Article · Wikipedia archive · Last revised Aug 9, 2026

Bukobay Svita

The Bukobay Svita is a Middle Triassic geological unit in Russia. 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).

Last revised
Aug 9, 2026
Read time
≈ 2 min
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Citations
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Source
Bukobay Svita
Stratigraphic range: Ladinian
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"Mastodonsaurus" torvus, an index fossil of the Bukobay Svita / Gorizont
TypeStratigraphic Formation
OverliesDonguz Svita
Lithology
PrimaryClaystone, siltstone
OtherSandstone
Location
Coordinates51°24′N 55°30′E / 51.4°N 55.5°E / 51.4; 55.5
Approximate paleocoordinates35°24′N 41°00′E / 35.4°N 41.0°E / 35.4; 41.0
RegionOrenburg, Bashkortostan
Country Russia
Bukobay Svita (Russia)

The Bukobay Svita (also anglicized as Bukobay or Bukobai Formation) is a Middle Triassic geological unit in Russia.123 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).

Fossil content

Notable components of the Bukobay fauna include Mastodonsaurus torvus (a giant capitosaur amphibian), Malutinisuchus gratus, Plagiosternum danilovi, Synesuchus muravjevi, Jushatyria vjushkovi4 and Energosuchus garjainovi, the insects Mesoneta uralensis and Triassomachilis uralensis, Elatosaurus facetus, dicynodonts Planitorostris pechoriensis, Elephantosaurus jachimovitschi (a large dicynodont), and Chalishevia cothurnata (the youngest known erythrosuchid). Temnospondyls include Bukobaja enigmatica, Plagioscutum caspiense and Plagiorophus paraboliceps, with Ceratodus orenburgensis, C. jecticristatus and C. bucobaensis as fish. The flora is also diverse, including Equisetites arenaceus (a species of giant horsetails), ferns Cladophlebis shensiensis, Danaeopsis rarinervisand, Lepidopteris microcellularis, ginkgophytes Sphenobaiera granulifer, Glossophyllum sp., cycadophytes Apoldia surakaica and Ladinian-age palynomorphs.56 Also found in the formation were unidentified species from the genus Mastodonsaurus sp., Cyclotosaurus sp., Pistosaurus sp., Bukobaja sp. and Chalishevia sp., as well as remains from the order Theriodontia indet., Kannemeyeroidea indet. and Mastodonsauridae indet..

See also

See also

References

References

Bibliography

Further reading

Further reading

  • I. A. Dobruskina. 1982. Triassic Floras of Eurasia. Akademia Nauk SSSR, Transactions 365:1-196