Cold mountain stream chironomids (Diptera) of the genus Diamesa indicate both historical and recent climate change
Language English Country Great Britain, England Media print
Document type Journal Article
Grant support
APVV-20-0358
Slovak Research and Development Agency
1/0400/21
Scientific Grant Agency of the Ministry of Education of Slovak Republic and the Academy of Sciences
I 4568-B
Austrian-Czech Lead Agency project-Austrian Science Fund
23-06075S
Czech Science foundation
I 4568
Austrian Science Fund FWF - Austria
PubMed
38869370
DOI
10.1093/ee/nvae052
PII: 7692858
Knihovny.cz E-resources
- Keywords
- Alps, Bohemian Forest, Pyrenees, Tatra Mountains, glacier retreat, snowfield/glacieret,
- MeSH
- Chironomidae * physiology MeSH
- Climate Change * MeSH
- Cold Temperature MeSH
- Rivers * MeSH
- Animal Distribution MeSH
- Animals MeSH
- Check Tag
- Animals MeSH
- Publication type
- Journal Article MeSH
Chironomids of the genus Diamesa (Meigen, 1835, Diptera: Chironomidae) inhabit cold, oxygen-rich running waters. We have investigated the presence of Diamesa and other freshwater macroinvertebrates at 22 stream sampling sites in 3 European high mountain regions (the Central Pyrenees, the Ötztal Alps, and the Tatra Mountains) to establish suitable temperature conditions for Diamesa dominance. It has been generally accepted that their high abundance was linked to the presence of glaciers; however, we have shown that in the Tatra Mountains, where there are no glaciers, the conditions for the dominance of Diamesa species are created due to permanent snowfields, the geographical orientation of the valley and shading by the surrounding high peaks. The historical connection of Diamesa to glaciers was investigated from the paleolimnological records of subfossil chironomid assemblages from the Bohemian Forest, where glaciers disappeared before or during the Late Glacial period. As expected, water temperature seems to be the main driver of Diamesa distribution, and we determined that the relative abundance of Diamesa species was significantly higher at the sites with a mean July water temperature below 6.5 °C. The Diamesa-dominated stream communities seems to be endangered due to ongoing climate warming and this assumption is supported by our paleolimnological results from the Bohemian Forest lakes, where Diamesa has disappeared due to warming of lake inflows at the beginning of the Holocene. These findings strengthen the former suggestions that some Diamesa species could be used as an indicator for tracking recent environmental changes in vulnerable ecosystems of cold mountain streams.
Faculty of Natural Sciences Matej Bel University Tajovského 40 SK 974 01 Banská Bystrica Slovakia
Institute for Zoology University of Innsbruck Technikerstrasse 25 A 6020 Innsbruck Austria
Institute of Zoology Slovak Academy of Sciences Dúbravská cesta 9 SK 845 06 Bratislava Slovakia
References provided by Crossref.org