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- W2380493353 abstract "The compositions of biogenic and mineral clastics from core 184 (16°99.5′N,117°54.17′E, water depth 3 947 m), which was taken from the northeastern South China Sea (SCS) and near the carbonate lysocline and compensation depth (CCD) of the modern SCS, have been quantitatively examined. It has been demonstrated that the component analysis is potential to be a simple and fast method in the marine paleoenvironmental study. The stratigraphy of this core was mainly based on the comparison of volcanic glass and carbonate contents with those of nearby cores that had planktonic foraminiferal (δ~(18)O) records. The variation in relative abundance of biogenic clastics is obviously controlled by the deep-sea dissolution related to water depth and climate change. Calcareous biogenic clastics remarkably increase in abundance while siliceous biogenic clastics decrease during the last glacial stage, and it was the opposite during the interglacial stage. The mineral clastics in core 184 mainly come from the Asian continent, with the Luzon Island as a secondary source of weathering materials. The distributions of these mineral clastics are controlled by the transportation related with the distance to shore and also the direction of surface currents." @default.
- W2380493353 created "2016-06-24" @default.
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- W2380493353 date "2005-01-01" @default.
- W2380493353 modified "2023-09-25" @default.
- W2380493353 title "COMPONENT ANALYSIS OF THE BIOGENIC AND MINERAL CLASTICS IN CORE 184 OF THE NORTHEASTERN SOUTH CHINA SEA AND ITS PALEOENVIRONMENTAL SIGNIFICANCE" @default.
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