Piburger See is a soft-water mountain lake located in the Central Eastern Alps (47°11'42''N, 10°53'18''E, Tyrol, Austria). The increase in recreational activities, tourism, and the application of fertilizer on nearby fields, resulted in enhanced primary production and rising hypolimnetic oxygen depletion in the lake during the 1950s and 1960s (Pechlaner, 1968). Lake restoration started in 1970 by exporting anoxic and nutrient-rich hypolimnetic waters with an Olszewski tube, and by reducing external nutrient loading by altering fertilizer application and by diverting sewage from a public bath. Lake oxygenation rapidly improved after 1970 (Pechlaner, 1979), while the response of total phosphorus (TP) and phytoplankton biomass to lake restoration was delayed by two decades (Fig. 1). Since the early 2000s, phytoplankton biovolume has increased again, suggesting a reversing trend in lake trophic status (Tolotti et al., 2012). Simultaneously, small changes in TP were recorded (Fig. 1). Although Piburger See was part of the OECD study on eutrophication and is currently included in the Austrian LTER network, the 45 year-long data-base includes several data gaps (e.g. for phytoplankton). To compensate for gaps in moniroring data, a paleolimnological study has been carried out on a radiometrically dated sediment core in order to reconstruct the lakes' trophic state since the late-19th century and to define the reference conditions for the lake (Thies et al., 2012). Limnological data recorded during the last four decades provided the validation of the inferred TP concentration (Fig. 2). Changes in phytoplankton biomass and species composition were analyzed in relation to nutrients and water temperature. Epilimnetic temperatures of Piburger See, reconstructed by long-term air temperature records, showed a pronounced increase during the mid-1940s and also since the late-20th century. Both periods also show increasing algal growth and changes in diatom species composition (i.e. increase in centric diatoms and recent blooms in Asterionella formosa). The combination of paleo- and neolimnology allowed the analysis of the role of climate and nutrients in driving phytoplankton changes in Piburger See. In particular, the study on sediments showed that long-term phytoplankton changes were mainly attributed to increasing lake temperature, while nutrients acted as modulating factor. On the other side, short-term changes in the phytoplankton of Piburger See since the 2000s were explained by varying nutrient concentrations and ratios (i.e. nitrogen and silica), while rising water temperature and enhanced thermal stability regulated the inter-annual lake variability. Our results underline that the combined impact of nutrients and climate on phytoplankton development can sustain short-time phytoplankton pulses, and thus mimic short-term increases in the trophic level of less productive lakes.
Combined effects of nutrient and climate change interaction of Piburger See (Austria). Results from Paleo- and Neolimnology
Piero Guilizzoni;Andrea Lami;Simona Musazzi;
2013
Abstract
Piburger See is a soft-water mountain lake located in the Central Eastern Alps (47°11'42''N, 10°53'18''E, Tyrol, Austria). The increase in recreational activities, tourism, and the application of fertilizer on nearby fields, resulted in enhanced primary production and rising hypolimnetic oxygen depletion in the lake during the 1950s and 1960s (Pechlaner, 1968). Lake restoration started in 1970 by exporting anoxic and nutrient-rich hypolimnetic waters with an Olszewski tube, and by reducing external nutrient loading by altering fertilizer application and by diverting sewage from a public bath. Lake oxygenation rapidly improved after 1970 (Pechlaner, 1979), while the response of total phosphorus (TP) and phytoplankton biomass to lake restoration was delayed by two decades (Fig. 1). Since the early 2000s, phytoplankton biovolume has increased again, suggesting a reversing trend in lake trophic status (Tolotti et al., 2012). Simultaneously, small changes in TP were recorded (Fig. 1). Although Piburger See was part of the OECD study on eutrophication and is currently included in the Austrian LTER network, the 45 year-long data-base includes several data gaps (e.g. for phytoplankton). To compensate for gaps in moniroring data, a paleolimnological study has been carried out on a radiometrically dated sediment core in order to reconstruct the lakes' trophic state since the late-19th century and to define the reference conditions for the lake (Thies et al., 2012). Limnological data recorded during the last four decades provided the validation of the inferred TP concentration (Fig. 2). Changes in phytoplankton biomass and species composition were analyzed in relation to nutrients and water temperature. Epilimnetic temperatures of Piburger See, reconstructed by long-term air temperature records, showed a pronounced increase during the mid-1940s and also since the late-20th century. Both periods also show increasing algal growth and changes in diatom species composition (i.e. increase in centric diatoms and recent blooms in Asterionella formosa). The combination of paleo- and neolimnology allowed the analysis of the role of climate and nutrients in driving phytoplankton changes in Piburger See. In particular, the study on sediments showed that long-term phytoplankton changes were mainly attributed to increasing lake temperature, while nutrients acted as modulating factor. On the other side, short-term changes in the phytoplankton of Piburger See since the 2000s were explained by varying nutrient concentrations and ratios (i.e. nitrogen and silica), while rising water temperature and enhanced thermal stability regulated the inter-annual lake variability. Our results underline that the combined impact of nutrients and climate on phytoplankton development can sustain short-time phytoplankton pulses, and thus mimic short-term increases in the trophic level of less productive lakes.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
