Toarcian

The Toarcian is, in the

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.^[6]

Stratigraphic definitions

The Toarcian takes its name from the city of Thouars, just south of Saumur in the Loire Valley of France. The stage was introduced by French palaeontologist Alcide d'Orbigny in 1842, after examining rock strata of this age in a quarry near Thouars.

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

The base of the Toarcian is defined as the place in the stratigraphic record where the

In the Tethys domain, the Toarcian contains the following ammonite biozones:

• zone of Pleydellia aalensis
• zone of Dumortieria pseudoradiosa
• zone of Phlyseogrammoceras dispansum
• zone of Grammoceras thouarcense
• zone of Haugia variabilis
• zone of Hildoceras bifrons
• zone of Harpoceras serpentinum
• zone of Dactylioceras tenuicostatum

References