FN Archimer Export Format
PT J
TI Deep Hydrography of the South China Sea and Deep Water Circulation in the Pacific Since the Last Glacial Maximum
BT 
AF WAN, Sui
   JIAN, Zhimin
   DANG, Haowen
AS 1:1,2;2:2;3:2;
FF 1:;2:;3:;
C1 Chinese Acad Sci, South China Sea Inst Oceanol, CAS Key Lab Ocean & Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China.
   Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China.
C2 CHINESE ACAD SCI, CHINA
   UNIV TONGJI, CHINA
IF 2.946
TC 11
UR https://archimer.ifremer.fr/doc/00437/54857/56344.pdf
   https://archimer.ifremer.fr/doc/00437/54857/56345.pdf
LA English
DT Article
CR MD 147 / MARCO-POLO1-IMAGESXII
   MD 190 / CIRCEA
BO Marion Dufresne
DE ;deep hydrographic structure;oxygen and carbon isotopes;deep circulation;Last Glacial Maximum;South China Sea
AB The oxygen (δ18O) and carbon (δ13C) isotopic compositions of benthic foraminifer Cibicidoides wuellerstorfi as reliable proxies of deep water properties were compiled from 50 core‐top and down‐core sites in the South China Sea (SCS) for two time slices of the late Holocene and Last Glacial Maximum (LGM) to reconstruct the glacial deep hydrographic structure. The bathymetric profiles of both δ18O and δ13C in the SCS show similar trends between the LGM and the late Holocene, but the δ18O gradients between intermediate (∼500‐1000 m) and deep (>1500 m) waters obviously increased during the LGM, indicating an intensified bathyal stratification and weakened vertical mixing between intermediate and deep waters in the SCS during the glacial period. A spatial comparison of bathymetric δ18O and δ13C profiles was also made for the Southern Ocean (Indo‐Pacific sector) and southwest Pacific, western equatorial Pacific (i.e. Ontong Java Plateau), off‐Japan margin as well as the SCS. The meridional δ13C profiles indicate a decreasing trend of δ13C (“aging effect”) in the deep layer (∼1200‐2600 m) from south to north, reflecting a northward flow pathway of deep waters from the southwest Pacific (upstream) to the low‐latitude northwest Pacific and the SCS (downstream) during the LGM. The gradients of deep water δ18O (∼1200‐2600 m) between these upstream and downstream regions were higher during the LGM relative to the Holocene, implying that a greater contribution of the northern‐sourced North Pacific Intermediate Water (NPIW) with a relatively low δ18O signature to the deep waters in the low‐latitude Pacific during the LGM. 
PY 2018
PD MAY
SO Geochemistry Geophysics Geosystems
SN 1525-2027
PU Amer Geophysical Union
VL 19
IS 5
UT 000436542200003
BP 1447
EP 1463
DI 10.1029/2017GC007377
ID 54857
ER

EF