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 (Asp225, Lys274, Lys278, Lys306, Asp332, and Lys367) and two noncharged residues (Asn255 and Leu257) 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 31P 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.