Did the Late Paleocene thermal maximum affect the evolution of larger foraminifers? Evidence from calcareous plankton of the Campo section (Pyrenees, Spain)

Marine Micropaleontology

Volumn 41, Issue 1-2, 2001, Pages 45-71

  Orue Etxebarria, X ^a   Pujalte, V ^a   Bernaola, G ^a   Apellaniz, E ^a   Baceta, J I ^b   Payros, A ^a   Nunez Betelu K ^a   Serra Kiel, J ^c   Tosquella, J ^b  

^a UNIVERSITY OF THE BASQUE COUNTRY UPV EHU   (Spain)

^b UNIVERSITY OF HUELVA   (Spain)

^c UNIVERSITY OF BARCELONA   (Spain)

Author keywords

Calcareous nannofossils; Campo section; Ilerdian; Larger foraminifers; Paleocene Eocene boundary; Planktic foraminifers; Southern Pyrenees

Indexed keywords

EVOLUTION; PALEOCENE; PALEOCLIMATE; PLANKTONIC FORAMINIFERA;

SPAIN;

EID: 0035126184     PISSN: 03778398     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0377-8398(00)00052-9     Document Type: Article

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