Bukobay Svita

Last updated
Bukobay Svita
Stratigraphic range: Ladinian
~242–235  Ma
Mastodonsaurus3.jpg
"Mastodonsaurus" torvus, an index fossil of the Bukobay Svita / Gorizont
Type Stratigraphic Formation
Overlies Donguz Svita
Lithology
Primary Claystone, siltstone
Other Sandstone
Location
Coordinates 51°24′N55°30′E / 51.4°N 55.5°E / 51.4; 55.5
Approximate paleocoordinates 35°24′N41°00′E / 35.4°N 41.0°E / 35.4; 41.0
Region Orenburg, Bashkortostan
CountryFlag of Russia.svg  Russia
Russia rel location map.png
Pink ff0080 pog.svg
Bukobay Svita (Russia)

The Bukobay Svita (also anglicized as Bukobay or Bukobai Formation) is a Middle Triassic geological unit in Russia. [1] [2] [3] It is composed primarily of red or grey lacustrine sediments, reconstructing a humid and marshy depositional environment. Bukobay is the youngest section of a Triassic terrestrial succession exposed south of the Ural Mountains. It is equivalent to a biostratigraphic unit, the Bukobay Gorizont , which is also called the "Bukobay Horizon" or "Mastodonsaurus" fauna).

Contents

Fossil content

Notable components of the Bukobay fauna include "Mastodonsaurus" torvus (a giant capitosaur amphibian), Malutinisuchus gratus and Energosuchus garjainovi , the insect Mesoneta uralensis , Elephantosaurus jachimovitschi (a large dicynodont), and Chalishevia cothurnata (the youngest known erythrosuchid). Temnospondyls include Bukobaja enigmatica , Cyclotosaurus , Plagioscutum caspiense and Plagiorophus paraboliceps , with Ceratodus orenburgensis and C. bucobaensis as fish. The flora is also diverse, including Equisetites arenaceus (a species of giant horsetails) and Ladinian-age palynomorphs. [4] [5]

See also

References

  1. Bukobay Formation at Fossilworks.org
  2. Bukobai Formation at Fossilworks.org
  3. Bukobaiskaya Suite at Fossilworks.org
  4. Tverdokhlebov et al., 2003
  5. Tverdokhlebov et al., 2020

Bibliography

Further reading