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    宁晋泊晚更新世以来气候变化的正构烷烃分子记录

    杨桂芳 陈正洪 张慧娟 贾晴

    杨桂芳, 陈正洪, 张慧娟, 贾晴, 2018. 宁晋泊晚更新世以来气候变化的正构烷烃分子记录. 地球科学, 43(11): 4001-4007. doi: 10.3799/dqkx.2018.575
    引用本文: 杨桂芳, 陈正洪, 张慧娟, 贾晴, 2018. 宁晋泊晚更新世以来气候变化的正构烷烃分子记录. 地球科学, 43(11): 4001-4007. doi: 10.3799/dqkx.2018.575
    Yang Guifang, Chen Zhenghong, Zhang Huijuan, Jia Qing, 2018. Paleoclimatic Variations in Ningjinpo Area since Late Pleistocene as Indicated by n-Alkanes. Earth Science, 43(11): 4001-4007. doi: 10.3799/dqkx.2018.575
    Citation: Yang Guifang, Chen Zhenghong, Zhang Huijuan, Jia Qing, 2018. Paleoclimatic Variations in Ningjinpo Area since Late Pleistocene as Indicated by n-Alkanes. Earth Science, 43(11): 4001-4007. doi: 10.3799/dqkx.2018.575

    宁晋泊晚更新世以来气候变化的正构烷烃分子记录

    doi: 10.3799/dqkx.2018.575
    基金项目: 

    北京市自然科学基金委项目 8162038

    中央高校经费基本科研业务项目 2652017216

    中央高校经费基本科研业务项目 2652017285

    详细信息
      作者简介:

      杨桂芳(1975-), 教授, 博士生导师, 长期从事全球变化与地貌演变的教学与科研工作

    • 中图分类号: P534.63

    Paleoclimatic Variations in Ningjinpo Area since Late Pleistocene as Indicated by n-Alkanes

    • 摘要: 华北地区晚更新世以来气候变化研究具有重要的意义.选择宁晋泊地区开展河湖相沉积物的分子化石研究.结果表明,沉积物中正构烷烃碳数分布范围为C15~C33,高碳数奇碳优势明显,多以C29和C31为主峰的单峰分布,少量样品出现以C17为次主峰的双峰分布,表明有机质以陆生植物和大型水生植物为主.结合正构烷烃参数,分析了宁晋泊地区晚更新世以来的气候演变过程,展现了"83~68 ka气候较为温和,湖泊水位较低;68~30 ka气候暖湿,湖泊扩张;30~22 ka气候冷干,湖泊萎缩;22~10 ka气候好转,湖泊水位上升;全新世气候温和适度,湖泊水位略有降低"的特征.区域对比分析表明,末次冰期以来宁晋泊地区与延庆盆地等地的气候变化基本一致,具有冰期-间冰期旋回特征,说明其主要受太阳辐射的控制.

       

    • 图  1  宁晋泊地理位置简图

      Fig.  1.  Sketch map showing the location of Ningjinpo area

      图  2  宁晋泊千户营剖面部分样品正构烷烃分布特征

      Fig.  2.  Distribution patterns of n-alkanes in typical samples from Qianhuying profile in Ningjinpo area

      图  3  千户营剖面正构烷烃参数与延庆盆地、太阳辐射量变化及深海氧同位素对比

      Linsley(1996)

      Fig.  3.  Distribution of n-alkanes from Qianhuying profile in Ningjinpo area in comparison with results from Yanqing basin, summer solar radiation, and oxygen isotope record in the Sulu Sea

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    • 收稿日期:  2018-02-28
    • 刊出日期:  2018-11-15

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