Paleoarchean Eon
3600–3200 million years ago
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Millions of years
A stromatolite formed by Paleoarchean miocrobial mats, preserved as a fossil, from Pilbara craton, Western Australia

The Paleoarchean (pronunciation: /ˌplɪ..ɑːrˈkən/; also spelled Palaeoarchaean (formerly known as early Archean)) is a geologic era within the Archaean Eon. It spans the period of time 3,600 to 3,200 million years agothe era is defined chronometrically and not is referenced to a specific level in a rock section on Earth. The name derives from Greek "Palaios" ancient. The oldest ascertained life form of fossilized bacteria in microbial mats, 3,480 million years old, found in Western Australia, is from this era.[1][2] The first supercontinent Vaalbara formed during this period.

During this era, a large asteroid, about 37 to 58 kilometres (23–36 mi) wide, collided with the Earth in the area of South Africa about 3.26 billion years ago, creating the features known as the Barberton greenstone belt.[3]


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