The Ladinian is a stage and age in the Middle Triassic series or epoch. It spans the time between annum and ~237 Ma (million years ago). The Ladinian was preceded by the Anisian and succeeded by the Carnian (part of the Late Triassic).For a detailed geologic timescale see Gradstein et al. (2004)
The Ladinian is coeval with the Falangian regional stage used in China.
The base of the Ladinian Stage is defined as the place in the stratigraphic record where the ammonite species Eoprotrachyceras 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 GSSP was established by Brack et al. (2005) The top of the Ladinian (the base of the Carnian) is at the first appearance of ammonite species Daxatina.
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:
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