Ordovician–Silurian true polar wander as a mechanism for severe glaciation and mass extinction

The Ordovician–Silurian transition experienced severe, but enigmatic, glaciation, as well as a paradoxical combination of mass extinction and species origination. Here we report a large and fast true polar wander (TPW) event that occurred 450–440 million years ago based on palaeomagnetic data from S...

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Detalles Bibliográficos
Autores principales: Jing, Xianqing, Yang, Zhenyu, Mitchell, Ross N., Tong, Yabo, Zhu, Min, Wan, Bo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9792554/
https://www.ncbi.nlm.nih.gov/pubmed/36572674
http://dx.doi.org/10.1038/s41467-022-35609-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9792554/
https://www.ncbi.nlm.nih.gov/pubmed/36572674
http://dx.doi.org/10.1038/s41467-022-35609-3

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