Early Cenozoic Decoupling of Climate and Carbonate Compensation Depth Trends

Our understanding of the long‐term evolution of the Earth system is based on the assumption that terrestrial weathering rates should respond to, and hence help regulate, atmospheric CO(2) and climate. Increased terrestrial weathering requires increased carbonate accumulation in marine sediments, whi...

Descripción completa

Detalles Bibliográficos
Autores principales: Greene, S. E., Ridgwell, A., Kirtland Turner, S., Schmidt, D. N., Pälike, H., Thomas, E., Greene, L. K., Hoogakker, B. A. A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6774345/
https://www.ncbi.nlm.nih.gov/pubmed/31598585
http://dx.doi.org/10.1029/2019PA003601

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6774345/
https://www.ncbi.nlm.nih.gov/pubmed/31598585
http://dx.doi.org/10.1029/2019PA003601

Ejemplares similares