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...

पूर्ण विवरण

में बचाया:
ग्रंथसूची विवरण
में प्रकाशित:Appl Environ Microbiol
मुख्य लेखकों: Laufer, Katja, Nordhoff, Mark, Røy, Hans, Schmidt, Caroline, Behrens, Sebastian, Jørgensen, Bo Barker, Kappler, Andreas
स्वरूप: Artigo
भाषा:Inglês
प्रकाशित: American Society for Microbiology 2016
विषय:
Geomicrobiology
ऑनलाइन पहुंच: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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