Abstract
In most lakes, nutrient limitation is synonymous with P-limitation. Low concentrations of P restrict the productivity of freshwater organisms and freshwater ecosystems, a fact that has been stressed over the years by algal physiologists (Beijerinck 1890; Pringsheim 1912; Tilman et al. 1982) and limnologists (Rodhe 1948; Vollenweider 1968; Sakamoto 1966; Schindler 1977). Although other elements than P sometimes may limit the growth of certain members of the phytoplankton, i.e. Si for diatoms (Tilman et al.1982), Se for Peridinium cinctum (Lindström and Rodhe 1978) and N for cyanobacteria (Schindler 1977), the role of P as the key limiting inorganic nutrient for the productivity of freshwater ecosystems is today accepted and little questioned (Shapiro 1988). The convincing results of P addition to whole lakes in the Experimental Lakes Area in Canada in the 1970s (Schindler 1977) put an end to the discussion about nutrient limitation in lakes for some decades.
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Jansson, M. (1998). Nutrient Limitation and Bacteria — Phytoplankton Interactions in Humic Lakes. In: Hessen, D.O., Tranvik, L.J. (eds) Aquatic Humic Substances. Ecological Studies, vol 133. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-03736-2_9
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DOI: https://doi.org/10.1007/978-3-662-03736-2_9
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