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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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| Опубликовано в: : | Nat Commun |
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| Главные авторы: | , , , , , , , , , , |
| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
Nature Publishing Group UK
2017
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| Предметы: | |
| Online-ссылка: | 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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