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

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (21 Nov 2019) by Alberto Reyes
AR by Louis Honegger on behalf of the Authors (21 Nov 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (13 Dec 2019) by Alberto Reyes
RR by Anonymous Referee #1 (28 Dec 2019)
ED: Publish as is (07 Jan 2020) by Alberto Reyes
AR by Louis Honegger on behalf of the Authors (08 Jan 2020)  Manuscript 
Download
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.