ATP sulfurylase from Penicillium chrysogenum: is the internal level of the enzyme sufficient to account for the rate of sulfate utilization?

Abstract

The in vivo rate of sulfate activation in Penicillium chrysogenum (wild-type strain ATCC 24791) was determined to be 0.19 +/- 0.09 mumol g(-1) (dry weight) min(-1) by the following methods. (i) The maximum growth of the organism in synthetic medium was a linear function of the initial Na(2)SO(4) concentration between 0 and 8 x 10(-4) Na(2)SO(4). The growth yield was 1.64 x 10(-2) g (dry weight) of mycelium per mumol of added sulfate, corresponding to a minimum sulfur requirement of 61 mumol/g (dry weight). Under these conditions (limiting sulfate) the minimum doubling time of P. chrysogenum in submerged culture was about 3.8 h, corresponding to a maximum exponential growth rate constant of 3.0 x 10(-3) min(-1). If all the sulfur in this mycelium passed through adenosine-5'-phosphosulfate, the rate of sulfate activation in vivo must have been 0.183 mumol min(-1) g(-1) (dry weight). (ii) In the presence of excess (35)SO(4) (2-), the total organic (35)S produced varied with the mycelial growth rate. However, until the culture approached maximum density, the product of [(growth rate constant) x (organic (35)S content)] was nearly constant at 0.24 to 0.28 mumol min(-1) g(-1) (dry weight). (iii) A sulfur-starved mycelium pulsed with 10(-4) M (35)SO(4) (2-) produced organic (35)S at a rate of about 0.10 mumol min(-1) g(-1) (dry weight) under conditions where the internal concentrations of ATP and sulfate would permit ATP sulfurylase to operate at about 70% of its V(max). Cell-free extracts of P. chrysogenum growing rapidly on excess sulfate contained 0.22 U of ATP sulfurylase per g (dry weight). Thus, in spite of the relatively low specific activity of homogeneous ATP sulfurylase (0.13 U/mg of protein, corresponding to an active site turnover of 7.15 min(-1)), the mycelial content of the enzyme was sufficient to account for the observed growth rate of the organism on inorganic sulfate as the sole sulfur source.