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Iron minerals within specific microfossil morphospecies of the 1.88 Ga Gunflint Formation
Problematic microfossils dominate the palaeontological record between the Great Oxidation Event 2.4 billion years ago (Ga) and the last Palaeoproterozoic iron formations, deposited 500–600 million years later. These fossils are often associated with iron-rich sedimentary rocks, but their affinities,...
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| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group
2017
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5376642/ https://ncbi.nlm.nih.gov/pubmed/28332570 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms14890 |
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