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创建日期 2001.02.05 更新日期 2005.10.6. E-mail shygaobnu.edu.cn. 主要学术贡献是与合作者一起就我国沙漠的形成时代演化规律发展模式和成因等进行了深入的研究并提出 中国沙漠形成于200多万年前是第四纪全球气候变冷和青藏高原隆起的产物 受冰期气候波动和青藏高原阶段性隆起过程的影响中国沙漠亦经历了阶段性逐步扩大的发展过程 中国沙漠特别是季风区沙漠在演化上基本服从于亚洲季风的变化规律经历了流沙活动扩大与缩小固定的交替变化过程
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高尚玉简历

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创建日期 2001.02.05 更新日期 2005.10.6. E-mail shygaobnu.edu.cn. 主要学术贡献是与合作者一起就我国沙漠的形成时代演化规律发展模式和成因等进行了深入的研究并提出 中国沙漠形成于200多万年前是第四纪全球气候变冷和青藏高原隆起的产物 受冰期气候波动和青藏高原阶段性隆起过程的影响中国沙漠亦经历了阶段性逐步扩大的发展过程 中国沙漠特别是季风区沙漠在演化上基本服从于亚洲季风的变化规律经历了流沙活动扩大与缩小固定的交替变化过程

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马玉贞-教授博士生导师

Vegetation changes and associated climate variations during the past 38,000 years reconstructed from the Shaamar eolian-paleosol section, northern Mongolia. Kam-biu Liu, Zhaodong Feng, Yanli Sang, Wei Wang, Aizhi Sun. A survey of modern pollen and vegetation along a north-south transect in Mongolia.

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