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Öösh Formation

Geological formation in Övörkhangai, Mongolia From Wikipedia, the free encyclopedia

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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]

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Vertebrate paleofauna

Dinosaurs

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

Mammals

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Pterosaurs

More information Pterosaurs of the Öösh Formation, Genus ...

Squamates

More information Squamates of the Öösh Formation, Genus ...
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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.
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See also

References

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