Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum

The Paleocene-Eocene Thermal Maximum (PETM; ~55.9 Ma) was a geologically rapid warming period associated with carbon release, which caused a marked increase in the hydrological cycle. Here, we use lithium (Li) isotopes to assess the global change in weathering regime, a critical carbon drawdown mech...

Descripción completa

Detalles Bibliográficos
Autores principales: Pogge von Strandmann, Philip A. E., Jones, Morgan T., West, A. Joshua, Murphy, Melissa J., Stokke, Ella W., Tarbuck, Gary, Wilson, David J., Pearce, Christopher R., Schmidt, Daniela N.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8519576/
https://www.ncbi.nlm.nih.gov/pubmed/34652934
http://dx.doi.org/10.1126/sciadv.abh4224

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8519576/
https://www.ncbi.nlm.nih.gov/pubmed/34652934
http://dx.doi.org/10.1126/sciadv.abh4224

Ejemplares similares