Kungurian

Source: Wikipedia, the free encyclopedia.
Kungurian
283.5 ± 0.6 – 273.01 ± 0.14 Ma
Chronology

In the

million years ago (Ma). It was preceded by the Artinskian and followed by the Roadian.[3]

Stratigraphy

The Kungurian is named after the Russian city of Kungur in Perm Krai. The stage was introduced into scientific literature by Russian geologist Alexandr Antonovich Stukenberg (Alexander Stuckenberg) in 1890.[4]

The base of the Kungurian Stage is defined as the place in the stratigraphic record where fossils of

GSSP) for the base of the Kungurian. The top of the Kungurian (the base of the Roadian and the Guadalupian series) is defined as the place in the stratigraphic record where fossils of conodont species Jinogondolella
nanginkensis first appear.

The Kungurian contains three conodont biozones:

  • zone of Neostreptognathodus sulcoplicatus
  • zone of Neostreptognathodus prayi
  • zone of Neostreptognathodus pnevi

References

  1. ^ "Chart/Time Scale". www.stratigraphy.org. International Commission on Stratigraphy.
  2. ^ "GSSP for Roadian Stage". International Commission on Stratigraphy. Retrieved 13 December 2020.
  3. Cambridge University
    Press
  4. ^ Chuvashov, B.I.; Chernykh, V.V.; Leven, E.Y.; Davydov, V.I.; Bowring, S.A.; Ramezani, J.; Glenister, B.F.; Henderson, C.M.; Schiappa, T.A.; Northrup, C.J.; Snyder, W.S.; Spinosa, C. & Wardlaw, B.R.; 2002: Progress report on the base of the Artinskian and base of the Kungurian by the Cisuralian Working Group, Permophiles 41: pp 13–16.

External links