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    黄土高原西部石笋记录的H2事件特征

    吴秀平 吴锦奎 侯典炯 丁明虎 孙维君 桑文翠 刘伟刚

    吴秀平, 吴锦奎, 侯典炯, 丁明虎, 孙维君, 桑文翠, 刘伟刚, 2013. 黄土高原西部石笋记录的H2事件特征. 地球科学, 38(3): 471-481. doi: 10.3799/dqkx.2013.047
    引用本文: 吴秀平, 吴锦奎, 侯典炯, 丁明虎, 孙维君, 桑文翠, 刘伟刚, 2013. 黄土高原西部石笋记录的H2事件特征. 地球科学, 38(3): 471-481. doi: 10.3799/dqkx.2013.047
    WU Xiu-ping, WU Jin-kui, HOU Dian-jiong, DING Ming-hu, SUN Wei-jun, SANG Wen-cui, LIU Wei-gang, 2013. Characteristics and Variability of Heinrich-2 Event Recorded by Stalagmite Oxygen Isotopic Composition in the Western Loess Plateau. Earth Science, 38(3): 471-481. doi: 10.3799/dqkx.2013.047
    Citation: WU Xiu-ping, WU Jin-kui, HOU Dian-jiong, DING Ming-hu, SUN Wei-jun, SANG Wen-cui, LIU Wei-gang, 2013. Characteristics and Variability of Heinrich-2 Event Recorded by Stalagmite Oxygen Isotopic Composition in the Western Loess Plateau. Earth Science, 38(3): 471-481. doi: 10.3799/dqkx.2013.047

    黄土高原西部石笋记录的H2事件特征

    doi: 10.3799/dqkx.2013.047
    基金项目: 

    国家自然科学基金委员会重点项目 41130638

    冰冻圈科学国家重点实验室开放基金项目 SKLCS 2010-10

    冰冻圈科学国家重点实验室自主研究项目 SKLCS-ZZ-2010-02

    详细信息
      作者简介:

      吴秀平(1983-), 女, 博士研究生, 主要从事全球变化与地球科学信息研究.E-mail: tunxp07@lzu.edu.cn

      通讯作者:

      吴锦奎, E-mail: jkwu@lzb.ac.cn

    • 中图分类号: P597

    Characteristics and Variability of Heinrich-2 Event Recorded by Stalagmite Oxygen Isotopic Composition in the Western Loess Plateau

    • 摘要: 青藏高原与黄土高原过渡带的甘肃武都万象洞位于现代夏季风的边缘区, 对气候变化极为敏感.通过洞内一支石笋WX40D的6个高精度TIMS-U系定年数据和616个样品的氧同位素测定, 建立了28.3~23.0 ka B.P., 分辨率约为10年的亚洲季风气候变化序列. 石笋δ18O记录揭示Marine Isotope Stage 2 (MIS2)早期东亚季风气候具有10~100 a尺度高频震荡特征, 从中识别出北大西洋Heinrich 2 (H2)特强冷事件, 且记录显示该事件开始于24.6 ka B.P., 呈突发式降温之后持续跌宕式降温变化. 对比研究发现, 万象洞石笋δ18O记录H2事件与葫芦洞、天鹅洞的石笋记录有差别, 但是与湖南金滩湾洞穴石笋δ18O记录、33°N太阳辐射强度以及极地GRIP冰心记录变化趋势一致, 表明季风边缘区气候变化主要受北半球中纬度太阳辐射能背景、北大西洋冰漂碎屑带的扩张以及低纬太平洋海表温度变化等因素的控制, 同时万象洞特殊的地理位置使得区域气候更易受到与极地气候有密切联系的亚洲冬季风和西风环流变化的影响.

       

    • 图  1  万象洞石笋WX40D剖面(白色箭头标示了年代采样点所在层位)

      Fig.  1.  Profile of stalagmite WX40D from Wanxiang Cave

      图  2  石笋WX40D年代-深度模型

      Fig.  2.  The relationship of WX40D stalagmite 230Th dating and depth

      图  3  万象洞WX40D石笋δ18O记录

      短线为WX40D石笋的实测年龄和误差;虚线为生长时段内WX40D石笋δ18O记录平均值;两处阴影分别为H2事件和Ⅰ、Ⅱ阶段的分界线

      Fig.  3.  The δ18O record of stalagmite WX40D from Wanxiang Cave, Gansu Province

      图  4  末次冰期晚期万象洞石笋WX40D δ18O与WX42A灰度记录(张德忠等, 2011)的H事件

      Fig.  4.  Comparison H events recorded by WX40D δ18O and WX42A gray scale during late last glacial

      图  5  万象洞WX40D石笋δ18O与格陵兰冰心记录GRIP温度记录(Rasmussen et al., 2008)

      Fig.  5.  Comparison of δ18O record of stalagmite WX40D Wanxiang Cave with GRIP

      图  6  万象洞WX40D石笋δ18O与东亚季风区石笋δ18O记录(葫芦洞,湖南金滩湾洞)

      灰色阴影为H2事件

      Fig.  6.  Comparison of δ18O record of WX40D stalagmite Wanxiang Cave with Hulu Cave

      表  1  万象洞石笋WX40D的MC-ICP-MS铀系定年结果

      Table  1.   Results of 230Th dating for WX40D

      样品编号 距离(mm) 238U(10-9) 232Th(10-12) d234U*测量值 230Th/238U活度比 230Th年龄(a)(未校正) 230Th年龄(a)(校正年龄)
      WX40D-1 38.0 7 075±6 793±16 604±2.0 0.311 2±0.000 5 23 212±50 23 150±50
      WX40D-2 50.5 4 087±3 339±8 559±1.8 0.329 8±0.000 4 25 559±50 25 497±50
      WX40D-3 54.0 6 301±5 311±8 554±1.8 0.331 0±0.000 4 25 747±47 25 686±47
      WX40D-4 73.0 4 178±3 619±13 531±1.7 0.339 5±0.000 4 26 944±51 26 881±51
      WX40D-5 79.0 2 143±2 504±11 525±2.1 0.350 1±0.0005 28 022±65 27 958±65
      WX40D-6 99.5 4 890±3 740±16 612±1.8 0.374 5±0.000 5 28 360±55 28 297±55
      注:λ230=9.157 7×10-6 a-1λ234=2.826 3×10-6 a-1λ238=1.551 25×10-10 a-1δ234U=([234U/238U]活度比-1)×1 000,δ234U初始值根据230Th年龄(T)计算获得,即δ234U初始值= δ234U测量值×e234× T230Th年龄的校正值是假设初始230Th/232Th原子比为(4.4±2.2)×10-6.
      下载: 导出CSV
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