Distribution of diatoms, chironomids and cladocera in surface sediments of thirty mountain lakes in south-eastern Switzerland

Bigler, Christian; Heiri, Oliver; Krskova, Renata; Lotter, André F.; Sturm, Michael (2006). Distribution of diatoms, chironomids and cladocera in surface sediments of thirty mountain lakes in south-eastern Switzerland. Aquatic Sciences, 68(2), pp. 154-171. Birkhäuser-Verlag; www.birkhauser.ch 10.1007/s00027-006-0813-x

[img]
Preview
Text
2006_AquatSci_68_154.pdf - Published Version
Available under License Publisher holds Copyright.

Download (294kB) | Preview

Surface sediments from 30 mountain lakes in south-eastern Switzerland (Engadine, Grisons) were analysed for subfossil diatom, chironomid, and cladoceran assemblages. Ordination techniques were used to identify relevant physical and chemical environmental parameters that best explain the distribution of these biota in the studied lakes. Diatom assemblage composition showed a strong relationship with physical (e.g., lake depth, temperature, organic content of surface sediments) and chemical variables (e.g., lake-water pH, alkalinity, silica concentration). The greatest variance in chironomid and cladoceran assemblages is explained by dissolved organic carbon (DOC) content of lake water, temperature, and the organic content of surface sediments, all parameters which are highly correlated with lake elevation. Increasing lake depth is reflected in diatom and cladoceran assemblages by higher percentages of planktonic species, whereas chironomid assemblages in the deep Engadine lakes are characterised by a high proportion of lotic taxa. In contrast to similar studies in the Northern and Southern Alps, subfossil assemblages in the Engadine mountain lakes showed a strong relationship with DOC, which in these weakly buffered lakes is negatively correlated with altitude. According to our findings, chironomid and cladocera remains have a considerable potential as quantitative palaeotemperature indicators in the Engadine area. This potential is somewhat weaker for diatoms which seem to be more strongly influenced by water chemistry and lake bathymetry.

Item Type:

Journal Article (Original Article)

Division/Institute:

10 Strategic Research Centers > Oeschger Centre for Climate Change Research (OCCR)
08 Faculty of Science > Department of Biology > Institute of Plant Sciences (IPS) > Palaeoecology
08 Faculty of Science > Department of Biology > Institute of Plant Sciences (IPS)

UniBE Contributor:

Heiri, Oliver, Lotter, André Franz

Subjects:

500 Science > 580 Plants (Botany)

ISSN:

1015-1621

Publisher:

Birkhäuser-Verlag; www.birkhauser.ch

Language:

English

Submitter:

Peter Alfred von Ballmoos-Haas

Date Deposited:

27 Oct 2016 15:23

Last Modified:

02 Mar 2023 23:28

Publisher DOI:

10.1007/s00027-006-0813-x

Uncontrolled Keywords:

Diatoms, chironomids, cladocera, mountain lakes, water chemistry, Engadine

BORIS DOI:

10.7892/boris.89210

URI:

https://boris.unibe.ch/id/eprint/89210

Actions (login required)

Edit item Edit item
Provide Feedback