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FIRST PERIOD OF THE MESOZOIC ERA 252–201 MILLION YEARS AGO
Triassic Period; Triassic System; Triassic Era; Triassic period; Triassic era; Triassic (geology); Trias era; The Triassic Era; Climate of the Triassic
  • isbn=978-0-7240-1250-3}}</ref>
  • View of the Tethys area during the Ladinian stage (230&nbsp;Ma)
  • The mass extinction event is marked by 'End Tr'
  • Reconstruction of the Triassic amphibian [[Mastodonsaurus]]
  • Triassic flora as depicted in ''[[Meyers Konversations-Lexikon]]'' (1885–90)
  • 230&nbsp;Ma continental reconstruction
  • Skull of a Triassic Period phytosaur found in the Petrified Forest National Park
  •  pages = 155–80 [173–74] }}</ref> largely displaced by an [[Australia]]-wide coniferous flora.
  • Middle Triassic marginal marine sequence, southwestern [[Utah]]
  • Marine vertebrate apex predators of the [[Early Triassic]] and [[Anisian]] (Middle Triassic)<ref>Scheyer et al. (2014): Early Triassic Marine Biotic Recovery: The Predators' Perspective. PLoS ONE  https://doi.org/10.1371/journal.pone.0088987</ref>

Triassic         
·noun The Triassic formation.
II. Triassic ·adj Of the age of, or pertaining to, the Trias.
Triassic         
[tr??'as?k]
¦ adjective Geology relating to or denoting the earliest period of the Mesozoic era (between the Permian and Jurassic periods, about 245 to 208 million years ago), a time when the first dinosaurs, ammonites, and primitive mammals appeared.
Origin
C19: from late L. trias (see triad), because the strata are divisible into three groups, + -ic.
Triassic–Jurassic extinction event         
  • CAMP]] volcanism at the Triassic-Jurassic boundary
  • Reptile extinction at the end of the Triassic is poorly understood, but  [[phytosaur]]s (such as this ''[[Redondasaurus]]'') went from abundant to extinct by the end of the Rhaetian.
  • Conodonts were a major vertebrate group which died out at the end of the Triassic
  • Manicouagan reservoir]] in [[Quebec]], a massive crater formed by a Late Triassic impact. Radiometric dating has determined that it is about 13 million years older than the Triassic–Jurassic boundary, and thus an unlikely candidate for a mass extinction.
  • Capitosaurs]] (such as this ''[[Mastodonsaurus]]'') were among the major amphibian groups which became extinct at the T-J boundary, though many may have died out earlier.
MASS EXTINCTION
Triassic-Jurassic event; Triassic-Jurassic extinction events; Triassic-Jurassic extinction event; Fourth extinction; Triassic Extinction; Triassic extinction; End-Triassic extinction; Jurassic extinction event; End-Triassic extinction event; End–Triassic extinction event; Tr/J extinction event; Triassic-Jurassic mass extinction; Triassic–Jurassic mass extinction; Fourth mass extinction; End-Triassic mass extinction
The Triassic–Jurassic (Tr-J) extinction event, often called the end-Triassic extinction, marks the boundary between the Triassic and Jurassic periods, ,Some sources (Whiteside et al 2010) give a date 181.8268 Ma.

ويكيبيديا

Triassic

The Triassic ( try-ASS-ik) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic.

The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archosaurs, called dinosaurs, first appeared in the Late Triassic but did not become dominant until the succeeding Jurassic Period. Archosaurs that became dominant in this period were primarily pseudosuchians, ancestors of modern crocodilians, while some archosaurs specialized in flight, the first time among vertebrates, becoming the pterosaurs.

Therapsids, the dominant vertebrates of the preceding Permian period, declined throughout the period. The first true mammals, themselves a specialized subgroup of therapsids, also evolved during this period. The vast supercontinent of Pangaea existed until the mid-Triassic, after which it began to gradually rift into two separate landmasses, Laurasia to the north and Gondwana to the south.

The global climate during the Triassic was mostly hot and dry, with deserts spanning much of Pangaea's interior. However, the climate shifted and became more humid as Pangaea began to drift apart. The end of the period was marked by yet another major mass extinction, the Triassic–Jurassic extinction event, that wiped out many groups, including most pseudosuchians, and allowed dinosaurs to assume dominance in the Jurassic.