Abstract

Glacial refugia of alpine and subnival biota have been intensively studied in the European Alps but the fate of forests and their understory species in that area remains largely unclear. In order to fill this gap, we aimed at disentangling the spatiotemporal diversification of disjunctly distributed black hellebore Helleborus niger (Ranunculaceae). We applied a set of phylogeographic analyses based on restriction-site associated DNA sequencing (RADseq) data and plastid DNA sequences to a range-wide sampling of populations. These analyses were supplemented with species distribution models generated for the present and the Last Glacial Maximum (LGM). We used exploratory analyses to delimit genomically coherent groups and then employed demographic modeling to reconstruct the history of these groups. We uncovered a deep split between two major genetic groups with western and eastern distribution within the Southern Limestone Alps, likely reflecting divergent evolution since the mid-Pleistocene in two glacial refugia situated along the unglaciated southern margin of the Alps. Long-term presence in the Southern Limestone Alps is also supported by high numbers of private alleles, elevated levels of nucleotide diversity and the species’ modeled distribution at the LGM. The deep genetic divergence, however, is not reflected in leaf shape variation, suggesting that the morphological discrimination of genetically divergent entities within H. niger is questionable. At a shallower level, populations from the Northern Limestone Alps are differentiated from those in the Southern Limestone Alps in both RADseq and plastid DNA data sets, reflecting the North-South disjunction within the Eastern Alps. The underlying split was dated to ca. 0.1 mya, which is well before the LGM. In the same line, explicit tests of demographic models consistently rejected the hypothesis that the partial distribution area in the Northern Limestone Alps is the result of postglacial colonization. Taken together, our results strongly support that forest understory species such as H. niger have survived the LGM in refugia situated along the southern, but also along the northern or northeastern periphery of the Alps. Being a slow migrator, the species has likely survived repeated glacial-interglacial circles in distributional stasis while the composition of the tree canopy changed in the meanwhile.

Highlights

  • The climatic changes during the Quaternary have had a major impact on the distribution of many plant and animal species by inducing shifts, expansions, contractions, and fragmentations of ranges as well as population extirpations (Comes and Kadereit, 1998; Hewitt, 2001; Petit et al, 2003)

  • The present study aims at shedding light on the underexplored biogeographic history of the forest vegetation of the European Alps by disentangling the spatiotemporal diversification of the disjunctly distributed, frequent, and abundant forest understory plant Helleborus niger, the black hellebore

  • Bayesian population clustering analysis based on 1,074 unlinked single nucleotide polymorphisms (SNPs) (Supplementary Table 2) resulted in the detection of two allopatrically distributed genetic groups (Figure 3A; Supplementary Figure 3), the Western Group distributed in the western part of the Southern Limestone Alps and the Eastern Group distributed in the eastern parts of the Northern and Southern Limestone Alps, from where it extends to the northwestern Balkan Peninsula

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Summary

Introduction

The climatic changes during the Quaternary have had a major impact on the distribution of many plant and animal species by inducing shifts, expansions, contractions, and fragmentations of ranges as well as population extirpations (Comes and Kadereit, 1998; Hewitt, 2001; Petit et al, 2003). In extensively glaciated mountain ranges such as the European Alps, species were forced into refugia during cold periods, from where they (re)colonized deglaciated areas during warmer periods including the Holocene (Schönswetter et al, 2005). The particular tectonic structure confers that calcicolous species, which are distributed in both the Northern and the Southern Limestone Alps, were either present in refugia adjacent to or overlapping with both areas during the last glacial period (Merxmüller, 1952, 1953, 1954; Tribsch and Schönswetter, 2003), or colonized one area from the other after the LGM (Schneeweiss and Schönswetter, 2010). Large-scale genetic exchange between both areas has likely been limited because of the scarcity of suitable substrate in the intervening siliceous Central Eastern Alps that acted as a strong barrier; in addition, any hypothetical populations in the Central Eastern Alps were extirpated during cold stages due to the area’s extensive glaciation (Ivy-Ochs et al, 2008)

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