Onset of main Phanerozoic marine radiation sparked by emerging Mid Ordovician icehouse

The Great Ordovician Biodiversification Event (GOBE) was the most rapid and sustained increase in marine Phanerozoic biodiversity. What generated this biotic response across Palaeozoic seascapes is a matter of debate; several intrinsic and extrinsic drivers have been suggested. One is Ordovician cli...

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Detalles Bibliográficos
Autores principales: Rasmussen, Christian M. Ø., Ullmann, Clemens V., Jakobsen, Kristian G., Lindskog, Anders, Hansen, Jesper, Hansen, Thomas, Eriksson, Mats E., Dronov, Andrei, Frei, Robert, Korte, Christoph, Nielsen, Arne T., Harper, David A.T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4702064/
https://www.ncbi.nlm.nih.gov/pubmed/26733399
http://dx.doi.org/10.1038/srep18884

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4702064/
https://www.ncbi.nlm.nih.gov/pubmed/26733399
http://dx.doi.org/10.1038/srep18884

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