Bakhar Formation

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]

Bakhar Formation
Stratigraphic range: Aalenian-Bathonian
~174–166 Ma
TypeGeological formation
Lithology
PrimaryClaystone
OtherCoal
Location
Coordinates44.9°N 100.9°E / 44.9; 100.9
Approximate paleocoordinates48.1°N 105.2°E / 48.1; 105.2
Country Mongolia
ExtentNorth Molasse Basin
Bakhar Formation (Mongolia)

Fossil content

An insect, Platyperla propera,[2] fish (Palaeonisciformes) and pterosaur remains of the family Anurognathidae have been recovered from the formation.[3][4] 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.[5]

See also

References

  1. Bakhar Formation at Fossilworks.org
  2. Sinitshenkova, 1987
  3. Bakhurina & Unwin, 1995
  4. Barret et al., 2008
  5. Kostina et al., 2015

Bibliography

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