A Cenozoic-style scenario for the end-Ordovician glaciation

The end-Ordovician was an enigmatic interval in the Phanerozoic, known for massive glaciation potentially at elevated CO(2) levels, biogeochemical cycle disruptions recorded as large isotope anomalies and a devastating extinction event. Ice-sheet volumes claimed to be twice those of the Last Glacial...

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Detalles Bibliográficos
Autores principales: Ghienne, Jean-François, Desrochers, André, Vandenbroucke, Thijs R.A., Achab, Aicha, Asselin, Esther, Dabard, Marie-Pierre, Farley, Claude, Loi, Alfredo, Paris, Florentin, Wickson, Steven, Veizer, Jan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4164773/
https://www.ncbi.nlm.nih.gov/pubmed/25174941
http://dx.doi.org/10.1038/ncomms5485

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4164773/
https://www.ncbi.nlm.nih.gov/pubmed/25174941
http://dx.doi.org/10.1038/ncomms5485

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