The Alagteeg Formation is a geological formation in Mongolia whose strata date back to the Late Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.[1] It predominantly consists of alternating reddish brown mudstone and horizontally laminated sandstone, with ripple cross laminations and rhizoliths. It was first formally defined as a unit by Hasegawa et al. in 2008 as a distinct unit from the overlying Djadochta Formation. The environment of deposition is suggested to be fluvial, originating in a sandy braided river, floodplain and ephemeral lake depositional environments, as opposed to the desert depositional environment of the Djadochta Formation.[2]
Fossil content
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Color key
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Notes Uncertain or tentative taxa are in small text; crossed out taxa are discredited. |
Turtles
| Turtles of the Alagteeg Formation |
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| Trionychidae Indet. |
Indeterminate |
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References
Bibliography
- Averianov, Alexander O.; Lopatin, Alexey V. (2020), "An unusual new sauropod dinosaur from the Late Cretaceous of Mongolia", Journal of Systematic Palaeontology, 18 (12): 1009–1032, Bibcode:2020JSPal..18.1009A, doi:10.1080/14772019.2020.1716402
- Hasegawa, Hitoshi; Tada, Ryuji; Ichinnorov, Niiden; Minjin, Chuluun (2009), "Lithostratigraphy and depositional environments of the Upper Cretaceous Djadokhta Formation, Ulan Nuur basin, southern Mongolia, and its paleoclimatic implication", Journal of Asian Earth Sciences, 35 (1): 13–26, Bibcode:2009JAESc..35...13H, doi:10.1016/j.jseaes.2008.11.010
- Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (2004), The Dinosauria, 2nd edition, Berkeley: University of California Press, pp. 1–880, ISBN 0-520-24209-2, retrieved 2019-02-21
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