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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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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4728401/ https://ncbi.nlm.nih.gov/pubmed/26813244 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep19808 |
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