2012
DOI: 10.1042/bst20120229
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The molecular biogeochemistry of manganese(II) oxidation

Abstract: Micro-organisms capable of oxidizing the redox-active transition metal manganese play an important role in the biogeochemical cycle of manganese. In the present mini-review, we focus specifically on Mn(II)-oxidizing bacteria. The mechanisms by which bacteria oxidize Mn(II) include a two-electron oxidation reaction catalysed by a novel multicopper oxidase that produces Mn(IV) oxides as the primary product. Bacteria also produce organic ligands, such as siderophores, that bind to and stabilize Mn(III). The reali… Show more

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Cited by 100 publications
(67 citation statements)
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“…It also encompasses numerous confirmed examples of Mn(II) oxidation in the Alpha-, Beta-, Gamma-, and Deltaproteobacteria (10,11,14,15,24,55). Indeed, many of the model Mn(II)-oxidizing bacteria used to elucidate mechanisms of oxidation belong to this phylum (23)(24)(25)58). However, since the relative abundance of proteobacterial taxa did not differ significantly between MRBs, even at increasingly fine taxonomic resolution, and the relative abundance of any of the other bacterial phyla did not differ, the taxonomic profile of the bacterial communities cannot be correlated with differences in the proportion of Mn(II) removed by the four MRBs.…”
Section: Discussionmentioning
confidence: 99%
“…It also encompasses numerous confirmed examples of Mn(II) oxidation in the Alpha-, Beta-, Gamma-, and Deltaproteobacteria (10,11,14,15,24,55). Indeed, many of the model Mn(II)-oxidizing bacteria used to elucidate mechanisms of oxidation belong to this phylum (23)(24)(25)58). However, since the relative abundance of proteobacterial taxa did not differ significantly between MRBs, even at increasingly fine taxonomic resolution, and the relative abundance of any of the other bacterial phyla did not differ, the taxonomic profile of the bacterial communities cannot be correlated with differences in the proportion of Mn(II) removed by the four MRBs.…”
Section: Discussionmentioning
confidence: 99%
“…Most of the Mn oxidation in aquatic environments is attributed to the activity of Mn-oxidizing bacteria, because abiotic Mn oxidation is kinetically limited at circumneutral pH, and Mn-oxidizing bacteria are widespread in aquatic environments, especially at oxic-anoxic interfaces, and contribute to the formation of Mn-oxides [53]. They are widely distributed across the bacterial phylogenetic tree, and various processes of Mn biomineralization have been described, involving either enzymatic processes [54,55] or the export of reactive oxygen species [56], in any case leading to the extracellular formation of Mn-oxides. Specific morphologies of Mn-oxides have been described that are similar to the present observations [57].…”
Section: Transition From Mn-to Fe-mineral Formation (50-60-m Depth)mentioning
confidence: 99%
“…Direct oxidation, on the other hand, can occur via the production of polysaccharides or enzymatic activity (as summarized in reference 2). Although Mn(IV) formation could generate energy for organisms, this has not been definitively shown for any organism (4,5). However, Mn oxidation was shown to increase the survival of Pseudomonas putida GB-1 in the presence of reactive oxygen species (ROS) (18).…”
mentioning
confidence: 99%
“…Therefore, environmental Mn oxides, such as birnessite, are presumed to be of biological origin, e.g., biogenic (3). Mn(II)-oxidizing bacteria (MOB) are phylogenetically diverse and are detected in many different environments, such as soils, water (fresh to marine), and sediments (4). While microorganisms readily oxidize Mn(II) and precipitate Mn oxides at pH Ïł7 under oxic and hypoxic conditions (5), little is known about biological oxidation at acidic pH.…”
mentioning
confidence: 99%