Extinction events[change | change source]
Great extinction events happened at both the beginning and end of the Triassic period. The Triassic began after the great extinction at the end of the Palaeozoic era, the Permian/Triassic extinction event. Nobody really knows the exact cause of the Permian/Triassic extinction, but many experts have different theories. Generally, experts agree that many things caused the extinction.
The Triassic had several more extinction events, whose causes are also unknown. The most significant of these took place at the end of the Triassic, which was one of the 'big five' Phanerozoic marine extinctions.
Geology[change | change source]
Name[change | change source]
- Red beds, laid down in desert conditions;
- Limestone, laid down in seas, mostly over continental shelves; and
- Black slate, laid down in rich organic conditions such as river deltas.
Overall climate[change | change source]
Paleogeography[change | change source]
During the Triassic period, there were no separate continents like there are today. Almost all the Earth's land mass was together in a single supercontinent called Pangaea ("all the land"). Pangaea was centered more or less on the equator. All the deep-ocean sediments (the things that settled at the bottom of the ocean) had disappeared. This happened because oceanic plates moved sideways and downward until they were finally on top of each other, or under each other.
The supercontinent Pangaea was rifting during the Triassic – especially late in the period – but had not yet separated into different continents.
Being a super-continental land mass, Pangaea had limited shoreline. Because of this, Triassic marine deposits – fossils from Triassic ocean life – are rare in most of the world. In North America, for example, marine deposits are limited to a few exposures in the west. However, they are common in Western Europe, where the Triassic was first studied.
Major adaptive radiations[change | change source]
The first part of the Triassic had much less variety than the Permian, and showed signs of a deteriorated environment. This situation lasted for about 5 million years, then steadily improved. Into the vacant ecological niches, new forms evolved, replacing old with new. This rapid adaptive radiation happened to the reptiles on land, the fish in the seas, and a number of other groups, like the insects. Diverse communities with complex ecology took 30 million years to re-establish.
Fish[change | change source]
The group of bony fish known as the teleosts first appeared during the Triassic period. The group now includes over 80% of all fish and 95% of all bony fish. The only other common group of fish are the Chondrichthyes (the sharks and rays). The rays also appeared during the Triassic.
Reptiles[change | change source]
Many reptile groups first appeared during the Triassic period, possibly because so many niches were vacant at the time. Some of these new groups died out in the End–Triassic extinction event, but those that survived ruled the Earth for the rest of the Mesozoic. Examples include:
The end-Triassic extinction[change | change source]
- Crocodilian Archosaurs:
- Other Archosaurs:
The Triassic was a period of great change in tetrapods: many new and important groups appeared, but many others became extinct. Of all the periods in the Mesozoic era, there are the least number of fossils from the Triassic period. This makes it difficult for scientists to explain these events.
Related pages[change | change source]
- Mesozoic era
- Geological period
- Extinction events
References[change | change source]
- Cohen, K.M.; Finney, S.; & Gibbard, P.L. (January 2013). "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. International Union of Geological Sciences. Retrieved June 12, 2016.CS1 maint: multiple names: authors list (link)
- User, Super. "ICS - Chart/Time Scale". www.stratigraphy.org.
- Logan A. (2016). "Triassic Period". Encyclopædia Britannica. Encyclopædia Britannica Inc. Retrieved June 12, 2016.
- Erwin D.H. 1993. The great Palaeozoic crisis: life & death in the Permian. Columbia University Press, New York. ISBN 978-0231074674.
- Hallam A. and Wignall P.B. 1997. Mass extinctions and their aftermath. Oxford, Cambridge. ISBN 978-0198549161.
- Raup D.M. and Sepkoski J.J. 1982. Mass extinctions in the marine fossil record. Science 215, 1590.
- Raup D.M. and Gould S.J. 1992. Extinction: bad luck or bad genes? Norton, New York. ISBN 978-0393309270.
- Sahney S. and Benton M.J. (2008). "Recovery from the most profound mass extinction of all time" (PDF). Proceedings of the Royal Society: Biological 275: 759. doi:10.1098/rspb.2007.1370. http://journals.royalsociety.org/content/qq5un1810k7605h5/fulltext.pdf.
- Benton M. 1990. The reign of the reptiles. Crescent, New York. ISBN 978-0517025574.