Abstract
Atomic C:N ratios in calanoid copepods were generally below the Redfield ratio (6.6), except for the fifth copepodid stage of Calanus sp. The C:P ratios in copepods were generally close to, or higher than the Redfield ratio of 106, but low C:P ratios were found in Acartia clausi (63 ± 7) and in the cladocerans (Podon sp.: 34 ± 5 and Evadne sp.: 59 ± 22).
Cite
CITATION STYLE
APA
Gismervik, I. (1997). Stoichiometry of some marine planktonic crustaceans. Journal of Plankton Research, 19(2), 279–285. https://doi.org/10.1093/plankt/19.2.279
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