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中国沙漠 ›› 2014, Vol. 34 ›› Issue (4): 982-991.DOI: 10.7522/j.issn.1000-694X.2013.00315

• 古气候与环境演变 • 上一篇    下一篇

全新世共和盆地沙地时空演化及其驱动机制

刘冰1, 靳鹤龄1, 孙忠1, 苏志珠2, 张彩霞1   

  1. 1. 中国科学院寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000;
    2. 山西大学 历史文化学院, 山西 太原 030006
  • 收稿日期:2013-01-06 修回日期:2013-02-14 出版日期:2014-07-20 发布日期:2014-07-20
  • 作者简介:刘冰(1985-),男,山西忻州人,博士,助理研究员,主要从事干旱区环境演变与气候变化的研究。Email:liubing900426@163.com
  • 基金资助:
    国家自然科学基金项目(41271215);中国科学院寒区旱区环境与工程研究所青年人才基金项目(51Y451211);中国科学院沙漠与沙漠化重点实验室开放基金项目(KLDD-2014-011)资助

Spatiotemporal Evolution of Sandy Land in the Gonghe Basin during the Holocene Period and Its Possible Driving Mechanism

Liu Bing1, Jin Heling1, Sun Zhong1, Su Zhizhu2, Zhang Caixia1   

  1. 1. Key Laboratory of Desert and Desertification, Cold and Arid Regions Environments and Engineering Research Institute, Chinese Academy of sciences, Lanzhou 730000, China;
    2. College of History and Culture, Shanxi University, Taiyuan 030006, China
  • Received:2013-01-06 Revised:2013-02-14 Online:2014-07-20 Published:2014-07-20
  • Contact: 靳鹤龄(Email:Jinhlster@gmail.com)

摘要: 通过分析青藏高原东北部共和盆地现代固定沙丘、半固定-半流动沙丘和流动沙丘的粒度与地球化学元素特征,建立了不同类型沙丘沉积物的理化指标体系,并尝试性地将其用于地质时期沙漠演化研究。同时,结合区域典型风成砂-古土壤剖面的相变特征,探讨了全新世共和盆地沙地的时空演化过程及其驱动机制。结果表明:全新世共和盆地沙地存在多次活化、扩张和固定、缩小,除11.8~10.1 ka为流动沙地以外,其余阶段多在半流动-半固定沙地和固定沙地之间频繁转换,这一变化特征与其相邻的柴达木盆地沙地和青海湖地区环境变化具有良好的可比性。此外,发现沙地环境变化对湿度状况十分敏感,而湿度又受控于区域冬,夏季风的强度,也就是说全新世共和盆地沙地演化是气候变化的产物。

关键词: 全新世, 共和盆地, 沙地演化, 气候变化

Abstract: The physical and chemical indicator system of different types of sand dune deposits was reconstructed by analyzing the characteristics of grain size and geochemical elements from the modern fixed, semi-fixed and semi-shifting and mobile sand dunes in Gonghe Basin, northeastern Qinghai-Tibetan plateau, and it is tentatively applied to the study the desert evolution in geological time. In the meanwhile, combined with variation of the sedimentary facies in typical aeolian sand-paleosol profile, we discussed the spatiotemporal changes of the Gonghe Basin sandy land during the Holocene period, and possible driving mechanism. The results indicate the region experiences the several activation, expansion and fixation, reduction. Specifically, the sandy land was dominated by the mobile dune in 11.8~10.0 ka, while frequently change among semi-fixed, semi-shifting and fixed sandy land were discovered in other periods. These characteristics are well comparative with the environmental change in adjacent Qaidam Basin desert and Qinghai lake region. In addition, we found the sandy land environment is very sensitive to the humid condition which is controlled by the winter and summer monsoonal strength. In other words, sandy land evolution in Gonghe Basin during the Holocene is product of climatic change.

Key words: Holocene, Gonghe Basin, sandy land evolution, climatic change

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