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Journal of Bacteriology, March 2002, p. 1481-1487, Vol. 184, No. 5
0021-9193/02/$04.00+0 DOI: 10.1128/JB.184.5.1481-1487.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.
-Proteobacterium Isolated from a Deep Subsurface Environment
Department of Biology and New York Center for Studies on the Origins of Life (NSCORT), Rensselaer Polytechnic Institute, Troy, New York 12180
Received 3 July 2001/ Accepted 2 November 2001
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-subdivision of Proteobacteria and isolated from a deep subsurface environment. The subsurface isolate SMCC D0715 was identified as belonging to the genus Pseudomonas. The group I intron from this isolate is the first to be reported for
-proteobacteria, and the first instance of a tRNALeu(UAA) group I intron to be found in a group of bacteria other than cyanobacteria. The 231-nucleotide (nt) intron's sequence has group I conserved elements and folds into a bona fide group I secondary structure with canonical base-paired segments P1 to P9 and a paired region, P10. The D0715 intron possesses the 11-nt motif CCUACG ... UAUGG in its P8 region, a feature not common in bacterial introns. To date, phylogenetic analysis has shown that bacterial introns form two distinct families, and their complex distribution suggests that both lateral transfer and common ancestry have taken part in the evolutionary history of these elements. |
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- and ß-proteobacteria, that have been shown to possess group I introns (6, 18, 23, 24, 26, 28, 35). All bacterial group I introns found to date reside in the anticodon loop regions of tRNA genes. While cyanobacteria have been demonstrated to possess a group I intron in either the tRNALeu(UAA) or tRNAfMet gene, or both (6, 24), introns from three divergent species of
-proteobacteria (23, 26) and one species of a ß-proteobacterium (26) interrupt the tRNAArg(CCU) and tRNAIle(CAU) genes, respectively.
It appears that tRNAfMet and tRNAArg(CCU) group I introns are sporadically distributed among cyanobacteria and
-proteobacteria, respectively, and they are thought to have arisen recently by horizontal transfer (23, 24). The data available on the ß-proteobacterial tRNAIle(CAU) intron are insufficient to draw any conclusions regarding its distribution and/or origin (26, 32). To date, the bacterial tRNALeu(UAA) group I intron has only been found in cyanobacteria. It has been suggested that there are at least two subfamilies of this intron originating by different evolutionary pathways and independently of each other. The phylogenetic distribution of this intron in one subfamily has been demonstrated to be consistent with an ancient origin and an inheritance through common ancestry (24). Conversely, the tRNALeu(UAA) introns in a second subfamily seem to share a more recent common ancestor with the
-proteobacterial tRNAArg(CCU) introns and originated from a tRNAArg(CCU)-like intron through horizontal transfer (27, 28).
Inasmuch as it has become evident from previous studies (5, 24) that determination of the phylogenetic distribution of group I introns is a valuable tool to assess their evolutionary history, we were interested in undertaking a systematic investigation of the abundance, phylogenetic distribution, and diversity of group I introns among
-, ß-, and
-proteobacteria obtained from deep subsurface environments. The earth's deep subsurface (depth of 100 to 1,000 m), once considered a lifeless place, has now firmly been shown to be home to a host of bacteria (1, 3, 13, 31). In such environments, bacteria often obtain only limited nutrients and energy and hence are capable of maintaining only very slow growth. The available geological data indicate that in certain subsurface environments, there has been no or minimal transport of microorganisms between different types of sediments (14, 16, 30). Bacteria in such environments are likely to be descendants from the original bacteria present at the time of deposition, being isolated from modern surface populations for hundreds of millions of years (14). Taken together with the possibility of reduced selective pressure for rapid multiplication and hence for genome streamlining in subsurface environments, such bacteria might have a higher probability of retaining genetic features of original ancestor bacteria and, as such, may provide a unique source of intron sequences mostly lost from surface populations.
The present study explores the presence and distribution of group I introns in proteobacteria isolated from subsurface environments. These isolates are part of the Deparment of Energy (DOE) Subsurface Microbial Culture Collection (SMCC) housed at the Florida State University in Tallahassee (1, 4) and obtained from sediments of different depths (up to 526 m) from the DOE Savannah River site in Aiken, S.C. (30). We report results of our survey of a limited number of subsurface
-proteobacterial isolates and the discovery of a novel group I intron, which resides in the anticodon loop of the tRNALeu(UAA) gene of a
-proteobacterium belonging to Pseudomonas strain D0715.
Bacterial strains and growth conditions.
Subsurface bacterial strains were obtained from the SMCC as living cultures recovered from glycerol stocks prior to shipping. All cultures originated from samples collected in 1986 to 1988 at the DOE Savannah River site in Aiken, S.C. (30). The cultures were grown in PTYG medium (2) at 30°C on a shaker. In our laboratory, the cultures were stored as glycerol stocks (at -80°C) and recovered only for DNA extraction as needed. Fifty subsurface isolates were screened for the presence of group I introns by dot blot hybridization with the group I intron-specific oligonucleotide probe Q20 (M. E. Frischer and S. A. Nierzwicki-Bauer, unpublished data). Fifteen of the 18 isolates, which were identified as potentially harboring group I introns, were shown to belong to the
-proteobacteria and were selected for the present study (Fig. 1).
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FIG. 1. Phylogenetic affiliations of 15 subsurface bacterial isolates with other members of the -subdivision of Proteobacteria as inferred from SSU 16S rRNA gene sequences. The SSU 16S ribosomal DNA (rDNA) from subsurface isolates was PCR amplified from purified DNA with universal oligonucleotide primers (4, 34). Bacterial SSU 16S rRNA gene sequences were retrieved from GenBank. The tree was constructed by the neighbor-joining method (29) and drawn by using TREECON 1.3b software (33). A distance matrix was calculated from the Galtier and Gouy two-parameter equation (15). Bootstrap percentage values, based on 100 resamplings, are shown at the internal nodes. Only values higher than 50% are shown. The scale bar corresponds to 10 nt substitutions per 100 sequence positions. The SSU rRNA gene sequence of the -proteobacterium Agrobacterium tumefaciens was used as an outgroup to position the root (not shown). The sediment depth from which the isolates were obtained is indicated in brackets next to the SMCC number.
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-proteobacteria.
The initial approach used was to PCR amplify genes coding for tRNAfMet, tRNAArg(CCU), and tRNALeu(UAA), because all group I introns discovered in bacteria to date reside only in the anticodon loop regions of tRNA genes. Amplification of an uninterrupted tRNA gene should result in a product of approximately 75 bp, whereas an amplification product of a gene with a residing intron should be 300 to 400 bp in size or greater, provided the intron contains an open reading frame. To exclude possible PCR-induced sequence errors, two to three different clones from independent PCRs were analyzed.
PCR amplification of tRNAfMet and tRNAArg genes.
Genes coding for tRNAfMet and tRNAArg(CCU) were amplified by PCR using previously published primers (6, 23). The results suggested that tRNAfMet and tRNAArg(CCU) genes in the subsurface
-proteobacteria were not interrupted by introns. However, with respect to the tRNAfMet genes from subsurface
-proteobacteria, in 14 of 15 isolates, amplification of tRNAfMet gene produced products of one of three sizes, namely 236, 263, or 376 bp, in addition to the tRNA-size (76 bp) product (data not shown). In all instances, the larger products were clusters of two uninterrupted tRNAfMet genes. A similar observation was reported by Biniszkiewicz et al. (6). Twelve isolates possessed identical tRNAfMet genes, with 2 other tRNAfMet gene sequences found in isolates B0138 and B0208 (Fig. 2). All of the gene sequences had hallmark diagnostic features for bacterial tRNAfMet, including 3 consecutive G-C bp closing the anticodon stem (25), and they shared identical sequences up to the T stem region. When pairwise comparisons were made, these sequences revealed 5.2 and 6.5% mismatches, most of which were in the T stem (see the legend to Fig. 2).
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FIG. 2. Alignment of three reconstructed tRNAfMet gene sequences amplified by PCR from subsurface -proteobacteria. The sequence of each tRNA was derived from the cloned PCR products of clusters of two uninterrupted tRNAfMet genes. In tandems, the 5" and 3" ends consisted primarily of the primer sequences. Presuming that tRNAs in tandems were identical, chimeric tRNA genes were reconstructed. The reconstructed genes consisted of the 5" end of the second tRNA gene (in the tandem) and the 3" end of the first, and the anticodon stem-loop region was a consensus of both. Base pairings (underline) in the acceptor stem (A), anticodon stem (Ac), D stem (D), and T stem (T), as well as the anticodon (double underline), are indicated. Sequences: 1, tRNAfMet from isolate B0138; 2, tRNAfMet from isolate B0208; 3, tRNAfMet from isolates B0205, B0251, B0252, B0259, B0280, B0307, B0310, B0361, B0608, B0628, B0631, and D0715. Pairwise comparison of sequences 1 and 2 and of 1 and 3 shows 5.2% mismatches; pairwise comparison of sequences 2 and 3 shows 6.5% mismatches.
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FIG. 5. (A) Secondary structure of the tRNALeu(UAA) intron from the subsurface -proteobacterium isolate D0715. The representation format is that of Cech et al. (8). Exon sequences are in lowercase, and intron sequences are in uppercase letters. P1 to P9 refer to conserved double-stranded segments of group I introns. Boxed sequences in P1 and the 3" exon show the P10 pairing. Putative splice sites are marked by arrows. The circled G-C pair in P7 locates the G-binding site (20). The 13-nt motif in P6 and the putative tertiary interaction between P2 and P8 are boxed. (B) Proposed secondary structure of the tRNALeu(UAA) from the subsurface isolate D0715. PCR-amplified portions of the anticodon loop and stem and the extra arm are shown in black. The sequences of the PCR primers are shown in light gray lowercase italics. Missing nucleotides in the 5" portion of the acceptor stem are shown as a dotted arrow. The D0715 intron insertion site is indicated by a solid arrow.
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FIG. 3. PCR amplification of tRNALeu genes from subsurface -proteobacteria. Shown is migration in a 2.5% agarose gel of the amplification products obtained by PCR with some tRNALeu primer pairs and various -proteobacterial DNAs. (A) tRNALeu PCR primers W5-W3. (B) tRNALeu PCR primers W5-V3. (C) tRNALeu PCR primers W5-P3. Lanes: 1, B0138; 2, B0205; 3, D0715; 4, B0208; 5, B0251; and 6, B0333. -, no DNA (negative control); M, 1-kb DNA marker (Gibco BRL). Sizes in base pairs are indicated on the left side of the gel.
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FIG. 4. Partial alignment of group I intron sequences from proteobacteria. Shown are (i) tRNAArg(CCU) introns from three -proteobacteria, Agrobacterium tumefaciens A136 (Ag. tumef) (26), Azospirillum halopraeferens Au5 (Az. halop) (23), and Anaplasma marginale (A. marg) (23); (ii) the tRNAIle(CAU) intron from the ß-proteobacterium Azoarcus sp. strain BH72 (Azoarcus) (26); and (iii) the tRNALeu(UAA) intron from the subsurface -proteobacterium isolate D0715. Group I intron secondary structure elements (P1 to P9) are indicated above the sequences. Putative base pairings are underlined. Numbers in brackets indicate the number of bases in the omitted sequence. Dashes represent gaps used to improve the alignment.
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Phylogenetic relationship between the D0715 group I intron and related bacterial introns.
To analyze the phylogenetic relationship between the D0715 group I intron and other bacterial group I introns, a representative sample of 20 sequences of known bacterial introns was aligned based on the potential secondary structure, rather than similarities in the primary sequence. There were 289 positions that could be unambiguously aligned. Five introns in this alignment represented proteobacteria: three were
-proteobacteria [tRNAArg(CCU) introns from Agrobacterium tumefaciens, Azospirillum halopraeferens, and Anaplasma marginale], one was a ß-proteobacterium [tRNAIle(CAU) intron from Azoarcus sp.], and one was a
-proteobacterium [tRNALeu(UAA) intron from subsurface isolate D0715]. All of the rest were tRNALeu(UAA) and tRNAfMet introns from various cyanobacteria. The phylogenetic analysis demonstrated that bacterial group I introns dichotomized, forming distinct families (Fig. 6). The branches separating two intron families were reasonably supported by bootstrap values between 53 and 100%. This separation was reproducible in trees inferred by the parsimony method (not shown). Within the families, however, not all branches were well supported, with bootstrap values below 50%. Additionally, the topology varied slightly, depending on the method used and the data set. This presumably reflects the small number of positions that could be used in this analysis and the high degree of divergence of these sequences. One intron family was homogeneous and consisted exclusively of group I tRNALeu(UAA) introns from various cyanobacteria, whereas in a second family, introns, interrupting different tRNAs, seemed to be scattered across bacterial phylogenetic boundaries, comprising tRNAArg(CCU) introns from
-proteobacteria, the tRNAIle(CAU) intron from a ß-proteobacterium, tRNAfMet introns from cyanobacteria, and tRNALeu(UAA) introns from a
-proteobacterium and cyanobacteria. In the second family, the tRNAfMet introns formed a very well supported tight cluster with bootstrap value of 98%, the topology remaining unchanged regardless of the data set and method used. The cyanobacterial tRNALeu(UAA) intron subtree within this family formed a stable cluster of two filamentous and one unicellular species with relatively good bootstrap values and a stable topology, whereas the
-proteobacterial tRNAArg(CCU) intron subtree was in general poorly supported. However, the tRNAArg(CCU) intron subtree was reasonably well supported (bootstrap values between 50 and 67%) in maximum parsimony trees (not shown). The D0715 tRNALeu(UAA) intron branched deeply and appeared to be more related to either tRNAArg(CCU) introns from
-proteobacteria or the tRNAIle(CAU) intron from Azoarcus sp. than to any tRNALeu(UAA) or tRNAfMet introns from cyanobacteria. In some distance trees, the D0715 intron clustered with the tRNAIle(CAU) intron from Azoarcus sp. (not shown), albeit with relatively low bootstrap values. Nevertheless, this clustering was well supported by bootstrap values of up to 85% in maximum parsimony trees (not shown). This intron never clustered with cyanobacterial tRNALeu(UAA) introns from either family or tRNAfMet introns.
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FIG. 6. Phylogenetic analysis of bacterial tRNA group I introns. The tree was inferred from an alignment of the intron core sequences (289 positions) by using the neighbor-joining algorithm (29) and drawn with the TREECON 1.3b software (33). A distance matrix was calculated from the Kimura two-parameter equation (17). Bootstrap percentage values, based on 100 resamplings, are shown at the internal nodes. Only values higher than 50% are shown. The scale bar corresponds to 10 nt substitutions per 100 sequence positions. The tRNALeu(UAA) intron sequence from the chloroplast of Marchantia polymorpha (CP) (22) was used as an outgroup to position the root. Branches separating two intron families are shown in boldface. [tArg], tRNAArg(CCU) intron; [tfMet], tRNAfMet intron; [tLeu], tRNALeu(UAA) intron. The intron sequences were obtained from the following sources: for - and ß-proteobacteria, see the legend to Fig. 4; for Anabaena cylindrica, Anabaena sp. strain PCC7120, Chlorogloeopsis fritschii, Cylindrospermum sp. strain PCC7417, Dermocarpa sp. strain PCC7437, Gloeobacter violaceus PCC7421, Oscillatoria sp. strain PCC6304, and Pseudoanabaena sp. strain PCC7403, see reference 24; and for Aphanizomenon flos-aquae NIVA-CYA 142(1) and 142(2), Microcystis aeruginosa NIVA-CYA 57, Nostoc sp. strain NIVA-CYA 246, Nostoc sp. strain NIVA-CYA 308(1) and 308(2), see reference 28. The clustering of Aphanizomenon flos-aquae NIVA-CYA 142(1) and 142(2) and of Nostoc sp. NIVA-CYA 308(1) and 308(2) is different from that in the original report (28). This discrepancy was caused by an error in the database (K. Rudi, personal communication).
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Nucleotide sequence accession number. The nucleotide sequences generated in this study have been deposited in GenBank under the following accession numbers: AF336311, isolate D0715 SSU 16S rRNA gene; AF336313, isolate D0715 tRNALeu(UAA) group I intron; AY029759, isolate B0333 SSU 16S rRNA gene; and AY029760, isolate B0333 tRNALeu(UAA) group I intron-like sequence.
We thank David Balkwill for providing us with the bacterial cultures; Jennifer C. Reineke for technical assistance; Ellen Braun-Howland and Marc Frischer for sharing unpublished data; and David Shub for helpful discussions, suggestions, and critical reading of the manuscript.
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-purple bacteria: evidence for horizontal transmission and transposition of a group I intron. J. Bacteriol. 181:1049-1053.
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