The onset of widespread marine red beds and the evolution of ferruginous oceans

Banded iron formations were a prevalent feature of marine sedimentation ~3.8–1.8 billion years ago and they provide key evidence for ferruginous oceans. The disappearance of banded iron formations at ~1.8 billion years ago was traditionally taken as evidence for the demise of ferruginous oceans, but...

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Détails bibliographiques
Publié dans:Nat Commun
Auteurs principaux: Song, Haijun, Jiang, Ganqing, Poulton, Simon W., Wignall, Paul B., Tong, Jinnan, Song, Huyue, An, Zhihui, Chu, Daoliang, Tian, Li, She, Zhenbing, Wang, Chengshan
Format: Artigo
Langue:Inglês
Publié: Nature Publishing Group UK 2017
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Article
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC5577183/
https://ncbi.nlm.nih.gov/pubmed/28855507
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-017-00502-x
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