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《Journal of Lanzhou University(Natural Sciences)》 2009-01
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Middle eocene-oligocene climatic changes recorded by sedimentary colors in the Xining Basin,in northeastern Tibetan Plateau,NW China

XU Li~1,MIAO Yun-fa~2,FANG Xiao-min~(2,1),SONG Chun-hui~1,XIA Wei-min~1, YAN Xiao-li~1,HAN Wen-xia~1,ZHANG Qi-bo~1,CHEN Chuan-fei~1,DAI Shuang~1 (1.Key Laboratory of Western China's Environmental Systems with the Ministry of Education, School of Resources and Environmental Sciences,Lanzhou University,Lanzhou 730000,China; 2.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China)  
The climatic changes at the boundary of the eocene-oligocene are most significant during the cenozoic.The records of the colors measured from the lacustrine sediments during 42.5~26.0 Ma in the Xining Basin,northeastern Tibetan Plateau,NW China,show that the color curves can be divided into two phases at 32.8 Ma.The lower phase(42.5~32.8 Ma)of L~* values fluctuated intensively and decreased slowly, and to the younger phase(32.8~26.0 Ma),they became smaller and the values rebounded.The trends of a~* and b~* were opposite to L~*,but both of them were low and fluctuated intensively at the bottom,then increased gradually with smaller fluctuations since 32.8 Ma.Combined with pollen,organic and CaCO_3,the color proxies might indicate that a great cooling period in this area occurred in 32.8 Ma,corresponding with the Oi-1 event.The drought and oxidation was faint,and fluctuation was intensive before 32.8 Ma.After Oi-1 event,the extent of drought eased up and the oxidation strengthened.But the fluctuation of climate became faint.The high resolution record obtained from this area around the Oi-1 event is very important for the research in that it may indicate that land system responded to global cooling during the Eocene-Oligocene.
【Fund】: 中国科学院知识创新工程重要方向项目(kzcx2-yw-104);; 国家“973”重点基础研究发展计划项目(2005CB422001);; 教育部科学技术研究重大项目(306016);; 国家自然科学基金项目(40872029)
【CateGory Index】: P512.2;P467
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