Abyssal oceanic circulation and acidification during the Middle Eocene Climatic Optimum (MECO)

The Middle Eocene Climatic Optimum (MECO) is a global warming event that occurred at around 40 Ma and lasted about 500 kyr. We study this event in an abyssal setting of the Tasman Sea, using the IODP Core U1511B-16R, collected during the expedition 371. We analyse magnetic, mineralogical, and chemic...

Descripción completa

Detalles Bibliográficos
Autores principales: Cornaggia, Flaminia, Bernardini, Simone, Giorgioni, Martino, Silva, Gabriel L. X., Nagy, André Istvan M., Jovane, Luigi
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/PMC7174310/
https://www.ncbi.nlm.nih.gov/pubmed/32317709
http://dx.doi.org/10.1038/s41598-020-63525-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7174310/
https://www.ncbi.nlm.nih.gov/pubmed/32317709
http://dx.doi.org/10.1038/s41598-020-63525-3

Ejemplares similares