supported by the National Basic Research Program of China(Grant No.2011CB808800);the 111 Project(Grant No.B08030);the National Natural Science Foundation of China(Grant Nos.40621002,40830212&40921062);the Fundamental Research Funds for the Central Universities(CUG130407)
The greatest Phanerozoic mass extinction happened at the end-Permian to earliest Triassic. About 95% species, 82% genera, and more than half families became extinct, constituting the sole macro-mass extinction in geol...
Supported by the National Basic Research Program of China (No. 2006CB701400);the National Natural Science Foundation of China (Nos. 40621002,40974035,40272074);Projects of Ministry of Education of China ("111" Project B07011,IRT0546)
Detailed mineral magnetic measurements, integrated with grain-size distribution and X-ray diffraction (XRD) analyses, were made on the marine sediments of Core MD98-2172, retrieved from the Eastern Timor Sea. Values...
the National Natural Science Foundation of China (Grant Nos. 40621002, 40572019);Ministry of Education of China (Grant Nos. IRT0546, NCET-04-0727, "111" Project B07011);the National Science Foundation of USA (Grant No. EAR 0745825)
In South China, the Wuqiangxi Formation of the Banxi Group and its equivalents underlie the early Cryogenian (Sturtian) glacial deposits but their thickness varies from <200 m to >2000 m. In the Guzhang section of wes...
Ministry of Education of China (Grant Nos. IRT0546 and NCET- 04-727);the National Natural Science Foundation of China (Grant Nos. 40621002, 40572019) ;the National Science Foundation of USA (Grant No. EAR0745825)
Stable isotope analyses in sections across a shelf to basinal transect of the Ediacaran Doushantuo basin show substantial isotope variabilities. In Songlin section where sediments were deposited in an intrashelf basi...
National Natural Science Foundation of China (Grant Nos. 40621002 and 40232025);the MOE Innovative Research Team Program (Grant No. IRT0546);the "111" Project (Grant No. B08030);the China Petroleum and Chemical Corporation (Grant No. G0800-06-ZS-319)
This paper systematically investigated the conodonts from the uppermost Permian to the Lower Triassic at the Dongpan Section, Southern Guangxi, South China, and obtained abundant Late Permian conodonts from the syndep...
the National Natural Science Foundation of China (Nos. 40621002, 90714010, 40574028);the State Key Laboratory of Geological Processes and Mineral Resources (GPMR2007).
The Lower Triassic in Chaohu (巢湖) area, Anhui (安徽) Province, China, is well developed and its sequence is typical in South China. After a brief introduction of the Induan-Olenekian boundary of Chaohu, this art...