- 1Department of Science and Agroforestry Technology and Genetics, University of Castilla-La Mancha, Albacete, Spain (nicolas.valiente@uclm.es)
- 2Centre for Biogeochemistry in the Anthropocene, Department of Biosciences, Section for Aquatic Biology and Toxicology, University of Oslo, Oslo, Norway
- 3Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden
- 4Department of Biology, Freshwater Biology section, University of Copenhagen, Copenhagen, Denmark
- 5Department of Biology, Wilfrid Laurier University, Waterloo, ON, Canada
- 6Institut National de la Recherche Scientifique, Centre Eau Terre Environnement, Québec City, QC, Canada
- 7Watershed Hydrology and Ecology Research Division, National Hydrology Research Centre, Environment and Climate Change Canada, Saskatoon, SK, Canada
- 8Alaska Center for Conservation Science, University of Alaska Anchorage, Anchorage, AK, U.S.A.
Northern freshwater ecosystems face a wide range of environmental changes, including climate change, eutrophication, and browning. In Arctic regions, climate warming is occurring nearly four times faster than the global average, leading to higher water temperatures, shorter ice-cover periods, and extended growing seasons for aquatic biota. These changes are expected to have both direct and indirect impacts on these ecosystems, including the microbial communities that underpin their biodiversity and functioning. Building on prior research by the authors, we tested the hypothesis that microbial communities, particularly prokaryotes (bacteria and archaea), exhibit similarities across circumpolar freshwater systems. To investigate this, we surveyed 46 lakes and 30 streams between 2019 and 2022 in Arctic (>70º N) and sub-Arctic (55–70º N) regions spanning Alaska, Canada, Greenland, Norway (including Svalbard), and Sweden. For each waterbody, we collected environmental DNA (eDNA) for 16S rRNA gene metabarcoding and water samples to analyze physical and chemical parameters (temperature, pH, electrical conductivity, and dissolved O2), major ions, and nutrients (organic C, P, and N).
Bacteria predominantly represented the main prokaryotic group in this study, with archaeal contributions limited to a few lakes in Svalbard and the Canadian Northwest Territories. Our results revealed that latitude (i.e., Arctic vs. sub-Arctic locations) strongly determined community composition (p = 0.001; pseudo-F = 2.634), whereas the type of waterbody (i.e., lakes vs. streams) had a weaker influence on beta diversity (p = 0.012; pseudo-F = 1.813). Latitude, along with water temperature and dissolved O2, were the main explanatory variables shaping prokaryotic community composition in our study. The core microbiome differed significantly in abundance between Arctic and sub-Arctic locations (p = 0.005). Arctic freshwaters showed the highest alpha diversity (Shannon and Chao1 indices) and were dominated by the genera Rhodoferax, Arcicella, and Polaromonas, all of which positively correlated with increasing dissolved O2 concentrations. In contrast, sub-Arctic freshwaters were primarily dominated by Limnohabitans, a genus widely distributed in inland freshwater habitats. Regarding waterbody types, lakes were predominantly characterized by Flavobacterium, which positively correlated with increasing nutrient concentrations, and exhibited higher alpha diversity compared to streams. Streams, in turn, were largely dominated by Rhodococcus species, which showed significant positive correlations with water temperature. This study enhances our understanding of prokaryotic diversity across the circumpolar region and aims to further provide valuable insights into the assembly mechanisms of freshwater microbial communities.
How to cite: Valiente Parra, N., Eiler, A., Bertilsson, S., Chaguaceda, F., Christoffersen, K. S., Culp, J., Lavoie, I., Musetta-Lambert, J., Shaftel, R., and Hessen, D. O.: Patterns of prokaryotic diversity in freshwaters across the circumpolar region, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-17219, https://doi.org/10.5194/egusphere-egu25-17219, 2025.