Ulaanoosh Formation

Ulaanoosh Formation
Ma PreꞒ Ꞓ O S D C P T J K Pg N
Type	Approximate paleocoordinates	47°36′N 95°30′E / 47.6°N 95.5°E / 47.6; 95.5
Region	Ömnögovi Province
Country	Mongolia
Ulaanoosh Formation (Mongolia)

The Ulaanoosh Formation, formerly Baruunbayan Formation, is a

The Ulaanoosh Formation was formerly considered to be the Baruunbayan Formation (or Baruunbayan Svita in Russian or Mongolian),[1] first documented by the Soviet-Mongolian Paleontological Expeditions between 1946 and 1949. These beds are now considered to be part of the Ulaanoosh Formation. Shuvalov (1982) recognized the red beds at Baruunbayan based on exposures near mountains adjacent to the towns of Baruunbayan and Zuunbayan. Later, the Baruunbayan Svita was more thoroughly studied during a large geological mapping project carried out in the same area by a variety of studies. Due to insufficient representation (only partial sections are exposed at these localities), Badamgarav et al. in 1995 proposed that the Ulaanoosh Formation represents a complete section of red beds in the Baruunbayan area based on drill logs. The Ulaanoosh Formation is distributed in the areas of Ulaanoosh, Alguu Ulaan Tsav, Baruunbayan, and Zuunbayan. The age of the Ulaanoosh Formation ranges from late Early to early Late Cretaceous (Albian-Cenomanian) based on vertebrate and invertebrate fossils such as dinosaurs, dinosaur eggs, molluscs, ostracods, and turtles.^[2]

The Ulaanoosh Formation is composed of two members: a lower and an upper. The lower member (Aptian to Albian) comprises white-colored

Absolute ages and stratigraphic correlation among many Gobi Desert localities are difficult to investigate and hindered by a lack of detailed geological mapping and sediments suitable for radiometric dating. The rock matrix embedding Beg is similar to sediments of the lowest upper member of Ulaanoosh Formation in being composed of reddish-brown conglomerate-breccia and sandstones. This suggests the age of this specimen can be constrained between 113~94 Ma, most likely at the boundary between Early and Late Cretaceous (~100.5 Ma).^[2]

Fossil content

The following fossils have been reported from the formation:^[1]

Group	Taxa	Images	Notes
Neoceratopsia	Beg tse		[2]
Saurischia	Macronaria indet.		[3]
	Sauropoda indet.		[4]
Turtles	Nanhsiungchelyidae indet.		[5]
Faveoloolithidae	Parafaveoloolithus sp.		[6]

See also

• List of dinosaur-bearing rock formations
• Alagteeg Formation
• Khuren Dukh Formation

References

Bibliography

• Yu, Congyu; Albert Prieto Márquez; Tsogtbaatar Chinzorig; Zorigt Badamkhatan, and Mark Norell. 2020. A neoceratopsian dinosaur from the Early Cretaceous of Mongolia and the early evolution of Ceratopsia.
  doi:10.1038/s42003-020-01222-7
• D'Emic, M. D. 2012. The early evolution of titanosauriform sauropod dinosaurs. Zoological Journal of the Linnean Society 166. 624–671. .
• Zhang, S.-K. 2010. A parataxonomic revision of the Cretaceous faveoloolithid eggs of China.
  Vertebrata PalAsiatica
  48. 203–219. .
• Danilov, I. G., and E. V. Syromyatnikova. 2008. New materials on turtles of the family Nanhsiungchelyidae from the Cretaceous of Uzbekistan and Mongolia, with a review of the Nanhsiungchelyid record in Asia. Proceedings of the Zoological Institute RAS 312. 3–25. .
• Mikhailov, K.; K. Sabath, and S. Kurzanov. 1994. Eggs and nests from the Cretaceous of Mongolia. In K. Carpenter, K. F. Hirsch, and J. R. Horner (eds.), Dinosaur Eggs and Babies, 88–115. Cambridge University Press, Cambridge.
• Sochava, A. V. 1969. Dinosaur eggs from the Upper Cretaceous of the Gobi Desert. Paleontological Journal 1969. 517–527. .