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Kurek Formation
Geologic formation in Uzbekistan From Wikipedia, the free encyclopedia
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The Kurek Formation (Russian: Kurek Svita) is a late Oxfordian (Late Jurassic) geologic formation of the Kugitang Svita in Turkmenistan and Uzbekistan. Fossil sauropod tracks have been reported from the formation.[1]
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Etymology
The formation is named after Mount Kurek (2,280 metres (7,480 ft)), near Langar, Uzbekistan.[2]
Description
The mudstones and limestones of the formation comprise a 2 centimetres (0.79 in) thick, massive micrite (mudstone) with sporadic and poorly preserved thin-walled bivalves. Also tracks were preserved at that were probably made in shallow water, showing, in some parts, ripple marks.[3]
Fossil content
Among the following fossils have been found in the Kurek Formation:[4]
Color key
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Notes Uncertain or tentative taxa are in small text; |
Dinosaurs
Ichnofossils
Molluscs
Bivalves
See also
- List of dinosaur-bearing rock formations
- Bissekty Formation
- Bostobe Formation
- Qiketai, Toutunhe, Shishugou and Qigu Formations, fossiliferous formations of the Junggar Basin, Xinjiang
- Haifanggou Formation, Hebei Basin, Hebei
- Oxfordian formations
- Oxford Clay, England
- Tendaguru Formation, fossiliferous formation of Tanzania
- Cañadón Calcáreo Formation, fossiliferous formation of the Cañadón Asfalto Basin, Argentina
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References
Further reading
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