It was previously known as theLower Nemegt Bedsoccurring beneath theNemegt Formationand above theDjadokhta Formation.It has been suggested that the Djadokhta and Barun Goyot Formations are lower and upper parts, respectively, of the same lithological unit and the boundary between the two does not exist. Thestratotypeof the Barun Goyot Formation is the Khulsan locality, east of Nemegt. At Nemegt, only the uppermost barungoyotian beds are visible. TheRed Beds of Khermeen Tsavare also considered part of the Barun Goyot Formation. It is approximately 110 metres (360 ft) in thickness,[1]and was laid down roughly 72-71 million years ago. Given the new date for the start of theMaastrichtian(72.1 MYA) a basal Maastrichtian age seems probable. The Barun Goyot Formation preserves an environment ofsand dunes,created from wind-eroded rocks (aeoliandunes).
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^abPenkalski, P.; Tumanova, T. (2017). "The cranial morphology and taxonomic status of Tarchia (Dinosauria: Ankylosauridae) from the Upper Cretaceous of Mongolia".Cretaceous Research.70:117−127.Bibcode:2017CrRes..70..117P.doi:10.1016/j.cretres.2016.10.004.
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^Elzanowski, A. (1977). Skulls of Gobipteryx (Aves) from the Upper Cretaceous of Mongolia. Results of the Polish-Mongolian Paleontological Expeditions - Part VII. Palaeontologica Polonica. 37, 153-165.
^Elzanowski, A. (1995). Cretaceous birds and avian phylogeny. Cour. Forschungsinst. Senckenb. 181, 37-53.
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^Bell, A.K., Chiappe, L.M., Suzuki, S., Watabe, M. (2008). "Phylogenetic and morphometric analysis of a new ornithuromorph from the Barun Goyot Formation, Southern Mongolia." Abstracts of the 7th International Meeting of the Society of Avian Paleontology and Evolution.1.
^Bell, A.K., Chiappe, L.M., Erickson, G.M., Suzuki, S., Watabe, M., Barsbold, R. and Tsogtbaatar, K. (2010). "Description and ecologic analysis ofHollanda luceria,a Late Cretaceous bird from the Gobi Desert (Mongolia). "Cretaceous Research,31(1): 16-26.doi:10.1016/j.cretres.2009.09.001
^Weishampel, D. B.; Barrett, P. M.; Coria, R. A.; Loeuff, J. L.; Xing, X.; Xijin, Z.; Sahni, A.; Gomani, E. M. P. (2004)."Dinosaur Distribution".In Weishampel, D. B.; Dodson, P.; Osmolska, H. (eds.).The Dinosauria(2nd ed.). University of California Press. pp. 596−598.ISBN0520242092.
^Kundrat, M. (2007). Avian-like attributes of a virtual brain model of the oviraptorid theropod Conchoraptor gracilis. Naturwissenschaften. 94: 499−504.
^Kundrat, M.; Janacek, J. (2007). Cranial pneumatization and auditory perceptions of the oviraptorid dinosaur Conchoraptor gracilis (Theropoda, Maniraptora) from the Late Cretaceous of Mongolia. Naturwissenschaften. 94(9): 769−778.
^abFunston, G. F.; Mendonca, S. E.; Currie, P. J.; Barsbold, R.; Barsbold, R. (2018). "Oviraptorosaur anatomy, diversity and ecology in the Nemegt Basin".Palaeogeography, Palaeoclimatology, Palaeoecology.494:101−120.Bibcode:2018PPP...494..101F.doi:10.1016/j.palaeo.2017.10.023.
^abFunston, G. F. (2019)."Chapter 4 – Oviraptoridae"(PDF).Anatomy, systematics, and evolution of Oviraptorosauria (Dinosauria, Theropoda)(PhD thesis). University of Alberta.