• 责任者：Chen Shuangxi (Key Laboratory of Marine Geology and Environment ; Institute of Oceanology ; Chinese Academy of Sciences ; Qingdao 266071 ; China) ; Li Tiegang
• 刊名：Marine Geology & Quaternary Geology
• 出版年：2011
• 卷期：31(3)
• 关键词：古温度 ; paleotemperature ; 有孔虫类 ; foraminiferas ; 太平洋 ; Pacific Ocean
• 页码：p.61-68
• 图表：3 illus., 1 table, 38 refs.
• 分类号：0200
• 出版序号：664
• issnNo：ISSN0256-1492
• isbnNo：CN37-1117/P

In paleoceanographic research, Sea Surface Temperature (SST) is usually reconstructed with planktonic foraminifera. The results from different methods are diverse. In order to better understand the difference of these methods, the authors reconstructed the SST since the last glacial using the methods of transfer function FP12-E, Modern Analog Technique (MAT), and Mg/Ca ratios with samples from the core MD06-3054, which is located at the bifurcation of North Equatorial Current in the northwestern Pacific. The SST was recovered by counting planktonic foraminiferal fauna and measuring the Mg/Ca ratios of surface dweller Globigerinoides rubber (white, G.ruber in short).