Paleoproterozoic Era

E44484

The Paleoproterozoic Era was an early division of Earth's history marked by the stabilization of continental cratons, widespread banded iron formations, and the Great Oxidation Event that significantly increased atmospheric oxygen.

Try in SPARQL Jump to: Surface forms Statements Referenced by

All labels observed (5)

Label Occurrences
Paleoproterozoic Era canonical 12
Paleoproterozoic 4
Paleoproterozoic Eon 2

Statements (50)

Predicate Object
instanceOf geologic era
subdivision of the Proterozoic Eon
associatedWithLife cyanobacterial mats
early eukaryote fossils (possible)
prokaryotic life
stromatolite abundance
containsEvent Great Oxidation Event
Huronian glaciation
Lomagundi–Jatuli carbon isotope excursion
major orogenic events on several cratons
containsSubdivision Orosirian Period
Rhyacian Period
Siderian Period
Statherian Period
duration about 900 million years
endTime approximately 1.6 billion years ago
fieldOfStudy geology
paleobiology
paleoclimatology
follows Archean Eon
hasConsequence change in ocean chemistry
cooling of global climate
drawdown of atmospheric methane
possible trigger of Paleoproterozoic glaciations
widespread oxidation of iron in oceans
hasFeature abundant banded iron formations in marine sediments
decline of banded iron formations toward its end
formation of red beds
oxidation of surface environments
rise of atmospheric oxygen above trace levels
sulfur mass-independent fractionation decline
hasGeologicalRecord extensive metamorphic belts
large igneous provinces
rocks preserved on multiple cratons worldwide
hasImpact establishment of modern-style biosphere–geosphere interactions
long-term habitability of Earth
hasKeyFeature first long-lived continental cratons
hasKeyProcess biological production of oxygen by cyanobacteria
development of plate tectonic style similar to modern
global-scale orogeny
growth of continental crust
intense weathering of continental surfaces
large-scale glaciations
oxygenation of Earth’s atmosphere
stabilization of continental cratons
widespread formation of banded iron formations
namedAfter Greek words for "ancient" and "earlier life"
partOf Proterozoic Eon
precedes Mesoproterozoic Era
startTime approximately 2.5 billion years ago

Referenced by (21)

Full triples — surface form annotated when it differs from this entity's canonical label.

Proterozoic Eon subdivision Paleoproterozoic Era
Vredefort Dome geologicalPeriod Paleoproterozoic Era
this entity surface form: Paleoproterozoic
Precambrian Supereon contains Paleoproterozoic Era
supercontinent Columbia (Nuna) formedIn Paleoproterozoic Era
subject surface form: Columbia
this entity surface form: Paleoproterozoic eon
supercontinent Columbia (Nuna) formedIn Paleoproterozoic Era
subject surface form: Nuna
this entity surface form: Paleoproterozoic eon
Mesoproterozoic Era follows Paleoproterozoic Era
Great Oxidation Event partOf Paleoproterozoic Era
this entity surface form: Paleoproterozoic era
Great Oxidation Event timePeriod Paleoproterozoic Era
this entity surface form: Paleoproterozoic
Statherian Period partOf Paleoproterozoic Era
Statherian Period geologicEra Paleoproterozoic Era
Siderian Period partOf Paleoproterozoic Era
Siderian Period era Paleoproterozoic Era
Rhyacian Period partOf Paleoproterozoic Era
Rhyacian Period era Paleoproterozoic Era
Orosirian Period partOf Paleoproterozoic Era
Huronian glaciation geologicalEon Paleoproterozoic Era
this entity surface form: Paleoproterozoic Eon
Huronian glaciation geologicalEra Paleoproterozoic Era
Lomagundi–Jatuli carbon isotope excursion geologicalAge Paleoproterozoic Era
this entity surface form: Paleoproterozoic Eon
Mesabi Range geologicAge Paleoproterozoic Era
this entity surface form: Paleoproterozoic
Neoarchean Era precedes Paleoproterozoic Era
East European Craton hasGeologicalAge Paleoproterozoic Era
this entity surface form: Paleoproterozoic