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Volatility and the Phanerozoic decline of background extinction intensity

Published online by Cambridge University Press:  08 February 2016

Norman L. Gilinsky*
Affiliation:
Department of Geological Sciences, Virginia Polytechnic Institute and State University, Blacksburg, Virginia 24061-0420

Abstract

The well-known decline of global background extinction intensity was caused by the sorting of higher taxonomic groups. Two factors were responsible. First, probabilities of familial origination and extinction in these groups (taxonomic orders) were highly correlated. Groups whose families had high probabilities of origination and extinction tended to have highly volatile diversity paths and, consequently, short life spans. Second, orders with high probabilities of familial origination and extinction were rarely replaced by new high-turnover orders. Thus, because high-turnover orders tended to become extinct without replacement, the global background extinction intensity declined. Since familial origination and extinction probabilities are correlated, global background origination intensity inevitably declined as well. As a consequence of these processes, virtually all groups of organisms now living have low probabilities of familial origination and extinction.

Simulations of branching evolution were used to obtain the expected relationships among probabilities (of origination and extinction), volatilities, and longevities for the entire range of possible probabilities, and these relationships were compared to those obtained from the empirical record. In the simulations, only the probabilities of origination and extinction were specified, so volatilities and clade longevities were determined entirely by the probabilities. The similarity between results obtained by simulation and those obtained by analysis of the empirical record further supports the inference that the observed decline of background extinction (and origination) intensity can be explained largely by the loss of high-probability groups to induced volatility.

Type
Research Article
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Allison, P. A., and Briggs, D. E. G. 1993. Paleolatitudinal sampling bias, Phanerozoic species diversity, and the end-Permian extinction. Geology 21:6568.2.3.CO;2>CrossRefGoogle Scholar
Bambach, R. K. 1977. Species richness in marine benthic habitats through the Phanerozoic. Paleobiology 3:152167.CrossRefGoogle Scholar
Bambach, R. K. 1983. Ecospace utilization and guilds in marine communities through the Phanerozoic. Pp. 719746in Tevesz, M. J. S. and McCall, P. L., eds. Biotic interactions in recent and fossil benthic communities. Plenum, New York.CrossRefGoogle Scholar
Bambach, R. K., and Sepkoski, J. J. Jr. 1992. Historical evolutionary information in the traditional Linnean hierarchy. Proceedings of the Fifth North American Paleontological Convention, Paleontological Society Special Publication no. 6, p. 16.Google Scholar
Bottjer, D. J., and Ausich, W. I. 1986. Phanerozoic development of tiering in soft substrata suspension-feeding communities. Paleobiology 12:400420.CrossRefGoogle Scholar
Boyajian, G. F. 1986. Phanerozoic trends in background extinction: consequences of an aging fauna. Geology 14:955958.2.0.CO;2>CrossRefGoogle Scholar
Eldredge, N. 1985. Unfinished synthesis: biological hierarchies and modern evolutionary thought. Oxford University Press, New York.Google Scholar
Flessa, K. W., and Jablonski, D. 1985. Declining Phanerozoic background extinction rates: effect of taxonomic structure? Nature (London) 313:216218.CrossRefGoogle Scholar
Foote, M. 1988. Survivorship analysis of Cambrian and Ordovician trilobites. Paleobiology 14:258271.CrossRefGoogle Scholar
Gilinsky, N. L. 1991a. Estimating probabilities of origination and extinction. Pp. 237255in Dudley, E. C., ed. The unity of evolutionary biology. Dioscorides Press, Portland, Ore.Google Scholar
Gilinsky, N. L. 1991b. The pace of taxonomic evolution. Pp. 157174in Gilinsky, N. L. and Signor, P. W., eds. Analytical paleobiology. Short courses in paleontology, no. 4. The Paleontological Society, Knoxville, Tenn.Google Scholar
Gilinsky, N. L., and Bambach, R. K. 1987. Asymmetrical patterns of origination and extinction in higher taxa. Paleobiology 13:427445.CrossRefGoogle Scholar
Gilinsky, N. L., and Good, I. J. 1991. Probabilities of origination and extinction of families of marine life. Paleobiology 17:145166.CrossRefGoogle Scholar
Gould, S. J. 1985. The paradox of the first tier: an agenda for paleobiology. Paleobiology 11:212.CrossRefGoogle Scholar
Gould, S. J., Raup, D. M., Sepkoski, J. J. Jr., Schopf, T. J. M., and Simberloff, D. S. 1977. The shape of evolution: a comparison of real and random clades. Paleobiology 3:2340.CrossRefGoogle Scholar
Harland, W. B., Armstrong, R. L., Cox, A. V., Craig, L. E., Smith, A. G., and Smith, D. G. 1990. A geologic time scale 1989. Cambridge University Press.Google Scholar
Mayr, E. 1970. Populations, species, and evolution. Belknap Press, Cambridge, Mass.Google Scholar
Palmer, A. R. 1983. The decade of North American geology 1983 geologic time scale. Geology 11:503504.2.0.CO;2>CrossRefGoogle Scholar
Pease, C. M. 1992. On the declining extinction and origination rates of fossil taxa. Paleobiology 18:8992.CrossRefGoogle Scholar
Raup, D. M. 1978. Cohort analysis of generic survivorship. Paleobiology 4:115.CrossRefGoogle Scholar
Raup, D. M. 1979. Biases in the fossil record of species and genera. Bulletin of the Carnegie museum of Natural History 13:8591.Google Scholar
Raup, D. M. 1985. Mathematical models of cladogenesis. Paleobiology 11:4252.CrossRefGoogle Scholar
Raup, D. M., and Boyajian, G. E. 1988. Patterns of generic extinction in the fossil record. Paleobiology 14:109125.CrossRefGoogle ScholarPubMed
Raup, D. M., and Sepkoski, J. J. Jr. 1982. Mass extinctions in the marine fossil record. Science 215:15011503.CrossRefGoogle ScholarPubMed
Raup, D. M., Gould, S. J., Schopf, T. J. M., and Simberloff, D. S. 1973. Stochastic models of phylogeny and the evolution of diversity. Journal of Geology 81:525542.CrossRefGoogle Scholar
Sepkoski, J. J. Jr. 1981. A factor analytic description of the Phanerozoic marine fossil record. Paleobiology 7:3653.CrossRefGoogle Scholar
Sepkoski, J. J. Jr. 1984. A kinetic model of Phanerozoic taxonomic diversity. III. Post-Paleozoic families and multiple equilibria. Paleobiology 10:246267.CrossRefGoogle Scholar
Sepkoski, J. J. Jr. 1992. A compendium of fossil marine animal families, 2d ed.Milwaukee Public Museum Contributions in Biology and Geology 83.Google ScholarPubMed
Sepkoski, J. J. Jr. 1993. Ten years in the library: new data confirm paleontological patterns. Paleobiology 19:4351.CrossRefGoogle ScholarPubMed
Sepkoski, J. J. Jr., and Kendrick, D. C. 1993. Numerical experiments with model monophyletic and paraphyletic taxa. Paleobiology 19:168184.CrossRefGoogle ScholarPubMed
Sepkoski, J. J. Jr., Bambach, R. K., Raup, D. M., and Valentine, J. W. 1981. Phanerozoic marine diversity and the fossil record. Nature (London) 293:435437.CrossRefGoogle Scholar
Stanley, S. M. 1979. Macroevolution. W. H. Freeman, San Francisco.Google Scholar
Stanley, S. M. 1986. Anatomy of a regional mass extinction: Plio-Pleistocene decimation of the western Atlantic bivalve fauna. Palaios 1:1736.CrossRefGoogle Scholar
Stanley, S. M. 1990. The general correlation between rate of speciation and rate of extinction: fortuitous causal linkages. Pp. 103127in Ross, R. M. and Allmon, W. D., eds. Causes of evolution: a paleontological perspective. University of Chicago Press.Google Scholar
Thayer, C. W. 1983. Sediment-mediated biological disturbance and the evolution of marine benthos. Pp. 479625in Tevesz, M. J. S. and McCall, P. L., eds. Biotic interactions in recent and fossil benthic communities. Plenum, New York.CrossRefGoogle Scholar
Van Valen, L. 1984. A resetting of Phanerozoic community evolution. Nature (London) 307:5052.CrossRefGoogle Scholar
Van Valen, L. 1985a. How constant is extinction? Evolutionary Theory 7:93106.Google Scholar
Van Valen, L. 1985b. A theory of origination and extinction. Evolutionary Theory 7:133142.Google Scholar
Van Valen, L. 1987. Comment (on “Phanerozoic trends in background extinction: consequence of an aging fauna”). Geology 15:875876.2.0.CO;2>CrossRefGoogle Scholar
Van Valen, L. M., and Maiorana, V. C. 1985. Patterns of origination. Evolutionary Theory 7:107125.Google Scholar
Vermeij, G. J. 1987. Evolution and escalation. An ecological history of life. Princeton University Press.Google Scholar
Vrba, E. S., and Eldredge, N. 1984. Individuals, hierarchies and processes: towards a more complete evolutionary theory. Paleobiology 10:146171.CrossRefGoogle Scholar