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

Autores

  • 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

Resumo

Abstract

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Publicado

2006-01-01

Como Citar

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), p. 500–501. doi: 10.11137/2006_1_500-501.

Edição

v. 29 n. 1 (2006)

Seção

Abstract - Micropaleontology of Critical Boundaries

Licença

Os artigos publicados nesta revista se encontram sob a llicença Creative Commons — Atribuição 4.0 Internacional — CC BY 4.0, que permite o uso, distribuição e reprodução em qualquer meio, contanto que o trabalho original seja devidamente citado.