[1]
Pujalte, V. et al. 2006. Correlation of the Thanetian-Ilerdian turnover of larger foraminifera and the Initial Eocene thermal maximum (IETM) confirming evidence from the Campo area (Pyrenees, Spain). Anuário do Instituto de Geociências. 29, 1 (Jan. 2006), 500–501. DOI:https://doi.org/10.11137/2006_1_500-501.