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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Dettagli Bibliografici
Pubblicato in:Appl Environ Microbiol
Autori principali: Laufer, Katja, Nordhoff, Mark, Røy, Hans, Schmidt, Caroline, Behrens, Sebastian, Jørgensen, Bo Barker, Kappler, Andreas
Natura: Artigo
Lingua:Inglês
Pubblicazione: American Society for Microbiology 2016
Soggetti:
Geomicrobiology
Accesso online: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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