	Hellenic Foundation of Research and Innovation (H.F.R.I) [1026]	Hellenic Foundation of Research and Innovation (H.F.R.I)	The study material was retrieved during the IODP Exp. 381. The research work was supported by the Hellenic Foundation of Research and Innovation (H.F.R.I) under the ?First Call for H.F.R.I. Research Projects to support Faculty members and Researchers and the procure-ment of high-cost research equipment grant? (Project Number: 1026, Quaternary Environmental Changes in the Corinth Rift Area: the IODP 381 palynological record: QECCoRA) . The authors are very grateful for the constructive comments from the two reviewers and the editor.	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Micropaleontol.	MAR	2023	179								102211	10.1016/j.marmicro.2023.102211	http://dx.doi.org/10.1016/j.marmicro.2023.102211		JAN 2023	16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	C7IF9					2025-03-11	WOS:000963605000001
J	Kim, SY; Park, T; Marret, F; Potvin, E; Cho, KH; Jung, J; Lee, Y; La, HS; Ha, SY; Kim, SK; Kang, SH; Yang, EJ; Nam, SI; Hong, JK				Kim, So -Young; Park, Taewook; Marret, Fabienne; Potvin, Eric; Cho, Kyoung-Ho; Jung, Jinyoung; Lee, Youngju; La, Hyoung Sul; Ha, Sun -Yong; Kim, Seung-Kyu; Kang, Sung -Ho; Yang, Eun Jin; Nam, Seung-Il; Hong, Jong Kuk			Strong regionalism in dinoflagellate cysts in recent sediments from the Chukchi-East Siberian Seas, Arctic Ocean	PROGRESS IN OCEANOGRAPHY			English	Review							SURFACE SEDIMENTS; HYDROGRAPHIC CONDITIONS; BERING STRAIT; PHYTOPLANKTON COMMUNITY; DINOCYST ASSEMBLAGES; MARINE-SEDIMENTS; LATE QUATERNARY; PACIFIC INFLOW; ICE; SHELF	The Pacific sector of the Arctic Ocean, a region with the fastest sea-ice loss in recent decades, is experiencing unprecedented biological regime shifts in its marine ecosystems today. However, a shelf-wide characterization of marine plankton communities over this region and environmental processes behind it remain largely unresolved, despite phytoplankton phenology is now considered to be an important factor for assessing how Arctic Ocean interacts with global climate change. Here, we present the first detailed description of recent dinoflagellate cyst assemblages in 32 surface sediment samples from the Chukchi-East Siberian Sea shelves, the Pacific Arctic Ocean, to examine their biogeographic patterns and associated environmental forcing factors. We find a strong regionalization in the species composition and distribution along the shallow-shelf cyst accumulation zone; in the Chukchi Sea sector, northward flow of warm-Pacific water along with extreme seasonality, sufficient nutrient supplies and higher light availability leads to a large occupation of cosmopolitan, opportunistic-nature taxa, whilst the East Siberian Sea sector with more extensive sea-ice cover and lower temperatures is primarily dominated by "round brown spiny cyst" taxa that have a strong affinity for cold, polar conditions. Specifically, an exclusive dominance of heterotrophic taxa at the East Siberian Sea region is inferred to be closely tied to Atlantic-origin water intrusions that lift nutrient-rich, cold bottom water up to oligotrophic surface layer to grow diatoms and other prey organisms. The observed contrast in this geographical "hot spot", where the Pacific-and Atlantic-origin waters face each other, clearly manifests a growing expansion of southern waters into an increasingly ice-free Arctic Ocean that reshapes Arctic Ocean biogeography from the base of marine food chains. Our study highlights considerable potential of dinoflagellate cysts as a valuable environmental proxy to indicate complex interactions between ocean physics and marine biology under the rapidly changing Arctic climate system.	[Kim, So -Young; Park, Taewook; Cho, Kyoung-Ho; Jung, Jinyoung; Lee, Youngju; La, Hyoung Sul; Ha, Sun -Yong; Kang, Sung -Ho; Yang, Eun Jin; Nam, Seung-Il; Hong, Jong Kuk] Korea Polar Res Inst, Div Ocean Sci, Incheon 21990, South Korea; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, England; [Potvin, Eric] Univ Concepcion, Inst Milenio Oceanog, POB 160-C, Concepcion, Chile; [Kim, Seung-Kyu] Incheon Natl Univ, Coll Nat Sci, Dept Marine Sci, Incheon 22012, South Korea	Korea Polar Research Institute (KOPRI); University of Liverpool; Universidad de Concepcion; Incheon National University	Kim, SY (通讯作者)，Korea Polar Res Inst, Div Ocean Sci, Incheon 21990, South Korea.; Marret, F (通讯作者)，Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, England.	kimsy@kopri.re.kr; F.Marret@liverpool.ac.uk		Marret-Davies, Fabienne/0000-0003-4244-0437	Korea Institute of Marine Science & Technology Promotion (KIMST) - Ministry of Oceans and Fisheries [20210605]; Korean Ministry of Ocean and Fisheries (KIMST) [20160247, 20210632]	Korea Institute of Marine Science & Technology Promotion (KIMST) - Ministry of Oceans and Fisheries(Korea Institute of Marine Science & Technology Promotion (KIMST)); Korean Ministry of Ocean and Fisheries (KIMST)	We thank the captain and crew of R/V ARAON for the logistic and technical assistance in collecting the investigated sediment samples. This research was supported by Korea Institute of Marine Science & Technology Promotion (KIMST) funded by the Ministry of Oceans and Fisheries (20210605, Korea-Arctic Ocean Warming and Response of Ecosystem, KOPRI). This work was also supported by the Korean Ministry of Ocean and Fisheries (KIMST, 20160247 and 20210632). We warmly thank Sebastien Zaragosi (University of Bordeaux) for his help with the extraction of environmental parameters from various data-bases. The authors wish to thank two anonymous reviewers and the editor for their constructive comments improving the manuscript.	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Oceanogr.	FEB	2023	211								102970	10.1016/j.pocean.2023.102970	http://dx.doi.org/10.1016/j.pocean.2023.102970		JAN 2023	15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	8O5NJ					2025-03-11	WOS:000925881400001
J	Mendes, M; Descamps, GS; Fernandes, P; Lopes, G; Jorge, RCGS; Pereira, Z				Mendes, Marcia; Descamps, Gabrielle S.; Fernandes, Paulo; Lopes, Gilda; Jorge, Raul Carlos G. S.; Pereira, Zelia			The upper Hauterivian-Barremian (Lower Cretaceous) Arrifes section (Algarve Basin, Southern Portugal): A palynostratigraphic and palaeoenvironmental approach	CRETACEOUS RESEARCH			English	Article						Hauterivian-Barremian; Shallow marine carbonates; Dinoflagellate cysts; Palynofacies; Algarve Basin	COASTAL DEPOSITS; WESTERN; STRATIGRAPHY; RECOGNITION; COMMUNITIES; PALYNOLOGY; RECORDS; POLLEN	Integrated sedimentological, palynological, and palynofacies analyses of the Arrifes section in the central Algarve Basin (southern Portugal) provided new information on the age and environments of this Lower Cretaceous sequence. The sedimentary succession at the Arrifes section consists of fossiliferous inter-bedded limestones, marly limestones, and marls, dated as latest Hauterivian to late Barremian age (Lower Cretaceous) based on key dinoflagellate taxa. During this interval, the Arrifes area records cli-matic shifts and, multiple sea-level fluctuations; overall deposition was in shallow subtidal to intertidal settings, with deposition of carbonate and marly sediments. During the latest Hauterivian to earliest Barremian interval, an evident sea-level fall culminated in the subaerial exposure of the local carbonate ramp with increased influx of clastic sediments. However, during the Barremian, both sedimentological and palynological analyses suggest an overall deepening of the water depth towards the top of the section. These overall increase in the water column are confirmed by oscillation of terrestrial/marine palynomorph groups and supported by dinosaur track levels at the top of the succession; the latter indicate that sedimentation occurred in intertidal to subtidal environments. Finally, an attempt was made to correlate the Arrifes section with other sections from the Algarve Basin, as well as with broader region. These new data suggest a setting in the Tethyan basin influenced during the latest Hauterivian to the end of the Barremian. These new data allow local correlations and new palynological ages and paleoenvironmental interpretations for the Lower Cretaceous succession of the Algarve Basin.(c) 2022 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).	[Mendes, Marcia; Pereira, Zelia] Natl Lab Energy & Geol, LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal; [Descamps, Gabrielle S.; Fernandes, Paulo; Lopes, Gilda] Univ Algarve, Ctr Marine & Environm Res, CIMA, Campus Gambelas, P-8005139 Faro, Portugal; [Lopes, Gilda] Univ Sheffield, Sch Biosci, Plants Photosynth & Soil Cluster, Alfred Denny Bldg,Western Bank, Sheffield S10 2TN, England; [Jorge, Raul Carlos G. S.] Univ Lisbon, Fac Ciencias, Inst Dom Luiz IDL, Edificio C6,Piso 4, P-1749016 Lisbon, Portugal	Laboratorio Nacional de Energia e Geologia IP (LNEG); Universidade do Algarve; University of Sheffield; Universidade de Lisboa	Mendes, M (通讯作者)，Natl Lab Energy & Geol, LNEG, Rua Amieira, P-4465965 Sao Mamede de Infesta, Portugal.	marcia.mendes@lneg.pt; gabriellesofiadescamps@gmail.com; pfernandes@ualg.pt; g.m.lopes@sheffield.ac.uk; rjorge@fc.ul.pt; zelia.pereira@lneg.pt	Pereira, Zelia/B-2740-2017; Jorge, Raul C. G. Santos/J-6992-2013; Fernandes, Paulo/J-6577-2014; Mendes, Marcia/E-2897-2019; Rodrigues Lopes, Gilda Maria/AAS-1742-2020	Pereira, Zelia/0000-0003-3056-6219; Jorge, Raul C. G. Santos/0000-0002-3875-6538; Fernandes, Paulo/0000-0003-4888-0230; Mendes, Marcia/0000-0003-2290-891X; Rodrigues Lopes, Gilda Maria/0000-0002-6866-5127	Portuguese Fundacao para a Ciencia e a Tecnologia (FCT) I.P./MCTES through national funds (PIDDAC) [UIDB/50019/2020]; FCT [UID/00350/2020CIMA]	Portuguese Fundacao para a Ciencia e a Tecnologia (FCT) I.P./MCTES through national funds (PIDDAC); FCT(Fundacao para a Ciencia e a Tecnologia (FCT))	We dedicate this work to the memory of Prof. Miguel Magalhaes Ramalho. This work was funded by the Portuguese Fundacao para a Ciencia e a Tecnologia (FCT) I.P./MCTES through national funds (PIDDAC) -UIDB/50019/2020. Gabrielle Descamps, Paulo Fernandes, and Gilda Lopes would like to acknowledge the financial support of the FCT to CIMA through UID/00350/2020CIMA. We would like to thank Dr. Robert Fensome and Dr. Pedro Callapez for taking the time and effort necessary to review the manuscript. We sincerely appreciate all valuable comments and suggestions, which helped us to improve the quality of the manuscript.	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Res.	APR	2023	144								105433	10.1016/j.cretres.2022.105433	http://dx.doi.org/10.1016/j.cretres.2022.105433		JAN 2023	19	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	8J9FA		Green Published, hybrid			2025-03-11	WOS:000922715500001
J	Mansour, A; Xia, GQ; Fu, XG; Wang, J				Mansour, Ahmed; Xia, Guoqing; Fu, Xiugen; Wang, Jian			Sea level changes and sequence stratigraphy of the Lower-Middle Jurassic Quse and Sewa formations in the Qiangtang Basin, central Tibet: Geochemical and palynological perspectives	INTERNATIONAL GEOLOGY REVIEW			English	Article						Sea level cycles; Transgressive-regressive sequences; chemostratigraphy; palynological analysis; toarcian oil shales; bilong co section	SEDIMENTARY ORGANIC-MATTER; HEMIPELAGIC CARBONATES; DYNAMIC TOPOGRAPHY; NORTHERN TIBET; BLACK SHALES; AREA; ENVIRONMENT; CONTINENTS; COLLISIONS; EVOLUTION	Sequence stratigraphy is a commonly used approach to understand basin-fill history and the occurrence of conventional reservoir and/or probable source rocks. Reconstructing a sequence stratigraphic framework in carbonates, marls, and organic-rich mudstones is challenging due to environmental, petrophysical, and sedimentological variations that can be subtle, whereas seismic data may be lacking or of limited use. For this reason, incorporation between palynological analysis and chemostratigraphic profiles is becoming increasingly common to facilitate sequence stratigraphic reconstruction. This study investigates the Quse (lower Toarcian) and Sewa formations (upper Bajocian-Bathonian) in the Bilong Co section from the Qiangtang Basin of central Tibet. Eighty-three rock samples were analysed for their whole-rock inorganic geochemical composition, of which 25 rock samples were tested for palynological and palynofacies analyses. The palynological composition defined two associations for the study section. The lower part of the Bilong Co section consisted is dominated by a moderate to high abundance of opaque phytoclasts versus low to moderate amorphous organic matter (AOM) content with a high concentration of sphaeromorphs pollen grains, revealing deposition of this interval at times of low relative sea level in fluvio-deltaic settings. The middle to upper parts of the section comprised of significantly high AOM content versus low phytoclasts and high content of sphaeromorphs pollen grains, but with increasing the relative abundance of dinoflagellate cysts, indicating a phase of high sea level. Chemostratigraphic variations relevant to changes in relative sea level delineated the subdivision of the Quse and Sewa formations into two and three third-order transgressive-regressive sequences, respectively. The collision between the Lhasa and Qiangtang blocks during the Early-Middle Jurassic is suggested to control consequent subduction and sea level highstand, especially during deposition of the Sewa Formation. Geochemical proxies that relate to shelf carbonate production are calcium, strontium, whereas proxies that relate to siliciclastics include titanium, zirconium, manganese, aluminium, and silicon, other redox-sensitive proxy like uranium is also implemented. This indicates that chemostratigraphic proxies are a promising tool for the interpretation of sea level cyclicity in terms of systems tracts and bounding surfaces.	[Mansour, Ahmed; Fu, Xiugen; Wang, Jian] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu, Peoples R China; [Mansour, Ahmed; Fu, Xiugen; Wang, Jian] Southwest Petr Univ, Sch Geosci & Technol, Chengdu, Peoples R China; [Mansour, Ahmed] Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt; [Xia, Guoqing] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China; [Xia, Guoqing] Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu, Peoples R China	Southwest Petroleum University; Southwest Petroleum University; Egyptian Knowledge Bank (EKB); Minia University; Chengdu University of Technology; Chengdu University of Technology	Mansour, A (通讯作者)，Minia Univ, Fac Sci, Geol Dept, Al Minya 61519, Egypt.; Xia, GQ (通讯作者)，Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploitat, Chengdu 610059, Peoples R China.	ahmedmans48@mu.edu.eg; xiaguoqing2012@cdut.cn	Mansour, Ahmed/AAR-4969-2020		National Natural Science Foundation, China [41772105, 41972115]	National Natural Science Foundation, China(National Natural Science Foundation of China (NSFC))	This work was financially supported by two research grants No. 41772105 and No. 41972115 from the National Natural Science Foundation, China. 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Geol. Rev.	OCT 11	2023	65	18					2879	2899		10.1080/00206814.2023.2167127	http://dx.doi.org/10.1080/00206814.2023.2167127		JAN 2023	21	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	T5WZ6					2025-03-11	WOS:000914371600001
J	Barrenechea Angeles, I; Romero-Martínez, ML; Cavaliere, M; Varrella, S; Francescangeli, F; Piredda, R; Mazzocchi, MG; Montresor, M; Schirone, A; Delbono, I; Margiotta, F; Corinaldesi, C; Chiavarini, S; Montereali, MR; Rimauro, J; Parrella, L; Musco, L; Dell'Anno, A; Tangherlini, M; Pawlowski, J; Frontalini, F				Barrenechea Angeles, Ines; Romero-Martinez, Maria Lorena; Cavaliere, Marco; Varrella, Stefano; Francescangeli, Fabio; Piredda, Roberta; Mazzocchi, Maria Grazia; Montresor, Marina; Schirone, Antonio; Delbono, Ivana; Margiotta, Francesca; Corinaldesi, Cinzia; Chiavarini, Salvatore; Montereali, Maria Rita; Rimauro, Juri; Parrella, Luisa; Musco, Luigi; Dell'Anno, Antonio; Tangherlini, Michael; Pawlowski, Jan; Frontalini, Fabrizio			Encapsulated in sediments: eDNA deciphers the ecosystem history of one of the most polluted European marine sites	ENVIRONMENT INTERNATIONAL			English	Article						Metabarcoding; Biota; Human impact; Contaminated marine sediments; Biodiversity reconstruction; Mediterranean Sea	ALEXANDRIUM-CATENELLA; DINOFLAGELLATE CYSTS; ECOLOGICAL QUALITY; BIOTIC INDEX; IDENTIFICATION; COMMUNITIES; ENRICHMENT; ESTUARINE; VESUVIUS; BAGNOLI	The Anthropocene is characterized by dramatic ecosystem changes driven by human activities. The impact of these activities can be assessed by different geochemical and paleontological proxies. However, each of these proxies provides only a fragmentary insight into the effects of anthropogenic impacts. It is highly challenging to reconstruct, with a holistic view, the state of the ecosystems from the preindustrial period to the present day, covering all biological components, from prokaryotes to multicellular eukaryotes. Here, we used sedimentary ancient DNA (sedaDNA) archives encompassing all trophic levels of biodiversity to reconstruct the two century -natural history in Bagnoli-Coroglio (Gulf of Pozzuoli, Tyrrhenian Sea), one of the most polluted marine-coastal sites in Europe. The site was characterized by seagrass meadows and high eukaryotic diversity until the beginning of the 20th century. Then, the ecosystem completely changed, with seagrasses and associated fauna as well as diverse groups of planktonic and benthic protists being replaced by low diversity biota dominated by dinophyceans and infaunal metazoan species. The sedaDNA analysis revealed a five-phase evolution of the area, where changes appear as the result of a multi-level cascade effect of impacts associated with industrial activities, urbanization, water circulation and land-use changes. The sedaDNA allowed to infer reference conditions that must be considered when restoration actions are to be implemented.	[Barrenechea Angeles, Ines] Univ Geneva, Dept Earth Sci, 13 Rue Maraichers, CH-1205 Geneva, Switzerland; [Barrenechea Angeles, Ines; Pawlowski, Jan] Univ Geneva, Dept Genet & Evolut, CH-1205 Geneva, Switzerland; [Romero-Martinez, Maria Lorena; Mazzocchi, Maria Grazia; Montresor, Marina; Margiotta, Francesca; Musco, Luigi; Tangherlini, Michael] Stn Zool Anton Dohrn, I-80121 Naples, Italy; [Cavaliere, Marco; Frontalini, Fabrizio] Univ Urbino Carlo Bo, Dept Pure & Appl Sci, I-61029 Urbino, Italy; [Varrella, Stefano; Corinaldesi, Cinzia] Polytech Univ Marche, Dept Mat Environm Sci & Urban Planning, I-60131 Ancona, Italy; [Francescangeli, Fabio] Univ Fribourg, Dept Geosci, CH-1700 Fribourg, Switzerland; [Piredda, Roberta] Univ Bari Aldo Moro, Dept Vet Med, I-70010 Bari, Italy; [Schirone, Antonio; Delbono, Ivana] ENEA, Marine Environm Res Ctr S Teresa, Dept Sustainabil, I-19032 Pozzuolo Di Lerici, Italy; [Chiavarini, Salvatore; Montereali, Maria Rita] ENEA, CR Casaccia, Dept Sustainabil, I-00123 Rome, Italy; [Rimauro, Juri; Parrella, Luisa] ENEA, CR Portici, Dept Sustainabil, I-80055 Naples, Italy; [Musco, Luigi] Univ Salento, Dipartimento Sci & Tecnol Biol Ambientali, I-73100 Lecce, Italy; [Dell'Anno, Antonio] Polytech Univ Marche, Dept Life & Environm Sci, I-60131 Ancona, Italy; [Pawlowski, Jan] ID Gene Ecodiagnost Ltd, CH-1228 Plan Les Ouates, Switzerland; [Pawlowski, Jan] Polish Acad Sci, Inst Oceanol, PL-81712 Sopot, Poland	University of Geneva; University of Geneva; Stazione Zoologica Anton Dohrn; University of Urbino; Marche Polytechnic University; University of Fribourg; Universita degli Studi di Bari Aldo Moro; Italian National Agency New Technical Energy & Sustainable Economics Development; Italian National Agency New Technical Energy & Sustainable Economics Development; Italian National Agency New Technical Energy & Sustainable Economics Development; University of Salento; Marche Polytechnic University; Polish Academy of Sciences; Institute of Oceanology of the Polish Academy of Sciences	Barrenechea Angeles, I (通讯作者)，Univ Geneva, Dept Earth Sci, 13 Rue Maraichers, CH-1205 Geneva, Switzerland.	Ines.BarrenecheaAngeles@unige.ch; maria.martinez@szn.it; m.cavaliere6@campus.uniurb.it; s.varrella@staff.univpm.it; fabio.francescangeli@unifr.ch; roberta.piredda@uniba.it; mazzocchi@szn.it; marina.montresor@szn.it; antonio.schirone@enea.it; ivana.delbono@enea.it; francesca.margiotta@szn.it; c.corinaldesi@univpm.it; salvatore.chiavarini@enea.it; mariarita.montereali@enea.it; juri.rimauro@enea.it; luisa.parrella@enea.it; luigi.musco@unisalento.it; a.dellanno@staff.univpm.it; michael.tangherlini@szn.it; janpawlowski@iopan.pl; fabrizio.frontalini@uniurb.it	Francescangeli, Fabio/AAS-1693-2020; Varrella, Stefano/GXF-3079-2022; Montereali, Maria Rita/AFU-8043-2022; Frontalini, Fabrizio/C-4819-2008; Tangherlini, Michael/AAL-8923-2021; Piredda, Roberta/ABC-8987-2020; Pawlowski, Jan/JNS-6857-2023; Margiotta, Francesca/IST-5703-2023; Dell'Anno, Antonio/G-9468-2012; Barrenechea Angeles, Ines/JAO-3559-2023; Musco, Luigi/AAY-8543-2021	Piredda, Roberta/0000-0002-6672-439X; Varrella, Stefano/0000-0002-8582-3502; Dell'Anno, Antonio/0000-0002-4324-7834; Romero Martinez, Maria Lorena/0000-0002-7608-9529; Francescangeli, Fabio/0000-0002-8309-3315; Margiotta, Francesca/0000-0003-0757-5934; Barrenechea Angeles, Ines/0000-0002-8051-4110	Project ABBaCo - Italian Ministry for Education, University and Research [C62F16000170001]; Stazione Zoologica Anton Dohrn; Swiss National Science Foundation [31003A_179125]; Swiss National Science Foundation (SNF) [31003A_179125] Funding Source: Swiss National Science Foundation (SNF)	Project ABBaCo - Italian Ministry for Education, University and Research; Stazione Zoologica Anton Dohrn; Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); Swiss National Science Foundation (SNF)(Swiss National Science Foundation (SNSF))	This study was supported by the project ABBaCo funded by the Italian Ministry for Education, University and Research, grant number C62F16000170001. M.L. Romero -Martinez was supported by a PhD fellowship from Stazione Zoologica Anton Dohrn. I.B.A and J.P were supported by the Swiss National Science Foundation grant 31003A_179125.	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Int.	FEB	2023	172								107738	10.1016/j.envint.2023.107738	http://dx.doi.org/10.1016/j.envint.2023.107738		JAN 2023	12	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	8L2AQ	36641836	Green Published, gold			2025-03-11	WOS:000923590000001
J	Liu, XH; Liu, YY; Chai, ZY; Hu, ZX; Tang, YZ				Liu, Xiaohan; Liu, Yuyang; Chai, Zhaoyang; Hu, Zhangxi; Tang, Ying Zhong			A combined approach detected novel species diversity and distribution of dinoflagellate cysts in the Yellow Sea, China	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate resting cysts; Diversity; Distribution pattern; Yellow Sea Cold Water Mass (YSCWM); Metabarcoding; Single-cyst morpho-molecular identification	HARMFUL ALGAL BLOOMS; SURFACE SEDIMENTS; ALEXANDRIUM DINOPHYCEAE; GYMNODINIUM-CATENATUM; PHYSICAL PROCESSES; NOV DINOPHYCEAE; BALLAST WATER; RESTING CYSTS; PHYTOPLANKTON; MORPHOLOGY	Resting cysts of dinoflagellates seed harmful algal blooms (HABs) and their geographic expansion, which makes it fundamentally important to obtain comprehensive inventories of dinoflagellate resting cysts in HABs-prone regions. The Yellow Sea (YS) of China has observed numerous outbreaks of dinoflagellate HABs with some novel species recorded recently indicating an underestimated HABs-causing species diversity. We report our investigation of dinoflagellate cysts of YS via an approach combining metabarcoding sequencing and single-cyst morpho-molecular identification, which identified many novel cyst species and a significant controlling effect of the Yellow Sea Cold Water Mass on cyst composition. The metabarcoding and single cyst-based sequencing detected 11 cyst species never being unambiguously reported in China, 10 never reported as cyst producers, and 3 HABs-causing species never reported from YS. Our detections of many potentially toxic or HABs-causative, particularly novel, cysts and distribution pattern provide important insights into the risks and ecology of dinoflagellate HABs.	[Liu, Xiaohan; Liu, Yuyang; Chai, Zhaoyang; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, CAS Key Lab Marine Ecol & Environm Sci, Inst Oceanol, Qingdao 266071, Peoples R China; [Liu, Yuyang; Chai, Zhaoyang; Hu, Zhangxi; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Liu, Yuyang; Chai, Zhaoyang; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Liu, Xiaohan] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, 7 Nanhai Rd, Qingdao 266071, Peoples R China; [Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, 7 Nanhai Rd, Qingdao 266071, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Institute of Oceanology, CAS	Hu, ZX; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, 7 Nanhai Rd, Qingdao 266071, Peoples R China.	huzx@gdou.edu.cn; yingzhong.tang@qdio.ac.cn	Li, Yang/KFB-5350-2024; Chai, Zhaoyang/F-7485-2017; ZHANG, hui jie/HTN-1690-2023		Science & Technology Basic Resources Investigation Program of China [2018FY100200]; Science and Technology Innovation Project of Laoshan Laboratory [LSKJ202203700]; National Science Foundation of China [42106199, 41976134]	Science & Technology Basic Resources Investigation Program of China; Science and Technology Innovation Project of Laoshan Laboratory; National Science Foundation of China(National Natural Science Foundation of China (NSFC))	This work was financially supported by the Science & Technology Basic Resources Investigation Program of China (2018FY100200) , the Science and Technology Innovation Project of Laoshan Laboratory (LSKJ202203700) , and the National Science Foundation of China (No. 42106199, 41976134) .	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J	Gao, JF; Su, Q				Gao, Junfeng; Su, Qiang			The relationship between inorganic nutrients and diversity of dinoflagellate cysts: An evaluation from the perspective of species abundance distribution	FRONTIERS IN MARINE SCIENCE			English	Article						dinoflagellate cysts; inorganic nutrients; coastal ecosystem; species abundance distribution; fractal model; Zipf's law	PLANT DIVERSITY; MARINE; PHYTOPLANKTON; SEDIMENTS; NITROGEN; EUTROPHICATION; ESTUARIES; PATTERNS; INDEXES; BAY	The relationships between the inorganic nutrients and diversity of dinoflagellate cysts (the N-Dc relationships) are one of the most central issues in coastal ecology. It is not only an important pathway to explore the ecological processes of plankton, but also a key element for assessing eutrophication in marine ecosystems. Although the N-Dc relationships have been studied for many years, they have remained controversial, which may be attributed to (1) using samples collected from a single source (2) considering an insufficient range of nutrient concentrations (3) rarely taking into account species abundance distributions (SAD) that could better represent diversity. In this study, the N-Dc relationships are evaluated according to a compiled dataset, which cover the wide range of nutrient concentrations. Species diversity of cysts are estimated by four common diversity metrics and a new SAD parameter. Results show that all diversity metrics are negative with nutrients, which supports that low diversity of cysts could be considered as a signal of eutrophication. Additionally, this study finds a new pattern that SAD of cysts (N-r/N-1, N-r and N-1 is the abundance of the r-th and the first species in descending order) with decreasing nutrients appears to gradually approach 1: 1/2: 1/3 horizontal ellipsis . In the future, if this pattern can be verified by more investigations, understanding the negative N-Dc relationships is more likely to provide new direction for assessing and managing eutrophication in coastal ecosystem, and even for exploring the general mechanisms determining diversity.	[Gao, Junfeng; Su, Qiang] Univ Chinese Acad Sci UCAS, Coll Earth & Planetary Sci CEPS, Beijing, Peoples R China		Su, Q (通讯作者)，Univ Chinese Acad Sci UCAS, Coll Earth & Planetary Sci CEPS, Beijing, Peoples R China.	sqiang@ucas.ac.cn	Su, Qiang/H-3616-2017; Gao, Junfeng/JDV-8786-2023	Gao, Junfeng/0000-0003-3334-3555	National Natural Science Foundation of China [42071137, 41676113]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	Funding This work was supported by the National Natural Science Foundation of China (Grant Nos. 42071137 and 41676113). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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Mar. Sci.	JAN 12	2023	9								1089331	10.3389/fmars.2022.1089331	http://dx.doi.org/10.3389/fmars.2022.1089331			9	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	8D6RT		gold			2025-03-11	WOS:000918418800001
J	Pires, E; Lana, PD; Mafra, LL Jr				Pires, Estela; Lana, Paulo da Cunha; Mafra Jr, Luiz Laureno			Phycotoxins and marine annelids - A global review	HARMFUL ALGAE			English	Review						Marine annelids; Algal toxins; Benthic dinoflagellates; Biomonitoring; Ecotoxicology; Biotoxins	ENCHYTRAEUS-CRYPTICUS ANNELIDA; OKADAIC ACID ACCUMULATION; HARMFUL ALGAL BLOOMS; RED-TIDE TOXINS; DOMOIC ACID; ANTIOXIDANT RESPONSES; VEGETATIVE CELLS; SHELLFISH TOXINS; PSEUDO-NITZSCHIA; RESTING CYSTS	Several species of microalgae can produce potent phycotoxins that negatively affect aquatic organisms and their consumers following different exposure routes, as well as toxicokinetic (TK) and toxicodynamic (TD) processes. Benthic organisms are especially vulnerable as they are exposed to both benthic and planktonic species causative of harmful algal blooms (HABs). While benthic algae can come into direct contact with annelids during substrate remobilization, planktonic cells can settle to the bottom mostly during senescence and/or encystment stages, and in shallow and calm waters. We performed a systematic, qualitative review of the literature on the phycotoxin TK and TD processes in marine annelids, summarizing the most relevant findings and general trends. Besides, by using innovative analytical/statistical approaches, we were able to detect patterns and gaps in the current literature, thus pointing to future research directions. We retrieved and analyzed studies involving diarrhetic shellfish toxins (DSTs), paralytic shellfish toxins (PSTs), brevetoxins (PbTXs), domoic acid (DA), as well as palytoxin and its congeners, the ovatoxins (treated together as PLTXs). It is worth mentioning that studies evaluating other phycotoxins (e.g., ciguatoxins, yessotoxins) were not found in the literature. The absence of data on PbTXs, PSTs and DA is the largest gap hampering TK assessment in annelids, although some relevant information on TD is already available. Whereas lethal effects from DSTs have not been reported, more potent toxins like PbTXs, PSTs, DA and those grouped as PLTX-like compounds can cause mortality and/or marked decrease in annelid abundance. In addition, phycotoxins have been linked to sublethal effects on annelid cells. Although very sparse, field and laboratory studies offer strong evidence that annelids may be reliable indicators of toxin exposure and their negative effects during both early and later stages of HABs in marine environments. Besides quickly responding to these compounds at both organismic and suborganismic levels, annelids are easily found in areas affected by HABs. The use of annelids in future investigations evaluating the action mechanisms of toxic microalgae on marine invertebrates should be thus encouraged. In this case, the choice for widely dispersed and numerically dominant species of annelids would strengthen the validation and extrapolation of results from risk assessments in areas affected by HABs worldwide.	[Pires, Estela; Lana, Paulo da Cunha; Mafra Jr, Luiz Laureno] Univ Fed Parana, Ctr Marine Studies, Ave Beira Mar S-N,POB 61, BR-83255976 Pontal do Parana, Parana, Brazil	Universidade Federal do Parana	Pires, E (通讯作者)，Univ Fed Parana, Ctr Marine Studies, Ave Beira Mar S-N,POB 61, BR-83255976 Pontal do Parana, Parana, Brazil.	estelapires@ufpr.br	Mafra, Luiz/J-6047-2012; Pires, Estela/KHE-4650-2024	Pires, Estela/0000-0003-2726-2070; Mafra, Luiz/0000-0001-5822-3619	CAPES (Brazil); International Atomic Energy Agency (IAEA) [18827]	CAPES (Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); International Atomic Energy Agency (IAEA)(International Atomic Energy Agency)	This work is heartfully dedicated to the memory of Paulo Lana, a brilliant scientist and our dearest friend. The authors would like to thank Pedro Wadt for the dinoflagellate art of graphic abstract. The authors are grateful to CAPES (Brazil) for the M.Sc. scholarship awarded to E.P. This study was partially supported by the International Atomic Energy Agency (IAEA) through the Research Contract #18827 ("Bentox" Project).	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J	Alsen, P; Piasecki, S; Nohr-Hansen, H; Pauly, S; Sheldon, E; Hovikoski, J				Alsen, Peter; Piasecki, Stefan; Nohr-Hansen, Henrik; Pauly, Sebastian; Sheldon, Emma; Hovikoski, Jussi			Stratigraphy of the Upper Jurassic to lowermost Cretaceous in the Rodryggen-1 and Brorson Halvo-1 boreholes, Wollaston Forland, North-East Greenland	GEUS BULLETIN			English	Article						ammonite stratigraphy; calcareous nannofossil stratigraphy; Jurassic-Cretaceous boundary; palynostratigraphy; Storsletten Member	PRAECHETAITES EXOTICUS ZONE; PANBOREAL CORRELATION; HIGH-LATITUDES; AMMONITE; BIOSTRATIGRAPHY; ZONATION; PALEOBIOGEOGRAPHY; POSITION	Two shallow cores drilled in northern Wollaston Forland, North-East Greenland, provide a combined section covering the upper Kimmeridgian (Upper Jurassic) - Barremian (Lower Cretaceous) and comprising the Bernbjerg, Lindemans Bugt, Palnatokes Bjerg and Stratumbjerg Formations. A new lithostratigraphic unit, the Storsletten Member, is defined within the Lindemans Bugt Formation. The black mudstone-dominated intervals are dated primarily by dinoflagellate cysts and ammonites, whereas the calcareous mudstones of the Palnatokes Bjerg Formation - sandwiched between the black mudstones - are dated by calcareous nannofossils. The stratigraphy demonstrates an almost complete succession in the Rodryggen-1 core, representing a deeper position in the basin, where the hiatus at the latest Jurassic rift climax predicted in previous models for the eastern Wollaston Forland Basin is absent. In contrast, the Brorson Halvo-1 core represents a position closer to a block crest where unconformities developed. In combination, the cores provide a key biostratigraphic reference section for the Jurassic-Cretaceous boundary interval in the Arctic.	[Alsen, Peter; Nohr-Hansen, Henrik; Sheldon, Emma] Geol Survey Denmark & Greenland GEUS, Dept Geoenergy & Storage, Copenhagen, Denmark; [Piasecki, Stefan; Hovikoski, Jussi] Geol Survey Denmark & Greenland GEUS, Dept Geophys & Sedimentary Basins, Copenhagen, Denmark; [Piasecki, Stefan] Univ Copenhagen, Globe Inst, Copenhagen, Denmark; [Pauly, Sebastian] Ruhr Univ Bochum, Bochum, Germany; [Pauly, Sebastian] INGENUM GmbH, Bottrop, Germany; [Hovikoski, Jussi] Geol Survey Finland GTK, Espoo, Finland	Geological Survey Of Denmark & Greenland; Geological Survey Of Denmark & Greenland; University of Copenhagen; Ruhr University Bochum; Geological Survey of Finland (GTK)	Alsen, P (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Geoenergy & Storage, Copenhagen, Denmark.	pal@geus.dk	Sheldon, Emma/H-5281-2018; Alsen, Peter/F-4849-2017; Hovikoski, Jussi/H-3280-2018	Alsen, Peter/0000-0001-6218-9054; Hovikoski, Jussi/0000-0001-6330-8713	consortium of industry energy companies; GEUS	consortium of industry energy companies; GEUS(General Electric)	Core drilling and fieldwork were undertaken during the Geological Survey of Denmark and Greenland (GEUS) field and drilling campaign in North-East Greenland in 2009 and 2010. 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J	Pavlishina, P; Dochev, D				Pavlishina, Polina; Dochev, Docho			Dinoflagellate cyst biostratigraphy of the upper Campanian-lower Maastrichtian interval in the Oslen-Krivodol section, Northwest Bulgaria: preliminary results	SPISANIE NA B LGARSKOTO GEOLOGICHESKO DRUZHESTOV-REVIEW OF THE BULGARIAN GEOLOGICAL SOCIETY			English	Article						biostratigraphy; upper Campanian; lower Maastrichtian.; Dinoflagellate cysts		A dinoflagellate cyst biostratigraphy for the upper Campanian-lower Maastrichtian interval in the newly described Oslen-Krivodol section, northwest Bulgaria, is proposed. The dinocyst scheme comprises the zones of Areoligera coronata and Cerodinium diebelii, in ascending order, and illustrates the sharp transition between the Campanian and Maastrichtian dinocyst assemblages. The presented results confirm the high potential of dinoflagellate cysts for biostratigraphic correlations in the Campanian-Maastrichtian boundary interval.	[Pavlishina, Polina; Dochev, Docho] Sofia Univ St Kliment Ohridski, Dept Geol Paleontol & Fossil Fuels, 15 Tsar Osvoboditel Blvd, Sofia 1504, Bulgaria	University of Sofia	Pavlishina, P (通讯作者)，Sofia Univ St Kliment Ohridski, Dept Geol Paleontol & Fossil Fuels, 15 Tsar Osvoboditel Blvd, Sofia 1504, Bulgaria.	polina@gea.uni-sofia.bg; dochev@gea.uni-sofia.bg	Dochev, Docho/AAL-3815-2021; Pavlishina, Polina/AAL-5710-2021		Sofia University [80-10-52]	Sofia University	Acknowledgements : This research is a contribu- tion to Project 80-10-52 funded by Sofia University.	Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; Dochev Docho, 2023, Geologica Balcanica, V52, P81, DOI 10.52321/GeolBalc.52.3.81; Fensome R. A., 2019, AASP Contribution Series, V48; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; Niechwedowicz M, 2022, NEWSL STRATIGR, V55, P21, DOI 10.1127/nos/2021/0639; Odin GS, 2001, EPISODES, V24, P229; Radmacher W, 2014, CRETACEOUS RES, V51, P309, DOI 10.1016/j.cretres.2014.07.004; Roncaglia L, 1997, NEWSL STRATIGR, V35, P29; Schioler P., 2001, Developments in Palaeontology and Stratigraphy, V19, P221; Wagreich M., 2023, 4 INT C STRAT STRATI, P110	10	0	0	0	0	BULGARIAN ACAD SCIENCE	SOFIA	CENTRAL LIBRARY 7 NOEMVRI NO 1, SOFIA, 00000, BULGARIA	0007-3938	1314-8680		SPISANIE B LGARSKOTO	Spis. B Lgarskoto Geol. Druz.		2023	84		3				189	192		10.52215/rev.bgs.2023.84.3.189	http://dx.doi.org/10.52215/rev.bgs.2023.84.3.189			4	Geosciences, Multidisciplinary	Emerging Sources Citation Index (ESCI)	Geology	HF8C6		Bronze			2025-03-11	WOS:001158159300010
J	Fafara, M; Dubicka, Z; Niechwedowicz, M; Ciurej, A; Walaszczyk, I				Fafara, Michal; Dubicka, Zofia; Niechwedowicz, Mariusz; Ciurej, Agnieszka; Walaszczyk, Ireneusz			Middle Campanian (Late Cretaceous) sea-level rise; microfossil record of bathymetric changes	ACTA GEOLOGICA POLONICA			English	Article						Foraminifera; C-dinocysts; Dinoflagellata; Phytoclasts; Chalk	WALLED DINOFLAGELLATE CYSTS; LOWER MAASTRICHTIAN SECTIONS; PLANKTONIC-FORAMINIFERA; BENTHIC FORAMINIFERS; BASIN; BIOSTRATIGRAPHY; SEDIMENTS; OXYGEN; CARBON; CHALK	A Middle Campanian (Late Cretaceous) eustatic sea-level rise recorded in the Belgorod succession (Russia; eastern North European Basin) was analyzed. The succession, dated for the Gavelinella annae and Globorotalites emdyensis foraminiferal zones (corresponding to the 'Inoceramus' azerbaydjanensis-'Inoceramus' vorhelmensis inoceramid Zone), records the deposition of pure chalk, with only trace terrigenous material. Its distal offshore position limited terrestrial nutrient delivery, driving oligotrophic conditions that influenced benthic foraminifera and organic-walled phytoplankton communities. Eustatic changes are recorded by planktonic foraminifera and additionally reflected in phytoclast abundance, organic-walled dinoflagellate cysts (dinocysts), calcareous dinoflagellate cysts (c-dinocysts), and delta C-13 and delta O-18 fluctuations. Most indices were primarily driven by variable terrestrial organic matter and freshwater influxes, acting as a function of sea depth and land topography.	[Fafara, Michal; Dubicka, Zofia; Niechwedowicz, Mariusz; Walaszczyk, Ireneusz] Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland; [Ciurej, Agnieszka] Pedag Univ Krakow, Inst Biol & Earth Sci, Dept Geol & Palaeontol, Podchorazych 2, PL-30084 Krakow, Poland	University of Warsaw; University of the National Education Commission	Fafara, M (通讯作者)，Univ Warsaw, Fac Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	m.fafara@student.uw.edu.pl	Niechwedowicz, Mariusz/LJL-9003-2024; Ciurej, Agnieszka/HNS-7682-2023; Walaszczyk, Ireneusz/ABE-7229-2021; Dubicka, Zofia/ABB-3388-2020	Niechwedowicz, Mariusz/0000-0002-1967-2945; Dubicka, Zofia/0000-0003-1105-4111	National Science Centre, Poland [2017/27/B/ST10/00687, PBU/2022/04/00194]	National Science Centre, Poland(National Science Centre, Poland)	We thank Danuta Peryt (Polish Academy of Sciences) and Jordan Todes (University of Chicago) for very useful comments and suggested improvements. Martin Pearce (Evolution Applied Limited, UK) is acknowledged for insightful discussion on dinocysts from the European chalks. This research was funded by the National Science Centre, Poland, grant no. 2017/27/B/ST10/00687 and by statutory research project no. PBU/2022/04/00194 UP.	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Pol.		2023	73	4					661	683		10.24425/agp.2023.145628	http://dx.doi.org/10.24425/agp.2023.145628			23	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	FB6G0		gold			2025-03-11	WOS:001143322300007
J	Holen, DA; Princiotta, S				Holen, Dale A.; Princiotta, Sarah			Encystment by the mixotrophic flagellate<i> Ochromonas</i><i> pinguis</i> Conrad (Chrysophyceae) under manipulated laboratory conditions	FOTTEA			English	Article						chrysophyte; cyst; dormancy; encystment; mixotrophy; Ochromonas; resting stage; stomatocyst	LIFE-CYCLE; DINOFLAGELLATE; STATOSPORE; STOMATOCYSTS; TEMPERATURE; POPULATION; PATTERNS; CULTURE; GROWTH; CYSTS	Chrysophyte stomatocysts are well documented in lake sediments, but except for a few studies on sexually reproducing colonial chrysophytes, little is known regarding encystment cues in these algae. Ochromonas pinguis Conrad, a mixotrophic chrysophyte with an unknown sexual history was observed to produce stomatocysts, albeit at a low frequency. To determine if the low rate of encystment was typical or whether manipulating environmental conditions might enhance the rate of resting cyst production O. pinguis was subjected to various physical and chemical conditions in a batch culture. O. pinguis cultures were manipulated by culturing them in DY-V inorganic medium in variable light, pH, and temperature conditions, and at varying levels of N and P limitation. Except for growth in continuous darkness, all treatments resulted in an increase in O. pinguis concentration. Five treatments resulted in a corresponding increase in stomatocyst concentration. In the remaining treatments stomatocyst production was steady although sporadic. The encystment frequency however was minimal in all manipulations and ranged from 0.008 to 0.03% of the population undergoing cyst formation. In this study, O. pinguis stomatocyst production was not influenced by laboratory manipulations but rather a minute proportion of the population produced stomatocysts regardless of environmental conditions.	[Holen, Dale A.] Penn State Univ Scranton, 120 Ridge View Dr, Dunmore, PA 18512 USA; [Princiotta, Sarah] Penn State Univ Schuylkill, 200 Univ Dr, Schuylkill Haven, PA 17972 USA	Pennsylvania Commonwealth System of Higher Education (PCSHE); Pennsylvania State University; Pennsylvania Commonwealth System of Higher Education (PCSHE); Pennsylvania State University	Holen, DA (通讯作者)，Penn State Univ Scranton, 120 Ridge View Dr, Dunmore, PA 18512 USA.	dah13@psu.edu	Holen, Dale/KFA-6039-2024					AGBETI MD, 1995, J PHYCOL, V31, P70, DOI 10.1111/j.0022-3646.1995.00070.x; ALBERTANO P, 1994, ARCH PROTISTENKD, V144, P75, DOI 10.1016/S0003-9365(11)80226-5; Andersen R. A., 2005, Algal Culturing Techniques; ANDERSEN R.A., 2007, Unravelling the algae. 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J	Rukminasari, N; Hidayani, AA; Parenrengi, A; Andriyono, S				Rukminasari, Nita; Hidayani, Andi Aliah; Parenrengi, Andi; Andriyono, Sapto			Detecting DNA of multispecies dinoflagellate cysts in the sediment from three estuaries of Makassar strait and fishing port using CO1 primer: Is it CO1 primer suitable for detecting DNA dinoflagellate?	BAGHDAD SCIENCE JOURNAL			English	Article						CO1 primer; DNA dinoflagellate cyst; Makassar Strait; Maros-Pangkep and Jeneberang Estuary; PCR method	LIFE-CYCLE; QPCR ASSAY; WATERS; GENE; ORGANIZATION; ALEXANDRIUM; PCR	Most dinoflagellate had a resting cyst in their life cycle. This cyst was developed in unfavorable environmental condition. The conventional method for identifying dinoflagellate cyst in natural sediment requires morphological observation, isolating, germinating and cultivating the cysts. PCR is a highly sensitive method for detecting dinoflagellate cyst in the sediment. The aim of this study is to examine whether CO1 primer could detect DNA of multispecies dinoflagellate cysts in the sediment from our sampling sites. Dinoflagellate cyst DNA was extracted from 16 sediment samples. PCR method using COI primer was running. The sequencing of dinoflagellate cyst DNA was using BLAST. Results showed that there were two clades of dinoflagellate cysts from four locations of study. Clade 1 was dominated by samples from the Jeneberang Estuary (JB), Maros Estuary (M) and Pangkep Estuary(P), while clade 2 was dominated by samples from the Paotere Port (PP). The genetic distance varied between DNA dinoflagellate cyst samples ranging from 0.5-0.6. The closest genetic distance was between sample of JB1 and sample of JB2, while the farthest genetic distance was sample PP1 and PP2. The primer CO1 was not suitable for dinoflagellate cyst DNA due to only picking one DNA, which was a diatom (Licmophora sp).	[Rukminasari, Nita; Hidayani, Andi Aliah] Univ Hasanuddin, Fac Marine Sci & Fisheries, Fisheries Dept, Makassar, South Sulawesi, Indonesia; [Parenrengi, Andi] Natl Res & Innovat Agcy, Res Ctr Fisheries, Central Jakarta, Indonesia; [Andriyono, Sapto] Univ Airlangga, Fac Fisheries & Marine, Dept Marine, East Java, Indonesia	Universitas Hasanuddin; Airlangga University	Rukminasari, N (通讯作者)，Univ Hasanuddin, Fac Marine Sci & Fisheries, Fisheries Dept, Makassar, South Sulawesi, Indonesia.	nita.r@unhas.ac.id; aliah@fikp.unhas.ac.id; andi053@brin.go.id; sapto.andriyono@fpk.unair.ac.id	Andriyono, Sapto/AAB-7229-2021; Parenrengi, Andi/JQV-5411-2023; Hidayani, Andi Aliah/H-8117-2017; Rukminasari, Nita/M-2410-2014	Parenrengi, Andi/0000-0002-2802-8617; Hidayani, Andi Aliah/0000-0002-4541-5539; Andriyono, Sapto/0000-0002-2566-1636; Rukminasari, Nita/0000-0003-2943-9538				Brosnahan ML, 2014, DEEP-SEA RES PT II, V103, P185, DOI 10.1016/j.dsr2.2013.05.034; Casabianca S, 2014, MAR POLLUT BULL, V88, P102, DOI 10.1016/j.marpolbul.2014.09.018; Casabianca S, 2013, ENVIRON SCI TECHNOL, V47, P3788, DOI 10.1021/es305018s; de Bustos A, 2020, HARMFUL ALGAE, V98, DOI 10.1016/j.hal.2020.101903; de la Espina SMD, 2005, EUR J CELL BIOL, V84, P137, DOI 10.1016/j.ejcb.2005.01.002; Deng YY, 2015, HARMFUL ALGAE, V50, P57, DOI 10.1016/j.hal.2015.10.007; Dias PJ, 2015, BIOINVASIONS REC, V4, P233, DOI 10.3391/bir.2015.4.4.01; Eckford-Soper LK, 2015, HARMFUL ALGAE, V48, P37, DOI 10.1016/j.hal.2015.06.009; Hidayani Andi Aliah, 2020, Biodiversitas, V21, P2097; Hoppenrath M, 2020, J PHYCOL, V56, P798, DOI 10.1111/jpy.12984; Figueroa RI, 2014, PROTIST, V165, P343, DOI 10.1016/j.protis.2014.04.001; Ishitani Y, 2014, MOL PHYLOGENET EVOL, V78, P215, DOI 10.1016/j.ympev.2014.05.021; Khalil MI, 2020, BAGHDAD SCI J, V17, P220, DOI 10.21123/bsj.2020.17.1(Suppl.).0220; Kim JH, 2016, PLOS ONE, V11, DOI 10.1371/journal.pone.0146843; Kumar S, 2016, MOL BIOL EVOL, V33, P1870, DOI [10.1093/molbev/msw054, 10.1093/molbev/msv279]; Lai JCY, 2010, RAFFLES B ZOOL, V58, P199; Mertens KN, 2012, PHYCOLOGIA, V51, P612, DOI 10.2216/11-89.1; Mohammed HA, 2018, BAGHDAD SCI J, V15, P381, DOI 10.21123/bsj.2018.15.4.0381; Park BS, 2014, HARMFUL ALGAE, V37, P133, DOI 10.1016/j.hal.2014.04.019; Park TG, 2016, HARMFUL ALGAE, V60, P36, DOI 10.1016/j.hal.2016.10.005; Pawlowski J, 2012, PLOS BIOL, V10, DOI 10.1371/journal.pbio.1001419; Perini F, 2011, PLOS ONE, V6, DOI 10.1371/journal.pone.0017699; Rachman Arief, 2021, Oseanologi dan Limnologi di Indonesia, V6, P37; Reñé A, 2013, PROTIST, V164, P673, DOI 10.1016/j.protis.2013.07.002; Rukminasari Nita, 2021, AACL Bioflux, V14, P1107; Tambaru R, 2019, J Ilmu Kelaut Spermonde, V4, P69; Yamaguchi A, 2006, PHYCOL RES, V54, P317, DOI 10.1111/j.1440-1835.2006.00438.x	27	0	0	1	2	COLL SCIENCE WOMEN, UNIV BAGHDAD	BAGHDAD	PO BOX 4732, AL- JADIRYA, BAGHDAD, 00000, IRAQ	2078-8665	2411-7986		BAGHDAD SCI J	Baghdad Sci. J.		2023	20	5					1635	1642		10.21123/bsj.2023.7181	http://dx.doi.org/10.21123/bsj.2023.7181			8	Multidisciplinary Sciences	Emerging Sources Citation Index (ESCI)	Science & Technology - Other Topics	U9SL2		gold			2025-03-11	WOS:001088130900001
J	Duxbury, S				Duxbury, Stan			Organic-walled marine microplankton from the Hauterivian and early Barremian of the North Sea Region- biostratigraphy and taxonomy	MICROPALEONTOLOGY			English	Article						Palynology; biozonation; dinocysts; Hauterivian; early Barremian; Speeton; U; K; C; S; Witch Ground Graben; Scapa Field	DINOFLAGELLATE CYST STRATIGRAPHY; MORAY FIRTH; PALYNOLOGY; MORPHOLOGY; COMPLEX; SPEETON; GENERA; CLAY	Quantitative palynofloral analysis of Hauterivian and early Barremian aged sediments at Speeton (northeast England) and in the UKCS, Witch Ground Graben has involved 39 outcrop samples and over 1000 samples from 40 wells in the Northern Area Clay-more (NAC), Scapa and Highlander fields, including extensive conventional core. Very close sampling, particularly within the early Hauterivian at Speeton, has allowed dinocyst events to be tied closely to ammonite zones and their extrapolation offshore. The timing of deposition of the Scapa Sandstone Member of the Valhall Formation is discussed for Scapa Field, and a transect across the field is pre-sented. Individual Scapa sedimentary units have been assigned to particular ammonite zones and the timing of paleoenvironmental changes at Speeton assessed in relation to them. The zonation scheme proposed by Duxbury (2001) has been re-visited, further refined and some boundaries adjusted, particularly in relation to ammonite zone equivalence. Eighty-five key palynofloral events have now been recognised in the Hauterivian and early Barremian, including many first occurrences. Thirty-seven new species and seven new subspe-cies of stratigraphically significant dinoflagellate cysts are described, four new combinations have been effected and the status of one taxon has been raised from subspecies to species rank. The diagnoses of one genus and one species have been emended.	[Duxbury, Stan] Church Lane, Chester CH2 1DJ, England		Duxbury, S (通讯作者)，Church Lane, Chester CH2 1DJ, England.	duxburydsc@aol.com						Abbink O.A., 1998, NSG Publication No. 980301. 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J	Pavlishina, P; Dochev, D; Wagreich, M; Koukal, V				Pavlishina, Polina; Dochev, Docha; Wagreich, Michael; Koukal, Veronika			Integrated biostratigraphy and palaeoenvironments of the Upper Cretaceous in the Petrich section (Central Srednogorie Zone, Bulgaria)	ACTA GEOLOGICA POLONICA			English	Article						Upper Cretaceous; Campanian; Calcareous nannofossils; Dinoflagellate cysts; Inoceramids; Biostratigraphy; Palaeoenvironments	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; VISTULA RIVER SECTION; WESTERN FORE-BALKAN; INOCERAMID BIOSTRATIGRAPHY; NORTHERN APENNINES; BASIN; BOUNDARY; SEA; CHALK; STRATIGRAPHY	The Upper Cretaceous succession (Coniacian to lowermost Maastrichtian, with focus on the Campanian) at Petrich, Central Srednogorie Zone in Bulgaria, is described and calibrated stratigraphically based on nannofos-sils, dinoflagellate cysts and inoceramids. The following standard nannofossil zones and subzones are identi-fied: UC10-UC11ab (middle to upper Coniacian), UC11c-UC12-UC13 (uppermost Coniacian to Santonian), UC14a (lowermost Campanian), UC14bTP-UC15cTP (lower Campanian to 'middle' Campanian), UC15dTP- UC15eTP (upper Campanian), UC16aTP (of Thibault et al. 2016; upper part of the upper Campanian), and UC16b (Campanian-Maastrichtian boundary). The base of the Campanian is defined by the FO of Broinsonia parca parca (Stradner) Bukry, 1969 and Calculites obscurus (Deflandre) Prins and Sissingh in Sissingh, 1977 (a morphotype with a wide central longitudinal suture). The Areoligera coronata dinoflagellate cyst Zone (upper lower Campanian to upper upper Campanian) is identified, corresponding to the UC14bTP-UC16aTP nannofossil subzones. The inoceramid assemblage indicates the 'Inoceramus' azerbaydjanensis-'Inoceramus' vorhelmensis Zone, correlated within the interval of nannofossil subzones UC15dTP-UC15eTP. The composition of the dino-flagellate cyst assemblages and palynofacies pattern suggest normal marine, oxic conditions and low nutrient availability within a distal shelf to open marine depositional environment during the Campanian.	[Pavlishina, Polina; Dochev, Docha] Sofia Univ St Kliment Ohridsk, Fac Geol & Geog, Dept Geol Paleontol & Fossil Fuels, Sofia, Bulgaria; [Wagreich, Michael; Koukal, Veronika] Univ Vienna, Dept Geol, A-1090 Vienna, Austria	University of Sofia; University of Vienna	Pavlishina, P (通讯作者)，Sofia Univ St Kliment Ohridsk, Fac Geol & Geog, Dept Geol Paleontol & Fossil Fuels, Sofia, Bulgaria.	polina@gea.uni-sofia.bg; dochev@gea.uni-sofia.bg; michael.wagreich@univie.ac.at; veronika.koukal@univie.ac.at	Pavlishina, Polina/AAL-5710-2021; Wagreich, Michael/D-2279-2013	Wagreich, Michael/0000-0002-8828-0857	Bilateral Bulgarian-Austrian [kappaP-06-Austria/9]	Bilateral Bulgarian-Austrian	This research was financed by the Bilateral Bulgarian-Austrian collaboration project 'Late Cretaceous palaeoclimate events and stage boundaries correlations-evidence from Tethyan key sections of Bulgaria and Austria"(kappa P-06-Austria/9) and is a contribution to IGCP 661 and IGCP 710. We are grateful to Dr. P. 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J	Mülayim, O; Yilmaz, IÖ; Ferré, B				Mulayim, Oguz; Yilmaz, Ismail Omer; Ferre, Bruno			Pithonellid calcitarch record in the middle? Cenomanian Derdere-A Member, SE Turkey: palaeoenvironmental changes and stratigraphic significance	TURKISH JOURNAL OF EARTH SCIENCES			English	Article						Pithonellid calcitarcha; Cenomanian; palaeoenvironment; SE Turkey	CALCAREOUS DINOFLAGELLATE CYSTS; PLANKTONIC-FORAMINIFERA; ARABIAN PLATFORM; HIGH-RESOLUTION; MARDIN GROUP; BIOSTRATIGRAPHY; ROVEACRINIDS; PALEOECOLOGY; ISOTOPE; BASIN	Pithonellid calcitarchs are studied in the organic-rich limestones of the Derdere-A Member from the middle? Cenomanian deposits of SE Turkey for the first time. Little is known about the distribution of pithonellid calcitarchs in the Cretaceous strata of Turkey. Three morphogroups of pithonellid calcitarchs are distinguished: they are represented by Pithonella sphaerica (Kaufmann, 1865) and P. ovalis (Kaufmann, 1865), both dominating the pithonellid assemblages, and by Bonetocardiella conoidea (Bonet, 1956), this latter being less abundant. Compared to the relative abundance of Upper Cretaceous pithonellid calcitarchs in the study area, the diversity is extremely low. The significant increase in abundance of pithonellid calcitarchs is particularly noticeable in the Cenomanian. We observed a significant increase in abundance of pithonellid calcitarchs in the Derdere-A Member, which is associated with an early transgressive phase of the middle? Cenomanian Arabian Platform. They are present in relative abundance and could therefore represent a potentially useful correlative marker horizon in SE Turkey. Pithonellid calcitarchs have been interpreted as indicators of increased nutrient input. A positive correlation exist between pithonellid calcitarchs abundance and nutrition input in the Derdere-A Member which is a sequence of carbonates deposite under eutrophic conditions, as evidenced by the low diversity and very low abundance of benthonic and planktonic foraminifers, and the high abundance of pithonellid calcitarchs. As a result, the increase of pithonellid calcitarchs indicates the increase of nutrient input in the Derdere-A Member. We noticed that a comparable trophic change also occurred throughout the SE Turkey carbonate platform in the middle? Cenomanian. The increase in the pithonellid abundance reported here may be a possible indicator of such a change.	[Mulayim, Oguz] Turkish Petr Corp, Adiyaman, Turkiye; [Yilmaz, Ismail Omer] Middle East Tech Univ, Dept Geol Engn, Ankara, Turkiye; [Ferre, Bruno] 2 Rue Guy Maupassant, F-76800 St Etienne Du Rouvray, France	Ministry of Energy & Natural Resources - Turkey; Middle East Technical University	Mülayim, O (通讯作者)，Turkish Petr Corp, Adiyaman, Turkiye.	oguzzmlym@gmail.com	Mulayim, Oguz/AAG-8666-2019; , Ferré/AAU-4099-2021					ADAMS T. 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Earth Sci.		2023	32	1					63	74		10.55730/1300-0985.1827	http://dx.doi.org/10.55730/1300-0985.1827			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	8K5IE		Bronze			2025-03-11	WOS:000923134500003
J	Machado, G; Casas-Gallego, M; Burliga, S				Machado, Gil; Casas-Gallego, Manuel; Burliga, Stanislaw			Salt biostratigraphy: The Miocene palynological assemblages from the Wieliczka Formation, southern Poland	AAPG BULLETIN			English	Article							POLISH CARPATHIAN FOREDEEP; BADENIAN SALINITY CRISIS; DINOFLAGELLATE CYSTS; CLIMATE DYNAMICS; MIDDLE; BASIN; VEGETATION; FRONT; EVOLUTION; DEPOSITS	Salt biostratigraphy has rarely been used in academic or industry studies, despite its potential to shed light on the stratigraphy, thermal maturity, paleoenvironments, and paleoecology of evap-orite successions. The upper section of the evaporite-dominated middle Miocene Wieliczka Formation in southern Poland was sampled and analyzed for its palynological content. The results show assemblages dominated by miospores with subordinate dinoflagellate cysts, which are interpreted as derived mainly from reworking. The reworked forms, both miospores and dino-flagellate cysts, were sourced from Cretaceous, Paleogene, and Miocene strata, with increasing amounts toward the top of the succession, which is interpreted to be a consequence of the nearby ongoing Carpathian thrusting. The influence of marine water in the basin sedimentation is difficult to estimate with the current data as the dinoflagellate cysts are, at least partially, reworked. The in situ miospore assemblages indicate the pres-ence of nearby mixed coniferous and broadleaved deciduous for-ests that developed under temperate and humid climatic conditions. The high percentages of bisaccate pollen are inter-preted to represent the proximity to high-elevation areas of the Carpathians, where conifers must have been dominant. The pal-ynological record also signals the development of swamp and marsh vegetation in the lowland areas. These wetlands were most likely inhabited by shrubby and arboreal elements with few thermophilic taxa. The apparent thermal maturation of the assemblages is very low, with dominant pale yellow palyno-morph colors. The study shows that palynological analyses in evaporite-dominated successions are helpful in the reconstruc-tion of local geodynamic events, paleoecology, and stratigraphic interpretation.					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JAN	2023	107	1					151	167		10.1306/07142221125	http://dx.doi.org/10.1306/07142221125			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	8G3FM					2025-03-11	WOS:000920232600003
J	Agafonova, E; Novichkova, E; Novigatsky, A; Kravchishina, M; Klyuvitkin, A; Bulokhov, A				Agafonova, Elizaveta; Novichkova, Ekaterina; Novigatsky, Alexander; Kravchishina, Marina; Klyuvitkin, Alexey; Bulokhov, Anton			Diatom and Dinocyst Production, Composition and Flux from the Annual Cycle Sediment Trap Study in the Barents Sea	GEOSCIENCES			English	Article						Arctic shelf; sinking material; diatoms; dinoflagellate cysts; photic layer; sediment trap; Arctic atlantification	MARGINAL ICE-ZONE; DINOFLAGELLATE CYST ASSEMBLAGES; ATLANTIC WATER-FLOW; BIOGENIC MATTER; NORTH-ATLANTIC; VERTICAL FLUX; ARCTIC-OCEAN; SEASONAL-VARIATION; SURFACE CONDITIONS; VARIABILITY	This paper presents the diatom and palynomorph data from a sediment trap deployed in the northern part of the East Barents Sea for an annual cycle from August 2017 to August 2018. The average monthly fluxes of diatoms and dinoflagellate cysts in the photic layer of the northeastern part of the Barents Sea varies from 10.4 x 10(3) to 640.8 x 10(3) valves m(-2) day(-1) and from 0.3 x 10(3) to 90.0 x 10(3) cysts m(-2) day(-1), respectively. Their fluxes are related to the low irradiance of the photic layer during the sea-ice cover period, dominance of southward currents, modern climate, and nepheloid layer conditions. Based on redundancy analysis of the relationship between the fluxes of diatoms and dinoflagellate cysts and organic carbon fluxes, sea-ice covers, and the seasonal cycle of light availability we determined the following. First, sea-ice-associated diatoms and dinocysts are exported to the sediment trap from the melting sea ice with a two-week delay. Second, the appearance of freshwater diatoms and green algae in the sinking material accumulating from March 2018 to July 2018 is also related to the melting of sea ice. And third, the presence of Coscinodiscus radiatus, C. perforatus, Shionodiscus oestrupii and Operculodinium centrocarpum in the diatoms and dinocysts species composition throughout the year indicates the advection of Atlantic waters into the Barents Sea up to 80 degrees N.	[Agafonova, Elizaveta; Novichkova, Ekaterina; Novigatsky, Alexander; Kravchishina, Marina; Klyuvitkin, Alexey; Bulokhov, Anton] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology	Agafonova, E; Novichkova, E (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia.	agafonovaelizaveta@mail.ru; enovichkova@mail.ru	Agafonova, Elizaveta/KCK-0835-2024; Klyuvitkin, Alexey/B-3788-2017; Kravchishina, Marina/B-3741-2017; Novichkova, Ekaterina/B-5807-2017; Novigatsky, A.N./D-5591-2017	Klyuvitkin, Alexey/0000-0002-8739-6321; Agafonova, Elizaveta/0000-0001-5451-9586; Kravchishina, Marina/0000-0001-9967-2891; Novichkova, Ekaterina/0000-0001-5687-1719; Novigatsky, A.N./0000-0003-2814-878X				Andreassen IJ, 1998, MAR ECOL PROG SER, V170, P1, DOI 10.3354/meps170001; [Anonymous], 1974, DIATOMS USSR FOSSIL; [Anonymous], 1949, PROC OCEANOL I USSR; [Anonymous], READY - Real-time Environmental Applications and Display sYstem; Arctic and Antarctic Research Institute, US; Ardyna M, 2014, GEOPHYS RES LETT, V41, P6207, DOI 10.1002/2014GL061047; Årthun M, 2012, J CLIMATE, V25, P4736, DOI 10.1175/JCLI-D-11-00466.1; Asbjornsen H, 2020, GEOPHYS RES LETT, V47, DOI 10.1029/2020GL088036; Backhaus JO, 1999, MAR ECOL PROG SER, V189, P77, DOI 10.3354/meps189077; Barton BI, 2018, J PHYS OCEANOGR, V48, P1849, DOI 10.1175/JPO-D-18-0003.1; BATTARBE.RW, 1973, LIMNOL OCEANOGR, V18, P647, DOI 10.4319/lo.1973.18.4.0647; Bauerfeind E, 2009, DEEP-SEA RES PT I, V56, P1471, DOI 10.1016/j.dsr.2009.04.011; Bogus K, 2014, J PHYCOL, V50, P254, DOI 10.1111/jpy.12170; Brice C, 2022, QUATERNARY RES, V108, P180, DOI 10.1017/qua.2020.2; Cloern JE, 2008, ECOL LETT, V11, P1294, DOI 10.1111/j.1461-0248.2008.01244.x; Coppola L, 2002, MAR CHEM, V80, P11, DOI 10.1016/S0304-4203(02)00071-3; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2020, MAR MICROPALEONTOL, V159, DOI 10.1016/j.marmicro.2019.101796; de Vernal A, 2013, QUATERNARY SCI REV, V79, P122, DOI 10.1016/j.quascirev.2013.06.022; Dmitrenko IA, 2015, J GEOPHYS RES-OCEANS, V120, P5158, DOI 10.1002/2015JC010804; Dolan JR, 2017, POLAR BIOL, V40, P1247, DOI 10.1007/s00300-016-2049-0; drao, 107CM SOLAR FLUX DA; Drits AV, 2021, OCEANOLOGY+, V61, P984, DOI 10.1134/S0001437021060217; Drits AV, 2020, OCEANOLOGY+, V60, P501, DOI 10.1134/S0001437020040074; Dzhinoridze R.N, 1978, MARINE MICROPALEONTO, P41; Fahl K, 2007, DEEP-SEA RES PT I, V54, P1256, DOI 10.1016/j.dsr.2007.04.014; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fetterer F., 2020, ARCTIC ANTARCTIC SE; Fourtanier Elisabeth, 1999, Diatom Research, V14, P1; Gaye B, 2007, CONT SHELF RES, V27, P2570, DOI 10.1016/j.csr.2007.07.003; Gordeev V.V., 2021, BARENTS SEA SYSTEM, P415, DOI [10.29006/978-5-6045110-0-8/(30), DOI 10.29006/978-5-6045110-0-8/(30)]; Grosfjeld K, 2009, NORW J GEOL, V89, P121; GUIRY M.D., AlgaeBase. 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J	Riding, JB; Fensome, RA; Soyer-Gobillard, MO; Medlin, LK				Riding, James B.; Fensome, Robert A.; Soyer-Gobillard, Marie-Odile; Medlin, Linda K.			A Review of the Dinoflagellates and Their Evolution from Fossils to Modern	JOURNAL OF MARINE SCIENCE AND ENGINEERING			English	Review						dinoflagellates; evolution; fossil record; morphology; 18S small sub-unit (SSU) rRNA phylogeny	OCEANIC ANOXIC EVENT; NORTH-WEST SHELF; PRIMITIVE DINOFLAGELLATE; CELL-CYCLE; MIDDLE; DIVERSITY; PHYTOPLANKTON; PALYNOLOGY; RADIATION; BAJOCIAN	Molecular clock and biogeochemical evidence indicate that the dinoflagellate lineage diverged at around 650 Ma. Unequivocal dinoflagellate cysts/zygotes appeared during the Triassic. These biotas were badly affected by the end-Triassic extinction and recovery from this was relatively slow. During the early Middle Jurassic, the family Gonyaulacaceae underwent an explosive diversification event and taxonomic richness steadily increased throughout the rest of the Jurassic. The entire Cretaceous also recorded increases in diversity. This trend reversed during the Oligocene, probably caused by global cooling. Marine cyst-forming peridiniaceans declined substantially through the Oligocene and Neogene, but protoperidiniaceans continued to diversify. Modern taxa, as evidenced by the molecular tree, comprise three major clades: the first two are composed largely of parasitic forms, marine alveolates of unknown identity and the Syndiniales; free-living dinoflagellates form the third clade, which diverges rapidly and bears short branch lengths with no real support for branching order. This suggests that morphological divergence preceded molecular divergence because, as the fossil record indicates, major groups appeared at different ages. Unique features of the dinoflagellates helped the group take on a predominant role in the marine phytoplankton. Living in marine or fresh water, dinoflagellates have demonstrated innovative capacities that have enabled them to live among the phytoplankton or benthos as autotrophic, heterotrophic, mixotrophic free-living organisms or symbiotic and/or as parasitic forms.	[Riding, James B.] British Geol Survey, Nottingham NG12 5GG, England; [Fensome, Robert A.] Geol Survey Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada; [Soyer-Gobillard, Marie-Odile] Sorbonne Univ, Lab Arago, CNRS Ctr Natl Rech Sci, F-66650 Banyuls Sur Mer, France; [Medlin, Linda K.] Marine Biol Assoc UK, Plymouth PL1 2PB, England	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; Sorbonne Universite; Marine Biological Association United Kingdom	Medlin, LK (通讯作者)，Marine Biol Assoc UK, Plymouth PL1 2PB, England.	lkm@mba.ac.uk	medlin, linda/G-4820-2010	Soyer-Gobillard, Marie-Odile/0000-0003-1622-081X; medlin, linda k/0000-0001-6014-8339	 [20220414]; NERC [bgs06001] Funding Source: UKRI	; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research received no external funding.	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Mar. Sci. Eng.	JAN	2023	11	1							1	10.3390/jmse11010001	http://dx.doi.org/10.3390/jmse11010001			34	Engineering, Marine; Engineering, Ocean; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Oceanography	7Y8ED		Green Accepted, gold			2025-03-11	WOS:000915104400001
J	Gedl, P; Smist, P; Worobiec, E				Gedl, Przemyslaw; Smist, Piotr; Worobiec, Elzbieta			PALYNOLOGY OF THE DEEP STRUCTURES OF THE CARPATHIAN FOREDEEP (3,950-5,467 M) AT THE FRONT OF CARPATHIAN OVERTHRUST, THE NS-1 BOREHOLE, SE POLAND	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						Key words : Dinoflagellate cysts; sporomorphs; biostratigraphy; palaeoenvironment; Stebnik Unit; autochthonous	DINOFLAGELLATE CYST STRATIGRAPHY; CENTRAL PARATETHYS; NEOGENE; BASIN	The current paper presents the results of palynological studies from deep structures at the front of the Carpathian overthrust, penetrated by the NS-1 Borehole. Both the method used and hardly accessible material from a depth of almost 5.5 km allow the presentation of new data from the Stebnik Unit, the underlying autochthonous Miocene succession, and the conglomerates that rest upon the crystalline basement. Samples collected from available cored intervals and cuttings from the lower part of the borehole provided the opportunity to study for the first time the palynological content of the strata under consideration. Samples yielded diversified material, composed of terrestrial and marine elements, commonly showing various stages of preservation. The latter indicate various origins for the material analysed, which is possibly at least partly recycled. The occurrence of this phenomenon, particularly in the Stebnik Unit and the upper part of the autochthonous Miocene sequence, confirmed also by results of earlier micropalaeontological studies, makes precise stratigraphic correlation highly debatable. The authors discuss the possibility of both Paleogene and Miocene ages for the material. Also highly debatable are the palaeoenvironmental reconstructions of this interval, although the general intense influx of terrestrial material recorded is probably responsible for the unfavourable conditions for planktonic biota. Different, optimal marine conditions can be deduced for the lower part of the autochthonous Miocene; an abundance of dinoflagellate cysts allows their precise correlation with coeval strata of the Carpathian Foredeep Basin. Palynological analysis of conglomerate matrix material gave negative results. However, this and the lithological characteristics indicate a different origin and age of these strata in comparison with other coarse-grained lithosomes, known from neighbouring areas. The generally immature state of preservation of the organic matter in the deepest part of the borehole indicates that this part of the succession was not affected by the high temperatures that would be expected at such a depth. This contrast with the much more mature palynomorphs of the overlying Stebnik Unit points to the fact that these strata were heated to a much higher degree prior to their final burial.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland; [Smist, Piotr] PETROGEO Ltd, Przemyslowa 11, PL-38200 Jaslo, Poland; [Worobiec, Elzbieta] Polish Acad Sci, W Szafer Inst Bot, Lubicz 46, PL-31512 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; W. Szafer Institute of Botany of the Polish Academy of Sciences	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl; smist@petrogeo.pl; e.worobiec@botany.pl			W. Szafer Institute of Botany, Polish Academy of Sciences, through its statutory funds	W. Szafer Institute of Botany, Polish Academy of Sciences, through its statutory funds	The authorities of the Polish Oil and Gas Company (PGNiG) are acknowledged for allowing us to present the results of our research on the material from the NS-1 Borehole. The study of pollen and spores (EW) was supported by the W. Szafer Institute of Botany, Polish Academy of Sciences, through its statutory funds. Pawel Filipiak (University of Silesia in Katowice) is thanked for editorial comments. Frank Simpson (Windsor, Canada) is acknowledged for the linguistic correction that improved quality of this paper. Marcin Barski (Warsaw University) and an anonymous reviewer kindly read the manuscript.	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Volume 2 Gymnosperms; Suchocka A, 2019, GEOL Q, V63, P539, DOI 10.7306/gq.1486; Szafran S., 1980, PRACE GEOLOGICZNE PA, V120, P1; Tolwinski K., 1956, Acta Geologica Polonica, VVI, P75; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Zielinski J.J., 1963, ROCZNIK PTG, V33, P387; Zytko K., 1989, Geological Atlas of the Western Outer Carpathians and their Foreland	60	0	0	0	0	POLISH GEOLOGICAL SOC	KRAKOW	UL. OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. Pol.		2023	93	4								10.14241/asgp.2023.20	http://dx.doi.org/10.14241/asgp.2023.20			24	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	X4V6B		gold			2025-03-11	WOS:001425347600001
J	Klug, CR				Klug, Curtis R.			A simple method for the recovery of palynomorphs from rock gypsum and rock anhydrite	PALYNOLOGY			English	Article						Anhydrite; calcium sulfate; dissolution; gypsum; hydrochloric acid; retrograde solubility	DISSOLUTION; EDTA	A method for the relatively fast, inexpensive, and safe dissolution of rock gypsum and rock anhydrite for the recovery of palynomorphs is described. Rock gypsum and rock anhydrite deposits are widely distributed geographically and throughout the geologic column. They represent deposition under environmental conditions unlike those of most other rock types. Consequently, palynomorphs and other microfossils recovered from these rocks may present unique paleontological and biostratigraphic insights not provided by other strata. Despite their relatively high solubility, rock gypsum and rock anhydrite tend to be difficult to process and do not yield to typical palynological methods. Consequently, potentially important sequences of sulfate rocks may be largely neglected in palynological investigations. The method described herein utilizes gently boiling dilute (10%) hydrochloric acid (HCl) and will completely dissolve 25 grams of rock gypsum in approximately 1.5 hours. Rock anhydrite can be similarly treated but takes substantially longer than gypsum to completely dissolve. Important aspects of the process include boiling HCl at or near 102 degrees C, a beaker without a pouring spout but with a loose-fitting cover to reduce evaporation, and quenching of the hot solution in cool, filtered water to prevent reprecipitation of the dissolved calcium sulfate. The size of the rock fragments treated by this process also appears to be of importance with larger pieces of gypsum but smaller pieces of anhydrite producing the best results. Palynomorphs recovered by this method show no apparent deterioration of the exines. In addition to palynomorphs (spores, pollen, dinoflagellates, etc.), the method also resulted in the recovery of other acid insoluble fossils such as foraminiferal test linings, scolecodonts, arthropod fragments and diatoms as well as amorphous inorganic material and acid insoluble minerals. The method is also safe as long as appropriate precautions are taken.				cklupal2@comcast.net						Blatt H.G., 1980, ORIGIN SEDIMENTARY R, P538; BODINE MW, 1973, J SEDIMENT PETROL, V43, P1152; CLAYPOOLE ST, 1990, J PALEONTOL, V64, P483, DOI 10.1017/S0022336000018783; Giles PS., 2003, WINDSOR GROUP STRATI, P1; Johnson K.S., 2021, Evaporite Karst in the Greater Permian Evaporite Basin (GPEB) of Texas, New Mexico, Oklahoma, Kansas, and Colorado, V113, P1; Klimchouk A., 1996, INT J SPELEOL, V25, P2, DOI [10.5038/1827-806X.25.3.2, DOI 10.5038/1827-806X.25.3.2]; Maughan E.K., 1980, COLORADO GEOLOGY, P103; Riding JB, 2021, PALYNOLOGY, V45, P1, DOI 10.1080/01916122.2021.1878305; RUEGER BF, 1986, J PALEONTOL, V60, P189, DOI 10.1017/S002233600002165X; SHEARMAN DJ, 1981, GEOL MAG, V118, P303, DOI 10.1017/S0016756800035792; Sigma-Aldrich Co. LLC, 2021, HYDR AC 10 EMPROVE E; Tweedley J.R., 2019, Coasts and estuaries, DOI DOI 10.1016/B978-0-12-814003-1.00030-7; Warren J., 2019, SALTY MATTERS, V2019, P1	13	1	1	1	4	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology	APR 3	2023	47	2								10.1080/01916122.2022.2158956	http://dx.doi.org/10.1080/01916122.2022.2158956		DEC 2022	7	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	I2WU3					2025-03-11	WOS:000907963800001
J	Hansen, G; Daugbjerg, N; Moestrup, O				Hansen, Gert; Daugbjerg, Niels; Moestrup, Ojvind			<i>Baldinia droopii sp. nov</i>. (Suessiales, Dinophyceae), a new species from a small rainwater rock pool near Tvarminne, south-western Finland	PHYCOLOGIA			English	Article						Circadian rhythm; Cyst; Life cycle; LSU rDNA; Sexual reproduction	ALEXANDRIUM-TAYLORI DINOPHYCEAE; LAKE TOVEL; LIFE-CYCLE; WATER DINOFLAGELLATE; COMB. NOV; ULTRASTRUCTURE; GEN.; PHYLOGENY; MORPHOLOGY; SYMBIODINIUM	A dinoflagellate isolated from a small rainwater rockpool in Finland was found to be a new species of Baldinia, here described as B. droopii sp. nov. This is only the third formally described Baldinia species and the second described by modern methods. The new species had a complement of generic characters that clearly affiliated it to Baldinia: presence of an internal honeycomb structure, termed a lamellar body, a ventral fibre associated with the longitudinal basal body and a pentagonal resting cyst; and the absence of an apical structure, thecal plates and trichocysts. The most distinctive species-specific characters were the presence of a resting cyst with tubiform processes, a paratabulation matching the pattern of the motile cell, and a life cycle exhibiting a diel rhythm, alternating between motile and non-motile coccoid cells. Motile cells occurred during the light period, peaking after 3-4 h of light period, while practically no motile cells occurred during the dark period. LSU rDNA sequences confirmed B. droopii as a new species, showing c. 14% sequence difference compared to B. anauniensis. Asexual reproduction occurred primarily by binary fission or via a so-called division cyst. Sexual reproduction occurred in the culture indicating that D. droopii is homothallic. The zygote may form a resistant cyst with tubiform processes, but there were indications that this stage may be by-passed. Different stages of the asexual and putative sexual reproduction were observed and documented by video recordings.	[Hansen, Gert; Daugbjerg, Niels; Moestrup, Ojvind] Univ Copenhagen, Dept Biol, Marine Biol Sect, Univ Pk 4, DK-2100 Copenhagen, Denmark	University of Copenhagen	Hansen, G (通讯作者)，Univ Copenhagen, Dept Biol, Marine Biol Sect, Univ Pk 4, DK-2100 Copenhagen, Denmark.	gerth@bio.ku.dk	Daugbjerg, Niels/D-3521-2014	Daugbjerg, Niels/0000-0002-0397-3073				Anderson D.M., 1995, MANUAL HARMFUL MARIN, V33, P229; Baldi E., 1938, Studi Trentini Trento, V19, P247; Baldi E., 1941, Memorie del Museo di Storia Naturale della Venezia Tridentina, V6, P1; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Biecheler B., 1952, Bull. Biol. Fr. Belg., V36, P1; Borghi B., 2006, STUDI TRENTINI SC NA, V81, P476; CHODAT R., 1924, Bull. Soc. Bot. 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J	Jarvis, I; Pearce, MA; Monkenbusch, J; Jurkowska, A; Ullmann, C; Dubicka, Z; Thibault, N				Jarvis, Ian; Pearce, Martin A.; Monkenbusch, Johannes; Jurkowska, Agata; Ullmann, Clemens, V; Dubicka, Zofia; Thibault, Nicolas			Carbon isotopes, palynology and stratigraphy of the Santonian- Campanian boundary: The GSSP auxiliary sections, Seaford Head (England) and Bocieniec (Poland), and correlation between the Boreal and Tethyan realms	CRETACEOUS RESEARCH			English	Article						Santonian; Campanian boundary; Campanian GSSP; Palynology; Dinoflagellate cysts; Carbon isotope stratigraphy	WALLED DINOFLAGELLATE CYSTS; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; UPPER CRETACEOUS CHALKS; WESTERN INTERIOR BASIN; ISLE-OF-WIGHT; PLANKTONIC-FORAMINIFERA; BOTTACCIONE SECTION; GLOBAL CORRELATION; BENTHIC FORAMINIFERA; GEOMAGNETIC POLARITY	The stratigraphy and palynology of the upper Santonian-lower Campanian (Uintacrinus socialis -Gonioteuthis quadrata zones) Newhaven Chalk are described for the Campanian auxiliary GSSP section at Seaford Head, England. A new high-resolution bulk-sediment carbonate carbon stable-isotope (813Ccarb) curve provides the basis to refine the carbon-isotope event (CIE) stratigraphy of the section. Results are compared to a complementary palynological study of a second Campanian auxiliary GSSP section (U. socialis-O. pilula zones) at Bocieniec, Poland. Palynological assemblages are dominated by organic-walled dinoflagellate cysts (dinocysts; 208 taxa) at both sites. A stratigraphic framework is established via review of published lithostratigraphic, macrofossil, foraminifera and calcareous nanno-fossil records from the study sites. Carbon isotope curves with 13 major named CIEs provide a basis for correlation of Seaford Head and Bocieniec to sections at: Trunch, England; Poigny, France; La euro gerdorf, Germany; and the Campanian GSSP at Gubbio, Italy. Correlations are constrained by biostratigraphic records, including dinocyst events. The Late Santonian 813C Event (LSE, previously termed the Santonian -Campanian Boundary Event, SCBE) provides a key correlation level between Boreal and Tethyan sec-tions and enables the placement of base Campanian markers: extinction levels of the crinoid Marsupites and the planktonic foraminifera Dicarinella asymetrica; the first appearance of the calcareous nannofossil Aspidolithus parcus parcus; and the C34n/C33r magnetozone boundary (the primary Campanian marker), in both Boreal and Tethyan sections. A holostratigraphy for the Santonian-Campanian boundary interval that integrates CIEs, macrofossils, benthic and planktonic foraminifera, calcareous nannofossils, dinocysts and magnetostratigraphy is presented. Rhynchodiniopsis juneae sp. nov. is described.(c) 2022 The Author(s). Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).	[Jarvis, Ian] Kingston Univ London, Dept Geog Geol & Environm, Penrhyn Rd, Kingston Upon Thames KT1 2EE, England; [Pearce, Martin A.] Nat Hist Museum, Dept Earth Sci, Cromwell Rd, London SW7 5BD, England; [Monkenbusch, Johannes; Thibault, Nicolas] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Jurkowska, Agata] Univ Sci & Technol, Fac Geol Geophys & Environm Protect AGH, Mickiewicza 30, PL-30059 Krakow, Poland; [Ullmann, Clemens, V] Univ Exeter, Camborne Sch Mines, Penryn Campus, Penryn TR10 9FE, Cornwall, England; [Ullmann, Clemens, V] Univ Exeter, Environm & Sustainabil Inst, Penryn Campus, Penryn TR10 9FE, Cornwall, England; [Dubicka, Zofia] Univ Warsaw, Fac Geol, Al Zwirki & Wigury 93, PL-02089 Warsaw, Poland	Kingston University; Natural History Museum London; University of Copenhagen; AGH University of Krakow; University of Exeter; University of Exeter; University of Warsaw	Jarvis, I (通讯作者)，Kingston Univ London, Dept Geog Geol & Environm, Penrhyn Rd, Kingston Upon Thames KT1 2EE, England.	i.jarvis@kingston.ac.uk	Ullmann, Clemens/I-3227-2019; Jurkowska, Agata/A-9734-2016; Thibault, Nicolas/B-1106-2013; Dubicka, Zofia/ABB-3388-2020; Jarvis, Ian/A-1637-2008	Pearce, Martin/0000-0001-7856-1076; Monkenbusch, Johannes/0000-0002-0833-836X; Jurkowska, Agata/0000-0001-5457-9968; Thibault, Nicolas/0000-0003-4147-5531; Dubicka, Zofia/0000-0003-1105-4111; Jarvis, Ian/0000-0003-3184-3097	UK Natural Environment Research Council (NERC) [NE/H020756/1]; Evolution Applied Limited [4502311303]; National Science Centre of Poland [2020/37/B/ST10/00287]; Carlsbergfondet [CF16-0456]	UK Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Evolution Applied Limited; National Science Centre of Poland(National Science Centre, Poland); Carlsbergfondet(Carlsberg Foundation)	Field assistance at Seaford Head was ably provided by Kevin Attree, Tara Brodie, Simon Crust, Delano Henry (Kingston Univer-sity London) , Kresten Anderskouv, Toms Buls (University of Copenhagen) and Madeleine Vickers (University of Oslo) . Malcolm Jones (Palynological Laboratory Services Limited, PLS) is thanked for the preparation of the palynological samples. Iain Prince (Shell USA) provided unpublished data from his palynological study of Whitecliff, IOW. IJ was funded by UK Natural Environment Research Council (NERC) grant NE/H020756/1. Support by Evolution Applied Limited to MAP and Equinor Energy AS (previously Statoil ASA) to IJ (contract 4502311303) is gratefully acknowledged. Preparation of palynological samples from Bocieniec was funded by the National Science Centre of Poland (grant 2020/37/B/ST10/00287 to AJ) . NT and JM acknowledge Carlsbergfondet CF16-0456 for funding travel expenses, sampling, and geochemical analysis. Poul Schi?ler, Irek Walaszczyk and editor Eduardo Koutsoukos are thanked for their careful reviews and suggestions for improving the manuscript.	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Memoir, V4, P589	204	3	3	1	12	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	MAR	2023	143								105415	10.1016/j.cretres.2022.105415	http://dx.doi.org/10.1016/j.cretres.2022.105415		DEC 2022	45	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	7M1XN		hybrid, Green Published			2025-03-11	WOS:000906448700001
J	Davtalab, E; Kalanat, B; Vahidinia, M				Davtalab, Elham; Kalanat, Behnaz; Vahidinia, Mohammad			Palynostratigraphy and paleoenvironments of the upper Turonian-lower Campanian Abderaz Formation in the east of Kopet- Dagh Basin (NE Iran)	CRETACEOUS RESEARCH			English	Article						Abderaz Formation; Dinocysts; Iran; Palynofacies; Kopet-Dagh Basin; Upper Cretaceous	DINOFLAGELLATE CYSTS; INTEGRATED BIOSTRATIGRAPHY; PLANKTONIC-FORAMINIFERA; SEQUENCE STRATIGRAPHY; CONIACIAN; BOUNDARY; RECORD; MIDDLE; PALEOCEANOGRAPHY; STRATOTYPE	The palynology and palynofacies of the Abderaz Formation have been studied to interpret the paleo-environments and sea-level changes in the Upper Cretaceous deposits of the Kopet-Dagh Basin. This formation in the Kalat-e-Naderi region (Gharesu section) is composed of 462 m of gray to cream shales, marlstone layers and three chalky limestone units. Seven dinoflagellate cyst (dinocysts) and four planktonic foraminiferal biozones have been identified in the studied succession, which suggest a late Turonian-early Campanian age for this interval. Four different depositional environments have been recognized in the studied section based on the relative proportion of organic matter (terrestrial organic matter, marine palynomorphs and amorphous organic matter). High abundance of marine palynomorphs in most samples indicates the predominance of an oxygenated distal shelf environment in the upper Turonian-lower Campanian interval. Seven third-order depositional sequences are proposed for the Abderaz Formation. A good correlation of sequence boundaries with the global sea-level fall events suggests that eustasy played an important role during the deposition of the Abderaz Formation.(c) 2022 Published by Elsevier Ltd.	[Davtalab, Elham] Univ Neyshabur, Fac Sci, Dept Geol, Neyshabur, Iran; [Kalanat, Behnaz] Agr Res Educ & Extens Org AREEO, Res Inst Forests & Rangelands, Bot Res Div, Tehran, Iran; [Vahidinia, Mohammad] Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran	Ferdowsi University Mashhad	Vahidinia, M (通讯作者)，Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran.	vahidinia@mail.um.ac.ir	Kalanat, Behnaz/AAB-7559-2020	Kalanat, Behnaz/0000-0002-4410-3453				Afshar-Harb A., 1994, GEOLOGY KOPPEH DAGH, P265; Angiolini L, 2007, GEOLOGY, V35, P1071, DOI 10.1130/G24031A.1; [Anonymous], 1996, Palynology: principles and applications; Ardestani Meysam Shafiee, 2012, Geologica Balcanica, V41, P21; Ardestani Meysam Shafiee, 2011, Egyptian Journal of Paleontology, V11, P1; Ardestani Meysam Shafiee, 2013, Open Journal of Geology, V3, P19; Aredestani MS, 2020, STRATIGRAPHY, V17, P121, DOI 10.29041/strat.17.2.121-134; Barrier E., 2008, PALAEOTECTONIC MAPS; Batten DJ, 2005, T GEOBIOL, V23, P203; BUJAK J P, 1978, Geological Survey of Canada Bulletin, P1; 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Res.	MAR	2023	143								105394	10.1016/j.cretres.2022.105394	http://dx.doi.org/10.1016/j.cretres.2022.105394		DEC 2022	16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	7L6CV					2025-03-11	WOS:000906052200001
J	Vallejo, JD; Piovesan, EK; Carvalho, MD; Guzman, J				Vallejo, Juan David; Piovesan, Enelise Katia; Carvalho, Marcelo de Araujo; Guzman, Juliana			Palynofacies analyses of Santana Group, upper Aptian of the Araripe Basin, northeast Brazil: Paleoenvironmental reconstruction	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sedimentary organic matter; Palynology; Post-rift sequence	EARLY CRETACEOUS PALEOGEOGRAPHY; SOUTH ATLANTIC; SEQUENCE STRATIGRAPHY; ROMUALDO FORMATION; ORGANIC-MATTER; FACIES; SUCCESSION	We present the paleoenvironmental analysis based on sedimentary organic matter (SOM) of alluvial-lacustrinetransitional deposits that crop out in the east portion of the Araripe Basin, Cear ' a State, Brazil. Samples were collected from the Barbalha, Crato, Ipubi and Romualdo formations, Santana Group. For the palynofacies analyses, the kerogen categories were counted and grouped. The described SOM were subdivided into six groups: Structureless, which consists of resin and amorphous organic matter (AOM); Terrigenous, which consists of nonopaque biostructured-phytoclast; Opaque, which consists of equidimensional, lath and corroded of black color; Sporomorphs, which consist of spores and pollen grains; Freshwater, constituted by Botryococcus and Pediastrum microplankton and Marine elements, represented by dinoflagellate cysts and foraminiferal lining. The stratigraphic distribution of the seven palynofacies reflects a change from fluvial system to a lacustrine environment, as well as the first marine incursion on Serra da Ma similar to ozinha section (Crato Formation). In the top of the Santana Group recorded a transition from a lacustrine environment close to a fluvio-deltaic source to an estuarine system, marked by the presence of Subtilisphaera, during the late Aptian. The palynological data presented indicates that the entire Santana Group is of Aptian age considering the conspicuous presence of Sergipea variverrucata in the sections.	[Vallejo, Juan David; Piovesan, Enelise Katia; Guzman, Juliana] Univ Fed Pernambuco UFPE, Ctr Tecnol & Geociencias CTG, Programa Posgrad Geociencias PPGEOC, Av Arquitetura,S-N Cidade Univ, BR-50740550 Recife, PE, Brazil; [Vallejo, Juan David; Piovesan, Enelise Katia; Guzman, Juliana] Univ Fed Pernambuco UFPE, Dept Geol DGEO, Lab Micropaleontol Aplicada LAGESE LITPEG, Av Arquitetura,S-N Cidade Univ, BR-50740550 Recife, PE, Brazil; [Carvalho, Marcelo de Araujo] Univ Fed Rio De Janeiro, Dept Geol & Paleontol, Museu Nacl, Lab Paleoecol Vegetal, Rio De Janeiro, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal do Rio de Janeiro	Vallejo, JD (通讯作者)，Univ Fed Pernambuco UFPE, Ctr Tecnol & Geociencias CTG, Programa Posgrad Geociencias PPGEOC, Av Arquitetura,S-N Cidade Univ, BR-50740550 Recife, PE, Brazil.	juandavidv85@gmail.com; enelise.katia@ufpe.br; mcarvalhomn@gmail.com	Piovesan, Enelise/Q-2953-2017	VALLEJO RAMIREZ, JUAN DAVID/0000-0002-2335-7008	Brazilian National Petroleum Agency (ANP); PETROBRAS [2017/00263-2, 2018/00320-9, 2019/00280-0]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq [309766/2021-4]; Forte [2019-00280] Funding Source: Forte	Brazilian National Petroleum Agency (ANP); PETROBRAS(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Forte(Swedish Research Council for Health Working Life & Welfare (Forte))	The authors would like to acknowledge the Brazilian National Petroleum Agency (ANP) and PETROBRAS for financial support through the following projects: "ARTUNJA: Correlacoes bioestratigraficas dos sistemas fluvio-lacustres das fases rifte e pos-rifte das bacias do Araripe, Jatoba e Tucano Norte, NE do Brasil/n. 2017/00263-2"; "Implantacao da infraestrutura do Laboratorio de Micropaleontologia Aplicada da Universidade Federal de Pernambuco/n. 2018/00320-9" and "Bio- estratigrafia de alta resolucao e paleoambientes das bacias do Araripe, Tucano Norte e Jatoba (secoes rifte e pos-rifte) /n. 2019/00280-0". EKP thanks the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq (grant n. 309766/2021-4) . We also thank the reviewers and the editor for their useful suggestions and comments.	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JAN	2023	121								104154	10.1016/j.jsames.2022.104154	http://dx.doi.org/10.1016/j.jsames.2022.104154		DEC 2022	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	7Q8OV		Bronze			2025-03-11	WOS:000909644800001
J	Mertens, KN; Morquecho, L; Carbonell-Moore, C; Meyvisch, P; Gu, HF; Bilien, G; Duval, A; Derrien, A; Pospelova, V; Sliwinska, KK; Gárate-Lizárraga, I; Pérez-Cruz, B				Mertens, Kenneth Neil; Morquecho, Lourdes; Carbonell-Moore, Consuelo; Meyvisch, Pjotr; Gu, Haifeng; Bilien, Gwenael; Duval, Audrey; Derrien, Amelie; Pospelova, Vera; Sliwinska, Kasia K.; Garate-Lizarraga, Ismael; Perez-Cruz, Beatriz			<i>Pentaplacodinium</i><i> lapazense</i> sp. nov. from Central and Southern Gulf of California, a new non-toxic gonyaulacalean resembling Protoceratium reticulatum	MARINE MICROPALEONTOLOGY			English	Article						Operculodinium; Yessotoxins; BahiaConcepcion; Bahia de La Paz; micro-FTIR spectroscopy	ROYAL-SOCIETY BOREHOLE; DINOFLAGELLATE CYSTS; BAHIA CONCEPCION; SURFACE SEDIMENTS; LA-PAZ; BENTHIC DINOFLAGELLATE; PLANKTONIC DIATOMS; DINOPHYCEAE; PHYTOPLANKTON; PERIDINIALES	A new Pentaplacodinium species with six precingular plates is described from Bahia Concepci ' on and Bahia de la Paz, Gulf of California. The non-fossil motile stage is described as Pentaplacodinium lapazense, whilst the fossil stage is described as Operculodinium lapazense. The cyst morphology is compared to topotype material of Oper-culodinium israelianum, which is larger, has longer processes and has a different wall structure. The motile cells display a plate formula of Po, Pt, X, 2 '+*2 ', 6 '', 6c, 7s, 5 ''', 1p, 1 ''''. A typical gonyaulacalean fission line and plate overlap are observed. SSU-ITS-LSU ribosomal DNA sequences demonstrate that Pentaplacodinium saltonense is its closest relative. The species is homothallic. This species occurs in relatively shallow and restricted coastal areas, and has a preference for higher sea-surface temperatures and salinities. Micro-FTIR spectra of the cysts are compared to spectra of cysts of other gonyaulacaleans and suggest very similar compositions. No yessotoxins were detected in any of the analyzed strains, hence, this species is unlikely to be responsible for the elevated yessotoxin concentration observed in shellfish on the southern and central coastal region of the Gulf of California.	[Mertens, Kenneth Neil; Bilien, Gwenael; Duval, Audrey; Derrien, Amelie] IFREMER, LITTORAL, F-29900 Concarneau, France; [Morquecho, Lourdes] Ctr Invest Biol Noroeste CIBNOR, Playa Palo Santa Rita Sur, Av IPN 195, La Paz 23096, Baja California, Mexico; [Carbonell-Moore, Consuelo] Oregon State Univ, Coll Agr Sci, Dept Bot & Plant Pathol, 2082 Cordley Hall, Corvallis, OR 97331 USA; [Meyvisch, Pjotr] Univ Ghent, Dept Geol, Krijgslaan 281, B-9000 Ghent, Belgium; [Gu, Haifeng] Minist Nat Resources, Dept Marine Biol & Ecol, Inst Oceanog 3, Xiamen 361005, Peoples R China; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, 116 Church St SE, Minneapolis, MN 55455 USA; [Sliwinska, Kasia K.] Geol Survey Denmark & Greenland, GEUS, Dept Geoenergy & Storage, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Garate-Lizarraga, Ismael] Ctr Interdisciplinario Ciencias Marinas, Inst Politecn Nacl, Playa Palo Santa Rita, Av IPN S-N, La Paz, Baja California, Mexico; [Perez-Cruz, Beatriz] Lab Estatal Salud PablicaDr Gale Soberon & Parra, Blvd Vicente Guerrero,Esq Juan R Escudero S-N, Acapulco, Guerrero, Mexico	Ifremer; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Oregon State University; Ghent University; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources; University of Minnesota System; University of Minnesota Twin Cities; Geological Survey Of Denmark & Greenland; Instituto Politecnico Nacional - Mexico	Mertens, KN (通讯作者)，IFREMER, LITTORAL, F-29900 Concarneau, France.	kenneth.mertens@ifremer.fr; lamorquecho@cibnor.mx; carbonem@oregonstate.edu; Pjotr.Meyvisch@UGent.be; guhaifeng@tio.org.cn; vpospe@umn.edu; kksl@geus.dk	Morquecho, Lourdes/JPY-0626-2023; Mertens, Kenneth/AAO-9566-2020; Meyvisch, Pjotr/ABB-1527-2021; Mertens, Kenneth/C-3386-2015; Sliwinska, Kasia K./G-9097-2018; Gu, Haifeng/ADN-4528-2022	Morquecho, Lourdes/0000-0003-2963-8836; Meyvisch, Pjotr/0000-0002-1270-2152; Mertens, Kenneth/0000-0003-2005-9483; Sliwinska, Kasia K./0000-0001-5488-8832; Pospelova, Vera/0000-0003-4049-8133; Derrien, Amelie/0000-0001-9656-7850; Gu, Haifeng/0000-0002-2350-9171	Regional Council of Brittany; CIBNOR project [SIP-20220515]; General Council of Finistere; urban community of Concarneau-Cornouaille-Agglomeration; CONACYT; Instituto Politecnico Nacional, Mexico; IGL;  [20449];  [A1-S-37026];  [SIP-20180551]	Regional Council of Brittany(Region Bretagne); CIBNOR project; General Council of Finistere(Region Bretagne); urban community of Concarneau-Cornouaille-Agglomeration; CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); Instituto Politecnico Nacional, Mexico; IGL; ; ; 	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. Oury Teboulle is gratefully acknowledged for help obtaining topotype material from the Geological Survey of Israel (GSI). This study was also supported by CIBNOR project 20449, and CONACYT A1-S-37026 grant. Amada Reyes-Salinas (CIB-NOR) provided technical assistance. Thelma Castellanos and Angel Carrillo (CIBNOR) provided technical advice and infrastructure of the Molecular Microbial Ecology Laboratory. The project was partially funded by Instituto Politecnico Nacional, Mexico (grants SIP-20180551 and SIP-20220515). IGL is a COFAA fellow. Two anonymous reviewers are acknowledged for comments that significantly improved the manuscript.	Alix B, 2012, NUCLEIC ACIDS RES, V40, pW573, DOI 10.1093/nar/gks485; Andersen R. 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Micropaleontol.	JAN	2023	178								102187	10.1016/j.marmicro.2022.102187	http://dx.doi.org/10.1016/j.marmicro.2022.102187		DEC 2022	22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	7B4SB		Green Submitted, Bronze, Green Published			2025-03-11	WOS:000899123900001
J	Versteegh, GJM; Zonneveld, KAF				Versteegh, Gerard J. M.; Zonneveld, Karin A. F.			Micro-Fourier transform infrared spectroscopy of degradation-resistant organic microfossils; Influence of preservation environment and phylogeny	FRONTIERS IN MARINE SCIENCE			English	Article						micro-FTIR (Fourier transform infrared spectroscopy); dinoflagellate cyst; particulate organic matter (POM) preservation; redox environments; molecular characteristics	WALLED DINOFLAGELLATE CYSTS; AEROBIC DEGRADATION; RESTING CYSTS; MATTER; SEDIMENTS	To gain more insight into the effect of early diagenetic processes in different redox environments on the molecular characteristics of degradation resistant particulate organic matter, the molecular cyst wall characteristics of the closely related dinoflagellates Impagidinium aculeatum and I. patulum from oxic and anoxic sedimentary environments in the Madeira Abyssal Plain F-turbidite and in the surface sediments of the eastern Mediterranean Sea have been analysed with micro-FTIR spectroscopy. Both species have cysts that are representatives of particulate organic matter being extremely resistant against degradation in natural environments. Their walls primarily consist of a carbohydrate-based polymer. Spectral differences could not be observed between cysts from oxic and anoxic environments, neither from different areas nor from different geological times. However, we identify consistent compositional differences between both species. Compared to I. patulum, cyst walls of I. aculeatum contain more C-O probably of secondary alcohols that might imply a slightly higher resistance to decay of I. patulum. Comparison with cyst species that represent particular organic matter being extremely sensitive and slightly resistant against aerobic degradation in natural settings reveals that cysts walls of the most vulnerable species show C=N, N-H, N-O, C-N bending/stretching, as well as the presence of C=O and C-O bounds. Cyst species that are somewhat less sensitive have a strong indication of the presence of nitrogen in their macromolecules. More resistant species lack nitrogen whereas the most resistant cyst species I. aculeatum and I. patulum show low amounts of C=O.	[Versteegh, Gerard J. M.; Zonneveld, Karin A. F.] Univ Bremen, Ctr Marine Environm Sci, MARUM, Bremen, Germany; [Versteegh, Gerard J. M.] Helmholtz Zent Polar und Meeresforschung, Alfred Wegener Inst, Marine Geochem, Bremerhaven, Germany; [Versteegh, Gerard J. M.] Jacobs Univ Bremen, Dept Phys & Earth Sci, Bremen, Germany; [Zonneveld, Karin A. 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Mar. Sci.	DEC 7	2022	9								1040543	10.3389/fmars.2022.1040543	http://dx.doi.org/10.3389/fmars.2022.1040543			13	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	7B7RP		gold			2025-03-11	WOS:000899326600001
J	Gao, JF; Su, Q				Gao, Junfeng; Su, Qiang			A multi-level exploration of the relationship between temperature and species diversity: Two cases of marine phytoplankton	ECOLOGY AND EVOLUTION			English	Article						coccolithophore; dinoflagellate cyst; fractal model; species abundance distribution; the asymptotic relationship	ABUNDANCE DISTRIBUTION; METABOLIC THEORY; SELF-SIMILARITY; RICHNESS; BIODIVERSITY; PATTERNS; EVENNESS; GRADIENTS; INDEXES; SIZE	The relationship between temperature (T) and diversity is one of the most important issues in ecology. It provides a key direction not only for exploring the determinants of diversity's patterns, but also for understanding diversity's responses to climate change. Previous studies suggested that T-diversity relationships could be positive, negative, or unimodal. Although these studies accumulated many informative achievements, they might be unsatisfied due to (1) investigating inadequate range of T, (2) selecting incomplete diversity metrics, and (3) making insufficiently detailed analysis of correlation. In this study, species diversity is estimated by four most commonly used diversity metrics and three parameters of species abundance distribution (SAD), and two global datasets of marine phytoplankton (covering a wider range of T) are used to evaluate the T-diversity relationships according to a piecewise model. Results show that all aspects of diversity (except evenness) have the similar relationship with T in the range of lower T, noting that diversity significantly increases as T increases. However, in the range of higher T, diversity may significantly decrease or nearly constant, which indicates that their relationships may be the unimodal or asymptotic. The asymptotic relationship found by this study is assumed that increasing diversity with T will gradually approach the Zipf's law (1:1/2:1/3 horizontal ellipsis ). If such assumption can be verified by future investigations, the intrinsic mechanism of the asymptotic relationship is likely to be crucial in understanding the T-diversity relationships.	[Gao, Junfeng; Su, Qiang] Univ Chinese Acad Sci UCAS, Coll Earth & Planetary Sci CEPS, Beijing, Peoples R China; [Su, Qiang] Univ Chinese Acad Sci UCAS, Coll Earth & Planetary Sci CEPS, 19A Yuquan Rd, Beijing 100049, Peoples R China		Su, Q (通讯作者)，Univ Chinese Acad Sci UCAS, Coll Earth & Planetary Sci CEPS, 19A Yuquan Rd, Beijing 100049, Peoples R China.	sqiang@ucas.ac.cn	Su, Qiang/H-3616-2017; Gao, Junfeng/JDV-8786-2023	Gao, Junfeng/0000-0003-3334-3555; , SU/0000-0002-8044-8176	National Natural Science Foundation of China;  [42071137];  [41676113]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); ; 	ACKNOWLEDGMENTS This work was supported by the National Natural Science Foundation of China, Grant No. 42071137 and No. 41676113. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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Evol.	DEC	2022	12	12							e9584	10.1002/ece3.9584	http://dx.doi.org/10.1002/ece3.9584			10	Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology	6Y6OX	36523537	gold, Green Published			2025-03-11	WOS:000897213300001
J	Anderson, DM; Fachon, E; Hubbard, K; Lefebvre, KA; Lin, PG; Pickart, R; Richlen, M; Sheffield, G; Van Hemert, C				Anderson, Donald M.; Fachon, Evangeline; Hubbard, Katherine; Lefebvre, Kathi A.; Lin, Peigen; Pickart, Robert; Richlen, Mindy; Sheffield, Gay; Van Hemert, Caroline			HARMFUL ALGAL BLOOMS IN THE ALASKAN ARCTIC AN EMERGING THREAT AS THE OCEAN WARMS	OCEANOGRAPHY			English	Article							PSEUDO-NITZSCHIA; DOMOIC ACID; CHUKCHI SEA; TOXINS; ABUNDANCE; SHIFTS; CYSTS; WATER	Harmful algal blooms (HABs) present an emerging threat to human and ecosystem health in the Alaskan Arctic. Two HAB toxins are of concern in the region: saxitoxins (STXs), a family of compounds produced by the dinoflagellate Alexandrium catenella, and domoic acid (DA), produced by multiple species in the diatom genus Pseudo-nitzschia. These potent neurotoxins cause paralytic and amnesic shellfish poisoning, respectively, in humans, and can accumulate in marine organisms through food web transfer, causing illness and mortality among a suite of wildlife species. With pronounced warming in the Arctic, along with enhanced transport of cells from southern waters, there is significant potential for more frequent and larger HABs of both types. STXs and DA have been detected in the tissues of a range of marine organisms in the region, many of which are important food resources for local residents. The unique nature of the Alaskan Arctic, including difficult logisticalaccess,lack of response infrastructure, and reliance of coastal populations on the noncommercial acquisition of marine resources for nutritional, cultural, and economic well-being, poses urgent and significant challenges as this region warms and the potential for impacts from HABs expands.	[Anderson, Donald M.; Richlen, Mindy] Woods Hole Oceanog Inst WHOI, Biol Dept, Woods Hole, MA 02543 USA; [Fachon, Evangeline] MIT, WHOI Joint Program Biol Oceanog, Woods Hole, MA USA; [Hubbard, Katherine] Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, St Petersburg, FL USA; [Lefebvre, Kathi A.] Northwest Fisheries Sci Ctr, NOAA, Seattle, WA USA; [Lin, Peigen; Pickart, Robert] WHOI, Phys Oceanog Dept, Woods Hole, MA USA; [Sheffield, Gay] Univ Alaska Fairbanks, Alaska Sea Grant, Fairbanks, AK USA; [Van Hemert, Caroline] US Geol Survey Alaska Sci Ctr, Res Wildlife Biologist, Anchorage, AK USA	Massachusetts Institute of Technology (MIT); Florida Fish & Wildlife Conservation Commission; National Oceanic Atmospheric Admin (NOAA) - USA; University of Alaska System; University of Alaska Fairbanks	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst WHOI, Biol Dept, Woods Hole, MA 02543 USA.	danderson@whoi.edu			NSF Office of Polar Programs [OPP-1823002, OPP-1733564]; NOAA's Arctic Research program (Cooperative Institute for the North Atlantic Region [CINAR]) [NA14OAR4320158, NA19OAR4320074]; NOAA's Center for Coastal and Ocean Studies ECOHAB Program [NA20NOS4780195]; US National Park Service Shared Beringian Heritage Program [P21AC12214-00]	NSF Office of Polar Programs(National Science Foundation (NSF)); NOAA's Arctic Research program (Cooperative Institute for the North Atlantic Region [CINAR]); NOAA's Center for Coastal and Ocean Studies ECOHAB Program; US National Park Service Shared Beringian Heritage Program	The authors acknowledge that the Alaskan Arctic as described here includes the lands and waters of the Inupiaq, Saint Lawrence Island Yupik, and Central Yupik peoples. Funding for DMA, RSP, EF, PL, and MLR was provided by grants from NSF Office of Polar Programs (OPP-1823002 and OPP-1733564) and NOAA's Arctic Research program (through the Cooperative Institute for the North Atlantic Region [CINAR]; NA14OAR4320158 and NA19OAR4320074), and for DMA, KH, and KAL through NOAA's Center for Coastal and Ocean Studies ECOHAB Program (NA20NOS4780195). Additional support was pro-vided for DMA, MLR, and EF by the US National Park Service Shared Beringian Heritage Program (P21AC12214-00). We also thank Natalie Renier (WHOI Graphic Services) and Emily Bowers (Northwest Fisheries Science Center) for creating figures. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the US Government. This is ECOHAB Contribution number 1007.	Alaska DHSS (Alaska Department of Health and Social Services), 2020, REC AL DEATH DUE PAR; Anderson CR, 2019, FRONT MAR SCI, V6, DOI 10.3389/fmars.2019.00250; Anderson DM, 2021, P NATL ACAD SCI USA, V118, DOI 10.1073/pnas.2107387118; Anderson DM, 2021, HARMFUL ALGAE, V102, DOI 10.1016/j.hal.2021.101975; Anderson DM, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; Anderson DM, 2012, ANNU REV MAR SCI, V4, P143, DOI 10.1146/annurev-marine-120308-081121; Bates SS, 2018, HARMFUL ALGAE, V79, P3, DOI 10.1016/j.hal.2018.06.001; Brosnahan ML, 2015, LIMNOL OCEANOGR, V60, P2059, DOI 10.1002/lno.10155; BURSA ADAM, 1963, ARCTIC JOUR ARCTIC INST N AMER, V16, P239; Deeds JR, 2008, MAR DRUGS, V6, P308, DOI [10.3390/md20080015, 10.3390/md6020308]; Doucette GJ, 2017, COMP ANAL C, V78, P411, DOI 10.1016/bs.coac.2017.06.006; Fair S.W., 1995, QAMANI COAST MY MIND; Fischer AD, 2018, PROTIST, V169, P645, DOI 10.1016/j.protis.2018.06.001; Grattan LM, 2018, TOXINS, V10, DOI 10.3390/toxins10030103; Gu HF, 2013, POLAR BIOL, V36, P427, DOI 10.1007/s00300-012-1273-5; Haroardóttir S, 2015, MAR DRUGS, V13, P3809, DOI 10.3390/md13063809; Hendrix AM, 2021, MAR MAMMAL SCI, V37, P1292, DOI 10.1111/mms.12822; Huntington HP, 2020, NAT CLIM CHANGE, V10, P342, DOI 10.1038/s41558-020-0695-2; Landsberg JH, 2014, TOXINS AND BIOLOGICALLY ACTIVE COMPOUNDS FROM MICROALGAE VOL 2: BIOLOGICAL EFFECTS AND RISK MANAGEMENT, P379; Lefebvre KA, 2001, MAR BIOL, V138, P693, DOI 10.1007/s002270000509; Lefebvre KA, 2022, HARMFUL ALGAE, V114, DOI 10.1016/j.hal.2022.102205; Lefebvre KA, 2016, HARMFUL ALGAE, V55, P13, DOI 10.1016/j.hal.2016.01.007; Lewitus AJ, 2012, HARMFUL ALGAE, V19, P133, DOI 10.1016/j.hal.2012.06.009; McCabe RM, 2016, GEOPHYS RES LETT, V43, P10366, DOI 10.1002/2016GL070023; McKibben SM, 2017, P NATL ACAD SCI USA, V114, P239, DOI 10.1073/pnas.1606798114; Miyazono A, 2012, HARMFUL ALGAE, V16, P81, DOI 10.1016/j.hal.2012.02.001; Natsuike M, 2017, HARMFUL ALGAE, V61, P80, DOI 10.1016/j.hal.2016.11.019; Natsuike M, 2013, HARMFUL ALGAE, V27, P52, DOI 10.1016/j.hal.2013.04.006; Olson RJ, 2007, LIMNOL OCEANOGR-METH, V5, P195, DOI 10.4319/lom.2007.5.195; Percopo I, 2016, J PHYCOL, V52, P184, DOI 10.1111/jpy.12395; Poulin Michel, 2011, Marine Biodiversity, V41, P13, DOI 10.1007/s12526-010-0058-8; Stevenson DE, 2019, POLAR BIOL, V42, P407, DOI 10.1007/s00300-018-2431-1; Tammilehto A, 2015, AQUAT TOXICOL, V159, P52, DOI 10.1016/j.aquatox.2014.11.026; Trainer VL, 2014, J SHELLFISH RES, V33, P531, DOI 10.2983/035.033.0222; Van Hemert C., 2021, AM ORNITHOLOGICAL SO; Van Hemert C, 2021, J WILDLIFE DIS, V57, P399, DOI 10.7589/JWD-D-20-00057; Weber C, 2021, PHYCOLOGIA, V60, P619, DOI 10.1080/00318884.2021.1973789; Wekell John C., 1994, Natural Toxins, V2, P197, DOI 10.1002/nt.2620020408	38	7	8	3	23	OCEANOGRAPHY SOC	ROCKVILLE	P.O. BOX 1931, ROCKVILLE, MD USA	1042-8275			OCEANOGRAPHY	Oceanography	DEC	2022	35	3-4			SI		130	139						10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	7W2GO					2025-03-11	WOS:000913331600014
J	Santos, AA; Piñuela, L; Rodríguez-Barreiro, I; García-Ramos, JC; Diez, JB				Santos, Artai A.; Pinuela, Laura; Rodriguez-Barreiro, Ivan; Carlos Garcia-Ramos, Jose; Diez, Jose B.			Jurassic Palynology from "The Dinosaur Coast" of Asturias (Lastres Fm., Northwestern Spain): Palynostratigraphical and Palaeoecological Insights	BIOLOGY-BASEL			English	Article						palynology; plant communities; wildfires; Late Jurassic; "The Dinosaur Coast"; North Spain	WESTERN PORTUGAL; LUSITANIAN BASIN; IN-SITU; EUROPE; BIOGEOGRAPHY; TERRESTRIAL; SUCCESSION; PATAGONIA; TOARCIAN; WEALDEN	The Upper Jurassic deposits of the Lastres Formation crop out on the Asturian coast (northwest of the Iberian Peninsula), in the so-called "The Dinosaur Coast". This formation presents a high abundance of dinosaur remains and other vertebrates. Despite the deep knowledge about its fauna and environment, practically nothing is known about the plant communities that formed the landscape of the region at the end of the Jurassic. We present here the first palynological data of the Lastres Fm., identifying a rich and abundant palynological assemblage formed by more than 60 different taxa. The presence of some taxa with biostratigraphic value suggests a Kimmeridgian-Tithonian age for this formation. On the other hand, the botanical affinities of the taxa found indicate that the vegetation of the "The Dinosaur Coast" of Asturias would not be homogeneous, but would be formed by a mosaic of different plant communities that would adapt to the variety of environments present in the region. The presence of forest areas probably represented a protected environment as well as a food source for herbivorous dinosaurs. Analysis of charcoalified wood remains suggests that palaeofires were relatively recurrent in the study area. Abundant fossils of vertebrates (mainly footprints and bones of dinosaurs) and numerous invertebrates occur in the Upper Jurassic deposits of the Lastres Formation in the Asturias region, North of Spain. However, no palynological study has been published from this geological formation; therefore, much palaeoenvironmental and palaeoecological information is still unknown. In this study, a total of 62 morphospecies, belonging to 49 different morphogenera were identified, including pollen, spores, algae remains, fungi spores, dinoflagellates, foraminifera, and scolecodonts from four different locations on the Asturian coast. Spores are the dominant group of palynomorphs, both in diversity and abundance, contrasting with the minor diversity of pollen grains. The age of some key taxa indicates that the palynological assemblage cannot be older than the Kimmeridgian, suggesting a Kimmeridgian-Tithonian age. The botanical and environmental affinities of the pollen and spores indicate the presence of different plant assemblages, including plant communities from humid areas such as the margin of rivers and small freshwater ponds that were dominated by bryophytes and ferns, and a coastal plant community that would inhabit arid areas and would be dominated by gymnosperms and some pteridophytes. The SEM analyses of wood remains show the abundance of charcoalified remains suggesting that wildfires were usual in "The Dinosaur Coast" of Asturias during the Kimmeridgian.	[Santos, Artai A.; Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo CIM UVIGO, Ctr Invest Marina, Vigo 36310, Spain; [Santos, Artai A.; Rodriguez-Barreiro, Ivan; Diez, Jose B.] Univ Vigo, Dept Xeociencias Marinas & OT, Vigo 36310, Spain; [Pinuela, Laura; Carlos Garcia-Ramos, Jose] MUJA Museo Juras Asturias, Rasa De San Telmo 33328, Colunga, Spain	Universidade de Vigo; CIM UVIGO; Universidade de Vigo	Santos, AA (通讯作者)，Univ Vigo CIM UVIGO, Ctr Invest Marina, Vigo 36310, Spain.; Santos, AA (通讯作者)，Univ Vigo, Dept Xeociencias Marinas & OT, Vigo 36310, Spain.	asantos@uvigo.es	Piñuela, Laura/ABB-9908-2020; Santos, Artai/AAM-4202-2021; Diez, Jose B./L-1004-2014	Diez, Jose B./0000-0001-5739-7270; Santos Lopez, Artai Anton/0000-0002-2399-8825; Rodriguez-Barreiro, Ivan/0000-0002-0938-662X	Ministerio de Ciencia, Innovacion y Universidades [PGC2018-094034-B-C22]; Strategic Priority Research Program (B) of the Chinese Academy of Sciences [XDB26000000]; Galician Government [ED481A-2019/243, ED481A-2020/175]; Universidade de Vigo; Sociedad Publica de Gestion y Promocion Turistica y Cultural del Principado de Asturias	Ministerio de Ciencia, Innovacion y Universidades(Spanish Government); Strategic Priority Research Program (B) of the Chinese Academy of Sciences(Chinese Academy of Sciences); Galician Government; Universidade de Vigo; Sociedad Publica de Gestion y Promocion Turistica y Cultural del Principado de Asturias	This research was funded by Ministerio de Ciencia, Innovacion y Universidades' (grant number PGC2018-094034-B-C22) and by the Strategic Priority Research Program (B) of the Chinese Academy of Sciences (grant number XDB26000000). A.A.S. and I.R.-B. are financially supported by the Galician Government (grants ED481A-2019/243 and ED481A-2020/175). A.A.S. was also supported by mobility grants from the Universidade de Vigo to take samples in the field. The financial support for L.P. and J.C.G.-R. was provided by Sociedad Publica de Gestion y Promocion Turistica y Cultural del Principado de Asturias.	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J	Li, FT; Yue, CX; Deng, YY; Tang, YZ				Li, Fengting; Yue, Caixia; Deng, Yunyan; Tang, Ying Zhong			Characterizing the Status of Energetic Metabolism of Dinoflagellate Resting Cysts under Mock Conditions of Marine Sediments via Physiological and Transcriptional Measurements	INTERNATIONAL JOURNAL OF MOLECULAR SCIENCES			English	Article						ATP content; energetic metabolism; resting cyst; Scrippsiella acuminata; tricarboxylic acid cycle; viability	HARMFUL ALGAL BLOOMS; TCA CYCLE; GONYAULAX-TAMARENSIS; CELL VIABILITY; ATP; EUTROPHICATION; GERMINATION; GLYCOLYSIS; COENZYME; CANCER	Similar to the seeds of higher plants, resting cysts, a non-motile, benthic, and dormant stage in the life history of many dinoflagellate species, play vital roles via germination in the seasonal dynamics and particularly the initiation of harmful algal blooms (HABs) of dinoflagellates. It is thus crucial for resting cysts to balance between the energetic catabolism for viability maintenance and the energy preservation for germination during their dormancy. Despite this importance, studies on how resting cysts of dinoflagellates accomplish energetic metabolism in marine sediment have been virtually absent. In this study, using the cosmopolitan HABs-causing species Scrippsiella acuminata as a representative, we measured the transcriptional activity of the most efficient pathway of the energy catabolism tricarboxylic acid (TCA) cycle, cell viability (via neutral red staining), and the cellular ATP content of resting cysts under a set of mock conditions in marine sediments (e.g., 4 degrees C, darkness, and anoxia) for a maximum period of one year. Based on the correlation analyses among the expression levels of genes, cyst viability, and ATP content, we revealed that the TCA cycle was still a crucial pathway of energetic catabolism for resting cysts under aerobic conditions, and its expression was elevated at higher temperatures, light irradiation, and the early stage of dormancy. Under anaerobic conditions, however, the TCA cycle pathway ceased expression in resting cysts, as also supported by ATP measurements. Our results have laid a cornerstone for the comprehensive revelation of the energetic metabolism and biochemical processes of dormancy of resting cysts in marine sediments.	[Li, Fengting; Yue, Caixia; Deng, Yunyan; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Li, Fengting; Deng, Yunyan; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Li, Fengting; Deng, Yunyan; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Yue, Caixia] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Deng, YY; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Deng, YY; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.; Deng, YY; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	yunyandeng@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	Yue, caixia/HHN-3747-2022	Tang, Ying-Zhong/0000-0003-0446-3128; Deng, Yunyan/0000-0001-5967-3611	Key Deployment Project of Centre for Ocean Mega - Research of Science, Chinese Academy of Sciences [COMS2019Q09]; National Science Foundation of China [42176207]; Marine Samp;T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) [2021QNLM040001]	Key Deployment Project of Centre for Ocean Mega - Research of Science, Chinese Academy of Sciences; National Science Foundation of China(National Natural Science Foundation of China (NSFC)); Marine Samp;T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao)	This research was funded by the Key Deployment Project of Centre for Ocean Mega - Research of Science, Chinese Academy of Sciences (Grant No. COMS2019Q09), the National Science Foundation of China (Grant No. 42176207), and the Marine S & T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) (Grant No. 2021QNLM040001).	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J	Persson, A; Smith, BC				Persson, Agneta; Smith, Barry C.			Preservation of Dinoflagellate Cysts in Different Oxygen Regimes: Differences in Cyst Survival between Oxic and Anoxic Natural Environments	PHYCOLOGY			English	Article						dinoflagellate; resting cyst; preservation; hypoxia; sediment	SCRIPPSIELLA-TROCHOIDEA CYSTS; THECA RELATIONSHIP; ORGANIC-MATTER; RESTING CYSTS; SP-NOV; DINOPHYCEAE PERIDINIALES; SELECTIVE PRESERVATION; AEROBIC DEGRADATION; FEEDING-BEHAVIOR; MARINE-SEDIMENTS	This quantitative dinoflagellate cyst study reveals an enormous difference in survival rates in oxygenated versus anoxic sediments. Replicate samples of concentrated natural dinoflagellate cysts with the same initial species composition (1.4 x 104 resting cysts<middle dot>cm-3 sediment, 61% filled with live-appearing contents) were placed in bags of 20 mu m plankton screen. Replicate bags containing 10.0 cm-3 concentrated cyst samples were placed on the seafloor in different environments in Long Island Sound, USA (anoxic and oxygenated), as well as refrigerated in test tubes in the laboratory. Three sets of 15 bags were placed in each environment. Once every year for four consecutive years, three bags were recovered from each set, and the contents were analyzed by cyst counting and germination experiments. An enormous difference in preservation potential between samples in oxygenated versus anoxic environments was revealed. The number of dinoflagellate cysts decreased abruptly within the first year in the oxygen-rich environment; living cysts became very rare (only 5% remained) and also empty walls of cysts disappeared (20% of total cysts remained). In anoxic sediment samples, living cysts also decreased significantly with time, but less quickly. After 1 year, 35% of the living cysts in the anoxic environment and 70% of the living cysts refrigerated in test tubes remained intact. After 4 years, 21% of the cysts with contents in the anoxic environment remained, and 31% in test tubes. The empty cyst walls remained intact for a longer time under anoxic conditions, especially of species known to fossilize well. Germination experiments showed that cysts with live-appearing contents were likely alive, because species with identifiable live-appearing cysts were also identified as vegetative cells in corresponding slurry cultures. The cyst assemblage was dominated by Protoperidinaceae, Dipolopsalidaceae, and Gonyaulacaceae. Of special interest is the ichthyotoxic Margalefodinium polykrikoides, the bloom-forming Peridinium quinquecorne, which has an undescribed resting cyst, and a previously undescribed Krypoperidinium species. The results show greater preservation of dinoflagellate cysts in "dead-zone sea bottoms" and may also provide an answer to the question of the absence of cyst beds in an area despite observed sedimentation of dense blooms.	[Persson, Agneta] Gothenburg Univ, Dept Marine Ecol, POB 461, SE-40530 Gothenburg, Sweden; [Smith, Barry C.] NOAA, Natl Marine Fisheries Serv, Northeast Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA; [Persson, Agneta] Smedjebacksvagen 13, SE-77190 Ludvika, Sweden	University of Gothenburg; National Oceanic Atmospheric Admin (NOAA) - USA	Persson, A (通讯作者)，Gothenburg Univ, Dept Marine Ecol, POB 461, SE-40530 Gothenburg, Sweden.	agnetapersson77@gmail.com			Swedish Royal Scientific Academy (KVA), CF Lundstroems Stiftelse [1390]; Ocar and Lili Lamm Foundation	Swedish Royal Scientific Academy (KVA), CF Lundstroems Stiftelse; Ocar and Lili Lamm Foundation	A.P. received travel grants from The Swedish Royal Scientific Academy (KVA), CF Lundstroems Stiftelse grant No. 1390, and grants from The Ocar and Lili Lamm Foundation.	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J	Mitra, A; Dutta, R; Halder, K				Mitra, Aniket; Dutta, Rakhi; Halder, Kalyan			A study on benthic molluscs and stable isotopes from Kutch, western India reveals early Eocene hyperthermals and pronounced transgression during ETM2 and H2 events	SWISS JOURNAL OF PALAEONTOLOGY			English	Article						Early Eocene hyperthermals; Transgression; Fossil mollusc; delta C-13; delta O-18; Carbon isotope excursion; Kutch; Western India	VASTAN LIGNITE MINE; SEA-LEVEL CHANGES; TERRESTRIAL ORGANIC-MATTER; THERMAL MAXIMUM; LATEST PALEOCENE; COASTAL-PLAIN; DEPOSITIONAL ENVIRONMENT; DINOFLAGELLATE CYSTS; MIDDLE EOCENE; KACHCHH BASIN	The early Eocene greenhouse Earth experienced several transient global warming events, indicated by sharp negative excursions in the stable isotope ratios of carbon and oxygen. A huge amount of CO2, enriched with C-12, was released in the ocean-atmosphere system leading to warming. The Paleocene-Eocene boundary is demarcated by the most significant and well-known hyperthermal event, Paleocene-Eocene thermal maximum (PETM). The PETM is documented to be accompanied by a transgression. The later hyperthermals are relatively less studied. Information on the hyperthermals from the palaeo-tropical basins are relatively few. Here, we present a high-resolution litho-, bio- and isotope-stratigraphic analysis of the early Eocene succession from the Kutch Basin, western India. Stable isotopes of carbon and oxygen were analysed from sediments (delta C-13(org)) and mollusc shells (delta C-13(carb) and delta O-18(carb)). The succession, prevailingly with lignite, along with carbonaceous black shale and plenty of fossil plant remains, is primarily a product of terrestrial environment. A pronounced marine transgression, characterised by marine mollusc bearing glauconitic shale in the middle of the succession, indicates a coastal transitional setting between the ocean and land. The delta C-13 curve of organic carbon reveals five negative excursions, which are identified as the PETM, Eocene thermal maximum 2 (ETM2)/H1, H2, I1 and I2 in ascending order. The hyperthermal pair of ETM2-H2 corresponds with the marine interval. delta C-13(carb) and delta O-18(carb) from the middle part of the succession reveal concomitant negative excursions. The association between these hyperthermals and transgression appears to be regionally and globally valid, which strongly suggests a causal link between them.	[Mitra, Aniket; Dutta, Rakhi; Halder, Kalyan] Presidency Univ, Dept Geol, 86-1 Coll St, Kolkata 700073, India	Presidency University, Kolkata	Dutta, R (通讯作者)，Presidency Univ, Dept Geol, 86-1 Coll St, Kolkata 700073, India.	rakhi.geol@gmail.com		DUTTA, RAKHI/0000-0002-4904-7550; Mitra, Aniket/0000-0002-8508-579X; Halder, Kalyan/0000-0003-1920-5535	Science and Engineering Research Board, Department of Science and Technology, India [EMR/2016/002583, PDF/2018/001909]	Science and Engineering Research Board, Department of Science and Technology, India	The authors acknowledge Presidency University, Kolkata for providing research facilities. The authors are thankful to Gujarat Mineral Development Corporation Limited (GMDC) authority for giving permission to work in the Umarsar mine and providing drill core samples. The funding provided by the Science and Engineering Research Board, Department of Science and Technology, India (SERB-DST project nos. EMR/2016/002583 and PDF/2018/001909) is acknowledged. The authors are earnestly thankful to Dr. Michael Hautmann and two anonymous reviewers for their suggestions on the manuscript.	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Palaeontol.	DEC	2022	141	1							13	10.1186/s13358-022-00255-1	http://dx.doi.org/10.1186/s13358-022-00255-1			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	3F5QT		gold			2025-03-11	WOS:000830724400001
J	Gurdebeke, PR; Mertens, KN; Rajter, L; Meyvisch, P; Potvin, E; Yang, EJ; André, C; Pospelova, V; Louwye, S				Gurdebeke, Pieter R.; Mertens, Kenneth Neil; Rajter, Lubomir; Meyvisch, Pjotr; Potvin, Eric; Yang, Eun Jin; Andre, Coralie; Pospelova, Vera; Louwye, Stephen			The ciliophoran affinity of<i> Radiosperma</i><i> textum,</i> and its relation to other marine ciliate cysts	MARINE MICROPALEONTOLOGY			English	Article						Acritarch; Affinity; Cysts; Ciliate; LSU and SSU rDNA	RESTING CYSTS; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; BALTIC SEA; ASKENASIA BLOCHMANN; BRITISH-COLUMBIA; BEAGLE CHANNEL; ACRITARCHS; DIVERSITY; PHYLOGENY	The acritarch genus Radiosperma has been reported from plankton and sediments since the late 19th century, with suggested biological affinities ranging from invertebrate eggs to tintinnids. Here, the genus description is improved and its two species, Radiosperma corbiferum and Radiosperma textum, are redescribed. Radiosperma textum is shown to be a ciliate cyst related to Askenasia based on new SSU and LSU rRNA sequences. The spatiotemporal distribution and ecology of both species are discussed. The chemical composition is documented based on micro-Fourier Transform Infrared spectroscopy. Furthermore, new SSU and LSU rRNA sequences for several flask shaped ciliate cysts (Fusopsis, Strombidium) are also included in the analysis and the occurrence of fossilizable cysts in the ciliophoran clade is reviewed.	[Gurdebeke, Pieter R.; Meyvisch, Pjotr; Andre, Coralie; Louwye, Stephen] Univ Ghent, Dept Geol, Krijgslaan 281,S8, B-9000 Ghent, Belgium; [Mertens, Kenneth Neil] IFREMER, LITTORAL, F-29900 Concarneau, France; [Rajter, Lubomir] Univ Duisburg Essen, Fac Biol, Phycol, Essen, Germany; [Potvin, Eric; Yang, Eun Jin] Korea Polar Res Inst, Div Polar Ocean Sci, Incheon 406840, Songdo, South Korea; [Potvin, Eric] Univ Concepcion, Inst Milenio Oceanog, POB 160-C, Concepcion, Chile; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA	Ghent University; Ifremer; University of Duisburg Essen; Korea Polar Research Institute (KOPRI); Universidad de Concepcion; University of Minnesota System; University of Minnesota Twin Cities	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; Meyvisch, Pjotr/ABB-1527-2021; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Pospelova, Vera/0000-0003-4049-8133; Meyvisch, Pjotr/0000-0002-1270-2152; Gurdebeke, Pieter R./0000-0003-1425-8515; Mertens, Kenneth/0000-0003-2005-9483; Louwye, Stephen/0000-0003-4814-4313	Ministry of Oceans and Fisheries, Korea [1525011760]; Regional Council of Brittany; General Council of Finistere; urban community of Concarneau-Cornouaille-Agglomeration; EPICE - Agence de l'Eau Loire-Bretagne; PhenoMap project - French National Research Agency (ANR)	Ministry of Oceans and Fisheries, Korea; Regional Council of Brittany(Region Bretagne); General Council of Finistere(Region Bretagne); urban community of Concarneau-Cornouaille-Agglomeration; EPICE - Agence de l'Eau Loire-Bretagne; PhenoMap project - French National Research Agency (ANR)(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco)	We would like to thank Nicolas Van Nieuwenhove who provided the sediment from the Labrador Sea used in this study for the genetic analyses. This research was a part of the project titled 'K-AWARE(KOPRI, 1525011760)', funded by the Ministry of Oceans and Fisheries, Korea. Astra Labuce (Latvian Institute of Aquatic Ecology) is thanked for sharing information in Radiosperma from the Gulf of Riga. 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. KNM was supported by the project EPICE, financed by Agence de l'Eau Loire-Bretagne and the PhenoMap project, financed by the French National Research Agency (ANR). We are grateful for the constructive manuscript reviews by the editor and two anonymous reviewers.	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J	Obrezkova, MS; Pospelova, V; Kolesnik, AN				Obrezkova, Maria S.; Pospelova, Vera; Kolesnik, Aleksandr N.			Diatom and dinoflagellate cyst distribution in surface sediments of the Chukchi Sea in relation to the upper water masses	MARINE MICROPALEONTOLOGY			English	Article						Diatoms; Dinocysts; Phytoplankton; Arctic Ocean; Coastal waters; Productivity; Alexandrium; Sediment	RECENT MARINE-SEDIMENTS; NORTHERN NORTH-ATLANTIC; LAPTEV SEA; HYDROGRAPHIC CONDITIONS; ORGANIC-MATTER; ARCTIC-OCEAN; SELECTIVE PRESERVATION; ESTUARINE SEDIMENTS; ABSOLUTE ABUNDANCE; BOTTOM SEDIMENTS	Diatom and dinoflagellate cyst analyses were performed on 22 surface sediment samples from the Chukchi Sea to document their geographical distributions in one of the most understudied sections of the Arctic Ocean and to examine the influence of upper water masses on these two major groups of phytoplankton. Total concentrations vary from 0.9 to 5.9 x 10(6) valves g(-1) for diatoms and from 0.8 to 12.5 x 10(3) cysts g(-1) for organic-walled dinoflagellate cysts, with the highest values for both groups observed in the southern part of the Chukchi Sea and away from the Bering Strait. Well-preserved microfossils were recovered, with a total of 35 and 88 taxa of dinoflagellate cysts and diatoms, respectively. The most abundant diatoms are Paralia sulcata, Thalassiosira antarctica, Thalassiosira nordenskioeldii, and resting spores of Chaetoceros spp., whereas cysts of phototrophic Alexandrium spp., Operculodinium centrocarpum sensu Wall and Dale (1966), and heterotrophic Islandinium minutum and Brigantedinium spp. were most common in the dinoflagellate cyst assemblages. Cysts of HAB-causing Alexandrium spp. were found in most of the samples, with the highest abundances in Herald Canyon where they contribute similar to 56.6% to the cyst assemblage. As expected, cysts produced by heterotrophic dinoflagellates were more abundant where sedimentary diatom concentrations were the highest. Statistical analysis identified three major diatom and dinoflagellate cyst clusters: 1. Sites influenced by the Alaska Coastal Current in the eastern part of the Chukchi Sea are characterized by high abundances of P. sulcata and O. centrocarpum sensu Wall and Dale (1966); 2. The western part and Herald Canyon in the northern part of the Chukchi Sea are distinguished by diatoms Chaetoceros spp., T. antarctica and dinoflagellate cysts of Alexandrium spp. and affected by the Siberian Coastal Current and Bering Shelf Water; and 3. Assemblages in the southern part of the Chukchi Sea are recognized by noticeable abundances of T. nordenskioeldii and cryophilic diatom taxa, and dinoflagellate cysts I. minutum, as well as by overall lower percentages of cysts of Pentapharsodinium dalei and Brigantedinium spp. This work revealed the potential applicability of the combined use of diatoms and dinoflagellate cysts for reconstructions of past dynamic water mass changes in the Chukchi Sea.	[Obrezkova, Maria S.; Kolesnik, Aleksandr N.] Russian Acad Sci POI FEB RAS, VI Ilichev Pacific Oceanol Inst, Far Eastern Branch, Vladivostok 690041, Russia; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA	Ilichev Pacific Oceanological Institute; University of Victoria; University of Minnesota System; University of Minnesota Twin Cities	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada.	vpospe@umn.edu	Obrezkova, Mariia/J-9869-2015	Obrezkova, Mariia/0000-0002-5884-5001; Pospelova, Vera/0000-0003-4049-8133	Russian Science Foundation [21-17-00081]; POI FEB RAS [121021700342-9]; Natural Science and Engineering Research Council of Canada (NSERC) [RGPIN/6388-2015]	Russian Science Foundation(Russian Science Foundation (RSF)); POI FEB RAS; Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors are very grateful to Prof. A.S. Astakhov and Dr. A.A. Bosin for providing sediment samples for this study. Special thanks to L. V. Osipova for processing samples and preparing diatom slides, as well as to Drs. I.B. Tsoy, N.K. Vagina, T.V. Morozova, and J. Ren for their scientific input. We thank D. Bina, the Copernicus Online Data Access team, the National Oceanographic and Atmospheric Administration (NOAA) , the National Aeronautics and Space Administration (NASA) , and the State of Alaska Open data Geoportal website for providing data on water quality parameters in the region. We are grateful to the associate editor Dr. X. Crosta and three anonymous reviewers for their detailed and constructive comments that helped to improve this manuscript. This work was funded by the Russian Science Foundation (project 21-17-00081) and research cruises through POI FEB RAS (project 121021700342-9) . Funding for this study was partially provided by the Natural Science and Engineering Research Council of Canada (NSERC) to V.P. (discovery grant RGPIN/6388-2015) .	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Micropaleontol.	JAN	2023	178								102184	10.1016/j.marmicro.2022.102184	http://dx.doi.org/10.1016/j.marmicro.2022.102184		NOV 2022	28	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	6Q7JP		Bronze			2025-03-11	WOS:000891787400001
J	Faye, S; Rochon, A; St-Onge, G; Vilanova, I; de Vernal, A; Desiage, PA				Faye, Simon; Rochon, Andre; St-Onge, Guillaume; Vilanova, Isabel; de Vernal, Anne; Desiage, Pierre-Arnaud			Southern westerly winds and paleoceanography of the San Jorge Gulf (SW-Atlantic ocean, Argentina) during the last 14,000 years	QUATERNARY SCIENCE REVIEWS			English	Article							SEA-SURFACE TEMPERATURE; LAGUNA POTROK-AIKE; DINOFLAGELLATE CYSTS; PRIMARY PRODUCTIVITY; EASTERN ATLANTIC; PATAGONIAN DUST; ATMOSPHERIC CO2; GLACIAL MAXIMUM; LEVEL CHANGES; EVOLUTION	We use pollen and dinocyst assemblages from three sedimentary sequences of the San Jorge Gulf (SJG) to document the vegetation history of the extra-Andean/eastern Patagonia (Argentina), and the latitudinal variations of the Southern Westerly Wind Belt (SWWB) in relation with ocean changes during the Late Pleistocene and Holocene. Our results suggest that prior to 14 cal ka BP, the vegetation of the SJG was dominated by halophytic taxa probably related to arid conditions in coastal environments. After 14 cal ka BP, pollen data suggest the development of shrub and herb vegetation in the Patagonian steppe then characterized by semi-arid conditions. The 14 cal ka BP transition is marked by increasing Nothofagus pollen abundances, suggesting strong westerlies at the onset of the Antarctic Cold Reversal (ACR). This transition is also marked by the occurrence of marine palynomorphs (dinocysts, organic linings of for-aminifers), which relate to sea-level rise. The dinocyst assemblages allowed us to quantitatively esti-mates changes in summer sea-surface temperature (SST) and annual net primary productivity. Between 14 and 10.8 cal ka BP, which encompasses the glacial termination and the early Holocene, dinocyst as-semblages are dominated by Operculodinium centrocarpum (-82%) and Spiniferites mirabilis (-8%) that suggest warmer conditions than at present. The transition from early to middle Holocene was marked by high SWWB intensity as suggested by pollen assemblages, and an increase of heterotrophic taxa such as Brigantedinium spp., Echinidinium sp., Dubridinium sp., and the cysts of Polykrikos kofoidii, suggesting increased primary productivity and gradual cooling of surface water. After 4 cal ka BP, pollen data suggest a decrease in the SWWB intensity that correlates with glacier advances in Patagonia and a further decrease in summer SST in the SJG.(c) 2022 Elsevier Ltd. All rights reserved.	[Faye, Simon; Rochon, Andre; St-Onge, Guillaume; de Vernal, Anne; Desiage, Pierre-Arnaud] Univ Quebec Rimouski, Inst Sci Mer Rimouski ISMER, Rimouski, PQ, Canada; [Faye, Simon; Rochon, Andre; St-Onge, Guillaume; de Vernal, Anne; Desiage, Pierre-Arnaud] Univ Quebec Montreal, Geotop Res Ctr, Montreal, PQ, Canada; [Faye, Simon; St-Onge, Guillaume; Desiage, Pierre-Arnaud] Canada Res Chair Marine Geol, Rimouski, PQ, Canada; [Vilanova, Isabel] Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat, Buenos Aires, Argentina; [Desiage, Pierre-Arnaud] Geol Survey Canada Atlantic Dartmouth, Dartmouth, NS, Canada	University of Quebec; Universite du Quebec a Rimouski; University of Quebec; University of Quebec Montreal; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN)	Faye, S (通讯作者)，Canada Res Chair Marine Geol, Rimouski, PQ, Canada.	si.faye@outlook.com	de Vernal, Anne/D-5602-2013; St-Onge, Guillaume/E-4828-2014	Desiage, Pierre-Arnaud/0000-0001-8039-8546; vilanova, isabel/0000-0002-8327-5207; Faye, Simon/0000-0002-5890-1085	FRQNT Fonds de recherche du Quebece - Nature et technologies; NSERC (Natural Sciences and Engineering Research Council of Canada); ISMER-UQAR; GEOTOP; Quebec-Ocean; Reseau Quebec maritime	FRQNT Fonds de recherche du Quebece - Nature et technologies; NSERC (Natural Sciences and Engineering Research Council of Canada)(Natural Sciences and Engineering Research Council of Canada (NSERC)); ISMER-UQAR; GEOTOP; Quebec-Ocean; Reseau Quebec maritime	This research was funded by the FRQNT (Fonds de recherche du Quebece - Nature et technologies grant to G. St-Onge and A. Rochon)and NSERC (Natural Sciences and Engineering Research Council of Canada) Discovery grants to A. Rochon and G. St-Onge. The first author received various financial support (for scholarships,congress and internship) from ISMER-UQAR, GEOTOP, Quebec-Ocean and the Reseau Quebec maritime. We thank Vera Markgraf and an anonymous reviewer for their constructive comments. We thank Raquel Guerstein for her help in the identification of Cretaceous and Miocene dinocysts. Special thanks to Sebastien Zaragosi for his help to extract environmental data. We are grateful to the captain, officers, crew and scientists of the MARGES expedition on board the R/V Coriolis II. 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J	Valdon, YB; Oboh-Ikuenobe, FE; Maigari, SA; Zobaa, MK				Valdon, Yunis B.; Oboh-Ikuenobe, Francisca E.; Maigari, Sadiq A.; Zobaa, Mohamed K.			Source-rock potential and paleoenvironment of the Coniacian Numanha Formation, northeastern Nigeria: An integrated palynofacies and geochemical approach	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynofacies; Paleoenvironment; Numanha formation; Yola arm; Cretaceous	UPPER BENUE BASIN; CRETACEOUS FORMATIONS; TROUGH; MARINE; CARBON	A study of source-rock characterization and paleoenvironmental interpretation has been carried out on a rela-tively thick Coniacian sedimentary succession from the Numanha Formation in the Guyuk area of the Yola arm in the Northern Benue Trough, northeastern Nigeria. The aim is to provide organic facies data for the assessment of its hydrocarbon generating potential owing to the high prospects of its lateral equivalent Fika Shale in the Gongola arm of the Northern Benue Trough. The investigation of 98 samples from three outcrop sections [09 degrees 50 ' N, 11 degrees 51 ' E; 09 degrees 54 ' N, 11 degrees 50 ' E; 09 degrees 54 ' N, 11 degrees 49 ' E] which includes palynofacies analysis, spore/pollen coloration, and geochemical analyses enabled an evaluation of organic matter richness and quality. Measured TOC ranges between 0.01 and 7.4% which reflects poor to good organic richness, while visual kerogen char-acterization shows thermally mature Type II-III kerogen indicative of oil and gas prone materials. Recovered palynomorphs comprised both marine (dinoflagellate cysts, microforaminiferal test linings) and terrestrial (spores, pollen, freshwater alga Pediastrum) taxa. These palynomorphs vary in proportion at different horizons of the sections indicating shoreline fluctuations. Except for the Kurnyi section, amorphous organic matter occurs in minor percentages, indicating low preservation potential during deposition. All data indicate that the Numanha Formation was deposited in a highly proximal to mud-dominated oxic shelf environment.	[Valdon, Yunis B.] Modibbo Adama Univ, Dept Geol, Yola, Nigeria; [Oboh-Ikuenobe, Francisca E.] Missouri Univ Sci Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA; [Maigari, Sadiq A.] Abubakar Tafawa Balewa Univ, Dept Appl Geol, Bauchi, Nigeria; [Zobaa, Mohamed K.] Univ Texas Permian Basin, Dept Geosci, Odessa, TX 79762 USA	University of Missouri System; Missouri University of Science & Technology; University of Texas System	Valdon, YB (通讯作者)，Modibbo Adama Univ, Dept Geol, Yola, Nigeria.	yunisvb@gmail.com	Zobaa, Mohamed/AAF-7062-2020					Abubakar M.B., 2001, J MIN GEOL, V37, P121; ADEGOKE O S, 1978, Revista Espanola de Micropaleontologia, V10, P267; Adegoke O.S., 1986, J AFRICAN EARTH SCI, V5, P249, DOI DOI 10.1016/0899-5362(86)90016-3; ALLIX P, 1981, CR ACAD SCI II, V292, P1291; Allix P., 1983, TRAV LAB SCI TERR ST, V21, P1; Amajor L.C., 1987, J MIN GEOL, V23, P109; Barber W., 1954, ANN REP GEOLOG SURV, P18; BENKHELIL J, 1987, GEOL J, V22, P467, DOI 10.1002/gj.3350220629; Benkhelil J., 1983, BCREP Elf-Aquitaine Spec. 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Afr. Earth Sci.	FEB	2023	198								104790	10.1016/j.jafrearsci.2022.104790	http://dx.doi.org/10.1016/j.jafrearsci.2022.104790		NOV 2022	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	6S8PG					2025-03-11	WOS:000893244500003
J	Hu, ZX; Song, XY; Wang, JX; Tao, Z; Sun, YY; Li, YH; Liu, YY; Deng, YY; Shang, LX; Chai, ZY; Tang, YZ				Hu, Zhangxi; Song, Xiaoying; Wang, Jinxiu; Tao, Zhe; Sun, Yuanyuan; Li, Yuhang; Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Yingzhong			Reviving and characterizing three species of dinoflagellate cysts dormant for about 70 years in the East China Sea: <i>Biecheleria brevisulcata, Biecheleriopsis adriatica</i>, and <i>Scrippsiella donghaienis</i>	JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						core sediment; dinoflagellate resting cyst; germination; Biecheleria brevisulcata; Biecheleriopsis adriatica; Scrippsiella donghaienis	SEDIMENT ARCHIVES; RESTING STAGES; SP-NOV; DINOPHYCEAE; GEN.; ULTRASTRUCTURE; PHYLOGENY; RECORD; GERMINATION; MORPHOLOGY	Many marine dinoflagellates can form resting cysts as a part of their life cycle, and the cysts could be buried in sediment and remained viable for as long as over 150 years. However, only a very limited number of cyst species have been revived from long-buried sediments and investigated in regard to a possible shift in the intra-specific genetic structure of a species detected from the historical record at a particular location. Here, we report a successful germination of three species of resting cysts that were sampled from the depth dated back to 1941 +/- 18 AD from a 44-cm sediment core from the East China Sea. Seven isolates were established from germination of single cyst isolation or multi-cyst germinations. LSU rRNA gene or ITS sequences of these strains were obtained, then they were identified to be Biecheleria brevisulcata (five strains), Biecheleriopsis adriatica (one strain), and Scrippsiella donghaienis (one strain) in terms of morphology and rRNA gene sequence. Biecheleria brevisulcata strain 1, Bps. adriatica strain 21, and S. donghaienis strain 23 were examined in detail with light microscope (LM) and scanning electron microscope (SEM), and analyzed with high performance liquid chromatography (HPLC) for their pigment compositions, and genetic diversity. We also confirmed the presence of a resting cyst of Bps. adriatica in the field for the first time. The LSU rRNA gene-based genetic distances of Bps. adriatica from that obtained from water sample, single-cell PCR sequencing for the cysts isolated from the surface sediment of the same sea area and that reported from other regions during the recent years, and ITS-based genetic distances of S. donghaienis from that obtained from cysts isolated from the surface sediment of the same location and that reported from other regions during the recent years indicated that the intra-specific genetic structure of each species in the sampling area may have shifted during the last 70 years. Our work confirms that B. brevisulcata, Bps. adriatica, and S. donghaienis, all described as new species around 2010, have inhabited the East China Sea for about 70 years. The present work reports for the first time the revival of dinoflagellate resting cysts long-buried in the coastal sediments of China, which facilitates further study on the historical occurrences of other harmful dinoflagellates and their relevance to the regional climate and environmental changes in China.	[Hu, Zhangxi] Guangdong Ocean Univ, Coll Fisheries, Zhanjiang 524088, Peoples R China; [Hu, Zhangxi; Song, Xiaoying; Wang, Jinxiu; Tao, Zhe; Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Yingzhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Yingzhong] Pilot Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Sun, Yuanyuan] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Expt Marine Biol, Qingdao 266071, Peoples R China; [Li, Yuhang] Chinese Acad Sci, Inst Oceanol, Lab Marine Organism Taxon & Phylogeny, Qingdao 266071, Peoples R China; [Hu, Zhangxi; Deng, Yunyan; Shang, Lixia; Chai, Zhaoyang; Tang, Yingzhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Song, Xiaoying; Wang, Jinxiu; Tao, Zhe] Univ Chinese Acad Sci, Beijing, Peoples R China	Guangdong Ocean University; Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	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)，Pilot 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	Chai, Zhaoyang/F-7485-2017; Li, Yuhang/J-2839-2019; ZHANG, hui jie/HTN-1690-2023; Li, Yang/KFB-5350-2024; Tao, Zhe/LIG-2380-2024		Science and Technology Basic Resources Investigation Program of China [2018FY100200]; National Natural Science Foundation of China [41976134]; Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao) [LMEES-YTSP-2018-01-04]; Program for Scientific Research Start-up Funds of Guangdong Ocean University [060302022201]	Science and Technology Basic Resources Investigation Program of China; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao); Program for Scientific Research Start-up Funds of Guangdong Ocean University	Supported by the Science and Technology Basic Resources Investigation Program of China (No. 2018FY100200), the National Natural Science Foundation of China (No. 41976134), the Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao) (No. LMEES-YTSP-2018-01-04), and the Program for Scientific Research Start-up Funds of Guangdong Ocean University (No. 060302022201)	ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Benico GA., 2019, Philippine Journal of Natural Sciences, V24, P34; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Boutrup PV, 2017, PROTIST, V168, P586, DOI 10.1016/j.protis.2017.08.001; Bravo Isabel, 2014, Microorganisms, V2, P11; Bringué M, 2016, PALAEOGEOGR PALAEOCL, V441, P787, DOI 10.1016/j.palaeo.2015.10.026; Dai XF, 2012, ESTUAR COAST SHELF S, V112, P192, DOI 10.1016/j.ecss.2012.07.016; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; de Freitas AD, 2020, RADIOCARBON, V62, P289, DOI 10.1017/RDC.2020.4; Delebecq G, 2020, J PHYCOL, V56, P1077, DOI 10.1111/jpy.13010; Ebenezer V, 2012, MAR BIOTECHNOL, V14, P129, DOI 10.1007/s10126-011-9427-y; Ellegaard M, 2013, MICROPALEAEONTOLOGIC, P149; Ellegaard M, 2020, COMMUN BIOL, V3, DOI 10.1038/s42003-020-0899-z; Ellegaard M, 2018, BIOL REV, V93, P166, DOI 10.1111/brv.12338; Ellegren H, 2016, NAT REV GENET, V17, P422, DOI 10.1038/nrg.2016.58; Erdner DL, 2011, PLOS ONE, V6, DOI 10.1371/journal.pone.0022965; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; García-Moreiras I, 2018, PALAEOGEOGR PALAEOCL, V504, P201, DOI 10.1016/j.palaeo.2018.05.032; Girault M, 2021, ISME J, V15, P2057, DOI 10.1038/s41396-021-00904-2; Gomez F., 2012, CICIMAR Oceanides, V27, P65; Gómez F, 2015, J PHYCOL, V51, P1088, DOI 10.1111/jpy.12346; Gu HF, 2008, J PHYCOL, V44, P478, DOI 10.1111/j.1529-8817.2008.00478.x; Gu HF, 2022, J PHYCOL, V58, P465, DOI 10.1111/jpy.13245; Guillard R. 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J	Zeng, YY; Sun, CH				Zeng Yong-Yao; Sun Chong-Hui			The timing of the Lhasa-Qiangtang collision revealed from the paleomagnetic age of the Qiangtang Basin, Tibetan Plateau	APPLIED GEOPHYSICS			English	Article; Early Access						Paleomagnetic ages; Biostratigraphy; Qiangtang Basin; Lhasa-Qiangtang collision	NORTHERN TIBET; DINOFLAGELLATE CYSTS; TECTONIC EVOLUTION; SHALLOW BIAS; CONSTRAINTS; GEOCHRONOLOGY; GEOCHEMISTRY; INSIGHTS; CHINA; INCLINATIONS	The timing of the Lhasa-Qiangtang collision is a major concern for the academic community. The Qiangtang Basin, located in the Tibetan Plateau, is an appropriate area to verify the Lhasa-Qiangtang collision, which was recorded by the middle-upper part of the Yanshiping Group (the Xiali and Suowa Fms) in the basin. However, the chronology of the Xiali and Suowa Fms is controversial, which limits comprehending the timing of the Lhasa-Qiangtang collision. In total, 544 paleomagnetic samples were collected from the Yanshiping section in the basin to draw the two formations' paleomagnetic ages. Paleomagnetic and rock magnetic measurements were performed, including isothermal remanent magnetization (IRM) analysis, three-component IRM thermal demagnetization, M-T analysis, thermal demagnetizations, and alternating field demagnetizations, to recognize the primary magnetic minerals and their grain sizes and concentrations. Finally, the leading magnetization carriers (magnetite and hematite) are extracted in the Xiali and Suowa Fms. The shallow bias in paleomagnetic inclinations is revised using elongation/inclination, yielding 13.7 degrees and 15.9 degrees of inclination shallowing of the Xiali and Suowa Fms, respectively. This study used 299 clear characteristic remanent magnetization directions to construct magnetostratigraphy. However, we did not give credible magnetostratigraphic ages of the two formations because of ammonite fossils, a global primary standard for the Jurassic strata correlation, without being found in the last study. Recently, Yin (2016) revised the long-term controversial paleontological age of the Suowa Fm. from a Tithonian age of the Late Jurassic or a Berriasian age of the Early Cretaceous, to a Middle Bathonian-Middle Callovian age of the Middle Jurassic based on new ammonite fossils. Considering ammonite fossils as a powerful tool and a global primary standard for the Jurassic strata correlation, we attempted to correlate the last magnetostratigraphy with the GPTS 2012 again. Magnetostratigraphic ages of 164.0-160.2 Ma and 160.2-156.8 Ma for the Xiali and Suowa Fms are suggested, respectively. The timing of the Lhasa-Qiangtang collision (156.8-154.9 Ma) is revealed from the magnetostratigraphic ages and the zircon U-Pb age of the Xueshan Fm, 154.9 (+6.8/-1.6) Ma, overlying the Suowa Fm in the Yanshiping section.	[Zeng Yong-Yao] Lanzhou Resources & Environm Voc Tech Univ, Lanzhou 730000, Peoples R China; [Sun Chong-Hui] Lanzhou Univ, Key Lab Western Chinas Mineral Resources Gansu Pr, Lanzhou 730000, Peoples R China	Lanzhou Resources & Environment Voc-Tech University; Lanzhou University	Zeng, YY (通讯作者)，Lanzhou Resources & Environm Voc Tech Univ, Lanzhou 730000, Peoples R China.	ruoshuizeng@126.com			National Basic Research Program of China [2011CB403003]	National Basic Research Program of China(National Basic Research Program of China)	This study was supported by the National Basic Research Program of China (Grant No. 2011CB403003).	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Geophys.	2022 NOV 17	2022										10.1007/s11770-022-0989-4	http://dx.doi.org/10.1007/s11770-022-0989-4		NOV 2022	20	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	6G3HC					2025-03-11	WOS:000884645600001
J	Premaor, E; Ferreira, EP; Guerstein, GR; Souza, PA; Arai, M				Premaor, Eduardo; Ferreira, Elizabete P.; Guerstein, G. Raquel; Souza, Paulo A.; Arai, Mitsuru			Cousteaudinium aubryae (Dinophyceae, Cribroperidinioideae) from the lower to middle Miocene of the Pelotas Basin, southern Brazil: Morphology, biochronostratigraphy and paleobiogeography	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Gonyaulacaleandinoflagellate cyst; Subfamily Cribroperidinioideae; Microplankton; Neogene; Pelotas Basin; Brazil	DINOFLAGELLATE CYSTS; NEOGENE SUCCESSION; NORTHERN BELGIUM; COLORADO BASIN; CARBON-CYCLE; STRATIGRAPHY; CLIMATE; WELL; PALEOENVIRONMENT; BIOSTRATIGRAPHY	In this paper, we present a detailed morphological study of Cousteaudinium aubryae (de Verteuil and Norris, 1996) from Miocene deposits of the Pelotas Basin, southern Brazil. C. aubryae is a cyst of an autotrophic dinofla-gellate with a great intraspecific morphological variability, evidenced by cavation type and degree, perforations and wall projections. Four morphotypes were identified, which are comparable with specimen records from other continents (e.g. North America and Europe). C. aubryae last occurred in the Pelotas Basin at levels chronocorrelated to the Helicosphaera ampliaperta calcareous nannofossil zone (N-570), suggesting age between Burdigalian and Langhian for the deposits of the Imbe and Cifreira formations. Integration of species records from different latitudes shows a paleobiogeographic distribution pattern predominantly in mid-latitudes, suggesting that C. aubryae was better adapted to non-tropical and no-polar climatic conditions during the early to mid Miocene.(c) 2022 Published by Elsevier B.V.	[Premaor, Eduardo; Souza, Paulo A.] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Lab Palinol Marleni Marques Toigo, Programa Pos grad Geociencias,Inst Geociencias, Ave Bento Goncalves 9500 Campus Vale, BR-91540000 Porto Alegre, Rio Grande do S, Brazil; [Ferreira, Elizabete P.] Petrobras Cenpes, Av Horacio Macedo 950 Ilha Fundao Predio 32, BR-21941915 Rio De Janeiro, RJ, Brazil; [Guerstein, G. Raquel] Univ Nacl sur, Dept Geol, Inst Geol Sur, CONICET, Ave Alem 1253 CP 8 000, Bahia Blanca, Argentina; [Arai, Mitsuru] Univ Estadual Paulista UNESP, Inst Geociencias & Ciencias Exatas, Ctr Geociencias Aplicadas ao Petr UNESPetro, Av 24 A 1515, BR-13506900 Rio Claro, SP, Brazil	Universidade Federal do Rio Grande do Sul; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade Estadual Paulista	Premaor, E (通讯作者)，Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Lab Palinol Marleni Marques Toigo, Programa Pos grad Geociencias,Inst Geociencias, Ave Bento Goncalves 9500 Campus Vale, BR-91540000 Porto Alegre, Rio Grande do S, Brazil.	eduardopremaor@gmail.com; elizabete@petrobras.com.br; raquel.guerstein@uns.edu.ar; paulo.alves.souza@ufrgs.br						Anjos G.S., 2004, Revista Brasileira de Paleontologia, V7, P127; Anjos-Zerfass G.S., 2009, THESIS U FEDERAL RIO; Anjos-Zerfass G.S., 2008, Rev. 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Palynology	JAN	2023	308								104799	10.1016/j.revpalbo.2022.104799	http://dx.doi.org/10.1016/j.revpalbo.2022.104799		NOV 2022	14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	6P1EL		Bronze			2025-03-11	WOS:000890677300004
J	Díaz, PA; Molinet, C; Seguel, M; Niklitschek, EJ; Díaz, M; Alvarez, G; Pérez-Santos, I; Varela, D; Guzmán, L; Rodríguez-Villegas, C; Figueroa, R				Diaz, Patricio A.; Molinet, Carlos; Seguel, Miriam; Niklitschek, Edwin J.; Diaz, Manuel; Alvarez, Gonzalo; Perez-Santos, Ivan; Varela, Daniel; Guzman, Leonardo; Rodriguez-Villegas, Camilo; Figueroa, Rosa, I			Modelling the Spatial and Temporal Dynamics of Paralytic Shellfish Toxins (PST) at Different Scales: Implications for Research and Management	TOXINS			English	Article						Alexandrium catenella; paralytic shellfish toxins (PST); paralytic shellfish poisoning (PSP); detoxification dynamics; spatial scales; Chilean fjords	SCALLOP PATINOPECTEN-YESSOENSIS; ALEXANDRIUM-CATENELLA; RESTING CYSTS; DINOFLAGELLATE; BLOOMS; VARIABILITY; DETOXIFICATION; ACCUMULATION; ABUNDANCE; TOXICITY	Harmful algal blooms, in particular recurrent blooms of the dinoflagellate Alexandrium catenella, associated with paralytic shellfish poisoning (PSP), frequently limit commercial shellfish harvests, resulting in serious socio-economic consequences. Although the PSP-inducing species that threaten the most vulnerable commercial species of shellfish are very patchy and spatially heterogeneous in their distribution, the spatial and temporal scales of their effects have largely been ignored in monitoring programs and by researchers. In this study, we examined the spatial and temporal dynamics of PSP toxicity in the clam (Ameghinomya antiqua) in two fishing grounds in southern Chile (Ovalada Island and Low Bay). During the summer of 2009, both were affected by an intense toxic bloom of A. catenella (up to 1.1 x 10(6) cells L-1). Generalized linear models were used to assess the potential influence of different environmental variables on the field detoxification rates of PSP toxins over a period of 12 months. This was achieved using a four parameter exponential decay model to fit and compare field detoxification rates per sampling site. The results show differences in the spatial variability and temporal dynamics of PSP toxicity, given that greater toxicities (+10-fold) and faster detoxification (20% faster) are observed at the Ovalada Island site, the less oceanic zone, and where higher amounts of clam are annually produced. Our observations support the relevance of considering different spatial and temporal scales to obtain more accurate assessments of PSP accumulation and detoxification dynamics and to improve the efficacy of fisheries management after toxic events.	[Diaz, Patricio A.; Niklitschek, Edwin J.; Perez-Santos, Ivan; Varela, Daniel; Rodriguez-Villegas, Camilo] Univ Los Lagos, Ctr i Mar, Casilla 557, Puerto Montt 5290000, Chile; [Diaz, Patricio A.; Rodriguez-Villegas, Camilo] Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt 5290000, Chile; [Molinet, Carlos; Diaz, Manuel] Univ Austral Chile, Inst Acuicultura, Programa Invest Pesquera, Puerto Montt 5489001, Chile; [Molinet, Carlos] Ctr Interdisciplinario Invest Acuicola INCAR, Programa Integrat, Concepcion 4030000, Chile; [Seguel, Miriam] Univ Austral Chile, Ctr Reg Anal Recursos & Medio Ambiente CERAM, Puerto Montt 5110566, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Dept Acuicultura, Larrondo 1281, Coquimbo 1780000, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Ctr Invest & Desarrollo Tecnol Algas CIDTA, Larrondo 1281, Coquimbo 1780000, Chile; [Perez-Santos, Ivan] Univ Concepcion, Ctr Invest Oceanograf COPAS Sur Austral & COPAS C, Concepcion 4030576, Chile; [Perez-Santos, Ivan] Ctr Invest Ecosistemas Patagonia CIEP, Coyhaique 5951369, Chile; [Guzman, Leonardo] Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Puerto Montt 5480000, Chile; [Figueroa, Rosa, I] Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain	Universidad de Los Lagos; Universidad de Los Lagos; Universidad Austral de Chile; Universidad Austral de Chile; Universidad Catolica del Norte; Universidad Catolica del Norte; Universidad de Concepcion; Instituto de Fomento Pesquero (Valparaiso); Spanish Institute of Oceanography	Díaz, PA (通讯作者)，Univ Los Lagos, Ctr i Mar, Casilla 557, Puerto Montt 5290000, Chile.; Díaz, PA (通讯作者)，Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt 5290000, Chile.	patricio.diaz@ulagos.cl	Varela, Daniel/D-9484-2013; Alvarez, Gonzalo/W-1262-2017; Díaz, Manuel/AAM-6225-2021; Figueroa, Rosa/M-7598-2015; Niklitschek, Edwin/A-7066-2008; Diaz, Patricio/B-8128-2018; Rodriguez Villegas, Camilo/AAB-8563-2022; Perez, Ivan/B-9321-2018	Guzman, Leonardo/0000-0002-9288-8320; Niklitschek, Edwin/0000-0001-5561-3494; Diaz, Patricio/0000-0002-9403-8151; Alvarez Vergara, Gonzalo/0000-0001-5812-1559; Rodriguez Villegas, Camilo/0000-0002-1429-2775; Perez, Ivan/0000-0001-5804-9761; molinet, carlos/0000-0003-3702-0526; , Ivan Perez-Santos/0000-0002-0184-1122				Aguirre C, 2012, J GEOPHYS RES-OCEANS, V117, DOI 10.1029/2011JC007379; Alexander J., 2010, EFSA J, V8, P1; Alvarez G., 2019, PERSPECTIVES PHYCOLO, V6, DOI DOI 10.1127/PIP/2019/0081; Alvarez G, 2019, TOXINS, V11, DOI 10.3390/toxins11040188; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Anderson DM, 2014, DEEP-SEA RES PT II, V103, P264, DOI 10.1016/j.dsr2.2013.09.018; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; [Anonymous], 2005, Official Methods of Analysis of AOAC International; Blanco J, 1997, MAR ECOL PROG SER, V158, P165, DOI 10.3354/meps158165; Bricelj V. 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J	Feki, N; Khannous, L; Keskes, FA; Ben Slama, A; Levacher, D				Feki, Nesma; Khannous, Lamia; Keskes, Fatma Abdmouleh; Ben Slama, Abdelwaheb; Levacher, Daniel			Mobility of trace metals and microbiological pollution from dredged sediments to the Gulf of Gabes, Tunisia	ENVIRONMENTAL MONITORING AND ASSESSMENT			English	Article						Dredged sediments; Hydrodynamic; Trace metals; Pathogenic germs; Microalgae; Eutrophication	DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; SEA; BAY; DINOPHYCEAE; ALEXANDRIUM; LAGOON; WATER; CONTAMINATION; VIABILITY	Sediments are periodically dredged from the major ports in the Gulf of Gabes (GG) during maintenance operations. These sediments are dumped near the coats of Sfax and Gabes cities. In the present study, 6 trace metals (Cd, Cu, Cr, Ni, Pb, and Zn) concentrations were assessed in both sediments and column water taken from the different basins of Sfax port. This study is the first to focus on the microbial and microalgae contaminations of Sfax port sediments. The spatial distributions of trace metals in dredged sediments from the different basins of Sfax port show that the maximum concentrations of Cd (13.75 mu g/g), Cu (892.5 mu g/g), and Zn (1447 mu g/g) exceeded the Geode standard thresholds. The same elements, also detected in the water column, exceeded the toxicity thresholds for phytoplankton, shellfish, and algae (Cd 0.095 mu g/l, Cu 4.52 mu g/l, and Zn 37 mu g/l). The presence of coliforms, indicators of sewage pollution, as pathogenic germs (Pseudomonas), was shown through microbiological examinations of the sediments and water column. The microalgae enumeration showed the abundance of dinoflagellate cysts (stressed form) which attests to the presence of severe conditions in Sfax port. Different toxic species were identified as Prorocentrum lima and Alexandrium minutum. The same trace metal sources and abundance in Sfax port and GG sediments suggest the hypothesis of their transfer from their disposal sites in coastal areas to deeper depths in the GG and until Boughrara lagoon (BL). As trace metals, microalgae species were also transferred by hydrodynamic currents inside the GG where they found suitable conditions to their proliferation causing the seawater coloration phenomenon, eutrophication, and degradation of the aquatic system.	[Feki, Nesma] Univ Sfax, Fac Sci, Adv Technol Environm & Smart City UR SSESO2, Soukra Rd,BP 1171, Sfax 3000, Tunisia; [Khannous, Lamia] Univ Sfax, Fac Sfax, Toxicol & Microbiol Hlth & Environm LR17ES06, Sfax, Tunisia; [Keskes, Fatma Abdmouleh] Univ Sfax, Fac Sci Sfax, Rd Soukra Km 3-5,BP 1171, Sfax 3000, Tunisia; [Ben Slama, Abdelwaheb] Univ Sfax, Lab Eau Energie & Environm, Ecole Natl Ingn Sfax, LR99ES35, Soukra Rd,BP 3000, Sfax, Tunisia; [Levacher, Daniel] ComUE Normandie Univ, Unicaen, UMR 6143, CNRS,Morphodynam Continentale & Cotiere M2C, 24 Rue Tilleuls, F-14000 Caen, France	Universite de Sfax; Faculty of Sciences Sfax; Universite de Sfax; Universite de Sfax; Faculty of Sciences Sfax; Universite de Sfax; Ecole Nationale dIngenieurs de Sfax (ENIS); Universite de Caen Normandie; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Feki, N (通讯作者)，Univ Sfax, Fac Sci, Adv Technol Environm & Smart City UR SSESO2, Soukra Rd,BP 1171, Sfax 3000, Tunisia.	nissma.feki@fss.usf.tn		Abdmouleh Keskes, fatma/0000-0001-8993-8182	Tunisian Ministry of Higher Education and Research	Tunisian Ministry of Higher Education and Research(Ministry of Higher Education & Scientific Research of Tunisia)	This study was supported by the Tunisian Ministry of Higher Education and Research.	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Monit. Assess.	NOV	2022	194	11							815	10.1007/s10661-022-10451-8	http://dx.doi.org/10.1007/s10661-022-10451-8			20	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	4S7DE	36131097				2025-03-11	WOS:000857596100004
J	Bosselaers, M; Munsterman, DK				Bosselaers, Mark; Munsterman, Dirk K.			The discovery of a Balaenomorpha (<i>Persufflatius renefraaijeni</i> n. gen., n. sp.) from the upper Miocene of the Netherlands sheds new light on the cranial anatomy of archaic rorqual relatives	GEODIVERSITAS			English	Article						Tortonian; Liessel; the Netherlands; early Balaenomorpha; phylogeny; rorqual lineage; pachyostosis; cranial endocast; new genus; new species	NORTH-SEA BASIN; DINOFLAGELLATE CYST; BALEEN WHALE; EARLY PLIOCENE; CETACEA; MAMMALIA; MYSTICETI; ZIPHIIDAE; BELGIUM; ODONTOCETI	A basal member of Balaenomorpha (Cetacea, Mysticeti), Persufflatius renefraaijeni, n. gen., n. sp., is described based on cranial material discovered in upper Miocene deposits of Liessel (the Netherlands). Thanks to the palynological analysis of an associated sediment sample, the specimen is dated from the late Tortonian (Dinozone SNS M14: c. 8.2-7.6 Ma). Our phylogenetic analysis recovers the new taxon at the base of the successful crown mysticete clade leading to modern rorquals. Though the holotype is only partially preserved (it consists of the partial right side of the neurocranium), it provides new data on the cranial anatomy of these early relatives of extant rorquals, which are poorly represented in the global fossil record. Several skull parts (postglenoid process of the squamosal, base of the zygomatic process of the squamosal, the anteromedioventral portion of the squamosal bone, and the exoccipital) show unusual swelling due to pachyostosis, giving the whole lateral basicranial region an inflated aspect.	[Bosselaers, Mark] OD Aarde Hist Van Leven, Koninklijk Belg Inst Nat Wetenschappen, Vautierstr 29, B-1000 Brussels, Belgium; [Bosselaers, Mark] Koninklijk Zeeuwsch Genooschap Wetenschappen, Koudsteensedijk 7, NL-4331 JE Middelburg, Netherlands; [Munsterman, Dirk K.] TNO, TNO Netherlands Org Appl Sci Res, Geol Survey Netherlands, Utrecht, Netherlands	Netherlands Organization Applied Science Research	Bosselaers, M (通讯作者)，OD Aarde Hist Van Leven, Koninklijk Belg Inst Nat Wetenschappen, Vautierstr 29, B-1000 Brussels, Belgium.; Bosselaers, M (通讯作者)，Koninklijk Zeeuwsch Genooschap Wetenschappen, Koudsteensedijk 7, NL-4331 JE Middelburg, Netherlands.	mark.bosselaers@telenet.be						Alfsen A, 2021, CR PALEVOL, V20, P807, DOI 10.5852/cr-palevol2021v20a39; Amson E, 2018, P ROY SOC B-BIOL SCI, V285, DOI 10.1098/rspb.2018.0270; Amson E, 2014, P ROY SOC B-BIOL SCI, V281, DOI 10.1098/rspb.2014.0192; [Anonymous], 2016, TOPICS PALEOBIOLOGY; Baker A.N., 1985, Handbook of Marine Mammals, V3, P345; Bisconti M, 2021, BRAIN BEHAV EVOLUT, DOI 10.1159/000519852; Bisconti M, 2021, BIOL J LINN SOC, V134, P498, DOI 10.1093/biolinnean/blab086; Bisconti M, 2021, RIV ITAL PALEONTOL S, V127, P231, DOI 10.13130/2039-4942/15745; Bisconti M, 2020, PEERJ, V8, DOI 10.7717/peerj.8315; Bisconti M, 2019, PEERJ, V7, DOI 10.7717/peerj.6915; Bisconti M, 2013, PALAEONTOLOGY, V56, P95, DOI 10.1111/j.1475-4983.2012.01168.x; Boessenecker RW, 2013, NATURWISSENSCHAFTEN, V100, P365, DOI 10.1007/s00114-013-1037-2; Bosselaers M, 2010, GEODIVERSITAS, V32, P331, DOI 10.5252/g2010n2a6; Bouetel V, 2006, GEODIVERSITAS, V28, P319; BREATHNACH AS, 1955, J ANAT, V89, P343; Clapham PJ, 2018, ENCYCLOPEDIA OF MARINE MAMMALS, 3RD EDITION, P1070; de Buffrenil V., 2000, Historical Biology, V14, P57; de Buffrenil V., 1990, Journal of Vertebrate Paleontology, V10, P455; de Buffrénil V, 2011, GEOBIOS-LYON, V44, P45, DOI 10.1016/j.geobios.2010.09.001; de Lavigerie GD, 2020, J SYST PALAEONTOL, V18, P1141, DOI 10.1080/14772019.2020.1746422; de Ricqles Armand, 2001, P289; DEBUFFRENIL V, 1995, ANN SCI NAT ZOOL, V16, P21; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Dewaele L, 2022, CURR BIOL, V32, P248, DOI 10.1016/j.cub.2021.10.065; Dewaele L, 2019, J MAMM EVOL, V26, P517, DOI 10.1007/s10914-018-9438-9; Dewaele L, 2018, ROY SOC OPEN SCI, V5, DOI 10.1098/rsos.171669; Dewaele L, 2017, PEERJ, V5, DOI 10.7717/peerj.3316; Dewaele L, 2017, PEERJ, V5, DOI 10.7717/peerj.3024; Dybkjær K, 2010, REV PALAEOBOT PALYNO, V161, P1, DOI 10.1016/j.revpalbo.2010.02.005; Ekdale EG, 2011, PLOS ONE, V6, DOI 10.1371/journal.pone.0021311; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Fettuccia DD, 2013, IHERINGIA SER ZOOL, V103, P255, DOI 10.1590/S0073-47212013000300007; Geisler JH, 2011, BMC EVOL BIOL, V11, DOI 10.1186/1471-2148-11-112; Girondot M, 2003, J VERTEBR PALEONTOL, V23, P458, DOI 10.1671/0272-4634(2003)023[0458:BPATTQ]2.0.CO;2; Gol'din P, 2014, BIOL J LINN SOC, V113, P510, DOI 10.1111/bij.12337; Houssaye A, 2015, PLOS ONE, V10, DOI 10.1371/journal.pone.0118409; Kazár E, 2014, J VERTEBR PALEONTOL, V34, P1216, DOI 10.1080/02724634.2014.857347; Kellogg R., 1968, United States National Museum Bulletin, V247, P103; Kemper CM, 2008, ENCY MARINE MAMMALS, P939; Köthe A, 2012, NEWSL STRATIGR, V45, P189, DOI 10.1127/0078-0421/2012/0021; Kompanje E.J.O., 1999, Zoologische Mededelingen (Leiden), V73, P99; Koretsky Irina A., 2008, Deinsea (Rotterdam), P53; Kuhlmann G, 2006, PALAEOGEOGR PALAEOCL, V239, P426, DOI 10.1016/j.palaeo.2006.02.004; Lambert O, 2005, GEODIVERSITAS, V27, P443; Lambert O, 2019, J VERTEBR PALEONTOL, V39, DOI 10.1080/02724634.2019.1660987; Lambert O, 2011, CR PALEVOL, V10, P453, DOI 10.1016/j.crpv.2011.03.012; Lambert O, 2010, NATURE, V466, P105, DOI 10.1038/nature09067; Lambert O, 2008, BULL INST R SC N B-S, V78, P277; Lambert Olivier, 2005, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V75, P211; Lambert Olivier, 2005, Deinsea (Rotterdam), P7; Leriche M, 1926, KONINKLIJK MUSEUM NA, V32, P369; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Louwye S, 2010, GEOL MAG, V147, P760, DOI 10.1017/S0016756810000191; Luo Z., 1999, U MICHIGAN PAPERS PA, V31, P1; Marx FG, 2019, ACTA PALAEONTOL POL, V64, P231, DOI 10.4202/app.00575.2018; Marx FG, 2019, PEERJ, V7, DOI 10.7717/peerj.6426; Marx FG, 2017, ROY SOC OPEN SCI, V4, DOI 10.1098/rsos.170560; Marx FG, 2015, ROY SOC OPEN SCI, V2, DOI 10.1098/rsos.140434; Marx FG, 2010, SCIENCE, V327, P993, DOI 10.1126/science.1185581; Marx FG, 2016, PEERJ, V4, DOI 10.7717/peerj.1572; Molino G, 2020, APPL SCI-BASEL, V10, DOI 10.3390/app10248939; MORGANE PJ, 1980, BRAIN RES BULL, V5, P1, DOI 10.1016/0361-9230(80)90272-5; Munsterman D. 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J	Tang, WJ; Geng, HX; Xi, YJ; Zhang, QC; Tang, XX; Yu, RC				Tang, Wenjiao; Geng, Huixia; Xi, Yanjuan; Zhang, Qingchun; Tang, Xuexi; Yu, Rencheng			Mapping the resting cysts of dinoflagellate <i>Alexandrium catenella</i> along the coast of Qinhuangdao, China	JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						harmful algal bloom (HAB); Alexandrium catenella; resting cyst; paralytic shellfish toxin (PST); Qinhuangdao	HARMFUL ALGAL BLOOMS; TIME PCR ASSAY; GENUS ALEXANDRIUM; YELLOW SEA; DINOPHYCEAE; GERMINATION; FUNDYENSE; TAMARENSE; BAY; ENUMERATION	Dinoflagellate Alexandrium catenella is a cosmopolitan bloom-forming species with complex life cycle, the formation and germination of resting cysts are critical for its bloom dynamics. In the coastal waters of Qinhuangdao, A. catenella has been identified as the major causative agent for paralytic shellfish poisoning, but there is little knowledge concerning its resting cysts in this region. In this study, three surveys were carried out along the coast of Qinhuangdao from 2020 to 2021 to map the distribution of A. catenella resting cysts, using a quantitative PCR (qPCR) assay specific for A. catenella. The resting cysts were detected in surface sediments during all the three surveys, and their distribution patterns were similar. High abundance of resting cysts (maximum 1 300 cysts/g sediment (wet weight)) were found in a region (119.62 degrees E-119.99 degrees E, 39.67 degrees N-39.98 degrees N) northeast to the coastal waters of Qinhuangdao, where surface sediments were mainly composed of clay and silt (percentage above 50%). Prior to the formation of the A. catenella bloom in March 2021, the abundance of A. catenella vegetative cells in seawater had extremely significant positive correlation with the abundance of resting cysts in surface sediments, reflecting the important role of resting cysts in the initiation of A. catenella blooms. As far as we know, this is the first report on the distribution of A. catenella cysts along the coast of Qinhuangdao. The results will offer a sound basis for the future monitoring and mitigation of toxic A. catenella blooms and paralytic shellfish poisoning events in this region.	[Tang, Wenjiao; Tang, Xuexi] Ocean Univ China, Coll Marine Life Sci, Qingdao 266003, Peoples R China; [Tang, Wenjiao; Geng, Huixia; Zhang, Qingchun; Yu, Rencheng] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Geng, Huixia; Zhang, Qingchun; Tang, Xuexi; Yu, Rencheng] Pilot Natl Lab Marine Sci & Technol Qingdao, Key Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Yu, Rencheng] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Geng, Huixia; Zhang, Qingchun; Yu, Rencheng] Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China; [Xi, Yanjuan] Hebei Acad Ocean & Fishery Sci, Qinhuangdao 066200, Hebei, Peoples R China	Ocean University of China; Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Chinese Academy of Sciences	Zhang, QC; Yu, RC (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Zhang, QC; Yu, RC (通讯作者)，Pilot Natl Lab Marine Sci & Technol Qingdao, Key Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.; Yu, RC (通讯作者)，Univ Chinese Acad Sci, Beijing 100049, Peoples R China.; Zhang, QC; Yu, RC (通讯作者)，Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China.	qczhang@qdio.ac.cn; rcyu@qdio.ac.cn	Geng, Hui-Xia/X-5380-2018; Yu, Rencheng/J-4450-2017					Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Anderson DM, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; Anderson DM, 2012, ANNU REV MAR SCI, V4, P143, DOI 10.1146/annurev-marine-120308-081121; [Anonymous], 2004, MAR BIOT; ASAKAWA M, 1995, TOXICON, V33, P691, DOI 10.1016/0041-0101(94)00177-A; Berdalet E, 2016, J MAR BIOL ASSOC UK, V96, P61, DOI 10.1017/S0025315415001733; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Brown AR, 2020, REV AQUACULT, V12, P1663, DOI 10.1111/raq.12403; Chen H.R., 2018, J. 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NOV	2022	40	6			SI		2312	2321		10.1007/s00343-022-2190-2	http://dx.doi.org/10.1007/s00343-022-2190-2		OCT 2022	10	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	7N1SD					2025-03-11	WOS:000870624200005
J	Gornik, SG; Flores, V; Reinhardt, F; Erber, L; Salas-Leiva, DE; Douvropoulou, O; Lassadi, I; Einarsson, E; Mörl, M; Git, A; Stadler, PF; Pain, A; Waller, RF				Gornik, Sebastian G.; Flores, Victor; Reinhardt, Franziska; Erber, Lieselotte; Salas-Leiva, Dayana E.; Douvropoulou, Olga; Lassadi, Imen; Einarsson, Elin; Moerl, Mario; Git, Anna; Stadler, Peter F.; Pain, Arnab; Waller, Ross F.			Mitochondrial Genomes in Perkinsus Decode Conserved Frameshifts in All Genes	MOLECULAR BIOLOGY AND EVOLUTION			English	Article						Myzozoa; Perkinsus; mitochondrial genome; frameshifts; programmed ribosomal frameshifting	SEQUENCE ALIGNMENT; EVOLUTION; APICOMPLEXAN; ALGORITHM; REVEAL; CODONS; ORIGIN; TREE	Mitochondrial genomes of apicomplexans, dinoflagellates, and chrompodellids that collectively make up the Myzozoa, encode only three proteins (Cytochrome b [COB], Cytochrome c oxidase subunit 1 [COX1], Cytochrome c oxidase subunit 3 [COX3]), contain fragmented ribosomal RNAs, and display extensive recombination, RNA trans-splicing, and RNA-editing. The early-diverging Perkinsozoa is the final major myzozoan lineage whose mitochondrial genomes remained poorly characterized. Previous reports of Perkinsus genes indicated independent acquisition of non-canonical features, namely the occurrence of multiple frameshifts. To determine both ancestral myzozoan and novel perkinsozoan mitochondrial genome features, we sequenced and assembled mitochondrial genomes of four Perkinsus species. These data show a simple ancestral genome with the common reduced coding capacity but disposition for rearrangement. We identified 75 frameshifts across the four species that occur as distinct types and that are highly conserved in gene location. A decoding mechanism apparently employs unused codons at the frameshift sites that advance translation either +1 or +2 frames to the next used codon. The locations of frameshifts are seemingly positioned to regulate protein folding of the nascent protein as it emerges from the ribosome. The cox3 gene is distinct in containing only one frameshift and showing strong selection against residues that are otherwise frequently encoded at the frameshift positions in cox1 and cob. All genes lack cysteine codons implying a reduction to 19 amino acids in these genomes. Furthermore, mitochondrion-encoded rRNA fragment complements are incomplete in Perkinsus spp. but some are found in the nuclear DNA suggesting import into the organelle. Perkinsus demonstrates further remarkable trajectories of organelle genome evolution including pervasive integration of frameshift translation into genome expression.	[Gornik, Sebastian G.] Heidelberg Univ, Ctr Organismal Studies, INF 230,Neuenheimer Feld 230, D-69120 Heidelberg, Germany; [Flores, Victor; Salas-Leiva, Dayana E.; Lassadi, Imen; Einarsson, Elin; Git, Anna; Waller, Ross F.] Univ Cambridge, Dept Biochem, Hopkins Bldg,Downing Site,Tennis Court Rd, Cambridge CB2 1QW, England; [Reinhardt, Franziska; Stadler, Peter F.] Univ Leipzig, Dept Comp Sci, Bioinformat Grp, Hartelstr 16-18, D-04107 Leipzig, Germany; [Reinhardt, Franziska; Stadler, Peter F.] Univ Leipzig, Interdisciplinary Ctr Bioinformat, Hartelstr 16-18, D-04107 Leipzig, Germany; [Erber, Lieselotte; Moerl, Mario] Univ Leipzig, Inst Biochem, Bruderstr 34, D-04103 Leipzig, Germany; [Douvropoulou, Olga; Pain, Arnab] King Abdullah Univ Sci & Technol KAUST, Biol & Environm Sci & Engn Div, Pathogen Genom Grp, Thuwal 239556900, Saudi Arabia; [Stadler, Peter F.] Max Planck Inst Math Sci, Discrete Biomath, D-04103 Leipzig, Germany; [Stadler, Peter F.] Univ Vienna, Inst Theoret Chem, Theoret Biochem Grp, Wahringer Str 17, A-1090 Vienna, Austria; [Stadler, Peter F.] Santa Fe Inst, 1399 Hyde Pk Rd, Santa Fe, NM 87501 USA; [Pain, Arnab] Hokkaido Univ, Int Inst Zoonosis Control, Kita Ku, 001-0020 North 20,West 10, Sapporo, Hokkaido 0010020, Japan	Ruprecht Karls University Heidelberg; University of Cambridge; Leipzig University; Leipzig University; Leipzig University; King Abdullah University of Science & Technology; Max Planck Society; University of Vienna; The Santa Fe Institute; Hokkaido University	Gornik, SG (通讯作者)，Heidelberg Univ, Ctr Organismal Studies, INF 230,Neuenheimer Feld 230, D-69120 Heidelberg, Germany.; Waller, RF (通讯作者)，Univ Cambridge, Dept Biochem, Hopkins Bldg,Downing Site,Tennis Court Rd, Cambridge CB2 1QW, England.	sebastian.gornik@googlemail.com; rfw26@cam.ac.uk	Waller, Ross/D-5761-2016; Stadler, Peter/L-7857-2015; Pain, Arnab/L-5766-2015; Flores, Victor/ABD-2096-2021	Gornik, Sebastian/0000-0002-8026-1336; Git, Anna/0000-0003-0973-9138; Douvropoulou, Olga/0000-0001-7672-5137; Morl, Mario/0000-0003-0972-9386	Gordon and Betty Moore Foundation; Australian Research Council [DP130100572]; King Abdullah University of Science and Technology (KAUST) [BAS/1/1020-01-01]; Deutsche Forschungsgemeinschaft (DFG) [MO 634/21-1, MO 634/8-2, INST 268/413-1]	Gordon and Betty Moore Foundation(Gordon and Betty Moore Foundation); Australian Research Council(Australian Research Council); King Abdullah University of Science and Technology (KAUST)(King Abdullah University of Science & Technology); Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	This work was supported by grants from the the Gordon and Betty Moore Foundation (doi:10.37807/GBMF9194), Australian Research Council (DP130100572), the King Abdullah University of Science and Technology (KAUST; BAS/1/1020-01-01) and the Deutsche Forschungsgemeinschaft (DFG; MO 634/21-1, MO 634/8-2 and INST 268/413-1).	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Biol. Evol.	OCT 7	2022	39	10							msac191	10.1093/molbev/msac191	http://dx.doi.org/10.1093/molbev/msac191			16	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	5E7TR	36108082	Green Published			2025-03-11	WOS:000865826400007
J	Brice, C; de Vernal, A; Francus, P; Forwick, M; Nam, SI				Brice, Camille; de Vernal, Anne; Francus, Pierre; Forwick, Matthias; Nam, Seung-Il			Millennial-scale oscillations and an environmental regime shift around the Middle to Late Holocene transition in the North Atlantic region based on a multiproxy record from Isfjorden, West Spitsbergen	BOREAS			English	Article							LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYSTS; THERMOHALINE CIRCULATION; SEDIMENTARY ENVIRONMENTS; CLIMATE; ICE; SVALBARD; MARINE; WATER; PALEOCEANOGRAPHY	Palynological and sedimentological analyses were performed on the sediment core HH16-1205-GC retrieved from the central Isfjorden, West Spitsbergen. The sequence, which spans the last 7000 years, revealed an overall cooling trend with an important climate shift between 4.4 and 3.8 cal. ka BP, in addition to millennial-scale oscillations. Sea-surface reconstruction from dinocyst assemblages indicates a decrease in summer sea-surface temperature, from 2.5 to 1.5 degrees C, and primary productivity, from 750 to 650 gC m(-2) a(-1) over the last 7000 years. From around 6.8 to 5.8 cal. ka BP, the sedimentological and palynological data suggest a predominant sediment supply from the inner part of the fjord, ice rafting, dense sea ice cover, strongly stratified water masses and high primary productivity. The interval from 4.4 to 3.8 cal. ka BP is marked by a layer of coarser material and a significant decrease in the grain-size mode. Our geochemical data show large-amplitude fluctuations after 2.0 cal. ka BP, while an increase in the dinocysts Impagidinium pallidum and Spiniferites elongatus from 2.0 to 1.2 cal. ka BP suggests enhanced Atlantic Water inflow. The dinocyst-based reconstructions also reveal large-amplitude millennial fluctuations in sea ice cover, summer sea-surface temperature and salinity. Wavelet analysis and cross-wavelet analysis on K/Ti ratio coupled with sea-ice estimates confirm a strong signal with a periodicity of 1200-1500 years.	[Brice, Camille; de Vernal, Anne] Univ Quebec Montreal, Montreal, PQ H3C 3P8, Canada; [Brice, Camille; de Vernal, Anne] GEOTOP, Montreal, PQ H3C 3P8, Canada; [Brice, Camille] Univ Quebec Rimouski, Inst Sci Mer, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [Brice, Camille] GEOTOP, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada; [Francus, Pierre] Ctr Eau Terre & Environm, Quebec City, PQ G1K 9A9, Canada; [Francus, Pierre] Inst Natl Rech Sci, GEOTOP, Quebec City, PQ G1K 9A9, Canada; [Forwick, Matthias] UiT Arctic Univ Norway Tromso, Dept Geosci, Postboks 6050 Langnes, N-9037 Tromso, Norway; [Nam, Seung-Il] Korea Polar Res Inst, Div Glacial Environm Res, Incheon 21990, South Korea	University of Quebec; University of Quebec Montreal; University of Quebec; Universite du Quebec a Rimouski; University of Quebec; Institut national de la recherche scientifique (INRS); UiT The Arctic University of Tromso; Korea Polar Research Institute (KOPRI)	Brice, C (通讯作者)，Univ Quebec Montreal, Montreal, PQ H3C 3P8, Canada.; Brice, C (通讯作者)，GEOTOP, Montreal, PQ H3C 3P8, Canada.; Brice, C (通讯作者)，Univ Quebec Rimouski, Inst Sci Mer, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.; Brice, C (通讯作者)，GEOTOP, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	camille.brice@hotmail.com	Francus, Pierre/H-3713-2019; de Vernal, Anne/D-5602-2013	Brice, Camille/0000-0002-7911-8161	Natural Sciences and Engineering Research Council of Canada; Fonds de recherche du Quebec-Nature et technologies; Basic Core Technology Development Program for the Oceans and the Polar Regions from the National Research Foundation of Korea (NRF) - Ministry of Science and ICT (MSIT), Republic of Korea [NRF-2021M1A5A1075512, PN22013]	Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); Fonds de recherche du Quebec-Nature et technologies(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Basic Core Technology Development Program for the Oceans and the Polar Regions from the National Research Foundation of Korea (NRF) - Ministry of Science and ICT (MSIT), Republic of Korea	This study is an ArcTrain contribution. We thank the captain and crews of RV `Helmer Hanssen', as well as S. Iversen, who supported the core and data collection during the cruise 2016, and T. Dahl, I. Hald and K. Monsen for their support during the laboratory work at the Department of Geosciences et UIT the Arctic University of Norway. We acknowledge the support provided by the Natural Sciences and Engineering Research Council of Canada through the Collaborative Research and Training Experience program andDiscoveryGranttoA. deVernalandascholarshipgrant toC. Brice. We also acknowledge complementary support from the Fonds de recherche du Qu~ebec -Nature et technologies. This research was also supported by the Basic CoreTechnologyDevelopment Program for the Oceans and the Polar Regions (NRF-2021M1A5A1075512, PN22013 to Seung-Il Nam) from the National Research Foundation of Korea (NRF) funded by the Ministry of Science and ICT (MSIT), Republic of Korea. Finally, we thank the people at Alfred Wegener Institut for radiocarbon analysis with the mini radiocarbon dating system. We thank S. de Schepper and one anonymous reviewer for their comments and recommendations that helped to improve this manuscript. The authors declare that they have no conflict of interest.	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J	Shen, PP; Li, Y; Tang, YN; Song, QS; Xue, Y				Shen, Ping-Ping; Li, Ying; Tang, Ya-Nan; Song, Qing-Shang; Xue, Yue			Sedimentary dinoflagellate cyst records of human-induced environmental changes in Daya Bay, the northern South China Sea	JOURNAL OF MARINE SYSTEMS			English	Article						Dinoflagellate cyst; Daya Bay; Sediment; Environmental changes	HARMFUL ALGAL BLOOMS; SURFACE SEDIMENTS; ORGANIC-MATTER; PHYTOPLANKTON; PRODUCTIVITY; NUTRIENT; PB-210; EUTROPHICATION; PERIDINIALES; INDICATORS	High resolution dinocyst records were established in sediment core to detect human-induced environmental changes in Daya Bay, the South China Sea. The grain was homogeneous except at depths of 17-18 cm, where the clay proportion increased dramatically from similar to 40% to similar to 80%. The Pb-210 activity varied from 25.1 Bq kg(-1) to 78.5 Bq kg(-1) and showed temporary interruption at depths 17-18 cm associated with 1978, while dinocysts showed no obvious hiatus. Totally 36 cyst species were identified, with the highest species richness (20) and cyst abundance (900 cysts g(-1)) occurring at 7-cm depth, associating with severe blooms of Scrippsiella acuminate from 1998 to 2000 in Daya Bay. Cyst assemblages showed high similarity (>70%), especially in the interrupted and upper layers, indicating similar marine-originated for these intervals. Moreover, autotrophic and heterotrophic cysts dominated alternately before and after 1978, indicating high potential of the cysts to trace human-induced environmental changes in Daya Bay.	[Shen, Ping-Ping; Song, Qing-Shang; Xue, Yue] Yantai Univ, Ocean Sch, Yantai 264005, Peoples R China; [Li, Ying] Bluepha Shenzhen Co Ltd, Shenzhen 518000, Peoples R China; [Tang, Ya-Nan] Westlake Univ, Biomed Res Core Facil, Hangzhou 310024, Peoples R China; [Shen, Ping-Ping] Yantai Univ, Ocean Sch, 30 Qingquan Rd, Yantai 264005, Peoples R China	Yantai University; Westlake University; Yantai University	Shen, PP (通讯作者)，Yantai Univ, Ocean Sch, 30 Qingquan Rd, Yantai 264005, Peoples R China.	pshen@ytu.edu.cn	Huang, xu/JDD-1638-2023; Shen, PP/S-1616-2016		National Basic Research Program of China [2015CB452903]; National Natural Science Foundation of China [41976114]; Natural Science Foundation of Guangdong Province [2017A030313216]	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)); Natural Science Foundation of Guangdong Province(National Natural Science Foundation of Guangdong Province)	This study was funded by the National Basic Research Program of China (2015CB452903), National Natural Science Foundation of China (41976114), and the Natural Science Foundation of Guangdong Province (2017A030313216). We want to thank our team members in South China Sea Institute of Oceanology, CAS, and Xiamen University for their technical support and assistance.	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Mar. Syst.	JAN	2023	237								103823	10.1016/j.jmarsys.2022.103823	http://dx.doi.org/10.1016/j.jmarsys.2022.103823		OCT 2022	8	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	5K3XE					2025-03-11	WOS:000869661700002
J	Qi, L; Wang, MH; Hu, CM; Holt, B				Qi, Lin; Wang, Menghua; Hu, Chuanmin; Holt, Benjamin			On the capacity of Sentinel-1 synthetic aperture radar in detecting floating macroalgae and other floating matters	REMOTE SENSING OF ENVIRONMENT			English	Article						Remote sensing; Sentinel-1; Sentinel-2; SAR; MSI; Macroalgae; Ulva Prolifera; Sargassum horneri; Sargassum fluitans/natans; Cyanobacteria; Microcystis; Nodularia spumigena; Trichodesmium; Floating matters; Sea snots; Brine shrimp cysts; Marine debris; Driftwood	ULVA-PROLIFERA; BLOOMS; JAPAN; SEA; SAR; CYANOBACTERIA; AVHRR; BAY	Various types of floating macroalgae and other floating matters have been reported in the global oceans and inland waters, and their remote detection has relied primarily on passive optical sensors. These sensors provide multiple spectral bands and frequent revisits, yet they all suffer from clouds. Synthetic aperture radar (SAR) imagers are active sensors that overcome this obstacle, yet their capacity in detecting macroalgae and other floating matters is generally unknown. Here, through statistical analysis and comparison of the Sentinel-2/MultiSpectral Instrument (MSI) and Sentinel-1/SAR imagery, we attempt to fill this knowledge gap. The types of floating matters considered in this study include macroalgae (Ulva Prolifera in the Yellow Sea, Sargassum horneri in the East China Sea, and Sargassum fluitans/natans in the Caribbean Sea), cyanobacteria (Microcystis, Nodularia spumigena, and Trichodesmium), dinoflagellates (green and red Noctiluca), organic matters (sea snots and brine shrimp cysts), and marine debris (driftwood). Of these, the only floating matter that can be definitively detected in Sentinel-1/SAR imagery is U. prolifera, followed by the occasional detection of S. fluitans/natans and driftwood. In all detection cases, the macroalgae features always appear in Sentinel-1/SAR imagery with positive contrast from the surrounding waters. Because of the all-weather measurements, SAR observations can therefore complement those from the optical sensors in monitoring and tracking U. prolifera and S. fluitans/natans in their respective regions.	[Qi, Lin; Wang, Menghua] NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA; [Qi, Lin] Global Sci & Technol Inc, Greenbelt, MD USA; [Hu, Chuanmin] Univ S Florida, Coll Marine Sci, St Petersburg, FL USA; [Holt, Benjamin] CALTECH, Jet Prop Lab, Pasadena, CA USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Aeronautics & Space Administration (NASA); State University System of Florida; University of South Florida; California Institute of Technology; National Aeronautics & Space Administration (NASA); NASA Jet Propulsion Laboratory (JPL)	Qi, L (通讯作者)，NOAA, Ctr Satellite Applicat & Res, College Pk, MD 20740 USA.	lin.qi@noaa.gov	hu, chuanmin/J-5021-2012; Wang, Menghua/F-5631-2010	Holt, Benjamin/0000-0003-4065-3076	NOAA; U.S. NASA [80NSSC20M0264, 80NSSC21K0422]	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); U.S. NASA(National Aeronautics & Space Administration (NASA))	This work was supported by the Joint Polar Satellite System (JPSS) funding for the NOAA ocean color calibration and validation (Cal/Val) project and by the U.S. NASA (80NSSC20M0264, 80NSSC21K0422, and NASA's Commercial SmallSat Data Acquisition (CSDA) Program). The research was carried out in part at the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration. We thank EUMETSAT and NOAA for providing all satellite data in this study, and thank Dr. Qiusheng Wu (University of Tennessee, USA) and Dr. Yongxue Liu (Nanjing University, China) for providing computer codes to download satellite data from the GEE platform. We also thank the two anonymous reviewers for providing valuable comments. The scientific results and conclusions, as well as any views or opinions expressed herein, are those of the author(s) and do not necessarily reflect those of NOAA or the Department of Commerce.	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Environ.	OCT	2022	280								113188	10.1016/j.rse.2022.113188	http://dx.doi.org/10.1016/j.rse.2022.113188			16	Environmental Sciences; Remote Sensing; Imaging Science & Photographic Technology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Remote Sensing; Imaging Science & Photographic Technology	8V6WV					2025-03-11	WOS:000930771300003
J	Pendea, IF; Chmura, GL				Pendea, I. Florin; Chmura, Gail L.			Reconstruction of wetland development across a postglacial chronosequence based on palynomorph and carbon/nitrogen modern analogues	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Hydrarch succession; Boreal wetlands; Chronosequence; Palynomorph analysis; Carbon -nitrogen ratios; James Bay	HUDSON-BAY LOWLANDS; CARBON ACCUMULATION; VEGETATION SUCCESSION; NORTHERN ONTARIO; RAISED BOG; PEAT BOG; PALEOECOLOGICAL RECONSTRUCTION; PALYNOLOGICAL RICHNESS; JAMES BAY; POLLEN	Postglacial isostatic uplift causes rapid land emergence and drives wetland development on Canada's James Bay providing a modern field laboratory to test models of wetland succession. In this study, we reconstruct wetland development in four Holocene sediment/peat records ranging in age from 6500 to 250 years based on a suite of palynomorph (pollen, spores, and dinoflagellate cysts) and carbon/nitrogen modern analogues from tidal marshes, fens, and bogs of eastern James Bay. The fossil palynomorph data was compared to the modern palynomorph signatures using Discriminant Analysis and a similarity measure (squared chord distance). Principal Components Analysis (PCA) was used to determine if gradients exist among samples from different ecosystems and which taxa are most important in defining these gradients. Palynological richness (rarefaction analysis) and evenness were used to explore the palynological diversity of various paleo-wetland types. Our results indicate that while wetland development generally progressed from nutrient-rich to nutrient-poor and/or ombrotrophic communities, the succession was reset at times and reversals occurred. Our study revealed that modern wetlands of James Bay are generally good analogues for their mid to late Holocene counterparts, although rapid glacio-isostatic uplift during the mid Holocene favored the formation of poor analogue, transitional tidal communities that were palynologically heterogenous and occasionally diverse. Inter-site comparisons suggest that a combination of autogenic processes and allogenic forcing have contributed to Holocene wetland development in eastern James Bay, the latter including factors such as changes in surface hydrology, fire, and climate.	[Pendea, I. Florin] McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 2K6, Canada; Global Environm & Climate Change Ctr GEC3, 805 Sherbrooke St West, Montreal, PQ H3A 2K6, Canada; [Pendea, I. Florin] Lakehead Univ, Dept Sustainabil Sci, 500 Univ Ave, Orillia, ON L3V0B9, Canada	Lakehead University	Pendea, IF (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St West, Montreal, PQ H3A 2K6, Canada.; Pendea, IF (通讯作者)，Lakehead Univ, Dept Sustainabil Sci, 500 Univ Ave, Orillia, ON L3V0B9, Canada.	ifpendea@lakeheadu.ca	Chmura, Gail/LNI-4648-2024		NSERC Postgraduate Fellowship; European Science Foundation EUROCORES Programme BOREAS, Project: SCENOP/2006-2009: Social Change and the Environment in Nordic Prehistory	NSERC Postgraduate Fellowship(Natural Sciences and Engineering Research Council of Canada (NSERC)); European Science Foundation EUROCORES Programme BOREAS, Project: SCENOP/2006-2009: Social Change and the Environment in Nordic Prehistory	Florin Pendea's project "Mid to late Holocene coastal landscape change in eastern James Bay" was supported by an NSERC Postgraduate Fellowship (PGS-D) 2007-2009. Fieldwork and lab work was funded by the European Science Foundation EUROCORES Programme BOREAS, Project: SCENOP/2006-2009: Social Change and the Environment in Nordic Prehistory.	[Anonymous], 2009, PASW Statistics for Windows, Version 18.0; [Anonymous], 2007, PSIMPOLL 4 26 C PROG; Beaulieu-Audy V, 2009, HOLOCENE, V19, P459, DOI 10.1177/0959683608101395; Beecher CB, 2004, CAN J BOT, V82, P663, DOI [10.1139/b04-037, 10.1139/B04-037]; BENNETT KD, 1992, J ECOL, V80, P241, DOI 10.2307/2261010; Birks HJB, 1992, HOLOCENE, V2, P1, DOI 10.1177/095968369200200101; Blaauw M, 2011, BAYESIAN ANAL, V6, P457, DOI 10.1214/ba/1339616472; Blondeau M., 2009, FLORE VASCULAIRE ENV; Bunbury J, 2012, QUATERNARY RES, V78, P275, DOI 10.1016/j.yqres.2012.05.013; Bysouth D, 2021, HOLOCENE, V31, P457, DOI 10.1177/0959683620972792; CASELDINE CJ, 1981, J BIOGEOGR, V8, P7, DOI 10.2307/2844589; Charman D., 2002, Peatlands and environmental change; Clements F.E., 1916, PLANT SUCCESSION ANA, V242; CLYMO R. 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Palaeobot. Palynology	OCT	2022	305								104730	10.1016/j.revpalbo.2022.104730	http://dx.doi.org/10.1016/j.revpalbo.2022.104730			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	8P2QB					2025-03-11	WOS:000926370700003
J	Wu, HY; Dong, CF; Zheng, GC; Zhang, ZH; Zhang, YY; Tan, ZJ; Gu, HF				Wu, Hai-Yan; Dong, Chen-Fan; Zheng, Guan-Chao; Zhang, Zhi-Hua; Zhang, Ya-Ya; Tan, Zhi-Jun; Gu, Hai-Feng			Formation mechanism and environmental drivers of Alexandrium catenella bloom events in the coastal waters of Qinhuangdao, China	ENVIRONMENTAL POLLUTION			English	Article						Alexandrium catenella; Mussel; Paralytic shellfish toxin; Biotransformation	PARALYTIC SHELLFISH TOXINS; TEMPERATURE; BAY; SAXITOXIN; SAMPLES; GROWTH; WIND	In the last 5 years, paralytic shellfish toxins (PSTs) have been recurrently detected in mollusks farmed in the mussel culture area of Qinhuangdao city, along with the occurrence of toxic outbreaks linked to dinoflagellate species of the Alexandrium genus. To understand the formation mechanism and variation of these events, continuous and comprehensive PSTs monitoring was carried out between 2017 and 2020. Through the analysis of both phytoplankton and cysts via light microscopy and quantitative polymerase chain reaction, it was shown that Alexandrium catenella was responsible for the production of PSTs, which consisted mainly of gonyautoxins 1,4 (GTX1/4, 87%) and GTX2/3 (13%). During bloom events in 2019, mussels accumulated the highest PSTs value (929 mu g STX di-HCl eq center dot kg 1) in conjunction with the peak of cell abundances, and toxin profiles were consistent with high distributions of GTX1/4, GTX2/3, and Neosaxitoxin. Toxin metabolites vary in different substances and mainly transferred to a stable proportion of a-epimer: ss-epimers 3:1. The environmental drivers of Alexandrium blooms included the continuous rise of water temperature (>4.C) and calm weather with low wind speed and no significant precipitation. By comparing toxin profiles and method sensitivity, it was found that dissolved toxins in seawater are more useful for early warning. These results have important implications for the effective monitoring and management of paralytic shellfish poisoning outbreaks.	[Wu, Hai-Yan; Dong, Chen-Fan; Zheng, Guan-Chao; Zhang, Ya-Ya; Tan, Zhi-Jun] Chinese Acad Fishery Sci, Yellow Sea Fisheries Res Inst, Minist Agr & Rural Affairs, Key Lab Testing & Evaluat Aquat Prod Safety & Qua, Qingdao 266071, Peoples R China; [Dong, Chen-Fan] Shanghai Ocean Univ, Coll Food Sci & Technol, Shanghai 201306, Peoples R China; [Zhang, Zhi-Hua] Hebei Prov Aquat Prod Qual Inspect & Testing Stn, Shijiazhuang 050011, Peoples R China; [Tan, Zhi-Jun] Pilot Natl Lab Marine Sci & Technol Qingdao, Qingdao 266071, Peoples R China; [Gu, Hai-Feng] Minist Nat Resources, Inst Oceanog 3, Xiamen 361005, Peoples R China	Chinese Academy of Fishery Sciences; Yellow Sea Fisheries Research Institute, CAFS; Ministry of Agriculture & Rural Affairs; Shanghai Ocean University; Laoshan Laboratory; Ministry of Natural Resources of the People's Republic of China; Third Institute of Oceanography, Ministry of Natural Resources	Tan, ZJ (通讯作者)，Chinese Acad Fishery Sci, Yellow Sea Fisheries Res Inst, Minist Agr & Rural Affairs, Key Lab Testing & Evaluat Aquat Prod Safety & Qua, Qingdao 266071, Peoples R China.		dong, chenfan/GZM-2060-2022; zhang, zhihua/AAW-6011-2020; Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171; dong, chenfan/0000-0001-5940-5422	National Key R&D Program of China, Beijing, China [2017YFC1600701]; National Natural Science Foundation of China, Beijign, China [31772075, 32072329]; Central Public-interest Scientific Institution Basal Research Fund, CAFS, Beijing, China [2020TD71]	National Key R&D Program of China, Beijing, China; National Natural Science Foundation of China, Beijign, China(National Natural Science Foundation of China (NSFC)); Central Public-interest Scientific Institution Basal Research Fund, CAFS, Beijing, China	This work was supported by the National Key R&D Program of China, Beijing, China (NO. 2017YFC1600701), the National Natural Science Foundation of China, Beijign, China (NO. 31772075, 32072329) and the Central Public-interest Scientific Institution Basal Research Fund, CAFS, Beijing, China (NO. 2020TD71).	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Pollut.	NOV 15	2022	313									10.1016/j.envpol.2022.120241	http://dx.doi.org/10.1016/j.envpol.2022.120241		SEP 2022	8	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	6Q1YN	36152713				2025-03-11	WOS:000891414700008
J	Salazar, OR; Arun, PN; Cui, G; Bay, LK; Van Oppen, MJH; Webster, NS; Aranda, M				Salazar, Octavio R.; Arun, Prasanna N.; Cui, Guoxin; Bay, Line K.; Van Oppen, Madeleine J. H.; Webster, Nicole S.; Aranda, Manuel			The coral <i>Acropora loripes</i> genome reveals an alternative pathway for cysteine biosynthesis in animals	SCIENCE ADVANCES			English	Article							CYSTATHIONINE BETA-SYNTHASE; PHOSPHO-L-SERINE; MYCOBACTERIUM-TUBERCULOSIS; SCHIZOSACCHAROMYCES-POMBE; CAENORHABDITIS-ELEGANS; HYDROGEN-SULFIDE; GENE ONTOLOGY; CBS DOMAINS; SEQUENCE; ANNOTATION	The metabolic capabilities of animals have been derived from well-studied model organisms and are generally considered to be well understood. In animals, cysteine is an important amino acid thought to be exclusively synthesized through the transsulfuration pathway. Corals of the genus Acropora have lost cystathionine.-synthase, a key enzyme of the transsulfuration pathway, and it was proposed that Acropora relies on the symbiosis with dinoflagellates of the family Symbiodiniaceae for the acquisition of cysteine. Here, we identify the existence of an alternative pathway for cysteine biosynthesis in animals through the analysis of the genome of the coral Acropora loripes. We demonstrate that these coral proteins are functional and synthesize cysteine in vivo, exhibiting previously unrecognized metabolic capabilities of animals. This pathway is also present in most animals but absent in mammals, arthropods, and nematodes, precisely the groups where most of the animal model organisms belong to, highlighting the risks of generalizing findings from model organisms.	[Salazar, Octavio R.; Arun, Prasanna N.; Cui, Guoxin; Aranda, Manuel] King Abdullah Univ Sci & Technol KAUST, Biol & Environm Sci & Engn Div, Marine Sci Program, Thuwal 239556900, Saudi Arabia; [Salazar, Octavio R.; Arun, Prasanna N.; Cui, Guoxin; Aranda, Manuel] King Abdullah Univ Sci & Technol, Red Sea Res Ctr, Thuwal, Saudi Arabia; [Bay, Line K.; Van Oppen, Madeleine J. H.; Webster, Nicole S.] Australian Inst Marine Sci, Townsville, Qld, Australia; [Bay, Line K.] James Cook Univ, Div Res & Innovat, AIMS JCU, Townsville, Qld, Australia; [Van Oppen, Madeleine J. H.] Univ Melbourne, Sch BioSci, Parkville, Vic 3010, Australia; [Webster, Nicole S.] Univ Queensland, Australian Ctr Ecogen, St Lucia, Qld, Australia; [Webster, Nicole S.] Australian Antarctic Div, Dept Agr Water & Environm, Kingston, Tas, Australia	King Abdullah University of Science & Technology; King Abdullah University of Science & Technology; Australian Institute of Marine Science; James Cook University; University of Melbourne; University of Queensland; Australian Antarctic Division	Salazar, OR; Aranda, M (通讯作者)，King Abdullah Univ Sci & Technol KAUST, Biol & Environm Sci & Engn Div, Marine Sci Program, Thuwal 239556900, Saudi Arabia.; Salazar, OR; Aranda, M (通讯作者)，King Abdullah Univ Sci & Technol, Red Sea Res Ctr, Thuwal, Saudi Arabia.	octavio.salazarmoya@kaust.edu.sa; manuel.aranda@kaust.edu.sa	Cui, Guoxin/Y-3028-2019; Bay, Line/D-4037-2009; van Oppen, Madeleine/C-3261-2008; Aranda Lastra, Manuel/D-9530-2011; Webster, Nicole/G-4980-2011	Cui, Guoxin/0000-0003-4951-1883; Aranda Lastra, Manuel/0000-0001-6673-016X; Salazar, Octavio R./0000-0001-6340-6524; Webster, Nicole/0000-0002-4753-5278; van Oppen, Madeleine JH/0000-0003-4607-0744; Bay, Line/0000-0002-9760-2977	AIMS; Australian Research Council [FL180100036]; KAUST; KAUST Office of Sponsored Research (OSR) [OSR-2018CPF-3627-3]	AIMS; Australian Research Council(Australian Research Council); KAUST(King Abdullah University of Science & Technology); KAUST Office of Sponsored Research (OSR)(King Abdullah University of Science & Technology)	This work was supported by the AIMS appropriation funding for the Evolution21 project, Australian Research Council Laureate Fellowship FL180100036, KAUST baseline funds, and KAUST Office of Sponsored Research (OSR) award no. 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Adv.	SEP 23	2022	8	38							eabq0304	10.1126/sciadv.abq0304	http://dx.doi.org/10.1126/sciadv.abq0304			12	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	6H2ZX	36149959	gold, Green Accepted, Green Published			2025-03-11	WOS:000885315600017
J	Smelror, M; Slagstad, T; Gautneb, H				Smelror, Morten; Slagstad, Trond; Gautneb, Havard			Palynomorphs and particulate organic matter in Late Pleistocene-Holocene deep-water sediments in the Nansen Basin (Arctic Ocean): From sources to sink	NORWEGIAN JOURNAL OF GEOLOGY			English	Article						Seabed sediments; Holocene-Pleistocene; Palynomorph; Reworking; Nansen Basin; Arctic Ocean; Particulate organic matter	DINOFLAGELLATE CYSTS; LATE QUATERNARY; BARENTS SEA; CONTINENTAL-MARGIN; SURFACE SEDIMENTS; FRESH-WATER; ZIRCON; ICE; SVALBARD; LAPTEV	Deep-sea surface clay sediments and ice-dropped clasts collected at 3998 m water depth in the Nansen Basin (88.4 degrees N-28.4 degrees E) have been examined for palynomorphs and particulate organic matter (POM). Quaternary-Holocene marine palynomorphs and dispersed organic particles are subordinate to pre-Quaternary material and the studied samples contain mostly terrigenous organic matter. Most of the palynomorphs and organic matter are reworked from strata ranging from Late Devonian to late Cenozoic in age. The Quaternary-Holocene marine assemblages contain mostly species with wide thermal tolerances, and only few Arctic to cold-water specimens. This points towards warmer water conditions than today during the time of deposition. Detrital U-Pb geochronology from one ice-dropped clast is compatible with deposition in the Devonian, with a detrital zircon age spectrum characterised by Palaeoproterozoic through Neoproterozoic ages and a youngest peak at c. 400 Ma. The possible provenance areas of most of the reworked POM and ice-dropped clasts in the Nansen Basin are far from the deep-basin sink, including areas on the Siberian Craton drained by the Lena River and other major rivers flowing into the Laptev Sea, as well as areas in the northern Barents Shelf between Svalbard and Severnaya Zemlya, where glacially eroded troughs run into the Nansen Basin.	[Smelror, Morten; Slagstad, Trond; Gautneb, Havard] Geol Survey Norway, NO-7491 Trondheim, Norway	Geological Survey of Norway	Smelror, M (通讯作者)，Geol Survey Norway, NO-7491 Trondheim, Norway.	morten.smelror@ngu.no	Gautneb, Håvard/AAP-2327-2020	Gautneb, Havard/0000-0003-1025-9342				AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; Adler RE, 2009, GLOBAL PLANET CHANGE, V68, P18, DOI 10.1016/j.gloplacha.2009.03.026; Andersen T, 2018, BASIN RES, V30, P132, DOI 10.1111/bre.12245; Backman J, 2004, QUATERNARY SCI REV, V23, P1435, DOI 10.1016/j.quascirev.2003.12.005; Blumenberg M, 2016, MAR PETROL GEOL, V76, P432, DOI 10.1016/j.marpetgeo.2016.05.031; Boucsein B, 2000, MAR GEOL, V162, P573, DOI 10.1016/S0025-3227(99)00066-3; Boucsein B, 2002, MAR GEOL, V183, P67, DOI 10.1016/S0025-3227(01)00249-3; Brozena JM, 2003, GEOLOGY, V31, P825, DOI 10.1130/G19528.1; de Vernal A, 2020, MAR MICROPALEONTOL, V159, DOI 10.1016/j.marmicro.2019.101796; Dipre G.R., 2018, ARKTOS, V4, P1, DOI [10.1007/s41063-018-0054-y, DOI 10.1007/S41063-018-0054-Y, 10.1007]; Drachev SS, 2010, PETROL GEOL CONF P, P591, DOI 10.1144/0070591; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Forman SL, 2004, QUATERNARY SCI REV, V23, P1391, DOI 10.1016/j.quascirev.2003.12.007; Galimov E.M., 2003, P MARINE SCI, V6; Gray DD, 2017, REV PALAEOBOT PALYNO, V247, P175, DOI 10.1016/j.revpalbo.2017.09.002; Grosfjeld K, 2009, NORW J GEOL, V89, P121; Gurdebeke PR, 2018, EUR J PROTISTOL, V66, P115, DOI 10.1016/j.ejop.2018.09.002; HARLAND R, 1982, Palynology, V6, P9; Harrison J. 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J. Geol.		2022	102								202208	10.17850/njg102-1-04	http://dx.doi.org/10.17850/njg102-1-04		SEP 2022	32	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	S1BK3		gold			2025-03-11	WOS:000862817800001
J	Rodríguez-Villegas, C; Figueroa, R; Pérez-Santos, I; Molinet, C; Saldías, GS; Rosales, SA; Alvarez, G; Linford, P; Díaz, PA				Rodriguez-Villegas, Camilo; Figueroa, Rosa, I; Perez-Santos, Ivan; Molinet, Carlos; Saldias, Gonzalo S.; Rosales, Sergio A.; Alvarez, Gonzalo; Linford, Pamela; Diaz, Patricio A.			Continental shelf off northern Chilean Patagonia: A potential risk zone for the onset of<i> Alexandrium</i><i> catenella</i> toxic bloom?	MARINE POLLUTION BULLETIN			English	Article						Alexandrium catenella; Paralytic shellfish toxins (PST); Cyst beds; Upwelling; Submarine canyons; Chilean Patagonia	RESTING CYSTS; VARIABILITY; SCALE; DYNAMICS; OCEAN	Harmful Algal Blooms (HAB) pose a severe socio-economic problem worldwide. The dinoflagellate species Alexandrium catenella produces potent neurotoxins called saxitoxins (STXs) and its blooms are associated with the human intoxication named Paralytic Shellfish Poisoning (PSP). Knowing where and how these blooms originate is crucial to predict blooms. Most studies in the Chilean Patagonia, were focused on coastal areas, considering that blooms from the adjacent oceanic region are almost non-existent. Using a combination of field studies and modelling approaches, we first evaluated the role of the continental shelf off northern Chilean Patagonia as a source of A. catenella resting cysts, which may act as inoculum for their toxic coastal blooms. This area is characterized by a seasonal upwelling system with positive Ekman pumping during spring-summer, and by the presence of six major submarine canyons. We found out that these submarine canyons increase the vertical advection of bottom waters, and thus, significantly enhance the process of coastal upwelling. This is a previously unreported factor, among those involved in bloom initiation. This finding put this offshore area at high risk of resuspension of resting cysts of A. catenella. Here, we discuss in detail the physical processes promoting this resuspension.	[Rodriguez-Villegas, Camilo; Linford, Pamela] Univ Los Lagos, Programa Doctorado Ciencias, Menc Conservac & Manejo Recursos Nat, Camino Chinquihue Km 6, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Perez-Santos, Ivan; Diaz, Patricio A.] Univ Los Lagos, Ctr i Mar, Casilla 557, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.] Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt, Chile; [Figueroa, Rosa, I] Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain; [Perez-Santos, Ivan; Saldias, Gonzalo S.] Univ Concepcion, Ctr Invest Oceanog COPAS COASTAL, Concepcion, Chile; [Perez-Santos, Ivan] Ctr Invest Ecosistemas Patagonia CIEP, Coyhaique, Chile; [Molinet, Carlos] Univ Austral Chile, Inst Acuicultura, Programa Invest Pesquera, Puerto Montt, Chile; [Molinet, Carlos] Ctr Interdisciplinario Invest Acuicola INCAR, Programa Integrat, Concepcion, Chile; [Saldias, Gonzalo S.] Univ Bio Bio, Fac Ciencias, Dept Fis, Concepcion, Chile; [Saldias, Gonzalo S.] Inst Milenio Socioecol Costera SECOS, Santiago, Chile; [Saldias, Gonzalo S.] Ctr Invest Dinam Ecosistemas Marinos Altas Latitu, Valdivia, Chile; [Rosales, Sergio A.] Univ Catolica Norte, Fac Ciencias Mar, Dept Biol Marina, Coquimbo, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Dept Acuicultura, Coquimbo 1281, Chile; [Alvarez, Gonzalo] Univ Catolica Norte, Fac Ciencias Mar, Ctr Invest & Desarrollo Tecnol Algas CIDTA, Coquimbo 1281, Chile	Universidad de Los Lagos; Universidad de Los Lagos; Universidad de Los Lagos; Spanish Institute of Oceanography; Universidad de Concepcion; Universidad Austral de Chile; Universidad del Bio-Bio; Universidad Catolica del Norte; Universidad Catolica del Norte; Universidad Catolica del Norte	Díaz, PA (通讯作者)，Univ Los Lagos, Ctr i Mar, Casilla 557, Puerto Montt, Chile.; Díaz, PA (通讯作者)，Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt, Chile.	patricio.diaz@ulagos.cl	Díaz, Patricio/B-8128-2018; Perez, Ivan/B-9321-2018; rosales, sergio/KEJ-0814-2024; Alvarez, Gonzalo/W-1262-2017; Saldías, Gonzalo/C-3577-2016; Rodriguez Villegas, Camilo/AAB-8563-2022; Figueroa, Rosa/M-7598-2015	/0000-0003-1798-9612; , Ivan Perez-Santos/0000-0002-0184-1122; Alvarez Vergara, Gonzalo/0000-0001-5812-1559; Rodriguez Villegas, Camilo/0000-0002-1429-2775; Figueroa, Rosa/0000-0001-9944-7993	Centre for Biotechnology and Bioengineering (CeBiB) (PIA project, ANID, Chile) [FB0001]; Universidad de Los Lagos; European Community (FEDER) [DIANAS-CTM2017-86066-R]; Innovation Agency of the Xunta de Galicia (GAIN) [GRC-VGOHAB IN607A-2019/04]; COPAS Sur-Austral [ANID AFB170006]; COPAS COASTAL [ANID FB210021]; CIEP [R20F002]; FONDECYT [1211037, 1220167]; FONDAP [15110027]; Millennium Science Initiative Program [ICN2019_015]; Spanish Ministry of Science and Innovation	Centre for Biotechnology and Bioengineering (CeBiB) (PIA project, ANID, Chile); Universidad de Los Lagos; European Community (FEDER)(European Union (EU)); Innovation Agency of the Xunta de Galicia (GAIN); COPAS Sur-Austral(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT PIA/BASAL); COPAS COASTAL; CIEP(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT Regional/CIEP); FONDECYT(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT); FONDAP; Millennium Science Initiative Program; Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government)	This research has been primarily funded by the Centre for Biotechnology and Bioengineering (CeBiB) (PIA project FB0001, ANID, Chile). Camilo Rodriguez-Villegas was funded by a Ph.D. fellowship from the Universidad de Los Lagos. Rosa I. Figueroa was funded by a national project from the Spanish Ministry of Science and Innovation and the European Community (FEDER) (Project DIANAS-CTM2017-86066-R) and a grant for Galician Networks of Excellence (GRC-VGOHAB IN607A-2019/04) from the Innovation Agency of the Xunta de Galicia (GAIN). Ivan Perez-Santos was funded by COPAS Sur-Austral (ANID AFB170006), COPAS COASTAL (ANID FB210021), CIEP R20F002, and FONDECYT 1211037. Carlos Molinet was partially financed by the FONDAP Project N.15110027 (INCAR). Gonzalo Saldias is partially funded by FONDECYT 1220167, the Millennium Science Initiative Program (Code ICN2019_015), and by COPAS COASTAL (ANID FB210021).	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Pollut. Bull.	NOV	2022	184								114103	10.1016/j.marpolbul.2022.114103	http://dx.doi.org/10.1016/j.marpolbul.2022.114103		SEP 2022	7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	5H4SF	36115195	Green Published			2025-03-11	WOS:000867669700008
J	Duncan, B; McKay, R; Levy, R; Naish, T; Prebble, JG; Sangiorgi, F; Krishnan, S; Hoem, F; Clowes, C; Jones, TD; Gasson, E; Kraus, C; Kulhanek, DK; Meyers, SR; Moossen, H; Warren, C; Willmott, ; Ventura, GT; Bendle, J				Duncan, B.; McKay, R.; Levy, R.; Naish, T.; Prebble, J. G.; Sangiorgi, F.; Krishnan, S.; Hoem, F.; Clowes, C.; Jones, T. Dunkley; Gasson, E.; Kraus, C.; Kulhanek, D. K.; Meyers, S. R.; Moossen, H.; Warren, C.; Willmott, V; Ventura, G. T.; Bendle, J.			Climatic and tectonic drivers of late Oligocene Antarctic ice volume	NATURE GEOSCIENCE			English	Article							OFFSHORE WILKES LAND; ORBITALLY-INDUCED OSCILLATIONS; ROSS SEA; SHEET VARIABILITY; DINOFLAGELLATE CYST; ATMOSPHERIC CO2; MIOCENE CLIMATE; LEVEL; RECORD; EOCENE	Cenozoic evolution of the Antarctic ice sheets is thought to be driven primarily by long-term changes in radiative forcing, but the tectonic evolution of Antarctica may also have played a substantive role. While deep-sea foraminiferal oxygen isotope records provide a combined measure of global continental ice volume and ocean temperature, they do not provide direct insights into non-radiative influences on Antarctic Ice Sheet dynamics. Here we present an Antarctic compilation of Cenozoic upper-ocean temperature for the Ross Sea and offshore Wilkes Land, generated by membrane lipid distributions from archaea. We find trends of ocean temperature, atmospheric carbon dioxide and oxygen isotopes largely co-vary. However, this relationship is less clear for the late Oligocene, when high-latitude cooling occurred despite interpretation of oxygen isotopes suggesting global warming and ice-volume loss. We propose this retreat of the West Antarctic Ice Sheet occurred in response to a tectonically driven marine transgression, with warm surface waters precluding marine-based ice-sheet growth. Marine ice-sheet expansion occurred only when ocean temperatures further cooled during the Oligocene-Miocene transition, with cold orbital conditions and low atmospheric carbon dioxide. Our results support a threshold response to atmospheric carbon dioxide, below which Antarctica's marine ice sheets grow, and above which ocean warming exacerbates their retreat. Retreat of the West Antarctic Ice Sheet during the late Oligocene was caused primarily by a tectonically driven marine transgression, according to a compilation of Ross Sea surface temperature estimates throughout the Cenozoic.	[Duncan, B.; McKay, R.; Levy, R.; Naish, T.; Kraus, C.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Levy, R.; Prebble, J. G.; Clowes, C.; Ventura, G. T.] GNS Sci, Lower Hutt, New Zealand; [Sangiorgi, F.; Hoem, F.] Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, Utrecht, Netherlands; [Krishnan, S.; Warren, C.] Yale Univ, Dept Earth & Planetary Sci, New Haven, CT USA; [Jones, T. Dunkley; Moossen, H.; Bendle, J.] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham, W Midlands, England; [Gasson, E.] Univ Exeter, Ctr Geog & Environm Sci, Exeter, Cornwall, England; [Kulhanek, D. K.] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA; [Meyers, S. R.] Univ Wisconsin, Dept Geosci, Madison, WI USA; [Willmott, V] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, Den Burg, Netherlands; [Krishnan, S.] CICERO Ctr Int Climate & Environm Res, Oslo, Norway; [Kraus, C.] Beca Ltd, Wellington, New Zealand; [Kulhanek, D. K.] Christian Albrechts Univ Kiel, Inst Geosci, Kiel, Germany; [Moossen, H.] Max Planck Inst Biogeochem, Jena, Germany; [Willmott, V] Alfred Wegener Inst, Int Cooperat Unit, Bremerhaven, Germany; [Ventura, G. T.] St Marys Univ, Dept Geol, Halifax, NS, Canada	Victoria University Wellington; GNS Science - New Zealand; Utrecht University; Yale University; University of Birmingham; University of Exeter; Texas A&M University System; Texas A&M University College Station; University of Wisconsin System; University of Wisconsin Madison; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Kiel; Max Planck Society; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Saint Marys University - Canada	Duncan, B (通讯作者)，Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand.	Bella.Duncan@vuw.ac.nz	Willmott Puig, Veronica/AGN-3478-2022; McKay, Robert/N-2449-2015; Duncan, Bella/IAR-0060-2023; Dunkley Jones, Tom/A-8441-2008	Krishnan, Srinath/0000-0002-6852-1924; Duncan, Bella/0000-0003-1108-6033; Willmott Puig, Veronica/0000-0002-6552-8901; Kraus, Christoph/0000-0002-0680-8532; Dunkley Jones, Tom/0000-0002-9518-8143; Hoem, Frida/0000-0002-8834-6799; Sangiorgi, Francesca/0000-0003-4233-6154; Meyers, Stephen/0000-0003-4422-720X	Scientific Committee of Antarctic Research Fellowship; Rutherford Foundation Postdoctoral Fellowship [RFT-VUW1804-PD]; Royal Society Te Aparangi Marsden Fund [MFP-VUW1808]; New Zealand Ministry of Business Innovation and Employment through the Antarctic Science Platform [ANTA1801, C05X1001]; Natural Environment Research Council [NE/P013112/1, Ne/I00646X/1]; US National Science Foundation [OCE-1326927]; IODP; University of Birmingham; Yale University; Antarctica New Zealand Sir Robin Irvine PhD Scholarship; NERC [NE/I00646X/1, NE/P013112/1] Funding Source: UKRI	Scientific Committee of Antarctic Research Fellowship; Rutherford Foundation Postdoctoral Fellowship(Royal Society of New Zealand); Royal Society Te Aparangi Marsden Fund(Royal Society of New Zealand); New Zealand Ministry of Business Innovation and Employment through the Antarctic Science Platform; Natural Environment Research Council(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); US National Science Foundation(National Science Foundation (NSF)); IODP; University of Birmingham; Yale University; Antarctica New Zealand Sir Robin Irvine PhD Scholarship; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The authors are grateful for access to samples from the IODP core repository at Texas A&M University for DSDP Sites 270 and 274 and to the Alfred Wegener Institute for access to samples from the Cape Roberts Project. This study was funded via an Antarctica New Zealand Sir Robin Irvine PhD Scholarship, Scientific Committee of Antarctic Research Fellowship and Rutherford Foundation Postdoctoral Fellowship (RFT-VUW1804-PD) awarded to B.D., with additional funding by the Royal Society Te Aparangi Marsden Fund award MFP-VUW1808 (B.D. and R.M.) and the New Zealand Ministry of Business Innovation and Employment through the Antarctic Science Platform (ANTA1801) and contract C05X1001 (B.D., R.M., R.L., T.N. and J.G.P.). The Natural Environment Research Council funded J.B. (standard grant Ne/I00646X/1). J.B. and T.D.J. also acknowledge support from Natural Environment Research Council grant NE/P013112/1. D.K.K. was supported by US National Science Foundation award OCE-1326927. The authors are grateful for support from IODP and support in kind from the University of Birmingham and Yale University. We thank S. Schouten (NIOZ) for laboratory support and assistance with temperature data and J. Super for assistance with sample analysis while at Yale University.	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OCT	2022	15	10					819	+		10.1038/s41561-022-01025-x	http://dx.doi.org/10.1038/s41561-022-01025-x		SEP 2022	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	5H7NV					2025-03-11	WOS:000854727400002
J	David, O; Penaud, A; Vidal, M; Fersi, W; Lambert, C; Goubert, E; Herledan, M; Stephan, P; Pailler, Y; Bourillet, JF; Baltzer, A				David, Ophelie; Penaud, Aurelie; Vidal, Muriel; Fersi, Wiem; Lambert, Clement; Goubert, Evelyne; Herledan, Maiwenn; Stephan, Pierre; Pailler, Yvan; Bourillet, Jean-Francois; Baltzer, Agnes			Sedimentological and palynological records since 10 ka BP along a proximal-distal gradient on the Armorican shelf (NW France)	QUATERNARY SCIENCE REVIEWS			English	Article						Holocene; South Brittany; Pollen; Dinoflagellate cysts; Paleoenvironmental changes; Turritella layer; Anthropogenic pollen indicators (API); Fluvial discharge	SEA-LEVEL CHANGES; NORTH-ATLANTIC OSCILLATION; DINOFLAGELLATE CYSTS; CLIMATE VARIABILITY; INCISED-VALLEY; NORTHWESTERN FRANCE; SOUTHERN BRITTANY; CONTINENTAL-SHELF; BISCAY FRANCE; PLANT TAXA	New findings acquired in Armorican shelf (core MD08-3204 CQ: Bay of Quiberon and core VK03-58bis: South Glenan islands) depict Holocene paleoenvironmental changes since 10 ka BP through a multi-proxy dataset including sedimentological and palynological data. First, grain-size analyses and AMS-C-14 dates show a common sedimentary history for both study cores. The slowdown of the relative sea level (RSL) rise was accompanied by a drop of the sedimentation rates between similar to 8.3 and 5.7 ka BP; the rates had been relatively higher at the onset of the Holocene. This interval led to the establishment of a shell-condensed level, identified in core VK03-58bis by the "Turritella layer" and interpreted as a marker for the Maximum Flooding Surface. Palynological data (pollen and dinoflagellate cyst assemblages) acquired in core MD08-3204 CQargue for an amplification of the fluvial influence since 5.7 ka BP; the establishment of the Highstand System Tract (i.e., mixed marine and fluviatile influences on the platform) then accompanied the slowdown of the RSL rise rates. On the shelf, the amplification of Anthropogenic Pollen Indicators (API) has been better detected since 4.2 ka BP, due not only to the increase of human impact but also due to a stronger fluvial influence on the shelf during the Late Holocene. Palynological data, recorded on the 8.5-8.3 ka BP interval along an inshore-offshore gradient, also demonstrate the complexity of the palynological signals such as i) the fluvial influence that promotes some pollen taxa (Alnus and Corylus) from proximal areas and ii) the macro-regionalization of palynomorph sources in distal cores. In addition, the comparison of palynological tracers, including API, over the last 7 kyrs BP, with South Brittany coastal and mid-shelf sites subject to northern vs. southern Loire catchment areas, shows a major hydro-climatic effect on the reconstructed palynological signals. Strengthened subpolar gyre (SPG) dynamics, combined with recurrent positive North Atlantic Oscillation (NAO) configurations, appear responsible for increased winter precipitation and fluvial discharge over northern Europe, as in Brittany. Conversely, weakened SPG intervals, associated with recurrent negative NAO-like modes, are characterized by intensified winter fluvial discharge over southern Europe. Interestingly, at an infra-orbital timescale, we record major peaks of API during periods of strengthened (/weakened) SPG dynamics in sites subject to detritic-organic matter inputs from Brittany (/Loire) watersheds. (C) 2022 Elsevier Ltd. All rights reserved.	[David, Ophelie; Penaud, Aurelie; Vidal, Muriel; Fersi, Wiem] Univ Brest, Geo ocean, CNRS, Ifremer,UMR 6538, F-29280 Plouzane, France; [David, Ophelie; Lambert, Clement; Goubert, Evelyne] Univ Brest, Univ Bretagne Sud, Geoocean, CNRS,Ifremer,UMR 6538, F-56000 Vannes, France; [Herledan, Maiwenn] Univ Lille, Lab Oce anol & Geosci, UMR 8187, F-59655 Villeneuve dAscq, France; [Stephan, Pierre] CNRS, Littoral Environm tect Geomatique, UMR 6554, IUEM, F-29280 Plouzane, France; [Pailler, Yvan] Univ Brest, Chaire Armerie, Inrap, Littoral Environnn Teledetect Geomat,UMR 6554,IUEM, F-29280 Plouzane, France; [Bourillet, Jean-Francois] Ifremer, Ctr Bretagne, Ressources Phys & cosystemes Fond Mer, 1625,Route Ste Anne,CS 10070, F-29280 Plouzane, France; [Baltzer, Agnes] Univ Nantes, Lab Geolittomer, IGARUN, UMR 6554, F-44300 Nantes, France	Ifremer; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ifremer; Universite de Bretagne Occidentale; Universite de Lille; 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 - Institute of Ecology & Environment (INEE); Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Ifremer; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Nantes Universite	David, O; Penaud, A (通讯作者)，Univ Brest, Geo ocean, CNRS, Ifremer,UMR 6538, F-29280 Plouzane, France.	ophelie.david@univ-ubs.fr; aurelie.penaud@univ-brest.fr; muriel.vidal@univ-brest.fr; wiem.fersi@univ-brest.fr; clement.lambert@univ-ubs.fr; evelyne.goubert@univ-ubs.fr; maiwenn.herledan.etu@univ-lille.fr; pierre.stephan@univ-brest.fr; yvan.pailler@inrap.fr; jean.francois.bourillet@ifremer.fr; agnes.baltzer@univ-nantes.fr	Bourillet, Jean-Francois/O-9761-2017; Lambert, Clément/ABF-5691-2020; Vidal, Muriel/B-7856-2014; Penaud, Aurelie/F-2485-2011	Penaud, Aurelie/0000-0003-3578-4549; Lambert, Clement/0000-0002-7746-8504; PAILLER, Yvan/0000-0002-4782-1389; David, Ophelie/0009-0009-8006-4349	CNRS-INSU project HCOG2 (2013-2014) "Forcages clima-tiques Holocene et repercussions Cotieres et Oceaniques dans le Golfe de Gascogne" as part of the LEFE-IMAGO research program; OSUNA (Observatoire des Sciences de l'Univers de Nantes Atlantique); UBO (Univ. Brest); ISblue project (Interdisciplinary graduate school for the blue planet); French government;  [ANR-17-EURE-0015]	CNRS-INSU project HCOG2 (2013-2014) "Forcages clima-tiques Holocene et repercussions Cotieres et Oceaniques dans le Golfe de Gascogne" as part of the LEFE-IMAGO research program; OSUNA (Observatoire des Sciences de l'Univers de Nantes Atlantique); UBO (Univ. Brest); ISblue project (Interdisciplinary graduate school for the blue planet); French government; 	This work was part of a PhD thesis (Ophelie David) financed by the UBS (Univ. Bretagne Sud) and UBO (Univ. Brest). We thank captains, crews, and scientific teams of the different cruises that collected both main study cores: the MD08-3204 CQ core (BISCOT campaign onboard the Marion Dufresne; MD169/MICROSYSTEMS cruise, 2008; IPEV) and the VK03-58bis core (Ifremer research project "Defi Golfe de Gascogne"; Vibarmor cruise, 2003 onboard the Cotes de la Manche). For the other cores discussed in the manu-script, we are indebted to the research projects involved in core retrieval and data acquisition (1) CBT-CS11 core (in Penaud et al., 2020): CABTEX cruise by the Ifremer onboard the R/V Pourquoi Pas? (Dussud, 2010); CNRS-INSU project HCOG2 (2013-2014) and ANR "HAMOC"; 2) VC 2012-08-PQP core (in Lambert et al., 2019): PROTEUS-DUNES cruises; Shom (2012); 3) GL3 core (in Fernane et al., 2015): ANR "COCORISCO", Brittany region project "PHILTRE"; 4) MD95-20 02 core (in Zumaque et al., 2017): IMAGES 101 expedition; Bassinot and Labeyrie (1996); ANR "HAMOC". The palynological analysis of core VK03-58bis received fundings from a CNRS-INSU project HCOG2 (2013-2014) "Forcages clima-tiques Holocene et repercussions Cotieres et Oceaniques dans le Golfe de Gascogne" (coord. A. Penaud) as part of the LEFE-IMAGO research program. We thank Muriel Georget (EPOC; Univ. Bordeaux) and Pierre-Olivier Coste (Geo-Ocean, Univ. Brest) for their palynological laboratory assistance for the VK03-58bis and MD08-3204 CQ cores, respectively. To the QUIPALPLO project (coord. A. Baltzer), financed by OSUNA (Observatoire des Sciences de l'Univers de Nantes Atlantique), made possible some palynological analyses realized during the M2 internship of M. Herledan (2019/2020). Some dates were obtained thanks to the French ARTEMIS 14C-AMS platform, and the others were acquired at the Poznan Radiocarbon Laboratory and Beta Analytics. We are also grateful to Anne Veronique Walter-Simonnet (UMR 6249 Chrono-environnement; Univ. Bour-gogne Franche-Comte) who carried out the grain size, calcimetry, and TOC analyses of core MD08-3204 CQ. The authors are grateful to the ZABrI ("Zone Atelier Brest Iroise", CNRS-INEE) and the ArM-eRIE program funded by the UBO (Univ. Brest) for fruitful inter-disciplinary exchanges about human dynamics and Holocene paleoenvironments. This work was supported by the ISblue project (Interdisciplinary graduate school for the blue planet, ANR-17-EURE-0015), co-funded by a grant from the French government under the program "Investissements d'Avenir".	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OCT 1	2022	293								107678	10.1016/j.quascirev.2022.107678	http://dx.doi.org/10.1016/j.quascirev.2022.107678		SEP 2022	22	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	4W6TF		Green Submitted, Bronze			2025-03-11	WOS:000860292000006
J	Chukwuma-Orji, JN				Chukwuma-Orji, Jacinta N.			Palynostratigraphy, biochronology and palaeobathymetry of a section of Awaizombe-1 well, eastern Niger Delta, Nigeria	EARTH AND ENVIRONMENTAL SCIENCE TRANSACTIONS OF THE ROYAL SOCIETY OF EDINBURGH			English	Article						age; palaeoenvironment; palynormorphs; palynozone		Ditch cuttings (69 samples) from a section of Awaizombe-1well located in the Northern Depobelt of the eastern Niger Delta Basin were used for this study. The lithology of the studied interval 1373-1812 m (439 m thick) consists of fissile grey shale and mudstone units. The scid method of sample preparation for palynormorphs' recovery was adopted. Analysis recorded a well-preserved and diverse assemblage of palynomorphs, rich in pollen, spores and dinoflagellate cysts (dinocysts). First and last occurrences of marker and age diagnostic species were used for palynostratigraphic interpretation. Four palynostratigraphic interval range zones were established: Psilatriporites sp.-Racemonocolpites hians Zone; early Oligocene (Rupelian age), Praedapollis africanus-Doualaidites laevigatus Zone; late Eocene (Priabonian age), middle Eocene (Lutetian and Bartonian ages), Doualaidites laevigatus-Praedapollis flexibilies Zone; and early Eocene (Ypresian age), Verrucatosporites usmensis-Retitricolpites ituensis Zone. The first downhole occurrence of D. laevigatus at the 1482 m marks the late Eocene/early Oligocene boundary. Established zones are useful for inter and intra basins correlation. Lithology and age of the studied section are suggestive of the lower Agbada Formation. Palaeoenvironmental interpretations using diagnostic species revealed two environments: brackish and inner neritic to upper bathyal (0-600 m) under relatively warm-water marine condition indicated by thermophilic dinocyst taxa, such as Lingulodinium machaerophorum, Polysphaeridium zoharyi and Homotryblium spp. The lithology and these types of environments are good sites for hydrocarbon generation.	[Chukwuma-Orji, Jacinta N.] Fed Univ Technol, Dept Geol, Minna, Nigeria		Chukwuma-Orji, JN (通讯作者)，Fed Univ Technol, Dept Geol, Minna, Nigeria.	jacinta@futminna.edu.ng	Chukwuma-Orji, Jacinta/AHH-9992-2022					Bankole S.I., 2010, THESIS TU BERLIN, P1; Chekar M, 2018, PALAEOGEOGR PALAEOCL, V507, P97, DOI 10.1016/j.palaeo.2018.07.004; Chukwuma-Orji J.N., 2021, J MINING GEOLOGY, V57, P193; Chukwuma-Orji J.N., 2017, PALEOECOLOGY AFRICA, V34, P87; Doust H., 1990, DIVERGENTPASSIVE MAR, V48, P201; EJEDAWE JE, 1981, AAPG BULL, V65, P1574; EVAMY BD, 1978, AAPG BULL, V62, P1; Legoux O., 1978, Bulletin du Center Rech. Explor-Prod. Elf-Aquitaine, V2, P265; Lemckert Francis, 2013, Proceedings of the International Academy of Ecology and Environmental Sciences, V3, P170; Murphy MA, 1999, EPISODES, V22, P255; Okosun E.A., 2014, EARTH SCI RES, V3, P72, DOI [10.5539/esr.v3n1p72, DOI 10.5539/ESR.V3N1P72]; Reijers T.J.A., 1996, NIGER DELTA BASIN SP, P100; Short K.C., 1967, American Association of Petroleum Geologists Bulletin, V51, P761; Stover L.E., 1982, P525; Stover L.E., 1996, Palynology: Principles and Applications, V2, P641	15	1	1	0	1	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	1755-6910	1755-6929		EARTH ENV SCI T R SO	Earth Environ. Sci. Trans. R. Soc. Edinb.	JUL	2023	114	1-2			SI		35	40	PII S1755691022000172	10.1017/S1755691022000172	http://dx.doi.org/10.1017/S1755691022000172		SEP 2022	6	Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	X3JK8					2025-03-11	WOS:000850367200001
J	Soliman, A; Piller, WE; Dybkjær, K; Slimani, H; Auer, G				Soliman, Ali; Piller, Werner E.; Dybkjaer, Karen; Slimani, Hamid; Auer, Gerald			Middle Miocene (Serravallian; upper Badenian-lower Sarmatian) dinoflagellate cysts from Bad Deutsch-Altenburg, Vienna Basin, Austria	PALYNOLOGY			English	Article						Austria; Baden Group; Central Paratethys; Miocene; reworking; Rabensburg Formation; Vienna Basin	LAKE PANNON; CENTRAL PARATETHYS; DEPOSITIONAL-ENVIRONMENTS; STRUCTURAL EVOLUTION; FORELAND BASIN; STRATIGRAPHY; EVENTS; SEA; BIOSTRATIGRAPHY; NORTHERN	Middle Miocene (Serravallian; upper Badenian-lower Sarmatian) strata recovered in 10 cored boreholes (83 samples) from Bad Deutsch-Altenburg, Vienna Basin, Austria, were analysed palynologically for the first time. The strata belong to the Rabensburg Formation of the Baden Group. The lateral distribution of the boreholes in reference to a Mesozoic ridge makes this area interesting for studying various aspects such as distribution of deposits, stratigraphy and palaeoenvironmental reconstruction. A diverse and well-preserved in situ dinoflagellate cyst association has been identified. Middle Miocene age-diagnostic species including Cannosphaeropsis passio, Cerebrocysta poulsenii, Habibacysta tectata, Labyrinthodinium truncatum, Operculodinium? borgerholtense and Unipontidinium aquaeductum are recorded. Their occurrences allow correlation with dinoflagellate cyst biozonations on a regional scale. Based on the identified dinoflagellate cysts and by correlation with calcareous nannoplankton and ostracods, from the same set of samples, a Serravallian age - corresponding to a late Badenian and early Sarmatian age (regional Paratethys stages) - is confirmed. Reworked (Cretaceous and Paleogene) dinoflagellate cyst assemblages, also well preserved, were recorded abundantly from boreholes HA 521 and HA 573 (south-west of the Mesozoic ridge). In accordance with ostracods, the Badenian-Sarmatian boundary can be traced in the upper part of borehole HA 66 based on an abrupt change in the dinoflagellate cyst assemblages. The upper Badenian strata were deposited in a coastal to inner shelf environment with terrigenous (siliceous sand and clay) and carbonate sediments. The recorded dinoflagellate cysts reflect marine, tropical to warm-temperate climatic conditions. The composition of the recorded dinoflagellate cyst assemblages is very close to that of the Middle Miocene assemblages of the Mediterranean, indicating water exchanges between the Central Paratethys and the Mediterranean during the late Badenian (early Serravallian).	[Soliman, Ali] Tanta Univ, Fac Sci, Geol Dept, Tanta 31527, Egypt; [Piller, Werner E.; Auer, Gerald] Karl Franzens Univ Graz, NAWI Graz Geoctr, Inst Earth Sci, Graz, Austria; [Dybkjaer, Karen] Geol Survey Denmark & Greenland GEUS, Copenhagen K, Denmark; [Slimani, Hamid] Mohammed V Univ Rabat, Geophys Nat Patrimony & Green Chem Res Ctr GEOPAC, Geobiodivers & Nat Patrimony Lab GEOBIO, Dept Geol & Remote Sensing,Sci Inst, Rabat, Morocco	Egyptian Knowledge Bank (EKB); Tanta University; University of Graz; Geological Survey Of Denmark & Greenland; Mohammed V University in Rabat	Soliman, A (通讯作者)，Tanta Univ, Fac Sci, Geol Dept, Tanta 31527, Egypt.	ali.soliman@science.tanta.edu.eg	Soliman, Ali/R-1583-2018; Auer, Gerald/AAE-5730-2021; Slimani, Hamid/AAL-4055-2020; Dybkjaer, Karen/G-5223-2018	Piller, Werner E./0000-0003-2808-4720; Soliman, Ali/0000-0001-7366-4607; Dybkjaer, Karen/0000-0002-8420-3379; Auer, Gerald/0000-0002-2574-0027; Slimani, Hamid/0000-0001-6392-1913	Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science	Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science	The laboratory work for this study was supported by the Commission for Stratigraphical and Palaeontological Research of the Austrian Academy of Science. 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J	Fernández-Herrera, LJ; Band-Schmidt, CJ; Zenteno-Savín, T; Leyva-Valencia, I; Hernández-Guerrero, CJ; Hernández-Sandoval, FE; Bustillos-Guzmán, JJ				Jose Fernandez-Herrera, Leyberth; Johanna Band-Schmidt, Christine; Zenteno-Savin, Tania; Leyva-Valencia, Ignacio; Judith Hernandez-Guerrero, Claudia; Eduardo Hernandez-Sandoval, Francisco; Jesus Bustillos-Guzman, Jose			Changes in Toxin Production, Morphology and Viability of <i>Gymnodinium catenatum</i> Associated with Allelopathy of <i>Chattonella marina</i> var. <i>marina</i> and <i>Gymnodinium impudicum</i>	TOXINS			English	Article						allelochemical; chemical ecology; paralytic shellfish toxins	GULF-OF-CALIFORNIA; HARMFUL ALGAL BLOOMS; DINOFLAGELLATE ALEXANDRIUM-OSTENFELDII; FATTY-ACID-COMPOSITION; CHEMICAL ECOLOGY; COCHLODINIUM-POLYKRIKOIDES; COMPETING PHYTOPLANKTON; SKELETONEMA-COSTATUM; KARENIA-MIKIMOTOI; MEXICAN PACIFIC	Allelopathy between phytoplankton organisms is promoted by substances released into the marine environment that limit the presence of the dominating species. We evaluated the allelopathic effects and response of cell-free media of Chattonella marina var. marina and Gymnodinium impudicum in the toxic dinoflagellate Gymnodinium catenatum. Additionally, single- and four-cell chains of G. catenatum isolated from media with allelochemicals were cultured to evaluate the effects of post exposure on growth and cell viability. Cell diagnosis showed growth limitation and an increase in cell volume, which reduced mobility and led to cell lysis. When G. catenatum was exposed to cell-free media of C. marina and G. impudicum, temporary cysts and an increased concentration of paralytic shellfish toxins were observed. After exposure to allelochemicals, the toxin profile of G. catenatum cells in the allelopathy experiments was composed of gonyautoxins 2/3 (GTX2/3), decarcarbamoyl (dcSTX, dcGTX2/3), and the sulfocarbamoyl toxins (B1 and C1/2). A difference in toxicity (pg STXeq cell(-1)) was observed between G. catenatum cells in the control and those exposed to the filtrates of C. marina var. marina and G. impudicum. Single cells of G. catenatum had a lower growth rate, whereas chain-forming cells had a higher growth rate. We suggest that a low number of G. catenatum cells can survive the allelopathic effect. We hypothesize that the survival strategy of G. catenatum is migration through the chemical cloud, encystment, and increased toxicity.	[Jose Fernandez-Herrera, Leyberth; Johanna Band-Schmidt, Christine; Leyva-Valencia, Ignacio; Judith Hernandez-Guerrero, Claudia] Inst Politecn Nacl, Ctr Interdisciplinario Ciencias Marinas IPN CICIM, Av Inst Politecn Nacl S-N, La Paz 23096, Bcs, Mexico; [Zenteno-Savin, Tania; Eduardo Hernandez-Sandoval, Francisco; Jesus Bustillos-Guzman, Jose] Inst Politecn Nacl 195, Ctr Invest Biol Noroeste CIBNOR, La Paz 23096, Bcs, Mexico; [Leyva-Valencia, Ignacio] CONACyT, IPN CICIMAR, Consejo Nacl Ciencia & Tecnol, Inst Politecn Nacl,Ctr Interdisciplinario Ciencia, La Paz 23096, Bcs, Mexico	Instituto Politecnico Nacional - Mexico; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Instituto Politecnico Nacional - Mexico	Fernández-Herrera, LJ; Band-Schmidt, CJ (通讯作者)，Inst Politecn Nacl, Ctr Interdisciplinario Ciencias Marinas IPN CICIM, Av Inst Politecn Nacl S-N, La Paz 23096, Bcs, Mexico.	lfernandezh1200@alumno.ipn.mx; cbands@ipn.mx	Hernandez-Guerrero, Claudia/AAD-9442-2020; Leyva, Ignacio/AAJ-5978-2020	HERNANDEZ SANDOVAL, FRANCISCO EDUARDO/0000-0003-2087-5835; Band-Schmidt, Christine Johanna/0000-0002-8251-9820; leyva valencia, ignacio/0000-0001-9904-1512; Zenteno-Savin, Tania/0000-0002-4080-9467	IPN, PLAYCO Programa de Planeacion Ambiental y Conservacion-CIBNOR, CIBNOR [SIP 20221652, 2021829, 10024, 20292]; Consejo Nacional de Ciencia y Tecnologia [A1-S-14968]	IPN, PLAYCO Programa de Planeacion Ambiental y Conservacion-CIBNOR, CIBNOR; Consejo Nacional de Ciencia y Tecnologia(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	This project was funded by institutional projects (SIP 20221652, 2021829 of IPN, 10024 PLAYCO Programa de Planeacion Ambiental y Conservacion-CIBNOR, 20292 CIBNOR) and by the Consejo Nacional de Ciencia y Tecnologia (Ciencia basica A1-S-14968).	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J	Slimani, H; Chekar, M				Slimani, Hamid; Chekar, Mouna			Dinoflagellate-based age control and biostratigraphic correlations of the Eocene and Oligocene (Lutetian-Chattian) sediments in the El Habt tectonic Unit, western External Rif Chain, Morocco (NW Africa)	NEWSLETTERS ON STRATIGRAPHY			English	Article						Eocene-Oligocene; Dinocysts; Biostratigraphy; Correlations; El Habt Unit; Southern Tethys	CYST BIOSTRATIGRAPHY; MIDDLE EOCENE; RESEARCH BOREHOLE; FORELAND BASIN; SEA; STRATIGRAPHY; TRANSITION; SECTION; BOUNDARY; MAGNETOSTRATIGRAPHY	This study aims to refine the age of sediments from the region of Ksar El-Kebir in the El Habt tectonic Unit, northwestern Morocco (southwestern Tethys) and establish biostratigraphic correlations between the sections studied, and also with other sections in the northerrn latitudes, particularly from the Mediterranean region and northwestern Europe, based on dinoflagellate cysts (dinocysts). The study is carried out on predominantly marly successions of the Ennayemiyene I, Ennayemiyene II and Bourkha sections, which were assigned previously to the Upper Cretaceous-Eocene interval in the geological map of the Rif Chain (1/500,000), based on lithostratigraphic correlations with other previously dated sections in the western External Rif. The palynological investigations of these three Tethyan sections revealed the presence of well-preserved and dinocyst-rich palynomorph assemblages. These investigations allowed for the recognition of the Bartonian-Priabonian interval (Eocene) in the Ennayemiyene I section, the Rupelian-Chattian interval (Oligocene) in the Ennayemiyene II section and the Priabonian-Rupelian interval (upper Eocene-lower Oligocene) in the Bourkha section. Biostratigraphic correlations have been established between these sections and also with the sections of Tattofte and Ibn Batouta, also located in the western External Rif, based on dinocysts. Correlations were also possible with biostratigraphically well-calibrated sections, mainly from the North Sea Basin and from other Tethyan regions, including the Priabonian stratotype, the Global Stratotype Section and Point (GSSP) for the base of Rupelian and the GSSP for the base of Chattian in Italy. Furthermore, we recognized dinocyst zones and subzones, previously defined in the Bartonian-Chattian interval of these sections, such as the Wetzeliella simplex (Bartonian), Schematophora speciosa Zone (Priabonian), Reticulato-sphaera actinocoronata, Hystrichokolpoma pusillum and Corrudinium incompositum zones (Rupelian), and Distatodinium biffii Zone (Chattian) with its Svalbardella cooksoniae and Caligodinium pychnum subzones.	[Slimani, Hamid; Chekar, Mouna] Mohammed V Univ Rabat, Sci Inst, Nat Patrimony & Green Chem Res Ctr GEOPAC, Dept Geol & Remote Sensing, Ave Ibn Batouta,POB 703, Rabat 10106, Morocco	Mohammed V University in Rabat	Slimani, H (通讯作者)，Mohammed V Univ Rabat, Sci Inst, Nat Patrimony & Green Chem Res Ctr GEOPAC, Dept Geol & Remote Sensing, Ave Ibn Batouta,POB 703, Rabat 10106, Morocco.	h_slimani@yahoo.com; hamid.slimani@is.um5.ac.ma	Slimani, Hamid/AAL-4055-2020					American Association of Stratigraphic Palynologists, CONTRIBUTION SERIES, V17, P105; [Anonymous], 1988, Geol. 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J	Cramwinckel, MJ; van der Ploeg, R; van Helmond, NAGM; Waarlo, N; Agnini, C; Bijl, PK; van der Boon, A; Brinkhuis, H; Frieling, J; Krijgsman, W; Mather, TA; Middelburg, JJ; Peterse, F; Slomp, CP; Sluijs, A				Cramwinckel, Margot J.; van der Ploeg, Robin; van Helmond, Niels A. G. M.; Waarlo, Niels; Agnini, Claudia; Bijl, Peter K.; van der Boon, Annique; Brinkhuis, Henk; Frieling, Joost; Krijgsman, Wout; Mather, Tamsin A.; Middelburg, Jack J.; Peterse, Francien; Slomp, Caroline P.; Sluijs, Appy			Deoxygenation and organic carbon sequestration in the Tethyan realm associated with the middle Eocene climatic optimum	GEOLOGICAL SOCIETY OF AMERICA BULLETIN			English	Article							GLYCEROL ETHER LIPIDS; BIOMARKER PALEOTHERMOMETRY; DINOFLAGELLATE CYSTS; ATMOSPHERIC MERCURY; TETRAETHER LIPIDS; SOUTHWEST PACIFIC; THERMAL MAXIMUM; BACTERIAL GMGTS; NORTH CAUCASUS; WATER-COLUMN	The middle Eocene climatic optimum (ca. 40 Ma) stands out as a transient global warming phase of -400 k.y. duration that interrupted long-term Eocene cooling; it has been associated with a rise in atmospheric CO2 concentrations that has been linked to a flare-up in Arabia-Eurasia continental arc volcanism. Increased organic carbon burial in the Tethys Ocean has been proposed as a carbon sequestration mechanism to bring the middle Eocene climatic optimum to an end. To further test these hypotheses, we assessed the sedimentary and geochemical expres-sion of the middle Eocene climatic optimum in the northern Peri-Tethys, specifically, the organic-rich Kuma Formation of the Be-laya River section, located on the edge of the Scythian Platform in the North Caucasus, Russia. We constructed an age-depth model using nannofossil chronobiostratigraphy. Throughout the studied middle Eocene inter-val (41.2-39.9 Ma), we documented sea -sur-face temperatures of 32-36 degrees C based on the tetraether index of tetraethers consisting of 86 carbons (TEX86), depending on proxy cali-bration, and during the early middle Eocene climatic optimum, we observed sea-surface warming of 2-3 degrees C. Despite the proximity of the section to the Arabia-Eurasia volcanic arc, the hypothesized source of volcanic CO2, we found no evidence for enhanced regional volcanism in sedimentary mercury concen-trations. Sedimentary trace-element concen- trations and iron speciation indicate reduc-ing bottom waters throughout the middle Eocene, but the most reducing, even euxinic, conditions were reached during late middle Eocene climatic optimum cooling. This ap-parent regional decoupling between ocean warming and deoxygenation hints at a role for regional tectonics in causing basin restric-tion and anoxia. Associated excess organic carbon burial, extrapolated to the entire re-gional Kuma Formation, may have been -8.1 Tg C yr-1, comprising -450 Pg C over this -55 k.y. interval. Combined with evidence for enhanced organic carbon drawdown in the western Peri-Tethys, this supports a quanti-tatively significant role for the basin in the termination of the middle Eocene climatic optimum by acting as a large organic carbon sink, and these results collectively illustrate that the closing Tethys Ocean might have af-fected global Paleogene climate. Moreover, this study highlights the importance of the in-terplay between global climate and regional oceanic gateway evolution in determining lo-cal climate and oceanographic change.	[Cramwinckel, Margot J.; van der Ploeg, Robin; van Helmond, Niels A. G. M.; Waarlo, Niels; Bijl, Peter K.; van der Boon, Annique; Brinkhuis, Henk; Frieling, Joost; Krijgsman, Wout; Middelburg, Jack J.; Peterse, Francien; Slomp, Caroline P.; Sluijs, Appy] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands; [Agnini, Claudia] Univ Padua, Dept Geosci, I-35131 Padua, Italy; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, NL-1790 Den Burg, Netherlands; [Frieling, Joost; Mather, Tamsin A.] Univ Oxford, Dept Earth Sci, Oxford OX1 3AN, England; [van der Boon, Annique] Univ Oslo, Ctr Earth Evolut & Dynam CEED, N-0315 Oslo, Norway	Utrecht University; University of Padua; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Oxford; University of Oslo	Cramwinckel, MJ (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands.	m.j.cramwinckel@uu.nl; r.vanderploeg@uu.nl	Sluijs, Appy/B-3726-2009; Peterse, Francien/AAY-1473-2021; Agnini, Claudia/AAB-9971-2020; Mather, Tamsin/A-7604-2011; Slomp, Caroline/A-9406-2012; Middelburg, Jack/B-4951-2011; Peterse, Francien/H-5627-2011	Peterse, Francien/0000-0001-8781-2826; van der Boon, Annique/0000-0003-0781-371X; van der Ploeg, Robin/0000-0001-5096-7496	Netherlands Earth System Science Centre (NESSC); Dutch Ministry of Education, Culture and Science; European Research Council (ERC) [ERC-2018-COG-818717-V-ECHO, 771497]; Dutch Research Council (NWO) Vici [865.13.005]; Ammodo Foundation; European Research Council (ERC) [771497] Funding Source: European Research Council (ERC)	Netherlands Earth System Science Centre (NESSC); Dutch Ministry of Education, Culture and Science; European Research Council (ERC)(European Research Council (ERC)); Dutch Research Council (NWO) Vici; Ammodo Foundation(ACEV Foundation); European Research Council (ERC)	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. We thank Sergey Popov and Larisa Golovina (Russian Academy of Sciences) , Michael Morton and Sarah Davies (University of Leicester) , Arjen Grothe and Kevin Vis (Utrecht University) , and Stephen Vincent (Cambridge Arctic Shelf Programme, CASP, University of Cambridge) for field support and discussions. We thank Kirsten de Haan, Arnold van Dijk, Coen Mulder, and Natasja Welters (Utrecht University) for analytical support. T.A. Mather and J. Frieling acknowledge funding from a European Research Council (ERC) consolidator grant (ERC-2018-COG-818717-V-ECHO) , A. Sluijs acknowledges ERC consolidator grant 771497 (SPANC) , and C.P. Slomp and N.A.G.M. van Helmond acknowledge funding from Dutch Research Council (NWO) Vici grant 865.13.005. M.J. Cram- winckel and A. Sluijs thank the Ammodo Foundation for funding unfettered research by laureate A. Sluijs.	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Soc. Am. Bull.	MAY 1	2022	135	5-6					1280	1296		10.1130/B36280.1	http://dx.doi.org/10.1130/B36280.1		SEP 2022	17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	F6NQ5		Green Published, Green Submitted, Bronze			2025-03-11	WOS:000855624800001
J	Yi, S; Hong, SW; Yoo, DG; Lee, GS; Lim, J				Yi, Sangheon; Hong, Seok-Whi; Yoo, Dong-Geun; Lee, Gwang-Soo; Lim, Jaesoo			Palynostratigraphy indication of the Pliocene-Pleistocene boundary in Hupo Basin of the East Sea, offshore Korea	MARINE GEOPHYSICAL RESEARCH			English	Article						Pollen; Dinocysts; Hupo Basin; Offshore Korea; Palynostratigraphy; Pliocene-Pleistocene boundary	DINOFLAGELLATE CYST; NORTH PACIFIC; SEDIMENTS; RECORD; BIOSTRATIGRAPHY; DEPOSITS	A palynological analysis was carried out for the first time on sediments from Hupo Basin, East Sea, offshore Korea, to locate the Pliocene-Pleistocene boundary and thus determine the depositional age of this stratigraphic unit. Core 19ESDP-101, taken from Hupo Basin, yielded diverse, abundant to common pollen and dinocysts. Age-diagnostic palynomorphs were present in certain core intervals (Zone I, depths 120-63.96 mbsf). However, those age indicators were dark brown, heavily broken representatives that appeared together with poorly sorted, opaque, dark phytoclasts in the lower part of Zone II (63.96-38.76 mbsf), and they were considered to have been recycled from reworked late Pliocene strata due to contour currents during the transgression. Biostratigraphically meaningful taxa were the pollen Carya, Liquidambar, and Fagus and the dinocysts Filisphaera filifera subsp. pilosa and Spiniferites pachyderma. The latest stratigraphic occurrence of these pollen taxa in northeast Asia is the Late Pliocene, and that of the dinocysts is the Late Pliocene across a wide range of aquatic areas, especially in the Pacific. The last appearance datum of the age indicators in this study suggested 63.96 mbsf (top boundary of Zone I) as the Pliocene-Pleistocene boundary in core 19ESDP-101.	[Yi, Sangheon; Hong, Seok-Whi; Yoo, Dong-Geun; Lee, Gwang-Soo; Lim, Jaesoo] Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea; [Yi, Sangheon; Yoo, Dong-Geun; Lim, Jaesoo] Korea Univ Sci & Technol, Daejeon 34113, South Korea	Korea Institute of Geoscience & Mineral Resources (KIGAM); University of Science & Technology (UST)	Yi, S (通讯作者)，Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea.; Yi, S (通讯作者)，Korea Univ Sci & Technol, Daejeon 34113, South Korea.	shyi@kigam.re.kr	Lim, Jaesoo/N-4219-2017; YI, Sangheon/D-4780-2011	Lim, Jaesoo/0000-0001-7478-0562; YI, Sangheon/0000-0002-2938-0380	"Study on submarine active faults and evaluation of possible submarine earthquakes in the southern part of the East Sea, Korea" of the KIGAM - Ministry of Ocean and Fisheries of Korea [NP2018-018]; KIGAM - Ministry of Science and ICT of Korea [GP2020-003]	"Study on submarine active faults and evaluation of possible submarine earthquakes in the southern part of the East Sea, Korea" of the KIGAM - Ministry of Ocean and Fisheries of Korea; KIGAM - Ministry of Science and ICT of Korea	This research was supported by the "Study on submarine active faults and evaluation of possible submarine earthquakes in the southern part of the East Sea, Korea (NP2018-018)" of the KIGAM, funded by the Ministry of Ocean and Fisheries of Korea, and also in part by basic research grants (GP2020-003) from the KIGAM, funded by the Ministry of Science and ICT of Korea. This paper was prepared for the special issue entitled "Geological implications for submarine geohazards, Ulleung Basin, East Sea". We sincerely thank Dr. Jaume Llopart, Guest Editor, and the anonymous reviewers for their constructive comments that improved the manuscript.	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Geophys. Res.	SEP	2022	43	3							28	10.1007/s11001-022-09490-0	http://dx.doi.org/10.1007/s11001-022-09490-0			16	Geochemistry & Geophysics; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics; Oceanography	2W7LP					2025-03-11	WOS:000824702200001
J	Wang, ZH; Peng, L; Xie, CL; Wang, WT; Zhang, YN; Xiao, LJ; Tang, YL; Yang, YF				Wang, Zhaohui; Peng, Liang; Xie, Changliang; Wang, Wenting; Zhang, Yuning; Xiao, Lijuan; Tang, Yali; Yang, Yufeng			Metabarcoding of harmful algal bloom species in sediments from four coastal areas of the southeast China	FRONTIERS IN MICROBIOLOGY			English	Article						eukaryotic algae; 18S rDNA; human activities; resting stages; the Yellow Sea; the East China Sea	AZADINIUM-POPORUM DINOPHYCEAE; SURFACE SEDIMENTS; MOLECULAR CHARACTERIZATION; ALEXANDRIUM-FUNDYENSE; KARLODINIUM-VENEFICUM; DINOFLAGELLATE CYSTS; RESTING STAGES; PHYTOPLANKTON; SEA; MORPHOLOGY	In the past three decades, harmful algal blooms (HAB) have become more frequent and widespread in southeast Chinese sea areas. Resting stages are regarded as the "seed bank" of algal blooms, and play an important role in initiating HABs. The distribution of resting stages in sediments especially those of HAB species can make good predictions about the potential risk of future blooms, however with limited reports. In this study, surface sediment samples were collected in the four sea areas along the southeast Chinese coasts, including Dafeng Port (DF) in the southern Yellow Sea, Xiangshan Bay (XS), Funing Bay (FN), and Dongshan Bay (DS) in the East China Sea. Diversity and community structure of eukaryotic microalgae in surface sediments were assessed by metabarcoding V4 region of the 18S rDNA, focusing on the distribution of HAB species. Biogenic elements including total organic carbon (TOC), total nitrogen (TN), total phosphorus (TP), biogenic silicon (BSi), and moisture content (MC) were analyzed. A total of 454 eukaryotic algal OTUs were detected, which belonged to 31 classes of 9 phyla. Altogether 149 algal species were detected in this study, and 59 taxa have been reported to form resting stages. Eukaryotic algal community was similar in XS, FN and DS of the East China Sea, which were predominated by dinoflagellates. However, algal community was different in DF of the Yellow Sea, and characterized by the dominance of chrysophytes and low OTU richness. The distribution of most abundant HAB species showed positive correlations with TN, BSi, and TOC, suggesting that eutrophication and consequent increase in diatom productivity may have a significant influence on the distribution of HAB species and facilitate the occurrence of HABs. Furthermore, HAB species occurred more abundantly and widely in FN. Our results suggest high potential risks of HABs in the southeast Chinese coast especially in Funing Bay.	[Wang, Zhaohui; Peng, Liang; Xie, Changliang; Wang, Wenting; Zhang, Yuning; Xiao, Lijuan; Tang, Yali; Yang, Yufeng] Jinan Univ, Coll Life Sci & Technol, Guangzhou, Peoples R China; [Yang, Yufeng] Southern Marine Sci & Engn Guangdong Lab, Zhuhai, Peoples R China	Jinan University	Xiao, LJ; Tang, YL (通讯作者)，Jinan Univ, Coll Life Sci & Technol, Guangzhou, Peoples R China.	tljxiao@jnu.edu.cn; litangyali@163.com	Zhang, Yuning/E-1449-2011		Science and Technology Basic Resources Investigation Program of China; National Natural Science Foundation of China [2018FY100200]; Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) [42076141];  [311021006]	Science and Technology Basic Resources Investigation Program of China; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai); 	This study was supported by the Science and Technology Basic Resources Investigation Program of China (No. 2018FY100200), the National Natural Science Foundation of China (No. 42076141), and Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (No. 311021006).	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Microbiol.	AUG 31	2022	13								999886	10.3389/fmicb.2022.999886	http://dx.doi.org/10.3389/fmicb.2022.999886			19	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	6Q6RO	36118226	Green Published, gold			2025-03-11	WOS:000891739800001
J	Tang, YZ; Deng, YY; Yue, CX; Chai, ZY; Shang, LX				Tang, Ying Zhong; Deng, Yunyan; Yue, Caixia; Chai, Zhaoyang; Shang, Lixia			Deficiency of nitrogen but not phosphorus triggers the life cycle transition of the dinoflagellate <i>Scrippsiella acuminata</i> from vegetative growth to resting cyst formation	HARMFUL ALGAE			English	Article						Resting cyst; Harmful algal blooms (HABs); Cell cycle; CyclinB; CDK1; Scrippsiella acuminata	HARMFUL ALGAL BLOOMS; CELL-CYCLE; PHOTOSYNTHETIC APPARATUS; B HOMOLOG; RED TIDE; DINOPHYCEAE; TEMPERATURE; ENCYSTMENT; PHOSPHATE; NUTRIENTS	Nitrogen (N) and phosphorus (P) are essential elements for algal growth. When N and P are deficient, dinoflagellates will take a series of measures to achieve population continuation including formation of resting cysts, an important ecological strategy of dinoflagellates that plays a key role in the initiation and termination of harmful algal blooms (HABs). How the deficiency of N and P affects algal growth and cyst formation has been investigated in some dinoflagellate species, but how it affects the life cycle transition in dinoflagellates has been poorly understood. In this study, we further explored the effect of N and P deficiency on the algal growth and resting cyst production in the cosmopolitan HABs-causing species Scrippsiella acuminata via refining the N and P concentration gradients. Further, we tracked the expression patterns of one CyclinB and one CDKI genes of S. acuminata at different growth stages under three deficiency concentrations (1/1000 dilutions of N, P, and both N and P). The results suggest that N deficiency always triggered the cyst formation but P deficiency mainly inhibited the vegetative growth instead of inducing cyst formation. We also observed the highest cyst production when S. acuminata was cultured in the f/2-Si medium that was a one-thousandth dilution of N and P (N similar to 0.882 mu M; P similar to 0.0362 mu M). Our results for the expressions of CyclinB and CDKI were well consistent with the results of algal growth and cyst formation at different deficiencies of N and P in terms of that higher expressions of these two genes were corresponding to higher rates of vegetative cell growth, while their expressions in resting cysts maintained to be moderate but significantly lower than that in fast-growing vegetative cells. Although we are still not sure whether the changing expressions of the two genes did regulate the transition of life cycle (i.e. cyst formation), or happened as parallels to the expressions of other truly regulating genes, our observations are surely inspirational for further investigations on the genetic regulation of life cycle transition in dinoflagellates. Our work will provide clues to probe the physiological and molecular mechanisms underlying the nutrient deficiency-induced alternation between life cycle stages in dinoflagellates.	[Tang, Ying Zhong; Deng, Yunyan; Yue, Caixia; Chai, Zhaoyang; Shang, Lixia] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Tang, Ying Zhong; Deng, Yunyan; Chai, Zhaoyang; Shang, Lixia] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Tang, Ying Zhong; Deng, Yunyan; Chai, Zhaoyang; Shang, Lixia] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Tang, Ying Zhong; Yue, Caixia] Univ Chinese Acad Sci, Beijing 100049, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Tang, YZ; Deng, YY (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	yingzhong.tang@qdio.ac.cn; yunyandeng@qdio.ac.cn	Yue, caixia/HHN-3747-2022; Chai, Zhaoyang/F-7485-2017		Key Deployment Project of Center for Ocean Mega -Research of Science, Chinese Academy of Sciences [COMS2019Q09]; National Science Foundation of China [42176207, 41976134]	Key Deployment Project of Center for Ocean Mega -Research of Science, Chinese Academy of Sciences; National Science Foundation of China(National Natural Science Foundation of China (NSFC))	This research was funded by the Key Deployment Project of Center for Ocean Mega -Research of Science, Chinese Academy of Sciences (Grant No. COMS2019Q09) and the National Science Foundation of China (Grant Nos. 42176207 and 41976134) .	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J	Dashtgard, SE; Wang, AH; Pospelova, V; Wang, PL; La Croix, A; Ayranci, K				Dashtgard, Shahin E.; Wang, Aihua; Pospelova, Vera; Wang, Pei-Ling; La Croix, Andrew; Ayranci, Korhan			Salinity indicators in sediment through the fluvial-to-marine transition (Fraser River, Canada)	SCIENTIFIC REPORTS			English	Article							INCLINED HETEROLITHIC STRATIFICATION; DINOFLAGELLATE CYSTS; SPATIAL-DISTRIBUTION; ORGANIC-CARBON; DELTA FRONT; ESTUARY; SAND; MASSACHUSETTS; MORPHOLOGY; TRANSPORT	Many sediment attributes have been proposed as proxies for determining salinity conditions under which sediment is deposited, and six attributes (Sr/Ba-HAc, Sr/Ba-NH4Ac, delta C-13(org), C/N, and the relative abundances and concentrations of dinoflagellate cysts) are compared here. In this paper, sediment attributes from the Fraser River Delta, Canada and surrounding coastal areas are compared by depositional position along the fluvial-to-marine transition, by salinity, and by sedimentological characteristics. Along the fluvial-to-marine transition, most attributes exhibit distinct trends between parts of the river that experience sustained marine water (saltwater) influence over seasonal and tidal timeframes, and parts that experience only freshwater or periodic saltwater influence. No attributes are reliable indicators of depositional position where saltwater incursion is short lived or where water is fresh. Where marine influence is sustained, Sr/Ba-HAc and Sr/Ba-NH4Ac are the most reliable positional indicators along the fluvial-to-marine transition. When compared strictly to salinity, Sr/Ba-HAc, Sr/Ba-NH4Ac, and delta C-13(org) all correlate predictably except in delta front and prodelta settings. Our data show that all six sediment attributes are heavily impacted by river-derived sedimentation, and it is not appropriate to compare values from strongly river-influenced settings (e.g., deltas) with those from weakly river-influenced settings (e.g., bays and estuaries).	[Dashtgard, Shahin E.] Simon Fraser Univ, Earth Sci, Burnaby, BC V5A 1S6, Canada; [Wang, Aihua] China Geol Survey, Nanjing Ctr, Nanjing 210016, Peoples R China; [Pospelova, Vera] Univ Minnesota, Earth & Environm Sci, Minneapolis, MN 55455 USA; [Wang, Pei-Ling] Natl Taiwan Univ, Inst Oceanog, Taipei, Taiwan; [La Croix, Andrew] Univ Waikato, Sch Sci, Earth & Environm Sci, Hamilton 3240, New Zealand; [Ayranci, Korhan] King Fahd Univ Petr & Minerals, Petr Engn & Geosci, Dhahran 31261, Saudi Arabia	Simon Fraser University; China Geological Survey; Nanjing Center, China Geological Survey; University of Minnesota System; University of Minnesota Twin Cities; National Taiwan University; University of Waikato; King Fahd University of Petroleum & Minerals	Dashtgard, SE (通讯作者)，Simon Fraser Univ, Earth Sci, Burnaby, BC V5A 1S6, Canada.	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J	Rodríguez-Villegas, C; Díaz, PA; Salgado, P; Tomasetti, SJ; Díaz, M; Marín, SL; Baldrich, AM; Niklitschek, E; Pino, L; Matamala, T; Espinoza, K; Figueroa, R				Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Salgado, Pablo; Tomasetti, Stephen J.; Diaz, Manuel; Marin, Sandra L.; Baldrich, Angela M.; Niklitschek, Edwin; Pino, Loreto; Matamala, Thamara; Espinoza, Katherine; Figueroa, Rosa, I			The role of physico-chemical interactions in the seasonality of toxic dinoflagellate cyst assemblages: The case of the NW Patagonian fjords system	ENVIRONMENTAL POLLUTION			English	Article						Resting cysts; Saxitoxins; Yessotoxins; Redox potential; Harmful algal blooms; Seasonality	HARMFUL ALGAL BLOOMS; SOUTHERN CHILE; RESTING CYSTS; ALEXANDRIUM-CATENELLA; SURFACE SEDIMENTS; DINOPHYCEAE; ABUNDANCE; YESSOTOXINS; SPP.; BAY	Harmful algal blooms (HABs) are recurrent in the NW Patagonia fjords system and their frequency has increased over the last few decades. Outbreaks of HAB species such as Alexandrium catenella, a causal agent of paralytic shellfish poisoning, and Protoceratium reticulatum, a yessotoxins producer, have raised considerable concern due to their adverse socioeconomic consequences. Monitoring programs have mainly focused on their planktonic stages, but since these species produce benthic resting cysts, the factors influencing cyst distributions are increasingly gaining recognition as potentially important to HAB recurrence in some regions. Still, a holistic understanding of the physico-chemical conditions influencing cyst distribution in this region is lacking, espe-cially as it relates to seasonal changes in drivers of cyst distributions, as the characteristics that favor cyst preservation in the sediment may change through the seasons. In this study, we analyzed the physico-chemical properties of the sediment (temperature, pH, redox potential) and measured the bottom dissolved oxygen levels in a "hotspot" area of southern Chile, sampling during the spring and summer as well as the fall and winter, to determine the role these factors may play as modulators of dinoflagellate cyst distribution, and specifically for the cysts of A. catenella and P. reticulatum. A permutational analysis of variance (PERMANOVA) showed the significant effect of sediment redox conditions in explaining the differences in the cyst assemblages between spring-summer and fall-winter periods (seasonality). In a generalized linear model (GLM), sediment redox po-tential and pH were associated with the highest abundances of A. catenella resting cysts in the spring-summer, however it was sediment temperature that most explained the distribution of A. catenella in the fall-winter. For P. reticulatum, only spring-summer sediment redox potential and temperature explained the variation in cyst abundances. The implications of environmental (physico-chemical) seasonality for the resting cysts dy-namics of both species are discussed.	[Rodriguez-Villegas, Camilo; Baldrich, Angela M.] Univ Los Lagos, Programa Doctorado Ciencias Menc Conservac & Mane, Camino Chinquihue Km 6, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Baldrich, Angela M.; Niklitschek, Edwin] Univ Los Lagos, Ctr I Mar, Casilla 557, Puerto Montt, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Baldrich, Angela M.] Univ Los Lagos, CeBiB, Casilla 557, Puerto Montt, Chile; [Salgado, Pablo] Inst Fomento Pesquero IFOP, Ctr Estudios Algas Noc CREAN, Enrique Abello 0552, Chile; [Tomasetti, Stephen J.] Hamilton Coll, Environm Studies Program, Clinton, NY 13323 USA; [Diaz, Manuel] Univ Austral Chile, Programa Invest Pesquera, Puerto Montt, Chile; [Diaz, Manuel; Marin, Sandra L.] Univ Austral Chile, Inst Acuicultura, Puerto Montt, Chile; [Pino, Loreto; Matamala, Thamara; Espinoza, Katherine] Univ Austral Chile, Inst Acuicultura, Programa Invest Pesquera, Puerto Montt, Chile; [Figueroa, Rosa, I] Inst Espanol Oceanog IEO CSIC, Ctr Oceanog Vigo, Subida Radio Faro 50, Vigo 36390, Spain	Universidad de Los Lagos; Universidad de Los Lagos; Universidad de Los Lagos; Instituto de Fomento Pesquero (Valparaiso); Hamilton College; Universidad Austral de Chile; Universidad Austral de Chile; Universidad Austral de Chile; Spanish Institute of Oceanography	Rodríguez-Villegas, C (通讯作者)，Univ Los Lagos, Ctr I Mar, Casilla 557, Puerto Montt, Chile.	camilorodriguezvillegas@gmail.com	Díaz, Patricio/B-8128-2018; Díaz, Manuel/AAM-6225-2021; Salgado, Pablo/KMA-0636-2024; Baldrich, Angela M./AAC-8054-2022; Niklitschek, Edwin/A-7066-2008; Figueroa, Rosa/M-7598-2015; Rodriguez Villegas, Camilo/AAB-8563-2022	Baldrich, Angela M./0000-0002-2624-7357; Pino Chandia, Loreto/0000-0002-5784-2730; Niklitschek, Edwin/0000-0001-5561-3494; Figueroa, Rosa/0000-0001-9944-7993; Tomasetti, Stephen/0000-0001-6947-5141; Rodriguez Villegas, Camilo/0000-0002-1429-2775	Fisheries Under secretary of Chile by Fondo Investigacion Pesquera y Acuicultura project [2016-02-ID 4728 _53_ LQ16]; Centro de Biotecnologa y Bioingeniera (CeBiB) [FB0001]; Spanish Ministry of Science and Innovation; European Community (FEDER) [DIANAS-CTM2017-86066-R]; Universidad de Los Lagos; Innovation Agency of the Xunta de Galicia (GAIN) [GRC-VGO-HAB IN607A-2019/04]	Fisheries Under secretary of Chile by Fondo Investigacion Pesquera y Acuicultura project; Centro de Biotecnologa y Bioingeniera (CeBiB); Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); European Community (FEDER)(European Union (EU)); Universidad de Los Lagos; Innovation Agency of the Xunta de Galicia (GAIN)	This work was funded by the Fisheries Under secretary of Chile by Fondo Investigacion Pesquera y Acuicultura project [FIPA No 2016-02-ID 4728 _53_ LQ16] and by the Centro de Biotecnologa y Bioingeniera (CeBiB) (PIA project FB0001, ANID, Chile) . Rosa I. Figueroa was funded by a national project from the Spanish Ministry of Science and Innovation and the European Community (FEDER) (Project DIANAS-CTM2017-86066-R) and a grant for Galician Networks of Excellence (GRC-VGO-HAB IN607A-2019/04) from the Innovation Agency of the Xunta de Galicia (GAIN) . The authors also acknowledge the Universidad Austral de Chile for the human and technical support of the oceanographic campaign. Camilo Rodrguez Villegas had a fellowship from Universidad de Los Lagos.	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J	Lin, SJ; Yu, LY; Wu, XM; Li, MZ; Zhang, YQ; Luo, H; Li, HF; Li, TC; Li, L				Lin, Senjie; Yu, Liying; Wu, Xiaomei; Li, Meizhen; Zhang, Yaqun; Luo, Hao; Li, Hongfei; Li, Tangcheng; Li, Ling			Active meiosis during dinoflagellate blooms: A 'sex for proliferation' hypothesis	HARMFUL ALGAE			English	Article						Sexual reproduction; Dinoflagellate bloom; Sex for encystment (SXE); Sex for proliferation (SXP); Meiosis genes	DOUBLE-STRAND BREAKS; LIFE-CYCLE; PFIESTERIA-PISCICIDA; REPRODUCTION; DINOPHYCEAE; CYSTS; PHYTOPLANKTON; SEXUALITY; EVOLUTION; ANCIENT	In dinoflagellates, sexual reproduction is best known to be induced by adverse environmental conditions and culminate in encystment for survival ('sex for encystment'). Although increasing laboratory observations indicate that sex can lead to production of vegetative cells bypassing encystment, the occurrence of this alternative pathway in natural populations and its ecological roles remain poorly understood. Here we report evidence that sex in dinoflagellates can potentially be an instrument for bloom proliferation or extension. By bloom meta-transcriptome profiling, we documented elevated expression of meiosis genes in two evolutionarily distinct species (Prorocentrum shikokuense and Karenia mikimotoi) during bloom, a timing unexpected of the 'sex for encystment' scenario. To link these genes to meiosis, we induced encystment and cyst germination in the cyst -forming species Scrippsiella acuminata, and found that five of these genes were upregulated during cyst germi-nation, when meiosis occurs. Integrating data from all three species revealed that SPO11, MND1, and DMC1 were likely common between cyst-forming and non-encysting sex in dinoflagellates. Furthermore, flow cytometric analyses revealed consecutive rounds of DNA halving during blooms of P. shikokuense and K. mikimotoi, evidencing meiosis. These data provided novel evidence that sexual reproduction in dinoflagellates might serve to promote cell proliferation, and along with the consequent enhancement of genetic diversity facilitating resistance against pathogens and environmental stress, to boost or extend a bloom ('sex for proliferation'). The putative meiosis-specific genes and insights reported here will prove to be helpful for rigorously testing the hypothesis and addressing whether the two modes of sex are genetically predisposed (i.e. species-specific) or environmentally induced (switchable within species), and if the latter what triggers the switch.	[Lin, Senjie] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; [Yu, Liying; Wu, Xiaomei; Li, Meizhen; Zhang, Yaqun; Luo, Hao; Li, Hongfei; Li, Tangcheng; Li, Ling] Xiamen Univ, Coll Ocean & Earth Sci, State Key Lab Marine Environm Sci, Xiamen 361102, Fujian, Peoples R China; [Yu, Liying] Fujian Med Univ, Cent Lab, Affiliated Hosp 2, Quanzhou 362000, Peoples R China; [Li, Meizhen] McGill Univ, Dept Biol, Montreal, PQ H3A 1B1, Canada; [Zhang, Yaqun] Chinese Acad Fishery Sci, Key Lab Aquat Genom, Minist Agr & Rural Affairs, Beijing 100141, Peoples R China; [Zhang, Yaqun] Chinese Acad Fishery Sci, Beijing Key Lab Fishery Biotechnol, Beijing 100141, Peoples R China; [Li, Hongfei] Zhejiang Ocean Univ, Natl Engn Res Ctr Marine Aquaculture, Zhoushan 316022, Zhejiang, Peoples R China; [Li, Tangcheng] Shantou Univ, Inst Marine Sci, Coll Sci, Shantou 515063, Guangdong, Peoples R China; [Li, Tangcheng] Shantou Univ, Biol Dept, Shantou 515063, Guangdong, Peoples R China	University of Connecticut; Xiamen University; Fujian Medical University; Ministry of Agriculture & Rural Affairs; Chinese Academy of Fishery Sciences; Chinese Academy of Fishery Sciences; Zhejiang Ocean University; Shantou University; Shantou University	Lin, SJ (通讯作者)，Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA.	senjie.lin@uconn.edu	Lin, Senjie/A-7466-2011; Luo, Hao/JEZ-3644-2023; Li, Zilin/AAB-1216-2019	Wu, Xiaomei/0000-0002-7425-8755; Lin, Senjie/0000-0001-8831-6111	Gordon and Betty Moore Foundation grant GBMF [4980.01]; National Natural Science Foundation of China [41330959]; Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) [2018SDKJ0406-3]	Gordon and Betty Moore Foundation grant GBMF; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao)	This work was supported by the Gordon and Betty Moore Foundation grant GBMF grant #4980.01, the National Natural Science Foundation of China grant #41330959, and the Marine S & T Fund of Shandong Province for Pilot National Laboratory for Marine Science andTechnology (Qingdao) grant #2018SDKJ0406-3.	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J	Wilson, JM; Erazo, N; Connors, E; Chamberlain, EJ; Clements, SM; Carter, ML; Smith, JE; Bowman, JS				Wilson, Jesse M.; Erazo, Natalia; Connors, Elizabeth; Chamberlain, Emelia J.; Clements, Samantha M.; Carter, Melissa L.; Smith, Jennifer E.; Bowman, Jeff S.			Substantial microbial community shifts in response to an exceptional harmful algal bloom in coastal Southern California	ELEMENTA-SCIENCE OF THE ANTHROPOCENE			English	Article						Phytoplankton bloom; Red tide; Microbial community; Carbon cycling	EARLY-WARNING SIGNALS; OPERON COPY NUMBER; RED TIDE; ALEXANDRIUM DINOPHYCEAE; CYST FORMATION; HIROSHIMA BAY; DINOFLAGELLATE; DYNAMICS; ASSEMBLAGES; BACTERIUM	Phytoplankton blooms create organic matter that stimulates entire marine ecosystems, including other components of the microbial community. How the ecosystem responds varies depending on the intensity, duration, and composition of the bloom. When the bloom has a direct or indirect negative impact on the ecosystem, it is termed a harmful algal bloom (HAB). HAB frequency is expected to increase in response to changing oceanic conditions and coastal nutrient supply. Characterizing the response of the bacterial and archaeal communities to HABs will improve our understanding of the ecological impacts of these phenomena. We utilized time series of chlorophyll a, phaeophytin, dissolved oxygen, flow cytometry cell counts, and microbial community structure (assessed via 16S rRNA gene sequences) maintained by several observing programs to investigate how the microbial community was affected by an exceptional bloom of Lingulodinium polyedra in coastal Southern California. These multi-year datasets allowed us to compare the microbial community response to past events, such as a smaller L. polyedra bloom the previous year. We demonstrated that the bacterial and archaeal response to the 2020 bloom was unique taxonomically, with many novel heterotrophs, and higher trophic state variance. The measured heterotrophic response to the bloom resulted in massive oxygen drawdown and may have impacted the length of the bloom and contributed to a secondary diatom bloom following the main HAB event. Taken together, these data illustrate how the massive 2020 L. polyedra bloom created unique ecological conditions for coastal Southern California.	[Wilson, Jesse M.; Erazo, Natalia; Connors, Elizabeth; Chamberlain, Emelia J.; Clements, Samantha M.; Carter, Melissa L.; Smith, Jennifer E.; Bowman, Jeff S.] Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA; [Bowman, Jeff S.] Univ Calif San Diego, Ctr Microbiome Innovat, San Diego, CA 92103 USA; [Bowman, Jeff S.] Univ Calif San Diego, Ctr Marine Biodivers & Conservat, San Diego, CA 92103 USA	University of California System; University of California San Diego; Scripps Institution of Oceanography; University of California System; University of California San Diego; University of California System; University of California San Diego	Wilson, JM (通讯作者)，Univ Calif San Diego, Scripps Inst Oceanog, San Diego, CA 92103 USA.	jmwilson@ucsd.edu		Connors, Elizabeth/0000-0002-4992-4218; Bowman, Jeff/0000-0002-8811-6280; Erazo, Natalia G./0000-0002-7498-0860; Chamberlain, Emelia Janthina/0000-0003-2218-3488	National Oceanic and Atmospheric Administration [NOAA NA16NOS0120022, NA11NOS120029, NA17RJ1231]; MacArthur Foundation; Simons Foundation Early Career Marine Microbial Ecology and Evolution award	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); MacArthur Foundation; Simons Foundation Early Career Marine Microbial Ecology and Evolution award	The Southern California Coastal Ocean Observing Harmful Algal Bloom Monitoring Program was supported by the National Oceanic and Atmospheric Administration (NOAA NA16NOS0120022, NA11NOS120029, and NA17RJ1231). 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Anthrop.	AUG 12	2022	10	1							1	10.1525/elementa.2021.00088	http://dx.doi.org/10.1525/elementa.2021.00088			21	Environmental Sciences; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences	4L4XZ		gold			2025-03-11	WOS:000852634600001
J	Kietzmann, DA; Iovino, F; Encinas, A				Kietzmann, Diego A.; Iovino, Franco; Encinas, Alfonso			New microbiostratigraphic data (calpionellids and calcispheres) from the tithonian of central Chile, type section (Rio Tinguiririca) of the banos del Flaco Formation	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Calpionellids; Calcareous dinoflagellate cysts; Biostratigraphy; Banos del flaco formation; Upper jurassic	VACA MUERTA FORMATION; JURASSIC-CRETACEOUS BOUNDARY; SOUTHERN MENDOZA AREA; NEUQUEN BASIN; JURASSIC/CRETACEOUS BOUNDARY; WESTERN BALKAN; STRATIGRAPHY; EVOLUTION; BIOSTRATIGRAPHY; MICROFACIES	This work presents new biostratigraphic data based on calpionellids and calcareous dinoflagellate cysts for the Tithonian in Central Chile. This stratigraphic interval is mostly represented by a thick marine succession of limestone and sandstone known as Banos del Flaco Formation. This formation originated in the shallow-water setting of a carbonate ramp and correlates with other well-studied units in the Neuquen basin of Argentina. Calpionellids and calcareous dinogflagellate cysts are studied on the Chilean side of the Andes for the first time. The recognition of several calpionellids and calcareous dinogflagellate cyst species within the lower Banos del Flaco Formation allowed the identification of a preliminary microbiostratigraphic zonation. Calcareous dinoflagellate cysts include eleven species that defines the Colomisphaera tenuis, and Colomisphaera fortis zones, whereas six chitinoidellid species allowed the identification of the Chitinoidella and Crassicollaria zones, with the Slovenica, Boneti and Remanei subzones. These new microbiostratigraphic data suggest a latest early to earliest late Tithonian age for the studied interval.	[Kietzmann, Diego A.; Iovino, Franco] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Universitaria, Pabellon II, Intendente Guiraldes, 2160, RA-1428 Buenos Aires, DF, Argentina; [Kietzmann, Diego A.] Univ Buenos Aires, Ciudad Universitaria, CONICET, Inst Geociencias Bas, Pabellon II, Intendente Guiraldes, 2160, RA-1428 Buenos Aires, DF, Argentina; [Encinas, Alfonso] Univ Concepcion, Fac Ciencias Quim, Dept Ciencias Tierra, Concepcion, Chile; [Kietzmann, Diego A.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, 2160, RA-1428 Buenos Aires, DF, Argentina	University of Buenos Aires; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad de Concepcion; University of Buenos Aires	Kietzmann, DA (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Universitaria, Pabellon II, Intendente Guiraldes, 2160, RA-1428 Buenos Aires, DF, Argentina.; Kietzmann, DA (通讯作者)，Univ Buenos Aires, Ciudad Universitaria, CONICET, Inst Geociencias Bas, Pabellon II, Intendente Guiraldes, 2160, RA-1428 Buenos Aires, DF, Argentina.; Kietzmann, DA (通讯作者)，Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, 2160, RA-1428 Buenos Aires, DF, Argentina.	diegokietzmann@gl.fcen.uba.ar	Kietzmann, Diego/S-4549-2019	Kietzmann, Diego Alejandro/0000-0003-1222-7811	Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT); Proyecto FONDECYT [1200428]; Agencia Nacional de Promocion Cientifica y Tecnologica (Argentina); Proyecto PICT [2018-02492]; Department of Geological Sciences of the University of Buenos Aires (Argentina)	Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)); Proyecto FONDECYT(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT); Agencia Nacional de Promocion Cientifica y Tecnologica (Argentina)(ANPCyT); Proyecto PICT; Department of Geological Sciences of the University of Buenos Aires (Argentina)	This research was supported by the Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT), Proyecto FONDECYT n.1200428, directed by Alfonso Encinas, and Agencia Nacional de Promocion Cientifica y Tecnologica (Argentina), Proyecto PICT 2018-02492, directed by Diego A. Kietzmann. The Department of Geological Sciences of the University of Buenos Aires (Argentina) supported with funding for the completion of the final degree project of the second author (Franco Iovino), which is part of this study. We especially thank Ioan I. Bucur and Sreepat Jain for constructive reviews that allowed to significantly improve the original version of the manuscript. We also thank Andres Folguera for editorial handling.	Altiner Demir, 1991, Geologica Romana, V27, P215; Andreini G, 2007, SWISS J GEOSCI, V100, P179, DOI 10.1007/s00015-007-1227-z; [Anonymous], 2014, THESIS U CHILE SANTI; [Anonymous], 1962, RECONOCIMIENTO GEOLO; [Anonymous], 1997, Mineral. 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J	Daners, G; Amenabar, CR; Guerstein, GR; Veroslavsky, G				Daners, G.; Amenabar, C. R.; Guerstein, G. R.; Veroslavsky, G.			Palynostratigraphical analysis of the late Maastrichtian - early Danian in the Gaviotin Formation, Punta del Este Basin, Uruguay	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cysts; Lithostratigraphy; Biostratigraphy; Palaeoceanography; Palaeoclimatology; K; Pg transition; Southwestern Atlantic basins	CRETACEOUS-PALEOGENE BOUNDARY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEA-LEVEL CHANGES; CHICXULUB IMPACT; MASS EXTINCTION; CONTINENTAL-MARGIN; DECCAN VOLCANISM; COLORADO BASIN; OULED HADDOU; EXTERNAL RIF	Palynological analysis were carried out for the uppermost Cretaceous - lowermost Palaeogene in the Gaviotin well, which was drilled in the marginal area of the offshore Punta del Este Basin (Uruguay). The studied interval (from 1582 to 1884 m) corresponds to the lower and middle parts of the Gaviotin Formation and the upper part of the underlying Mercedes Formation. The samples provided assemblages dominated by fairly well preserved organic walled dinoflagellate cysts. A total of 117 taxa were identified, several of them are recorded for the first time in the basin. The purpose of this study is to typify the uppermost Cretaceous - lowermost Palaeocene marine sediments of the Punta del Este Basin, which are part of the Gaviotin Formation, focused on their stratigraphical and palynological characteristics. According to the lithology, well logs and microfossil content, three intervals were recognized. The upper part of Mercedes Formation was deposited in a deltaic environment. The lower part of the Gaviotin Formation represents a shallow marine environment. The analysis of the middle part of the Gaviotin Formation (i.e. the upper part of the interval here studied) also reflects shallow marine conditions. Abrupt lithological changes around 1700 m depth, along with a sonic shift probably corresponding to a para-conformity and some biostratigraphical events allowed us to suggest that the K/Pg transition might be close to this depth. These assemblages bear several species that characterize the upper Maastrichtian - Danian interval in many sites from low, middle and high latitudes studied with high sampled resolution. These records demonstrate that the dinoflagellate provincialism suggested more than four decades ago for the Campanian cannot be recognized for successions younger than Maastrichtian. Our results permit the definition of a biostratigraphy that will assist drilling and hydrocarbon exploration in this and other mid-latitude Southwestern Atlantic basins.	[Daners, G.; Veroslavsky, G.] Univ Republ UDELAR, Fac Ciencias, Montevideo, Uruguay; [Amenabar, C. R.] Inst Antartico Argentino, Buenos Aires, Argentina; [Amenabar, C. R.] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Inst Estudios Andinos Don Pablo Grober, IDEAN CONICET,Dept Ciencias Geolog, Buenos Aires, Argentina; [Guerstein, G. R.] Univ Nacl, Dept Geol, CONICET, INGEOSUR,UNS, Buenos Aires, Argentina	Universidad de la Republica, Uruguay; Instituto Antartico Argentino; University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Daners, G (通讯作者)，Univ Republ UDELAR, Fac Ciencias, Montevideo, Uruguay.	lagluar@gmail.com	Veroslavsky, Gerardo/IYS-3313-2023	Guerstein, G. 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Pet. Geol.	SEP	2022	143								105728	10.1016/j.marpetgeo.2022.105728	http://dx.doi.org/10.1016/j.marpetgeo.2022.105728		AUG 2022	12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	4Z7TR					2025-03-11	WOS:000862406600001
J	Jackson, R; Andreasen, N; Oksman, M; Andersen, TJ; Pearce, C; Seidenkrantz, MS; Ribeiro, S				Jackson, Rebecca; Andreasen, Nanna; Oksman, Mimmi; Andersen, Thorbjorn J.; Pearce, Christof; Seidenkrantz, Marit-Solveig; Ribeiro, Sofia			Marine conditions and development of the Sirius Water polynya on the North-East Greenland shelf during the Younger Dryas-Holocene	QUATERNARY SCIENCE REVIEWS			English	Review						Holocene; Younger dryas; Paleoceanography; Micropaleontology; Dinocysts; Foraminifera; Greenland; North-East Greenland; Polynyas; Sirius water polynya	SEA-ICE VARIABILITY; EAST GREENLAND; BENTHIC FORAMINIFERA; FRAM STRAIT; ARCTIC-OCEAN; BENTHONIC FORAMINIFERA; ENVIRONMENTAL-CHANGES; DINOFLAGELLATE CYSTS; ABSOLUTE ABUNDANCE; WOLLASTON FORLAND	The Fram Strait is one of the largest gateways through which meltwater and sea ice are exported to the subarctic North Atlantic, transiting the North-East Greenland shelf via the southward flowing East Greenland Current. Observations indicate a recent freshening of the East Greenland Current that may have implications for wider oceanic circulation regimes. The North-East Greenland shelf is an opportune region to assess these changes back through time. Paleoceanographic reconstructions from the North-East Greenland shelf are sparse and their temporal coverage is limited to the Holocene, limiting our ability to assess the impact of rapid climatic variations on marine conditions, such as during the Younger Dryas/Holocene transition. Here, we present data from a well-dated marine sediment core retrieved from the North-East Greenland shelf (74 degrees N; east of Young Sound-Tyrolerfjord system) that captures the late Younger Dryas Stadial through to the Mid-Holocene at sub-centennial resolution. We apply a multi-proxy approach to reconstruct changes in productivity, surface and bottom ocean conditions. We show that at 74 degrees N the presence of warm Atlantic waters on the inner North-East Greenland shelf was limited to the late Younger Dryas, as the Greenland Ice Sheet retreated landward and isostatic rebound caused the area to uplift. A unique dimension to this record is its location within one of the few biological hotspots on the East Greenland shelf today; the Sirius Water polynya. Archaeological studies indicate the polynya was forming as early as 4500 years ago, but nothing is known about its evolution from a marine perspective. Cooling of bottom waters, increasing sea-surface productivity and more frequent open water conditions indicate an Early Holocene onset of the Sirius Water (ca. 10-8.7 ka BP). (C) 2022 The Authors. Published by Elsevier Ltd.	[Jackson, Rebecca; Andreasen, Nanna; Oksman, Mimmi; Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Jackson, Rebecca] Univ Copenhagen, Globe Inst, Oster Voldgade 5-7, DK-1350 Copenhagen K, Denmark; [Andreasen, Nanna; Andersen, Thorbjorn J.] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Pearce, Christof; Seidenkrantz, Marit-Solveig] Aarhus Univ, Arctic Res Ctr, Dept Geosci, Paleoceanog & Paleoclimate Grp, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Pearce, Christof; Seidenkrantz, Marit-Solveig] Aarhus Univ, iClimate Ctr, Dept Geosci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark; [Jackson, Rebecca] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Oster Voldgade 10, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland; University of Copenhagen; University of Copenhagen; Aarhus University; Aarhus University; Geological Survey Of Denmark & Greenland	Jackson, R (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	rjac@geus.dk	Andersen, Thorbjørn/N-7560-2014; Andreasen, Nanna/JQJ-2592-2023; Ribeiro, Sofia/AAZ-2782-2021; Jackson, Rebecca/G-5485-2018; Pearce, Christof/M-4852-2013; Seidenkrantz, Marit-Solveig/A-3451-2012; Ribeiro, Sofia/G-9213-2018	Pearce, Christof/0000-0002-4866-3204; Andreasen, Nanna/0000-0002-0134-4003; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Ribeiro, Sofia/0000-0003-0672-9161; Jackson, Rebecca/0000-0002-0861-3173	EO-CENTER Denmark (project GreenShift); European Union [846142]; Natural Science and Engineering Research Council of Canada; Danish Centre for Marine Research; Danish Council for Inde-pendent Research [9064-00 039B, 7014-00113B, 0135-00165B]; European Union's Horizon 2020 research and innovation program [869383]; Marie Curie Actions (MSCA) [846142] Funding Source: Marie Curie Actions (MSCA)	EO-CENTER Denmark (project GreenShift); European Union(European Union (EU)); Natural Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Danish Centre for Marine Research; Danish Council for Inde-pendent Research(Det Frie Forskningsrad (DFF)); European Union's Horizon 2020 research and innovation program(Horizon 2020); Marie Curie Actions (MSCA)(Marie Curie Actions)	RJ is funded by the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No. 846142. The project received support from GEO-CENTER Denmark (project GreenShift) . The NorthGreen17 expedi-tion was funded by the Danish Centre for Marine Research and the Natural Science and Engineering Research Council of Canada. The project also received funding from the Danish Council for Inde-pendent Research (DFF-Sapere Aude grant no. 9064-00 039B to SRI, and grants no. 7014-00113B (G-Ice project) and 0135-00165B (GreenShelf) , to MSS with additional funding from the European Union's Horizon 2020 research and innovation program under Grant Agreement No. 869383 (ECOTIP; AU/MSS as partner) .	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SEP 1	2022	291								107647	10.1016/j.quascirev.2022.107647	http://dx.doi.org/10.1016/j.quascirev.2022.107647		AUG 2022	19	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	4Y0NM		Green Published, hybrid			2025-03-11	WOS:000861231300003
J	Li, J; Ruan, YF; Wu, RB; Cui, YS; Shen, JC; Mak, YL; Wang, Q; Zhang, K; Yan, M; Wu, JX; Lam, PKS				Li, Jing; Ruan, Yuefei; Wu, Rongben; Cui, Yongsheng; Shen, Jincan; Mak, Yim Ling; Wang, Qi; Zhang, Kai; Yan, Meng; Wu, Jiaxue; Lam, Paul K. S.			Occurrence, spatial distribution, and partitioning behavior of marine lipophilic phycotoxins in the Pearl River Estuary, South China	ENVIRONMENTAL POLLUTION			English	Article						Partitioning behavior; Marine lipophilic phycotoxins; Seawater; Particulate organic matter; Sediment	AZADINIUM-POPORUM DINOPHYCEAE; MICROBIAL COMMUNITY STRUCTURE; HARMFUL ALGAL BLOOMS; ENVIRONMENTAL-FACTORS; DEVELOPMENTAL TOXICITY; DINOFLAGELLATE CYSTS; AZASPIRACID PROFILE; SHELLFISH TOXINS; YELLOW SEA; PHYTOPLANKTON	The occurrence, spatial distribution, and partitioning behavior of 17 marine lipophilic phycotoxins (MLPs) in surface and bottom seawater, particulate organic matter (POM), and surface sediment from the Pearl River Estuary (PRE) were investigated to understand current contamination and the potential risks to marine ecosystems in this region. Nine MLPs were detected, including azaspiracid1- 3, gymnodimine, okadaic acid, dinophysistoxin 1 - 2, pectenotoxin2 (PTX2), and homoyessotoxin, with Sigma 17MLP concentrations ranging 545-12,600 pg L-1 and 619 8,800 pg L-1 in surface and bottom seawater, respectively; 0-294 ng g(-1) and 0.307-300 ng g(-1) dry weight (dw) in surface and bottom POM, respectively; and 3.90-982 pg g(-1) dw in surface sediment. Lower S17MLP levels in the seawater were found at the mouth of the PRE, and gradually increased with increasing distance offshore. According to the calculated partition coefficient, the affinity of MLPs for the aquatic environment components was as follows (from highest to lowest): POM > seawater > sediment. Overall, the distribution and migration of MLPs in the PRE may depend on partition coefficients, the organic carbon fraction, and environmental factors.	[Li, Jing; Ruan, Yuefei; Wu, Rongben; Mak, Yim Ling; Wang, Qi; Zhang, Kai; Yan, Meng; Lam, Paul K. S.] City Univ Hong Kong, State Key Lab Marine Pollut SKLMP, Hong Kong, Peoples R China; [Li, Jing; Ruan, Yuefei; Wu, Rongben; Mak, Yim Ling; Wang, Qi; Zhang, Kai; Yan, Meng; Lam, Paul K. S.] City Univ Hong Kong, Dept Chem, Hong Kong, Peoples R China; [Li, Jing; Ruan, Yuefei; Wu, Rongben; Cui, Yongsheng; Wang, Qi; Zhang, Kai; Yan, Meng; Wu, Jiaxue; Lam, Paul K. S.] Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai 519080, Peoples R China; [Ruan, Yuefei; Wang, Qi; Yan, Meng] City Univ Hong Kong, Shenzhen Res Inst, Res Ctr Oceans & Human Hlth, Shenzhen 518057, Peoples R China; [Cui, Yongsheng; Wu, Jiaxue] Sun Yat Sen Univ, Sch Marine Sci, Zhuhai 519082, Peoples R China; [Shen, Jincan] Shenzhen Acad Inspect Quarantine, Food Inspect & Quarantine Technol Ctr Shenzhen Cu, Key Lab Detect Technol R&D Food Safety, Shenzhen 518026, Peoples R China; [Lam, Paul K. S.] Hong Kong Metropolitan Univ, Off President, 30 Good Shepherd St, Hong Kong, Peoples R China; [Li, Jing] Shenzhen Inst Informat Technol, Dept Transportat & Environm, Shenzhen 518172, Peoples R China	City University of Hong Kong; City University of Hong Kong; Southern Marine Science & Engineering Guangdong Laboratory; Southern Marine Science & Engineering Guangdong Laboratory (Zhuhai); City University of Hong Kong; Shenzhen Research Institute, City University of Hong Kong; Sun Yat Sen University; Shenzhen Academy of Inspection & Quarantine; Hong Kong Metropolitan University; Shenzhen Institute of Information Technology	Ruan, YF (通讯作者)，City Univ Hong Kong, State Key Lab Marine Pollut SKLMP, Hong Kong, Peoples R China.; Ruan, YF (通讯作者)，City Univ Hong Kong, Dept Chem, Hong Kong, Peoples R China.	yruan8@cityu.edu.hk	Yan, Meng/GWP-5833-2022; zhang, kai/C-6432-2013; LI, Jing/AGY-5995-2022; Ruan, Yuefei/R-1323-2018; LAM, Kwan Sing Paul/B-9121-2008; Wang, Qi/ABF-4155-2020	Cui, Yongsheng/0009-0006-6127-9895; Ruan, Yuefei/0000-0003-4696-5708; LAM, Kwan Sing Paul/0000-0002-2134-3710; Wang, Qi/0000-0002-3156-9246; LI, Jing/0000-0001-7467-9667; WU, Rongben/0000-0002-1860-3294	Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) [311020004]; Science, Technology, and Innovation Commission of Shenzhen Municipality [JCYJ20190812155805559]; Research Support Project of Shenzhen Institute of Information Technology [SZIIT2022KJ074]	Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai); Science, Technology, and Innovation Commission of Shenzhen Municipality; Research Support Project of Shenzhen Institute of Information Technology	The present work was supported by the Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (No. 311020004), the Science, Technology, and Innovation Commission of Shenzhen Municipality (No. JCYJ20190812155805559), and Research Support Project of Shenzhen Institute of Information Technology (No. SZIIT2022KJ074).	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Pollut.	OCT 1	2022	310								119875	10.1016/j.envpol.2022.119875	http://dx.doi.org/10.1016/j.envpol.2022.119875		AUG 2022	9	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	4U6YR	35926733				2025-03-11	WOS:000858937500005
J	Coussin, V; Penaud, A; Combourieu-Nebout, N; Peyron, O; Schmidt, S; Zaragosi, S; de Vernal, A; Babonneau, N				Coussin, V.; Penaud, A.; Combourieu-Nebout, N.; Peyron, O.; Schmidt, S.; Zaragosi, S.; de Vernal, A.; Babonneau, N.			Distribution of modern dinocysts and pollen in the western Mediterranean Sea (Algerian margin and Gulf of Lion)	MARINE MICROPALEONTOLOGY			English	Article						Western Mediterranean Sea; Gulf of Lion; Algerian margin; Dinoflagellate cysts; Productivity; Fluvial discharge; Upwelling cells; Pollen and spores; Vegetation gradients; Non-pollen palynomorphs	ARBUSCULAR MYCORRHIZAL FUNGI; RECENT MARINE-SEDIMENTS; NORTH-ATLANTIC OSCILLATION; EASTERN ALBORAN-SEA; DARK SEPTATE FUNGI; DINOFLAGELLATE CYSTS; SPATIAL-DISTRIBUTION; INTERMEDIATE-WATER; CARBON EXPORT; RHONE RIVER	The Mediterranean Sea is generally described as an oligotrophic area where primary productivity is limited to a few coastal environments with nutrient-enriched fluvial input. However, several studies have revealed that the hydrology of the western Mediterranean has major seasonal productive patterns linked either to significant riverine input or to seasonal upwelling cells. This study aims to: i) discuss organic microfossils (i.e. pollen and dinoflagellate cyst assemblages, as well as other non-pollen palynomorphs) from two different productive areas of the western Mediterranean Sea, and ii) examine the importance of the interconnections between marine and continental influences responsible for modern palynomorph distributions. Based on 25 samples from the Gulf of Lion (GoL) and Algerian Margin, this study key findings are: i) that GoL marine productivity is driven by the combination of discharge from the Rho<SIC>ne River and seasonal upwelling mechanisms, ii) that the strong pro-ductive pattern of the northern African coast is driven by water density front mixings and related upwelling. These two patterns are discussed in the light of major links that provide a better understanding of the signatures of marine and continental bio-indicators. Typical differences in vegetation across the north-south climate gradient in the western Mediterranean Basin are highlighted by the larger ratio of Euro-Siberian to Mediterra-nean pollen taxa in the northern sector. Synoptic maps also illustrate the complex interactions of environmental drivers determining the distributions of continental and marine palynomorphs in the western Mediterranean Sea.	[Coussin, V.; Penaud, A.; Babonneau, N.] Univ Brest, CNRS, Ifremer, Geoocean,UMR 6538, F-29280 Plouzane, France; [Combourieu-Nebout, N.] HNHP, Dept Pre Hist Museum dHist Naturelle, CNRS, UMR 7194, F-75013 Paris, France; [Peyron, O.] Univ Montpellier, Inst Sci Evolut Montpellier ISEM, CNRS, UMR 5554, F-34095 Montpellier 05, France; [Schmidt, S.; Zaragosi, S.] Univ Bordeaux, CNRS, UMR Environm & Paleoenvironnements Ocean & Contine, UMR 5805, F-33615 Pessac, France; [de Vernal, A.] Univ Quebec Montreal UQAM, Geotop, 201 Ave President Kennedy, Montreal, PQ 338, Canada	Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ifremer; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; University of Quebec; University of Quebec Montreal	Coussin, V (通讯作者)，Univ Brest, CNRS, Ifremer, Geoocean,UMR 6538, F-29280 Plouzane, France.	vincent.coussin@univ-brest.fr	BABONNEAU, Nathalie/F-8034-2012; de Vernal, Anne/D-5602-2013; ZARAGOSI, Sébastien/JXL-2488-2024; Schmidt, Sabine/G-1193-2013; Penaud, Aurelie/F-2485-2011	Schmidt, Sabine/0000-0002-5985-9747; Penaud, Aurelie/0000-0003-3578-4549; Babonneau, Nathalie/0000-0003-1213-0059	Region Bretagne; UBO (University of Brest); French national programme (CNRS) LEFE-EC2CO; 'ISblue' project (Interdisciplinary graduate school for the blue planet) [ANR-17-EURE-0015]; French government under the program Investissements d'Avenir; ANR BRAISE project [ANR-19-CE01-0001-01]; Agence Nationale de la Recherche (ANR) [ANR-19-CE01-0001] Funding Source: Agence Nationale de la Recherche (ANR)	Region Bretagne(Region Bretagne); UBO (University of Brest); French national programme (CNRS) LEFE-EC2CO; 'ISblue' project (Interdisciplinary graduate school for the blue planet); French government under the program Investissements d'Avenir(Agence Nationale de la Recherche (ANR)); ANR BRAISE project(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)); Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	This work was part of a PhD thesis (Coussin V.) financed by the R ' egion Bretagne and UBO (University of Brest). This work was supported by the French national programme (CNRS) LEFE-EC2CO (`DATAPOL'), by the `ISblue' project (Interdisciplinary graduate school for the blue planet; ANR-17-EURE-0015), and was co-funded by a grant from the French government under the program Investissements d'Avenir. We thank the captains, crews and scientific teams of the cruises that collected studied cores: GMO1 (Pierre Cochonat, Bernard Dennielou), GMO2-CARNAC (Nabil Sultan, Michel Voisset), BEACHMED (Catherine Satra Le Bris) and RHOSOS (Serge Bern ' e, Bernard Dennielou). We also thank the Ifremer for access to the sedimentology laboratory and Marion Genet for the sample sharing. We acknowledge the ANR BRAISE project, grant ANR-19-CE01-0001-01, for the funding of the 210Pbxs measurements of the Gulf of Lion sediments. We thank Yannick Miras for his help with the determination of non-pollen palynomorphs and discussion about their ecological signature. 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Micropaleontol.	AUG	2022	175								102157	10.1016/j.marmicro.2022.102157	http://dx.doi.org/10.1016/j.marmicro.2022.102157		AUG 2022	20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	3X8IR		Green Submitted, Bronze			2025-03-11	WOS:000843278800001
J	Matejová, MM; Gedl, P				Matejova, Marina Molcan; Gedl, Przemyslaw			The Orava segment of the Pieniny Klippen Belt: Lithology, structure and stratigraphy based on the organic-walled dinoflagellate cysts (Saris Unit)	GEOLOGICA CARPATHICA			English	Article						Pieniny Klippen Belt; Saris Unit; Orava region; Jurassic black flysch; biostratigraphy; dinoflagellate cysts	WESTERN CARPATHIANS; GEOLOGICAL STRUCTURE; BLACK FLYSCH; SLOVAKIA; TOARCIAN; POLAND; BIOSTRATIGRAPHY; DEFORMATION; EVOLUTION; STRATA	The Pieniny Klippen Belt of the Western Carpathians is built up by Jurassic to Eocene Oravic units, with the saris Subpieniny, and Pieniny Unit on the top. Major emphasis was placed on the dark fine-grained clastic deposits exposed in the vicinity of the villages of Benova Lehota and Revisne (Orava sector of the Pieniny Klippen Belt). Through investigation of palynological material, the age of dark flysch strata was determined as predominantly uppermost Toarcian to Middle Aalenian and affiliated with the Szlachtowa and/or Skrzypny formations, belonging to the saris Unit. The results from the dinoflagellate cysts were supplemented by a structural investigation of the saris Unit. The complicated tectonic evolution of the Pieniny Klippen Belt is documented by intermixing of the soft shale deposits of Jurassic and Cretaceous age and by the presence of folds and cleavages. Based on the acquired data, the D-1 event records a compression with a NE-SW direction and is represented by folds with axial-plane cleavage. The younger D-2 phase is marked by the presence of south-vergent backthrusts, resulting from the ongoing compression and subsequent tilting of the originally north-vergent nappe stack of the Oravic units.	[Matejova, Marina Molcan] Comenius Univ, Fac Nat Sci, Dept Geol & Paleontol, Mlynska Dolina G, Bratislava 84215, Slovakia; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, Res Ctr Krakow, Senacka 1, PL-31002 Krakow, Poland	Comenius University Bratislava; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Matejová, MM (通讯作者)，Comenius Univ, Fac Nat Sci, Dept Geol & Paleontol, Mlynska Dolina G, Bratislava 84215, Slovakia.	marina.matejova@uniba.sk; ndgedl@cyf-kr.edu.pl	Molcan Matejova, Marina/MCY-5588-2025	Molcan Matejova, Marina/0000-0002-5581-279X; Gedl, Przemyslaw/0000-0003-4319-2658	 [APVV-17-0170];  [APVV-0212-12];  [VEGA 1/0435/21]	; ; 	The authors would like to express their gratitude to prof. Dusan Plasienka for his valuable and -constructive comments. The financial support from the scientific projects APVV-17-0170, APVV-0212-12 and VEGA 1/0435/21 is much appreciated. Dr. Edyta Jurewicz, an anonymous reviewer, and Dr. Anna Becker are acknowledged for their constructive comments that helped us to substantially improve the quality of the manuscript.	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Carpath.	AUG	2022	73	4					293	317		10.31577/GeolCarp.73.4.2	http://dx.doi.org/10.31577/GeolCarp.73.4.2			25	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	6M0TK		gold			2025-03-11	WOS:000888590800002
J	Yi, S; Jun, CP; Hong, SW; Choi, J; Kim, JC; Yoo, DG; Lee, GS				Yi, Sangheon; Jun, Chang-Pyo; Hong, Seok-Whi; Choi, Jooah; Kim, Jin Cheul; Yoo, Dong-Geun; Lee, Gwang-Soo			Palynological implications for paleoenvironmental changes over the past 81,000 years on the Jeju Strait shelf, off southwestern Korea	MARINE GEOLOGY			English	Article						Pollen; Dinoflagellate cyst; Late Quaternary; Jeju Strait shelf; South Korea	SOUTHEASTERN YELLOW-SEA; LATE PLEISTOCENE; ASIAN MONSOON; SURFACE SEDIMENTS; HIGH-RESOLUTION; RIVER SEDIMENT; POLLEN RECORD; MUD DEPOSITS; SOUTH-KOREA; SAND RIDGES	Age-controlled palynostratigraphy has revealed changes in the depositional environment, vegetation, and climate of the southwestern Korean Peninsula since marine isotope stage (MIS) 5a. During MIS 5a (ca. 74-81 ka), the Jeju Strait shelf was an inner shelf with deposition influenced by the Jeju Warm Current (JWC), surrounded by land covered by mixed conifer and deciduous broadleaf forests under warm temperate conditions. The paleoenvironment during MIS 4 (57-71 ka) remains unknown due to a lack of palynomorphs from this stage. During mid-late MIS 3 (ca. 29-50 ka), the Jeju Strait shelf was an inner shelf influenced by cold-water masses from the Korean Coastal Current combined with weaker influences by the JWC, and the surrounding land was covered by mixed conifer and deciduous broadleaf forests that were less dense than in MIS 5a under warm and relatively dry conditions. A cold, slightly wet climate during MIS 2 (ca. 12-29 ka) led to the extension of pre-dominantly cold-tolerant conifer forests due to lowstand sea levels, although inland East Asia remained cold and dry. During MIS 1 (ca. 0-12 ka), cold-tolerant conifer forests persisted into the early Holocene, and were sub-sequently replaced by mixed conifer and deciduous broadleaf forests as a warm climate was restored in the mid-late Holocene, when the depositional environment became an outer shelf due to highstand sea levels, as it remains today.	[Yi, Sangheon; Hong, Seok-Whi; Kim, Jin Cheul; Yoo, Dong-Geun; Lee, Gwang-Soo] Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea; [Yi, Sangheon; Kim, Jin Cheul; Yoo, Dong-Geun] Univ Sci & Technol UST, Daejeon 34113, South Korea; [Jun, Chang-Pyo] Chonnam Natl Univ, Gwangju 61186, South Korea; [Choi, Jooah] Tourism Planning & Dev Off, Kangnung 24040, Gangwon Do, South Korea	Korea Institute of Geoscience & Mineral Resources (KIGAM); University of Science & Technology (UST); Chonnam National University	Yi, S (通讯作者)，Korea Inst Geosci & Mineral Resources, Daejeon 34132, South Korea.; Jun, CP (通讯作者)，Chonnam Natl Univ, Gwangju 61186, South Korea.	shyi@kigam.re.kr; cpjun@jnu.ac.kr	Kim, Jin-Soo/AAF-3359-2019; Yi, Sangheon/D-4780-2011	Jun, Chang-Pyo/0000-0002-6626-7918	Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Oceans and Fisheries of Korea [NP2016-030]; KIGAM - Ministry of Science and ICT of Korea [GP2020-003]; Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Oceans and Fisheries of Korea [NP2016-030, GP2020-003]; KIGAM [NP2016-030]; Ministry of Science and ICT of Korea;  [NP2018-018]	Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Oceans and Fisheries of Korea; KIGAM - Ministry of Science and ICT of Korea; Korea Institute of Geoscience and Mineral Resources (KIGAM) - Ministry of Oceans and Fisheries of Korea; KIGAM; Ministry of Science and ICT of Korea; 	This research was supported by research grants (NP2016-030 and part of NP2018-018) from the Korea Institute of Geoscience and Mineral Resources (KIGAM), funded by the Ministry of Oceans and Fisheries of Korea, and in part by basic research grants (GP2020-003) from the KIGAM, funded by the Ministry of Science and ICT of Korea. 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Geol.	SEP	2022	451								106876	10.1016/j.margeo.2022.106876	http://dx.doi.org/10.1016/j.margeo.2022.106876		AUG 2022	20	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	3S2UV					2025-03-11	WOS:000839457400004
J	Mansour, A; Wagreich, M; Ahmed, MS; Tahoun, SS; Gentzis, T				Mansour, Ahmed; Wagreich, Michael; Ahmed, Mohamed S.; Tahoun, Sameh S.; Gentzis, Thomas			Short-Term Sea-Level Changes and Sequence Stratigraphy of the Mid-Cretaceous Kharita Formation Reservoirs in Egypt: Insights from Geochemical and Palynological Data	ACS OMEGA			English	Article							NORTHERN WESTERN DESERT; ABU GHARADIG BASIN; DINOFLAGELLATE DIVERSITY; HEMIPELAGIC CARBONATES; ORGANIC PETROLOGY; OIL-FIELD; PALYNOFACIES; SYSTEMS; WELL; BOREHOLE	Widespread deposition of siliciclastic sediments with consequent alternations between fine-grained siltstones and shales versus coarse-grained sandstones in the north Western Desert of Egypt provides an archive for mid-Cretaceous sea-level oscillations. This study presents elemental geochemical data as well as palynofacies and palynomorph components of upper Albian reservoirs in the Abu Gharadig Basin, north Western Desert. During the mid-Cretaceous, the studied area is located in the transition zone between the fluvio-deltaic and shallow marine settings at the southern margin of the Tethys Ocean. Thirty rock cutting samples were collected from the Kharita Formation and analyzed for major and trace elements, total organic carbon, and palynological composition. These data, together with geophysical gamma ray log values and lithological composition, allowed us to reconstruct the changes in relative sea level at this time in the framework of a third-order transgressive-regressive (T-R) sequence stratigraphic model. Palynomorph composition, represented by a fairly diverse assemblage of terrestrial plant spores and pollen grains versus marine dinoflagellate cysts and other microplankton, was employed along with the variation in the particulate organic matter composition. Chemical proxies, including Si, Ti, and often K and Fe, and their ratios normalized to Al, as well as the carbonate content and the Sr/Ca ratio, provided significant stratigraphic variations with respect to sea-level changes. The above proxies allowed for the subdivision of the studied reservoir intervals into three T-R sequences.	[Mansour, Ahmed] Minia Univ, Dept Geol, Fac Sci, Al Minya 61519, Egypt; [Wagreich, Michael] Univ Vienna, Fac Earth Sci Geog & Astron, Dept Geol, A-1090 Vienna, Austria; [Ahmed, Mohamed S.] King Saud Univ, Dept Geol & Geophys, Coll Sci, POB 2455, Riyadh 11451, Saudi Arabia; [Tahoun, Sameh S.] Cairo Univ, Dept Geol, Fac Sci, Giza 12613, Egypt; [Gentzis, Thomas] Core Labs Inc, Houston, TX 77040 USA	Egyptian Knowledge Bank (EKB); Minia University; University of Vienna; King Saud University; Egyptian Knowledge Bank (EKB); Cairo University	Mansour, A (通讯作者)，Minia Univ, Dept Geol, Fac Sci, Al Minya 61519, Egypt.	ahmedmans48@mu.edu.eg	Wagreich, Michael/D-2279-2013; Mansour, Ahmed/AAR-4969-2020; Ahmed, Mohamed/GQP-1116-2022	Gentzis, Thomas/0000-0003-4592-9318; Wagreich, Michael/0000-0002-8828-0857; Mansour, Ahmed/0000-0003-2466-7494; Ahmed, Mohamed/0000-0001-9249-6231	Egyptian General Petroleum Corporation (EGPC) in Cairo, Egypt; Researchers Supporting project, King Saud University, Riyadh, Saudi Arabia [RSP2022R455]	Egyptian General Petroleum Corporation (EGPC) in Cairo, Egypt; Researchers Supporting project, King Saud University, Riyadh, Saudi Arabia	We thank the Egyptian General Petroleum Corporation (EGPC) in Cairo, Egypt, for the permission to obtain cutting rock samples and electrical and composite logs of the studied interval from Bedr-Eldin Petroleum Company. This work was funded by Researchers Supporting project number (RSP2022R455) , King Saud University, Riyadh, Saudi Arabia. We thank two anonymous reviewers who provided insightful comments that enhanced this manuscript. We would express our sincere gratitude to Krishna Ganesh (Coeditor of ACS Omega) and Mohamed Mahmoud (Associate Editor) for the way of handling the original and revised copies of the paper.	Alsharhan AS, 2008, J PETROL GEOL, V31, P191, DOI 10.1111/j.1747-5457.2008.00416.x; [Anonymous], 1984, SEPM Society for. Sed. Geol.; [Anonymous], 1992, Western Desert, oil and gas fields (A comprehensive overview), P431; Batten D. J., 1999, FOSSIL PLANTS SPORES, P194; Bayoumi T., 1994, P EG GEN PETR CORP 1, P351; Bowen D. 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J	Ingrams, S; Jolley, DW; Schneider, S				Ingrams, Stephen; Jolley, David W.; Schneider, Simon			Sequence stratigraphy and microplankton palaeoenvironmental dynamics across the Jurassic-Cretaceous transition in the Canadian Arctic	EARTH AND ENVIRONMENTAL SCIENCE TRANSACTIONS OF THE ROYAL SOCIETY OF EDINBURGH			English	Article						Berriasian; palynology; Sverdrup Basin; Tithonian; Valanginian	SVERDRUP BASIN; WESTERN INTERIOR; CYST; BIOSTRATIGRAPHY; ASSEMBLAGES; CALIBRATION; SUCCESSION; STRATEGIES; SECTION; MIDDLE	The Jurassic to Cretaceous strata exposed in the Rollrock Section, Sverdrup Basin, Arctic Canada, represent one of the northernmost continuous outcrops spanning this poorly understood transition. The Oxfordian-Valanginian mudstones of the Rollrock Section were deposited in a shallow marine environment and, as such, provide the ideal lithology to investigate the response of high latitude dinoflagellate cyst populations to the frequent environmental perturbations of this time. Using a multivariate statistical approach, distinct palaeoecologically significant groups are identified and directly linked to time and palaeoenvironments, allowing for the reconstruction of underlying long term palaeoenvironmental trends. These palaeoenvironmental trends are identified to be driven by sequence stratigraphic cycles. For the first time, fourth order sequences are recorded from this pivotal period in the Sverdrup Basin and reveal an additional level of short term climatic events that complicate the identification of long term trends. The relationship existing between marine phytoplankton and climate is utilised to decipher the interplay of long-term and short-term climate fluctuations, distinguishing them from evolutionary trends. Two groups of dinoflagellate cysts, identified by process morphology, are recorded to act as environmental proxies. High percentages of proximochorate dinoflagellate cysts, such as Trichodinium erinaceoides, indicate more proximal, high energy, nutrient rich conditions and are dominant in fourth order transgressive systems tracts. High percentages of chorate dinoflagellate cysts, such as Oligosphaeridium complex, signify distal, low energy, nutrient depleted conditions and are dominant in fourth order highstand systems tracts.	[Ingrams, Stephen; Jolley, David W.] Univ Aberdeen, Kings Coll, Sch Geosci, Dept Geol & Geophys, Aberdeen AB24 3UE, Scotland; [Schneider, Simon] Cambridge Arctic Shelf Programme, West Bldg,Madingley Rd, Cambridge CB3 0UD, England	University of Aberdeen; University of Cambridge	Ingrams, S (通讯作者)，Univ Aberdeen, Kings Coll, Sch Geosci, Dept Geol & Geophys, Aberdeen AB24 3UE, Scotland.	r01si18@abdn.ac.uk		Jolley, David/0000-0003-0909-2952; Ingrams, Stephen/0000-0003-2610-8135	CASP	CASP	The authors thank the following people and institutions for their valuable support: Sylvie LeBlanc (Department of Culture and Heritage, Iglooik, Canada); Jane Chisholm and rangers of Parks Canada (Iqaluit and Tanquary Camp, Canada); John Innis (Universal Helicopters); and the staff of Polar Continental Shelf Programme at Resolute Bay (Canada). Fellow geologists Berta Lopez-Mir and Peter Hulse (both Cambridge Arctic Shelf Programme (CASP), Cambridge, UK) participated in fieldwork in 2015. The help of field assistant Alex Chavanne (California, USA) with logging and sampling the Rollrock Section was instrumental. Dave Bodman of MB Stratigraphy Ltd. (Sheffield, UK) prepared part of the palynological slides used in this study. CASP's industry sponsors are acknowledged for their funding of the Canadian Arctic Islands Project. The authors also thank reviewers James Riding (British Geological Survey, Nottingham, UK) and an unknown second reviewer, for their constructive criticism of this paper and the Earth and Environmental Science Transactions of the Royal Society of Edinburgh editorial office.	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Sci. Trans. R. Soc. Edinb.	SEP	2022	113	3					159	174	PII S1755691022000081	10.1017/S1755691022000081	http://dx.doi.org/10.1017/S1755691022000081		JUL 2022	16	Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	8B3TT		hybrid, Green Published			2025-03-11	WOS:000832491500001
J	Zonneveld, KAF; Grotheer, H; Versteegh, GJM				Zonneveld, Karin A. F.; Grotheer, Hendrik; Versteegh, Gerard J. M.			Dinoflagellate cysts production, excystment and transport in the upwelling off Cape Blanc (NW Africa)	FRONTIERS IN MARINE SCIENCE			English	Article						dinoflagellate cysts; fluxes; succession; excystment; dispersal; ecology; upwelling	SEDIMENT TRAP; ENVIRONMENTAL-CHANGE; SEASONAL PRODUCTION; SINKING VELOCITY; RESTING CYSTS; COASTAL; VARIABILITY; DIATOM; HARMFUL; BLOOMS	To extend the understanding of dinoflagellate cysts production, excystment and vertical/lateral transport in the water column, we compared upper water cyst export production with cysts associations and concentrations in the subsurface nepheloid layer, bottom nepheloid layer and deeper water column during active upwelling off Cape Blanc (NW Africa) in August 2020. Export production was collected by two drifting trap surveys; DTS1 in an active upwelling cell for 4 days and DTS2 in an offshore drifting upwelling filament for 2 days. Subsurface, bottom nepheloid layers and deeper waters were sampled by in-situ pumps along two transects perpendicular to the shelf break. During DTS1, light limitation hampered phytoplankton production which might have influenced cyst production negatively due to up- and downward movement of water masses. Cyst export production increased at the rim of the upwelling cell. For DTS2, upwelling filament cyst export production was up to 3 times lower than that of DTS1. Echinidinium delicatum had highest relative and absolute abundances in the active upwelling, Echinidinium zonneveldiae and Bitectatodinium spongium in the upwelling filament, and Impagidinium spp. and cysts of Gymnodinium microreticulatum/nolleri at the most distal stations. Comparison of concentrations of cysts with and without cell contents showed that the majority of cysts hatched before reaching deeper waters and displayed a dormancy period of less than 6 days. About 5% of the living cysts reached deeper waters and/or the ocean floor. Living cysts were transported offshore in the upwelling filament. In case ships exchange ballast waters in the studied region, they will take up laterally transported living cysts. Upon release of the ballast waters in the port of arrival, these cysts have the potential to become "invader species" that can threaten economy and/or health. Lateral transport of cysts was observed in the bottom nepheloid layer and in deeper waters (800 - 1200m depth) with a maximal extension of about 130km off the shelf break. Therefore, sediments in the region will contain a mixture of regionally and locally produced dinoflagellate cysts. This insight contributes to the improvement of environmental reconstructions of the Cape blanc upwelling system based on downcore cyst associations.	[Zonneveld, Karin A. F.; Grotheer, Hendrik; Versteegh, Gerard J. M.] Univ Bremen, Ctr Marine Environm Sci, MARUM, Bremen, Germany; [Zonneveld, Karin A. F.] Univ Bremen, Geosci Dept, Bremen, Germany; [Grotheer, Hendrik; Versteegh, Gerard J. M.] Helmholtz Zent Polar & Meeresforsch, Alfred Wegener Inst, Marine Geochem, Bremerhaven, Germany; [Versteegh, Gerard J. M.] Jacobs Univ Bremen, Dept Phys & Earth Sci, Bremen, Germany	University of Bremen; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Jacobs University	Zonneveld, KAF (通讯作者)，Univ Bremen, Ctr Marine Environm Sci, MARUM, Bremen, Germany.; Zonneveld, KAF (通讯作者)，Univ Bremen, Geosci Dept, Bremen, Germany.	kzonneveld@marum.de	Versteegh, Gerardus/H-2119-2011; Grotheer, Hendrik/IST-3434-2023		Deutsche Forschungsgemeinschaft [GPF 18-1_18]; MARUM Cluster of Excellence "The Ocean Floor - Earth's Uncharted Interface"	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); MARUM Cluster of Excellence "The Ocean Floor - Earth's Uncharted Interface"	The expedition was funded by the Deutsche Forschungsgemeinschaft GPF 18-1_18. The financial support in the form of scholarships and positions of participants of the cruise was provided by the Deutsche Forschungsgemeinschaft GPF 18-1_18 and the MARUM Cluster of Excellence "The Ocean Floor - Earth's Uncharted Interface".	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Mar. Sci.	JUL 26	2022	9								915755	10.3389/fmars.2022.915755	http://dx.doi.org/10.3389/fmars.2022.915755			21	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	3Q6PJ		gold			2025-03-11	WOS:000838350400001
J	Agharanya, PU; Ekwenye, OC; Okogbue, CO; Mode, AW; Okeke, KK				Agharanya, P. U.; Ekwenye, O. C.; Okogbue, C. O.; Mode, A. W.; Okeke, K. K.			Stratigraphic palynology and micropaleontological study of the Cretaceous-Paleogene succession of the Nani-1 well of the Anambra and Niger Delta basins: Implications for hydrocarbon exploration	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynostratigraphy; Biozonation; Depositional environment; Sequence stratigraphy; Cretaceous-Paleogene boundary; Anambra Basin; Niger Delta	PALYNOFACIES; SEDIMENTS; PALYNOSTRATIGRAPHY; PALEOCENE	Integrated palynological and micropaleontological analyses were carried out on the Nani-1 well drilled into the Anambra and Niger Delta basins of Nigeria. The study is aimed at reconstructing biozones and paleoenviron-ments of deposition, as well as deducing the sequence stratigraphic framework of the Cretaceous-Paleogene successions of an area containing key elements for hydrocarbon exploration. Encountered lithofacies succes-sion of sandstone, siltstone, dark-grey to black shale, and coal beds comprises six lithostratigraphic units, namely the Nkporo Group (Campanian-Maastrichtian), Mamu Formation (Middle Maastrichtian), Ajali Formation (Middle-Late Maastrichtian), Nsukka Formation (Late Maastrichtian), Imo Formation (Danian-Thanetian) and Ameki Group (Eocene). Fourteen dinoflagellate zones (A-N) and seven pollen and spore subzones (A1-G1) are recognized based on the first occurrence of two or more species. Two major stratigraphic events are documented: (1) dinoflagellate cyst (dinocyst) zone G at 880 m depth marked by first appearance ofDanea aff. californica and Danea cf. mutabilis in association with Cordosphaeridium fibrospinosum, and the last occurrence of Danea aff. californica and Phelodinium magnificum place the Cretaceous-Paleogene (K/Pg) boundary in the lowermost part of the Imo Formation; and (2) a hiatus characterized by a starved section observed at 380 m directly overlain by the Early Eocene assemblages of the Ameki Group indicates a sequence boundary at Imo/Ameki Boundary. Thus, a chronostratigraphic chart is developed for parts of the Anambra Basin and the Niger Delta. Six depositional environments which include marginal to shallow marine, marshy lagoon to estuarine, shallow neritic and tidally influenced fluvial channel are identified, and palynostratigraphic evidences indicate that fresh water paly-nomorphs are present in the Lower Maastrichtian strata. Four sequence boundaries and four maximum flooding surfaces are also identified within the Maastrichtian-Early Eocene sediments. The paleoenvironmental recon-struction shows that possible hydrocarbon reservoirs in the basin are the marine sandstone facies of the Nkporo Group and Mamu Formation. Their shale members constitute potential source rocks, while the overlying shale units of the Nsukka and Imo formations may provide regional seals for hydrocarbon habitation.	[Agharanya, P. U.; Ekwenye, O. C.; Okogbue, C. O.; Mode, A. W.; Okeke, K. K.] Univ Nigeria, Dept Geol, Nsukka, Nigeria	University of Nigeria	Ekwenye, OC (通讯作者)，Univ Nigeria, Dept Geol, Nsukka, Nigeria.	ogechi.ekwenye@unn.edu.ng			Petroleum Technology Development Fund (PTDF)	Petroleum Technology Development Fund (PTDF)	The authors are grateful to the Petroleum Technology Development Fund (PTDF) for funding this research and providing other assistance needed for the work. We also acknowledge the oilcompanies that pro-vided the well-logs and biostratigraphic data used for this study and are equally indebted to the editor and the reviewers for their constructive criticisms, suggestions and reviews, which helped to bring out the best of this paper.	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Min. Geol., V43, P147; Vail P.R., 1991, INTEGRATED APPROACH, V61, P630; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams G.L., 1975, GEOL SURV CAN B, V236, P1; WILLIAMS GL, 1966, BRIT MUSEUM NATURAL, V3, P182; Williams GL., 1977, American Association of Stratigraphic Palynologists Contribution Series A, V5, P14; Williams Graham L., 2017, AASP Contributions Series, V48, P1	102	3	3	2	6	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1464-343X	1879-1956		J AFR EARTH SCI	J. Afr. Earth Sci.	NOV	2022	195								104637	10.1016/j.jafrearsci.2022.104637	http://dx.doi.org/10.1016/j.jafrearsci.2022.104637		JUL 2022	19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	5C0ZG					2025-03-11	WOS:000863995700003
J	Balaji-Prasath, B; Wang, Y; Su, YP; Lin, H; Feng, SL; Zheng, LW				Balaji-Prasath, Barathan; Wang, Ying; Su, Yu Ping; Lin, Hong; Feng, Shenglin; Zheng, Luwei			Distribution of dinoflagellate cysts in the modern sediments from the coastal aquaculture area and its adjacent oceanic shelf in southeast China	REGIONAL STUDIES IN MARINE SCIENCE			English	Article						Dinoflagellate cysts; Toxic species and heterotrophic; Surface sediment	ALEXANDRIUM-CATENELLA; SPATIAL-DISTRIBUTION; SURFACE SEDIMENTS; RESTING CYSTS; EAST-COAST; SEA; ASSEMBLAGES; HARBOR; BLOOM; GULF	Changes in nutrient loading due to coastal aquaculture and the targeted expansion of monitoring programs over the past few decades have amply demonstrated a marked increase in harmful algal blooms (HABs). In this study, viable dinoflagellate cyst composition and assemblages were investigated by evaluating and classifying their distribution patterns in surface sediments of the Fujian aquaculture coastal region of southeast China. The surface sediment at 5 stations during the spring and summer of 2019 to classify the dinoflagellate cysts present and identified 36 species representing six known and three uncertain taxa groups. The highest cyst was recorded at coastal station P11 in the spring (744.7 cysts g(-1) DW), while the lowest cyst was observed at coastal station P5 in spring (50.9 cysts g(-1) DW). The number and abundance of the heterotrophic species were greater than the autotrophic species, with the highest species volume belonging to the protoperidinioid group. We also detected potentially harmful algae bloom cysts that hold the potential to form their initial blooms in the sediments. It is important to note that six dinoflagellate cysts were found in the waters along the Fujian coast, as compared to historical data. Although the abundance of these cysts was not high, their presence indicates a potentially grave risk for toxic red tides. More alarmingly, these results suggest that seedbeds may trigger future blooms and outbreaks of toxic species in the present study area. (C) 2022 Elsevier B.V. All rights reserved.	[Balaji-Prasath, Barathan; Wang, Ying; Su, Yu Ping; Lin, Hong; Feng, Shenglin; Zheng, Luwei] Fujian Normal Univ, Coll Environm Sci & Engn, Fuzhou 350007, Peoples R China; [Balaji-Prasath, Barathan; Su, Yu Ping] Fujian Key Lab Pollut Control & Resource Recyclin, Fuzhou 350007, Peoples R China; [Balaji-Prasath, Barathan; Su, Yu Ping] Fujian Prov Res Ctr River & Lake Hlth Assessment, Fuzhou 350007, Peoples R China	Fujian Normal University	Su, YP (通讯作者)，Fujian Normal Univ, Coll Environm Sci & Engn, Fuzhou 350007, Peoples R China.	ypsu@fjnu.edu.cn	Su, Yu-Ping/J-7534-2012; Barathan, Balaji Prasath/AAE-3189-2022	Barathan, Dr. Balaji Prasath/0000-0001-7896-2208; Feng, Shenglin/0000-0002-6898-8022	National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation'' [2016YFE0202100]; Marine Red Tide Early Warning and Prevention in Pingtan coastal area [PT2021006]	National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation''; Marine Red Tide Early Warning and Prevention in Pingtan coastal area	This study was supported by National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation'' (2016YFE0202100) and Marine Red Tide Early Warning and Prevention in Pingtan coastal area (PT2021006). We also thank the crew of the research vessel china Marine Surveillance 203; and the chief Lirong Song for his organization during the cruises.	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Stud. Mar. Sci.	SEP	2022	55								102502	10.1016/j.rsma.2022.102502	http://dx.doi.org/10.1016/j.rsma.2022.102502		JUL 2022	11	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	4F0YQ					2025-03-11	WOS:000848242500003
J	Guerrero-Murcia, LA; Helenes, J; di Pasquo, M; Martin, J				Guerrero-Murcia, Luis-Andres; Helenes, Javier; di Pasquo, Mercedes; Martin, James			Dinoflagellate cysts from the Upper Cretaceous (Campanian-Maastrichtian) from The Naze Peninsula, James Ross Island, Antarctica	CRETACEOUS RESEARCH			English	Article						Dino flagellates cysts; Biostratigraphy; Paleoecology; Antarctic Peninsula; Paleoproductivity	SEYMOUR-ISLAND; PALYNOLOGICAL EVIDENCE; SURFACE SEDIMENTS; CAPE LAMB; STRATIGRAPHY; QUATERNARY; VEGETATION; SALINITY; AREA; ICE	We present the results of the quantitative and qualitative study of dinoflagellate cysts in outcrop samples from a section of the Snow Hill Island Formation (SHF) in James Ross Island, Antarctic. Dinoflagellate cysts assemblages are abundant and dominated by gonyaulacoid taxa. The last occurrence of the dino-flagellate cyst Kallosphaeridium? helbyi and Chatangiella granulifera, together with the first occurrence of Pterodinium cretaceum, indicates a probable late Campanian age (-76.4--72.1 Ma) for the lower strata. Whereas the first occurrence of Manumiella bertodano and the last occurrence of Odontochitina oper-culata, Xenascus ceratioides, and Stiphrosphaeridium anthophorum indicate an early Maastrichtian (-72.1--70.0 Ma) age for the upper strata. Our results, combined with paleobotanical and palynological published data, indicate medium-high continental and marine productivity with temperate paleo-climate free of glaciers for this interval. Lithological and paleontological data indicate mainly inner neritic marine depositional environments. The predominance of shales in the lower part of the lower Maas-trichtian interval indicates a slightly deeper environment. In contrast, in the middle part of the lower Maastrichtian, a shallower, transitional environment is marked by the presence of theropod dinosaurs and decapod crustaceans.& COPY; 2022 Elsevier Ltd. All rights reserved.	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Res.	JAN	2023	141								105367	10.1016/j.cretres.2022.105367	http://dx.doi.org/10.1016/j.cretres.2022.105367		JUL 2022	14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	L9TG8					2025-03-11	WOS:001026618300001
J	Gruetzner, J; Matthiessen, J; Geissler, WH; Gebhardt, AC; Schreck, M				Gruetzner, Jens; Matthiessen, Jens; Geissler, Wolfram H.; Gebhardt, A. Catalina; Schreck, Michael			A revised core-seismic integration in the Molloy Basin (ODP Site 909): Implications for the history of ice rafting and ocean circulation in the Atlantic-Arctic gateway	GLOBAL AND PLANETARY CHANGE			English	Article						Fram Strait; Arctic Ocean; Seismic reflections; Ocean Circulation; Stratigraphy; Neogene; ODPSite909	DEEP-WATER CIRCULATION; BARENTS SEA MARGIN; NORTHERN NORTH-ATLANTIC; LATE CENOZOIC EROSION; CENTRAL FRAM STRAIT; EAST GREENLAND; MIDDLE MIOCENE; DINOFLAGELLATE CYST; LATE PLIOCENE; ACRITARCH BIOSTRATIGRAPHY	Today's cryosphere reflects an extreme climate state that developed through stepwise global Cenozoic cooling. In this context the opening of the Fram Strait, the Atlantic-Arctic Gateway (AAG), enabled deep-water exchange between the northern North Atlantic and the Arctic Ocean and thereby influenced global ocean circulation and climate.Here we present a new age model for Ocean Drilling Program Site 909 located in the Molloy Basin, a key site to investigate the late opening phase of the central Fram Strait and the early history of oceanic circulation in the AAG. Our results are based on a revised magnetostratigraphy calibrated by new palynomorph bioevents, which shifts previously used stratigraphies for Site 909 to significantly younger ages in the time interval from c. 15 Ma to 3 Ma. The revised late Miocene to present chronology combined with an improved core-log-seismic integration leads to a new high-resolution seismic stratigraphy for the central Fram Strait that allows a more comprehensive correlation with seismic markers from the western Barents Sea margin and also the adjacent Yermak Plateau. The new stratigraphy implies that prominent maxima in coarse sand particles and kaolinite, often interpreted as evidence for ice rafting in the Fram Strait occur at c. 10.8 Ma, c. 3 Myr later as previously inferred and thus well after the Middle Miocene Climate Transition (c. 15-13 Ma). In the late Tortonian (<7.5 Ma), sediment transport became current controlled, mainly through a western, recirculating branch of the West Spitsbergen Current. This transport was strongly enhanced between c. 6.4 and 4.6 Ma and likely linked to the subsiding Hovgaard (Hovgard) Ridge and the widening of the AAG.Late Pliocene to Pleistocene seismic reflectors correlate with episodes of elevated ice-rafted detritus input related to major steps in Northern Hemisphere ice sheet growth such as the prominent glacial inception MIS M2 that predates the mid-Piacenzian Warm Period and the intensification of Northern Hemisphere glaciation starting at c. 2.7 Ma. At the beginning of the Mid Pleistocene Transition (c. 1.2-0.8 Ma), sediment accumulation in the Fram Strait significantly decreased.	[Gruetzner, Jens; Matthiessen, Jens; Geissler, Wolfram H.; Gebhardt, A. Catalina; Schreck, Michael] Alfred Wegener Inst Helmholtz, Zent Polar & Meeresforschung, Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Gruetzner, J (通讯作者)，Alfred Wegener Inst Helmholtz, Zent Polar & Meeresforschung, Bremerhaven, Germany.	jens.gruetzner@awi.de	Gebhardt, Catalina/AHI-6432-2022	Gruetzner, Jens/0000-0001-5445-2393; Geissler, Wolfram/0000-0001-6807-555X	Deutsche Forschungsgemeinschaft (DFG) [GEI 1783/6-1]; Open Access Publication Funds of Alfred-Wegener-Institut Helmholtz-Zentrum fur Polarund Meeresforschung	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); Open Access Publication Funds of Alfred-Wegener-Institut Helmholtz-Zentrum fur Polarund Meeresforschung	Funding was provided by the Deutsche Forschungsgemeinschaft (DFG) under contract GEI 1783/6-1. Support by the Open Access Publication Funds of Alfred-Wegener-Institut Helmholtz-Zentrum fur Polarund Meeresforschung is acknowledged. The authors would like to thank Emerson E&P Software, Emerson Automation Solutions, for providing licenses for the seismic software Paradigm in the scope of the Emerson Academic Program. Constructive comments from three anonymous reviewers helped to improve the manuscript.	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Planet. Change	AUG	2022	215								103876	10.1016/j.gloplacha.2022.103876	http://dx.doi.org/10.1016/j.gloplacha.2022.103876		JUL 2022	20	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	3B7XX		Green Published, hybrid			2025-03-11	WOS:000828150900001
J	Kietzmann, DA; Llanos, MPI; Iovino, F				Kietzmann, Diego A.; Llanos, Maria Paula Iglesia; Iovino, Franco			Tithonian-Berriasian calcisphere (calcareous dinoflagellate cysts) zones in the Neuquen Basin, Argentina: correlation between Southern Andes and Tethyan regions	NEWSLETTERS ON STRATIGRAPHY			English	Article						calcareous dinoflagellate cysts; biostratigraphy; Vaca Muerta Formation; Jurassic/Cretaceous boundary	JURASSIC-CRETACEOUS BOUNDARY; VACA MUERTA FORMATION; CARBONATE RAMP; MENDOZA AREA; SOURCE-ROCK; CALPIONELLIDS; STRATIGRAPHY; CARPATHIANS; BIOSTRATIGRAPHY; SUCCESSION	This work presents a regional biostratigraphic study on the calcisphere (calcareous dinoflagellate cysts) zones of the Tithonian-Berriasian in the Neuquen Basin, Western Argentina. This stratigraphic interval is mostly represented by a thick rhythmic succession of marlstone and limestone, with an abundant fossil content and a remarkable stratigraphic continuity along several hundred meters, known as Vaca Muerta Formation. This formation was originated in distal hemipelagic setting of a carbonate ramp and is one of the most important unconventional hydrocarbon reservoirs in the world. The detailed study of six stratigraphic sections, allowed the elaboration of a reliable biostratigraphic scheme and its correlation with Andean ammonites, calpionellids, and polarity zones. Calcareous dinoflagellate cysts within the Vaca Muerta Formation are moderately preserved. Despite that, twenty-nine species and nine biozones have been identified: Committosphaera pulla, Parastomiosphaera malmica, Colomisphaera tenuis, Colomisphaera fortis, Stomiosphaerina proxima, Stomiosphaera wanneri, Colomisphaera vogleri and Colomisphaera conferta. These results allow to contribute to an increasingly solid chronostratigraphic framework in the Neuquen Basin.	[Kietzmann, Diego A.; Llanos, Maria Paula Iglesia; Iovino, Franco] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina; [Kietzmann, Diego A.; Llanos, Maria Paula Iglesia] Univ Buenos Aires, CONICET, Inst Geociencias Basicas Ambient & Aplicadas Buen, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina	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, Fac Ciencias Exactas & Nat, Dept Ciencias Geol, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina.; Kietzmann, DA (通讯作者)，Univ Buenos Aires, CONICET, Inst Geociencias Basicas Ambient & Aplicadas Buen, Ciudad Univ,Pabellon II,Intendente Guiraldes 2160, Buenos Aires, DF, Argentina.	diegokietzmann@gl.fcen.uba.ar	Kietzmann, Diego/S-4549-2019	Kietzmann, Diego Alejandro/0000-0003-1222-7811	Agencia Nacional de Promocion Cientifica y Tecnologica, Argentina [PICT 2018-02492]	Agencia Nacional de Promocion Cientifica y Tecnologica, Argentina(ANPCyT)	This research was supported by projects PICT 2018-02492 financed by Agencia Nacional de Promocion Cientifica y Tecnologica, Argentina. We acknowledge YPF and Chevron for publication permission. We are especially indebted to Alberto C. Riccardi (Universidad Nacional de La Plata y Museo, Argentina) for the identification of the ammonite zones from the studied outcropping sections. We especially thank Justyna KowalKasprzyk and Ioan I. Bucur for meticulous and constructive reviews that allowed to significantly improve the original version of the manuscript. We also thank Jochen Erbacher for editorial handling.	Aguirre-Urreta B, 2019, J S AM EARTH SCI, V92, P350, DOI 10.1016/j.jsames.2019.03.019; Aguirre-Urreta M. 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Stratigr.	MAR	2023	56	2					157	185		10.1127/nos/2022/0729	http://dx.doi.org/10.1127/nos/2022/0729		JUL 2022	29	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	Z5AF1					2025-03-11	WOS:000829046200001
J	Brice, C; de Vernal, A; Ivanova, E; van Bellen, S; Van Nieuwenhove, N				Brice, Camille; de Vernal, Anne; Ivanova, Elena; van Bellen, Simon; Van Nieuwenhove, Nicolas			Palynological evidence of sea-surface conditions in the Barents Sea off northeast Svalbard during the postglacial period	QUATERNARY RESEARCH			English	Article						Barents Sea; Sea ice; Salinity; Sea-surface temperature; Holocene	LAST GLACIAL MAXIMUM; FRANZ VICTORIA TROUGH; ICE-SHEET EXTENT; ATLANTIC WATER; DINOFLAGELLATE CYSTS; NORDIC SEAS; PALEOCEANOGRAPHIC EVOLUTION; HOLOCENE PALEOCEANOGRAPHY; NORWEGIAN SEA; FRESH-WATER	Postglacial changes in sea-surface conditions, including sea-ice cover, summer temperature, salinity, and productivity were reconstructed from the analyses of dinocyst assemblages in core S2528 collected in the northwestern Barents Sea. The results show glaciomarine-type conditions until about 11,300 +/- 300 cal yr BP and limited influence of Atlantic water at the surface into the Barents Sea possibly due to the proximity of the Svalbard-Barents Sea ice sheet. This was followed by a transitional period generally characterized by cold conditions with dense sea-ice cover and low-salinity pulses likely related to episodic freshwater or meltwater discharge, which lasted until 8700 +/- 700 cal yr BP. The onset of "interglacial" conditions in surface waters was marked by a major change in dinocyst assemblages, from dominant heterotrophic to dominant phototrophic taxa. Until 4100 +/- 150 cal yr BP, however, sea-surface conditions remained cold, while sea-surface salinity and sea-ice cover recorded large amplitude variations. By similar to 4000 cal yr BP optimum sea-surface temperature of up to 4 degrees C in summer and maximum salinity of similar to 34 psu suggest enhanced influence of Atlantic water, and productivity reached up to 150 gC/m(2)/yr. After 2200 +/- 1300 cal yr BP, a distinct cooling trend accompanied by sea-ice spreading characterized surface waters. Hence, during the Holocene, with exception of an interval spanning about 4000 to 2000 cal yr BP, the northern Barents Sea experienced harsh environments, relatively low productivity, and unstable conditions probably unsuitable for human settlements.	[Brice, Camille; de Vernal, Anne; van Bellen, Simon; Van Nieuwenhove, Nicolas] Univ Quebec Montreal, GEOTOP, CP 8888, Montreal, PQ H3C 3P8, Canada; [Ivanova, Elena; Van Nieuwenhove, Nicolas] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia; [Van Nieuwenhove, Nicolas] Univ New Brunswick, 2 Bailey Dr, Fredericton, NB E3B 5A3, Canada	University of Quebec; University of Quebec Montreal; Russian Academy of Sciences; Shirshov Institute of Oceanology; University of New Brunswick	de Vernal, A (通讯作者)，Univ Quebec Montreal, GEOTOP, CP 8888, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	van Bellen, Simon/AAK-9401-2021; Van Nieuwenhove, Nicolas/IAQ-1532-2023; Ivanova, Elena/B-3775-2016; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Van Nieuwenhove, Nicolas/0000-0001-6369-2751	Fonds de Recherche du Quebec sur la Nature et les Technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada; Russian Federation state [0149-2019-0007]	Fonds de Recherche du Quebec sur la Nature et les Technologies (FRQNT); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Russian Federation state	We thank the scientific party of Cruise 25 of R/V Akademik Nikolaj Strakhov for offering the samples from core S2528. This study was supported by the Fonds de Recherche du Quebec sur la Nature et les Technologies (FRQNT) and the Natural Sciences and Engineering Research Council (NSERC) of Canada (grants to AdV) and by the Russian Federation state (assignment No. 0149-2019-0007 to EI). The laboratory analyses have been made at Geotop. We are grateful to the guest editor, Nicole Mirsati, Manuel Bringue, and one anonymous reviewer of the journal for their critical and constructive comments, which helped to prepare the revised version of the manuscript.	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Res.	JUL	2022	108				SI		180	194	PII S0033589420000022	10.1017/qua.2020.2	http://dx.doi.org/10.1017/qua.2020.2			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	3N7MW					2025-03-11	WOS:000836331500013
J	Vitacca, JJ; Sinclair, N; Mantle, DJ; Marshall, N; Peyrot, D				Vitacca, Jesse J.; Sinclair, Natalie; Mantle, Daniel J.; Marshall, Neil; Peyrot, Daniel			The taxonomy of selected marine microplankton from the Middle and Upper Jurassic (Callovian-Kimmeridgian) of the North West Shelf, Australia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinocysts; Systematics; North West Shelf; Jurassic; Callovian -Kimmeridgian	BAYU-UNDAN FIELD; DINOFLAGELLATE CYST; TIMOR SEA; SEQUENCE STRATIGRAPHY; BONAPARTE BASIN; PALYNOLOGY; PALEOENVIRONMENTS; BIOSTRATIGRAPHY; ACRITARCHS; RADIATION	The palynological assemblages of 134 legacy and 212 new palynological preparations from the Callovian- Kimmeridgian of the North West Shelf of Western Australia, were used to identify new species of dinoflagellate cysts with biostratigraphic utility. Samples were derived from cores and sidewall cores from nine wells; four from the Bonaparte Basin, and five from the Northern Carnarvon Basin. This work describes 11 new species of dinofla-gellate cyst, one species of acritarch, and emends the descriptions of two genera and five species of dinoflagellate cyst. The new forms include: Batiacasphaera elongata, Cleistosphaeridium? oxfordianum, Egmontodinium twiggii, Evansia? rotundata, Jansonia thormalleus, Lanterna foveolata, Lanterna reticulata, Lanterna spongiosa, Orobodinium tantillum, Oligosphaeridium? varifenestratum, and Sepispinula florida, and the acritarch Triovalium attenuatum. Emendations are proposed for the genera Lanterna and Tringadinium, and the species Broomea fusticula, Egmon-todinium toryna, Pyxidiella pandora, Microdinium jurassicum, Jansonia jurassica, and Tringadinium bjaerkei. (c) 2022 Published by Elsevier B.V.	[Vitacca, Jesse J.; Marshall, Neil; Peyrot, Daniel] Univ Western Australia, Sch Earth Sci, Crawley, WA 6009, Australia; [Sinclair, Natalie] Sinclair Siratig Serv, Eltham, Vic 3095, Australia; [Mantle, Daniel J.] MGpalaeo Geol & Stratig Consultants, Malaga, WA 6090, Australia	University of Western Australia	Vitacca, JJ (通讯作者)，Univ Western Australia, Sch Earth Sci, Crawley, WA 6009, Australia.	jesse.vitacca@research.uwa.edu.au	peyrot, Daniel/AAI-6091-2020	Marshall, Neil/0009-0007-6708-9213; peyrot, Daniel/0000-0002-3897-6733	Australian Government Research Training Program Scholarship; American Association of Petroleum Geologists David Worthington Grant	Australian Government Research Training Program Scholarship(Australian GovernmentDepartment of Industry, Innovation and Science); American Association of Petroleum Geologists David Worthington Grant	This research was conducted at the University of Western Australia School of Earth and Environment, supported by an Australian Govern- ment Research Training Program Scholarship. This work represents part of a larger project investigating the palynoflora, palaeoenvironments and stratigraphic successions of the Laminaria High and Vulcan Sub-basin. It incorporates unpublished descriptive observations and plate figures from Dr. Natalie Sinclair's Doctoral Thesis (Sinclair, 2012) . The authors wish to thank the two reviewers of the original manuscript for their feedback which has undoubtedly improved this article. Thanks is given to Assoc. Prof. Peta Clode of the University of Western Australia CMCA for her assistance with the technical aspects of SEM imaging tech- niques. SEM imaging was partially funded by the American Association of Petroleum Geologists David Worthington Grant.	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Palaeobot. Palynology	SEP	2022	304								104668	10.1016/j.revpalbo.2022.104668	http://dx.doi.org/10.1016/j.revpalbo.2022.104668		JUN 2022	31	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	3D9TD					2025-03-11	WOS:000829635300001
J	Wang, ZH; Zhang, YN; Lei, MD; Ji, SH; Chen, JZ; Zheng, H; Tang, YL; Hu, R				Wang, Zhaohui; Zhang, Yuning; Lei, Mingdan; Ji, Shuanghui; Chen, Jiazhuo; Zheng, Hu; Tang, Yali; Hu, Ren			Distribution of Dinoflagellate Cysts in Surface Sediments From the Qingdao Coast, the Yellow Sea, China: The Potential Risk of Harmful Algal Blooms	FRONTIERS IN MARINE SCIENCE			English	Article						dinoflagellate cysts; sediment; harmful algal bloom; Qingdao Coast; the Yellow Sea; biogenic elements	AZADINIUM-POPORUM DINOPHYCEAE; JIAOZHOU BAY; PHYTOPLANKTON; ASSEMBLAGES; EUTROPHICATION; MORPHOLOGY; PHYLOGENY; DIVERSITY; ABUNDANCE; POLLUTION	Surface sediments were collected from three sea areas of the Qingdao coast, the Yellow Sea, China, namely, the inner Jiaozhou Bay, the Laoshan coast, and the Amphioxus Reserve area in November to December 2017. Dinoflagellate cysts were observed in the sediments, focusing on the distribution of toxic and harmful species. Contents of biogenic elements were analyzed to reveal their relationships to cysts. A total of 32 cyst taxa were identified, including 23 autotrophic and 9 heterotrophic taxa. Cyst concentrations ranged from 83.3 to 346.5 cysts/g D Wt with an average of 210.7 cysts/g D Wt. Generally, cysts of autotrophic dinoflagellates dominated in sediments from the Qingdao coast with proportions of 41.05%-90.25%. There were no dominant group in cyst assemblages; cysts of Protoperidiniaceae, Suessiales, and Calciodinelloideae showed similar contributions. Cyst assemblages were quite different in the inner Jiaozhou Bay reflected by the lower species richness, diversity, and cyst concentration. Results from the redundancy analysis (RDA) demonstrated the influence of biogenic elements on cyst assemblages, which explained well why the three sea areas with different degrees of human activities showed different dinocyst storages. Notably, 17 harmful algal bloom (HAB) dinoflagellate cysts were identified in this study, including cysts of those producing toxins that may damage human health and marine animals. Some of these cysts occurred widely and dominantly in this study, such as cysts of Gonyaulax spinifera, Azadinium trinitatum, Scrippsiella acuminata, and Biecheleria halophila, suggesting the potential risk of HABs in the Qingdao coastal area.	[Wang, Zhaohui; Zhang, Yuning; Lei, Mingdan; Ji, Shuanghui; Chen, Jiazhuo; Zheng, Hu; Tang, Yali; Hu, Ren] Jinan Univ, Coll Life Sci & Technol, Dept Ecol, Guangzhou, Peoples R China	Jinan University	Wang, ZH; Tang, YL; Hu, R (通讯作者)，Jinan Univ, Coll Life Sci & Technol, Dept Ecol, Guangzhou, Peoples R China.	twzh@jnu.edu.cn; litangyali@163.com; thuren@jnu.edu.cn						Anderson DM, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; Aydin H, 2015, MAR POLLUT BULL, V94, P144, DOI 10.1016/j.marpolbul.2015.02.038; Balkis N, 2011, J MAR BIOL ASSOC UK, V91, P771, DOI 10.1017/S0025315410000081; Bravo Isabel, 2014, Microorganisms, V2, P11; Castaneda-Quezada R, 2021, J MAR BIOL ASSOC UK, V101, P895, DOI 10.1017/S0025315421000795; Chikwililwa C, 2019, HARMFUL ALGAE, V85, DOI 10.1016/j.hal.2019.101626; Dong YL, 2020, ECOTOX ENVIRON SAFE, V191, DOI 10.1016/j.ecoenv.2020.110226; Dzhembekova N, 2018, BIOTECHNOL BIOTEC EQ, V32, P1507, DOI 10.1080/13102818.2018.1532816; Ellegaard M, 2018, BIOL REV, V93, P166, DOI 10.1111/brv.12338; 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Wang Zhao-hui, 2001, Marine Sciences (Beijing), V25, P47; Wang ZH, 2022, J OCEANOL LIMNOL, V40, P2322, DOI 10.1007/s00343-021-1200-0; Yao P, 2010, ESTUAR COAST SHELF S, V89, P234, DOI 10.1016/j.ecss.2010.07.003; Yu L, 2019, J ENVIRON MANAGE, V232, P499, DOI 10.1016/j.jenvman.2018.11.084; Yu R.C., 2020, OCEANOL LIMNOL SIN, V51, P768, DOI 10.11693/hyhz20200400127; Yuan HM, 2018, CONT SHELF RES, V171, P140, DOI 10.1016/j.csr.2018.11.004; [周健 Zhou Jian], 2020, [海洋环境科学, Marine Environmental Science], V39, P537; Zingone A, 2000, OCEAN COAST MANAGE, V43, P725, DOI 10.1016/S0964-5691(00)00056-9; Zinssmeister C, 2011, SYST BIODIVERS, V9, P145, DOI 10.1080/14772000.2011.586071; Zonneveld KAF, 2015, PALYNOLOGY, V39, P387, DOI 10.1080/01916122.2014.990115; Zou C, 2014, MAR POLLUT BULL, V89, P209, DOI 10.1016/j.marpolbul.2014.09.056	63	7	7	8	57	FRONTIERS MEDIA SA	LAUSANNE	AVENUE DU TRIBUNAL FEDERAL 34, LAUSANNE, CH-1015, SWITZERLAND		2296-7745		FRONT MAR SCI	Front. Mar. Sci.	JUN 22	2022	9								910327	10.3389/fmars.2022.910327	http://dx.doi.org/10.3389/fmars.2022.910327			11	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	3A4MJ		gold			2025-03-11	WOS:000827235600001
J	Singh, VP; Singh, BD; Mathews, RP; Singh, A; Mendhe, VA; Mishra, S; Banerjee, M				Singh, Vikram P.; Singh, Bhagwan D.; Mathews, Runcie P.; Singh, Alpana; Mendhe, Vinod A.; Mishra, Subhashree; Banerjee, Mollika			Paleodepositional and Hydrocarbon Source-Rock Characteristics of the Sonari Succession (Paleocene), Barmer Basin, NW India: Implications from Petrography and Geochemistry	NATURAL RESOURCES RESEARCH			English	Article						Petrography; Palynofacies; Biomarkers; Dinoflagellate cysts; Immature; Gaseous hydrocarbon; Paleocene deposits	GIRAL LIGNITE MINE; WESTERN INDIA; ORGANIC GEOCHEMISTRY; AKLI FORMATION; DEPOSITIONAL ENVIRONMENT; COAL PETROLOGY; SAURASHTRA BASIN; EARLY DIAGENESIS; TIBETAN PLATEAU; TERTIARY COALS	Lignite deposits, associated with Akli Formation (Paleocene), from the Sonari mine of Barmer Basin, Rajasthan, were investigated by applying organic petrography, palynofacies, and geochemistry in order to understand the origin, nature, and character of these lignite-bearing deposits and to assess their thermal maturation and hydrocarbon generation potentiality. The studied samples contained an abundance of huminite group of macerals (av. 54.0 vol.%) and relatively higher abundance of C-27 and C(29)n-alkane hydrocarbons. High carbon preference index (CPI: 5.03-9.44) and high terrigenous aquatic ratio (TAR: 5.09-20.01), together with the liptinite macerals (av. 10.3 vol.%), inform the prevailing contribution of higher plants. Besides, the significant amount of detrohuminites (av. 26.8 vol.%) and non-biostructure phytoclasts (av. 42.25%), along with hopanoids, denote a meaningful herbaceous plants input and/or high level of tissue destruction (bacterial activity). The terpenoid composition was mainly constituted by pentacyclic triterpenoids and A-ring-degraded angiosperm-derived compounds and diterpenoids. The inertinite contents (av. 22.3 vol.%) and the pristane/phytane (Pr/Ph) ratio imply the variation in the redox conditions during the accumulation. The petrographic indices revealed that the paleo-flora were accumulated in a limno-telmatic condition, with fluctuating groundwater level. Likewise, the palynofacies data displayed that the peat was deposited in dysoxic-suboxic settings under proximal condition. Subsequently, the incidence of dinoflagellate cysts in the studied samples suggests a marine intrusion. The considerable total of pyrite (up to 16.7 vol.%, comprising framboidal) suggests a coastal swamp condition (marginal marine). The thermal alteration index (TAI: av. 2.15), T-max (av. 411 degrees C for lignite and 414 degrees C for associated shale) and the gross calorific values (av. 4601 cal/g) showed the immaturity of the studied samples. The lignites contained low to moderate ash yields (av. 12.57 wt.%) and moisture (av. 12.79 wt.%) contents, whereas the carbon(daf) (daf = dry ash-free basis) contents were high (av. 67.22 wt.%) and corroborated well with the inertinite group of macerals. The fuel ratio varied from 0.77 to 1.32. The volatile matter yield(daf) (av. 51.09 wt.%), fixed carbon(daf) (av. 48.91 wt.%), and the oxygen(daf) (av. 22.16 wt.%) contents were moderately high. The total organic carbon contents (TOC: 1.17-54.84 wt.%, av. 24.78 wt.%) and hydrogen index values (HI: 32-361 mg HC/g rock) exhibit that the studied samples mostly have type III kerogen and show an excellent potentiality to generate gaseous hydrocarbons.	[Singh, Vikram P.; Singh, Bhagwan D.; Mathews, Runcie P.; Singh, Alpana] DST Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India; [Mendhe, Vinod A.; Banerjee, Mollika] CSIR Cent Inst Min & Fuel Res, Barwa Rd, Dhanbad 826015, Bihar, India; [Mishra, Subhashree] CSIR Natl Inst Oceanog, Panaji 403004, Goa, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Council of Scientific & Industrial Research (CSIR) - India; CSIR - Central Institute of Mining & Fuel Research (CIMFR); Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Singh, VP (通讯作者)，DST Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	vikram_chauhan@bsip.res.in	Singh, Anoop Kumar/IXR-0763-2023; Singh, Prakash/AAE-6396-2020	SINGH, VIKRAM PARTAP/0000-0002-0136-7918	BSIP (Lucknow) [BSIP/RDCC/23/2021-22]; SERB, Dept. of Science and Technology (Govt. of India) [PDF/2018/000883]	BSIP (Lucknow); SERB, Dept. of Science and Technology (Govt. of India)	The Director, BSIP (Lucknow), is thanked for constant support, encouragement and permitting the publication of this paper (BSIP/RDCC/23/2021-22). Authors are grateful to the officials of Rajasthan State Mines and Minerals Limited (RSMML, Jaipur) and Sonari Lignite Mine Project (Barmer), Govt. of Rajasthan, for their assistance and cooperation during the field work. We acknowledge the help of Dr. Mahesh Shivanna (Ex-BSRA) and Mr. V.P. Singh (Ex-TO) of BSIP during the field visit and laboratory analyses, respectively. We are also thankful to Prof. Suryendu Dutta (Dept. of Earth Science, Indian Institute of Technology Bombay, Mumbai) for extending support for the Rock-Eval pyrolysis and biomarker analyses. VAM and MB are thankful to the Director, CIMFR (Dhanbad), and SM is thankful to the Director, NIO (Goa), for associating with this work. VPS acknowledge SERB, Dept. of Science and Technology (Govt. of India), for granting the National Postdoctoral Fellowship (PDF/2018/000883). We are also grateful to Dr. John Carranza for his editorial support and to all anonymous reviewers for their valuable suggestions and constructive comments that helped us to improve the earlier version of this article.	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Resour. Res.	OCT	2022	31	5					2943	2971		10.1007/s11053-022-10079-y	http://dx.doi.org/10.1007/s11053-022-10079-y		JUN 2022	29	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	4O8FY					2025-03-11	WOS:000811405200002
J	Galasso, F; Feist-Burkhardt, S; Schneebeli-Hermann, E				Galasso, Francesca; Feist-Burkhardt, Susanne; Schneebeli-Hermann, Elke			The palynology of the Toarcian Oceanic Anoxic Event at Dormettingen, southwest Germany, with emphasis on changes in vegetational dynamics	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Early Jurassic; Posidonia Shale Formation; Palynology; T-OAE; Mass extinction	ORGANIC-WALLED PHYTOPLANKTON; EARLY JURASSIC EXTINCTION; OSMIUM ISOTOPE EVIDENCE; EARLY CRETACEOUS FERNS; LUSITANIAN BASIN; SEA-LEVEL; TRIASSIC/JURASSIC BOUNDARY; DINOFLAGELLATE CYSTS; PERMIAN EXTINCTION; POLLEN MORPHOLOGY	The Toarcian Oceanic Anoxic Event (T-OAE; -183 Ma) represents an episode of marine anoxia that lasted for several hundred thousand years. Abiotic factors contributing to the formation of the T-OAE, such as global warming, changes in weathering intensity, or sea-level change, are associated with a marked change in carbon cycling. While these factors are well studied, detailed palynological data, including marine and terrestrial palynomorphs, is still missing. Here we present comprehensive palynological data from the sedimentologically and geochemically well constrained T-OAE section in Dormettingen (SW Germany). Palynological assemblages prior to the T-OAE reflect a mixed gymnosperm-pteridophyte vegetation on land. They also include unseparated spore tetrads and sporomorphs with darkened walls indicative of environmental stress. During the early stage of the T-OAE, gymnosperms decline and only pteridophytes are recorded in the palynological assemblages, terrestrial vegetation recovery commenced before the end of the T-OAE. Contrastingly, dinoflagellate cyst diversity declines significantly in the first stage of the T-OAE and is reduced to zero towards the end of the T-OAE. Our data shows that the terrestrial ecosystems reacted early to the abiotic disturbances reflected in carbon isotope data even before the T-OAE. (c) 2022 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY license (http:// creativecommons.org/licenses/by/4.0/).	[Galasso, Francesca; Schneebeli-Hermann, Elke] Univ Zurich, Palaontol Inst & Museum, Karl Schmid Str 4, CH-8006 Zurich, Switzerland; [Feist-Burkhardt, Susanne] Geol Consulting & Serv, Odenwaldstr 18, D-64372 Ober Ramstadt, Germany; [Feist-Burkhardt, Susanne] Univ Geneva, Dept Earth Sci, 13 Rue Maraichers, Geneva, Switzerland	University of Zurich; University of Geneva	Galasso, F (通讯作者)，Univ Zurich, Palaontol Inst & Museum, Karl Schmid Str 4, CH-8006 Zurich, Switzerland.	francesca.galasso@pim.uzh.ch; feistburkhardt@gmail.com; elke.schneebeli@pim.uzh.ch	Feist-Burkhardt, Susanne/B-1522-2009; Galasso, Francesca/AAH-4005-2021; Schneebeli, Elke/F-4873-2011	Schneebeli, Elke/0000-0002-1552-4785; Feist-Burkhardt, Susanne/0000-0001-6019-6242	Swiss National Science Foundation [200021_175540/1]; Swiss National Science Foundation (SNF) [200021_175540] Funding Source: Swiss National Science Foundation (SNF)	Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); Swiss National Science Foundation (SNF)(Swiss National Science Foundation (SNSF))	We owe many thanks to the Holcim (Suddeutschland) GmbH company (Dotternhausen) for providing access to the quarry and its Head of the Fossil Museum, Dr. Annette Schmid-Rohl, for the precious help and technical support during the data acquisition phase. Furthermore, we would like to thank Editor Prof. Henk Brinkhuis, Dr. Jim Riding, and an anonymous reviewer for the valuable and helpful comments that have improved the manuscript. This work was supported by the Swiss National Science Foundation (project n degrees 200021_175540/1 to Elke Schneebeli-Hermann).	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J	Lambert, O; Wanzenböck, G; Pfaff, C; Louwye, S; Kriwet, J; Marx, FG				Lambert, Olivier; Wanzenboeck, Gerhard; Pfaff, Cathrin; Louwye, Stephen; Kriwet, Juergen; Marx, Felix G.			First eurhinodelphinid dolphin from the Paratethys reveals a new family of specialised echolocators	HISTORICAL BIOLOGY			English	Article						Odontoceti; cochlea; 90var; head movements; hearing; echolocation	DINOFLAGELLATE CYST STRATIGRAPHY; MIDDLE MIOCENE; NORTH-SEA; BASIN; ALLOSTRATIGRAPHY; EVOLUTION; BELGIUM; WHALES; AREA	Eurhinodelphinids are a family of extremely long-snouted dolphins that once was widespread across the North Atlantic realm, but so far has not been recorded from the epicontinental Paratethys Sea. Here, we describe a new specimen of Xiphiacetus cristatus, including the cranium, left ear bones and a partial mandible, from the Middle Miocene (Badenian) of Austria. Our new fossil is the first record of this species outside the North Atlantic proper, and the first unequivocal record of eurhinodelphinids from the Paratethys. Its presence suggests a local invasion via the Mediterranean, and corroborates the persistence of an active marine gateway between the Mediterranean and the Central Paratethys throughout the Middle Miocene. Measurements of the bony labyrinth reveal that X. cristatus likely employed narrow-band high-frequency echolocation, making eurhinodelphinids only the second extinct odontocete family with this trait. Marked non-orthogonality of the semicircular canals suggests that X. cristatus was unsuited to rapid head movements, and thus more likely a benthic forager than a snap feeder.	[Lambert, Olivier] Royal Belgian Inst Nat Sci, Directorate Earth & Hist Life, Brussels, Belgium; [Wanzenboeck, Gerhard] Breitegasse 7, A-2540 Bad Voslau, Austria; [Pfaff, Cathrin; Kriwet, Juergen] Univ Vienna, Dept Palaeontol, Vienna, Austria; [Louwye, Stephen] Univ Ghent, Dept Geol, Ghent, Belgium; [Marx, Felix G.] Museum New Zealand Te Papa Tongarewa, Wellington, New Zealand; [Marx, Felix G.] Univ Otago, Dept Geol, Dunedin, New Zealand	Royal Belgian Institute of Natural Sciences; University of Vienna; Ghent University; University of Otago	Marx, FG (通讯作者)，Museum New Zealand Te Papa Tongarewa, Wellington, New Zealand.	felix.marx@tepapa.govt.nz	Marx, Felix/AAI-3480-2021; Lambert, Olivier/AEN-2469-2022; Kriwet, Jürgen/B-3165-2011; Louwye, Stephen/D-3856-2012	Pfaff, Cathrin/0000-0001-5539-2097; Lambert, Olivier/0000-0003-0740-5791; Kriwet, Jurgen/0000-0002-6439-8455; Marx, Felix Georg/0000-0002-1029-4001; Louwye, Stephen/0000-0003-4814-4313	Marie Sklodowska-Curie Global Postdoctoral Fellowship [656010/MYSTICETI]	Marie Sklodowska-Curie Global Postdoctoral Fellowship	This work was partly funded by a Marie Sklodowska-Curie Global Postdoctoral Fellowship [656010/MYSTICETI] to FGM.	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Biol.	JUL 3	2023	35	7					1074	1091		10.1080/08912963.2022.2077645	http://dx.doi.org/10.1080/08912963.2022.2077645		JUN 2022	18	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	J2AU5					2025-03-11	WOS:000809553200001
J	Zhong, YP; Su, YP; Zhang, DY; She, CX; Chen, NW; Chen, JX; Yang, H; Balaji-Prasath, B				Zhong, Yanping; Su, Yuping; Zhang, Dayi; She, Chenxing; Chen, Nengwang; Chen, Jixin; Yang, Hong; Balaji-Prasath, Barathan			The spatiotemporal variations in microalgae communities in vertical waters of a subtropical reservoir	JOURNAL OF ENVIRONMENTAL MANAGEMENT			English	Article						Microalgae community; Seasonal variations; Phosphorus release; Bottom water; Reservoir	PHYTOPLANKTON FUNCTIONAL-GROUPS; FRESH-WATER; ENVIRONMENTAL-FACTORS; DINOFLAGELLATE CYSTS; TEMPORAL VARIATION; SURFACE SEDIMENTS; DRIVING FACTORS; JIULONG RIVER; SHALLOW LAKE; PHOSPHORUS	The construction of cascade reservoirs increases eutrophication and exacerbates algal blooms and thus threatens water quality. Previous studies on the microalgae in reservoir have mainly focused on the spatio-temporal patterns of surface microalgae communities at the horizontal scale, while few studies have simultaneously considered the successions of microalgae in vertical profiles including the sediments and the effects of the nutrients release and microalgae in sediments on microalgae in upper waters. In this study, we investigated the effects of microalgae and physico-chemical parameters in waters and sediments on the successions of vertical microalgae communities in Xipi Reservoir, Southeast China. The seasonal variations in microalgae compositions decreased gradually from the surface water (the dominance of Cryptophyta and Chlorophyta in spring, Chlorophyta and Cyanophyta in summer, and relatively uniform in autumn and winter) to the sediment (the dominance of Bacillariophyta throughout the year), which was influenced by the variations of physico-chemical factors in different layers. The spatio-temporal variations in microalgae communities in waters was attributing to not only the heterogeneities of the stratification, and the physico-chemical factors such as water temperature, pH, and nutrient concentrations, especially for phosphorus in the water column, but also the combinations of phosphorus release and microalgae composition in sediments. Environmental changes would be especially problematic for microalgae groups such as Cryptophyta, Dinophyta and Chlorophyta that were sensitive to the changes of temperature and nutrients. Our results are helpful for an extensive understanding of the dynamics of microalgae communities in reservoir, and contribute to reservoir management for ensuring the safety of drinking water.	[Zhong, Yanping; Su, Yuping; She, Chenxing; Balaji-Prasath, Barathan] Fujian Normal Univ, Environm Sci & Engn Coll, Fuzhou 350007, Peoples R China; [Zhong, Yanping] Quanzhou Normal Univ, Coll Resources & Environm Sci, Quanzhou 362000, Peoples R China; [Chen, Nengwang; Chen, Jixin] Xiamen Univ, Coll Environm & Ecol, Fujian Prov Key Lab Coastal Ecol & Environm Studie, Xiamen 361005, Peoples R China; [Zhang, Dayi] Tsinghua Univ, Sch Environm, Beijing 100084, Peoples R China; [Yang, Hong] Univ Reading, Dept Geog & Environm Sci, Reading RG66AB, England	Fujian Normal University; Quanzhou Normal University; Xiamen University; Tsinghua University; University of Reading	Su, YP (通讯作者)，Fujian Normal Univ, Environm Sci & Engn Coll, Fuzhou 350007, Peoples R China.	ypsu@fjnu.edu.cn	ZHANG, DAYI/F-7858-2010; Su, Yu-Ping/J-7534-2012; Barathan, Balaji Prasath/AAE-3189-2022; Yang, Hong/C-1739-2008	Barathan, Dr. Balaji Prasath/0000-0001-7896-2208; Zhang, Dayi/0000-0002-1647-0408	National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation" [2016YFE0202100]; National Natural Science Foundation of China [41573075]; Research Projects of Water Resources Department of Fujian Province [SC-292, DH-1558, 21NB000922, MSK202202]; Research Projects of Water Resources Department of Fujian Province; Minjiang Scholar Program	National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation"; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Research Projects of Water Resources Department of Fujian Province; Research Projects of Water Resources Department of Fujian Province; Minjiang Scholar Program	We thank Xuejing You, Qiongli Mo, and Xingpeng Zhou for their assistance in microalgae sample collections and analyses. This study was supported by the National Key Research & Development Plan "Strategic International Scientific and Technological Innovation Cooperation" (2016YFE0202100) , National Natural Science Foundation of China (41573075) , Research Projects of Water Resources Department of Fujian Province (SC-292, DH-1558, 21NB000922,MSK202202) , and Minjiang Scholar Program.	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J	Bouquet, A; Perdrau, MA; Laabir, M; Foucault, E; Chomérat, N; Rolland, JL; Abadie, E				Bouquet, Aurelien; Perdrau, Marie Anais; Laabir, Mohamed; Foucault, Elodie; Chomerat, Nicolas; Rolland, Jean Luc; Abadie, Eric			<i>Liza ramada</i> Juveniles after Exposure to the Toxic Dinoflagellate <i>Vulcanodinium rugosum</i>: Effects on Fish Viability, Tissue Contamination and Microalgae Survival after Gut Passage	TOXINS			English	Article						Vulcanodinium rugosum; Liza ramada; contamination; pinnatoxins; portimines; food chain; fish; dissemination	MULLET MUGIL-CEPHALUS; HARMFUL ALGAL BLOOMS; DOMOIC ACID; PINNATOXIN G; TROPHIC TRANSFER; SEED DISPERSAL; PHYTOPLANKTON; MIGRATION; COASTAL; LAKE	Pinnatoxins (PnTX) and Portimines (Prtn), two toxins produced by the benthic dinoflagellate Vulcanodinium rugosum, are known to be lethal to mice after intraperitoneal or oral administration. They are also known to accumulate in shellfish such as mussels and clams, but their effect on fish and the upper food chain remains unknown. In this work, juveniles of the fish Liza ramada (Mullet) were exposed to a strain of V. rugosum producing PnTX G and Prtn A. The fishes' viability and contamination were recorded at times interval. Results showed that L. ramada juveniles were able to feed on V. rugosum and that their tissues could be contaminated by PnTX G and Prtn A without impact on fish viability. Furthermore, the microalgae temporary cysts survived and germinated after fish gut passage. This study showed the potential of L. ramada to transfer PnTX and Prtn toxins to the upper food chain and to disseminate V. rugosum in environment.	[Bouquet, Aurelien; Perdrau, Marie Anais; Foucault, Elodie; Rolland, Jean Luc; Abadie, Eric] Univ Montpellier, MARBEC, CNRS, Ifremer, 87 Ave Jean Monnet, F-34200 Sete, France; [Laabir, Mohamed] Univ Montpellier, MARBEC, CNRS, Ifremer,IRD, F-34095 Montpellier, France; [Chomerat, Nicolas] IFREMER, Stn Biol Marine, Pl Croix, F-29900 Concarneau, France; [Abadie, Eric] IFREMER, Biodivenv, 79 Route Pointe Ft, F-97231 Martinique, France	Ifremer; Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Ifremer; Ifremer	Bouquet, A; Rolland, JL (通讯作者)，Univ Montpellier, MARBEC, CNRS, Ifremer, 87 Ave Jean Monnet, F-34200 Sete, France.	aurelien.bouquet@ifremer.fr; perdrauanais@gmail.com; mohamed.laabir@umontpellier.fr; elodie.foucault@ifremer.fr; nicolas.chomerat@ifremer.fr; jean.luc.rolland@ifremer.fr; eric.abadie@ifremer.fr		Rolland, jean-luc/0000-0001-9823-6588; ABADIE, Eric/0000-0001-9431-2010; Chomerat, Nicolas/0000-0001-9691-6344	MARBEC (MARine Biodiversity, Exploitation and Conservation); French Ministry of Agriculture and Food	MARBEC (MARine Biodiversity, Exploitation and Conservation); French Ministry of Agriculture and Food	This research was supported by MARBEC (MARine Biodiversity, Exploitation and Conservation) and by the French Ministry of Agriculture and Food. This research received no external funding.	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Toxicology	2K8XG	35737062	gold, Green Published			2025-03-11	WOS:000816611500001
J	Johnson, ALA; Valentine, AM; Schöne, BR; Leng, MIJ; Goolaerts, S				Johnson, Andrew L. A.; Valentine, Annemarie M.; Schoene, Bernd R.; Leng, Melanie J.; Goolaerts, Stijn			Sclerochronological evidence of pronounced seasonality from the late Pliocene of the southern North Sea basin and its implications	CLIMATE OF THE PAST			English	Article							DINOFLAGELLATE CYST STRATIGRAPHY; OXYGEN-ISOTOPE FRACTIONATION; MID-PIACENZIAN; BIOGENIC ARAGONITE; ARCTICA-ISLANDICA; TEMPERATURE; CLIMATE; SHELLS; PALEOECOLOGY; VARIABILITY	Oxygen isotope (delta O-1(8)) sclerochronology of benthic marine molluscs provides a means of reconstructing the seasonal range in seafloor temperature, subject to use of an appropriate equation relating shell delta O-1(8) to temperature and water delta O-1(8), a reasonably accurate estimation of water delta O-1(8), and due consideration of growth-rate effects. Taking these factors into account, delta O-1(8) data from late Pliocene bivalves of the southern North Sea basin (Belgium and the Netherlands) indicate a seasonal seafloor range a little smaller than now in the area. Microgrowth-increment data from Aequipecten opercularis, together with the species composition of the bi-valve assemblage and aspects of preservation, suggest a setting below the summer thermocline for all but the latest material investigated. This implies a higher summer temperature at the surface than on the seafloor and consequently a greater seasonal range. A reasonable (3 degrees C) estimate of the difference between maximum seafloor and surface temperature under circumstances of summer stratification points to seasonal surface ranges in excess of the present value (12.4 degrees C nearby). Using a model-derived estimate of water delta O-1(8) (0.0 %0), summer surface temperature was initially in the cool temperate range (< 20 degrees C) and then (during the Mid-Piacenzian Warm Period; MPWP) increased into the warm temperate range (> 20 degrees C) before reverting to cool temperate values (in conjunction with shallowing and a loss of summer stratification). This pattern is in agreement with biotic-assemblage evidence. Winter temperature was firmly in the cool temperate range (< 10 degrees C) throughout, contrary to previous interpretations. Averaging of summer and winter surface temperatures for the MPWP provides a figure for annual sea surface temperature that is 2-3 degrees C higher than the present value (10.9 degrees C nearby) and in close agreement with a figure obtained by averaging alkenone and TEX86 temperatures for the MPWP from the Netherlands. These proxies, however, respectively, underestimate summer temperature and overestimate winter temperature, giving an incomplete picture of seasonality. A higher annual temperature than now is consistent with the notion of global warmth in the MPWP, but a low winter temperature in the southern North Sea basin suggests regional reduction in oceanic heat supply, contrasting with other interpretations of North Atlantic oceanography during the interval. Carbonate clumped isotope (Delta(47)) and biomineral unit thermometry offer means of checking the delta O-1(8)-based temperatures.	[Johnson, Andrew L. A.] Univ Derby, Sch Built & Nat Environm, Derby DE22 1GB, England; [Valentine, Annemarie M.] Nottingham Trent Univ, Sch Geog & Environm Sci, Southwell NG25 0QF, England; [Schoene, Bernd R.] Johannes Gutenberg Univ Mainz, Inst Geosci, D-55128 Mainz, Germany; [Leng, Melanie J.] British Geol Survey, Natl Environm Isotope Fac, Keyworth NG12 5GG, Notts, England; [Goolaerts, Stijn] Royal Belgian Inst Nat Sci, Earth Hist Life & Sci Heritage Serv, B-1000 Brussels, Belgium	University of Derby; Nottingham Trent University; Johannes Gutenberg University of Mainz; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Royal Belgian Institute of Natural Sciences	Johnson, ALA (通讯作者)，Univ Derby, Sch Built & Nat Environm, Derby DE22 1GB, England.	a.l.a.johnson@derby.ac.uk	Schöne, Bernd/B-6294-2011; Johnson, Andrew/ABC-1334-2021	Johnson, Andrew/0000-0001-5727-1889; Leng, Melanie/0000-0003-1115-5166; Schone, Prof. Dr. Bernd R./0000-0002-6879-1633	British Geological Survey [BUFI S157]; Alexander von Humboldt-Stiftung; Natural Environment Research Council [IP-1108-0509, IP-1155-1109]; NERC [NE/V003917/1, bgs06003] Funding Source: UKRI	British Geological Survey; Alexander von Humboldt-Stiftung(Alexander von Humboldt Foundation); Natural Environment Research Council(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was supported by the British Geological Survey (grant no. BUFI S157 for the PhD research of Annemarie M. Valentine), the Alexander von Humboldt-Stiftung (study visit to Mainz by Andrew L. A. Johnson), and the Natural Environment Research Council (Isotope analytical services: grant nos. IP-1108-0509, IP-1155-1109).	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Past.	MAY 30	2022	18	5					1203	1229		10.5194/cp-18-1203-2022	http://dx.doi.org/10.5194/cp-18-1203-2022			27	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	1P7CG		Green Accepted, gold, Green Published			2025-03-11	WOS:000802162000001
J	Boukhamsin, H; Peyrot, D; Vecoli, M				Boukhamsin, Hani; Peyrot, Daniel; Vecoli, Marco			Angiosperm pollen assemblages from the Lower Cretaceous (Barremian-lower Aptian) of offshore Saudi Arabia and their implications for early patterns of angiosperm radiation	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Angiosperm; Palynology; Arabian Plate; Barremian; Aptian; Gondwana	APTICORE SOUTHERN ALPS; DINOFLAGELLATE CYST; PSEUDOASTEROPHYLLITES-CRETACEUS; PHYLOGENETIC ANALYSES; ZONASULCULATE POLLEN; BASAL ANGIOSPERM; FOSSIL RECORD; SP-NOV; BASIN; PLANT	Early flowering plants constituted a minor component of the Early Cretaceous conifer- and fern- dominated flora. However, their pollen provides a rich, albeit incomplete, record of the group's early evolutionary history. Palynological analysis of Barremian-lower Aptian successions from the Biyadh and Shu'aiba formations in the Arabian Gulf reveals remarkably high angiosperm diversity. While Chloranthaceae, magnoliids, monocots, eudicots, and other "basal" groups represent the bulk of flowering plants, pollen with uncertain affinities is also a significant component of the angiosperm assemblage. Analysis of the palaeobiogeographic distribution of angiosperm pollen during the late Barremian-early Aptian allowed us to discern three groups of angiosperms. The first group, including Clavatipollenites, produced pollen with a near-cosmopolitan distribution. The second group, including Stellatopollis, had a somewhat restricted distribution in northern Gondwana and western Laurasia. The pollen distribution of the third group, which includes Dichastopollenites, is restricted to central and/ or northeastern Gondwana. These varied patterns of palaeobiogeographical spread of early angiosperms reflect different migration and colonisation abilities. When compared with coeval palynological successions from other Gondwanan localities, the composition and diversity of the Arabian angiosperm assemblages support early hypotheses on the radiation of angiosperms that identify northeastern Gondwana as one of the most important centres of angiosperm diversification.The following new taxa are described: Splitipollis gen. nov., Splitipollis reticulatus sp. nov., Tucanopollis doylei sp. nov., Pennipollis spinosus sp. nov., Clavamonocolpites woodii sp. nov., and Retimonoporites arabiensis sp. nov.	[Boukhamsin, Hani; Peyrot, Daniel] Univ Western Australia, Sch Earth Sci, Crawley, WA 6101, Australia; [Boukhamsin, Hani; Vecoli, Marco] Saudi Aramco, Dhahran 31311, Saudi Arabia; [Boukhamsin, Hani; Peyrot, Daniel] Univ Western Australia, Ctr Energy Geosci, Crawley, WA 6101, Australia	University of Western Australia; University of Western Australia	Boukhamsin, H (通讯作者)，Univ Western Australia, Sch Earth Sci, Crawley, WA 6101, Australia.	hani.boukhamsin@research.uwa.edu.au	peyrot, Daniel/AAI-6091-2020	peyrot, Daniel/0000-0002-3897-6733	Microscopy Australia at the Centre for Microscopy,	Microscopy Australia at the Centre for Microscopy,	The authors gratefully acknowledge assistance of laboratory tech-nicians Fayez Bokhashaim, Hussain Alhilal, Mortada Alali, and Mohammed Jaroodi (Dhahran, Saudi Arabia) . The authors acknowledge the facilities and the scientific and technical assistance of Microscopy Australia at the Centre for Microscopy, Characterisation & Analysis, the University of Western Australia, a facility funded by the University, State, and Commonwealth Governments. Alysia Hubbard (UWA CMCA) is gratefully acknowledged for assistance with the Confocal Laser Scanning Microscope. We very much appreciate their efforts, without which this study would not have been possible. Sa?id Al-Hajri, Nigel Hooker, and Ahmed Al-Shawareb (Saudi Aramco) are thanked for their discussion, contribution and support in various matters during this research. Dr. James A. Doyle and two anonymous reviewers are also thanked for their comments and suggestions, which have enhanced the quality of this manuscript. Dr. Kailah Thorn, curator of Edward de Courcy Clark Earth Science Museum, is thanked for her support and help in curating the type specimens.	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Paleoclimatol. Paleoecol.	AUG 1	2022	599								111052	10.1016/j.palaeo.2022.111052	http://dx.doi.org/10.1016/j.palaeo.2022.111052		MAY 2022	22	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	1U2BN					2025-03-11	WOS:000805222300002
J	Coats, DW; Moon, E				Coats, D. Wayne; Moon, Eunyoung			Ultrastructure of selected life history stages of the parasitic dinoflagellate <i>Euduboscquella cachoni</i>	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Amphiesma; chromosome; flagellar apparatus; food vacuole; micropore; nutrition; parasite egress	IN-VITRO CULTIVATION; N. SP DINOFLAGELLATA; ATLANTIC SNOW CRAB; HEMATODINIUM SP; PARASITOPHOROUS VACUOLE; INTRACELLULAR PARASITE; DUBOSCQUELLA-CACHONI; AMOEBOPHRYA SP; INFECTION; DINOPHYCEAE	Euduboscquella species differ from most other syndinean dinoflagellates by having mononucleate trophonts, but resemble species of Amoebophrya and Sphaeripara by episome-hyposome differentiation and cortical complexity. Cytology and development of Euduboscquella species are well characterized, but their ultrastructure remains essentially unexplored. Transmission electron microscopy of Euduboscquella cachoni trophonts, tomont, and sporocytes revealed previously unrecognized structures. Initially dense, fibrous chromosomes uncoiled during early infection, with condensed chromosomes absent over much of the growth cycle recondensing at trophont maturity. The hyposomal amphiesma was two appressed membranes, the episomal cortex was alveolate, and a supraepisomal cavity limited by membrane enclosed the episome. Pseudopod-like extensions of the hyposome during mid infection may facilitate osmotrophic nutrition. The pharyngeal lamina appears to lack ingestatory function; however, transcortical transport of particles occurred via the supraepisomal cavity and episomal micropores. Microtubules originating from the electron-opaque perinema bordering the episome, formed an episomal skeleton hypothesized to function with the pharyngeal lamina, perinema, and the paired membranes of the supraepisomal cavity to effect parasite egress and ingestion of host material. Trichocysts absent during early infection developed during late infection and reached maturity during sporogenesis, suggesting functional importance in spore survival or infection.	[Coats, D. Wayne] Smithsonian Environm Res Ctr, POB 28, Edgewater, MD 21037 USA; [Moon, Eunyoung] Korean Basic Sci Inst, Div Electron Microscop Res, Cheongju, South Korea	Smithsonian Institution; Smithsonian Environmental Research Center; Korea Basic Science Institute (KBSI)	Coats, DW (通讯作者)，318 Bayard Rd, Lothian, MD 20711 USA.	coatsw1@gmail.com		Coats, D Wayne/0000-0002-0636-189X	Korean Basic Science Institute, RD Program [C140440]; National Science Foundation [OCE--8515834]	Korean Basic Science Institute, RD Program; National Science Foundation(National Science Foundation (NSF))	Korean Basic Science Institute, R&D Program, Grant/Award Number: C140440; National Science Foundation, Grant/Award Number: OCE--8515834	Anderson D.M., 2013, BIOL ECOLOGY TINTINN, VG41, P315; Appleton PL, 1996, PARASITOL RES, V82, P279, DOI 10.1007/s004360050113; Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; Bateman KS, 2011, ICES J MAR SCI, V68, P2044, DOI 10.1093/icesjms/fsr148; Batista MF, 2020, FRONT CELL DEV BIOL, V8, DOI 10.3389/fcell.2020.00396; Brugerolle G, 2002, EUR J PROTISTOL, V37, P379, DOI 10.1078/0932-4739-00837; CACHON J, 1984, BIOL CELL, V52, P61; Cachon J., 1964, Annales des Sciences Naturelles (12), V6, P1; Cachon J., 1969, Protistologica, V5, P535; Cachon J., 1987, Botanical Monographs (Oxford), V21, P571; Cachon J., 1966, Protistologica, V2, P17; CACHON J, 1970, Protistologica, V6, P57; Cachon J., 1964, ANN SCI NAT ZOOL, V6, P779; Cachon J., 1965, ARCH ZOOLOGIE EXP RI, V105, P369; Chambouvet A, 2011, PROTIST, V162, P637, DOI 10.1016/j.protis.2010.12.001; Chatton E., 1920, Archives de Zoologie Experimentale Paris, V59; Chatton E., 1952, TRAIT ZOOLOGIE, V1, P309; Choi JM, 2021, FRONT MAR SCI, V8, DOI 10.3389/fmars.2021.720424; Clough B, 2017, TRENDS PARASITOL, V33, P473, DOI 10.1016/j.pt.2017.02.007; Coats DW, 2012, J EUKARYOT MICROBIOL, V59, P1, DOI 10.1111/j.1550-7408.2011.00588.x; COATS DW, 1988, J PROTOZOOL, V35, P607, DOI 10.1111/j.1550-7408.1988.tb04159.x; COATS DW, 1989, MAR BIOL, V101, P401, DOI 10.1007/BF00428137; Fensome R.A., 1993, MICROPALEONTOLOGY SP, V7, P1; FRITZ L, 1992, J PHYCOL, V28, P312, DOI 10.1111/j.0022-3646.1992.00312.x; Gaudet PH, 2014, J INVERTEBR PATHOL, V121, P14, DOI 10.1016/j.jip.2014.06.006; Gaudet P.H., 2014, THESIS U P EDWARD IS; Gaudet PH, 2015, PARASITOLOGY, V142, P598, DOI 10.1017/S0031182014001656; Gestal C, 2006, ENVIRON MICROBIOL, V8, P1105, DOI 10.1111/j.1462-2920.2006.01008.x; Guillou L, 2008, ENVIRON MICROBIOL, V10, P3349, DOI 10.1111/j.1462-2920.2008.01731.x; Harada A, 2007, PROTIST, V158, P337, DOI 10.1016/j.protis.2007.03.005; HOLLANDE A, 1974, Protistologica, V10, P413; HUDSON DA, 1994, DIS AQUAT ORGAN, V19, P109, DOI 10.3354/dao019109; HUDSON DA, 1993, J FISH DIS, V16, P273, DOI 10.1111/j.1365-2761.1993.tb01258.x; Jeon BS, 2020, PROTIST, V171, DOI 10.1016/j.protis.2020.125743; Jeon BS, 2018, ALGAE-SEOUL, V33, P1; John U, 2019, SCI ADV, V5, DOI 10.1126/sciadv.aav1110; Jung JH, 2016, J EUKARYOT MICROBIOL, V63, P3, DOI 10.1111/jeu.12231; Kemp LE, 2013, FEMS MICROBIOL REV, V37, P607, DOI 10.1111/1574-6976.12013; Magno RC, 2005, MICROSC MICROANAL, V11, P166, DOI 10.1017/S1431927605050129; Maire J, 2021, ISME J, V15, P2028, DOI 10.1038/s41396-021-00902-4; Maranda L, 2001, J PHYCOL, V37, P245, DOI 10.1046/j.1529-8817.2001.037002245.x; Matz JM, 2020, NAT REV MICROBIOL, V18, P379, DOI 10.1038/s41579-019-0321-3; Miller JJ, 2012, PROTIST, V163, P720, DOI 10.1016/j.protis.2011.11.007; Moon E, 2015, PROTIST, V166, P569, DOI 10.1016/j.protis.2015.08.005; Onda DFL, 2015, ARCH MICROBIOL, V197, P965, DOI 10.1007/s00203-015-1133-0; RIS H, 1974, J CELL BIOL, V60, P702, DOI 10.1083/jcb.60.3.702; ROBERTS KR, 1991, SYST ASSOC SPEC VOL, V45, P285; ROBERTS KR, 1991, PROTOPLASMA, V164, P105, DOI 10.1007/BF01320818; Seibold A, 2001, AQUAT MICROB ECOL, V25, P229, DOI 10.3354/ame025229; Simdyanov T G, 2016, Dokl Biol Sci, V468, P125, DOI 10.1134/S001249661603008X; Soyer M.O, 1974, VIE MILIEU SER, V24, P191; Stentiford Grant D, 2012, Aquat Biosyst, V8, P24, DOI 10.1186/2046-9063-8-24	52	3	3	4	9	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1066-5234	1550-7408		J EUKARYOT MICROBIOL	J. Eukaryot. Microbiol.	JUL	2022	69	4							e12921	10.1111/jeu.12921	http://dx.doi.org/10.1111/jeu.12921		MAY 2022	16	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	2Y0VY	35506426				2025-03-11	WOS:000799910700001
J	Fischer, AD; Brosnahan, ML				Fischer, Alexis D.; Brosnahan, Michael L.			Growing Degree-Day Measurement of Cyst Germination Rates in the Toxic Dinoflagellate Alexandrium catenella	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article						dinoflagellate cyst bed; population comparison; microbial resting stages; temperature-dependent phenology	RESTING CYSTS; FUNDYENSE CYSTS; PUGET-SOUND; DYNAMICS; GULF; TIME; TEMPERATURE; DINOPHYCEAE; POPULATIONS; EXCYSTMENT	Blooms of many dinoflagellates, including several harmful algal bloom (HAB) species, are seeded and revived through the germination of benthic resting cysts. Temperature is a key determinant of cysts' germination rate, and temperature-germination rate relationships are therefore fundamental to understanding species' germling cell production, cyst bed persistence, and resilience to climate warming. This study measured germination by cysts of the HAB dinoflagellate Alexandrium catenella using a growing degree-day (DD) approach that accounts for the time and intensity of warming above a critical temperature. Time courses of germination at different temperatures were fit to lognormal cumulative distribution functions for the estimation of the median days to germination. As temperature increased, germination times decreased hyperbolically. DD scaling collapsed variability in germination times between temperatures after cysts were oxygenated. A parallel experiment demonstrated stable temperature-rate relationships in cysts collected during different phases of seasonal temperature cycles in situ over three years. DD scaling of the results from prior A. catenella germination studies showed consistent differences between populations across a wide range of temperatures and suggests selective pressure for different germination rates. The DD model provides an elegant approach to quantify and compare the temperature dependency of germination among populations, between species, and in response to changing environmental conditions. IMPORTANCE Germination by benthic life history stages is the first step of bloom initiation in many, diverse phytoplankton species. This study outlines a growing degree-day (DD) approach for comparing the temperature dependence of germination rates measured in different populations. Germination by cysts of Alexandrium catenella, a harmful algal bloom dinoflagellate that causes paralytic shellfish poisoning, is shown to require a defined amount of warming, measured in DD after cysts are aerated. Scaling by DD, the time integral of temperature difference from a critical threshold, enabled direct comparison of rates measured at different temperatures and in different studies. Germination by benthic life history stages is the first step of bloom initiation in many, diverse phytoplankton species. This study outlines a growing degree-day (DD) approach for comparing the temperature dependence of germination rates measured in different populations.	[Fischer, Alexis D.; Brosnahan, Michael L.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Fischer, AD (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	afischer@whoi.edu	Fischer, Alexis/M-4531-2019	Brosnahan, Michael/0000-0002-2620-7638; Fischer, Alexis/0000-0002-8028-487X	Woods Hole Center for Oceans and Human Health (National Science Foundation) [OCE-0430724, OCE-0911031, OCE-1314642, OCE-1840381]; Woods Hole Center for Oceans and Human Health (National Institutes of Health) [NIEHS-1P50-ES02192301, P01ES028938]; National Institute of Environmental Health Sciences [P01ES028938] Funding Source: NIH RePORTER	Woods Hole Center for Oceans and Human Health (National Science Foundation); Woods Hole Center for Oceans and Human Health (National Institutes of Health)(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH Division of Research Services (DRS)); 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))	We gratefully acknowledge support to A.D.F. and M.L.B. through the Woods Hole Center for Oceans and Human Health (National Science Foundation grants OCE-0430724, OCE-0911031, OCE-1314642, and OCE-1840381 and National Institutes of Health grants NIEHS-1P50-ES02192301 and P01ES028938).	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Environ. Microbiol.	JUN 28	2022	88	12								10.1128/aem.02518-21	http://dx.doi.org/10.1128/aem.02518-21		MAY 2022	13	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	2O1TF	35604227	Green Published, hybrid			2025-03-11	WOS:000803948400006
J	Wu, XM; Li, L; Lin, SJ				Wu, Xiaomei; Li, Ling; Lin, Senjie			Energy metabolism and genetic information processing mark major transitions in the life history of<i> Scrippsiella</i><i> acuminata</i> (Dinophyceae)	HARMFUL ALGAE			English	Article						Dinoflagellate; Scrippsiella acuminata; Transcriptome; Cyst; Energy metabolism; Genetic information processing	DINOFLAGELLATE-AKASHIWO-SANGUINEA; CYST PRODUCTION; ALEXANDRIUM; TROCHOIDEA; THORACOSPHAERACEAE; IDENTIFICATION; EVOLUTIONARY; VALIDATION; EXCYSTMENT; EXPRESSION	Many dinoflagellates perform sexual reproduction and form cysts as a life history strategy to survive adverse environmental conditions and seed annual harmful algal blooms (HABs). The molecular mechanisms underpinning the life stage transitions can provide clues about how key environmental factors induce encystment and initiation of a HAB but are still poorly understood. Here, we conducted an integrated physiological and transcriptomic study to unravel the mechanisms in Scrippsiella acuminata. We established a culture from a bloom, induced cyst formation, and divided the process into four life stages. Transcriptomic analysis of these stages revealed 19,900 differentially expressed genes (DEGs). The expression of genes related to photosynthesis was significantly up-regulated from vegetative stage to immature cyst stage, consistent with the marked increase in cell contents of energy-storing macromolecules (carbohydrates and lipids). When proceeding to resting cysts, most photosynthesis genes were down-regulated while "genetic information processing" related genes were up regulated. Comparing germinating cysts with resting cysts revealed 100 DEGs involved in energy metabolism, indicating a high energy requirement of germination. In addition, the transition from germinating cysts to vegetative cells featured up-regulation of photosynthesis. Our results demonstrate that energy storage and consumption play a pivotal role in cyst formation and germination respectively and genetic information processing is crucial in cyst dormancy.	[Wu, Xiaomei; Li, Ling; Lin, Senjie] Xiamen Univ, Coll Ocean & Earth Sci, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China; [Lin, Senjie] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA	Xiamen University; University of Connecticut	Lin, SJ (通讯作者)，Xiamen Univ, Coll Ocean & Earth Sci, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China.	senjie.lin@uconn.edu	Lin, Senjie/A-7466-2011	Wu, Xiaomei/0000-0002-7425-8755; Lin, Senjie/0000-0001-8831-6111	Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) [2018SDKJ0406-3]; National Natural Science Foundation of China [NSFC 41776116, 31661143029]	Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We wish to thank Dazhi Wang (Xiamen University) for providing the opportunity to join the research cruise. We also thank Mr. Huatao Yuan (Xiamen University) for collecting the field samples for the isolation of S. acuminata, Dr. Liying Yu (Xiamen University) for depositing data to NCBI and to the SAGER database (http://sampgr.org.cn/) , and Ms. Chentao Guo and Mr. Yujie Wang for logistic support. We are indebted to the four anonymous reviewers for their kind and constructive comments that led to significant improvement of the manuscript. This work was supported by the Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) (No.2018SDKJ0406-3) , and the National Natural Science Foundation of China grants NSFC 41776116 and 31661143029.	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nullJ	Munsterman, DK; Deckers, J				Munsterman, Dirk K.; Deckers, Jef			Biostratigraphic ages and depositional environments of the upper Oligocene to lower Miocene Veldhoven Formation in the central Roer Valley Rift System (SE Netherlands-NE Belgium)	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						dinoflagellate cysts; upper Palaeogene; lowermost Neogene; sedimentary facies; southern North Sea Basin; well-log correlation	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; LOWER RHINE BASIN; NORTHERN BELGIUM; SOUTHERN BORDER; CENOZOIC EVOLUTION; STRATIGRAPHY; AREA; TRANSITION; PLIOCENE; BOUNDARY	Discussions on the age and the depositional environments of the Veldhoven Formation and its members are persistent in Belgium and the Netherlands. Uncertainties on stratigraphy and the constructive process of sediment accumulation continue today as a result of lack of data on this succession within the Roer Valley Rift System. The present study provides new information on the bio- and lithostratigraphy and facies from two boreholes based on dinoflagellate cyst taxa. The results were correlated by gamma-ray logs towards other key boreholes in the region and show a good consistency for stratigraphy and depositional environments for the members of the Veldhoven Formation. After marginal to restricted marine conditions in the latest Rupelian (early Oligocene), the start of deposition of the Veldhoven Formation marked the transition towards a higher sea level, expressed by increased glauconite contents and gamma-ray values. The Voort Member in the lower part of the Veldhoven Formation has an early to late Chattian (Late Oligocene) age and comprises predominantly shallow marine (fluctuating restricted to open marine) conditions. The lithology in the lower part of this unit is often very clayey but is coarsening upward into sands. The superjacent Wintelre Member has a latest Chattian to early Aquitanian (early Miocene) age. This member is distinct by its clayey nature which is expressed by relatively high gamma-ray values. Earlier studies suggest a deeper marine facies for the Wintelre Member compared to the Someren and Voort members. However, the dinoflagellate cyst assemblages in this unit are mostly dominated by a single genus indicating a restricted marine setting, including salinities that deviate from normal marine conditions, most probably due to minor ventilation by narrow or lack of connection to the Atlantic Ocean. A glacio-eustatic sea-level fall around the Oligocene/Miocene boundary limited the sea coverage to the strongest subsiding areas, where deposition of the Wintelre Member is recorded, while non-deposition or erosion occurred in the surrounding highs, hence creating an isolated (sub)basin. The superjacent Someren Member was deposited during the late Aquitanian to middle Burdigalian and consists of shallow to open marine clayey fine sands. Increasing clay contents indicate a gradual development towards a higher sea level, which coincide with upward increasing gamma-ray values. The biostratigraphic results of this study suggest that no major hiatuses are present in the differentially subsiding blocks of the Roer Valley Rift System during the late Oligocene to early Miocene.	[Munsterman, Dirk K.] TNO, Geol Survey Netherlands, Utrecht, Netherlands; [Deckers, Jef] VITO, Flemish Inst Technol Res, Mol, Belgium	Netherlands Organization Applied Science Research; VITO	Munsterman, DK (通讯作者)，TNO, Geol Survey Netherlands, Utrecht, Netherlands.	dirk.munsterman@tno.nl		Munsterman, Dirk/0000-0003-1774-4615	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	The authors gratefully acknowledge financial support from the Land and Soil Protection, Subsoil, and Natural Resources Division of the Flemish Government. We would like to thank Katleen van Baelen for her excellent work on the figures. The three reviewers, Karin Dybkjaer, Noel Vandenberghe and Frank Wesselingh are thanked for their very helpful suggestions and corrections improving the manuscript substantially. Finally we are much obliged to our editor Rick Donselaar (TU-Delft, the Netherlands) for his logistical support and corrections in the text.	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J. Geosci.	MAR 7	2022	101								e6	10.1017/njg.2022.3	http://dx.doi.org/10.1017/njg.2022.3			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	ZN8OM		gold, Green Published			2025-03-11	WOS:000765288500001
J	Petersen, HI; Fyhn, MBW; Nytoft, HP; Dybkjær, K; Nielsen, LH				Petersen, Henrik, I; Fyhn, Michael B. W.; Nytoft, Hans Peter; Dybkjaer, Karen; Nielsen, Lars Henrik			Miocene coals in the Hanoi Trough, onshore northern Vietnam: Depositional environment, vegetation, maturity, and source rock quality	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Coal; Depositional environment; Vegetation; Source rock; Maturity; Miocene; Vietnam	SONG-HONG BASIN; POLYCYCLIC AROMATIC-HYDROCARBONS; SEA-LEVEL CONTROL; PETROLEUM GENERATION; QIONGDONGNAN BASINS; CRUDE OILS; FLUORESCENCE SPECTROMETRY; GEOCHEMICAL COMPOSITION; VITRINITE REFLECTANCE; MOLECULAR INDICATORS	The Hanoi Trough in northern Vietnam forms the landward extension of the large Song Hong Basin in the South China Sea. Several gas and condensate discoveries have been made in the offshore part while exploration in the Hanoi Trough has been less successful. Encountered hydrocarbons suggest a terrigenous source rock, the most likely candidate being Miocene coals. The composition of these is poorly documented in the public domain, but in the Hanoi Trough with a thinner Cenozoic succession numerous Miocene coal beds have been penetrated by several wells. The current study examines by organic petrography, geochemistry, and sedimentology the depositional environment, paleo-vegetation, thermal maturity and source rock potential of Miocene coal samples from two about 1000 m fully cored wells in the Hanoi Trough. The sedimentological facies, dinoflagellate cyst content and pyrite nodules suggest the coals were formed in coastal mires, in particular the younger section, testifying to an overall relative sea-level rise in the Miocene. This is supported by abundant framboidal pyrite and high TS contents in the coals. Dominance of huminite in all samples suggests water-logged mire conditions while abundant funginite and high concentrations of hopanes indicate high bacterial and fungal activity. Reduced fluorescence, oxidation rims, and elevated reflectance of resinite in a sample with concentrations of liptinite composed of resinite, cutinite, suberinite, sporinite and liptodetrinite might suggest the liptinite-enrichment was the result of degradational removal of less resistant organic matter. Biomarkers indicate the mire vegetation consisted of gymnosperms related to Podocapaceae or Cupressaceae, and perhaps Pinaceae. Presence of angiosperms is indicated by oleanane and aromatic oleananes, lupanes and ursanes. An unknown diterpane derived from Araucaria nemorosa (conifer in the Araucariaceae family) and/or Araucaria cunninghamii (pine) may be the first occurrence in a geological sample. The coals are of lignite to sub-bituminous A rank and are thermally immature with regard to hydrocarbon generation. They are today not at maximum burial depth due to c. 480-1450 m of Miocene uplift before reburial in Plio-Pleistocene time. HImax values around 200 mg HC/g TOC reveal the coals primarily are gas-prone, but exsudatinite in cleats in huminite and cell lumens in funginite is evidence for in situ generation from labile macerals. Oil droplets in cleats/cracks suggest migration of liquid hydrocarbons from deeper buried source rocks and are indicative of a working petroleum system in the Hanoi Trough.	[Petersen, Henrik, I; Fyhn, Michael B. W.; Dybkjaer, Karen; Nielsen, Lars Henrik] Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Nytoft, Hans Peter] HPN Kemi, Helsebakken, DK-2900 Hellerup, Denmark	Geological Survey Of Denmark & Greenland	Petersen, HI (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	hip@geus.dk	Nytoft, Hans/H-1985-2018; Fyhn, Michael/AAI-7559-2020; Petersen, Henrik/ABB-4663-2020; Dybkjær, Karen/G-5223-2018	Petersen, Henrik I./0000-0001-6606-7062	Geocenter Denmark; Carlsberg Foundation	Geocenter Denmark; Carlsberg Foundation(Carlsberg Foundation)	Geological Survey of Vietnam is thanked for putting the core material at disposal for the study and for their warm hospitality and collaboration. Carlsberg Foundation is acknowledged for logistical funding. Analyses were funded by a grant from Geocenter Denmark. Ditte KielDuhring and Carsten Guvad assisted with the laboratory work and Jette Halskov drafted figures. 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J. Coal Geol.	MAR 15	2022	253								103953	10.1016/j.coal.2022.103953	http://dx.doi.org/10.1016/j.coal.2022.103953		MAR 2022	23	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	2Q7WK					2025-03-11	WOS:000820629900004
J	Aksu, AE; Hiscott, RN				Aksu, A. E.; Hiscott, R. N.			Persistent Holocene outflow from the Black Sea to the eastern Mediterranean Sea still contradicts the Noah's Flood Hypothesis: A review of 1997-2021 evidence and a regional paleoceanographic synthesis for the latest Pleistocene-Holocene	EARTH-SCIENCE REVIEWS			English	Review						Bosphorus; Dardanelles; Marmara Sea; Strontium isotopes; Seismic stratigraphy; Unconformities; Density currents; Deltas; Sapropel; Catastophism	MARMARA SHELF SOUTH; LATE QUATERNARY CORES; LAST GLACIAL MAXIMUM; ICE-DAMMED LAKES; AEGEAN SEA; POSTGLACIAL TRANSGRESSION; BOSPORUS STRAIT; BENTHIC FORAMINIFERA; DINOFLAGELLATE CYSTS; SAPROPEL DEPOSITION	This review and synthesis weaves various multiproxy data into a single coherent narrative for the latest Pleistocene-Holocene paleoclimatic and paleoceanographic evolution of the Black Sea, Marmara Sea and the Aegean Sea. This narrative, referred to as the "Outflow Hypothesis " rests on several key observations and interpretations which are incompatible with the suggestion that the post-LGM reconnection of the Black Sea basin to the global ocean occurred as a catastrophic flood. The widespread occurrence of sub-storm-wavebase uppermost Pleistocene to lower Holocene sediments across the southwestern Black Sea shelf at elevations as shallow as -78 m shows that the level of the Neoeuxine Lake (today's Black Sea) between 12.3 cal ka and 9.5 cal ka was high enough to spill outward into the Marmara Sea over the shallow sill in the southern Strait of Bosphorus (-37 m today). Southwest-prograded clinoforms immediately south of the strait in the northeastern Marmara Sea record the development of an early Holocene (11.1-10.2 cal ka) mid-shelf delta (delta 1) showing 3.3 km of aggressive progradation while its topset-to-foreset break climbed 8-9 m into a rising Marmara Sea. A streamlined southprograded barform in the throat of the strait and giant megaflutes along its thalweg confirm the vigorous outflow from the early Holocene Neoeuxine Lake required to explain the climbing delta 1 lobe. Multiproxy data from the northeastern Marmara Sea and southwestern Black Sea shelves indicate that the post-Last Glacial Maximum (LGM) reconnection of the Black Sea with the eastern Mediterranean occurred in a gradual fashion: first, at 10.2 cal ka, a salt wedge lifted the brackish outflow off the floor of the Strait of Bosphorus terminating delta 1 progradation; second, a more persistent density underflow introduced enough seawater strontium into the Black Sea to be taken up in mollusc shells by 9.5 cal ka, and finally a range of euryhaline marine organisms replaced lacustrine faunas when salinity levels became favourable by 7.5 cal ka. The onset of sapropel M1 deposition across the Marmara Sea followed the breach of the Strait of Dardanelles at 13.8 cal ka when, as originally suggested by other researchers, nutrient-rich highly saline Mediterranean waters forced lower density relict lacustrine waters to the surface and then out through the Strait of Dardanelles, initiating water-column stratification. Once the low-salinity cap was expelled, the deep waters of the fully saline Marmara Sea remained stagnant and sapropel accumulation continued. The onset of outflow from the Neoeuxine Lake at 11.1 cal ka reestablished water-column stratification, induced effective deep circulation across the Marmara Sea, and created a low salinity lid across the northern Aegean Sea, initiating sapropel S1 deposition in that area.	[Aksu, A. E.; Hiscott, R. 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Rev.	APR	2022	227								103960	10.1016/j.earscirev.2022.103960	http://dx.doi.org/10.1016/j.earscirev.2022.103960		MAR 2022	56	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	1C1NA		Green Submitted			2025-03-11	WOS:000792893400001
J	Kuwae, M; Tsugeki, NK; Amano, A; Agusa, T; Suzuki, Y; Tsutsumi, J; Leavitt, PR; Hirose, K				Kuwae, Michinobu; Tsugeki, Narumi K.; Amano, Atsuko; Agusa, Tetsuro; Suzuki, Yoshiaki; Tsutsumi, Jun; Leavitt, Peter R.; Hirose, Kotaro			Human-induced marine degradation in anoxic coastal sediments of Beppu Bay, Japan, as an Anthropocene marker in East Asia	ANTHROPOCENE			English	Article						Anthropocene; Eutrophication; Coastal; Sediments; Diatoms; Pigments	SETO INLAND SEA; DINOFLAGELLATE CYST; DIATOM ASSEMBLAGES; YOKOHAMA-PORT; HEAVY-METALS; TOKYO-BAY; LAND-USE; EUTROPHICATION; WATER; RECORD	The timing and magnitude of coastal marine degradation in East Asia during a possible transition from the Holocene to the proposed Anthropocene have still not been quantified with well-dated proxy records over centennial-to millennial timescales. This study uses multi-proxy sedimentary records to address this issue and to document biological and environmental changes in an anoxic coastal marine basin, Beppu Bay, Japan. Analysis of sedimentary diatom and pigment records revealed a notable change in diatom and phytoplankton communities and an abrupt increase in their productivity beginning 1960 s CE. Biogeochemical indices, including total organic carbon, total nitrogen, biogenic opal, bromine, and nickel as well as total sulfur, showed a notable increase in values, reflecting the enhanced primary productivity in the water column due to eutrophication, and reduced oxygen-levels in bottom conditions. Biological changes seen in diatom concentrations and communities were unprecedented over the last 1300 and-670 years, respectively. The eutrophication-associated proxy records demonstrate that anthropogenic degradation of the coastal marine environment occurred in the 1960 s, a time which was associated with the exponential, world-wide spread of coastal marine degradation during the Anthropocene, proposed to commence in the mid-20th century. Beppu Bay sediments have a wealth of excellent anthropogenic proxy records and, therefore, could be a representative archive of coastal Holocene-Anthropocene transitions in East Asia.	[Kuwae, Michinobu] Ehime Univ, Ctr Marine Environm Studies, Bunkyo Cho 2-5, Matsuyama, Ehime 7908577, Japan; [Tsugeki, Narumi K.] Matsuyama Univ, Fac Law, Matsuyama, Ehime 7908578, Japan; [Amano, Atsuko; Suzuki, Yoshiaki] Geol Survey Japan, Natl Inst Adv Ind Sci & Technol, Tsukuba, Ibaraki 308567, Japan; [Agusa, Tetsuro] Prefectural Univ Kumamoto, Fac Environm & Symbiot Sci, Kumamoto 8628502, Japan; [Tsutsumi, Jun] Univ Tsukuba, Sch Life & Environm Sci, Tsukuba, Ibaraki 3058572, Japan; [Leavitt, Peter R.] Univ Regina, Dept Biol, Regina, SK S4S 0A2, Canada; [Hirose, Kotaro] Waseda Univ, Fac Sci & Engn, Tokyo 1698555, Japan	Ehime University; National Institute of Advanced Industrial Science & Technology (AIST); University of Tsukuba; University of Regina; Waseda University	Kuwae, M (通讯作者)，Ehime Univ, Ctr Marine Environm Studies, Bunkyo Cho 2-5, Matsuyama, Ehime 7908577, Japan.	mkuwae@sci.ehime-u.ac.jp	Kuwae, Michinobu/AAG-3846-2020; Leavitt, Peter/A-1048-2013; Tsugeki, Narumi/AAV-2862-2021; Amano, Atsuko/P-5614-2016	Tsugeki, Narumi/0000-0003-1236-906X	Japan Society for the Promotion of Science [22340155, 21244073, 17K20045, 18H03609, 19H04284, 20K04089, 21H01170]; Mitsui & Co., Ltd. Environment Fund [R09-B022]; Grants-in-Aid for Scientific Research [21H01170, 20K04089, 21244073, 17K20045, 22340155, 18H03609, 19H04284] 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); Mitsui & Co., Ltd. Environment 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 study was supported financially by Grants-in-Aid for Scientific Research (grant number 22340155, 21244073, 17K20045, 18H03609, 19H04284, 20K04089, and 21H01170) from the Japan Society for the Promotion of Science and a research grant from Mitsui & Co., Ltd. Environment Fund (grant number R09-B022).	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J	Wu, XE; de Vernal, A; Fréchette, B; Moros, M; Perner, K				Wu, Xiner; de Vernal, Anne; Frechette, Bianca; Moros, Matthias; Perner, Kerstin			The signal of climate changes over the last two millennia in the Gulf of St. Lawrence, eastern Canada	QUATERNARY RESEARCH			English	Article						Gulf of St; Lawrence; Sea-surface temperature; Sea-surface salinity; Sea-ice cover; Dinocysts; Pollen; Late Holocene; Palynology; Paleoclimate	SEA-SURFACE CONDITIONS; NORTHERN NORTH-ATLANTIC; RECENT MARINE-SEDIMENTS; DINOFLAGELLATE CYSTS; ICE COVER; HOLOCENE; POLLEN; VARIABILITY; VEGETATION; RECORD	Climate changes over the past two millennia in the central part of the Gulf of St. Lawrence are documented in this paper with the aim of determining and understanding the natural climate variability and the impact of anthropogenic forcing at a regional scale. The palynological content (dinocysts, pollen, and spores) of the composite marine sediment core MSM46-03 collected in the Laurentian Channel was used to reconstruct oceanographic and climatic changes with a multidecadal temporal resolution. Sea-surface conditions, including summer salinity and temperature, sea-ice cover, and primary productivity, were reconstructed from dinocyst assemblages. Results revealed a remarkable cooling trend of about 4 degrees C after 1230 cal yr BP (720 CE) and a culmination with a cold pulse dated to 170-40 cal yr BP (1780-1910 CE), which likely corresponds to the regional signal of the Little Ice Age. This cold interval was followed by a rapid warming of about 3 degrees C. In the pollen assemblages, the decrease of Pinus abundance over the past 1700 yr suggests changes in wind regimes, likely resulting from increased southerly incursions of cold and dry Arctic air masses into southeastern Canada.	[Wu, Xiner; de Vernal, Anne; Frechette, Bianca] Univ Quebec Montreal UQAM, Geotop, 201 Ave President Kennedy, Montreal, PQ H3C 3P8, Canada; [Moros, Matthias; Perner, Kerstin] Leibniz Inst Balt Sea Res Warnemunde, Seestr 15, D-18119 Rostock, Germany	University of Quebec; University of Quebec Montreal; Leibniz Institut fur Ostseeforschung Warnemunde	Wu, XE (通讯作者)，Univ Quebec Montreal UQAM, Geotop, 201 Ave President Kennedy, Montreal, PQ H3C 3P8, Canada.	xiner.wu02@gmail.com	Wu, Xiner/KBQ-9897-2024; de Vernal, Anne/D-5602-2013	, Xiner/0000-0002-4072-392X	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); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	We thank the scientific party of the R/V Maria S. Merian for offering the samples from core MSM46-03. This study was supported by the Fonds de Recherche du Quebec-Nature et technologies (FRQNT) and the Natural Sciences and Engineering Research Council (NSERC) of Canada. We thank Matthew Peros for constructive comments on an earlier version of the article and Estelle Allan for help in the palynological laboratory. We are grateful to the editor Thomas Lowell and the reviewers Francine McCarthy and Jennifer Galloway for their thoughtful comments and suggestions.	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Res.	MAR	2022	106						28	43	PII S0033589421000569	10.1017/qua.2021.56	http://dx.doi.org/10.1017/qua.2021.56			16	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	ZZ8MS					2025-03-11	WOS:000773519500004
J	Singh, YR; Rudra, A; Singh, SP; Dutta, S; Devi, MS; Devi, NR				Singh, Y. Raghumani; Rudra, Arka; Singh, Sh Priyokumar; Dutta, Suryendu; Devi, M. Sapana; Devi, N. Reshma			Palynological and organic geochemical studies of the middle Eocene Siju Formation of Garo Hills, Meghalaya, India	JOURNAL OF EARTH SYSTEM SCIENCE			English	Article						Rock-Eval pyrolysis; MECO; biomarker; palynology; Siju Formation; Meghalaya	DINOFLAGELLATE CYSTS; DEPOSITIONAL ENVIRONMENT; MOLECULAR COMPOSITION; CORALLINE ALGAE; SEDIMENTS; BIOMARKER; INDICATORS; PALEOCENE; BIOSTRATIGRAPHY; HYDROCARBONS	Detailed palynological and organic geochemical analysis of middle Eocene marlstones from the Siju Formation, Garo Hills of Meghalaya, were undertaken. All marl samples contained abundant organic wall dinoflagellate cysts and a few number of spores-pollen grains, foraminiferal linings and calcareous foraminifera. The palynological assemblage consists of 21 genera and 35 species with fungal remains. The occurrence of palynofloral assemblage indicates the prevalence of tropical-subtropical with humid climatic conditions. The deposition environment of the Siju Formation has been interpreted as the neritic setting. Organic matter is thermally immature representing type III-type IV kerogen with low total organic carbon (<0.72%). The biomarkers suggest microbial degradation of both reworked and terrestrial organic matter. Occurrence of polycyclic aromatic hydrocarbons indicate charred biomass transported from the land.	[Singh, Y. Raghumani; Singh, Sh Priyokumar; Devi, M. Sapana; Devi, N. Reshma] Manipur Univ, Dept Earth Sci, Imphal 795003, Manipur, India; [Rudra, Arka; Dutta, Suryendu] Indian Inst Technol, Dept Earth Sci, Mumbai 400076, Maharashtra, India; [Rudra, Arka] Aarhus Univ, Dept Geosci, Aarhus, Denmark	Manipur University; Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Bombay; Aarhus University	Singh, YR (通讯作者)，Manipur Univ, Dept Earth Sci, Imphal 795003, Manipur, India.	yengmani@gmail.com		Rudra, Arka/0000-0001-9970-2544	Science and Research Board, Government of India [EEQ/2016/000062]; Indian National Science Academy, New Delhi [INSA/SP/VS-27/2017-2018/518]; ONGC, India	Science and Research Board, Government of India; Indian National Science Academy, New Delhi; ONGC, India	YRS would like to acknowledge the Science and Research Board, Government of India (Grant No. EEQ/2016/000062) and Indian National Science Academy, New Delhi (INSA/SP/VS-27/2017-2018/518) for financial support. YRS and SPS acknowledge to the ONGC, India for supporting to carry out Rock-Eval analysis. The authors are grateful to Dr Robert A Fensome (Natural Resources Canada, Geological Survey of Canada) and Dr Przemyslaw Gedl (Polish Academy of Sciences, Institute of Geological Sciences, Research Centre in Cracow) for helping identification of dinoflagellate cysts and Mr Sumit, Dr Anuradha, Research Scholars of IIT, Mumbai for their valuable support during organic geochemical analysis. We also are thankful to W Ajoykumar Singh, T Ngathoi Chanu and N Sanjit Singh for help during sample analysis.	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Earth Syst. Sci.	MAR	2022	131	1							19	10.1007/s12040-021-01760-6	http://dx.doi.org/10.1007/s12040-021-01760-6			15	Geosciences, Multidisciplinary; Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Science & Technology - Other Topics	YE8SR					2025-03-11	WOS:000741389900001
J	Hu, ZX; Liu, YY; Deng, YY; Tang, YZ				Hu, Zhangxi; Liu, Yuyang; Deng, Yunyan; Tang, Ying Zhong			The Notorious Harmful Algal Blooms-Forming Dinoflagellate <i>Prorocentrum donghaiense</i> Produces Sexual Resting Cysts, Which Widely Distribute Along the Coastal Marine Sediment of China	FRONTIERS IN MARINE SCIENCE			English	Article						resting cyst mapping; fluorescence in situ hybridization (FISH); harmful algal blooms (HABs); life cycle (history); Prorocentrum donghaiense	MULTIPLE SEQUENCE ALIGNMENT; TOXIC DINOFLAGELLATE; GYMNODINIUM-CATENATUM; ANNOTATED CHECKLIST; TIME-SERIES; NEW-ZEALAND; YELLOW SEA; PHYTOPLANKTON; DINOPHYCEAE; IDENTIFICATION	The armored dinoflagellate Prorocentrum donghaiense distributes globally and has been forming large scale and dense ecosystem disruptive algal blooms (EDABs) in the East China Sea (ECS) almost every year since the 1990s and often in other coastal waters of the world. It has long been a mystery, however, about how these blooms were seeded or where the initiating population came from. In this work, we provide a more feasible and universal seeding mechanism, formation of resting cysts. Using light microscopy, we confirmed sexual reproduction according to the observations of mating cells in pairs, planozygotes having two similar flagella, darkened and thick-walled resting cysts with smooth surface, and germination processes of resting cyst. Using morpho-molecular detection, we confirmed P. donghaiense resting cyst in the field, including the positive detections of polymerase chain reaction (PCR) using species-specific primers and then the fluorescence in situ hybridization (FISH) using species-specific probes, and further confirmation via single-cell sequencing for the individual FISH-detected cysts. Furthermore, the distribution and abundance of P. donghaiense cysts along the coast of China Seas were mapped using an approach combining real-time PCR (qPCR) and FISH, with the qPCR quantification taking into account the doubled copy number of LSU rRNA gene in resting cysts. Resting cysts of this species were found to widely distribute in the Yellow Sea (YS), ECS, and South China Sea (SCS), with a relatively low abundance at most sampling sites, but to be absent in the eight samples from the Bohai Sea (BS). Resting cyst production confirmed with evidences from both laboratory cultures and field sediments and the extensive distribution of cysts in the China Seas, as the first case in planktonic species of Prorocentrum, not only filled up a knowledge gap about the life history of P. donghaiense but also provided a possible mechanistic facility to seed the annual blooms in the ECS and the global distribution of the species.	[Hu, Zhangxi; Liu, Yuyang; Deng, Yunyan; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Hu, Zhangxi; Deng, Yunyan; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Hu, Zhangxi; Liu, Yuyang; Deng, Yunyan; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, 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, Peoples R China.; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China.; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China.	yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023; Li, Yang/KFB-5350-2024		National Science Foundation of China [41476142]; Science & Technology Basic Resources Investigation Program of China [2018FY100200]; Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao) [2018SDKJ0504-2]; National Natural Science Foundation of China [41976134, 41776125]; Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao) [LMEES-YTSP-2018-01-04]	National Science Foundation of China(National Natural Science Foundation of China (NSFC)); Science & Technology Basic Resources Investigation Program of China; Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao)	& nbsp;This research was funded by the National Science Foundation of China, grant number 41476142, the Science & Technology Basic Resources Investigation Program of China, grant number 2018FY100200, the Marine S&T Fund of Shandong Province for Pilot National Laboratory for Marine Science and Technology (Qingdao), grant number 2018SDKJ0504-2, the National Natural Science Foundation of China, grant numbers 41976134 and 41776125, and the Youth Talent Support Program of the Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao), grant number LMEES-YTSP-2018-01-04.	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Mar. Sci.	FEB 28	2022	9								826736	10.3389/fmars.2022.826736	http://dx.doi.org/10.3389/fmars.2022.826736			16	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	ZZ0AU		gold			2025-03-11	WOS:000772940600001
J	Emmanouilidis, A; Panagiotopoulos, K; Kouli, K; Avramidis, P				Emmanouilidis, Alexandros; Panagiotopoulos, Konstantinos; Kouli, Katerina; Avramidis, Pavlos			Late-Holocene paleoenvironmental and land-use changes in Western Greece based on a sediment record from Klisova lagoon	HOLOCENE			English	Article						coastal geomorphology; Eastern Mediterranean; micropaleontology; palynology; XRF	ACHELOOS RIVER DELTA; SEA-LEVEL CHANGE; CLIMATE VARIABILITY; ENVIRONMENTAL-CHANGES; VEGETATION HISTORY; DEPOSITIONAL ENVIRONMENT; MEDITERRANEAN REGION; COASTAL-PLAIN; EVOLUTION; LAKE	In this study, we present the findings of a sediment core retrieved from Klisova lagoon, Western Greece, an area with a long record of documented human presence. The recovered deposits were subjected to sedimentological, XRF, and micropaleontological analyses. For the last 4700 cal BP, the freshwater influx, the progradation of the Evinos river delta and related geomorphological changes control the environmental conditions in the lagoon. Considering the centennial temporal resolution of our analyses, small offsets of c.a. 50 years due to lack of regional reservoir correction do not considerably impact the reported radiocarbon ages. Prior to 4000 cal BP, a relatively shallow water depth, significant terrestrial/freshwater input and increased weathering in the lagoon area are inferred. Elemental proxies and increased dinoflagellate cyst and foraminiferal abundances, which indicate marine conditions with prominent freshwater influxes, point to the gradual deepening of the lagoon up to 2000 cal BP. The marine and freshwater condition equilibrium sets at 1300 cal BP, with the lagoonal system reaching its present state. Maxima of anthropogenic pollen indicators during the Mycenaean (3200 cal BP), Hellenistic (2200 cal BP), and Late Byzantine (800 cal BP) periods suggest intervals of increased anthropogenic activities in the area.	[Emmanouilidis, Alexandros; Avramidis, Pavlos] Univ Patras, Dept Geol, Panepistimioupolh Patrwn, Patras 26504, Greece; [Panagiotopoulos, Konstantinos] Univ Cologne, Inst Geol & Mineral, Cologne, Germany; [Panagiotopoulos, Konstantinos; Kouli, Katerina] Natl Kapodistrian Univ Athens, Fac Geol & Geoenvironm, Athens, Greece	University of Patras; University of Cologne; National & Kapodistrian University of Athens	Emmanouilidis, A (通讯作者)，Univ Patras, Dept Geol, Panepistimioupolh Patrwn, Patras 26504, Greece.	alex.emman@upatras.gr	Panagiotopoulos, Konstantinos/P-3823-2019; Emmanouilidis, Alexandros/GQI-3205-2022; Kouli, Katerina/M-8243-2013; AVRAMIDIS, PAVLOS/AAA-3097-2021; Panagiotopoulos, Konstantinos/H-1190-2012	Kouli, Katerina/0000-0003-1656-1091; Emmanouilidis, Alexandros/0000-0002-1403-8080; AVRAMIDIS, PAVLOS/0000-0002-8204-970X; Panagiotopoulos, Konstantinos/0000-0002-3158-7962	European Union (European Social Fund -ESF) [MIS-5000432]	European Union (European Social Fund -ESF)(European Union (EU)European Social Fund (ESF))	The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This research is co-financed by Greece and the European Union (European Social Fund -ESF) through the Operational Programme << Human Resources Development, Education and Lifelong Learning >> in the context of the project "Strengthening Human Resources Research Potential via Doctorate Research" (MIS-5000432), implemented by the State Scholarships Foundation (...).	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J	Rodrigues, RV; Patil, JS; Anil, AC				Rodrigues, R., V; Patil, J. S.; Anil, A. C.			Dinoflagellates cyst assemblage concerning trophic index for eutrophication from major ports along the west coast of India	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Ports; Eutrophication; Trophic index; Harmful Algal Blooms	HARMFUL ALGAL BLOOMS; RECENT SEDIMENTS; WATER-QUALITY; EAST-COAST; SOUTHWEST COAST; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; COCHIN BACKWATERS; SURFACE SEDIMENTS; TOKYO-BAY	An overview of dinoflagellates cysts assemblage is presented as a trophic index for three monsoon-influenced estuarine and marine ports along the Indian coast. The cyst distribution (including harmful species) showed a trend of highest abundance and species number in highly eutrophicated estuarine (Cochin-south) followed by medium (New-Mangalore-central) and low (Kandla-north) levels of eutrophicated marine ports. The investigation revealed four new species in the region (Bitectatodinium spongium, Gonyaulax elongatum, Brigantedinium sp. and potential harmful species Blixaea quinquecornis-cyst similar to planktonic). Autotrophs dominance in the highly productive Cochin and New-Mangalore ports reveals that, in eutrophic systems, heterotrophs need not always be dominant. The indicator taxa (Polykrikos, Protoperidnium, and Lingulodinium) presence in high density indicated a eutrophic system. This study concludes cyst (species numbers/Fisher-alpha index/indicator species) as potential eutrophication proxies and emphasizes greater harmful-algal-bloom risks in the high trophic-index ports (Cochin and New-Mangalore).	[Rodrigues, R., V; Patil, J. S.; Anil, A. C.] CSIR Natl Inst Oceanog, Panaji 403004, Goa, India; [Rodrigues, R., V] Goa Univ, Sch Earth Ocean & Atmospher Sci, Taleigao Plateau 403206, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO); Goa University	Patil, JS (通讯作者)，CSIR Natl Inst Oceanog, Panaji 403004, Goa, India.	patilj@nio.org			DG Shipping, Ministry of Shipping, Govt. of India [6880]; UGC, India [6880];  [GAP 2429]	DG Shipping, Ministry of Shipping, Govt. of India; UGC, India(University Grants Commission, India); 	The authors are grateful to the Director of CSIR-National Institute of Oceanography for providing support and encouragement. The authors thank DG Shipping, Ministry of Shipping, Govt. of India for providing the funding for BAMPI-Ballast Water Management Program India (GAP 2429) . We thank Dr. S.S. Sawant, Dr. D. Desai, Dr. L. Khandeparker, Mr. K. Venkat, and Mr. K. Mapari for coordinating Port Biological Baseline Survey (PBBS) at Cochin, New Mangalore, and Kandla port. We also thank the project staff, who were involved in the PBBS, for their help during sampling. We acknowledge two reviewers for their suggestions to improve the manuscript. First author also acknowledges UGC, India for Maulana Azad National Fellowships. This is an NIO contribution No. 6880.	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Pollut. Bull.	JUN	2022	176								113423	10.1016/j.marpolbul.2022.113423	http://dx.doi.org/10.1016/j.marpolbul.2022.113423		FEB 2022	14	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	1A8PB	35219079				2025-03-11	WOS:000792010400004
J	Pinzon, D; Rodriguez, G; Rincon-Martinez, D; Prampard, MB; Restrepo, S; Vento, B; Martinez, J; Guerstein, GR; Panera, JPP; de la Parra, F; Vargas, MC				Pinzon, Diego; Rodriguez, Guillermo; Rincon-Martinez, Daniel; Prampard, Mercedes B.; Restrepo, Sandra; Vento, Barbara; Martinez, Jhonatan; Guerstein, G. Raquel; Panera, Juan P. Perez; De la Parra, Felipe; Vargas, Maria Carolina			Late Neogene chronostratigraphy and integrated paleoecological trends in the southwestern Caribbean Sea	MARINE MICROPALEONTOLOGY			English	Article						Biostratigraphy; Palynology; Calcareous nannofossils; Benthic foraminifera; Tortonian-Gelasian; Paleoceanography	CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; WALLED DINOFLAGELLATE CYSTS; RECENT BENTHIC FORAMINIFERA; EASTERN EQUATORIAL PACIFIC; GULF-OF-MEXICO; LATE MIOCENE; NORTH-ATLANTIC; PLIOCENE TAXONOMY; PALYNOLOGICAL EVIDENCE; GENUS CATINASTER	Palynology of the Neogene marine stratigraphic sequences in tropical latitudes is poorly studied Most studies focus on lower to middle Miocene deposits in the Caribbean, emphasizing the biostratigraphic value of dinoflagellate cysts. The palynological and calcareous nannofossil analysis of 50 samples from DSDP Hole 502A and their integration with the paleomagnetic and planktonic foraminifera data reveal a detailed and reliable chronostratigraphic framework, and the interpretation of the paleobathymetric and paleoenvironmental evolution of the sequence. Fossil content in a continuous late Tortonian to late Gelasian (-7.56-1.80 Ma) sequence of deep marine sediments serves to calibrate ages of dinoflagellate cysts, and comparison with high latitude records reveals synchronous (Operculodinium janduchenei, Selenopemphix dionaeacysta, Barssidinium taxandrianum, and Lejeunecysta interrupta) and asynchronous events (Quadrina? condita) with biostratigraphic potential for the southwestern Caribbean Sea. Our results highlight the importance of analyzing continental palynomorphs in deep-marine deposits to increase the temporal resolution of future palynostratigraphic schemes. Micropaleontogical data indicate a lower bathyal-abyssal environment and four paleoceanographic settings defined by changes in surface water productivity. These intervals fluctuate from mesotrophic-oligotrophic (-7.56-6.31 Ma) to eutrophic (-6.18-4.98 Ma), oligotrophic (-4.74-3.41 Ma), and mesotrophic surface water conditions (-3.26-1.80 Ma). Changes in trophic conditions are strongly related to the paleoceanographic reorganization associated with the constriction and complete closure of the Central American Seaway, seasonal upwelling episodes, and the input of terrigenous organic matter probably transported from southern Central America and northern South America by turbidity currents.	[Pinzon, Diego; Prampard, Mercedes B.; Vento, Barbara] Consejo Nacl Invest Cient & Tecn, IANIGLA, CCT, Mendoza, Argentina; [Rodriguez, Guillermo; Rincon-Martinez, Daniel; Restrepo, Sandra; De la Parra, Felipe; Vargas, Maria Carolina] ECOPETROL, Inst Colombiano Petr, Santander, Spain; [Guerstein, G. Raquel] Univ Nacl Sur, Dept Geol, CONICET, INGEOSUR, Bahia Blanca, Buenos Aires, Argentina; [Panera, Juan P. Perez] UNLP, CONICET, FCNyM, Museo La Plata, Paseo Bosque S-N, La Plata, Argentina; [Martinez, Jhonatan] Smithsonian Trop Res Inst, Ancon, Panama; [Martinez, Jhonatan] Univ Caldas, Inst Invest Estratig, Manizales, Colombia	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University Nacional Cuyo Mendoza; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Museo La Plata; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Smithsonian Institution; Smithsonian Tropical Research Institute; Universidad de Caldas	Pinzon, D (通讯作者)，Consejo Nacl Invest Cient & Tecn, IANIGLA, CCT, Mendoza, Argentina.	dpinzon@mendoza-conicet.gob.ar	Martinez, Jhonatan/JMQ-9384-2023; Rodriguez, Guillermo/JPA-4743-2023; Perez Panera, Juan/HSI-3366-2023	Pinzon, Diego Alberto/0000-0001-8582-2756; Guerstein, G. Raquel/0000-0003-1623-1084; Perez Panera, Juan Pablo/0000-0002-2326-0732	Ph.D. Thesis of Diego Pinzon; Consejo Nacional de Investigaciones Cientif-icas y Tecnicas (CONICET, Argentina); AASP-The Palynological Society (Student Research Grant); Integrated Ocean Drilling Program (IODP); Gulf Coast Repository (GCR)	Ph.D. Thesis of Diego Pinzon; Consejo Nacional de Investigaciones Cientif-icas y Tecnicas (CONICET, Argentina)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); AASP-The Palynological Society (Student Research Grant); Integrated Ocean Drilling Program (IODP); Gulf Coast Repository (GCR)	This study is part of the Ph.D. Thesis of Diego Pinzon, supported with financial assistance of the Consejo Nacional de Investigaciones Cientif-icas y Tecnicas (CONICET, Argentina) . Partial funding was also provided by the AASP-The Palynological Society (Student Research Grant) . Samples were provided by the Integrated Ocean Drilling Program (IODP) -Gulf Coast Repository (GCR) . We also thank to the Instituto Colombiano del Petroeo-ECOPETROL for providing the facilities for the palynological sample processing. We are grateful for the suggestions made by the reviewers that improved our manuscript.	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J	Over, JS; Pospelova, V				Over, Jin-Si; Pospelova, Vera			Last Interglacial (MIS 5e) sea surface hydrographic conditions in coastal southern California based on dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cysts; Last Interglacial; Marine isotope stages 6-5d; Santa Barbara Basin; ODP Hole 893A; Paleo-climate; Sea-surface temperature; Marine primary productivity	SANTA-BARBARA BASIN; CURRENT SYSTEM; NORTH-ATLANTIC; PRIMARY PRODUCTIVITY; CLIMATE VARIABILITY; EASTERN ATLANTIC; HIGH-LATITUDES; SEDIMENT TRAP; PACIFIC-OCEAN; RECORD	The first high resolution record of dinoflagellate cysts-110-155 kyr over Termination II and the Last Interglacial in the Santa Barbara Basin, California from ODP Hole 893A details a complex paleoceanographic history. Variation in cyst relative abundances, concentrations, and diversity reflects climatic and ocean circulation changes, and the assemblages are used to make qualitative reconstructions of sea surface temperature (SST) and annual primary productivity. The dominance of heterotrophic Brigantedinium spp. throughout the section indicates an important influence of coastal upwelling on the basin. Based on the dinoflagellate cyst assemblages, five zones are identified, which approximately correspond to the marine isotope stage boundaries and their associated changes in SST and sea level. Cooler intervals, MIS 6 and MIS 5d, are characterized by cold-water indicator species Selenopemphix undulata whereas thermophilic taxon Spiniferites mirabilis characterizes a warm MIS 5e. In contrast to other studies in the Pacific, the data exhibits a one to two-thousand-year cooling event-129 kyr that correlates to the Termination II sea level still-stand of the two-step deglaciation. A significant increase in cyst concentrations in the latest MIS 5e implies enhanced primary production due to increased seasonal upwelling and the warm, nutrient rich waters entering the basin after sea level stabilizes near modern levels. The hydrological evolution and cyst signal of the Last Interglacial is similar to the development of the Holocene in the Santa Barbara Basin, but the sustained presence of Spiniferites mirabilis across MIS 5e indicates SSTs were higher than modern conditions.	[Over, Jin-Si; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, 3800 Finnerty Rd, Victoria, BC V8P 5C2, Canada; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, 116 Church St SE, Minneapolis, MN 55455 USA; [Over, Jin-Si] 384 Woods Hole Rd, Woods Hole, MA 02543 USA	University of Victoria; University of Minnesota System; University of Minnesota Twin Cities	Over, JS (通讯作者)，384 Woods Hole Rd, Woods Hole, MA 02543 USA.	jover@uvic.ca		Pospelova, Vera/0000-0003-4049-8133	Natural Science and Engineering Research Council of Canada (NSERC) [RGPIN/6388-2015]; University of Victoria; Arne Lane Graduate Fellowships	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); University of Victoria; Arne Lane Graduate Fellowships	Sediment samples were provided by the Integrated Ocean Drilling Program (IODP) . We thank C. Broyles and P. Rumford for their assis-tance in subsampling the sediments. Funding for this research was provided by the Natural Science and Engineering Research Council of Canada (NSERC) to V.P. (Grant RGPIN/6388-2015) . Graduate research of J.R.O was supported by the University of Victoria and the Arne Lane Graduate Fellowships. We are grateful to the Editor (Dr. Alex Dickson) and two anonymous reviewers for constructive suggestions which improved this manuscript.	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Paleoclimatol. Paleoecol.	APR 1	2022	591								110875	10.1016/j.palaeo.2022.110875	http://dx.doi.org/10.1016/j.palaeo.2022.110875		FEB 2022	20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	1A9LI					2025-03-11	WOS:000792068300001
J	Riding, JB; Mariani, E; Fensome, RA				Riding, James B.; Mariani, Erica; Fensome, Robert A.			A review of the Jurassic dinoflagellate cyst genus <i>Gonyaulacysta</i> Deflandre 1964 emend. nov	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Biostratigraphy; Dinoflagellate cysts; Gonyaulacysta; Middle-Late Jurassic; Provincialism; Taxonomy	RAYNAUD 1978 LENTIN; ROSS-ISLAND AREA; NORTH-WEST SHELF; GUSTAV-GROUP; MIDDLE; ASSEMBLAGES; PALYNOLOGY; BASIN; BAJOCIAN; PALYNOSTRATIGRAPHY	The Middle-Late Jurassic gonyaulacacean dinoflagellate cyst genus Gonyaulacysta is characterised by an epicyst which is around twice the length of the hypocyst. The sulcus is L-type and may be slightly sigmoidal in shape, but is never S-type sensu stricto. The forms with slightly sigmoidal L-type sulcuses may have developed into species with S-type sulcuses. Gonyaulacysta jurassica, the holotype of which is the nomenclatural type of the genus, had a global distribution. A total of 151 species have been assigned to Gonyaulacysta although 126 of these have been transferred to other genera. Prior to this contribution, 25 species were accepted in the current Lentin and Williams Index. This is herein reduced to eight and 18 species are transferred to other genera. The accepted species are: Gonyaulacysta adecta stat. nov., emend. nov.; Gonyaulacysta australica comb. nov., emend. nov.; Gonyaulacysta ceratophora; Gonyaulacysta desmos stat. nov., emend. nov.; Gonyaulacysta dualis emend. nov.; Gonyaulacysta fenestrata emend. nov.; Gonyaulacysta jurassica emend. nov.; and Gonyaulacysta longicornis stat nov., emend. nov. These species form a closely related plexus, and are distinguished on differences in cavation style, form of sutural crests/ridges and size of the apical horn. All except Gonyaulacysta australica are reliable marker taxa. Our main taxonomic proposals involve the elevation of all subspecies and varieties of species here retained in Gonyaulacysta to species rank. or their synonymisation. This avoids cumbersome infraspecific names. Gonyaulacysta exhibits substantial provincialism; for example Gonyaulacysta dualis is confined to the Oxfordian-Kimmeridgian of the Boreal Realm. Gonyaulacysta adecta, Gonyaulacysta desmos and Gonyaulacysta longicornis are present in the Bathonian to Oxfordian of Laurasia and surrounding areas. Three species, Gonyaulacysta australica, Gonyaulacysta ceratophora and Gonyaulacysta fenestrata, are restricted to the Oxfordian to Tithonian of Australasia. Gonyaulacysta adecta and the cosmopolitan Gonyaulacysta jurassica both exhibit overall size increases throughout the Bathonian to Kimmeridgian of Europe. Crown Copyright (C) 2022 Published by Elsevier B.V. All rights reserved.	[Riding, James B.] British Geol Survey, Keyworth NG12 5GG, Notts, England; [Mariani, Erica] Univ Exeter, Coll Engn Math & Phys Sci, Camborne Sch Mines, Penryn Campus,Treliever Rd, Penryn TR10 9FE, Cornwall, England; [Fensome, Robert A.] Geol Survey Canada Atlantic, Bedford Inst Oceanog, POB 1006, Dartmouth, NS B2Y 4A2, Canada	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Exeter; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; em608@exeter.ac.uk; rob.fensome@canada.ca						[Anonymous], 1983, DINOFLAGELLATE OPPEL, DOI DOI 10.4095/119736; [Anonymous], 1994, BRIT GEOLOGICAL SURV; [Anonymous], 2016, B ASOC LATINOAM PALE; [Anonymous], 1985, Canadian Technical Report of Hydrography and Ocean Sciences; [Anonymous], 1992, ARCTIC GEOLOGY PETRO; ARHUS N, 1989, NORSK GEOL TIDSSKR, V69, P39; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; Balech E., 1988, Los dinoflagelados del Atlantico Sudoccidental, V1, P310; BEJU D, 1980, Palynology, V4, P234; Beju D, 1979, PALYNOLOGY, V3, P279; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BJAERKE T, 1977, Norsk Polarinstitutt Arbok, P83; Brenner W., 1988, T B MIKROPAL ON MITT, V6, P115; Brideaux W.W., 1976, Geological Survey of Canada Bulletin, V259, DOI [10.4095/119813, DOI 10.4095/119813]; Bujak J.P, 1983, AM ASS STRATIGRAPHIC, V13, P203; Burger D., 1996, Palynology, V20, P49; Butschli O, 1885, PROTOZOA HG BRONNS K, P865; Carbonell-Moore MC, 2022, PHYCOLOGIA, V61, P195, DOI 10.1080/00318884.2021.2024413; Churchill D. 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Palaeobot. Palynology	APR	2022	299								104605	10.1016/j.revpalbo.2022.104605	http://dx.doi.org/10.1016/j.revpalbo.2022.104605		FEB 2022	37	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ZP1OR		Green Accepted			2025-03-11	WOS:000766194900001
J	Guerrero-Murcia, LA; Helenes, J				Guerrero-Murcia, Luis-Andres; Helenes, Javier			Statistic biostratigraphy and paleoecology of tropical Upper Cretaceous dinoflagellate cysts	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Fossil dinoflagellates; Upper cretaceous; Tropical localities; Statistic biostratigraphy	EASTERN EQUATORIAL PACIFIC; MAASTRICHTIAN PALYNOMORPHS; BENTHIC FORAMINIFERA; SURFACE SEDIMENTS; WESTERN; SEA; BASIN; COAST; INDICATORS; RANKING	The statistical and probabilistic analyses of a database of Upper Cretaceous tropical dinoflagellate cysts from Venezuela allow us to recognize 21 species in the optimal stratigraphic sequence. Compilation of the dinoflagellate cysts reported in ten studies of Upper Cretaceous tropical localities from northern South America and the Gulf of Guinea allow the recognition of a rich assemblage (262 species), dominated by gonyaulacoid (129 spp), followed by protoperidinioid (82 spp), areoligeroid (29 spp), gymnodinioid (12 spp) and ceratioid (10 spp) taxa. Seventy-three species in the tropical database are reported in both regions, allowing the age calibration of the optimal sequence from Venezuela. The proposed final sequence of bioevents allows recognition of most stages in tropical Upper Cretaceous strata. The high diversity of the Spiniferites-Achomosphaera group and scarcity of Impagidinium indicates shallow marine depositional environments for most of the Upper Cretaceous tropical localities included.The dominance of gonyaulacoid species in the tropical database suggests that these were the dominant primary producers in the tropical Late Cretaceous oceans.	[Guerrero-Murcia, Luis-Andres; Helenes, Javier] Ctr Estudios Cient & Educ Super Ensenada, Geol Dept, Km 107 Carretera Tijuana, Ensenada 22860, Baja California, Mexico		Guerrero-Murcia, LA (通讯作者)，Ctr Estudios Cient & Educ Super Ensenada, Geol Dept, Km 107 Carretera Tijuana, Ensenada 22860, Baja California, Mexico.	lguerrero@cicese.edu.mx		GUERRERO, LUIS/0000-0003-1751-0341	CONACYT -CICESE [675403]	CONACYT -CICESE	Thanks to CONACYT -CICESE, for financial support to the first author throughout this study with the Ph.D. scholarship 675403. Professor Felix Gradstein (University of Oslo, Norway) is greatly thanked for help in the formation of the subject of this study, advising on the RASC method and its applications, and giving invaluable and vital assistance with the dataset. The author wishes to thank Carlos Reinoza (CICESE investigator) for making the map. Thanks, are also due to Antonio Gonz ' alez, Loic Peiffer, and Gabriel Flores for constructive comments on early versions of the manuscript. We thank the editor and reviewers for their useful comments that improved the paper.	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L., 2017, Am. Assoc. Stratigraphic Palynologist Data Ser.; WILLIAMS GL, 1977, MAR MICROPALEONTOL, V2, P223, DOI 10.1016/0377-8398(77)90012-3; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Yepes Oscar, 2001, Palynology, V25, P217, DOI 10.2113/0250217; Yoris F., 1997, GEOLOGY VENEZUELA GE, V1, P1; Zegarra M, 2011, MAR MICROPALEONTOL, V81, P107, DOI 10.1016/j.marmicro.2011.09.005	115	5	5	0	0	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	APR	2022	115								103730	10.1016/j.jsames.2022.103730	http://dx.doi.org/10.1016/j.jsames.2022.103730		FEB 2022	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	0M7AI					2025-03-11	WOS:000782301900001
J	Mohamed, Z; Alamri, S; Hashem, M				Mohamed, Zakaria; Alamri, Saad; Hashem, Mohamed			Inhibitory effects of the brown macroalga <i>Turbinaria ornata</i> on cyst germination and progeny cells of five harmful dinoflagellate species	OCEANOLOGIA			English	Article						Cysts; Dinoflagellates; Harmful blooms; Macroalgal allelopathy	RED-SEA; HETEROSIGMA-AKASHIWO; RESTING CYSTS; BLOOMS; DINOPHYCEAE; MICROALGAE; EXTRACTS; COASTS	This study investigates the inhibitory effects of thalli and their extracts of the macroalga Turbinaria ornata on the germination of dinoflagellate cysts, previously isolated from Red Sea surface sediments . The experiments were conducted on cysts of five harmful dinoflagellate species including Alexandrium catenella, Cochlodinium polykrikos, Dinophysis accuminata, Prorocentrum cordatum and Scrippsiella trochoidea. The results showed neither macroalgal thalli nor their extracts had direct impact on the cyst germination of all species. Instead, these macroalgal materials remarkably affected the germling viability and culturability of progeny cells of these cysts. Dry macroalgal thalli exhibited stronger inhibitory effects on germling viability and cell culturability (IC50= 0.235-0.543, 0.385-1.43 mg mL (-1), respectively) than fresh thalli (IC50= 2.201-4.716, 2.17-7.18 mg mL (-1), respectively). The macroalgal ethanol extract was approximately 2-5 times more effective (IC50 = 0.012-0.047 and 0.024- 0.089 mg mL (-1), respectively) than aqueous extract (IC50 = 0.04-0.1 and 0.054-0.207 mg mL (-1), respectively) against the germling viability and vegetative progeny cells of all cyst species. Among different species, A. catenella and C. polykrikos germlings were more sensitive to macroalgal thalli and their extracts than those of S. trochoidea, P. cordatum and D. acuminata. Meanwhile, progeny cells of A. catenella exhibited the highest sensitivity to all macroalgal materials. Our results suggest that the use of T. ornata may be a promising strategy for inhibiting the division of progeny cells of dinoflagellate cysts and impairing the recurrence of HABs in confined coastal areas. (c) 2021 Institute of Oceanology of the Polish Academy of Sciences. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license ( http://creativecommons.org/licenses/by-nc-nd/4.0/ ).	[Mohamed, Zakaria] Sohag Univ, Fac Sci, Dept Bot, Sohag 82524, Egypt; [Alamri, Saad; Hashem, Mohamed] King Khalid Univ, Fac Sci, Biol Sci Dept, Abha, Saudi Arabia; [Hashem, Mohamed] Assiut Univ, Fac Sci, Bot & Microbiol Dept, Assiut, Egypt	Egyptian Knowledge Bank (EKB); Sohag University; King Khalid University; Egyptian Knowledge Bank (EKB); Assiut University	Mohamed, Z (通讯作者)，Sohag Univ, Fac Sci, Dept Bot, Sohag 82524, Egypt.	Zakaria.attia@science.sohag.edu.eg	Alamri, Saad/AGM-5459-2022; Hashem, Mohamed/AAG-3894-2020; Hashem, Mohamed/JVE-0875-2024	Hashem, Mohamed/0000-0003-2593-3387	Deanship of Scientific Research, King Khalid University [R.G.P. 1/25/42]	Deanship of Scientific Research, King Khalid University(King Khalid University)	The authors extend their appreciation to the Deanship of Scientific Research, King Khalid University for funding this work through research groups program under grant number R.G.P. 1/25/42. The authors have approved the final article.	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World-wide electronic publication, National University of Ireland; His E, 2000, ADV MAR BIOL, V37, P1; Jeong JH, 2000, J APPL PHYCOL, V12, P37, DOI 10.1023/A:1008139129057; Jin Q, 2003, J EXP MAR BIOL ECOL, V293, P41, DOI 10.1016/S0022-0981(03)00214-4; Kientz B, 2011, BOT MAR, V54, P457, DOI 10.1515/BOT.2011.053; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; Lewitus AJ, 2012, HARMFUL ALGAE, V19, P133, DOI 10.1016/j.hal.2012.06.009; Mardones JI, 2016, HARMFUL ALGAE, V55, P238, DOI 10.1016/j.hal.2016.03.020; Miyazono A, 2012, HARMFUL ALGAE, V16, P81, DOI 10.1016/j.hal.2012.02.001; Mohamed ZA, 2007, OCEANOLOGIA, V49, P337; Mohamed ZA, 2018, MAR ENVIRON RES, V140, P234, DOI 10.1016/j.marenvres.2018.06.019; Mohamed ZA, 2012, OCEANOLOGIA, V54, P287, DOI 10.5697/oc.54-2.287; Mohamed ZA, 2011, OCEANOLOGIA, V53, P121, DOI 10.5697/oc.53-1.121; Nagayama K, 2003, AQUACULTURE, V218, P601, DOI 10.1016/S0044-8486(02)00255-7; Nelson TA, 2013, NAUTILUS, V127, P156; Oh MY, 2010, J APPL PHYCOL, V22, P453, DOI 10.1007/s10811-009-9478-x; Patil V, 2020, MAR POLLUT BULL, V161, DOI 10.1016/j.marpolbul.2020.111752; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Salama AJ, 2018, J APPL PHYCOL, V30, P1943, DOI 10.1007/s10811-017-1345-6; Sultana B, 2009, MOLECULES, V14, P2167, DOI 10.3390/molecules14062167; Sun Aimei, 2007, Marine Science Bulletin (Beijing), V9, P36; Sun X, 2016, CHIN J OCEANOL LIMN, V34, P781, DOI 10.1007/s00343-016-4383-z; Sun YY, 2018, ENVIRON SCI POLLUT R, V25, P7844, DOI 10.1007/s11356-017-0958-2; Tang YZ, 2015, J APPL PHYCOL, V27, P531, DOI 10.1007/s10811-014-0338-y; Vahtera E, 2014, DEEP-SEA RES PT II, V103, P112, DOI 10.1016/j.dsr2.2013.05.010; Wang ZH, 2007, J PLANKTON RES, V29, P209, DOI 10.1093/plankt/fbm008; Ye CP, 2013, IERI PROC, V5, P209, DOI 10.1016/j.ieri.2013.11.094; Zeng HH, 2018, RSC ADV, V8, P17797, DOI 10.1039/c8ra01881b	37	0	0	2	15	POLISH ACAD SCIENCES INST OCEANOLOGY	SOPOT	POWSTANCOW WASZAWY 55, PL-81-712 SOPOT, POLAND	0078-3234	2300-7370		OCEANOLOGIA	Oceanologia	JAN-MAR	2022	64	1					63	74		10.1016/j.oceano.2021.09.002	http://dx.doi.org/10.1016/j.oceano.2021.09.002		FEB 2022	12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	ZD7NE		gold			2025-03-11	WOS:000758382500005
J	Potvin, M; Rautio, M; Lovejoy, C				Potvin, Marianne; Rautio, Milla; Lovejoy, Connie			Freshwater Microbial Eukaryotic Core Communities, Open-Water and Under-Ice Specialists in Southern Victoria Island Lakes (Ekaluktutiak, NU, Canada)	FRONTIERS IN MICROBIOLOGY			English	Article						Arctic; chrysophytes; cryptophytes; season; ciliates	RIBOSOMAL-RNA; PERIDINIUM-ACICULIFERUM; CRYPTOCARYON-IRRITANS; PHYLOGENETIC ANALYSIS; RESTING CYSTS; ECOSYSTEMS; GEN.; STRATEGY; SHALLOW; IMPACT	Across much of the Arctic, lakes and ponds dominate the landscape. Starting in late September, the lakes are covered in ice, with ice persisting well into June or early July. In summer, the lakes are highly productive, supporting waterfowl and fish populations. However, little is known about the diversity and ecology of microscopic life in the lakes that influence biogeochemical cycles and contribute to ecosystem services. Even less is known about the prevalence of species that are characteristic of the seasons or whether some species persist year-round under both ice cover and summer open-water conditions. To begin to address these knowledge gaps, we sampled 10 morphometrically diverse lakes in the region of Ekaluktutiak (Cambridge Bay), on southern Victoria Island (NU, Canada). We focused on Greiner Lake, the lakes connected to it, isolated ponds, and two nearby larger lakes outside the Greiner watershed. The largest lakes sampled were Tahiryuaq (Ferguson Lake) and the nearby Spawning Lake, which support commercial sea-run Arctic char (Salvelinus alpinus) fisheries. Samples for nucleic acids were collected from the lakes along with limnological metadata. Microbial eukaryotes were identified with high-throughput amplicon sequencing targeting the V4 region of the 18S rRNA gene. Ciliates, dinoflagellates, chrysophytes, and cryptophytes dominated the lake assemblages. A Bray-Curtis dissimilarity matrix separated communities into under-ice and open-water clusters, with additional separation by superficial lake area. In all, 133 operational taxonomic units (OTUs) occurred either in all under-ice or all open-water samples and were considered "core" microbial species or ecotypes. These were further characterized as seasonal indicators. Ten of the OTUs were characteristic of all lakes and all seasons sampled. Eight of these were cryptophytes, suggesting diverse functional capacity within the lineage. The core open-water indicators were mostly chrysophytes, with a few ciliates and uncharacterized Cercozoa, suggesting that summer communities are mixotrophic with contributions by heterotrophic taxa. The core under-ice indicators included a dozen ciliates along with chrysophytes, cryptomonads, and dinoflagellates, indicating a more heterotrophic community augmented by mixotrophic taxa in winter.	[Potvin, Marianne; Lovejoy, Connie] Univ Laval, Quebec Ocean, Quebec City, PQ, Canada; [Potvin, Marianne; Lovejoy, Connie] Univ Laval, Inst Integrat & Syst IBIS, Quebec City, PQ, Canada; [Rautio, Milla] Univ Quebec Chicoutimi, Dept Sci Fondament, Saguenay, PQ, Canada; [Rautio, Milla] Grp Rech Interuniv Limnol GRIL, Montreal, PQ, Canada; [Rautio, Milla] Ctr Etudes Nord CEN, Quebec City, PQ, Canada	Laval University; Laval University; University of Quebec; University of Quebec Chicoutimi	Lovejoy, C (通讯作者)，Univ Laval, Quebec Ocean, Quebec City, PQ, Canada.; Lovejoy, C (通讯作者)，Univ Laval, Inst Integrat & Syst IBIS, Quebec City, PQ, Canada.	connie.lovejoy@bio.ulaval.ca	Lovejoy, Connie/A-3756-2008		Polar Knowledge Canada; Natural Sciences and Engineering Research Council of Canada (NSERC); ArcticNet, a Canadian Center of Research and Excellence; Fonds de recherche du Quebec-Nature et Technologies (FRQNT)	Polar Knowledge Canada; Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); ArcticNet, a Canadian Center of Research and Excellence; Fonds de recherche du Quebec-Nature et Technologies (FRQNT)	The study was funded by Polar Knowledge Canada, the Natural Sciences and Engineering Research Council of Canada (NSERC) Discovery, Northern Supplement and Strategic Projects grants to CL and MR, and ArcticNet, a Canadian Center of Research and Excellence. Additional support was by way of the Fonds de recherche du Quebec-Nature et Technologies (FRQNT) to Quebec Ocean and Center Etudes Nordiques. The analyses were conducted using Compute Canada facilities.	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Microbiol.	FEB 11	2022	12								786094	10.3389/fmicb.2021.786094	http://dx.doi.org/10.3389/fmicb.2021.786094			17	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	ZI2PO	35222298	Green Published, gold			2025-03-11	WOS:000761468900001
J	Remize, M; Planchon, F; Loh, A; Le Grand, F; Bideau, A; Puccinelli, E; Volety, A; Soudant, P				Remize, Marine; Planchon, Frederic; Loh, Ai Ning; Le Grand, Fabienne; Bideau, Antoine; Puccinelli, Eleonora; Volety, Aswani; Soudant, Philippe			Origin and fate of long-chain polyunsaturated fatty acids in the Kerguelen Islands region (Southern Ocean) in late summer	JOURNAL OF MARINE SYSTEMS			English	Article						Essential fatty acids; Vertical distribution; Fatty acid export; Phytoplankton diversity; Diatoms; Heterotrophic interactions; Nutritional quality	NATURAL IRON-FERTILIZATION; DIATOM RESTING SPORES; EUPHAUSIA-SUPERBA DANA; SEA-ICE DIATOM; COMMUNITY STRUCTURE; FOOD-WEB; PHAEOCYSTIS-POUCHETII; PHYTOPLANKTON BLOOM; LIPID-COMPOSITION; CARBON EXPORT	Long-chain polyunsaturated fatty acids (LC-PUFA) are molecules produced at the basis of marine food webs and essential for ecosystem functioning. This study reports detailed fatty acid (FA) composition including the two LCPUFA 20:5n-3 and 22:6n-3, in suspended organic matter (SPOM) from the upper 300 m collected in the Kerguelen Island region in the Southern Ocean during the post-bloom period (February-March 2018; project MOBYDICK). FA profiles were largely dominated by PUFA (53-69% of Total Fatty Acid, TFA) regardless of stations and among PUFA, proportions of LC-PUFA were especially high, making up 27-44% of TFA both in the ML and upper mesopelagic. 20:5n-3 and 22:6n-3 co-occurred in the ML as a result of the post-bloom phytoplankton community showing a mixed composition dominated by small size phytoplankton (prymnesiophytes and prasinophytes) supplying 22:6n-3, and with diatoms in lower proportions supplying 20:5n-3. Elevated levels of LC-PUFA were observed both inside the iron-fertilized area on the Kerguelen Plateau and downstream, and outside in High Nutrient Low Chlorophyll waters located upstream of the Plateau, and appeared unrelated to site. In the upper mesopelagic, both LC-PUFA were maintained at high relative proportions suggesting an efficient and possibly fast vertical transfer from the surface. Transfer with depth seems to proceed via distinct pathways according to LC-PUFA. 20:5n-3 may be exported along with diatoms, presumably in the form of large intact cells, aggregates as well as resting spores. For 22:6n-3, transfer may involve a channeling through the heterotrophic food web resulting in its association with fecal material at depth. Channeling of 22:6n-3 could involve heterotrophic protists such as dinoflagellates and ciliates grazing on small phytoplankton, as well as larger zooplankton such as copepods and salps, possibly feeding on microzooplankton and producing fecal pellets rich in 22:6n-3. According to LC-PUFA content, SPOM present throughout the upper water column (0-300 m) appeared of high nutritional quality both on-and off-plateau, and represented a valuable source of food for secondary consumers and suspension feeders.	[Remize, Marine; Planchon, Frederic; Le Grand, Fabienne; Bideau, Antoine; Puccinelli, Eleonora; Soudant, Philippe] Univ Brest, CNRS, IRD, Ifremer,UMR 6539 LEMAR, F-29280 Plouzane, France; [Remize, Marine; Loh, Ai Ning] Univ North Carolina Wilmington, Dept Earth & Ocean Sci, Ctr Marine Sci, 5600 Marvin K Moss Ln, Wilmington, NC 28403 USA; [Volety, Aswani] Elon Univ, 50 Campus Dr, Elon, NC 27244 USA	Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); CNRS - Institute of Ecology & Environment (INEE); Universite de Bretagne Occidentale; University of North Carolina; University of North Carolina Wilmington; Elon University	Planchon, F; Soudant, P (通讯作者)，Univ Brest, CNRS, IRD, Ifremer,UMR 6539 LEMAR, F-29280 Plouzane, France.	frederic.planchon@univ-brest.fr; philippe.soudant@univ-brest.fr	Puccinelli, Eleonora/M-3562-2018	Puccinelli, Eleonora/0000-0002-6144-6650	French oceanographic fleet ("Flotte oceanographique francaise"); French ANR ("Agence Nationale de la Recherche", AAPG 2017 program, MOBYDICK) [ANR-17-CE01-0013]; French Research program of INSU-CNRS LEFE/CYBER ("Les enveloppes fluides et l'environnement" - "Cycles biogeochimiques, environnement et ressources"); University of Brest (UBO, France); Center of Marine Sciences (CMS) of the University of North Carolina Wilmington (UNCW, USA); "Laboratoire d'Excellence" LabexMer [ANR-10-LABX-19]; Walter-Zellidja grant of the Academie Francaise; ISblue project, Interdisciplinary graduate school for the blue planet [ANR-17-EURE-0015]; French government under the program "Investissements d'Avenir"	French oceanographic fleet ("Flotte oceanographique francaise"); French ANR ("Agence Nationale de la Recherche", AAPG 2017 program, MOBYDICK)(Agence Nationale de la Recherche (ANR)Agence nationale pour le developpement de la recherche en sante (ANDRS)Agence Nationale Des Plantes Medicinales Et Aromatiques, ANPMA, Morocco); French Research program of INSU-CNRS LEFE/CYBER ("Les enveloppes fluides et l'environnement" - "Cycles biogeochimiques, environnement et ressources"); University of Brest (UBO, France); Center of Marine Sciences (CMS) of the University of North Carolina Wilmington (UNCW, USA); "Laboratoire d'Excellence" LabexMer; Walter-Zellidja grant of the Academie Francaise; ISblue project, Interdisciplinary graduate school for the blue planet; French government under the program "Investissements d'Avenir"(Agence Nationale de la Recherche (ANR))	We thank B. Queguiner, the PI of the MOBYDICK project, for providing us the opportunity to participate to this cruise, the chief scientist I. Obernosterer and the captain and crew of the R/V Marion Dufresne for their enthusiasm and support aboard during the MOBYDICK-THEMISTO cruise (doi:10.17600/18000403). This work was supported by the French oceanographic fleet ("Flotte oceanographique francaise"), the French ANR ("Agence Nationale de la Recherche", AAPG 2017 program, MOBYDICK Project number: ANR-17-CE01-0013), the French Research program of INSU-CNRS LEFE/CYBER ("Les enveloppes fluides et l'environnement" - "Cycles biog ' eochimiques, environnement et ressources"). Marine Remize PhD fellowship and studies was supported by the University of Brest (UBO, France), the Center of Marine Sciences (CMS) of the University of North Carolina Wilmington (UNCW, USA), the "Laboratoire d'Excellence" LabexMer (ANR-10-LABX-19), and the Walter-Zellidja grant of the Academie Francaise. E. Puccinelli was supported by ISblue project, Interdisciplinary graduate school for the blue planet (ANR-17-EURE-0015) and co-funded by a grant from the French government under the program "Investissements d'Avenir". We would like to thank our colleagues of the Technical Division of the INSU, Emmanuel de Saint-Leger, Lionel Scouarnec, Lionel Fischen, and Olivier Desprez De Gesincourt for their logistical and technical help with the insitu pumps, the colleagues of the UBO Open Factory for their help in designing and preparing the NITEX membranes, and also to Stephane Blain and Bernard Queguiner for their helpful comments and suggestions on the manuscript.	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Wilson SE, 2010, DEEP-SEA RES PT I, V57, P1278, DOI 10.1016/j.dsr.2010.07.005	112	2	2	1	13	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0924-7963	1879-1573		J MARINE SYST	J. Mar. Syst.	APR	2022	228								103693	10.1016/j.jmarsys.2021.103693	http://dx.doi.org/10.1016/j.jmarsys.2021.103693		FEB 2022	17	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	ZO7RU		Bronze, Green Published, Green Submitted			2025-03-11	WOS:000765925400001
J	Bijl, PK				Bijl, Peter K.			DINOSTRAT: a global database of the stratigraphic and paleolatitudinal distribution of Mesozoic-Cenozoic organic-walled dinoflagellate cysts	EARTH SYSTEM SCIENCE DATA			English	Article							MIDDLE MIOCENE; MAGNETOSTRATIGRAPHIC CALIBRATION; ACRITARCH BIOSTRATIGRAPHY; PALEOENVIRONMENTAL CHANGE; CALCAREOUS NANNOFOSSILS; MARINE PALYNOMORPHS; RESEARCH BOREHOLE; EOCENE SEDIMENTS; NORTH YORKSHIRE; EARLY OLIGOCENE	Mesozoic-Cenozoic organic-walled dinoflagellate cyst (dinocyst) biostratigraphy is a crucial tool for relative and numerical age control in complex ancient sedimentary systems. However, stratigraphic ranges of dinocysts are found to be strongly diachronous geographically. A global compilation of state-of-the-art calibrated regional stratigraphic ranges could assist in quantifying regional differences and evaluating underlying causes. For this reason, DINOSTRAT is here introduced - an open-source, iterative, community-fed database intended to house all regional chronostratigraphic calibrations of dinocyst events (https://github.com/bijlpeter83/DINOSTRAT.git, last access: 1 February 2022) (DOI - https://doi.org/10.5281/zenodo.5772616, Bijl, 2021). DINOSTRAT version 1.0 includes >8500 entries of the first and last occurrences (collectively called "events") of >1900 dinocyst taxa and their absolute ties to the chronostratigraphic timescale of Gradstein et al. (2012). Entries are derived from 199 publications and 188 sedimentary sections. DINOSTRAT interpolates paleolatitudes of regional dinocyst events, allowing evaluation of the paleolatitudinal variability in dinocyst event ages. DINOSTRAT allows for open accessibility and searchability, based on region, age and taxon. This paper presents a selection of the data in DINOSTRAT: (1) the (paleo)latitudinal spread and evolutionary history of modern dinocyst species, (2) the evolutionary patterns and paleolatitudinal spread of dinocyst (sub)families, and (3) a selection of key dinocyst events which are particularly synchronous. Although several dinocysts show - at the resolution of their calibration - quasi-synchronous event ages, in fact many species have remarkable diachroneity. DINOSTRAT provides the data storage approach by which the community can now start to relate diachroneity to (1) inadequate ties to chronostratigraphic timescales, (2) complications in taxonomic concepts, and (3) ocean connectivity and/or the affinities of taxa to environmental conditions.	[Bijl, Peter K.] Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands	Utrecht University	Bijl, PK (通讯作者)，Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands.	p.k.bijl@uu.nl		Bijl, Peter/0000-0002-1710-4012	LPP Foundation	LPP Foundation	The LPP Foundation has financially supported the development of DINOSTRAT.	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Data	FEB 9	2022	14	2					579	617		10.5194/essd-14-579-2022	http://dx.doi.org/10.5194/essd-14-579-2022			39	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	ZD4MV		gold, Green Submitted			2025-03-11	WOS:000758174500001
J	Hoorn, C; Kukla, T; Bogotá-Angel, G; van Soelen, E; González-Arango, C; Wesselingh, FP; Vonhof, H; Val, P; Morcote-Rios, G; Roddaz, M; Dantas, EL; Santos, RV; Damsté, JSS; Kim, JH; Morley, RJ				Hoorn, Carina; Kukla, Tyler; Bogota-Angel, Giovanni; van Soelen, Els; Gonzalez-Arango, Catalina; Wesselingh, Frank P.; Vonhof, Hubert; Val, Pedro; Morcote-Rios, Gaspar; Roddaz, Martin; Dantas, Elton Luiz; Santos, Roberto Ventura; Damste, Jaap S. Sinninghe; Kim, Jung-Hyun; Morley, Robert J.			Cyclic sediment deposition by orbital forcing in the Miocene wetland of western Amazonia? New insights from a multidisciplinary approach	GLOBAL AND PLANETARY CHANGE			English	Article						Amazon, palynology; Sequence stratigraphy, geochemistry; Biomarkers; Estuarine; Marine incursions	TRACE-ELEMENT GEOCHEMISTRY; SEA FAN EVIDENCE; MARINE INCURSIONS; ORGANIC-MATTER; FORELAND BASIN; SOLIMOES BASIN; NORTHWESTERN AMAZONIA; CONTINENTAL-MARGIN; TETRAETHER LIPIDS; MIDDLE MIOCENE	In the Miocene, a large wetland system extended from the Andean foothills into western Amazonia. This system has no modern analogue and the driving mechanisms are not yet fully understood. Dynamic topography and Andean uplift are thought to have controlled deposition, with allocyclic base level changes driven by eustasy and orbital forcing also playing a role. In this study we investigate the presumed orbital cyclicity that controlled sediment deposition, while also assessing sediment source and biomes in the Miocene wetland. We do this by integrating lithological, palynological, malacological and geochemical data from the Los Chorros site (Amazon River, Colombia), and by placing our data in a sequence stratigraphic framework. In this sequence biostratigraphic evaluation, the Los Chorros succession is visualized to be composed of a series of flood-fill packages, with a rapid initial flood, marine-influenced conditions at the time of maximum flood, followed by a longer regressive infill phase. Based on the palynology we could differentiate local vegetation, such as palm swamps, from regional origin such as terra firme vegetation (non-flooded Amazonian forest) and Andean montane forest, while from sediment geochemistry we could separate local and regional sediment sources. At the times of flooding, oligotrophic and eutrophic aquatic conditions alternatively characterized the wetland, as is shown by the presence of algae, floating ferns, and mollusc assemblages, while intervening subaquatic debris points to proximal submerged lowlands. In the lower 20 m of the section, marine influences are intermittently evident and shown by short-lived maxima of mangrove pollen, foraminiferal test linings, dinoflagellate cysts, coastal mollusc species, and an episodic decline in terrestrial biomarkers. The upper 5 m of the section is characterized by floodplain forest taxa with a diversity in tropical rain forest taxa and relatively few lacustrine indicators. These marine, mangrove, and lacustrine indicators suggest that the outcrops at Los Chorros represent predominant marine-influenced lacustrine conditions during periods of sea level highstand. The sequence biostratigraphic evaluation further points to eight 41 kyr obliquity-driven depositional cycles, with rapid phases of transgression. Mangrove elements would have colonised within the timeframe of each sea level rise. Based on this relative age constraint and comparison to regional records, deposition likely took place prior to the 13.8 Myr global sea level fall, and most likely during the period just after 14.5 Ma, between Middle Miocene Climatic Optimum (MMCO; 17-14 Ma) and Middle Miocene Climate Transition (MMCT; 14.7-13.8 Ma). Palynological evidence further suggests that to the west, surface elevation ranged from similar to 1000 up to similar to 3500 m and hosted protoparamo vegetation, the oldest yet reported and in agreement with predictions from molecular studies. In contrast, contemporaneous sites to the northeast of the wetland consisted of fluvial and cratonic formations, as shown by their Nd and Sr isotopic sediment signature. In summary, our data lead to an improved understanding of how geological and astronomical mechanisms controlled the floral and faunal distribution and controlled sediment deposition in western Amazonia during the middle Miocene. As Miocene conditions strongly contrast with modern western Amazonia, our data provide an important context for the deep time history and evolution of the modern western Amazon rainforest.	[Hoorn, Carina] Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, NL-1098 XH Amsterdam, Netherlands; [Kukla, Tyler] Stanford Univ, Dept Geol Sci, Stanford, CA 94305 USA; [Bogota-Angel, Giovanni] Univ Dist Francisco Jose de Caldas, Fac Medio Ambiente & Recursos Nat, Bogota, Colombia; [van Soelen, Els; Damste, Jaap S. Sinninghe] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Microbiol & Biogeochem, POB 59, NL-1790 AB Den Burg, Texel, Netherlands; [Gonzalez-Arango, Catalina] Univ Los Andes, Dept Ciencias Biol, Bogota, Colombia; [Wesselingh, Frank P.] Nat Biodivers Ctr, POB 9517, NL-2300 RA Leiden, Netherlands; [Wesselingh, Frank P.; Damste, Jaap S. Sinninghe] Univ Utrecht, Fac Geosci, Dept Earth Sci, POB 80-121, NL-3508 TA Utrecht, Netherlands; [Vonhof, Hubert] Max Planck Inst Chem, Climate Geochem Dept, Hahn Meitner Weg 1, D-55128 Mainz, Germany; [Val, Pedro] Univ Fed Ouro Preto, Dept Geol, Escola Minas, Degeo 58, Ouro Preto, Brazil; [Morcote-Rios, Gaspar] Univ Nacl Colombia, Inst Ciencias Nat, Bogota, Colombia; [Roddaz, Martin] Univ Toulouse, Geosci Environm Toulouse, UPS SVT OMP CNRS IRD, 14 Ave Edouard Belin, F-31400 Toulouse, France; [Dantas, Elton Luiz; Santos, Roberto Ventura] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Kim, Jung-Hyun] Korea Polar Res Inst, 26 Songdomirae Ro, Incheon 21990, South Korea; [Morley, Robert J.] Palynova Ltd, Littleport, England; [Morley, Robert J.] Royal Holloway Univ London, Earth Sci Dept, Egham TW20 0EX, Surrey, England	University of Amsterdam; Stanford University; Universidad Distrital Francisco Jose de Caldas; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Universidad de los Andes (Colombia); Naturalis Biodiversity Center; Utrecht University; Max Planck Society; Universidade Federal de Ouro Preto; Universidad Nacional de Colombia; Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Universidade de Brasilia; Korea Polar Research Institute (KOPRI); University of London; Royal Holloway University London	Hoorn, C (通讯作者)，Univ Amsterdam, Inst Biodivers & Ecosyst Dynam, NL-1098 XH Amsterdam, Netherlands.; Morley, RJ (通讯作者)，Palynova Ltd, Littleport, England.; Morley, RJ (通讯作者)，Royal Holloway Univ London, Earth Sci Dept, Egham TW20 0EX, Surrey, England.	m.c.hoorn@uva.nl; bobmorley100@gmail.com	Wesselingh, Frank/C-1367-2018; Dantas, Elton/AAK-8464-2021; Kukla, Tyler/AAQ-6967-2021; Damste, Jaap/F-6128-2011; Arango, Catalina/D-2308-2011; Santos, Roberto/B-8163-2015; Roddaz, Martin/AFR-7875-2022; Val, Pedro/F-3702-2019; Hoorn, Carina/A-9372-2015	Gonzalez Arango, Catalina/0000-0003-1709-4405; Hoorn, Carina/0000-0001-5402-6191; Val, Pedro/0000-0001-5370-4122; Roddaz, Martin/0000-0001-8562-8582	joint Brazilian-European facility for climate and geodynamic research on the Amazon River Basin sediment (CLIM-AMAZON) project; European Research Council under the European Union's Seventh Framework Program (FP7/2007-2013)/ERC grant [226600]; Programa de Investigaciones, Facultad de Ciencias	joint Brazilian-European facility for climate and geodynamic research on the Amazon River Basin sediment (CLIM-AMAZON) project; European Research Council under the European Union's Seventh Framework Program (FP7/2007-2013)/ERC grant(European Research Council (ERC)); Programa de Investigaciones, Facultad de Ciencias	This research was partly funded by the joint Brazilian-European facility for climate and geodynamic research on the Amazon River Basin sediment (CLIM-AMAZON) project. The research leading to these results has also received funding from the European Research Council under the European Union's Seventh Framework Program (FP7/2007-2013) /ERC grant agreement n? [226600] . Samples were collected in the framework of the Tropenbos International Program. We thank Jeane Grasyelle, Iris Dias, Rachel Bezerra and other analysts and students working at the Geochro-nology Laboratory of the University of Brasilia for help with the Sr and Nd analyses. We also like to thank Denise Dorhout, Marianne Baas, Monique Veenstra, Angelique Mets, Jort Ossebaar, and Kevin Donkers for analytical assistance at the NIOZ. C.G.-A. acknowledges the support from the Programa de Investigaciones, Facultad de Ciencias (2021) . We thank Anne-marie Philip for processing the palynological samples at the University of Amsterdam.	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Planet. Change	MAR	2022	210								103717	10.1016/j.gloplacha.2021.103717	http://dx.doi.org/10.1016/j.gloplacha.2021.103717		FEB 2022	26	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	ZX7JW		Green Published, hybrid			2025-03-11	WOS:000772071200005
J	de Freitas, AD; Santos, ADD; Félix, LD; dos Santos, RF; Bila, DM; Aguiar, VMD; da Fonseca, EM; Neto, JAB				de Freitas, Alex da Silva; de Oliveira Santos, Ana Dalva; Felix, Louise da Cruz; dos Santos, Rejany Ferreira; Bila, Daniele Maia; de Carvalho Aguiar, Valquiria Maria; da Fonseca, Estefan Monteiro; Baptista Neto, Jose Antonio			Multiproxy analysis in contaminated sediments from Niteroi Harbour (Guanabara Bay), Brazil	MARINE POLLUTION BULLETIN			English	Article						Artemia; Dinoflagellate cysts; Guanabara Bay; Pollution; Trace metals; Vibrio fischeri	RIO-DE-JANEIRO; HEAVY-METALS; NEARSHORE ENVIRONMENT; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; JURUJUBA SOUND; RIVER ESTUARY; BIOAVAILABILITY	Harbours are located in major urban centres around the world and are of great economic importance to the cities in their surroundings. However, the intense traffic of boats and ships can generate environmental impacts that can directly affect the local biota as well as the population that lives in surrounding areas. Therefore, this work aimed to analyse the surface sediment of the Niteroi Harbour using chemical, biological and micro-palaeontological tools to investigate the environmental condition of this important harbour in Rio de Janeiro State. The pseudototal trace metal data analysed in the surface samples showed values far above those of the greater Guanabara Bay background. These data were corroborated by a high mortality rate of Artemia sp. and elevated presence of the bacterium Vibrio fischeri, indicating a high rate of local pollution. Dinoflagellate cysts also showed a direct response to high values of pseudototal trace metals. The data obtained in this study emphasize a need for greater monitoring of ports since the experience gained through this study in a Brazilian harbour can serve as an example for the management of other harbours located in large urban centres around the world.	[de Freitas, Alex da Silva; de Oliveira Santos, Ana Dalva; de Carvalho Aguiar, Valquiria Maria; da Fonseca, Estefan Monteiro; Baptista Neto, Jose Antonio] Univ Fed Fluminense, Inst Geociencias, Dept Geol, Rio De Janeiro, RJ, Brazil; [Felix, Louise da Cruz; Bila, Daniele Maia] Univ Estado Rio de Janeiro, Fac Engn, Dept Engn Sanit & Meio Ambiente, Rio De Janeiro, RJ, Brazil; [dos Santos, Rejany Ferreira] Fundacao Oswaldo Cruz, Cooperacao Social, Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense; Universidade do Estado do Rio de Janeiro; Fundacao Oswaldo Cruz	de Freitas, AD (通讯作者)，Univ Fed Fluminense, Inst Geociencias, Dept Geol, Rio De Janeiro, RJ, Brazil.	alexsilfre@gmail.com	Aguiar, Valquiria/HZJ-5714-2023; Bila, Daniele/B-8135-2016; de Freitas, Alex/IUQ-2116-2023; Neto, José/AAL-2773-2021; Felix, Louise da Cruz/JFS-0398-2023	Felix, Louise da Cruz/0000-0002-3497-8598; da Silva de Freitas, Alex/0000-0002-8665-7649	Fundacao de Amparo `a Pesquisa do Estado do Rio de Janeiro (FAPERJ); Conselho Nacional de Desenvolvimento Cientifico e Tecnol 'ogico (CNPq); CAPES (Coordenac ~ao de Aperfeicoamento de Pessoal de Nivel Superior)	Fundacao de Amparo `a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnol 'ogico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES (Coordenac ~ao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was sponsored by the Fundacao de Amparo `a Pesquisa do Estado do Rio de Janeiro (FAPERJ), the Conselho Nacional de Desenvolvimento Cientifico e Tecnol ' ogico (CNPq) and CAPES (Coordenac ~ao de Aperfeicoamento de Pessoal de Nivel Superior).	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Pollut. Bull.	FEB	2022	175								113348	10.1016/j.marpolbul.2022.113348	http://dx.doi.org/10.1016/j.marpolbul.2022.113348		FEB 2022	8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	2P7SM	35124378				2025-03-11	WOS:000819935800003
J	Rigel, CQ; Javier, H; Ernesto, GM; Rafael, RM				Quezada Rigel, Castaneda; Javier, Helenes; Mendoza Ernesto, Garcia; Mendoza Rafael, Ramirez			Assemblages of dinoflagellate resistance cysts and copepod eggs in superficial sediments at the upper Gulf of California	CONTINENTAL SHELF RESEARCH			English	Article						Autotrophic dinoflagellate cysts; Heterotrophic dinoflagellate cysts; Copepods eggs; Concentrations	RECENT MARINE-SEDIMENTS; RED-TIDE; GYMNODINIUM-CATENATUM; SURFACE SEDIMENTS; PROTOCERATIUM-RETICULATUM; PRIMARY PRODUCTIVITY; EPIPELAGIC COPEPODS; BAJA-CALIFORNIA; LIFE-CYCLE; SALINITY	The diversity, abundance, and geographic distribution of dinoflagellate cysts in recent sediments serve as bioindicators to specific regions' environmental conditions and productivity. We present dinoflagellate cysts assemblages from 53 superficial sediment samples from the upper Gulf of California (uGC) obtained in July 2016 and February 2017. Forty-seven species were identified, of which twenty-seven are considered heterotrophic (Het) and twenty autotrophic (Aut). Ten species of this last group are potentially toxin producers (PTxS). The total concentration (Tot) of cysts in all the samples was 3481 cysts/g in 2016 and 4223 cysts/g in 2017. Aut represented 59%, Het 41%, while the PTxS represented ~36.5% of the Tot cysts. The higher abundance of the Aut is likely to manifest the local high sea surface temperature and salinity. The increase in the Tot of cysts in the 2017 set was related to a Gymnodinium catenatum harmful algal bloom. Copepod eggs abundance was 7137 eggs/ g in 2016 and 6555 eggs/g in 2017. The Aut Gymnodinium spp., Spiniferites spp., Operculodinium spp, and the Het Protoperidinium americanum, Quinquecuspis concreta, Selenopemphix nephroides, Brigantedinium spp., and Echinidinium spp., were typical in both seasons but differed on their concentrations between each season. The cysts distribution between both sampling periods reflects local currents and the sediment dynamics of the uGC, and the high species diversity in this area reflects the elevated primary productivity in this area.	[Quezada Rigel, Castaneda] Ctr Invest Cient & Educ Super Ensenada, Posgrad Ecol Marina, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Javier, Helenes] Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Ciencias Tierra, Carr Ensenada Tijuana 39918, Ensenada 22860, Baja California, Mexico; [Mendoza Ernesto, Garcia] Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Biol, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Mendoza Rafael, Ramirez] Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Fis, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Javier, H (通讯作者)，Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Ciencias Tierra, Carr Ensenada Tijuana 39918, Ensenada 22860, Baja California, Mexico.	jhelenes@cicese.mx		Garcia-Mendoza, Ernesto/0000-0003-1738-7419	CONACYT scholarship [24805 - CV617226]; FORDECYT - CONACYT [260040-2015]	CONACYT scholarship(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); FORDECYT - CONACYT	This work was funded by CONACYT scholarship 24805 - CV617226; FORDECYT - CONACYT project number 260040-2015.	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Van Nieuwenhove N, 2020, MAR MICROPALEONTOL, V159, DOI 10.1016/j.marmicro.2019.101814; Vásquez-Bedoya LF, 2008, MAR MICROPALEONTOL, V68, P49, DOI 10.1016/j.marmicro.2008.03.002; Verleye TJ, 2011, MAR MICROPALEONTOL, V78, P65, DOI 10.1016/j.marmicro.2010.10.001; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; ZEITZSCHEL B, 1969, MAR BIOL, V3, P201, DOI 10.1007/BF00360952; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6; 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	108	3	4	0	10	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0278-4343	1873-6955		CONT SHELF RES	Cont. Shelf Res.	FEB 15	2022	235								104648	10.1016/j.csr.2022.104648	http://dx.doi.org/10.1016/j.csr.2022.104648		FEB 2022	15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	1A7QY					2025-03-11	WOS:000791947700001
J	Sobrino, CM; Cartelle, V; Martínez-Carreño, N; Ramil-Rego, P; García-Gil, S				Sobrino, C. Munoz; Cartelle, V.; Martinez-Carreno, N.; Ramil-Rego, P.; Garcia-Gil, S.			New multiproxy data obtained from the sedimentary fill of the Ria de Ferrol, NW Iberia	DATA IN BRIEF			English	Article; Data Paper						Radiocarbon dates; Sedimentary facies; Geochemical data; Pollen content; Dinoflagellate cysts content; Non-pollen palynomorphs content		Several gravity cores and vibro-cores were recovered from selected sites in the inner sector of Ria de Ferrol, NW Iberia (Munoz Sobrino et al., 2021) [1] . These sediment cores were obtained during the surveys ECOMER-2014 and ECOMER-2015, developed from 2014 to 2015 on-board the R/V Mytilus (Consejo Superior de Investigacion Cientifica) and the Amar-radores Mil (Amarradores del Puerto y Ria de Ferrol, S.L.), re-spectively. Sedimentary and other multiproxy data presented here belong to four selected sediment cores located in the in-nermost part of the study area. Two were recovered using a gravity corer and another two using a vibro-corer. The depth of the cores and samples obtained is referred to the NMMA (the mean sea level in Alicante), which is the Spanish ortho-metric datum. One half of each core was subjected to non-destructive analysis using an ITRAX core scanner providing X-ray fluorescence (XRF) elemental data. Particle size distribution was characterised by laser diffraction. For radiocarbon dating, well-preserved articulated valves, small remains of wood and very organic bulk sediment from one location free of biogenic gas were selected. Palynological analyses were performed on selected sections of the sediment. All samples were spiked with Lycopodium spores for absolute palynomorph estimation and analysed using 400x and 600x magnifications. The ratio of dinoflagellate cyst concentrations to pollen, fern spore and dinoflagellate cyst concentrations (D/P ratio, ranging between 0 and 1) was calculated for each sample to show the temporal variation. Combined seismic, litho logical, elemental, chronological and palynological data enable reconstructing the environmental changes that occurred during the local marine transgression. Besides, the combination of evidence identified may also be applied to other areas or periods in order to perform local reconstructions of changing coastal ecosystems. This type of high-resolution spatial temporal reconstructions of past changes in estuarine environments may be a valuable tool for modelling, predicting and managing the changes and threats linked to the global warming and sea-level rise associated. (C) 2021 The Authors. Published by Elsevier Inc.	[Sobrino, C. Munoz; Cartelle, V.; Martinez-Carreno, N.; Garcia-Gil, S.] Univ Vigo, Ctr Invest Marina, Edificio Filomena Dato,Campus Marcosende S-N, Vigo 36310, Spain; [Sobrino, C. Munoz] Univ Vigo, Fac Ciencias, Dept Biol Vexetal Ciencias Solo, Campus Marcosende S-N, Vigo 36310, Spain; [Cartelle, V.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Cartelle, V.; Martinez-Carreno, N.; Garcia-Gil, S.] Univ Vigo, Fac Ciencias, Dept Xeociencias Marinas, Campus Marcosende S-N, Vigo 36310, Spain; [Ramil-Rego, P.] Univ Santiago de Compostela, Lab Bot & Bioxeog, IBADER, Gl 1934 TB,Campus Univ S-N, Lugo 27002, Spain	Universidade de Vigo; CIM UVIGO; Universidade de Vigo; University of Leeds; Universidade de Vigo; Universidade de Santiago de Compostela	Sobrino, CM (通讯作者)，Univ Vigo, Ctr Invest Marina, Edificio Filomena Dato,Campus Marcosende S-N, Vigo 36310, Spain.; Sobrino, CM (通讯作者)，Univ Vigo, Fac Ciencias, Dept Biol Vexetal Ciencias Solo, Campus Marcosende S-N, Vigo 36310, Spain.	bvcastor@uvigo.es	Martínez-Carreño, Natalia/AAA-5634-2019; Sobrino, Castor/N-6281-2019; Cartelle Álvarez, Víctor/AFR-6659-2022; Munoz Sobrino, Castor/H-2948-2015	Martinez-Carreno, Natalia/0000-0002-0305-0543; Munoz Sobrino, Castor/0000-0001-8191-3001; Cartelle, Victor/0000-0002-8894-7172	Spanish Ministry of Education and Science [CGL2012-33584]; (ERDF funds); Xunta de Galicia [GRC 2015/020, ED431C 2019/28]; FPI-MINECO research programme [BES-2013-06 6901]	Spanish Ministry of Education and Science(Spanish Government); (ERDF funds); Xunta de Galicia(Xunta de Galicia); FPI-MINECO research programme	This work was funded by the Spanish Ministry of Education and Science CGL2012-33584 (cofinanced with ERDF funds) and the Xunta de Galicia GRC 2015/020 and ED431C 2019/28 projects. Victor Cartelle acknowledges the predoctoral funding provided by the FPI-MINECO research programme (BES-2013-06 6901).	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J	Nishikawa, T; Harada, K; Watanabe, T				Nishikawa, Tetsuya; Harada, Kazuhiro; Watanabe, Tsuyoshi			Seasonal and annual dynamics of phytoplankton off Tajima, southwestern Sea of Japan	PLANKTON & BENTHOS RESEARCH			English	Article						diatom; phytoplankton structure; Sea of Japan; size-fractionated chlorophyll a; Tsushima Warm Current	COCHLODINIUM-POLYKRIKOIDES DINOPHYCEAE; JELLYFISH NEMOPILEMA-NOMURAI; MARINE PLANKTONIC DIATOM; RESTING SPORE FORMATION; SETO INLAND SEA; NORTHERN JAPAN; GROWTH; COMMUNITY; COAST; BAY	In the Sea of Japan, changes in the oceanographic conditions affect fisheries, and new phenomena such as blooms of the harmful dinoflagellate Margalefidinium polykrikoides and mass occurrences of the giant jellyfish Nemopilema nomurai have been observed since the 2000s. In order to elucidate and formulate countermeasures to such new issues, it is essential to enhance the oceanographic/biological data. However, data especially on the phytoplankton assemblage are limited. In the present study, we investigated the population dynamics of the phytoplankton community together with environmental factors at two stations off Tajima, southwestern Sea of Japan for seven fiscal years from September 2009 to March 2016. The oceanographic observations revealed the general pattern in the seasonal and annual abundance of phytoplankton off Tajima. The major component of size-fractionated chlorophyll a concentrations were micro-size (filtered pore size: >10 mu m). The results indicated that there was usually a low abundance of phytoplankton in this area. Relatively high abundances (cell densities over 100 cells mL(-1)) of micro-sized phytoplankton were observed only in spring, but total cell densities were less than 10 cells mL(-1) in most months of the other three seasons. The major phytoplankton component was diatoms. Based on the abundance and frequency, the dominant seven diatom taxa were classified into three groups: Skeletonema spp., Thalassiosira spp. and Eucampia zodiacus were dominant in spring, Chaetoceros spp. and Pseudo-nitzschia spp. were dominant in spring and autumn, and Rhizosolenia spp. and Leptocylindrus danicus were dominant in autumn.	[Nishikawa, Tetsuya; Harada, Kazuhiro] Hyogo Prefectural Technol Ctr Agr Forestry & Fish, Fisheries Technol Inst, 22-2 Minami Futami, Akashi, Hyogo 6740093, Japan; [Watanabe, Tsuyoshi] Japan Fisheries Res & Educ Agcy, Tohoku Natl Fisheries Res Inst, 3-7-25 Shinhama Cho, Shiogama, Miyagi 9850001, Japan; [Watanabe, Tsuyoshi] Japan Fisheries Res & Educ Agcy, Fisheries Resource Inst, 116 Katsurakoi, Kushiro, Hokkaido 0850802, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA)	Nishikawa, T (通讯作者)，Hyogo Prefectural Technol Ctr Agr Forestry & Fish, Fisheries Technol Inst, 22-2 Minami Futami, Akashi, Hyogo 6740093, Japan.	tetsuya_nishikawa@pref.hyogo.lg.jp			Fisheries Agency of Japan	Fisheries Agency of Japan	We are grateful to the captain and crew of the R/V Tajima and members of the Tajima Fisheries Technology Institute, Hyogo Prefectural Technology Center for Agriculture, Forestry and Fisheries for their cooperation in sampling and measurement of water samples. We also thank Dr. Kazutaka Miyahara, Fisheries Technology Institute, Hyogo Prefectural Technology Center for Agriculture, Forestry and Fisheries for his support of Chl a measurement. This study was partially supported by the Fisheries Agency of Japan.		0	2	2	1	13	PLANKTON SOC JAPAN	HOKKAIDO	C/O MAR. BIODIVERSITY LAB, 3-1-1 MINATOMACHI, HAKODATE, HOKKAIDO, 041-8611, JAPAN	1880-8247	1882-627X		PLANKTON BENTHOS RES	Plankton Benthos Res.	FEB	2022	17	1					83	90		10.3800/pbr.17.83	http://dx.doi.org/10.3800/pbr.17.83			8	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	ZP2RN		gold			2025-03-11	WOS:000766272100007
J	Hegseth, EN; von Quillfeldt, C				Hegseth, Else Nost; von Quillfeldt, Cecilie			The Sub-Ice Algal Communities of the Barents Sea Pack Ice: Temporal and Spatial Distribution of Biomass and Species	JOURNAL OF MARINE SCIENCE AND ENGINEERING			English	Article						Barents Sea; ice algae; algal species; algal biomass; spatial distribution; temporal distribution; over-vintering	SOUTHEASTERN HUDSON-BAY; CENTRAL ARCTIC-OCEAN; HORIZONTAL PATCHINESS; PRIMARY PRODUCTIVITY; ECOLOGICAL PROCESSES; CALANUS-GLACIALIS; MANITOUNUK SOUND; CHLOROPHYLL-A; FRAM STRAIT; LAPTEV SEA	This work summarizes ice algal studies, presented as biomass and species temporal and spatial distribution, during 11 cruises conducted between 1986 and 2012. The majority of the biomass was found as loosely attached sub-ice algal layers, and sampling required diving. A maximum of 40 mg chlorophyll m(-2) and 15.4 x 10(9) cells m(-2) was measured in May. The species diversity was separated in zones based on ice thickness, with the highest biodiversity in the medium-thick ice of 30-80 cm. Nitzschia frigida was the most common species. There was a significant positive relationship between the dominance of this species and ice thickness, and it dominated completely in thick ice. Other common species, such as N. promare and Fossulaphycus arcticus reacted oppositely, by becoming less dominant in thick ice, but the positive correlation between total cell numbers and number of these three species indicated that they would most likely dominate in most populations. Melosira arctica was found several times below medium-thick annual ice. Algae occurred from top to bottom in the ice floes and in infiltration layers, but in very low numbers inside the ice. The bipolar dinoflagellates Polarella glacialis inhabited the ice, both as vegetative cells and cysts. The algal layers detached from the ice and sank in late spring when melting started. The cells in the sediments form an important food source for benthic animals throughout the year. Fjord populations survive the winter on the bottom and probably form next year's ice algal inoculum. A few 'over-summer' populations found in sheltered locations might provide supplementary food for ice amphipods in late summer. The future faith of the ice flora is discussed in view of a warmer climate, with increased melting of the Arctic ice cover.	[Hegseth, Else Nost] Univ Tromso, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, Tromso, Norway; [von Quillfeldt, Cecilie] Norwegian Polar Res Inst, N-9296 Tromso, Norway	UiT The Arctic University of Tromso; Norwegian Polar Institute	Hegseth, EN (通讯作者)，Univ Tromso, Fac Biosci Fisheries & Econ, Dept Arctic & Marine Biol, Tromso, Norway.	Else.Hegseth@uit.no; cecilie.von.quillfeldt@npolar.no			Norwegian Research Council [150356]; Norwegian Polar Institute; Statoil [3579]; University of Tromso	Norwegian Research Council(Research Council of Norway); Norwegian Polar Institute; Statoil; University of Tromso	This work was financed by the Norwegian Research Council (`Pro Mare' 1984-1988 and `On Thin Ice' 2003-2005, funding no. 150356), the Norwegian Polar Institute (ICEBAR 1995-1996 and MariClim 2006-2008), Statoil (Ice Edge Program 2006-2008, funding no. 3579), and the University of Tromso. This work is a result of data collection over a long period, sometimes as an added value of other ongoing projects, particularly cruise opportunities.	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Mar. Sci. Eng.	FEB	2022	10	2							164	10.3390/jmse10020164	http://dx.doi.org/10.3390/jmse10020164			29	Engineering, Marine; Engineering, Ocean; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Oceanography	ZX6XW		Green Published, gold			2025-03-11	WOS:000772039900001
J	Penaud, A; Eynaud, F; Etourneau, J; Bonnin, J; de Vernal, A; Zaragosi, S; Kim, JH; Kang, S; Gal, JK; Oliveira, D; Waelbroeck, C				Penaud, A.; Eynaud, F.; Etourneau, J.; Bonnin, J.; de Vernal, A.; Zaragosi, S.; Kim, J-H; Kang, S.; Gal, J-K; Oliveira, D.; Waelbroeck, C.			Ocean Productivity in the Gulf of Cadiz Over the Last 50 kyr	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						dinocysts; stable isotopes; alkenones; last glacial maximum; Heinrich Stadials; primary productivity; remineralization	DINOFLAGELLATE CYST DISTRIBUTION; CARBON ISOTOPIC COMPOSITION; SEA-SURFACE CONDITIONS; BENTHIC FORAMINIFERA; GLACIAL MAXIMUM; NORTHERN-HEMISPHERE; TEMPERATURE-CHANGES; EASTERN ATLANTIC; HEINRICH EVENTS; GROWTH HISTORY	Reconstructions of ocean primary productivity (PP) help to explain past and present biogeochemical cycles and climate changes in the oceans. We document PP variations over the last 50 kyr in a currently oligotrophic subtropical region, the Gulf of Cadiz. Data combine refined results from previous investigations on dinocyst assemblages, alkenones, and stable isotopes (O-18, C-13) in planktonic (Globigerina bulloides) and endobenthic (Uvigerina mediterranea) foraminifera from cores MD04-2805 CQ and MD99-2339, with new isotopic measurements on epibenthic (Cibicides pachyderma-Cibicidoides wuellerstorfi) foraminifera and dinocyst-based estimates of PP using the new n = 1,968 modern database. We constrain PP variations and export production by integrating qualitative information from bioindicators with dinocyst-based quantitative reconstructions such as PP and seasonal sea surface temperature and information about remineralization from the benthic Delta delta C-13 (difference between epibenthic and endobenthic foraminiferal delta C-13 signatures). This study also includes new information on alkenone-based SST and total organic carbon which provides insights into the relationship between past regional hydrological activity and PP regime change. We show that PP, carbon export, and remineralization were generally high in the NE subtropical Atlantic Ocean during the last glacial period and that the Last Glacial Maximum (LGM) had lower Delta delta C-13 than the Heinrich Stadials with sustained high PP, likely allowing enhanced carbon sequestration. We link these PP periods to the dynamics of upwelling, active almost year-round during sadials, but restricted to spring-summer during interstadials and LGM, like today. During interstadials, nutrient advection through freshwater inputs during autumn-winter needs also to be considered to fully understand PP regimes.	[Penaud, A.] Univ Brest, CNRS, IFREMER, Geoocean UMR 6538, Plouzane, France; [Eynaud, F.; Etourneau, J.; Bonnin, J.; Zaragosi, S.] Univ Bordeaux, CNRS, EPOC, Pessac, France; [Etourneau, J.] PSL Res Univ, EPHE, Paris, France; [de Vernal, A.] Univ Quebec Montreal UQAM, Geotop, Montreal, PQ, Canada; [Kim, J-H; Gal, J-K] KOPRI Korea Polar Res Inst, Incheon, South Korea; [Kang, S.] Hayang Univ ERICA, Gyeonggi Do, South Korea; [Oliveira, D.] Univ Algarve, CCMAR, Ctr Ciencias Mar, Campus Gambelas, Faro, Portugal; [Oliveira, D.] Inst Portugues Mar & Atmosfera IPMA, Div Geol & Georecursos Marinhos, Alges, Portugal; [Waelbroeck, C.] Sorbonne Univ, LOCEAN IPSL, CNRS, UIRD,MNHN, Paris, France	Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); Ifremer; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); University of Quebec; University of Quebec Montreal; Korea Polar Research Institute (KOPRI); Universidade do Algarve; Instituto Portugues do Mar e da Atmosfera; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite	Penaud, A (通讯作者)，Univ Brest, CNRS, IFREMER, Geoocean UMR 6538, Plouzane, France.	aurelie.penaud@univ-brest.fr	ZARAGOSI, Sébastien/JXL-2488-2024; Gal, Jong-Ku/JMC-5276-2023; Penaud, Aurelie/F-2485-2011; de Vernal, Anne/D-5602-2013; Oliveira, Dulce/H-9855-2018	Zaragosi, Sebastien/0000-0002-1456-8129; Penaud, Aurelie/0000-0003-3578-4549; de Vernal, Anne/0000-0001-5656-724X; Oliveira, Dulce/0000-0002-3016-532X	French CNRS; European Research Council Grant ACCLIMATE [339108]; National Research Foundation of Korea (NRF) - Ministry of Science and ICT [NRF-2021M1A5A1075512]; French Ministry for Europe and Foreign Affairs (MEAE); Ministry of Higher Education, Research and Innovation (MESRI); National Research Foundation of Korea (NRF); Korean Ministry of Science and ICT (MSIT) [MD99-2339]; Portuguese Foundation for Science and Technology (FCT) through the CCMAR FCT Research Unit [UIDB/04326/2020, CEECIND/02208/2017]; European Research Council (ERC) [339108] Funding Source: European Research Council (ERC)	French CNRS(Centre National de la Recherche Scientifique (CNRS)); European Research Council Grant ACCLIMATE(European Research Council (ERC)); National Research Foundation of Korea (NRF) - Ministry of Science and ICT(National Research Foundation of KoreaMinistry of Science, ICT & Future Planning, Republic of Korea); French Ministry for Europe and Foreign Affairs (MEAE); Ministry of Higher Education, Research and Innovation (MESRI)(Ministry of Higher Education, Research & Innovation (MESRI)); National Research Foundation of Korea (NRF)(National Research Foundation of Korea); Korean Ministry of Science and ICT (MSIT)(Ministry of Science & ICT (MSIT), Republic of Korea); Portuguese Foundation for Science and Technology (FCT) through the CCMAR FCT Research Unit; European Research Council (ERC)(European Research Council (ERC))	Thanks are due 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. Part of the analyses of 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 climate." CW and FE acknowledge support from the European Research Council Grant ACCLIMATE/No. 339108. This study was also partly supported by the National Research Foundation of Korea (NRF) grant funded through the Ministry of Science and ICT (NRF-2021M1A5A1075512). We acknowledge the French Ministry for Europe and Foreign Affairs (MEAE), the Ministry of Higher Education, Research and Innovation (MESRI), the National Research Foundation of Korea (NRF) as well as the Korean Ministry of Science and ICT (MSIT) through its international Hubert Curien (PHC) partnership programme STAR between France and Republic of Korea to financially support the MEDKO (Abrupt Climate events in the past Mediterranean and Korean basins) project that financially supported the alkenone-based SST record of core MD99-2339. We are also grateful to Prof. Shin for his considerable analytical support and access to lab facilities at Hanyang University, Republic of Korea. DO acknowledges funding from Portuguese Foundation for Science and Technology (FCT) through the CCMAR FCT Research Unit-project UIDB/04326/2020 and contract (CEECIND/02208/2017). Finally, we would like to thank the Bureau de traduction of the University of Brest for the improvement of English, and the two reviewers, including Andre Bahr, for their constructive and precise comments.	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Paleoclimatology	FEB	2022	37	2							e2021PA004316	10.1029/2021PA004316	http://dx.doi.org/10.1029/2021PA004316			21	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	ZL2FZ		Green Published, Green Submitted			2025-03-11	WOS:000763496800009
J	Cavion, F; Pelin, M; Ponti, C; Della Loggia, R; Tubaro, A; Sosa, S				Cavion, Federica; Pelin, Marco; Ponti, Cristina; Della Loggia, Roberto; Tubaro, Aurelia; Sosa, Silvio			Ecotoxicological Impact of the Marine Toxin Palytoxin on the Micro-Crustacean <i>Artemia franciscana</i>	MARINE DRUGS			English	Article						Artemia; palytoxin; ecotoxicology; mortality; oxidative stress; antioxidant enzyme activity	OSTREOPSIS CF. OVATA; ANTIOXIDANT ENZYME-ACTIVITIES; GLUTATHIONE-S-TRANSFERASE; LIPID-PEROXIDATION; OXIDATIVE STRESS; GRAPHENE OXIDE; GENUS ARTEMIA; DAPHNIA-MAGNA; TOXICITY; MODEL	Palytoxin (PLTX) is a highly toxic polyether identified in various marine organisms, such as Palythoa soft corals, Ostreopsis dinoflagellates, and Trichodesmium cyanobacteria. In addition to adverse effects in humans, negative impacts on different marine organisms have been often described during Ostreopsis blooms and the concomitant presence of PLTX and its analogues. Considering the increasing frequency of Ostreopsis blooms due to global warming, PLTX was investigated for its effects on Artemia franciscana, a crustacean commonly used as a model organism for ecotoxicological studies. At concentrations comparable to those detected in culture media of O. cf. ovata (1.0-10.0 nM), PLTX significantly reduced cysts hatching and induced significant mortality of the organisms, both at larval and adult stages. Adults appeared to be the most sensitive developmental stage to PLTX: significant mortality was recorded after only 12 h of exposure to PLTX concentrations > 1.0 nM, with a 50% lethal concentration (LC50) of 2.3 nM (95% confidence interval = 1.2-4.7 nM). The toxic effects of PLTX toward A. franciscana adults seem to involve oxidative stress induction. Indeed, the toxin significantly increased ROS levels and altered the activity of the major antioxidant enzymes, in particular catalase and peroxidase, and marginally glutathione-S-transferase and superoxide dismutase. On the whole, these results indicate that environmentally relevant concentrations of PLTX could have a negative effect on Artemia franciscana population, suggesting its potential ecotoxicological impact at the marine level.	[Cavion, Federica; Pelin, Marco; Ponti, Cristina; Tubaro, Aurelia; Sosa, Silvio] Univ Trieste, Dept Life Sci, I-34127 Trieste, Italy; [Della Loggia, Roberto] Univ Trieste, Dept Chem & Pharmaceut Sci, I-34127 Trieste, Italy	University of Trieste; University of Trieste	Pelin, M (通讯作者)，Univ Trieste, Dept Life Sci, I-34127 Trieste, Italy.	federica.cavion@phd.units.it; mpelin@units.it; cponti@units.it; rdellaloggia@units.it; tubaro@units.it; ssosa@units.it		SOSA, SILVIO/0000-0002-2909-6603; PONTI, CRISTINA/0000-0002-9904-0074; Cavion, Federica/0000-0001-6901-5866; Pelin, Marco/0000-0002-4306-7411				Abatzopoulos T J., 2002, Artemia: Basic and Applied Biology; Accoroni Stefano, 2016, Advances in Oceanography and Limnology, V7, P1, DOI 10.4081/aiol.2016.5591; Ajuzie CC, 2007, J APPL PHYCOL, V19, P513, DOI 10.1007/s10811-007-9164-9; [Anonymous], 2003, Biol Ambient, DOI DOI 10.1021/AC060250J; Barata C, 2005, COMP BIOCHEM PHYS C, V140, P175, DOI 10.1016/j.cca.2005.01.013; Barata C, 2005, COMP BIOCHEM PHYS B, V140, P81, DOI 10.1016/j.cbpc.2004.09.025; Beattie KA, 2003, AQUAT TOXICOL, V62, P219, DOI 10.1016/S0166-445X(02)00091-7; Boyland E., 2006, ADV ENZYMOLOGY AND R, V173, P219; Louzao MC, 2010, TOXICON, V56, P842, DOI 10.1016/j.toxicon.2010.02.027; Casabianca S, 2019, ENVIRON POLLUT, V244, P617, DOI 10.1016/j.envpol.2018.09.110; Cavion F, 2020, ENVIRON SCI-NANO, V7, P3605, DOI 10.1039/d0en00747a; Cen JY, 2019, FISH SHELLFISH IMMUN, V95, P670, DOI 10.1016/j.fsi.2019.11.001; COOPER SD, 1984, J ANIM ECOL, V53, P51, DOI 10.2307/4341; Faimali M, 2012, MAR ENVIRON RES, V76, P97, DOI 10.1016/j.marenvres.2011.09.010; GLEIBS S, 1995, TOXICON, V33, P1531, DOI 10.1016/0041-0101(95)00079-2; Gonçalves-Soares D, 2012, MAR ENVIRON RES, V75, P54, DOI 10.1016/j.marenvres.2011.07.007; Gorbi S, 2013, FISH SHELLFISH IMMUN, V35, P941, DOI 10.1016/j.fsi.2013.07.003; Gorbi S, 2012, CHEMOSPHERE, V89, P623, DOI 10.1016/j.chemosphere.2012.05.064; Granéli E, 2011, HARMFUL ALGAE, V10, P165, DOI 10.1016/j.hal.2010.09.002; Guerrini F, 2010, TOXICON, V55, P211, DOI 10.1016/j.toxicon.2009.07.019; Guppy R, 2019, TOXICON, V167, P117, DOI 10.1016/j.toxicon.2019.06.020; Ingarao Cristina C., 2014, Harmful Algae News, V48, P2; Jemec A, 2008, COMP BIOCHEM PHYS C, V147, P61, DOI 10.1016/j.cbpc.2007.07.006; Kerbrat AS, 2011, MAR DRUGS, V9, P543, DOI 10.3390/md9040543; Larsson ME, 2018, MAR ECOL PROG SER, V596, P49, DOI 10.3354/meps12579; Libralato G, 2016, ECOL INDIC, V69, P35, DOI 10.1016/j.ecolind.2016.04.017; Livingstone D.R., 1991, Advances in Comparative and Environmental Physiology, V7, P45; LIVINGSTONE DR, 1990, FUNCT ECOL, V4, P415, DOI 10.2307/2389604; Mackie JA, 2010, LIMNOL OCEANOGR-METH, V8, P337, DOI 10.4319/lom.2010.8.337; Masó M, 2003, SCI MAR, V67, P107, DOI 10.3989/scimar.2003.67n1107; Migliore L, 1997, WATER RES, V31, P1801, DOI 10.1016/S0043-1354(96)00412-5; Mme-Sophie P, 2019, J EXP MAR BIOL ECOL, V516, P103, DOI 10.1016/j.jembe.2019.05.004; MOORE RE, 1971, SCIENCE, V172, P495, DOI 10.1126/science.172.3982.495; Neves RAF, 2018, MAR ENVIRON RES, V135, P11, DOI 10.1016/j.marenvres.2018.01.014; Neves RAF, 2017, PLOS ONE, V12, DOI 10.1371/journal.pone.0175168; Nunes B, 2006, CHEMOSPHERE, V62, P581, DOI 10.1016/j.chemosphere.2005.06.013; Nunes BS, 2006, ENVIRON POLLUT, V144, P453, DOI 10.1016/j.envpol.2005.12.037; Olsen T, 2001, ENVIRON TOXICOL CHEM, V20, P1725, DOI [10.1897/1551-5028(2001)020<1725:VIAAGS>2.0.CO;2, 10.1002/etc.5620200815]; Ott M, 2007, APOPTOSIS, V12, P913, DOI 10.1007/s10495-007-0756-2; Pagliara P, 2012, TOXICON, V60, P1203, DOI 10.1016/j.toxicon.2012.08.005; Papadopoulos AI, 2004, MAR BIOL, V144, P295, DOI 10.1007/s00227-003-1203-8; Pelin M, 2011, TOXICOLOGY, V282, P30, DOI 10.1016/j.tox.2011.01.010; Pelin M, 2014, TOXICOL LETT, V229, P440, DOI 10.1016/j.toxlet.2014.07.022; Pelin M, 2013, TOXICOL APPL PHARM, V266, P1, DOI 10.1016/j.taap.2012.10.023; Persoone G., 1987, Artemia Res. 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Drugs	FEB	2022	20	2							81	10.3390/md20020081	http://dx.doi.org/10.3390/md20020081			14	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	ZM8MY	35200611	Green Published, gold			2025-03-11	WOS:000764605400001
J	Wei, ZC; Ding, W; Li, ML; Shi, JX; Wang, HZ; Wang, YR; Li, YB; Xu, YQ; Hu, JJ; Bao, ZM; Hu, XL				Wei, Zhongcheng; Ding, Wei; Li, Moli; Shi, Jiaoxia; Wang, Huizhen; Wang, Yangrui; Li, Yubo; Xu, Yiqiang; Hu, Jingjie; Bao, Zhenmin; Hu, Xiaoli			The Caspase Homologues in Scallop <i>Chlamys farreri</i> and Their Expression Responses to Toxic Dinoflagellates Exposure	TOXINS			English	Article						caspase; development; paralytic shellfish toxin; Zhikong scallop; Chlamys farreri	ALEXANDRIUM-CATENELLA; INFLAMMATORY CASPASES; PHYLOGENETIC ANALYSIS; APOPTOSIS; OYSTER; GENE; DIFFERENTIATION; METAMORPHOSIS; HEMOCYTES; CLONING	The cysteine aspartic acid-specific protease (caspase) family is distributed across vertebrates and invertebrates, and its members are involved in apoptosis and response to cellular stress. The Zhikong scallop (Chlamys farreri) is a bivalve mollusc that is well adapted to complex marine environments, yet the diversity of caspase homologues and their expression patterns in the Zhikong scallop remain largely unknown. Here, we identified 30 caspase homologues in the genome of the Zhikong scallop and analysed their expression dynamics during all developmental stages and following exposure to paralytic shellfish toxins (PSTs). The 30 caspase homologues were classified as initiators (caspases-2/9 and caspases-8/10) or executioners (caspases-3/6/7 and caspases-3/6/7-like) and displayed increased copy numbers compared to those in vertebrates. Almost all of the caspase-2/9 genes were highly expressed throughout all developmental stages from zygote to juvenile, and their expression in the digestive gland and kidney was slightly influenced by PSTs. The caspase-8/10 genes were highly expressed in the digestive gland and kidney, while PSTs inhibited their expression in these two organs. After exposure to different Alexandrium PST-producing algae (AM-1 and ACDH), the number of significantly up-regulated caspase homologues in the digestive gland increased with the toxicity level of PST derivatives, which might be due to the higher toxicity of GTXs produced by AM-1 compared to the N-sulphocarbamoyl analogues produced by ACDH. However, the effect of these two PST-producing algae strains on caspase expression in the kidney seemed to be stronger, possibly because the PST derivatives were transformed into highly toxic compounds in scallop kidney, and suggested an organ-dependent response to PSTs. These results indicate the dedicated control of caspase gene expression and highlight their contribution to PSTs in C. farreri. This work provides a further understanding of the role of caspase homologues in the Zhikong scallop and can guide future studies focussing on the role of caspases and their interactions with PSTs.	[Wei, Zhongcheng; Ding, Wei; Li, Moli; Shi, Jiaoxia; Wang, Huizhen; Wang, Yangrui; Li, Yubo; Xu, Yiqiang; Hu, Jingjie; Bao, Zhenmin; Hu, Xiaoli] Ocean Univ China, Coll Marine Life Sci, MOE Key Lab Marine Genet & Breeding, Qingdao 266003, Peoples R China; [Wang, Huizhen; Bao, Zhenmin; Hu, Xiaoli] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Fisheries Sci & Food Prod Proc, Qingdao 266237, Peoples R China; [Hu, Jingjie; Bao, Zhenmin] Ocean Univ China, Sanya Oceanog Inst, Lab Trop Marine Germplasm Resources & Breeding En, Sanya 572000, Peoples R China	Ocean University of China; Laoshan Laboratory; Ocean University of China	Wang, HZ; Hu, XL (通讯作者)，Ocean Univ China, Coll Marine Life Sci, MOE Key Lab Marine Genet & Breeding, Qingdao 266003, Peoples R China.; Wang, HZ; Hu, XL (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Fisheries Sci & Food Prod Proc, Qingdao 266237, Peoples R China.	weizhongcheng@stu.ouc.edu.cn; dingwei@ouc.edu.cn; ml940520@163.com; shijiaoxia@ouc.edu.cn; wanghuizhen@ouc.edu.cn; yangrui1121@126.com; liyubo@stu.ouc.edu.cn; 21200631119@stu.ouc.edu.cn; hujingjie@ouc.edu.cn; zmbao@ouc.edu.cn; hxl707@ouc.edu.cn	zhang, jinsheng/GXF-8167-2022; Chen, Zhaoying/IAN-5249-2023; DING, Wei/CVK-8505-2022	Wei, Zhongcheng/0000-0002-5300-1141; DING, Wei/0000-0002-1847-244X	National Key RD Project [2018YFD0900604, 2019YFC1605704]; Sanya Yazhou Bay Science and Technology City [SKJC-KJ-2019KY01]	National Key RD Project; Sanya Yazhou Bay Science and Technology City	Funding:This research was funded by the National Key R&D Project (2018YFD0900604 and 2019YFC1605704) and Sanya Yazhou Bay Science and Technology City (SKJC-KJ-2019KY01).	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J	Zhang, MZ; Du, BX; Wu, ZX; Dou, LH; Zhumahun, A; Jiaoba, DZ; Jin, PH; Du, Z; Wang, S; Xia, YQ				Zhang, Mingzhen; Du, Baoxia; Wu, Zhixiong; Dou, Longhui; Zhumahun, Abduljan; Jiaoba, Dunzhu; Jin, Peihong; Du, Zhen; Wang, Sen; Xia, Yanqing			Dinoflagellate cyst biostratigraphy of initial Neotethys transgression deposits from the Cenomanian and Turonian in the Tarim Basin, western China	MARINE AND PETROLEUM GEOLOGY			English	Article						Dinoflagellate cysts; Biostratigraphy; Transgression; Cenomanian-turonian transition; Tarim basin	PALEOENVIRONMENTAL ANALYSIS; SEA; DINOCYST; BOUNDARY; STRATIGRAPHY; REEVALUATION; ASSEMBLAGES; OLIGOCENE; RECORD; MARGIN	Under the great transgressions of the Late Cretaceous, the Neotethys Sea firstly invaded the western Tarim Basin, center Asian and this continued until the Paleogene. This study presents successive dinoflagellate cyst (dinocyst) records from the Kukebai Formaion deposited during initial transgressive periods. A total of 45 samples from the Core ZK 5-2 drilled in the southern part of the western Tarim Basin yield 78 taxa including 74 taxa of dinocysts, two genera of chlorophyte algae, and two acritarch species. Upwardly, three dinoflagellate zones are distinguished in the Kukebai Formation: Subtilisphaera perlucida (interval Zone), Cyclonephelium brevispinatum (interval zone), and Heterosphaeridium difficile (interval zone) respectively. Successive dinocyst records in this study calibrate the chronostratigraphy of the Kukebai Formation from the lower Cenomanian to the lowermost Turonian. A high abundance of Subtilisphaera perlucida and sporadic Litosphaeridium siphoniphorum can be observed in the lowest Kukebai Formation, probably indicating initial sea transgression in the Tarim Basin that took place in early Cenomanian. The distribution events of key dinocyst taxa such as the first occurrence of the H. difficile and the last occurrence of consistent occurrence of Litosphaeridium siphoniphorum, indicate that the C/T boundary interval should be approximately 183 m deep in Core ZK 5-2, at the uppermost Middle Kukebai Formation.	[Zhang, Mingzhen; Jiaoba, Dunzhu; Jin, Peihong; Xia, Yanqing] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China; [Zhang, Mingzhen; Jiaoba, Dunzhu; Jin, Peihong; Xia, Yanqing] Key Lab Petr Resources, Lanzhou 730000, Gansu, Peoples R China; [Du, Baoxia; Du, Zhen; Wang, Sen] Lanzhou Univ, Key Lab Mineral Resources Western China, Lanzhou 730000, Gansu, Peoples R China; [Du, Baoxia; Du, Zhen; Wang, Sen] Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China; [Wu, Zhixiong] PetroChina Qinghai Oilfield Co, Res Inst Explorat & Dev, Dunhuang 736202, Peoples R China; [Dou, Longhui; Zhumahun, Abduljan] Xinjiang Uygur Autonomous Reg Coalfield Geol Bur, Comprehens Geol Explorat Team, Urumqi 830009, Peoples R China	Chinese Academy of Sciences; Lanzhou University; Lanzhou University; China National Petroleum Corporation	Zhang, MZ (通讯作者)，Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Peoples R China.	zhangmzh08@lzb.ac.cn		zhang, ming zhen/0000-0002-5624-1511	Second Tibetan Plateau Scientific Expedition (STEP) program [2019QZKK0704]; National Natural Science Foundation of China [41602023, 41872010]; Youth Innovation Promotion Association CAS	Second Tibetan Plateau Scientific Expedition (STEP) program; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Youth Innovation Promotion Association CAS	Constructive comments by the section editor Istvan Csato and three reviewers Przemyslaw Gedl and two anonymous reviewers significantly improved the manuscript. 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Pet. Geol.	APR	2022	138									10.1016/j.marpetgeo.2022.105531	http://dx.doi.org/10.1016/j.marpetgeo.2022.105531		JAN 2022	16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	YQ0EP					2025-03-11	WOS:000748992300002
J	Heikkilä, M; Ribeiro, S; Weckström, K; Pienkowski, AJ				Heikkila, Maija; Ribeiro, Sofia; Weckstrom, Kaarina; Pienkowski, Anna J.			Predicting the future of coastal marine ecosystems in the rapidly changing Arctic: The potential of palaeoenvironmental records	ANTHROPOCENE			English	Review						Cryosphere; Coastal ecosystems; Sea ice; Terrestrial runoff; Climate proxies; Sediment archives	NORTHERN NORTH-ATLANTIC; SEA-ICE CONDITIONS; EASTERN FRAM STRAIT; ORGANIC-MATTER; DINOFLAGELLATE CYSTS; ENVIRONMENTAL-CHANGE; SPATIAL VARIABILITY; SURFACE CONDITIONS; WEST GREENLAND; BARENTS SEA	Frozen components on land and in the ocean (sea ice, ice sheets, glaciers and permafrost) form the cryosphere, which, together with the ocean, moderates the physical and chemical habitat for life in the Arctic and beyond. Changes in these components, as a response to rapidly warming climate in the Arctic, are intensely expressed in the coastal zone. These areas receive increased terrestrial runoff while subject to a changing sea-ice and ocean environment. Proxies derived from marine sediment archives provide long-term data that extend beyond instrumental measurements. They are therefore fundamental in disentangling human-driven versus natural processes, changes and responses. This paper (1) provides an overview of current Arctic cryosphere change, (2) reviews state-of-the-art palaeoecological approaches, (3) identifies methodological and knowledge gaps, and (4) discusses the strengths and future potential of palaeoecology and palaeoceanography to respond to societally relevant coastal marine ecosystem challenges. We utilise responses to an open survey conducted by the Future Earth Past Global Changes (PAGES) working group Arctic Cryosphere Change and Coastal Marine Ecosystems (ACME). Significant research advancements have taken place in recent decades, including the increasingly common use of multi-proxy (multiple lines of evidence) studies, improved understanding of species-environment relationships, and development of novel proxies. Significant gaps remain, however, in the understanding of proxy sources and behaviour, the use of quantitative techniques, and the availability of reference data from coastal environments. We highlight the need for critical methodological refinement, interdisciplinary collaboration on research approaches, and enhanced communication across the scientific community.	[Heikkila, Maija; Weckstrom, Kaarina] Univ Helsinki, Fac Biol & Environm Sci, Environm Change Res Unit, Ecosyst & Environm Res Programme, POB 65, Helsinki 00014, Finland; [Heikkila, Maija; Weckstrom, Kaarina] Univ Helsinki, Helsinki Inst Sustainabil Sci HELSUS, Helsinki, Finland; [Ribeiro, Sofia; Weckstrom, Kaarina] Geol Survey Denmark & Greenland GEUS, Dept Glaciol & Climate, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Pienkowski, Anna J.] Univ Ctr Svalbard UNIS, Dept Arctic Geol, N-9171 Longyearbyen, Svalbard, Norway; [Pienkowski, Anna J.] Adam Mickiewicz Univ, Inst Geol, Makow Polnych 16, PL-61606 Poznan, Poland	University of Helsinki; University of Helsinki; Geological Survey Of Denmark & Greenland; University Centre Svalbard (UNIS); Adam Mickiewicz University	Heikkilä, M (通讯作者)，Univ Helsinki, Fac Biol & Environm Sci, Environm Change Res Unit, Ecosyst & Environm Res Programme, POB 65, Helsinki 00014, Finland.	maija.heikkila@helsinki.fi	Pieńkowski, Anna/AAL-1312-2020; Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018; Pienkowski, Anna/J-9339-2013; Heikkila, Maija/N-7659-2013	Ribeiro, Sofia/0000-0003-0672-9161; Pienkowski, Anna/0000-0002-3606-7130; Heikkila, Maija/0000-0003-3885-8670; Weckstrom, Kaarina/0000-0002-3889-0788	Academy of Finland [1296895, 1308272, 1328540, 1334509]; Independent Research Fund of Denmark [9064-0039B]; Geocenter Denmark; Natural Sciences and Engineering Council of Canada [RGPIN-2016-05457]	Academy of Finland(Research Council of Finland); Independent Research Fund of Denmark; Geocenter Denmark; Natural Sciences and Engineering Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC))	The authors are grateful for the continuing support from the Past Global Changes International Project Office (PAGES-IPO) and the valuable contributions from the respondents to the open PAGES Arctic Cryosphere Change and Coastal Marine Ecosystems Working Group (http://pastglobalchanges.org/acme) community questionnaire. M.H. received funding from the Academy of Finland (Grants 1296895, 1308272, 1328540, 1334509) . S.R received funding from the Independent Research Fund of Denmark (Grant 9064-0039B) and Geocenter Denmark. A.J.P. acknowledges funding from the Natural Sciences and Engineering Council of Canada (Discovery Grant RGPIN-2016-05457) . We thank the editors and two anonymous reviewers whose comments contributed to improving the manuscript.	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J	Fuchsman, CA; Cherubini, L; Hays, MD				Fuchsman, Clara A.; Cherubini, Luca; Hays, Matthew D.			An analysis of protists in Pacific oxygen deficient zones: implications for Prochlorococcus and N-2-producing bacteria	ENVIRONMENTAL MICROBIOLOGY			English	Article							EASTERN TROPICAL PACIFIC; PLANKTONIC NAKED AMEBAS; MINIMUM ZONE; AEROBIC RESPIRATION; EPIBIOTIC BACTERIA; DIVERSITY; SEA; GROWTH; COMMUNITIES; FJORD	Ocean oxygen deficient zones (ODZs) host 30%-50% of marine N-2 production. Cyanobacteria photosynthesizing in the ODZ create a secondary chlorophyll maximum and provide organic matter to N-2-producing bacteria. This chlorophyll maximum is thought to occur due to reduced grazing in anoxic waters. We first examine ODZ protists with long amplicon reads. We then use non-primer-based methods to examine the composition and relative abundance of protists in metagenomes from the Eastern Tropical North and South Pacific ODZs and compare these data to the oxic Hawaii Ocean Time-series (HOT) in the North Pacific. We identify and quantify protists in proportion to the total microbial community. From metagenomic data, we see a large drop in abundance of fungi and protists such as choanoflagellates, radiolarians, cercozoa and ciliates in the ODZs but not in the oxic mesopelagic at HOT. Diplonemid euglenozoa were the only protists that increased in the ODZ. Dinoflagellates and foraminifera reads were also present in the ODZ though less abundant compared to oxic waters. Denitrification has been found in foraminifera but not yet in dinoflagellates. DNA techniques cannot separate dinoflagellate cells and cysts. Metagenomic analysis found taxonomic groups missed by amplicon sequencing and identified trends in abundance.	[Fuchsman, Clara A.; Hays, Matthew D.] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA; [Cherubini, Luca] Maryland Sea Grant Coll, College Pk, MD 20740 USA	University System of Maryland; University of Maryland Center for Environmental Science	Fuchsman, CA (通讯作者)，Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA.	cfuchsman@umces.edu	Fuchsman, Clara/AAM-3641-2021	Fuchsman, Clara/0000-0002-9151-4984	Maryland Sea Grant REU program - National Science Foundation [OCE-1756244];  [OCE-1046017]	Maryland Sea Grant REU program - National Science Foundation; 	We would like to thank the captain and the crew of the RV Thompson and RV Palmer as well as chief scientist A.H. Devol. These cruises on which these samples were obtained were funded by OCE-1046017 to A. H. Devol. L. Cherubini was funded by the Maryland Sea Grant REU program which in turn was funded by National Science Foundation grant OCE-1756244. This work was funded by Horn Point Laboratory.	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J	Lim, YK; Hong, S; Baek, SH				Lim, Young Kyun; Hong, Seongjin; Baek, Seung Ho			Potential influence of the proliferation of sediment-based diatoms on blooms of a harmful dinoflagellate <i>Cochlodinium polykrikoides</i>: a microcosm approach	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Typhoon; Sediment resuspension; Diatoms competition; Bloom control; Cochlodinium polykrikoides	SAGAMI BAY; MARINE BACTERIOPLANKTON; MICROBIAL COMMUNITY; GROWTH-INHIBITION; COASTAL WATERS; RED TIDES; PHYTOPLANKTON; DIVERSITY; SEA; SUCCESSION	Typhoons cause significant environmental damage in coastal areas and one of their effects is the suspension of the resting stage cells of diatoms from the surface sediment. We performed microcosm experiments in 10-L containers using natural sediments from three different sites of southern Korean coastal waters (Geoje, Goheung, and Tongyeong) to simulate the effect of suspension of sediment-based diatoms by a typhoon on blooms of the harmful dinoflagellate Cochlodinium polykrikoides. This dinoflagellate grew well under control conditions and exhibited a maximum abundance of 985 cells mL(-1) on day 10, but all treatment groups (Geoje, Goheung, and Tongyeong) had decreased abundances by day 4 and fewer than 50 cells mL(-1) on day 10. As C. polykrikoides declined, two diatoms (Skeletonema spp. and Chaetoceros spp.) dominated in the three treatment groups. In particular, these diatoms increased to 2.9 x 10(4) cells mL(-1) on day 5 and 2.3 x 10(4) cells mL(-1) on day 7 in the Geoje group. A multivariate redundancy analysis indicated a negative correlation between the abundances of C. polykrikoides and Chaetoceros spp., and this corresponded to the sharpest decrease of C. polykrikoides in the Geoje group. There were also changes in the bacterial community associated with changes in phytoplankton. During the early phase, when C. polykrikoides was dominant, Rhodobacterales prevailed (> 50%) in all treatment groups, and the proportion of these bacteria in the Geoje group decreased earlier than in the other groups. At the end of the experiment, there was a high proportion of Verrucomicrobiales, suggesting that sediment addition led to changes in the bacterial community. Overall, our microcosm experiments suggest that the significant environmental changes following the passage of a typhoon, especially the suspension and proliferation of sediment-based diatoms, directly affects the bacterial community and decreases blooms of C. polykrikoides.	[Lim, Young Kyun; Baek, Seung Ho] KIOST Korea Inst Ocean Sci & Technol, Risk Assessment Res Ctr, Geoje 53201, South Korea; [Lim, Young Kyun; Baek, Seung Ho] Univ Sci & Technol, Dept Ocean Sci, Daejeon 34113, South Korea; [Hong, Seongjin] Chungnam Natl Univ, Dept Ocean Environm Sci, Daejeon 34134, South Korea	Korea Institute of Ocean Science & Technology (KIOST); University of Science & Technology (UST); Chungnam National University	Baek, SH (通讯作者)，KIOST Korea Inst Ocean Sci & Technol, Risk Assessment Res Ctr, Geoje 53201, South Korea.; Baek, SH (通讯作者)，Univ Sci & Technol, Dept Ocean Sci, Daejeon 34113, South Korea.	baeksh@kiost.ac.kr	Hong, Seongjin/AAO-8503-2020; Hong, Seongjin/B-5933-2013	BAEK, SEUNG HO/0000-0002-5402-2518; Hong, Seongjin/0000-0002-6305-8731	Korea Institute of Ocean Science and Technology (KIOST) [PE99912]; Ministry of Food and Drug Safety [20163MFDS641]	Korea Institute of Ocean Science and Technology (KIOST); Ministry of Food and Drug Safety(Ministry of Food & Drug Safety (MFDS), Republic of Korea)	This research was supported by the Korea Institute of Ocean Science and Technology (KIOST; PE99912) and by a grant (20163MFDS641) from Ministry of Food and Drug Safety.	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Appl. Phycol.	APR	2022	34	2					953	964		10.1007/s10811-021-02674-y	http://dx.doi.org/10.1007/s10811-021-02674-y		JAN 2022	12	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	ZY4KI					2025-03-11	WOS:000742604700002
J	Danise, S; Slater, SM; Vajda, V; Twitchett, RJ				Danise, Silvia; Slater, Sam M.; Vajda, Vivi; Twitchett, Richard J.			Land-sea ecological connectivity during a Jurassic warming event	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						global warming; Toarcian; extinction; pollen and spores; phytoplankton; benthos	OCEANIC ANOXIC EVENT; EARLY TOARCIAN; ISOTOPE EVIDENCE; CARBON-CYCLE; LUSITANIAN BASIN; MASS EXTINCTION; PERTURBATION; TERRESTRIAL; DEPOSITION; MERCURY	Knowledge on how climate change affects land-sea ecological connectivity in deep time is scarce. To fill this knowledge gap we have assembled a unique dataset through a Jurassic (early Toarcian) warming event that includes quantitative abundance data from pollen and spores, organic-walled marine plankton and benthic macro-invertebrates, in association with geochemical data derived from the same sampled horizons, from the Cleveland Basin, UK. Using this dataset we: (i) reconstruct the timing of degradation and recovery of land-plants, marine primary producers and benthic fauna in response to this event, and (ii) test for connectivity between changes in land and marine ecosystems. We find a discrepancy between the timing of the response of land-plant and marine ecosystems to the event. Land-plants were the first to be affected by initial warming, but also recovered relatively quickly after the peak of warmth to return to pre-event levels of richness and diversity. Plankton and benthic fauna instead experienced a delayed response to initial warming, but as warming peaked, they suffered a rapid and extreme turnover. Recovery in the shelf sea was also delayed (particularly for the benthos) compared to the vegetation. Ecological connectivity analyses show a strong link between changes in terrestrial and marine ecosystems. The loss of large trees on land contributed to changes in marine plankton, from dinoflagellate-to prasinophyte algal-dominated communities, by enhancing erosion, runoff and nutrient-supply into shallow seas. Eutrophication and changes in primary productivity contributed to the decrease of dissolved oxygen in the water column and in bottom waters, which in turn affected benthic communities. Such cause-effect mechanisms observed in the Cleveland Basin are likely to have occurred in other basins of the Boreal Realm, and in part also in basins of the Sub-Boreal and Tethyan realms. Although palaeolatitudinal and palaeoceanographic gradients may have controlled local and regional changes in land-plants and marine ecosystems during the Early Jurassic, the main climatic and environmental changes linked to rapid global warming, enhanced weathering and high primary productivity, are shared among all the examined realms. (c) 2021 The Authors. Published by Elsevier B.V.	[Danise, Silvia] Univ Firenze, Dipartimento Sci Terra, Florence, Italy; [Slater, Sam M.; Vajda, Vivi] Swedish Museum Nat Hist, Dept Palaeobiol, Stockholm, Sweden; [Twitchett, Richard J.] Nat Hist Museum, Dept Earth Sci, London SW7 5BD, England	University of Florence; Swedish Museum of Natural History; Natural History Museum London	Danise, S (通讯作者)，Univ Firenze, Dipartimento Sci Terra, Florence, Italy.; Slater, SM (通讯作者)，Swedish Museum Nat Hist, Dept Palaeobiol, Stockholm, Sweden.	silvia.danise@unifi.it; sam.slater@nrm.se	Vajda, Vivi/N-7693-2018	Danise, Silvia/0000-0002-6098-609X	Swedish Research Council [2019-04524, 2019-04061]; Natural Environment Research Council (NERC) [NE/I005641/1]; NERC [NE/I005641/2, NE/I005641/1] Funding Source: UKRI; Swedish Research Council [2019-04061, 2019-04524] Funding Source: Swedish Research Council	Swedish Research Council(Swedish Research Council); Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Swedish Research Council(Swedish Research Council)	We are grateful to M. Anderson for advice on statistical anal-yses. We also thank A. Caruthers, two anonymous reviewers, and the editor T. Lyons, for their constructive comments. This research was funded by a Swedish Research Council grant to S.M.S. [grant no. 2019-04524] and to V.V. [grant no. 2019-04061] , and a Natu-ral Environment Research Council (NERC) grant to R.J.T. [grant no. NE/I005641/1] .	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Sci. Lett.	JAN 15	2022	578								117290	10.1016/j.epsl.2021.117290	http://dx.doi.org/10.1016/j.epsl.2021.117290		JAN 2022	11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	0M4IX		Green Published, hybrid			2025-03-11	WOS:000782120900010
J	Kihika, JK; Wood, SA; Rhodes, L; Smith, KF; Thompson, L; Challenger, S; Ryan, KG				Kihika, Joseph Kanyi; Wood, Susanna A.; Rhodes, Lesley; Smith, Kirsty F.; Thompson, Lucy; Challenger, Sarah; Ryan, Ken G.			Cryoprotectant treatment tests on three morphologically diverse marine dinoflagellates and the cryopreservation of <i>Breviolum</i> sp. (Symbiodiniaceae)	SCIENTIFIC REPORTS			English	Article							HARMFUL ALGAL BLOOMS; ALEXANDRIUM-FUNDYENSE; NEW-ZEALAND; MICROALGAE; DINOPHYCEAE; CYSTS; PINNATOXINS; TOXICITY; STORAGE; DIATOM	Dinoflagellates are among the most diverse group of microalgae. Many dinoflagellate species have been isolated and cultured, and these are used for scientific, industrial, pharmaceutical, and agricultural applications. Maintaining cultures is time-consuming, expensive, and there is a risk of contamination or genetic drift. Cryopreservation offers an efficient means for their long-term preservation. Cryopreservation of larger dinoflagellate species is challenging and to date there has been only limited success. In this study, we explored the effect of cryoprotectant agents (CPAs) and freezing methods on three species: Vulcanodinium rugosum, Alexandrium pacificum and Breviolum sp. A total of 12 CPAs were assessed at concentrations between 5 and 15%, as well as in combination with dimethyl sulfoxide (DMSO) and other non-penetrating CPAs. Two freezing techniques were employed: rapid freezing and controlled-rate freezing. Breviolum sp. was successfully cryopreserved using 15% DMSO. Despite exploring different CPAs and optimizing the freezing techniques, we were unable to successfully cryopreserve V. rugosum and A. pacificum. For Breviolum sp. there was higher cell viability (45.4 +/- 2.2%) when using the controlled-rate freezing compared to the rapid freezing technique (10.0 +/- 2.8%). This optimized cryopreservation protocol will be of benefit for the cryopreservation of other species from the family Symbiodiniaceae.	[Kihika, Joseph Kanyi; Wood, Susanna A.; Rhodes, Lesley; Smith, Kirsty F.; Thompson, Lucy; Challenger, Sarah] Cawthron Inst, Private Bag 2, Nelson 7042, New Zealand; [Kihika, Joseph Kanyi; Ryan, Ken G.] Victoria Univ Wellington, Sch Biol Sci, POB 600, Wellington 6140, New Zealand; [Smith, Kirsty F.] Univ Auckland, Sch Biol Sci, Private Bag 92019, Auckland 1142, New Zealand	Cawthron Institute; Victoria University Wellington; University of Auckland	Kihika, JK (通讯作者)，Cawthron Inst, Private Bag 2, Nelson 7042, New Zealand.; Kihika, JK (通讯作者)，Victoria Univ Wellington, Sch Biol Sci, POB 600, Wellington 6140, New Zealand.	joseph.kihika@vuw.ac.nz	Kihika, Joseph/LZF-7151-2025	kihika, Joseph/0000-0002-4855-8826; Kihika, Joseph Kanyi/0000-0001-6805-5890; Wood, Susanna/0000-0003-1976-8266	New Zealand Ministry of Business, Innovation and Employment [CAWX0902]; Cawthron Institute Internal Capability Investment Fund scholarship; New Zealand Ministry of Business, Innovation & Employment (MBIE) [CAWX0902] Funding Source: New Zealand Ministry of Business, Innovation & Employment (MBIE)	New Zealand Ministry of Business, Innovation and Employment(New Zealand Ministry of Business, Innovation and Employment (MBIE)); Cawthron Institute Internal Capability Investment Fund scholarship; New Zealand Ministry of Business, Innovation & Employment (MBIE)(New Zealand Ministry of Business, Innovation and Employment (MBIE))	This research was supported by funding from the New Zealand Ministry of Business, Innovation and Employment, Contract number: CAWX0902 and a Cawthron Institute Internal Capability Investment Fund scholarship.	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J	Dhifallah, F; Rochon, A; Simard, N; McKindsey, CW; Gosselin, M; Howland, KL				Dhifallah, F.; Rochon, A.; Simard, N.; McKindsey, C. W.; Gosselin, M.; Howland, K. L.			Dinoflagellate communities in high-risk Canadian Arctic ports	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Dinoflagellates; Canadian arctic; Ballast water; Non-indigenous species; Toxic species	BALLAST WATER EXCHANGE; HARMFUL ALGAL BLOOMS; DINOPHYSIS-ACUMINATA; CERATIUM-FURCA; SEA-ICE; CYST ASSEMBLAGES; SPATIAL-PATTERNS; CLIMATE-CHANGE; HUDSON-BAY; SAGAMI BAY	The expected increase of shipping activities in the Canadian Arctic is predicted to enhance potential introductions of non-indigenous species (NIS), including dinoflagellate taxa, which may have important ecological and economic impacts once released in a new environment. The lack of information about native species represents an obstacle in detecting the arrival of NIS. In this context, the present study characterizes dinoflagellate communities in high-risk Canadian Arctic ports to provide baseline data and to verify the presence of potential NIS and harmful taxa. In total, we identified 49 dinoflagellate taxa from 9 families in the ports of Churchill, Deception Bay, Iqaluit and Milne Inlet, including 7 taxa known to be potential toxin producers. Dinoflagellate communities differed significantly between ports and among time periods in the heavily used ports, those of Churchill (between 2007 and 2015) and Iqaluit (between 2015 and 2019). Comparisons between dinoflagellate communities in the ports and those in ballast water showed that 12 taxa found in ballast water of vessels discharging in Churchill and Deception Bay are potential NIS, confirming the introduction of new species by shipping activities. This may be exacerbated in the near future as a result of extended/prolonged ice-free conditions due to global warming.	[Dhifallah, F.; Rochon, A.; Gosselin, M.] Univ Quebec Rimouski, Inst Sci Mer Rimouski, Rimouski, PQ, Canada; [Simard, N.; McKindsey, C. W.] Inst Maurice Lamontagne Peches & Oceans Canada, Mont Joli, PQ, Canada; [Howland, K. L.] Fisheries & Ocean Canada, Freshwater Inst, Arctic & Aquat Div, Winnipeg, MB, Canada	University of Quebec; Universite du Quebec a Rimouski; Fisheries & Oceans Canada; Fisheries & Oceans Canada	Dhifallah, F (通讯作者)，Univ Quebec Rimouski, Inst Sci Mer Rimouski, Rimouski, PQ, Canada.	Fatma_dhifallah@uqar.ca	McKindsey, Chris/AAH-6773-2020; Gosselin, Michel/B-4477-2014	Gosselin, Michel/0000-0002-1044-0793; Dhifallah, Fatma/0000-0002-2835-2070	Polar Knowledge Canada; Nunavik Marine Region Wildlife Board; Nunavut Wildlife Management Board; Fisheries and Oceans Canada (DFO) (AIS Monitoring Ocean Protection Plan, Strategic Program for Ecosystem-based Research and Advice, and Arctic Science Program Funds); Natural Resources Canada	Polar Knowledge Canada; Nunavik Marine Region Wildlife Board; Nunavut Wildlife Management Board; Fisheries and Oceans Canada (DFO) (AIS Monitoring Ocean Protection Plan, Strategic Program for Ecosystem-based Research and Advice, and Arctic Science Program Funds); Natural Resources Canada(Natural Resources CanadaCanadian Forest Service)	This work was supported by Polar Knowledge Canada, Nunavik Marine Region Wildlife Board, Nunavut Wildlife Management Board, Fisheries and Oceans Canada (DFO) (AIS Monitoring Ocean Protection Plan, Strategic Program for Ecosystem-based Research and Advice, and Arctic Science Program Funds) and Natural Resources Canada (Polar Continental and Shelf Program logistic support) to K. Howland, and DFO Ocean Protection Plan and Ocean and Freshwater Science Contribution Program, Natural Sciences and Engineering Research Council of Canada and Fonds de recherche du Quebec -Nature et technologies through Quebec-Ocean to M. Gosselin and A. Rochon. We wish to thank Baffinland and Raglan mines staff and FedNav ship crews for their logistics support. We are grateful to local community members, DFO and university collaborators who participated in sampling; Heather Clark, Colin Gallagher, and Christie Morrison who helped with fieldwork preparation and data/sample management; and O. Lacasse and S. Lessard for their help in the identification of dinoflagellates and ballast water samples; and A. Caron for his advice in statistics. We thank M.N Bourassa and P. Guillot for processing CTD data. This paper benefited from constructive comments from G. Winkler, C. Lovejoy, and the anonymous referees. This is a contribution to the research programs of the Institut des sciences de la mer de Rimouski, Quebec-Ocean, and DFO Arctic Science.	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Coast. Shelf Sci.	MAR 5	2022	266								107731	10.1016/j.ecss.2021.107731	http://dx.doi.org/10.1016/j.ecss.2021.107731		JAN 2022	16	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	0V1ZL					2025-03-11	WOS:000788143400004
J	Hao, XD; Li, LX; Ouyang, XH; Qin, LJ; Jiang, XY; Li, JF; Wang, F				Hao, Xiudong; Li, Lixue; Ouyang, Xuhong; Qin, Linjuan; Jiang, Xingyu; Li, Jianfen; Wang, Fu			Holocene vegetation evolution, hydrologic variability and sea-level fluctuations on the south coastal plain of Laizhou Bay, Bohai Sea, China: new evidence from pollen, freshwater algae and dinoflagellate cysts	JOURNAL OF PALEOLIMNOLOGY			English	Article						Pollen assemblage; Freshwater algae; Dinoflagellate cysts; Holocene; Laizhou Bay	ENVIRONMENTAL-CHANGE; SEDIMENTARY RECORD; THERMAL HISTORY; RIVER DELTA; CLIMATE; BASIN; RECONSTRUCTION; PLEISTOCENE; CONSTRAINTS; SUBSIDENCE	Holocene palynological evidence from the Bohai Sea coastal areas have not been sufficiently discovered. In this study, we carry out analyses using detailed palynological records of pollen, spores, freshwater algae and marine dinoflagellate cysts from Borehole X1 on the south coastal plain of Laizhou Bay, Bohai Sea, northern China. The results based on radiocarbon chronology show vegetation evolution, hydrologic variability and sea-level fluctuations during the Holocene. Abundant non-arboreal pollen (mainly, Artemisia, Chenopodiaceae and grass-type Poaceae) and small amounts of arboreal pollen (mainly Pinus and Quercus-deciduous) and fern spores were identified in this study, suggesting that coastal steppes and coniferous and broadleaved mixed forests flourished in the study area and its adjacent areas, and a cold and dry climate with less precipitation and lower sea-level than the present during the Early Holocene, ca. 9910-7440 cal. yr BP. After that, the steppe areas began to shrink, and coniferous and broadleaved mixed forest areas began to expand, indicating a relatively warm and humid climatic conditions, with more precipitation and marine transgression processes during the Mid-Holocene, ca. 7440-3650 cal. yr BP. Afterwards, relatively cool and dry climatic conditions predominated, with less precipitation. While sea-level continued to rise slowly during the Late Holocene, ca. 3650 cal. yr BP to the present, and the steppe areas shrank, the coniferous and broadleaved mixed forest areas continued to expand.	[Hao, Xiudong; Li, Lixue; Ouyang, Xuhong; Qin, Linjuan] Nanning Normal Univ, Minist Educ, Key Lab Environm Change & Resource Use Beibu Gulf, 175 Mingxiu East Rd, Nanning 530001, Peoples R China; [Hao, Xiudong; Li, Lixue; Ouyang, Xuhong; Qin, Linjuan] Guangxi Key Lab Earth Surface Proc & Intelligent, Nanning 530001, Peoples R China; [Hao, Xiudong] Guangxi Acad Sci, Guangxi Mangrove Res Ctr, Guangxi Key Lab Mangrove Conservat & Utilizat, Beihai 536000, Peoples R China; [Hao, Xiudong] Minist Nat Resources, State Ocean Adm, Key Lab Submarine Geosci, Hangzhou 310012, Peoples R China; [Hao, Xiudong] Minist Nat Resources, Inst Oceanog 2, Hangzhou 310012, Peoples R China; [Jiang, Xingyu; Li, Jianfen; Wang, Fu] China Geol Survey, Tianjin Ctr, Key Lab Muddy Coastal Geoenvironm, Tianjin 300170, Peoples R China	Nanning Normal University; Guangxi Academy of Sciences; Ministry of Natural Resources of the People's Republic of China; Ministry of Natural Resources of the People's Republic of China; Second Institute of Oceanography, Ministry of Natural Resources; China Geological Survey; Tianjin Center, China Geological Survey	Ouyang, XH (通讯作者)，Nanning Normal Univ, Minist Educ, Key Lab Environm Change & Resource Use Beibu Gulf, 175 Mingxiu East Rd, Nanning 530001, Peoples R China.; Ouyang, XH (通讯作者)，Guangxi Key Lab Earth Surface Proc & Intelligent, Nanning 530001, Peoples R China.	20170742@nnnu.edu.cn	Hao, Xiudong/AAX-6221-2020; jiang, xingyu/IXN-0087-2023		National Natural Science Foundation of China [41861020, 42001076, U20A2048]; Natural Science Foundation of Guangxi Province [2018GXNSFAA281264]; Guangxi Science and Technology Plan Project [AD19245018, AD20159025]; Open Research Fund Program of Guangxi Key Lab of Mangrove Conservation and Utilization [GKLMC-201902]; Open Foundation of Key Laboratory of Submarine Geosciences, MNR [KLSG-2006]; Open Fund of Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education [NNNU-KLOP-X1919, NNNU-KLOP-X2101]; Scientific Research Staring Foundation of Nanning Normal University [0819-2019L39]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Natural Science Foundation of Guangxi Province(National Natural Science Foundation of Guangxi Province); Guangxi Science and Technology Plan Project; Open Research Fund Program of Guangxi Key Lab of Mangrove Conservation and Utilization; Open Foundation of Key Laboratory of Submarine Geosciences, MNR; Open Fund of Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education; Scientific Research Staring Foundation of Nanning Normal University	This research was funded by the National Natural Science Foundation of China (Nos. 41861020, 42001076, and U20A2048), Natural Science Foundation of Guangxi Province (No. 2018GXNSFAA281264), Guangxi Science and Technology Plan Project (Nos. AD19245018 and AD20159025), Open Research Fund Program of Guangxi Key Lab of Mangrove Conservation and Utilization (No. GKLMC-201902), Open Foundation of Key Laboratory of Submarine Geosciences, MNR (No. KLSG-2006), Open Fund of Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education (Nos. NNNU-KLOP-X1919 and NNNU-KLOP-X2101), and Scientific Research Staring Foundation of Nanning Normal University (No. 0819-2019L39).	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Paleolimn.	JUN	2022	68	1			SI		155	167		10.1007/s10933-021-00229-2	http://dx.doi.org/10.1007/s10933-021-00229-2		JAN 2022	13	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	0U6VT					2025-03-11	WOS:000739816300001
J	Pearce, MA; Jarvis, I; Monkenbusch, J; Thibault, N; Ullmann, CV; Martinez, M				Pearce, Martin A.; Jarvis, Ian; Monkenbusch, Johannes; Thibault, Nicolas; Ullmann, Clemens V.; Martinez, Mathieu			Coniacian-Campanian palynology, carbon isotopes and clay mineralogy of the Poigny borehole (Paris Basin) and its correlation in NW Europe	COMPTES RENDUS GEOSCIENCE			English	Article						Poigny borehole; Dinoflagellate cysts; Biostratigraphy; Santonian; Campanian; Carbon isotopes; Sea-level change	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CHALK; STRATIGRAPHY; CALIBRATION; EVENT; SEA; SUCCESSION; EVOLUTION; INSIGHTS; TETHYAN	The Poigny borehole near Provins (Seine-et-Marne) provides the most complete single pristine section through the Upper Cretaceous Chalk of the Paris Basin. A well preserved and diverse palynoflora including 236 species and subspecies of organic-walled dinoflagellate cysts (dinocysts) is documented from the borehole, together with a high-resolution carbon-isotope curve (delta C-13(carb)) for the Coniacian-Campanian interval. Integration of the palynological and delta C-13(carb) data provides a basis for a chemostratigraphic and biostratigraphic correlation to England and Germany. Carbon isotope events (CIEs) are used to refine the placement of sub-stage boundaries in the core, and to calibrate and correlate distinctive palynological events with those from other European sections. Thirty-three palynological events in the upper Coniacian-Campanian, judged to be of biostratigraphic significance, are described. Palynological assemblages, the peridinioid/gonyaulacoid (P/G) dinocyst ratio and clay mineralogy are compared to depositional sequences and implicate sea-level as a major driver of palaeoenvironmental change.	[Pearce, Martin A.] Evolut Appl Ltd, 33 Gainsborough Dr, Sherborne DT9 6DS, Dorset, England; [Pearce, Martin A.; Jarvis, Ian] Kingston Univ London, Dept Geog Geol & Environm, Penrhyn Rd, Kingston Upon Thames KT1 2EE, Surrey, England; [Monkenbusch, Johannes; Thibault, Nicolas] Univ Copenhagen, Dept Geosci & Nat Resource Management, DK-1350 Copenhagen C, Denmark; [Ullmann, Clemens V.] Univ Exeter, Camborne Sch Mines, Penryn Campus, Penryn TR10 9FE, Cornwall, England; [Ullmann, Clemens V.] Univ Exeter, Environm & Sustainabil Inst, Penryn Campus, Penryn TR10 9FE, Cornwall, England; [Martinez, Mathieu] Univ Rennes, UMR 6118, Geosci Rennes, CNRS, F-35000 Rennes, France	Kingston University; University of Copenhagen; University of Exeter; University of Exeter; Universite de Rennes; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Jarvis, I (通讯作者)，Kingston Univ London, Dept Geog Geol & Environm, Penrhyn Rd, Kingston Upon Thames KT1 2EE, Surrey, England.	info@evolutionapplied.com; i.jarvis@kingston.ac.uk; johannes.monkenbusch@web.de; nt@ign.ku.dk; c.ullmann@exeter.ac.uk; mathieu.martinez@univ-rennes1.fr	Ullmann, Clemens/I-3227-2019; Jarvis, Ian/A-1637-2008; Martinez, Mathieu/N-9746-2015; Thibault, Nicolas/B-1106-2013	Jarvis, Ian/0000-0003-3184-3097; Pearce, Martin/0000-0001-7856-1076; Martinez, Mathieu/0000-0003-0741-2940; Thibault, Nicolas/0000-0003-4147-5531				Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P235; AZEMA C, 1981, REV PALAEOBOT PALYNO, V35, P237, DOI 10.1016/0034-6667(81)90111-1; Blakey R., 2012, PALEOGEOGRAPHY EUROP; Blanc P, 2000, B INF GEOL BASSIN PA, V37, P87; BRUNET MF, 1982, J GEOPHYS RES, V87, P8547, DOI 10.1029/JB087iB10p08547; Burnett J.A., 1998, P132; Chenot E, 2016, PALAEOGEOGR PALAEOCL, V447, P42, DOI 10.1016/j.palaeo.2016.01.040; Chenot E, 2018, GLOBAL PLANET CHANGE, V162, P292, DOI 10.1016/j.gloplacha.2018.01.016; Cramer BD., 2020, Geologic Time Scale, V2020, P309, DOI [DOI 10.1016/B978-0-12-824360-2.00011-5, 10.1016/B978-0-12-824360-2.00011-5]; Deconinck J. 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R. Geosci.		2022	354				3		45	65		10.5802/crgeos.118	http://dx.doi.org/10.5802/crgeos.118			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	F7RN5		Green Submitted, gold			2025-03-11	WOS:000984281100004
J	Bujak, J; Bringué, M; Goryacheva, AA; Lebedeva, NK; Pestchevitskaya, EB; Riding, JB; Smelror, M				Bujak, Jonathan; Bringue, Manuel; Goryacheva, Anna A.; Lebedeva, Natalia K.; Pestchevitskaya, Ekaterina B.; Riding, James B.; Smelror, Morten			Jurassic palynoevents in the circum-Arctic region	ATLANTIC GEOLOGY			English	Article							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; HIGH-RESOLUTION STRATIGRAPHY; RAYNAUD 1978 LENTIN; NORTH-WEST SHELF; CRETACEOUS BOUNDARY; NORDVIK-PENINSULA; SVERDRUP BASIN; KEY SECTION; SIBERIA; MIDDLE	Successions of Jurassic strata located in the Arctic region normally yield rich assemblages of terrestrially-derived and marine palynomorphs, reflecting relatively warm air and sea-surface temperatures. The land plant floras were prone to the development of local communities and regional provincialism, whereas the marine biotas thrived across extensive open marine areas with high productivity, resulting in the rapid evolution of dinoflagellate cysts (dinocysts) following their earliest fossil record in the Triassic. Dinocysts exhibit low taxonomic richness and provide low biostratigraphic resolution throughout the Lower Jurassic sections. By contrast, they are diverse in Middle and Upper Jurassic strata where they provide excellent biostratigraphic markers for correlating and dating both surface and subsurface sections. Over twenty formal and informal biozonations based on the first and last occurrences of dinocysts have been erected in Alaska, Arctic Canada, the Barents Sea region, Greenland and northern Russia, many of which are correlated with macrofossils, including ammonites, that occur in the same sections. This paper presents a compilation of 214 Jurassic palynostratigraphic events (118 first occurrences and 96 last occurrences) that have regional chronostratigraphic value in the Circum-Arctic, based on their published records. Each event is correlated with the base of a chronostratigraphical unit (including formal stages and sub-Boreal ammonite zones), or as an estimated percentage above the base of the chronostratigraphical unit relative to the entire unit. The relationships of each event to stages and key fossil zonal schemes is shown on chronostratigraphic plots using the 2020 version of TimeScale Creator (R).	[Bujak, Jonathan] Bujak Res Int, 200 Queens Promenade, Blackpool FY2 9JS, Lancs, England; [Bringue, Manuel] Geol Survey Canada, 3303-3333 St NW, Calgary, AB T2L 2A7, Canada; [Goryacheva, Anna A.; Lebedeva, Natalia K.; Pestchevitskaya, Ekaterina B.] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia; [Goryacheva, Anna A.] Novosibirsk State Univ, Ul Pirogova 2, Novosibirsk 630090, Russia; [Riding, James B.] British Geol Survey, Nottingham NG12 5GG, England; [Smelror, Morten] Geol Survey Norway, Leiv Eirikssons Vei 39, N-7040 Trondheim, Norway	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Novosibirsk State University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Geological Survey of Norway	Bujak, J (通讯作者)，Bujak Res Int, 200 Queens Promenade, Blackpool FY2 9JS, Lancs, England.	jonathanbujak@outlook.com	Lebedeva, Natalia/T-6040-2017; Bringue, Manuel/KIH-8224-2024; Anna, Goryacheva/T-5116-2017		Russian Foundation for Basic Research (RFBR) [20-05-00076]; Program of Russian Fundamental Scientific Research project [0331-2019-0004]; NERC [bgs06001] Funding Source: UKRI	Russian Foundation for Basic Research (RFBR)(Russian Foundation for Basic Research (RFBR)); Program of Russian Fundamental Scientific Research project; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We are grateful to Eva Bjorseth and Bill MacMillan who helped draft the figures, to Jan Hennissen who provided advice about key events, and to Vania Correia who provided feedback on the manuscript. Special thanks to Rob Fensome for editing the paper and his advice on some of the trickier aspects of dinocyst nomenclature and taxonomy. We thank Karen Dybkjaer and Dave Shaw for their very useful feedback on the original manuscript. This paper was supported by the Russian Foundation for Basic Research (RFBR) project number 20-05-00076 and the Program of Russian Fundamental Scientific Research project number 0331-2019-0004. It is a contribution to the TransGEM Event Stratigraphy activity of the Geological Survey of Canada's Geo-Mapping for Energy and Minerals Program. James B. Riding publishes with the approval of the Chief Executive Officer, British Geological Survey (NERC).	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J	Mishra, AK; Singh, AD; Prasad, V				Mishra, Ashish K.; Singh, Arun Deo; Prasad, Vandana			Santonian-Campanian dinoflagellate cyst biostratigraphy and paleoenvironment of the Krishna-Godavari Basin, India	ISLAND ARC			English	Article						biostratigraphy; dinoflagellate cyst; Krishna-Godavari Basin; Santonian	SANTA-MARTA FORMATION; ROSS-ISLAND AREA; CAUVERY BASIN; EAST-COAST; NEW-JERSEY; STRATIGRAPHY; PIRIPAUAN; SEDIMENTS; ASSEMBLAGES; PALYNOLOGY	The present study deals with the biostratigraphic framework of Late Cretaceous sediments of the subsurface Well (DNG) "A" (2085-1840 m depth) from the Raghavapuram/Chintalapalli Shale of the Krishna-Godavari Basin and analyzed the palynological assemblage. The recorded palynological assemblage is dominated by marker dinoflagellate cyst viz. Areoligera coronata, Areoligera senonensis, Heterosphaeridium spinaconjunctum, Nelsoniella aceras, Nelsoniella semireticulata, Odontochitina porifera, Xenascus ceratioides, and Xenascus gochtii species. The last occurrence (LO) of significant species of dinoflagellate cysts is considered for the biostratigraphic establishment. On the basis of dinoflagellate cyst biostratigraphy, the examined sequences correspond to the Santonian-Campanian age. The dominance of gonyaulacoid dinoflagellate cysts is interpreted in terms of sea-level fluctuation and other paleoenvironmental signals through this biostratigraphic establishment. The recorded dinoflagellate cysts indicate the outer neritic, cool depositional environment. The sea-level rise, recorded in our study is linked with the transgressive phase during the Late Cretaceous (Santonian-Campanian) period.	[Mishra, Ashish K.; Prasad, Vandana] Birbal Sahni Inst Palaeosci, Marine Micropalaeontol Lab, Lucknow, Uttar Pradesh, India; [Singh, Arun Deo] Banaras Hindu Univ, Dept Geol, Varanasi, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Banaras Hindu University (BHU)	Mishra, AK (通讯作者)，Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow, Uttar Pradesh, India.	ashish.mishra.14111994@gmail.com	Mishra, Ashish/E-8002-2012		Ministry of Earth Science (MoES) [MoESGeo.Sci Po/36/2014]	Ministry of Earth Science (MoES)(Ministry of Earth Sciences (MoES) - India)	Ministry of Earth Science (MoES), Govt. of India, Grant/Award Number: MoESGeo.Sci. 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J	Shin, J; Kim, SM				Shin, Jisun; Kim, Soo Mee			Temporal Prediction of Paralytic Shellfish Toxins in the Mussel <i>Mytilus galloprovincialis</i> Using a LSTM Neural Network Model from Environmental Data	TOXINS			English	Article						paralytic shellfish toxins; Mytilus galloprovincialis; LSTM neural network model	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; HARMFUL ALGAL BLOOMS; HYBRID ARIMA; CHINHAE BAY; CYST	Paralytic shellfish toxins (PSTs) are produced mainly by Alexandrium catenella (formerly A. tamarense). Since 2000, the National Institute of Fisheries Science (NIFS) has been providing information on PST outbreaks in Korean coastal waters at one- or two-week intervals. However, a daily forecast is essential for immediate responses to PST outbreaks. This study aimed to predict the outbreak timing of PSTs in the mussel Mytilus galloprovincialis in Jinhae Bay and along the Geoje coast in the southern coast of the Korea Peninsula. We used a long-short-term memory (LSTM) neural network model for temporal prediction of PST outbreaks from environmental data, such as water temperature (WT), tidal height, and salinity, measured at the Geojedo, Gadeokdo, and Masan tidal stations from 2006 to 2020. We found that PST outbreaks is gradually accelerated during the three years from 2018 to 2020. Because the in-situ environmental measurements had many missing data throughout the time span, we applied LSTM for gap-filling of the environmental measurements. We trained and tested the LSTM models with different combinations of environmental factors and the ground truth timing data of PST outbreaks for 5479 days as input and output. The LSTM model trained from only WT had the highest accuracy (0.9) and lowest false-alarm rate. The LSTM-based temporal prediction model may be useful as a monitoring system of PSP outbreaks in the coastal waters of southern Korean.	[Shin, Jisun] Pusan Natl Univ, BK21 Sch Earth & Environm Syst, Busan 46241, South Korea; [Kim, Soo Mee] Korea Inst Ocean Sci & Technol KIOST, Maritime ICT R&D Ctr, Busan 49111, South Korea; [Kim, Soo Mee] Korea Maritime & Ocean Univ, Dept Convergence Study Ocean Sci & Technol, Busan 49111, South Korea	Pusan National University; Korea Institute of Ocean Science & Technology (KIOST); Korea Maritime & Ocean University	Kim, SM (通讯作者)，Korea Inst Ocean Sci & Technol KIOST, Maritime ICT R&D Ctr, Busan 49111, South Korea.; Kim, SM (通讯作者)，Korea Maritime & Ocean Univ, Dept Convergence Study Ocean Sci & Technol, Busan 49111, South Korea.	sjs1008@pusan.ac.kr; smeekim@kiost.ac.kr	Shin, Jisun/AAA-6182-2022	Kim, Soo Mee/0000-0001-8414-1297; Shin, Jisun/0000-0002-0700-1175	National Research Foundation of Korea (NRF) - Korea government (MSIT) [NRF-2021R1A2C2006682]; Ministry of Oceans and Fisheries, Korea	National Research Foundation of Korea (NRF) - Korea government (MSIT)(National Research Foundation of KoreaMinistry of Science, ICT & Future Planning, Republic of KoreaMinistry of Science & ICT (MSIT), Republic of Korea); Ministry of Oceans and Fisheries, Korea	This research was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (MSIT), grant number NRF-2021R1A2C2006682 and by the project titled "Development of Smart Processing Technology for Sea Foods", funded by the Ministry of Oceans and Fisheries, Korea.	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J	Shang, LX; Zhai, XY; Tian, W; Liu, YY; Han, YC; Deng, YY; Hu, ZX; Tang, YZ				Shang, Lixia; Zhai, Xinyu; Tian, Wen; Liu, Yuyang; Han, Yangchun; Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong			<i>Pseudocochlodinium profundisulcus</i> Resting Cysts Detected in the Ballast Tank Sediment of Ships Arriving in the Ports of China and North America and the Implications in the Species' Geographic Distribution and Possible Invasion	INTERNATIONAL JOURNAL OF ENVIRONMENTAL RESEARCH AND PUBLIC HEALTH			English	Article						biological invasion; dinoflagellate; harmful algal blooms (HABs); Pseudocochlodinium profundisulcus; resting cyst; ships' ballast tank sediment	HARMFUL ALGAL BLOOMS; COCHLODINIUM-GEMINATUM BLOOM; MULTIPLE SEQUENCE ALIGNMENT; PEARL RIVER ESTUARY; DINOFLAGELLATE CYSTS; GYMNODINIUM-CATENATUM; GENETIC-VARIATION; TERM SURVIVAL; EAST-COAST; WATER	Over the past several decades, much attention has been focused on the dispersal of aquatic nonindigenous species via ballast tanks of shipping vessels worldwide. The recently reclassified dinoflagellate Pseudocochlodinium profundisulcus (previously identified as Cochlodinium sp., Cochlodinium geminatum, or Polykrikos geminatus) was not reported in China until 2006. However, algal blooming events caused by this organism have been reported almost every year since then in the Pearl River Estuary and its adjacent areas in China. Whether P. profundisulcus is an indigenous or an invasive species has thus become an ecological question of great scientific and practical significance. In this study, we collected the sediments from ballast tanks of ships arriving in the ports of China and North America and characterized dinoflagellate resting cysts via a combined approach. We germinated two dark brownish cysts from the tank of an international ship (Vessel A) arriving at the Jiangyin Port (China) into vegetative cells and identified them as P. profundisulcus by light and scanning electron microscopy and phylogenetic analyses for partial LSU rDNA sequences. We also identified P. profundisulcus cyst from the ballast tank sediment of a ship (Vessel B) arriving in the port of North America via single-cyst PCR and cloning sequencing, which indicated that this species could be transported as resting cyst via ship. Since phylogenetic analyses based on partial LSU rDNA sequences could not differentiate all sequences among our cysts from those deposited in the NCBI database into sub-groups, all populations from China, Australia, Japan, and the original sources from which the cysts in the two vessels arrived in China and North America were carried over appeared to share a very recent common ancestor, and the species may have experienced a worldwide expansion recently. These results indicate that P. profundisulcus cysts may have been extensively transferred to many regions of the world via ships' ballast tank sediments. While our work provides an exemplary case for both the feasibility and complexity (in tracking the source) of the bio-invasion risk via the transport of live resting cysts by ship's ballast tanks, it also points out an orientation for future investigation.	[Shang, Lixia; Zhai, Xinyu; Liu, Yuyang; Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Shang, Lixia; Liu, Yuyang; Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Shang, Lixia; Liu, Yuyang; Deng, Yunyan; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China; [Tian, Wen; Han, Yangchun] Comprehens Tech Serv Ctr Jiangyin Customs, State Key Lab Ballast Water Res, Wuxi 214440, Jiangsu, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences	Hu, ZX; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Hu, ZX; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.; Hu, ZX; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao 266071, Peoples R China.	lxshang@qdio.ac.cn; zhaixinyu16@mails.ucas.edu.cn; tianwen@jytc.org.cn; liuyuyang@qdio.ac.cn; hanyangchun@jytc.org.cn; yunyandeng@qdio.ac.cn; zhu@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	Zhang, Xing/ACQ-5035-2022; ZHANG, hui jie/HTN-1690-2023; Li, Yang/KFB-5350-2024	Liu, Yuyang/0000-0003-0418-4989; Deng, Yunyan/0000-0001-5967-3611; Tang, Ying-Zhong/0000-0003-0446-3128; Hu, Zhangxi/0000-0002-4742-4973	National Natural Science Foundation of China [41976134]; Science and Technology Basic Resources Investigation Program of China [2018FY100200]; Research Projects of General Administration of Customs [2021HK157]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Science and Technology Basic Resources Investigation Program of China; Research Projects of General Administration of Customs	This research was funded by the National Natural Science Foundation of China (grant number 41976134), the Science and Technology Basic Resources Investigation Program of China (grant number 2018FY100200), and Research Projects of General Administration of Customs (grant number 2021HK157).	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J	Choudhury, TR; Banerjee, S; Khanolkar, S; Meena, SS				Choudhury, Tathagata Roy; Banerjee, Santanu; Khanolkar, Sonal; Meena, Sher Singh			Paleoenvironmental Conditions during the Paleocene-Eocene Transition Imprinted within the Glauconitic Giral Member of the Barmer Basin, India	MINERALS			English	Article						glauconite; lignite; authigenic mineral formation; PETM; Barmer Basin; shallow marine; iron sequestration	AKLI FORMATION; WESTERN KUTCH; LIGNITE MINE; DINOFLAGELLATE CYSTS; NAREDI FORMATION; RAJASTHAN; FE; MOSSBAUER; OLIGOCENE; SEDIMENTS	The roughly 6 m thick limestone-green shale alternation within the lignite-bearing Giral Member of the Barmer Basin corresponds to a marine flooding event immediately after the Paleocene-Eocene transition. A detailed characterization of the glauconite using Electron Probe Micro Analyzer (EPMA), X-Ray Diffraction (XRD), Mossbauer and Field Emission Gun-Scanning Electron Microscope (FEG-SEM) reveals its origin in the backdrop of prevailing warm climatic conditions. The glauconite pellets vary from fine silt-sized to coarse sand-sized pellets, often reaching ~60% of the rock by volume. Mineralogical investigation reveals a 'nascent' to 'slightly evolved' character of the marginal marine-originated glauconite showing considerable interstratification. The chemical composition of the glauconite is unusual with a high Al2O3 (>10 wt%) and moderately high Fe2O3(total) contents (>15 wt%). While the K2O content of these glauconites is low, the interlayer sites are atypically rich in Na2O, frequently occupying ~33% of the total interlayer sites. The Mossbauer spectrum indicates 10% of the total iron is in ferrous form. High tetrahedral Al3+ of these glauconites suggests a high-alumina substrate that transformed to glauconite by octahedral Al-for-Fe substitution followed by the addition of K into the interlayer structure. The unusually high Na2O suggests the possibility of a soda-rich pore water formed by the dissolution of alkaline volcanic minerals. The Giral glauconite formation could have been a part of the major contributors in the Fe-sequestration cycle in the Early Eocene shelves. Warm climate during the Early Eocene time favored the glauconitization because of the enhanced supply of Fe, Al, and Si and proliferation of an oxygen-depleted depositional environment.	[Choudhury, Tathagata Roy; Banerjee, Santanu] Indian Inst Technol, Dept Earth Sci, Mumbai 400076, Maharashtra, India; [Khanolkar, Sonal] Max Planck Inst Chem, Dept Climate Geochem, D-55128 Mainz, Germany; [Meena, Sher Singh] Bhabha Atom Res Ctr, Solid State Phys Div, Mumbai 400085, Maharashtra, India	Indian Institute of Technology System (IIT System); Indian Institute of Technology (IIT) - Bombay; Max Planck Society; Bhabha Atomic Research Center (BARC)	Banerjee, S (通讯作者)，Indian Inst Technol, Dept Earth Sci, Mumbai 400076, Maharashtra, India.	tathagata_rc@iitb.ac.in; sonal.k.12@gmail.com; sonal.k.12@gmail.com; ssingh@barc.gov.in	Banerjee, Santanu/H-4617-2018; Meena, Sher Singh/J-9179-2016	Meena, Sher Singh/0000-0003-4978-2528; Banerjee, Santanu/0000-0002-9548-7047; Roy Choudhury, Tathagata/0000-0002-9842-9061; Khanolkar, Sonal/0000-0002-7911-1699	FundingCouncil of Scientific and Industrial Research (CSIR); Department of Science and Technology (DST), India [INT/RUS/RFBR/390]	FundingCouncil of Scientific and Industrial Research (CSIR); Department of Science and Technology (DST), India(Department of Science & Technology (India))	FundingCouncil of Scientific and Industrial Research (CSIR) provided the fund to T.R.C. for research work. Department of Science and Technology (DST), India provided grant (INT/RUS/RFBR/390) to S.B. for analysis related to this research.	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J	Niechwedowicz, M; Walaszczyk, I				Niechwedowicz, Mariusz; Walaszczyk, Ireneusz			Dinoflagellate cysts of the upper Campanian-basal Maastrichtian (Upper Cretaceous) of the Middle Vistula River section (central Poland): stratigraphic succession, correlation potential and taxonomy	NEWSLETTERS ON STRATIGRAPHY			English	Article						Key words; Dinoflagellate cysts; taxonomy; biostratigraphy; Campanian-Maastrichtian boundary; Middle Vistula River section; central Poland	NORTHERN APENNINES; BIOSTRATIGRAPHY; ZONATION; BOUNDARY; BOREHOLE; NANNOFOSSILS; INOCERAMIDS; DEPOSITS; BELGIUM; MARGIN	A dinoflagellate cyst biostratigraphy for the upper Campanian-basal Maastrichtian (Upper Cretaceous) of the Middle Vistula River section, central Poland, is developed. Two zones, subdivided further into subzones, are proposed. The zonal boundary interval corresponds to a pronounced latest Campanian turnover within the dinoflagellate cyst assemblages. The chronostratigraphic distribution of particular dinoflagellate cyst events, or groups of events, used to define particular zones/subzones in the Middle Vistula River section is shown to correspond well to those in other regions of Europe - including the Campanian-Maastrichtian boundary stratotype section - and beyond. Apart from dinoflagellate cyst events previously recognized as significant for the definition of the Campanian-Maastrichtian boundary (i. e., the last occurrences of Raetiaedinium evittigratia, R. truncigerum, Samlandia carnarvonensis, and S. mayi), the importance of some other events, such as the last occurrences of Apteodinium deflandrei, Areoligera jeantii, and Xenascus spp., and the first occurrences of Cladopyxidium saeptum, C. velatum, C. verrrucosum, Glaphyrocysta expansa, Florentinia mayi, Pervosphaeridium tubuloaculeatum, and Riculacysta? pala, is ascertained. This study expands the knowledge of dinoflagellate cyst distribution in the Campanian-Maastrichtian boundary interval, and contributes to a better understanding of the correlations between the Boreal and Tethyan Realms during this timeframe. The presented results confirm the high potential of dinoflagellate cysts for biostratigraphic correlations on a regional and global scale - at least in the Campanian-Maastrichtian boundary interval. The systematic palaeontology of selected taxa, critical for biostratigraphy in the Campanian-Maastrichtian boundary interval, is provided. Two species (Callaiosphaeridium bicoronatum sp. nov., and Samlandia paucitabulata sp. nov.) are newly described.	[Niechwedowicz, Mariusz; Walaszczyk, Ireneusz] Univ Warsaw, Fac Geol, Ul Zwirki & Wigury 93, PL-02089 Warsaw, Poland	University of Warsaw	Niechwedowicz, M (通讯作者)，Univ Warsaw, Fac Geol, Ul Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	niechwedowicz.m@uw.edu.pl	Niechwedowicz, Mariusz/LJL-9003-2024; Walaszczyk, Ireneusz/ABE-7229-2021					ABDEL-GAWAD G I, 1986, Acta Geologica Polonica, V36, P69; Aleksandrova GN, 2008, STRATIGR GEO CORREL+, V16, P295, DOI 10.1134/S0869593808030052; Aleksandrova GN, 2012, STRATIGR GEO CORREL+, V20, P426, DOI 10.1134/S0869593812050024; ALVAREZ W, 1977, GEOL SOC AM BULL, V88, P383, DOI 10.1130/0016-7606(1977)88<383:UCMSAG>2.0.CO;2; [Anonymous], 1996, GRONLANDS GEOLOGISKE; [Anonymous], 1997, ANN SOC GEOLOGIQUE B; [Anonymous], 1995, THESIS U GENT GENT; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P235; Aurisano R.W., 1989, Palynology, V13, P143; BINT A N, 1986, Palynology, V10, P135; Blaszkiewicz A., 1980, PRACE INSTTYTUTU GEO, V92, P1; Bojanowski MJ, 2017, PALAEOGEOGR PALAEOCL, V465, P193, DOI 10.1016/j.palaeo.2016.10.032; 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]; BURNETT JA, 1992, NEWSL STRATIGR, V27, P157; Chen YY, 2013, PALYNOLOGY, V37, P259, DOI 10.1080/01916122.2013.782367; Christensen Walter Kegel, 1995, Special Papers in Palaeontology, V51, P1; Christensen Walter Kegel, 1999, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V69, P97; COOKSON I C, 1968, Journal of the Royal Society of Western Australia, V51, P110; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; Costa L.I., 1992, P99; Davey R.J., 1978, INIT REPS DSDP, V40, P883, DOI [10.2973/dsdp.proc.40.125.1978, DOI 10.2973/DSDP.PROC.40.125.1978]; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; Downie C., 1971, Geoscience Man, V3, P29; Dubicka Z, 2012, CRETACEOUS RES, V37, P272, DOI 10.1016/j.cretres.2012.04.009; Fensome R.A., 1993, CLASSIFICATION FOSSI; Fensome RA., 2019, AM ASS STRATIGRAPHIC, V50, P1173; Fensome RA, 2019, PALYNOLOGY, V43, P1, DOI 10.1080/01916122.2019.1596391; Fensome Robert A., 2016, Geological Survey of Denmark and Greenland Bulletin, V36, P1; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; FIRTH J V, 1987, Palynology, V11, P199; Foucher J.-C., 1979, Palaeontographica Abteilung B Palaeophytologie, V169, P78; GAZDZICKA E, 1978, Acta Geologica Polonica, V28, P335; González F, 2012, MAR MICROPALEONTOL, V96-97, P63, DOI 10.1016/j.marmicro.2012.08.005; Gorka H., 1983, Acta Palaeontologica Polonica, V27, P45; GuErka, 1963, ACTA PALAENTOL POL, V8, P3; HABIB D, 1989, PALAEOGEOGR PALAEOCL, V74, P23, DOI 10.1016/0031-0182(89)90018-7; HARKER S D, 1990, Palaeontographica Abteilung B Palaeophytologie, V219, P1; HARLAND R, 1977, Palaeontology (Oxford), V20, P179; Heine C.J., 1991, Micropaleontology Special Publication, V5, P117; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Hoek RP, 1996, MICROPALEONTOLOGY, V42, P125, DOI 10.2307/1485866; Houlik C.W. 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Stratigr.	JAN	2022	55	1					21	67		10.1127/nos/2021/0639	http://dx.doi.org/10.1127/nos/2021/0639			47	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	YD3SW					2025-03-11	WOS:000740337200001
J	De Freitas, AD; Barreto, CF; Silva, RCDE; Dias, GTD; Neto, JAB				de Freitas, Alex da Silva; Barreto, Cintia Ferreira; de Oliveira E Silva, Rafael Cuellar; de Macedo Dias, Gilberto Tavares; Baptista Neto, Jose Antonio			Mid- to Late Holocene (5200-980 cal YR BP) paleoenvironmental dynamics in the Ilha Grande, Brazil, assessed by terrestrial and marine microfossils	PALYNOLOGY			English	Article						charcoal fragments; C-14; dinocysts; pollen grains; Ilha Grande; sea-level	RIO-DE-JANEIRO; NON-POLLEN PALYNOMORPHS; SEA-LEVEL CHANGES; LATE QUATERNARY; GUANABARA BAY; PRIMARY PRODUCTIVITY; SOUTHEASTERN BRAZIL; BIOLOGICAL-RESERVE; FIRE HISTORY; COAST	Ilha Grande is a Brazilian island that has a high vegetal biodiversity with a well-documented prehistoric human occupation but has few paleoenvironmental studies developed in this area. In view of this, multiproxy analysis of lagoonal sediments including radiocarbon dating were carried out on a 139 cm-long continental sediment core. The aim of our study was to recognise and explain environmental dynamics in this region during the Holocene (similar to 5200 cal yr BP). The palynomorphs indicate the continuous presence of Atlantic Forest under humid conditions during the last Holocene sea-level highstand, after 5200 cal yr BP. A phase of low palynomorph concentrations was followed by a marked increase in palynomorph accumulation and diversity which may be linked to the subsequent drop of the sea-level. Dinoflagellate cysts showed a higher accumulation at the base of the sediment core. The high accumulation of charcoal particles identified between approximately 3700 and 3000 cal years BP might indicate human activity related to the long-lasting bonfires kept burning by the inhabitants of the archaeological site of Ilhote do Leste.	[de Freitas, Alex da Silva; Barreto, Cintia Ferreira; de Oliveira E Silva, Rafael Cuellar; de Macedo Dias, Gilberto Tavares; Baptista Neto, Jose Antonio] Univ Fed Fluminense, Inst Geociencias, Dept Geol, BR-24210346 Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense	De Freitas, AD (通讯作者)，Univ Fed Fluminense, Inst Geociencias, Dept Geol, BR-24210346 Rio De Janeiro, RJ, Brazil.	alexsilfre@gmail.com	de Freitas, Alex/IUQ-2116-2023; De Macedo Dias, Gilberto/AAM-3350-2021; Neto, José/AAL-2773-2021; Silva, Rafael/HPG-7311-2023	Silva, Rafael/0000-0002-0079-1661; Baptista Neto, Jose Antonio/0000-0002-3638-4435	Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)	Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was sponsored by the Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ), the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) and CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior). The authors are thankful to Instituto Estadual do Ambiente (INEA), for the research licence granted and for the support to the field work.	Abrmoff M. 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J	Baranyi, V; Mudie, PJ; Magyar, I; Kovács, A; Süto-Szentai, M; Bakrac, K				Baranyi, Viktoria; Mudie, Peta J.; Magyar, Imre; Kovacs, Adam; Suto-Szentai, Maria; Bakrac, Koraljka			Revision of the endemic dinoflagellate cyst genus <i>Pontiadinium</i> Stover & Evitt, 1978 from Lake Pannon and the Paratethys realm (Late Miocene-Early Pliocene, Central Europe)	PALYNOLOGY			English	Article						brackish-water; lacustrine; dinoflagellate cysts; Pontiadinium; endemism; Paratethys; Ponto-Caspian; Neogene	GALEACYSTA-ETRUSCA; THECA RELATIONSHIP; GONYAULAX-BALTICA; CASPIAN SEA; BLACK-SEA; LAGO MARE; BASIN; SALINITY; MORPHOLOGY; EVOLUTION	The biota of the brackish-water Lake Pannon in the Pannonian Basin is characterised by remarkable endemism due to the isolated evolution of the lake for 8 myr after the last Miocene marine connection ceased (similar to 11.6Ma). A conspicuous feature of this endemism is the large, probably ecophenotypic variation in the morphology of brackish-water dinoflagellate cysts that challenges taxonomy and complicates biostratigraphical and ecological interpretations. We conclude that a widely debated Lake Pannon genus, Pontiadinium, includes several proximate dinoflagellate cyst species with prominent apical and antapical protuberances, and we show how the genus differs from the morphologically similar gonyaulacacean cyst genera Impagidinium, Leptodinium, Cribroperidinium and Komewuia. The generic description of Pontiadinium is emended together with the species descriptions of Pontiadinium inequicornutum, Pontiadinium obesum and Pontiadinium pecsvaradanesis. A new species is described as Pontiadinium szentaiae sp. nov. from Nasice (northern Croatia) that is characterised by unique trabeculate sutural septa formed from a beaded tegillum supported by columellae or rod-like luxuriae. The dinoflagellate cyst assemblages of the long-lived brackish-water Lake Pannon clearly demonstrate that dinoflagellate cysts in low-salinity, isolated epicontinental seas display greater morphological plasticity than their normal-marine relatives. The development of an antapical horn appears to be a previously undocumented example of phenotypic morphological features that developed in response to subnormal salinities within at least two dinoflagellate cyst genera endemic to Lake Pannon and the Post-Paratethyan seas of the Ponto-Caspian realm. This ecophenotypic variation resulted in a higher level of morphological adaptation, leading to the evolutionary development of new dinoflagellate cyst species and genera.	[Baranyi, Viktoria; Bakrac, Koraljka] Croatian Geol Survey, Dept Geol, Sachsova 2, Zagreb 10000, Croatia; [Mudie, Peta J.] Geol Survey Canada Atlantic, Dartmouth, NS, Canada; [Magyar, Imre] MOL Hungarian Oil & Gas Plc, Budapest, Hungary; [Magyar, Imre] MTA MTM ELTE Res Grp Palaeontol, Budapest, Hungary; [Kovacs, Adam] Eotvos Lorand Univ, Dept Geol, Budapest, Hungary; [Suto-Szentai, Maria] Lab Deep Well Drilling Co, Komlo, Hungary	Croatian Geological Survey; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Eotvos Lorand University	Baranyi, V (通讯作者)，Croatian Geol Survey, Dept Geol, Sachsova 2, Zagreb 10000, Croatia.	vbaranyi@hgi-cgs.hr	Baranyi, Viktoria/HSI-1752-2023; Bakrac, Koraljka/G-1085-2012	Baranyi, Viktoria/0000-0002-1194-9903; Bakrac, Koraljka/0000-0002-2520-411X	Croatian Geological Survey - Croatian Ministry of Science and Education; Hungarian National Research, Development and Innovation Office [NKFIH-116618]; Hungarian-Croatian bilateral project 'Stratigraphy and correlation of Upper Miocene-Pliocene sediments along the Croatian-Hungarian border' [TET_16-1-2016-0004]	Croatian Geological Survey - Croatian Ministry of Science and Education; Hungarian National Research, Development and Innovation Office(National Research, Development & Innovation Office (NRDIO) - Hungary); Hungarian-Croatian bilateral project 'Stratigraphy and correlation of Upper Miocene-Pliocene sediments along the Croatian-Hungarian border'	This work was supported by the Croatian Geological Survey through programme funding provided by the Croatian Ministry of Science and Education; the Hungarian-Croatian bilateral project 'Stratigraphy and correlation of Upper Miocene-Pliocene sediments along the Croatian-Hungarian border' [under grant number TET_16-1-2016-0004]; and the Hungarian National Research, Development and Innovation Office [under grant number NKFIH-116618]. This is MTA-MTM-ELTE Paleo contribution 357.	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J	Bielsa, GB; Berasategui, AA; Dutto, MS; Uibrig, R; Hoffmeyer, MS				Bielsa, G. Barnech; Berasategui, A. A.; Dutto, M. S.; Uibrig, R.; Hoffmeyer, M. S.			The effect of untreated sewage discharge in food availability, egg production, and female survival of the copepod <i>Acartia tonsa</i> in a southwestern Atlantic estuary	REGIONAL STUDIES IN MARINE SCIENCE			English	Article						Natural food; Sewage pollution; Copepods; Acartia tonsa plasticity; Bahia Blanca Estuary	BAHIA-BLANCA ESTUARY; REPRODUCTIVE TOXICITY; DINOFLAGELLATE CYSTS; TEMPORAL VARIATIONS; EUTROPHIC ESTUARY; VITAL-RATES; DIET; QUALITY; MESOZOOPLANKTON; MICROPLANKTON	Estuarine copepods are considered ecological relevant components in the marine trophic webs and have high phenotypic plasticity and adaptability to face the environmental variations coastal marine ecosystems typically show. This work aims to assess the Acartia tonsa food availability, egg production, and female survival in an urban-industrial sewage discharge site (Canal Vieja, CV) and a non-disturbed site by sewage (Bahia del Medio, BM) from the Bahia Blanca Estuary, Argentina. Acartia tonsa females and microplankton samples, used as natural food, were taken during the austral warm season 2008-2009. The experimental incubations of the females were performed in a laboratory simulating the in situ environmental conditions. The microplankton showed different composition and abundance values between both studied sites. The survival of females showed significant differences between the sites, but the egg production did not show clear differences between them. A positive correlation was found among egg production, diatom, and tintinnid-ciliate abundances. A low female survival (16.5%) was observed when high ammonium concentrations (35.15 mu M) were recorded at CV. The concentration of nitrogenous nutrients, especially ammonium, along with pH and turbidity, were the drivers explaining the variation in the reproductive performance and survival of A. tonsa. Our findings further understand the reproductive performance, plasticity, and survival of key planktonic organisms in polluted coastal areas. (C) 2021 Published by Elsevier B.V.	[Bielsa, G. Barnech] Univ Nacl Comahue, Fac Ciencias & Tecnol Alimentos, Villa Regina, Argentina; [Berasategui, A. A.; Dutto, M. S.; Uibrig, R.; Hoffmeyer, M. S.] Inst Argentino Oceanog IADO CONICET UNS, Camino La Carrindanga Km 7-5, Bahia Blanca, Buenos Aires, Argentina	Universidad Nacional del Comahue	Berasategui, AA (通讯作者)，Inst Argentino Oceanog IADO CONICET UNS, Camino La Carrindanga Km 7-5, Bahia Blanca, Buenos Aires, Argentina.	aberasa@criba.edu.ar			 [FONCYT-PICT1713];  [FONCYT-PICT1795]	; 	We thank the technical and professional staff from the Instituto Argentino de Oceanografia (IADO-CONICET-UNS) for their support during the sampling period and the use of the Mastersizer Particle Analyzer. We would also thank M. Sonia Barria de Cao for her assistance in the taxonomic characterization of microplankton. This study was supported by the FONCYT-PICT1713, Argentina, FONCYT-PICT1795, Argentina.	Aguilera VM, 2013, ESTUAR COAST, V36, P1084, DOI 10.1007/s12237-013-9615-2; Baldini M. D., 1999, Revista Argentina de Microbiologia, V31, P19; Barría de Cao María Sonia, 2003, Iheringia, Sér. 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Stud. Mar. Sci.	JAN	2022	49								102139	10.1016/j.rsma.2021.102139	http://dx.doi.org/10.1016/j.rsma.2021.102139		DEC 2021	8	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	YO0FP					2025-03-11	WOS:000747624700007
J	Mahanipour, A; Mutterlose, J; Parandavar, M				Mahanipour, Azam; Mutterlose, Joerg; Parandavar, Mohammad			Integrated bio- and chemostratigraphy of the Cretaceous - Paleogene boundary interval in the Zagros Basin (Iran, central Tethys)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Calcareous nannofossils; Paleocology; K; Pg boundary; Stable isotopes; Gurpi Formation	CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; EOCENE THERMAL MAXIMUM; CARBON-ISOTOPE STRATIGRAPHY; K-T BOUNDARY; CHICXULUB IMPACT; MASS EXTINCTION; GURPI FORMATION; BRAARUDOSPHAERA-BIGELOWII; TERTIARY BOUNDARY; DEZFUL EMBAYMENT	An expanded Upper Cretaceous - Lower Paleocene succession, which encompasses the Cretaceous - Paleogene boundary (K - Pg), was studied in detail from the Zagros Basin (southwest Iran, central Tethys). In order to characterize the K - Pg transition, high resolution sampling was performed in the upper part of the Gurpi Formation. The studied interval consists of dark grey marly shales and marls with interbedded limestones. Based on calcareous nannofossils, the studied section is attributed to calcareous nannofossil zones CC26b to NP3 (latest Maastrichtian - early Paleogene). High relative abundances of the nannofossil species Micula staurophora (= Micula decussata) in the Maastrichtian part (CC26) might delineate cool surface water conditions, which are followed by an increase in abundance of Micula murus about 2 m below the K - Pg boundary. Reworked Cretaceous taxa were found at the K - Pg boundary and in the overlying Danian (NP 1-3). These findings hamper a reliable determination of the last occurrence of Cretaceous calcareous nannofossil taxa at the K - Pg boundary. The K - Pg boundary is located in the uppermost part of a positive carbon isotope excursion. Diversity and absolute abundances of calcareous nannofossils show a significant decrease at the K - Pg boundary. A bloom of the dinoflagellate cyst Cervisiella operculata (formerly Thoracosphaera operculata), which is indicating environmental stress, is recorded slightly below the boundary. Throughout the lowermost Danian (NP1), the assemblages are dominated by a bloom of small species like Neobiscutum romeinii, Neobiscutum parvulum, Futyania petalosa and small Cruciplacolithus primus. These taxa indicate stressful, and eutrophic surface water conditions throughout the initial recovery phase. The Dan-C2 and Lower C29n events, recorded in the lower Danian NP1 and lower NP2 biozones, are marked by negative carbon isotope excursions. High relative abundances of Prinsius dimorphosus followed by a Coccolithus pelagicus bloom in the full recovery phase (middle Danian, NP 3), are attributed to a short term cooling phase followed by warm surface water environments recorded along with the highest absolute abundance of calcareous nannofossils.	[Mahanipour, Azam] Shahid Bahonar Univ Kerman, Fac Sci, Dept Geol, Kerman, Iran; [Mutterlose, Joerg] Ruhr Univ Bochum, Dept Geol Mineral & Geophys, Univ Str 150, D-44801 Bochum, Germany; [Parandavar, Mohammad] Explorat Directorate, Dept Geol & Geochem Studies & Res, Sheikh Bahaei Sq, Tehran, Iran	Shahid Bahonar University of Kerman (SBUK); Ruhr University Bochum	Mahanipour, A (通讯作者)，Shahid Bahonar Univ Kerman, Fac Sci, Dept Geol, Kerman, Iran.	a_mahanipour@uk.ac.ir; joerg.mutterlose@rub.de	Parandavar, Mohammad/ABA-5548-2020; Mahanipour, Azam/N-5067-2017; Mutterlose, Joerg/IYJ-0031-2023	Mahanipour, Azam/0000-0001-6202-6933; Mutterlose, Joerg/0000-0003-3449-4507	National Iranian Oil Company (NIOC) [832134]	National Iranian Oil Company (NIOC)(National Iranian Oil Company (NIOC))	The authors are grateful to the National Iranian Oil Company (NIOC) for providing the samples and financial supports (Grant number 832134). Special thanks to the nannofossil laboratory of Shahid Bahonar University of Kerman for providing the laboratory facilities. We are grateful to Dr. N. Thibault and anonymous reviewer for their thoughtful reviews that greatly improved the manuscript.	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Paleoclimatol. Paleoecol.	FEB 1	2022	587								110785	10.1016/j.palaeo.2021.110785	http://dx.doi.org/10.1016/j.palaeo.2021.110785		DEC 2021	12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	XY9AE					2025-03-11	WOS:000737255400004
J	Lambert, C; Penaud, A; Poirier, C; Goubert, E				Lambert, Clement; Penaud, Aurelie; Poirier, Clement; Goubert, Evelyne			Distribution of modern dinocysts in surface sediments of southern Brittany (NW France) in relation to environmental parameters: Implications for paleoreconstructions	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Marine palynology; Taphonomic issues; Southern Brittany shelf; Paleoenvironmental reconstructions	DINOFLAGELLATE CYST ASSEMBLAGES; MARINE-SEDIMENTS; BAY; ATLANTIC; NORTH; EUTROPHICATION; PRESERVATION; HOLOCENE; EASTERN; BISCAY	Dinoflagellate cyst assemblages from 15 modern surface sediment samples of the Bay of Quiberon (Southern Brittany shelf) have been examined to assess their potential as marine bio-indicators for paleoenvironmental reconstructions in a shallow coastal environment. Some discrepancies are noted in the distribution of dinocyst taxa in the study area, and particularly regarding dinocyst concentration and diversity (26 different taxa identified in total) as well as heterotrophic taxa percentages. We suggest that the proportion of heterotrophic taxa is, in an embayment of 15 m deep in average, mainly attributed to bottom water oxygenation and sediment granulometry, both acting on species-selective degradation after dinocyst deposition. More precisely, higher heterotrophic abundances are found under lower oxic conditions and in fine grain-size sediment samples, leading to caution about their use as productivity indicators in coastal environments when these parameters are not fully addressed. The comparison of the Bay of Quiberon data with surface sediment samples and top cores from previously published data makes it possible to establish a transect of the modern dinocyst distribution from inshore to offshore areas in the northern Bay of Biscay, allowing to identify different ecological groups according to the hydrological and bathymetric contexts: i) an estuarine assemblage strongly dominated by Lingulodinium machaerophorum, ii) a proximal coastal assemblage dominated by L. machaerophorum and, to a lesser extent, Spiniferites bentodi, iii) a neritic assemblage dominated by L. machaerophorum, Spiniferites ramosus and cysts of Pentapharsodinium dalei, and iv) an oceanic group dominated by Spiniferites mirabilis and Operculodinium centrocarpum. (C) 2021 Elsevier B.V. All rights reserved.	[Lambert, Clement; Goubert, Evelyne] Univ Vannes UBS, UMR 6538, Lab Geosci Ocean LGO, F-56000 Vannes, France; [Penaud, Aurelie] Univ Brest UBO, CNRS, UMR 6538, Lab Geosci Ocean LGO, F-29280 Plouzane, France; [Poirier, Clement] Univ Normandie, UNICAEN, UNIROUEN, CNRS,M2C, F-14000 Caen, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Universite Le Havre Normandie; Universite de Caen Normandie; Universite de Rouen Normandie; Centre National de la Recherche Scientifique (CNRS)	Lambert, C (通讯作者)，Univ Vannes UBS, UMR 6538, Lab Geosci Ocean LGO, F-56000 Vannes, France.	clement.lambert@univ-ubs.fr	Lambert, Clément/ABF-5691-2020; Poirier, Clement/B-9652-2015; Penaud, Aurelie/F-2485-2011	Lambert, Clement/0000-0002-7746-8504; Poirier, Clement/0000-0002-8311-8463; Penaud, Aurelie/0000-0003-3578-4549	Conseil Regional de Bretagne	Conseil Regional de Bretagne(Region Bretagne)	The sediment sample collect as well as the environmental parameter measurements were carried out within the framework of the RISCO project (2010-2013; coord: J. Mazurie) coordinated by the 'Comite regional de la conchyliculture Bretagne Sud', labeled 'PoleMer Bretagne' and set up jointed by the 'Laboratoire Environnement Ressources' (Ifremer). RISCO projectwas funded by the 'Conseil Regional de Bretagne'. Analysis also benefited credits by a CNRS-INSU project HCOG2 'Forcages climatiques Holocene et repercussions Cotieres et Oceaniques dans le Golfe de Gascogne' (2013-2014; coord. A. Penaud) in the context of the LEFE-IMAGO research axis.	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Palynology	FEB	2022	297								104578	10.1016/j.revpalbo.2021.104578	http://dx.doi.org/10.1016/j.revpalbo.2021.104578		DEC 2021	11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	YU1TN		Green Published, Green Submitted			2025-03-11	WOS:000751832000011
J	Marschalek, JW; Zurli, L; Talarico, F; van de Flierdt, T; Vermeesch, P; Carter, A; Beny, F; Bout-Roumazeilles, ; Sangiorgi, F; Hemming, SR; Pérez, LF; Colleoni, F; Prebble, JG; van Peer, TE; Perotti, M; Shevenell, AE; Browne, ; Kulhanek, DK; Levy, R; Harwood, D; Sullivan, NB; Meyers, SR; Griffith, EM; Hillenbrand, CD; Gasson, E; Siegert, MJ; Keisling, B; Licht, KJ; Kuhn, G; Dodd, JP; Boshuis, C; De Santis, L; McKay, RM				Marschalek, J. W.; Zurli, L.; Talarico, F.; van de Flierdt, T.; Vermeesch, P.; Carter, A.; Beny, F.; Bout-Roumazeilles, V; Sangiorgi, F.; Hemming, S. R.; Perez, L. F.; Colleoni, F.; Prebble, J. G.; van Peer, T. E.; Perotti, M.; Shevenell, A. E.; Browne, I; Kulhanek, D. K.; Levy, R.; Harwood, D.; Sullivan, N. B.; Meyers, S. R.; Griffith, E. M.; Hillenbrand, C-D; Gasson, E.; Siegert, M. J.; Keisling, B.; Licht, K. J.; Kuhn, G.; Dodd, J. P.; Boshuis, C.; De Santis, L.; McKay, R. M.		IODP Expedition 374	A large West Antarctic Ice Sheet explains early Neogene sea-level amplitude	NATURE			English	Article							MARIE-BYRD-LAND; CENTRAL TRANSANTARCTIC MOUNTAINS; SOUTHERN VICTORIA LAND; WALLED DINOFLAGELLATE CYSTS; LARGE IGNEOUS PROVINCE; MAGNETIZATION LOCK-IN; U-PB GEOCHRONOLOGY; ROSS SEA; CONTINENTAL-SHELF; DETRITAL ZIRCONS	Early to Middle Miocene sea-level oscillations of approximately 40-60 m estimated from far-field records(1-3) are interpreted to reflect the loss of virtually all East Antarctic ice during peak warmth(2). This contrasts with ice-sheet model experiments suggesting most terrestrial ice in East Antarctica was retained even during the warmest intervals of the Middle Miocene(4,5). Data and model outputs can be reconciled if a large West Antarctic Ice Sheet (WAIS) existed and expanded across most of the outer continental shelf during the Early Miocene, accounting for maximum ice-sheet volumes. Here weprovide the earliest geological evidence proving large WAIS expansions occurred during the Early Miocene (similar to 17.72-17.40 Ma). Geochemical and petrographic data show glacimarine sediments recovered at International Ocean Discovery Program (IODP) Site U1521 in the central Ross Sea derive from West Antarctica, requiring the presence of a WAIS covering most of the Ross Sea continental shelf. Seismic, lithological and palynological data reveal the intermittent proximity of grounded ice to Site U1521. The erosion rate calculated from this sediment package greatly exceeds the long-term mean, implying rapid erosion of West Antarctica. This interval therefore captures akey step in the genesis of a marine-based WAIS and a tipping point in Antarctic ice-sheet evolution.	[Marschalek, J. W.; van de Flierdt, T.; Siegert, M. J.] Imperial Coll London, Dept Earth Sci & Engn, London, England; [Zurli, L.; Talarico, F.; Perotti, M.] Univ Siena, Dept Phys Earth & Environm Sci, Siena, Italy; [Vermeesch, P.; van Peer, T. E.] UCL, Dept Earth Sci, London, England; [Carter, A.] Birkbeck Univ London, Dept Earth & Planetary Sci, London, England; [Beny, F.; Bout-Roumazeilles, V] Univ Lille, ULCO, Lab Oceanol & Geosci, UMR 8187 CNRS, Villeneuve Dascq, France; [Sangiorgi, F.; Boshuis, C.] Univ Utrecht, Dept Earth Sci Marine Palynol & Paleoceanog, Utrecht, Netherlands; [Hemming, S. R.; Keisling, B.] Columbia Univ Palisades, Lamont Doherty Earth Observ, New York, NY USA; [Perez, L. F.; Hillenbrand, C-D] British Antarctic Survey, Cambridge, England; [Perez, L. F.] Geol Survey Denmark & Greenland, Dept Marine Geol, Aarhus, Denmark; [Colleoni, F.; De Santis, L.] Natl Inst Oceanog & Appl Geophys OGS, Trieste, Italy; [Prebble, J. G.; Levy, R.] GNS Sci, Lower Hutt, New Zealand; [van Peer, T. E.] Univ Southampton, Natl Oceanog Ctr Southampton, Waterfront Campus, Southampton, Hants, England; [Shevenell, A. E.; Browne, I] Univ S Florida, Coll Marine Sci, St Petersburg, FL USA; [Kulhanek, D. K.] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA; [Kulhanek, D. K.] Christian Albrechts Univ Kiel, Inst Geosci, Kiel, Germany; [Levy, R.; McKay, R. M.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Harwood, D.] Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE USA; [Sullivan, N. B.; Meyers, S. R.] Univ Wisconsin, Dept Geosci, Madison, WI USA; [Griffith, E. M.] Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA; [Gasson, E.] Univ Exeter, Ctr Geog & Environm Sci, Penryn, Cornwall, England; [Siegert, M. J.] Imperial Coll London, Grantham Inst, London, England; [Licht, K. J.] Indiana Univ Purdue Univ, Dept Earth Sci, Indianapolis, IN 46202 USA; [Kuhn, G.] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany; [Dodd, J. P.] Northern Illinois Univ, Dept Geol & Environm Geosci, De Kalb, IL 60115 USA	Imperial College London; University of Siena; University of London; University College London; University of London; Birkbeck University London; Universite de Lille; Universite du Littoral-Cote-d'Opale; Utrecht University; Columbia University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; Geological Survey Of Denmark & Greenland; Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; GNS Science - New Zealand; NERC National Oceanography Centre; University of Southampton; State University System of Florida; University of South Florida; Texas A&M University System; Texas A&M University College Station; University of Kiel; Victoria University Wellington; University of Nebraska System; University of Nebraska Lincoln; University of Wisconsin System; University of Wisconsin Madison; University System of Ohio; Ohio State University; University of Exeter; Imperial College London; Purdue University System; Purdue University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Northern Illinois University	Marschalek, JW (通讯作者)，Imperial Coll London, Dept Earth Sci & Engn, London, England.	j.marschalek18@imperial.ac.uk	Keisling, Benjamin/HDN-5682-2022; Roumazeilles, Viviane/A-8278-2008; McKay, Robert/N-2449-2015; Colleoni, Florence/JMQ-7847-2023; Siegert, Martin/M-9939-2019; Vermeesch, Pieter/IAN-8896-2023; Shevenell, Amelia/C-2757-2015; van Peer, Tim/R-8157-2016; Griffith, Elizabeth/KBB-3072-2024; Carter, Andrew/C-1371-2008; Perez, Lara/H-3572-2015; Zurli, Luca/AGQ-5087-2022	Colleoni, Florence/0000-0003-4582-812X; McKay, Robert/0000-0002-5602-6985; Licht, Kathy/0000-0002-2233-2853; Meyers, Stephen/0000-0003-4422-720X; van de Flierdt, Tina/0000-0001-7176-9755; Vermeesch, Pieter/0000-0003-3404-1209; Gales, Jenny/0000-0003-4402-5800; Sangiorgi, Francesca/0000-0003-4233-6154; Carter, Andrew/0000-0002-0090-5868; Kim, Sookwan/0000-0001-9960-2295; Hemming, Sidney/0000-0001-8117-2303; Sullivan, Nicholas/0000-0003-2009-8992; Perez, Lara/0000-0002-6229-4564; Marschalek, James/0000-0003-2057-4012; Zurli, Luca/0000-0002-7669-7305; Beny, Francois/0000-0002-2322-4299; Bout-Roumazeilles, Viviane/0000-0001-6917-818X	US National Science Foundation (NSF); NERC DTP studentship [NE/L002515/1]; NERC UK IODP grant [NE/R018219/1]; Italian National Antarctic Research Program (PNRA, Programma Nazionale Ricerche in Antartide) [PNRA18-00233, PNRA16-00016, PNRA18-00002]; Royal Society Te Aparangi Marsden Fund [18-VUW-089]; New Zealand Ministry for Business Innovation and Employment grant [ANTA1801]; NERC Standard Grant [NE/T001518/1]; European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant [792773 WAMSISE]; NERC [NE/R018235/1, NE/T012285/1]; IODP JOIDES Resolution Science Operator; National Science Foundation [OCE-1326927, OPP-2000995, OPP-1643713]; US Science Support Program; Grants-in-Aid for Scientific Research [20H00626] Funding Source: KAKEN; New Zealand Ministry of Business, Innovation & Employment (MBIE) [ANTA1801] Funding Source: New Zealand Ministry of Business, Innovation & Employment (MBIE); NERC [NE/R018189/1, NE/T012285/1, NE/R018235/1, NE/T001518/1, NE/R018219/1, bas0100030] Funding Source: UKRI	US National Science Foundation (NSF)(National Science Foundation (NSF)); NERC DTP studentship(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC UK IODP grant; Italian National Antarctic Research Program (PNRA, Programma Nazionale Ricerche in Antartide); Royal Society Te Aparangi Marsden Fund(Royal Society of New Zealand); New Zealand Ministry for Business Innovation and Employment grant; NERC Standard Grant(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant(Marie Curie Actions); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); IODP JOIDES Resolution Science Operator; National Science Foundation(National Science Foundation (NSF)); US Science Support Program; 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)); New Zealand Ministry of Business, Innovation & Employment (MBIE)(New Zealand Ministry of Business, Innovation and Employment (MBIE)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research used data and samples provided by the International Ocean Discovery Program (IODP), which is sponsored by the US National Science Foundation (NSF) and participating countries under the management of Joint Oceanographic Institutions. J.W.M. was supported by a NERC DTP studentship (grant number NE/L002515/1). Neodymium and Sr isotope analysis and U-Pb dating of detrital zircons was funded through NERC UK IODP grant NE/R018219/1. Clast counts performed by L.Z., F.T. and M.P. and the participation of L.D. and F.C. was funded by the Italian National Antarctic Research Program (PNRA, Programma Nazionale Ricerche in Antartide), grant numbers PNRA18-00233, PNRA16-00016 and PNRA18-00002. R.M.M. was supported by Royal Society Te Aparangi Marsden Fund (18-VUW-089). R.M.M., J.G.P. and R.L. were supported by the New Zealand Ministry for Business Innovation and Employment grant ANTA1801. P.V. was partially funded by NERC Standard Grant NE/T001518/1. L.F.P. has been funded by the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement no. 792773 WAMSISE. T.E.v.P. has been funded by NERC grants NE/R018235/1 and NE/T012285/1. D.K.K. was supported by the IODP JOIDES Resolution Science Operator and National Science Foundation (grant numbers OCE-1326927 and OPP-2000995). A.E.S. and I.B. were supported by the US Science Support Program. Southern Transantarctic Mountain rock samples for Nd and Sr isotope analysis were provided by the Polar Rock Repository with support from the National Science Foundation, under Cooperative Agreement OPP-1643713. We thank B. Coles, K. Kreissig and P. Simoes Pereira for technical support. We also thank the numerous scientists who collected invaluable site survey data and developed the proposals and hypotheses that ultimately led to IODP Expedition 374. Expedition 374 was conducted under Antarctic Conservation Act Permit Number: ACA 2018-027 (permit holder: Bradford Clement, JRSO, IODP, TAMU, College Station, TX 77845).	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J	Castaneda-Quezada, R; Garcia-Mendoza, E; Ramirez-Mendoza, R; Helenes, J; Rivas, D; Romo-Curiel, AE; Lago-Leston, A				Castaneda-Quezada, Rigel; Garcia-Mendoza, Ernesto; Ramirez-Mendoza, Rafael; Helenes, Javier; Rivas, David; Romo-Curiel, Alfonsina E.; Lago-Leston, Asuncion			Distribution of Gymnodinium catenatum Graham cysts and its relation to harmful algae blooms in the northern Gulf of California	JOURNAL OF THE MARINE BIOLOGICAL ASSOCIATION OF THE UNITED KINGDOM			English	Article						Circulation patterns; cyst relocation; Gymnodinium catenatum; HAB; PSP; seedbeds	DINOFLAGELLATE RESTING CYSTS; ALEXANDRIUM-FUNDYENSE CYSTS; RECENT MARINE-SEDIMENTS; BAHIA-CONCEPCION; COLORADO RIVER; SPATIAL-DISTRIBUTION; SURFACE SEDIMENTS; MICRORETICULATE CYST; SEASONAL OCCURRENCE; LIFE-CYCLE	Germination of cysts serves as inoculum for the proliferation of some dinoflagellates, and cyst abundance in sediments represents crucial information to understand and possibly predict Harmful Algae Blooms (HABs). Cyst distribution is related to the physical characteristics of the sediments and the hydrodynamics (circulation) of a particular region. In the northern Gulf of California (nGC) several Gymnodinium catenatum HABs have been recorded. However, the presence of resting cysts and the effect of hydrodynamics on their distribution in the nGC have not been investigated. This study evaluated cyst abundance, distribution and their relation to local circulation in surface sediments during two periods that coincided with a non-bloom year condition (July 2016) and after a major HAB registered in the nGC that occurred in January 2017. Also, a numerical ocean model was implemented to characterize the transport and relocation of cysts and sediments in the region. Gymnodinium catenatum cysts were heterogeneously distributed with some areas of high accumulation (as high as 158 cyst g(-1), and 27% of total cyst registered). Cysts seemed to be transported in an eastward direction after deposition and accumulated in an extensive area that probably is the seedbed responsible for the initiation of HABs in the region. The nGC is a retention area of cysts (and sediments) that permit the formation of seedbeds that could be important for G. catenatum HAB development. Our results provide key information to understand G. catenatum ecology and specifically, to understand the geographic and temporal appearance of HABs in the nGC.	[Castaneda-Quezada, Rigel] Ctr Invest Cient & Educ Super Ensenada, Posgrad Ecol Marina, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Garcia-Mendoza, Ernesto; Rivas, David; Romo-Curiel, Alfonsina E.] Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Biol, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Ramirez-Mendoza, Rafael] Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Fis, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Helenes, Javier] Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico; [Lago-Leston, Asuncion] Ctr Invest Cient & Educ Super Ensenada, Dept Innovac Biomed, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Garcia-Mendoza, E (通讯作者)，Ctr Invest Cient & Educ Super Ensenada, Dept Oceanog Biol, Carr Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico.	ergarcia@cicese.mx	Rivas, David/B-3439-2017; Lago-Lestón, Asunción/AFS-1438-2022; Ramirez-Mendoza, Rafael/G-6805-2019; Helenes, Javier/J-5033-2016; Romo Curiel, Alfonsina Eugenia/F-7988-2019	Ramirez-Mendoza, Rafael/0000-0001-6349-6806; Rivas, David/0000-0002-7855-4797; Garcia-Mendoza, Ernesto/0000-0003-1738-7419; Lago-Leston, Asuncion/0000-0003-4361-7732; Helenes, Javier/0000-0002-0135-1879; Castaneda Quezada, Rigel/0000-0002-2679-9522; Romo Curiel, Alfonsina Eugenia/0000-0001-7162-1806	CONACYT scholarship [24805 CV617226]; FORDECYT - CONACYT [260040-2015]; CICESE [625118]	CONACYT scholarship(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); FORDECYT - CONACYT; CICESE	This work was funded by CONACYT scholarship 24805 CV617226; FORDECYT - CONACYT project number 260040-2015. 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Mar. Biol. Assoc. U.K.	SEP	2021	101	6					895	909	PII S0025315421000795	10.1017/S0025315421000795	http://dx.doi.org/10.1017/S0025315421000795		DEC 2021	15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	ZE6ZL					2025-03-11	WOS:000728569400001
J	Agüero, LS; Quattrocchio, ME				Aguero, Luis S.; Quattrocchio, Mirta E.			Maastrichtian-Danian palynomorphs from the Pedro Luro Formation, Ombucta 1 Borehole, Colorado Basin, Argentina	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Maastrichtian -Danian interval; Palynomorphs; Dinoflagellate cysts; Biostratigraphy; Provincialism; Palaeobiogeographic affinities; Colorado Basin; Argentina	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CRETACEOUS-PALEOGENE BOUNDARY; SEA-LEVEL CHANGES; TERTIARY BOUNDARY; CALCAREOUS NANNOFOSSIL; ENVIRONMENTAL-CHANGE; EQUATORIAL ATLANTIC; NORTHERN PATAGONIA; AUSTRAL BASIN; PALEOCENE	In this contribution, the palynomorphs of the Pedro Luro Formation, Ombucta 1 Borehole, Colorado Basin, Argentina, were recorded to perform palinostratigraphic analysis, evaluate dinoflagellate cyst provincialism, recognise trends in sea surface temperature (SST) and estimate palaeobiogeographic affinities. Sixty eight species of palynomorphs were identified and three informal biostratigraphic intervals were recognised. The first, determined by Hafniasphaera australis associated with Alterbidinium acutulum, implies that deposits below 984 mbrf would not be younger than late Maastrichtian (calcareous nannofossil biozone CC26). The second interval between 982 and 954 mbrf is assigned to the upper Maastrichtian-Danian. It is difficult to give more accuracy to the age of this interval due to the absence of species with LADs (last appearance datum) in the latest Maastrichtian and the lack of early Danian taxa. This together with the recognition of CC26 (Maastrichtian) followed by NP2-NP3 (Danian) could suggest that the K/Pg boundary is not represented. The third interval includes Senoniasphaera inornata (LAD: 62.6 Ma), suggesting an age no younger than Danian for deposits between 952 and 946 mbrf (NP2-NP3). The typical taxa of the Tropical-subtropical Province predominate (Phelodinium magnificum, Lejeunecysta spp. and Senegalinium leavigatum) followed by genera from the Warm-temperate Province (Alterbidinium acutulum, Spinidinium macmurdoense, Spinidinium styloniferum and Diconodinium lurense), suggesting changes in SST trends, from tropical-subtropical to warm-temperate conditions. The coincidences of dinoflagellate cyst species recorded between the Colorado Basin and basins of equatorial South America, the African counterpart, Brazil and Uruguay, would suggest the exchange of dinoflagellates, reflecting palaeobiogeographic affinities.	[Aguero, Luis S.; Quattrocchio, Mirta E.] Univ Nacl Sur UNS, Inst Geol Sur INGEOSUR, Dept Geol, CONICET, Av Alem 1253,Cuerpo B-1 Piso,B8000CPB, Bahia Blanca, Buenos Aires, Argentina	National University of the South; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Agüero, LS (通讯作者)，Univ Nacl Sur, Dept Geol, Av Alem 1253,Cuerpo B-2 Piso,B8000CPB, Bahia Blanca, Buenos Aires, Argentina.	luisaguero@ingeosur-conicet.gob.ar		Aguero, Luis Sebastian/0009-0003-5590-5544	Comision de Investigaciones Cientificas de la Provincia de Buenos Aires (CIC)	Comision de Investigaciones Cientificas de la Provincia de Buenos Aires (CIC)	The authors of this manuscript thank Y-Tec company for providing the samples to carry out the study. Within the team of people who conform the company, special thanks to Dr. Juan Pablo Perez Panera for his cordial treatment and predisposition. Thanks to Pedro Kress for the valuable suggestions made. This work was supported by the Comision de Investigaciones Cientificas de la Provincia de Buenos Aires (CIC) .	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South Am. Earth Sci.	JAN	2022	113								103660	10.1016/j.jsames.2021.103660	http://dx.doi.org/10.1016/j.jsames.2021.103660		DEC 2021	13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	XU6TB					2025-03-11	WOS:000734393400002
J	Pestchevitskaya, EB; Lidskaya, AV; Rostovtseva, YI				Pestchevitskaya, E. B.; Lidskaya, A., V; Rostovtseva, Yu, I			Kimmeridgian-Volgian Palynological Assemblages of the Eganovo Section (Moscow Region) and Their Possible Application for Biostratigraphy, Correlation, and Facies Analysis	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Russian Plate; Upper Jurassic; palynomorphs; biostratigraphy; correlation; biofacies	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; BOUNDARY STRATA; KEY SECTION; BASIN; STRATIGRAPHY; SIBERIA; PALEOENVIRONMENTS; PALYNOFACIES; PALEOCLIMATE; INDICATORS	The results of study of marine and terrestrial palynomorphs in the Lower Kimmeridgian and Middle-Upper Volgian in the Eganovo section (Moscow region) are presented. The section is well characterized by ammonites providing a biostratigraphic control of the palynostratons. Beds with spores and pollen are identified for the Volgian interval and beds with dinocysts are distinguished for the entire section. Certain taxa allow comparison of synchronous successions of dinocysts of the European part of Russia, Siberia, and Western Europe. By spores and pollen, a correlation is possible with coeval rocks of the northern Urals, Western Europe, and Australia. The facies analysis of two palynological groups allowed reconstruction of features of marine algoflora and their interrelation with transgressive-regressive dynamics of the paleobasin, climatic fluctuations, and change in coastal landscapes. The comparative analysis of the lateral distribution of coeval dinocyst assemblages from the Eganovo section and other Boreal regions showed a significant similarity of algoflora of European Russia, the North Sea region, and Bulgaria in the Kimmeridgian, but the lateral differentiation of algoflora increased to the end of the Volgian. At the same time, the diversity of the dinocyst assemblages in the European part of Russia remained high. It is suggested that this was caused by favorable temperature and trophic conditions, which are interpreted using the results of facies analysis of terrestrial palynomorphs. The features of their taxonomic composition are typical of the Euro-Sinian paleogeographic area with a subtropical climate. Gradual cooling in the second half of the Volgian was accompanied by recovery of small climatic maxima, which are also traced in Western Europe, Siberia and the northern Urals. No period of aridization typical of the terminal Jurassic of Western Europe was revealed. Wet conditions led to the formation of specific palynoflora with abundant gleicheniaceous ferns in the European part of Russia and adjacent territories of the Urals and margins of Western Siberia.	[Pestchevitskaya, E. B.] Russian Acad Sci, Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia; [Lidskaya, A., V] Russian Acad Sci, Geol Inst, Moscow 119017, Russia; [Rostovtseva, Yu, I] Moscow MV Lomonosov State Univ, Moscow 119991, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Lomonosov Moscow State University	Pestchevitskaya, EB (通讯作者)，Russian Acad Sci, Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia.	PeschevickayaEB@ipgg.sbras.ru			Russian Foundation for Basic Research [20-05-00076]; GIN RAS	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); GIN RAS	This work was supported by the Russian Foundation for Basic Research, project no. 20-05-00076. The work of A.V. Lidskaya was supported by state contract of GIN RAS.	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Geol. Correl.	DEC	2021	29	SUPPL 1		1			S68	S95		10.1134/S0869593822020058	http://dx.doi.org/10.1134/S0869593822020058			28	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	ZY8UO					2025-03-11	WOS:000772856400004
J	Fenizia, S; Weissflog, J; Pohnert, G				Fenizia, Simona; Weissflog, Jerrit; Pohnert, Georg			Cysteinolic Acid Is a Widely Distributed Compatible Solute of Marine Microalgae	MARINE DRUGS			English	Article						cysteinolic acid; osmoadaptation; osmoregulation; ectoine; DMSP; diatoms; phytoplankton; salinity; LC; MS analysis	SULFONIC-ACID; SULFUR; GROWTH; PHYTOPLANKTON; ACCUMULATION; WEISSFLOGII; SALINITY; LIGHT	Phytoplankton rely on bioactive zwitterionic and highly polar small metabolites with osmoregulatory properties to compensate changes in the salinity of the surrounding seawater. Dimethylsulfoniopropionate (DMSP) is a main representative of this class of metabolites. Salinity-dependent DMSP biosynthesis and turnover contribute significantly to the global sulfur cycle. Using advanced chromatographic and mass spectrometric techniques that enable the detection of highly polar metabolites, we identified cysteinolic acid as an additional widely distributed polar metabolite in phytoplankton. Cysteinolic acid belongs to the class of marine sulfonates, metabolites that are commonly produced by algae and consumed by bacteria. It was detected in all dinoflagellates, haptophytes, diatoms and prymnesiophytes that were surveyed. We quantified the metabolite in different phytoplankton taxa and revealed that the cellular content can reach even higher concentrations than the ubiquitous DMSP. The cysteinolic acid concentration in the cells of the diatom Thalassiosira weissflogii increases significantly when grown in a medium with elevated salinity. In contrast to the compatible solute ectoine, cysteinolic acid is also found in high concentrations in axenic algae, indicating biosynthesis by the algae and not the associated bacteria. Therefore, we add this metabolite to the family of highly polar metabolites with osmoregulatory characteristics produced by phytoplankton.	[Fenizia, Simona; Pohnert, Georg] Friedrich Schiller Univ Jena, Inst Inorgan & Analyt Chem, Bioorgan Analyt, Lessingstr 8, D-07743 Jena, Germany; [Fenizia, Simona; Weissflog, Jerrit; Pohnert, Georg] Max Planck Inst Chem Ecol, MPG Fellow Grp, Hans Knoll Str 8, D-07745 Jena, Germany	Friedrich Schiller University of Jena; Max Planck Society	Pohnert, G (通讯作者)，Friedrich Schiller Univ Jena, Inst Inorgan & Analyt Chem, Bioorgan Analyt, Lessingstr 8, D-07743 Jena, Germany.; Pohnert, G (通讯作者)，Max Planck Inst Chem Ecol, MPG Fellow Grp, Hans Knoll Str 8, D-07745 Jena, Germany.	simona.fenizia@uni-jena.de; jweissflog@ice.mpg.de; georg.pohnert@uni-jena.de	Fenizia, Simona/KPB-2675-2024; Pohnert, Georg/D-3721-2013	Fenizia, Simona/0000-0002-3592-9368; Pohnert, Georg/0000-0003-2351-6336	International Max Planck Research School Exploration of Ecological Interactions with Molecular Techniques; Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) [EXC 2051, 390713860]	International Max Planck Research School Exploration of Ecological Interactions with Molecular Techniques; Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)(German Research Foundation (DFG))	This research was funded by the International Max Planck Research School Exploration of Ecological Interactions with Molecular Techniques and by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) under Germany's Excellence Strategy-EXC 2051-Project-ID 390713860.	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Drugs	DEC	2021	19	12							683	10.3390/md19120683	http://dx.doi.org/10.3390/md19120683			10	Chemistry, Medicinal; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	YA2DQ	34940682	gold, Green Published			2025-03-11	WOS:000738150800001
J	Rubino, F; Belmonte, G				Rubino, Fernando; Belmonte, Genuario			Habitat Shift for Plankton: The Living Side of Benthic-Pelagic Coupling in the Mar Piccolo of Taranto (Southern Italy, Ionian Sea)	WATER			English	Article						plankton; life cycles; resting stages; cysts; benthic-pelagic coupling; resurrection ecology	LIFE-HISTORY TRAITS; DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; RESTING CYSTS; BIOTURBATION; SCRIPPSIELLA; SEDIMENTS; DIAPAUSE; EGGS; RESURRECTION	Resting stages represent the answer for species to the variability of environmental conditions. In confined marine habitats, variability of conditions is high, and bottoms host plankton resting stages in the so-called "marine cyst banks". The Mar Piccolo of Taranto was chosen as a pilot site in which to investigate how marine cyst banks and plankton affect each other in the living part of the benthic-pelagic coupling. The attempt was based on the use of multiple devices for integrated sampling of benthic and pelagic stages and allowed us to identify 207 taxa/categories in the whole system (127 as active forms, 91 as resting stages). The sediments added 80 taxa to the plankton list obtained only from the water column, thus confirming the importance of this kind of approach in perceiving the actual diversity of the studied site. The sediment cyst bank involved 0.15-1.00% of its content in daily benthic-pelagic exchanges, in terms of cyst germination and import, respectively. In addition, the cyst production, which was higher than the cyst germination, is responsible for the existence of a permanent biological reservoir in the sediments. The benthic-pelagic coupling, however, was completely depicted in the present investigation only for seven taxa. This result is due to the still scant knowledge of the life cycles and life histories of single species. Apart from the identification difficulties that still have to be clarified (which cysts belong to which species), the cycle presence/absence is also characterized by the diversification of strategies adopted by each species. The observation of plankton dynamics from the benthos point of view was useful and informative, unveiling a huge assemblage of resting forms in the sediments only minimally affected by cyst import/export, because it is more devoted to a storing role over long periods. Consequently, the continuation of life cycle studies appears necessary to understand the diversity of strategies adopted by the majority of plankton species.	[Rubino, Fernando] Natl Res Council Italy, Water Res Inst CNR IRSA, Unit Taranto, I-72100 Taranto, Italy; [Belmonte, Genuario] Univ Salento, Dipartimento Sci & Tecnol Biol & Ambientali, Lab Zoogeog & Fauna, I-73100 Lecce, Italy	Consiglio Nazionale delle Ricerche (CNR); Istituto di Ricerca sulle Acque (IRSA-CNR); University of Salento	Belmonte, G (通讯作者)，Univ Salento, Dipartimento Sci & Tecnol Biol & Ambientali, Lab Zoogeog & Fauna, I-73100 Lecce, Italy.	rubino@irsa.cnr.it; genuario.belmonte@unisalento.it	BELMONTE, GENUARIO/AAG-4029-2020; Rubino, Fernando/GOP-0332-2022	belmonte, genuario/0000-0002-7473-116X				Alabiso G, 1997, MAR CHEM, V58, P373, DOI 10.1016/S0304-4203(97)00063-7; Anderson DM, 2012, HARMFUL ALGAE, V14, P10, DOI 10.1016/j.hal.2011.10.012; ARPA Puglia, 2014, MAR PICC TAR SCI TEC, V4, P175; Belmonte G, 1995, OLSEN INT S, P53; Belmonte G, 1998, TRENDS ECOL EVOL, V13, P4, DOI 10.1016/S0169-5347(97)01234-2; Belmonte G., 2010, Metodologie di Studio del Plancton Marino, ISPRAIstituto Superiore per la Protezione e la Ricerca Ambientale, P507; Belmonte G, 2019, OCEANOGR MAR BIOL, V57, P1; Belmonte G, 2013, J MARINE SYST, V128, P222, DOI 10.1016/j.jmarsys.2013.05.007; Belmonte G, 2007, J PLANKTON RES, V29, pI39, DOI 10.1093/plankt/fbl064; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; BOERO F, 1994, MAR ECOL-P S Z N I, V15, P3, DOI 10.1111/j.1439-0485.1994.tb00038.x; Bravo Isabel, 2014, Microorganisms, V2, P11; COHEN D, 1966, J THEOR BIOL, V12, P119, DOI 10.1016/0022-5193(66)90188-3; Dale B., 1983, P69; Drillet G, 2008, AQUACULTURE, V279, P47, DOI 10.1016/j.aquaculture.2008.04.010; Ferraro L, 2017, MAR BIODIVERS, V47, P887, DOI 10.1007/s12526-016-0523-0; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; GIANGRANDE A, 1994, OCEANOGR MAR BIOL, V32, P305; Hairston N.G., 2010, PLANKTON INLAND WATE, P247; HAIRSTON NG, 1995, ECOLOGY, V76, P1706, DOI 10.2307/1940704; Ianora A, 1998, J MARINE SYST, V15, P337, DOI 10.1016/S0924-7963(97)00085-7; Ichimi K, 2001, FISHERIES SCI, V67, P1178, DOI 10.1046/j.1444-2906.2001.00378.x; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Kerfoot WC, 2004, LIMNOL OCEANOGR, V49, P1300, DOI 10.4319/lo.2004.49.4_part_2.1300; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Marcus NH, 1998, LIMNOL OCEANOGR, V43, P763, DOI 10.4319/lo.1998.43.5.0763; MARCUS NH, 1984, MAR ECOL PROG SER, V15, P47, DOI 10.3354/meps015047; Meier KJS, 2003, MAR MICROPALEONTOL, V48, P321, DOI 10.1016/S0377-8398(03)00028-8; Menu F, 2000, AM NAT, V155, P724, DOI 10.1086/303355; Montresor M., 2010, Metodologie di Studio del Plancton Marino, ISPRAIstituto Superiore per la Protezione e la Ricerca Ambientale, P271; Moscatello S, 2004, SCI MAR, V68, P85, DOI 10.3989/scimar.2004.68s185; Moscatello Salvatore, 2009, Saline Syst, V5, P3, DOI 10.1186/1746-1448-5-3; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Pastore M, 1993, MAR PICCOLO, P164; Pati A. 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J	Rodriguez-Villegas, C; Diaz, PA; Riobo, P; Rossignoli, AE; Rodriguez, F; Loures, P; Baldrich, AM; Varela, D; Sandoval-Sanhueza, A; Figueroa, RI				Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Riobo, Pilar; Rossignoli, Araceli E.; Rodriguez, Francisco; Loures, Patricia; Baldrich, Angela M.; Varela, Daniel; Sandoval-Sanhueza, Alondra; Figueroa, Rosa I.			Latitudinal Variation in the Toxicity and Sexual Compatibility of <i>Alexandrium catenella</i> Strains from Southern Chile	TOXINS			English	Article						dinoflagellate; saxitoxins; mating systems; resting cysts; PSP outbreak; Chilean Patagonia	PARALYTIC SHELLFISH TOXINS; DINOFLAGELLATE BLOOMS; LIQUID-CHROMATOGRAPHY; DINOPHYCEAE STRAINS; GENUS ALEXANDRIUM; RESTING CYSTS; DYNAMICS; PROFILE; GROWTH; VARIABILITY	The bloom-forming toxic dinoflagellate Alexandrium catenella was first detected in southern Chile (39.5-55 degrees S) 50 years ago and is responsible for most of the area's cases of paralytic shellfish poisoning (PSP). Given the complex life history of A. catenella, which includes benthic sexual cysts, in this study, we examined the potential link between latitude, toxicity, and sexual compatibility. Nine clones isolated from Chilean Patagonia were used in self- and out-crosses in all possible combinations (n = 45). The effect of latitude on toxicity, reproductive success indexes, and cyst production was also determined. Using the toxin profiles for all strains, consisting of C1, C2, GTX4, GTX1, GTX3, and NeoSTX, a latitudinal gradient was determined for their proportions (%) and content per cell (pg cell(-1)), with the more toxic strains occurring in the north (-40.6 degrees S). Reproductive success also showed a latitudinal tendency and was lower in the north. None of the self-crosses yielded resting cysts. Rather, the production of resting cysts was highest in pairings of clones separated by distances of 1000-1650 km. Our results contribute to a better understanding of PSP outbreaks in the region and demonstrate the importance of resting cysts in fueling new toxic events. They also provide additional evidence that the introduction of strains from neighboring regions is a cause for concern.	[Rodriguez-Villegas, Camilo; Baldrich, Angela M.] Univ Los Lagos, Programa Doctorado Ciencias Menc Conservac & Mane, Camino Chinquihue Km 6, Puerto Montt 5480000, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Baldrich, Angela M.; Varela, Daniel; Sandoval-Sanhueza, Alondra] Univ Los Lagos, Ctr I Mar, Puerto Montt 5480000, Chile; [Rodriguez-Villegas, Camilo; Diaz, Patricio A.; Baldrich, Angela M.] Univ Los Lagos, Ctr Biotechnol & Bioengn, Puerto Montt 5480000, Chile; [Riobo, Pilar] IIM, CSIC, Eduardo Cabello 6, Vigo 36208, Spain; [Rossignoli, Araceli E.] Ctr Invest Marinas, Pedras Coron S-N,Apartado 13, Vilanova De Arousa 36620, Spain; [Rodriguez, Francisco; Loures, Patricia; Figueroa, Rosa I.] IEO, Ctr Oceanog Vigo, CSIC, Subida Radio Faro 50, Vigo 36390, Spain	Universidad de Los Lagos; Universidad de Los Lagos; Universidad de Los Lagos; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC)	Rodriguez-Villegas, C (通讯作者)，Univ Los Lagos, Programa Doctorado Ciencias Menc Conservac & Mane, Camino Chinquihue Km 6, Puerto Montt 5480000, Chile.; Rodriguez-Villegas, C; Diaz, PA (通讯作者)，Univ Los Lagos, Ctr I Mar, Puerto Montt 5480000, Chile.; Rodriguez-Villegas, C; Diaz, PA (通讯作者)，Univ Los Lagos, Ctr Biotechnol & Bioengn, Puerto Montt 5480000, Chile.; Figueroa, RI (通讯作者)，IEO, Ctr Oceanog Vigo, CSIC, Subida Radio Faro 50, Vigo 36390, Spain.	camilo.rodriguez@ulagos.cl; patricio.diaz@ulagos.cl; pilarriobo@iim.csic.es; araceli.escudeiro.rossignoli@xunta.gal; francisco.rodriguez@ieo.es; patricia.loures@ieo.es; ambaldrich@gmail.com; dvarela@ulagos.cl; alondrasandovalsanhueza@gmail.com; francisco.rodriguez@ieo.es	Varela, Daniel/D-9484-2013; Riobo, Pilar/K-1945-2017; Escudeiro Rossignoli, Araceli/ABF-5476-2020; Diaz, Patricio/B-8128-2018; Rodriguez Villegas, Camilo/AAB-8563-2022; Baldrich, Angela M./AAC-8054-2022; Figueroa, Rosa/M-7598-2015; Rodriguez, Francisco/A-5934-2019	Sandoval-Sanhueza, Alondra/0000-0002-4889-4563; Riobo, Pilar/0000-0002-1921-6229; Escudeiro Rossignoli, Araceli/0000-0002-6052-9067; Diaz, Patricio/0000-0002-9403-8151; Rodriguez Villegas, Camilo/0000-0002-1429-2775; Baldrich, Angela M./0000-0002-2624-7357; Figueroa, Rosa/0000-0001-9944-7993; Rodriguez, Francisco/0000-0002-6918-4771	national project from the Spanish Ministry of Science and Innovation and the European Community (FEDER)	national project from the Spanish Ministry of Science and Innovation and the European Community (FEDER)	FundingThis work was funded by a national project from the Spanish Ministry of Science and Innovation and the European Community (FEDER) (Project DIANAS-CTM2017-86066-R) to RIF, a grant for Galician Networks of Excellence (GRC-VGOHAB IN607A-2019/04) from the Innovation Agency of the Xunta de Galicia (GAIN) to RIF, and supported by projects REDES170101 and REDI170575 from the International Cooperation Program of the Chilean National Research and Development Agency (ANID) to PAD.	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Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology; Toxicology	XZ0GS	34941737	Green Published, gold			2025-03-11	WOS:000737341800001
J	Singh, K; Singh, SD; Prasad, B; Whiso, K; Shefali, S				Singh, Kamla; Singh, S. D.; Prasad, B.; Whiso, K.; Shefali, S.			High Resolution Biostratigraphy of Post-Gondwana Pre-Cretaceous and Cretaceous successions from Pennar Sub-basin, Krishna-Godavari Basin, India	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						High resolution; Post-Gondwanic; synrift; Late Cretaceous; passive-margin		High resolution integrated palynostratigraphic and foraminiferal studies are undertaken on the Post- Gondwana Pre - Cretaceous and Cretaceous sediments encountered in the exploratory wells A and B drilled in the shallow offshore regions of Pennar Subbasin of Krishna-Godavari Basin. This study has been undertaken with an objective to determine precise age and depositional environment of various post-Gondwana Late Jurassic-Early Cretaceous synrift and Late Cretaceous passive-margin lithounits. The oldest Post-Gondwanic synrift sediments of Late Jurassic (Kimmeridgian - Tithonian) are recorded above the Precambrian basement in well A. The Kimmeridgian-Tithonian boundary is tentatively marked at 1650 m depth in well A and 3545 m in well B on the basis of record of LAD of age marker dinoflagellate cyst Senoniasphaera jurassica. The top of Tithonian is marked on the basis of recognition of LAD of dinoflagellate cyst Pseudoceratium weymouthense at 1420 m depth in well A and 2945 m in well B. The characteristic palynofossils of Permo - Triassic Gondwana and Lower to Middle Jurassic are not recorded, indicating the absence of complete Gondwana and major part of the Jurassic sediments from Hettangian to Oxfordian in the Pennar Subbasin. The post-Gondwana Late JurassicEarly Cretaceous synrift sediments directly rest over the Precambrian Basement. Fifteen globally established Late Jurassic to Late Cretaceous dinoflagellate cyst bio-events, ranging from Kimmeridgian-Tithonian (155-145 Ma) to Turonian-Coniacian(89-85 Ma) are recognized in the studied sequences of above two wells that helped in precisely recognizing the stratigraphic boundaries of Kimmeridgian, Tithonian, Berriasian, Valanginian, Hauterivian, Barremian, Aptian, Albian, Cenomanian, Turonian and Coniacian in the Pennar Subbasin. Four important planktonic foraminiferal events are recorded in the Aptian-Albian-Cenomanian interval of the two wells. Aptian marker planktonic foraminifera Hedbergella sigali and Globigerinelloides blowi have been recorded. Planomalina buxtorfi and Hedbergella gorbachikae have been useful in demarcating Albian. Besides, Favusella washitensis, Rotalipora gandolfi and benthic aragonitic foraminifera Epistomina sp. are useful forms in the Albian-Cenomanian transition. The recorded palynofloral assemblages indicate the presence of oldest synrift sediments of Kimmeridgian-Tithonian age of Late Jurassic in the Pennar Sub-basin, deposited under the shallow marine conditions, whereas, middle to outer shelf conditions prevailed during Early Cretaceous. The Late Cretaceous sediments are deposited under inner shelf conditions. The present record of oldest synrift sediments of Late Kimmeridgian predates the break-up time of Indian Plate from East Gondwana land.	[Singh, Kamla; Singh, S. D.; Prasad, B.; Whiso, K.; Shefali, S.] Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Geol Grp, 9 Kaulagarh Rd, Dehra Dun 248195, Uttarakhand, India	Oil & Natural Gas Corporation	Singh, K (通讯作者)，Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Geol Grp, 9 Kaulagarh Rd, Dehra Dun 248195, Uttarakhand, India.	kamla_singh@ongc.co.in						Aswal H. 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J	Vieira, M; Mahdi, S				Vieira, Manuel; Mahdi, Salih			New Late Cretaceous to earliest Paleogene (Campanian-Danian) dinoflagellate cysts from the More Basin, offshore Norway	PALYNOLOGY			English	Article						dinoflagellate cysts; Cretaceous; Paleogene; taxonomy; More Basin; biostratigraphy	NORTH-SEA; PALEOCENE; BIOSTRATIGRAPHY; ZONATION; FIELD	The Late Cretaceous and Paleogene strata of the Norwegian continental shelf are rich and diverse in dinoflagellate cysts. The assemblages are generally well-preserved, which allows high-resolution biostratigraphic studies and sometimes the identification of new species with chronostratigraphic significance. This paper proposes the formal description of eight new species from the More Basin, offshore Norway: Adnatosphaeridium tubulosum, Canningia crassimura, Canningia exilimura, Palaeohystrichophora elongata, Palaeoperidinium minusculatum, Senoniasphaera porosa, Trithyrodinium ioannidesii and Trithyrodinium verrucatum. 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 here have been recognised in a stratigraphic interval ranging from the early Campanian to the early Danian; their occurrence can be used in conjunction with previously published markers to enhance the stratigraphic breakdown of wells across the region and wider offshore Northwest Europe.	[Vieira, Manuel] Shell UK Ltd, Aberdeen, Scotland; [Vieira, Manuel] Lundin Energy Norway, Strandveien 4, N-1366 Lysaker, Norway; [Mahdi, Salih] Petrostrat Ltd, Gadbrook Business Ctr, Century House, Northwich, England	Royal Dutch Shell	Vieira, M (通讯作者)，Lundin Energy Norway, Strandveien 4, N-1366 Lysaker, Norway.	manuel.vieira@lundin-energy.com	Vieira, Manuel/AAY-4474-2020	Vieira, Manuel/0000-0002-2389-4583				Alberti G., 1959, Mitteilungen aus dem Geologischen Staatsinstitut in Hamburg, V28, P93; Alberti G., 1961, Palaeontographica, V116, P1; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BUTSCHLI O., 1885, KLASSEN ORDNUNGEN TH, P865; Clarke R. F. A., 1967, Verb K ned Akad Wet Amst, V24, P1; Cookson I. C., 1962, Micropaleontology, V8, P485, DOI 10.2307/1484681; Cookson I. C., 1961, Proceedings of the Royal Society of Victoria N S, V74, P69; Cookson I. 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J	Bijl, PK; Frieling, J; Cramwinckel, MJ; Boschman, C; Sluijs, A; Peterse, F				Bijl, Peter K.; Frieling, Joost; Cramwinckel, Margot J.; Boschman, Christine; Sluijs, Appy; Peterse, Francien			Maastrichtian-Rupelian paleoclimates in the southwest Pacific - a critical re-evaluation of biomarker paleothermometry and dinoflagellate cyst paleoecology at Ocean Drilling Program Site 1172	CLIMATE OF THE PAST			English	Article							DIALKYL GLYCEROL TETRAETHERS; EOCENE THERMAL MAXIMUM; CLIMATIC OPTIMUM EECO; SEA-LEVEL RISE; SURFACE-TEMPERATURE; SOUTHERN-OCEAN; LIPID DISTRIBUTIONS; OLIGOCENE CLIMATE; ENVIRONMENTAL CONTROLS; TERRESTRIAL CLIMATE	Sea surface temperature (SST) reconstructions based on isoprenoid glycerol dialkyl glycerol tetraether (isoGDGT) distributions from the Eocene southwest (SW) Pacific Ocean are unequivocally warmer than can be reconciled with state-of-the-art fully coupled climate models. However, the SST signal preserved in sedimentary archives can be affected by contributions of additional isoGDGT sources. Methods now exist to identify and possibly correct for overprinting effects on the isoGDGT distribution in marine sediments. Here, we use the current proxy insights to (re-)assess the reliability of the isoGDGT-based SST signal in 69 newly analyzed and 242 reanalyzed sediments at Ocean Drilling Program (ODP) Site 1172 (East Tasman Plateau, Australia) following state-of-the-art chromatographic techniques. We compare our results with paleoenvironmental and paleoclimatologic reconstructions based on dinoflagellate cysts. The resulting similar to 130 kyr resolution Maastrichtian-Oligocene SST record based on the TetraEther indeX of tetraethers with 86 carbon atoms (TEX86) confirms previous conclusions of anomalous warmth in the early Eocene SW Pacific and remarkably cool conditions during the midPaleocene. Dinocyst diversity and assemblages show a strong response to the local SST evolution, supporting the robustness of the TEX86 record. Soil-derived branched GDGTs stored in the same sediments are used to reconstruct mean annual air temperature (MAAT) of the nearby land using the Methylation index of Branched Tetraethers with 5-methyl bonds (MBT'(5me)) proxy. MAAT is consistently lower than SST during the early Eocene, independent of the calibration chosen. General trends in SST and MAAT are similar, except for (1) an enigmatic absence of MAAT rise during the Paleocene-Eocene Thermal Maximum and Middle Eocene Climatic Optimum, and (2) a subdued middle-late Eocene MAAT cooling relative to SST. Both dinocysts and GDGT signals suggest a mid-shelf depositional environment with strong river runoff during the Paleocene-early Eocene progressively becoming more marine thereafter. This trend reflects gradual subsidence and more pronounced wet/dry seasons in the northward-drifting Australian hinterland, which may also explain the subdued middle Eocene MAAT cooling relative to that of SST. The overall correlation between dinocyst assemblages, marine biodiversity and SST changes suggests that temperature exerted a strong influence on the surface-water ecosystem. Finally, we find support for a potential temperature control on compositional changes of branched glycerol monoalkyl glycerol tetraethers (brGMGTs) in marine sediments. It is encouraging that a critical evaluation of the GDGT signals confirms that most of the generated data are reliable. However, this also implies that the high TEX86-based SSTs for the Eocene SW Pacific and the systematic offset between absolute TEX86-based SST and MBT'(5me)-based MAAT estimates remain without definitive explanation.	[Bijl, Peter K.; Frieling, Joost; Cramwinckel, Margot J.; Boschman, Christine; Sluijs, Appy; Peterse, Francien] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Frieling, Joost] Univ Oxford, Dept Earth Sci, South Parks Rd, Oxford OX1 3AN, England; [Cramwinckel, Margot J.] Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton, Hants, England	Utrecht University; University of Oxford; NERC National Oceanography Centre; University of Southampton	Bijl, PK (通讯作者)，Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands.	p.k.bijl@uu.nl	Peterse, Francien/AAY-1473-2021; Sluijs, Appy/B-3726-2009; Peterse, Francien/H-5627-2011	Bijl, Peter/0000-0002-1710-4012; Peterse, Francien/0000-0001-8781-2826; Frieling, Joost/0000-0002-5374-1625	NWO Vernieuwingsimpuls Veni [863.13.002]; Dutch Ministry of Education, Culture and Science; Ammodo Foundation; European Research Council [802835, 771497]; European Research Council (ERC) [802835] Funding Source: European Research Council (ERC)	NWO Vernieuwingsimpuls Veni; Dutch Ministry of Education, Culture and Science; Ammodo Foundation(ACEV Foundation); European Research Council(European Research Council (ERC)); European Research Council (ERC)(European Research Council (ERC))	Peter K. Bijl acknowledges funding through NWO Vernieuwingsimpuls Veni (grant no. 863.13.002). 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. Margot J. Cramwinckel and Appy Sluijs acknowledge the Ammodo Foundation for funding unfettered research of laureate Appy Sluijs. Peter K. Bijl and Appy Sluijs thank the European Research Council for starting grant no. 802835 (OceaNice) and consolidator grant no. 771497 (SPANC), respectively.	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Past.	NOV 25	2021	17	6					2393	2425		10.5194/cp-17-2393-2021	http://dx.doi.org/10.5194/cp-17-2393-2021			33	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	XD9RD		Green Submitted, gold			2025-03-11	WOS:000723036100001
J	Vieira, M; Mahdi, S; Casas-Gallego, M; Ayress, M				Vieira, Manuel; Mahdi, Salih; Casas-Gallego, Manuel; Ayress, Michael			Using microplankton proxies to evaluate marine palaeonvironmental changes during late Maastrichtian: Evidence from the More Basin (Norwegian continental shelf)	CRETACEOUS RESEARCH			English	Article						Planktonic foraminifera; Phytoplankton; Biostratigraphy; Taxonomy; Dinoflagellate cysts	CRETACEOUS-TERTIARY BOUNDARY; WALLED DINOFLAGELLATE CYSTS; SEQUENCE STRATIGRAPHY; ENVIRONMENTAL-CHANGE; OULED HADDOU; NORTH-SEA; BIOSTRATIGRAPHY; SECTION; FORAMINIFERA; ASSEMBLAGES	This work presents high-resolution palynological and micropalaeontological analyses of a cored succession across the upper Maastrichtian from a well in the More Basin (Norwegian continental shelf). Diverse assemblages of dinoflagellate cysts and foraminifera provide insights into the palaeobiogeography and palaeoenvironmental conditions during the late Maastrichtian in this region. An outer neritic setting is interpreted based on the general high abundance of planktonic foraminifera. A subdivision of the biostratigraphic record into three Ecozones has allowed for a detailed documentation of the phytoplankton communities during the late Maastrichtian until the K-Pg boundary. Ecozone A is characterised by a predominance of peridinoid cysts which together with abrupt fluctuations in planktonic foraminifera suggests high nutrient availability and, possibly, high terrestrial input potentially associated with regional turbiditic currents. Also, the occurrence of taxa characteristic of boreal affinity suggests colder waters for this Ecozone. Ecozone B is characterised by consecutive influxes of areoligeracean species such as Palynodinium grallator, Areoligera senonensis and Circulodinium distinctum in the dinoflagellate cyst assemblages. The increase abundances of planktonic foraminifera across this interval suggests an increase in palaeowater depth into a more outer shelf to upper slope. Immediately before the K-Pg boundary (Ecozone C), an increase in abundance of low latitude dinoflagellate species and the planktonic foraminifera Pseudotextularia elegans may represent the local signal of the global latest Maastrichtian Warming Event. Two new dinoflagellate cyst species restricted to the late Maastrichtian, Glaphyrocysta turgida sp. nov. and Heterosphaeridium silybum sp. nov. are also formally described. (c) 2021 Elsevier Ltd. All rights reserved.	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Res.	FEB	2022	130								105071	10.1016/j.cretres.2021.105071	http://dx.doi.org/10.1016/j.cretres.2021.105071		NOV 2021	15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	XE9YQ					2025-03-11	WOS:000723737500007
J	Jerney, J; Rengefors, K; Nagai, S; Krock, B; Sjöqvist, C; Suikkanen, S; Kremp, A				Jerney, Jacqueline; Rengefors, Karin; Nagai, Satoshi; Krock, Bernd; Sjoqvist, Conny; Suikkanen, Sanna; Kremp, Anke			Seasonal genotype dynamics of a marine dinoflagellate: Pelagic populations are homogeneous and as diverse as benthic seed banks	MOLECULAR ECOLOGY			English	Article						adaptation; Alexandrium ostenfeldii; evolution; phytoplankton; resting stage; selection	ALEXANDRIUM-OSTENFELDII BLOOM; GENETIC-STRUCTURE; LIFE-CYCLE; CLONAL DIVERSITY; TOXIN PRODUCTION; DNA EXTRACTION; RESTING CYSTS; SPRING BLOOM; DIATOM; PHYTOPLANKTON	Genetic diversity is the basis for evolutionary adaptation and selection under changing environmental conditions. Phytoplankton populations are genotypically diverse, can become genetically differentiated within small spatiotemporal scales and many species form resting stages. Resting stage accumulations in sediments (seed banks) are expected to serve as reservoirs for genetic information, but so far their role in maintaining phytoplankton diversity and in evolution has remained unclear. In this study we used the toxic dinoflagellate Alexandrium ostenfeldii (Dinophyceae) as a model organism to investigate if (i) the benthic seed bank is more diverse than the pelagic population and (ii) the pelagic population is seasonally differentiated. Resting stages (benthic) and plankton (pelagic) samples were collected at a coastal bloom site in the Baltic Sea, followed by cell isolation and genotyping using microsatellite markers (MS) and restriction site associated DNA sequencing (RAD). High clonal diversity (98%-100%) combined with intermediate to low gene diversity (0.58-0.03, depending on the marker) was found. Surprisingly, the benthic and pelagic fractions of the population were equally diverse, and the pelagic fraction was temporally homogeneous, despite seasonal fluctuation of environmental selection pressures. The results of this study suggest that continuous benthic-pelagic coupling, combined with frequent sexual reproduction, as indicated by persistent linkage equilibrium, prevent the dominance of single clonal lineages in a dynamic environment. Both processes harmonize the pelagic with the benthic population and thus prevent seasonal population differentiation. At the same time, frequent sexual reproduction and benthic-pelagic coupling maintain high clonal diversity in both habitats.	[Jerney, Jacqueline; Suikkanen, Sanna; Kremp, Anke] Univ Helsinki, Tvarminne Zool Stn, Hango, Finland; [Jerney, Jacqueline] Finnish Environm Inst, Ctr Marine Res, Agnes Sjobergin Katu 2, Helsinki 00790, Finland; [Rengefors, Karin] Lund Univ, Dept Biol, Lund, Sweden; [Nagai, Satoshi] Natl Res Inst Fisheries Sci, Yokohama, Kanagawa, Japan; [Krock, Bernd] Alfred WegenerInst Helmholtz Zentrum Polarund & M, Bremerhaven, Germany; [Sjoqvist, Conny] Abo Akad Univ, Fac Sci & Engn Environm & Marine Biol, Turku, Finland; [Kremp, Anke] Leibniz Inst Ostseeforsch Warnemunde, Rostock, Germany	University of Helsinki; Finnish Environment Institute; Lund University; Japan Fisheries Research & Education Agency (FRA); Abo Akademi University; Leibniz Institut fur Ostseeforschung Warnemunde	Jerney, J (通讯作者)，Finnish Environm Inst, Ctr Marine Res, Agnes Sjobergin Katu 2, Helsinki 00790, Finland.	jacqueline.jerney@gmx.at	Rengefors, Karin/K-5873-2019; Sjöqvist, Conny/AAL-1053-2020; Nagai, Satoshi/HOA-8686-2023; Krock, Bernd/ABB-7541-2020	Sjoqvist, Conny/0000-0003-2562-0217; Nagai, Satoshi/0000-0001-7510-0063; Rengefors, Karin/0000-0001-6297-9734; Jerney, Jacqueline/0000-0002-2736-5179; Kremp, Anke/0000-0001-9484-6899; Suikkanen, Sanna/0000-0002-0768-8149	Academy of Finland [310449, 251564]; Japan Society for the Promotion of Science [18KK0182]; Grants-in-Aid for Scientific Research [18KK0182, 21H02274, 23K21233] Funding Source: KAKEN; Academy of Finland (AKA) [251564, 310449] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); 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)); Academy of Finland (AKA)(Research Council of Finland)	Academy of Finland, Grant/Award Number: 310449 and 251564; 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Ecol.	JAN	2022	31	2					512	528		10.1111/mec.16257	http://dx.doi.org/10.1111/mec.16257		NOV 2021	17	Biochemistry & Molecular Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Environmental Sciences & Ecology; Evolutionary Biology	YD9IG	34716943	Green Published, hybrid			2025-03-11	WOS:000717063700001
J	Falzoni, F; Petrizzo, MR				Falzoni, Francesca; Petrizzo, Maria Rose			Evidence for changes in sea-surface circulation patterns and ∼20° equatorward expansion of the Boreal bioprovince during a cold snap of Oceanic Anoxic Event 2 (Late Cretaceous)	GLOBAL AND PLANETARY CHANGE			English	Article						Plenus Cold Event; Oceanic Anoxic Event 2; Cenomanian-Turonian boundary interval; Cretaceous supergreenhouse planktonic foraminifera; Praeactinocamax plenus	CENOMANIAN-TURONIAN BOUNDARY; WESTERN INTERIOR SEAWAY; PLANKTONIC-FORAMINIFERA; HIGH-RESOLUTION; VOCONTIAN BASIN; NORTH-ATLANTIC; ENVIRONMENTAL PERTURBATIONS; NEOGLOBOQUADRINA-PACHYDERMA; BELEMNITE PRAEACTINOCAMAX; TEMPERATURE-GRADIENT	The Plenus Cold Event (PCE) temporarily interrupted the supergreenhouse conditions exacerbated during much of the Cenomanian-Turonian Oceanic Anoxic Event 2 (OAE 2). The PCE is coeval to the occurrence of Boreal benthic macroinvertebrates and of the nektonic belemnite Praeactinocamax plenus (after which the event is named) in Europe, and to the re-oxygenation of bottom waters in the Northern Hemisphere. However, its effects on the sea-surface circulation are unknown and evidence for changes in the biogeography of planktonic organisms are limited to the equatorward migration of the dinoflagellate cysts grouped in the Cyclonephelium compactum-membraniphorum morphological plexus. This study presents new planktonic foraminiferal quantitative data from two complete OAE 2 records of the Anglo-Paris (Eastbourne, SE England) and Vocontian (Clot Chevalier, SE France) basins that registered the equatorward pulse of Boreal macroinvertebrates during the PCE and have been extensively studied for bio- and chemostratigraphy. At the onset of OAE 2 (before the PCE), planktonic foraminifera are mainly represented by oligo-mesotrophic Tethyan taxa (rotaliporids and whiteinellids) in both localities, but this assemblage is sharply replaced by cold and meso-to-eutrophic species (praeglobotruncanids, dicarinellids and muricohedbergellids) during the PCE. The cold-water assemblage shows strong affinities with the coeval fauna of the Norwegian Sea and yields the Boreal endemic species Muricohedbergella kyphoma and Praeglobotruncana plenusiensis. This observation combined with previously published data collected in other localities of the Northern Hemisphere and on other fossil groups suggests a similar to 20 degrees equatorward expansion of the Boreal marine bioprovince during the PCE. Moreover, contrarily to the nektonic belemnitellids that were able to move independently of ocean circulation, planktonic organisms are passively transported by currents and changes in the planktonic foraminiferal assemblages documented in the Anglo-Paris and Vocontian basins have been interpreted to reflect the transition from a dominant influence of warm, saline, and thermally stratified waters carried by the proto-Gulf Stream before the PCE to cold and low-saline Boreal waters originated in the Norwegian Sea during the PCE. We suggest that such changes were forced by the equatorward shift of the proto-Arctic Front (i.e., the boundary between warm saline Tethyan-Atlantic and cold low-saline Boreal waters) from offshore Norway to Southern England. In this southerly position, the proto-Arctic Front represented an oceanographic barrier that limited the influence of the proto-Gulf Stream in the Anglo-Paris Basin, and favored the inflow of Boreal waters from the North to the European epicontinental basins. The sea-surface cooling and equatorward expansion of Boreal planktonic assemblages during the PCE are of the same order of magnitude of those reconstructed between some glacial and interglacial intervals of the Plio-Pleistocene. Despite obvious differences between Cretaceous and Plio-Pleistocene paleogeography and climate dynamics, this study reviews the extent of environmental changes occurred during the PCE, provides evidence for a profound re-organization of the sea-surface circulation patterns and a more comprehensive overview of the equatorward migration of Boreal marine communities in the Northern Hemisphere.	[Falzoni, Francesca] Univ Napoli Federico II, Dipartimento Sci Terra Ambiente & Risorse, Via Vicinale Cupa Cintia 21, I-80126 Naples, Italy; [Petrizzo, Maria Rose] Univ Milan, Dipartimento Sci Terra A Desio, Via Mangiagalli 34, I-20133 Milan, Italy	University of Naples Federico II; University of Milan	Falzoni, F (通讯作者)，Univ Napoli Federico II, Dipartimento Sci Terra Ambiente & Risorse, Via Vicinale Cupa Cintia 21, I-80126 Naples, Italy.	francesca.falzoni1@gmail.com; mrose.petrizzo@unimi.it	Petrizzo, Maria/M-8672-2013	Falzoni, Francesca/0000-0002-5694-9827	Italian Ministry of University and Research (MUR) [PRIN 2017RX9XXY]	Italian Ministry of University and Research (MUR)(Ministry of Education, Universities and Research (MIUR))	We warmly thank the editor Maoyan Zhu for handling the manuscript, Mark Leckie and an anonymous reviewer for their careful revisions and thoughtful comments and suggestions that greatly improved the quality of this manuscript. 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Planet. Change	JAN	2022	208								103678	10.1016/j.gloplacha.2021.103678	http://dx.doi.org/10.1016/j.gloplacha.2021.103678		NOV 2021	22	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	XO3FW		Green Published			2025-03-11	WOS:000730075400001
J	Sauermilch, I; Whittaker, JM; Klocker, A; Munday, DR; Hochmuth, K; Bijl, PK; LaCasce, JH				Sauermilch, Isabel; Whittaker, Joanne M.; Klocker, Andreas; Munday, David R.; Hochmuth, Katharina; Bijl, Peter K.; LaCasce, Joseph H.			Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling	NATURE COMMUNICATIONS			English	Article							ANTARCTIC CIRCUMPOLAR CURRENT; SOUTHWEST PACIFIC-OCEAN; DINOFLAGELLATE CYSTS; ATMOSPHERIC CO2; DRAKE PASSAGE; ROSS SEA; CIRCULATION; MODEL; FLOW; HEAT	Declining atmospheric CO2 concentrations are considered the primary driver for the Cenozoic Greenhouse-Icehouse transition, similar to 34 million years ago. A role for tectonically opening Southern Ocean gateways, initiating the onset of a thermally isolating Antarctic Circumpolar Current, has been disputed as ocean models have not reproduced expected heat transport to the Antarctic coast. Here we use high-resolution ocean simulations with detailed paleobathymetry to demonstrate that tectonics did play a fundamental role in reorganising Southern Ocean circulation patterns and heat transport, consistent with available proxy data. When at least one gateway (Tasmanian or Drake) is shallow (300 m), gyres transport warm waters towards Antarctica. When the second gateway subsides below 300 m, these gyres weaken and cause a dramatic cooling (average of 2-4 degrees C, up to 5 degrees C) of Antarctic surface waters whilst the ACC remains weak. Our results demonstrate that tectonic changes are crucial for Southern Ocean climate change and should be carefully considered in constraining long-term climate sensitivity to CO2.	[Sauermilch, Isabel; Whittaker, Joanne M.; Klocker, Andreas] Univ Tasmania, Inst Marine & Antarctic Stud, Hobart, Tas, Australia; [Sauermilch, Isabel; Bijl, Peter K.] Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands; [Klocker, Andreas] Univ Tasmania, Australian Res Council Ctr Excellence Climate Ext, Hobart, Tas, Australia; [Munday, David R.] British Antarctic Survey, Cambridge, England; [Hochmuth, Katharina] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany; [Hochmuth, Katharina] Univ Leicester, Sch Geog Geol & Environm, Leicester, Leics, England; [LaCasce, Joseph H.] Univ Oslo, Dept Geosci, Oslo, Norway	University of Tasmania; Utrecht University; University of Tasmania; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Leicester; University of Oslo	Sauermilch, I (通讯作者)，Univ Tasmania, Inst Marine & Antarctic Stud, Hobart, Tas, Australia.; Sauermilch, I (通讯作者)，Univ Utrecht, Fac Geosci, Dept Earth Sci, Utrecht, Netherlands.	i.sauermilch@uu.nl	Hochmuth, Katharina/LJL-9426-2024; Whittaker, Joanne/B-3695-2010; Klocker, Andreas/E-4632-2011; Munday, David/R-1986-2016	Hochmuth, Katharina/0000-0003-2789-2179; Whittaker, Joanne/0000-0002-3170-3935; Bijl, Peter/0000-0002-1710-4012; Klocker, Andreas/0000-0002-2038-7922; Sauermilch, Dr Isabel/0000-0003-4639-6699; Munday, David/0000-0003-1920-708X	Australian Research Council Special Research Initiative for Antarctic Gateway Partnership [SR140300001, 180102280]; ORCHESTRA project [NE/N018095/1]; Deutsche Forschungsgemeinschaft (DFG) [GO724/15-1]; ERC Starting Grant OceaNice [802835]; Rough Ocean project from the Norwegian Research Council [302743]; University of Tasmania; NERC [bas0100033, NE/N018095/1] Funding Source: UKRI; European Research Council (ERC) [802835] Funding Source: European Research Council (ERC)	Australian Research Council Special Research Initiative for Antarctic Gateway Partnership(Australian Research Council); ORCHESTRA project; Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); ERC Starting Grant OceaNice(European Research Council (ERC)); Rough Ocean project from the Norwegian Research Council(Research Council of Norway); University of Tasmania; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); European Research Council (ERC)(European Research Council (ERC))	This research was undertaken with support from Australian Research Council Special Research Initiative for Antarctic Gateway Partnership (Project ID SR140300001), Discovery Project 180102280, and computational resources from the Australian National Computational Infrastructure. We thank Dave Hutchinson for providing the forcing input data for our model. D.R.M. is supported by the ORCHESTRA project (NE/N018095/1). K.H.'s research has been funded by the Deutsche Forschungsgemeinschaft (DFG) under the project GO724/15-1 and institutional resources from the Research Program PACES-II, Workpackage 3.2, of the Alfred Wegener Institute (AWI). The European Research Council under the European Community's Seventh Framework Program provided funding by ERC Starting Grant OceaNice #802835 to P.K.B.; J.H.L. was supported by the Rough Ocean project (number 302743) from the Norwegian Research Council. D.R.M., K.H. and J.H.L. received a "Visiting Scholarship" from the University of Tasmania. We thank Max Nikurashin and Eivind Straume for constructive discussions and comments.	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Commun.	NOV 9	2021	12	1							6465	10.1038/s41467-021-26658-1	http://dx.doi.org/10.1038/s41467-021-26658-1			8	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	WU5MJ	34753912	gold, Green Published			2025-03-11	WOS:000716589100009
J	Zhao, XQ; Dupont, L; Kölling, M; Baqloul, A; Reddad, H; Bouimetarhan, I				Zhao, Xueqin; Dupont, Lydie; Koelling, Martin; Baqloul, Asmae; Reddad, Hanane; Bouimetarhan, Ilham			Evidence for anthropogenic, climatic and oceanographic variability off southwestern Morocco during the last three millennia	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cysts; Upwelling; Fluvial input; Lingulodinium machaerophorum; Gymnodinium; Late Holocene	DINOFLAGELLATE CYST PRODUCTION; NORTH-ATLANTIC OSCILLATION; UPWELLING INTENSITY; MIDDLE ATLAS; CANARY BASIN; NW-AFRICA; OCEAN; CIRCULATION; SEDIMENTS; INDICATORS	In order to obtain a better knowledge of oceanic changes in the Canary Upwelling region during the Late Holocene, marine surface samples and two sediment cores retrieved off southwestern Morocco, GeoB8601-3 and GeoB4223-1, were investigated for organic-walled dinoflagellate cysts (dinocysts). The results were compared with pollen, microcharcoal particles, geochemical records, stable hydrogen and carbon isotope composition (delta 2H and delta 13C) of plant-waxes of the same material. The dinocyst results indicate active upwelling prior to 750 BCE and a longer upwelling season between 750 BCE and 950 CE, which is attributed to increased northeast trade winds. After 950 CE, a marked increase of Lingulodinium machaerophorum and Gymnodinium species indicates high fluvial input probably due to a combination of climate (possibly negative NAO) and anthropogenic (terrestrial erosion related to Early Arab conquest) impacts.	[Zhao, Xueqin; Dupont, Lydie; Koelling, Martin; Bouimetarhan, Ilham] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Zhao, Xueqin] Shanghai Ocean Univ, Coll Marine Sci, Shanghai, Peoples R China; [Baqloul, Asmae; Bouimetarhan, Ilham] Ibn Zohr Univ Agadir, Appl Geol & Geoenvironm Lab, Agadir, Morocco; [Reddad, Hanane] Univ Sultan Moulay Slimane Beni Mellal, Fac Lettres & Sci Humaines, Beni Mellal, Morocco; [Bouimetarhan, Ilham] Ibn Zohr Univ Agadir, Fac Sci Appl, CUAM, Agadir, Morocco	University of Bremen; Shanghai Ocean University; Ibn Zohr University of Agadir; Sultan Moulay Slimane University of Beni Mellal; Ibn Zohr University of Agadir	Zhao, XQ (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany.	snowybolter@gmail.com; dupont@uni-bremen.de; koelling@uni-bremen.de; h.reddad@usms.ma; bouimetarhan@uni-bremen.de	Bouimetarhan, Ilham/D-2388-2011; REDDAD, Hanane/E-2713-2019	Bouimetarhan, Ilham/0000-0003-3369-3811; Koelling, Martin/0000-0003-2720-2211; REDDAD, Hanane/0000-0002-6238-165X; Zhao, Xueqin/0000-0003-3354-3768	German Federal Ministry of Education and Research (BMBF) , Germany [PMARS2015-100]	German Federal Ministry of Education and Research (BMBF) , Germany(Federal Ministry of Education & Research (BMBF))	This work was funded by the German Federal Ministry of Education and Research (BMBF) , Germany with grant number (PMARS2015-100) through the PMARS initiative "Programme Marocco-Allemand de la Recherche Scientifique (PMARS III) " granted to Dr. Ilham Bouime-tarhan. The investigations were conducted within the ECHo project (Environmental-Climate-Human interaction in southern Morocco dur-ing the past 2000 years: inferences from high-resolution marine re-cords) . We would like to thank Jawad El Hawari for his help with processing the samples. Thanks to Martin J. Head and editor Alexander Dickson for their useful comments that have helped us to improve the manuscript. Data of this study and those cited from Holzwarth et al. (2010a) are available in PANGAEA: "https://doi.pangaea.de/10.1594/PANGAEA.922632" for marine surface dinocyst data in this study; "https://doi.pangaea.de/10.1594/PANGAEA.922629" for dinocyst data of core GeoB8601-3 in this study; "https://doi.pangaea.de/10.1594/PA NGAEA.922096" for dinocyst data of core GeoB4223-1 in this study; "https://doi.pangaea.de/10.1594/PANGAEA.710758" for marine sur-face dinocyst data in Holzwarth et al. (2010a) .	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J	de Freitas, AD; Aguiar, VMD; Neto, JAB				de Freitas, Alex da S.; Aguiar, Valquiria Maria de C.; Baptista Neto, Jose Antonio			Modern Dinoflagellate Cyst Abundance and Trace Metals as Biomonitoring Tools in a Tropical Bay in Brazil	JOURNAL OF COASTAL RESEARCH			English	Article						&nbsp; Estuary; pollution; eutrophication; dinocysts; inorganic pollutants	RIO-DE-JANEIRO; RECENT MARINE-SEDIMENTS; GUANABARA-BAY; HEAVY-METALS; EUTROPHICATION; ASSEMBLAGES; POLLUTION; HARBOR; WATER; SEA	The spatial distribution of the dinoflagellate cyst assemblages in 11 surface sediment samples collected in Guanabara Bay embayments and associated trace metals revealed the applicability of dinocysts as bioindicators of environmental conditions in estuarine systems. The surface sediment samples presented coarse to fine granulometry. The dinoflagellate cyst analysis followed the standard methodology through the elimination of carbonates and silica. Trace metals were extracted by the evaluation of 1 g of sediment plus a mixture of HNO3 and HCl in a microwave digestion system. Dinoflagellate cyst assemblages were dominated by Operculodinium centrocarpum, Spiniferites spp., and Lingulodinium machaerophorum. Trace metals (Cu, Zn, Pb, Cr, and Ni) showed variations at the different sampling points. The values obtained were Cu (6.7-82.8 mg kg-1), Zn (29.5-355.4 mg kg-1), Pb (18.3-86.2 mg kg-1), Cr (5.1-196.2 mg kg-1), and Ni (19.6-286.0 mg kg-1). Several samples showed high pseudototal concentrations of trace metals, which were above the natural concentrations found in nature. Statistical analysis showed a strong correlation between dinocysts species and some trace metals. Lingulodinium machaerophorum showed a high correlation with 4/5 analysed trace metals and is a eutrophication-sensitive species. However, Brigantedinium sp. presented a positive correlation with all trace metals analysed. The high frequency of L. machaerophorum cysts in all analysed samples associated with several trace metals is indicative of environmental eutrophication. The high availability of trace metals in the surface sediments of Guanabara Bay may be related to the untreated industrial wastes that are dumped directly into the bay.	[de Freitas, Alex da S.; Aguiar, Valquiria Maria de C.; Baptista Neto, Jose Antonio] Univ Fed Fluminense, Inst Geociencias, Dept Geol & Geofis LAGEMAR, Rio De Janeiro, Brazil	Universidade Federal Fluminense	de Freitas, AD (通讯作者)，Univ Fed Fluminense, Inst Geociencias, Dept Geol & Geofis LAGEMAR, Rio De Janeiro, Brazil.	alexsilfre@gmail.com	DE SOUSA NETO, JOSE/KGL-2012-2024; de Freitas, Alex/IUQ-2116-2023; Aguiar, Valquiria/HZJ-5714-2023		Fundacao de Amparo 'a Pesquisa do Estado do Rio de Janeiro (FAPERJ); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)	Fundacao de Amparo 'a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was sponsored by the Fundacao de Amparo 'a Pesquisa do Estado do Rio de Janeiro (FAPERJ), the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), and CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior).	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Coast. Res.	NOV	2021	37	6					1247	1259		10.2112/JCOASTRES-D-21-00030.1	http://dx.doi.org/10.2112/JCOASTRES-D-21-00030.1			13	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	YS7VG					2025-03-11	WOS:000750880400013
J	Xu, LJ; Yang, DZ; Yu, RC; Feng, XR; Gao, GD; Cui, X; Bai, T; Yin, BS				Xu, Lingjing; Yang, Dezhou; Yu, Rencheng; Feng, Xingru; Gao, Guandong; Cui, Xuan; Bai, Tao; Yin, Baoshu			Nonlocal Population Sources Triggering Dinoflagellate Blooms in the Changjiang Estuary and Adjacent Seas: A Modeling Study	JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES			English	Article						dinoflagellate; Changjiang Estuary and adjacent seas; nonlocal population source; adjoint model; coupled physical-biological model	EAST CHINA SEA; YELLOW SEA; ECOSYSTEM MODEL; SURFACE; SYSTEM; SEDIMENTS; IMPACTS; ADJOINT; GROWTH; CYSTS	Dinoflagellates frequently cause harmful, large-scale spring algal blooms in the Changjiang Estuary and adjacent seas of China. However, the population source of some dinoflagellates in this area remains unknown. We deployed an adjoint model and a coupled physical-biological model to explore the possible nonlocal dinoflagellate population sources to the Changjiang Estuary and adjacent seas. Our simulation results revealed that the Taiwan Strait and the area east of Taiwan are two nonlocal source regions of May dinoflagellate blooms in the study area. Under different hydrodynamic and biochemical conditions, dinoflagellates from the Taiwan Strait directly triggered dinoflagellate blooms from south to north along the coast of China. Dinoflagellates from the area east of Taiwan first concentrated and bred in the offshore temperature frontal area and then spread southwestward, triggering dinoflagellate blooms along the Zhejiang coast. Due to the different influence mechanisms, it took longer for the initial dinoflagellate population in the Taiwan Strait to exert the same impact on dinoflagellate blooms in the study area as that from the area east of Taiwan. Moreover, the density and appearance time of the initial dinoflagellate population in the Taiwan Strait affected their biomass and bloom range in the study area. Even a small initial dinoflagellate population east of Taiwan could trigger a bloom in the study area. This study suggests the target domains for finding nonlocal dinoflagellate cysts and provides a strategy to predict dinoflagellate blooms in the Changjiang Estuary adjacent area by monitoring dinoflagellate biomass in the nonlocal source regions.	[Xu, Lingjing; Yang, Dezhou; Feng, Xingru; Gao, Guandong; Cui, Xuan; Yin, Baoshu] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China; [Xu, Lingjing; Yang, Dezhou; Feng, Xingru; Gao, Guandong; Cui, Xuan; Yin, Baoshu] Chinese Acad Sci, Inst Oceanol, CAS Engn Lab Marine Ranching, Qingdao, Peoples R China; [Xu, Lingjing; Yang, Dezhou; Feng, Xingru; Gao, Guandong; Cui, Xuan; Yin, Baoshu] Qingdao Natl Lab Marine Sci Technol, Funct Lab Ocean Dynam & Climate, Qingdao, Peoples R China; [Xu, Lingjing; Yang, Dezhou; Yu, Rencheng; Feng, Xingru; Gao, Guandong; Cui, Xuan; Yin, Baoshu] Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China; [Yang, Dezhou; Yu, Rencheng; Cui, Xuan; Yin, Baoshu] Univ Chinese Acad Sci, Beijing, Peoples R China; [Yu, Rencheng] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao, Peoples R China; [Bai, Tao] North China Sea Marine Forecasting Ctr State Ocea, Qingdao, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; Chinese Academy of Sciences; Institute of Oceanology, CAS	Yang, DZ; Yin, BS (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China.; Yang, DZ; Yin, BS (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Engn Lab Marine Ranching, Qingdao, Peoples R China.; Yang, DZ; Yin, BS (通讯作者)，Qingdao Natl Lab Marine Sci Technol, Funct Lab Ocean Dynam & Climate, Qingdao, Peoples R China.; Yang, DZ; Yin, BS (通讯作者)，Chinese Acad Sci, Ctr Ocean Mega Sci, Qingdao, Peoples R China.; Yang, DZ; Yin, BS (通讯作者)，Univ Chinese Acad Sci, Beijing, Peoples R China.	yangdezhou@qdio.ac.cn; bsyin@qdio.ac.cn	Gao, Guandong/KBD-1950-2024; Yu, Rencheng/J-4450-2017	Cui, Xuan/0000-0002-7725-0687; Xu, Lingjing/0000-0002-7230-7752; Gao, Guandong/0000-0002-7348-876X; Yu, Rencheng/0000-0001-6430-9224	Strategic Priority Research Program of the Chinese Academy of Sciences [XDB42000000, XDA19060203, XDA19060202]; National Natural Science Foundation of China (NSFC) [41876019, 42076022, 42090044]; Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Science [COMS2020Q01]; NSFC-Shandong Joint Fund [U1806227]; CAS-CSIRO BAU project [133137KYSB20180141]; High Performance Computing Center at the IOCAS; Youth Innovation Promotion Association CAS; East China Sea ocean observation and research station of OMORN	Strategic Priority Research Program of the Chinese Academy of Sciences(Chinese Academy of Sciences); National Natural Science Foundation of China (NSFC)(National Natural Science Foundation of China (NSFC)); Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Science; NSFC-Shandong Joint Fund; CAS-CSIRO BAU project; High Performance Computing Center at the IOCAS; Youth Innovation Promotion Association CAS; East China Sea ocean observation and research station of OMORN	This study was supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Nos. XDB42000000, XDA19060203, and XDA19060202), the National Natural Science Foundation of China (NSFC) (Nos. 41876019, 42076022, and 42090044), Key Deployment Project of Centre for Ocean Mega-Research of Science, Chinese Academy of Science (No. COMS2020Q01), the NSFC-Shandong Joint Fund (No U1806227), the CAS-CSIRO BAU project (No. 133137KYSB20180141). It was also supported by the High Performance Computing Center at the IOCAS, East China Sea ocean observation and research station of OMORN, and the Youth Innovation Promotion Association CAS.	Cao L, 2021, OCEAN DYNAM, V71, P237, DOI 10.1007/s10236-020-01427-8; [岑竞仪 Cen Jingyi], 2017, [海洋与湖沼, Oceanologia et Limnologia Sinica], V48, P1022; Chai F, 2002, DEEP-SEA RES PT II, V49, P2713, DOI 10.1016/S0967-0645(02)00055-3; Chen C. T. 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Geophys. Res.-Biogeosci.	NOV	2021	126	11							e2021JG006424	10.1029/2021JG006424	http://dx.doi.org/10.1029/2021JG006424			19	Environmental Sciences; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	XD1KF					2025-03-11	WOS:000722469900016
J	Black, RD; Dodsworth, P				Black, Roderick D.; Dodsworth, Paul			The palynology of the Kimmeridge Clay and Carstone Formations (Upper Jurassic-Lower Cretaceous) at Middlegate Quarry, North Lincolnshire, UK, and its biostratigraphical and palaeoenvironmental significance	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							DINOFLAGELLATE CYSTS; BOUNDARY STRATOTYPE; STRATIGRAPHY; YORKSHIRE; ENGLAND; ONSHORE; SPEETON	At Middlegate Quarry, the Carstone Formation is a c. 0.8 m thick unit of oolitic ferruginous sandstone. It rests unconformably on the lower Kimmeridge Clay Formation (KCF) and is overlain by the Hunstanton Formation (Red Chalk) with an apparently gradational junction. Marine dinoflagellate cysts (dinocysts) are present at a concentration of 9520 to 13 600 specimens per gram in the 0.15 m of KCF below the unconformity, and include taxa that confirm ammonite evidence for the intra-Lower Kimmeridgian Substage (Upper Jurassic, Cymodoce Ammonite Zone). A rich recovery of well-preserved Lower Cretaceous palynomorphs is reported for the first time from the overlying Carstone. Reworking of mudstone from the KCF into the formation appears to have provided a local argillaceous preservation matrix at Middlegate. The basal 0.15 m is dominated by palynomorphs derived from the KCF but the interval from 0.15 to 0.55 m above the unconformity mainly contains indigenous Lower Cretaceous palynomorphs. Dinoflagellate cysts are present in the Carstone at an average concentration of 454 specimens per gram, and include taxa that probably have stratigraphical range bases above the Aptian-Albian stage boundary: Cyclonephelium compactum, Cyclonephelium intonsum, Endoscrinium heikeae, Leptodinium cancellatum (consistent), Stephodinium coronatum and Stephodinium spinulosum. The additional presence of taxa with range tops/event tops in the Lower Albian Tardefurcata Ammonite Zone (common Cauca parva, frequent Canninginopsis monile and Kleithriasphaeridium eoinodes, and rare Dingodinium albertii, Discorsia nannus and Kiokansium prolatum) indicate probable assignment to this zone. The new palynological data support previous macrofossil (brachiopod) study of the Carstone at Middlegate and nearby Melton Bottom Quarry which tentatively assigns its highest part to the Tardefurcata Zone. The palynological and palynofacies assemblages are interpreted to confirm a relatively proximal to shoreline site of deposition, possibly inner to middle neritic. Supplementary material: Quarry photographs and a palynological distribution chart are available at	[Black, Roderick D.] Balfour Beatty, 5 Churchill Pl, London E14 5HU, England; [Dodsworth, Paul] Stockton Heath, StrataSolve Ltd, 15 Francis Rd, Warrington WA4 6EB, Cheshire, England		Dodsworth, P (通讯作者)，Stockton Heath, StrataSolve Ltd, 15 Francis Rd, Warrington WA4 6EB, Cheshire, England.	dodsworth@stratasolve.com		Dodsworth, Paul/0000-0002-8895-9472	NERC Master of Science (Palynology) grant	NERC Master of Science (Palynology) grant	Fieldwork and palynological laboratory processing were supported by a NERC Master of Science (Palynology) grant, awarded to RDB at the University of Sheffield, 1993-1994. The grant number was unavailable at the time of publication (2021). This research received no further specific grant from any funding agency in the public, commercial, or not-for-profit sectors.	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Yorks. Geol. Soc.	NOV	2021	63	4							pygs2021-005	10.1144/pygs2021-005	http://dx.doi.org/10.1144/pygs2021-005			16	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	WB6LW		hybrid			2025-03-11	WOS:000703682600001
J	Bista, D; Hoyle, TM; Simon, D; Sangiorgi, F; Richards, DA; Flecker, R				Bista, Diksha; Hoyle, Thomas M.; Simon, Dirk; Sangiorgi, Francesca; Richards, David A.; Flecker, Rachel			Sr isotope-salinity modelling constraints on Quaternary Black Sea connectivity	QUATERNARY SCIENCE REVIEWS			English	Article						Black sea; Sr isotopes; Quaternary; Salinity; Modelling; Connectivity; Caspian sea; Mediterranean	DINOFLAGELLATE CYSTS; CASPIAN SEA; ARAL SEA; MARMARA SEA; WATER; HOLOCENE; PLEISTOCENE; LAKE; RECONNECTION; SR-87/SR-86	Reconstruction of the Black Sea's connectivity history during the Quaternary is based on high-resolution isotope data and longer-term biotic records. These demonstrate that the Black Sea experienced rapidly changing hydrologic configurations involving, at different times, isolation from and/or connection with the Mediterranean and Caspian seas. Here, we simulate these connectivity scenarios using a numerical box model of Black Sea hydrography. This allows us to explore the magnitude of the different water fluxes and their consequences for Black Sea salinity and Sr isotope ratio; parameters that we can measure today and reconstruct in the past. We show that the model is able to replicate the present-day hydrography using new Sr isotopic data measured on modern Black Sea water (0.709143 +/- 0.000008) and that the Black Sea has a homogenous Sr isotope ratio despite its strongly stratified water column. We then create a 1.2 Myr record of paired Sr isotope (ostracods) and palaeosalinity (dinoflagellate cysts) data, using samples from DSDP Site 379. We also provide the first constraints on the Sr isotope ratio of the Amu Darya River, a substantial fluvial system that previously fed the Caspian Sea and therefore influenced the Black Sea when the two basins were connected. Modelling the different connectivity scenarios and incorporating both new and previously published geochemical and biotic data indicates that influx from the Caspian Sea dominated Black Sea hydrography between 1.2 to around 0.5 Ma. In contrast, Mediterranean input has exerted increasing influence since 0.6 Ma, particularly during interglacial periods. The hypothesis that an interval of anomalously high Sr isotope ratios in the Black Sea during the late Saalian deglaciation (MIS 6) was caused by input from the Amu Darya is demonstrably unrealistic. Instead the high Sr ratios may have been driven by variations in glacial extent within the Dnieper catchment and the resultant erosion of Sr from granitic basement rocks. Our new combined model-data approach tests and refines interpretations of the glacio-hydrographic development of the Black Sea during the second half of the Quaternary. (C) 2021 Elsevier Ltd. All rights reserved.	[Bista, Diksha; Simon, Dirk; Richards, David A.; Flecker, Rachel] Univ Bristol, Sch Geog Sci, BRIDGE, Univ Rd, Bristol BS8 1SS, Avon, England; [Bista, Diksha; Simon, Dirk; Richards, David A.; Flecker, Rachel] Univ Bristol, Cabot Inst, Univ Rd, Bristol BS8 1SS, Avon, England; [Bista, Diksha; Richards, David A.] Univ Bristol, Bristol Isotope Grp, Bristol, Avon, England; [Hoyle, Thomas M.; Sangiorgi, Francesca] Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands; [Simon, Dirk] Univ Utrecht, Dept Earth Sci, Princetonlaan 8a, NL-3584 CB Utrecht, Netherlands	University of Bristol; University of Bristol; University of Bristol; Utrecht University; Utrecht University	Bista, D (通讯作者)，British Geol Survey, Nicker Hill, Nottingham NG12 5GG, England.	diksha.bista@bristol.ac.uk	Richards, David/B-7298-2008	Richards, David/0000-0001-8389-8079; Flecker, Rachel/0000-0002-9369-5328; Sangiorgi, Francesca/0000-0003-4233-6154; Hoyle, Thomas M./0000-0002-6611-2254; Bista, Diksha/0000-0003-1510-7735	European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant [642973]; GeoEcoMar cruise MN167 [PN 16 45 01 01]	European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant(Marie Curie Actions); GeoEcoMar cruise MN167	This work was part of the PRIDE project, which received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement No 642973. This research used samples provided by the International Ocean Discovery Program (IODP). We acknowledge Holger Kuhlman for facilitating access to the cores and Sergei Lazarev for help sampling. We also acknowledge GeoEcoMar cruise MN167 (project PN 16 45 01 01) and the scientific crew onboard for all the help during the research cruise. Thanks to the PRIDE ESRs for providing assistance during sampling and, in some cases, for collecting water samples. We also thank Dr. Jamie Lewis (BIG, Bristol) for his help with mass spectrometry and Sr chemistry troubles and Dr. Georg Schettler (GFZ, Germany) for providing Aral Sea water samples. We gratefully acknowledge the careful reviews that we received which have substantially improved the manuscript we submitted.	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J	Hoem, FS; Sauermilch, I; Hou, SN; Brinkhuis, H; Sangiorgi, F; Bijl, PK				Hoem, Frida S.; Sauermilch, Isabel; Hou, Suning; Brinkhuis, Henk; Sangiorgi, Francesca; Bijl, Peter K.			Late Eocene-early Miocene evolution of the southern Australian subtropical front: a marine palynological approach	JOURNAL OF MICROPALAEONTOLOGY			English	Article							ICE-SHEET VARIABILITY; ANTARCTIC CIRCUMPOLAR CURRENT; OFFSHORE WILKES LAND; DINOFLAGELLATE CYSTS; MARSHALL PARACONFORMITY; OLIGOCENE TRANSITION; LATE PLIOCENE; NEW-ZEALAND; SEA-LEVEL; ROSS SEA	Improvements in our capability to reconstruct ancient surface-ocean conditions based on organic-walled dinoflagellate cyst (dinocyst) assemblages from the Southern Ocean provide an opportunity to better establish past position, strength and oceanography of the subtropical front (STF). Here, we aim to reconstruct the late Eocene to early Miocene (37-20 Ma) depositional and palaeoceanographic history of the STF in the context of the evolving Tasmanian Gateway as well as the potential influence of Antarctic circumpolar flow and intense waxing and waning of ice. We approach this by combining information from seismic lines (revisiting existing data and generating new marine palynological data from Ocean Drilling Program (ODP) Hole 1168A) in the western Tasmanian continental slope. We apply improved taxonomic insights and palaeoecological models to reconstruct the sea surface palaeoenvironmental evolution. Late Eocene-early Oligocene (37-30.5 Ma) assemblages show a progressive transition from dominant terrestrial palynomorphs and inner-neritic dinocyst taxa as well as cysts produced by heterotrophic dinoflagellates to predominantly outer-neritic/oceanic autotrophic taxa. This transition reflects the progressive deepening of the western Tasmanian continental margin, an interpretation supported by our new seismic investigations. The dominance of autotrophic species like Spiniferites spp. and Operculodinium spp. reflects relatively oligotrophic conditions, like those of regions north of the modern-day STF. The increased abundance in the earliest Miocene of Nematosphaeropsis labyrinthus, typical for modern subantarctic zone (frontal) conditions, indicates a cooling and/or closer proximity of the STF to the site . The absence of major shifts in dinocyst assemblages contrasts with other records in the region and suggests that small changes in surface oceanographic conditions occurred during the Oligocene. Despite the relatively southerly (63-55 degrees S) location of Site 1168, the rather stable oceanographic conditions reflect the continued influence of the proto-Leeuwin Current along the southern Australian coast as Australia continued to drift northward. The relatively "warm" dinocyst assemblages at ODP Site 1168, compared with the cold assemblages at Antarctic Integrated Ocean Drilling Program (IODP) Site U1356, testify to the establishment of a pronounced latitudinal temperature gradient in the Oligocene Southern Ocean.	[Hoem, Frida S.; Sauermilch, Isabel; Hou, Suning; Brinkhuis, Henk; Sangiorgi, Francesca; Bijl, Peter K.] Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, Utrecht, Netherlands; [Brinkhuis, Henk] Royal Netherlands Inst Sea Res NIOZ, Texel, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Hoem, FS (通讯作者)，Univ Utrecht, Dept Earth Sci, Marine Palynol & Paleoceanog, Utrecht, Netherlands.	f.s.hoem@uu.nl	Brinkhuis, Henk/IUO-8165-2023	Hou, Suning/0000-0002-8902-6367; Hoem, Frida/0000-0002-8834-6799; Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012	Dutch Research councile, Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO) polar programme [ALW.2016.001]; European Research Council [802835]; European Research Council (ERC) [802835] Funding Source: European Research Council (ERC)	Dutch Research councile, Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO) polar programme; European Research Council(European Research Council (ERC)); European Research Council (ERC)(European Research Council (ERC))	This research has been supported by the Dutch Research councile, Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO) polar programme (grant no. ALW.2016.001), and the European Research Council, H2020 programme (grant no. OceaNice 802835).	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J	Galloway, JM; Fensome, RA; Swindles, GT; Hadlari, T; Fath, J; Schroder-Adams, C; Herrle, JO; Pugh, A				Galloway, Jennifer M.; Fensome, Robert A.; Swindles, Graeme T.; Hadlari, Thomas; Fath, Jared; Schroder-Adams, Claudia; Herrle, Jens O.; Pugh, Adam			Exploring the role of High Arctic Large Igneous Province volcanism on Early Cretaceous Arctic forests	CRETACEOUS RESEARCH			English	Article						Cretaceous; Arctic; Palynology; Paleoecology; High Arctic Large Igneous Province; OAE 1a	SEA-SURFACE TEMPERATURES; CARBON-ISOTOPE EVENT; APTIAN BLACK SHALES; AXEL-HEIBERG ISLAND; U-PB GEOCHRONOLOGY; SVERDRUP BASIN; FOSSIL ASSEMBLAGES; TERTIARY BOUNDARY; CLIMATE-CHANGE; BARENTS SEA	The HauterivianeAptian Isachsen Formation at Glacier Fiord, Axel Heiberg Island, in the Sverdrup Basin of the Canadian Arctic Archipelago was deposited contemporaneous with initiation of the High Arctic Large Igneous Province (HALIP). New palynological biostratigraphy and paleoenvironmental reconstruction, in coordination with the emerging geochronology of HALIP igneous rocks, permits exploration of the effects of volcanism on Arctic vegetation during the Early Cretaceous. Four informal terrestrial palynofloral zones are defined and used to reconstruct vegetation change over the Isachsen Formation's ca. 17 million year history and explore the role of the HALIP in these changes. Climate warming during the Hauterivian promoted expansion of a hinterland community dominated by members of the Pinaceae. By the middle Barremian, this community was replaced by mixed heathland and mire, represented by up to 70% fern spores in the uppermost Paterson Island Member, that may be, in part, in response to environmental disturbance associated with volcanic flows of the HALIP. Above the fern spore spike, dinoflagellate cyst assemblages suggest an early Aptian age and a marine setting for mudstones of the Rondon Member in which Ocean Anoxic Event 1a is recorded. An interval of floral instability is recorded in the overlying Walker Island Member, characterized by fluctuations in Pinaceae and Cupressaceae pollen and fern spores, possibly as a result of post-OAE 1a temperature variabilty and landscape disturbance associated with lava flows of the HALIP that were repeatedly extruded onto the subsiding delta plain during deposition of the member. Crown Copyright (c) 2021 Published by Elsevier Ltd. All rights reserved.	[Galloway, Jennifer M.; Hadlari, Thomas; Fath, Jared] Geol Survey Canada, Commiss Geol Canada, 3303-33 St NW, Calgary, AB T2L 2A7, Canada; [Galloway, Jennifer M.] Aarhus Univ, Aarhus Inst Adv Studies, DK-8000 Aarhus, Denmark; [Fensome, Robert A.] Geol Survey Canada, Commiss Geol Canada, Bedford Inst Oceanog, POB 1006,1 Challenger Dr, Dartmouth, NS B2Y 4A2, Canada; [Swindles, Graeme T.] Queens Univ, Sch Nat & Build Environm, Univ Rd, Belfast BT7 1NN, Antrim, North Ireland; [Schroder-Adams, Claudia; Pugh, Adam] Carleton Univ, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada; [Herrle, Jens O.] Goethe Univ Frankfurt, Inst Geosci, D-60438 Frankfurt, Germany; [Fath, Jared] Univ Alberta, Dept Renewable Resources, Edmonton, AB T6G 2R3, Canada; [Pugh, Adam] Cenovus Energy, 225 6 Ave SW, Calgary, AB T2P 0M5, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Aarhus University; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Queens University Belfast; Carleton University; Goethe University Frankfurt; University of Alberta	Galloway, JM (通讯作者)，Geol Survey Canada, Commiss Geol Canada, 3303-33 St NW, Calgary, AB T2L 2A7, Canada.	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Res.	JAN	2022	129								105022	10.1016/j.cretres.2021.105022	http://dx.doi.org/10.1016/j.cretres.2021.105022		OCT 2021	26	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	WP2YD		Green Accepted, Bronze			2025-03-11	WOS:000713002200001
J	Rodrigues, RV; Patil, JS				Rodrigues, Roy Valentino; Patil, Jagadish Siddalingappa			Salinity changes may influence dinoflagellate cyst morphometry: data from monsoon-influenced tropical coastal ecosystems	JOURNAL OF PLANKTON RESEARCH			English	Article						dinoflagellate; cyst morphometry; Pyrophacus steinii; Protoperidinium pentagonum; salinity; estuarine; marine	STEINII SCHILLER WALL; SPATIAL-DISTRIBUTION; RECENT SEDIMENTS; RESTING CYSTS; LIFE-CYCLE; WEST-COAST; BALTIC SEA; BLACK-SEA; MORPHOLOGY; DINOPHYCEAE	Generally, dinoflagellate cyst morphology is species specific. Their variability due to environmental factors (temperature and salinity) makes them potential proxies for such factors. However, there is a dearth of information on the variability of cystmorphology from monsoon-influenced coastal ecosystems. This study on distribution and variability in the dinocyst morphometry of Pyrophacus steinii and Protoperidinium pentagonum from estuarine (Cochin port and Zuari estuary) and marine (New Mangalore port) ecosystems along the Indian west coast revealed that both are common and euryhaline species. However, variability in cyst morphometry was observed and correlated salinity values between the ecosystems. Other parameters (i.e. the prevalence of narrow temperature ranges and nutrient-rich conditions) may not be dominant in influencing cysts morphometry. Cyst length, breadth and processes length (only in P. steinii) of both were relatively larger and smaller at salinity ranges higher and lower than 25 psu, respectively. The data presented for different ecosystems are comparable in most parameters except salinity variations. This study extends the ranges of records for both species. Pyrophacus steinii cysts were significantly larger (up to 120 mu m in Zuari estuary) than literature reports on cysts from higher salinity systems and salinity-related variability in P. pentagonum cyst size indicates notable potential proxy indicator of salinity.	[Rodrigues, Roy Valentino; Patil, Jagadish Siddalingappa] CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India; [Rodrigues, Roy Valentino] Goa Univ, Sch Earth Ocean & Atmospher Sci, Taleigao Plateau 403206, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO); Goa University	Patil, JS (通讯作者)，CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India.	patilj@nio.org			DG Shipping, Ministry of Shipping, Govt. of India [GAP 2429]	DG Shipping, Ministry of Shipping, Govt. of India	DG Shipping, Ministry of Shipping, Govt. of India funded project Ballast Water Management Program India-BAMPI (GAP 2429).	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Plankton Res.	NOV-DEC	2021	43	6					853	864		10.1093/plankt/fbab072	http://dx.doi.org/10.1093/plankt/fbab072		OCT 2021	12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	XO1OH					2025-03-11	WOS:000729961900009
J	Iakovleva, AI; Quesnel, F; Dupuis, C				Iakovleva, Alina I.; Quesnel, Florence; Dupuis, Christian			New insights on the Late Paleocene - Early Eocene dinoflagellate cyst zonation for the Paris and Dieppe basins	BSGF-EARTH SCIENCES BULLETIN			English	Article						dinoflagellate cysts; Late Paleocene; Early Eocene; "Sparnacian"; zonation; Paris and Dieppe-Hampshire basins	BIOSTRATIGRAPHY; STRATIGRAPHY	The Anglo-Belgo-Paris Basin, historical cradle of the Paleogene stratigraphy since the 19th century, is known by the presence of very specific so-called "Sparnacian" deposits (very diverse and laterally highly variable, predominantly lagoonal to terrestrial facies), which encompass the short stratigraphic interval of the Paleocene-Eocene Thermal Maximum (PETM). Due to the insufficient nature of the paleontological record, the "Sparnacian" succession of the Paris and Dieppe-Hampshire basins still needs to be robustly chronostratigraphically correlated with other Paleogene records worldwide. In order to refine the stratigraphy of the Thanetian-Lower Ypresian succession in northern France a number of cores and outcrop sections have been investigated palynologically. As a result, an updated version of the dinoflagellate cyst zonation for the Paris and Dieppe basins is proposed and contains six new or revised biozones for this stratigraphical interval: Alisocysta margarita, Apectodinium hyperacanthum, Apectodinium-acme, Biconidinium longissimum-acme, Dracodinium astra, and Axiodinium lunare/Stenodinium meckelfeldense. Based on combined bio-, litho- and chemostratigraphic data, it appears that the dinocyst assemblages, corresponding to the PETM event interval ("Sparnacian" deposits, Soissonnais and upper Mortemer formations), are characterized by an acme of Apectodinium spp. (70-98%) in both basins, sometimes alternating with an acme of a few gonyaulacoid groups in the Dieppe Basin. Dinocyst assemblages from the PETM interval contain a significant number of atypical, longer specimens of Apectodinium parvum, which could represent an ecological onshore substitute for Axiodinium augustum in the Paris and Dieppe-Hampshire basins. The establishment of a new Biconidinium longissimum-acme Zone suggests that the stratigraphic hiatus previously inferred within this sequence in the Paris Basin does not exist.	[Iakovleva, Alina I.] Russian Acad Sci, Geol Inst, Pyzhevsky Pereulok 7, Moscow 119017, Russia; [Quesnel, Florence] BRGM French Geol Survey, DGR CGEO, BP 36009, F-45060 Orleans 2, France; [Quesnel, Florence] Univ Orleans, CNRS, UMR 7327, ISTO,INSU, Campus Geosci 1A,Rue Ferollerie, F-45071 Orleans 2, France; [Dupuis, Christian] Univ Mons, Fundamental & Appl Geol, 9 Rue Houdain, B-7000 Mons, Belgium	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Bureau de Recherches Geologiques et Minieres (BRGM); Bureau de Recherches Geologiques et Minieres (BRGM); Centre National de la Recherche Scientifique (CNRS); Universite de Orleans; CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Mons	Iakovleva, AI (通讯作者)，Russian Acad Sci, Geol Inst, Pyzhevsky Pereulok 7, Moscow 119017, Russia.	alina.iakovleva@gmail.com	QUESNEL, Florence/AAR-9253-2021	IAKOVLEVA, Alina Igorevna/0000-0001-8569-1880; QUESNEL, florence/0000-0002-4081-1911	BRGM PaleoScene research project; BRGM "Paleosurface eocene-PETM" research project; BRGM "Regolithe" Scientific Program; Geological Institute, Russian Academy of Sciences [0135-2019-0045]	BRGM PaleoScene research project; BRGM "Paleosurface eocene-PETM" research project; BRGM "Regolithe" Scientific Program; Geological Institute, Russian Academy of Sciences	Dinocyst study from the Paris and Dieppe-Hampshire basins was financially supported by the BRGM PaleoScene and "Paleosurface eocene-PETM" research projects, the BRGM "Regolithe" Scientific Program and since mid-2018 by the Paris Basin Research Projects of the "Referentiel Geologique de la France" Program, of which it is the first publication. The research of AI was also supported by the Russian State Program No.0135-2019-0045 (Geological Institute, Russian Academy of Sciences). We thank Jean-Jacques Chateauneuf (now retired from the BRGM) for his precious help during the search for some samples of the historical BRGM cores. We are also grateful to the British Geological Survey, particularly James Riding and Tracey Gallagher for the access to the BGS core material. Two anonymous reviewers are thanked for very helpful remarks and advices on the manuscript.	[Anonymous], 1829, TABLEAU TERRAINS QUI; [Anonymous], 1880, B SOC GEOLOGIQUE NOR; AUBRY M., 2005, STRATIGRAPHY, V2, P65; Aubry M. -P., 1983, BIOSTRATIGRAPHIE PAL; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; Bignot G., 1965, Bull. Soc. geol. 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Bull.	OCT 19	2021	192								44	10.1051/bsgf/2021035	http://dx.doi.org/10.1051/bsgf/2021035			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	WI9AL		Green Published, gold			2025-03-11	WOS:000708645900005
J	McLachlan, SMS; Pospelova, V				McLachlan, Sandy M. S.; Pospelova, Vera			Calcareous dinoflagellate cyst distribution across the K/Pg boundary at DSDP site 577, Shatsky Rise, western North Pacific Ocean	MARINE MICROPALEONTOLOGY			English	Article						Cretaceous; Paleogene; Paleocene; Danian; Pacific Ocean; Shatsky rise; DSDP	CRETACEOUS-TERTIARY BOUNDARY; SEA-DRILLING-PROJECT; PLATINUM-GROUP ELEMENTS; DANIAN STAGE PALEOCENE; PALEOGENE BOUNDARY; MASS EXTINCTION; SURFACE SEDIMENTS; BENTHIC FORAMINIFERA; SPATIAL-DISTRIBUTION; MARINE PRODUCTIVITY	An analysis of calcareous dinoflagellate cysts has been carried out on sixteen samples from across the K/Pg boundary interval from Deep Sea Drilling Project Site 577 situated on Shatsky Rise in the western North Pacific. This is the first time that a detailed study of this microfossil group has been undertaken from deep sea sediments of Late Cretaceous-early Paleocene age in the North Pacific realm. Eight species of calcareous dinoflagellate cysts were found to comprise low diversity assemblages of which half are representative of extant taxa. The most pronounced bioevent is that of Cervisiella operculata reaching its highest proportions at the K/Pg boundary transition underscoring the utility and cosmopolitan distribution of the species with its acme as a marker for the earliest Danian. We also identify an indirect sea surface paleotemperature signal as represented by variance in wall thickness in two distinct morphotypes of Thoracosphaera heimii (morphotypes A and B). The cyst concentrations and relative abundances of these taxa are interpreted to reflect the late Maastrichtian warming event and subsequent late Maastrichtian cooling phase prior to the interval of gradual warming in the early Danian marked by the opportunistic capitalization of Cervisiella operculata during a time of ocean recovery following the terminal Cretaceous.	[McLachlan, Sandy M. S.; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, STN CSC, POB 1700, Victoria, BC V8W 2Y2, Canada; [Pospelova, Vera] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA	University of Victoria; University of Minnesota System; University of Minnesota Twin Cities	McLachlan, SMS (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, STN CSC, 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	National Science and Engineering Research Council, Ottawa, Canada; Geological Society of America, Boulder, Colorado, U.S.A.; Paleontological Research Institute, Ithaka, New York, U.S.A.	National Science and Engineering Research Council, Ottawa, Canada; Geological Society of America, Boulder, Colorado, U.S.A.; Paleontological Research Institute, Ithaka, New York, U.S.A.	The authors would like to thank the staff of the International Ocean Discovery Program's Gulf Coast Repository, Texas A&M University (College Station, Texas, USA), for supplying the DSDP material used in this study. Gratitude is also extended to Dr. Elaine Humphrey, Advanced Microscopy Facility, University of Victoria (Victoria, BC, Canada), for lending technical assistance with SEM imaging and Dr. Jon Husson, School of Earth and Ocean Sciences, University of Victoria (Victoria, BC, Canada), for discussions relating to data presentation. The manuscript benefited greatly from feedback provided by Dr. Manuel Vieira, Shell UK Ltd., and an anonymous reviewer. Funding for this project was provided by the National Science and Engineering Research Council, Ottawa, Canada, the Geological Society of America, Boulder, Colorado, U.S.A., and the Paleontological Research Institute, Ithaka, New York, U.S.A.	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F., 2005, Palaeontologische Zeitschrift, V79, P61	188	1	1	0	2	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	SEP	2021	168								102057	10.1016/j.marmicro.2021.102057	http://dx.doi.org/10.1016/j.marmicro.2021.102057		OCT 2021	18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	WM9UA					2025-03-11	WOS:000711422200002
J	Shin, HH; Li, Z; Kim, HJ; Park, BS; Lee, J; Shin, AY; Park, TG; Lee, KW; Han, KH; Youn, JY; Kwak, KY; Seo, MH; Kim, D; Son, MH; Kim, DJ; Shin, K; Lim, WA				Shin, Hyeon Ho; Li, Zhun; Kim, Hyun Jung; Park, Bum Soo; Lee, Jihoon; Shin, A-Young; Park, Tae-Gyu; Lee, Kyun-Woo; Han, Kyung Ha; Youn, Joo Yeon; Kwak, Kyung Yoon; Seo, Min Ho; Kim, Daekyung; Son, Moon Ho; Kim, Dug-Jin; Shin, Kyoungsoon; Lim, Weol-Ae			<i>Alexandrium catenella</i> (Group I) and <i>A</i>. <i>pacificum</i> (Group IV) cyst germination, distribution, and toxicity in Jinhae-Masan Bay, Korea	HARMFUL ALGAE			English	Article						Germination temperature; Ellipsoidal alexandrium cyst; Morphology; Phylogeny; GTX-3; GTX-4	SPECIES COMPLEX DINOPHYCEAE; PARALYTIC SHELLFISH TOXINS; TAMARENSE RESTING CYSTS; GENUS ALEXANDRIUM; DINOFLAGELLATE CYSTS; YELLOW SEA; FUNDYENSE; SAXITOXIN; DYNAMICS; BLOOMS	To better understand the outbreaks of paralytic shellfish poisoning and bloom dynamics caused by Alexandrium species in Jinhae-Masan Bay, Korea, the germination and distributions of ellipsoidal Alexandrium cysts were investigated, and paralytic shellfish toxins (PSTs) profiles and contents were determined using strains established from germling cells. The phylogeny and morphological observations revealed that the germinated vegetative cells from ellipsoidal cysts collected from the surface sediments in Jinhae-Masan Bay belong to Alexandrium catenella (Group I) and A. pacificum (Group IV) nested within A. tamarense species complex. Cyst germinations of A. catenella (Group I) were observed at only 10 degrees C, whereas cysts of A. pacificum (Group IV) could germinate at temperature ranges of 10 to 25 degrees C. Maximum germination success (85%) for isolated cysts occurred at 15 degrees C, and the germling cells were A. pacificum (Group IV). The results indicate that the variation in water temperature in Jinhae-Masan Bay can control the seasonal variations in germination of cysts of A. catenella (Group I) and A. pacificum (Group IV). The germination rates of ellipsoidal Alexandrium cysts were different among sampling sites in Jinhae-Masan Bay, probably because of differences in distribution and abundance of A. catenella (Group I) and A. pacificum (Group IV) in the sediments. The ellipsoidal Alexandrium cyst concentrations were much higher in February than in August, however the distributions were similar. Gonyautoxins 3 and 4 (GTX-3 and GTX-4) contributed a large proportion (>90%) of the toxins produced by strains A. catenella (Group I) and A. pacificum (Group IV) established from germling cells, and the total cellular contents were higher in A. catenella (Group I) than in A. pacificum (Group IV).	[Shin, Hyeon Ho; Kim, Hyun Jung; Han, Kyung Ha; Youn, Joo Yeon; Kwak, Kyung Yoon] Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea; [Li, Zhun] Korea Res Inst Biosci & Biotechnol, Korean Collect Type Cultures KC, Biol Resource Ctr, Jeonbuk 56212, South Korea; [Han, Kyung Ha] Pukyong Natl Univ, Busan 48513, South Korea; [Park, Bum Soo] Korea Inst Ocean Sci & Technol, Marine Ecosyst Res Ctr, Busan 49111, South Korea; [Lee, Jihoon; Shin, A-Young; Lee, Kyun-Woo] Korea Inst Ocean Sci & Technol, Marine Biotechnol Res Ctr, Busan 49111, South Korea; [Park, Tae-Gyu] Natl Inst Fisheries Sci, Tongyeong 53085, South Korea; [Seo, Min Ho] Marine Ecol Res Ctr, Yeosu 59697, South Korea; [Kim, Daekyung] Korea Basic Sci Inst KBSI, Biol Daegu Ctr, Daegu, South Korea; [Son, Moon Ho; Lim, Weol-Ae] Natl Inst Fisheries Sci, Busan 619705, South Korea; [Kim, Dug-Jin] Korea Inst Ocean Sci & Technol, Marine Observat Team, Geoje 656830, South Korea; [Shin, Kyoungsoon] Korea Inst Ocean Sci & Technol, Ballast Water Res Ctr, Geoje 53201, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Research Institute of Bioscience & Biotechnology (KRIBB); Pukyong National University; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST); National Institute of Fisheries Science; Korea Basic Science Institute (KBSI); National Institute of Fisheries Science; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Shin, HH (通讯作者)，Korea Inst Ocean Sci & Technol, Lib Marine Samples, Geoje 656830, South Korea.	shh961121@kiost.ac.kr	Park, Bum/W-3178-2017; Li, Zhun/IUQ-5309-2023	LI, ZHUN/0000-0001-8961-9966; Shin, A-Young/0000-0002-9799-7999; Shin, Hyeon Ho/0000-0002-9711-6717	MarineBiotics project - Ministry of Oceans and Fisheries [20210469]; NIFS [R2021064]; KIOST [PE99921]	MarineBiotics project - Ministry of Oceans and Fisheries; NIFS; KIOST	This work was supported by grants from MarineBiotics project (20210469) funded by the Ministry of Oceans and Fisheries, NIFS (R2021064) and KIOST (PE99921) projects. Two anonymous reviewers are thanked for constructive suggestions that greatly improved the manuscript.	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J	Liu, YY; Deng, YY; Shang, LX; Yi, L; Hu, ZX; Tang, YZ				Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Yi, Liang; Hu, Zhangxi; Tang, Ying Zhong			Geographic distribution and historical presence of the resting cysts of <i>Karenia mikimotoi</i> in the seas of China	HARMFUL ALGAE			English	Article						Harmful algal blooms (HABs); Karenia mikimotoi; Resting cyst; Cyst mapping; Historical presence	DINOFLAGELLATE COCHLODINIUM-POLYKRIKOIDES; TIME PCR ASSAY; RED TIDE; GONYAULAX-TAMARENSIS; BLOOM; EUTROPHICATION; DINOPHYCEAE; GULF; BAY; IDENTIFICATION	The toxic dinoflagellate Karenia mikimotoi frequently forms harmful algal blooms (HABs) and thus causes massive kills of fish and shellfish in worldwide coastal waters, which has led to intensive investigations on multiple facets of the species. Following our recent discovery of K. mikimotoi forming resting cyst, a very possible mechanism for the inoculation of blooms and geographic expansion for this and many other HABs-causing species, here we report our detection of K. mikimotoi resting cysts in 125 surface sediment samples collected from the coastal waters (covering a latitude range from 18.29 degrees N to 39.85 degrees N) and 3 sediment cores (accumulated in 70-100 years) collected from the East China Sea where are adjacent to the frequent blooming areas of K. mikimotoi. Via applications of quantitative real-time PCR (LSU rDNA-targeted), species-specific fluorescence in situ hybridization (FISH), and nested-PCR-and-sequencing to both types of the sediment samples that were pretreated with sodium polytungstate solution (SPT), we demonstrated that 1) K. mikimotoi cysts are widely present in surface sediments of the China seas (Bohai Sea (BS), Yellow Sea (YS), East China Sea (ECS), and South China Sea (SCS)), 2) the abundance of cysts is generally low (0 to 33 cysts in 32 g wet sediment), with that in the ECS and the SCS being higher than that in the YS and the BS, and the highest abundance was observed in sites of the ECS (e.g., Ningde, Fujian province) where the blooms of the species occurred frequently, as quantified by both methods, and 3) the cysts of K. mikimotoi have been present in the sediments of the ECS since 1970s, a short time prior to the first recorded bloom of K. mikimotoi in the SCS at 1980s. Our results not only demonstrated the wide geographic distribution of resting cyst of K. mikimotoi along the coast of China, but also proved a 50 years preservation of the cysts in the sediments of coastal area prone to forming frequent blooms. We consider our results have provided critical insights into the mechanisms of frequent bloom outbreaks and global distribution of K. mikimotoi in general, and particularly into the historical origin of K. mikimotoi in China. Further investigations are suggested to focus on on-site surveys for the cyst production and germination rates.	[Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Hu, Zhangxi; Tang, Ying Zhong] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China; [Liu, Yuyang; Deng, Yunyan; Shang, Lixia; Hu, Zhangxi; Tang, Ying Zhong] Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China; [Yi, Liang] Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Laoshan Laboratory; Chinese Academy of Sciences; Tongji University	Hu, ZX; Tang, YZ (通讯作者)，Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.; Hu, ZX; Tang, YZ (通讯作者)，Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266237, Peoples R China.; Hu, ZX; Tang, YZ (通讯作者)，Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China.	zhu@qdio.ac.cn; yingzhong.tang@qdio.ac.cn	ZHANG, hui jie/HTN-1690-2023; Li, Yang/KFB-5350-2024; Yi, Liang/AAM-9737-2020	Hu, Zhangxi/0000-0002-4742-4973				Al-Kandari MA, 2011, HARMFUL ALGAE, V10, P636, DOI 10.1016/j.hal.2011.04.017; ANDERSON DM, 1989, ICLARM CONT, V21, P81; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anderson DM, 2014, DEEP-SEA RES PT II, V103, P6, DOI 10.1016/j.dsr2.2013.10.002; [Anonymous], 2013, HARMFUL MARINE MICRO; Chen BH, 2021, ESTUAR COAST SHELF S, V249, DOI 10.1016/j.ecss.2020.107034; Brand LE, 2012, HARMFUL ALGAE, V14, P156, DOI 10.1016/j.hal.2011.10.020; Bravo Isabel, 2014, Microorganisms, V2, P11; Brosnahan ML, 2017, LIMNOL OCEANOGR, V62, P2829, DOI 10.1002/lno.10664; Cosgrove S, 2014, HARMFUL ALGAE, V31, P114, DOI 10.1016/j.hal.2013.10.015; Dai L, 2020, HARMFUL ALGAE, V93, DOI 10.1016/j.hal.2020.101794; Dai XF, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0064188; 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J	Baek, SS; Pyo, J; Kwon, YS; Chun, SJ; Baek, SH; Ahn, CY; Oh, HM; Kim, YO; Cho, KH				Baek, Sang-Soo; Pyo, JongCheol; Kwon, Yong Sung; Chun, Seong-Jun; Baek, Seung Ho; Ahn, Chi-Yong; Oh, Hee-Mock; Kim, Young Ok; Cho, Kyung Hwa			Deep Learning for Simulating Harmful Algal Blooms Using Ocean Numerical Model	FRONTIERS IN MARINE SCIENCE			English	Article						harmful algal blooms; deep learning; convolutional neural network; classification; regression	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; TOXIC DINOFLAGELLATE; TRANSPORT PATHWAYS; FRESH-WATER; BAY; CATENELLA; SALINITY; CYST; DINOPHYCEAE; GERMINATION	In several countries, the public health and fishery industries have suffered from harmful algal blooms (HABs) that have escalated to become a global issue. Though computational modeling offers an effective means to understand and mitigate the adverse effects of HABs, it is challenging to design models that adequately reflect the complexity of HAB dynamics. This paper presents a method involving the application of deep learning to an ocean model for simulating blooms of Alexandrium catenella. The classification and regression convolutional neural network (CNN) models are used for simulating the blooms. The classification CNN determines the bloom initiation while the regression CNN estimates the bloom density. GoogleNet and Resnet 101 are identified as the best structures for the classification and regression CNNs, respectively. The corresponding accuracy and root means square error values are determined as 96.8% and 1.20 [log(cells L-1)], respectively. The results obtained in this study reveal the simulated distribution to follow the Alexandrium catenella bloom. Moreover, Grad-CAM identifies that the salinity and temperature contributed to the initiation of the bloom whereas NH4-N influenced the growth of the bloom.	[Baek, Sang-Soo; Cho, Kyung Hwa] Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, Ulsan, South Korea; [Pyo, JongCheol] Korea Environm Inst, Ctr Environm Data Strategy, Sejong, South Korea; [Kwon, Yong Sung] Natl Inst Ecol, Div Ecol Assessment Res, Natl Inst Ecol, Environm Impact Assessment Team, Seocheon, South Korea; [Chun, Seong-Jun] Natl Inst Ecol NIE, LMO Res Team, Bur Ecol Res, Seocheon, South Korea; [Baek, Seung Ho] Korea Inst Ocean Sci & Technol, Risk Assessment Res Ctr, Geoje, South Korea; [Ahn, Chi-Yong; Oh, Hee-Mock] Korea Res Inst Biosci & Biotechnol KRIBB, Cell Factory Res Ctr, Daejeon, South Korea; [Kim, Young Ok] Korea Inst Ocean Sci & Technol, Marine Ecosyst Res Ctr, Busan, South Korea	Ulsan National Institute of Science & Technology (UNIST); Korea Environment Institute (KEI); National Institute of Ecology; Korea Institute of Ocean Science & Technology (KIOST); Korea Research Institute of Bioscience & Biotechnology (KRIBB); Korea Institute of Ocean Science & Technology (KIOST)	Cho, KH (通讯作者)，Ulsan Natl Inst Sci & Technol, Sch Urban & Environm Engn, Ulsan, South Korea.; Kim, YO (通讯作者)，Korea Inst Ocean Sci & Technol, Marine Ecosyst Res Ctr, Busan, South Korea.	yokim@kiost.ac.kr; khcho@unist.ac.kr	Ahn, Chi-Yong/AAI-8370-2020; KIM, YOUNG JIN/E-9374-2011; Baek, SangSoo/LFT-3581-2024	Pyo, JongCheol/0000-0001-9204-5879; Chun, Seong Jun/0000-0001-7037-6968	Ministry of Science, ICT & Future Planning [NRF-2016M1A5A1027457]; Korean Institute of Ocean Science and Technology [PE99912]	Ministry of Science, ICT & Future Planning(Ministry of Science, ICT & Future Planning, Republic of Korea); Korean Institute of Ocean Science and Technology	Funding This study was supported by the Ministry of Science, ICT & Future Planning (grant NRF-2016M1A5A1027457) and Korean Institute of Ocean Science and Technology (PE99912).	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Mar. Sci.	OCT 12	2021	8								729954	10.3389/fmars.2021.729954	http://dx.doi.org/10.3389/fmars.2021.729954			13	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	WP6NC		Green Published, gold			2025-03-11	WOS:000713244900001
J	Anderson, DM; Fachon, E; Pickart, RS; Lin, PG; Fischer, AD; Richlen, ML; Uva, V; Brosnahan, ML; McRaven, L; Bahr, F; Lefebvre, K; Grebmeier, JM; Danielson, SL; Lyu, YH; Fukai, Y				Anderson, Donald M.; Fachon, Evangeline; Pickart, Robert S.; Lin, Peigen; Fischer, Alexis D.; Richlen, Mindy L.; Uva, Victoria; Brosnahan, Michael L.; McRaven, Leah; Bahr, Frank; Lefebvre, Kathi; Grebmeier, Jacqueline M.; Danielson, Seth L.; Lyu, Yihua; Fukai, Yuri			Evidence for massive and recurrent toxic blooms of <i>Alexandrium catenella</i> in the Alaskan Arctic	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA			English	Article						harmful algal bloom; HAB; Alexandrium; Alaskan Arctic; climate	CHUKCHI-SEA; DINOFLAGELLATE CYSTS; RESTING CYSTS; FUNDYENSE BLOOMS; PACIFIC WATER; TIME-SERIES; GULF; MAINE; DINOPHYCEAE; PATTERNS	Among the organisms that spread into and flourish in Arctic waters with rising temperatures and sea ice loss are toxic algae, a group of harmful algal bloom species that produce potent biotoxins. Alexandrium catenella, a cyst-forming dinoflagellate that causes paralytic shellfish poisoning worldwide, has been a significant threat to human health in southeastern Alaska for centuries. It is known to be transported into Arctic regions in waters transiting northward through the Bering Strait, yet there is little recognition of this organism as a human health concern north of the Strait. Here, we describe an exceptionally large A. catenella benthic cyst bed and hydrographic conditions across the Chukchi Sea that support germination and development of recurrent, locally originating and self-seeding blooms. Two prominent cyst accumulation zones result from deposition promoted by weak circulation. Cyst concentrations are among the highest reported globally for this species, and the cyst bed is at least 6x larger in area than any other. These extraordinary accumulations are attributed to repeated inputs from advected southern blooms and to localized cyst formation and deposition. Over the past two decades, warming has likely increased the magnitude of the germination flux twofold and advanced the timing of cell inoculation into the euphotic zone by 20 d. Conditions are also now favorable for bloom development in surface waters. The region is poised to support annually recurrent A. catenella blooms that are massive in scale, posing a significant and worrisome threat to public and ecosystem health in Alaskan Arctic communities where economies are subsistence based.	[Anderson, Donald M.; Fachon, Evangeline; Fischer, Alexis D.; Richlen, Mindy L.; Uva, Victoria; Brosnahan, Michael L.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Pickart, Robert S.; Lin, Peigen; McRaven, Leah; Bahr, Frank] Woods Hole Oceanog Inst, Phys Oceanog Dept, Woods Hole, MA 02543 USA; [Lefebvre, Kathi] NOAA, Environm & Fisheries Sci Div, Northwest Fisheries Sci Ctr, Natl Marine Fisheries Serv, Seattle, WA 98112 USA; [Grebmeier, Jacqueline M.] Univ Maryland, Chesapeake Biol Lab, Ctr Environm Sci, Solomons, MD 20688 USA; [Danielson, Seth L.] Univ Alaska Fairbanks, Coll Fisheries & Ocean Sci, Fairbanks, AK 99775 USA; [Lyu, Yihua] State Ocean Adm, South China Sea Environm Monitoring Ctr, Guangzhou 510300, Peoples R China; [Fukai, Yuri] Hokkaido Univ, Grad Sch Environm Sci, Sapporo, Hokkaido 0600810, Japan	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; National Oceanic Atmospheric Admin (NOAA) - USA; University System of Maryland; University of Maryland Center for Environmental Science; University of Alaska System; University of Alaska Fairbanks; Hokkaido University	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Fischer, Alexis/M-4531-2019; Grebmeier, Jacqueline/L-9805-2013	McRaven, Leah/0000-0002-4552-4313; Bahr, Frank/0000-0002-1736-309X; Anderson, Donald/0000-0002-3983-6388; Brosnahan, Michael/0000-0002-2620-7638; Fachon, Evangeline/0000-0003-2933-7283; Lin, Peigen/0000-0002-2410-976X; Grebmeier, Jacqueline/0000-0001-7624-3568	NSF Office of Polar Programs [OPP-1823002, OPP-1733564]; National Ocanic and Atmospheric Administration (NOAA) Arctic Research program (through the Cooperative Institute for the North Atlantic Region [CINAR] [NA14OAR4320158, NA19OAR4320074]; University of Maryland Center for Environmental Science [CINAR 22309.07 UMCES]; NOAA's Center for Coastal and Ocean Studies Ecology and Oceanography of Harmful Algal Blooms (ECOHAB) Program [NA20NOS4780195]; NSF [OCE-1840381]; NIH through the Woods Hole Center for Oceans and Human Health [1P01-ES028938-01]; North Pacific Research Board IERP [A91-99a, A91-00a]; National Institute of Environmental Health Sciences [P01ES028938] Funding Source: NIH RePORTER	NSF Office of Polar Programs(National Science Foundation (NSF)); National Ocanic and Atmospheric Administration (NOAA) Arctic Research program (through the Cooperative Institute for the North Atlantic Region [CINAR]; University of Maryland Center for Environmental Science; NOAA's Center for Coastal and Ocean Studies Ecology and Oceanography of Harmful Algal Blooms (ECOHAB) Program; NSF(National Science Foundation (NSF)); NIH through the Woods Hole Center for Oceans and Human Health; North Pacific Research Board IERP; 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))	We acknowledge that the western and northern coasts of Alaska, along which this research was conducted, are the ancestral lands of the Yup'ik and Inupiat People past, present, and future. We honor with gratitude these lands and waters and the Yup'ik and Inupiat People. We gratefully acknowledge the following: Lee Cooper, Christina Goethel, Caitlin Meadows, and Laura Gemery for benthic sampling assistance; Matthew Capucci, Madison Shankle, and Anna Apostel for plankton sam-pling; Olga Kosnyrev and Valery Kosnyrev for cyst mapping support; Finn Morrison for cruise preparation and sample processing; Anna Mounsey for IERP sample collection; and the USCGC Healy crew and Ship-based Science Technical Support in the Arctic (STARC) technicians for general shipboard assistance. Thanks also to Hai-Feng Gu for generously providing sediments collected from the Chukchi Sea. Funding for D.M.A., R.S.P., E.F., P.L., A.D.F., V.U., M.L.B., L.M., F.B., and M.L.R. was provided by grants from the NSF Office of Polar Programs (Grants OPP-1823002 and OPP-1733564) and the National Ocanic and Atmospheric Administration (NOAA) Arctic Research program (through the Cooperative Institute for the North Atlantic Region [CINAR; Grants NA14OAR4320158 and NA19OAR4320074] ) , for J.M.G. through CINAR 22309.07 UMCES (University of Maryland Center for Environmental Science) , and for D.M.A. and K.L. through NOAA's Center for Coastal and Ocean Studies Ecology and Oceanography of Harmful Algal Blooms (ECOHAB) Program (NA20NOS4780195) . Funding for D.M.A., M.L.R., M.L.B., E.F., V.U., and A.D.F. was also provided by NSF (Grant OCE-1840381) and NIH (Grant 1P01-ES028938-01) through the Woods Hole Center for Oceans and Human Health. S.L.D. was supported by North Pacific Research Board IERP Grants A91-99a and A91-00a. This is IERP publication ArcticIERP-41 and ECOHAB Contribution No. ECO983.	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Natl. Acad. Sci. U. S. A.	OCT 12	2021	118	41							e2107387118	10.1073/pnas.2107387118	http://dx.doi.org/10.1073/pnas.2107387118			11	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	WI8YT	34607950	Green Submitted, hybrid, Green Published			2025-03-11	WOS:000708641500009
J	Silva, WG; Souza, PA; Garcia, MJ; Carvalho, MD; Dillenburg, SR; Cancelli, RR; Kuhn, LA				Silva, Wagner G.; Souza, Paulo A.; Garcia, Maria Judite; Carvalho, Marcelo de Araujo; Dillenburg, Sergio R.; Cancelli, Rodrigo R.; Kuhn, Lidia A.			Middle to Late Holocene paleoenvironmental changes in the coastal plain of southern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Santa Catarina; Pinheira; Palynofacies; Sea-level; Paleoenvironmental changes; Holocene	TIERRA-DEL-FUEGO; RELATIVE SEA-LEVEL; GRANDE-DO-SUL; WALLED DINOFLAGELLATE CYSTS; BEAGLE CHANNEL; SANTA-CATARINA; MARINE-SEDIMENTS; LATE QUATERNARY; ORGANIC-MATTER; C/N RATIOS	The coastal plain of southern Brazil documents several environmental changes mainly related to sea-level fluctuation and climatic variations during the Quaternary. Comprehensive studies have been carried out, of local and regional scope, in order to improve the knowledge about the geological evolution of this portion of the South American. In this paper we present the results of stable isotope, palynological and palynofaciological analysis of the PSC-03 core (7744 cal yr BP - Modern) was performed to provide the sedimentary evolution of the Santa Catarina coastal plain. Palynological and palynofacies analyses revealed abundant and diversified palynological associations, including terrestrial palynomorphs (spores, pollen grains, fungi, and freshwater algae), marine elements (dinoflagellate cysts and foraminiferal linings), besides abundant phytoclasts and amorphous organic matter. Based on the combined analysis of delta C-13 isotopes (-20.7 parts per thousand to -29.6 parts per thousand) and the C/N ratio (15.5-68) of the selected samples, we deduce that the organic matter is derived from marine phytoplankton and terrestrial C3 plants. The integrated approach of palynofacies and stable isotopes (delta C-13 and C/N) analyses revealed three distinct intervals, which characterize the environmental evolution of this portion of the coastal plain. The Interval I (7744 to 2844 cal yr BP) is related to a marginal marine environment, followed by the Interval II (2857 to 2276 cal yr BP), which indicates shallow water conditions, with wetland or soggy soils, while the Interval III (2124 cal yr BP to Modern) shows a subaerial scenario, strongly influenced by arboreal forms of the Atlantic Forest. Comparisons with other sites in southeastern South America were carried out, especially from Uruguay and Argentina, showing similarities in the palynological succession, as response to broader climatic conditions.	[Silva, Wagner G.] IFRS, Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, Campus Restinga,Rua Aberto Hoffman 285, BR-91791508 Porto Alegre, RS, Brazil; [Silva, Wagner G.; Souza, Paulo A.; Kuhn, Lidia A.] Univ Fed Rio Grande do Sul, Inst Geociencias, Lab Palinol Marleni Marques Toigo, Programa Posgrad Geociencias, Ave Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Garcia, Maria Judite] Univ Sao Paulo, Inst Geociencias IGc, Dept Geol Sedimentar & Ambiental GSA, Lab Paleobot Palinol & Micropaleontol, R Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Carvalho, Marcelo de Araujo] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Lab Paleoecol Vegetal LAPAV, Museu Nacl, Quinta Boa Vista S-N, BR-20940040 Rio De Janeiro, RJ, Brazil; [Dillenburg, Sergio R.; Cancelli, Rodrigo R.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Geol Costeira & Ocean, Ave Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil	Instituto Federal do Rio Grande do Sul (IFRS); Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio Grande do Sul	Silva, WG (通讯作者)，IFRS, Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, Campus Restinga,Rua Aberto Hoffman 285, BR-91791508 Porto Alegre, RS, Brazil.	wagner.guimaraes.silva@gmail.com; paulo.alves.souza@ufrgs.br; mj-garcia@uol.com.br; mcarvalho@mn.ufrj.br; sergio.dillenburg@ufrgs.br; rodrigocancelli@hotmail.com.br; lidiaak.lak@gmail.com	Dillenburg, Sergio/C-4027-2013	Dillenburg, Sergio/0000-0003-0072-7018; Guimaraes da Silva, Wagner/0000-0002-6356-6445; Kuhn, Lidia/0000-0003-2120-1824	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [1012119]; CNPq (Brazilian Research Agency) [313440/2018-8, 304894/2016-8]; 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)); CNPq (Brazilian Research Agency)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); 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; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS, proc. 1012119) and CNPq (Brazilian Research Agency, proc. 313440/2018-8 - PAS; 304894/2016-8 - MJG) 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. 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South Am. Earth Sci.	NOV	2021	111								103514	10.1016/j.jsames.2021.103514	http://dx.doi.org/10.1016/j.jsames.2021.103514		OCT 2021	18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	WI3BE					2025-03-11	WOS:000708239400001
