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Pathways for abiotic organic synthesis at submarine hydrothermal fields
Open accessAbstract
Significance: Arguments for an abiotic origin of organic compounds in deep-sea hot springs are compelling because of their potential role in the origin of life and sustaining microbial communities. Theory predicts that warm H 2 -rich fluids circulating through serpentinizing systems create a favorable thermodynamic drive for inorganic carbon reduction to organic compounds. We show that abiotic synthesis proceeds by two spatially and temporally distinct mechanisms. Abundant dissolved CH 4 and higher hydrocarbons are likely formed in H 2 -rich fluid inclusions over geologic timescales. Conversely, formate production by ΣCO 2 reduction occurs rapidly during subsurface mixing, which may support anaerobic methanogenesis. We confirm models for abiotic metastable organic compound formation and argue that alkanes in all ultramafic-influenced vents may form independently of actively circulating serpentinizing fluids.
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Metadata
- Authors
- McDermott, J. M., Seewald, J. S., German, C. R., & Sylva, S. P.
- Venue
- Proceedings of the National Academy of Sciences
- Published
- 2015-06-08
- Volume
- 112
- Issue
- 25
- Pages
- 7668-7672
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- OpenAlex
- W1607885691
- Cited by
- 340
- References
- 5
- FWCI
- 17.56
- Type
- journal article
- Language
- en
- Open access
- green
- Funders
- National Aeronautics and Space Administration (NNX-327 09AB75G)
- National Science Foundation (OCE-1061863)
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