Abstract: The section of Huang Shan is one of the standard sections of quaternary stratigraphy in northeast China,it is situated in the northeast suburbs of Haerbin.Having studied it for many times,we obtained results on the sporepollen association consistent with those on C¹⁴ plant fossil,animals fossils,etc.The Huang Shan section of the late period of late pleistocene was dividedinto two sporepollen association.In the late half of the period,Picea was predominant,except having a little Selaginella and Bctrychium.The climate was verycold and wet.In the last part of the period,Artermisia,Chenopodiaceae and otherherbacous pollen increased,and Picea and tree pollen dccreased,The climate changed to drycold.The above mentioned pollen association feature was representative of periglacial vegetation and periglacial climate.It also proved that the climate of DaiLi glaciation had spread to Huang Shah region.