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Genetics, Vol. 169, 485-488, January 2005, Copyright © 2005
doi:10.1534/genetics.104.031971
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Center for Ecology and Evolutionary Biology, University of Oregon, Eugene, Oregon 97403-5289
1 Corresponding author: CEEB, 5289 University of Oregon, Eugene, OR 97403-5289.
E-mail: wyomya{at}aol.com
| ABSTRACT |
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This generation of additive from epistatic variation has been invoked to explain the increase in additive genetic variation for photoperiodic response among populations of the pitcher-plant mosquito, Wyeomyia smithii, dispersing along a latitudinal gradient into postglacial northern North America (HARD et al. 1992, 1993). HARD et al.'s argument was based on three observations and two fundamental assumptions. The observations were, first, that contrary to the expectations of directional selection on a latitudinal scale and stabilizing selection on a local scale, the additive genetic variance for photoperiodic response increased with latitude. Second, genetic differences in photoperiodic response between southern and northern populations involved differences in epistasis. Third, the contribution of different forms of digenic epistasis (additive x additive, additive x dominance, dominance x dominance) was unique to each cross. The latter observation was important because it implied stochastic reordering of genic interactions as would be expected as a consequence of random drift following independent founder events. The two assumptions were that postglacial dispersal had taken place by sequential founder events along a latitudinal gradient and that there is actually epistatic variation for photoperiodic response within populations. The first of these assumptions was supported by ARMBRUSTER et al. (1998) who showed that average heterozygosity at 10 allozyme loci decreased with latitude from the approximate southern limit of the Laurentide Ice Sheet (
40° N in New Jersey) northward. The second of these assumptions is the topic of the present article.
Hybridization experiments have revealed genetic differences attributable to epistasis among species (DOEBLEY et al. 1995) and among populations within species (HARD et al. 1993; LAIR et al. 1997; FENSTER and GALLOWAY 2000; GALLOWAY and FENSTER 2000; CARROLL et al. 2001, 2003). In theory, one might expect little epistatic variation within populations as selection should favor an optimal combination of alleles (WHITLOCK et al. 1995), but crosses between selected lines within populations reveal that such epistatic variation can exist (MATHER and JINKS 1982; CHEVERUD 2000). We use the latter approach to ask whether lines of W. smithii, selected for divergent photoperiodic response, differ in epistasis. W. smithii enters a larval dormancy that is initiated, maintained, and terminated by photoperiod (day length; BRADSHAW and LOUNIBOS 1977). The critical photoperiod is the length of day at which an individual switches between active development and dormancy and, in direct response to seasonal selection, increases with latitude and altitude of population origin (BRADSHAW and LOUNIBOS 1977; BRADSHAW et al. 2003). The range of W. smithii extends from the Gulf of Mexico to northern Canada. We collected mosquitoes from a mid-latitude locality along a stream meandering through a cedar swamp in the New Jersey Pine Barrens (40° N, locality "PB" of earlier studies from this lab). To increase independence of the replicate lines, we collected from three subpopulations within a 200-m radius of each other (BRADSHAW et al. 2003): "streamside" from along the stream itself; "backwater" from a backwater of the stream
100 m north of the first collection site; and "sandy bog" from a sandy bog
300 m to the west of the stream and separated from it by dry pine woodlands. We imposed divergent selection for long and short critical photoperiods and then crossed the selected lines from within each subpopulation (Table 1). We tested the specific prediction that, if there were genetic variation at epistatically acting loci in the original population, then genetic differences in photoperiodic response between selected lines derived from the same starting subpopulation should include epistasis.
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These distinct genetic fingerprints indicate that either population subdivision is occurring over a very fine microscale (e.g., FENSTER and GALLOWAY 2000) or unique genetic trajectories underlie similar phenotypic trajectories in response to a uniform selection gradient (e.g., TRAVISANO and LENSKI 1996), or a combination of these processes. Regardless of which of these processes is operating in W. smithii, our results show that diverse genetic trajectories of genic interactions are available to respond to short-term selection within a natural population of W. smithii. This availability may have contributed not only to the generation of additive genetic variation over millennial time scales since the recession of the Laurentide Ice Sheet, but also to the rapid genetic response of W. smithii to recent climate change (BRADSHAW and HOLZAPFEL 2001).
| ACKNOWLEDGEMENTS |
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