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A revised macroevolutionary history for Ordovician — Early Silurian crinoids

Published online by Cambridge University Press:  08 April 2016

William I. Ausich  and
Shanan E. Peters
William I. Ausich
Affiliation:
Department of Geological Sciences, 125 South Oval, Ohio State University, Columbus, Ohio 43210. E-mail: [email protected]
Shanan E. Peters
Affiliation:
Department of Geological Sciences and Museum of Paleontology, University of Michigan, Ann Arbor, Michigan 48109. E-mail: [email protected]
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Abstract

Much of what is known about the long-term history of biodiversity and rates of taxonomic evolution in the fossil record derives from literature-based compilations of fossil stratigraphic ranges. It has been suggested that taxonomic and stratigraphic errors in these compilations are randomly distributed and, therefore, introduce no significant bias to macroevolutionary patterns. Here we compare a new, comprehensive global database of Ordovician and Early Silurian crinoids to Sepkoski's global genus compendium.

Approximately 44% of the crinoid genera resolved to substage in Sepkoski's compendium are taxonomically inaccurate (i.e., invalid, nomina dubia, or column genera) or have incorrect first and/or last occurrences. Errors in Sepkoski's compendium result from incomplete coverage of existing taxonomic work and incorrect stratigraphic correlations that, in some cases, are propagated throughout the taxonomic literature. Stratigraphic range errors are nonrandomly distributed among substages in Sepkoski's compendium. The result is underestimated richness in the Early Silurian and significantly overestimated rates of extinction in the Late Ordovician. There is no similar bias in Sepkoski's substage origination rates for crinoids.

At the stage-level of temporal resolution, Sepkoski's crinoid data are more accurate. In this case, only 32% of the compendium's crinoid genera contain some stratigraphic or taxonomic inaccuracy. However, errors still result in incorrect macroevolutionary patterns, particularly with respect to rate of origination in the Ashgill, which is significantly underestimated in Sepkoski's compendium. Genera described since the completion of Sepkoski's compendium have had relatively little effect on estimated rates of evolution at both stage and substage resolution.

These results suggest that macroevolutionary patterns among some taxa in Sepkoski's compilation may be significantly influenced by nonrandomly distributed taxonomic inaccuracies and stratigraphic range errors. In the case of the apparent end-Ordovician mass extinction among crinoids, the revised history reveals a dramatically reduced role for extinction at the substage-level of temporal resolution. At the stage level, Sepkoski's original compilation strongly exaggerates the excess of extinction over origination in the Ashgill. Although biases inherent in the stratigraphic record remain unaccounted for, removing taxonomic and stratigraphic errors in Sepkoski's compendium substantially changes our understanding of the nature of large-scale biotic change for an important Paleozoic taxon during the end-Ordovician.

Type
Articles
Information
Paleobiology , Volume 31 , Issue 3 , Summer 2005 , pp. 538 - 551
Copyright
Copyright © The Paleontological Society 

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References

Literature Cited

Adrain, J. M., and Westrop, S. R. 2000. An empirical assessment of taxic paleobiology. Science 289:110–112.Google Scholar
Allison, P. A., and Briggs, D. E. G. 1993. Exceptional fossil record: distribution of soft-tissue preservation through the Phanerozoic. Geology 21:527–530.Google Scholar
Alroy, J. 2002. How many named species are valid? Proceedings of the National Academy of Sciences USA 99:3706–3711.CrossRefGoogle ScholarPubMed
Alroy, J., Marshall, C. R., Bambach, R. K., Bezusko, K., Foote, M., Fürsich, F. T., Hansen, T. A., Holland, S. M., Ivany, L. C., Jablonski, D., Jacobs, D. K., Jones, D. C., Kosnik, M. A., Lidgard, S., Low, S., Miller, A. I., Novack-Gottshall, P. M., Olszewski, T. D., Patzkowsky, M. E., Raup, D. M., Sepkoski, J. J. Jr., Sommers, M. G., Wagner, P. J., and Webber, A. 2001. Effects of sampling standardization on estimates of Phanerozoic marine diversity. Proceedings of the National Academy of Sciences USA 98:6261–6266.Google Scholar
Ausich, W. I. 1984. Calceocrinids from the Early Silurian (Llandoverian) Brassfield Formation of southwestern Ohio. Journal of Paleontology 58:1167–1185.Google Scholar
Ausich, W. I. 1987. Revisions of Rowley's Ordovician (?) and Silurian crinoids from Missouri. Journal of Paleontology 61:563–578.Google Scholar
Ausich, W. I. 1998. Phylogeny of Arenig to Caradoc crinoids (phylum Echinodermata) and suprageneric classification of the Crinoidea. University of Kansas Paleontological Contributions, new series 9:1–36.Google Scholar
Ausich, W. I., and Copper, P. 2002. New latest Ordovician (Rawtheyan and Hirnantian) crinoid faunas from Anticosti Island, Quebec, Canada. Geological Society of America Abstracts with Programs 34:428.Google Scholar
Ausich, W. I., and Copper, P. 2003. Silurian (Llandovery) crinoids from Anticosti Island, Quebec, Canada. Geological Society of America Abstracts with Programs 35:162.Google Scholar
Ausich, W. I., Kammer, T. W., and Baumiller, T. K. 1994. Demise of the Middle Paleozoic crinoid fauna. Paleobiology 20:345–361.Google Scholar
Bassler, R. S., and Moodey, M. W. 1943. Bibliographic and faunal index of Paleozoic pelmatozoan echinoderms. Geological Society of America Special Paper 45.Google Scholar
Baumiller, T. K. 1993. Survivorship analysis of Paleozoic Crinoidea: effect of filter morphology on evolutionary rates. Paleobiology 19:304–321.Google Scholar
Bergström, S. M. 1971. Conodont biostratigraphy of the Middle and Upper Ordovician of Europe and eastern North America. Geological Society of America Memoir 127:83–157.Google Scholar
Botting, J. P. 2003. Llanvirn (Middle Ordovician) echinoderms from Llandegley Rocks, central Wales. Palaeontology 46:685–708.Google Scholar
Brower, J. C. 1982. Phylogeny of primitive calceocrinids. In Sprinkle, J., ed. Echinoderm faunas from the Bromide Formation (Middle Ordovician) of Oklahoma. University of Kansas Paleontological Contributions Monograph 1:90–110.Google Scholar
Brower, J. C. 2001. Flexible crinoids from the Upper Ordovician Maquoketa Formation of the northern midcontinent and the evolution of early flexible crinoids. Journal of Paleontology 75:370–382.Google Scholar
Cherns, L., and Wright, V. P. 2000. Missing molluscs as evidence of large-scale, early skeletal aragonite dissolution in a Silurian sea. Geology 28:791–794.Google Scholar
Culver, S. J., Buzas, M. A., and Collins, L. S. 1987. On the value of taxonomic standardization in evolutionary studies. Paleobiology 13:169–176.Google Scholar
Donovan, S. K. 1983. Tetrameric crinoid columnals from the Ordovician of Wales. Palaeontology 26:845–849.Google Scholar
Donovan, S. K. 1985. The Ordovician crinoid genus Caleidocrinus Waagen and Jahn, 1899. Geological Journal 20:109–121.Google Scholar
Donovan, S. K. 1988. The British Ordovician crinoid fauna. Lethaia 21:424.Google Scholar
Donovan, S. K. 1989. The significance of the British Ordovician crinoid fauna. Modern Geology 13:243–255.Google Scholar
Donovan, S. K. 2001. Evolution of Caribbean echinoderms during the Cenozoic: moving towards a complete picture using all of the fossils. Palaeogeography, Palaeoclimatology, Palaeoecology 106:177–192.CrossRefGoogle Scholar
Eckert, J. D. 1988. Late Ordovician extinction of North America and British crinoids. Lethaia 21:147–167.CrossRefGoogle Scholar
Eckert, J. D., and Brett, C. E. 2001. Early Silurian (Llandovery) crinoids from the Lower Clinton Group, western New York State. Bulletins of American Paleontology 360:1–88.Google Scholar
Foote, M. 2000. Origination and extinction components of taxonomic diversity: general problems. In Erwin, D. H. and Wing, S. L., eds. Deep time: Paleobiology's perspective. Paleobiology 26(Suppl. to No. 4):181–194.Google Scholar
Foote, M. 2001. Inferring temporal patterns of preservation, origination, and extinction from taxonomic survivorship analysis. Paleobiology 27:602–630.Google Scholar
Foote, M. 2003. Origination and extinction through the Phanerozoic: a new approach. Journal of Geology 111:125–148.Google Scholar
Fortey, R. A., Harper, D. A. T., Ingham, J. K., Owen, A. W., Parks, M. A., Rushton, A. W. A., and Woodcock, N. H. 2000. A revised correlation of Ordovician rocks in the British Isles. Geological Society of London Special Report 24:1–83.Google Scholar
Jeffery, C. H. 2001. Heart urchins at the Cretaceous/Tertiary boundary: a tale of two clades. Paleobiology 27:140–158.Google Scholar
Kolata, D. R. 1982. Camerates. In Sprinkle, J., ed. Echinoderm faunas from the Bromide Formation (Middle Ordovician) of Oklahoma. University of Kansas Paleontological Contributions Monograph 1:170–205.Google Scholar
Lane, N. G., and Moore, R. C. 1978. Superfamily Heterocrinacea. Pp. T549–T550in Ubaghs, G. et al. Echinodermata 2, Crinoidea. Part T ofMoore, R. C., and Teichert, K., eds. Treatise on invertebrate paleontology. Geological Society of America, Boulder, Colorado, and University of Kansas, Lawrence.Google Scholar
Leslie, S. A., and Bergström, S. M. 1997. Use of K-bentonite beds as time-planes for high-resolution lithofacies analysis and assessment of net rock accumulation rate: an example from the upper Middle Ordovician of eastern North America. Geological Society of America Special Paper 321:11–21.Google Scholar
Miller, A. I., and Foote, M. 1996. Calibrating the Ordovician radiation of marine life: implications for Phanerozoic diversity trends. Paleobiology 22:304–309.Google Scholar
Mitchell, C. E., Melchin, M. J., Sheets, H. D., Chen, X., and Fan, J.-X. 2002. Graptolite diversity dynamics during the end-Ordovician mass extinction: insights from multiple analytical approaches. Canadian Paleontology Conference Program and Abstracts 12:34–36.Google Scholar
Peters, S. E., and Foote, M. 2001. Biodiversity in the Phanerozoic: a reinterpretation. Paleobiology 27:583–601.Google Scholar
Peters, S. E., and Foote, M. 2002. Determinants of extinction in the fossil record. Nature 416:6879.Google Scholar
Raup, D. M. 1976. Species diversity in the Phanerozoic: an interpretation. Paleobiology 2:289–297.CrossRefGoogle Scholar
Raup, D. M., and Sepkoski, J. J. Jr. 1982. Mass extinctions in the marine fossil record. Science 215:1501–1503.Google Scholar
Ronov, A. B. 1978. The Earth's sedimentary shell. International Geology Review 24:1313–1363.Google Scholar
Ronov, A. B., Khain, V. E., Balukhovsky, A. N., and Seslavinsky, K. B. 1980. Quantitative analysis of Phanerozoic sedimentation. Sedimentary Geology 25:311–325.Google Scholar
Ross, R. J. Jr., Alder, F. J., Amsden, T. W., Bergström, D., Bergström, S. M., Carter, C., Churkin, M., Cressman, E. A., Derby, J. R., Dutro, J. T. Jr., Ethington, R. L., Finney, S. C., Fisher, D. W., Fisher, J. H., Harris, A. G., Hintze, L. F., Ketner, K. B., Kolata, D. L., Landing, E., Neuman, R. B., Sweet, W. C., Pojeta, J. Jr., Potter, A. W., Rader, E. K., Repetski, J. E., Shaver, R. H., Thompson, T. L., and Webers, G. F. 1982. The Ordovician System in the United States: correlation chart and explanatory notes. International Union of Geological Sciences 12:1–73.Google Scholar
Sepkoski, J. J. Jr. 1981. A factor analytic description of the Phanerozoic marine fossil record. Paleobiology 7:36–53.Google Scholar
Sepkoski, J. J. Jr. 1982. A compendium of fossil marine families. Milwaukee Public Museum Contribution to Biology and Geology No. 51.Google Scholar
Sepkoski, J. J. Jr. 1992. A compendium of fossil marine families, 2d ed. Milwaukee Public Museum Contribution to Biology and Geology No. 83.Google Scholar
Sepkoski, J. J. Jr. 2002. A compendium of fossil marine animal genera. Bulletins of American Paleontology 363:1–560.Google Scholar
Sepkoski, J. J. Jr., Bambach, R. K., Raup, D. M., and Valentine, J. W. 1981. Phanerozoic marine diversity and the fossil record. Nature 293:435–437.Google Scholar
Sheehan, P. M. 2001. The Late Ordovician mass extinction. Annual Review of Earth and Planetary Sciences 29:331–364.Google Scholar
Signor, P. W. III, and Lipps, J. H. 1982. Sampling bias, gradual extinction patterns and catastrophes in the fossil record. Geological Society of America Special Paper 190:291–296.Google Scholar
Smith, A. B. 2001. Large-scale heterogeneity of the fossil record: implications for Phanerozoic biodiversity studies. Philosophical Transactions of the Royal Society of London B 356:351–367.Google Scholar
Smith, A. B., and Jeffery, C. H. 2000. Changes in the diversity, taxic composition, and life-history patterns of echinoids over the past 145 million years. Pp. 181–194in Culver, S. J. and Rawson, P. F., eds. Biotic response to global change: the last 145 million years. Cambridge University Press, Cambridge.Google Scholar
Smith, A. B., Gale, A. S., and Monks, N. E. A. 2001. Sea-level change and rock-record bias in the Cretaceous: a problem for extinction and biodiversity studies. Paleobiology 27:241–253.2.0.CO;2>CrossRefGoogle Scholar
Smith, M. P., and Bjerreskov, M. 1994. The Ordovician System in Greenland. International Union of Geological Sciences Publication 29A:1–46.Google Scholar
Sprinkle, J., and Guensburg, T. E. 2004. Crinozoan, blastozoan, echinozoan, asterozoan, and homalozoan echinoderms. Pp. 266–290in Webby, B. D., Paris, F., Droser, M. L., and Percival, I. G., eds. The great Ordovician biodiversification event. Columbia University Press, New York.Google Scholar
Wang, S. C. 2003. On the continuity of background and mass extinction. Paleobiology 29:455–467.Google Scholar
Warn, J. M., and Strimple, H. L. 1977. The disparid inadunate superfamilies Homocrinacea and Cincinnaticrinacea (Echinodermata: Crinoidea), Ordovician—Silurian, North America. Bulletins of American Paleontology No. 72(296).Google Scholar
Webster, G. D. 2002. Bibliography and index of Paleozoic crinoids, coronates, and hemistreptocrinoids 1758–1999. Geological Society of America Special Paper 363 [online only].Google Scholar
Witzke, B. J., and Strimple, H. L. 1981. Early Silurian crinoids of eastern Iowa. Proceedings of the Iowa Academy of Science 88:101–137.Google Scholar
Wright, V. P., Cherns, L., and Hodges, P. 2003. Missing mollusks: field testing taphonomic loss in the Mesozoic through early large-scale aragonite dissolution. Geology 31:211–214.Google Scholar