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Identification of an essential cysteine residue in human glutathione synthase.

ABSTRACT: Glutathione is essential for a variety of cellular functions, and is synthesized from gamma-glutamylcysteine and glycine by the action of glutathione synthase (EC 6.3.2.3). Human glutathione synthase is a dimer of two identical subunits, each composed of 474 amino acids. Little is known about the structure-function relationships of mammalian glutathione synthases and, in order to gain a greater understanding of this critical enzyme, we have probed the role of cysteine residues by chemical modification and site-directed mutagenesis. Preincubation with thiol reagents such as p-chloromercuribenzoate, N-ethylmaleimide, iodoacetate and 5,5'-dithiobis-(2-nitrobenzoate) resulted in significant inhibition of recombinant human glutathione synthase. Each subunit contains cysteine residues at positions 294, 409 and 422, and we have prepared four different mutants by replacing individual cysteine residues, or all of the cysteine residues, with alanine. The C294A and C409A cysteine mutants retained significant residual activity, indicating that these two cysteine residues are not essential for activity. In contrast, substantial decreases in enzymic activity were detected with the C422A and cysteine-free mutants. This suggests that Cys-422 may play a significant structural or functional role in human glutathione synthase.

SUBMITTER: Gali RR

PROVIDER: S-EPMC1218055 | biostudies-other | 1997 Jan

REPOSITORIES: biostudies-other

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Project description:BackgroundThiamine (vitamin B1) is synthesized de novo by certain yeast, fungi, plants, protozoans, bacteria and archaea. The pathway of thiamine biosynthesis by archaea is poorly understood, particularly the route of sulfur relay to form the thiazole ring. Archaea harbor structural homologs of both the bacterial (ThiS-ThiF) and eukaryotic (THI4) proteins that mobilize sulfur to thiazole ring precursors by distinct mechanisms.ResultsBased on comparative genome analysis, halophilic archaea are predicted to synthesize the pyrimidine moiety of thiamine by the bacterial pathway, initially suggesting that also a bacterial ThiS-ThiF type mechanism for synthesis of the thiazole ring is used in which the sulfur carrier ThiS is first activated by ThiF-catalyzed adenylation. The only ThiF homolog of Haloferax volcanii (UbaA) was deleted but this had no effect on growth in the absence of thiamine. Usage of the eukaryotic THI4-type sulfur relay was initially considered less likely for thiamine biosynthesis in archaea, since the active-site cysteine residue of yeast THI4p that donates the sulfur to the thiazole ring by a suicide mechanism is replaced by a histidine residue in many archaeal THI4 homologs and these are described as D-ribose-1,5-bisphosphate isomerases. The THI4 homolog of the halophilic archaea, including Hfx. volcanii (HVO_0665, HvThi4) was found to differ from that of methanogens and thermococci by having a cysteine residue (Cys165) corresponding to the conserved active site cysteine of yeast THI4p (Cys205). Deletion of HVO_0665 generated a thiamine auxotroph that was trans-complemented by a wild-type copy of HVO_0665, but not the modified gene encoding an HvThi4 C165A variant.ConclusionsBased on our results, we conclude that the archaeon Hfx. volcanii uses a yeast THI4-type mechanism for sulfur relay to form the thiazole ring of thiamine. We extend this finding to a relatively large group of archaea, including haloarchaea, ammonium oxidizing archaea, and some methanogen and Pyrococcus species, by observing that these organisms code for THI4 homologs that have a conserved active site cysteine residue which is likely used in thiamine biosynthesis. Thus, archaeal members of IPR002922 THI4 family that have a conserved cysteine active site should be reexamined for a function in thiamine biosynthesis.

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Identification of an essential cysteine residue in human glutathione synthase.

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