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The Kungurian (also known as Irenian or Filippovian) is the last stage of the Cisuralian epoch of Permian period. It spans the time between 275.6 ± 0.7 Ma and 270.6 ± 0.7 Ma (million years ago). Faunal stages are a subdivision of geologic time used primarily by paleontologists who study fossils rather than by geologists who study rock formations. ... Jump to: navigation, search Cisuralian is the first of the three epoches of the Permian. ... The word epoch can mean either an interval of time, or a particular point in time used as a reference point. ... Jump to: navigation, search The Permian is a geologic period that extends from about 299. ... The table and timeline of geologic periods presented here is in accordance with the dates and nomenclature proposed by the International Commission on Stratigraphy. ... Mega-annum, usually abbreviated as Ma, is a unit of time equal to one million years. ...


References

Permian period
Cisuralian Guadalupian Lopingian
Asselian Sakmarian Roadian Wordian Wuchiapingian
Artinskian Kungurian Capitanian Changhsingian

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Palaeos Paleozoic: Permian: The Kungurian Age (998 words)
Paleozoic vascular flora, which appeared in the Middle Ordovician epoch, died out quite a few millions of years before the end of the Paleozoic, in the Kungurian or earlier.
During the Kungurian these herbivores were generally 2 to 4 meters in length with the largest species reaching 5 or 6 meters
But now in the Kungurian we see an environment dominated by medium to large sized herbivores (the pelycosaur family Caseidae).
LOWER PERMIAN PERRINITID AMMONOID FAUNAS FROM THAILAND Journal of Paleontology - Find Articles (794 words)
ABSTRACT-The Artinskian Metaperrinites and Kungurian Perrinites faunas are recognized from the Ratburi Group of the Loei area, northcentral Thailand, and the Saraburi Group of the Saraburi area, southcentral of the country, respectively.
The age was assigned as part of the Leonard/Road Canyon sequence of the American southwest, or the Artinskian/"Kungurian" Kochusu Suite (Formation) of the southeastern Pamirs, based mainly on the occurrence of Perrinites Bose, 1917.
The assemblage was determined to be representative of the upper Artinskian Baigendzhinian Substage; however, this was merely an inference in response to the knowledge that the Russian Kungurian ammonoids were considered as late Artinskian and pre-Roadian by Bogoslovskaya (1976).
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