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

Marine GeologyCampo SectionEngineeringPaleoenvironmental ChangePaleoceanographyEvolutionary BiologyCalcareous PlanktonGeologyLarger ForaminifersGeochronologyPaleoclimatologyCretaceous-paleogene BoundaryEarth Science