Alcobaça Formation

The Alcobaça Formation, previously known as the Guimarota Formation and also known as the Consolação Unit,  is a geological formation in Portugal. It dates back to the Kimmeridgian stage of the Late Jurassic. It is an important source of information on the diversity of Late Jurassic mammals. 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. Dinosaur tracks are geographically located in Leiria District, Portugal.

Ornithischians
Indeterminate euornithopod remains located in Lisbon District. Indeterminate stegosaurid remains present in Lisbon District.

Saurischians
Indeterminate sauropod remains located in Leiria and Lisboa.