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Microbial reduction of ferric iron [Fe(III)] is an important biogeochemical process in anoxic aquifers. Depending on groundwater pH, dissimilatory metal-reducing bacteria can also respire alternative electron acceptors to survive, including elemental sulfur (S0). To understand the interplay of Fe/S cycling under alkaline conditions, we combined thermodynamic geochemical modeling with bioreactor experiments using Shewanella oneidensis MR-1. Under these conditions, S. oneidensis can enzymatically reduce S0 but not goethite (α-FeOOH). The HS- produced subsequently reduces goethite abiotically. Because of the prevalence of alkaline conditions in many aquifers, Fe(III) reduction may thus proceed via S0-mediated electron-shuttling pathways. [ABSTRACT FROM AUTHOR]

The article analyzes the role of immunoglobulin A (IgA), the most abundant mammalian antibody isotype, in containing the resident commensal microbiota in the intestines. IgA is particularly prevalent at barrier surfaces and offers protection against enteric pathogens. Cloning of monoclonal antibodies (mAbs) from single murine IgA plasma cells is done to study the specificity of homeostatic IgA.