The Öösh Formation, also known as the Tevsh Formation is a geological formation of Lower Cretaceous strata in Övörkhangai Province, Mongolia. Dinosaur remains are among the fossils that have been recovered from the formation.[1] It overlies folded and metamorphosed basement strata of the Gobi region, and is capped by basalt. The succession is around 600 metres thick and consists of red claystones and sandstones, along with black thinly laminated shales. The claystones and sandstones were deposited as part of an alluvial fan system, while the shales were deposited in lakes present in the foot of the fan.[2] Many of the fossils come from the "Cannonball beds", which comprise the lowest 60 metres of the unit and consist of green siltstone.[2]
| Pterosaurs of the Öösh Formation
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| Genus |
Species |
Location |
Stratigraphic position |
Material |
Notes |
Images
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| Indeterminate tapejaroid[2][7]
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"Single cervical vertebra (IGM 100/1321)"[2]
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| Squamates of the Öösh Formation
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| Genus |
Species |
Location |
Stratigraphic position |
Material |
Notes |
Images
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| Norellius[8]
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N. nyctisaurops
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"Nearly complete skull with mandibles and partial hyoid"
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Gekkonomorph
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Color key
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Notes Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
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- ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Asia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 563-570. Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value)..
- ^ a b c d Andres, B. and Norell, M.A. 2005. The first record of a pterosaur from the Early Cretaceous strata of Öösh (Övörkhangai; Mongolia). American Museum Novitates 3472: 1–6. [1]
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