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...

Descripció completa

Guardat en:
Dades bibliogràfiques
Publicat a:Front Microbiol
Autors principals: Walter, Xavier A., Picazo, Antonio, Miracle, Maria R., Vicente, Eduardo, Camacho, Antonio, Aragno, Michel, Zopfi, Jakob
Format: Artigo
Idioma:Inglês
Publicat: Frontiers Media S.A. 2014
Matèries:
Microbiology
Accés en línia: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
Etiquetes: Afegir etiqueta
Sense etiquetes, Sigues el primer a etiquetar aquest registre!

Ítems similars