Pelagic photoferrotrophy and iron cycling in a modern ferruginous basin

Iron-rich (ferruginous) ocean chemistry prevailed throughout most of Earth’s early history. Before the evolution and proliferation of oxygenic photosynthesis, biological production in the ferruginous oceans was likely driven by photoferrotrophic bacteria that oxidize ferrous iron {Fe(II)} to harness...

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Detalles Bibliográficos
Autores principales: Llirós, Marc, García–Armisen, Tamara, Darchambeau, François, Morana, Cédric, Triadó–Margarit, Xavier, Inceoğlu, Özgül, Borrego, Carles M., Bouillon, Steven, Servais, Pierre, Borges, Alberto V., Descy, Jean–Pierre, Canfield, Don E., Crowe, Sean A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4562300/
https://www.ncbi.nlm.nih.gov/pubmed/26348272
http://dx.doi.org/10.1038/srep13803

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4562300/
https://www.ncbi.nlm.nih.gov/pubmed/26348272
http://dx.doi.org/10.1038/srep13803

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