留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

南海东沙海域HD319岩心富甲烷环境底栖有孔虫群落结构

周洋 陈芳 苏新 刘广虎 陈超云

周洋, 陈芳, 苏新, 刘广虎, 陈超云. 南海东沙海域HD319岩心富甲烷环境底栖有孔虫群落结构[J]. 海洋地质与第四纪地质, 2009, 29(3): 1-8. doi: 10.3724/SP.J.1140.2009.03001
引用本文: 周洋, 陈芳, 苏新, 刘广虎, 陈超云. 南海东沙海域HD319岩心富甲烷环境底栖有孔虫群落结构[J]. 海洋地质与第四纪地质, 2009, 29(3): 1-8. doi: 10.3724/SP.J.1140.2009.03001
ZHOU Yang, CHEN Fang, SU Xin, LIU Guanghu, CHEN Chaoyun. BENTHIC FORAMINIFERA COMMUNITIES IN METHANE-RICH ENVIRONMENT SHOWED BY CORE HD319 IN DONGSHA SEA AREA OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 1-8. doi: 10.3724/SP.J.1140.2009.03001
Citation: ZHOU Yang, CHEN Fang, SU Xin, LIU Guanghu, CHEN Chaoyun. BENTHIC FORAMINIFERA COMMUNITIES IN METHANE-RICH ENVIRONMENT SHOWED BY CORE HD319 IN DONGSHA SEA AREA OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(3): 1-8. doi: 10.3724/SP.J.1140.2009.03001

南海东沙海域HD319岩心富甲烷环境底栖有孔虫群落结构


doi: 10.3724/SP.J.1140.2009.03001
详细信息
    作者简介:

    周洋(1980-),男,硕士,工程师,主要从事海洋地质与微体古生物学研究,E-mail:xtpuzy@yahoo.com.cn

  • 基金项目:

    国家自然科学基金项目(40742007,40730844)

    中国地质调查局"天然气水合物资源评价及勘探开发战略研究"基金项目(GZH200200203-02-01)

  • 中图分类号: P736.2

BENTHIC FORAMINIFERA COMMUNITIES IN METHANE-RICH ENVIRONMENT SHOWED BY CORE HD319 IN DONGSHA SEA AREA OF THE SOUTH CHINA SEA

More Information
  • 摘要: 对南海东北部东沙海域HD319岩心富甲烷环境和非富甲烷环境底栖有孔虫进行对比研究,旨在探讨富甲烷环境对底栖有孔虫群落结构的影响。结果表明,该岩心富甲烷环境和非富甲烷环境的底栖有孔虫组成有所差异:富甲烷缺氧环境底栖有孔虫群落中耐低氧类内生种群占绝对优势,Uvigerina(U.peregerina,U.hispido-costata,U.rugosa,U.probscidea,U.spp.),Bulimina(B.aculeata,B.mexicana),Bolivina(B.bradyi,B.quadrilatera),Globocassidulina subglobosa,Brizalina superba,Hoglundina elegans等冷泉甲烷相关种大量出现;非富甲烷一般低氧环境下底栖有孔虫以内生种含量占优势,表生种和旋向种零星出现;富氧环境下底栖有孔虫以表生种和旋向种占优势,受有机碳含量变化控制明显。推测底栖有孔虫这种群落结构的差异是适应高甲烷含量的结果,底栖有孔虫对富甲烷环境的响应通过群落结构的差异表现出来。
  • [1] Jones R W. Preliminary observations on benthic foraminifera associated with biogenic gas seep in the North Sea[C]//Applied Micropaleontology. Kluwer Academic, Dordrecht, 1993:69-80.
    [2] Akimoto K, Tanaka T, Hattori M, et al. Recent benthic foraminiferal assemblages from the cold seep communities-a contribution to the methane gas indicator[C]//Pacific Neogene Events in Time and Space. Tokyo, University of Tokyo Press, 1994:11-25.
    [3] Sen Gupta B K, Aharon P. Benthic foraminifera of bathyal hydrocarbon vents of the Gulf of Mexico:initial report on communities and stable isotopes[J]. Geo-Marine Letters, 1994, 14:88-96.
    [4] Sen Gupta B K, Platon E, Bernhard J M, et al. Foraminiferal colonization of hydrocarbon-seep bacterial mats and underlying sediment, Gulf of Mexico slope[J]. Journal of Foraminiferal Research, 1997, 27:292-300.
    [5] Robinson C A, Bernhard J M, Levin L A, et al. Surficial hydrocarbon seep infauna from the Blake Ridge(Atlantic Ocean, 2150 m) and the Gulf of Mexico (690~2240 m)[J]. Marine Ecology, 2004, 25(4):313-336.
    [6] Bernhard J M, Buck K R, Barry J P. Monterey Bay cold-seep biota:assemblages, abundance, and ultrastructure of living foraminifera[J]. Deep-Sea Research, 2001, 48:2233-2249.
    [7] Rathburn A E, Levin L A, Held Z, et al. Benthic foraminifera associated with cold methane seeps on the northern California margin:ecology and stable isotopic composition[J]. Marine Micropaleontology, 2000, 38:247-266.
    [8] Hill T M, Kennett J P, Spero H J. Foraminifera as indicators of methane-rich environments:a study of modern methane seeps in Santa Barbara Channel, California[J]. Marine Micropaleontology, 2003, 49:123-138.
    [9] Rathburn A E, Perez M E, Martin J B, et al. Relationships between the distribution and stable isotopic composition of living benthic foraminifera and cold methane seep biogeochemistry in Monterey Bay, California[J]. Geochemistry,Geophysics,Geosystems, 2003,4(12):1106-1122.
    [10] Hill T M, Kennett J P, Spero H J. High-resolution records of methane hydrate dissociation:ODP site 893, Santa Barbara Basin[J]. Earth and Planetary Science Letters, 2004, 223:127-140.
    [11] Heinz P, Sommer S, Pfannkuche O,et al.Living benthic foraminifera in sediments influenced by gas hydrates at the Cascadia convergent margin, NE Pacific[J]. Marine Ecology, 2005, 304:77-89.
    [12] Torres M E, Mix A C, Kinports K, et al. Is methane venting at the seafloor recorded by δ13C of benthic foraminifera shells?[J]. Paleoceanography, 2003,18(3):1062-1075.
    [13] Parnieri G, Sen Gupta, B K. Benthic foraminifera of the Blake Ridge hydrate mound, Western North Atlantic Ocean[J]. Marine Micropaleontology, 2008, 66:91-102.
    [14] Panieri G. Benthic foraminifera associated with a hydrocarbon seep in the Rockall Trough (NE Atlantic)[J]. Geobios, 2005,38:247-255.
    [15] Mackensen A, Wollenburg J, Licari L. Low δ13C in tests of live epibenthic and endobenthic foraminifera at a site of active methane seepage[J]. Paleoceanography, 2006, 21:1196-2022.
    [16] Panieri G. Benthic foraminifera response to methane release in an Adriatic Sea pockmark[J]. Rivista Italiana Paleontologia Stratigrafia (Milano), 2003, 109(3):549-562.
    [17] Chi-Yue Huang, Chih-Wei Chien, Meixun Zhao, et al. Geological study of active cold seeps in the syn-collision accretionary prism Kaoping slope off SW Taiwan[Z]. Terr. Atmos. Ocean. Sci., 2006, 17(4):679-702.
    [18] 陈芳,苏新,陆红锋,等,南海北部浅表层沉积底栖有孔虫碳同位素及其对富甲烷环境的指示[J]. 海洋地质与第四纪地质, 2007, 27(4):1-7.

    [CHEN Fang,SU Xin,LU Hongfeng, et al. Carbon stable isotopic composition of benthic foraminifers from the north of the South China Sea:indicator of methane-rich environment[J]. Marine Geology and Quaternary Geology, 2007, 27(4):1-7.]
    [19] Guo T M, Wu B H, Zhu Y H, et al. A review on the gas hydrate research in China[J]. Journal of Petroleum Science and Engineering, 2004, 41:11-20.
    [20] Fontanier C,Jorissen F J, Licari L, et al. Live benthic foraminiferal faunas from the Bay of Biscay:faunal density, composition and microhabitats[J]. Deep-Sea Research I, 2002, 49:751-785.
    [21] Abu-Zied R, Rohling E J, Jorissen F J, et al. Benthic foraminiferal response to changes in bottom-water oxygenation and organic carbon flux in the eastern Mediterranean during LGM to Recent times[J]. Marine Micropaleontology, 2008, 67:46-68.
    [22] 陈芳,苏新,Nurnberg D, 等. 南海东沙海域末次冰期最盛期以来的沉积特征[J].海洋地质与第四纪地质,2006,26(6):9-17.

    [CHEN Fang, SU Xin, Nurnberg D, et al. Sedimentation since last glaciation maximum in Dongsha area of the South China Sea[J].Marine Geology and Quaternary Geology,2006,26(6):9-17.]
    [23] 黄宝琦, 翦知湣, 林慧玲. 南海东北部晚第四纪古生产力变化[J]. 海洋地质与第四纪地质, 2000, 20(2):65-68.

    [HUANG Baoqi, JIAN Zhimin, LIN Huiling. Late Quaternary changes of paleoproductivity in the Northeastern South China Sea[J]. Marine Geology and Quaternary Geology,2000,20(2):65-68.]
    [24] 翦知湣,王律江,Kiensat M. 南海晚第四纪表层古生产力与东亚季风变迁[J].第四纪研究,1999,19(1):32-40.

    [JIAN Zhimin,WANG Lüjiang, Kienast M. Late Quaternary surface paleoproductivity and variations of the east asian monsoon in the South China Sea[J].Quaternary Sciences, 1999,19(1):30-40.]
    [25] 汪品先,卞云华,王律江,等,十五万年来的南海[M].上海:同济大学出版社,1995:115-124.[WANG Pinxian, BIAN Yunhua,WANG Lüjiang. The South China Sea since 150

    ka[M]. Shanghai:Tongji University Press,1955:115-124.]
    [26] 卞云华,王律江,汪品先. 底栖有孔虫指示含氧量与生产力——南海北部陆坡晚第四纪的实例[C]//南海晚第四纪古海洋学研究. 青岛:青岛海洋大学出版社,1992:227-233.[BIAN Yunhuan,WANG Lüjiang, WANG Pinxian. Benthonic foraminifera as indicator of oxygen content and paleoproductivity:a late Quaternary example from the northern slope of the South China Sea[C]//Contributions to Late Quaternary Paleoceanography of the South China Sea. Qingdao:Qingdao Ocean University Press,1992.

    227-233.]
    [27] 陈忠,颜文,陈木宏,等. 海底天然气水合物分解与甲烷归宿研究进展[J].地球科学进展, 2006, 21(4):394-400.

    [CHEN Zhong, YAN Wen, CHEN Muhong,et al. Advances in gas hydrate dissociation and fate of methane in marine sediment[J], Advances in Earth Science. 2006, 21(4):394-400.]
    [28] Bhaumik A K, Gupta A K. Deep-sea benthic foraminifera from gas hydrate-rich zone, Blake Ridge, Northwest Atlantic (ODP Hole 997A)[J]. Current Science, 2005, 88:12-22.
    [29] Rathburn A E, Corliss B H. The ecology of living (stained) deep-sea benthic foraminifera from the Sulu Sea[J]. Paleoceanography, 1994, 9:87-150.
    [30] Sen Gupta B K, Machin-Castillo M L. Benthic foraminifera in oxygen-poor habitats[J]. Mar. Micropaleontol, 1993, 20:183-201.
    [31] JIAN Z M,WANG L J,Kienast M, et al.Benthic foraminifera paleoceanography of the South China Sea over the last 40000 years[J].Marine Geology,1999,156(1/4):159-186.
    [32] 王律江. 南海北部晚第四纪碳同位素记录与古生产力——以SQ49-8KL柱状样为例[C]//南海晚第四纪古海洋学研究. 青岛:青岛海洋大学出版社,1992:219-226.[WANG Lüjiang. Late Quaternary carbon isotope records from the South China Sea and their bearing on paleoproductivity[C]//Contributions to Late Quaternary Paleoceanography of the South China Sea. Qingdao:Qingdao Ocean University Press, 1992

    :217-226.]
    [33] Miao Q, Thunell R C. Recent deep-sea benthic foraminiferal distributions in the South China and Sulu Seas[J]. Marine Micropaleontology, 1993, 22:1-32.
  • [1] 谢世文, 王宇辰, 舒誉, 吴宇翔, 刘冬青, 王菲.  珠一坳陷湖盆古环境恢复与优质烃源岩发育模式 . 海洋地质与第四纪地质, 2022, 42(1): 1-11. doi: 10.16562/j.cnki.0256-1492.2021081001
    [2] 李鑫, 曹红, 孙治雷, 耿威, 张喜林, 徐翠玲, 吴能友, 闫大伟, 秦双双, 张现荣, 翟滨, 王利波.  生物载体对海底冷泉-热液极端环境的地球化学记录 . 海洋地质与第四纪地质, 2021, 41(6): 1-11. doi: 10.16562/j.cnki.0256-1492.2020121401
    [3] 王小杰, 颜中辉, 刘俊, 刘欣欣, 杨佳佳.  基于模型优化的广义自由表面多次波压制技术在印度洋深水海域的应用 . 海洋地质与第四纪地质, 2021, 41(5): 221-230. doi: 10.16562/j.cnki.0256-1492.2020101202
    [4] 刘德政, 夏非.  江苏中部海岸晚第四纪沉积物的粒度与磁化率特征及其古环境意义 . 海洋地质与第四纪地质, 2021, 41(5): 210-220. doi: 10.16562/j.cnki.0256-1492.2021051901
    [5] 兰蕾, 李友川, 王一博.  南海南部海陆过渡相烃源岩的两类分布模式 . 海洋地质与第四纪地质, 2021, 41(5): 173-180. doi: 10.16562/j.cnki.0256-1492.2021011802
    [6] 秦亚超, 蓝先洪, 陆凯, 胡刚, 栾锡武, 陈珊珊.  东海南部陆架水体2011年夏季温盐结构及其对台湾暖流和黑潮入侵的指示 . 海洋地质与第四纪地质, 2021, 41(5): 151-159. doi: 10.16562/j.cnki.0256-1492.2021032402
    [7] 李法坤, 戴黎明, 杜晓东, 蔡国富, 李三忠, 董昊, 王宇.  构造-沉积耦合过程的数值模拟:以南海北部阳江凹陷为例 . 海洋地质与第四纪地质, 2021, 41(5): 139-150. doi: 10.16562/j.cnki.0256-1492.2021040601
    [8] 马晓理, 刘丽华, 徐行, 金光荣, 魏雪芹, 翟梦月.  南海南部浅表层柱状沉积物孔隙水地球化学特征对甲烷渗漏活动的指示 . 海洋地质与第四纪地质, 2021, 41(5): 112-125. doi: 10.16562/j.cnki.0256-1492.2020123101
    [9] 肖倩文, 冯秀丽, 苗晓明.  南海北部神狐海域SH37岩芯浊流沉积及其物源分析 . 海洋地质与第四纪地质, 2021, 41(5): 101-111. doi: 10.16562/j.cnki.0256-1492.2021011901
    [10] 陈唯, 赵彦彦, 李三忠, 唐智能, 杨俊, 魏浩天, 吴佳庆, 朱俊江, 刘盛, 董涛, 张广璐, 杨丹丹, 孙国静.  南海北部陆坡神狐海域SH-CL38站位的粒度特征及沉积记录 . 海洋地质与第四纪地质, 2021, 41(5): 90-100. doi: 10.16562/j.cnki.0256-1492.2021011001
    [11] 李晶, 刘昌岭, 吴能友, 贺行良, 孟庆国, 许晓晴, 陈烨.  海洋环境中甲烷好氧氧化过程的研究进展 . 海洋地质与第四纪地质, 2021, 41(5): 67-76. doi: 10.16562/j.cnki.0256-1492.2020112302
    [12] 辛友志, 孙治雷, 王红梅, 陈烨, 徐翠玲, 耿威, 曹红, 张喜林, 张现荣, 李鑫, 闫大伟, 吴能友.  海洋沉积物中金属依赖型甲烷厌氧氧化作用研究进展及展望 . 海洋地质与第四纪地质, 2021, 41(5): 58-66. doi: 10.16562/j.cnki.0256-1492.2020122801
    [13] 曾志刚, 张玉祥, 陈祖兴, 李晓辉, 齐海燕, 王晓媛, 陈帅, 殷学博.  西太平洋弧后盆地的热液系统及其岩浆环境研究 . 海洋地质与第四纪地质, 2021, 41(5): 12-24. doi: 10.16562/j.cnki.0256-1492.2021070101
    [14] 程琳燕, 李磊, 高毅凡, 张威, 龚广传, 杨志鹏, 王潘.  琼东南盆地陵水凹陷海底周期阶坎底形的特征及成因 . 海洋地质与第四纪地质, 2021, 41(5): 1-8. doi: 10.16562/j.cnki.0256-1492.2021041902
    [15] 许明, 陈建文, 袁勇, 张银国, 梁杰, 李慧君, 王建强, 吴淑玉.  华南下扬子区早寒武世幕府山组沉积环境:来自于全岩地球化学的启示 . 海洋地质与第四纪地质, 2021, 41(5): 1-9. doi: 10.16562/j.cnki.0256-1492.2020101601
    [16] 徐俊杰, 刘道涵, 陈松, 刘慧, 刘磊, 刘盼, 刘广宁.  北康盆地基底卷入断层特征及其对南海南部构造演化的启示 . 海洋地质与第四纪地质, 2021, 41(4): 116-128. doi: 10.16562/j.cnki.0256-1492.2020101701
    [17] 刘家岐, 兰晓东.  中太平洋莱恩海山富钴结壳元素地球化学特征及成因探讨 . 海洋地质与第四纪地质, 2021, 41(): 1-11.
    [18] 陈俊锦, 张经纬, 刘时桥, 陈万利, 秦永鹏, 吴时国.  中沙群岛海域表层沉积物粒度特征及其输运趋势 . 海洋地质与第四纪地质, 2021, 41(): 1-12. doi: 10.16562/j.cnki.0256-1492.2021090901
    [19] 雷雁翔, 何磊, 王玉敏, 张朋朋, 张斌, 胡蕾, 吴治国, 叶思源.  渤海湾西岸晚更新世以来的沉积环境演化及碳埋藏评价 . 海洋地质与第四纪地质, 2021, (): 1-12. doi: 10.16562/j.cnki.0256-1492.2021020101
  • 加载中
计量
  • 文章访问数:  782
  • HTML全文浏览量:  88
  • PDF下载量:  2
  • 被引次数: 0
出版历程
  • 收稿日期:  2009-01-20
  • 修回日期:  2009-05-08

南海东沙海域HD319岩心富甲烷环境底栖有孔虫群落结构

doi: 10.3724/SP.J.1140.2009.03001
    作者简介:

    周洋(1980-),男,硕士,工程师,主要从事海洋地质与微体古生物学研究,E-mail:xtpuzy@yahoo.com.cn

基金项目:

国家自然科学基金项目(40742007,40730844)

中国地质调查局"天然气水合物资源评价及勘探开发战略研究"基金项目(GZH200200203-02-01)

  • 中图分类号: P736.2

摘要: 对南海东北部东沙海域HD319岩心富甲烷环境和非富甲烷环境底栖有孔虫进行对比研究,旨在探讨富甲烷环境对底栖有孔虫群落结构的影响。结果表明,该岩心富甲烷环境和非富甲烷环境的底栖有孔虫组成有所差异:富甲烷缺氧环境底栖有孔虫群落中耐低氧类内生种群占绝对优势,Uvigerina(U.peregerina,U.hispido-costata,U.rugosa,U.probscidea,U.spp.),Bulimina(B.aculeata,B.mexicana),Bolivina(B.bradyi,B.quadrilatera),Globocassidulina subglobosa,Brizalina superba,Hoglundina elegans等冷泉甲烷相关种大量出现;非富甲烷一般低氧环境下底栖有孔虫以内生种含量占优势,表生种和旋向种零星出现;富氧环境下底栖有孔虫以表生种和旋向种占优势,受有机碳含量变化控制明显。推测底栖有孔虫这种群落结构的差异是适应高甲烷含量的结果,底栖有孔虫对富甲烷环境的响应通过群落结构的差异表现出来。

English Abstract

参考文献 (33)

目录

    /

    返回文章
    返回