Abstract:The plant spores and pollen are more desirable indicators to the recovery of environmental change.It had great significance using palynological indicators for the Quaternary stratigraphic subdivision and regional paleoclimate contrast.In this paper,theⅠ~Ⅲ terraces profiles of Anning river at Lugu township,Mianning county in western Sichuan province are selected to do chronology measurement and analysis of pollen samples.The results show that the terrace I formed during the Holocene(Q4),climate was wet or light wet.The terrace Ⅱ deposited during the end of Late-pleistocene(Q33)or the early Holocene(Q14),both temperature and humidity were lower than that of terrace Ⅰ,and vegetation and climate had more than two obvious changes and fluctuations.The terrace Ⅲ deposited during the middle Late-pleistocene(Q32),climate was wet or light wet,the temperature and humidity were higher than terrace Ⅱ,lower than terrace Ⅰ.The tectonic and climate change during the formation of Anning river terraces are discussed.According to the speed of river downcutting,it is indicated that the uplift rate of epipleistocene to be bigger than the end of epipleistocene-Holocene.