Chaotian (geology)

Chaotian
4568 – 4404 Ma
Chronology
SubdivisionsSee text
Usage information
Celestial bodyEarth
Regional usageProposed subdivision of the Hadean eon
Definition
Chronological unitEra
Stratigraphic unitErathem
First proposed byC., Zahnle, K. J., Sleep, N. H., and Nisbet, E. G., 2010
Lower boundary definitionFormation of the Earth
Upper boundary definitionCollision between Proto-Earth and the Protoplanet Theia

The Chaotian is a proposed time division of the geologic time scale. First proposed in 2010[1] as an eon, it is named after Chaos, the primeval void in Greek mythology. This proposal defines the Chaotian eon as a Solar System-wide time between the initiation of planetary formation and the hypothesised collision of the trojan dwarf planet Theia with the proto-Earth.

A revised proposal in 2012[2] suggested the Chaotian as the first era of the Hadean representing the time between the formation of the Solar System c. 4.567 Ga[3] and the oldest preserved crustal material on Earth, a detrital zircon c. 4.404 Ga[4] from the Jack Hills of the Narryer Terrane in Western Australia.

As of September 2023, neither proposal had been adopted or officially ratified by the International Union of Geological Sciences.[5]

  1. ^ Goldblatt, C.; Zahnle, K.J.; Sleep, N.H.; Nisbet, E.G. (2 February 2010). "The Eons of Chaos and Hades". Solid Earth. 1 (1): 1–3. Bibcode:2010SolE....1....1G. doi:10.5194/se-1-1-2010.
  2. ^ Van Kranendonk, Martin J. (2012), "A Chronostratigraphic Division of the Precambrian", The Geologic Time Scale, Altermann, Wladyslaw; Beard, Brian L.; Hoffman, Paul F.; Johnson, Clark M.; Kasting, James F.; Melezhik, Victor A.; Nutman, Allen; Papineau, Dominic; Pirajno, Franco, Elsevier, pp. 299–392, doi:10.1016/b978-0-444-59425-9.00016-0, ISBN 978-0-444-59425-9, retrieved 2020-07-31
  3. ^ Connelly, J.N.; Bollard, J.; Bizzarro, M. (2017). "Pb–Pb chronometry and the early Solar System". Geochimica et Cosmochimica Acta. 201: 345–363. Bibcode:2017GeCoA.201..345C. doi:10.1016/j.gca.2016.10.044.
  4. ^ Wilde, Simon A.; Valley, John W.; Peck, William H.; Graham, Colin M. (11 January 2001). "Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago". Nature. 409 (6817): 175–178. Bibcode:2001Natur.409..175W. doi:10.1038/35051550. PMID 11196637. S2CID 4319774.
  5. ^ "International Commission on Stratigraphy".