BIOGENIC MANGANESE OXIDES: PROPERTIES AND MECHANISMS OF FORMATION

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dc.contributor.author Tebo B.M.
dc.contributor.author Clement B.G.
dc.contributor.author Dick G.J.
dc.contributor.author Murray K.J.
dc.contributor.author Parker D.
dc.contributor.author Verity R.
dc.contributor.author Bargar J.R.
dc.contributor.author Webb S.M.
dc.date.accessioned 2022-04-17T09:21:29Z
dc.date.available 2022-04-17T09:21:29Z
dc.date.issued 2004
dc.identifier https://www.elibrary.ru/item.asp?id=14447819
dc.identifier.citation Annual Review of Earth and Planetary Sciences, 2004, 32, С. 2, 287-328
dc.identifier.issn 0084-6597
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/37188
dc.description.abstract Manganese(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.subject bacterial Mn(II) oxidation
dc.subject δ-MnO 2
dc.subject birnessite
dc.subject Mn bacteria
dc.subject multicopper oxidase
dc.subject X-ray absorption spectroscopy
dc.subject Mn minerals
dc.title BIOGENIC MANGANESE OXIDES: PROPERTIES AND MECHANISMS OF FORMATION
dc.type Статья


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