supported by the China Geological Survey project(DD20221649);the National Natural Science Foundation of China(Nos.U19B6003,42072135,and 42172119);Chongqing Research Program of Basic Research and Frontier Technology(Grant No.cstc2021jcyj-msxm X0023);Open Fund(DGERA 20211105)of Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications of Ministry of Natural Resources,Chengdu University of Technology。
The northeastern Sichuan area in the northern Yangtze margin has unique Ediacaran geological records,especially the Doushantuo Formation(DST),and become a hot research area in recent years.However,the Cryogenian-Ediac...
Under the auspices of the National Natural Science Foundation of China(No.41971101,41571187,41071137)。
In the present work,15400 yr old geochemical records of a core from the subalpine Daping swamp are presented with the aim to examine the relationship between the chemical weathering and the climatic changes in the reg...
supported by the National Natural Science Foundation of China (Grant Nos. 41771225 & 41620104007);the Primary Supports for Scientific Research of Lanzhou University (Grant Nos. LZUJBKY-2016-254, LZUJBKY-2016-279 & LZUJBKY-2018-144);China Scholarship Council
The study of prehistoric hunter-gatherer subsistence strategies on the Tibetan Plateau is important for understanding the mechanisms and processes of human adaption to high altitude environments.But to date,only a few...
the joint support by the National Natural Science Foundation of China(41807298,41672211,41572346);the Special Project of Fundamental Scientific Research of the Institute of Geology,China Earthquake Administration(IGCEA1713)
The eastern margin of the Tibetan Plateau is characterized by frequent earthquakes; however, research of paleo-earthquakes in the area has been limited^ owing to the alpine topography and strong erosion. Detailed inve...
the Ministry of Earth Sciences of India for funding the study
Understanding the past and present changes is critical for evaluating the future climatic changes. In order to understand the paleoproductivity and depositional environments of Northern In- dian Ocean, two sediment co...
supported by JSPS KAKENHI grant numbers 23501255,21253001
We present relative sea level (RSL) curves in Antarctica derived from glacial isostatic adjustment (GIA)predictions based on the melting scenarios of the Antarctic ice sheet since the Last Glacial Maximum (LGM)g...
National Natural Science Foundation of China, No.41102112; No.41021061; Fundamental Research Funds for the Central Universities, No.CCNU12A01001; 111 Program of Chinese Ministry of Science and Technology, No.B06026
Paleoenvironmental history in the monsoonal margin in the northeast Tibetan Pla- teau provides important clue to the regional climate. Previous researches have been limited by either poor chronology or low resolution....
supported by the National Basic Research Program of China (2007CB815903);the Pilot Project of the National Knowledge Innovation Program of the Chinese Academy of Sciences (KZCX2-YW-221);the National Natural Science Foundation of China (41076030 and 40906038)
The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Ple...
Based on the analyses of Loss-on-Ignition (LOI), carbonate content and sediment characteristics, this paper reconstructs the climatic and environmental evolution of the Gahai lake area since the late Last Deglacial ...