Within the dicynodont genus Turfanodon,there are two recognized species,T.bogdaensis and T.jiufengensis.Both species are known by relatively complete cranial materials,but the mandibles and most postcranial bones have...
supported by the Fundamental and Commonwealth Geological Survey of Oil and Gas of China(Grant No.DD 20221662);the National Natural Science Foundation of China(NSFC)Program(Grant No.42302124).
The Late Permian was marked by a series of important geological events and widespread organic-rich black shale depositions,acting as important unconventional hydrocarbon source rocks.However,the mechanism of organic m...
supported by the National Natural Science Foundation of China(Grant nos.41172202,40839903 and 41372030);the Ministry of Education of China(Grant No.20110145130001);the 111 Project(Grant No.B08030);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan(Grant No.MSFGPMR201502)。
The Permian radiolarian zones and their correlations with conodont zones or other chronostratigraphic schemes are still under debate. In this study, four genera, 21 species and two subspecies of radiolarians together ...
Supported by National Natural Science Foundation of China(No.31670215).
The Permian is one of the most important periods during which the vegetative earth witnessed the transition from icehouse to greenhouse climate and the global environment changes.Organisms on the planet encountered gr...
financially supported by the National Key Research and Development Program(Grant No.2016YFC0601003);the scientific team foundation of Department of Geology,China Northwest University;the National Natural Science Foundation of China(Grant No.41172101)。
The calibration of sedimentary rock absolute dates is one of the difficulties in sedimentological and stratigraphic research.Since strontium(Sr)resides in seawater much longer(≈10^(6) a)than the seawater intermixing ...
This work was supported by a National Natural Science Foundation of China(Grant No.91958210);the Government Finance Level II Project(No.DD20190083);‘the 13th Five-Year Plan’National Science and Technology Major Project(No.2016ZX05034001-003).
The late Permian(Lopingian)was a crucial climate transition period from the late Paleozoic Ice Age to the early Triassic of exceptionally high temperatures.However,the origins of the third-order sea-level changes duri...
supported by the National Natural Science Foundation of China(41688103 and41425013);the Strategic Priority Research Program B of the Chinese Academy of Sciences(XDB18030505)
Precise geochronology is essential for constraining rates of sedimentary,biotic;climatic and magmatic processes over a wide range of timescales throughout Earth's history.Targets for high-precision geochronology inclu...
supported by the Euregio Science Fund (call 2014, IPN16: "The end-Permian mass extinction in the Southern and Eastern Alps: extinction rates vs taphonomic biases in different depositional environments") of the Europaregion/Euregio Tirol-Südtirol-Trentino/Tirolo-Alto Adige-Trentino;SYNTHESYS (access call 4, 2016, GB-TAF-6751: "Diversity changes of spores and pollen during the Permian-Triassic mass extinction")
Terrestrial floras underwent important changes during the Lopingian (Late Permian), Early Triassic, and Middle Triassic, i.e., before, during, and after the end-Permian mass extinction. An accurate account of these ...
supported by the National Natural Science Foundation of China(Grant No.41706063);the Basic Scientific Fund for National Public Research Institute of China(Grant No.2017Q08);the China Postdoctoral Science Foundation(Grant No.2016M602087)
The Shan 2 Member, Shan 1 Member and He 8 Member of the Mid-Late Permian Shanxi and lower Xiashihezi formations, in the southeastern Ordos Basin, together comprise -150 m of deltaic deposits. This sequence records an ...