Abstract

International cooperation between Canada and the United States is necessary to sustain water quality and quantity of numerous cross-border water bodies. We used Lake Memphremagog as a case study for highlighting how paleolimnological and historical research can be insightful in developing conservation plans for transboundary waters. To investigate how the lake and its phosphorus (P) input from agricultural activity in the watershed have changed over the past ∼100 years, we developed decadal-scale, diatom-based records from analyses of sediment cores taken from the south and northwest ends of the lake and calculated watershed agricultural P budgets from Canadian and US agricultural census data. Based on these analyses, we observed substantial changes in diatom flora over the past century, and our diatom-based P transfer function demonstrated that lake trophic state in both basins has substantially varied. Correlation analyses between our diatom-inferred P concentrations and watershed P budgets identified agricultural inputs of P as a significant driver of lake trophic state, particularly from the 1930s to the 1970s. Recent dynamics in lake-water P concentrations are no longer tracking agricultural P budgets; instead, they likely reflect P arising from urban activities and possibly the slow release of P that previously accumulated in watershed soils or lake sediments. Given the complex network of regulatory agencies responsible for Lake Memphremagog and its watershed, as well as lessons learned from a neighboring transboundary lake, we predict that future lake management will be most effective if collaborations among local conservation groups and regional to national government agencies are fostered.

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