Triassic: Wikis


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Triassic Period
251 - 199.6 million years ago
Mean atmospheric O2 content over period duration ca. 16 Vol %[1]
(80 % of modern level)
Mean atmospheric CO2 content over period duration ca. 1750 ppm[2]
(6 times pre-industrial level)
Mean surface temperature over period duration ca. 17 °C [3]
(3 °C above modern level)

The Triassic is a geologic period that extended from about 250 to 200 Ma (million years ago). As the first period of the Mesozoic Era, the Triassic follows the Permian and is followed by the Jurassic. Both the start and end of the Triassic are marked by major extinction events. The extinction event that closed the Triassic Period has recently been more accurately dated, but as with most older geologic periods, the rock beds that define the start and end are well identified, but the exact dates of the start and end of the period are uncertain by a few million years.

During the Triassic, both marine and continental life show an adaptive radiation beginning from the starkly impoverished biosphere that followed the Permian-Triassic extinction. Corals of the hexacorallia group made their first appearance. The first flying vertebrates, the pterosaurs, evolved during the Triassic.


Dating and subdivisions

Key events in the Triassic
view • discuss • edit
-255 —
-250 —
-245 —
-240 —
-235 —
-230 —
-225 —
-220 —
-215 —
-210 —
-205 —
-200 —
Full recovery of woody trees[4]
Coals return[5]
corals & calcified sponges[6]
An approximate timescale of key Triassic events.
Axis scale: millions of years ago.

The Triassic was named in 1834 by Friedrich Von Alberti from the three distinct layers (Latin trias meaning triad)—red beds, capped by chalk, followed by black shales—that are found throughout Germany and northwest Europe, called the 'Trias'.

The Triassic is usually separated into Early, Middle, and Late Triassic Epochs, and the corresponding rocks are referred to as Lower, Middle, or Upper Triassic. The faunal stages from the youngest to oldest are:

Upper/Late Triassic (Tr3)
  Rhaetian (203.6 ± 1.5 – 199.6 ± 0.6 Ma)
  Norian (216.5 ± 2.0 – 203.6 ± 1.5 Ma)
  Carnian (228.0 ± 2.0 – 216.5 ± 2.0 Ma)
Middle Triassic (Tr2)
  Ladinian (237.0 ± 2.0 – 228.0 ± 2.0 Ma)
  Anisian (245.0 ± 1.5 – 237.0 ± 2.0 Ma)
Lower/Early Triassic (Scythian)
  Olenekian (249.7 ± 0.7 – 245.0 ± 1.5 Ma)
  Induan (251.0 ± 0.4 – 249.7 ± 0.7 Ma)


230 Ma plate tectonic reconstruction

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"). From the east a vast gulf entered Pangaea, the Tethys sea. It opened farther westward in the mid-Triassic, at the expense of the shrinking Paleo-Tethys Ocean, an ocean that existed during the Paleozoic. The remaining shores were surrounded by the world-ocean known as Panthalassa ("all the sea"). All the deep-ocean sediments laid down during the Triassic have disappeared through subduction of oceanic plates; thus, very little is known of the Triassic open ocean. The supercontinent Pangaea was rifting during the Triassic—especially late in the period—but had not yet separated. The first nonmarine sediments in the rift that marks the initial break-up of Pangaea—which separated New Jersey from Morocco—are of Late Triassic age; in the U.S., these thick sediments comprise the Newark Group.[7] 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. Thus Triassic stratigraphy is mostly based on organisms living in lagoons and hypersaline environments, such as Estheria crustaceans.


At the beginning of the Mesozoic Era, Africa was joined with Earth's other continents in Pangaea.[8] Africa shared the supercontinent's relatively uniform fauna which was dominated by theropods, prosauropods and primitive ornithischians by the close of the Triassic period.[8] Late Triassic fossils are found through-out Africa, but are more common in the south than north.[8] The boundary separating the Triassic and Jurassic marks the advent of an extinction event with global impact, although African strata from this time period have not been thoroughly studied.[8]


Middle Triassic marginal marine sequence, southwestern Utah

The Triassic climate was generally hot and dry, forming typical red bed sandstones and evaporites. There is no evidence of glaciation at or near either pole; in fact, the polar regions were apparently moist and temperate, a climate suitable for reptile-like creatures. Pangaea's large size limited the moderating effect of the global ocean; its continental climate was highly seasonal, with very hot summers and cold winters.[9] It probably had strong, cross-equatorial monsoons.[9]


Triassic flora as depicted in Meyers Konversations-Lexikon (1885-90)

Three categories of organisms can be distinguished in the Triassic record: holdovers from the Permian-Triassic extinction, new groups which flourished briefly, and other new groups which went on to dominate the Mesozoic world.


On land, the holdover plants included the lycophytes, the dominant cycads, ginkgophyta (represented in modern times by Ginkgo biloba) and glossopterids. The spermatophytes, or seed plants came to dominate the terrestrial flora: in the northern hemisphere, conifers flourished. Glossopteris (a seed fern) was the dominant southern hemisphere tree during the Early Triassic period.

Marine fauna

In marine environments, new modern types of corals appeared in the Early Triassic, forming small patches of reefs of modest extent compared to the great reef systems of Devonian times or modern reefs. The shelled cephalopods called ammonites recovered, diversifying from a single line that survived the Permian extinction. The fish fauna was remarkably uniform, reflecting the fact that very few families survived the Permian extinction. There were also many types of marine reptiles. These included the Sauropterygia, which featured pachypleurosaurs and nothosaurs (both common during the Middle Triassic, especially in the Tethys region), placodonts, and the first plesiosaurs; the first of the lizardlike Thalattosauria (askeptosaurs); and the highly successful ichthyosaurs, which appeared in Early Triassic seas and soon diversified, some eventually developing to huge size during the late Triassic.

Terrestrial fauna

Reconstruction of Proterosuchus, a genus of carnivorous reptile, classified under Archosauromorpha, that existed in the Early Triassic period.
Coelophysis, one of the first Dinosaurs, appeared in the mid-Triassic.

The Permian-Triassic extinction devastated terrestrial life. Biodiversity rebounded with the influx of disaster taxa, however these were short lived. Diverse communities with complex trophic structures took 30 million years to reestablish.[10]

Temnospondyl amphibians were among those groups that survived the Permian-Triassic extinction, some lineages (e.g. Trematosaurs) flourishing briefly in the Early Triassic, while others (e.g. capitosaurs) remained successful throughout the whole period, or only came to prominence in the Late Triassic (e.g. plagiosaurs, metoposaurs). As for other amphibians, the first Lissamphibia, characterized by the first frogs, are known from the Early Triassic, but the group as a whole did not become common until the Jurassic, when the temnospondyls had become very rare.

Archosauromorph reptiles — especially archosaurs — progressively replaced the synapsids that had dominated the Permian. Although Cynognathus was a characteristic top predator in earlier Triassic (Olenekian and Anisian) Gondwana, and both kannemeyeriid dicynodonts and gomphodont cynodonts remained important herbivores during much of the period. By the end of the Triassic, synapsids played only bit parts. During the Carnian (early part of the Late Triassic), some advanced cynodont gave rise to the first mammals. At the same time the Ornithodira, which until then had been small and insignificant, evolved into pterosaurs and a variety of dinosaurs. The Crurotarsi were the other important archosaur clade, and during the Late Triassic these also reached the height of their diversity, with various groups including the phytosaurs, aetosaurs, several distinct lineages of Rauisuchia, and the first crocodylians (the Sphenosuchia). Meanwhile the stocky herbivorous rhynchosaurs and the small to medium-sized insectivorous or piscivorous Prolacertiformes were important basal archosauromorph groups throughout most of the Triassic.

Among other reptiles, the earliest turtles, like Proganochelys and Proterochersis, appeared during the Norian (middle of the Late Triassic). The Lepidosauromorpha—specifically the Sphenodontia—are first known in the fossil record a little earlier (during the Carnian). The Procolophonidae were an important group of small lizard-like herbivores.

Archosaurs were initially rarer than the therapsids which had dominated Permian terrestrial ecosystems, but they began to displace therapsids in the mid-Triassic.[11] This "Triassic Takeover" may have contributed to the evolution of mammals by forcing the surviving therapsids and their mammaliform successors to live as small, mainly nocturnal insectivores; nocturnal life probably forced at least the mammaliforms to develop fur and higher metabolic rates.[12]


At the start of the Triassic period coal is noticeable by its absence throughout the world. This is known as the "coal gap" and can be seen as part of the Permian–Triassic extinction event.[5] Sharp drops in sea level across the Permo Triassic boundary may be partially to blame.[13] During the preceding Permian period the hot desert conditions had contributed to the evaporation of many inland seas and the inundation of these seas, perhaps by a number of tsunami events may have been responsible for the drop in sea level.[14] There are large salt basins in the southwest United States and a very large basin is suspected in central Canada.[15]

Immediately above the boundary the glossopteris flora was suddenly[16] largely displaced by an Australia wide coniferous flora containing few species and containing a lycopod herbaceous under story. Conifers became common in Eurasia also. Each of these groups of conifers arose from endemic species because conifers are very poor at crossing ocean barriers and they remained separated for hundreds of millions of years, largely to the present. Podocarpis was south and Pines, Junipers, and Sequoias were north, for instance. The dividing line ran through the Amazon Valley, across the Sahara, and north of Arabia, India, Thailand, and Australia.[17][18] It has been suggested that there was a climate barrier for the conifers.[19] although water barriers are more plausible. If so, something that can cross at least short water barriers must have been involved in producing the coal hiatus. Hot climate could have been an important auxiliary factor across Antarctica or the Bering Strait, however. There was a spike of fern and lycopod spores immediately after the close of the Permian.[20] In addition there was also a spike of fungal spores immediately after the Permian-Triassic boundary.[21] This spike may have lasted 50,000 years in Italy and 200,000 years in China and must have contributed to the climate warmth.

If so, something besides an instant catastrophe must have been involved to cause the coal hiatus because fungi would surely have removed all dead vegetation and coal forming detritus in a few decades in most tropical places. Besides, the fungal spores rose gradually and declined similarly. There was also much woody debris. Each phenomenon would hint at widespread vegetative death. Whatever caused the coal hiatus must have started in North America 25 million years sooner.[22].


Triassic sandstone near Stadtroda, Germany.

The Monte San Giorgio lagerstätte, now in the Lake Lugano region of northern Italy and Switzerland, was in Triassic times a lagoon behind reefs with an anoxic bottom layer, so there were no scavengers and little turbulence to disturb fossilization, a situation that can be compared to the better-known Jurassic Solnhofen limestone lagerstätte. The remains of fish and various marine reptiles (including the common pachypleurosaur Neusticosaurus, and the bizarre long-necked archosauromorph Tanystropheus), along with some terrestrial forms like Ticinosuchus and Macrocnemus, have been recovered from this locality. All these fossils date from the Anisian/Ladinian transition (about 237 million years ago).

Late Triassic extinction event

The Triassic period ended with a mass extinction, which was particularly severe in the oceans; the conodonts disappeared, and all the marine reptiles except ichthyosaurs and plesiosaurs. Invertebrates like brachiopods, gastropods, and molluscs were severely affected. In the oceans, 22% of marine families and possibly about half of marine genera went missing according to University of Chicago paleontologist Jack Sepkoski.

Though the end-Triassic extinction event was not equally devastating everywhere in terrestrial ecosystems, several important clades of crurotarsans (large archosaurian reptiles previously grouped together as the thecodonts) disappeared, as did most of the large labyrinthodont amphibians, groups of small reptiles, and some synapsids (except for the proto-mammals). Some of the early, primitive dinosaurs also went extinct, but other more adaptive dinosaurs survived to evolve in the Jurassic. Surviving plants that went on to dominate the Mesozoic world included modern conifers and cycadeoids.

What caused this Late Triassic extinction is not known with certainty. It was accompanied by huge volcanic eruptions that occurred as the supercontinent Pangaea began to break apart about 202 to 191 million years ago [(40Ar/39Ar dates[23])], forming the Central Atlantic Magmatic Province [(CAMP)],[24] one of the largest known inland volcanic events since the planet cooled and stabilized. Other possible but less likely causes for the extinction events include global cooling or even a bolide impact, for which an impact crater containing Manicouagan Reservoir in Quebec, Canada, has been singled out. At the Manicouagan impact crater, however, recent research has shown that the impact melt within the crater has an age of 214±1 Ma. The date of the Triassic-Jurassic boundary has also been more accurately fixed recently, at 201.58±0.28 Ma. Both dates are gaining accuracy by using more accurate forms of radiometric dating, in particular the decay of uranium to lead in zircons formed at the impact. So the evidence suggests the Manicouagan impact preceded the end of the Triassic by approximately 10±2 Ma. Therefore it could not be the immediate cause of the observed mass extinction.[25]

The number of Late Triassic extinctions is disputed. Some studies suggest that there are at least two periods of extinction towards the end of the Triassic, between 12 and 17 million years apart. But arguing against this is a recent study of North American faunas. In the Petrified Forest of northeast Arizona there is a unique sequence of latest Carnian-early Norian terrestrial sediments. An analysis in 2002 found no significant change in the paleoenvironment.[26] Phytosaurs, the most common fossils there, experienced a change-over only at the genus level, and the number of species remained the same. Some aetosaurs, the next most common tetrapods, and early dinosaurs, passed through unchanged. However, both phytosaurs and aetosaurs were among the groups of archosaur reptiles completely wiped out by the end-Triassic extinction event.

It seems likely then that there was some sort of end-Carnian extinction, when several herbivorous archosauromorph groups died out, while the large herbivorous therapsids— the kannemeyeriid dicynodonts and the traversodont cynodonts— were much reduced in the northern half of Pangaea (Laurasia).

These extinctions within the Triassic and at its end allowed the dinosaurs to expand into many niches that had become unoccupied. Dinosaurs became increasingly dominant, abundant and diverse, and remained that way for the next 150 million years. The true "Age of Dinosaurs" is the Jurassic and Cretaceous, rather than the Triassic.

See also


  1. ^ Image:Sauerstoffgehalt-1000mj.svg
  2. ^ Image:Phanerozoic Carbon Dioxide.png
  3. ^ Image:All palaeotemps.png
  4. ^ McElwain, J.C.; Punyasena, S.W. (2007). "Mass extinction events and the plant fossil record". Trends in Ecology & Evolution 22 (10): 548-557. doi:10.1016/j.tree.2007.09.003. 
  5. ^ a b Retallack GJ Veevers JJ & Morante R (1996). "Global coal gap between Permian–Triassic extinctions and middle Triassic recovery of peat forming plants". GSA Bulletin 108 (2): 195–207. Retrieved 2007-09-29. 
  6. ^ Payne, J.L.; Lehrmann, D.J.; Wei, J.; Orchard, M.J.; Schrag, D.P.; Knoll, A.H. (2004). "Large Perturbations of the Carbon Cycle During Recovery from the End-Permian Extinction". Science 305 (5683): 506. doi:10.1126/science.1097023. 
  7. ^ Lecture 10 - Triassic: Newark, Chinle
  8. ^ a b c d Jacobs, Louis, L. (1997). "African Dinosaurs." Encyclopedia of Dinosaurs. Edited by Phillip J. Currie and Kevin Padian. Academic Press. p. 2-4.
  9. ^ a b Stanley, 452-3.
  10. ^ 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. 
  11. ^ Tanner LH, Lucas SG & Chapman MG (2004). "Assessing the record and causes of Late Triassic extinctions" (PDF). Earth-Science Reviews 65 (1-2): 103–139. doi:10.1016/S0012-8252(03)00082-5. Retrieved 2007-10-22. 
  12. ^ Ruben, J.A., and Jones, T.D. (2000). "Selective Factors Associated with the Origin of Fur and Feathers". American Zoologist 40 (4): 585–596. doi:10.1093/icb/40.4.585. 
  13. ^ Holser WT Schonlaub H_P,Moses AJr Boekelmann K Klein P Magaritz MOrth CJ Fenninger A Jenny C Kralik M Mauritsch EP Schramm J_M Sattagger K Schmoller R 1989 A unique geochemical record at the Permian/Triassic boundary. Nature 337; 39, on p42
  14. ^ Knauth LP 1998 Salinity history of the earth's early ocean, Nature 395; 554-555.
  15. ^ Dott, R.H. and Batten, R.L. (1971) Evolution of the Earth, 4th ed. McGraw Hill, NY.
  16. ^ Hosher WT Magaritz M Clark D 1987 Events near the Permian-Triassic boundary. Mod. Geol. 11; 155-180, on p173-174.
  17. ^ Florin R (1963) The distribution of Conifer and Taxad genera in time and space. Acta Horti Bergiani. 20, 121-312.
  18. ^ Melville R (1966) Continental drift, Mesozoic continents, and the migrations of the angiosperms. Nature 211, 116.
  19. ^ Darlington PJ, (1965) Biogeography of the southern end of the world. Harvard University Press, Cambridge Mass., on p168.
  20. ^ Retallack GJ (1995) Permian -Triassic life crises on land. Science 267, 77-79.
  21. ^ Eshet Y Rampino MR (1995) Fungal event and palynological record of ecological crises and recovery across Permian-Triassic boundary. Geology 23, 967-970, on p969.
  22. ^ Retallack GJ Veevers JJ Morante R (1996) Global coal gap between Permian-Triassic extinctions and middle Triassic recovery of peat forming plants (review). Geological Society Am. Bull. 108, 195-207.
  23. ^ Nomade et al.,2007 Palaeogeography, Palaeoclimatology, Palaeoecology 244, 326-344.
  24. ^ Marzoli et al., 1999, Science 284. Extensive 200-million-year-old continental flood basalts of the Central Atlantic Magmatic Province, pp. 618-620.
  25. ^ Hodych & Dunning, 1992.
  26. ^ No Significant Nonmarine Carnian-Norian (Late Triassic) Extinction Event: Evidence From Petrified Forest National Park


  • Emiliani, Cesare. (1992). Planet Earth: Cosmology, Geology, & the Evolution of Life & the Environment. Cambridge University Press. (Paperback Edition ISBN 0-521-40949-7)
  • Ogg, Jim; June, 2004, Overview of Global Boundary Stratotype Sections and Points (GSSP's), Accessed April 30, 2006
  • Stanley, Steven M. Earth System History. New York: W.H. Freeman and Company, 1999. ISBN 0-7167-2882-6
  • van Andel, Tjeerd, (1985) 1994, New Views on an Old Planet: A History of Global Change, Cambridge University Press

External links

Triassic Period
Lower/Early Triassic Middle Triassic Upper/Late Triassic
Induan | Olenekian Anisian | Ladinian Carnian | Norian
Preceded by Proterozoic Eon 542 Ma - Phanerozoic Eon - Present
542 Ma - Paleozoic Era - 251 Ma 251 Ma - Mesozoic Era - 65 Ma 65 Ma - Cenozoic Era - Present
Cambrian Ordovician Silurian Devonian Carboniferous Permian Triassic Jurassic Cretaceous Paleogene Neogene Quaternary


Up to date as of January 15, 2010

Definition from Wiktionary, a free dictionary

Wikipedia has an article on:






Triassic (not comparable)


not comparable

none (absolute)

  1. (geology) Of a geologic period within the Mesozoic era; comprises lower, middle and upper epochs from about 250 to 200 million years ago.





Triassic (uncountable)

  1. (geology) The Triassic period.


See also

Simple English

The Triassic period is the first period of the Mesozoic era. It lasted from about 250 to 200 million years ago. 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.

The causes of the Permian/Triassic extinction has been widely discussed, but no single cause has been identified. The consensus is that several causes acting together produced the enent.[1][2] 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.[3][4]




The name 'Triassic' comes from a rock sequence found widely in European Triassic, the three distinct layers: red beds, capped by limestone, followed by black shales.[5]

Dates, epochs and stages

Upper Triassic (Tr3)
  Rhaetian 203.6 ± 1.5 – 199.6 ± 0.6 million years ago (mya)
  Norian 216.5 ± 2.0 – 203.6 ± 1.5 mya
  Carnian 228.0 ± 2.0 – 216.5 ± 2.0 mya
Middle Triassic (Tr2)
  Ladinian 237.0 ± 2.0 – 228.0 ± 2.0 mya
  Anisian 245.0 ± 1.5 – 237.0 ± 2.0 mya
Lower Triassic (Scythian)
  Olenekian 249.7 ± 0.7 – 245.0 ± 1.5 mya
  Induan 251.0 ± 0.4 – 249.7 ± 0.7 mya

Overall climate

On average, the Triassic was:

  1. 80% of modern oxygen level
  2. 6 times pre-industrial CO2 level
  3. Average surface temperature +3oC compared with present


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 laid down during the Triassic have disappeared through subduction of oceanic plates; thus, very little is known of the Triassic open ocean.

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

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.[6]


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'.


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.[7] examples are:

This was an extaordinary turn-around, for in the middle Triassic the ancestors of mammals, the Synapsids, were still dominant. All the same, many reptile groups went extinct in the Triassic:[7]p41

  • Crocodilian Archosaurs:
  • Other Archosaurs:
  • Proto-Archosaurs
  • Anapsids

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.


  1. Erwin D.H. 1993. The great Palaeozoic crisis: life & death in the Permian. Columbia, N.Y.
  2. Hallam A. and Wignall P.B. 1997. Mass extinctions and their aftermath. Oxford.
  3. Raup D.M. and Sepkoski J.J. 1982. Mass extinctions in the marine fossil record. Science 215, 1590.
  4. Raup D.M. Extinction: bad luck or bad genes? Norton, N.Y.
  5. paleo online [1]
  6. 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. 
  7. 7.0 7.1 Benton M. 1990. The reign of the reptiles. Crescent, N.Y.

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