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Alteration of phytoplankton structure in Lake Lucerne due
to trophic conditions
H. R. Bürgi1
and P Stadelmann2
1Department
of Limnology, ETH/EAWAG, CH-8600 Dübendorf-Switzerland
E-mail: buergi@eawag.ch
2Agency
of Environmental Protection of Canton Lucerne, Libellenrain
15,
CH-6002 Lucerne-Switzerland
E-mail: pius.stadelmann@afu.mpud.lu.ch
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Abstract
During the last 45 years, Lake Lucerne
(Switzerland) was characterized by four major periods of varying
trophic state: 1) the oligotrophic period (1955 to 1969): total
phosphorus concentrations below 20 mg m-3,
nitrate-nitrogen 300 to 400 mg m-3;
2) a period of accelerated eutrophication (1970 to 1977): total
phosphorus concentration 20 to 30 mg m-3
nitrate-nitrogen 400 to 500 mg m-3;
3) a moderate mesotrophic period (1978 to 1988): total phosphorus
concentration 20 to 25 mg m-3,
nitrate-nitrogen 500 to 600 mg m-3
and 4) a period of growth limiting phosphorus concentration (1989-2001):
total phosphorus concentration 5 to 10 mg m-3
nitrate-nitrogen 600 to 700 mg m-3.
The biomass, evenness, species richness and biodiversity
of the plankton community was analyzed over 40 years. Annual means
of biomass were not closely correlated with nutrient loading. Biodiversity,
evenness and monthly changes in biomass proved to be better indicators
of environmental changes. Clear water periods due to zooplankton
overgrazing were observed during the mesotrophic period. The growth
of phytoplankton appeared to be limited by phosphorus. Blooms of
nitrogen gas-fixing (N2) cyanobacteria
occurred only during the 1971 to 1983 period.
Keywords: Biodiversity, evenness, long-term monitoring,
resilience, restoration of a pre-alpine lake
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