Permian

The Permian is a geological period which started about 299 million years ago (mya), and ended about 252 mya. It is the sixth and last period of the Paleozoic era and the sixth period in the Phanerozoic eon, and ended in the largest mass extinction known to science.

Dimetrodon is a pelycosaur that lived in the Permian.

Data

• Oxygen content of atmosphere: 23% (115% of modern level).
• Average CO₂ content: 900 ppm (3 times pre-industrial level)
• Average surface temperature: ~16^oC (2^oC above modern level)
• Sea level: 60 metres above present day level; plummeting during the middle Permian to a constant minus 20 m in the late Permian.

Climate

The climate in the Permian was quite varied. At the start of the Permian, the Earth was still at the grip of an ice age from the Carboniferous. Glaciers receded in the mid-Permian period as the climate gradually warmed, drying the continent's interiors. In the late Permian period, the drying continued although the temperature cycled between warm and cool cycles.

Life

During the Permian, tetrapod life, (amphibians, Sauropsids and Synapsids) which evolved in the Carboniferous, became widespread and diverse. The first modern trees (conifers, ginkgos and cycads) appeared in the Permian.

Insects

The Permian was also a period of adaptive radiation in insects. Beetles (Coleoptera) appeared; so did flies (Diptera). 22 out of a total of 36 known orders of insects are known from the Permian. Some became extinct in the end-Permian event, but more radiation followed in the Mesozoic. Insects were probably, by the end of the Permian, the largest phylum, in terms of number of species.

Early relatives of cockroaches (Blattopterans) were the most common insects. and dragonflies ruled the air. True Odonata appeared in the Permian.

Pangaea

All the major land masses were collected together in the super-continent Pangaea. At the end of the period, the greatest flood basalt lava flows in the Phanerozoic raised world temperatures, and damaged the environment. These formed the extensive Siberian traps. The causes of the Permian/Triassic extinction event are not yet agreed between scientists. Trilobites, once a dominant life-form in the ocean, became extinct, together with 90% of all marine species.

Permian Media

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  Geography of the Permian world

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  Selwyn Rock, South Australia, an exhumed glacial pavement of Permian age

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  Hercosestria cribrosa, a reef-forming productid brachiopod (Middle Permian, Glass Mountains, Texas)

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  Fossil and life restoration of Permocupes sojanensis, a permocupedid beetle from the Middle Permian of Russia

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  Restoration of Weigeltisaurus jaekeli, a weigeltisaurid from the Late Permian of Europe. Weigeltisaurids represent the oldest known gliding vertebrates.

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  Map of the world at the Carboniferous-Permian boundary, showing the four floristic provinces

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  Life reconstruction of Permian wetland environment, showing an Eryops

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  The Permian–Triassic extinction event, labeled "End P" here, is the most significant extinction event in this plot for marine genera which produce large numbers of fossils

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  Edaphosaurus pogonias and Platyhystrix – Early Permian, North America and Europe

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  Dimetrodon grandis and Eryops – Early Permian, North America