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Partial Characterization of K⁺ and Ca²⁺ Uptake Systems in the Halotolerant Alga Dunaliella salina¹

Department of Biochemistry, Weizmann Institute of Science, Rehovot 76100, Israel

The uptake of K⁺ and Ca²⁺ in Dunaliella salina is mediated by two distinct carriers: a K⁺ carrier with a high selectivity against Na⁺, Li⁺, and choline⁺ but not towards Rb⁺, K⁺, Cs⁺, or NH₄⁺, and a Ca²⁺ carrier with a high selectivity against Mg²⁺. The latter is specifically blocked by La³⁺ and by Cd²⁺. Apparent K_m values for K⁺ and Ca²⁺ uptake are 2.5 and 0.8 millimolar, respectively, and their maximal calculated fluxes are 22 and 0.8 nanomoles per square meter per second, respectively. Effects of permeable ions and ionophores on K⁺ and Ca²⁺ uptake suggest that the driving force for their uptake is the transmembrane electrical potential. Inhibitors of ATP production, typical inhibitors of plasma membrane H⁺-ATPases and protonionophores inhibit K⁺ and Ca²⁺ uptake and accelerate K⁺ efflux. The results suggest that an H⁺-ATPase in the cell membrane provides the driving force for K⁺ and Ca²⁺ uptake. Efflux measurements from ⁸⁶Rb⁺ and ⁴⁵Ca²⁺ loaded cells suggest that part of the intracellular K⁺ and most of the intracellular Ca²⁺ is nonexchangeable with the extracellular pool. Correlations between phosphate and K⁺ contents and the effect of phosphate on K⁺ efflux suggest intracellular associations between K⁺ and polyphosphates. On the basis of these results, it is suggested that: (a) K⁺ and Ca²⁺ uptake in D. salina is driven by the transmembrane electrical potential which is generated by the action of an H⁺-ATPase of the plasma membrane. (b) Part of the intracellular K⁺ is associated with polyphosphate bodies, while most of the intracellular Ca²⁺ is accumulated in intracellular organelles in the algal cells.

¹ Supported by the W. T. Hogan Career Development Chair.