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| 1 | Thirty million year deep-sea records in the South China Sea显示文摘In the spring of 1999 the Ocean Drilling Pro-gram (ODP) Leg 184 Shipboard Party cored 17 holes at 6 deep water sites in the northern and southern parts of the South China Sea (SCS). Chinese scientists actively partici-pated in the entire process of this first deep-sea drilling leg off China, from proposal to post-cruise studies. More than 30 categories of analyses have been conducted post-cruise in various Chinese laboratories on a large number of core sam-ples, and the total number of analyses exceeded 60 thousand. The major scientific achievements of the Leg 184 studies are briefly reported in three successive papers, with the first one presented here dealing with deep-sea stratigraphy and evolu-tion of climate cycles. This ODP leg has established the best deep-sea stratigraphic sequences in the Western Pacific: the 23-Ma isotope sequence from the Dong-Sha area is unique worldwide because of its continuity; the last 5-Ma sequence from the Nansha area represents one of the best 4 ODP sites worldwide with the highest time-resolution for that time in-terval, and the sequences of physical properties enable a de-cadal-scale time resolution. All these together have provided for the first time high-quality marine records for paleoenvi-ronmental studies in the Asian-Pacific region. This new set of stratigraphic records has revealed changes in climate cyclic-ity over the last 20 Ma with the fluctuating power of the 100 ka, 400 ka, 2000 ka eccentricity cycles, indicating the evolv-ing response of the climate system to orbital forcing along with the growth of the Antarctic and Northern Hemisphere ice sheets. | WANGPinxian ZHAOQuanhong JIANZhimin CHENGXinrong HUANGWei TIANJun WANGJiliang LIQianyu LIBaohua SUXin | 2003 | Chinese Science Bulletin2003，48，23： | 41 |
| 2 | Evolution of the South China Sea and monsoon history revealed in deep-sea records显示文摘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. | WANGPinxian JIANZhimin ZHAOQuanhong LIQianyu WANGRujian LIUZhifei WUGuoxuan SHAOLei WANGJiliang HUANGBaoqi FANGDianyong TIANJun LIJianru LIXianhua WEIGangjian SUNXiangjun LUOYunli SUXin MAOShaozhi CHENMuhong | 2003 | Chinese Science Bulletin2003，48，23： | 34 |
| 3 | Carbon isotopic record of foraminifers in surface sediments from the South China Sea and its significance显示文摘The study is based on stable carbon isotopic measurements of 112 foraminiferal samples from surface sediments at 40 sites in the South China Sea (SCS). δ 13C of foraminifers and ?δ C between planktonic and benthic 13 foraminiferal species exhibit a low value area at the north- eastern and southern ends of the SCS. It is correlated with the nutrient distributional pattern in the SCS and circumja- cent area, the influence of the northeastern and southwestern monsoons on water flow and water chemistry in the SCS. The monsoons have not only brought nutrients to the upper part of the sea but also disturbed water and decreased dif- ference between the surface and bottom water. Its influence is most obvious at both ends, which resulted in the low value areas in δ 13C and ?δ 13C at the ends. The distributional pat- tern of the stable carbon isotope in the SCS is a reflection of the East Asian monsoons. | CHENGXinrong WANGPinxian HUANGBaoqi LIUChuanlian JIANZhimin ZHAOQuanhong LIJianru TIANJun XUJian | 2005 | Chinese Science Bulletin2005，50，2： | 7 |
| 4 | Planktonic Foraminiferal Assemblage Variations of Ontong-Java Plateau during Late Quaternary and Their Implications for Paleotemperature in the Western Pacific Warm Pool显示文摘Ocean Drilling Program (ODP) Site 807A was recovered from the Ontong-Java plateau, western equatorial Pacific. Quantitative analysis of planktonic foraminifera, combined with oxygen and carbon isotope data, reveals the glacial-interglacial variations of sea-surface temperature and the upper water vertical structure in this region during the late Quaternary. Our results indicate that since 530 ka sea-surface temperature (SST) and the depth of thermocline (DOT) have changed significantly in the western Pacific warm pool (WPWP). The average glacial-interglacial annual SST difference was up to 4.2 ℃, and the DOT fluctuations could exceed more than 100 m, further suggesting the instability of the WPWP. The spectral analyses of SST and DOT reveal two dominating cyclicities—the typical 100 ka cycle and the semi-precessional cycle, which is significant in the tropical spectrum, indicating that late Quaternary paleoceanographic changes in the study area were influenced not only by a high latitude forcing but also by tropic-driving factors. | JinHaiyan JianZhimin TianJun | 2004 | Journal of China University of Geosciences2004，15，4： | 0 |
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