Clay hydroxyl isotopes show an enhanced hydrologic cycle during the Paleocene-Eocene Thermal Maximum

The Paleocene-Eocene Thermal Maximum (PETM) was an abrupt global warming event associated with a large injection of carbon into the ocean-atmosphere system, as evidenced by a diagnostic carbon isotope excursion (CIE). Evidence also suggests substantial hydrologic perturbations, but details have been...

Descripción completa

Detalles Bibliográficos
Autores principales: Walters, Gregory L., Kemp, Simon J., Hemingway, Jordon D., Johnston, David T., Hodell, David A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9780225/
https://www.ncbi.nlm.nih.gov/pubmed/36550174
http://dx.doi.org/10.1038/s41467-022-35545-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9780225/
https://www.ncbi.nlm.nih.gov/pubmed/36550174
http://dx.doi.org/10.1038/s41467-022-35545-2

Ejemplares similares