The Triassic is the first geological period in the Mesozoic that began 252.17 million years ago, and ended at 201.3 million years ago. Before it was the Permian, and it was followed by the Jurassic.
Both the start and the end of the Triassic are marked by great extinction events. The period began after the great extinction at the end of the Palaeozoic era, the P/Tr extinction event. Many new groups arose during its 50 million years, including the dinosaurs.
Nobody really knows the exact cause of the Permian/Triassic extinction, but it has been discussed by many experts. Generally, it is agreed that many things caused it. The Triassic had several more extinction events, whose causes are also obscure. 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]
The name 'Triassic' comes from the rock strata. "Tri" means "three": there are three layers:
- red beds, laid down in desert conditions
- limestone, laid down in seas, mostly over continental shelves.
- black slate, laid down in rich organic conditions such as river deltas.
Overall climate[change | change source]
On average, the Triassic was:
- 80% of modern oxygen level
- 6 times pre-industrial CO2 level
- Average surface temperature +3oC compared with present
Paleogeography[change | change source]
During the Triassic, almost all the Earth's land mass was concentrated into a single supercontinent centered more or less on the equator, called Pangaea ("all the land"). All the deep- ocean sediments, or the things that settled at the bottom of the ocean, have disappeared because oceanic plates moved sideways and downward until they finally were on top of or under each other. The supercontinent Pangaea was rifting during the Triassic–especially late in the period–but had not yet separated. Because of the limited shoreline of one super-continental mass, Triassic marine deposits are globally relatively rare, despite their prominence in Western Europe, where the Triassic was first studied. In North America, for example, marine deposits are limited to a few exposures in the west.
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 and the fish in the seas, and to a number of other groups, such as the insects. Diverse communities with complex ecology took 30 million years to reestablish.
Fish[change | change source]
The group of bony fish known as the teleosts first appeared in the Triassic. 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, and the rays are also a Triassic 'invention'.
Reptiles[change | change source]
Many reptile goups originated in the Triassic, possibly because so many niches were vacant at the time. Some of these new groups were caught in the end-Triassic extinction, but those that survived ruled the Earth for the rest of the Mesozoic. examples are:
- Crocodilian Archosaurs:
- Other Archosaurs:
And, amongst the Synapsids (formerly Mammal-like reptiles), the End-Triassic extinction saw the last of the Dicynodonts. Thus the Triassic is seen to be a period of great turnover in tetrapods: many new and important groups, but many extinctions. The fossil record of the Triassic is the poorest in the Mesozoic, which makes it difficult to explain these events.
References[change | change source]
- Erwin D.H. 1993. The great Palaeozoic crisis: life & death in the Permian. Columbia, N.Y.
- Hallam A. and Wignall P.B. 1997. Mass extinctions and their aftermath. Oxford.
- Raup D.M. and Sepkoski J.J. 1982. Mass extinctions in the marine fossil record. Science 215, 1590.
- Raup D.M. Extinction: bad luck or bad genes? Norton, N.Y.
- 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, N.Y.
|Precambrian (4.567 gya – 541 mya)|
|In the left column are Eons, bold are Eras, not bold are Periods. gya = billion years ago, mya = million years ago|
|Hadean (4.567 gya – 4 gya)||Chaotian Zirconian|
|Archaean (4 gya – 2.5 gya)||Eoarchaean (4 gya – 3.6 gya)|
|Proterozoic (2.5 gya – 541 mya)||Palaeoproterozoic (2.5 gya – 1.6 gya) Siderian (2.5 gya – 2.3 gya) Rhyacian (2.3 gya – 2.05 gya) Orosirian (2.05 gya – 1.8 gya) Statherian (1.8 gya – 1.6 gya)|
|Phanerozoic (541 mya – today)|
|In the left column are Eras, bold are Periods, not bold or italics are Epochs, Italics are stages. kya = thousand years ago, mya = million years ago|
|Palaeozoic (541 mya – 252.17 mya)||Cambrian (541 mya – 485.4 mya)|
|Mesozoic (252.17 mya – 66.0 mya)||Triassic (252.17 mya – 201.3 mya) Lower Triassic (252.17 mya – 247.2 mya) Middle Triassic (247.2 mya – 237 mya) Upper Triassic (237 mya – 201.3 mya)|
|Cainozoic (66.0 mya – today)||Palaeogene (66.0 mya – 23.03 mya) Palaeocene (66.0 mya – 56 mya) Eocene (56 mya - 33.9 mya) Oligocene (33.9 mya – 23.03 mya)|