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The Toarcian is, in the ICS' geologic timescale, an age and stage in the . It spans the time between 184.2 and 174.7 ±0.8 Ma.

(2025). 9780756699109, Dorling Kindersley.
It follows the and is followed by the .For a detailed geologic timescale see Gradstein et al. (2004)

The Toarcian Age began with the Toarcian Oceanic Anoxic Event, a major associated with marine extinctions and increased global temperatures that sets its fossil faunas apart from the previous age. It is believed to have ended with a global cooling event known as the Comptum Cooling Event, although whether it represented a worldwide event is controversial.


Stratigraphic definitions
The Toarcian takes its name from the city of , just south of in the of . The stage was introduced by French palaeontologist Alcide d'Orbigny in 1842, after examining of this age in a near Thouars.

In Europe this period is represented by the upper part of the .

The base of the Toarcian is defined as the place in the stratigraphic record where the first appears. A global reference profile (a ) for the base is located at Peniche, Portugal. The top of the stage is at the first appearance of ammonite genus .

In the , the Toarcian contains the following ammonite :


Sources
  • ; 2004: A Geologic Time Scale 2004, Cambridge University Press.
  • ; 1842: Paléontologie française. 1. Terrains oolitiques ou jurassiques, Bertrand, Paris.
  • Elmi, S., Rulleau, L., Gabilly, J. & Mouterde, R. 1997: Toarcien. In: Cariou, E. & Hantzpergue, P. (eds): Biostratigraphie du Jurassique ouest-européen et méditerranéen. Bulletin du Centre des Recherches, Elf Explor. Prod. Mém., 17.


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