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Ecosystem remodelling among vertebrates during the Permian-Triassic extinction
November 4, 2004
The biggest mass extinction of all time happened 251 million years ago, at the Permian-Triassic boundary. Virtually all of life was wiped out, but the pattern of how life was killed off on land has been mysterious until now. A team from Bristol University and Saratov University, Russia, have now laid the evidence bare.
The Bristol and Russian researchers have documented the event in Russia after looking at 675 specimens of amphibians and reptiles from 289 areas spanning 13 successive geological time zones in the South Urals basin. The study will be reported in Nature tomorrow [Thursday, November 4].
The mass extinction at the Permian-Triassic boundary is accepted as the most profound loss of life on record. Records indicate a loss of 50 per cent of animal groups or more, in both sea and on land, with a loss of 80 to 96 per cent of species. Local and regional-scale studies of marine specimen confirm the loss, but the terrestrial record has been harder to analyse in such close detail.
There was a profound loss of animal groups, and simplification of ecosystems, with the loss of small fish eaters and insect eaters, medium and large herbivores and large carnivores. Plant life also changed, from high rates of turnover through the Late Permian period to greater stability at low diversity through the Early Triassic period. Even after 15 million years of ecosystem rebuilding, some groups were still absent--small fish eaters, small insect eaters, large herbivores and top carnivores.
The end-Permian mass extinction is now thought to have been caused by gigantic volcanic eruptions, which triggered a runaway greenhouse effect and nearly put an end to life on earth.
Mike Benton, Professor of Vertebrate Palaeontology and Head of the Department of Earth Sciences at Bristol University, said: "At the end of the Permian there was a high turnover in animal families on land however these were largely destroyed by the Permian-Triassic extinction. However, after that the animal groups recovered slowly and diversity gradually increased."
University of Bristol
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| The protracted Permo-Triassic crisis and multi-episode extinction around the Permian-Triassic boundary [An article from: Global and Planetary Change] by H. Yin, Q. Feng, X. Lai, A. Baud, J. Tong
This digital document is a journal article from Global and Planetary Change, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: The Permo-Triassic crisis was a major turning point in geological history. Following the end-Guadalupian extinction phase,...
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| Events during Early Triassic recovery from the end-Permian extinction [An article from: Global and Planetary Change] by J. Tong, S. Zhang, J. Zuo, X. Xiong
This digital document is a journal article from Global and Planetary Change, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: The Palaeozoic-Mesozoic transition is characterized not only by the biggest Phanerozoic mass extinction, at the end of...
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| Pyrite framboid evidence for oxygen-poor deposition during the Permian-Triassic crisis in Kashmir [An article from: Palaeogeography, Palaeoclimatology, Palaeoecology] by P.B. Wignall, R. Newton, M.E. Brookfield
This digital document is a journal article from Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier in 2005. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: The Khunamuh Formation of the Guryul Ravine section in Kashmir provides one of the most detailed...
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| Cerium negative anomaly just before the Permian and Triassic boundary event - The upward expansion of anoxia in the water column [An article from: Palaeogeography, Palaeoclimatology, Palaeoecology] by Y. Kakuwa, R. Matsumoto
This digital document is a journal article from Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier in . The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: A negative excursion of Ce and a succeeding steep decline in @d^1^3C found just before the Permian and...
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| Causes and consequences of extreme Permo-Triassic warming to globally equable climate and relation to the Permo-Triassic extinction and recovery [An article ... Palaeoclimatology, Palaeoecology] by D.L. Kidder, T.R. Worsley
This digital document is a journal article from Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier in 2004. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: Permian waning of the low-latitude Alleghenian/Variscan/Hercynian orogenesis led to a long...
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| Differential severity of Permian-Triassic environmental changes on Tethyan shallow-water carbonate platforms [An article from: Global and Planetary Change] by O. Weidlich, M. Bernecker
This digital document is a journal article from Global and Planetary Change, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: Significantly different Guadalupian-Late Triassic patterns are observed in the evolution of attached and isolated carbonate...
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| Environmental and biotic changes across the Permian-Triassic boundary in western Tethys: The Bulla parastratotype, Italy [An article from: Global and Planetary Change] by E. Farabegoli, M.C. Perri, R. Posenato
This digital document is a journal article from Global and Planetary Change, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: The sedimentary and biotic evolution of a 190 m interval of shallow marine and lagoonal facies in the Bellerophon and...
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| Return to Coalsack Bluff and the Permian-Triassic boundary in Antarctica [An article from: Global and Planetary Change] by G.J. Retallack, T. Greaver, A.H. Jahren
This digital document is a journal article from Global and Planetary Change, published by Elsevier in 2007. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: Coalsack Bluff was the first discovery site in Antarctica for the latest Permian to earliest Triassic reptile Lystrosaurus....
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| Early Triassic recovery of the brachiopod faunas from the end-Permian mass extinction: A global review [An article from: Palaeogeography, Palaeoclimatology, Palaeoecology] by Z.Q. Chen, K. Kaiho, A.D. George
This digital document is a journal article from Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier in . The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: Brachiopod faunas in Lower Triassic deposits from Spitzbergen, Primorye of Russia, Japan, Mangyslak of...
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| Close-up of the end-Permian mass extinction horizon recorded in the Meishan section, South China: Sedimentary, elemental, and biotic characterization and ... Palaeoclimatology, Palaeoecology] by K. Kaiho, Z.Q. Chen, H. Kawahata, Y. Kajiwara, Sat
This digital document is a journal article from Palaeogeography, Palaeoclimatology, Palaeoecology, published by Elsevier in 2006. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.Description: The Permian/Triassic (P/Tr) boundary beds of the Meishan section, South China, have been re-studied...
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