摘要
根据孢粉分析结果，探讨了神农架２５０００～１２０００ａ．Ｂ．
Based on the sporo pollen analysis, the changes of paleovegetation and paleoclimate from 25 000 to 12 000 years before present in Shengnongjia Mountain are discussed.
出处
《湖北大学学报（自然科学版）》
CAS
1996年第3期306-308,共3页
Journal of Hubei University：Natural Science
关键词
神农架
孢粉组合
古植被
古气候
第四纪
Shengnongjia
Sporo pollen assemblage
Paleovegetation
Paleoclimate
