Abstract
The four original stipulations of the definition ofpunctuated equilzbrium (PE; Eldredge & Gould, 1972) are shown to be unsupported, and even contradicted, by the two evidential examples these authors supplied: the trilobite Phacops rana of the Middle Devonian, and the land snail Poectlozonites bermudensis of Late Pleistocene Bermuda. The additional, much-discussed example of Bellamya unicolor and the accompanying suite of molluscan species of Pliocene-Recent African Lake Turkana, studied by Williamson, also fails to exemplify PE. In particular, the data produced for these cases appear to represent counterexamples to Mayr’s paradigm of peripatric speciation, embraced by Eldredge and Gould as the central effective mechanism of PE. The data actually illustrate instead a prevailingly centrifugal pattern of speciation that will accommodate and explain episodic aspects of microevolution in a more realistic way.
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