Growth of Iron(III)-Reducing Bacteria on Clay Minerals as the Sole Electron Acceptor and Comparison of Growth Yields on a Variety of Oxidized Iron Forms

Smectite clay minerals are abundant in soils and sediments worldwide and are typically rich in Fe. While recent investigations have shown that the structural Fe(III) bound in clay minerals is reduced by microorganisms, previous studies have not tested growth with clay minerals as the sole electron a...

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Опубліковано в::	Appl Environ Microbiol
Автори:	Kostka, Joel E., Dalton, Dava D., Skelton, Hayley, Dollhopf, Sherry, Stucki, Joseph W.
Формат:	Artigo
Мова:	Inglês
Опубліковано:	American Society for Microbiology (ASM) 2002
Предмети:	Geomicrobiology
Онлайн доступ:	https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC134413/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/12450850/ https://ncbi.nlm.nih.govhttps://doi.org/10.1128/AEM.68.12.6256-6262.2002
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