Page 1
極限環境微生物学会誌 Vol. 4, 2005
25
Journal of Japanese Society for Extremophiles (2005), Vol. 4, 25-31
Tamegai Ha, Nakamura Sa, Miyazaki Mb, Nogi Yb, Kasahara R a,b, Kato Cb and Horikoshi Kb
Physiological properties of Pseudomonas sp. strain MT-1, denitrifier from the 11,000 m-depth of Mariana Trench a Department of Chemistry, College of Humanities and Sciences, Nihon University
3-25-40, Sakurajosui, Setagaya-ku, Tokyo 156-8550, Japan b Extremobiosphere Research Center, Japan Agency for Marine-Earth Science and Technology
2-15, Natsushima-cho, Yokosuka 237-0061, Japan
Corresponding author: Tamegaia H, [email protected]
TEL +81-3-3329-1151 ext. 5740 FAX +81-3-5317-9433
Received: March 4, 2005, Accepted: March 24, 2005
Abstract In the present study, we investigated the
physiological properties of Pseudomonas sp. strain
MT-1 isolated from the mud of Mariana Trench.
Strain MT-1 was closely related with members of the
genus Pseudomonas, especially with Pseudomonas
chloritidismutans and Pseudomonas stutzeri on the basis
of 16S rDNA sequence. The DNA-DNA
hybridization values between strain MT-1 and
Pseudomonas reference strains were significantly lower
than those accepted as the phylogenetic definition of a
species. MT-1 had polar flagellum, and was
facultative anaerobe. The growth occurred in an
NaCl concentration of about 0-10% (optimum: 1-2%), in
pH of about 6-10 (optimum: 7-8), and in temperature of
about 4-45 °C (optimum: 32-35 °C). The G+C
content of the DNA was 60.5% mol%. The major
quinone was ubiquinone-9. The major fatty acid in
strain MT-1 was C16:0 (hexadecanoic acid), C16:1
(hexadecenoic acid) and C18:1 (octadecenoic acid).
The organism showed adaptational properties to
deep-sea environment compared with the reference
strains.
Key words: Pseudomonas sp. strain MT-1, denitrifier,
Mariana Trench
Introduction
Denitrification is one of the systems of anaerobic
respiration, and constitutes one of the main branches of
the environmental nitrogen cycle 26). Nitrogen is
incorporated into the biosphere with the biological
conversion from N2 to NH4+ (nitrogen fixation). It is
removed from there by oxidative conversion from NH4+
to NO3- (nitrification) and respiratory process which
reduce NO3- to NO2
-, NO, N2O and N2 subsequently
(denitrification). Many of the proteins are
participated in the system, and they have been studied
by many researchers 25, 26). In addition,
denitrification system is worthy to notice because it is
thought to be the ancient form of aerobic respiration
system 4, 13). Thus, the study of aerobic and
anaerobic respiratory system of the organism in the
isolated world (like deep sea) may provide a novel
knowledge for evolution of respiratory system.
However, little is known about respiratory system of
deep-sea organisms 9, 10, 17, 20, 24).
Denitrification is carried out by a number of
taxonomically diverse facultatively anaerobic
microorganisms. Pseudomonads contribute a large
number of denitrifying bacteria within a single genus 5,
7). Pseudomonas sp. strain MT-1 is one of the
denitrifying Pseudomonads isolated from the mud of
Mariana Trench (11°22.10'N, 142°25.85'E, 10898 m
dept), which was collected by the sterilized mud
sampler using the unmanned submersible KAIKO
operated by Japan Agency for Marine-Earth Science and
Technology (JAMSTEC) 16). This is the only
identified denitrifier isolated from deep sea, and some
genes for denitrification have been identified 18, 19).
Quite recently the organism have been classified as
原著論文
Page 2
極限環境微生物学会誌 Vol. 4, 2005
26
novel genomovar of Pseudomonas stutzeri by Sikorski
et al. (Sikorski, J., personal communication) They
performed the sequence analysis of 16s rDNA and
16S-23S rDNA internally transcribed spacer regions and
DNA-DNA hybridizations between many strains of P.
stutzeri. They also carried out the basic metabolic
tests on MT-1. However, detailed physiological
properties of the strain were still unclear. P. stutzeri
is known to show quite strong strain diversity, and the
members of the strain have been isolated world-wide
from various habitats including aquatic and terrestrial
ecosystems 14). Though, even each strain is closely
related with each other, they should adapt their own
environments. Thus, strain MT-1 is expected to
adapt its own environment, 11000-m depth of Mariana
Trench. However little is known about physiological
properties of this denitrifier from deep sea.
In the present study, we investigated the
physiological properties on strain MT-1, and found that
the organism displays adaptational properties to
deep-sea environment compared with the reference
strain. The organism can be a good object for the
study of physiological properties including
denitrification in the deep sea.
Materials and Methods
Organisms and cultivation conditions
Strain MT-1 was grown in MT-1 medium (0.5%
yeast extract, 1% tryptone, 3% NaCl, 0.01%
MgSO4·7H2O, 0.1% CaCl2·2H2O) 16), normally at 30 °C.
The reference strains used in this study, P. stutzeri IFO
14165T and Pseudomonas chloritidismutans DSM
13592T, was obtained from IFO and DSMZ, respectively.
These bacterial strains were maintained on MT-1 agar
medium (MT-1 medium containing 1.5% agar) at 30 °C.
Bacterial growth under various pressures was tested by
the methods described previously 16) with slight
modifications. Terminal electron acceptor (NaNO3
for MT-1 and P. stutzeri, and NaClO3 for P.
chloritidismutans) was added to each MT-1 medium for
maintaining the growth with anaerobic respiration.
Physiological analyses
Physiological tests were performed with a slight
modification of the general procedures as described
previously 1) Acid production from sugar was
assessed using MT-1 medium containing 1% of each
substrate and 0.03% of bromothymol blue.
Physical and Chemical analyses
Morphology of the cells of MT-1 was determined
by transmission electron microscopy as described
previously 6). Cellular fatty acids and isoprenoid
quinones were analyzed according to the methods
described previously 6).
Molecular biological studies
Chromosomal DNA was extracted from each
strain by the method of Saito and Miura 11). The G+C
content was determined by the method of Tamaoka and
Komagata 15). DNA-DNA hybridization was carried
out by the method of Ezaki et al.2) at 40 °C for 3h and
the results were measured fluorometrically.
Phylogenetic analysis
A phylogenetic tree was constructed based on the
16S rDNA sequences. Database search was carried
out by FASTA 8) on Internet. Nucleotide substitution
rates 3) were determined and a distance-matrix tree was
constructed by the neighbour-joining method 12) using
the CLUSTAL_W program 21) on internet.
Results and Discussion
In order to determine phylogenetic relationships
in detail, 16S rDNA sequence of strain MT-1 16) and
other known organisms were re-analyzed with
constructing phylogenetic tree. The results of
phylogenetic analyses (Fig. 1) clearly showed that the
strain MT-1 was classified into the genus Pseudomonas,
and were closely related to P. chloritidismutans and P.
stutzeri. On the results of DNA-DNA hybridization,
strain MT-1 showed quite low level of DNA-DNA
relatedness with P. chloritidismutans (<30%) and P.
stutzeri (<30%). This is significantly lower than that
accepted as the phylogenetic definition of a species 22).
These results were consistent with recent study
(Sikorski, J., personal communication).
Page 3
極限環境微生物学会誌 Vol. 4, 2005
27
Fig. 1 Phylogenetic tree showing the relationships of strain MT-1 within Pseudomonads.
The tree was constructed by the neighbor-joining method and based on 16S rDNA sequences.
Escherichia coli was used as the outgroup for the phylogenetic tree. Numbers indicated bootstrap values greater
than 500. Bar indicated 0.1 nucleotide substitutions per site.
Fig. 2 Transmission electron micrograph of negatively stained cells of strain
MT-1.
Bar indicated 1 µm.
Cells of the strain MT-1 were rod-shaped with
single polar flagellum (Fig. 2). Growth occurred in
an NaCl concentration of about 0-10% (optimal: 1-2%),
in pH of 6-10 (optimal: 7-8), and in temperature of
about 4-45 °C (optimal: 32-35 °C). MT-1 showed
optimal growth at comparatively higher temperature
than that at deep-sea. However, the organism showed
significant growth even at 4 °C although it was quite
Page 4
極限環境微生物学会誌 Vol. 4, 2005
28
slow 16). Further MT-1 showed optimal growth at
lower NaCl concentration than that of sea water.
This finding may be due to the fact that this organism
was isolated from mud of sea floor. Tolerance to
higher NaCl concentration may contribute to survival of
MT-1 in sea water. In the case of P.
chloritidismutans, growth occurs in an NaCl
concentration of about 0.1-4% (optimal: 2-4%), in pH of
7-9 (optimal: 7), and in temperature of about 10-37 °C
(optimal: 30 °C) 23). It is clear that MT-1 adapts to
wide-range environments compared with the reference
strain.
Characteristics of strain MT-1 and the reference
strains were shown in Table 1. Strain MT-1 was
facultatively anaerobic chemoorganotroph, displaying
respiratory type of metabolism. Nitrate was available
for growth with denitrification. However, nitrite did
not support the denitrification growth. The organism
cannot grow with fermentation. The G+C content of
the DNA was 60.5% mol%. The major quinone was
ubiquinone-9 (Q-9)
Table 1 Phenotypic characteristics of strain MT-1 and reference strains
Characteristic 1 2 3
yellow pigment + - + flagellum polar polar polar denitrification with nitrate + + - denitrification with nitrite - ND - chlorate respiration - - + gelatin hydrolysis - - - casein hydrolysis - - - starch hydrolysis - + + Tween 80 hydrolysis + + + growth at 40 °C + + - growth at 4 °C + - - GC content (%) 60.5 60.6-66.3 63.9 Acid production from: glucose + + + xylose - - - mannitol + - + glycerol + - + fructose + - - L-arabinose + - - sucrose - - - sorbitol - - - raffinose - - - rhamnose - - - myo-inositol - - - lactose - - - trehalose - - - cellobiose - - - maltose - - + galactose + - - mannose + + +
Strains: 1; Strain MT-1, 2; P. stutzeri IFO 14165T, 3; P. chloritidismitans DSM 13592T. Data were from this study
and references 7, 16 and 23. ND; no data available.
Page 5
極限環境微生物学会誌 Vol. 4, 2005
29
Fatty acid compositions of MT-1 and reference
strains were summarized in Table 2. The major fatty
acid in strain MT-1 was C16:0 (hexadecanoic acid),
C16:1 (hexadecenoic acid) and C18:1 (octadecenoic
acid). The composition of fatty acid in strain MT-1
showed similarity with those in reference strain to some
extent. Significant difference was that percentage of
unsaturated fatty acids in total fatty acids was
significantly higher in strain MT-1 (66%) than in the
reference strains ( P. stutzeri: 22%, P. chloritidismutans:
56%).
Table 2 Fatty acid composition of strain MT-1 and reference strains
Fatty acid 1 2 3
3-OH-10:0 2 3 3
12:0 5 7 9
3-OH-12:0 1 2 2
14:0 1 1 2
14:1 1
16:0 21 23 26
16:1 29 21 24
17:0 2 3 1
18:0 2 34 1
18:1 35 32
19:1 1 1
Values are percentages of total fatty acids. Strains: 1; Strain MT-1, 2; P. stutzeri IFO 14165T, 3; P.
chloritidismitans DSM 13592T. Empty cells; not detected.
Table 3 Effect of pressure on the growth of MT-1 and reference strains.
Pressure (MPa) 1 2 3
0.1 100 100 100
30 33 10 26
Strains: 1; Strain MT-1, 2; P. stutzeri IFO 14165T, 3; P. chloritidismitans DSM 13592T. Growth under each
pressure was checked by OD at 660 nm after cultivation for 22 h. Values are percentages when OD under a
pressure of 0.1 MPa is defined as 100%. A pressure of 30 MPa corresponds to the pressure at about 3,000-m depth
of sea.
It has been already demonstrated that strain MT-1
shows optimal growth under atmospheric pressure.
However it shows adaptational property for high
hydrostatic pressure to some extent 16). Table 3
showed the effect of pressure on the growth of MT-1
and reference strains. MT-1 and P. chloritidismutans
seemed to adapt high hydrostatic pressure compared
with P. stutzeri to some extent. From the result of
phylogenetic analysis (Fig. 1), it appeared that the
phylogenetic relationship between MT-1 and P.
chloritidismutans is closer than that between MT-1 and
P. stutzeri. It is possible that adaptational property
for high hydrostatic pressure is specific to MT-1 and
closely related strains.
In the present study, we investigated about the
physiological properties on Pseudomonas sp. strain
MT-1 in detail. The results showed that the organism
can adapt to wide-range environments compared with
Page 6
極限環境微生物学会誌 Vol. 4, 2005
30
the reference strains. This fact may allow MT-1 for
life in deep-sea environment. The organism can be a
good object for the study of physiological properties
including denitrification in the deep sea.
Acknowledgements
We wish to express our thanks to Mr. Uematsu
(JAMSTEC) for operating electron microscopic system.
This work was supported by the Nihon University
Individual Research Grant and the Moritani Scholarship
Foundation for H. T.
References
1) Barrow G.I. and Feltham R.K.A. 1993. Cowan
and Steel's Manual for the Identification of
Medical Bacteria, 3rd edn. Cambridge University
Press, New York.
2) Ezaki T., Hashimoto Y. and Yabuuchi E. 1989.
Fluorometric deoxyribonucleic
acid-deoxyribonucreic acid hybridization in
microdilution wells as an alternative to
membrane filter hybridization in which
radioisotopes are used to determine genetic
relatedness among bacterial strains. Int. J. Syst.
Bacteriol. 39:224-229.
3) Kimura M. 1980. A simple method for estimating
evolutionary rates of base substitutions through
comparable studies of nucleotide sequences. J.
Mol. Evol. 16:111-120.
4) Mogi T., Tsubaki M., Hori H., Miyoshi H.,
Nakamura H. and Anraku Y. 1998. Two terminal
quinol oxidase families in Escherichia coli:
variations on molecular machinery for dioxygen
reduction. J. Biochem. Mol. Biol. Biophys.
2:79-110.
5) Moore E.R.B., Mau M., Arnscheidt A., Böttger
E.C., Hutson R.A., Collins M.D., Van de Peer Y.,
De Wachter R. and Timmis K.N. 1996. The
determination and comparison of the 16S rRNA
gene sequences of species of the genus
Pseudomonas (sensu stricto) and estimation of
the natural intragenetic relationships. Syst. Appl.
Microbiol. 19:478-492.
6) Nogi Y., Kato C. and Horikoshi K. 1998.
Taxonomic studies of deep-sea barophilic
Shewanella strains and description of Shewanella
violacea sp. nov. Arch. Microbiol. 170:331-338.
7) Palleroni N.J. 1984. Genus I. Pseudomonas
Migula 1984, 237AL (Nom. cons. Opin. 5, Jud.
Comm. 1952, 237). In: Krieg N.R. and Holt J.G.,
(eds) Bergey's Manual of Systematic
Bacteriology. Williams & Wilkins, Baltimore,
141-199.
8) Pearson W.R. and Lipman D.J. 1988. Improved
tools for biological sequence comparison. Proc.
Natl. Acad. Sci. USA 85:2444-2448.
9) Qureshi M.H., Kato C. and Horikoshi K. 1998.
Purification of two pressure-regulated c-type
cytochromes from a deep-sea bacterium,
Shewanella sp. strain DB-172F. FEMS Microbiol.
Lett. 161:301-309.
10) Qureshi M.H., Kato C. and Horikoshi K. 1998.
Purification of a ccb-type quinol oxidase
specifically induced in a deep-sea barophilic
bacterium, Shewanella sp. strain DB-172F.
Extremophiles 2:93-99.
11) Saito H. and Miura K. 1963. Preparation of
transforming deoxyribonucleic acid by phenol
treatment. Biochim. Biophys. Acta 72:619-629.
12) Saitou N. and Nei M. 1987. The
neighbour-joining method: a new method for
reconstituting phylogenetic trees. Mol. Biol. Evol.
4:406-425.
13) Saraste M. and Castresana J. 1994. Cytochrome
oxidase evolved by tinkering with denitrification
enzymes. FEBS Lett. 341:1-4.
14) Sikorski J., Möhle M. and Wackernagel W. 2002.
Identification of complex composition, strong
strain diversity and directional selection in local
Pseudomonas stutzeri populations from marine
sediment and soils. Environ. Microbiol.
4:465-476.
15) Tamaoka J. and Komagata K. 1984.
Determination of DNA base composition by
reversed phase high-performance liquid
chromatography. FEMS Microbiol. Lett.
25:125-128.
16) Tamegai H., Li L., Masui N. and Kato C. 1997. A
denitrifying bacterium from the deep sea at
11000-m depth. Extremophiles 1:207-211.
17) Tamegai H., Kato C. and Horikoshi K. 1998.
Pressure-regulated respiratory system in
Page 7
極限環境微生物学会誌 Vol. 4, 2005
31
barotolerant bacterium, Shewanella sp. strain
DSS12. J. Biochem. Mol. Biol. Biophys.
1:213-220.
18) Tamegai H., Kato C. and Horikoshi K. 2002.
Gene cluster of nitrous oxide reduction in the
deep sea of Mariana Trench. J. Biochem. Mol.
Biol. Biophys 6:221-224.
19) Tamegai H., Kato C. and Horikoshi K. 2004.
Lateral gene transfer in the deep sea of Mariana
Trench: Identification of nar gene cluster
from Pseudomonas sp. strain MT-1. DNA Seq.
15:338-343.
20) Tamegai H., Kawano H., Ishii A., Chikuma S.,
Nakasone K. and Kato C. 2005.
Pressure-regulated biosynthesis of cytochrome bd
in piezo- and psychrophilic deep-sea bacterium
Shewanella violacea DSS12. Extremophiles in
press
21) Thompson J.D., Higgins D.G. and J. G.T. 1994.
CLUSTAL_W: improving the sensitivity of
progressive multiple sequence alignment through
sequence weighting, position-specific gap
penalties and weight matrix choice. Nucleic
Acids Res. 22:4673-4680.
22) Wayne L.G., Brenner D.J., Colwell R.R., Grimont
P.A.D., Kandler O., Krichevsky M.I., Moore L.H.,
Moore W.E.C., Murray R.G.E., Stackebrandt E.,
Starr M.P. and Trüper H.G. 1987. Report of the
Ad Hoc Committee on reconciliation of
approaches to bacterial systematics. Int. J. Syst.
Bacteriol. 37:463-464.
23) Wolterink A.F.W.M., Jonker A.B., Kengen
S.W.M. and Stams A.J.M. 2002. Pseudomonas
chloritidismutans sp. nov., a non-denitrifying,
chlorate-reducing bacterium. Int. J. Syst. Evol.
Microbiol. 52:2183-2190.
24) Yamada M., Nakasone K., Tamegai H., Kato C.,
Usami R. and Horikoshi K. 2000.
Pressure-regulation of soluble cytochromes c in a
deep-sea piezophilic bacterium, Shewanella
violacea. J. Bacteriol. 182:2945-2952.
25) Yamanaka T. and Okunuki K. 1962. Crystalline
Pseudomonas cytochrome oxidase I. enzymic
properties with special reference to the biological
specificity. Biochim. Biophys. Acta 67:379-393.
26) Zumft W.G. 1997. Cell biology and molecular
basis of denitrification. Microbiol. Mol. Biol.
Rev. 61:533-616.