收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 2003, Vol. 26 ›› Issue (4): 367-371.doi: 10.13826/j.cnki.cn65-1103/x.2003.04.013

• 自然地理与气候变化 • 上一篇    下一篇

艾比湖 Ash 浅孔沉积信息揭示的环境演变过程

苗壮1, 穆桂金1, 阎顺1, 谢宏琴2   

  1. 1 中国科学院新疆生态与地理研究所,乌鲁木齐 830011;
    2 中国科学院广州地球化学研究所,广州 510640
  • 收稿日期:2003-03-10 修回日期:2003-10-17 出版日期:2003-04-25 发布日期:2025-12-22
  • 作者简介:苗壮(1976–),男,硕士,研究方向为干旱区环境演变,E-mail:xjgmz@yahoo.com
  • 基金资助:
    国家重大基础研究发展规划项目(TG1999043502)课题成果

Environmental Evolution of Aiby Lake Indicated by Ash core Sediment’ s Information

MIAO Zhuang1, MU Gui-jin1, YAN Shun1, XIE Hong-qin2   

  1. 1 Xinjiang Institute of Ecology and Geography,CAS,Urumqi 830011,China;
    2 Guangzhou Institute of Geochemistry ,CAS,Guangzhou 510640,China
  • Received:2003-03-10 Revised:2003-10-17 Published:2003-04-25 Online:2025-12-22

摘要: 通过对艾比湖西南湖底1.8m浅孔的沉积特征、粒度组成、有机地化分析结合14C测年数据重建湖泊沉积时代的环境面貌。研究显示近3000年来艾比湖地区的环境总体上是相对稳定的,全球的气候波动曾引起艾比湖水位和周边环境发生一定的变化。其中艾比湖在2600~2450aBP年间湖水相对较浅,气候相对冷干。2300aBP年左右湖泊深度变浅,剖面处受到河流的影响。2300~440aBP年间是艾比湖的高水位时期,气候温暖湿润,水陆生植物繁茂。440aBP以来湖泊变浅,气候变得更加干旱。艾比湖作为一内陆干旱区封闭型湖泊,对全球环境变化的响应较为敏感,艾比湖的形成演变具有典型的干旱区代表性。

关键词: 艾比湖, 粒度特征, 有机地化, 环境演变

Abstract: As a typical closed lake in inland of arid area,Aiby lake has very sensitive response to the change of environment.The forming and evolution of Aiby lake are representative in arid area,therefore the study on forming and evolution of Aiby lake can reveals the environmental change in Aiby lake area during the geologic period.Based on the analysis of the sediment faces,granularity by Malvern2000laser granularity instrument, organic geochemical used analytical instrument of CHN in1.8m Ash core of Aiby lake southwest bottom,we rebuild the environment according different sediment era of Aiby lake with the 14C dating data.The results of this study indicate that as a whole the environment of Aiby lake area is comparatively stable in the past 3000years, but the water level of Aiby lake and the environment around the lake varied obviously mainly because of climatic vibration.During2600~2450a BP,the water level of the lake was low and the climate was cold and dry. Around2300a BP,the water level was lower than that of before.The river influenced the lake sharply.During 2300~440a BP,the water level became high ,the weather was warm and wet and the plants in land and water luxuriated.After440a BP,the Aiby lake got shallow.The climate became much more arid.As a typical closed lake in inland of arid area,Aiby lake has sensitive response to the change of globe environment.The forming and evolution of Aiby lake are representative in arid area.

Key words: Aiby Lake, grainsize characteristic, organic geochemical environmental evolution

中图分类号: 

  • F114.46