HCO(3) Influx Across the Plasmalemma of Chara corallina: Divalent Cation Requirement

Abstract

An absolute requirement for divalent cations is reported for H(14)CO(3) (-) influx in Chara corallina. Effective substitution of eluted Ca(2+) by Mg(2+) and Sr(2+) was observed, but Mn(2+) was completely ineffective in restoring H(14)CO(3) (-) transport activity. Similarly, La(3+) could not substitute for Ca(2+) in this system. Low concentrations of ethylenediaminetetraacetate (0.01 to 0.06 mm) significantly enhanced the rate at which H(14)CO(3) (-) transport capacity was lost.Examination of the response of OH(-) efflux, during Ca(2+)-free treatment, indicated that the cellular control over OH(-) efflux remained unaffected until membrane integrity became severely affected. This conclusion was supported by the response of OH(-) efflux to 10 mm K(+). Therefore, assimilation of H(14)CO(3) (-) is not rate-limited by an effect of Ca(2+) elution on the OH(-) transport system. Kinetic experiments indicated that Ca(2+) removal from the membrane resulted in noncompetitive inhibition of H(14)CO(3) (-) assimilation; the apparent Michaelis constant remained unaltered over a wide range of conditions. An hypothesis is presented which suggests that membrane integrity is necessary for HCO(3) (-) transport to occur, but Ca(2+) (Mg(2+), Sr(2+)), per se, must be bound to the transport complex before activity is established.