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Batylykh Formation

Coordinates: 62°42′N 117°36′E / 62.7°N 117.6°E / 62.7; 117.6
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Batylykh Formation
Stratigraphic range: Early Cretaceous
?Berriasian–Barremian
Teete locality with stratigaphic column
TypeGeological formation
Unit ofSangar Series
UnderliesEksenyakh Formation
Lithology
PrimaryClaystone, siltstone, sandstone
Location
Coordinates62°42′N 117°36′E / 62.7°N 117.6°E / 62.7; 117.6
Approximate paleocoordinates66°30′N 110°06′E / 66.5°N 110.1°E / 66.5; 110.1
RegionYakutia
Country Russia
ExtentVilyuy River Basin
Batylykh Formation is located in Russia
Batylykh Formation
Batylykh Formation
Batylykh Formation (Russia)

The Batylykh Formation is a geological formation in Yakutia, Russia. It is of an uncertain Early Cretaceous age, probably dating between the Berriasian and the Barremian. It is the oldest unit of the 1,500 metres (4,900 ft) thick Sangar Series within the Vilyuy syneclise. The mudstones, sandstones and shales of the formation were deposited in a fluvial to lacustrine environment.

Fossil content

The formation is best known for the Teete locality, which has revealed remains of numerous vertebrates, including sauropods[1], and other dinosaur teeth as well as numerous species of mammal, including Sangarotherium, Khorotherium[2] and tritylodontid Xenocretosuchus[3]. as well as choristodere Khurendukhosaurus.[4]

Other fossils recovered from the formation are:[5]

See also

References

  1. ^ Averianov et al., 2019
  2. ^ Averianov et al., 2018
  3. ^ Lopatin & Agadjanian, 2008
  4. ^ Kolosov et al., 2009
  5. ^ Batylykh Formation at Fossilworks.org
  6. ^ Averianov et al., 2020
  7. ^ Skutschas et al., 2020
  8. ^ Skutschas et al., 2018
  9. ^ a b Lukashevich, 1995

Bibliography

  • Template:Cite LSA doi:10.1080/02724634.2019.1762089
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  • Template:Cite LSA doi:10.1111/let.12362
  • Template:Cite LSA doi:10.1371/journal.pone.0199983 ISSN 1932-6203 PMC 6059412 PMID 30044817
  • Template:Cite LSA
  • Template:Cite LSA
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Further reading

  • I. P. Tolmachoff. 1904. Neue Funde zur Geologie Sibiriens [New discoveries about the geology of Siberia]. Centralblatt für Mineralogie, Geologie und Paläontologie 1904(1):233-234