Delayed postglacial colonization of Betula in Iceland and the circum North Atlantic

• Published in: eLife
• Main Authors: Harning, David J, Sacco, Samuel, Anamthawat-Jónsson, Kesara, Ardenghi, Nicolò, Thordarson, Thor, Raberg, Jonathan H, Sepúlveda, Julio, Geirsdóttir, Áslaug, Shapiro, Beth, Miller, Gifford H
• Format: Text
• Language: English
• Published: eLife Sciences Publications, Ltd 2023
• Subjects: Ecology; Arctic; Iceland; North Atlantic; Tundra
• Online Access: http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10642962/; http://www.ncbi.nlm.nih.gov/pubmed/37955570; https://doi.org/10.7554/eLife.87749

As the Arctic continues to warm, woody shrubs are expected to expand northward. This process, known as ‘shrubification,’ has important implications for regional biodiversity, food web structure, and high-latitude temperature amplification. While the future rate of shrubification remains poorly constrained, past records of plant immigration to newly deglaciated landscapes in the Arctic may serve as useful analogs. We provide one new postglacial Holocene sedimentary ancient DNA (sedaDNA) record of vascular plants from Iceland and place a second Iceland postglacial sedaDNA record on an improved geochronology; both show Salicaceae present shortly after deglaciation, whereas Betulaceae first appears more than 1000 y later. We find a similar pattern of delayed Betulaceae colonization in eight previously published postglacial sedaDNA records from across the glaciated circum North Atlantic. In nearly all cases, we find that Salicaceae colonizes earlier than Betulaceae and that Betulaceae colonization is increasingly delayed for locations farther from glacial-age woody plant refugia. These trends in Salicaceae and Betulaceae colonization are consistent with the plant families’ environmental tolerances, species diversity, reproductive strategies, seed sizes, and soil preferences. As these reconstructions capture the efficiency of postglacial vascular plant migration during a past period of high-latitude warming, a similarly slow response of some woody shrubs to current warming in glaciated regions, and possibly non-glaciated tundra, may delay Arctic shrubification and future changes in the structure of tundra ecosystems and temperature amplification.