Demise of the Barra Honda Carbonate Shoal (Costa Rica) at the Paleocene‐Eocene Boundary Linked to Climate Change and Forearc Tectonics

Abstract The latest Cretaceous(?)–Paleocene Barra Honda Formation represents one of the largest carbonate shoals (>900 km2, 350 m thick) of the convergent margin of Costa Rica. Although the mode of formation of the carbonate shoal is well understood, how environmental and tectonic factors interac...

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Bibliographic Details
Main Authors: Goran Andjić, Claudia Baumgartner‐Mora, Peter O. Baumgartner, Maria Rose Petrizzo, Torsten Vennemann, André N. Paul, Valentin Lorenzo
Format: Article
Language:English
Published: Wiley 2025-05-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2024GC012080
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