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.

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All labels observed (1)

Label Occurrences
Paleoarchean Era canonical 4

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

Referenced by (4)

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