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...

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Detalles Bibliográficos
Autores principales: Ullmann, C. V., Boyle, R., Duarte, L. V., Hesselbo, S. P., Kasemann, S. A., Klein, T., Lenton, T. M., Piazza,  V., Aberhan, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
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

Internet

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

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