Mesoarchean Era

E234966

The Mesoarchean Era is a division of early Earth history, roughly 3.2 to 2.8 billion years ago, marked by the stabilization of continental crust and the continued evolution of early life.

All labels observed (2)

Label Occurrences
Mesoarchean Era canonical 4
Mesoarchean 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf Archean subdivision ⓘ
geologic era ⓘ
associatedWith early oxygenic photosynthesis ⓘ
low but increasing atmospheric oxygen levels locally ⓘ
atmosphericState largely oxygen-poor atmosphere ⓘ
biosignaturesInclude carbon isotope fractionation indicative of biological activity ⓘ
stromatolitic carbonates ⓘ
biosphereDominatedBy prokaryotic microorganisms ⓘ
characterizedBy anoxic atmosphere ⓘ
continued evolution of early life ⓘ
development of more stable cratons ⓘ
greenstone belt formation ⓘ
growth of continental nuclei ⓘ
high heat flow from Earth’s interior ⓘ
microbial life dominance ⓘ
photosynthetic microbial communities ⓘ
significant volcanic activity ⓘ
stabilization of continental crust ⓘ
stromatolite development ⓘ
climate faint young Sun conditions ⓘ
likely greenhouse-gas-rich atmosphere ⓘ
definedBy International Commission on Stratigraphy (conceptually, though not formally ratified as a chronostratigraphic unit) ⓘ
duration approximately 400 million years ⓘ
endTime 2.8 billion years ago ⓘ
environmentalConditions higher global heat flow than present day ⓘ
hotter mantle than present day ⓘ
lack of complex multicellular life ⓘ
followedBy Neoarchean Era ⓘ
follows Paleoarchean Era ⓘ
geologicSignificance important for formation of long-lived cratonic blocks ⓘ
major phase of continental crust stabilization ⓘ
hasRepresentativeCratons Kaapvaal Craton ⓘ
Pilbara Craton ⓘ
Superior Craton (older parts) ⓘ
linked to: Superior craton
hydrosphereState presence of liquid water oceans ⓘ
lifeEvolutionStage early diversification of microbial ecosystems ⓘ
partOf Archean Eon ⓘ
positionInArchean third era of the Archean Eon ⓘ
precededBy early Archean crustal growth phases ⓘ
rockRecordIncludes banded iron formations ⓘ
komatiitic lavas ⓘ
tonalite–trondhjemite–granodiorite suites ⓘ
startTime 3.2 billion years ago ⓘ
succeededBy further continental stabilization in the Neoarchean ⓘ
temporalRelationToEarthFormation about 1.3 to 1.7 billion years after Earth formed ⓘ
timeScaleCategory Precambrian geologic time division ⓘ
usedIn Precambrian time scale ⓘ

How these facts were elicited

Referenced by (5)

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

Precambrian Supereon → contains → Mesoarchean Era ⓘ
Archean Eon → subdividedInto → Mesoarchean Era ⓘ
Paleoarchean Era → precedes → Mesoarchean Era ⓘ
Neoarchean Era → follows → Mesoarchean Era ⓘ