Influenced by various factors, high-resolution sedimentary records overlap the whole Holocene in the North China Plain are lacking, that makes us have not enough knowledge about the environmental and climate change during the Holocene in the North China Plain, especially for the rapid change climate events. Baiyangdian is the largest freshwater lake in the North China Plain and an ideal area for studying the climate change during the Holocene. A profile(38°52'27.764〃N,115°53'45.789"E; 29 m a.s.l.)is selected at Dongleitou in the southwest Anxin County, Hebei Province, which was 382 cm in depth, the top of the profile(42 cm) was 1035 cal. a B.P. and the bottom ( 424 cm ) was 11335 cal. a B.P. 189 samples ( from BD-22 to BD-210 ) were collected from Dongleitou profile, and geochemical elements, grain size and magnetic susceptibility analysis were used to reconstruct Holocene climate change based on the 8 AMS - ~(14)C dating data. The results are shown as follows:(1) From 11335 cal. a B.P. to 10300 cal. a B.P., the ratio values of CaO/MgO( higher than 4.8),the ratio values of( CaO+K_2O+Na_2O)/Al_2O_3(higher than 1.3),the content of CaCO_3( higher than 12% ) and the median particle size (higher than 15 mum) reached to the maximum in the whole profile, the values of the drought index ( average 0.019) were the second maximum in the whole profile, but the values of CIA (lower than 45),the content of Ti element(lower than 0.38% ) and the values of magnetic susceptibility ( lower than 10 * 10~(-8) m~3/kg) were the minimum of the profile,indicating cold and dry climate in the study area,affected by YD event. ( 2) From 10300 cal. a B.P. to 8500 cal. a B.P., the ratio values of CaO/MgO and( CaO + K_2O + Na_2O)/Al_2O_3, the values of the drought index, the content of CaC03 and the median particle size all significantly declined, yet the values of CIA,the content of Ti element and the values of magnetic susceptibility increased in different degree,indicating that the climate became relative warm and wet. ( 3 ) From 8500 cal. a B.P. to 6000 cal. a B. P., it was the most humid period with minimum of the drought index(average 0.014) and the high contents of CIA and Ti element and the low ratio values of CaO/MgO and( CaO+K_2O+Na_2O)/Al_2O_3,but all of them obviously fluctuated and the ratio values of CaO/MgO and ( CaO + K_2O + Na_2O )/Al_2O_3, the values of the drought index, the content of CaC03 appeared high peak values, while the values of CIA, the content of Ti element appeared low peak values at about 8200 cal. a B.P., 6800 cal. a B.P., indicating two cold and dry events. (4) From 6000 cal. a B.P. to 4200 cal. a B.P., the content of CaC03 was the minimum in the whole profile, but the values of the drought index was higher, the ratio values of CaO/MgO and( CaO+K_2O+Na_2O)/Al_2O_3 increased, indicating humidity decreased, but at about 4500 cal. a B.P., the values of the drought index were the highest, suggesting a cold and dry event.(5) From 4200 cal. a B.P. to 1035 cal. a B.P., the content of sand(lower than 2% ) and the median particle size(lower than 10 mum) were the minimum in the whole profile, the values of the drought index, the ratio values of CaO/MgO and ( CaO + K20 + Na20 )/Al203 and the content of CaC03 all clearly increased, indicating that the climate became cool and dry, the values of the drought index appeared a high peak value at 2800 cal. a B. P., indicating an obvious cold and dry event; while the values of magnetic susceptibility( higher than 20* 10~(-8)m~3/kg) were higher compared with other periods, indicating intensive human activities.