“…Lignified remains of plants, sponges and invertebrate marks are represented in the Vespella marls member (Farrés, 2003). Osteichthyan fishes were discovered at the base of the Terminal Complex (CT, in Farrés et al, 2016;Carnevale et al, 2018) at a level which is positioned in lateral passage with the Sant Martí Xíc Formation that provided Eocenochelus: this level corresponds to the end of the Eocene marine deposits and is situated just below the continental Artés Formation s. l. (Farrés, 1961(Farrés, , 1993(Farrés, , 2003Farrés and Altimiras, 2007;Farrés and Fierstine, 2009;Staid-Staadt, 1964, 2009;Farrés et al, 2005Farrés et al, , 2016Farrés i Malián, 1960, 2002) (See additive fossils in the series and sedimentology in Farrés et al, 2016. ) All these discoveries highlight the great diversity of fossils from Osona County, deposited in the Ebro Basin and coming from both the littoral zone and the shore of the continental region.…”