Record of palaeoclimate across the Cretaceous–Palaeogene boundary from palaeosols in the west‐central San Juan Basin, New Mexico, USA

Abstract The mass extinction at the Cretaceous–Palaeogene boundary is widely attributed to sudden and severe climate changes forced by bolide impact and/or flood basalt volcanism. In terrestrial depositional settings, these changes may potentially be recorded by palaeosols. To test the ability of pe...

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Bibliographic Details
Main Authors: Lawrence H. Tanner, Spencer G. Lucas
Format: Article
Language:English
Published: Wiley 2023-11-01
Series:The Depositional Record
Subjects:
Online Access:https://doi.org/10.1002/dep2.251