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Quantifying human-induced eutrophication in Swiss mountain lakes since AD 1800 using diatomsUniversity of Berne, Institute of Plant Sciences, Altenbergrain 21, 3013 Berne, Switzerland, christian.bigler @emg.umu.se, University of Berne, National Centre of Competence in Research on Climate (NCCR Climate), Erlachstrasse 9a, 3012 Berne, Switzerland
University of Berne, Institute of Plant Sciences, Altenbergrain 21, 3013 Berne, Switzerland, University of Berne, Institute of Geography, Erlachstrasse 9a, 3012 Berne, Switzerland
University of Utrecht, Institute of Environmental Biology, Palaeoecology, Laboratory of Palaeobotany and Palynology, Budapestlaan 4, 3584 CD Utrecht, The Netherlands
University of Arkansas, Department of Geosciences, 113 Ozark Hall, Fayetteville AR 72701, USA
University of Berne, National Centre of Competence in Research on Climate (NCCR Climate), Erlachstrasse 9a, 3012 Berne, Switzerland, Swiss Federal Institute for Environmental Science and Technology (EAWAG), Department of Surface Waters (SURF), 8600 Dübendorf, Switzerland
University of Bremen, Institute of Geography, GEOPOLAR, Celsiusstrasse FVG-M, 28359 Bremen, Germany
Swiss Federal Institute for Environmental Science and Technology (EAWAG), Department of Surface Waters (SURF), 8600 Dübendorf, Switzerland Sedimentary diatom assemblages from three lakes in the southeastern Swiss Alps were analysed at high temporal resolution since AD 1800. Altered land-use patterns, increasing population and exploitation through tourism are clearly reflected in annually laminated sediments of Lej da San Murezzan (Lake St Moritz) and Lej da Silvaplauna (Lake Silvaplana). Diatom assemblages originally dominated by Cyclotella taxa are replaced by taxa indicating higher total phosphorus (TP) concentrations, such as Asterionella formosa, Fragilaria crotonensis and Stephanodiscus parvus. In Lej da la Tscheppa, located well above the treeline in a catchment that was hardly exposed to human impact, Cyclotella comensis prevails throughout the entire sediment sequence. Quantitative estimates of past TP concentrations were inferred using a newly developed regional diatom-TP inference model based on 119 modern samples. In Lej da la Tscheppa diatoms imply stable, low TP concentrations (~10 µg/l), which can be considered as natural background concentration. Elevated TP levels are inferred for Lej da San Murezzan (max. 60 µg/l) since AD 1910 and for Lej da Silvaplauna (max. 40 µg/l) since AD 1950, corroborated by changes in sedimentary biogenic silica concentration and organic carbon content. Since ~AD 1970 improved waste water management led to a considerable reduction in TP loading in Lej da Silvaplauna and Lej da San Murezzan.
Key Words: Eutrophication diatoms Switzerland annual laminations varved sediments land use waste water management human impact Alpine lakes.
The Holocene, Vol. 17, No. 8,
1141-1154 (2007) This article has been cited by other articles:
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