Bostobe Formation Explained

Bostobe Formation
Type:Geological formation
Age:Santonian-early Campanian
~
Period:Campanian
Prilithology:Sandstone
Otherlithology:Claystone
Namedfor:Bostobe River
Region:Qaraghandy & Qyzylorda
Country: Kazakhstan
Coordinates:45.9°N 64.7°W
Paleocoordinates:38.7°N 58°W
Underlies:Akzhar Formation
Overlies:Zhirkindek Formation
Thickness:About 45m (148feet)

The Bostobe Formation (Kazakh: Boztóbe svıtasy) is a geological formation in Qaraghandy & Qyzylorda, Kazakhastan whose strata date back to the Late Cretaceous (Santonian to early Campanian stages, approximately 85 Ma).

The sandstones and claystones of the formation were deposited in estuarine, fluvial-lacustrine and fluvial-deltaic environments.

Dinosaur remains are among the fossils that have been recovered from the formation.[1] The formation is about 45m (148feet) thick and consists primarily of clay with interbeds of sand, representing an estuarine environment.[2]

Fossil content

Khunnuchelys lophorhothon, a trionychid turtle recovered from the formation, was initially thought to belong to a hadrosaurid dinosaur and classified as cf. Lophorhothon sp.[3]

Mammals
Ankylosaurs
Ornithopods
Sauropods
Theropods
Pterosaurs
Turtles
Other reptiles
Amphibians
Fish
Flora

See also

References

Bibliography

Further reading

Notes and References

  1. Weishampel et al., 2004, pp.593-600
  2. Kordikova et al., 2001
  3. Danilov et al., 2014
  4. Averianov et al., 2014b
  5. Averianov et al., 2014a
  6. Averianov, 2016
  7. Averianov, 2004