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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Detalles Bibliográficos
Autores principales: El Albani, Abderrazak, Bengtson, Stefan, Canfield, Donald E., Riboulleau, Armelle, Rollion Bard, Claire, Macchiarelli, Roberto, Ngombi Pemba, Lauriss, Hammarlund, Emma, Meunier, Alain, Moubiya Mouele, Idalina, Benzerara, Karim, Bernard, Sylvain, Boulvais, Philippe, Chaussidon, Marc, Cesari, Christian, Fontaine, Claude, Chi-Fru, Ernest, Garcia Ruiz, Juan Manuel, Gauthier-Lafaye, François, Mazurier, Arnaud, Pierson-Wickmann, Anne Catherine, Rouxel, Olivier, Trentesaux, Alain, Vecoli, Marco, Versteegh, Gerard J. M., White, Lee, Whitehouse, Martin, Bekker, Andrey
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4070892/
https://www.ncbi.nlm.nih.gov/pubmed/24963687
http://dx.doi.org/10.1371/journal.pone.0099438

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4070892/
https://www.ncbi.nlm.nih.gov/pubmed/24963687
http://dx.doi.org/10.1371/journal.pone.0099438

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