FN Archimer Export Format
PT J
TI Deepwater circulation variation in the South China Sea since the Last Glacial Maximum
BT 
AF ZHENG, Xufeng
   KAO, ShuhJi
   CHEN, Zhong
   MENVIEL, Laurie
   CHEN, Han
   DU, Yan
   WAN, Shiming
   YAN, Hong
   LIU, Zhonghui
   ZHENG, Liwei
   WANG, Shuhong
   LI, Dawei
   ZHANG, Xu
AS 1:1;2:2;3:1;4:3;5:4;6:5;7:6;8:7;9:8;10:2;11:1;12:2;13:9;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;
C1 Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China.
   Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China.
   Univ New South Wales, Climate Change Res Ctr, ARC Ctr Excellence Climate Syst Sci, Sydney, NSW, Australia.
   State Ocean Adm, Isl Res Ctr, Fuzhou, Peoples R China.
   Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China.
   Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China.
   Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Peoples R China.
   Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China.
   Helmholtz Zentrum Polar & Meeresforsch, Alfred Wegener Inst, Bremerhaven, Germany.
C2 CHINESE ACAD SCI, CHINA
   UNIV XIAMEN, CHINA
   UNIV NEW SOUTH WALES, AUSTRALIA
   STATE OCEAN ADM, CHINA
   CHINESE ACAD SCI, CHINA
   CHINESE ACAD SCI, CHINA
   CHINESE ACAD SCI, CHIN
   UNIV HONG KONG, CHINA
   INST A WEGENER, GERMANY
IF 4.253
TC 32
UR https://archimer.ifremer.fr/doc/00421/53224/54800.pdf
   https://archimer.ifremer.fr/doc/00421/53224/54801.xlsx
   https://archimer.ifremer.fr/doc/00421/53224/54802.pdf
LA English
DT Article
CR IMAGES 4-MD111
   MD 122 / WEPAMA
   MD 147 / MARCO-POLO1-IMAGESXII
BO Marion Dufresne
DE ;South China Sea;deep current;anisotropy of magnetic susceptibility;Heinrich 1;Atlantic-Pacific seesaw
AB Deepwater circulation plays a central role in global climate. Compared with the Atlantic, the Pacific deepwater circulation's history remains unclear. The Luzon overflow, a branch of the North Pacific deep water, determines the ventilation rate of the South China Sea (SCS) basin. Sedimentary magnetic properties in the SCS reflect millennial-scale fluctuations in deep current intensity and orientation. The data suggest a slightly stronger current at the Last Glacial Maximum compared to the Holocene. But, the most striking increase in deep current occurred during Heinrich stadial 1 (H1) and to a lesser extent during the Younger Dryas (YD). Results of a transient deglacial experiment suggest that the northeastern current strengthening at the entrance of the SCS during H1 and the YD, times of weak North Atlantic Deep Water formation, could be linked to enhanced formation of North Pacific Deep Water. 
PY 2016
PD AUG
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 43
IS 16
UT 000384443800031
BP 8590
EP 8599
DI 10.1002/2016GL070342
ID 53224
ER

EF