myo-Inositol-1-phosphate synthase (mIPS) catalyzes the conversion of glucose-6-phosphate (G-6-P) to inositol-1-phosphate. In the sulfate-reducing archaeon Archaeoglobus fulgidus it is a metal-dependent thermozyme that catalyzes the first step in the biosynthetic pathway of the unusual osmolyte di-myo-inositol-1,1 -phosphate. Several site-specific mutants of the archaeal mIPS were prepared and characterized to probe the details of the catalytic mechanism that was suggested by the recently solved crystal structure and by the comparison to the yeast mIPS. Six charged residues in the active site (Asp 225 , Lys 274 , Lys 278 , Lys 306 , Asp 332 , and Lys 367 ) and two noncharged residues (Asn 255 and Leu 257 ) have been changed to alanine. The charged residues are located at the active site and were proposed to play binding and/or direct catalytic roles, whereas noncharged residues are likely to be involved in proper binding of the substrate. Kinetic studies showed that only N255A retains any measurable activity, whereas two other mutants, K306A and D332A, can carry out the initial oxidation of G-6-P and reduction of NAD ؉ to NADH. The rest of the mutant enzymes show major changes in binding of G-6-P (monitored by the 31 P line width of inorganic phosphate when G-6-P is added in the presence of EDTA) or NAD ؉ (detected via changes in the protein intrinsic fluorescence). Characterization of these mutants provides new twists on the catalytic mechanism previously proposed for this enzyme.myo-Inositol-1-phosphate synthase (mIPS) 1 catalyzes the conversion of D-glucose-6-phosphate to L-myo-inositol-1-phosphate, the first step in de novo biosynthesis of myo-inositol. Compounds containing inositol are critical components of signal transduction pathways (1), cell walls in some pathogenic bacteria (2), and various stress responses (3, 4). In some hyperthermophilic archaea and bacteria, inositol is used for the synthesis of unique solutes accumulated to balance external osmotic pressure and protect intracellular macromolecules from heat and/or salt shock (for reviews of osmolytes in hyperthermophiles see Ref. 5). The solute di-myo-inositol-1,1Ј-phosphate (DIP) has been detected in Archaeoglobus fulgidus (6), Methanococcus igneus (7), Pyrococcus sp. (8, 9), and several bacteria of the Thermotogales family when the cells are grown at temperatures above 80°C (10). The DIP synthesized by M. igneus is chiral and composed of L-I-1-P units that are synthesized by mIPS (11). Because the archaeal mIPS enzymes commit significant cell resources to DIP synthesis, the production of DIP must be tightly regulated.The mIPS gene has been identified in the A. fulgidus genome, and the gene product was heterologously expressed in Escherichia coli (12). The recombinant A. fulgidus mIPS is an extremely heat-stable tetramer of 44-kDa subunits (much smaller than the eukaryotic homolog that is a tetramer of 60-kDa subunits). The catalytic activity of the enzyme was also shown to be absolutely dependent on divalent metal ions (Zn 2ϩ , Mn 2ϩ , or Mg 2ϩ ...