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Paleoenvironmental Implications of Grain-Size Component Variations in the Mud Area Southwest off Cheju Island, ECS

XIANG Rong1, YANG Zuo-sheng2, GUO Zhi-gang2, Saito Y.3, FAN De-jiang2, XIAO Shang-bin1, CHEN Mu-hong1 1.Key Lab of Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou510301, China 2.College of Marine Geosciences, China Ocean University, Qingdao266003, China 3.Geological Survey of Japan, Tsukuba, Ibaraki305-8567, Japan  
Grain-size analysis of sediment core B2, retrieved from mud area southwest off Cheju Island, East China Sea (ECS), was carried out using a Malvern 2000 grain-size analyzer. 4 grain-size components, 65.6, 65.6-10.5, 10.5-1.3 and 1.3μm, can be easily identified according to variations in the grain-size standard deviation. Mainly containing benthic foraminifera, the coarse component (65.6μm) has a very low content, and can be neglected. Downcore variations of the mean-size and content of the other 3 components show that the 65.6-10.5mm component 1 is relatively high, 21%-30%, and fluctuates most strongly, suggesting it is the environmentally sensitive grain-size component (ESGSC) in core B2. The mean-size and content of ESGSC in the studied mud area appears to have been mainly controlled by variations in the strength of the East Asian winter monsoon, with high content and mean-size of ESGCS when the winter monsoon was strong. The winter monsoon variations reconstructed according to this relationship are consistent with climate series records from eastern China over the past 2000 years, indicating that the grain-size component of 65.6-10.5mm can be used as a proxy of the East Asian winter monsoon variation.
【Fund】: 国家自然科学基金项目(Nos.90211022 40206007);; 中国科学院知识创新工程项目(KZCX3-SW-220).
【CateGory Index】: P736.22
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