Correlation of the Thanetian-Ilerdian turnover of larger foraminifera and the Initial Eocene thermal maximum (IETM) confirming evidence from the Campo area (Pyrenees, Spain)

Authors

  • Victoriano Pujalte Univ. of the Basque Country; Fac. of Science and Technology; Dept. of Stratigraphy and Paleontology
  • B. Schmitz Univ. of Lund S¶lvegatan; Dept. of Geology
  • J. I. Baceta Univ. of the Basque Country; Fac. of Science and Technology; Dept. of Stratigraphy and Paleontology
  • G. Bernaola Univ. of the Basque Country; Fac. of Science and Technology; Dept. of Stratigraphy and Paleontology
  • J. Dinarès-Turell Inst. Nazionale Geofisica-Vulcanologia; Lab. Paleomagnetismo
  • X. Orue-Etxebarria Univ. of the Basque Country; Fac. of Science and Technology; Dept. of Stratigraphy and Paleontology
  • A. Payros Univ. of the Basque Country; Fac. of Science and Technology; Dept. of Stratigraphy and Paleontology

DOI:

https://doi.org/10.11137/2006_1_500-501

Abstract

Abstract

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Published

2006-01-01

Issue

Vol. 29 No. 1 (2006)

Section

ABSTRACT - MICROPALEONTOLOGY OF CRITICAL BOUNDARIES

License

This journal is licensed under a Creative Commons — Attribution 4.0 International — CC BY 4.0, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.