O. Mateus, et al., Ciências da Terra / Earth Sciences Journal 19 (1), 2017, 75-97 The Lourinhã Formation: the Upper Jurassic to lowermost Cretaceous of the Lusitanian Basin, Portugal – landscapes where dinosaurs walked O. Mateus1, 2, J. Dinis3 & P. P. Cunha3 1 GeoBioTec, Earth Sciences Department, Faculty of Sciences and Technology, Universidade NOVA Lisboa, Campus de Caparica. 2829-516 Caparica, Portugal.
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[email protected] Abstract Journal webpage: This work, as a fieldtrip guide, aims to provide a glimpse into the palaeoenvironments, palaeon- http://cienciasdaterra.novaidfct.pt/index. tology, and diagenesis of one of the most productive areas for Late Jurassic dinosaurs and other ver- php/ct-esj/article/view/355 tebrates in Europe, namely, the sites of the Lourinhã Formation, which is coeval with the Morrison Copyright: Formation of the midwest USA. The Late Jurassic rifting phase of the Lusitanian Basin created several sub-basins separated by © 2017 O. Mateus et al. This is an open access article distributed under the terms major crustal faults. In the western and central areas of the basin, the Caldas da Rainha structure sep- and conditions of the Creative Commons arates three sub-basins with different subsidence and infill characteristics (Consolação to the west, Attribution License (CC BY), which Bombarral–Alcobaça to the northeast, and Turcifal to the southeast). The Upper Jurassic–lowermost permits unrestricted use, distribution, Cretaceous succession exposed in the coastal cliffs located between Nazaré and Santa Cruz belongs and reproduction in any medium, to the Consolação Sub-basin, whereas the coastal outcrops between Santa Cruz and Ericeira show provided the original author and source units of the Turcifal Sub-basin.