Metabolism and elemental composition of zooplankton from the Barents Sea during early Arctic summer
Marine Biology, ISSN: 0025-3162, Vol: 100, Issue: 2, Page: 173-183
1989
- 77Citations
- 79Captures
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Article Description
Rates of oxygen consumption, ammonia excretion and phosphate excretion were measured on a hydromedusae (Aglantha digitale), pteropods (Limacia helicina, Clione limacina), copepods (Calanus finmarchicus, C. glacialis, C. hyperboreus, Metridia longa), an amphipod (Parathemisto libellula), a euphausiid (Thysanoessa inermis) and a chaetognath (Sagitta elegans), all of which were dominant species in the Barents Sea during early summer 1987. Water and ash contents and elemental composition (C and N) were also analysed on the specimens used in these metabolic experiments. Between species variations were 67.8% to 94.7% of wet weight in water content, 6.4% to 56.5% of dry weight in ash content, 16.7% to 61.0% of dry weight in carbon content, and 4.3% to 11.2% of dry weight in nitrogen content. Oxygen consumption rates ranged from 0.33 to 13.8 μl O individual h, ammonia excretion rates, from 0.0072 to 0.885 μgN individual h and phosphate excretion rates, from 0.0036 to 0.33 μg P individual h. In general, higher rates were associated with larger species, but considerable differences were also seen between species. The ratios between the rates (O : N, N : P, O : P) exhibited a wide species-specific variation, indicating differences in dominant metabolic substrates. Typical protein oriented metabolism was identified only in S. elegans. From the results of metabolic rate measurements and elemental analyses, daily losses of body carbon and nitrogen were estimated to be 0.50 to 4.15% and 0.084 to 1.87%, respectively, showing faster turnover rates of carbon than that of nitrogen. Comparison of daily loss of body carbon of the Barents Sea zooplankton with that of the Antarctic zooplankton indicated reduced rates of the former (63% on average). © 1989 Springer-Verlag.
Bibliographic Details
http://www.scopus.com/inward/record.url?partnerID=HzOxMe3b&scp=0000138990&origin=inward; http://dx.doi.org/10.1007/bf00391956; http://link.springer.com/10.1007/BF00391956; http://www.springerlink.com/index/pdf/10.1007/BF00391956; https://dx.doi.org/10.1007/bf00391956; https://link.springer.com/article/10.1007/BF00391956; http://www.springerlink.com/index/10.1007/BF00391956
Springer Science and Business Media LLC
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