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    济州岛西南泥质区粒度组分变化的古环境应用

    向荣 杨作升 郭志刚 SaitoY. 范德江 肖尚斌 陈木宏

    向荣, 杨作升, 郭志刚, SaitoY., 范德江, 肖尚斌, 陈木宏, 2005. 济州岛西南泥质区粒度组分变化的古环境应用. 地球科学, 30(5): 582-588.
    引用本文: 向荣, 杨作升, 郭志刚, SaitoY., 范德江, 肖尚斌, 陈木宏, 2005. 济州岛西南泥质区粒度组分变化的古环境应用. 地球科学, 30(5): 582-588.
    XIANG Rong, YANG Zuo-sheng, GUO Zhi-gang, Saito Y., FAN De-jiang, XIAO Shang-bin, CHEN Mu-hong, 2005. Paleoenvironmental Implications of Grain-Size Component Variations in the Mud Area Southwest off Cheju Island, ECS. Earth Science, 30(5): 582-588.
    Citation: XIANG Rong, YANG Zuo-sheng, GUO Zhi-gang, Saito Y., FAN De-jiang, XIAO Shang-bin, CHEN Mu-hong, 2005. Paleoenvironmental Implications of Grain-Size Component Variations in the Mud Area Southwest off Cheju Island, ECS. Earth Science, 30(5): 582-588.

    济州岛西南泥质区粒度组分变化的古环境应用

    基金项目: 

    国家自然科学基金项目 90211022

    国家自然科学基金项目 40206007

    中国科学院知识创新工程项目 KZCX3-SW-220

    详细信息
      作者简介:

      向荣(1972-),男,副研究员,博士,主要从事古海洋环境研究.E-mail:rxiang@scsio.ac.cn

    • 中图分类号: P53

    Paleoenvironmental Implications of Grain-Size Component Variations in the Mud Area Southwest off Cheju Island, ECS

    • 摘要: 利用激光粒度仪对位于东海陆架济州岛西南泥质区的B2孔进行了沉积物粒度分析, 根据标准偏差变化检出了B2孔含有4个粒度组分 > 65.6、65.6~10.5、10.5~1.3和 < 1.3μm, 其中 > 65.6μm粗组分含量很低, 主要是以底栖有孔虫为主的生源沉积.各组分平均粒径和粒度含量随孔深的变化显示了65.6~10.5μm组分在B2孔含量较高(21%~30%), 变化最明显, 是该孔对环境变化最敏感的粒度组分.研究表明该敏感组分的粒度含量和平均粒径变化主要受东亚冬季风的强弱变化制约, 其变化恢复的近2ka来东亚冬季风变化和中国东部气候变化序列具有很好的一致性, 证明65.6~10.5μm粒度组分可以作为东亚冬季风的替代指标.

       

    • 图  1  研究区流系和B2孔站位分布(据刘健等, 1999改绘)

      阴影部分对应泥质沉积区

      Fig.  1.  Location of the studied core B2 and current system in the study area

      图  2  B2孔粒度频率分布曲线(a) 和标准偏差随粒级的变化(b)

      Fig.  2.  Grain-size frequency distribution (a) and grain-size standard deviation variation (b) in core B2

      图  3  B2孔3个主要粒度组分的粒度含量(a) 和平均粒径变化(b)

      Fig.  3.  Content (a) and mean-size variations (b) of 3 main grain-size components in core B2

      图  4  B2孔记录的东亚冬季风演化与中国其他气候变化序列的对比

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    • 收稿日期:  2005-05-17
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