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《Quaternary Sciences》 2007-04
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A PRELIMINARY SURVEY ON LOESS DEPOSIT IN EASTERN QINLING MOUNTAINS (CENTRAL CHINA) AND ITS IMPLICATION FOR ESTIMATING AGE OF THE PLEISTOCENE LITHIC ARTIFACTS

Lu Huayu①② Zhang Hongyan②③ Wang Shejiang④⑤ R.Cosgrove④Zhao Cunfa②③ T.Stevens⑥ Zhao Jun②③(①School of Geographical and Oceanographical Sciences,Nanjing University,Nanjing210093;②State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an710075;③Graduate University of Chinese Academy of Sciences,Beijing100049;④Archaeology Program,School of Historical and European Studies,La Trobe University,Melbourne,Australia;⑤Shaanxi Provincial Institute of Archaeology,Xi'an710054;⑥Oxford University Centre for the Environment,Parks Road,Oxford,OX1 3QY,UK)  
A large number of lithic artifacts of Pleistocene age have been collected from the Luonan Basin,located in the Eastern Qinling Mountains(Central China) over the past ten years.This area is regarded as one of the most important places for understanding hominid behavior in the recent geological time.However,the lack of suitable dating material and sedimentary records has restricted our investigation of human evolution,behavior,and environmental changes.The Luonan Basin and the South Luohe River catchment contain typical loess sequences,in which lithic artifacts are buried.These deposits can be well dated and used as a proxy record of past environmental change.The loess sequence provides a secure time-scale for dating the associated artifacts,and they also provide a basis for climatic and environmental reconstruction as a background to past human settlement.In this study two loess sections,one located in Shangbaichuan with a thickness of 24.8 meters,and the other in Liuwan with a thickness of 13 meters,have been investigated by an interdisciplinary research team.Our results show that these loess deposits are aeolian in origin with strong weathering process.The loess-paleosol alternations are related with the glacial-interglacial changes of the Northern Hemisphere environment during the Pleistocene.Analyses of the stratigraphy and depositional processes,plus optically stimulated luminescence dating,palaeomagnetic stratigraphic analyses,as well as magnetic susceptibility measurements show that the loess deposit in this region started accumulating at least 1.10 million years ago.There are clear warm/cold and humid/arid alternating phases indicated by loess and paleosol sequences in the Eastern Qinling Mountains during this time.The discovery of lithic artifacts in the lower parts of the loess indicate that early hominids were living in this region at least 0.8 million years ago.The hand-axes and cleavers found in this region indicate that Mode 2 Acheulian tools were distributed beyond the “Movius line” in Eastern Asia.However,more survey and systematic excavation is needed to further understand human evolution,technological behaviors,and environmental changes in this important geographic transition zone in Central China.
【Fund】: 澳大利亚研究理事会基金项目(ARC编号:DP0665250);; 南京大学985、211工程建设项目(编号:211-(2)-I-10)联合资助
【CateGory Index】: P942.74;P531
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