Nuanhe Cave locates at Huanren county in Liaoning Province, a typical site influenced by the East Asian monsoon. The climates here are characterized by cold/dry atmospheric circulation during the winter and warm/humid air masses during the summer. The stalagmite δ18O record, ranging from -7.96‰ to -0.19‰, indicates that the EASM experienced three stages. Comparison of the record with other stalagmite records from Oman, Cuizhou, Hubei Province at different latitudes reveals that there is no time-transgressive character of Holocene Optimum.