Carbon, nitrogen and phosphorus stoichiometry of crustacean zooplankton in the Baltic Sea: implications for nutrient recycling

The carbon (C), nitrogen (N) and phosphorus (P) contents (%of dry weight) of some crustacean zooplankton were studied inthe Baltic Sea. The copepod Acartia sp. had a stable C and Ncontent (48.3 ± 0.8% C, 12.4 ± 0.2% N, C:N ratio4.5 ± 0.1). The P content was variable (1–2%),probably depending on developmental stage and season. Copepodsaccumulating fat, like Pseudocalanus minutus elongatus, hadhigher and more variable C content (50–60%), and lowerN and P content (7–12% N, 0.6–1.5% P). The highestC and lowest N and P contents were found in adult Limnocalanusmacrurus. However, the N:P ratio was apparently independentof fat content and between 14 and 27 for all copepods. The cladoceransBosmina longispina maritima and Evadne nordmanni had lower Ncontent (9.3–10.8%) and higher C:N ratio (5.1–5.7)than Acartia sp. The P content (1.2–1.4%) was similarto Acartia sp. and the N:P ratios (16–19) were in thelower range of that found for the copepods. The N:P ratio wasgenerally somewhat higher in the copepods than in seston, whichmost of the year had nearly Redfield C:N:P ratios. Potentially,nutrient recycling from crustacean zooplankton could enhanceN limitation of phytoplankton, but small stoichiometric differencessuggest that this effect is probably weak. The extent is dependenton the structure of the zooplankton community and the grossgrowth efficiencies. Acartia copepodites, which had nearly RedfieldN:P ratios, would have the opposite effect and enhance P limitationin late summer when seston N:P ratios increased.