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内蒙古东南缘晚第四纪以来的气候环境演化

田飞 王永 迟振卿 刘瑾 江南 汤文坤 姚培毅

田飞, 王永, 迟振卿, 等, 2017. 内蒙古东南缘晚第四纪以来的气候环境演化. 地质力学学报, 23 (4): 602-611.
引用本文: 田飞, 王永, 迟振卿, 等, 2017. 内蒙古东南缘晚第四纪以来的气候环境演化. 地质力学学报, 23 (4): 602-611.
TIAN Fei, WANG Yong, CHI Zhenqing, et al., 2017. LATER QUATERNARY CLIMATIC AND ENVIRONMENTAL CHANGES IN THE SOUTHEASTERN MARGIN OF INNER MONGOLIA. Journal of Geomechanics, 23 (4): 602-611.
Citation: TIAN Fei, WANG Yong, CHI Zhenqing, et al., 2017. LATER QUATERNARY CLIMATIC AND ENVIRONMENTAL CHANGES IN THE SOUTHEASTERN MARGIN OF INNER MONGOLIA. Journal of Geomechanics, 23 (4): 602-611.

内蒙古东南缘晚第四纪以来的气候环境演化

基金项目: 

中国地质调查局项目 DD20160345

中国地质调查局项目 121201102000150010-07

中国地质调查局项目 1212011120115

详细信息
    作者简介:

    田飞(1985-), 女, 博士, 从事第四纪古环境重建研究.E-mail:tianfei_cags@foxmail.com

    通讯作者:

    王永(1968-), 男, 研究员, 从事第四纪地质与新构造研究.E-mail:wangyong@cags.ac.cn

  • 中图分类号: P534.63

LATER QUATERNARY CLIMATIC AND ENVIRONMENTAL CHANGES IN THE SOUTHEASTERN MARGIN OF INNER MONGOLIA

  • 摘要: 基于内蒙古东南缘西拉木伦河上游刘家店河湖相剖面的粒度、磁化率、微量元素地球化学指标,重建该区35 ka BP以来的气候演化过程。结果表明,在MIS 3晚期(35.23~25.15 ka BP)研究区气候条件总体温暖湿润,并伴有区域变干的趋势;MIS 2阶段(25.15~11.13 ka BP)气候整体寒冷干燥,但叠加有短暂回暖气候事件。剖面记录的末次盛冰期(LGM)出现于22.25~18.47 ka BP,此时气候极度干冷;MIS 2阶段叠加了两个短暂气候适宜期,分别出现于18.47~16.24 ka BP和14.72~11.13 ka BP。在11.13 ka BP前后研究区进入全新世,气候变得暖湿。刘家店剖面的气候记录与周边气候记录具有可对比性,揭示了区域上东亚夏季风进退具有一致性,并认为自MIS 3晚期以来东亚夏季风受北半球太阳辐射及冰量的共同驱动。此外,刘家店剖面记录揭示的千年尺度气候变化对典型气候事件具有一定的响应,推测这些千年尺度的季风强度变化可能与北大西洋经向翻转环流(AMOC)相关。

     

  • 图  1  刘家店剖面位置图

    a—研究区位置图;b—研究区地质简图(根据文献[10]修改);c—克什克腾旗年均降水和年均温统计图(1981—2010)(数据来自:http://data.cma.gov.cn/)

    Figure  1.  Location map of the Liujiadian section

    图  2  刘家店剖面粒度及磁化率特征

    Figure  2.  Grain-size distributions and magnetic susceptibility results of the Liujiadian section

    图  3  端元组分分析结果

    Figure  3.  Analysis results of end-member composition

    图  4  刘家店剖面微量元素特征

    Figure  4.  Trace elements characteristics of Liujiadian section

    图  5  刘家店剖面指标PCA分析结果

    Figure  5.  PCA results of the selected proxies from the Liujiadian section

    图  6  区域气候记录对比

    a—第一主成分(PC1);b—中值粒径;c—Rb/Sr;d—乔木花粉百分含量(AP);e—蒿藜比(A/C);f—石笋δ18O曲线来自葫芦洞PD和MSD石笋(23.50°N、119.17°E,100 m a.s.l)[26]及董哥洞D4石笋(25.28°N、108.08°E,680 m a.s.l.)[29];g—格陵兰冰芯(NGRIP,75.10°N、42.32°W,2917 m a.s.l.)δ18O曲线[30];h—北半球夏季(6月—8月)太阳辐射曲线[31];蓝色条带—Heinrich事件及新仙女木事件(YD)

    Figure  6.  Comparison of the results of the climate reconstructions from the Liujiadian section with other climate records

    表  1  刘家店剖面测年结果

    Table  1.   Dating results of the Liujiadian Section

    AMS14C测年
    样品编号深度/
    m
    测试
    材料
    年龄/
    (a BP)
    校正年龄/
    Cal a BP
    P38BF-1524全有机质6269±1157166±115
    P38-12817全有机质11751±17513606±175
    OSL测年
    样品编号深度/
    m
    等效剂量
    E.D/Gy
    环境剂量率/
    (Gy/ka)
    年龄/
    (ka BP)
    P38OSL-1172857.74±3.393.6915.64±0.92
    P38OSL-834967.22±4.583.7717.84±1.21
    P38OSL-1094129.68±6.904.7527.28±1.45
    08XL-5099124.31±6.493.3736.9±2.4
    下载: 导出CSV
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