Fe-phyllosilicate redox cycling organisms from a redox transition zone in Hanford 300 Area sediments

Microorganisms capable of reducing or oxidizing structural iron (Fe) in Fe-bearing phyllosilicate minerals were enriched and isolated from a subsurface redox transition zone at the Hanford 300 Area site in eastern Washington, USA. Both conventional and in situ “i-chip” enrichment strategies were emp...

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Autores principales: Benzine, Jason, Shelobolina, Evgenya, Xiong, Mai Yia, Kennedy, David W., McKinley, James P., Lin, Xueju, Roden, Eric E.
Formato: Artigo
Lenguaje:Inglês
Publicado: Frontiers Media S.A. 2013
Materias:
Microbiology
Acceso en línea:https://ncbi.nlm.nih.gov/pmc/articles/PMC3863755/
https://ncbi.nlm.nih.gov/pubmed/24379809
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2013.00388
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