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- W2384657953 abstract "Major elements of the terrestrial detritus in the sediments collected from ODP site 1144 in the South China Sea were reported in this paper. The Ti normalized ratios of the major elements exhibit significant climatecontrolling patterns. In details, during interglacials, the Al/Ti, K/Ti and Mg/Ti ratios were higher than during glacials, while Na/Ti and Ca/Ti ratios were lower than those during glacials. Considering that these terrestrial detritus mainly come from weathering products in South China, such variations of major element indicate that chemical weathering in South China was strong during interglacials. The enhanced chemical weathering might have something to do with the more humid climate in interglacials than in glacials, which agrees with pollen records in the sediment cores from SCS. Such climate patterns indicate that summer monsoons were strengthened during interglacials, which brought about more precipitation to South China and enhanced the chemical weathering there." @default.
- W2384657953 created "2016-06-24" @default.
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- W2384657953 date "2003-01-01" @default.
- W2384657953 modified "2023-09-25" @default.
- W2384657953 title "CLIMATIC RECORDS IN THE MAJOR ELEMENTS OF THE TERRESTRIAL DETRITUS FROM THE SOUTH CHINA SEA" @default.
- W2384657953 hasPublicationYear "2003" @default.
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