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Warm afterglow from the Toarcian Oceanic Anoxic Event drives the success of deep-adapted brachiopods
Many aspects of the supposed hyperthermal Toarcian Oceanic Anoxic Event (T-OAE, Early Jurassic, c. 182 Ma) are well understood but a lack of robust palaeotemperature data severely limits reconstruction of the processes that drove the T-OAE and associated environmental and biotic changes. New oxygen...
| Autores principales: | , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7162941/ https://www.ncbi.nlm.nih.gov/pubmed/32300235 http://dx.doi.org/10.1038/s41598-020-63487-6 |