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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...
Αποθηκεύτηκε σε:
| Τόπος έκδοσης: | Front Microbiol |
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| Κύριοι συγγραφείς: | , , , , , , |
| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Frontiers Media S.A.
2014
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| Θέματα: | |
| Διαθέσιμο Online: | 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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