Abstract

A MAJOR area of speculation in palaeobiology is the search for the “causes” of massive cross-group extinctions such as that at the end of the Cretaceous. A controversial recent addition to the literature on the phenomenon of extinction itself is the work of Van Valen1, who attempts to show that extinctions are stochastically constant over time for given groups of organisms. Lacking from Van Valen's study of group survivorship, however, is consideration of the history of diversification within each group. In an empirical study I have attempted to demonstrate features common to the diversifications of lower vertebrates and other organisms.

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