Articles | Volume 16, issue 1
https://doi.org/10.5194/cp-16-227-2020
https://doi.org/10.5194/cp-16-227-2020
Research article
 | 
04 Feb 2020
Research article |  | 04 Feb 2020

Alluvial record of an early Eocene hyperthermal within the Castissent Formation, the Pyrenees, Spain

Louis Honegger, Thierry Adatte, Jorge E. Spangenberg, Jeremy K. Caves Rugenstein, Miquel Poyatos-Moré, Cai Puigdefàbregas, Emmanuelle Chanvry, Julian Clark, Andrea Fildani, Eric Verrechia, Kalin Kouzmanov, Matthieu Harlaux, and Sébastien Castelltort

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Latest update: 22 Nov 2024
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Short summary
A geochemical study of a continental section reveals a rapid global warming event (hyperthermal U), occurring ca. 50 Myr ago, only described until now in marine sediment cores. Documenting how the Earth system responded to rapid climatic shifts provides fundamental information to constrain climatic models. Our results suggest that continental deposits can be high-resolution recorders of these warmings. They also give an insight on the climatic conditions occurring during at the time.