Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-03T01:09:31.818Z Has data issue: false hasContentIssue false

Asymmetrical patterns of origination and extinction in higher taxa.

Published online by Cambridge University Press:  08 April 2016

Norman L. Gilinsky
Affiliation:
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061-0796
Richard K. Bambach
Affiliation:
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061-0796

Abstract

Using Sepkoski's compendium of fossil marine families (1982a, and updates), we have analyzed the changing pace of familial origination and extinction within 55 extinct and 44 extant higher taxa of marine organisms. Eight different metrics were calculated, and least-squares regression analysis was used to identify within-taxon trends in the data. All metrics and analyses gave essentially the same results. Origination metrics decline significantly with time during the histories of higher taxa, while extinction metrics increase significantly. The number of statistically significant declines of origination metric, however, substantially and invariably exceeds the number of statistically significant increases of extinction metric for each pair of corresponding metrics analyzed. It follows, therefore, that temporal trends in the pace of origination and extinction within higher taxa are highly asymmetrical.

Further analysis shows that truncating data from temporal endpoints has little effect upon the intensity of origination trends, implying that declining pace of origination is a sustained property of the long term histories of taxa. Such truncation, however, reduces the intensity of extinction trends to statistical insignificance and confirms Van Valen's (1985a) suggestion that extinction behaves largely as a stationary process. If the histories of higher taxa are characterized by substantial declines in the pace of origination while the pace of extinction remains largely stationary, it follows that declining pace of origination is an important controlling factor in long term taxic evolution.

Type
Articles
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Literature Cited

Carr, T. R. and Kitchell, J. A. 1980. Dynamics of taxonomic diversity. Paleobiol. 6:427443.Google Scholar
Carson, H. L. and Templeton, A. R. 1984. Genetic revolutions in relation to speciation phenomena: the founding of new populations. Ann. Rev. Ecol. Syst. 15:97131.Google Scholar
Gilinsky, N. L. and Bambach, R. K. 1985. The roots beneath patterns of taxonomic diversity: implications for extinction. Geol. Soc. Amer. Abstracts with Programs. 17:592.Google Scholar
Gingerich, P. D. 1983. Rates of evolution: effects of time and temporal scaling. Science. 222:159161.CrossRefGoogle ScholarPubMed
Hoffman, A. and Ghiold, J. 1985. Randomness in the pattern of‘mass extinctions’ and ‘waves of origination.’ Geol. Mag. 122:14.CrossRefGoogle Scholar
Kitchell, J. A. and Pena, D. 1984. Periodicity of extinctions in the geologic past: deterministic vs. stochastic explanations. Science. 226:689692.Google Scholar
Quinn, J. F. 1983. Mass extinctions in the fossil record. Science. 219:1239.Google Scholar
Raup, D. M. 1976. Species diversity in the Phanerozoic: an interpretation. Paleobiol. 2:289297.CrossRefGoogle Scholar
Raup, D. M. 1978. Cohort analysis of generic survivorship. Paleobiol. 4:115.Google Scholar
Raup, D. M. and Sepkoski, J. J. Jr. 1982. Mass extinctions in the marine fossil record. Science. 215:15011502.CrossRefGoogle ScholarPubMed
Raup, D. M. and Sepkoski, J. J. Jr. 1984. Periodicity of extinctions in the geologic past. Proc. Nat. Acad. Sci. USA. 81:801805.Google Scholar
Raup, D. M. and Sepkoski, J. J. Jr. 1986. Periodic extinction of families and genera. Science. 231:833836.Google Scholar
Sadler, P. M. 1981. Sediment accumulation rates and the completeness of stratigraphic sections. Geology. 89:569584.Google Scholar
Schindel, D. E. 1980. Microstratigraphic sampling and the limits of paleontologic resolution. Paleobiol. 6:408426.Google Scholar
Sepkoski, J. J. Jr. 1982a. A compendium of fossil marine families. Milwaukee Pub. Mus. Cont. Biol. Geol. 51:1125.Google Scholar
Sepkoski, J. J. Jr. 1982b. Mass extinctions in the Phanerozoic oceans: a review. Pp. 283290. In: Silver, L. T. and Schults, P. H., eds. Geological Implications of Impact of Large Asteroids and Comets on the Earth. Geol. Soc. Amer. Spec. Paper 190.Google Scholar
Sepkoski, J. J. Jr. 1984. A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and mass extinctions. Paleobiol. 10:246267.CrossRefGoogle Scholar
Sepkoski, J. J. Jr. 1987. Environmental trends in extinction during the Paleozoic. Science. 235:6466.CrossRefGoogle ScholarPubMed
Sepkoski, J. J. Jr. and Raup, D. M. 1986. Periodicity in marine extinction events. Pp. 336. In: Elliott, D., ed. Dynamics of Extinction. Wiley; Somerset, New Jersey.Google Scholar
Stanley, S. M. 1979. Macroevolution. 332 pp. W. H. Freeman & Co.; San Francisco.Google Scholar
Van Valen, L. M. 1984. A resetting of Phanerozoic community evolution. Nature. 307:5052.Google Scholar
Van Valen, L. M. 1985a. How constant is extinction? Evol. Theory. 7:93106.Google Scholar
Van Valen, L. M. 1985b. A theory of origination and extinction. Evol. Theory. 7:133142.Google Scholar
Van Valen, L. M. and Maiorana, V. C. 1985. Patterns of origination. Evol. Theory. 7:107125.Google Scholar