A microbial carbonate response in synchrony with the end-Triassic mass extinction across the SW UK

The eruption of the Central Atlantic Magmatic Province (CAMP)—the largest igneous province known—has been linked to the end-Triassic mass extinction event, however reconciling the response of the biosphere (at local and nonlocal scales) to potential CAMP-induced geochemical excursions has remained c...

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Detalles Bibliográficos
Autores principales: Ibarra, Yadira, Corsetti, Frank A., Greene, Sarah E., Bottjer, David J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4728401/
https://www.ncbi.nlm.nih.gov/pubmed/26813244
http://dx.doi.org/10.1038/srep19808

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4728401/
https://www.ncbi.nlm.nih.gov/pubmed/26813244
http://dx.doi.org/10.1038/srep19808

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