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Critical nitrogen deposition loads in high-elevation lakes of the western US inferred from paleolimnological records

January 1, 2011

Critical loads of nitrogen (N) from atmospheric deposition were determined for alpine lake ecosystems in the western US using fossil diatom assemblages in lake sediment cores. Changes in diatom species over the last century were indicative of N enrichment in two areas, the eastern Sierra Nevada, starting between 1960 and 1965, and the Greater Yellowstone Ecosystem, starting in 1980. In contrast, no changes in diatom community structure were apparent in lakes of Glacier National Park. To determine critical N loads that elicited these community changes, we modeled wet nitrogen deposition rates for the period in which diatom shifts first occurred in each area using deposition data spanning from 1980 to 2007. We determined a critical load of 1.4 kg N ha−1 year−1 wet N deposition to elicit key nutrient enrichment effects on diatom communities in both the eastern Sierra Nevada and the Greater Yellowstone Ecosystem.

Citation Information

Publication Year 2011
Title Critical nitrogen deposition loads in high-elevation lakes of the western US inferred from paleolimnological records
DOI 10.1007/s11270-010-0526-6
Authors J.E. Saros, David W. Clow, T. Blett, A.P. Wolfe
Publication Type Article
Publication Subtype Journal Article
Series Title Water, Air, & Soil Pollution
Index ID 70035705
Record Source USGS Publications Warehouse

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