Neoarchean Era

E252555

The Neoarchean Era was the final phase of the Archean Eon, marked by significant continental growth, stabilization of cratons, and the emergence of early oxygen-producing photosynthetic life.

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All labels observed (1)

Label Occurrences
Neoarchean Era canonical 3

Statements (47)

Predicate Object
instanceOf geological era
subdivision of the Archean Eon
associatedWith banded iron formation deposition
development of early sedimentary basins
early oxygenation of surface environments
early plate tectonic-style processes
emergence of shallow marine platforms
evolution of cyanobacteria-like organisms
formation of proto-continents
komatiitic volcanism
microbial mat ecosystems
stabilization of Archean cratons
stromatolite development
characterizedBy development of large stable continental blocks
emergence of oxygen-producing photosynthetic life
granite–greenstone terranes
growth of continental lithosphere
high heat flow from Earth’s interior
intense volcanic activity
major crustal differentiation
significant continental growth
stabilization of cratons
widespread greenstone belts
definedBy International Commission on Stratigraphy
duration approximately 300 million years
endMarkedBy increasing atmospheric oxygen trends
transition to Paleoproterozoic tectonic regimes
endTime 2500 million years ago
follows Mesoarchean Era
geologicTimeScaleRank era
hasGlobalExtent Earth
importantFor reconstruction of early atmosphere composition
study of early biosphere development
study of early continental evolution
understanding early Earth tectonics
isFinalEraOf Archean Eon
leadsTo conditions for the Great Oxidation Event
overlapsWith late Archean crust-forming events
partOf Archean Eon
precededBy low atmospheric oxygen levels
precedes Paleoproterozoic Era
startTime 2800 million years ago
timeScaleType Precambrian Supereon
surface form: Precambrian
typicalRockRecordIncludes chemical sedimentary rocks such as banded iron formations
granitoid plutons
metamorphosed volcanic sequences
usedIn international geologic time scale

Referenced by (3)

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

Archean Eon subdividedInto Neoarchean Era
Mesoarchean Era followedBy Neoarchean Era
Siderian Period follows Neoarchean Era