Ladinian
The Ladinian is coeval with the Falangian regional stage used in China.
Stratigraphic definitions
The Ladinian was established by Austrian geologist Alexander Bittner in 1892. Its name comes from the Ladin people that live in the Italian Alps (in the Dolomites, then part of Austria-Hungary).
The base of the Ladinian Stage is defined as the place in the stratigraphic record where the ammonite species Eoprotrachyceras curionii first appears or the first appearance of the conodont Budurovignathus praehungaricus. The global reference profile for the base (the GSSP) is at an outcrop in the river bed of the Caffaro river at Bagolino, in the province of Brescia, northern Italy. The top of the Ladinian (the base of the Carnian) is at the first appearance of ammonite species Daxatina canadensis.
The Ladinian is sometimes subdivided into two subages or substages, the Fassanian (early or lower) and the Longobardian (late or upper). The Ladinian contains four ammonite biozones, which are evenly distributed among the two substages:
- zone of Frechites regoledanus
- zone of Protrachyceras archelaus
- zone of Protrachyceras gredleri
- zone of Eoprotrachyceras curionii
Ladinian life
Notable formations
- Upper Besano Formation (Switzerland and Italy)
- Bukobay Svita* (Russia)
- Erfurt Formation / Lower Keuper (Germany)
- Jilh Formation (Saudi Arabia)
- Meride Limestone (Switzerland and Italy)
- Upper Muschelkalk (central Europe)
- Perledo-Varenna Formation (Italy)
- Prosanto Formation (Switzerland)
- Lower Santa Maria Formation* (late Ladinian - early Carnian) (Rio Grande do Sul, Brazil)
- Zhuganpo Formation / Zhuganpo Member of the Falang Formation (late Ladinian - early Carnian) (Guizhou and Yunnan, China)
* Tentatively assigned to the Ladinian; age estimated primarily via terrestrial tetrapod biostratigraphy (see Triassic land vertebrate faunachrons)