Ladinian
ColorLadinian
Time start241.464
Time start uncertainty0.28
Time end237
Time end prefix~
Caption outcropMonte San Giorgio exhibits exceptionally preserved Ladinian vertebrate fossils
TimelineTriassic
Name formalityFormal
Celestial bodyearth
UsageGlobal (ICS)
Timescales usedICS Time Scale
Chrono unitAge
Strat unitStage
Timespan formalityFormal
Lower boundary defFAD of the Ammonite Eoprotrachyceras curionii
Lower gssp locationBagolino, Lombardian pre-Alps, Italy
Lower gssp coords45.8193°N 10.4710°E
Lower gssp accept date2005[1]
Upper boundary defFAD of the Ammonite Daxatina canadensis
Upper gssp locationPrati di Stuores, Dolomites, Italy
Upper gssp coords46.5269°N 11.9303°E
Upper gssp accept date2008[2]

The Ladinian is a stage and age in the Middle Triassic series or epoch. It spans the time between Ma and ~237 Ma (million years ago).[3] The Ladinian was preceded by the Anisian and succeeded by the Carnian (part of the Upper or Late Triassic).[4]

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.[5] 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:

Ladinian life

Notable formations

References

Notes

  1. ^ Brack, Peter; Rieber, Hans; Nicora, Alda; Mundil, Roland (December 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): 233–244. doi:10.18814/epiiugs/2005/v28i4/001. Retrieved 23 December 2020.
  2. ^ Mietto, Paolo; Manfrin, Stefano; Preto, Nereo; Rigo, Manuel; Roghi, Guido; Furin, Stefano; Gianolla, Piero; Posenato, Renato; Muttoni, Giovanni; Nicora, Alda; Buratti, Nicoletta; Cirilli, Simonetta; Spötl, Christoph; Ramezani, Jahandar; Bowring, Samuel (September 2012). "The Global Boundary Stratotype Section and Point (GSSP) of the Carnian Stage (Late Triassic) at Prati Di Stuores/Stuores Wiesen Section (Southern Alps, NE Italy)". Episodes. 35 (3): 414–430. doi:10.18814/epiiugs/2012/v35i3/003. Retrieved 13 December 2020.
  3. ^ "ICS - Chart/Time Scale". Archived 2025-01-01 at the Wayback Machine. Retrieved 2025-01-14.
  4. ^ For a detailed geologic timescale see Gradstein et al. (2004)
  5. ^ The GSSP was established by Brack et al. (2005)

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.