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Deep water exchanges between the South China Sea and the Pacific since the last glacial period ArchiMer
Wan, Sui; Jian, Zhimin.
Deep ocean circulation is widely considered as one of the important factors for increasing CO2 concentration and decreasing radiocarbon activity (C-14) of the atmosphere during the last deglaciation. The AMS C-14 ages of benthic and planktonic foraminifers from 18 samples of Core MD05-2904 (water depth of 2066m) in the northern South China Sea (SCS) and 15 samples of Core MD05-2896 (water depth of 1657m) in the southern SCS were analyzed in this study for reconstructing the intrabasin deep oceanic processes and hence exploring the deep water exchanges between the SCS and the Pacific since the last glacial period. The results show that during the Holocene the average apparent ventilation age of deep water was younger in the southern SCS (1350years) than in...
Tipo: Text Palavras-chave: Deep water renewal; AMS 14C dating; Last glacial cycle; South China Sea.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00289/40040/39257.pdf
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