| PALEOMONSOONS OF CHINA OVER THE LAST 130,000 YEARS——PALEOMONSOON VARIATION |
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| 引用本文： | 安芷生,吴锡浩,汪品先,王苏民,董光荣,孙湘君,张德二,卢演俦,郑绍华,赵松龄.PALEOMONSOONS OF CHINA OVER THE LAST 130,000 YEARS——PALEOMONSOON VARIATION[J].中国科学B辑(英文版),1991(8). |
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| 作者姓名： | 安芷生 吴锡浩 汪品先 王苏民 董光荣 孙湘君 张德二 卢演俦 郑绍华 赵松龄 |
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| 作者单位： | Xi'an Laboratory of Loess and Quaternary Geology，Academia Sinica，Institute of Geomechanics，Ministry of Geology and Mineral Resources，Marine Geology Department，Tongji University，Naming Institute of Geography & Limnology，Academia Sinica，Institute of Desert Research，Academia Sinica，Institute of Botany，Academia Sinica，State Bureau of Meteorology，Institute of Geology，State Seismological Bureau，Institute of Vertebrate Paleontology and Paleoanthropology，Academia Sinica，Institute of Oceanology，Academia Sinica |
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| 基金项目： | This research program is supported by the National Natural Science Foundation of China and the Xi'an Laboratory of Loess and Quaternary Geology, Academia Sinica. |
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| 摘 要： | Based upon the effect of land-sea interaction on the paleomonsoon variation and the time series of climatic proxy-indicators, the historical Asian monsoon variation over the last 130,000 and 18,000 years has been reconstructed with an emphasis on the basic characteristics of summer monsoon circulation. The monsoon-climatic cycles and associated model of environmental development over the central and eastern China are proposed and the mechanism of paleomonsoon variation of China preliminarily discussed. The variation of East Asian monsoon circulation should be regarded as a regional result of both solar-radiation changes and the global glacial-interglacial cycles. The episodic uplifting of the Qinghai-Xizang Plateau since the late Miocene has to a large extent controlled the forming and evolution of the paleomonsoon circulation of China.
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