Cisuralian
Sign in to saveThe Cisuralian, also known as the Early Permian, is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 274.4 ± 0.4 Ma.
Key facts
- Geologic timespan.name
- Cisuralian
- Geologic timespan.color
- Cisuralian
- Geologic timespan.time_start
- 298.9
- Geologic timespan.time_start_uncertainty
- 0.15
- Geologic timespan.time_end
- 274.4
- Geologic timespan.time_end_uncertainty
- 0.4
- Geologic timespan.image_map
- Mollweide Paleographic Map of Earth, 285 Ma (Artinskian Age).png
- Geologic timespan.caption_map
- A map of Earth 285 million years ago during the Cisuralian Epoch, Artinskian Age
- Geologic timespan.timeline
- Permian
- Geologic timespan.name_formality
- Formal
- Geologic timespan.synonym1
- Early/Lower Permian
- Geologic timespan.celestial_body
- earth
- Geologic timespan.usage
- Global (ICS)
- Geologic timespan.timescales_used
- ICS Time Scale
- Geologic timespan.chrono_unit
- Epoch
- Geologic timespan.strat_unit
- Series
- Geologic timespan.timespan_formality
- Formal
- Geologic timespan.lower_boundary_def
- FAD of the conodont Streptognathodus isolatus within the morphotype Streptognathodus wabaunsensis chronocline
via Wikipedia infobox
Article
8 sectionsContents
- Name and background
- Geography
- Climate
- Biodiversity
- Subdivisions
- Global
- Regional
- References
The Cisuralian, also known as the Early Permian, is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 274.4 ± 0.4 Ma.
In the regional stratigraphy of southwestern North America, the Cisuralian encompasses two series: the Wolfcampian (Asselian to mid-Artinskian) and Leonardian (mid-Artinskian to Kungurian).