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PHYSICAL SCIENCES / BIOLOGICAL SCIENCES / GEOLOGY / ENVIRONMENTAL SCIENCES
Biological formation of ethane and propane in the deep marine subsurface
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Deutsche ForschungsgemeinschaftResearch Center Ocean Margins, Department of Geosciences, University of Bremen, P.O. Box 330440, 28334 Bremen, Germany; Departments of
Geology and Geophysics and ¶Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institute, Woods Hole, MA 02543; ||Graduate School of Oceanography, University of Rhode Island, Narragansett, RI 02882; and 
Department of Geology and Geochemistry, Stockholm University, 10691 Stockholm, Sweden
Contributed by John M. Hayes, July 31, 2006
Concentrations and isotopic compositions of ethane and propane in cold, deeply buried sediments from the southeastern Pacific are best explained by microbial production of these gases in situ. Reduction of acetate to ethane provides one feasible mechanism. Propane is enriched in 13C relative to ethane. The amount is consistent with derivation of the third C from inorganic carbon dissolved in sedimentary pore waters. At typical sedimentary conditions, the reactions yield free energy sufficient for growth. Relationships with competing processes are governed mainly by the abundance of H2. Production of C2 and C3 hydrocarbons in this way provides a sink for acetate and hydrogen but upsets the general belief that hydrocarbons larger than methane derive only from thermal degradation of fossil organic material.
ethanogenesis | hydrocarbon gases | marine sediments | propanogenesis | stable carbon isotopes
The authors declare no conflict of interest.

Claypool, G. E., AAPG Hedberg Conference Abstracts, Natural Gas Formation and Occurrence, June 611, 1999, Durango, CO, pp. 2729 (abstr.).
To whom correspondence may be addressed. E-mail: khinrichs{at}uni-bremen.de or jhayes{at}whoi.edu
© 2006 by The National Academy of Sciences of the USA
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