A major sea-level drop briefly precedes the Toarcian oceanic anoxic event: implication for Early Jurassic climate and carbon cycle

Sea-level change is an important parameter controlling the expansion of oxygen-depleted conditions in neritic settings during oceanic anoxic events (OAEs). Despite this fundamental role, it remains on a short timescale (<1 Myr) one of the least constrained parameters for numerous OAEs. Here we pr...

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Detalles Bibliográficos
Autores principales: Krencker, François-Nicolas, Lindström, Sofie, Bodin, Stéphane
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/PMC6715628/
https://www.ncbi.nlm.nih.gov/pubmed/31467345
http://dx.doi.org/10.1038/s41598-019-48956-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6715628/
https://www.ncbi.nlm.nih.gov/pubmed/31467345
http://dx.doi.org/10.1038/s41598-019-48956-x

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