The Artinskian is named after the small Russian city of Arti (formerly Artinsk), situated in the southern Ural mountains, about 200 km southwest of Yekaterinburg. The stage was introduced into scientific literature by Alexander Karpinsky in 1874.[2]
U-Pb radiometric dating found that the base of the Artinskian was approximately 290.1 million years old (Ma), based on the position of the rock layer at the Dal'ny Tulkas roadcut containing the FAD of S. whitei relative to three precisely dated ash beds surrounding it.[3] Earlier radiometric reported a much younger age of 280.3 Ma for the Sakmarian-Artinskian boundary.
Top of the Artinskian
The top of the Artinskian (and the base of the Kungurian) is defined as the place in the stratigraphic record where fossils of conodonts Neostreptognathodus pnevi and Neostreptognathodus exculptus first appear.[2]
New Mexico; Utah-Arizona border region, both in USA; possibly England
The English specimen known as S?. brittanicus) is now generally classified as Sphenacodontidaeincertae sedis, separate from the other Sphenacodon species so may need reassigning.