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《地球科学》 2004-06
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Mg/Ca Ratio in Planktonic Foraminifera Shells: A Proxy for the SST

CHEN Ping~1, FANG Nian-qiao~2, HU Chao-yong~2, DING Xuan~2 1.Department of Resources and Environment Engineering, Anhui University of Science and Technology, Huainan232001, China 2.Institute of Marine Geology and Geophysics, China University of Geosciences, Beijing100083, China  
A series of Mg/Ca ratios of planktonic foraminifera shell Globigerinoides sacculifer in two cores in the NE Indian Ocean were measured by ICP-MS after careful cleaning and dissolving. The results show Mg/Ca ratio and δ~(18)O change accordingly. The Mg/Ca ratio increases with the rise of temperature. This study demonstrates Mg/Ca ratio of planktonic foraminifera shell may serve as a proxy for the past sea surface temperatures (SST).The formula Mg/Ca=0.471 7exp(0.082 5*SST) was applied to calculating and the result shows that in low and middle latitudes, including the NE Indian Ocean, the difference of SST between LGM and the Holocene is about 4 ℃ which is higher than the 2 ℃ estimated by CLIMAP.
【Fund】: 国家自然科学基金项目“西太平洋 -北印度洋热传输与云贵地区降雨的耦合史研究”(No .40 2 72 0 74) ;; 安徽省教育厅自然科学基金项目 ;; 安徽理工大学博士基金项目“海洋生物沉积物化学指标的古环境意义研究” .
【CateGory Index】: P736.22
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