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 Open Fund of the Key Laboratory of Marine Geology and Environment,Chinese Academy of Sciences,the Innovative Program of Chinese Academy of Sciences(No.KZCX2-YW-221);the National Basic Research Program of China(No.2007CB815903);the National Natural Science Foundation of China(Nos. 41106043 and 40906038)
Paleoenvironmental changes in the northern Okinawa trough covering the last 25 ka were synthetically reconstructed using REE and organic carbon indices of core CSH1.Variations of these parameters revealed three distin...
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...
supported by 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 (40906030,40976026and40906038);the National Basic Research Program of China (2007CB815903)
Two sediment cores, MD06-3050 and MD06-3047, were analyzed to study the Quaternary calcareous nannofossil and microtektite records. We dated bioevents and the microtektite impact event by calibrating with oxygen isoto...
Supported by the Pilot Project of the National Knowledge Innovation Program of the Chinese Academy of Sciences(No.KZCX2-YW-221);the National Basic Research Program of China(973 Program)(No.2007CB815903);the Pilot Project of the National Knowledge Innovation Program of Institute of Oceanology,Chinese Academy of Sciences(No.2007-10);the National Natural Science Foundation of China(No.40906038);the Open Foundation of the State Key Laboratory of Marine Geology(No.MG0903)
Redox-sensitive elements in sediments, such as manganese (Mn), vanadium (V), molybdenum (Mo), and uranium (U), are promising indicators of past redox conditions during sedimentation and early diagenesis. Howev...