Supported by the National Natural Science Foundation of China(No.31470324),the Strategic Priority Program(B)of CAS(No.XDB18000000,XDB 26000000).
Recently,more attention has been paid to Glossopteris,the most significant representative fossil of the Gondwanan Supercontinent in the Paleozoic.It has been regarded as an important clade of Angiophytes on the basis ...
supported by the National Natural Science Foundation of China(Grant Nos.40739903 and 41872137)。
The in situ zircon U-Pb-Lu-Hf isotope records from end-Permian volcanic interlayers in southwest China,integrated with previous studies,restructure the evolutionary history of the Yangtze Craton from Precambrian to La...
supported by the National Natural Science Foundation of China(grants No.41402194, 41390441,41230207 and 41302177)
Objective The modem Earth is characterized by two types of orogens: collisional orogen and accretionary orogen. It is widely accepted that the Central Asian Orogenic Belt (CAOB) is made up of widespread multiple an...
supported by the National Natural Scientific Foundation of China (Nos. 40472015 and 40802001);the State Key Laboratory of Modern Paleontology and Stratigraphy (No. 083113);the postdoctoral funds of China (No. 20070420523);the State Key Laboratory of Geological Processes and Mineral Resources (GPMR200701)
A continuous Permian-Triassic boundary (PTB) section has been found and studied for the first time in Xiushui, Jiangxi Province, South China. Evidence for a large sealevel fall has been found in the horizon of 0.8 m...
In the last 15 years,the discovery of several new actinopterygian fish faunas from the Early and Middle Triassic of the Tethys,cast new light on the timing,speed and range of their recovery after the end-Permian cris...
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...
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...
Supported by the National Natural Science Foundation of China (Grant No. 40472015);the State Key Laboratory of Modern Paleontology and Stratigraphy (Grant No. 053102);as well as the Key Laboratory for Minerals and Resources, the Chinese Academy of Sciences
Spherical microfossils are present in the Hindeodus parvus zone of the Lower Triassic in Ziyun,Guizhou Province. They generally range from 0.15 to 0.30 mm across,with micritic wall and filled by micro-sparry calcites,...
This paper is supported by the National Natural Science Foundation ofChina ( Nos .40232025 ,40572002);the National Science Fund forDistinguished Young Scholars (No .40325004) .
The calimicrobialites of Chongyang (崇阳), Hubei (湖北) Province, occur above the mass extinction line in the Late Permian reef facies. Below the boundary are the sponge reef limestone, crinoid limestone and algae...
This work was partly supported by the National Natural Science Foundation of China (Grant Nos. 40072055 and 40043010).
The event Permian-Triassic boundary (EPTB) is well marked by the famous 'white clay' of bed 25 in Mei-shan Section located in Changxing county, Zhejiang province of China. In this note, the white clay as well as its o...