Cisuralian

From Palaeos.org

Jump to: navigation, search
Parent menu:
(the following menu links to parent and sibling pages of this page)


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.

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


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

Personal tools