Variations in upper water structure during MIS 3 from the western South China Sea

Core 17954 is located in the modern summer upwelling area in western South China Sea, its sediments recorded the variations of upwelling generated by East Asia Summer Monsoon (EASM) during MIS 3. Based on the strict age model of AMS (14)C dating, the paleo-Sea Surface Temperature (SST) and Salinity...

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Bibliographic Details
Published in:Chinese Science Bulletin
Main Authors: Du JiangHui, Huang BaoQi
Other Authors: Huang, BQ (reprint author), Peking Univ, MOE Key Lab Orogen Belst & Crustal Evolut, Sch Earth & Space Sci, Beijing 100871, Peoples R China., Peking Univ, MOE Key Lab Orogen Belst & Crustal Evolut, Sch Earth & Space Sci, Beijing 100871, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: 科学通报 英文版 2010
Subjects:
Mg/Ca
MIS 3
East Asia Summer Monsoon
upwelling
Paleoceangraphy
EAST-ASIAN MONSOON
NORTHERN-HEMISPHERE CLIMATE
INTERTROPICAL CONVERGENCE ZONE
LAST GLACIAL PERIOD
SURFACE TEMPERATURE
FORAMINIFERAL MG/CA
ISOTOPE STAGE-3
ATLANTIC-OCEAN
ICE
VARIABILITY
Hulu
NGRIP
Planktonic foraminifera
Online Access:https://hdl.handle.net/20.500.11897/155893
https://doi.org/10.1007/s11434-009-0388-8

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