• 责任者：Guo Qimei (Nanjing Institute of Geology and Palaeontotogy ; Chinese Academy of Sciences ; Nanjing 210008 ; China)
• 刊名：Acta Petrologica Sinica
• 出版年：2013
• 卷期：52(3)
• 关键词：晚第四纪 ; Late Quaternary ; 古温度 ; paleotemperature
• 页码：p.399-406
• 图表：70 refs.
• 分类号：1400
• issnNo：ISSN1000-0569
• isbnNo：CN11-1922/P

     Sea surface temperature （SST） is one o~ the most important parameters in marine environment. During the Quaternary glacial/interglacial periods, environmental changes have been evidenced by SST reconstruction, which is significant to understand the evolution of global climate change, and has at-  tracted so many studies since the 1950＇s. From thepaleonto function TEXss , dogical in s, stable dex spec isotopes, es to faunal transfer Mg/Ca ratio, U/k 37 and SST reconstructions experienced a process from qualitative, semi-quantitative to quantitative.