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...
The Late Permian succession of the Upper Indus Basin in northeastern Pakistan is represented by the carbonatedominated Zaluch Group, which consists of the Amb, Wargal and Chhidru formations, which accumulated on the s...
supported by the Natural Science Foundation of China(Nos.41572002,41830320,41272044,41472087,4183000426,41802016)
Deep-water facies sections have advantages of recording complete information across the Permian-Triassic boundary(PTB). Here we present a detailed study on the conodont biostratigraphy and carbon isotope profile range...
supported by the Foundation of the Geological Survey of China [grant no. 121201004000150021]
Samples were collected continuously and systematically from Beds 2 to 30 of the Meishan D section, and nearly 4,000 foraminiferal specimens were recognized. In total, 72 species (partially including undetermined spec...
supported by the National Natural Science Foundation of China (Grant Nos. 40839903,40921062);special funding from the GPMR
Abundant siliceous micro-fossils were found from the Dalong Formation,Xinmin section,Guizhou,which include nine species of radiolarians belonging to seven genera as well as nine types of siliceous spongy spicules.The ...
supported jointly by the National Natural Science Foundation of China (40972092);the Special Program for National Science and Technology (2008ZX05005-01-08);the United Foundation of NSFC and China's Petroleum Chemical Industry (40739902)
High resolution carbon isotope analyses of carbonate and organic carbon from Meishan, South China showed that the variation of δ13Ccarb is marked by three large positive excursions during the Changhsingian (end-Permi...
supported by the National Natural Science Foundation of China (Nos. 40839903 and 40621002);the 111 Project (No. B08030)
This article reports a radiolarian fauna from the upper Dalong(大隆) Formation,Ping-dingshan(平顶山),Chaohu(巢湖),Anhui(安徽) Province,which includes 15 genera and 23 species.One new species,Copicyntra tongi G...
NSFC Inovation Research Group Programm (Grant No. 40621002);MOE Innovative Research Team Progam (Grant No. IRT0546);"111" Project (Grant No. B08030);the SINOPEC Project (Grant No. G0800-06-ZS-319)
A well-preserved, abundant radiolarian fauna was obtained from three sections: the Dongpan, Liuqiao, and Paibi sections, in southern Guangxi, South China. Sixteen species belonging to Albaillella and Neoalbaillella, i...
the National Natural Science Foundation of China (Grant No. 40272016); the State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology,CAS (Grant No.043105)
Sedimentary environment and distribution of brachiopods during the Changhsingian in Xingwen, Si-chuan Province of the upper Yangtze region, are statistically analyzed. Changing regularity in diversity of brachiopod is...
The Global Stratotype Section and Point (GSSP) for the base-Changhsingian Stage is defined at the First Appearance Datum (FAD) of the conodont Clarkina wangi within the lineage from C. longicuspidata to C. wangi a...