Cisuralian
From Palaeos.org
| 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 |
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
| Period | Epoch | Age | When began | Duration (Ma) |
|---|---|---|---|---|
| Permian | Guadalupian | Roadian | 270.6 | 2.6 |
| Cisuralian | Kungurian | 275.6 | 5.0 | |
| Artinskian | 284.4 | 8.8 | ||
| Sakmarian | 294.6 | 10.2 | ||
| Asselian | 299.0 | 4.4 | ||
| Carboniferous | Pennsylvanian | Gzhelian | 303.9 | 4.9 |
| 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
