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

It has long been known that a major larger foraminifera turnover (LFT) occurred at the boundary between the Thanetian and Ilerdian stages, but its possible correlation with the Paleocene-Eocene thermal maximum (PETM) was unsuspected until the work of Baceta (1996), and has been controversial ever si...

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Detalhes bibliográficos

Principais autores:	V. PUJALTE, B. SCHMITZ, J.I. BACETA CABALLERO, X. ORUE-ECHEBARRÍA, G. BERNAOLA BILBAO, J. DINARÈS-TURELL, A. PAYROS AGIRRE, E. APELLANIZ INGUNZA, F. CABALLERO SANTAMARIA
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Universitat de Barcelona (UB); Universitat Autònoma de Barcelona (UAB); Institut Cartogràgic i Geològic de Catalunya (ICGC); i Institut Català de Paleontologia (ICP) 2009-03-01
coleção:	Geologica Acta
Assuntos:	PETM Paleocene-Eocene boundary Larger foraminifera Isotopes Campo section
Acesso em linha:	https://revistes.ub.edu/index.php/GEOACTA/article/view/2052
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