The Toarcian is, in the ICS' geologic timescale, an age and stage in the Early Jurassic. It spans the time between 184.2 Megaannum and 174.7 ±0.8 Ma. It follows the Pliensbachian and is followed by the Aalenian.For a detailed geologic timescale see Gradstein et al. (2004)
The Toarcian Age began with the Toarcian Oceanic Anoxic Event, a major anoxic event associated with marine extinctions and increased global temperatures that sets its fossil faunas apart from the previous Pliensbachian 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.
In Europe this period is represented by the upper part of the Lias Group.
The base of the Toarcian is defined as the place in the stratigraphic record where the ammonite genus Eodactylites first appears. A global reference profile (a GSSP) for the base is located at Peniche, Portugal. The top of the stage is at the first appearance of ammonite genus Leioceras.
In the Tethys Ocean, the Toarcian contains the following ammonite :
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