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Paleoarchean

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Paleoarchean

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Also known as Paleoarchean Era, Palaeoarchaean

The Paleoarchean ( ), also spelled Palaeoarchaean (formerly known as the early Archean), is a geologic era within the Archean Eon. The name derives from Greek "Palaios" ancient. It spans the period of time . The era is defined chronometrically and is not referenced to a specific level of a rock section on Earth. The earliest confirmed evidence of life comes from this era, and Vaalbara, one of Earth's earliest supercontinents, may have formed during this era.

Key facts

Geologic timespan.color
Paleoarchean
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all time
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Vaalbara Continent.jpg
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Vaalbara, a hypothetical continent dating from 3.6 to 2.7 billion years ago
Geologic timespan.timeline
Paleoarchean
Geologic timespan.proposed_boundaries1
4031–3490 Ma
Geologic timespan.proposed_boundaries1_ref
Gradstein et al., 2012
Geologic timespan.proposed_subdivision1
Acastan Period, 4031–3810 Ma
Geologic timespan.proposed_subdivision1_coined
Gradstein et al., 2012
Geologic timespan.proposed_subdivision2
Isuan Period, 3810–3490 Ma
Geologic timespan.proposed_subdivision2_coined
Gradstein et al., 2012
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Formal
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Palaeoarchaean
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Early Archean
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earth
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Global (ICS)
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ICS Time Scale
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Era

via Wikipedia infobox

~5 min read

Encyclopedic overview

5 sections
Contents
  • Early life
  • Continental development
  • Impacts
  • References
  • External links

The Paleoarchean ( ), also spelled Palaeoarchaean (formerly known as the early Archean), is a geologic era within the Archean Eon. The name derives from Greek "Palaios" ancient. It spans the period of time . The era is defined chronometrically and is not referenced to a specific level of a rock section on Earth. The earliest confirmed evidence of life comes from this era, and Vaalbara, one of Earth's earliest supercontinents, may have formed during this era.

== Early life == thumb|left|upright 1.2| A stromatolite formed by Paleoarchean microbial mats, preserved as a [[fossil, from Pilbara craton, Western Australia.]] The geological record from the Paleoarchean era is very limited. Due to deformation and metamorphism, most rocks from the Paleoarchean era cannot provide any useful information. There are only two locations in the world containing rock formations that are intact enough to preserve evidence of early life: the Kaapvaal Craton in Southern Africa and the Pilbara Craton in Western Australia.

Excerpted from Wikipedia’s “Paleoarchean” article, available under the CC BY-SA 4.0 licence.

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