Concordance of chemically inferred and assayed nutrient limitation of phytoplankton along a depth gradient of alpine lakes in the Canadian Rockies
Autor: | Rolf D. Vinebrooke, Jenna Cook, Mitchell A. Johnsen, Blake R. Stuparyk |
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Rok vydání: | 2019 |
Předmět: |
0106 biological sciences
010504 meteorology & atmospheric sciences Ecology Primary producers 010604 marine biology & hydrobiology Phosphorus fungi Lake ecosystem Amendment chemistry.chemical_element Aquatic Science 01 natural sciences Nutrient chemistry Environmental chemistry Phytoplankton Environmental science Bioassay Deposition (chemistry) Ecology Evolution Behavior and Systematics 0105 earth and related environmental sciences Water Science and Technology |
Zdroj: | Aquatic Sciences. 82 |
ISSN: | 1420-9055 1015-1621 |
DOI: | 10.1007/s00027-019-0683-7 |
Popis: | Deposition of nutrients over mountainous regions in many parts of the world is increasing due to human activities. To assess the level of agreement between chemically-inferred and experimental evidence of the potential sensitivity of alpine lake ecosystems along the Eastern Front range of the Canadian Rockies to increased deposition of nitrogen (N) and phosphorus (P), nutrient limitation was investigated in 29 sites using water chemistry and nutrient amendment bioassays of phytoplankton. The two lines of evidence agreed in 55% of all cases with discrepancies mainly involving instances of co-limitation. Dissolved inorganic N:total P (DIN:TP) mass ratios frequently suggested P limitation while the corresponding bioassays supported meta-analytical evidence of the prevalence of co-limitation of freshwater primary producers. Based on previous evidence of low DIN:TP mass ratios and experimental N amendments stimulating algal communities in shallower alpine sites, we hypothesized that nutrient limitation of phytoplankton shifts from being P- to N-driven with decreasing lake depth. However, we found little evidence of N limitation from bioassays of phytoplankton from the shallower ( |
Databáze: | OpenAIRE |
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