Join Dr. Eric Roden, from the University of Wisconsin-Madison, as he presents "Rust Never Sleeps: Biogeochemical and Genomic Aspects of Microbial Fe Redox Cycling".
Redox cycling of iron (Fe) is a key process governing energy flow as well as the speciation and mobility of a wide variety of aqueous and solid-phase constituents in sedimentary environments. Both reduction and oxidation of Fe are microbially catalyzed, and available evidence suggests that microbial Fe redox metabolism takes place across a wide range of spatial and temporal scales natural systems. The coupling of microbial Fe reduction and oxidation has been proposed in various situations where a redox transition zone is observed. Here we review and synthesize several case studies of the potential for Fe redox cycling in subsurface environments. Of specific interest are novel pathways and organisms involved in the oxidation of insoluble reduced Fe phases with oxygen or nitrate, and the coupling of Fe oxidation and reduction in field and experimental systems that model potential redox gradients and fluctuations in the subsurface. Recent cultivation studies and physiological experiments indicate that a variety of Proteobacteria are capable of oxidizing Fe-silicate and other insoluble Fe(II)-bearing minerals. These findings set the stage for rapid expansion in our knowledge of the range of extracellular electron transfer mechanisms utilized by subsurface microorganisms. The observation that closely coupled oxidation and reduction of Fe can take place under conditions common to the subsurface motivates this expansion in pursuit of molecular tools for dissecting in situ Fe redox cycling communities.
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