BIOGENIC MANGANESE OXIDES: PROPERTIES AND MECHANISMS OF FORMATION
| 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.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.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.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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