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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...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| 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 |