黄淮平原区晚新生代气候变迁

李宗盟, 朱文敏, 高红山, 刘芬良, 邢伟. 黄淮平原区晚新生代气候变迁[J]. 海洋地质与第四纪地质, 2021, 41(4): 179-191. doi: 10.16562/j.cnki.0256-1492.2020112303
引用本文: 李宗盟, 朱文敏, 高红山, 刘芬良, 邢伟. 黄淮平原区晚新生代气候变迁[J]. 海洋地质与第四纪地质, 2021, 41(4): 179-191. doi: 10.16562/j.cnki.0256-1492.2020112303
LI Zongmeng, ZHU Wenmin, GAO Hongshan, LIU Fenliang, XING Wei. Late Cenozoic climate changes in the Huanghuai Plain[J]. Marine Geology & Quaternary Geology, 2021, 41(4): 179-191. doi: 10.16562/j.cnki.0256-1492.2020112303
Citation: LI Zongmeng, ZHU Wenmin, GAO Hongshan, LIU Fenliang, XING Wei. Late Cenozoic climate changes in the Huanghuai Plain[J]. Marine Geology & Quaternary Geology, 2021, 41(4): 179-191. doi: 10.16562/j.cnki.0256-1492.2020112303

黄淮平原区晚新生代气候变迁

  • 基金项目: 国家自然科学基金项目“晚更新世以来淮河上游河流地貌对气候变化的响应过程研究”(41901007);信阳师范学院南湖学者奖励计划青年项目(Nanhu Scholars Program for Young Scholars of XYNU)
详细信息
    作者简介: 李宗盟(1987—),男,博士,讲师,主要从事流域地貌演化研究,E-mail:lizm@xynu.edu.cn
  • 中图分类号: P532

Late Cenozoic climate changes in the Huanghuai Plain

  • 通过梳理黄淮平原内的黄土、湖沼和石笋等剖面及钻孔沉积记录,探讨了该区晚新生代以来的气候变化特征,并对比分析了该区气候变化的时空差异。结果表明,新近纪期间东亚季风系统开始逐渐建立,研究区气候带由干旱区转为湿润区。晚新生代以来,黄淮平原区构造尺度气候变化符合东亚气候变化的一般趋势,即经历了较显著的阶段性冷干化演变。第四纪期间,黄淮平原区气候表现出典型的轨道尺度冷暖波动(冰期-间冰期旋回),可能是在全球宏观气候背景下对东亚季风强弱变化的响应。然而在千年尺度,受区域地形等局地因素的影响,黄淮平原区全新世气候变化在空间上表现出一定的差异性和穿时性。

  • 加载中
  • 图 1  黄淮平原地理位置

    Figure 1. 

    图 2  晚新生代黄淮平原区主要气候记录分布位置图

    Figure 2. 

    图 3  新生代期间中国气候带分布

    Figure 3. 

    图 4  东亚季风区晚新生代以来气候记录对比

    Figure 4. 

    图 5  黄淮平原区第四纪气候记录对比

    Figure 5. 

    图 6  黄淮平原区全新世气候记录对比

    Figure 6. 

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出版历程
收稿日期:  2020-11-23
修回日期:  2021-01-28
刊出日期:  2021-08-28

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