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中国沙漠 ›› 1992, Vol. 12 ›› Issue (4): 13-19.

• 论文 • 上一篇    下一篇

全新世呼伦贝尔沙地环境演变的初步研究

汪佩芳   

  1. 中国科学院长春地理研究所
  • 出版日期:1992-12-20 发布日期:1992-12-20

Preliminary Study on the Environmental Changes of Hulun Buir Sandy Land Since the Holocene

Wang Peifang   

  1. Changchun Institute of Geography, Academia Sinica
  • Online:1992-12-20 Published:1992-12-20

摘要: 呼伦贝尔盟从南往北横亘着三条大沙带,在浅黄色细砂层中普遍有2-3层古土壤间夹在内。通过对古土壤的孢粉分析和14C测年分析,反映全新世以来呼伦贝尔盟沙地经历了四次固定期和四次扩展期。古土壤中孢粉组合特征是草本花粉居优势,其中蒿、藜花粉为主,植被演替由早全新世的半荒漠草原景观-中全新世的蒿类草原或榆为主的疏林草原-晚全新世的杂类草草原,它们均属于沙地草场的类型,对固定沙丘和发展当地畜牧业起着极重要的作用。因此,根据占植被的演替规律,应对现有沙地草场采取保护措施,防止该区沙地再次扩大。

关键词: 呼伦贝尔沙地, 孢粉分析, 中新世环境变化

Abstract: There are three layers of paleosols in the light-yellow fine sand layer of the Hulun Buir Sandy-land,The analytical results of spore-pollen and 14C dating reflect that the sandy land experienced four fixed periods and four mobile periods since the Holocene.The spore-pollen assemblages in the paleosol indicated that the wood pollens were lese herb pollens occupied a dominant place and the paleobotanical successive series were subdesert steppe→Artemisia stepper→Sparse forest steppe→Chenopodi aceae and weed steppe.all of these vegetation types belongs to the type of sandyland grassland.According to the successive laws of ancient vegetation we must protect the sandland grassland and avoid the expansion of shifting sand.