Abstract-The distribution of phosphorus (P) was assessed in homogeneously 33 P-labeled Daphnia magna, Daphnia galeata and Eudiaptomus gracilis. The specific P contents were 1.48, 1.41, and 0.50% of dry weight (DW), respectively. The results support the view of low intraspecific variability in P : DW ratios in crustacean zooplankton. The fraction of P allocated to nucleic acids, phospholipids, and other P compounds was assessed in D. galeata and E. gracilis. In both species, the major pool, 35-69% of the total P content, was associated with nucleic acids. This fraction decreased with both body size (age) of D. galeata and E. gracilis and with the reproductive rate of D. galeata. D. magna and D. galeata revealed similar patterns of P allocation between body, carapace, and eggs. The carapace contained approximately 14% of the total P content. If most P is not reabsorbed from the exoskeleton prior to molting, the molting will result in a substantial P drain both from the individual and, at times, from the entire planktonic system. Zooplankton production has long been considered to be mainly energy (or carbon) limited, but recently much attention has been paid to the importance of food quality for the growth of crustacean zooplankton. One of the potentially important factors, which may place constraints on zooplankton growth, is phosphorus (P) (Hessen 1992;Urabe et al. 1997). Typically, daphnids have low carbon : phosphorus (C : P) ratios, while copepods have high C : P ratios in their somatic tissues Hessen and Lyche 1991). Furthermore, the sestonic P concentration is often below predicted and observed thresholds for P limitation of zooplankton growth (Hessen and Andersen 1992;Sommer 1992;Urabe and Watanabe 1992). This implies that in order to maintain a nearly homeostatic C : P ratio, a grazer must balance its net intake of elements relative to its bodily demands. At high C : P ratios in the food, some proportion of C (''excess C'') must be disposed off, invariably reducing the growth rate. Similarly, the relationship between the P content in zooplankton and in their food also has implications in terms of the amount of P that is recycled by zooplankton .Expected major pools of P in crustaceans are nucleic acids (deoxyribonucleic acid [DNA] , and calcium-associated P (hydroxyapatite) in the exoskeleton. Only limited information exists on the occurrence and dynamics of these compounds in crustaceans. The distribution of P between these pools, as well as between reproduction and somatic growth, reflects metabolic and physiologic constraints but is also a consequence of the animals' life histories (Elser et al. 1996). The allocation pattern will also have implications for P flow within the planktonic food web because of differences in turnover time and bioavailability between different pools of P. While the high specific P content of Daphnia relative to that of other zooplankton, particularly relative to that of copepods, is settled, there is no obvious reason why this is so. If a high specific P content may lead to ...