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The 2.1 Ga Old Francevillian Biota: Biogenicity, Taphonomy and Biodiversity
The Paleoproterozoic Era witnessed crucial steps in the evolution of Earth's surface environments following the first appreciable rise of free atmospheric oxygen concentrations ∼2.3 to 2.1 Ga ago, and concomitant shallow ocean oxygenation. While most sedimentary successions deposited during thi...
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| Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Public Library of Science
2014
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4070892/ https://ncbi.nlm.nih.gov/pubmed/24963687 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1371/journal.pone.0099438 |
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