National Natural Science Foundation of China(Grant No.42062011);Natural Science Foundation of Shaanxi Province of China(Grant No.2022JM-162);Natural Science Foundation in Yulin of Shaanxi Province(Grant No.2023-CXY-142);Doctoral Foundation of Yulin University(Grant No.22GK12).
The Triassic lacustrine organic-rich shale(LORS)in Member 7 of the Yanchang Formation(Carnian stage)in the southern Ordos Basin is relatively well developed.Additionally,its organic matter abundance,lake biomass and b...
supported by the National Natural Science Foundation of China(Grant Nos.42172109,41872113,42172108);China National Petroleum Corporation-China University of Petroleum(Beijing)Strategic Cooperation Science and Technology Project(Grant No.ZLZX2020-02);State's Key Project of Research and Development Plan(Grant No.2018YFA0702405);Science Foundation of China University of Petroleum(Beijing)(Grant Nos.2462020BJRC002,2462020YXZZ020)。
The Carnian Pluvial Episode(CPE)fingerprints global environmental perturbations and biological extinction on land and oceans and is potentially linked to the Wrangellia Large Igneous Province(LIP).However,the correlat...
financially supported by the National Natural Sciences Foundation of China (grant No.41762001);the Basic Research Funds Project of China Geological Survey (grant No. JYYWF201818)
Objective Critical review of the Colobodontidae reveals that this family has important research value.Colobodontidae was universally accepted as a significant taxon among all Triassic ichthyolite in 2002.However,most ...
Supported by Project of National Natural Science Foundation of China(No.41572056)
The Wulonggou area located in the Eastern Kunlun Orogen in NW China is characterized by extensive granitoid magmatism,ductile faulting and orogenic gold mineralization.The Huanglonggou granodiorite is cut by an orogen...
Support for this Mid-Carnian preparation wasprovided by a visiting professorship at the State Key Laboratory of Geobiology and Environmental Geology of the China University of Geosciences at Wuhan, China,and by a visiting-scholar sabbatical hosted by the Geosciences Australia in Canberra, Australia
Approximately 230 million years ago in the middle of the Carnian stage of the Upper Triassic, the sedimentary records in different regional basins display dramatic changes. Tropical carbonate platforms abruptly ended,...
Successive evolutionary trends control the genera Paragondolella Mosher and Meta- polygnathus Hayashi over the about 20 Ma long Aegean-Tuvalian timespan. In consideration of their evolutionary criteria, these genera h...
A rich foraminiferal assemblage,consisting of abundant Aulotortus sinuosus and A.tumidus in association with Lamelliconus multispirus,Endoteba ex gr.controversa,E.ex gr.badouxi,Endotebanella kocaeliensis,Endotriada ty...
Financial support for this study was also provided by the National Natural Science Foundation of China(Project No.40302009);Peking University.
After a slow recovery from the end-Permian extinction during the Early Triassic and rapid radiation in the Middle Triassic, evolution of organisms reached a new peak phase in the Late Triassic. The Guanling Biota from...