Chaotian (geology)
Topic: Earth
From HandWiki - Reading time: 3 min
| Chaotian | |
|---|---|
| 4568 – 4404 Ma | |
| Chronology | |
| Subdivisions | See text |
| Usage information | |
| Celestial body | Earth |
| Regional usage | Proposed subdivision of the Hadean eon |
| Definition | |
| Chronological unit | Era |
| Stratigraphic unit | Erathem |
| First proposed by | C., Zahnle, K. J., Sleep, N. H., and Nisbet, E. G., 2010 |
| Lower boundary definition | Formation of the Earth |
| Upper boundary definition | Collision 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]
Subdivisions
The original proposal in 2010 divided the Chaotian into two eras and four periods. No numerical upper age limits were provided, only the younger age limit of ~4.5 Ga for the boundary between the proposed Chaotian and Hadean boundary.
The revised proposal in 2012 did not subdivide the proposed Chaotian era (of the Hadean eon) into periods.
| Eon | Era | Period | Age (Ga) |
|---|---|---|---|
| Chaotian | Neochaotian | Titanomachaen | > ~4.5 |
| Hyperitian | |||
| Eochaotian | Erebrean | ||
| Nephelean |
| Eon | Era | Age (Ga) |
|---|---|---|
| Hadean | Jack Hillsian or Zirconian | 4.404 to 4.030 |
| Chaotian | 4.568 to 4.404 |
See also
References
- ↑ 1.0 1.1 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. doi:10.5194/se-1-1-2010. Bibcode: 2010SolE....1....1G. https://www.solid-earth.net/1/1/2010/se-1-1-2010.html.
- ↑ 2.0 2.1 Van Kranendonk, Martin J. (2012), Altermann, Wladyslaw; Beard, Brian L.; Hoffman, Paul F.; Johnson, Clark M.; Kasting, James F.; Melezhik, Victor A.; Nutman, Allen; Papineau, Dominic; Pirajno, Franco, "A Chronostratigraphic Division of the Precambrian" (in en), The Geologic Time Scale (Elsevier): pp. 299–392, doi:10.1016/b978-0-444-59425-9.00016-0, ISBN 978-0-444-59425-9, https://linkinghub.elsevier.com/retrieve/pii/B9780444594259000160, retrieved 2020-07-31
- ↑ Connelly, J.N.; Bollard, J.; Bizzarro, M. (2017). "Pb–Pb chronometry and the early Solar System" (in en). Geochimica et Cosmochimica Acta 201: 345–363. doi:10.1016/j.gca.2016.10.044.
- ↑ 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. doi:10.1038/35051550. PMID 11196637. Bibcode: 2001Natur.409..175W.
- ↑ https://stratigraphy.org/chart
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