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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| Główni autorzy: | , , , , , , |
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| Format: | Artigo |
| Język: | Inglês |
| Wydane: |
Frontiers Media S.A.
2014-12-01
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| Seria: | Frontiers in Microbiology |
| Hasła przedmiotowe: | |
| Dostęp online: | http://journal.frontiersin.org/Journal/10.3389/fmicb.2014.00713/full |
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