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《Acta Sedimentologica Sinica》 2006-06
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Grain Size Characteristics of the Holocene Peat Sediment in Eastern Tibetan Plateau and Its Paleoclimatic Significance

YU Xue-feng 1 ZHOU Wei-jian 1 LIU Xiao-qing 2 ZHENG Yan-hong 3 SONG Shao-hua 1(1. State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xi′an 710075; 2.College of Tourism and Environment, Shaanxi Normal University, Xi′an 710062; 3. Department of Geology, Northwest University, Xi′an 710069)  
Based on the comparison of the grain size characteristics of the Holocene peat sediment in eastern Tibetan Plateau with that of typical eolian sediments, fluvial sediments, and lacustrine sediments, the authors find that the grain size characteristics of peat sediment in the study site closely resemble that of eolian sediments (e.g. loess and paleosol), but differ from that of fluvial sediments, and lacustrine sediments, no matter in the distribution curves or the cumulative curves. The discriminant parameter for the sedimentological environment determining, calculated by the statistical parameters of grain size, also shows the same result. So, the ash content in peat sediment can be used as a proxy to indicate the winter monsoon intensity, higher ash content shows stronger winter monsoon, and the vice versa.
【Fund】: 国家自然科学基金项目(批准号:40121303;40531003);; 黄土与第四纪地质国家重点实验室开放基金共同资助.
【CateGory Index】: P618.117
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