Cisuralian

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Permian period
299-251
Cisuralian
299-271
Guadalupian
271-260
Lopingian
260-251
Asselian
299-295
Sakmarian
295-284
Artinskian
284-276
Kungurian
276-271
Roadian
271-268
Wordian
268-266
Capitanian
266-260
Wuchiapingian
260-254
Changhsingian
254-251


The Cisuralian Epoch of the Permian Period
299 to 271 million years ago


The Cisuralian epoch, a period of well over 20 million years, was - as far as the terrestrial ecosystem went - a fairly stable period ruled over by a diverse selection of pelycosaurs, including the large sphenacodontid finbacks such as the carnivorous Dimetrodon, Ctenospondylus, and Secodontosaurus, all of which attained a lengths of up to 3 meters, as well as semi-aquatic ophiacodonts and the big temnospondyl Eryops and smaller eel-like anthracosaur Archeria. This was a biome strongly tied to water and to a plant-arthropod-fish food chain; Diadectes and Edaphosaurus were the only herbivores. In this respect it continued the pattern of the great Carboniferous coal swamps. The drier upland was inhabited by a different fauna, mostly smaller insectivores with the herbivorous caseids and proto-therapsid Tetraceratops as significant newcomers. Both in the uplands and the lowlands insects continued to represent an astonishing diversity of forms.

[edit] Stratigraphy

PeriodEpochAgeWhen beganDuration (Ma)
PermianGuadalupianRoadian270.62.6
CisuralianKungurian275.65.0
Artinskian284.48.8
Sakmarian294.610.2
Asselian299.04.4
CarboniferousPennsylvanianGzhelian303.94.9




Top: Geological Timescale
Up: Permian Period
Previous: Pennsylvanian | Next: Guadalupian


[edit] Credits

page uploaded on Kheper Site on 24 August 2000, page uploaded on Palaeos Site 10 April 2002, last modified 4 May
text content © M. Alan Kazlev 2000-2002
checked ATW031216
wikified HAJ091222
this material may be freely used for non-commercial purposes

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