- published: 09 Jan 2010
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The Ladinian is a stage and age in the Middle Triassic series or epoch. It spans the time between ~242 Ma and ~235 Ma (million years ago). The Ladinian was preceded by the Anisian and succeeded by the Carnian (part of the Upper or Late Triassic).
The Ladinian is coeval with the Falangian Chinese regional stage.
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. 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:
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Dinosaurs evolved within a single lineage of archosaurs 232-234 Ma in the Ladinian age, the latter part of the middle Triassic. Dinosauria is a well-supported clade, present in 98% of bootstraps. It is diagnosed by many features including loss of the postfrontal on the skull and an elongate deltopectoral crest on the humerus. The process leading up to the Dinosauromorpha and the first true dinosaurs can be followed through fossils of the early Archosaurs such as the Proterosuchidae, "Erythrosuchidae" and "Euparkeria" which have fossils dating back to 250 Ma, through mid-Triassic archosaurs such as "Ticinosuchus" 232-236 Ma. Crocodiles are also descendants of mid-Triassic archosaurs. Dinosaurs can be defined as the last common ancestor of birds and "Triceratops" and all the desc...
""Cyamodus"" is a genus of placodonts discovered from fossil remains in Germany in the early-to-mid-19th century and was named by Christian Erich Hermann von Meyer in 1863. The fossils have been dated to the Triassic Period, from the Anisian to Ladinian stages. Considered a possible turtle ancestor due to its wide flattened torso covered in dermal ossicles, but now is considered to only be closely related. Derived from a sister to "Paraplacodus", "Cyamodus" phylogenetically preceded "Placochelys". Meyer created the genus name "Cyamodus" for the "Schnabelplacodus" "Cyamodus rostratus" holotype skull material from Bindlach, which is today preserved and displayed in the Urwelt-Museum Oberfranken, Bayreuth. "Cyamodus" is the type genus of the monotypic family "Cyamodontidae". ...
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