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Research Article

A scale of greatness and causal classification of mass extinctions: Implications for mechanisms

A. M. Celâl Şengör, Saniye Atayman, and Sinan Özeren
PNAS September 16, 2008 105 (37) 13736-13740; https://doi.org/10.1073/pnas.0805482105
A. M. Celâl Şengör
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  • For correspondence: sengor@itu.edu.tr
Saniye Atayman
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Sinan Özeren
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  1. Contributed by A. M. Celâl Şengör, June 9, 2008 (received for review February 18, 2008)

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Abstract

A quantitative scale for measuring greatness, G, of mass extinctions is proposed on the basis of rate of biodiversity diminution expressed as the product of the loss of biodiversity, called magnitude (M), and the inverse of time in which that loss occurs, designated as intensity (I). On this scale, the catastrophic Cretaceous–Tertiary (K-T) extinction appears as the greatest since the Ordovician and the only one with a probable extraterrestrial cause. The end-Permian extinction was less great but with a large magnitude (M) and smaller intensity (I); only some of its individual episodes involved some semblance of catastrophe. Other extinctions during the Phanerozoic, with the possible exception of the end-Silurian diversity plunge, were parts of a forced oscillatory phenomenon and seem caused by marine- and land-habitat destruction during continental assemblies that led to elimination of shelves and (after the Devonian) rain forests and enlargement of deserts. Glaciations and orogenies that shortened and thickened the continental crust only exacerbated these effects. During the Mesozoic and Cainozoic, the evolution of life was linearly progressive, interrupted catastrophically only at the K-T boundary. The end-Triassic extinction was more like the Paleozoic extinctions in nature and probably also in its cause. By contrast, the current extinction resembles none of the earlier ones and may end up being the greatest of all.

  • greatness scale
  • intensity
  • magnitude
  • mass dying
  • shelf destruction

Footnotes

  • ‡To whom correspondence should be addressed. E-mail: sengor{at}itu.edu.tr
  • Author contributions: A.M.C.Ş. designed research; A.M.C.Ş., S.A., and S.Ö. performed research; S.Ö. contributed analytic tool; and A.M.C.Ş., S.A., and S.Ö. wrote the paper.

  • The authors declare no conflict of interest.

  • ↵§ “Emfylostasiogenic” is a new word we created from the classical Greek words 'έμφῡλος (emfylos), meaning kinsfolk, tribe; στάσις (stasis), meaning sedition, discord; and γένησις (genesis), meaning producing, engendering.

  • ↵¶ Şengör AMC, Atayman S, Özeren S, Hüsrevoğlu S (2007) Was Palaeo-Tethys the most effective killer in earth history? 2007 GSA Annual Meeting & Exposition, October 18–31, 2007, Denver, CO, Vol 39, p 586 (abstr).

  • © 2008 by The National Academy of Sciences of the USA
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A scale of greatness and causal classification of mass extinctions: Implications for mechanisms
A. M. Celâl Şengör, Saniye Atayman, Sinan Özeren
Proceedings of the National Academy of Sciences Sep 2008, 105 (37) 13736-13740; DOI: 10.1073/pnas.0805482105

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A scale of greatness and causal classification of mass extinctions: Implications for mechanisms
A. M. Celâl Şengör, Saniye Atayman, Sinan Özeren
Proceedings of the National Academy of Sciences Sep 2008, 105 (37) 13736-13740; DOI: 10.1073/pnas.0805482105
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  • Geology
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    • Abstract
    • Extinction Greatness as a Function of Extinction Magnitude and Extinction Intensity
    • A Causal Classification of Extinctions
    • What Is Special About the Permian Extinction?
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