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The Ladinian is a stage and age in the series or epoch. It spans the time between and ~237 Ma (million years ago). The Ladinian was preceded by the and succeeded by the (part of the ).For a detailed geologic timescale see Gradstein et al. (2004)

The Ladinian is coeval with the regional stage used in .


Stratigraphic definitions
The Ladinian was established by Austrian geologist Alexander Bittner in 1892. Its name comes from the that live in the (in the , then part of ).

The base of the Ladinian Stage is defined as the place in the stratigraphic record where the species first appears or the first appearance of the conodont Budurovignathus praehungaricus. The global reference profile for the base (the ) is at an in the of the Caffaro river at , in the province of Brescia, northern .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 .

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:


Ladinian life

Notable formations


Notes

Literature
  • ; 2005: The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale, Episodes 28(4), pp. 233–244.
  • ; 2004: A Geologic Time Scale 2004, Cambridge University Press.


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