When and how did the terrestrial mid-Permian mass extinction occur? Evidence from the tetrapod record of the Karoo Basin, South Africa

A mid-Permian (Guadalupian epoch) extinction event at approximately 260 Ma has been mooted for two decades. This is based primarily on invertebrate biostratigraphy of Guadalupian–Lopingian marine carbonate platforms in southern China, which are temporally constrained by correlation to the associated...

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Dades bibliogràfiques
Publicat a:Proc Biol Sci
Autors principals: Day, Michael O., Ramezani, Jahandar, Bowring, Samuel A., Sadler, Peter M., Erwin, Douglas H., Abdala, Fernando, Rubidge, Bruce S.
Format: Artigo
Idioma:Inglês
Publicat: The Royal Society 2015
Matèries:
Research Articles
Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC4528552/
https://ncbi.nlm.nih.gov/pubmed/26156768
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspb.2015.0834
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