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Journal of Bacteriology, January 2002, p. 318-322, Vol. 184, No. 1
0021-9193/01/$04.00+0 DOI: 10.1128/JB.184.1.318-322.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.
Sequencing of Flagellin Genes from Natrialba magadii Provides New Insight into Evolutionary Aspects of Archaeal Flagellins
Inna Serganova,1 Vladimir Ksenzenko,1 Alexander Serganov,1,
Irina Meshcheryakova,1 Michael Pyatibratov,1 Olesya Vakhrusheva,1 Antonina Metlina,2 and Oleg Fedorov1*
Institute of Protein Research, Russian Academy of Sciences, Pushchino, Moscow Region 142290, Russia,1
A. N. Belozersky Institute of Physico-Chemical Biology, Moscow State University, Moscow 119899, Russia2
Received 7 May 2001/
Accepted 3 October 2001

ABSTRACT
We have determined the nucleotide sequence of a flagellin gene
locus from the haloalkaliphilic archaeon
Natrialba magadii,
identified the gene products among proteins forming flagella,
and demonstrated cotranscription of the genes. Based on the
sequence analysis we suggest that different regions of the genes
might have distinct evolutionary histories including possible
genetic exchange with bacterial flagellin genes.

TEXT
Representatives of the two kingdoms
Archaea and
Bacteria have
analogous motility systems composed of long thin appendages
(flagella), which rotate to produce thrust (
1). The bacterial
flagellum filament is mainly composed of a single type of protein.
In contrast, the archaeal filament is formed from multiple types
of flagellin, encoded by a few genes. Surprisingly, the archaeal
flagellins (and related proteins) have homology with bacterial
proteins from the type IV pilin family (
4,
8) but not with bacterial
flagellins (
15). This fact, together with the presence of leader
peptides (
3,
21) and posttranslational modifications (
15) in
archaeal flagellins, suggests that archaeal flagella form in
a manner similar to that in which bacterial pili form but not
similar to that in which bacterial distal tip assembly occurs
(
8). The recent finding of a close relationship between the
chemotaxis systems in gram-positive bacteria and archaea implies
that the entire bacterial system was acquired by archaea (
9).
Since the chemotaxis system is involved in motility, this, in
turn, raises a question about the origins and evolution of archaeal
flagellin genes.
We sequenced flagellin genes from poorly understood haloalkaliphilic archaeon Natrialba magadii, analyzed their expression, and demonstrated their mosaic structure. We suggest that horizontal transmissions might be involved in the evolution of the genes.
Cloning, sequencing, and analysis of N. magadii flagellin genes.
In the present study a 1.2-kbp DNA fragment containing Halobacterium halobium flgA1 and flgA2 genes (33) was used to search for flagellin genes in the genome of the haloalkaliphilic N. (formerly Natronobacterium) magadii. Using Southern blot hybridization (32) we identified 1.4- and 5.5-kbp fragments that gave positive signals with PstI-digested genomic DNA and 6.3- and 12.0-kbp fragments with BamHI-digested DNA. We cloned the 1.4- and 6.3-kbp fragments using plasmid-based libraries. The nucleotide sequences of the 1.4-kbp fragment and part of the 6.3-kbp fragment revealed the presence of two complete open reading frames (ORFs) and one partial ORF (Fig. 1). To sequence the distal part of the operon, we performed four rounds of inverse PCR using as templates SalI-, PstI-, HincII-, and XhoI-digested genomic DNA. The total 4,029-bp nucleotide sequence of the gene cluster contains four complete ORFs of 202, 260, 396, and 262 codons, located close to each other. In addition, we identified the 5' end of the ORF (127 codons), 125 nucleotides (nt) away from the cluster comprising ORF1 to ORF4 (Fig. 1). ORF1, ORF2, and ORF4 are preceded by putative ribosome binding sites with the sequences 5'-GGGTG-3', 5'-GGTGA-3', and 5'-GTGA-3' (25). The most favorable ribosome binding sites for ORF3 (5'-GGTGA-3') and ORF5 (5'-GGAGT-3') are located, however, far from initiation codons: 43 and 35 nt for ORF3 and ORF5, respectively. Thus, ribosomal subunits might bind trinucleotide sequences close to the translation initiation codon.
ORF1 to ORF4 were assigned to the flagellin gene family based
on homology of the deduced amino acid sequences with archaeal
flagellins (Fig.
2A) and were designated genes
flaB1,
flaB2,
flaB3, and
flaB4, respectively (Fig.
1). The amino acid sequence
encoded by ORF5 has some similarity to putative flagellum-related
protein FlaF from
Methanococcus voltae and
Methanococcus jannaschii (24% identity and 49% positives in 93 N-terminal amino acids)
(
4). Flagellins from
N. magadii and other archaea, including
archaea that inhabit very different niches, display high sequence
similarity at the N termini (amino acids [aa] 13 to 60) (Fig.
2A). This indicates that the hydrophobic N termini in all flagellated
archaea have an important role in flagellum core formation (
30).
The less well conserved nine N-terminal residues represent a
signal peptide, which is most likely cleaved between glycine
and glutamine in the RGQ sequence (Fig.
2A) (
20). Although central
regions of the
N. magadii flagellins have limited similarity,
the C-terminal 25 amino acids are very similar to each other
(50% identity) but not to the corresponding flagellin regions
from other archaeal species. FlaB3, the product of the
flaB3 gene, contains an insertion in the middle region and, therefore,
is significantly larger (395 aa) than other flagellins (mostly
195 to 260 aa). The only other example of a large flagellin
(580 aa) was identified in
Pyrococcus kodakaraensis (
27). As
an adaptation to living at high pH, the
N. magadii flagellins
contain a threefold-lower content of arginine and lysine residues
(1.9 to 3.5%) than flagellins of halophile
H. halobium (8.6
to 10.9%). Since the extracellular pH approaches the pK values
of amide groups in Arg and Lys, it can affect the charge of
these residues and may influence stability, folding, or solubility
of the proteins (
17).
Identification of flaB gene transcript and mapping of its 5' terminus.
To identify the transcript(s) for the flagellin gene cluster,
we performed Northern blot hybridization (
32,
37) with the total
RNA isolated from
N. magadii cells and the random
32P-labeled
probe synthesized with the HexaLabel DNA labeling kit (Fermentas
AB, Vilnius, Lithuania). The probe carries the majority of the
flaB3 gene and the conserved 5' end of the
flaB4 gene. Only
one RNA transcript of about 4.5 kb in size was detected, indicating
cotranscription of all flagellin genes and possibly ORF5 as
described earlier for
M. voltae (
4,
21) (Fig.
3A). Extension
of primer 5'-CCGTATTGATCAGCACGCCCGCGGCAATCG-3' by reverse transcriptase
mapped the transcription start point at position 102 of the
sequence (Fig.
3B), 31 nt upstream of the translation start
codon of the first flagellin gene,
flaB1 (Fig.
3C). Sequence
5'-CTTAAG-3', identified 23 nt upstream of the transcription
initiation site, resembles TATA box consensus sequences of halophiles
(
7,
28), methanogenes, and
Crenarchaeota (
35) (Fig.
3C). On
the other hand, the second transcription signal, the initiator
element -1 CACTGC +5 is distinct from the +1 GGG +3 sequence
from methanogenes but is similar to the -1 YRNG +3 and -1 TRSSSC
+5 consensus sequences of halophiles and
Crenarchaeota (
35).
This emphasizes the absence of a strict sequence requirement
in this box for promoter activity. It is probably a general
rule that promoters of archaeal flagellin genes do not significantly
differ from transcription signals found in other archaeal genes
(
16,
21). The transcription of
N. magadii flagellin genes appears
to be similar to the "single-RNA" transcription start mechanism
in
H. halobium (
15), which contrasts with the initiation of
a few transcripts of different lengths from the same transcription
start point found in
P. kodakaraensis (
27) and
M. voltae (
21).
Although
H. halobium flagellins have the strongest homology
to
N. magadii proteins, we must point out that the flagellin
gene organization is different in
H. halobium, where two transcriptional
units comprise two and three genes (
15).
Search for flaB1 to flaB4 gene products among proteins isolated from flagella.
N. magadii flagella consist of four different proteins, FM1
to FM4, with molecular masses of 105, 60, 59, and 45 kDa, respectively,
as estimated by sodium dodecyl sulfate (SDS)-polyacrylamide
gel electrophoresis (
11). In this study we identified four transcribed
flagellin genes,
flaB1 to
flaB4, which encode proteins FlaB1
to FlaB4, with molecular masses of 21.4, 26.5, 41.7, and 27.0
kDa, respectively. The poor agreement between the molecular
masses estimated by SDS-gel electrophoresis and those expected
from the gene sequences is common for flagellins due to (i)
the high content of acidic amino acids, which can decrease SDS
binding and result in slower migration of the proteins in gels
(
26), and (ii) posttranslation modifications of flagellins (
36).
To identify the genes encoding flagellum proteins FM1 and FM4,
we performed N-terminal sequencing of tryptic fragments derived
from these flagellins. Sequences AEVVFELDGXPGSYD and VPSTFIEDE
from FM4 match the amino acid sequences of the FlaB1 protein
at positions 144 to 158 and 188 to 196, respectively. Thus,
flaB1 encodes flagellin FM4. In turn, FM1-derived sequence AIELP
coincides with the unique amino acid sequence of FlaB3 (positions
117 to 121); therefore, FM1 is encoded by the
flaB3 gene. Since
our attempts to obtain proteins FM2 and FM3 without cross-contamination
failed due to the similar molecular masses of these flagellins,
we performed tryptic digestion and sequencing of their mixture.
Sequence IDTTIAVGTVST, determined in the course of this analysis,
is identical to the unique sequence of the FlaB2 protein (positions
61 to 72), encoded by
flaB2. We strongly suggest that FlaB2
is the FM2 protein based on the observation that only FM2 and
FM4 are glycosylated (
11). A search for potential N-glycosylation
sites (Asn-X-Thr/Ser) (
4,
14,
16,
21) revealed the presence
of these signals in FlaB1 (positions 81, 98, and 114), identified
here as FM4, and FlaB2 (positions 105 and 158) proteins. Since
the sequencing result indicates that FlaB2 is present in the
FM2-FM3 mixture, only the product of the
flaB2 gene, the FlaB2
protein, can be considered to be glycosylated protein FM2. It
was shown that FM2 and FM3 give similar proteolysis patterns
(
11); therefore, they should be encoded by the same gene or
similar genes. FlaB4 has a high degree of homology to FlaB2;
thus, FM3 might be the
flaB4 gene product. The slightly faster
SDS-gel migration of this flagellin compared to that of FM2
(
11) may be attributed to the absence of glycosylation. In theory,
the FM3 protein can also contain the nonglycosylated product
of the
flaB2 gene. These results and transcription analyses
suggest that all four flagellin genes of
N. magadii are expressed
and that at least three of them participate in the assembly
of flagella. It is unclear why archaeal flagella are composed
of different flagellins, whereas bacterial flagella contain
only a single flagellin. The work from our laboratory has recently
shown that in
H. halobium only flagellins FlaA1 and FlaA2 are
needed for the formation of the flagellar spiral filament. The
function of the other three flagellins is auxiliary (
37). Similar
conclusions were also made for
M. voltae flagellins (
19).
Possible mode of N. magadii flagellin gene evolution.
The G+C content of the sequenced DNA locus is 54%. This is less than the average G+C content in randomly sequenced DNA fragments from N. magadii (63%) (data not presented), in known genes encoding proteins from other haloalkaliphilic archaea (63 and 61%), and in known genes from halophiles (64%, excluding gas vesicle genes [18]). Such a value is due to a low G+C frequency (49 to 60%) in the third codon position (GC3), which is considerably less than that found in halophilic and haloalkaliphilic species (77 to 85%) and even in the sequence of the downstream ORF5 (74%). To prove unusual codon bias in N. magadii flagellin genes, we estimate the differences in codon usage in distinct organisms by a simple pairwise comparison using the following espression:
where
ai and
bi are the frequencies (in percent)
of the same codon within a codon family of two organisms under
comparison and
n is the number of codon pairs analyzed. C, H,
K, R, W, Y, and P codons are poorly represented or not represented
at all in the
N. magadii flagellins and were therefore excluded
from the analyses. As expected, our calculations revealed the
least difference in codon usage, with a value of 2,350 to 4,050,
among the genes from halophiles and haloalkalophiles
H. halobium,
Natrialba asiatica, and
Natromonas (
Natronobacterium)
pharaonis.
The maximum differences found, 33,050 and 27,100, were between
the most divergent pairs of organisms analyzed,
Escherichia coli and
H. halobium, and
E. coli and
N. asiatica, respectively.
Pairs with
N. magadii flagellins demonstrate intermediate values
(11,335 to 20,056), but, strikingly, the smallest value found
(8,374) was that for the average
E. coli codon usage. Thus,
the codon usage of
N. magadii flagellin genes is rather different
from that for the genes of its relatives and surprisingly resembles
that for typical mesophilic bacterium
E. coli. Two other observations,
low G+C average and GC
3 content, also raise questions as to
the origins of the
N. magadii flagellin genes and strongly support
an idea that the locus has a mixed, probably unique, evolutionary
history. Remarkably, the conserved 5' regions of each
N. magadii flagellin gene (encoding aa 13 to 60) are enriched by G and
C (58 to 60%) compared to the rest of the sequence (47 to 57%)
and demonstrate a similar distribution of G+C in codon positions.
The values for the remaining parts, especially the GC
3 content,
vary significantly (data not shown). The least conserved central
region (aa 71 to 280) of the largest flagellin FlaB3 shows the
lowest GC
3 percentage, 15 to 20% less than those for other fragments.
Since this region does not show any similarity to the other
N. magadii flagellin genes and known archaeal genes, it has
most likely been transferred to the locus, probably from another
organism. Calculation of the codon usage differences in distinct
parts of the flagellin genes, although less relevant because
of poorer statistics, also emphasizes the strong divergence
of the 71-to-280 region. Indeed, the sum of the differences
between the 71-to-280 region and other flagellin sequences,
namely, the N-terminal (aa 11 to 60) and the middle-to-C-terminal
parts (aa 281 to 395 for FlaB3 and from aa 60 to the end for
the other proteins) is 124,334. This is higher than the corresponding
values, which range from 69,382 to 104,231, calculated for the
other regions. Such diverse codon usage in the central region
of the
flaB3 gene may result in lower expression levels of the
gene and may explain the relatively low content of the FlaB3
protein in the flagella (
11). Remarkably, BLAST (
2) and FASTA
(
29) searches revealed homology between this region (extended
to aa 57 and 353) and central variable parts of four
E. coli flagellins of the EPEC 1 group (
31) (Fig.
2B). These homologies
(about 25% identity and 41% similarity) are plausible, since
their scores and E values are comparable to the values for some
archaeal flagellins. These include the flagellins from the close
relative
H. halobium, found in the same search, even if the
comparison was between the genes encoding conserved N termini.
These results suggest that different parts of the
N. magadii flagellin genes might have a different evolutionary histories.
Horizontal transfer may be one of the causes of such diversity.
A mosaic gene structure resulting from horizontal transmission
of gene parts for some extracellular systems has been already
described: in the pilin gene cluster from gram-negative bacteria
(
5,
12) and in bacterial flagellin genes from
E. coli (
31) and
Salmonella (
34). Growing evidence for horizontal gene transfer
between
Archaea and
Bacteria (
13), including pathogenic bacteria
(
10), provides support for our model of flagellin gene exchange
between
E. coli and
N. magadii. Although the mechanism of such
transfers and the possible involvement of mediators remain to
be investigated, our hypothesis is indirectly supported by the
fact that one of the EPEC 1 group representatives,
E. coli strain
DEC 2a, and
N. magadii have been found in geographical areas
close to each other, e.g., in Congo and Kenya, respectively
(
31,
38). Moreover, the borders between constant and variable
parts of the
E. coli flagellin coincide with the borders found
in the archaeal flagellin region. Therefore, this region of
the
E. coli flagellin genes may have been moved to the archaeal
genome and may have been integrated into the analogous locations
between the most homologous regions of the
E. coli flagellin
gene and the
N. magadii flaB3 gene (positions 55 to 70 and 280
to 353). It is necessary to mention that the sequence similarity
between archaeal and bacterial flagellins was not described
earlier, although it was intensively searched (
3,
8,
15).
Nucleotide sequence accession number.
The nucleotide sequence determined in this study was assigned GenBank accession no. AJ277988.

ACKNOWLEDGMENTS
We are indebted to N. Matvienko, T. Ivashina, and J. Coyle for
helpful discussions and carefully reading the manuscript.
This work was supported by a grant from the Russian Foundation for Basic Research (no. 98-04-48318).

FOOTNOTES
* Corresponding author. Mailing address: Institute of Protein Research, Russian Academy of Sciences, Pushchino, Moscow Region 142290, Russia. Phone and fax: 7 095 9240493. E-mail:
fedorov{at}vega.protres.ru.

Present address: Laboratory of Nucleic Acid and Protein Structures, Memorial Sloan-Kettering Cancer Center, New York, N.Y. 10021. 

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Journal of Bacteriology, January 2002, p. 318-322, Vol. 184, No. 1
0021-9193/01/$04.00+0 DOI: 10.1128/JB.184.1.318-322.2002
Copyright © 2002, American Society for Microbiology. All Rights Reserved.