National Natural Science Foundation of China(NSFC,No.41972104)。
After the extinction of Archaeocyatha(sponges),microbial bioherms were well developed in the lower Cambrian of the Yangtze cratonic basin,especially in the Qingxudong Formation(Cambrian(Stage 4))of the Huayuan area,no...
supported by the International Innovation Resources Cooperation Project“The Precambrian last glaciation and the evolution of paleoenvironment and life on Earth”from Beijing Science and Technology Committee(Grant No.Z201100008320007);the National Natural Science Foundation of China(Grant No.42072135);the National Key Research and Development Program of China(Grant No.2016YFC601001);the China Geological Survey Project(Grant Nos.DD20190002 and DD20190005);the second-level sub-project of“Prospecting prediction and technology application demonstration in integrated exploration area”from the China Geological Survey;the mineral investigation and prospecting prediction of integrated manganese exploration area in Chengkou,Chongqing(Grant No.121201004000150017-91);the mineral geological survey of Chengkou manganese ore concentration area in Chongqing(Grant No.DD20190166-18);the integrated exploration projects in Chengkou manganese mine integrated exploration area from the Chongqing Planning and Natural Resources Bureau。
The origin process of manganese ores remains unsolved worldwide.Exploring the origins of stromatolites that contain manganese may be a key to deciphering the sedimentary environments and metallogenic processes of thes...
financially supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (No. XDA13010103);the National Natural Science Foundation of China (No. 41506061);Special Fund for Strategic Pilot Technology of Chinese Academy of Sciences (type B,No. XDB26000000)。
A comprehensive study on the accretion and diagenesis of the Permian–Triassic boundary microbialites is conducive to a better understanding of the ecological community after the end-Permian mass extinction. Here we s...
This study was supported by the National Natural Science Foundation of China(Grant No.41972320);National Major Science and Technology Projects of China(Grant No.2016ZX05004004-005);the Strategic Priority Research Program(B)of Chinese Academy of Sciences(Grant No.XDB26000000)。
The fabrics of microbialites preserved in limestones are generally better than in dolostones. What are the fabrics of the microbialites preserved in heavily dolomitized dolostones? This paper presents an example of a ...
National Major Science and Technology Projects (2016ZX05004–002,2017ZX05008–005);PetroChina Major Science and Technology Projects(2018A-01,2019B-0403);PetroChina Science and Technology Project(2019D-5009-16)。
This study describes a sequence of microbialites and volcanics of the Lower Cretaceous Shipu Group, an example of microbialites influenced by volcanic activity. It is located at Shipu town in eastern Zhejiang Province...
supported by the National Natural Science Foundation of China (Grants No. 41730320 and No. 41572001);the 111 project (B08030)
Microbialites, often considered as a signal of extreme marine environment, are common in the Lower Triassic strata of South China where they flourished in the aftermath of the end-Permian mass extinction. Early Triass...
supported by National Natural Science Foundation of China(41602166);National Scientific and Technology Major Project(2016ZX05004002-001);PetroChina Innovation Fund(2018D-5007-0105);Scientific Research Starting Project of SWPU(2017QHZ005);Shandong Provincial Key Laboratory of Depositional Mineralization(DMsMzO1TO35)
The reefs in the Xiannüdong Formation(Cambrian Series 2) are the oldest archaeocyathan–microbial bioconstructions in China,but the details of their microbial structures have not been previously described.However,a n...
Being involved in the organization of IGCP 572 field workshops in Turkey (2009), in Oman (2010), as in the following IGCP 630 field workshops in Kashmir (India, 2014) and in Armenia (2017), I co-wrote for each...
support in Southwest Petroleum University;National Scientific and Technology Major Project (Grant No. 2016ZX05004002-001);National Natural Science Foundation of China (Grant No. 41602166)
Carbonate sediments deposited in normally-oxygenated shallow ocean waters of the latest Permian period, immediately prior to the end-Permian mass extinction, contain well-developed diverse shelly faunas. After the ext...
Shallow marine carbonate sediments that formed after the end-Permian mass extinction are rich in a thin(maximum ca.15 m) deposit of microbialites.Microbial communities that constructed the microbialites have geographi...