Transient micropaleontological turnover across a late Eocene (Priabonian) carbon and oxygen isotope shift on Blake Nose (NW Atlantic)

<p>The Gulf Stream, a western boundary current transporting warm water into the North Atlantic, plays a key role in climate regulation and oceanographic stability at a regional and global scale as part of the Atlantic Meridional Overturning Circulation (AMOC). Evidence suggests that an ancestr...

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Bibliographic Details
Main Authors: J. de Entrambasaguas, T. Westerhold, H. L. Jones, L. Alegret
Format: Article
Language:English
Published: Copernicus Publications 2024-08-01
Series:Journal of Micropalaeontology
Online Access:https://jm.copernicus.org/articles/43/303/2024/jm-43-303-2024.pdf