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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
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Dinosaurs

More information Dinosaurs of the Kurek Formation, Genus ...

Ichnofossils

More information Ichnofossils of the Kurek Formation, Genus ...

Molluscs

Bivalves

More information Bivalves of the Kurek Formation, Genus ...

See also

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References

Further reading

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