The Alcobaça Formation is a geological formation in Portugal. It dates back to the Oxfordian stage of the Late Jurassic.[1] It is an important source of information on the diversity of Late Jurassic mammals.[2][3] Many of the fossils were collected from the now disused and flooded Camadas de Guimarota coal mine.
Vertebrate paleofauna
Dinosaur eggs are geographically located in Lisbon District, Portugal.[4] Dinosaur tracks are geographically located in Leiria District, Portugal.[5]
^ abcdefghijklmnopqrstuvwxyzaaabac"16.4 Distrito do Lisboa, Portugal; 1. Camadas de Alcobaça," in Weishampel, et al. (2004). Page 548.
^ abcd"16.1 Distrito do Leiria, Portugal; 3. Camadas de Alcobaça," in Weishampel, et al. (2004). Page 548.
^"16.1 Distrito do Leiria, Portugal; 3. Camadas de Alcobaça," and "16.4 Distrito do Lisboa, Portugal; 1. Camadas de Alcobaça," in Weishampel, et al. (2004). Pages 548-549.
^"Table 13.1," in Weishampel, et al. (2004). Page 265.
Weishampel, David B.; Peter Dodson, and Halszka (eds.) Osmólska. 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21. ISBN0-520-24209-2