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A provincial model of Phanerozoic marine diversity

Published online by Cambridge University Press:  08 April 2016

James W. Valentine ,
Theodore C. Foin  and
David Peart
James W. Valentine
Affiliation:
Department of Geological Sciences, University of California; Santa Barbara, California 93106
Theodore C. Foin
Affiliation:
Division of Environmental Studies, University of California; Davis, California 95616
David Peart
Affiliation:
Division of Environmental Studies, University of California; Davis, California 95616
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Abstract

Much new empirical evidence on the levels of Phanerozoic paleoprovinciality and of species diversity within paleocommunities now permits a reevaluation of marine diversity patterns. Data on paleoprovincial patterns are assembled from the literature and evaluated by means of a stochastic computer simulation model. The simulation is based on the statistics of modern patterns of diversity and endemism extrapolated conservatively to the paleoprovincial patterns and on estimates of species duration from the fossil record. The species diversities associated with the paleoprovincial patterns are then corrected for temporal changes in species packing in communities as determined by Bambach (1977) from studies of paleocommunities. The model thus has an empirical basis throughout. Furthermore it is free of biases that can arise due to the differential preservation of taxa in space and time.

The Paleozoic and Mesozoic were characterized by low provinciality and low average species diversity, on the order of 38,000 to 40,000 species, although there were significant fluctuations in standing diversities. In the Cenozoic, provinciality rose markedly, primarily through the appearance of latitudinal provincial chains, and average species diversity rose to about 240,000. Today it stands over 350,000; this is an order of magnitude greater than the Paleozoic average.

Type
Research Article
Information
Paleobiology , Volume 4 , Issue 1 , Winter 1978 , pp. 55 - 66
Copyright
Copyright © The Paleontological Society 

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