Coexistence of Microaerophilic, Nitrate-Reducing, and Phototrophic Fe(II) Oxidizers and Fe(III) Reducers in Coastal Marine Sediment

Iron is abundant in sediments, where it can be biogeochemically cycled between its divalent and trivalent redox states. The neutrophilic microbiological Fe cycle involves Fe(III)-reducing and three different physiological groups of Fe(II)-oxidizing microorganisms, i.e., microaerophilic, anoxygenic p...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Appl Environ Microbiol
Prif Awduron: Laufer, Katja, Nordhoff, Mark, Røy, Hans, Schmidt, Caroline, Behrens, Sebastian, Jørgensen, Bo Barker, Kappler, Andreas
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: American Society for Microbiology 2016
Pynciau:
Geomicrobiology
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC4771319/
https://ncbi.nlm.nih.gov/pubmed/26682861
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1128/AEM.03527-15
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