Planktic foraminiferal turnover across the Paleocene-Eocene transition in the Bay of Biscay, North Atlantic, supplement to: Pardo, Alfonso; Keller, Gerta; Molina, Eustoquio; Canudo, José I (1997): Planktic foraminiferal turnover across the Paleocene-Eocene transition at DSDP Site 401, Bay of Biscay, North Atlantic. Marine Micropaleontology, 29(2), 129-158

Alfonso Pardo, Gerta Keller, Eustoquio Molina & José I Canudo
Planktic foraminifera across the Paleocene-Eocene transition at DSDP Site 401 indicate that the benthic foraminiferal mass extinction occurred within Subzone P 6a of Berggren and Miller (1988), or PS of Berggren et al. (1995) and coincident with a sudden 2.0‰ excursion in 6r3C values. The benthic foraminiferal extinction event (BFEE) and Sr3C excursion was accompanied by a planktic foraminiferal turnover marked by an influx of warm water species (Morozovella and Acarinina), a decrease in cooler...
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