Hostname: page-component-8448b6f56d-sxzjt Total loading time: 0 Render date: 2024-04-24T07:25:38.963Z Has data issue: false hasContentIssue false

Testing the Darwinian legacy of the Cambrian radiation using trilobite phylogeny and biogeography

Published online by Cambridge University Press:  20 May 2016

Bruce S. Lieberman*
Affiliation:
Department of Geology, University of Kansas, Lawrence 66045

Abstract

Since the publication of Darwin (1859), the biological meaning of the Cambrian radiation has been debated. Most commentators agree, however, that the Cambrian radiation is fundamentally a time of major metazoan cladogenesis. In and of itself this does not necessarily mean that unique evolutionary processes operated during the Cambrian radiation. Phylogenetic analysis has been used to study the tempo of speciation during the radiation, and thus far there is no need to invoke special rules relating to the tempo of evolution. Instead, what seems unique about the Cambrian radiation is its place as an important episode in the history of life—that is, as the first major radiation of the Metazoa. Although the tempo of evolution during the Cambrian radiation may not have been uniquely high, there were largely unique tectonic events that transpired during the late Neoproterozoic and Early Cambrian, such as extensive cratonic fragmentation. Biogeographic analysis of Early Cambrian olenelloid trilobites reveals that these tectonic events powerfully influenced evolutionary and distributional patterns in this diverse and abundant trilobite group. This emphasizes the importance of physical earth history in generating evolutionary patterns. In the general study of macroevolutionary patterns and processes, earth history phenomena emerge as powerful forces influencing the history of life and provide insights into evolution that can best be inferred by paleontological data.

Type
Research Article
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

Bengston, S., and Yue, Z. 1997. Fossilized metazoan embryos from the earliest Cambrian. Science, 277:16451648.Google Scholar
Bowler, P. J. 1996. Life's Splendid Drama. University of Chicago Press, Chicago, 525 p.Google Scholar
Briggs, D. E. G., Fortey, R. A., and Wills, M. A. 1992. Morphological disparity in the Cambrian. Science, 256:16701673.Google Scholar
Brooks, D. R., and McLennan, D. A. 1991. Phylogeny, Ecology, and Behavior. University of Chicago Press, Chicago, 434 p.Google Scholar
Browne, J. 1983. The Secular Ark: Studies in the History of Biogeography. Yale University Press, New Haven, Connecticut, 273 p.Google Scholar
Dalziel, I. W. D. 1991. Pacific margins of Laurentia and East Antarctica-Australia as a conjugate rift pair: evidence and implications for an Eocambrian supercontinent. Geology, 19:598601.Google Scholar
Dalziel, I. W. D. 1997. Neoproterozoic-Paleozoic geography and tectonics: review, hypothesis, and environmental speculation. Geological Society of America Bulletin, 109:1642.2.3.CO;2>CrossRefGoogle Scholar
Darwin, C. 1859. On the Origin of Species by Means of Natural Selection; or the Preservation of Favored Races in the Struggle for Life. (Reprinted 1st Edition) Harvard University Press, Cambridge, Massachusetts, 502 p.Google Scholar
Darwin, C. 1872. On the Origin of Species by Natural Selection; or the Preservation of Favored Races in the Struggle for Life. (Reprinted 6th Edition) New American Library, 479 p.Google Scholar
Davidson, E. H., Peterson, K. J., and Cameron, R. A. 1995. Origin of bilaterian body plans: evolution of developmental regulatory mechanisms. Science, 270:13191325.Google Scholar
Edgecombe, G. D. 1992. Trilobite phylogeny and the Cambrian-Ordovician “event”: a cladistic reappraisal, p. 144177. In Novacek, M. J. and Wheeler, Q. D., (eds.), Extinction and Phylogeny. Columbia University Press, New York.Google Scholar
Eldredge, N. 1979. Alternative approaches to evolutionary theory. Bulletin of the Carnegie Museum of Natural History, 13:719.Google Scholar
Eldredge, N. 1985. Unfinished Synthesis. Oxford University Press, New York, 237 p.Google Scholar
Eldredge, N. 1989. Macroevolutionary Dynamics. McGraw Hill, New York, 226 p.Google Scholar
Eldredge, N., and Cracraft, J. 1980. Phylogenetic Patterns and the Evolutionary Process: Method and Theory in Comparative Biology. Columbia University Press, New York, 349 p.Google Scholar
Eldredge, N., and Gould, S. J. 1972. Punctuated equilibria: an alternative to phyletic gradualism, p. 82115. In Schopf, T. J. M., (ed.), Models in Paleobiology. Freeman, Cooper and Co., San Francisco, California.Google Scholar
Fortey, R. A., Briggs, D. E. G., and Wills, M. A. 1996. The Cambrian evolutionary ‘explosion': decoupling cladogenesis from morphological disparity. Biological Journal of the Linnaean Society, 57:1333.Google Scholar
Gould, S. J. 1989. Wonderful Life. W. W. Norton, New York, 347 p.Google Scholar
Gould, S. J. 1990. Speciation and sorting as the source of evolutionary trends, or “things are seldom what they seem,” p. 3-27. In McNamara, K. J., (ed.), Evolutionary Trends. Belhaven Press, London.Google Scholar
Gould, S. J. 1991. The disparity of the Burgess Shale arthropod fauna and the limits of cladistic analysis: why we must strive to quantify morphospace. Paleobiology, 17:411423.Google Scholar
Gould, S. J. 1994. Tempo and mode in the macroevolutionary reconstruction of Darwinism. Proceedings of the National Academy of Sciences, U.S.A., 91:67646771.Google Scholar
Hallam, A. 1998. Speciation patterns and trends in the fossil record. Geobios, 30:921930.Google Scholar
Hoffman, P. H. 1991. Did the breakout of Laurentia turn Gondwanaland inside out? Science, 252:14091413.Google Scholar
Hughes, N. C. 1991. Morphological plasticity and genetic flexibility in a Cambrian trilobite. Geology, 19:913916.Google Scholar
Knoll, A. H. 1991. End of the Proterozoic eon. Scientific American, 265:6473.CrossRefGoogle ScholarPubMed
Knoll, A. H. 1996. Daughter of time. Paleobiology, 22:17.Google Scholar
Knoll, A. H., Bambach, R. K., Canfield, D. E., and Grotzinger, J. P. 1996. Comparative earth history and late permian mass extinction. Science, 273:452457.Google Scholar
Lieberman, B. S. 1997. Early Cambrian paleogeography and tectonic history: a biogeographic approach. Geology, 25:10391042.Google Scholar
Lieberman, B. S. 1998. Cladistic analysis of the Early Cambrian olenelloid trilobites. Journal of Paleontology, 72:5978.Google Scholar
Lieberman, B. S. In press. Systematic Revision of the Olenelloidea (Trilobita, Cambrian), and Patterns of Evolution in Trilobites During the Cambrian Radiation. Bulletin of the Yale University Peabody Museum Natural History.Google Scholar
Lieberman, B. S., and Eldredge, N. 1996. Trilobite biogeography in the Middle Devonian: geological processes and analytical methods. Paleobiology, 22:6679.Google Scholar
Matthew, W. D. 1928. Outline and General Principles of the History of Life. University of California Press, Berkeley, 253 p.Google Scholar
Matthew, W. D. 1939. Climate and Evolution. (2nd Edition) New York Academy of Sciences, New York, 223 p.Google Scholar
Mayr, E. 1982. The Growth of Biological Thought. Harvard University Press, Cambridge, 974 p.Google Scholar
Moores, E. M. 1991. Southwest U.S.-East Antarctic (SWEAT) connection: a hypothesis. Geology, 19:425428.2.3.CO;2>CrossRefGoogle Scholar
Raff, R. A. 1996. The Shape of Life. University of Chicago Press, Chicago, 520 p.Google Scholar
Sepkoski, J. J. Jr. 1979. A kinetic model of Phanerozoic taxonomic diversity II. Early Phanerozoic families and multiple equilibria. Paleobiology, 5:222251.Google Scholar
Signor, P. W., and Lipps, J. H. 1992. Origin and early radiation of the Metazoa, p. 323. In Lipps, J. H. and Signor, P. W. (eds.), Origin and Early Evolution of the Metazoa. Plenum Press, New York.Google Scholar
Simpson, G. G. 1944. Tempo and Mode in Evolution. Columbia University Press, New York, 237 p.Google Scholar
Smith, A. B. 1994. Systematics and the Fossil Record: Documenting Evolutionary Patterns. Blackwell Scientific, Boston, 223 p.Google Scholar
Smith, L. H. 1998. Species level phenotypic variation in lower Paleozoic trilobites. Paleobiology, 24:1736.Google Scholar
Stanley, S. M. 1979. Macroevolution: Pattern and Process. W. H. Freeman, San Francisco, California, 332 p.Google Scholar
Stanley, S. M., Signor, P. W. III, Lidgard, S., and Karr, A. F. 1981. Natural clades differ from “random” clades: simulations and analyses. Paleobiology, 7:115127.Google Scholar
Torsvik, T. J., Smethurst, M. A., Meert, J. G., van der Voo, R., McKerrow, W. S., Brasier, M. D., Sturt, B. A., and Walderhaug, H. J. 1996. Continental break-up and collision in the Neoproterozoic and Paleozoic—a tale of Baltica and Laurentia. Earth Science Reviews, 40:229258.Google Scholar
Vrba, E. S. 1980. Evolution, species and fossils: how does life evolve? South African Journal of Science, 76:6184.Google Scholar
Vrba, E. S. 1989. Levels of selection and sorting with special reference to the species level. Oxford Surveys in Evolutionary Biology, 6:111168.Google Scholar
Vrba, E. S. 1992. Mammals as a key to evolutionary theory. Journal of Mammalogy, 73:128.Google Scholar
Vrba, E. S., and Eldredge, N. 1984. Individuals, hierarchies and processes: Toward a more complete evolutionary theory. Paleobiology, 10:146171.Google Scholar
Wiley, E. O. 1979. An annotated Linnaean hierarchy, with comments on natural taxa and competing systems. Systematic Zoology, 28:308337.Google Scholar
Wray, G. A., Levinton, J. S., and Shapiro, L. H. 1996. Molecular evidence for deep Precambrian divergences among metazoan phyla. Science, 274:568573.Google Scholar
Xiao, S., Zhang, Y., and Knoll, A. H. 1998. Three-dimensional preservation of algae and animal embryos in a Neoproterozoic phosphorite. Nature, 391:553558.Google Scholar
Young, G. M. 1992. Late Proterozoic stratigraphy and the Canada-Australia connection. Geology, 20:215218.2.3.CO;2>CrossRefGoogle Scholar