Abstract: Guanyindong Cave, situated at Qianxi County in Guizhou Province, with an abundance of paleolithic artifactsand of fossil remains, is considered as one of the most important paleolithic sites' in South China. The Ailuropoda-Stegodon fauna of Group B deposits was assumed to be formed in early Middle Pleistocene judging mainly by the existence of Tertiary survivals, and Group A deposits without Tertiary survivals in Middle Pleistocene. The biostrati-graphic conclusion contradicts sharply with the results of U-series dating of fossil hones whichgive an age range of 57--l15 ka for all the artifact and fos'sil containing layers.
Based on the U-series dating of speleothem samples, the GroupA deposits of this site should be younger than 40 ka, the 3rd layer of Group B younger than 50 ka, and 4--8 iayersof Group B between 50 and 240 ka. If the stratigraphic study may prove theuniformity of Group B deposits, the age of 4--8 lavers may be further narrowed to 100--190 ka. The results of this paper do not support the biostratigraphic relative age, but confirm that the lower part of Group B belongs to a late period of MiddIe Pleistocene, beingthe latest fossil record of Gomphotheriidae. This site may represent the cultural evolution traversing the lower, middle and upper paleolithic periods in South China.

Key words: Guanyindong; Speleothem; U-series dating