The driving mechanisms of the carbon cycle perturbations in the late Pliensbachian (Early Jurassic)

The Early Jurassic (late Pliensbachian to early Toarcian) was a period marked by extinctions, climate fluctuations, and oceanic anoxia. Although the causes of the early Toarcian Oceanic Anoxia Event (OAE) have been fairly well studied, the events that lead to the Toarcian OAE, i.e. the events in the...

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Detalles Bibliográficos
Autores principales: De Lena, Luis F., Taylor, David, Guex, Jean, Bartolini, Annachiara, Adatte, Thierry, van Acken, David, Spangenberg, Jorge E., Samankassou, Elias, Vennemann, Torsten, Schaltegger, Urs
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6895128/
https://www.ncbi.nlm.nih.gov/pubmed/31804521
http://dx.doi.org/10.1038/s41598-019-54593-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6895128/
https://www.ncbi.nlm.nih.gov/pubmed/31804521
http://dx.doi.org/10.1038/s41598-019-54593-1

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