Post-Cambrian Trilobite Diversity and Evolutionary Faunas

Author:

Adrain Jonathan M.12,Fortey Richard A.12,Westrop Stephen R.12

Affiliation:

1. J. M. Adrain and R. A. Fortey, Department of Palaeontology, Natural History Museum, Cromwell Road, London SW7 5BD, UK.

2. S. R. Westrop, Oklahoma Museum of Natural History and School of Geology and Geophysics, University of Oklahoma, Norman, OK 73019, USA.

Abstract

A cluster analysis of the stratigraphic distribution of all Ordovician trilobite families, based on a comprehensive taxonomic database, identified two major faunas with disjunct temporal diversity trends. The Ibex Fauna behaved as a cohort, declining through the Ordovician and disappearing at the end-Ordovician mass extinction. In contrast, the Whiterock Fauna radiated rapidly during the Middle Ordovician and gave rise to all post-Ordovician trilobite diversity. Its pattern of diversification matches that of the Paleozoic Evolutionary Fauna; hence, trilobites were active participants in the great Ordovician radiations. Extinction patterns at the end of the Ordovician are related to clade size: Surviving trilobite families show higher genus diversity than extinguished families.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference40 articles.

1. A. T. Thomas and R. A. Fortey in Atlas of Invertebrate Macrofossils J. W. Murray Ed. (Longman London 1985) pp. 199-229

2. R. A. Robison in Fossil Invertebrates R. S. Boardman A. H. Cheetham A. J. Rowell Eds. (Blackwell Palo Alto CA 1987) pp. 221-241.

3. J. J. Sepkoski Jr. Milwaukee Public Mus. Contrib. Biol. Geol. 83 1 (1992).

4. The full data set has not yet been published but preliminary plots are given by J. J. Sepkoski Jr. in (22) pp. 393–396.

5. ___ Paleobiology 7 36 (1981).

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