Supported by the Knowledge Innovation Engineering Project of Chinese Academy of Sciences(No.XDA10010305);the National Special Project for‘Global Change and Air-Sea Interaction’(No.GASI-04-01-02);the National Natural Science Foundation of China(Nos.41230959,41076030,41576051)
In the warming world, tropical Pacific sea surface temperature (SST) variation has received considerable attention because of its enormous influence on global climate change, particularly the El Nino-Southern Oscill...
Supported by the National Natural Science Foundation of China(Nos.41230959,41076030,41106042,40906038,41206044);the Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDA11030104);the Project of Global Change and Air-Sea Interaction
Changes in sea surface temperature (SST), seawater oxygen isotope (δ18Osw), and local salinity proxy (δ18Osw-ss ) in the past 155 ka were studied using a sediment core (MD06-3052) from the northern edge of t...
Supported by the National Natural Science Foundation of China(Nos.41230959,41076030,40906038,41106042,41006032);the Pilot Project of the Knowledge Innovation Program of Chinese Academy of Sciences(No.KZCX2-YW-221);the Foundation of Key Laboratory of Marine Geology and Environment of Chinese Academy of Sciences(No.MGE2011KG01)
In order to reconstruct the paleoproductivity evolution history of the West Philippine Sea during the last 700 ka, the vertical gradient of Δδ13C in dissolved inorganic carbon Δδ13C between those of foraminifera P...
supported by the Public Science and Technology Research Funds Projects of Ocean,State Oceanic Administration of the People’s Republic of China (201005003);the National Natural Science Foundation of China (41230959,41106043,41076030);the National Basic Research Program of China (2007CB815903)
Rare earth elements (REE) compositions and discriminant function were successfully used to examine high resolution sediment source changes in the northern Okinawa Trough over the last 24.1 ka, especially for the inf...
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...