Bostobe Formation

Stratigraphic Unit in Kazakhstan From Wikipedia, the free encyclopedia

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).

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Bostobe Formation
Stratigraphic range: Santonian-early Campanian
~85 Ma
TypeGeological formation
UnderliesAkzhar Formation
OverliesZhirkindek Formation
ThicknessAbout 45 m (148 ft)
Lithology
PrimarySandstone
OtherClaystone
Location
Coordinates45.9°N 64.7°E / 45.9; 64.7
Approximate paleocoordinates38.7°N 58.0°E / 38.7; 58.0
RegionQaraghandy & Qyzylorda
Country Kazakhstan
Type section
Named forBostobe River
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Bostobe Formation (Kazakhstan)
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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 45 metres (148 ft) 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]

See also

References

Further reading

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