Cargando…
Initial pulse of Siberian Traps sills as the trigger of the end-Permian mass extinction
Mass extinction events are short-lived and characterized by catastrophic biosphere collapse and subsequent reorganization. Their abrupt nature necessitates a similarly short-lived trigger, and large igneous province magmatism is often implicated. However, large igneous provinces are long-lived compa...
Autores principales: | Burgess, S. D., Muirhead, J. D., Bowring, S. A. |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2017
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5537227/ https://www.ncbi.nlm.nih.gov/pubmed/28761160 http://dx.doi.org/10.1038/s41467-017-00083-9 |
Ejemplares similares
-
Nickel isotopes link Siberian Traps aerosol particles to the end-Permian mass extinction
por: Li, Menghan, et al.
Publicado: (2021) -
Global nickel anomaly links Siberian Traps eruptions and the latest Permian mass extinction
por: Rampino, Michael R., et al.
Publicado: (2017) -
Different triggers for the two pulses of mass extinction across the Permian and Triassic boundary
por: Li, Guoshan, et al.
Publicado: (2021) -
Felsic volcanism as a factor driving the end-Permian mass extinction
por: Zhang, Hua, et al.
Publicado: (2021) -
Remnant of the late Permian superplume that generated the Siberian Traps inferred from geomagnetic data
por: Li, Shiwen, et al.
Publicado: (2023)