Articles | Volume 11, issue 12
https://doi.org/10.5194/cp-11-1653-2015
https://doi.org/10.5194/cp-11-1653-2015
Research article
 | 
11 Dec 2015
Research article |  | 11 Dec 2015

A massive input of coarse-grained siliciclastics in the Pyrenean Basin during the PETM: the missing ingredient in a coeval abrupt change in hydrological regime

V. Pujalte, J. I. Baceta, and B. Schmitz

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 (20 Sep 2015) by Gerald Dickens
AR by Victoriano Pujalte on behalf of the Authors (13 Nov 2015)
ED: Publish subject to technical corrections (18 Nov 2015) by Gerald Dickens
AR by Victoriano Pujalte on behalf of the Authors (23 Nov 2015)  Author's response   Manuscript 
Download
Short summary
An abrupt increase in seasonal precipitation during the PETM in the Pyrenean Gulf has been proposed, based on the occurrence of extensive fine-grained siliciclastic deposits. This paper provides evidence that coarse-grained siliciclastics were also delivered, indicative of episodes of intense rainy intervals in an otherwise semiarid PETM climate. Further, evidence is presented that PETM kaolinites were most likely resedimented from Cretaceous lateritic profiles developed in the basement.