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The Journal of General Physiology, Vol 64, 608-621, Copyright © 1974 by The Rockefeller University Press


ARTICLE

Relationship of Cation Influxes and Effluxes in Yeast

Aser Rothstein 1

1 From the Department of Radiation Biology and Biophysics, University of Rochester School of Medicine and Dentistry, Rochester, New York.

Dr. Rothstein's present address is the Research Institute, The Hospital for Sick Children, Toronto, Ontario, Canada M5G 1X8.

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.

Submitted on February 14, 1974


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M. L. Jennings and J. Cui
Chloride Homeostasis in Saccharomyces cerevisiae: High Affinity Influx, V-ATPase-dependent Sequestration, and Identification of a Candidate Cl- Sensor
J. Gen. Physiol., March 31, 2008; 131(4): 379 - 391.
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