Subtropical Plant Science ›› 2009, Vol. 38 ›› Issue (02): 1-5.DOI: 10.3969/j.issn.1009-7791.2009.02.001

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Floristic Elements of Sediment Spore-pollen between Western and Eastern Sample Plots beside Main Peak of Ailao Mountain in Yunnan

HAO Cheng-yuan1, CHEN Zhi-chao1, WU Shao-hong2   

  1. 1. Henan Polytechnic University, Jiaozuo 454000, Henan China;
    2. Institute of Geographic Sciences and Natural Resource Research, Chinese Academy of Sciences, Beijing 100101, China
  • Received:2008-12-08 Online:2009-06-10 Published:2009-06-10

云南哀牢山主峰两侧沉积物孢粉区系成分对比分析

郝成元1,陈志超1,吴绍洪2   

  1. 1. 河南理工大学, 河南 焦作 454000;
    2. 中国科学院 地理科学与资源研究所, 北京 100101
  • 作者简介:郝成元(1969-),男,山东曹县人,博士,副教授,从事自然地理综合研究。
  • 基金资助:

    河南理工大学博士基金(B2006-11);国家重点基础研究发展计划:"纵向岭谷区生态系统变化及西南跨境生态安全"(973项目2003CB415101)联合资助

Abstract: As the natural boundary between the eastern Yunnan plateau and the southwestern Yunnan in Hengduan Mountains, the large-scale prominent terrain leads to obvious regional difference of climate and vegetation on both sides of Ailao Mountain. In this article, a comparative analysis is made on plant species floristic elements of sediment spore-pollen in two sample plots beside the main peak respectively. The results show that there is a remarkable difference on sediment spore-pollens between these two sample spots while there is no on the topsoil spore-pollens. The tropical genera elements of sediment spore-pollens is higher in the western sample plot (6.8%) than one in eastern part (4.7%) because the western plot is controlled by India summer monsoon at all times. And the north temperate elements of sediment spore-pollens is lower in the western sample plot (13.4%) than one in eastern part (26.4%) because the eastern plot is influenced evidently sometimes by East Asia winter monsoon. In a word, Ailao Mountain is one of important boundaries between India summer monsoon and East Asia winter monsoon.

Key words: Ailao Mountain, sediment spore-pollen, flora, India summer monsoon, East Asia winter monsoon

摘要: 哀牢山作为滇东高原与横断山系南段滇西南山地的分界线,其高大山脉造就了山体两侧气候、植被差异显著。本研究以沉积物孢粉为媒介,对山脉主峰两侧的植物物种区系成分进行对比分析。结果显示,哀牢山西坡样地受印度夏季风影响程度高于东坡样地,沉积物孢粉中热带成分大于东坡,分别为6.8%和4.7%;哀牢山东坡样地则受北来东亚冬季风影响显著,造成东坡样地孢粉中北温带成分远大于西坡样地,分别为26.4%和13.4%。哀牢山成为印度夏季风与东亚冬季风的重要分界之一。

关键词: 哀牢山, 沉积物孢粉, 植物区系, 印度夏季风, 东亚冬季风

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