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Seasonal ecosystem variability in remote mountain lakes: implications for detecting climatic signals in sediment records
Authors:J Catalan  M Ventura  A Brancelj  I Granados  H Thies  U Nickus  A Korhola  AF Lotter  A Barbieri  E Stuchlík  L Lien  P Bitu?ík  T Buchaca  L Camarero  GH Goudsmit  J Kopá?ek  G Lemcke  DM Livingstone  B Müller  M Rautio  M ?i?ko  S Sorvari  F ?porka  O Strunecký  M Toro
Institution:(1) Department of Ecology, University of Barcelona, Diagonal 645, E-08028 Barcelona, Spain;(2) National Institute of Biology, Vecna pot 111, Sl 1000 Ljubliana, Slovenia;(3) Departamento de Ecología, Facultad de Ciencias, Universidad Autónoma de Madrid, E-28049 Cantoblanco, Madrid, Spain;(4) Institut für Zoologie und Limnologie, Leopold Franzens Universität Innsbruck, Technikerstr. 25, A-6020 Innsbruck, Austria;(5) Institute of Meteorology and Geophysics, University of Innsbruck, Innrain 52, A- 6020 Innsbruck, Austria;(6) Department of Ecology and Systematics, Division of Hydrology, University of Helsinki, P.O. Box 17, Helsinki, FIN-00014, Finland;(7) Laboratory of Palaeobotany and Palynology, Budapestlaan 4, 3584 CD Utrecht, The Netherlands;(8) Dipartimento del Territorio, SPAA Laboratorio di Studi Ambientali, Riva Paradisco 15, 6900 Lugano-Paradiso, Switzerland;(9) Department of Hydrobiology, Charles University, Viniccaronná 7, CZ 128 44 Prague 2, Czech Republic;(10) NIVA, Post Box 173, Kjelsås, 0411 Oslo, Norway;(11) Department of General Ecology, Technical University, Masarykova 24, Zvolen, Slovakia;(12) Swiss Federal Institute of Environmental Science and Technology, EAWAG, Überlandstrasse 133, CH-8600 Düdendorf, Switzerland;(13) Hydrological Institute, AS CR, Na Sádkách 7, 370 05 Ccaroneské Budecaronjovice, Czech Republic;(14) Department of Hydrobiology, Institute of Zoology, Slovak Academy of Sciences, Dubravska cesta 9, SK-942 06 Bratislava, Slovakia;(15) CEAB-CSIC, Accés Cala St. Francesc 14, 17300 Blanes, Spain
Abstract:Weather variation and climate fluctuations are the main sources of ecosystem variability in remote mountain lakes. Here we describe the main patterns of seasonal variability in the ecosystems of nine lakes in Europe, and discuss the implications for recording climatic features in their sediments. Despite the diversity in latitude and size, the lakes showed a number of common features. They were ice-covered between 5–9 months, and all but one were dimictic. This particular lake was long and shallow, and wind action episodically mixed the water column throughout the ice-free period. All lakes showed characteristic oxygen depletion during the ice-covered-period, which was greater in the most productive lakes. Two types of lakes were distinguished according to the number of production peaks during the ice-free season. Lakes with longer summer stratification tended to have two productive periods: one at the onset of stratification, and the other during the autumn overturn. Lakes with shorter stratification had a single peak during the ice-free period. All lakes presented deep chlorophyll maxima during summer stratification, and subsurface chlorophyll maxima beneath the ice. Phosphorus limitation was common to all lakes, since nitrogen compounds were significantly more abundant than the requirements for the primary production observed. The major chemical components present in the lakes showed a short but extreme dilution during thawing. Certain lake features may favour the recording of particular climatic fluctuations, for instance: lakes with two distinct productive periods, climatic fluctuations in spring or autumn (e.g., through chrysophycean cysts); lakes with higher oxygen consumption, climatic factors affecting the duration of the ice-cover (e.g., through low-oxygen tolerant chironomids); lakes with higher water retention time; changes in atmospheric deposition (e.g., through carbon or pigment burial); lakes with longer stratification, air temperature changes during summer and autumn (e.g., through all epilimnetic species).
Keywords:alpine lakes  thermal regime  chlorophyll  nutrients  major chemicals  oxygen
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