Paleoarchean Era

E226440

The Paleoarchean Era is an early division of Earth's geologic history marked by the stabilization of the first continental crust and the emergence of some of the oldest known life forms.

All labels observed (2)

Label Occurrences
Paleoarchean Era canonical 4
Paleoarchean era 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf Archean era ⓘ
geologic era ⓘ
associatedWith early plate tectonic activity or proto-plate tectonics ⓘ
formation of early oceanic crust ⓘ
growth of early continental crust ⓘ
characterizedBy anoxic atmosphere ⓘ
development of early continental nuclei ⓘ
emergence of some of the oldest known life forms ⓘ
formation of some of the first stable cratons ⓘ
greenhouse atmosphere dominated by CO2 and other gases ⓘ
high heat flow from Earth’s interior ⓘ
intense volcanic activity ⓘ
lack of free molecular oxygen in the atmosphere ⓘ
presence of early microbial life ⓘ
rapid tectonic processes compared with later eons ⓘ
stabilization of early continental crust ⓘ
warm surface temperatures ⓘ
chronostratigraphicRank era ⓘ
contains some of the oldest known microfossils ⓘ
some of the oldest known sedimentary rocks ⓘ
some of the oldest known stromatolites ⓘ
definedBy absolute age boundaries rather than global stratotype section ⓘ
endTime 3.2 Ga ⓘ
about 3.2 billion years ago ⓘ
environmentalCondition largely ice-free oceans despite lower solar output ⓘ
reduced solar luminosity compared with present ⓘ
strong greenhouse effect compensating for faint young Sun ⓘ
follows Eoarchean Era ⓘ
geologicTimeScaleUsedBy International Commission on Stratigraphy ⓘ
hasGlobalContext Earth’s surface dominated by oceans with small protocontinents ⓘ
high meteorite impact rate relative to later eons ⓘ
importance records early evolution of Earth’s biosphere ⓘ
records early evolution of Earth’s crust ⓘ
lifeEvidenceType carbon isotopic signatures consistent with biological activity ⓘ
microbial mat structures ⓘ
stromatolitic structures ⓘ
lifeForms archaea-like organisms ⓘ
bacteria-like organisms ⓘ
prokaryotic microorganisms ⓘ
partOf Archean Eon ⓘ
positionInArchean earliest formally recognized era after the Eoarchean ⓘ
precededBy Hadean Eon in broader Earth history ⓘ
precedes Mesoarchean Era ⓘ
startTime 3.6 Ga ⓘ
about 3.6 billion years ago ⓘ
tectonicStyle frequent crustal recycling ⓘ
possibly dominated by smaller, more mobile plates ⓘ

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 → Paleoarchean Era ⓘ
Archean Eon → subdividedInto → Paleoarchean Era ⓘ
Eoarchean Era → precedes → Paleoarchean Era ⓘ
Mesoarchean Era → follows → Paleoarchean Era ⓘ
Vaalbara supercraton → locatedInPeriod → Paleoarchean era ⓘ
linked to: Paleoarchean Era