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• W2978369320 abstract "The geochemistry of foraminiferal tests from the core MD06-3040,that was taken from the shelf mud area of the East China Sea(27°43.3663′N, 121°46.8822′E,water depth 47 m,core length 19.36 m),provides a high-resolution Mg/Ca and δ18O records of benthic foraminifera(Rotalinoides gaimardii) and planktonic foraminifera(Globigerina bulloides).By comparing with micropaleontological and sediment grain-size data,it is suggested that the changes in Mg/Ca and δ18O are controlled principally by the coastal current,warm current and the monsoon related.The paleoenvironmental history of the last 8 000 years has been proposed as following: between 8.0 and 4.1 cal.kaBP,the summer monsoon and the corresponding Taiwan Warm Current and Kuroshio Current were markedly enhanced,particularly during the 5.7～5.2 and 4.6～4.1 cal.kaBP periods,providing both the bottom and surface water with higher temperature,salinity and δ18O;during 4.1～0.7cal.kaBP period,the winter monsoon and the Zhe-Min Coastal Current prevailed,resulting in a marked decrease in temperature,salinity and δ18O of both the bottom and surface water,due to a great increase in the supply of the diluted water originated from the Changjiang and Qiantang rivers;after 0.4 cal.kaBP the summer monsoon and the warm currents prevailed again,causing a paleoceanographical condition similar to the early period." @default.
• W2978369320 created "2019-10-10" @default.
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• W2978369320 date "2010-08-09" @default.
• W2978369320 modified "2023-09-25" @default.
• W2978369320 title "FORAMINIFERAL Mg/Ca AND δ<SUP>18</SUP>O RECORDS IN THE MUD AERA OF THE EAST CHINA SEA DURING THE LAST 8 000 YEARS AND THEIR PALAEOENVIRONMENTAL IMPLICATIONS" @default.
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• W2978369320 doi "https://doi.org/10.3724/sp.j.1140.2010.03079" @default.
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