• 责任者：Wang Fei (Key Laboratory of West China’s Environmental Systems ; Ministry of Education ; Lanzhou University ; Lanzhou 730000 ; China) ; Sun Donghuai
• 刊名：Quaternary Sciences
• 出版年：2012
• 卷期：32(5)
• 关键词：新近纪 ; Neogene Period ; 第四纪 ; Quaternary ; 古温度 ; paleotemperature ; 古环境 ; paleoenvironment ; 甘肃 ; Gansu Province
• 页码：p.1022-1035
• 图表：illus., 1 table, 94 refs.
• 分类号：1200
• isbnNo：CN11-2708/P

Based on the research about the quantitative relationship between surface soil and climatic parameter, many authors have established magnetic susceptibility-annual rainfall transfer function and redess-annual temperature transfer function. In this paper,the authors chose the representative Jiuzhoutai loess profile and Nanshan red-clay profile and calculated the paleo-rainfall and paleo-temperature of Lanzhou Basin during the past 8 Ma by using these transfer function.Combining the magnetic susceptibility-paleorainfall transfer function and redess-paleotemperature transfer function with plenty of paleobiological and geological evidence,the results of quantitative reconstruction of paleoclimate and paleoelevation for the past 8 Ma in Lanzhou Basin indicate that the evolution of three paleo-parameters can be divided into four stages.