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3 The New York Years (1931–1953)

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A Modern Unified <strong>The</strong>ory of Evolution 213<br />

(1985) “recognition concept” of species. Evolutionists need to distinguish between<br />

genetic isolation, reproductive isolation, and ecological isolation of species (Bock<br />

1979, 1986, 2004d). Genetic isolation must be complete before the neospecies establish<br />

secondary contact in order not to hybridize, but reproductive and ecological<br />

isolation may be perfected in sympatry through natural selection and mutual<br />

selective demands.<br />

<strong>The</strong> “horizontal” biological species concept refers to genetically separated<br />

groups of populations which live during a particular time plane like the Present or<br />

any time plane of the geological past (Fig. 5.3). Under this concept, species have,<br />

strictly speaking, no origin, age or duration. <strong>The</strong>y represent horizontal “cross sections”<br />

of vertical phyletic species lineages in the time dimension (Bock 1979, 1986,<br />

1992a; Szalay and Bock 1991). A phyletic lineage is the continuum of a species<br />

intimeanddocumentsitshistory;itdoesnotparticipateinthedevelopmentof<br />

species (populations do). <strong>The</strong> “phyletic lineage” and the “species” should be kept<br />

separate conceptually.<br />

Mayr’s (1931b, 1942e) consistent application of the superspecies concept in his<br />

systematic work was of general significance because it permitted the combination<br />

of several closely related geographical representatives under one superspecific<br />

name without reducing these allo- or paraspecies to subspecies status. Such<br />

‘superlumping’ had been advocated by several workers (e.g., Kleinschmidt and<br />

Fig.5.3. Several imaginary phyletic lineages illustrate “species” limits under the cladistic<br />

concept (clad.) and the paleontological concept (pal.). Schematic representation. Groups<br />

of populations representing the various lineages at particular time levels (t1–t4) aredifferent<br />

biological species (oval circles). Vertical scale–geological time; horizontal scale–<br />

morphological and other biological changes. A–L represent paleontological “species,” except<br />

C–F, which together are one paleontological “species” but represent 2 cladistic “species.”<br />

<strong>The</strong> current time level is t4

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