Literature DB >> 25329406

The interplay of microbially mediated and abiotic reactions in the biogeochemical Fe cycle.

Emily D Melton1, Elizabeth D Swanner1, Sebastian Behrens1, Caroline Schmidt1, Andreas Kappler1.   

Abstract

Many iron (Fe) redox processes that were previously assumed to be purely abiotic, such as photochemical Fe reactions, are now known to also be microbially mediated. Owing to this overlap, discerning whether biotic or abiotic processes control Fe redox chemistry is a major challenge for geomicrobiologists and biogeochemists alike. Therefore, to understand the network of reactions within the biogeochemical Fe cycle, it is necessary to determine which abiotic or microbially mediated reactions are dominant under various environmental conditions. In this Review, we discuss the major microbially mediated and abiotic reactions in the biogeochemical Fe cycle and provide an integrated overview of biotic and chemically mediated redox transformations.

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Year:  2014        PMID： 25329406     DOI： 10.1038/nrmicro3347

Source DB:  PubMed          Journal:  Nat Rev Microbiol        ISSN： 1740-1526            Impact factor:   60.633


  107 in total

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