Late Quaternary climatic impact on the woodland strawberry genome: a perennial herb's tale
Toivainen, T.; Salonen, J. S.; Kirshner, J.; Lembinen, S.; De Kort, H.; Lyyski, A.; Edger, P. P.; Hilmarsson, H. S.; Hallsson, J. H.; Sargent, D. J.; Olbricht, K.; Sanchez-Sevilla, J. F.; Jaakola, L.; Stenberg, J. A.; Duralija, B.; Labokas, J.; Vare, H.; Salojarvi, J.; Auvinen, P.; Pose, D.; Albert, V. A.; Hytonen, T.
Show abstract
Exploring a species paleohistory is crucial for understanding its responsiveness to climatic events, identifying drivers of adaptation, and developing effective biodiversity conservation strategies in the face of ongoing climate change. We analyzed 200 genomes of the perennial herb woodland strawberry (Fragaria vesca L.) from across Europe and investigated the population structure and demographic history of the species during past geoclimatic events. We found a clear division of populations into western and eastern genetic clusters, indicative of distinct glacial refugia and adaptations to variation in temperature seasonality. The eastern core populations were several times larger (defined as effective population size, NE) than populations in other regions, showed no evidence of inbreeding, and were resilient to several glacial maxima. However, we observed decreasing NE and higher inbreeding in populations toward range edges, particularly in the north, where these individuals went through bottlenecks during glaciations. Population divergence suggested that western and eastern Europe were colonized from separate refugia in multiple waves during the Holocene, while the largest current populations from the northern Mediterranean to southern regions of the Nordic countries formed a connected population chain with gene flow between eastern core populations and western Europe, primarily occurring through Central Europe. Similar patterns of colonization and hybridization may have occurred during past interglacial periods, contributing to the present-day population structure of woodland strawberry. We suggest that the unprecedented resolution of the species climatic history across six glacial-interglacial cycles presented here holds the promise of transforming the general understanding of species paleohistory through geoclimatically tracing ancestral haplotypes.
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