REFERENCES

Angori, E., and Monechi, S., 1996. High-resolution calcareous nannofossil biostratigraphy across the Paleocene/Eocene boundary at Caravaca (southern Spain). Israel J. Earth Sci., 44:197–206.

Bralower, T.J., 2002. Evidence for surface water oligotrophy during the late Paleocene–Eocene Thermal Maximum: nannofossil assemblages data from Ocean Drilling Program Site 690, Maud Rise, Weddell Sea. Paleoceanography, 17(2):1–12. doi:10.1029/2001PA000662

Bybell, L.M., and Self-Trail, J.M., 1995. Evolutionary, biostratigraphic, and taxonomic study of calcareous nannofossils from a continuous Paleocene/Eocene boundary section in New Jersey. Geol. Surv. Prof. Pap. U.S., 1554.

Kahn, A., and Aubry, M.-P., 2004. Provincialism associated with the Paleocene/Eocene Thermal Maximum: temporal constraint. Mar. Micropaleontol., 52(1–4):117–131. doi:10.1016/j.marmicro.2004.04.003

Kelly, D.C., Bralower, T.J., and Zachos, J.C., 1998. Evolutionary consequences of the latest Paleocene Thermal Maximum for tropical planktonic foraminifera. Palaeogeogr., Palaeoclimatol., Palaeoecol., 141(1–2):139–161. doi:10.1016/S0031-0182(98)00017-0

Martini, E., 1971. Standard Tertiary and Quaternary calcareous nannoplankton zonation. In Farinacci, A. (Ed.), Proc. 2nd Int. Conf. Planktonic Microfossils Roma: Rome (Ed. Tecnosci.), 2:739–785.

Monechi, S., Angori, E., and von Salis, K., 2000. Calcareous nannofossil turnover around the Paleocene/Eocene transition at Alamedilla (southern Spain). Bull. Soc. Geol. Fr., 171:477–489.

Orue-Etxebarria, X., Bernaola, G., Baceta, J.I., Angori, E., Caballero, F., Monechi, S., Pujalte, V., Dinarès-Turell, J., Apellaniz, E., and Payros, A., 2004. New constraints on the evolution of planktic foraminifera and calcareous nannofossils across the Paleocene–Eocene boundary interval: the Zumaia section revisited. Neues Jahrb. Geol. Palaeontol., Abh., 234:223–259.

Steinmetz, J.C., 1979. Calcareous nannofossils from the North Atlantic Ocean, Leg 49, Deep Sea Drilling Project. In Luyendyk, B.P., Cann, J.R., et al., Init. Repts. DSDP, 49: Washington (U.S. Govt. Printing Office), 519–531.

Thomas, E., and Shackleton, N., 1996. The Palaeocene–Eocene benthic foraminiferal extinction and stable isotope anomalies. In Knox, R.W.O'B., Corfield, R.M., and Dunay, R.E. (Eds.), Correlation of the Early Paleogene in Northwest Europe. Geol. Soc. Spec. Publ., 101:401–441.

Tremolada, F., and Bralower, T.J., 2004. Nannofossil assemblage fluctuations during the Paleocene–Eocene Thermal Maximum at Sites 213 (Indian Ocean) and 401 (North Atlantic Ocean): paleoceanographic implications. Mar. Micropaleontol., 52(1–4):107–116. doi:10.1016/j.marmicro.2004.04.002

Zachos, J.C., Kroon, D., Blum, P., et al., 2004. Proc. ODP, Init. Repts., 208: College Station, TX (Ocean Drilling Program). doi:10.2973/odp.proc.ir.208.2004

Zachos, J.C., Röhl, U., Schellenberg, S.A., Sluijs, A., Hodell, D.A., Kelly, D.C., Thomas, E., Nicolo, M., Raffi, I., Lourens, L.J., McCarren, H., and Kroon, D., 2005. Rapid acidification of the ocean during the Paleocene–Eocene Thermal Maximum. Science, 308(5728):1611–1615. doi:10.1126/science.1109004

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