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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 empl...

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書誌詳細
主要な著者: Jason eBenzine, Evgenya eShelobolina, Mai Yia eXiong, David W. Kennedy, James P. McKinley, Xueju eLin, Eric eRoden
フォーマット: Artigo
言語:Inglês
出版事項: Frontiers Media S.A. 2013-12-01
シリーズ:Frontiers in Microbiology
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オンライン・アクセス:http://journal.frontiersin.org/Journal/10.3389/fmicb.2013.00388/full
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