【摘要】 <正> 黑龙江省哈尔滨东北郊的黄山（又名荒山）,由于盛产哺乳动物化石和石器,引起第四纪工作者的普遍注意,成为我国东北第四纪地质研究的典型地区之一。但是,对黄山第四纪地层划分、时代、成因及其沉积环境的认识,至今尚未统一,1974年曾与有关单位协作,对哈尔滨黄山和肇源三站的第四纪地层进行了考察和初步总结。本文是在此基础上,对1978年于该剖面下部进行加密取样和补充分析,并结合植物残体分析和C¹⁴年龄测定结果的进一步总结。更多还原

【Abstract】 The section of Huang Shan is one of the standard sections of quaternary stra-tigraphy in northeast China,it is situated in the northeast suburbs of Haerbin.Having studied it for many times,we obtained results on the spore-pollen asso-ciation consistent with those on C¹⁴plant fossil,animals fossils,etc.The Huang Shan section of the late period of late pleistocene was dividedinto two spore-pollen association.In the late half of the period,Picea was pre-dominant,except having a little Selaginella and B（?）trychium.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 chan-ged to dry-cold.The above mentioned pollen association feature was representative of peri-glacial vegetation and periglacial climate.It also proved that the climate of Dai-Li glaciation had spread to Huang Shah region.更多还原