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Marine siliceous ecosystem decline led to sustained anomalous Early Triassic warmth
In the wake of rapid CO(2) release tied to the emplacement of the Siberian Traps, elevated temperatures were maintained for over five million years during the end-Permian biotic crisis. This protracted recovery defies our current understanding of climate regulation via the silicate weathering feedba...
| Autores principales: | , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2022
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9206662/ https://www.ncbi.nlm.nih.gov/pubmed/35717338 http://dx.doi.org/10.1038/s41467-022-31128-3 |