The Permian is a geological period which started about 299 million years ago (mya), and ended about 252 mya. It is the last period of the Paleozoic era, and ended in the largest mass extinction known to science.
Data[change | change source]
- Oxygen content of atmosphere: 23% (115% of modern level).
- Average CO2 content: 900 ppm (3 times pre-industrial level)
- Average surface temperature: ~16oC (2oC 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[change | change source]
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 around 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[change | change source]
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[change | change source]
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.
Pangaea[change | change source]
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.
References[change | change source]
- Haq B.U. & Schutter S.R. 2008.. "A chronology of Paleozoic sea-level changes". Science 322 (5898): 64–68. doi:10.1126/science.1161648. PMID 18832639.
- Levin, Harold L. 2005. The Earth through time. 8th ed, Wiley, N.Y. Chapter 4: The fossil record.
- or class, depending on how they are classified.
- Wooton R.J. 1990. Major insect radiations. In P.D. Taylor & G.P. Larwood eds. Major evolutionary radiations. Oxford.
- Zimmerman E.C. 1948. Insects of Hawaii. vol II, Univ. Hawaii Press
- Grzimek, Bernhard (ed) 1975. Grzimek's animal life encyclopedia, vol 22 Insects. Van Nostrand Reinhold, N.Y.
- Riek E.F. & Kukalova-Peck J. 1984. A new interpretation of dragonfly wing venation based on early Upper Carboniferous fossils from Argentina (Insecta: Odonatoida) and basic character states in pterygote wings. Can. J. Zool. 62; 1150-1160.
- Erwin D.H. 1993. The great Palaeozoic crisis: life & death in the Permian. Columbia, N.Y.