TY - JOUR
T1 - Arctic-boreal bryophyte dynamics since the last glacial inferred from ancient DNA metabarcoding
AU - Herzschuh, Ulrike
AU - Liu, Ying
AU - Liu, Sisi
AU - Stoof-Leichsenring, Kathleen R.
AU - Porada, Philipp
AU - Courtin, Jérémy
AU - Farkas, Luca Zofia
AU - Böhmer, Thomas
AU - Biskaborn, Boris K.
AU - Diekmann, Bernhard
AU - Huang, Yongsong
AU - Kaufman, Darrell
AU - Melles, Martin
AU - Meyer, Hanno
AU - Pestryakova, Luidmila A.
AU - Russell, James M.
AU - Wagner, Bernd
N1 - Publisher Copyright:
© 2025 The Author(s). Journal of Biogeography published by John Wiley & Sons Ltd.
PY - 2025
Y1 - 2025
N2 - Aim: This study investigates the main changes in bryophyte diversity and composition during the last 30,000 years in arctic and boreal ecosystems. Turnover in biological and ecological trait compositions of recorded bryophytes is assessed to explore changes in dominant life-strategies and habitats. Location: The study area covers Siberia and Alaska (55°–90° N, 50°–150° E and 40°–90° N, 150° E-140° W). Taxon: Bryophytes. Methods: We leveraged a dataset of plant DNA metabarcoding (chloroplast, trnL) of sedimentary ancient DNA from 26 lake sediment cores. Our statistical analyses only target DNA reads assigned to bryophytes. Results: A total of 120 amplicon sequence variants were obtained, which could be assigned 100% to bryophyte taxa. Our results indicate that the dominant families in the palaeo-record reflect well the dominant families observed in Siberia and Alaska, and compositional changes reflect mainly the modern latitudinal gradient. For example, Sphagnum shows a clear post-glacial expansion pattern. Richness was high in times of high habitat diversity. Our data reveal a turnover from biological traits characteristic of an r-strategy (colonists/short-lived, small size, monoicous, long sporophyte season, small spores) during the glacial towards a K-strategy (long-lived, large size, dioicous, short sporophyte season, large spores) during the Holocene. The ecological traits indicate a shift towards taxa with a preference for high summer temperature, forested habitats, soil acidity and wetlands. Main Conclusions: Our results indicated substantial changes in the diversity and taxonomic composition, and dominant biological and ecological traits of bryophyte communities along with past warming and related habitat changes at the transition from glacial period to Holocene. This may to some extent represent an analogue for ongoing ecological change in northern high latitudes. Leveraging bryophyte records in sedimentary ancient DNA reveals promising results which could be enhanced once bryophyte representation in biodiversity and genetic databases has increased and bryophyte-specific ancient DNA methods become established.
AB - Aim: This study investigates the main changes in bryophyte diversity and composition during the last 30,000 years in arctic and boreal ecosystems. Turnover in biological and ecological trait compositions of recorded bryophytes is assessed to explore changes in dominant life-strategies and habitats. Location: The study area covers Siberia and Alaska (55°–90° N, 50°–150° E and 40°–90° N, 150° E-140° W). Taxon: Bryophytes. Methods: We leveraged a dataset of plant DNA metabarcoding (chloroplast, trnL) of sedimentary ancient DNA from 26 lake sediment cores. Our statistical analyses only target DNA reads assigned to bryophytes. Results: A total of 120 amplicon sequence variants were obtained, which could be assigned 100% to bryophyte taxa. Our results indicate that the dominant families in the palaeo-record reflect well the dominant families observed in Siberia and Alaska, and compositional changes reflect mainly the modern latitudinal gradient. For example, Sphagnum shows a clear post-glacial expansion pattern. Richness was high in times of high habitat diversity. Our data reveal a turnover from biological traits characteristic of an r-strategy (colonists/short-lived, small size, monoicous, long sporophyte season, small spores) during the glacial towards a K-strategy (long-lived, large size, dioicous, short sporophyte season, large spores) during the Holocene. The ecological traits indicate a shift towards taxa with a preference for high summer temperature, forested habitats, soil acidity and wetlands. Main Conclusions: Our results indicated substantial changes in the diversity and taxonomic composition, and dominant biological and ecological traits of bryophyte communities along with past warming and related habitat changes at the transition from glacial period to Holocene. This may to some extent represent an analogue for ongoing ecological change in northern high latitudes. Leveraging bryophyte records in sedimentary ancient DNA reveals promising results which could be enhanced once bryophyte representation in biodiversity and genetic databases has increased and bryophyte-specific ancient DNA methods become established.
UR - https://www.scopus.com/pages/publications/105011071501
U2 - 10.1111/jbi.70015
DO - 10.1111/jbi.70015
M3 - Article
AN - SCOPUS:105011071501
SN - 0305-0270
JO - Journal of Biogeography
JF - Journal of Biogeography
M1 - e70015
ER -