ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
宁晋泊地区全新世温暖期以来气候与环境变化研究
  
关键词:high resolution  climatic and environmental changes  Ningjin Lake
基金项目:国家自然科学基金,地质矿产部环境地质开放研究实验室资助
作者单位
郭盛乔 水文地质工程地质研究所 
曹家栋 水文地质工程地质研究所 
张静 水文地质工程地质研究所 
林防 水文地质工程地质研究所 
石英 水文地质工程地质研究所 
杨丽娟 水文地质工程地质研究所 
张文卿 水文地质方法研究所,河北保定 
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摘要:
Research on Climatic and Environmental Changes in the Ningjin Lake since the Holocene Climatic Optimum
      Climatic fluctuation and process of lake changes were revealed through high resolution analysis on environmental indices based on sediments of Ningjin Lake. In the period of climatic optimum( p CO ), climate was warm and stable,precipitation was high, and there were a lot of herbs and trees aroud lakes. But there was a short period of low temperature from 6000 aBP to 5500 aBP. In late of p CO , climate was unstable and obviously fluctuated. In Late Holocene, the temperature fluctuated regularly, and this was very coincident with the record in historical data.
GUO Sheng-qiao,CAO Jia-dong,ZHANG Jing,LIN Fang,SHI Ying,YANG Li-juan,ZHANG Wen-qin.1998.Research on Climatic and Environmental Changes in the Ningjin Lake since the Holocene Climatic Optimum[J].Acta Geoscientica Sinica,19(4):364-370.
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