| Sakmarian | |
| Color: | Sakmarian |
| Time Start: | 293.52 |
| Time Start Uncertainty: | 0.17 |
| Time End: | 290.1 |
| Time End Uncertainty: | 0.26 |
| Timeline: | Permian |
| Name Formality: | Formal |
| Celestial Body: | earth |
| Usage: | Global (ICS) |
| Timescales Used: | ICS Time Scale |
| Chrono Unit: | Age |
| Strat Unit: | Stage |
| Timespan Formality: | Formal |
| Lower Boundary Def: | FAD of the Conodont Mesogondolella monstra |
| Lower Gssp Location: | Usolka section, Southern Ural Mountains, Russia |
| Lower Gssp Accept Date: | 2018[1] |
| Upper Boundary Def: | FAD of the Conodont Sweetognathus whitei |
| Upper Gssp Location: | Dalny Tulkas section, Southern Ural Mountains, Russia |
| Upper Gssp Accept Date: | February 2022[2] |
In the geologic timescale, the Sakmarian is an age or stage of the Permian period. It is a subdivision of the Cisuralian Epoch or Series. The Sakmarian lasted between 293.52 and million years ago (Ma). It was preceded by the Asselian and followed by the Artinskian.[3]
The Sakmarian Stage is named after the Sakmara River in the Ural Mountains, a tributary to the Ural River. The stage was introduced into scientific literature by Alexander Karpinsky in 1874. In Russian stratigraphy, it originally formed a substage of the Artinskian Stage. Currently, the ICS (International Commission on Stratigraphy) uses it as an independent stage in its international geologic timescale.
The base of the Sakmarian Stage is defined by the first appearance of conodont species Streptognathodus postfusus in the fossil record. A global reference profile for the stage's base (a GSSP), located in the southern Ural Mountains, Russia, was ratified in 2018. The top of the Sakmarian (the base of the Artinskian) is defined as the level in the stratigraphic record where fossils of conodont species Sweetognathus whitei and Mesogondolella bisselli first appear.