“…On the basis of present information, the occurrence of simoceratin species in the Americas is inter− preted as relating the arrival of Tethyan (ubiquitous) taxa to available shelf environments in these areas, a phenomenon that largely involved ammonites throughout Jurassic times. This scenario is compatible with a general model for inter− preting patterns of ammonoid biogeography (Olóriz 1985(Olóriz , 1990, identified in the Americas (Mexican areas included) under a rather variable degree of understanding (see Olóriz 1985Olóriz , 1987Olóriz , 1990Olóriz , 1992Leanza and Olóriz 1987;Olóriz et al 1988Olóriz et al , 1990Leanza and Zeiss 1992;Cecca 1999;Parent and Capello 1999;Villaseñor et al 2000aVillaseñor et al , 2003Par− ent 2001;Villaseñor and Olóriz 2001, 2004, 2009, Parent et al 2006, among others, for precise appliance of the model and/or compatible interpretations). A conceptual comple− ment to this template is provided by assuming biogeographic dynamics as recognised from present cephalopods (e.g., Nor− man 2003; Yoshida et al 2006;Bolstad 2009;Gillanders et al 2009) and the potential application to past cephalopod re− cords (e.g., Olóriz and Villaseñor 2010; and references therein)-see Notes on Simoceratinae chapter above.…”