Evolution of the South China Sea and monsoon history revealed in deep-sea records  

作　　者：WANGPinxian JIANZhimin ZHAOQuanhong LIQianyu WANGRujian LIUZhifei WUGuoxuan SHAOLei WANGJiliang HUANGBaoqi FANGDianyong TIANJun LIJianru LIXianhua WEIGangjian SUNXiangjun LUOYunli SUXin MAOShaozhi CHENMuhong 

机构地区：[1]LaboratoryofMarineGeology,MOE,TongjiUniversity,Shanghai200092,China [2]GuangzhouInstituteofGeochemistry,ChineseAcademyofSciences,Guangzhou510640,China [3]InstituteofBotany,ChineseAcademyofSciences,Beijing100093.China [4]ChinaUniversityofGeosciences,Beijing100083,China [5]SouthChinaSeaInstituteofOceanology,ChineseAcademyofSciences,Guangzhou510301,China

出　　处：《Chinese Science Bulletin》2003年第23期2549-2561,共13页

基　　金：supported by the National Natural Science Foundation of China(Grant No.4999560);the National Key Basic Research Special Foundation(Grant No.G2000078500).

摘　　要：As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolution of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropaleontology, pollen and other analyses, was adopted for reconstructing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkable diagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful comparison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ～3 Ma.As the third summary report of ODP Leg 184 to the South China Sea (SCS), this paper discusses the evolu-tion of the East Asian monsoon and the SCS basin. A multi-proxy approach, involving geochemistry, micropale-ontology, pollen and other analyses, was adopted for recon-structing the evolutionary history of the East Asian monsoon, which was characterized by a series of paleo-climate events especially at 8, 3.2, 2.2 and 0.4 Ma. The new record indicates similar stages in the development of the East and South Asian monsoons, with an enhanced winter monsoon over East Asia being the major difference. The rich spectrums of monsoon variability from the southern SCS also reveal other characteristic features of the low latitude ocean. Evidence for the evolution of the SCS includes the hemipelagic Oligocene sediments, implying the existence of deep water environ-ments during the early seafloor spreading stage of the SCS basin. The four major unconformities and some remarkable diagenetic features in upper Oligocene deposits indicate the strongest tectonic events in the region. From a careful com-parison of lithologies and sedimentation rates, we conclude that the prominent differences in sedimentary environments between the southern and northern SCS were established only by ~3 Ma.

关 键 词：南中国海 深海沉积 ODP 海洋钻探工程 东亚季风 

分 类 号：P732[天文地球—海洋科学] P736.21