. "Perry, R. H." . "The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation" . . . "191951" . "Jacobson Jr, G. L." . . "Kop\u00E1\u010Dek, Ji\u0159\u00ED" . . . "000293144700009" . "Fernandez, I. J." . "Wilson, T. A." . "oligotrophication; climate change; phosphorus; sediment; aluminum"@en . . "Z(AV0Z60170517)" . "1" . "The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation"@en . . "SanClements, M. D." . "The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation" . . "RIV/60077344:_____/11:00360220" . "Saros, J. E." . . . "1"^^ . "10.1007/s10933-011-9526-9" . . . "RIV/60077344:_____/11:00360220!RIV12-AV0-60077344" . "The sediment record from a 5.3-m core from Sargent Mountain Pond, Maine USA indicates strong co-evolutionary relationships among climate, vegetation, soil development, runoff chemistry, lake processes, diatom community, and water and sediment chemistry. The lake was transformed from a more productive, high P, high pH, low DOC system into an oligotrophic, relatively low P, acidic, humic lake over a period of 16,600 years, a natural trend that continues. In contrast to many human-affected lakes that become increasingly eutrophic, many lakes become more oligotrophic during their history. The precursors for that are: (1) absence of human land-use in watersheds, (2) bedrock lithology and soil with a paucity of soluble Ca-rich minerals, and (3) vegetation that promotes the accumulation of soil organic matter, podzolization, and increased export of metal-DOC complexes, particularly Al."@en . "[DD668CA5B0FB]" . "16"^^ . "Norton, S. A." . "NL - Nizozemsko" . . . "0921-2728" . . "The sediment record from a 5.3-m core from Sargent Mountain Pond, Maine USA indicates strong co-evolutionary relationships among climate, vegetation, soil development, runoff chemistry, lake processes, diatom community, and water and sediment chemistry. The lake was transformed from a more productive, high P, high pH, low DOC system into an oligotrophic, relatively low P, acidic, humic lake over a period of 16,600 years, a natural trend that continues. In contrast to many human-affected lakes that become increasingly eutrophic, many lakes become more oligotrophic during their history. The precursors for that are: (1) absence of human land-use in watersheds, (2) bedrock lithology and soil with a paucity of soluble Ca-rich minerals, and (3) vegetation that promotes the accumulation of soil organic matter, podzolization, and increased export of metal-DOC complexes, particularly Al." . "Journal of Paleolimnology" . "8"^^ . "The controls on phosphorus availability in a Boreal lake ecosystem since deglaciation"@en . . "46" . .