Eoarchean

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In the geologic record the Eoarchean (/ˌ.ɑrˈkən/; also spelled Eoarchaean) Era or erathem 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 4,000 to 3,600 million years ago when atmospheric pressure values ranged from ca. 100 to 10 bar.[1][2][3]

Chronology[edit]

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.

The International Commission on Stratigraphy now officially recognizes the Eoarchean Era as the first part of the Archaean Eon, preceded by the Hadean Eon, during which the Earth is believed to be essentially molten.

The International Commission on Stratigraphy currently does not recognize the lower boundary of the era which has been provisionally placed at 4,000 million years ago[4] nor that of the preceding Hadean Eon.

The Eoarchean was followed by the Paleoarchean Era.

The name comes from two Greek words: eos (dawn) and archaios (ancient). The first supercontinent Vaalbara appeared around the end of this period around 3,600 million years ago.

Geology[edit]

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 4,280 million years ago.[5] These formations are presently under intense investigation.[6]

References[edit]

  1. ^ 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. 
  2. ^ 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 109 (14): E821–30. Bibcode:2012PNAS..109E.821M. doi:10.1073/pnas.1117774109. PMC 3325685. PMID 22331915. 
  3. ^ 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. 
  4. ^ Recent ICS provisional chart
  5. ^ O'Neil, J.; Carlson, R. W.; Francis; D.; Stevenson, R. K. (2008). "Neodymium-142 Evidence for Hadean Mafic Crust". Science 321: 1828–1831. Bibcode:2008Sci...321.1828O. doi:10.1126/science.1161925. PMID 18818357. 
  6. ^ 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[edit]

External links[edit]

Archean Eon
Eoarchean Paleoarchean Mesoarchean Neoarchean