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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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Publicado no: | Nat Commun |
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Main Authors: | , , , , , , , , , , |
Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
Nature Publishing Group UK
2017
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Assuntos: | |
Acesso em linha: | 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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