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 empl...

Descripción completa

Detalles Bibliográficos

Autores principales:	Jason eBenzine, Evgenya eShelobolina, Mai Yia eXiong, David W. Kennedy, James P. McKinley, Xueju eLin, Eric eRoden
Formato:	Artigo
Lenguaje:	Inglês
Publicado:	Frontiers Media S.A. 2013-12-01
Colección:	Frontiers in Microbiology
Materias:	Iron Metabolism sediment subsurface Microbial Enrichment
Acceso en línea:	http://journal.frontiersin.org/Journal/10.3389/fmicb.2013.00388/full
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!