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- W2349552479 abstract "For the first time in the southern South China Sea, a long sequence of deep sea sediment has been disclosed in two sedimentary corse (17957 and 17958) for the reconstruction of the paleoceanographic history. Based on the evidence of planktonic foraminifera, there existed at least three bio events during the last 800 000 years: First, the pink pigmented Globigerinoides ruber appeared and Globigerina rubescens became abundant at the oxygen isotopic stage 11 (around 400 ka BP); Second, pink pigmented Globigerinoides ruber disappeared, Globoquadrina conglomerata came out, right coiled Globorotalia truncatulinoides began to dominate in these cores at the isotopic stage 5e(120 ka BP); and finally, Globorotalia truncatulinoides disappeared at the boundary of isotopic stages 4 and 5 (80 ka BP). The evolution of planktonic foraminifera from the southern South China Sea implies that the sea surface water became warmer or the thermocline became deeper during the period between 400 and 120 ka BP, and the exchange of water masses between the South China Sea and the West Pacific is relatively free during 120-80 ka BP because of the stronger influence of the West Pacific Intermediate Water." @default.
- W2349552479 created "2016-06-24" @default.
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- W2349552479 date "2001-01-01" @default.
- W2349552479 modified "2023-09-23" @default.
- W2349552479 title "LATE QUATERNARY EVOLUTION OF PLANKTONIC FORAMINIFERA IN THE SOUTHERN SOUTH CHINA SEA AND THEIR PALEOCEANOGRAPHIC SIGNIFICANCE" @default.
- W2349552479 hasPublicationYear "2001" @default.
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