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

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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Chi tiết về thư mục
Những tác giả chính: 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
Định dạng: Bài viết
Ngôn ngữ:English
Được phát hành: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2009-03-01
Loạt:Geologica Acta
Những chủ đề:
PETM
Paleocene-Eocene boundary
Larger foraminifera
Isotopes
Campo section
Truy cập trực tuyến:https://revistes.ub.edu/index.php/GEOACTA/article/view/2052

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/2052

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