Bakhar Formation | |
---|---|
Stratigraphic range: Aalenian-Bathonian ~ | |
Type | Geological formation |
Lithology | |
Primary | Claystone |
Other | Coal |
Location | |
Coordinates | 44°54′N100°54′E / 44.9°N 100.9°E |
Approximate paleocoordinates | 48°06′N105°12′E / 48.1°N 105.2°E |
Country | Mongolia |
Extent | North Molasse Basin |
The Bakhar Formation (Russian: Bakhar Svita) is a geological formation in Mongolia whose strata date back to the Aalenian to Bathonian stages of the Middle Jurassic, comprising claystones deposited in a lacustrine environment. [1]
Insects; Platyperla propera , [2] Ano da , A. net, A. nym, Blattula anuniversala , B. bacharensis, B. flamma, B. mikro, B. mini, B. universala, B. velika, B. vulgara, Caloblattina vremeni , Dostavba pre , Hra disko , H. bavi, H. nie, Nuurcala cela , Okras sarko , Perlucipecta cosmopolitana , Polliciblattula analis , P. tatosanerata, P. vana, Praeblattella jurassica , Raphidiomima chimnata , R. krajka, Rhipidoblattina bakharensis , R. konserva, R. sisnerahkab, Solemnia togokhudukhensis , Truhla vekov , [3] fish (Palaeonisciformes) and pterosaur remains of the family Anurognathidae have been recovered from the formation. [4] [5] The formation has also provided many fossil flora in its coal layers, known as the Tsagan-Ovoo Flora containing 32 megafossil plant taxa belonging to horsetails, ferns, cycadaleans, ginkgoaleans, leptostrobaleans, conifers and gymnosperms. Three new species were named; Ginkgo badamgaravii , Pseudotorellia gobiense and P. mongolica . [6]