Chattian


The Chattian is, in the geologic timescale, the younger of two ages or upper of two stages of the Oligocene epoch/series. It spans the time between . The Chattian is preceded by the Rupelian and is followed by the Aquitanian.

Stratigraphic definition

The Chattian was introduced by Austrian palaeontologist Theodor Fuchs in 1894. Fuchs named the stage after the Chatti, a Germanic tribe. The original type locality was near the German city of Kassel.
The base of the Chattian is at the extinction of the foram genus Chiloguembelina. An official GSSP for the Chattian stage was ratified in October of 2016.
The top of the Chattian stage is at the first appearance of foram species Paragloborotalia kugleri, the extinction of calcareous nanoplankton species Reticulofenestra bisecta, and the base of magnetic C6Cn.2n.
The Chattian is coeval with regionally used stages or zones such as the upper Avernian European mammal zone ; the upper Geringian and lower Arikareean mammal zones of North America; most of the Deseadan mammal zone of South America; the upper Hsandgolian and whole Tabenbulakian mammal zone of Asia; the upper Kiscellian and lower Egerian Paratethys stages of Central and eastern Europe; the upper Janjukian and lower Longfordian Australian regional stages; the Otaian, Waitakian, and Duntroonian stages of the New Zealand geologic time scale; and part of the Zemorrian Californian stage and Chickasawhayan regional stage of the eastern US.

Volcanic event

During the Chattian the largest known single-event volcanic eruption occurred: the Fish Canyon eruption of La Garita with a magnitude of 9.2 and VEI of 8. It has been dated to ago.

Literature