摘要
本文通过对武汉地区2个钻孔的孢粉组合分析,揭示了本区全新世的古植被和古气候。古植被可划分为5个植物群,相应地可划分5个气候期。古气候变化与长江中下游地区基本一致。
This paper studies sporopollen assemblages from three drilling cores and reveals the changes of palaeovegetation and palaeoclimate in Wuhan area during Holocene. Palaeovegetation can be divided into five plant communities,corresponding to five stages of climate. It is similar to that of the mid-lower Yangtze River region.
出处
《湖北大学学报(自然科学版)》
CAS
1992年第2期188-191,195,共5页
Journal of Hubei University:Natural Science
关键词
全新世
孢粉组合
古气候
武汉地区
Holocene,Sporopollen assemblages, Palaeoclimate, Wuhan area.