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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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Detaylı Bibliyografya
Yayımlandı:Sci Rep
Asıl Yazarlar: 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.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group 2015
Konular:
Online Erişim: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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