| PALEOMONSOONS OF CHINA OVER THE LAST 130,000 YEARS——PALEOMONSOON RECORDS |
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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 RECORDS[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： | The characteristics of the modern monsoon climate o?China may be used as clues for recognizing the records of paleomonsoon climate. The present paper deals primarily with the various paleomonsoon records of the last 130,000 years in the southeast monsoon area. These records mainly come from the following three fields: (i) the historical, (ii) the geological, including loess-paleosol sequence, deserts, lakes, snowlines, timberlines, the phenomena of continental desertization and so on, and (iii) the biological, presented by vegetation and mammals. Among these records, the loess-paleosol sequence in the Loess Plateau reflects a climatic history characterized by alternation of two different climatic periods when the Asian winter monsoon and summer monsoon showed pronounced effects on environment, respectively.
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