Tereñes Formation Explained

Tereñes Formation
Type:Geological formation
Age:Kimmeridgian
~
Period:Kimmeridgian
Prilithology:Marl
Otherlithology:Sandstone
Region:Asturias
Country: Spain
Coordinates:43.5°N -5.2°W
Paleocoordinates:35.6°N 7°W
Thickness:400 metres

The Tereñes Formation or Tereñes Marl is a Late Jurassic (Kimmeridgian) geologic formation in Asturias, Spain. The grey marls of the formation were deposited in a lagoonal environment at a muddy coast along a temporary inland sea. The lower section of the formation comprises silty and chalky sandstones with desiccation cracks and ripple marks, then becomes a bituminous, prominently ostracod-bearing, pelecypod shell chalk, lime chalk marl and marl.[1] Fossil tracks have been reported from the formation.[2]

Fossil content

The following fossils were reported from the formation:[1]

Dinosaurs
Crocodylimorphs
Ichnofossils

See also

References

Bibliography

Notes and References

  1. http://www.fossilworks.org/cgi-bin/bridge.pl?action=displayStrata&geological_group=&formation=Tere%F1es&group_formation_member=Tere%F1es Tereñes Formation
  2. Rauhut. Oliver W. M.. Piñuela. Laura. Castanera. Diego. García-Ramos. José-Carlos. Cela. Irene Sánchez. 2018-07-05. The largest European theropod dinosaurs: remains of a gigantic megalosaurid and giant theropod tracks from the Kimmeridgian of Asturias, Spain. PeerJ. en. 6. e4963. 10.7717/peerj.4963. 30002951 . 2167-8359. 6035862 . free .
  3. Ruiz Omeñaca et al., 2012
  4. Ruiz Omeñaca et al., 2007
  5. Ruiz Omeñaca et al., 2010
  6. Young et al., 2014
  7. Mensink & Mertmann, 1984