1986
DOI: 10.1017/s0094837300013658
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Tempo of evolution in a Neogene bryozoan: rates of morphologic change within and across species boundaries

Abstract: Inadequacies in stratigraphic resolution or completeness can make true rates of morphologic change through geologic time impossible to estimate precisely. However, relative rates may be sufficient to test whether the tempo of change within species can account for morphologic differences across species boundaries, and hence to distinguish between gradual and punctuated patterns of evolution. The conditions under which these patterns can be distinguished statistically are explored by simulating varying degrees o… Show more

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Cited by 146 publications
(185 citation statements)
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“…Maynard Smith, in 1966, Kondrashov (1983a, 1983b, 1986 and others have developed a number of models of speciation in sympatry, due to habitat shift or behavioral isolation. The conditions necessary for speciation in sympatry to go forward are rather restrictive.…”
Section: Systematics and Taxonomy]mentioning
confidence: 99%
See 1 more Smart Citation
“…Maynard Smith, in 1966, Kondrashov (1983a, 1983b, 1986 and others have developed a number of models of speciation in sympatry, due to habitat shift or behavioral isolation. The conditions necessary for speciation in sympatry to go forward are rather restrictive.…”
Section: Systematics and Taxonomy]mentioning
confidence: 99%
“…There are several studies of punctuated fossil sequences; Cheetham's (1986) work on the Miocene to Pliocene bryozoans is a well-worn example. Cheetham shows almost static lineages coexisting with lineages that appear, from polygenetic analysis, to be their descendants.…”
Section: Rates Of Evolution and Punctuated Equilibriummentioning
confidence: 99%
“…It is noteworthy that Cheetham (1986) arrived at the same number through different criteria, using five observations per specimen in a study of cheilostome bryozoans.…”
Section: Evaluation Of Datamentioning
confidence: 99%
“…10 and 11). This is despite quantitative estimates of the probability of completeness of the fossil record of nearly 100 percent and near maximum probability of the occurrence of ancestors of PA¼0.5 (Foote, 1996;Cheetham andJackson, 1998, 2000). Resolution of this issue will require cladistic reexamination of eight or more Eocene to Recent principally eastern Atlantic species traditionally assigned to Cupuladria but intermediate in a number of characters between Discoporella and Cupuladria (Lagaaij, 1963;Cook, 1965aCook, , 1965bCook, , 1985Boardman et al, 1970;Cadée, 1975).…”
mentioning
confidence: 99%