Multiple Pleistocene refugia for Arctic Bell-Heather revealed with genomic analyses of modern and historic plants

Cassandra Elphinstone*, Fernando Hernández, Marco Todesco, Jean Sébastien Légaré, Winnie Cheung, Paul C. Sokoloff, Annika Hofgaard, Casper T. Christiansen, Esther R. Frei, Esther Lévesque, Gergana N. Daskalova, Haydn J.D. Thomas, Isla H. Myers-Smith, Jacob A. Harris, Jeffery M. Saarela, Jeremy L. May, Joachim Obst, Julia Boike, Karin Clark, Katie MacIntoshKatlyn R. Betway-May, Liam Case, Mats P. Björkman, Michael L. Moody, Niels Martin Schmidt, Per Molgaard, Robert G. Björk, Robert D. Hollister, Roger D. Bull, Sofie Agger, Vincent Maire, Greg H.R. Henry, Loren H. Rieseberg

*Corresponding author for this work

Research output: Contribution to journal/Conference contribution in journal/Contribution to newspaperJournal articleResearchpeer-review

Abstract

Aim: Arctic plants survived the Pleistocene glaciations in unglaciated refugia. The number, ages, and locations of these refugia are often unclear. We use high-resolution genomic data from present-day and Little-Ice-Age populations of Arctic Bell-Heather to re-evaluate the biogeography of this species and determine whether it had multiple independent refugia or a single refugium in Beringia. Location: Circumpolar Arctic and Coastal British Columbia (BC) alpine. Taxon: Cassiope tetragona L., subspecies saximontana and tetragona, outgroup C. mertensiana (Ericaceae). Methods: We built genotyping-by-sequencing (GBS) libraries using Cassiope tetragona tissue from 36 Arctic locations, including two ~250- to 500-year-old populations collected under glacial ice on Ellesmere Island, Canada. We assembled a de novo GBS reference to call variants. Population structure, genetic diversity and demography were inferred from PCA, ADMIXTURE, fastsimcoal2, SplitsTree, and several population genomics statistics. Results: Population structure analyses identified 4–5 clusters that align with geographic locations. Nucleotide diversity was highest in Beringia and decreased eastwards across Canada. Demographic coalescent analyses dated the following splits with Alaska: BC subspecies saximontana (5 mya), Russia (~1.4 mya), Europe (>200–600 kya), and Greenland (~60 kya). Northern Canada populations appear to have formed during the current interglacial (7–9 kya). Admixture analyses show genetic variants from Alaska appear more frequently in present-day than historic plants on Ellesmere Island. Conclusions: Population and demographic analyses support BC, Alaska, Russia, Europe and Greenland as all having had independent Pleistocene refugia. Northern Canadian populations appear to be founded during the current interglacial with genetic contributions from Alaska, Europe and Greenland. We found evidence, on Ellesmere Island, for continued recent gene flow in the last 250–500 years. These results suggest that a re-analysis of other Arctic species with shallow population structure using higher resolution genomic markers and demographic analyses may help reveal deeper structure and other circumpolar glacial refugia.

Original languageEnglish
JournalJournal of Biogeography
Volume51
Issue10
Pages (from-to)1958-1973
Number of pages16
ISSN0305-0270
DOIs
Publication statusPublished - Oct 2024

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