Volume 28, Issue 9 p. 1129-1136

Allozyme variation in Polyommatus coridon (Lepidoptera: Lycaenidae): identification of ice-age refugia and reconstruction of post-glacial expansion

Thomas Schmitt

Thomas Schmitt

Institut für Zoologie, Abt. V Ökologie, Saarstraße 21, D-55099 Mainz, Germany,

Institut für Biogeographie, Geozentrum, D-54286 Trier, Germany

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Alfred Seitz

Alfred Seitz

Institut für Zoologie, Abt. V Ökologie, Saarstraße 21, D-55099 Mainz, Germany,

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First published: 21 December 2001
Citations: 68
Dr Thomas Schmitt Institut für Biogeographie, Fachbereich VI, Geozentrum Gebäude H 857, D-54286 Trier, Germany. E-mail: [email protected]

Abstract

Aim

The effects of glacial disjunctions on intraspecific differentiations are in the focus of phylogeographical studies. Several studies investigate the consequences of post-glacial expansions from glacial refugia on the composition within major genetic lineages.

Location and methods

We analysed the geographical pattern of allozyme variation of twenty loci of Polyommatus coridon (Poda, 1761) (Lepidoptera: Lycaenidae) from thirty-six localities spread throughout large regions of its European range. A total of 1566 individuals were analysed.

Results

We obtained a significant genetic differentiation (FST 0.060 ± 0.007). Further analyses showed a division into two major genetic lineages with a mean genetic distance (Nei, 1978) of 0.041 (± 0.010 SD). Applying an AMOVA, more than three quarters of the variance between populations was between these lineages and less than one quarter within these lineages. Both genetic lineages showed a significant decline in the number of alleles from southern to northern populations. Furthermore, we found a contact zone of these two major genetic lineages in eastern Central Europe extending throughout north-eastern Germany, then following the mountain regions along the Czech-German border and passing through the eastern Alps in a north–south direction.

Main conclusions

We assume that this differentiation evolved during the last ice-age as a result of isolation in the Adriato- and the Ponto-Mediterranean region. The loss of genetic diversity from the south to the north within both lineages reflects the decline of diversity during the post-glacial expansion.

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