Effects of Lake Size on Phytoplankton Nutrient Status

Authors:
  • SGS. J. Guildford
    S. J. Guildford
  • LHL. L. Hendzel
    L. L. Hendzel
  • HKH. J. Kling
    H. J. Kling
  • EFE. J. Fee
    E. J. Fee
  • GRG. G. C. Robinson
    G. G. C. Robinson
  • RHR. E. Hecky
    R. E. Hecky
  • SKS. E. M. Kasian
    S. E. M. Kasian
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Abstract
Phytoplankton nutrient status measurements (C/P, C/N, C/chlorophyll, N/P, alkaline phosphatase activity, and N debt) were measured for 6 yr in seven remote Canadian Shield lakes. Lakes Nipigon and Superior were also studied for 2 yr. These lakes varied in surface area from 29 to 8.223 × 10 ha, they all stratified fully during the summer and had water renewal times > 5 yr. All lakes were severely P deficient; however, the large lakes (> 2000 ha) were consistently less P deficient than small lakes. A growth-rate indicator (photosynthesis normalized to particulate C) agreed with nutrient status indicators, in that small lakes had lower rates than large lakes. Total P was a good predictor of chlorophyll, but factors related to lake size (temperature and mixed depth) were equally good or better predictors of nutrient status. Decreasing mean water column light intensity could not explain the lower P deficiency of large lakes. The deeper, more energetic mixed layers in large lakes apparently cause P to be recycled more efficiently. Extrapolation of observations or experimental results from small to large lakes requires recognition that phytoplankton in large lakes are less nutrient deficient and may have higher growth rates.

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