Ice-age endurance: DNA evidence of a white spruce refugium in Alaska

• Published in: Proceedings of the National Academy of Sciences
• Main Authors: Anderson, Lynn L., Hu, Feng Sheng, Nelson, David M., Petit, Remy, Paige, Ken N.
• Other Authors: University of Illinois, University of Illinois System, Biodiversité, Gènes et Ecosystèmes (BioGeCo), Institut National de la Recherche Agronomique (INRA)-Université Sciences et Technologies - Bordeaux 1 (UB)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2006
• Subjects: REFUGIA; CHLOROPLAST; CLIMATIC CHANGE; BERINGIA; EPICEA; PICEA GLAUCA; ADN CHLOROPLASTIQUE; [SDV.BC]Life Sciences [q-bio]/Cellular Biology; Yukon; Ice Sheet; Alaska; Beringia; Siberia
• Online Access: https://hal.inrae.fr/hal-02667187; https://doi.org/10.1073/pnas.0605310103

International audience Paleorecords offer key information for evaluating model simulations of species migration in response to forecast climatic change. However, their utility can be greatly compromised by the existence of glacial refugia that are undetectable in fossil records (cryptic refugia). Despite several decades of investigation, it remains controversial whether Beringia, the largely unglaciated area extending from northeastern Siberia to the Yukon Territory, harbored small populations of certain boreal tree species during the last glaciation. Here, we present genetic evidence for the existence of a glacial refuge in Alaska that helps to resolve this long-standing controversy. We sequenced chloroplast DNA (cpDNA) of white spruce (Picea glauca), a dominant boreal tree species, in 24 forest stands across northwestern North America. The majority of cpDNA haplotypes are unique, and haplotype diversity is relatively high in Alaska, arguing against the possibility that this species migrated into the region from areas south of the Laurentide Ice Sheet after the end of the last glaciation. Thus, white spruce apparently survived long glacial episodes under climatic extremes in a heterogeneous landscape matrix. These results suggest that estimated rates of tree migration from fossil records may be too high and that the ability of trees to track anthropogenic warming may be more limited than previously thought