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《Quaternary Sciences》 2005-04
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LOESS RESEARCH AND PALEOLITHIC ARCHAEOLOGY IN CHINA

Yang Xiaoyan~① Xia Zhengkai~② Liu Tungsheng~①(①Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; ②College of Environmental Sciences, Peking University, Beijing 100871)  
Paleolithic archaeology is closely associated with Quaternary research. Most paleolithic sites were commonly found in loess deposits covering northern China. At the beginning of the study on Chinese paleolithic archaeology, loess and paleolithic archaeology researchers cooperated with each other, and developed together. In the last forty years, Chinese loess study has made great progress. How to apply new loess concepts and technology to the paleolithic archaeology? The paper gives two case studies to elucidate applications of the loess-paleosol sequences to dating Paleolithic sites. The Zhijidong site is located in a limestone basin in the Xingyang City, Henan Province. Thick Loess deposited in piedmont area. Based on the loess strata of the third terrace, we conclude that the river running across the basin incised the loess tableland during the late L_(1)S development, resulting in the Zhijidong Cave being disclosed and occupied by the past man consequently. Namely the cultural deposits of the Zhijidong site formed during 60~30kaB.P., especially 40~30kaB.P. The Dayao site, located in the Inner Mongolia, is considered as an early-paleolithic site embedded in the Lishi and Malan Loess. But field surveys showed that “Lishi-Malan loess” make up of gully deposits and colluvium, with horizontal beddings now and then in the profile. Thus, it's not the original loess and the age of the Dayao siue should be redetermined. We propose that paleolithic archaeologists should pay more attention to the advancement in Quaternary science and cooperate with the Quaternary scientists closely.
【Fund】: 国家自然科学基金青年科学基金项目(批准号:40401008);; 2003年度刘东生国家最高科学技术奖专项项目共同资助
【CateGory Index】: P941.74;K871.11
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7 Lu Houyuan; Liu Tungsheng; Wu Naiqin; Han Jiamao; Guo Zhengtang(Institute of Geology, Chinese Academy of Sciences, Beijing 100029);PHYTOLITH RECORD OF VEGETATION SUCCESSION IN THE SOUTHERN LOESS PLATEAU SINCE LATE PLEISTOCENE[J];QUATERNARY SCIENCES;1999-04
8 Gu Zhaoyan Han Jiamao Liu Tungsheng (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029);PROGRESS IN GEOCHEMICAL RESEARCH ON THE LOESS AND OTHER QUATERNARY DEPOSITS IN CHINA[J];QUATERNARY SCIENCES;2000-01
9 Liu Jiaqi; Liu Qiang (Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029);QUATERNARY STRATIGRAPHY IN CHINA[J];QUATERNARY SCIENCES;2000-02
10 Song Yougui; Fang Xiaomin; Li Jijun; An Zhisheng; Yang Deng; Lu Lianqing (Department of Geography, Lanzhou University Lanzhou 730000 State Key Laboratory of Loess and Quaternary Geology, Chinese Aeademy of Scineces Xi'an 710054);AGE OF RED CLAY AT CHAONA SECTION NEAR EASTERN LIUPAN MOUNTAIN AND ITS TECTONIC SIGNIFICANCE[J];QUATERNARY SCIENCES;2000-05
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