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《Marine Geology & Quaternary Geology》 2005-04
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HUANG Yuan-hui,LAN Dong-zhao (Third Institute of Oceanography,State Oceanic Administration,Xiamen 361005,China)  
The process of sedimentary environmental change in the northeastern South China Sea since the last glacial stage was studied by using core D(water depth 405 m,core length 130 cm)sampled from the upper slope in this sea area to carry out diatom,grain size and detrital mineral analyses.The results of grain size and diatom analyses matched with each other perfectly by which core D could be divided into surface and lower layers.The surface sand layer(0~2 cm) consists of residual or palimpsest sediments which were formed in the late Pleistocene and transformed in the post glacial transgression.The lower layer (2~130 cm) was mainly formed in a neritic sedimentary environment in the last glacial stage.Two sedimentary rhythms can be detected in core D: MIS 4 regression to MIS 3 transgression and MIS 2 regression to the post glacial transgression.
【Fund】: 海洋沉积与环境地质国家海洋局重点实验室开放基金(MASEG200401)
【CateGory Index】: P736.21;
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