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内蒙古正蓝旗地区全新世古环境变迁的孢粉记录
引用本文:王燕,叶青培,乔彦松.内蒙古正蓝旗地区全新世古环境变迁的孢粉记录[J].地质力学学报,2006,12(3):324-328.
作者姓名:王燕  叶青培  乔彦松
作者单位:1. 中国地质科学院地质力学研究所,北京,100081
2. 中国地质博物馆,北京,100000
摘    要:通过对正蓝旗闪电河剖面孢粉资料的分析,重建了内蒙古中部地区全新世以来古植被及古气候的演变过程。全新世早期气候温凉略干,为草原型植被或稀疏草原型植被;中期气候相对暖湿,为森林型植被;后期气候温凉偏干或凉爽偏干,为稀疏草原型植被或草原型植被。

关 键 词:全新世  古环境变迁  孢粉记录
文章编号:1006-6616(2006)03-0324-05
收稿时间:2005-08-04
修稿时间:2005年8月4日

PALYNOLOGICAL RECORDS OF THE HOLOCENE ENVIRONMENTAL CHANGES IN ZHENGLAN QI, INNER MONGOLIA
WANG Yan,YE Qing-pei,QIAO Yan-song.PALYNOLOGICAL RECORDS OF THE HOLOCENE ENVIRONMENTAL CHANGES IN ZHENGLAN QI, INNER MONGOLIA[J].Journal of Geomechanics,2006,12(3):324-328.
Authors:WANG Yan  YE Qing-pei  QIAO Yan-song
Institution:Institute of Ceomechanics, Chinese Academy of Geological Sciences, Beijing 100081,Geology Museum of China, Beijing 100000 and Institute of Ceomechanics, Chinese Academy of Geological Sciences, Beijing 100081
Abstract:The according to the Holocene vegetation and climatic evolution in central Inner Mongolia was reconstructed palynological records of the Shandlanhe section in Zhenglan Qi. The vegetation was dominated by steppe or sparse steppe in the early Holocene, corresponding to a warm and dry climate The vegetation in the middle Holocene was forest-type, indicating a relatively warm-wet climate. the late Holocene, the vegetation again changed During to steppe or sparse steppe, suggesting that the climate tended to be warm-slightly dry or cool-slightly dry.
Keywords:paleoenvironmental evolution  Holocene  palynological record
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