Cargando…
Chromite oxidation by manganese oxides in subseafloor basalts and the presence of putative fossilized microorganisms
Chromite is a mineral with low solubility and is thus resistant to dissolution. The exception is when manganese oxides are available, since they are the only known naturally occurring oxidants for chromite. In the presence of Mn(IV) oxides, Cr(III) will oxidise to Cr(VI), which is more soluble than...
Autores principales: | Ivarsson, Magnus, Broman, Curt, Holm, Nils G |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
BioMed Central
2011
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3118183/ https://www.ncbi.nlm.nih.gov/pubmed/21639896 http://dx.doi.org/10.1186/1467-4866-12-5 |
Ejemplares similares
-
Biogenic Mn-Oxides in Subseafloor Basalts
por: Ivarsson, Magnus, et al.
Publicado: (2015) -
A Fungal-Prokaryotic Consortium at the Basalt-Zeolite Interface in Subseafloor Igneous Crust
por: Ivarsson, Magnus, et al.
Publicado: (2015) -
Radiolytic Hydrogen Production in the Subseafloor Basaltic Aquifer
por: Dzaugis, Mary E., et al.
Publicado: (2016) -
Iron-rich Smectite Formation in Subseafloor Basaltic Lava in Aged Oceanic Crust
por: Yamashita, Seiya, et al.
Publicado: (2019) -
Messengers from the deep: Fossil wadsleyite-chromite microstructures from the Mantle Transition Zone
por: Satsukawa, Takako, et al.
Publicado: (2015)