Cited ReferencesBeasley, D.B., Monke, E.J. Miller, E.R., 1985. Using simulation to assess the impacts ofconservation tillage on movement of sediment and phosphorus into <strong>Lake</strong> Erie. Journalof Soil & <strong>Water</strong> Conservation 40, 233-237.Cooke, S.E. Prepas, E.E., 1998. Stream phosphorus and nitrogen export fromagricultural and forested watersheds on the northern Boreal Plain. Canadian Journalof Fisheries and Aquatic Sciences 55, 2292-2299.Genkai-Kato, M. Carpenter, S.R., 2005. Eutrophication due to phosphorus recycling inrelation to lake morphometry, temperature, and macrophytes. Ecology 86, 210-219.Hutchinson, N.J., Munro, J.R., Clark, B.J., Neary, B.P. Beaver, J., 1994. Rice andSturgeon <strong>Lake</strong>s nutrient budget study. Ministry of the Environment, Technical <strong>Report</strong>No. 2.KLSA, <strong>2006</strong>. Weeding out the answers - lake water quality 2005 report. Contact:kawarthalakestewards@yahoo.caMetcalfe, R.A., Schmidt, B. Pyrce, R., 2005. A surface water quality threatsassessment method using landscape-based indexing. WSC <strong>Report</strong> No. 01-2005, 58.MNR, 2002. Technical reference guide for end-users of Ontario digital geospatialdatabase (Natural Resources & Values Information). Ministry of Natural Resources.MNR, <strong>2006</strong>. <strong>Water</strong> Resources and Information Project (WRIP).www.mnr.gov.on.ca/mnr/water/p742.html.MOE, 1976. The Kawartha <strong>Lake</strong>s water management study - water quality assessment(1972-1976). Ministry of the Environment.Novotny, V. Olem, H., 1994. <strong>Water</strong> quality: Prevention, identification, and managementof diffuse pollution. John Wiley and Sons, Inc, New York.Robillard, M.M. Fox, M.G., <strong>2006</strong>. Historical changes in abundance and communitystructure of warmwater piscivore communities associated with changes in waterclarity, nutrients, and temperature. Canadian Journal of Fisheries and AquaticSciences 63, 798-809.44
How Much Algae Sticks to Macrophytes in the Kawartha <strong>Lake</strong>s?by Wynona Marleau and Eric SagerIn the 2004 KLSA report, Bev Clark of the Ontario Ministry of the Environment veryeloquently described the alternative states in which shallow lake systems can exist –either a macrophyte (water weeds) dominated state such as we have in the Kawarthasor a phytoplankton (suspended algae) dominated state such as existed in <strong>Lake</strong> Erie inthe late 1970s. (Previous KLSA reports can be found at the KLSA page on the OliverCentre website: www.trentu.ca/olivercentre.) The latter state often gives the waterthe appearance of thick pea soup. Under high loadings of nutrients, mainlyphosphorus, the potential exists for lakes to shift from a clear-water, macrophytedominated state to one that is dominated by suspended algae. It is believed that oneof the precursors to this shift is the excessive growth of epiphyton (algae that isattached to submersed macrophytes) and metaphyton (algae that commonly originatesfrom true floating algal populations but gets tangled up among macrophytes and otherfloating debris). This excessive growth can lead to photo-inhibition of themacrophytes – they don’t get enough sunlight – which then allows phytoplankton, the45