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Dryad

A range-wide postglacial history of Swiss stone pine based on molecular markers and palaeoecological evidence

Gugerli, Felix1; Brodbeck, Sabine1; Lendvay, Bertalan2; Dauphin, Benjamin1; Bagnioli, Francesca3; van der Knaap, Willem O.4; Tinner, Willy4; Höhn, Maria5; Vendramin, Giovanni G.3; Morales-Molino, César4; Schwörer, Christoph4

Published Feb 20, 2023; Updated Aug 17, 2026 on Dryad. https://doi.org/10.5061/dryad.866t1g1v6

Data files

Abstract

Aim: Knowing a species’ response to historical climate shifts helps understanding its perspectives under global warming. We infer the hitherto unresolved postglacial history of Pinus cembra. Using independent evidence from genetic structure and demographic inference of extant populations, and from palaeoecological findings, we derive putative refugia and re-colonisation routes.

Location: European Alps and Carpathians.

Taxa: Pinus cembra.

Methods: We genotyped nuclear and chloroplast microsatellite markers in nearly 3,000 individuals from 147 locations across the entire natural range of P. cembra. Spatial genetic structure (Bayesian modelling) and demographic history (Approximate Bayesian Computation) were combined with palaeobotanical records (pollen, macrofossils) to infer putative refugial areas during the Last Glacial Maximum (LGM) and re-colonisation of the current range.

Results: We found distinct spatial genetic structure, despite low genetic differentiation even between the two disjunct mountain ranges. Nuclear markers revealed five genetic clusters aligned East–West across the range, while chloroplast haplotype distribution suggested nine clusters. Spatially congruent separation at both marker types highlighted two main genetic lineages in the East and West of the range. Demographic inference supported early separation of these lineages dating back to a previous interstadial or interglacial c. 210,000 years ago. Differentiation into five biologically meaningful genetic clusters likely established during post-glacial re-colonisation.

Main conclusions: Combining genetic and palaeoecological evidence suggests that P. cembra primarily survived the LGM in “cold period” refugia south of the Central European Alps and near the Carpathians, from where it expanded during the Late Glacial into its current Holocene “warm period” refugia. This colonisation history has led to the distinct East–West structure of five genetic clusters. The two main genetic lineages likely derived from ancient divergence during an interglacial or interstadial. The respective contact zone (Brenner line) matches a main biogeographic break in the European Alps also found in herbaceous alpine plant species.