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Triassic

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The Triassic is a major geologic period that shaped the modern world. It is the first and shortest period of the Mesozoic Era. This period lasted for 50.5 million years. It began 251.902 million years ago at the end of the Permian Period. It concluded 201.4 million years ago when the Jurassic Period started. The Triassic is also the seventh period of the Phanerozoic Eon. This era began immediately following the Permian–Triassic extinction event. That event had significantly reduced the biosphere of Earth.

Extinction Intensity
Extinction Intensity

Geologists divide the Triassic into three distinct epochs. These are the Early Triassic, the Middle Triassic, and the Late Triassic. Scientists often refer to the corresponding rock layers as the Lower, Middle, and Upper Triassic. The name itself has a specific historical origin. In 1834, Friedrich August von Alberti named the period. He chose the name after observing three distinct rock layers in southern Germany. These layers are the Buntsandstein, which is colorful sandstone. They also include the Muschelkalk, a shell-bearing limestone. Finally, there is the Keuper, which is composed of colored clay. The term comes from a Greek word meaning a triad or a group of three.

Triassic Utah
Triassic Utah

During this time, the Earth's geography was dominated by a supercontinent called Pangaea. This massive landmass stretched from the north to the south polar regions. It was centered near the equator. The Paleo- and Neo-Tethys oceans were located within the arc of Pangaea. Beyond the supercontinent lay the vast Panthalassa Ocean.

Pangaea (230 million years ago)
Pangaea (230 million years ago)

During the Late Triassic and Early Jurassic, Pangaea began to rift apart. It split into two large landmasses. These were Laurasia in the north and Gondwana in the south. This movement changed the global climate significantly. While the interior of Pangaea was mostly hot and dry with many deserts, the climate became more humid as the landmasses drifted apart.

The Triassic biosphere was defined by three categories of organisms. These included animals that survived the previous extinction, animals that flourished briefly, and new animals that evolved to dominate the Mesozoic Era. Reptiles were the primary terrestrial vertebrates. A specialized group called archosaurs was very successful. Some archosaurs were pseudosuchians, which were relatives of modern crocodilians. Other archosaurs became the pterosaurs, which were the first vertebrates to achieve flight. The first dinosaurs appeared during the Late Triassic. However, they did not become the dominant animals until the Jurassic Period.

Mastodonsaurus3
Mastodonsaurus3

Other groups also underwent major changes during these millions of years. Therapsids had been the dominant vertebrates in the Permian. In the Triassic, dicynodonts and cynodonts saw a brief surge in diversification. However, most therapsids declined and faced extinction by the end of the period. Interestingly, the first stem-group mammals, known as mammaliamorphs, appeared during this time. These were a specialized subgroup of cynodonts. They survived the eventual extinction and later radiated during the Jurassic.

Triassic plants MKL Bd. 15 1890 (128662915)
Triassic plants MKL Bd. 15 1890 (128662915)

Life in the water was also highly diverse. The earliest known neopterygian fish appeared near the start of the Triassic. This group includes early holosteans and teleosts. These fish quickly became dominant in both freshwater and marine habitats.

Birgeria recon
Birgeria recon

In the water, amphibians were represented by temnospondyls. These were giant aquatic predators that survived the end-Permian extinction. They saw a burst of diversification before going extinct at the end of the Triassic. Meanwhile, early crown-group lissamphibians, such as stem-group frogs and salamanders, became more common.

Triassic marine vertebrate apex predators
Triassic marine vertebrate apex predators

The end of the Triassic was marked by a major mass extinction event. This is known as the Triassic–Jurassic extinction event. This event wiped out many groups of animals, including most pseudosuchians. This loss of competition allowed dinosaurs to assume dominance in the following Jurassic Period. The geological changes were also driven by intense volcanic activity. The Siberian Traps eruptions persisted into the Early Triassic. Later, the Central Atlantic Magmatic Province was active during the Late Triassic. These events helped set the stage for the shifting oceans and continents of the future.

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🖼️ Images & Media (11)
File:230 Ma plate tectonic reconstruction.png
230 Ma plate tectonic reconstruction.png
File:Pangaea (230 million years ago).png
Pangaea (230 million years ago).png
File:(1)Saunders Quarry-1.jpg
(1)Saunders Quarry-1.jpg
File:Triassic plants MKL Bd. 15 1890 (128662915).jpg
Triassic plants MKL Bd. 15 1890 (128662915).jpg
File:Prospect Hill Monterey Pine Forest.jpg
Prospect Hill Monterey Pine Forest.jpg
File:Triassic Utah.JPG
Triassic Utah.JPG
File:Birgeria recon.jpg
Birgeria recon.jpg
File:Mastodonsaurus3.jpg
Mastodonsaurus3.jpg
File:Triassic marine vertebrate apex predators.png
Triassic marine vertebrate apex predators.png
File:Extinction Intensity.svg
Extinction Intensity.svg
File:Petrified Forest National Park-Rainbow Forest Museum-1.jpg
Petrified Forest National Park-Rainbow...
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