Kinetics of sulfate transport by Penicillium notatum. Interactions of sulfate, protons, and calcium

Abstract

The active transport of inorganic sulfate by an ATP sulfurylase-negative strain of Penicillium notatum is promoted by H+ ions and metal ions (divalent metal ions being more effective than monovalent metal ions). Initial velocity studies suggest that H+ and SO4(2-) add to the carrier in an ordered sequence (H+ before SO4(2-)), with H+ at equilibrium with free carrier and carrier-H+ complex. The linear reciprocal plots and replots suggest a 1:1 stoichiometry between H+ and SO4(2-). Ca2+ and other divalent metal ions stimulate sulfate transport markedly in buffered suspensions of low ionic strength. The kinetics of the Ca2+/SO4(2-) interaction suggest that Ca2+ (like H+) adds to the carrier before SO4(2-) and is at equilibrium with free carrier and carrier-Ca2+ complex. The linear reciprocal plots and replots indicate a 1:1 stoichiometry between Ca2+ and SO4(2-). Thus the fully loaded carrier-SO4(2-) -Ca2+ -H+ complex has a net positive charge relative to that of the free carrier, a fact consistent with the chemiosmotic hypothesis of membrane transport. The kinetics of the H+/Ca2+ interaction point to a random A-B (rapid equilibrium), ordered C sequence with A = H+, B = Ca2+, and C = SO4(2-). Selenate (an alternate substrate competitive with sulfate) is an uncompetitive inhibitor with respect to Ca2+, in agreement with the suggested mechanism. Internal charge balance is not accomplished by a stoichiometric coaccumulation of Ca2+ and SO4(2-). Sulfate transport does, however, promote 45Ca2+ uptake. A significant fraction of the added Ca2+ is bound by the mycelial surface. Binding is extremely rapid, but reversible.