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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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| Autors principals: | , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Frontiers Media S.A.
2013
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| Matèries: | |
| Accés en línia: | 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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