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《Marine Geology Letters》 2010-09
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FU Shuqing 1,2,ZHU Zhaoyu 2,OUYANG Tingping2,QIU Yan3(1.Guangzhou Institute of Geography,Guangzhou 510070,China 2.Key Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China 3.Guangzhou Marine Geological Survey,Guangzhou 510760,China)  
The column sample of 86GC recovered from the southern South China Sea was analyzed in order to reveal the paleoenvironmental evolution.Mainly based on the stable oxygen and carbon isotopic records of planktonic foraminifera and AMS 14C dating,the stratiqraphy of the sediment sequence was preliminarily constructed.It suggests that the calumn represents the deposifs formed since ca.31 400 BP in the late period of Marine Oxygen Isotope Stage 3(MIS 3).The last glacial maximum(LGM) in this area began at ca.29 kaBP and ended at ca.19 kaBP.The worst condition occurred in the early part(ca.26~28 kaBP) which is defined as the peak of the LGM.It is likely that a sudden and short sea level rise event happened during ca.21~20 kaBP The δ18O records show that the climate and oceanography were comparatively stable during the Holocene,but both the δ13C and some other paleoclimatic proxies are rather complicated,including several times of short abrupt reversals,suggesting the instability of environment in Holocene due to briefly enhanced northeast winter monsoon.
【Fund】: 国家自然科学基金(40901013 40872111);; 广东省科学院青年基金(qnjj200912);; 中科院边缘海地质重点实验室开放基金(MSGL08-07)
【CateGory Index】: P736.22
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