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Statherian

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Also 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
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via Wikidata · CC0

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Article

3 sections
Contents
  • 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.

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