Kurek Formation | |
---|---|
Stratigraphic range: Late Oxfordian ~ | |
Type | Geological formation |
Unit of | Kugitang Svita |
Lithology | |
Primary | Limestone |
Other | Mudstone |
Location | |
Coordinates | 38°30′N68°36′E / 38.5°N 68.6°E |
Approximate paleocoordinates | 43°12′N73°12′E / 43.2°N 73.2°E |
Region | Lebap (Turkmenistan) Kashkadarya (Uzbekistan) |
Country | Turkmenistan, Uzbekistan |
Type section | |
Named for | Mount Kurek |
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]
The formation is named after Mount Kurek (2,280 metres (7,480 ft)), near Langar, Uzbekistan. [2]
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]
Among the following fossils have been found in the Kurek Formation: [4]
Color key
| Notes Uncertain or tentative taxa are in small text; |
Dinosaurs of the Kurek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Gissarosaurus | G. tetrafalangensis | |||||
Ichnofossils of the Kurek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Megalosauripus | M. uzbekistanicus | |||||
Mirsosauropus | M. tursunzadei | |||||
Regarosauropus | R. manovi | |||||
Shirkentosauropus | S. shirkentensis | |||||
Therangospodus | T. pandemicus | |||||
Bivalves of the Kurek Formation | ||||||
---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Bivalvia Indet. | Indeterminate | |||||
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