Abstract

4-Thiouridine (s(4)U) is a conserved modified nucleotide at position 8 of bacterial and archaeal tRNAs and plays a role in protecting cells from near-UV killing. Escherichia coli employs the following two enzymes for its synthesis: the cysteine desulfurase IscS, which forms a Cys persulfide enzyme adduct from free Cys; and ThiI, which adenylates U8 and transfers sulfur from IscS to form s(4)U. The C-terminal rhodanese-like domain (RLD) of ThiI is responsible for the sulfurtransferase activity. The mechanism of s(4)U biosynthesis in archaea is not known as many archaea lack cysteine desulfurase and an RLD of the putative ThiI. Using the methanogenic archaeon Methanococcus maripaludis, we show that deletion of ThiI (MMP1354) abolished the biosynthesis of s(4)U but not of thiamine. MMP1354 complements an Escherichia coli ΔthiI mutant for s(4)U formation, indicating that MMP1354 is sufficient for sulfur incorporation into s(4)U. In the absence of an RLD, MMP1354 uses Cys(265) and Cys(268) located in the PP-loop pyrophosphatase domain to generate persulfide and disulfide intermediates for sulfur transfer. In vitro assays suggest that S(2-) is a physiologically relevant sulfur donor for s(4)U formation catalyzed by MMP1354 (K(m) for Na(2)S is ∼1 mm). Thus, methanogenic archaea developed a strategy for sulfur incorporation into s(4)U that differs from bacteria; this may be an adaptation to life in sulfide-rich environments.

Highlights

  • Bacterial ThiI catalyzes 4-thiouridine biosynthesis by using a rhodanese-like domain for sulfur transfer

  • Using the methanogenic archaeon Methanococcus maripaludis, we show that deletion of ThiI (MMP1354) abolished the biosynthesis of sulfide-rich environments common on ancient earth.4-Thiouridine (s4U) but not of thiamine

  • Methanogenic archaea developed a strategy for sulfur incorporation into s4U that differs from bacteria; this may be an adaptation to life in sulfide-rich environments

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Summary

Background

Bacterial ThiI catalyzes 4-thiouridine biosynthesis by using a rhodanese-like domain for sulfur transfer. Results: ThiI in methanogenic archaea employs a conserved CXXC motif to generate persulfide and disulfide intermediates for sulfur transfer. In the absence of an RLD, MMP1354 uses Cys265 and Cys268 located in the PP-loop pyrophosphatase domain to generate persulfide and disulfide intermediates for sulfur transfer. The methanogens use a tRNA-dependent pathway for cysteine biosynthesis [45] and produce a much smaller pool of free cysteine in comparison with E. coli [46] These archaea use sulfide instead of cysteine as the sulfur source for Fe-S cluster and methionine biosynthesis [46]. A conserved CXXC motif located in the PP-loop domain is essential for both in vitro and in vivo activities of s4U formation These two cysteines form persulfide and disulfide intermediates during sulfur transfer. A model of s4U biosynthesis in methanogenic archaea is proposed

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