Relationship of Cation Influxes and Effluxes in Yeast

Abstract

The Na⁺ efflux from Na⁺-rich yeast cells into a cation-free medium is largely balanced by the excretion of organic anions. In the presence of Rb⁺, K⁺, or high levels of H⁺ (pH 3–4), the Na⁺ efflux is increased and the organic anion excretion is suppressed so that stoichiometric cation exchanges occur. H⁺ participates in the exchanges, moving into or out of the cells depending on the external pH and on the concentration of external Rb⁺(K⁺). The total cation efflux is dependent on the external Rb⁺ concentration in a "saturation" relationship, but the individual cations in the efflux stream are not. The discrimination factor in the efflux pathway between H⁺ and Na⁺ is very large (of the order of 10,000), and between Na⁺ and K⁺ considerable (of the order of 50). For the latter pair, the recycling of K⁺ from the cell wall space is an important factor in the discrimination. In addition, the Na⁺ efflux as a function of Na⁺ content follows a sigmoidal curve so that the discrimination factor is increased at high levels of cellular Na⁺. Although the influx and efflux pathways behave as a tightly coupled system, the mechanism of coupling is not entirely clear. A single system with different cation specificities and kinetic behaviors on the inside and outside faces of the membrane could account for the data.

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