Rapid calcium exchange for protons and potassium in cell walls of Chara

Net fluxes of Ca²⁺, H⁺ and K⁺ were measured from intact Chara australis cells and from isolated cell walls, using ion-selective microelectrodes. In both systems, a stimulation in Ca²⁺ efflux (up to 100 nmol m^?2 s^?1, from an influx of ～40 nmol m^?2 s^?1) was detected as the H⁺ or K⁺ concentration was progressively increased in the bathing solution (pH 7.0 to 4.6 or K⁺ 0.2 to 10mol m^?3, respectively). A Ca²⁺ influx of similar size occurred following the reverse changes. These fluxes decayed exponentially with a time constant of about 10 min. The threshold pH for Ca²⁺ efflux (pH 5.2) is similar to a reported pH threshold for acid-induced wall extensibility in a closely related characean species. Application of NH₄⁺ to intact cells caused prolonged H⁺ efflux and also transient Ca²⁺ efflux. We attribute all these net Ca²⁺ fluxes to exchange in the wall with H⁺ or K⁺. A theoretical treatment of the cell wall ion exchanges, using the ‘weak acid Donnan Manning’ (WADM) model, is given and it agrees well with the data. The role of Ca²⁺ in the cell wall and the effect of Ca²⁺ exchanges on the measured fluxes of other ions, including bathing medium acidification by H⁺ efflux, are discussed.