File:Mollweide_Paleographic_Map_of_Earth,_225_Ma_(Norian_Age).png · Wikimedia Commons · See Wikimedia Commons
Triassic
Sign in to saveAlso known as Triassic Period, Triassic System
The Triassic (; sometimes symbolized as 🝈) is a geologic period and a stratigraphic system that spans 50.5 million years from the end of the Permian Period 251.902 Ma (million years ago) to the beginning of the Jurassic Period 201.4 Ma. The Triassic Period is the first and shortest geologic period of the Mesozoic Era, and the seventh period of the Phanerozoic Eon. The start and the end of the Triassic Period featured major extinction events.
The Triassic is a geologic period that lasted about 50.5 million years, starting 251.902 million years ago after the Permian Period ended and ending 201.4 million years ago when the Jurassic Period began. It matters because it was the first and shortest period of the Mesozoic Era, and both its beginning and end were marked by major extinction events that reshaped life on Earth.
AI-generated from the Wikipedia summary — may contain errors.
Key facts
- Geologic timespan.color
- Triassic
- Geologic timespan.time_start
- 251.902
- Geologic timespan.time_start_uncertainty
- 0.024
- Geologic timespan.time_end
- 201.4
- Geologic timespan.time_end_uncertainty
- 0.2
- Geologic timespan.image_map
- Mollweide Paleographic Map of Earth, 225 Ma (Norian Age).png
- Geologic timespan.caption_map
- A map of Earth as it appeared during the Norian age of the Late Triassic
- Geologic timespan.timeline
- Triassic
- Geologic timespan.name_formality
- Formal
- Geologic timespan.celestial_body
- earth
- Geologic timespan.usage
- Global (ICS)
- Geologic timespan.timescales_used
- ICS Time Scale
- Geologic timespan.chrono_unit
- Period
- Geologic timespan.strat_unit
- System
- Geologic timespan.timespan_formality
- Formal
- Geologic timespan.lower_boundary_def
- First appearance of the conodont Hindeodus parvus
- Geologic timespan.lower_gssp_location
- Meishan, Zhejiang, China
- Geologic timespan.lower_gssp_accept_date
- 2001
via Wikipedia infobox
Wikidata facts
- Image
- Trossingen formation NT.jpg
Show 5 more facts
- Commons category
- Triassic
- start time
- 251902000-
- end time
- 201400000-
- sRGB color hex triplet
- 812B92
- IPA transcription
- /traɪˈæsɪk/
via Wikidata · CC0
~41 min read
Article
33 sectionsContents
- Etymology
- Dating and subdivisions
- Paleogeography
- Northern Pangea (Laurussia)
- Southern Pangea (Gondwana)
- Closure of the Paleo-Tethys
- Opening of the Central Atlantic
- Panthalassic Ocean
- Paleooceanography
- Climate
- Early Triassic
- Middle Triassic
- Late Triassic
- Flora
- Land plants
- Coal
- Phytoplankton
- Fauna
- Marine invertebrates
- Insects
- Fish
- Amphibians
- Reptiles
- Archosauromorphs
- Marine reptiles
- Other reptiles
- Synapsids
- Lagerstätten
- Triassic–Jurassic extinction event
- See also
- Notes
- References
- External links
The Triassic (; sometimes symbolized as 🝈) is a geologic period and a stratigraphic system that spans 50.5 million years from the end of the Permian Period 251.902 Ma (million years ago) to the beginning of the Jurassic Period 201.4 Ma. The Triassic Period is the first and shortest geologic period of the Mesozoic Era, and the seventh period of the Phanerozoic Eon. The start and the end of the Triassic Period featured major extinction events.
Chronologically, the Triassic Period is divided into three epochs: (i) the Early Triassic, (ii) the Middle Triassic, and (iii) the Late Triassic. The Triassic Period began after the Permian–Triassic extinction event that much reduced the biosphere of planet Earth. The fossil record of the Triassic Period presents three categories of organisms: (i) animals that survived the Permian–Triassic extinction event, (ii) new animals that briefly flourished in the Triassic biosphere, and (iii) new animals that evolved and dominated the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized group 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, relatives and 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, saw a brief surge in diversification in the Triassic, with dicynodonts and cynodonts quickly becoming dominant, but they declined throughout the period with the majority becoming extinct by the end. However, the first stem-group mammals (mammaliamorphs), themselves a specialized subgroup of cynodonts, appeared during the Triassic and would survive the extinction event, allowing them to radiate during the Jurassic. Amphibians were primarily represented by the temnospondyls, giant aquatic predators that had survived the end-Permian extinction and saw a new burst of diversification in the Triassic, before going extinct by the end; however, early crown-group lissamphibians (including stem-group frogs, salamanders and caecilians) also became more common during the Triassic and survived the extinction event. The earliest known neopterygian fish, including early holosteans and teleosts, appeared near the beginning of the Triassic, and quickly diversified to become among the dominant groups of fish in both freshwater and marine habitats.
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