墨西哥湾布什山冷泉碳酸盐岩沉积岩石学及地球化学

邸鹏飞, 冯东, 陈多福, Harry H Roberts. 墨西哥湾布什山冷泉碳酸盐岩沉积岩石学及地球化学[J]. 海洋地质与第四纪地质, 2009, 29(2): 49-57. doi: 10.3724/SP.J.1140.2009.02049
引用本文: 邸鹏飞, 冯东, 陈多福, Harry H Roberts. 墨西哥湾布什山冷泉碳酸盐岩沉积岩石学及地球化学[J]. 海洋地质与第四纪地质, 2009, 29(2): 49-57. doi: 10.3724/SP.J.1140.2009.02049
DI Pengfei, FENG Dong, CHEN Duofu, Harry H Roberts. GEOLOGY AND GEOCHEMISTRY OF SEEP CARBONATES FROM BUSH HILL OF THE GULF OF MEXICO[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 49-57. doi: 10.3724/SP.J.1140.2009.02049
Citation: DI Pengfei, FENG Dong, CHEN Duofu, Harry H Roberts. GEOLOGY AND GEOCHEMISTRY OF SEEP CARBONATES FROM BUSH HILL OF THE GULF OF MEXICO[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 49-57. doi: 10.3724/SP.J.1140.2009.02049

墨西哥湾布什山冷泉碳酸盐岩沉积岩石学及地球化学

  • 基金项目:

    中国科学院广州天然气水合物研究中心项目(o807s4)

    国家杰出青年基金项目(40725011)

    国家重点基础研究规划项目(2009CB219506)

    NSFC-广东联合基金项目(U0733003)

详细信息
    作者简介: 邸鹏飞(1982-),男,博士生,主要从事海底冷泉及天然气水合物研究,E-mail:dipf06@gig.ac.cn
  • 中图分类号: P736.3

GEOLOGY AND GEOCHEMISTRY OF SEEP CARBONATES FROM BUSH HILL OF THE GULF OF MEXICO

  • 对墨西哥湾布什山采集的7块冷泉碳酸盐岩样品进行了沉积岩石学及地球化学研究,结果表明:冷泉碳酸盐岩以结壳的形式产出,结壳中双壳类和管状蠕虫等冷泉生物碎屑发育,结壳主要由泥晶、微晶和亮晶文石组成(含量89%~99%,平均94%)。碳酸盐岩13C中等亏损(δ13C最负值为-29.4‰,PDB),表明碳的来源主要是非甲烷的碳烃化合物,18O相对富集(δ18O为+2.4‰~+5.0‰,PDB),可能与原地水合物分解形成富集18O的孔隙水有关。碳酸盐矿物相(5%硝酸可溶部分)的稀土元素总量较低(0.40×10-6~20.85×10-6),稀土元素Ce异常特征和页岩标准化配分模式在不同样品、甚至同一样品结晶程度不同的碳酸盐矿物相(泥晶、微晶和亮晶)中变化显著,表明布什山冷泉碳酸盐岩形成过程中氧化还原条件复杂多变,控制氧化环境变化的主要因素可能是流体的渗漏速率。
  • 加载中
  • [1]

    Roberts H H, Aharon P. Hydrocarbon-derived carbonate buildups of the northern Gulf of Mexico continental slope:A review of submersible investigations[J]. Geo-Marine Letters, 1994, 14:135-148.

    [2]

    Peckmann J, Reimer A, Luth U, et al. Methane-derived carbonates and authigenic pyrite from the northwestern Black Sea[J]. Marine Geology, 2001, 177:129-150.

    [3]

    Hinrichs K U, Hayes J M, Sylva S P. Methane-consuming archaebacteria in marine sediments[J]. Nature, 1999, 398:802-805.

    [4]

    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.

    [5]

    冯东,陈多福,苏正,等.海底甲烷缺氧氧化与冷泉碳酸盐岩沉淀动力学研究进展[J].海洋地质与第四纪地质,2006,26(3):125-131.

    [FENG Dong, CHEN Duofu, SU Zheng, et al. Anaerobic oxidation of methane and seep carbonate precipitation kinetics at seafloor[J]. Marine Geology and Quaternary Geology, 2006, 26(3):125-131.]

    [6]

    Chen D F, Huang Y Y, Yuan X L, et al. Seep carbonates and preserved methane oxidizing archaea and sulfate reducing bacteria fossils suggest recent gas venting on the seafloor in the northeastern South China Sea[J]. Marine and Petroleum Geology, 2005, 22:613-621.

    [7]

    Aloisi G, Pierre C, Rouchy J M, et al. Methane-related authigenic carbonates of eastern Mediterranean Sea mud volcanoes and their possible relation to gas hydrate destabilization[J]. Earth and Planetary Science Letters, 2000, 184:321-338.

    [8]

    陈忠, 颜文, 陈木宏, 等. 南海北部大陆坡冷泉碳酸盐结核的发现:海底天然气渗漏活动的新证据[J]. 科学通报, 2006, 51(9):1065-1072.

    [CHEN Zhong,YAN Wen,CHEN Muhong,et al. Discovery of seep carbonate nodules as new evidence for gas venting on the northern continental slope of South China Sea[J]. Chinese Science Bulletin,2006,51(10):1228-1237.]

    [9]

    蒋干清,史晓颖,张世红.甲烷渗漏构造、水合物分解释放与新元古代冰后期盖帽碳酸盐岩[J]. 科学通报, 2006, 51(10):1121-1138.

    [JIANG Ganqing, SHI Xiaoying, ZHANG Shihong. Methane seep, methane hydrate destabilization, and the late Neoproterozoic postglacial cap carbonates[J]. Chinese Science Bulletin, 2006, 51(10):1152-1173.]

    [10]

    Aloisi G, Bouloubassi I, Heijs S K, et al. CH4-consuming microorganisms and the formation of carbonate crusts at cold seeps[J]. Earth and Planetary Science Letters, 2002, 203:195-203.

    [11]

    Paull C K, Hecker B, Commeau, R, et al. Biological communities at the Florida escarpment resemble hydrothermal vent Taxa[J]. Science, 1984, 226:965-967.

    [12]

    Peckmann J, Thiel V. Carbon cycling at ancient methane-seeps[J]. Chemical Geology, 2004, 205:443-467.

    [13]

    Campbell K A. Hydrocarbon seep and hydrothermal vent paleoenvironments and paleontology:Past developments and future research directions[J]. Palaeogeography Palaeoclimatology Palaeoecology, 2006, 232:362-407.

    [14]

    陈多福,陈先沛,陈光谦.冷泉流体沉积碳酸盐岩的地质地球化学特征[J].沉积学报,2002,20(1):34-40.

    [CHEN Duofu, CHEN Xianpei, CHEN Guangqian. Geology and geochemistry of cold seepage and venting-related carbonates[J]. Acta Sedimentologica sinica, 2002, 20(1):34-40.]

    [15]

    冯东,陈多福,苏正,等. 海底天然气渗漏系统微生物作用及冷泉碳酸盐岩的特征[J]. 现代地质, 2005, 19(1):26-32.

    [FENG Dong,CHEN Duofu,SU Zheng,et al.characteristics of cold seep carbonates and microbial processes in gas seep system[J].Geosciences, 2005, 19(1):26-32.]

    [16]

    Hovland M, Talbot M R, Qvale H, et al. Methane-related carbonate cements in pockmarks of the North Sea[J]. Journal of Sedimentary Research, 1987, 57:881-892.

    [17]

    Naehr T H, Rodriguez N M, Bohrmann G, et al. Methane derived authigenic carbonates associated with gas hydrate decomposition and fluid venting above the Blake Ridge Diapir[C]//In:Paull C K, Matsumoto R, Wallace P J, et al (Eds.). Proceedings of the Ocean Drilling Program. Scientific Results, 2000,164:285-300.

    [18]

    Hesse R. Pore water anomalies of submarine gas-hydrate zone as tool to assess hydrate aboundance and distribution in subsurface:what have we learned in the past decade[J]. Earth-Science Reviews, 2003, 61:149-179.

    [19]

    Sholkovitz E, Shen G T. The incorporation of rare earth elements in modern coral[J]. Geochimica et Cosmochimica Acta, 1995, 59:2749-2756.

    [20]

    Barrat J A, Boulegue J, Tiercelin J J, et al. Strontium isotopes and rare-earth element geochemistry of hydrothermal carbonate deposits from Lake Tanganyika, East Africa[J]. Geochimica et Cosmochimica Acta, 2000, 64:287-298.

    [21]

    Feng D, Chen D F, Qi L, et al. Petrographic and geochemical characterization of seep carbonate from Alaminos Canyon, Gulf of Mexico[J]. Chinese Science Bulletin, 2008, 53:1716-1724.

    [22]

    Feng D, Chen D F, Roberts H H. Sedimentary fabrics in the authigenic carbonates from Bush Hill:implication for seabed fluid flow and its dynamic signature[J]. Geofluids, 2008, 8:301-310.

    [23]

    Feng D,Chen D F,Peckmann J. Rare earth elements in seep carbonates as tracers of variable redox conditions of ancient hydrocarbon seeps[J]. Terra Nova, 2009, 21:49-56.

    [24]

    陈多幅, 王茂春, 徐文新. 墨西哥湾西北陆坡天然气水合物资源评价[J]. 海洋地质动态. 2003,19(12):14-17

    [CHEN Duofu, WANG Maochun, XU Wenxin. Assessment of resources and economic potential of gas hydrate in the northwestern Gulf of Mexico continental slope[J]. Marine Geology Letters, 2003, 19(12):14-17.]

    [25]

    MacDonald I R, Boland G S, Baker J S, et al. Gulf of Mexico hydrocarbon seep communities[J]. Marine Biology, 1989, 101:235-247.

    [26]

    Tryon M D, Brown K M. Fluid and chemical cycling at Bush Hill:Implications for gas and hydrate-rich environments[J]. Geochemistry Geophysics Geosystems, 2004,5,doi:10.1029/2004GC000778.

    [27]

    Chen D F, Cathles L M. A kinetic model for the pattern and amounts of hydrate precipitated from a gas steam:Application to the Bush Hill vent site, Green Canyon Block 185, Gulf of Mexico[J]. Journal of Geophysical Research-Solid Earth, 2003, 108:1-7.

    [28]

    Chen D F, Cathles L M, Roberts H H. The geochemical signatures of variable gas venting at gas hydrate sites[J]. Marine and Petroleum Geology, 2004, 21:317-326.

    [29]

    Sassen R, Milkov A V, Ozgul E, et al. Gas venting and subsurface charge in the Green Canyon area, Gulf of Mexico continental slope:evidence of a deep bacterial methane source?[J]. Organic Geochemistry, 2003, 34:1455-1464.

    [30]

    Joye S B, Boetius A, Orcutt B N, et al. The anaerobic oxidation of methane and sulfate reduction in sediments from Gulf of Mexico cold seeps[J]. Chemical Geology, 2004, 205:219-238.

    [31]

    Roberts H, Wiseman W Jr, Hooper J, et al. Surficial gas hydrates of the Louisiana continental slope initial results of direct observations and in situ data collection[J]. Offshore Technology Conf, Houston, TX, 1999, 10770:259-272.

    [32]

    Leifer I, MacDonald I. Dynamics of the gas flux from shallow gas hydrate deposits:interaction between oily hydrate bubbles and the oceanic environment[J]. Earth and Planetary Science Letters, 2003, 210:411-424.

    [33]

    Taylor J C. Computer programs for standardless quantitative analysis of minerals using the full power diffraction profile[J]. Power Diffration,1991, 6:2-9.

    [34]

    Qi L, Gregoire D C. Determination of trace elements in twenty six Chinese geochemistry reference materials by inductively coupled plasma-mass spectrometry[J]. Geostandards and Geoanalytical Research, 2000, 24:51-63.

    [35]

    Qi L, Zhou M F, Malpas J, et al. Determination of rare earth elements and Y in ultramafic rocks by ICP-MS after preconcentration using Fe(OH)3 and Mg(OH)2 coprecipitation[J]. Geostandards and Geoanalytical Research, 2005, 29:131-141.

    [36]

    Feng D, Chen D F, Roberts H H. Petrographic and geochemical characterization of seep carbonate from Bush Hill (GC 185) gas vent and hydrate site of the Gulf of Mexico[J]. Marine and Petroleum Geology,2009, in press.

    [37]

    Roberts H H, Aharon P, Walsh M M. Cold-seep carbonates of the Louisiana continental slope-to-basin floor[C]//In:Rezak R, Lavoie D L (Eds.). Carbonate Microfabrics. Springer,Berlin, 1993:95-104.

    [38]

    Goedert J L, Peckmann J, Reitner J. Worm tubes in an allochthonous cold-seep carbonate from lower Oligocene rocks of western Washington[J]. Journal of Paleontology, 2000, 74:992-999.

    [39]

    Chen D F, Liu Q, Zhang Z W, et al. Biogenic fabrics in seep carbonates from an active gas vent site in Green Canyon Block 238, Gulf of Mexico[J]. Marine and Petroleum Geology, 2007, 24:313-320.

    [40]

    Popa R, Kinkle B K, Badescu A. Pyrite framboids as biomarkers for iron-sulfur systems[J]. Geomicrobiology Journal, 2004, 21:193-206.

    [41]

    Sackett W M. Carbon and hydrogen isotope effects during the thermocatalytic production of hydrocarbons in laboratory simulation experiments[J]. Geochimica et Cosmochimica Acta, 1978, 42:571-580.

    [42]

    Whiticar M J, Faber E, Schoell M. Biogenic methane formation in marine and freshwater environments:CO2 reduction vs. acetate fermentation——Isotope evidence[J]. Geochimica et Cosmochimica Acta, 1986, 50:693-709.

    [43]

    Anderson T F, Arthur M A. Stable isotopes of oxygen and carbon and their application to sedimentologic and paleoenvironmental problems[C]//In:Arthur M. A, Anderson T F, Kaplan I R, et al (Eds.).Stable Isotopes in Sedimentary Geology Society of Economic Paleontologists and Mineralogists, Dallas, 1983:1-151.

    [44]

    Formolo M J, Lyons T W, Zhang C, et al. Quantifying carbon sources in the formation of authigenic carbonates at gas hydrate sites in the Gulf of Mexico[J]. Chemical Geology, 2004, 205:253-264.

    [45]

    Hudson J C, Anderson T F. Ocean temperatures and isotopic compositions through time[C]//In:Clarkson E N K, Curry G B, Rolfe W D I (Eds.). Environments and Physiology of Fossil Organisms[C]. Transactions Royal Society of Edinburgh:Earth Sciences, 1989, 80:183-192.

    [46]

    Sassen R, MacDonald I R, Guinasso N L, et al. Bacterial methane oxidation in sea-floor gas hydrate; significance to life in extreme environments[J]. Geology, 1998, 26:851-854.

    [47]

    Aharon P, Schwarcz H P, Roberts H H. Radiometric dating of submarine hydrocarbon seeps in the Gulf of Mexico[J]. Geol. Soc. Am. Bull.,1997, 109:568-579.

    [48]

    MacDonald I R, Bender L C, Vardaro M, et al. Thermal and visual time-series at a seafloor gas hydrate deposit on the Gulf of Mexico slope[J]. Earth and Planetary Science Letters, 2005, 233:45-59.

    [49]

    Piper D Z. Rare earth elements in the sedimentary cycle:A summary[J]. Chemical Geology, 1974, 14:285-304.

    [50]

    Feng D, Chen D F, Lin Z J, et al.Redox variations in hydrocarbon seep sites recorded by rare earth elements in seep carbonates[C]//Proceedings of the 6th International Conference on Gas Hydrates (ICGH 2008), Vancouver, British Columbia, CANADA, July 6-10, 2008:1-8.

    [51]

    Solomon E A, Kastner M, Jannasch H, et al. Dynamic fluid flow and chemical fluxes associated with a seafloor gas hydrate deposit on the northern Gulf of Mexico slope[J]. Earth and Planetary Science Letters, 2008:270(1-2):95-105.

    [52]

    McLennan S M. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes[C]//In:Lipin B R, McKay G A(Eds.). Geochemistry and Mineralogy of Rare Earth Elements. Reviews in Mineralogy, 1989, 21:169-200.

  • 加载中
计量
  • 文章访问数:  1071
  • PDF下载数:  3
  • 施引文献:  0
出版历程
收稿日期:  2008-11-13
修回日期:  2009-03-04

目录