BIOGENIC MANGANESE OXIDES: PROPERTIES AND MECHANISMS OF FORMATION

dc.contributor.authorTebo B.M.
dc.contributor.authorClement B.G.
dc.contributor.authorDick G.J.
dc.contributor.authorMurray K.J.
dc.contributor.authorParker D.
dc.contributor.authorVerity R.
dc.contributor.authorBargar J.R.
dc.contributor.authorWebb S.M.
dc.date.accessioned2022-04-17T09:21:29Z
dc.date.available2022-04-17T09:21:29Z
dc.date.issued2004
dc.description.abstractManganese(IV) oxides produced through microbial activity, i.e., bio-genic Mn oxides or Mn biooxides, are believed to be the most abundant and highly reactive Mn oxide phases in the environment. They mediate redox reactions with or-ganic and inorganic compounds and sequester a variety of metals. The major pathway for bacterial Mn(II) oxidation is enzymatic, and although bacteria that oxidize Mn(II) are phylogenetically diverse, they require a multicopper oxidase-like enzyme to oxidize Mn(II). The oxidation of Mn(II) to Mn(IV) occurs via a soluble or enzyme-complexed Mn(III) intermediate. The primary Mn(IV) biooxide formed is a phyllomanganate most similar to δ-MnO 2 or acid birnessite. Metal sequestration by the Mn biooxides occurs predominantly at vacant layer octahedral sites.
dc.identifierhttps://www.elibrary.ru/item.asp?id=14447819
dc.identifier.citationAnnual Review of Earth and Planetary Sciences, 2004, 32, С. 2, 287-328
dc.identifier.issn0084-6597
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/37188
dc.subjectbacterial Mn(II) oxidation
dc.subjectδ-MnO 2
dc.subjectbirnessite
dc.subjectMn bacteria
dc.subjectmulticopper oxidase
dc.subjectX-ray absorption spectroscopy
dc.subjectMn minerals
dc.titleBIOGENIC MANGANESE OXIDES: PROPERTIES AND MECHANISMS OF FORMATION
dc.typeСтатья

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