Cofactor F 420 is an electron carrier with a major role in the oxidoreductive reactions of Mycobacterium tuberculosis, the causative agent of tuberculosis. A ␥-glutamyl ligase catalyzes the final steps of the F 420 biosynthesis pathway by successive additions of L-glutamate residues to F 420 -0, producing a poly-␥-glutamate tail. The enzyme responsible for this reaction in archaea (CofE) comprises a single domain and produces F 420 -2 as the major species. The homologous M. tuberculosis enzyme, FbiB, is a two-domain protein and produces F 420 with predominantly 5-7 L-glutamate residues in the poly-␥-glutamate tail. The N-terminal domain of FbiB is homologous to CofE with an annotated ␥-glutamyl ligase activity, whereas the C-terminal domain has sequence similarity to an FMN-dependent family of nitroreductase enzymes. Here we demonstrate that full-length FbiB adds multiple L-glutamate residues to F 420 -0 in vitro to produce F 420 -5 after 24 h; communication between the two domains is critical for full ␥-glutamyl ligase activity. We also present crystal structures of the C-terminal domain of FbiB in apo-, F 420 -0-, and FMN-bound states, displaying distinct sites for F 420 -0 and FMN ligands that partially overlap. Finally, we discuss the features of a full-length structural model produced by small angle x-ray scattering and its implications for the role of N-and C-terminal domains in catalysis.The cofactor F 420 is a flavin derivative that is sporadically distributed among microorganisms, mainly archaea and actinobacteria (including mycobacteria). F 420 has been emerging as a new player in the biology of mycobacteria (1), with increasing numbers of F 420 -utilizing proteins characterized from different mycobacterial species (2-8). This cofactor has been suggested to protect Mycobacterium tuberculosis, the causative agent of tuberculosis, against oxidative and nitrosative stress during pathogenesis (9 -11). At the biochemical level, cofactor F 420 functions as a hydride transfer agent in oxidoreductive reactions with a lower redox potential than that of NAD(P) ϩ (12). The biosynthesis pathway of cofactor F 420 has been investigated in both archaeal and mycobacterial species. In the current view of the proposed pathway, the first intermediate with the complete chromophore (7, ) is produced by FO synthase (FbiC in mycobacteria (13) and CofGH in archaea (14)). A transferase enzyme (FbiA in mycobacteria (15) and CofD in archaea (16)) subsequently catalyzes the addition of a 2-phospho-L-lactate moiety to FO to produce F 420 -0 (F 420 with no poly-␥-glutamate tail). The final step of the pathway is performed by a ␥-glutamyl ligase (FbiB in mycobacteria (15) and CofE in archaea (17)) that catalyzes successive additions of L-glutamate residues to F 420 -0 (Fig. 1A).The length of the poly-␥-glutamate tail varies between archaeal and mycobacterial species; in archaea, two L-glutamate residues are seen (18), whereas in mycobacteria, up to nine residues are present (3, 19). There exists an intriguing difference between the ...