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The deep northern basin of Lake Lugano was permanently stratified over the last 4 decades because of mineralization in response to strong eutrophication. However, two consecutive cold and windy winte...
We use stable carbon isotope values (δ13C) in sedimented organic matter and carbonate as proxy indicators of productivity changes in a highly eutrophic to hypertrophic lake. Stable isotope data from a...
Nutrient and organic matter dynamics were evaluated for a glacial river-floodplain system in the Swiss Alps (Val Roseg). Glacial melt water was the primary source of particulate organic and inorganic ...

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