financially supported by the Youth Innovation Promotion Association of the Chinese Academy of Sciences(Grant No.2023324);the Hubei Key Laboratory of Paleontology and Geological Environment Evolution,Wuhan Center of China Geological Survey(PEL-202301);the Science and Technology Fundamental Resources Investigation Program(Grand No.2023FY100900);the Natural Science Foundation of China(Grant No.41802018).
The Middle Devonian ostracods from the Jiwozhai patch reef in Dushan, Guizhou Province, South China were described for the first time in this study. Twenty-nine species belonging to 20 genera were identified and figur...
developed in association with the R&D project registered as Brazilian National Agency of Petroleum,Natural Gas and Biofuels—ANP 18993—6(SACL—Sedimentary geological analysis of Cretaceous carbonate successions in a Brazilian Sedimentary Basin);financial support from PETROBRAS 2023/00305—8(PALEOCLIMA project—Paleoclimatic evolution and paleobathymetry of the Southern Hemisphere during the Jurassic(Tithonian)and Cretaceous)。
Despite their potential for providing important information for paleobiogeography,studies using ostracod assemblages compiled from global datasets have been scarce so far.In this study,the paleogeographic implications...
financially supported by the Second Tibetan Plateau Scientific Expedition and Research Program(Grant No.2019QZKK0706);the National Natural Science Foundation of China(Grant Nos.41802002 and 91855205);the Strategic Priority Research Program(B)of Chinese Academy of Sciences(Grant No.XDB26000000)。
The overall occurrence,stratigraphical distribution,palaeoenvironmental and palaeobiogeographical significances of the ostracod faunas from the Silurian Pulu Formation in the Yalai West Ⅱ section,Nyalam region,southe...
financially supported by the National Natural Science Foundation of China (Grant Nos. 41802002,41872035 and 41702003);Strategic Priority Research Program (B) of Chinese Academy of Sciences(Grant No. XDB26000000)。
Ostracods are described for the first time from the red-coloured marine sandstones of Arisu section(Arisu red beds)of the Upper Ordovician Tierekeawati Formation in Kalpin area of northwestern Tarim Basin, Xinjiang Uy...
supported by EU-funded project PIRSES-GA 2009 247512;project "CLIMSEAS":Climate Change and Inland Seas:Phenomena, Feedback and Uncertainties, the Physical Science Basis;project IGCP630:"Permian-Triassic climatic and environmental extremes and biotic response"
The modern Black Sea has a mixed upper layer in the top 150-200 m of the water column, below which the water is anoxic, separated from the mixed layer by a redox boundary. There is limited vertical movement of water. ...