Metagenomic Evidence for H(2) Oxidation and H(2) Production by Serpentinite-Hosted Subsurface Microbial Communities

Ultramafic rocks in the Earth’s mantle represent a tremendous reservoir of carbon and reducing power. Upon tectonic uplift and exposure to fluid flow, serpentinization of these materials generates copious energy, sustains abiogenic synthesis of organic molecules, and releases hydrogen gas (H(2)). In...

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Detalles Bibliográficos
Autores principales: Brazelton, William J., Nelson, Bridget, Schrenk, Matthew O.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Research Foundation 2012
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3252642/
https://www.ncbi.nlm.nih.gov/pubmed/22232619
http://dx.doi.org/10.3389/fmicb.2011.00268

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3252642/
https://www.ncbi.nlm.nih.gov/pubmed/22232619
http://dx.doi.org/10.3389/fmicb.2011.00268

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