2.5 Ma以来黄土稳定同位素记录的植被及夏季风变化

张普, 刘卫国, 强小科. 2.5 Ma以来黄土稳定同位素记录的植被及夏季风变化[J]. 海洋地质与第四纪地质, 2013, 33(1): 137-143. doi: 10.3724/SP.J.1140.2013.01137
引用本文: 张普, 刘卫国, 强小科. 2.5 Ma以来黄土稳定同位素记录的植被及夏季风变化[J]. 海洋地质与第四纪地质, 2013, 33(1): 137-143. doi: 10.3724/SP.J.1140.2013.01137
ZHANG Pu, LIU Wei-guo, QIANG xiao-ke. VEGETATION COVERAGE AND MONSOON VARIATION RECORDED BY STABLE CARBON ISOTOPE OF LOES SINCE 2.5MA[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 137-143. doi: 10.3724/SP.J.1140.2013.01137
Citation: ZHANG Pu, LIU Wei-guo, QIANG xiao-ke. VEGETATION COVERAGE AND MONSOON VARIATION RECORDED BY STABLE CARBON ISOTOPE OF LOES SINCE 2.5MA[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 137-143. doi: 10.3724/SP.J.1140.2013.01137

2.5 Ma以来黄土稳定同位素记录的植被及夏季风变化

  • 基金项目:

    科技部全球变化专项项目(2013CB955902);国家自然科学基金项目(41203003);西北大学博士科研启动金项目(PR10056);黄土与第四纪地质国家重点实验室开放基金课题(SKLLQG1019)

详细信息
    作者简介: 张普(1982-),女,讲师,第四纪地质专业,E-mail:zhangpu@nwu.edu.cn
  • 中图分类号: P532

VEGETATION COVERAGE AND MONSOON VARIATION RECORDED BY STABLE CARBON ISOTOPE OF LOES SINCE 2.5MA

  • 洛川剖面2.5 Ma以来有机碳同位素组成显示δ13C值的变化范围为-18.7%~-23.5‰;剖面有机碳同位素变化可分为3个阶段,均与磁化率曲线对应且呈现一致的冰期-间冰期波动。表明研究区第四纪以来主要为C3植物为主的C3、C4混合草原植被类型;黄土序列有机碳同位素δ13C值对应磁化率曲线在冰期-间冰期尺度上较好地记录了夏季风强度变化;与段家坡和渭南剖面有机碳结果对比显示,2.5 Ma以来3个剖面在构造尺度上均出现了两次明显的转变。
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收稿日期:  2012-08-19
修回日期:  2012-10-23

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