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- W2384792949 abstract "Sea surface temperature (SST) estimates of the southern South China Sea over the last 2 Ma indicate that, the water temperature kept warm with lower variation compared with the northern South China Sea during the Pleistocene glacial-interglacial cycles. However, for the long-time scale, the transfer-function estimated SST still has an evident trend. The low-temperature periods were not consistent with the glacial times, which implies that there exists characteristic evolution for the sea surface water in the southern South China Sea. The transfer-function estimated SST might reflect the subsurface water and upper water-column structure of the low-latitude marine environment. Evolution of planktonic foraminiferal fauna over the last 2 Ma indicated that the thermocline of the southern South China Sea shoaled gradually from marine isotope stage (MIS) 79 to ~53, deepened from MIS 53 to the Brunhes/Matuyama boundary, and shoaled again after B/M boundary." @default.
- W2384792949 created "2016-06-24" @default.
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- W2384792949 date "2004-01-01" @default.
- W2384792949 modified "2023-09-25" @default.
- W2384792949 title "SEA SURFACE TEMPERATURE ESTIMATE AND SUBSURFACE WATER EVOLUTION IN THE SOUTHERN SOUTH CHINA SEA" @default.
- W2384792949 hasPublicationYear "2004" @default.
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