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- W2356056922 abstract "Planktonic foraminifer records from 228 samples from ODP Site 1146, located at the northern continental slope of the South China Sea, were used to study the variations in upper water temperatures, including sea surface temperature (SST) and subsurface temperature (SSBT). The planktonic foraminiferal transfer function (FP-12E) and sum of abundance of G. menarddi and P. obliquiloculata were regarded as proxies of sea surface and subsurface temperature, respectively. Results showed that SST and SSBT decreased gradually since 1.5 MaBP, and its distinct changes took place during 0.86~0.94 Ma and 0.64~0.68 Ma at ODP Site 1146. Different from the results of Site 1146, Core 17957 colleted by Sonne 95 cruise at the southern South China Sea in 1994,found SST and SSBT increase gradually since 1.5 Ma, and its significant changes took place during 1.23~1.3 Ma and 0.64~0.68 Ma. Locations of Cores 1146 and 17957 were mainly controlled by East Asian winter monsoon and West Pacific Warm Pool, respectively. Therefore, variations of upper water temperatures in the two cores indicated that East Asian winter monsoon and West Pacific Warm Pool were strengthened since 1.5 Ma, especially after 0.68 Ma." @default.
- W2356056922 created "2016-06-24" @default.
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- W2356056922 date "2004-01-01" @default.
- W2356056922 modified "2023-09-25" @default.
- W2356056922 title "COMPARISON OF VARIATIONS IN UPPER WATER TEMPERATURES BETWEEN THE NORTHERN AND SOUTHERN SOUTH CHINA SEA SINCE 1.5 MaBP" @default.
- W2356056922 hasPublicationYear "2004" @default.
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