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    晚冰期以来月亮湖孢粉记录反映的古植被与古气候演化

    伍婧 刘强

    伍婧, 刘强, 2012. 晚冰期以来月亮湖孢粉记录反映的古植被与古气候演化. 地球科学, 37(5): 947-954. doi: 10.3799/dqkx.2012.103
    引用本文: 伍婧, 刘强, 2012. 晚冰期以来月亮湖孢粉记录反映的古植被与古气候演化. 地球科学, 37(5): 947-954. doi: 10.3799/dqkx.2012.103
    WU Jing, LIU Qiang, 2012. Pollen-Recorded Vegetation and Climate Changes from Moon Lake since Late Glacial. Earth Science, 37(5): 947-954. doi: 10.3799/dqkx.2012.103
    Citation: WU Jing, LIU Qiang, 2012. Pollen-Recorded Vegetation and Climate Changes from Moon Lake since Late Glacial. Earth Science, 37(5): 947-954. doi: 10.3799/dqkx.2012.103

    晚冰期以来月亮湖孢粉记录反映的古植被与古气候演化

    doi: 10.3799/dqkx.2012.103
    基金项目: 

    科技部"973计划"项目 2010CB950201

    国家自然科学基金面上项目 40872206

    详细信息
      作者简介:

      伍婧(1982-), 女, 博士, 主要从事第四纪孢粉学研究.E-mail: wujing@mail.iggcas.ac.cn

    • 中图分类号: P534.63

    Pollen-Recorded Vegetation and Climate Changes from Moon Lake since Late Glacial

    • 摘要: 地处季风/非季风影响过渡地带的月亮湖是大兴安岭中段阿尔山-柴河火山区中的一个火山口湖.其长8.86 m的沉积岩心孢粉记录, 揭示了末次冰期晚期以来的古植被演化和古气候变化历史: 20.9~18.0 cal. ka B.P.期间研究区的植被为典型草原, 气候寒冷干旱; 18.0~15.3 cal. ka B.P.期间研究区的植被为草甸草原, 气候寒冷湿润; 15.3~14.0 cal. ka B.P.期间乔木开始在当地发育, 植被开始由草甸草原向森林草原转变, 气候向较为温暖湿润的方向转变; 14.0~12.8 cal. ka B.P.期间森林草原在温暖湿润的气候影响下, 森林扩张, 草原退缩, 与Bølling-Allerød暖期相对应; 12.8~11.8 cal. ka B.P.期间草原在寒冷气候下扩张, 可与新仙女木期相对应; 11.8~0.8 cal. ka B.P. 期间在较为温暖的气候条件下, 草原在气候快速变冷事件的影响下发生了多次扩张, 其中, 较为明显的6次气温突降事件分别发生在9.0~8.9, 8.2~7.8, 7.0~6.8, 6.1~5.6, 5.4~5.2, 2.3~1.8 cal. ka B.P..这些快速气候变化事件与全球和区域中其他高分辨率古气候记录具有可比性, 揭示出月亮湖敏感地记录了全球和区域气候的变化, 同时也表明研究区的高分辨率孢粉分析是研究东亚季风强度变化的良好指标.

       

    • 图  1  研究区植被分布及取样点位置

      Fig.  1.  Sample site location and vegetation surrounding

      图  2  月亮湖沉积序列主要孢粉类型百分含量

      Fig.  2.  Pollen percentage of major taxa of Moon Lake

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    • 收稿日期:  2011-11-09
    • 网络出版日期:  2021-11-10
    • 刊出日期:  2012-09-15

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