Caranguejeira Conglomerate

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Caranguejeira Conglomerate
Stratigraphic range: Aptian-Cenomanian
TypeGeological formation
Lithology
PrimaryConglomerate
Location
Coordinates39°42′N 8°36′W / 39.7°N 8.6°W / 39.7; -8.6Coordinates: 39°42′N 8°36′W / 39.7°N 8.6°W / 39.7; -8.6
Approximate paleocoordinates29°36′N 1°54′W / 29.6°N 1.9°W / 29.6; -1.9
RegionSantarém
Country Portugal
ExtentLusitanian Basin
Caranguejeira Conglomerate is located in Portugal
Caranguejeira Conglomerate
Caranguejeira Conglomerate (Portugal)

The Caranguejeira Conglomerate (Portuguese: Conglomerados de Caranguejeira) is an Aptian to Cenomanian geologic formation in Portugal. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.[1]

Paleofauna[]

Correlation[]

Early Cretaceous stratigraphy of Iberia
Ma Age Paleomap \ Basins Olanyà Lusitanian
100 Cenomanian
Cenomanian-Coniacian Iberia.jpg
Caranguejeira
125 Albian -
Monte Grande Escucha Escucha
-
Aptian - - Castrillo
En Gp. - Morella/ Morella
- En Gp. - Forcall Upper
Bedoulian
Barremian Xert Alacón Xert Huérguina
Artoles Collado Papo Seco
Rúbies Tera Gp. - Alacón/Blesa Blesa Camarillas
150 Hauterivian Iberia 120Ma Barremian zoom.tif Ur Gp. - Castellar Tera Gp. -
hiatus
Valanginian Ur Gp. - -
- - Piedrahita
Berriasian Iberia 150Ma Tithonian.jpg - hiatus
- Rupelo Arzobispo hiatus
On Gp. -
Tithonian Lastres Tera Gp. - Higuereles Tera Gp. - Lourinhã
Arzobispo
Legend Major fossiliferous, oofossiliferous, ichnofossiliferous, coproliferous, minor formation
Sources


See also[]

References[]

  1. ^ a b Weishampel et al. 2004, pp.517-607
  2. ^ a b c d Ourém at Fossilworks.org

Bibliography[]

  • Weishampel, David B.; Peter Dodson, and Halszka Osmólska (eds.). 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21.ISBN 0-520-24209-2

Further reading[]

  • H.-E. Sauvage. 1895. Les dinosauriens du terrain jurassique supérieur du Boulonnais [The dinosaurs from the Upper Jurassic terrain of the Boulonnais]. Bulletin de la Société Géologique de France, 3e série 22:465-470
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