Back Maastricht (tydperk) Afrikaans الماسترخي Arabic Maastrichianu AST Maastrichtià Catalan Maastrichtium German Mastriĥta Esperanto Maastrichtiense Spanish Maastrichtiar Basque ماستریختین Persian Maastricht-vaihe Finnish
| Maastrichtian | |||||||||
|---|---|---|---|---|---|---|---|---|---|
 Opening of the western Indian Ocean in the Maastrichtian | |||||||||
| Chronology | |||||||||
| |||||||||
| Etymology | |||||||||
| Name formality | Formal | ||||||||
| Usage information | |||||||||
| Celestial body | Earth | ||||||||
| Regional usage | Global (ICS) | ||||||||
| Time scale(s) used | ICS Time Scale | ||||||||
| Definition | |||||||||
| Chronological unit | Age | ||||||||
| Stratigraphic unit | Stage | ||||||||
| Time span formality | Formal | ||||||||
| Lower boundary definition | Mean of 12 biostratigraphic criteria | ||||||||
| Lower boundary GSSP | Grande Carrière quarry, Landes, France 43°40′46″N 1°06′48″W / 43.6795°N 1.1133°W | ||||||||
| Lower GSSP ratified | February 2001[2] | ||||||||
| Upper boundary definition | Iridium enriched layer associated with a major meteorite impact and subsequent K-Pg extinction event. | ||||||||
| Upper boundary GSSP | El Kef Section, El Kef, Tunisia 36°09′13″N 8°38′55″E / 36.1537°N 8.6486°E | ||||||||
| Upper GSSP ratified | 1991 | ||||||||
The Maastrichtian ( /mɑːˈstrɪktiən/ mah-STRICK-tee-ən) is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from 72.1 to 66 million years ago. The Maastrichtian was preceded by the Campanian and succeeded by the Danian (part of the Paleogene and Paleocene).[3]
The Cretaceous–Paleogene extinction event (formerly known as the Cretaceous–Tertiary extinction event)[a] occurred at the end of this age.[3] In this mass extinction, many commonly recognized groups such as non-avian dinosaurs, plesiosaurs and mosasaurs, as well as many other lesser-known groups, died out. The cause of the extinction is most commonly linked to an asteroid about 10 to 15 kilometres (6.2 to 9.3 mi) wide[4][5] colliding with Earth, ending the Cretaceous.
- ^ International Commission on Stratigraphy. "ICS - Chart/Time Scale". www.stratigraphy.org.
- ^ Odin, Gilles S.; Michèle A. Lamaurelle (2001). "The global Campanian-Maastrichtian stage boundary". Episodes. 24 (4): 229–238. doi:10.18814/epiiugs/2001/v24i4/002.
- ^ a b Ogg, James G.; Gradstein, Felix M.; Smith, A.G. (2004). A geologic time scale 2004. Cambridge, UK: Cambridge University Press. ISBN 0-521-78142-6. Retrieved 8 May 2022.
- ^ Sleep, Norman H.; Lowe, Donald R. (9 April 2014). "Scientists reconstruct ancient impact that dwarfs dinosaur-extinction blast". American Geophysical Union. Retrieved 15 March 2018.
- ^ Amos, Jonathan (15 May 2017). "Dinosaur asteroid hit 'worst possible place'". BBC News Online. Retrieved 16 March 2018.
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