Dissimilatory Fe(III) and Mn(IV) reduction.
The oxidation of organic matter coupled to the reduction of Fe(III) or Mn(IV) is one of the most important biogeochemical reactions in aquatic sediments, soils, and groundwater. This process, which may have been the first globally significant mechanism for the oxidation of organic matter to carbon d...
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| Publicado en: | Microbiol Rev |
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| Autor Principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
American Society for Microbiology (ASM)
1991
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| Acceso en liña: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC372814/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/1886521/ https://ncbi.nlm.nih.govhttps://doi.org/10.1128/mr.55.2.259-287.1991 |
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