Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.
Hydrocarbons in Hydrothermal Vent Fluids: The Role of Chromium-Bearing Catalysts
Dionysis I. Foustoukos* and
William E. Seyfried, Jr.
Fischer-Tropsch type (FTT) synthesis has long been proposedto account for the existence of hydrocarbons in hydrothermalfluids. We show that iron- and chromium-bearing minerals catalyzethe abiotic formation of hydrocarbons. In addition to productionof methane (CH4aq), we report abiotic generation of ethane (C2H6aq)and propane (C3H8aq) by mineral-catalyzed hydrothermal reactionsat 390°Cand 400 bars. Results suggest that the chromiumcomponent in ultramafic rocks could be an important factor forFTT synthesis during water-rock interaction in mid-ocean ridgehydrothermal systems. This in turn could help to support microbialcommunities now recognized in the subsurface at deep-sea vents.
Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA.
* To whom correspondence should be addressed. E-mail: fous0009{at}umn.edu
The editors suggest the following Related Resources on Science sites:
In Science Magazine
PERSPECTIVES
Barbara Sherwood Lollar (14 May 2004) Science304 (5673), 972.
[DOI: 10.1126/science.1098112] |Summary »|Full Text »|PDF »
THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Biogenic origin for Earth's oldest putative microfossils.
B. T. De Gregorio, T. G. Sharp, G. J. Flynn, S. Wirick, and R. L. Hervig (2009)
Geology
37, 631-634
|Abstract »|Full Text »|PDF »
Excess methane in continental hydrothermal emissions is abiogenic.
J. Fiebig, A. B. Woodland, W. D'Alessandro, and W. Puttmann (2009)
Geology
37, 495-498
|Abstract »|Full Text »|PDF »
Abiogenic Hydrocarbon Production at Lost City Hydrothermal Field.
G. Proskurowski, M. D. Lilley, J. S. Seewald, G. L. Fruh-Green, E. J. Olson, J. E. Lupton, S. P. Sylva, and D. S. Kelley (2008)
Science
319, 604-607
|Abstract »|Full Text »|PDF »
The origin and emergence of life under impact bombardment.
Implications of a 3.472-3.333 Gyr-old subaerial microbial mat from the Barberton greenstone belt, South Africa for the UV environmental conditions on the early Earth.
F. Westall, C. E.J de Ronde, G. Southam, N. Grassineau, M. Colas, C. Cockell, and H. Lammer (2006)
Phil Trans R Soc B
361, 1857-1876
|Abstract »|Full Text »|PDF »
Biological formation of ethane and propane in the deep marine subsurface.
K.-U. Hinrichs, J. M. Hayes, W. Bach, A. J. Spivack, L. R. Hmelo, N. G. Holm, C. G. Johnson, and S. P. Sylva (2006)
PNAS
103, 14684-14689
|Abstract »|Full Text »|PDF »
Cell evolution and Earth history: stasis and revolution.
V. Formisano, S. Atreya, T. Encrenaz, N. Ignatiev, and M. Giuranna (2004)
Science
306, 1758-1761
|Abstract »|Full Text »|PDF »
Generation of methane in the Earth's mantle: In situ high pressure-temperature measurements of carbonate reduction.
H. P. Scott, R. J. Hemley, H.-k. Mao, D. R. Herschbach, L. E. Fried, W. M. Howard, and S. Bastea (2004)
PNAS
101, 14023-14026
|Abstract »|Full Text »|PDF »