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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Опубликовано в: :Sci Rep
Главные авторы: 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.
Формат: Artigo
Язык:Inglês
Опубликовано: Nature Publishing Group 2015
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Article
Online-ссылка:https://ncbi.nlm.nih.gov/pmc/articles/PMC4562300/
https://ncbi.nlm.nih.gov/pubmed/26348272
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep13803
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