节点文献

云南点苍山全新世以来的冰川湖泊沉积

Glacial Lacustrine Sediment’s Response to Climate Change since Holocene in Diancang Mountain

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 杨建强崔之久易朝露张威刘克新

【Author】 YANG Jianqiang1, CUI Zhijiu1, YI Chaolu2, ZHANG Wei3, LIU Kexin4(1. College of Environmental Sciences, Peking University, Beijing 100871, China;2. Department of Urban and Resources Sciences, Nanjing University, Nanjing 210093, China;3. College of Resource and Environment, Liaoning Technical University, Fuxin 123000, China;4. Institute of Heavy Ion Physics, Peking University, Beijing 100871, China)

【机构】 北京大学环境学院辽宁工程技术大学北京大学重离子物理研究所 北京100871北京100871阜新123000北京100871

【摘要】 根据对点苍山冰川湖泊沉积的粒度、磁化率、元素地球化学以及孢粉等环境指标的综合分析,结合冰川地貌特征,以点、面两方面资料结合的方式综合分析,试图建立该地全新世以来的气候变化系列,共划分为6个气候阶段,以冷湿与暖干的组合为其特征。与其他西南季风区的环境变迁对比表明,点苍山受西南季风影响加强的时间晚于阿拉伯海而早于青藏高原,可以认为是联系以上两者的纽带。当西南季风在青藏高原逐步强盛以后,因地形作用致使本区湿度有所降低

【Abstract】 On the basis of the physical and chemical analyses of glacial lacustine sediment and glacial geomorphology in Diancang Mountain, the series of climate change since Holocene is expected to be rebuilt, including 6 stages with the alternation of cold-wet and warm-dry climate. The comparison with other areas affected by southwest monsoon shows that the time when southwest monsoon arrived at Diancang Mountain was later than that of the Arabian Sea and earlier than that of the Tibetan Plateau. This fact implies that Diancang Mountain is the joint linkage of the above place. Another phenomenon is that after southwest monsoon arrived at the Tibetan Plateau, the climate of Diancang Mountain change slightly drier. The record presents that this area was influenced by southeast monsoon between 6.0 ka BP and 5.3 ka BP.

【基金】 国家自然科学基金(40071015);云南大理州城建局项目~~
  • 【文献出处】 地理学报 ,Acta Geographica Sinica , 编辑部邮箱 ,2004年04期
  • 【分类号】P512.2
  • 【被引频次】40
  • 【下载频次】643
节点文献中: 

本文链接的文献网络图示:

本文的引文网络