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《Journal of Glaciology and Geocryology》 1992-04
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Holocene Periglacial Processes and Environmental Changes in the Daqingshan Mountains, Inner Mongolia, China

Cui Zhijiu and Song Changqing (Department of Geography, Peking University)  
Many periglacial phenomena and paleobotany evidinces of environmental changes were retained in the Daqingshan area of northern China. This arid-semiarid area is sensitive to climatic changes. There were four climatic periods with the time range of one thousand years during Holocene. The annual mean temperature during Hypsithermal is 1-2℃ higher than today. On the other hand, the annual mean temperature is 2.0- 2.5℃ lower during Neoglaciation and about 7℃ lower during the late period of Late Pleistocene than that of the present time. The fluctuation range of vertical vegetation belts was about 200-600 m during Holocene.
【Fund】: 自然科学基金委员会资助项目
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