The onset of widespread marine red beds and the evolution of ferruginous oceans
The onset of widespread marine red beds and the evolution of ferruginous oceans
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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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 recent geochemical studies show that ferruginous...
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The onset of widespread marine red beds and the evolution of ferruginous oceans
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TN_cdi_doaj_primary_oai_doaj_org_article_c138e0aff57547d3bf50fc2586fc540b
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_c138e0aff57547d3bf50fc2586fc540b
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-017-00502-x