In the geologic record the Eoarchean Era or erathem pron.: // (also spelled Eoarchaean) is the earliest time following the solidification of Earth's crust. It follows the Hadean and precedes the Paleoarchean Era of the geologic timescale. The approximate abiotic origins of life (abiogenesis) have been dated to a time window from when atmospheric pressure values ranged from ca. 100 to 10 bar.
It was formerly officially unnamed and usually referred to as the first part of the Early Archean (now an obsolete name) together with the later Paleoarchean Era. It is the first part of the Archaean Eon, preceded by the Hadean Eon, during which the Earth was considered to be essentially molten.
The Eoarchean was followed by the Paleoarchean Era.
A characteristic of the Eoarchean is that Earth possessed a firm crust for the first time. However, this crust may have been incomplete at many sites and areas of lava may have existed at the surface. The beginning of the Eoarchean is characterized by heavy asteroid bombardment within the inner solar system: the Late Heavy Bombardment. The Eoarchean is the first phase of our planet from which solid rock formations survived. The largest is the Isua greenstone belt at the south-west coast of Greenland. It appeared during the Eoarchean around 3.8 billion years ago. The Acasta Gneiss within the Canadian Shield have been dated to be 4,030 Ma and are therefore the oldest preserved rock formations. In 2008 another rock formation was discovered in the Nuvvuagittuq greenstone belt in northern Québec in Canada which has been dated to be . These formations are presently under intense investigation.
Today it seems well supported that the first oceans existed during the Eoarchean.
- Mulkidjanian, A. Y. (2009). "On the origin of life in the zinc world: 1. Photosynthesizing, porous edifices built of hydrothermally precipitated zinc sulfide as cradles of life on Earth.". Biol. Direct 4: 26.
- Mulkidjanian, A. Y.; Bychkov, A. Y.; Dibrova, D. V.; Galperin, M. Y.; Koonin, E. V. (2012). "Origin of first cells at terrestrial, anoxic geothermal fields". Proc. Natl. Acad. Sci. USA. Bibcode:2012PNAS..109E.821M. doi:10.1073/pnas.1117774109.
- Mulkidjanian, A. Y. (2011). "Energetics of the First Life". In R. Egel, D.-H. Lankenau, and A. Y. Mulkidjanian (ed.), Origins of Life: The Primal Self-Organization. Springer Verlag, Heidelberg.(book): 3–33.
- Recent ICS provisional chart
- O'Neil, J.; Carlson, R. W.; Francis; D.; Stevenson, R. K. "Neodymium-142 Evidence for Hadean Mafic Crust". Science 321: 1828–1831. Bibcode:2008Sci...321.1828O. doi:10.1126/science.1161925. PMID 18818357. Text "2008 " ignored (help)
- Jean David, Laurent Godin, Ross Stevenson, Jonathan O'Neil and Don Francis: U-Pb ages (3.8–2.7 Ga) and Nd isotope data from the newly identified Eoarchean Nuvvuagittuq supracrustal belt, Superior Craton, Canada. GSA Bulletin, Bd. 121; No. 1-2; pp. 150-163; January 2009, doi:10.1130/B26369.1
Further reading 
- Egel, R.; Lankenau, D.-H.; Mulkidjanian, A. Y. (2011). Origins of Life: The Primal Self-Organization. Berlin Heidelberg: Springer-Verlag. pp. 1–366,. doi:10.1007/978-3-642-21625-1. ISBN 978-3-642-21624-4. Unknown parameter
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