Immigration and in situ glacial survival of the low‐alpine Erinus alpinus (Scrophulariaceae)

It has been hypothesized that the subalpine Erinus alpinus survived the Pleistocene glaciation in southern French refugia peripheral to the Alps and postglacially immigrated to its northern Alpine distribution (tabula rasa hypothesis). However, E. alpinus is also known from nunataks in the northern Prealps. PCR–RFLP of the cpDNA revealed no variation, whereas AFLPs identified three phylogeographical groups among the 22 populations: (1) a central Swiss group, (2) a single central Swiss population on Mount Rigi, and (3) all other populations located to the west and east of the central Swiss group (west‐eastern populations). The population representing the putative French refugium was not distinct from the west‐eastern populations but was different from the populations of central Switzerland. We consider this support for locally restricted in situ survival of E. alpinus in the northern Prealps or nearby Jura mountains (dating back to 60–28 ky BP). However, the west‐eastern gene‐pool probably immigrated postglacially from southern France through the prealpine lowlands (not before 14.6 kyr BP), skirting central Switzerland. The near‐absence of gene flow among the central Swiss and the west‐eastern populations may be the reason why these historical genetic patterns are still detectable. © 2002 The Linnean Society of London, Biological Journal of the Linnean Society , 2002, 77, 87–103.