A species possesses an internal genetic structure that is compounded on the genetic architecture of constituent local populations. Each local population may be subtly unique in its coadapted gene ensemble, including the fine tuning of its genic regulatory system. More obviously and more approachably, populations may be differentiated in allele frequencies at single structural loci. This study describes the regional genetic patterns of allozyme loci in the amphipod crustacean Gammarus minus Say in a karst area of southeastern West Virginia. It is a part of an investigation of this species throughout the mid-Appalachian portion of its range, whose initial purpose is to map the genetic relationships among populations onto the highly structured environment of this region. Gammarus minus is highly differentiated in allele frequencies at several loci over short distances. There are at least three possible reasons for this fact. (1) As in other pericardians, females of G. minus brood their young in a ventral marsupium, and there is no specific migratory stage in the life history. (2) This species is principally found in freshwater lotic streams. Individual streams are essentially one-dimensional habitats from the viewpoint of gene flow, and drainage networks have a dimensionality between one and two (analogous to roads in Cavalli-Sforza and Bodmer, 1971). There is a greater decrease of genetic correlation with distance as dimensionality decreases in stepping-stone models of isotropic gene flow (Kimura and Weiss, 1964; Kimura and Maruyama, 1971). (3) G. minus in the Mid-Appalachians is largely confined to springs, spring runoff, and stream caves situated in carbonate strike valleys. Each local population is partially isolated from others in the local drainage system, and more profoundly isolated from populations in other streams and in other regions of carbonate outcrop. Holsinger (1969) discusses the Appalachian zoogeography of the Gammaridae in greater detail. In Virginia and West Virginia this species is widely distributed in the Ridge and Valley physiographic province and flanking areas, where its populations are mainly located in the headward reaches of feeders of trunk streams that trend northeast-southwest along linear strike valleys floored by Paleozoic limestones and dolomites. Some of these valleys are marked by karst development. A particularly extensive karst topography is displayed on the Greenbrier Limestone of Mississippian age in Pocahontas, Greenbrier, and Monroe Counties of southeastern West Virginia. This is a highly structured environment in which G. minus is found in three ecophenotypic forms. The primary aim of this study has been to map allozyme allele frequencies and levels of heterozygosity onto the structured topography to determine their concordance. The second goal has been to determine if the ecophenotypic
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