Bukobay Svita

The Bukobay Svita (also anglicized as Bukobay or Bukobai Formation) 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).

Bukobay Svita
Stratigraphic range: Ladinian
~
"Mastodonsaurus" torvus, an index fossil of the Bukobay Svita / Gorizont
TypeStratigraphic Formation
OverliesDonguz Svita
Lithology
PrimaryClaystone, siltstone
OtherSandstone
Location
Coordinates51.4°N 55.5°E / 51.4; 55.5
Approximate paleocoordinates35.4°N 41.0°E / 35.4; 41.0
RegionOrenburg, Bashkortostan
Country Russia
Bukobay Svita (Russia)
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