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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Detalles Bibliográficos
Autores principales: Walter, Xavier A., Picazo, Antonio, Miracle, Maria R., Vicente, Eduardo, Camacho, Antonio, Aragno, Michel, Zopfi, Jakob
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Frontiers Media S.A. 2014
Materias:
Microbiology
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4258642/
https://www.ncbi.nlm.nih.gov/pubmed/25538702
http://dx.doi.org/10.3389/fmicb.2014.00713

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4258642/
https://www.ncbi.nlm.nih.gov/pubmed/25538702
http://dx.doi.org/10.3389/fmicb.2014.00713

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