Anchoring the Late Devonian mass extinction in absolute time by integrating climatic controls and radio-isotopic dating

The Devonian Frasnian–Famennian (F–F) boundary marks one of the five main extinction intervals of the Phanerozoic Aeon. This time was characterized by two pulses of oceanic anoxia, named the Lower and Upper Kellwasser events, during which massive marine biodiversity losses occurred. This paper prese...

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Detalles Bibliográficos
Autores principales: Da Silva, Anne-Christine, Sinnesael, Matthias, Claeys, Philippe, Davies, Joshua H. F. L., de Winter, Niels J., Percival, L. M. E., Schaltegger, Urs, De Vleeschouwer, David
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7395115/
https://www.ncbi.nlm.nih.gov/pubmed/32737336
http://dx.doi.org/10.1038/s41598-020-69097-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7395115/
https://www.ncbi.nlm.nih.gov/pubmed/32737336
http://dx.doi.org/10.1038/s41598-020-69097-6

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