supported by the National Key Research and Development Program of China(Grant No.2017YFA0603104);the State Key Program of the National Natural Science Foundation of China(Grant No.41531069);the Independent Scientific Research Program for Crossdisciplinary of Wuhan University(Grant No.2042017kf0209)。
Due to the scarcity of data, modeling the glacial isostatic adjustment(GIA) for Antarctica is more difficult than it is for the ancient ice sheet area in North America and Northern Europe. Large uncertainties are obse...
supported by the National Natural Science Foundation of China and Russian Foundation for Basic Research (FRBR) on “Formation, evolution and changes of Pleistocene cryogenic deposits in Eastern Asia” (Grant No. 41811530093);the Key Program of the Department of International Cooperation of the Chinese Academy of Sciences (Assessment of changes in permafrost in China, Russia and Mongolia and their impacts on key engineering infrastructures), (Permafrost extent in China during the Last Glaciation Maximum and Megathermal) of the Strategic Pilot Science and Technology Program of the Chinese Academy of Sciences (Grant No. XDA05120302);the CAS Overseas Professorship of Sergey S. Marchenko, and under the auspices of the International Permafrost Association Working Group on Global Permafrost Extent During the Last Permafrost Maximum (LPM)
The formation and evolution of permafrost in China during the last 20 ka were reconstructed on the basis of large amount of paleo-permafrost remains and paleo-periglacial evidence, as well as paleo-glacial landforms, ...
supported by the Chinese Academy of Sciences Strategic Priority Research Program (Grant No. XDA01020304);the National Natural Science Foundation of China (Grant Nos. 41730319, 41372175 & 41602361);the National Basic Research Program of China (Grant No. 2015CB953803)
Since the Last Glacial Maximum(LGM), the global climate has experienced several stages, such as cold and warming events, which provide an ideal model for evaluating climate change in the future. Based on the pollen re...
supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA20070103);the National Natural Science Foundation of China (Grant Nos. 41625018 & 41421004)
Based on numerical experiments undertaken with nine climate models, the glacier equilibrium line altitudes(ELAs)in western China during the last glacial maximum(LGM) are investigated to deepen our understanding of the...
supported by the “Strategic Priority Research Program” of the Chinese Academy of Sciences (Grant No. XDA05120103);the National Natural Science Foundation of China (Grant Nos. 41603013 & 41572163)
To date, few research have been reported on the evolution of C3/C4 vegetation in southern China, and the main mechanism influencing the evolution of C3/C4 vegetation is unclear. That makes it difficult for researchers...
supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant No. XDA05120202);the National Natural Science Foundation of China (Grant Nos. 41702184 & 41630753);the National Key Research and Development Program of China (Grant No. 2017YFA0603403);the Science Foundation of Hebei Normal University (Grant No. L2018B29)
Reconstructing the spatial patterns of regional climate and vegetation during specific intervals in the past is important for assessing the possible responses of the ecological environment under future global warming ...
supported by the National Key Research and Development Program of China (Grant No. 2017YFA0603403);the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant Nos. XDB26000000 & XDA05120204);the National Natural Science Foundation of China (Grant Nos. 41672175 & 41725010)
The impact of global warming on the climate of northern China has been investigated intensively, and the behavior of the East Asian monsoon during previous intervals of climatic warming may provide insight into future...
supported by the National Natural Science Foundation of China(Grant No.41172149);the Science Fund for Creative Research Groups of NSFC(Grant No.41321062);the National Key Basic Research Program of China(Grant No.2015CB953804)
Significant uncertainties remain regarding the temporal evolution of natural vegetation during the Quaternary, and drivers of past vegetation change, on the Chinese Loess Plateau (CLP). This study presents analyses ...
supported by the National Natural Science Foundation of China(Grant No.41174067)
The glacial trough is a common glacier erosion landscape, which plays an important role in the study of glacier erosion processes. In a sharp contrast with the developing river, which is generally meandering, the deve...
supported by the Public Science and Technology Research Funds Projects of the Ocean;State Oceanic Administration of the People’s Republic of China(Grant No.201005003);the National Natural Science Foundation of China(Grant Nos.41376064,41230959,41106043,and 41076033);the National Basic Research Program of China(Grant No.2007CB815903)
Based on a δ180 chronology, rare earth elements (REE) and other typical elements in sediments from core MD06-3047 in the western Philippine Sea were analyzed to constrain the provenances of the sediments and invest...