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Abiogenic Hydrocarbon Production at the Geosphere-Biosphere Interface via Serpentinization Reactions

  • G. Proskurowski

Abstract:

The production of hydrocarbons via mechanisms not associated with biological processes has far reaching implications to the fields of petroleum geochemistry, astrobiology, and the study of early life and life in extreme environments. Despite an intense focus on discovering abiotic hydrocarbon sources in natural settings, only a handful of sites convincingly suggest that abiotic organic synthesis occurs within the geosphere. Although experimental studies in aqueous settings clearly demonstrate the potential for abiotic synthesis, the scope of abiotic hydrocarbon production in natural settings has yet to be defined. As theoretical and experimental studies indicate that abiotic hydrocarbon synthesis is maximized in highly reducing environments, it is not surprising that the strongest evidence for abiotic organic synthesis in natural settings is associated with the alteration (serpentinization) of reduced mantle rocks. The crux of this topic is that currently there is no foolproof approach to distinguishing abiotic versus biotic organic synthesis. Thus, it is especially important to be cognizant of the possibilities and limitations of abiotic hydrocarbon production when considering a deep subsurface biosphere where the organic matter may be synthesized by both abiotic and biotic processes.

Keywords

Ultramafic Rock High Hydrocarbon Increase Chain Length Lost City Abiotic Reaction 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Notes

Acknowledgments

This work was supported in part by the National Science Foundation under Grant No. OCE-0647800.

References

  1. Abrajano TA et al. (1988) Methane-hydrogen gas seeps, Zambales Ophiolite, Philippines; deep or shallow origin? In Origins of Methane in the Earth. Chemical Geology. M Schoell (eds.). Amsterdam, The Netherlands: Elsevier, pp. 211–222.Google Scholar
  2. Abrajano TA et al. (1990). Geochemistry of reduced gas related to serpentinization of the Zambales Ophiolite, Philippines. In Water-Rock Interactions. Applied Geochemistry. YK Kharaka, HL Barnes (eds.). Oxford/New York/Beijing, International: Pergamon, pp. 625–630.Google Scholar
  3. Allen DE, Seyfried WE Jr. (2003) Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges; an experimental study at 400°C, 500 bars. Geochimi Cosmochim Acta 67(8): 1531–1542.CrossRefGoogle Scholar
  4. Allen DE, Seyfried WE Jr. (2004) Serpentinization and heat generation: constraints from Lost City and Rainbow hydrothermal systems. Geochim Cosmochim Acta 68(6): 1347–1354.CrossRefGoogle Scholar
  5. Alt JC, Shanks WC III (2003) Serpentinization of abyssal peridotites from the MARK area, Mid-Atlantic Ridge; sulfur geochemistry and reaction modeling. Geochim Cosmochim Acta 67(4): 641–653.CrossRefGoogle Scholar
  6. Anderson RB (1984) The Fischer-Tropsch Synthesis. Orlando, FL: Academic, 301 pp.Google Scholar
  7. Bach W et al. (2006) Unraveling the sequence of serpentinization reactions: petrography, mineral chemistry, and petrophysics of serpentinites from MAR 15°N (ODP Leg 209, Site 1274). Geophys Res Lett 33(13): 4.CrossRefGoogle Scholar
  8. Berndt ME, Allen DE, Seyfried WE Jr. (1996) Reduction of CO2 during serpentinization of olivine at 300°C and 500 bar. Geology 24(4): 351–354.CrossRefGoogle Scholar
  9. Blank JG, Delaney JR, Des MDJ (1993) The concentration and isotopic composition of carbon in basaltic glasses from the Juan de Fuca Ridge, Pacific Ocean. Geochim Cosmochim Acta 57(4): 875–887.PubMedCrossRefGoogle Scholar
  10. Bogdanov Y et al. (1995) A study of the hydrothermal field at 14°45∋N on the Mid-Atlantic Ridge using the MIR submersibles. BRIDGE Newslett. 9: 9–13.Google Scholar
  11. Bradley AS, Hayes JM, Summons RE (2009) Extraordinary 13C enrichment of diether lipids at the Lost City Hydrothermal Field indicates a carbon-limited ecosystem. Geochimica et Cosmochimica Acta 73(1): 102–118.Google Scholar
  12. Burdige DJ (2006) Geochemistry of Marine Sediments. Princeton, NJ: Princeton University Press.Google Scholar
  13. Charlou JL, Donval JP, Fouquet Y, Jean BP, Holm N (2002) Geochemistry of high H2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36°14∋N, MAR). Chem Geol 191(4): 345–359.CrossRefGoogle Scholar
  14. Cody GD et al. (2000) Primordial carbonylated iron-sulfur compounds and the synthesis of pyruvate. Science 289(5483): 1337–1340.PubMedCrossRefGoogle Scholar
  15. Cruse AM, Seewald JS (2006) Geochemistry of low-molecular weight hydrocarbons in hydrothermal fluids from Middle Valley, northern Juan de Fuca Ridge. Geochim Cosmochim Acta 70(8): 2073–2092.CrossRefGoogle Scholar
  16. Des Marais DJ, Donchin JH, Nehring NL, Truesdell AH (1981) Molecular carbon isotopic evidence for the origin of geothermal hydrocarbons. Nature 292(5826): 826–8.CrossRefGoogle Scholar
  17. Dick HJB, Lin J, Schouten H (2003) An ultraslow-spreading class of ocean ridge. Nature 426(6965): 405–412.PubMedCrossRefGoogle Scholar
  18. Douville E et al. (2002) The Rainbow Vent fluids (36°14∋N, MAR); the influence of ultramafic rocks and phase separation on trace metal content in Mid-Atlantic Ridge hydrothermal fluids. Chem Geol 184(1–2): 37–48.CrossRefGoogle Scholar
  19. Du J, Jin Z, Xie H, Bai L, Liu W (2003) Stable carbon isotope compositions of gaseous hydrocarbons produced from high pressure and high temperature pyrolysis of lignite. Org Geochem 34(1): 97.CrossRefGoogle Scholar
  20. Fiebig J, Woodland AB, Spangenberg J, Oschmann W (2007) Natural evidence for rapid abiogenic hydrothermal generation of CH4. Geochim Cosmochim Acta 71(12): 3028–3039.CrossRefGoogle Scholar
  21. Foustoukos DI, Qi F, Seyfried WE Jr. (2004) Abiotic synthesis of methane under alkaline hydrothermal conditions: the effect of pH in heterogeneous catalysis. EOS Trans Am Geophys Union 85(47): Abstract B13A-0212.Google Scholar
  22. Foustoukos DI, Seyfried WE Jr. (2004) Hydrocarbons in hydrothermal vent fluids: the role of chromium-bearing catalysts. Science 304(5673): 1002–1005.PubMedCrossRefGoogle Scholar
  23. Foustoukos DI, Savov IP, Janecky DR (2008) Chemical and isotopic constraints on water/rock interactions at the Lost City hydrothermal field, 30∞N Mid-Atlantic Ridge. Geochim Cosmochim Acta 72(22): 5457–5474.CrossRefGoogle Scholar
  24. Fritz P, Clark ID, Fontes JC, Whiticar MJ, Faber E (1992) Deuterium and 13C evidence for low-temperature production of hydrogen and methane in a highly alkaline groundwater environment in Oman. In Proceedings of the 7th international symposium on water-rock interaction; Volume 1, Low temperature environments. Proceedings – International Symposium on Water-Rock Interaction. YK Kharaka, AS Maest (eds.). International Association of Geochemistry and Cosmochemistry and Alberta Research Council, Sub-Group on Water-Rock Interaction, Edmonton, AB, International, pp. 793–796.Google Scholar
  25. Früh-Green GL et al. (2003) 30,000 years of hydrothermal activity at the Lost City vent field. Science 301(5632): 495–498.PubMedCrossRefGoogle Scholar
  26. Früh-Green GL, Connollly JAD, Plas A, Kelley Deborah S, Grobety B (2004) Serpentinization of oceanic Peridotites: implications for geochemical cycles and biological activity. In The Subseafloor Biosphere at Mid-Ocean Ridges. WSD Wilcock, EF Delong, DS Kelley, JA Baross, CS Cary (eds.). Washington, DC: American Geophysical Union, pp. 119–136.Google Scholar
  27. Fu Q, Sherwood Lollar B, Horita J, Lacrampe-Couloume G, Seyfried WE Jr. (2007) Abiotic formation of hydrocarbons under hydrothermal conditions: Constraints from chemical and isotope data. Geochim Cosmochim Acta 71(8): 1982–1998.CrossRefGoogle Scholar
  28. Fyfe WS, Lonsdale PF (1981) Ocean floor hydrothermal activity. In The Oceanic Lithosphere. C Emiliani (ed.). New York: Wiley, pp. 589–638.Google Scholar
  29. Gold T (1999) The Deep Hot Biosphere. New York: Copernicus.Google Scholar
  30. Holloway JR (1984) Graphite-CH4-H2O-CO2 equilibria at low-grade metamorphic conditions. Geology 12(8): 455–458.CrossRefGoogle Scholar
  31. Holm NG, Andresson EM (1998) Hydrothermal Systems. In The Molecular Origins of Life. A Brack (ed.). Cambridge: Cambridge University Press, pp. 86–99.Google Scholar
  32. Horita J (2001) Carbon isotope exchange in the system CO2-CH4 at elevated temperatures. Geochim Cosmochim Acta 65(12): 1907–1919.CrossRefGoogle Scholar
  33. Horita J, Berndt ME (1999) Abiogenic methane formation and isotopic fractionation under hydrothermal conditions. Science 285(5430): 1055–1057.PubMedCrossRefGoogle Scholar
  34. Hosgormez H (2006) Origin of the natural gas seep of Cirali (Chimera), Turkey: site of the first Olympic fire. J Asian Earth Sci 30: 131–141.CrossRefGoogle Scholar
  35. Hu G, Ouyang Z, Wang X, Wen Q (1998) Carbon isotopic fractionation in the process of Fischer-Tropsch reaction in primitive solar nebula. Sci China Ser D: Earth Sci 41(2): 202–207.CrossRefGoogle Scholar
  36. Huber C et al. (1997) Activated acetic acid by carbon fixation on (Fe,Ni)S under primordial conditions. Science 276(5310): 245–247.PubMedCrossRefGoogle Scholar
  37. Janecky DR, Seyfried WE Jr. (1986) Hydrothermal serpentinization of peridotite within the oceanic crust; experimental investigations of mineralogy and major element chemistry. Geochim Cosmochim Acta 50(7): 1357–1378.CrossRefGoogle Scholar
  38. Kadko D, Butterfield DA (1998) The relationship of hydrothermal field composition and crustal residence time to maturity of vent fields on the Juan de Fuca Ridge. Geochim Cosmochim Acta 62(9): 1521–1533.CrossRefGoogle Scholar
  39. Karl DM (1995) Ecology of free-living, hydrothermal vent microbial communities. In The Microbiology of Deep-Sea Hydrothermal Vents. DM Karl (eds.). Boca Raton, FL: CRC Press, pp. 35–124.Google Scholar
  40. Kelley DS (1996) Methane-rich fluids in the oceanic crust. J Geophys Res B, Solid Earth Planet 101(2): 2943–2962.CrossRefGoogle Scholar
  41. Kelley DS, Früh-Green GL (1999) Abiogenic methane in deep-seated mid-ocean ridge environments; insights from stable isotope analyses. J Geophys Res, B, Solid Earth Planet 104(5): 10, 439–10, 460.Google Scholar
  42. Kelley DS et al. (2001) An off-axis hydrothermal vent field near the Mid-Atlantic Ridge at 30°N. Nature 412(6843): 145–149.PubMedCrossRefGoogle Scholar
  43. Kelley DS, Baross JA, Delaney JR (2002) Volcanoes, fluids, and life at mid-ocean ridge spreading centers. Annu Rev Earth Planet Sci 30: 385–491.CrossRefGoogle Scholar
  44. Kelley DS et al. (2005) A Serpentinite-hosted ecosystem: the Lost City Hydrothermal Field. Science 307(5714): 1428–1434.PubMedCrossRefGoogle Scholar
  45. Kniemeyer O et al. (2007) Anaerobic oxidation of short-chain hydrocarbons by marine sulphate-reducing bacteria. Nature 449(7164): 898–901.PubMedCrossRefGoogle Scholar
  46. Krasnov SG et al. (1995) Detailed geological studies of hydrothermal fields in the North Atlantic. In Hydrothermal Vents and Processes. LM Parson, CL Walker, DR Dixon (eds.). London: Geological Society Special Publication, pp. 43–64.Google Scholar
  47. Lancet MS, Anders E (1970) Carbon isotope fractionation in the Fischer-Tropsch synthesis and in meteorites. Science 170(3961): 980–982.PubMedCrossRefGoogle Scholar
  48. Lilley MD et al. (1993) Anomalous CH4 and NH4 + concentrations at an unsedimented mid-ocean-ridge hydrothermal system. Nature 364(6432): 45–47.CrossRefGoogle Scholar
  49. Macleod G, McKeown C, Hall AJ, Russell MJ (1994) Hydrothermal and oceanic pH conditions of possible relevance to the origin of life. Origin Life Evol Biosph 24: 19–41.CrossRefGoogle Scholar
  50. Martin W, Baross J, Kelley D, Russell MJ (2008) Hydrothermal vents and the origin of life. Nat Rev Micro 6(11): 805–814.Google Scholar
  51. McCollom TM, Seewald JS (2006) Carbon isotope composition of organic compounds produced by abiotic synthesis under hydrothermal conditions. Earth Planet Sci Lett 243(1–2): 74–84.CrossRefGoogle Scholar
  52. McCollom TM, Seewald JS (2007) Abiotic synthesis of organic compounds in deep-sea hydrothermal environments. Chem Rev 107(2): 382–401.PubMedCrossRefGoogle Scholar
  53. McCollom TM, Bach WG (2009) Thermodynamic constraints on hydrogen generation during serpentinization of ultramafic rocks. Geochimica Et Cosmochimica Acta 73(3): 856–875.Google Scholar
  54. Mottl MJ, Komor SC, Fryer P, Moyer CL (2003) Deep-slap fluids fuel extremophilic Archaea on a Mariana forearc serpentinite mud volcano: Ocean Drilling Program Leg 195. Geochem Geophys Geosyst 4(11): 9009.Google Scholar
  55. Neal C, Stanger G (1983) Hydrogen generation from mantle source rocks in Oman. Earth Planet Sci Lett 66: 315–320.CrossRefGoogle Scholar
  56. O’Hanley DS (1992) Solution to the volume problem in serpentinization. Geology 20: 705–708.CrossRefGoogle Scholar
  57. Proskurowski G, Lilley MD, Brown TA (2004) Isotopic evidence of magmatism and seawater bicarbonate removal at the Endeavour hydrothermal system. Earth Planet Sci Lett 225(1–2): 53–61.CrossRefGoogle Scholar
  58. Proskurowski G et al. (2008) Abiogenic hydrocarbon production at lost city hydrothermal field. Science 319(5863): 604–607.PubMedCrossRefGoogle Scholar
  59. Reeves E, Seewald JS, Sylva SP (2007) Rapid hydrogen isotopic exchange between aqueous hydrocarbons and water under hydrothermal conditions. Geochim Cosmochim Acta 71(15, Suppl. 1): A825.Google Scholar
  60. Russell MJ, Hall AJ (2006) The onset and early evolution of life. In Evolution of Early Earth’s Atmosphere, Hydrosphere, and Biosphere- Constraints from Ore Deposits. SE Kesler and H Ohmoto (eds.). Boulder, CO: Geological Society of America, pp. 1–32.CrossRefGoogle Scholar
  61. Schmidt K, Koschinsky A, Garbe-Schonberg D, de Carvalho LM, Seifert R (2007) Geochemistry of hydrothermal fluids from the ultramafic-hosted Logatchev hydrothermal field, 15°N on the Mid-Atlantic Ridge: temporal and spatial investigation. Chem Geol 242(1–2): 1–21.CrossRefGoogle Scholar
  62. Schoell M (1980) The hydrogen and carbon isotopic composition of methane from natural gases of various origins. Geochim Cosmochim Acta 44(5): 649–662.CrossRefGoogle Scholar
  63. Schoell M (1988) Multiple origins of methane in the Earth. In Origins of Methane in the Earth. Chemical Geology. M Schoell (ed.). Amsterdam, The Netherlands: Elsevier, pp. 1–10.Google Scholar
  64. Seewald JS (2003) Organic-inorganic interactions in petroleum-producing sedimentary basins. Nature 426(6964): 327–333.PubMedCrossRefGoogle Scholar
  65. Seewald JS, Seyfried WE Jr. Thornton, EC (1990) Organic-rich sediment alteration; an experimental and theoretical study at elevated temperatures and pressures. In Organic matter in hydrothermal systems; maturation, migration, and biogeochemistry, selected papers from the symposium held at the Third chemical congress of North America and the 195th American Chemical Society national meeting. Applied Geochemistry. BRT Simoneit (ed.). Oxford/New York/Beijing, International: Pergamon, pp. 193–209.Google Scholar
  66. Seewald JS, Zolotov MY, McCollom T (2006) Experimental investigation of single carbon compounds under hydrothermal conditions. Geochim Cosmochim Acta 70(2): 446–460.CrossRefGoogle Scholar
  67. Seyfried WE Jr. Ding K (1995) Phase equilibria in subseafloor hydrothermal systems; a review of the role of redox, temperature, pH and dissolved Cl on the chemistry of hot spring fluids at mid-ocean ridges. In Seafloor Hydrothermal Systems; Physical, Chemical, Biological, and Geological Interactions. Geophysical Monograph. SE Humphris, RA Zierenberg, LS Mullineaux, and RE Thomson (eds.). Washington, DC: American Geophysical Union, pp. 248–272.Google Scholar
  68. Seyfried WE Jr., Foustoukos DI, Allen DE (2004) Ultramafic-hosted hydrothermal systems at mid-ocean ridges: chemical and physical controls on pH, redox and carbon reduction reactions. In Mid-Ocean Ridges: Hydrothermal Interactions Between the Lithosphere and Oceans. CR German, J Lin, and LM Parson (eds.), Washington, D.C.: American Geophysical Union, pp. 267–284.Google Scholar
  69. Seyfried WE Jr. Foustoukos DI, Fu Q (2007) Redox evolution and mass transfer during serpentinization: An experimental and theoretical study at 200°C, 500 bar with implications for ultramafic-hosted hydrothermal systems at Mid-Ocean Ridges. Geochim Cosmochim Acta 71(15): 3872–3886.CrossRefGoogle Scholar
  70. Sherwood Lollar B, Westgate TD, Ward JA, Slater GF, Lacrampe CG (2002) Abiogenic formation of alkanes in the Earth’s crust as a minor source for global hydrocarbon reservoirs. Nature 416(6880): 522–524.PubMedCrossRefGoogle Scholar
  71. Sherwood Lollar B et al. (2006) Unravelling abiogenic and biogenic sources of methane in the Earth’s deep subsurface. Chem Geol 226(3–4): 328.CrossRefGoogle Scholar
  72. Sherwood Lollar B et al. (2008) Isotopic signatures of CH4 and higher hydrocarbon gases from Precambrian Shield sites: a model for abiogenic polymerization of hydrocarbons. Geochim et Cosmochim Acta 72(19): 4778–4795.CrossRefGoogle Scholar
  73. Simoneit BRT, Kawka OE, Brault M (1988) Origin of gases and condensates in the Guaymas Basin hydrothermal system (Gulf of California). In Origins of Methane in the Earth. Chemical Geology. M Schoell (ed.). Amsterdam, The Netherlands: Elsevier, pp. 169–182.Google Scholar
  74. Simoneit BRT, Goodfellow WD, Franklin JM (1992) Hydrothermal petroleum at the seafloor and organic matter alteration in sediments of Middle Valley, Northern Juan de Fuca Ridge. Appl Geochem 7(3): 257–264.CrossRefGoogle Scholar
  75. Sleep NH, Meibom A, Fridriksson T, Coleman RG, Bird DK (2004) H2-rich fluids from serpentinization: Geochemical and biotic implications. PNAS 101(35): 12818–12823.PubMedCrossRefGoogle Scholar
  76. Takai K et al. (2008) Cell proliferation at 122°C and isotopically heavy CH4 production by a hyperthermophilic methanogen under high-pressure cultivation. Proc Natl Acad Sci USA 105(31): 10949–10954.PubMedCrossRefGoogle Scholar
  77. Taran YA, Kliger GA, Sevastianov VS (2007) Carbon isotope effects in the open-system Fischer-Tropsch synthesis. Geochim Cosmochim Acta 71(18): 4474–4487.CrossRefGoogle Scholar
  78. Welhan JA, Craig H (1983) Methane, hydrogen and helium in hydrothermal fluids at 21°N on the East Pacific Rise. In Hydrothermal Processes at Seafloor Spreading Centers. PA Rona, K Bostroem, L Laubier, and KL Smith Jr. (eds.). New York: Plenum, pp. 391–409.Google Scholar
  79. Welhan JA, Lupton JE (1987) Light hydrocarbon gases in Guaymas Basin hydrothermal fluids; thermogenic versus abiogenic origin. AAPG Bull 71(2): 215–223.Google Scholar
  80. Wetzel LR, Shock EL (2000) Distinguishing ultramafic- from basalt-hosted submarine hydrothermal systems by comparing calculated vent fluid compositions. J Geophys Res, B, Solid Earth Planet 105(4): 8319–8340.CrossRefGoogle Scholar
  81. Whiticar MJ (1990) A geochemical perspective of natural gas and atmospheric methane. In Advances in Organic Geochemistry 1989; Part I, Organic Geochemistry in Petroleum Exploration. Organic Geochemistry. B Durand, F Behar (eds.). Oxford/New York, International: Pergamon, pp. 531–547.Google Scholar
  82. You CF et al. (1994) Boron and halide systematics in submarine hydrothermal systems; effects of phase separation and sedimentary contributions. Earth Planet Sci Lett 123(1–4): 227–238.CrossRefGoogle Scholar

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© Springer-Verlag Berlin Heidelberg 2010

Authors and Affiliations

  • G. Proskurowski
    • 1
  1. 1.Woods Hole Oceanographic Institution, Department of Marine Chemistry and GeochemistryWoods HoleUSA

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