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    山东东营凹陷古近纪湖相藻礁群落结构及古生态特征

    李国山 王永标 卢宗盛 廖卫 侯玮伟

    李国山, 王永标, 卢宗盛, 廖卫, 侯玮伟, 2011. 山东东营凹陷古近纪湖相藻礁群落结构及古生态特征. 地球科学, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110
    引用本文: 李国山, 王永标, 卢宗盛, 廖卫, 侯玮伟, 2011. 山东东营凹陷古近纪湖相藻礁群落结构及古生态特征. 地球科学, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110
    LI Guo-shan, WANG Yong-biao, LU Zong-sheng, LIAO Wei, HOU Wei-wei, 2011. Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China. Earth Science, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110
    Citation: LI Guo-shan, WANG Yong-biao, LU Zong-sheng, LIAO Wei, HOU Wei-wei, 2011. Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China. Earth Science, 36(6): 1044-1052. doi: 10.3799/dqkx.2011.110

    山东东营凹陷古近纪湖相藻礁群落结构及古生态特征

    doi: 10.3799/dqkx.2011.110
    基金项目: 

    国家油气重大专项 2009ZX05009

    国家自然科学基金 40730209

    详细信息
      作者简介:

      李国山(1986-), 男, 硕士研究生, 主要从事古生物学与地层学研究

      通讯作者:

      王永标, E-mail: Wangyb@cug.edu.cn

    • 中图分类号: P52;P534

    Community Structure and Paleoecology of Paleogene Lacustrine Cladosiphonia Reefs in the Dongying Depression, Shandong Province, China

    • 摘要: 地质历史上的生物礁主要为海相生物礁.海相生物礁中生物种类丰富, 而且常常出现在正常的海洋环境中.陆相湖泊生物礁则极为少见, 而且造礁生物种类单调, 常常出现在特有的湖泊环境.山东东营凹陷古近纪湖相藻礁主要由绿藻门的枝管藻形成礁体的骨架, 蓝细菌藻纹层起粘结作用.居礁生物种类十分单调, 但数量丰富, 主要包括广盐性的介形类、小型腹足类和龙介类.在湖相藻礁建造过程中, 早期碳酸盐成岩作用产生的纤维状方解石十分发育, 对加固枝管藻骨架起到了重要作用.同时, 大量早期碳酸盐胶结物的存在表明当时湖泊水体的碳酸盐饱和度较高.藻礁发育的古近纪在世界许多地方出现蒸发岩沉积, 反映藻礁总体是在气候比较干旱的时期形成的.枝管藻藻礁不但对古生态和气候具有重要的指示意义, 而且对油气储集层的研究勘探也有重要价值.

       

    • 图  1  东营凹陷新生代沉积地层序列(据中国石油地质志·卷六,1993修改)

      Fig.  1.  Lithologic column profile and facies showing the Paleogene and Neogene reefs in Dongying depression

      图  2  济阳坳陷第三纪湖相生物礁分布(据杜韫华,1996修改)

      1.藻礁;2.藻礁丘;3.藻生物层

      Fig.  2.  Locality of the Jiyang sag and Paleogene lacustrine reefs

      图  3  山东东营凹陷古近纪藻礁中的中国枝管藻

      滨斜171井,沙河街组四段,井深1854~1859m,光面

      Fig.  3.  Cladosiphonia sinensis in the Paleogene reefs in Dongying depression, Shandong Province

      图  4  山东东营凹陷古近纪藻礁中不同类型的枝管藻

      a和b.中国枝管藻;c和d.山东枝管藻.滨斜171井,沙河街组四段,井深1854~1859m,显微镜下照片

      Fig.  4.  Species of Cladosiphonia in the Paleogene reefs in Dongying depression, Shandong Province

      图  5  山东东营凹陷古近纪藻礁中的藻粘结灰岩(a)和藻粘结岩中的藻纹层(b)

      Ⅰ.腹足类,被藻粘结层包裹或充填在粘结岩之间;Ⅱ.藻粘结岩;滨斜171井,沙河街组四段,井深1854~1859m,光面;b图为显微镜下照片

      Fig.  5.  Bindstone (a) and algae laminar (b) in the Paleogene reefs in Dongying depression, Shandong Province

      图  6  山东东营凹陷古近纪藻礁中的居礁生物化石

      a.介形类化石,偏光镜下照片;b.腹足类化石,手标本照片;c.龙介虫管横断面,扫描电镜照片;d.龙介虫管分层的微细构造,扫描电镜照片.滨斜171井,沙河街组四段,井深1854~1859m

      Fig.  6.  Reef-dwelling organisms in the Paleogene reef in Dongying depression, Shandong Province

      图  7  早期成岩作用形成的纤维状方解石和埋藏成岩作用形成的粗晶方解石

      a.纤维状方解石;白色部分为粗晶方解石.滨斜171井,沙河街组四段,井深1854~1859m,显微镜下照片

      Fig.  7.  Fibrous calcite as the product of early diagenesis in marine environment and sparry calcite formed under the condition of burial diagenesis

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    出版历程
    • 收稿日期:  2011-06-09
    • 网络出版日期:  2021-11-10
    • 刊出日期:  2011-06-15

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