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

How to Cite

Pujalte, V. (2006) “Correlation of the Thanetian-Ilerdian turnover of larger foraminifera and the Initial Eocene thermal maximum (IETM) confirming evidence from the Campo area (Pyrenees, Spain)”, Anuário do Instituto de Geociências. Rio de Janeiro, BR, 29(1), pp. 500–501. doi: 10.11137/2006_1_500-501.

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.