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Hydrogen generation from low-temperature water–rock reactions

Published:2013-05-26 Issue:6 Volume:6 Page:478-484
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nature Geosci

Author:

Mayhew L. E.,Ellison E. T.,McCollom T. M.,Trainor T. P.,Templeton A. S.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://www.nature.com/articles/ngeo1825.pdf

Reference50 articles.

1. Schrenk, M. O., Kelley, D. S., Bolton, S. A. & Baross, J. A. Low archaeal diversity linked to subseafloor geochemical processes at the Lost City Hydrothermal Field, Mid-Atlantic Ridge. Environ. Microbiol. 6, 1086–1095 (2004).

2. Kelley, D. S. et al. A serpentinite-hosted ecosystem: The lost city hydrothermal field. Science 307, 1428–1434 (2005).

3. Charlou, J. L., Donval, J. P., Fouquet, Y., Jean-Baptiste, P. & Holm, N. Geochemistry of high H-2 and CH4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal field (36 degrees 14’N, MAR). Chem. Geol. 191, 345–359 (2002).

4. Flores, G. E. et al. Microbial community structure of hydrothermal deposits from geochemically different vent fields along the Mid-Atlantic Ridge. Environ. Microbiol. 13, 2158–2171 (2011).

5. Moody, J. B. Serpentinization: A review. Lithos 9, 125–138 (1976).

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