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Kurek Formation

The Kurek Formation () 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.

Etymology

The formation is named after Mount Kurek (), near Langar, Uzbekistan.

Description

The mudstones and limestones of the formation comprise a 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.

Fossil content

Among the following fossils have been found in the Kurek Formation:

Dinosaurs

Ichnofossils

Molluscs

Bivalves

See also

References

Bibliography

Further reading

  • F. Fanti, M. Contessi, A. Nigarov and P. Esenov. 2013. New data on two large dinosaur tracksites from the Upper Jurassic of eastern Turkmenistan (Central Asia). Ichnos 20:54-71
  • V. P. Novikov and M. R. Dzhalilov. 1988. Litologicheskaya interpretatsiya mestonakhozhdeniy sledov dinozavrov i Tadzhikistane [A lithological interpretation of localities with dinosaurian traces in Tajikistan]. In T. N. Bogdanova, L. I. Khosatzky, & A. A. Istchenko (eds.), Sledy Zhiznedeyatel'nosti i Dinamika Sredy v Drevnikh Biotopakh. Trudy XXX Sessii Vsesoyuznogo Paleontologicheskogo Obshchestva i VII Sessii Ukrainskogo Paleontologicheskogo Obshchestva [Fossil Traces of Vital Activity and Dynamics of the Environment in Ancient Biotopes. Transactions of the XXX Session of All-Union Paleontological Society and the VII Session of the Ukrainian Paleontological Society]. Naukova Dumka, Kiev 58–69
  • K. N. Amanniyazov. 1985. Ob unikalnykh sledakh verkhneyurskikh dinozavrov v Turkmenistane [Unique tracks of dinosaurs in the Upper Jurassic of Turkmenistan]. In M. P. Dzhalilov, V. P. Novikov (eds.), Problemy Osvoeniya Pustyn [Problems of Desert Development], Institute of Geology, Academy of Sciences Turkmenistan 2:23-29