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黄土高原东南部黄土记录的全新世东亚季风变化

许晨曦 郝青振 杨石岭 赵淑君 周鑫 葛俊逸 肖国桥

许晨曦, 郝青振, 杨石岭, 等, 2011. 黄土高原东南部黄土记录的全新世东亚季风变化. 地质力学学报, 17 (2): 175-184.
引用本文: 许晨曦, 郝青振, 杨石岭, 等, 2011. 黄土高原东南部黄土记录的全新世东亚季风变化. 地质力学学报, 17 (2): 175-184.
XU Chen-xi, HAO Qing-zhen, YANG Shi-ling, et al., 2011. EAST ASIAN MONSOON CHANGES DURING THE HOLOCENE———RECORDS FROM THE SOUTHEASTERN LOESS PLATEAU. Journal of Geomechanics, 17 (2): 175-184.
Citation: XU Chen-xi, HAO Qing-zhen, YANG Shi-ling, et al., 2011. EAST ASIAN MONSOON CHANGES DURING THE HOLOCENE———RECORDS FROM THE SOUTHEASTERN LOESS PLATEAU. Journal of Geomechanics, 17 (2): 175-184.

黄土高原东南部黄土记录的全新世东亚季风变化

基金项目: 

中国科学院知识创新工程重要方向项目 KZCX2-YW-Q1-03

详细信息
    作者简介:

    许晨曦(1985-), 男(满族), 辽宁人, 硕士。研究方向:第四纪环境.联系电话:010-82998408, Email:xuchenxi@gmail.com

  • 中图分类号: P588.23;P512.2+1

EAST ASIAN MONSOON CHANGES DURING THE HOLOCENE———RECORDS FROM THE SOUTHEASTERN LOESS PLATEAU

  • 摘要: 在全球变暖背景下,未来东亚季风的变化一直备受关注,而东亚季风演化规律的研究能够为未来的预测提供重要基础。黄土-古土壤序列几乎连续地记录了古东亚季风变化的信息,本文选取黄土高原东南部的荥阳、偃师、灵宝、吉县、丁村五个剖面进行磁化率和古风化强度分析,重建了黄土高原东南部两万年以来的东亚夏季风演化历史: 18~12 ka B. P.,季风强度较弱; 12~10 ka B. P.,季风强度显著增强; 10~6 ka B. P.,季风强度最强; 6 ka B. P.以后季风强度逐渐减弱。对比发现黄土高原东南缘全新世东亚夏季风的演化与东亚季风区不同纬度代表性记录基本同步,没有显著的区域性差别; 东亚夏季风变化主要受控于北半球低纬太阳辐射,但存在明显滞后。同时发现全新世古土壤磁化率与古风化强度峰值在地层中的位置往往不一致,在风化较强的地区,古风化强度最大值位置偏下,两个指标相比,古风化强度能够更客观地反映东亚夏季风强度。

     

  • 图  1  黄土高原观测剖面分布图

    (黑圆点为本文研究剖面位置,黑框表示有明确测年结果剖面位置)

    Figure  1.  Locations of XY, YS, LB, DC and JX sections

    图  2  黄土高原东南部荥阳、偃师、灵宝、丁村、吉县剖面磁化率与FeD/FeT值

    灰色矩形代表的是FeD/FeT的峰值位置,实线为磁化率,虚线为FeD/FeT值

    Figure  2.  Magnetic susceptibility and FeD/FeT values on XY, YS, LB, DC and JX sections Grey bar indicates maximum values of FeD/FeT. Dashed lines, FeD/FeT. Solid line, magnetic susceptibility

    图  3  黄土高原东南部黄土古风化强度与东亚夏季风指标、冰芯记录的对比

    a. GISP2冰芯中氧同位素[29]; b.三宝洞石笋氧同位素[30]; c.北纬30°太阳辐射[31]; d.黄土高原东南部古风化强度(虚线为5个剖面FeD/FeT值,实线为5个剖面平均的FeD/FeT值); e.东亚季风有效湿度指数[32]; f.渭南黄土剖面的植硅体组合重建过去20 ka的降雨量[33]; g.岱海钻孔中10 ka以来的木本花粉浓度的变化[34]; h.巴彦查干湖钻孔中10 ka以来盘星藻浓度的变化[35]

    Figure  3.  Comparison of paleo-weathering intensity in southeastern Loess Plateau and several proxies such as EAM and oxygen isotope record of ice core

    图  4  末次冰盛期与全新世气候适宜期古季风强度的空间分布

    Figure  4.  Spatial changes of paleo-monsoon intensity during the Holocene Optimum and Last Glacial Maximum

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