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...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí: 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
Formáid: Alt
Teanga:English
Foilsithe / Cruthaithe: 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
Sraith:Geologica Acta
Ábhair:
PETM
Paleocene-Eocene boundary
Larger foraminifera
Isotopes
Campo section
Rochtain ar líne:https://revistes.ub.edu/index.php/GEOACTA/article/view/2052

Ar líne

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

Míreanna comhchosúla