Articles | Volume 11, issue 12
https://doi.org/10.5194/cp-11-1653-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-11-1653-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
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
CORRESPONDING AUTHOR
Dept. of Stratigraphy and Paleontology, Faculty of Science and Technology, University of the Basque Country (UPV/EHU), Ap. 644, 48080 Bilbao, Spain
J. I. Baceta
Dept. of Stratigraphy and Paleontology, Faculty of Science and Technology, University of the Basque Country (UPV/EHU), Ap. 644, 48080 Bilbao, Spain
B. Schmitz
Division of Nuclear Physics, Department of Physics, University of Lund, P.O. Box 118, 22100 Lund, Sweden
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Latest update: 15 Nov 2024
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.
An abrupt increase in seasonal precipitation during the PETM in the Pyrenean Gulf has been...
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