The cultural eutrophication of Lac la Biche, Alberta, Canada: a paleoecological study

A multiproxy paleoecological investigation of Lac la Biche, a large boreal lake in northeastern Alberta, Canada, revealed that the lake was eutrophic before European settlement but has undergone additional cultural eutrophication in the past 30 to 50 years. Annual fluxes to sediments of phosphorus,...

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Bibliographic Details
Published in:Canadian Journal of Fisheries and Aquatic Sciences
Main Authors: Schindler, D. W., Wolfe, Alexander P., Vinebrooke, Rolf, Crowe, Angela, Blais, Jules M., Miskimmin, Brenda, Freed, Rina, Perren, Bianca
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2008
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Online Access:http://dx.doi.org/10.1139/f08-117
http://www.nrcresearchpress.com/doi/full-xml/10.1139/F08-117
http://www.nrcresearchpress.com/doi/pdf/10.1139/F08-117
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Summary:A multiproxy paleoecological investigation of Lac la Biche, a large boreal lake in northeastern Alberta, Canada, revealed that the lake was eutrophic before European settlement but has undergone additional cultural eutrophication in the past 30 to 50 years. Annual fluxes to sediments of phosphorus, nitrogen, carbon, and inorganic sediments have increased with time. A declining N–P ratio has increasingly favored nitrogen-fixing cyanobacteria. Increased deposition of microbial pigments and diatom frustules and a recent shift in diatom species also indicate increasing eutrophication. Biogenic silica increased with time, but there is no evidence of a near-surface decline that would indicate silica limitation. Stable isotopes suggest that an increasing proportion of carbon deposited in sediments is of in-lake origin, indicating increased productivity. In the basin nearest the town of Lac La Biche, an increase in δ 15 N followed the construction of the sewage treatment plant, but more recently, decreased δ 15 N in both basins suggests that nitrogen fixation has become a more important source of nitrogen. Despite documented damage to the fishery of the lake, zooplankton fossils do not show evidence of a strong trophic cascade. The study illustrates the power of a multiproxy approach in obtaining reliable paleolimnological conclusions.