A deep Tasman outflow of Pacific waters during the last glacial period

The interoceanic exchange of water masses is modulated by flow through key oceanic choke points in the Drake Passage, the Indonesian Seas, south of Africa, and south of Tasmania. Here, we use the neodymium isotope signature (ε(Nd)) of cold-water coral skeletons from intermediate depths (1460‒1689 m)...

Descripción completa

Detalles Bibliográficos
Autores principales: Struve, Torben, Wilson, David J., Hines, Sophia K. V., Adkins, Jess F., van de Flierdt, Tina
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/PMC9246942/
https://www.ncbi.nlm.nih.gov/pubmed/35773248
http://dx.doi.org/10.1038/s41467-022-31116-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9246942/
https://www.ncbi.nlm.nih.gov/pubmed/35773248
http://dx.doi.org/10.1038/s41467-022-31116-7

Ejemplares similares