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《Journal of Glaciology and Geocryology》 1991-02
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Buried Humus Soil and Syngenetic Permafrost around the Daxigou Meteorological Station at the Source of the Urumqi River

Zhao Ling and Qiu Guoqing (Lanzhou Institute of Glaciolagy and Geocryology, Chinese Academy of Sciences)  
Buried humus soils were commonly found around the Daxigou Meteorological Station. For example, three humus soil layers, formed in 201± 59 a B.P., 3 211 ±74 a B.P. and 4 301 ± 96 a B.P., respectively were found in Pit 89-1. The presence of buried humus soils indicates the aggregation of sediments, the rising of permafrost table, and the fluctuation of climate.
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