Dissimilatory Fe(III) and Mn(IV)-reducing Prokaryotes

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Geobacter: the microbe electric's physiology, ecology, and practical applications. (2011, background): “Geobacter species can be conveniently grown with soluble chelated, Fe(III) forms (Lovley, 2000b), but whole genome gene expression (Holmes et al., 2011b) and proteomic (Ding et al., 2008) studies have suggested that cells grown with soluble Fe(III) have significantly different physiologies than…”
Phylogenetic diversity of Fe(III)-reducing microorganisms in rice paddy soil: enrichment cultures with different short-chain fatty acids as electron donors (2011, methodology): “…containing 22 mM of synthetic amorphous ferrihydrite (FeOOH), 0.11 mM MgCl2, 0.61 mM CaCl2, 2 mM NaHCO3, 0.5 mM NH4Cl, 0.05 mM KH2PO4, and vitamin and trace element solutions (Lovley 2000) was prepared, autoclaved, and cooled to room temperature under an anoxic atmosphere of N2 (99.999% purity).”
Fungal involvement in bioweathering and biotransformation of rocks and minerals (2003, background): “Many bacteria use minerals for respiration, a process that involves using the mineral as a terminal electron acceptor, resulting in mineral components being chemically reduced (Lovley, 1991; Nealson and Saffarini, 1994; Lower et al., 2001a).”