Freshwater microbial community diversity in a rapidly changing High Arctic watershed
Language English Country Great Britain, England Media print
Document type Journal Article, Research Support, Non-U.S. Gov't
PubMed
31599931
DOI
10.1093/femsec/fiz161
PII: 5585388
Knihovny.cz E-resources
- Keywords
- Arctic, Lake Hazen, biogeochemistry, freshwaters, glacial rivers, microbial ecology, soil active layer streams, watersheds,
- MeSH
- Ecosystem MeSH
- Lakes microbiology MeSH
- Climate Change MeSH
- Water Microbiology * MeSH
- Microbiota * MeSH
- Soil MeSH
- Soil Microbiology MeSH
- Rivers microbiology MeSH
- RNA, Ribosomal, 16S MeSH
- Seasons MeSH
- Fresh Water microbiology MeSH
- Publication type
- Journal Article MeSH
- Research Support, Non-U.S. Gov't MeSH
- Geographicals
- Arctic Regions MeSH
- Nunavut MeSH
- Names of Substances
- Soil MeSH
- RNA, Ribosomal, 16S MeSH
Current models predict increases in High Arctic temperatures and precipitation that will have profound impacts on the Arctic hydrological cycle, including enhanced glacial melt and thawing of active layer soils. However, it remains uncertain how these changes will impact the structure of downstream resident freshwater microbial communities and ensuing microbially driven freshwater ecosystem services. Using the Lake Hazen watershed (Nunavut, Canada; 82°N, 71°W) as a sentinel system, we related microbial community composition (16S rRNA gene sequencing) to physicochemical parameters (e.g. dissolved oxygen and nutrients) over an annual hydrological cycle in three freshwater compartments within the watershed: (i) glacial rivers; (ii) active layer thaw-fed streams and waterbodies and (iii) Lake Hazen, into which (i) and (ii) drain. Microbial communities throughout these freshwater compartments were strongly interconnected, hydrologically, and often correlated with the presence of melt-sourced chemicals (e.g. dissolved inorganic carbon) as the melt season progressed. Within Lake Hazen itself, water column microbial communities were generally stable over spring and summer, despite fluctuating lake physicochemistry, indicating that these communities and the potential ecosystem services they provide therein may be resilient to environmental change. This work helps to establish a baseline understanding of how microbial communities and the ecosystem services they provide in Arctic watersheds might respond to future climate change.
Department of Biological Sciences University of Alberta Edmonton Alberta T6G 2E9 Canada
Department of Biology University of Waterloo Waterloo Ontario N2L 3G1 Canada
Department of Ecology Faculty of Science Charles University Prague 128 44 Czechia
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