Terrestrial Response to Maastrichtian Climate Change Determined from Paleosols of the Dawson Creek Section, Big Bend National Park, Texas

Climate during the Late Cretaceous is characterized by a long-term cooling trend interrupted by several periods of increased warming. This study focuses on the terrestrial response to two rapid climate events just prior to the K-Pg boundary marked by the Chicxulub impact: the Mid-Maastrichtian Event...

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Bibliographic Details
Main Authors: Anna K. Lesko, Steve I. Dworkin, Stacy C. Atchley
Format: Article
Language:English
Published: MDPI AG 2025-03-01
Series:Geosciences
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Online Access:https://www.mdpi.com/2076-3263/15/4/119
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