Abstract
The causes of mass extinctions and the nature of biological selectivity at extinction events are central questions in palaeobiology. It has long been recognized, however, that the amount of sedimentary rock available for sampling may bias perceptions of biodiversity1,2,3,4,5,6,7 and estimates of taxonomic rates of evolution5,6,7,8. This problem has been particularly noted with respect to the principal mass extinctions5,6,7,8,9,10,11,12. Here we use a new compilation of the amount of exposed marine sedimentary rock to predict how the observed fossil record of extinction would appear if the time series of true extinction rates were in fact smooth. Many features of the highly variable record of apparent extinction rates within marine animals can be predicted on the basis of temporal variation in the amount of exposed rock. Although this result is consistent with the possibility that a common geological cause determines both true extinction rates and the amount of exposed rock, it also supports the hypothesis that much of the observed short-term volatility in extinction rates is an artefact of variability in the stratigraphic record.
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References
Raup, D. M. Taxonomic diversity during the Phanerozoic. Science 177, 1065–1071 (1972).
Raup, D. M. Species diversity in the Phanerozoic: an interpretation. Paleobiology 2, 289–297 (1976).
Miller, A. I. & Foote, M. Calibrating the Ordovician radiation of marine life: implications for Phanerozoic diversity trends. Paleobiology 22, 304–309 (1996).
Miller, A. I. in Deep Time: Paleobiology's Perspective (eds Erwin, D. H. & Wing, S. L.) Paleobiology 26(4), (Suppl.), 53–73 (2000).
Smith, A. B. Large-scale heterogeneity of the fossil record: implications for Phanerozoic biodiversity studies. Phil. Trans. R. Soc. Lond. B 356, 351–367 (2001).
Peters, S. E. & Foote, M. Biodiversity in the Phanerozoic: a reinterpretation. Paleobiology 27, 583–601 (2001).
Smith, A. B., Gale, A. S. & Monks, N. E. A. Sea-level change and rock-record bias in the Cretaceous: a problem for extinction and biodiversity studies. Paleobiology 27, 241–253 (2001).
Patterson, C. & Smith, A. B. Is the periodicity of extinction a taxonomic artefact? Nature 330, 248–251 (1987).
Raup, D. M. & Sepkoski, J. J. Jr Mass extinctions in the marine fossil record. Science 215, 1501–1503 (1982).
Pease, C. M. Biases in total extinction rates of fossil taxa. J. Theor. Biol. 130, 1–7 (1988).
MacLeod, N. & Keller, G. Hiatus distributions and mass extinctions at the Cretaceous/Tertiary boundary. Geology 19, 497–501 (1991).
Ross, C. A. & Ross, J. R. P. Foraminiferal zonation of late Paleozoic depositional sequences. Mar. Micropaleontol. 26, 469–478 (1995).
Holland, S. M. The stratigraphic distribution of fossils. Paleobiology 21, 92–109 (1995).
Holland, S. M. in Deep Time: Paleobiology's Perspective (eds Erwin, D. H. & Wing, S. L.) Paleobiology 26(4), (Suppl.) 148–163 (2000).
Foote, M. in Deep Time: Paleobiology's Perspective (eds Erwin, D. H. & Wing, S. L. ) Paleobiology 26(4), (Suppl.) 74–102 (2000).
Raup, D. M. Cohort analysis of generic survivorship. Paleobiology 4, 1–15 (1978).
Fortey, R. A. There are extinctions and extinctions: examples from the Lower Palaeozoic. Phil. Trans. R. Soc. Lond. B 325, 327–332 (1989).
Johnson, J. G. Extinction of perched faunas. Geology 2, 479–482 (1974).
Hallam, A. & Wignall, P. B. Mass extinctions and sea level changes. Earth Sci. Rev. 48, 217–250 (1999).
Alroy, J. et al. Effects of sampling standardization on estimates of Phanerozoic marine diversification. Proc. Natl Acad. Sci. USA 98, 6261–6266 (2001).
Foote, M. Inferring temporal patterns of preservation, origination, and extinction from taxonomic survivorship analysis. Paleobiology 27, 602–630 (2001).
Alvarez, W. et al. Extraterrestrial cause for the Cretaceous–Tertiary extinction: experimental results and theoretical interpretation. Science 208, 1095–1108 (1980).
Becker, L. et al. Impact event at the Permian–Triassic boundary: evidence from extraterrestrial noble gases in fullerenes. Science 287, 443–446 (2001).
Raup, D. M. Large-body impact and extinction in the Phanerozoic. Paleobiology 18, 80–88 (1992).
Keroher, G. C. et al. Lexicon of geologic names of the United States for 1936–1960. US Geol. Surv. Bull. 1200, 1–1434 (1967).
Sepkoski, J. J. Jr in Global Events and Event Stratigraphy (ed. Walliser, O. H.) 35–42 (Springer, Berlin, 1996).
Bowring, S. A. & Erwin, D. H. A new look at evolutionary rates in deep time: uniting paleontology and high-precision geochronology. GSA Today 8, 1–6 (1998).
Golonka, J. & Kiessling, W. in Phanerozoic Reef Patterns (eds Kiessling, W., Flügel, E. & Golonka, J.) 11–20 (SEPM Special Publication 27, Tulsa, 2002).
Van Valen, L. A resetting of Phanerozoic community evolution. Nature 307, 50–52 (1984).
Smith, A. B. & Patterson, C. The influence of taxonomic method on the perception of patterns of evolution. Evol. Biol. 23, 127–216 (1988).
Acknowledgements
We thank R. H. De Simone, E. G. Hunt, S. M. Kidwell, A. McGowan and A. M. Ziegler for discussions. D. B. Rowley provided rock area data. We also thank R. H. De Simone, J. Huss, D. Jablonski, A. I. Miller, D. M. Raup and A. B. Smith for reading the manuscript. This work was supported by the US Environmental Protection Agency, the US National Science Foundation, the Paleontological Society, and the Society of Sigma Xi.
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Peters, S., Foote, M. Determinants of extinction in the fossil record. Nature 416, 420–424 (2002). https://doi.org/10.1038/416420a
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DOI: https://doi.org/10.1038/416420a
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