GSSP for Sakmarian Stage
Definition:
The base of the Sakmarian Stage is defined in Bed 26/3 at 55.4m above the base of the Usolka Section, Southern Urals, Russia. It coincides with the first occurrence of conodont Mesogondolella monstra.
Sedimentology:The GSSP level is located in an interval with continuous limestone and marl deposition 55.4m from the base of the section in Bed 26/3. Bed 26 in the Usolka Section consists of thin alternations of brownish-grey micritic limestone, marl and argillite. |
Primary Markers:
First appearance of conodont Mesogondolella monstra within the evolutionary lineage from Mesogondolella uralensis ? Mesogondolella monstra ? Mesogondolella manifesta in Bed 26/3 in the Usolka Section.Secondary Markers:
Conodonts:Sweetognathus binodosus first occurs close to the base of the Sakmarian.
Carbon 13:
A double negative shift in δ13 Ccarb is near the Asselian/Sakmarian boundary. The younger excursion nearly coincides with the first appearance of Mesogondolella monstra.
Correlation Events:
Conodont FAD Mesogondolella monstraOther Locations around the World:
Mesogondolella monstra marks the base of the Sakmarian Stage in the Raanes Formation (latest Asselian to late Sakmarian) at the East Blind Fiord section in the Sverdrup Basin, Arctic Canada.References:
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