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Phototrophic Fe(II)-oxidation in the chemocline of a ferruginous meromictic lake
Precambrian Banded Iron Formation (BIF) deposition was conventionally attributed to the precipitation of iron-oxides resulting from the abiotic reaction of ferrous iron (Fe(II)) with photosynthetically produced oxygen. Earliest traces of oxygen date from 2.7 Ga, thus raising questions as to what may...
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| Опубликовано в: : | Front Microbiol |
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| Главные авторы: | , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Frontiers Media S.A.
2014
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| Предметы: | |
| Online-ссылка: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4258642/ https://ncbi.nlm.nih.gov/pubmed/25538702 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.3389/fmicb.2014.00713 |
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