Paleobiology, 4(2), 1978, pp. 201-202 A test for evolutionary equilibrium revisited Graham A. Mark, Department of Ecology and Evolution, State University of New York at Stony Brook, Stony Brook, New York 11794 Karl W. Flessa, Department of Geosciences, University of Arizona, Tucson, Arizona 85721 Accepted: February 2,1978 Cowen and Stockton (1978) seem to agree with one of our main conclusions (Mark and Flessa 1977, p. 21): "Problems of ecological classification, taxonomic consistency and temporal and geographic scale need resolution before evolutionary equilibrium models can be more than heuristic." Their discussion points out other difficulties with hypotheses of evolutionary equilibrium and with tests for their validity. How much observed fluctuation is consistent with the notion of "equilibrium"? We tried to avoid this problem in our particular test. Our version of "the" equilibrium hypothesis postulated that "within biologically coherent regions and during times of relatively uniform environmental conditions, the number of taxa is usually constant" (Mark and Flessa 1977, p. 18). We stated the hypothesis this narrowly because we hoped to distinguish it conceptually from qualitatively different models, especially those picturing unlimited diversity and those in which diversity fluctuates unsystematically. To expect exact constancy is surely unreasonable, as Cowen and Stockton correctly insist and, in fact, our test was not this narrow. We tested for positive correlation, not for equality, because we were unwilling to specify just how constant an equilibrium must be. On a more technical level, Cowen and Stockton claim that the correlations that we found were methodological artifacts. As a point of formal statistical method, their "low number effect" is real enough. Their use of it to criticize our analysis, however, is misdirected. © 1978 The Paleontological Society. All rights reserved. Their error stems from their confusion of standing crop and turnover rates. We generated our sets of "net" originations and extinctions by eliminating short-ranging genera from consideration. Consequently, as Cowen and Stockton note, if our results indicate low diversity (as is the case throughout the Mesozoic and Cenozoic), then correspondingly low levels of "net" originations and extinctions (low turnover) are also necessary. Note, however, that actually existing low diversity does not require low turnover; low diversity can be maintained by high turnover if the taxa are short-ranging. Eliminating the short-ranging brachiopod genera prevented us from detecting high turnover in low diversity situations. We used this method anyway because, as we pointed out (p. 20), "By including genera which arose and vanished within the same time interval, the correlation of origination and extinction will increase, but this inflated correlation is not a consequence of a true evolutionary equilibrium among different genera." Evidently, an analysis of either gross or net data sets will produce unwanted biases. Cowen and Stockton incorrectly assume that high diversity (as in the Paleozoic) requires high turnover rates. But in fact, in either net or gross data sets, high diversity can be maintained by low levels of originations and extinctions (low turnover) provided the taxa are long-ranging. Thus, although intervals characterized by low diversity are artificially constrained to show low turnover, intervals of high diversity are not required to have high turnover. Cowen and Stockton's attempts to discredit the other correlations that we found are similarly incorrect. Our present intention is not, however, to defend the statistical or evolutionary importance of a correlation that explains, at best, only 16% of the variation in extinctions and originations. We are content to conclude that our test failed to find substantial evidence for evolutionary equilibria. Although Cowen and 0094-8873/78/0402-0009/$1.00 Downloaded from https:/www.cambridge.org/core. IP address: 88.99.165.207, on 12 Jul 2017 at 17:36:50, subject to the Cambridge Core terms of use, available at https:/www.cambridge.org/core/terms. https://doi.org/10.1017/S009483730000587X 202 MARK & FLESSA Stockton are concerned that our test was "so narrow that the predictions . . . [we] . . . made from it are denied" (p. 199), we caution against granting the hypothesis of an evolutionary equilibrium such flexibility that it is immune to contrary evidence. Literature Cited C O W E N , R. AND W. L. STOCKTON. evolutionary equilibria. 1978. Testing for Paleobiology. 4:195-200. MARK, G. A. AND K. W . FLESSA. 1977. A test for evolutionary equilibria: Phanerozoic brachiopods and Cenozoic mammals. Paleobiology. 3:17-22. S T U D E N T CONTEST In keeping with the aims of Paleobiology, we seek original essays on the following topics: 1. The problem(s) in biological paleontology most in need of intensive work over the next few years. 2. The role of technology in advancing paleontology. 3. The role of ideas in advancing paleontology. Essays in each category should be on the order of 20 to 40 typed pages (double spaced). Manuscripts must be received by December 31, 1978, and submission gives consent for the essay to be considered for publication in Paleobiology. An anonymous donor has made available $100.00 for the writer(s) of an essay in each category. Awards will be decided by a panel of three judges. One essay in each category will appear in Paleobiology. Any student interested is urged to submit an essay. No consideration will be given to whether a person is or is not a member of any of the paleontological societies. For purposes of the contest, manuscripts must be received not more than one year after the date of receipt of Ph.D. (or equivalent degree). An original and three copies of your essay(s) should be sent to: Editorial Office, Paleobiology, Dept. of Geophysical Sciences, University of Chicago, 5734 Ellis Avenue, Chicago, Illinois 60637. Downloaded from https:/www.cambridge.org/core. IP address: 88.99.165.207, on 12 Jul 2017 at 17:36:50, subject to the Cambridge Core terms of use, available at https:/www.cambridge.org/core/terms. https://doi.org/10.1017/S009483730000587X
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