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Middle Ordovician astrochronology decouples asteroid breakup from glacially-induced biotic radiations

Meso-Cenozoic evidence suggests links between changes in the expression of orbital changes and millennia-scale climatic- and biotic variations, but proof for such shifts in orbital cyclicity farther back in geological time is lacking. Here, we report a 469-million-year-old Palaeozoic energy transfer...

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Detalles Bibliográficos
Autores principales: Rasmussen, Jan Audun, Thibault, Nicolas, Mac Ørum Rasmussen, Christian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8571325/
https://www.ncbi.nlm.nih.gov/pubmed/34741034
http://dx.doi.org/10.1038/s41467-021-26396-4