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新疆伊犁河谷晚全新世以来的风砂沉积与环境演化

陈秀玲 ,  李志忠 ,  凌智永 ,  靳建辉 ,  曹相东

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文章导航 > 海洋地质与第四纪地质  > 2010 >  30(6): 35-42
陈秀玲, 李志忠, 凌智永, 靳建辉, 曹相东. 新疆伊犁河谷晚全新世以来的风砂沉积与环境演化[J]. 海洋地质与第四纪地质, 2010, 30(6): 35-42. doi: 10.3724/SP.J.1140.2010.06035
引用本文: 陈秀玲, 李志忠, 凌智永, 靳建辉, 曹相东. 新疆伊犁河谷晚全新世以来的风砂沉积与环境演化[J]. 海洋地质与第四纪地质, 2010, 30(6): 35-42. doi: 10.3724/SP.J.1140.2010.06035
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CHEN Xiuling, LI Zhizhong, LING Zhiyong, JIN Jianhui, CAO Xiangdong. HOLOCENE AEOLIAN DEPOSITS AND ENVIRONMENTAL EVOLUTION IN YILI VALLEY, XINJIANG[J]. Marine Geology & Quaternary Geology, 2010, 30(6): 35-42. doi: 10.3724/SP.J.1140.2010.06035
Citation: CHEN Xiuling, LI Zhizhong, LING Zhiyong, JIN Jianhui, CAO Xiangdong. HOLOCENE AEOLIAN DEPOSITS AND ENVIRONMENTAL EVOLUTION IN YILI VALLEY, XINJIANG[J]. Marine Geology & Quaternary Geology, 2010, 30(6): 35-42. doi: 10.3724/SP.J.1140.2010.06035
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新疆伊犁河谷晚全新世以来的风砂沉积与环境演化


doi: 10.3724/SP.J.1140.2010.06035
详细信息

  • 1 福建师范大学 地理科学学院, 福州 350007;

  • 2 福建省 亚热带资源与环境重点实验室, 福州 350007;

  • 3 新疆师范大学 地理科学与旅游学院, 乌鲁木齐 830054

    • 作者简介:

    陈秀玲(1978-),女,博士,讲师,主要研究方向为第四纪环境演变,E-mail:xiulingchen@163.com

  • 基金项目:

    国家"十一五"科技支撑计划项目(2007BAC15B07)

    新疆维吾尔自治区自然科学基金项目(200821103)

  • 中图分类号: P534

HOLOCENE AEOLIAN DEPOSITS AND ENVIRONMENTAL EVOLUTION IN YILI VALLEY, XINJIANG

More Information

  • 1 Geography Science College of Fujian Normal University, Fuzhou 350007, China;

  • 2 Provincial Key Lab of Subtropical Resources and Environment of Fujian, Fuzhou 350007, China;

  • 3 Geography Science and Tourism College of Xinjiang Normal University, Urumqi 830054, China

  • 摘要: 通过对新疆伊犁塔克尔莫乎尔沙漠可克达拉剖面(TKP)有机碳(TOC)、氧化铁(Fe2O3)及频率磁化率(Xfd)的分析,探讨了新疆伊犁河谷晚全新世以来的气候演变。结果显示:3.71~1.50 kaBP期间该区气候总体上比较干旱,气候干湿变化复杂,并经历了凉湿(3.71~3.06 kaBP)、极端干旱(3.06~2.63 kaBP)和相对湿润(2.63~1.50 kaBP)的演变过程。1.50~0.50 kaBP期间TOC、Fe2O3和Xfd的平均含量均达到全剖面的最高值,可能代表着这段时期区域降水比较丰沛,为伊犁河谷地区近4 ka以来气候最为适宜的时期。0.5 kaBP以来,伊犁河谷气候迅速地向干旱化发展。
    Abstract: This paper discusses the Late Holocene climate evolution in the Yili Valley of Xinjinag, based on the TOC, Fe2O3 and Xfd from the Keledala profile in Takermohur Desert. The result shows that, in the stage of 3.71~1.50 kaBP, the climate in this area, as a whole, was relatively dry and experienced complicated changes. It was cold and humid during the period of 3.70~3.06 kaBP; extremely dry during the period of 3.06~2.63 kaBP, and relatively humid during the period of 2.63~1.50 kaBP. The average contents of TOC, Fe2O3 and Xfd reached the peak in 1.50~0.5 kaBP. It indicates that precipitation in this area was relatively high then, and the climate reached the best since 4 kaBP. Since 0.5 kaBP, the Yili valley has remained in drought.
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  • 收稿日期:  2009-12-22
  • 修回日期:  2010-09-13

新疆伊犁河谷晚全新世以来的风砂沉积与环境演化

doi: 10.3724/SP.J.1140.2010.06035
  • 1 福建师范大学 地理科学学院, 福州 350007;
  • 2 福建省 亚热带资源与环境重点实验室, 福州 350007;
  • 3 新疆师范大学 地理科学与旅游学院, 乌鲁木齐 830054
    • 作者简介:

    陈秀玲(1978-),女,博士,讲师,主要研究方向为第四纪环境演变,E-mail:xiulingchen@163.com

  • 收稿日期: 2009-12-22
  • 修回日期: 2010-09-13
基金项目:

国家"十一五"科技支撑计划项目(2007BAC15B07)

新疆维吾尔自治区自然科学基金项目(200821103)

  • 中图分类号: P534

摘要: 通过对新疆伊犁塔克尔莫乎尔沙漠可克达拉剖面(TKP)有机碳(TOC)、氧化铁(Fe2O3)及频率磁化率(Xfd)的分析,探讨了新疆伊犁河谷晚全新世以来的气候演变。结果显示:3.71~1.50 kaBP期间该区气候总体上比较干旱,气候干湿变化复杂,并经历了凉湿(3.71~3.06 kaBP)、极端干旱(3.06~2.63 kaBP)和相对湿润(2.63~1.50 kaBP)的演变过程。1.50~0.50 kaBP期间TOC、Fe2O3和Xfd的平均含量均达到全剖面的最高值,可能代表着这段时期区域降水比较丰沛,为伊犁河谷地区近4 ka以来气候最为适宜的时期。0.5 kaBP以来,伊犁河谷气候迅速地向干旱化发展。

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