Abstract: | Effects of removal of external Ca2+ on the cytoplasmic pH (pHc)of Chara corallina have been measured with the weak acid 5,5-dimethyl-oxazolidine-2,4-dione(DMO) as a function of external pH (pH0) and of the externalconcentration of K+. Removal of Ca2+ always decreased pHc whenpH0 was below about 6.0; the decrease was about 0.20.4units at pH0 5.0, increasing to about 0.5 units at pH0 4.3.When pH0 was 6.0 or higher the removal of Ca2+ had little orno effect on pHc. This situation was not altered by changingthe concentration of K+, though in some experiments at pH0 5.05.2there was a slight decrease in pH0 (about 0.2 units) when K+was increased from 0.2 to 2.0 mol m3, an effect apparentlyreversed when K+ was higher (5.0 or 10.0 mol m3). Theresults suggest that H+ transport continues in the absence ofexternal Ca2+, despite previous suggestions to the contrary,and that the H+ pump does not necessarily run near thermodynamicequilibrium with its chemical driving reaction. They indicate,rather, that the H+ pump is under kinetic control and providefurther evidence for the inadequacy of present models for theoperation of the H+ pump in charophyte cells, especially inrelation to its proposed role in regulating pHc. Key words: Chara corallina, Cytoplasmic pH, Calcium |