Proterozoic Eon Summary
Proterozoic Eon Overview
Characteristics: Many rocks exposed; fossils uncommon; includes komatiites, greenstone belts, granite-gneiss complexes; passive continental margins; banded iron formations (BIFs).
Geologic Timeframe
Duration: Encompasses >2 billion years (42.5% of Earth's history).
Divisions: Paleoproterozoic (2.5-1.6 Ga), Mesoproterozoic (1.6-1.0 Ga), Neoproterozoic (1.0-0.541 Ga).
Laurentia's Growth
Formation: Ancient continent formed from Archean cratons.
Major Events: Several orogenies (Wopmay, Thelon), significant accretion events from 1.8 to 1.0 Ga.
Midcontinent Rift
Opening: Formed around 1.1 Ga, a failed spreading zone, active for ~20 million years.
Deposits: Sandstones and volcanics recorded in the area.
Supercontinents
Rodinia: Assembled 1.3-1.0 Ga, fragmented ~750 Ma; possible earlier supercontinent Nuna around 1.8 Ga.
Ophiolites: Indicators of oceanic-continental convergence, containing some of the oldest known sequences.
Glaciation Events
Paleoproterozoic & Neoproterozoic: Two major glacial episodes; Neoproterozoic glaciers extensive even in equatorial regions, leading to 'Snowball Earth' conditions.
Atmospheric Changes
Oxygen Levels: Increased from <1% to <10% current levels by end of Proterozoic; Great Oxidation Event occurred.
Banded Iron Formations: Mounted during periods of low atmospheric oxygen;
Formed in shallow-water environments 2.5-2.0 Ga, indicating photosynthetic activity.
Life in the Proterozoic
Fossil Record: Dominated by prokaryotic bacteria; stromatolites were common.
Eukaryote Evolution: Eukaryotes evolved through endosymbiosis; significant microfossil discoveries track early life forms.
Ediacaran Fauna: First complex multicellular life forms appeared around 575 Ma, includes diverse organisms yet to be classified.
Microfossil Discovery
Acritarchs: Acid-resistant microfossils of variable origins; first index fossils.
Early Multicellularity: Cells developed specialization; limited information on origins from fossils, insights gained from modern analogs.