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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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Bibliografske podrobnosti
izdano v:Geologica Acta: an international earth science journal
Principais autores: V. PUJALTE, B. SCHMITZ, J. I. BACETA, X. ORUE-ETXEBARRIA, G. BERNAOLA, J. DINARÈS-TURELL, A. PAYROS, E. APELLANIZ, F. CABALLERO
Format: Artigo
Jezik:Inglês
Izdano: Universitat de Barcelona 2009
Teme:
Online dostop:https://www.redalyc.org/articulo.oa?id=50513109010
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