Ja. Kowalak et al., Identities and phylogenetic comparisons of posttranscriptional modifications in 16 S ribosomal RNA from Haloferax volcanii, J BIOL CHEM, 275(32), 2000, pp. 24484-24489
Small subunit (16 S) rRNA from the archaeon Haloferax volcanii, for which s
ites of modification were previously reported, was examined using mass spec
trometry. A census of all modified residues was taken by Liquid chromatogra
phy/electrospray ionization-mass spectrometry analysis of a total nucleosid
e digest of the rRNA. Following rRNA hydrolysis by RNase T-1, accurate mole
cular mass values of oligonucleotide products were measured using liquid ch
romatography/electrospray ionization-mass spectrometry and compared with va
lues predicted from the corresponding gene sequence. Three modified nucleos
ides, distributed over four con served sites in the decoding region of the
molecule, were characterized: 3-(3-amino-3-carboxypropyl)uridine-966, N-6-m
ethyladenosine-1501, and N-6,N-6-dimethyladenosine-1518 and -1519 tall Esch
erichia coli numbering). Nueleoside 3-(3-amino-3-carboxypropyl)uridine, pre
viously unknown in rRNA, occurs at a highly conserved site of modification
in all three evolutionary domains but for which no structural assignment in
archaea has been previously reported. Nucleoside N-6-methyladenosine, not
previously placed in archaeal rRNAs, frequently occurs at the analogous loc
ation in eukaryotic small subunit rRNA but not in bacteria. H, volcanii sma
ll subunit rRNA appears to reflect the phenotypically low modification leve
l in the Crenarchaeota kingdom and is the only cytoplasmic small subunit rR
NA shown to lack pseudouridine.