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《Journal of Glaciology and Geocryology》 1982-03
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PERIGLACIAL PHENOMEMA AT THE EAST OPENCUT COAL MINE OF ZHALIANUOER IN INNER MONGOLIA AND THEIR GEOCHRONOLOGY

Li Xingguo, Liu Guanglian, Xu Guoying,Li Fengchao, Wang Fulin ( Institute of Vertebrate Paleontology and Paleoanthropology,Academia Sinica )  
The little city of Zhalianuoer is situated in the southeast of Manzhouli ( Lat.49°20'N Long 117°35'E ) .In May 1980 at the east opencut of the coal mine of Zhalianuoer, two fossil mammoth skeletons were discovered in the old river bed 35-40 metres below the surface.The C14 age of the mammoth coprolites is 33,760±1,700 years B.P. ( PV-170 ) . Mammoth is the representative of the Mammuthus-Coelodontas fauna of the Late Pleistocene in Northeast China, representing a climatic cold environment. We divide the periglacial phenomena of Zhalianuoer stage into three substages: 1. Lingquan Periglacial Substage happened about 33,700 years B.P. 2. Huangshan Interperiglacial Substage: predominantly between Lingquan Periglacial Substage and Zhalianuoer New Glacial Substage interposed a relatvely warmer period of glacial retreat, extending from about 33,000 years to 23,000 years B.P. 3. Zhalianuoer New Glacial Substage: the C14 determinnation of the silt (black clay ) is 3,080±80 years B. P. ( PV-201 ) , 0.5 metres below the surface, happened about 3,000-5,000 years B.P.
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