Statherian
Sign in to saveAlso known as Statherian Period, Statherian System
The Statherian (; , meaning "stable, firm") is the fourth and final geologic period in the Paleoproterozoic Era, lasting from to million years ago (Ma) and spanning 200 million years. It follows the Orosirian Period and precedes the Calymmian Period, with the latter belonging to the Mesoproterozoic Era. Instead of being based on stratigraphy, these dates are defined chronometrically.
Key facts
- Geologic timespan.name
- Statherian
- Geologic timespan.color
- Statherian
- Geologic timespan.top_bar
- all time
- Geologic timespan.image_map
- 1740 Ma paleoglobe.png
- Geologic timespan.caption_map
- Map of Earth during the Statherian, c. 1740 Ma
- Geologic timespan.timeline
- Statherian
- Geologic timespan.name_formality
- Formal
- Geologic timespan.celestial_body
- earth
- Geologic timespan.usage
- Global (ICS)
- Geologic timespan.timescales_used
- ICS Time Scale
- Geologic timespan.chrono_unit
- Period
- Geologic timespan.strat_unit
- System
- Geologic timespan.timespan_formality
- Formal
- Geologic timespan.lower_boundary_def
- Defined chronometrically
- Geologic timespan.upper_boundary_def
- Defined chronometrically
via Wikipedia infobox
Wikidata facts
Show 5 more facts
- IPA transcription
- /stəˈθɪəriən/
- Commons category
- Statherian
- start time
- 1800000000
- end time
- 1600000000
- sRGB color hex triplet
- F875A7
Sources (2)
via Wikidata · CC0
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Article
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- See also
- References
- Further reading
The Statherian (; , meaning "stable, firm") is the fourth and final geologic period in the Paleoproterozoic Era, lasting from to million years ago (Ma) and spanning 200 million years. It follows the Orosirian Period and precedes the Calymmian Period, with the latter belonging to the Mesoproterozoic Era. Instead of being based on stratigraphy, these dates are defined chronometrically.
The period was characterized on most continents by either new platforms or final cratonization of fold belts. Oxygen levels were 10% to 20% of current values.