| Bukobay Svita | |
|---|---|
| Stratigraphic range: Ladinian ~ | |
| "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 |
| Approximate paleocoordinates | 35°24′N41°00′E / 35.4°N 41.0°E |
| Region | Orenburg, Bashkortostan |
| Country | |
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).
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]