Statherian

Fourth and last period of the Paleoproterozoic Era From Wikipedia, the free encyclopedia

The Statherian ( /stəˈθɪəriən/; Ancient Greek: σταθερός, romanized: statherós, meaning "stable, firm") is the fourth and final geologic period in the Paleoproterozoic Era, lasting from 1800 to 1600 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.

Name formalityFormal
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Quick facts Chronology, Etymology ...
Statherian
1800 – 1600 Ma
Map of Earth during the Statherian, c. 1740 Ma[citation needed]
Chronology
1820 
1800 
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1700 
1680 
1660 
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Paleoproterozoic
 
 
Rafatazmia evolves, Chuanlinggou Formation preserves oldest macroscopic eukaryotes
Beginning of the Boring Billion
Events of the Statherian Period
Vertical axis scale: Millions of years ago
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitPeriod
Stratigraphic unitSystem
Time span formalityFormal
Lower boundary definitionDefined chronometrically
Lower GSSA ratified1990[1]
Upper boundary definitionDefined chronometrically
Upper GSSA ratified1990[1]
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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.[2]

Rafatazmia, controversially[3] claimed to be present in Statherian beds in India, may be the oldest known confirmably eukaryotic fossil organism.[4]

By the beginning of the Statherian, the supercontinent Columbia had assembled.[5]

Approximately 1.7 billion years ago, natural nuclear fission reactors were generating power in what is now Oklo, Gabon.[6]

See also

References

Further reading

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