Late Triassic

E196698

The Late Triassic was a geologic period and epoch, roughly 237–201 million years ago, marked by the diversification of early dinosaurs and the end-Triassic mass extinction that paved the way for Jurassic ecosystems.

All labels observed (2)

Label Occurrences
Late Triassic canonical 6
Late Triassic Epoch 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf epoch
geologic period
chronostratigraphicUnit Upper Triassic Series
climate generally warm
seasonally arid in many regions
contains Carnian
Norian
Rhaetian
dominantTerrestrialVertebrates early dinosaurs
non-dinosaurian archosaurs
therapsids in some regions
endBoundary Rhaetian age
endTime approximately 201 million years ago
flora conifers
ginkgophytes
seed ferns
followedBy Hettangian stage
surface form: Hettangian
follows Middle Triassic
geochronologicUnit Late Triassic self-linksurface differs
surface form: Late Triassic Epoch
majorEvent diversification of early dinosaurs
diversification of marine reptiles
end-Triassic mass extinction
evolution of first true crocodile-line archosaurs
origin and diversification of pterosaurs
radiation of early mammals
marineLife ammonoids
bivalves
conodonts
ichthyosaurs
plesiosaurs (late in the interval)
massExtinction end-Triassic extinction event
massExtinctionConsequence ecological expansion of dinosaurs in the Jurassic
massExtinctionImpact decline of many archosaur groups
severe losses in marine faunas
massExtinctionSeverity one of the five largest Phanerozoic mass extinctions
massExtinctionTiming at or near the Triassic–Jurassic boundary
ocean Panthalassa Ocean dominant
Tethys Ocean
surface form: Tethys Ocean extensive in low latitudes
paleogeography supercontinent Pangaea largely intact
partOf Mesozoic Era
Triassic
precededBy Anisian
Ladinian
precedes Early Jurassic
startBoundary Carnian age
startTime approximately 237 million years ago
stratigraphicBoundaryDefinition Global Boundary Stratotype Section and Point
surface form: Global Boundary Stratotype Section and Point (GSSP) used for stage limits
timeScale Mesozoic Era
usedIn International Chronostratigraphic Chart

How these facts were elicited

Referenced by (7)

Full triples — surface form annotated when it differs from this entity's canonical label.

Early Jurassic follows Late Triassic
Triassic subdividedInto Late Triassic
Watchung Mountains geologicalPeriod Late Triassic
Palisades hasGeologicalAge Late Triassic
Late Triassic geochronologicUnit Late Triassic self-linksurface differs
this entity surface form: Late Triassic Epoch
Jasper Forest geologicalAge Late Triassic
Coelophysis geologicalPeriod Late Triassic