“…Although dinosaurs, charophytes, ostracodes, plant remains (Legarreta & Uliana, 1999) and palynomorphs (Vallati, 2002(Vallati, , 2010(Vallati, , 2013 are abundant in the continental sequences of Neuqu en Basin, the precise ages of the different formations remain loosely constrained. According to published palaeontological and geochronological data (Bonaparte, 1996;Hugo & Leanza, 2001;Leanza et al, 2004;S anchez et al, 2008;Garrido, 2010), in the present paper, we use the following ages (Figs 1 and 2): Aptian-Albian p.p.…”