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    南海表层沉积物中放射虫的组合特征与海洋环境

    陈木宏 张兰兰 张丽丽 向荣 陆钧

    陈木宏, 张兰兰, 张丽丽, 向荣, 陆钧, 2008. 南海表层沉积物中放射虫的组合特征与海洋环境. 地球科学, 33(6): 775-782.
    引用本文: 陈木宏, 张兰兰, 张丽丽, 向荣, 陆钧, 2008. 南海表层沉积物中放射虫的组合特征与海洋环境. 地球科学, 33(6): 775-782.
    CHEN Mu-hong, ZHANG Lan-lan, ZHANG Li-li, XIANG Rong, LU Jun, 2008. Radiolarian Assemblages in Surface Sediments of the South China Sea and Their Marine Environmental Correlations. Earth Science, 33(6): 775-782.
    Citation: CHEN Mu-hong, ZHANG Lan-lan, ZHANG Li-li, XIANG Rong, LU Jun, 2008. Radiolarian Assemblages in Surface Sediments of the South China Sea and Their Marine Environmental Correlations. Earth Science, 33(6): 775-782.

    南海表层沉积物中放射虫的组合特征与海洋环境

    基金项目: 

    国家自然科学基金课题 40476024

    国家自然科学基金课题 40631007

    国家“973”项目课题 2007CB815905

    国家科技支撑计划课题 2006BAB19B03

    详细信息
      作者简介:

      陈木宏(1956-), 男, 研究员, 主要从事微体古生物与海洋沉积地质学研究.E-mail:mhchen@scsio.ac.cn

    • 中图分类号: Q911.6

    Radiolarian Assemblages in Surface Sediments of the South China Sea and Their Marine Environmental Correlations

    • 摘要: 南海拥有较齐全的边缘海地理地貌与生态环境, 沉积物中保存的放射虫种类繁多, 个体丰富.本文采用数理统计与聚类分析方法, 对表层沉积物中放射虫的组合特征进行了较为详细的定量分析, 以期获得可靠的放射虫组合与分布的特征.聚类分析结果显示, 放射虫组合在南海表层沉积物中的分布大致可区分为5种类型: 陆架浅水区型、陆坡珊瑚礁区型、中央海盆区型、南部富营养区型和夏季上升流区型, 它们分别对应于特有的海洋环境, 并由含有某些优势种类的放射虫群落所组成.进一步分析还表明, 南海的北部、中部和南部分别表现为3个不同生态环境的海区: 北部海区受陆源影响较为明显; 中部海区被中央水团、海底火山活动和夏季上升流活动所控制; 南部海区总体上属于典型的珊瑚礁海洋环境, 生态与沉积环境明显优越于北部海区.南海表层沉积物中放射虫的组合分布特征较好地响应和反映了所在海区的生态环境与沉积条件, 是探讨古海洋环境的重要依据.

       

    • 图  1  南海表层沉积物中放射虫组合的站位聚类树状图

      Fig.  1.  Hierarchical cluster diagram of sampling stations analyzed using radiolarian assemblage similarity in the South China Sea surface sediments

      图  2  南海表层沉积物中放射虫组合的区域分布

      Ⅰ.陆架浅水区; Ⅱ-1.陆坡珊瑚礁区; Ⅱ-2.冬季上升流区; Ⅲ.中央海盆区; Ⅳ.南部富营养区; Ⅴ.夏季上升流区

      Fig.  2.  Sketch map showing regional distributions of radiolarian assemblages in the South China Sea surface sediments

      图  3  南海表层沉积物中放射虫优势种类的组合树状图

      Fig.  3.  Hierarchical cluster of radiolarian dominant species assemblages in the South China Sea surface sediments

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    • 收稿日期:  2008-04-29
    • 刊出日期:  2008-11-25

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