“…2). These were followed during the late Sinemurian -Aalenian by mid-to outer-ramp marls and marly limestones (middle and upper parts of the Coimbra Formation in the northwest of the basin; and the Água de Madeiros, Vale das Fontes, Lemede, Fórnea, São Gião, Cabo Carvoeiro, Cabo Mondego, Póvoa da Lomba and Barranco do Zambujal Formations elsewhere) (Duarte and Soares, 2002;Azerêdo et al, 2003Azerêdo et al, , 2010Azerêdo et al, , 2014Azerêdo, 2007;Duarte, 2007;Duarte et al, 2010Duarte et al, , 2022Silva et al, 2021) (Fig. 2).…”