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

自生碳酸盐岩与底栖有孔虫碳同位素特征对多幕次甲烷事件的耦合响应——以IODP 311航次1328和1329站位为例

李清 王家生 蔡峰 梁杰 胡高伟 孙治雷 邵和宾

李清, 王家生, 蔡峰, 梁杰, 胡高伟, 孙治雷, 邵和宾. 自生碳酸盐岩与底栖有孔虫碳同位素特征对多幕次甲烷事件的耦合响应——以IODP 311航次1328和1329站位为例[J]. 海洋地质与第四纪地质, 2015, 35(5): 37-46. doi: 10.16562/j.cnki.0256-1492.2015.05.005
引用本文: 李清, 王家生, 蔡峰, 梁杰, 胡高伟, 孙治雷, 邵和宾. 自生碳酸盐岩与底栖有孔虫碳同位素特征对多幕次甲烷事件的耦合响应——以IODP 311航次1328和1329站位为例[J]. 海洋地质与第四纪地质, 2015, 35(5): 37-46. doi: 10.16562/j.cnki.0256-1492.2015.05.005
LI Qing, WANG Jiasheng, CAI Feng, LIANG Jie, HU Gaowei, SUN Zhilei, SHAO Hebin. CARBON STABLE ISOTOPES OF AUTHIGENIC CARBONATES AND BENTHIC FORAMINIFERA RECOVERED FROM SITES U1328 AND U1329 AS CO-INDICATORS OF EPISODIC METHANE SEEP EVENTS IN THE CASCADIA MARGIN[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 37-46. doi: 10.16562/j.cnki.0256-1492.2015.05.005
Citation: LI Qing, WANG Jiasheng, CAI Feng, LIANG Jie, HU Gaowei, SUN Zhilei, SHAO Hebin. CARBON STABLE ISOTOPES OF AUTHIGENIC CARBONATES AND BENTHIC FORAMINIFERA RECOVERED FROM SITES U1328 AND U1329 AS CO-INDICATORS OF EPISODIC METHANE SEEP EVENTS IN THE CASCADIA MARGIN[J]. Marine Geology & Quaternary Geology, 2015, 35(5): 37-46. doi: 10.16562/j.cnki.0256-1492.2015.05.005

自生碳酸盐岩与底栖有孔虫碳同位素特征对多幕次甲烷事件的耦合响应——以IODP 311航次1328和1329站位为例


doi: 10.16562/j.cnki.0256-1492.2015.05.005
详细信息
    作者简介:

    李清(1984-),男,助理研究员,主要从事天然气水合物地质与地球化学调查与研究,E-mail:qing.li@live.cn

  • 基金项目:

    国家自然科学基金项目(41306062,40772073,41273066,41472085)

    国土资源部水合物重点实验室开放基金项目(SHW[2014]-DX-04)

    国土资源部海洋油气与环境地质重点实验室开放基金项目(MRE201213)

  • 中图分类号: P736.4

CARBON STABLE ISOTOPES OF AUTHIGENIC CARBONATES AND BENTHIC FORAMINIFERA RECOVERED FROM SITES U1328 AND U1329 AS CO-INDICATORS OF EPISODIC METHANE SEEP EVENTS IN THE CASCADIA MARGIN

More Information
  • 摘要: 甲烷渗漏活动及其甲烷厌氧氧化(AOM)在自生碳酸盐岩沉淀的同时,也通过影响孔隙水溶解无机碳(DIC)进而影响着周围环境中底栖有孔虫,以往的文章鲜有报道二者的耦合响应。研究开展了综合大洋钻探计划IODP 311航次两个钻孔(1328和1329)中获得的自生碳酸盐岩和底栖有孔虫(Uvigerina peregrina)同位素研究,发现晚更新世以来多个层位获得的自生碳酸盐岩和底栖有孔虫的稳定碳同位素变化趋势均呈现一致的负偏碳同位素特征,但是,同层位的自生碳酸盐岩碳同位素负偏程度要比底栖有孔虫大一个数量级。自生碳酸盐岩与底栖有孔虫碳同位素变化趋势的一致性表明二者对于甲烷渗漏作用有较好的共同响应。AOM作用对孔隙水中溶解无机碳(DIC)的影响可在重碳酸氢根通过局部环境的过饱和沉淀自生碳酸盐岩的同时,也能部分参与底栖有孔虫的成壳,两者在成因方面是耦合的。综合结合自生碳酸盐岩和底栖有孔虫的碳同位素特征可以避免单一载体易受后期成岩改造影响而掩盖甲烷渗漏活动的识别。
  • [1] Suess E.Marine Cold Seeps[M]//In:Timmis K N eds. Handbook of Hydrocarbon and Lipid Microbiology. Berlin:Springer:2010:187-203.
    [2] Gieskes J, Rathburn A E, Martin J B, et al.Cold seeps in Monterey Bay, California:Geochemistry of pore waters and relationship to benthic foraminiferal calcite[J]. Applied Geochemistry, 2011,26:738-746.
    [3] Boetius A, Ravenschlag K, Schubert C J, et al. A marine microbial consortium apparently mediating anaerobic oxidation of methane[J]. Nature, 2000,407:623-626.
    [4] Borowski WS, Rodriguez N M, Paull C K, et al. Are 34S-enriched authigenic sulfide minerals a proxy for elevated methane flux and gas hydrates in the geologic record?[J]. Marine and Petroleum Geology, 2013,43:381-395. doi:10.1016/j.marpetgeo.2012.12.009.
    [5] Joseph C, Campbell K A, Torres M E, et al. 2013. Methane-derived authigenic carbonates from modern and paleoseeps on the Cascadia margin:Mechanisms of formation and diagenetic signals[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 390:52-67.
    [6] Michaelis W, Seifert R, Nauhaus K, et al. Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane[J]. Science, 2002,297:1013-1015. doi:10.1126/science.1072502.
    [7] Treude T, Niggemann J, Kallmeyer J, et al. Anaerobic oxidation of methane and sulfate reduction along the Chilean continental margin[J]. Geochimica et Cosmochimica Acta, 2005,69:2767-2779. doi:10.1016/j.gca.2005.01.002.
    [8] Magalhães V H, Pinheiro L M, Ivanov M K, et al. Formation processes of methane-derived authigenic carbonates from the Gulf of Cadiz[J]. Sedimentary Geology, 2012,243-244:155-168.
    [9] Panieri G, Camerlenghi A, Conti S, et al. Methane seepages recorded in benthic foraminifera from Miocene seep carbonates, Northern Apennines (Italy)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009,284:271-282.
    [10] 李清, 王家生, 王晓芹, 等. IODP 311航次底栖有孔虫碳稳定同位素对天然气水合物地质系统的指示[J]. 地球科学进展, 2008,23:1161-1166.[LI Qing,WANG Jiasheng,WANG Xiaoqin, et al. Stable carbon isotopic response of the benthic foraminifera from IODP 311

    to the marine methane hydrate geo-system[J]. Advances in Earth Science, 2008,23:1161-1166.]
    [11] 李清, 王家生, 蔡峰, 等. 天然气水合物系统多幕次甲烷渗漏作用的底栖有孔虫同位素响应-以IODP311航次为例[J]. 海洋地质前沿, 2011,27:29-36.[LI Qing,WANG Jiasheng,CAI Feng,et al.Carbon and oxygen stable isotopes of benthic foraminifera as possible indicators of episodic methane seeps in gas hydrate geo-system-A study from IODP Expedition 311

    [J].Marine Geology Frontiers,2011,27:29-36.]
    [12] Hill T M, Kennett J P and 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.
    [13] Hill T M, Kennett J P, Valentine D L. Isotopic evidence for the incorporation of methane-derived carbon into foraminifera from modern methane seeps, Hydrate Ridge, Northeast Pacific[J]. Geochimica et Cosmochimica Acta, 2004,68:4619-4627.
    [14] Hill T M, Kennett J P, Valentine D L, et al. Climatically driven emissions of hydrocarbons from marine sediments during deglaciation[J]. Proceedings of the National Academy of Sciences, 2006,103:13570-13574.
    [15] Kennett J P, Cannariato K G, Hendy I L, et al. Carbon isotopic evidence for methane hydrate instability during Quaternary interstadials[J]. Science, 2000,288:128-133.
    [16] Li Q, Wang J, Chen J, et al. Stable carbon isotopes of benthic foraminifers from IODP Expedition 311 as possible indicators of episodic methane seep events in a gas hydrate geosystem[J]. Palaios, 2010,25:671-681.
    [17] Mackensen A, Wollenburg J and Licari L. Low δ13C in tests of live epibenthic and endobenthic foraminifera at a site of active methane seepage[J]. Paleoceanography, 2006,21:PA2022, doi:10.1029/2005PA001196.
    [18] Martin J B, Day S A, Rathburn A E, et al. Relationships between the stable isotopic signatures of living and fossil foraminifera in Monterey Bay, California[J]. Geochemistry Geophysics Geosystems, 2004,5. doi:10.1029/2003GC000629.
    [19] Martin R A, Nesbitt E A and Campbell K A. The effects of anaerobic methane oxidation on benthic foraminiferal assemblages and stable isotopes on the Hikurangi Margin of eastern New Zealand[J]. Marine Geology, 2010,272:270-284.
    [20] Panieri G. Benthic foraminifera associated with a hydrocarbon seep in the Rockall Trough (NE Atlantic)[J]. Geobios, 2005,38:247-255.
    [21] Panieri G, Camerlenghi A, Cacho I, et al. Tracing seafloor methane emissions with benthic foraminifera:Results from the Ana submarine landslide (Eivissa Channel, Western Mediterranean Sea)[J]. Marine Geology, 2012,291-294:97-112.
    [22] Rathburn A E, Pérez 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, 2003,4:1106. doi:10.1029/2003GC000595.
    [23] 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.
    [24] Wefer G, Heinze P-M, Berger W H. Clues to ancient methane release[J]. Nature, 1994,369:282.
    [25] Kennett J P, Cannariato K G, Hendy I L, et al. Methane Hydrates in Quaternary Climate Change:The Clathrate Gun Hypothesis[M]. Washington, DC:American Geophysical Union. 2003,216.
    [26] Uchida M, Shibata Y, Ohkushi K, et al. Episodic methane release events from last Glacial marginal sediments in the western North Pacific[J]. Geochemistry Geophysics Geosystems, 2004,5. doi:10.1029/2004GC000699.
    [27] Gieskes J, Mahn C, Day S, et al. A study of the chemistry of pore fluids and authigenic carbonates in methane seep environments:Kodiak Trench, Hydrate Ridge, Monterey Bay, and Eel River Basin[J]. Chemical Geology, 2005,220:329-345.
    [28] 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, 2003,18:1062. doi:10.1029/2002PA000824.
    [29] Riddihough R. Recent movements of the Juan de Fuca plate system[J]. Journal of Geophysical Research, 1984,89:6980-6994.
    [30] Expedition 311 Scientists. Site U1328. In:Riedel M, Collett T S, Malone M J et al. eds. Proceedings of the Integrated Ocean Drilling Program, Volume 311[R]. Washington, DC:(Integrated Ocean Drilling Program Management International, Inc.),2006, doi:10.2204/iodp.proc.311.106.2006.
    [31] Expedition 311 Scientists. Site U1329. In:Riedel M, Collett T S, Malone M J et al. eds. Proceedings of the Integrated Ocean Drilling Program, Volume 311[R]. Washington, DC:(Integrated Ocean Drilling Program Management International, Inc.),2006, doi:10.2204/iodp.proc.311.107.2006.
    [32] Expedition 311 Scientists. Cascadia Margin Gas Hydrates. Integrated Ocean Drilling Program Expedition 311 Preliminary Report[R]. 2005,141.
    [33] Pierre C, Blanc Valleron M M, Rouchy J M, et al. Data report:stable isotope composition of authigenic carbonates from the northern Cascadia margin, IODP Expedition 311, Site U1325-U1329[R]. In:Riedel M, Collett T S, Malone M J et al. eds. Proceedings of the Integrated Ocean Drilling Program, Volume 311. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.). 2009,doi:10.2204/iodp.proc.311.210.2009.
    [34] Blanc Valleron M M, Pierre C, Bartier D, et al. Mineralogy of authigenic carbonates from the northern Cascadia margin, IODP Expedition 311[C]. IODP Expedition 311-2nd Post-Expedition Meeting. 2007, 9-13.
    [35] Hesse R. Pore water anomalies of submarine gas-hydrate zones as tool to assess hydrate abundance and distribution in the subsurface:What have we learned in the past decade?[J]. Earth-Science Reviews, 2003,61(1-2):149-179.
    [36] Hesse R, Harrison W E. Gas hydrates (clathrates) causing pore-water freshening and oxygen isotope fractionation in deep-water sedimentary sections of terrigenous continental margins[J]. Earth and Planetary Science Letters, 1981, 55:453-462.
    [37] Pierre C, Rouchy J M, Gaudichet A. Diagenesis in the gas hydrate sediments of the Blake Ridge:Mineralogy and stable isotope compositions of the carbonate and sulfide minerals[R]. In:Paull C K, Matsumoto R, Wallace P J et al. eds. Proceedings of the Ocean Drilling Program, Scientific Results, 2000, 164:139-146.
    [38] Hyndman R D, Davis E E. A mechanism for the formation of methane hydrate and seafloor bottom-simulating reflectors by vertical fluid expulsion[J]. Journal of Geophysical Research, 1992,97:7025-7041.
    [39] Bernhard J M, Martin J B, Rathburn A E. Combined carbonate carbon isotopic and cellular ultrastructural studies of individual benthic foraminifera:2. Toward an understanding of apparent disequilibrium in hydrocarbon seeps[J]. Paleoceanography,2010, 25:PA4206.doi:10.1029/2010PA001930.
    [40] Torres M E, Martin R A, Klinkhammer G, et al. Post depositional alteration of foraminiferal shells in cold seep settings:New insights from flow-through time-resolved analyses of biogenic and inorganic seep carbonates[J]. Earth and Planetary Science Letters, 2010,299:10-22.
  • [1] 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): 1-14. doi: 10.16562/j.cnki.0256-1492.2020123101
    [2] 张云山, 贾永刚, 尉建功.  海底冷泉原位观测装置研究回顾与展望 . 海洋地质与第四纪地质, 2021, 41(5): 1-14. doi: 10.16562/j.cnki.0256-1492.2021052002
    [3] 孔丽茹, 罗敏, 陈多福.  新西兰Hikurangi俯冲带沉积物成岩作用示踪研究:来自孔隙流体Sr同位素证据 . 海洋地质与第四纪地质, 2021, 41(5): 1-9.
    [4] 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
    [5] 李法坤, 戴黎明, 李三忠, 董昊, 刘泽, 占华旺, 王亮亮, 盛世强, 胡泽明, 王迪, 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): 1-12. doi: 10.16562/j.cnki.0256-1492.2021040601
    [6] 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): 1-8. doi: 10.16562/j.cnki.0256-1492.2021011802
    [7] 刘佳辉, 曲扬, 李伟强, 魏广祎, 孙倩元, 凌洪飞, 陈天宇.  西太平洋铁锰结壳中两类不同成因磷酸盐的元素特征、形成机制及指示意义 . 海洋地质与第四纪地质, 2021, 41(): 1-9.
    [8] 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:  721
  • HTML全文浏览量:  186
  • PDF下载量:  5
  • 被引次数: 0
出版历程
  • 收稿日期:  2014-10-13
  • 修回日期:  2015-01-11

自生碳酸盐岩与底栖有孔虫碳同位素特征对多幕次甲烷事件的耦合响应——以IODP 311航次1328和1329站位为例

doi: 10.16562/j.cnki.0256-1492.2015.05.005
    作者简介:

    李清(1984-),男,助理研究员,主要从事天然气水合物地质与地球化学调查与研究,E-mail:qing.li@live.cn

基金项目:

国家自然科学基金项目(41306062,40772073,41273066,41472085)

国土资源部水合物重点实验室开放基金项目(SHW[2014]-DX-04)

国土资源部海洋油气与环境地质重点实验室开放基金项目(MRE201213)

  • 中图分类号: P736.4

摘要: 甲烷渗漏活动及其甲烷厌氧氧化(AOM)在自生碳酸盐岩沉淀的同时,也通过影响孔隙水溶解无机碳(DIC)进而影响着周围环境中底栖有孔虫,以往的文章鲜有报道二者的耦合响应。研究开展了综合大洋钻探计划IODP 311航次两个钻孔(1328和1329)中获得的自生碳酸盐岩和底栖有孔虫(Uvigerina peregrina)同位素研究,发现晚更新世以来多个层位获得的自生碳酸盐岩和底栖有孔虫的稳定碳同位素变化趋势均呈现一致的负偏碳同位素特征,但是,同层位的自生碳酸盐岩碳同位素负偏程度要比底栖有孔虫大一个数量级。自生碳酸盐岩与底栖有孔虫碳同位素变化趋势的一致性表明二者对于甲烷渗漏作用有较好的共同响应。AOM作用对孔隙水中溶解无机碳(DIC)的影响可在重碳酸氢根通过局部环境的过饱和沉淀自生碳酸盐岩的同时,也能部分参与底栖有孔虫的成壳,两者在成因方面是耦合的。综合结合自生碳酸盐岩和底栖有孔虫的碳同位素特征可以避免单一载体易受后期成岩改造影响而掩盖甲烷渗漏活动的识别。

English Abstract

参考文献 (40)

目录

    /

    返回文章
    返回