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Journal of Bacteriology, September 2003, p. 5483-5490, Vol. 185, No. 18
0021-9193/03/$08.00+0 DOI: 10.1128/JB.185.18.5483-5490.2003
Copyright © 2003, American Society for Microbiology. All Rights Reserved.
Rebecca Guymon,1 Pamela F. Crain,1 James A. McCloskey,1,2* Michael Thomm,3 Julianne Lim,4 and Ricardo Cavicchioli4
Department of Medicinal Chemistry, University of Utah, Salt Lake City, Utah 84112,1 Department of Biochemistry, University of Utah, Salt Lake City, Utah 84132,2 Institut für Allgemeine Mikrobiologie, Christian Albrechts Universität Kiel, 24118 Kiel, Germany,3 School of Microbiology and Immunology, The University of New South Wales, Sydney 2052, Australia4
Received 24 March 2003/ Accepted 3 July 2003
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From a phylogenetic perspective, it is interesting that the nucleoside structural motifs used for RNA stabilization at higher temperatures are known to be different in bacterial thermophiles (13, 24) and archaeal thermophiles (17), but tRNA modifications in low-temperature archaea have not previously been examined. We report here a detailed study of the identities and levels of nucleoside modifications in unfractionated tRNA from the psychrotolerant archaeon Methanococcoides burtonii (20). Cultures were grown at 23°C (the optimum growth temperature) and at 4°C (closer to the natural habitat temperature of 1 to 2°C [20]) in order to examine the overall level of tRNA modifications in comparison with that in bacteria, as well as recently studied mesophilic and thermophilic methanococci (32), and to assess the influence of a significant reduction in culture temperature upon modification. For contrast within the archaeal domain, we examined tRNA from the hyperthermophile Stetteria hydrogenophila (25) cultured at 93°C, near the growth optimum of 95°C. In both cases nucleoside modifications were measured by analysis of total enzymatic digests of tRNA using combined LC/MS, a definitive method for structural identification of RNA nucleoside modifications (7, 39).
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, pseudouridine; Um, 2'-O-methyluridine; m1
, 1-methylpseudouridine; s2U, 2-thiouridine; s4U, 4-thiouridine; mnm5s2U, 5-methylaminomethyl-2-thiouridine; m5C, 5-methylcytidine; m5Cm, 5,2'-O-dimethylcytidine; Cm, 2'-O-methylcytidine;
Cm, N4,N4,2'-O-trimethylcytidine; ac4C, N4-acetylcytidine; ac4Cm, N4-acetyl-2'-O-methylcytidine; m1A, 1-methyladenosine; m2A, 2-methyladenosine; m6A, N6-methyladenosine;
A, N6,N6-dimethyladenosine; t6A, N6-threonylcarbamoyladenosine; m6t6A, N6-methyl-N6-threonylcarbamoyladenosine; hn6A, N6-hydroxynorvalylcarbamoyladenosine; hn6A + CH3, monomethyl derivative of hn6A; ms2t6A, 2-methylthio-N6-threonylcarbamoyladenosine; ms2hn6A, 2-methylthio-N6-hydroxynorvalylcarbamoyladenosine; Am, 2'-O-methyladenosine; I, inosine; m1I, 1-methylinosine; m1G, 1-methylguanosine; m2G, N2-methylguanosine; m7G, 7-methylguanosine; Gm, 2'-O-methylguanosine; m22G, N2,N2-dimethylguanosine; m2Gm, N2,2'-O-dimethylguanosine;
Gm, N2,N2,2'-O-trimethylguanosine; m3G, trimethylguanosine; m2,7Gm, N2,7,2'-O-trimethylguanosine; o8G, 8-oxoguanosine; imG, wyosine; imG2, isomer of imG; imG*, demethyl isomer of wyosine; mimG, methylwyosine; G+, archaeosine; MH+, molecular ion, corresponding to the protonated molecule;
, base fragment ion, corresponding to the protonated free base of a nucleoside; SME medium, synthetic marine medium; HPLC, high-performance liquid chromatography; LC/MS, liquid chromatography-electrospray ionization mass spectrometry; Tm, melting temperature. Cell sources and culture conditions. M. burtonii (DSM 6242) was isolated from Ace Lake in Antarctica, where the in situ temperature is annually 1 to 2°C (20). It has an optimal growth temperature of 23°C and an upper growth temperature limit of approximately 28°C (20). To prepare biomass for tRNA extraction, cells were grown anaerobically in a modified methanogen growth medium (47) at 4 and and 23°C, the cells were harvested by centrifugation (10,000 x g), and the pellet was lyophilized.
S. hydrogenophila (DSM 11227) was cultivated in half-strength SME medium as described previously (25). Mass cultures were grown in a 100-liter enamel-coated fermentor at 93°C at pH 6.0. The agitation rate was 100 rpm, and the gassing rate was 2 liters/min (H2/CO2 = 80:20).
Isolation and enzymatic digestion of tRNA. tRNAs were isolated as described previously (5) and totally digested to nucleosides using nuclease P1, phosphodiesterase I, and bacterial alkaline phosphatase (8), usually on a scale of several tens of micrograms of tRNA.
Analysis of tRNA digests by LC/MS. Nucleoside mixtures produced by enzymatic hydrolysis of tRNA were analyzed using an LC/MS system consisting of a Quattro II (Micromass) triple-quadrupole mass spectrometer with a Z-spray ion source interfaced to an HP 1090 (Hewlett-Packard) liquid chromatograph with a photodiode array detector, with both instruments under the control of MassLynx 3.4 (Micromass) software. Under typical operating conditions, mass spectra of quality suitable for nucleoside identification using this system can be obtained at limits of detection of approximately one modified nucleoside per 5 x 103 total nucleosides in a digest of unfractionated tRNA, a ratio constrained largely by HPLC column loading limits.
Chromatographic separation of nucleosides (see Fig. 1 and 2) was carried out with a Luna C18 (Phenomenex) reversed-phase column (2.0 by 250 mm), thermostatted at 40°C, with a buffer gradient system composed of 5 mM ammonium acetate (pH 5.3) (buffer A) and acetonitrile-water (40:60, vol/vol) (buffer B) at a flow rate of 0.3 ml/min, essentially as described previously (19). Analysis of dihydrouridine in M. burtonii tRNAs (see Fig. 3) was made with a Develosil RP-Aqueous (C30) (Phenomenex) reversed-phase column (250 by 2 mm), with the same buffer system as above but using a multilinear gradient from 100% A to 100% B over 24 min. The procedures for the LC/MS experiments and the interpretation of resulting data for identification of nucleosides were similar to those detailed earlier for a thermospray, rather than electrospray, ionization-based protocol (39).
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FIG. 1. LC/MS analysis of nucleosides from unfractionated tRNA of M. burtonii cultured at 4°C (A) or 23°C (B). Components: 1, D; 2, ; 3, m1 ; 4, m1A; 5, m7G; 6, Cm; 7, s4U; 8, m1G; 9, Gm; 10, m2G; 11, G+; 12, G; 13, t6A; 14, m6A; 15, imG*; 16, hn6A; 17, A (non-tRNA nucleoside; see the text); 18, ms2hn6A.
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FIG. 2. LC/MS analysis of nucleosides from unfractionated tRNA of S. hydrogenophila cultured at 90°C. Components: 1, ; 2, m5C; 3, m1A; 4, Cm; 5, I; 6, m7G; 7, o8G (non-tRNA nucleoside; see the text); 8, Um; 9, m5Cm; 10, m1I; 11, m1G; 12, Gm; 13, ac4C; 14, m2G; 15, t6A; 16, m3G isomer of unknown structure; 17, G; 18, Am; 19, m24Cm (non-tRNA nucleoside, see the text); 20, ac4Cm; 21, m2A; 22, m6A; 23, m2Gm; 24, hn6A; 25, ms2t6A; 26, m2,7Gm; 27, imG; 28, Gm; 29, hn6A + CH3; ms2hn6A; 30, 31, imG isomer of unknown structure; 32, unknown nucleoside N415; 33, A (non-tRNA nucleoside, see text); 34, mimG.
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FIG. 3. LC/MS detection of D in tRNA from M. burtonii cultured at 4°C (A) and 23°C (C), based on response using the MH+ ion, m/z 247. Relative peak areas (407 and 429 units) compared with corresponding responses from uridine (26,500 and 25,300 units) (B and D) show relative levels of D of 1.54% at 4°C and 1.69% at 23°C. The baselines used for area integrations are indicated in panels A and C.
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Calculation of relative tRNA modification levels. Crude estimates of overall modification levels for each tRNA were calculated from HPLC peak areas from UV detection at 260 nm, using MassLynx chromatography software routines. Based on total peak areas of 100% (including unmodified A, U, G, and C), the sum of modified nucleoside peak areas for each organism is presented as a portion of the total. Although individual nucleosides exhibit different molar absorptivities, for example in purines versus pyrimidines, the aggregate absorptivities and molar ratios of purines and pyrimidines are considered sufficiently similar to allow crude estimates of modification levels to be derived in this fashion. Responses from deoxynucleosides resulting from residual DNA impurities, readily recognized from their mass spectra, were excluded from the calculations.
Estimates of the average numbers of residues of modified nucleosides m2G, m2Gm,
G, and
Gm per tRNA molecule were calculated as follows. Percents A, U, G, and C were calculated from respective HPLC peak areas using the following relative 260 nm UV response values, which were established from an equimolar nucleoside digest that had been analyzed by HPLC using the same buffered gradient as for LC/MS measurements: A, 1.0; U, 0.685; G, 0.80; and C, 0.49. Individual nucleoside abundances were then referenced via HPLC peak areas to percent G, assuming a molar absorptivity (
) ratio of 0.86 for
G:
G (22) (and therefore for
G:
Gm as well), and a molar absorptivity ratio of 1.22 for
G:
m2G (and therefore for
G:
Gm), all at 260 nm (22). The residue-per-tRNA abundance values were calculated assuming 76 nucleotides per tRNA molecule.
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A) and three in S. hydrogenophila (o8G,
Cm, and
A) were judged not to be native nucleosides from tRNA (see below). Therefore, a total of 17 nucleosides from M. burtonii tRNA and 31 nucleosides from S. hydrogenophila tRNA were characterized. All isolates were found to contain 2'-deoxyribonucleosides resulting from DNA impurities, which were readily identified from their characteristic mass spectra and relative retention times (39). |
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TABLE 1. Summary of ribonucleosides identified in unfractionated tRNA
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The detection of D, a modified nucleoside having essentially no UV-absorbing chromophore and thus not detectable with a conventional UV detector, was based on mass analysis using the MH+ ion, m/z 247 (Fig. 3A and C). For this purpose a C30 reversed-phase HPLC column was used in which D (Mr, 246) separates completely from
(Mr, 244). Use of this column avoids overlapping (in time) signals from D and the second isotope peak of
(both m/z 247), as found with the more commonly used C18 reversed-phase system (39). The D/uridine ion current ratios shown in Fig. 3 reflect an average D level of between one and two residues per tRNA molecule. This estimate is based on comparison with D and uridine ion current signals from unfractionated Escherichia coli tRNA in which the amounts of the two nucleosides had been accurately determined by a stable-isotope dilution method (11) and the assumption that uridine contents of E. coli and M. burtonii tRNAs are similar.
s4U (component 7) was distinguished from the 2-thio isomer by its UV spectrum:
max, 331 nm for component 7; the values in the literature (21) are 331 nm for s4U and 275 nm for s2U. The 17-min HPLC peak in Fig. 1A and B is composed of two nucleoside isomers (components 8 and 9) with the same molecular mass (Mr, 297) corresponding to monomethyl guanosines and having essentially the same retention times (39). They are recognized and assigned as m1G and Gm, as indicated by presence of both protonated base ions m/z 166 and 152, respectively, occurring within approximately the same elution profile (7). Similarly, the hypermodified nucleoside G+ (component 11 in Fig. 1) elutes in the leading edge of a much larger amount of 2-deoxyadenosine from DNA impurity but is easily mass detected by using its unusual molecular ion (MH+, m/z 325) and base ion (
, m/z 193) mass values. The complex amino acid-containing nucleoside hn6A (component 16 in Fig. 1) was distinguished from an isomer known in bacterial tRNA (m6t6A), which differs from hn6A by the placement of a methyl group in the amino acid side chain (40). Differentiation between the two isomers was based on further fragmentation of the base ion (
, m/z 295), whose mass is common to both possibilities. Formation of m/z 136 from adenine and m/z 134 from protonated hydroxynorvaline, rather than m/z 150 (methyladenine) and m/z 120 (threonine), as would be required for the isomer m6t6A, indicated the identity of component 16 as hn6A. One nucleoside with a partially known structure was encountered in M. burtonii tRNA, designated imG* in Fig. 1 and Table 1. This nucleoside (Mr, 321), previously found in tRNAs from five methanococci (32), is a member of the imG tricyclic nucleoside family, as shown by its characteristic UV spectrum (26) (UV
max, 228 and 282 nm). The molecular mass corresponds to a nucleoside having two fewer methyl groups than the archaeal nucleoside mimG (Mr, 349), which has three methyls (31). The structure of nucleoside imG* is under investigation. Component 17 in Fig. 1,
A, is a common minor product in tRNA preparations, arising as an easily detected impurity derived from 16S rRNA, in which its presence is unique and ubiquitous in highly conserved sequences (48, 49). Unannotated peaks in Fig. 1 were shown from their mass spectra not to be nucleosides.
S. hydrogenophila nucleosides.
Nucleosides released by hydrolysis of S. hydrogenophila tRNA are represented in a chromatogram of unusual complexity (Fig. 2). o8G (component 7 in Fig. 2) coelutes with m7G (MH+, m/z 298; BH2+, m/z 168) and was identified following deuterium labeling (m/z 300 shift to 308; m/z 168 shift to 174), which showed seven exchangeable hydrogen atoms in the neutral molecule, one more than in guanosine. Component 7 therefore exhibits 16 Da of modification in the base compared with guanosine and no modification in ribose. Assignment of the likely structure as o8G was confirmed by rigorous comparison against authentic material (gift of T. Hashizume, University of Utah): HPLC retention time, 13.7 min; MS (MH+, m/z 300;
, m/z 168). This unexpected component is viewed as a likely product of adventitious oxidation of guanosine, as might result from xenobiotic or metabolic oxidation processes (for discussion and leading references to the sources of this nucleoside in RNA, see references 23 and 52). Support for what we view as the unlikely authenticity of o8G as being native to tRNA would require at a minimum its localization to specific tRNA sequence sites, which was not undertaken. Similar observations and conclusions regarding trace amounts of o8G in some archaeal hyperthermophile tRNAs have been previously made (J. A. McCloskey and K. O. Stetter, unpublished results).
The assignments of site of cytosine methylation in components 2 and 9 as position C-5 (i.e., m5C and m5Cm) rather than as the likewise biologically plausible N4- or N-3 methyl isomers, were made by deuterium labeling. Component 2 showed five exchangeable hydrogens in the neutral molecule and three in the neutral base, while component 9 showed four and three, respectively. Those values mandate methylation at C-5. Substitution at heteroatom positions (N4-or N-3) would result in one fewer exchangeable hydrogen in each case.
The unusual diversity of modifications exhibited by S. hydrogenophila tRNA includes m2A, not previously reported for any type of archaeal RNA (34). Deuterium exchange experiments were used to confirm the assignments shown for the methyladenosine isomers m2A and m6A (Fig. 2) made initially by relative retention times and mass spectra. Their isotopic exchange patterns likewise differ due to C versus N alkylation sites, respectively: m2A contains five exchangeable hydrogens in the neutral molecule (component 21), while m6A contains four (component 22).
The presence of both methylguanosine isomers m1G and Gm (components 11 and 12 in Fig. 2) was established by using the base ions as in the case of M. burtonii (Fig. 1) described previously. All other assignments of multiple components eluting in unresolved HPLC peaks were made on the basis of molecular ion and base ion mass values and relative retention times, as appropriate (39).
Three additional nucleosides with partially known structures and one with an unknown structure were found in the S. hydrogenophila digest. In all four cases, the characteristic 132- mass-unit spacing between MH+ and
ions (due to loss of ribose) was used to identify each component as a ribonucleoside, without a substitution in ribose. Component 16 (Fig. 1) (UV
max, 261.5 nm) is judged from its molecular mass (Mr, 325) and base mass as likely to be a base-trimethylated derivative of guanosine. The potential mass isomer acetylguanosine (not a known RNA component) cannot be excluded, although its elution position would likely be much later. Component 29 is assigned as a methyl homolog of the complex amino acid-containing nucleoside hn6A (40), based on a molecular mass of 440, which is 14 higher than that of hn6A (Mr, 426). Upon deuterium exchange the MH+ ion m/z 441 shifted to m/z 449, requiring seven exchangeable hydrogens in the neutral molecule. This shift value is the same as for nucleoside hn6A, consistent with substitution by the additional methyl group to be on carbon rather than a heteroatom (N or O).
Two nucleosides observed are considered likely to arise as minor impurities from small-subunit rRNA:
A and
Cm (components 33 and 19 in Fig. 2). The arguments concerning the origin of
A are presented above. The novel trimethylcytidine
Cm was recently discovered and characterized in trace amounts in a tRNA isolate from the hyperthermophilic archaeon Aeropyrum pernix; it was concluded to arise as an impurity from 16S rRNA, where it was found in greater abundance (R. Van Wagoner, E. Bruenger, G. M. Caballero, N. Nomura, Y. Sako, and J. A. McCloskey, unpublished data), and is therefore similarly assigned in the present case to rRNA.
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TABLE 2. Structural diversity and modification levels of nucleosides in selected unfractionated tRNAs
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It is important to note that the overall extent of modification is also subject to the influence of phylogeny, the effects of which cannot always be clearly distinguished from those associated with temperature. An unusual but notable example is the similarity of modification levels between M. maripaludis and M. igneus (Table 2), which grow optimally at very different temperatures. However, if the levels of specific modifications closely tied to thermostability are considered, a clearer picture of temperature effects emerges: e.g., the trimethylated guanosine
Gm, believed to be a stabilizing entity at tRNA stem junctions, is present in M. igneus (85°C) but absent in M. maripaludis (37°C) (32). (Further discussion of
Gm is given below in the section on S. hydrogenophila.) For comparison of organisms not closely related the phylogeny, temperature distinction is also confounded by the present lack of sufficient data to gain a refined picture, particularly with regard to bacterial thermophiles, for comparison with a large body of data on archaeal thermophiles (17, 27, 33).
The differences between M. burtonii and S. hydrogenophila in overall modification, when considered in terms of the numbers of structural motifs employed at the nucleoside level (Table 2), are similarly great. The finding of 31 different modified nucleosides in S. hydrogenophila tRNAs is the greatest number of which we are aware, based on earlier reports of tRNA modification in various archaeal hyperthermophiles (17, 32, 33) and eukarya, including unfractionated calf liver tRNA (21). The occurrence of nine different methylated guanosines is particularly striking. The structural diversity of nucleosides in M. burtonii, 17 modified nucleosides, is greater than that in the bacterium ANT-300 but still significantly below that of other representative organisms (Table 2). The strong apparent correlation between temperature of growth and number of modification motifs recruited by the RNA-processing enzymes seems to be more pronounced at higher temperatures, at least within the archaea. This probably reflects the essential need for mechanisms of tRNA stabilization at growth temperatures generally above the melting points of unmodified tRNA base-paired stems (a summary of Tm values in relation to G+C content and the role of modification can be found in reference 27). Additional comparisons of modification patterns, between closely related archaeal mesophiles and thermophiles from selected methanococci, have been reported (32).
M. burtonii is shown (Fig. 3) to contain significant amounts of D, a nucleoside associated with maintenance of polynucleotide flexibility in RNA (12). This modification is absent in S. hydrogenophila and in most other archaeal hyperthermophiles and mesophiles examined (17), unlike its wide occurrence in eukarya and bacteria, including the bacterial thermophiles (45). Within archaea, the finding of D in abundance only in M. burtonii supports and extends the interpretation of its functional importance in psychrophilic bacteria (10). The occurrence of more than one D residue per tRNA molecule in M. burtonii is about the same as that in E. coli (1.79 mol%) (11) but is greater than that in other archaea studied to date. Thus, posttranscriptional enzymatic processing to form D appears to be a common mechanism for adaptation to the cold in both archaea and bacteria.
Quantitative data for D incorporation is not available for other cold-adapted archaea. Recently, however, putative D synthase genes were identified in the partial genome sequences of M. burtonii and the psychrophilic methanogen Methanogenium frigidum (44). This indicates that D incorporation may be a general characteristic of cold-adapted archaea. No convincing evidence was obtained that levels of D are responsive to a decrease in growth temperature (Fig. 3), although it will be interesting to examine regulation of expression of the D synthase gene.
We know of no previous effort to document the presence versus the absence of D or the level of D as a function of temperature in tRNA from any given organism. Thus, there is no evidence for a response opposite to that found for bacterial (2, 51) and archaeal (27) thermophiles (increase in abundance of selected stabilizing modifications with culture temperature). However, it was shown that in small D-containing oligonucleotides the fractional population of the inherently more flexible C-2'-endo ribose conformer of D increases at lower temperatures (12). Therefore, in contrast to a presence-versus-absence mechanism for preservation of conformational flexibility at lower temperatures, the influence of D in those organisms may reside to some extent in a thermodynamic preference for favored ribose conformers in existing D residues present in the D and T loops.
Both M. burtonii and S. hydrogenophila contain tRNA modifications that have been formed potentially under the direction of small RNAs known under the generic name of guide RNAs (15, 38). These modifications are pseudouridines (in both organisms) and ribose-methylated nucleosides (in S. hydrogenophila). Modification targeting by sRNAs has been studied mostly with regard to rRNA modification in eukarya but has been reported to operate also in some archaeal tRNAs (15, 38, 46). The extent to which these mechanisms of modification operate in the present case is unknown, and progress is confounded by the absence of knowledge regarding isoacceptor tRNA sequences, which remains a worthwhile area for future investigation.
Modifications in M. burtonii.
The strikingly low levels of tRNA modification that occur in M. burtonii include nine nucleosides that are common to RNA in all three phylogenetic domains (34) (Archaea, Bacteria, and Eukarya) and thus constitute a minimalist core of modifications that probably evolved prior to the separation of these domains. These modified species are D,
, and the simple monomethylated nucleosides Cm, Gm, m1G, m7G, m1A, and m6A. Two of the modifications, m1
and G+, are unique hallmarks of archaeal modification that occur widely but are each highly conserved at single sequence locations, tRNA positions 54 and 15, respectively (45). The remaining nucleosides are evenly divided from the perspective of phylogenetic commonality: s4U, hn6A, and ms2hn6A are shared with bacteria, while the guanosine derivatives m2G,
G, and imG* are otherwise characteristically eukaryotic (34). Notably absent in tRNA from M. burtonii is the complex anticodon nucleoside mnm5s2U, recently detected in four mesophilic and thermophilic methanococci (32). However, mnm5s2U is usually considered a bacterial modification (in tRNA-Glu and -Lys [45]) which is otherwise unknown in archaeal tRNA and may be restricted only to the methanococci. Overall, these findings substantially add to our limited understanding of the mechanisms of adaptation in psychrotolerant archaea (6).
Modifications in S. hydrogenophila.
A significant fraction of the unusual number and diversity of modifications in S. hydrogenophila, 9 of 31 nucleosides, are modified by methylation at O-2' of ribose and are therefore assumed to exert influences through points of regional stabilization of the folded tRNA molecule. This effect is attributed to thermodynamic stabilization of the C-3'-endo sugar conformation, thus avoiding base-O-2' steric interactions in the alternate C-2'-endo conformation (14), resulting in higher Tms (9) and reduced dynamic motion at elevated temperatures. Previous studies have demonstrated increased levels of ribose methylation as a function of culture temperature, in both tRNA (2, 27, 28) and rRNA (37). Two nucleosides found in S. hydrogenophila, ac4Cm and
Gm (and the related modification m2Gm), were reported to be temperature responsive in tRNA from the archaeal hyperthermophile Pyrococcus furiosus (27). The family of structurally related nucleosides, m2G,
G, m2Gm, and
Gm, are from known archaeal tRNA sequences, conserved at only two locations, positions 10 and 26 (45). Nucleotides at these locations are at the junctions of the acceptor and D-loop stems and of the D-loop and anticodon stems, respectively, where they play crucial roles in the control and stabilization of the tertiary L fold of the tRNA (42). The unusual abundance of
Gm in Fig. 2, taking UV molar absorptivities into account, corresponds to an average of approximately 0.6
Gm residues per tRNA molecule, while the estimated sum of the four modifications is approximately two residues per molecule. This implies that essentially all tRNAs from S. hydrogenophila are modified at both positions, in contrast to M. burtonii (Fig. 1, components 10 and 12), in which an average of only
0.2 residues per molecule are modified in this fashion. This result further extends the implication of these residues in tRNA stabilization in the archaeal thermophiles (27, 32) and their greatly reduced role in tRNA from M. burtonii.
This study was supported by grants from the National Institute of General Medical Sciences (J.A.M.), by the Fonds der Chemischen Industrie (M.T.), and by grants from the Australian Research Council (R.C.).
Present address: Department of Biological Chemistry, University of Michigan, Ann Arbor, MI 48109-0606. ![]()
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