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Applied and Environmental Microbiology, September 2001, p. 4177-4185, Vol. 67, No. 9
0099-2240/01/$04.00+0 DOI: 10.1128/AEM.67.9.4177-4185.2001
Copyright © 2001, American Society for Microbiology. All rights reserved.
Detection of Methanotroph Diversity on Roots of
Submerged Rice Plants by Molecular Retrieval of
pmoA, mmoX, mxaF, and
16S rRNA and Ribosomal DNA, Including pmoA-Based
Terminal Restriction Fragment Length Polymorphism Profiling
Hans-Peter
Horz,
Merlin
Tchawa
Yimga, and
Werner
Liesack*
Max-Planck-Institut für terrestrische
Mikrobiologie, D-35043 Marburg, Germany
Received 22 December 2000/Accepted 26 June 2001
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ABSTRACT |
The diversity of methanotrophic bacteria associated with roots of
submerged rice plants was assessed using cultivation-independent techniques. The research focused mainly on the retrieval of
pmoA, which encodes the
subunit of the particulate
methane monooxygenase. A novel methanotroph-specific
community-profiling method was established using the terminal
restriction fragment length polymorphism (T-RFLP) technique. The T-RFLP
profiles clearly revealed a more complex root-associated methanotrophic
community than did banding patterns obtained by
pmoA-based denaturing gradient gel electrophoresis. The
comparison of pmoA-based T-RFLP profiles obtained from
rice roots and bulk soil of flooded rice microcosms suggested that there was a substantially higher abundance of type I methanotrophs on
rice roots than in the bulk soil. These were affiliated to the genera
Methylomonas, Methylobacter,
Methylococcus, and to a novel type I methanotroph
sublineage. By contrast, type II methanotrophs of the
Methylocystis-Methylosinus group
could be detected with high relative signal intensity in both soil and
root compartments. Phylogenetic treeing analyses and a set of
substrate-diagnostic amino acid residues provided evidence that a novel
pmoA lineage was detected. This branched distinctly from
all currently known methanotrophs. To examine whether the retrieval of
pmoA provided a complete view of root-associated
methanotroph diversity, we also assessed the diversity detectable by
recovery of genes coding for subunits of soluble methane monooxygenase
(mmoX) and methanol dehydrogenase (mxaF).
In addition, both 16S rRNA and 16S ribosomal DNA (rDNA) were retrieved
using a PCR primer set specific to type I methanotrophs. The overall
methanotroph diversity detected by recovery of mmoX,
mxaF, and 16S rRNA and 16S rDNA corresponded well
to the diversity detectable by retrieval of pmoA.
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INTRODUCTION |
The atmospheric trace gas
methane (CH4) is a prominent "greenhouse"
gas. Its atmospheric concentration has been increasing until recently
at a rate of about 1% a year (8). Up to 70 to 80% of
atmospheric CH4 is biogenic (55).
Flooded rice fields are one of the major sources of biogenic
CH4 (34, 50). Estimations of the
annual emission rate from flooded rice fields range between 60 and 110 Tg (8, 21, 45). The upper limit of this emission rate accounts for approximately 25% of the total annual
CH4 emission into the atmosphere (8,
21).
Approximately 90% of the CH4 that is emitted
from rice paddies escapes through the aerenchyma of the rice plants,
whereas only 10% escapes through the floodwater (19, 52).
However, the aerenchyma does not merely function as a gas transport
system but rather constitutes a dynamic, oxygenated biofilter. The
diffusive input of oxygen into the below-ground plant surface area
enables aerobic methanotrophs to oxidize CH4.
Gilbert and Frenzel (22) showed that the activities of
methanotrophs were directly dependent on the oxygen availability in the
rice root environment. It was shown that up to 30% of the
CH4 produced in rice paddy soil is oxidized by
root-associated methanotrophs (5, 9, 15).
Based on phylogenetic, physiological, morphological, and biochemical
characteristics, methanotrophs are divided into two major subgroups
(27). The
-proteobacterial type I methanotroph
group comprises the genera Methylomonas,
Methylocaldum, Methylomicrobium, Methylobacter, Methylosarcina,
Methylosphaera, and Methylococcus (also
classified as type X) (4, 6, 27, 58), while the
-proteobacterial type II methanotroph group consists of the genera Methylocystis and Methylosinus (27)
and one more distant species, Methylocella palustris
(14).
The methanotrophic diversity in rice field soil has been assessed in
detail (28, 30), but knowledge about the diversity of
methanotrophic populations associated with rice roots is still limited.
Type II strains were isolated from the terminal positive-dilution steps
of a most-probable-number dilution series (23).
However, whether these results reflect the natural situation on rice
roots, i.e., predominance of type II methanotrophs, or instead were the consequence of cultivation bias, is unclear.
We assessed the methanotrophic diversity associated with roots of
submerged rice plants using various cultivation-independent techniques.
This assessment was carried out in relation to the methanotrophic
diversity detectable in rice paddy bulk soil. Despite the phylogenetic
distance between type I and type II methanotrophs, almost all known
methanotrophs possess a pmoA gene, which encodes the
subunit (PmoA) of the particulate methane monooxygenase (pMMO). The
only exception is Methylocella palustris (13,
14). Consequently, this study focused mainly on the retrieval of
pmoA using PCR primers described previously
(32). These primers also target amoA,
which encodes the
subunit (AmoA) of the ammonia monooxygenase in
autotrophic ammonia oxidizers. Based on the pmoA sequence
database created in this study, we established a novel methanotroph-specific community-profiling method using the
terminal restriction fragment length polymorphism (T-RFLP)
technique (37, 39). The methanotroph diversity
detectable by pmoA-based T-RFLP profiling was compared
with those detectable by comparative sequence analysis of
cloned pmoA and by pmoA-based denaturing
gradient gel electrophoresis (DGGE).
To examine the meaningfulness of the pmoA-based results, we
also assessed the methanotrophic diversity detectable by retrieval of mmoX (25) and mxaF
(42). The mmoX gene encodes the
subunit (MmoX) of the hydroxylase component of the soluble methane
monooxygenase (sMMO). This monooxygenase is present in most
type II methanotrophs, in members of the genus
Methylococcus, and in some Methylomonas strains
(53) but not in most of the other type I methanotrophs (27). The mxaF gene codes for the
subunit
of the methanol dehydrogenase, which is present in all
methylotrophs. In addition, both 16S ribosomal DNA (rDNA) and 16S rRNA
were retrieved using PCR primers specific to type I methanotrophs
(57).
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MATERIALS AND METHODS |
Rice microcosms.
Rice (Oryza sativa var. Roma,
type japonica) was grown in three flooded, unfertilized microcosms for
70, 84, or 90 days using conditions described previously (20,
26).
Rice root samples obtained from the three microcosms were used as
source material for the molecular analyses. This material, which we
will refer to as root samples M70, M84, and M90, was washed by careful
shaking in phosphate-buffered saline (7 mM
Na2HPO4, 3 mM
NaH2PO4, 130 mM NaCl [pH
7.2]) to remove adhering soil particles. Cores were obtained from the
bulk soil between the plants by pressing a plastic corer into the soil
to a depth of about 15 cm. Because of the dense surface root mat, only
the lower 10-cm portions of the cores were used. The three microcosms
were cultivated using soil sampled in 1995 (M90), 1997 (M84), and 1999 (M70) from drained rice fields of the Italian Rice Research Institute
in Vercelli, Italy.
Extraction of total DNA.
Total DNA from the bulk soil of the
flooded rice microcosms was extracted and purified using a protocol
reported previously (38). In this protocol,
microbial cells were lysed directly in the soil matrix by bead beating.
For extraction of total DNA from rice roots, the samples M84 and M90
were lyophilized, and the dried root material was subsequently
pulverized with a mortar under liquid N
2. The
pulverized root
material was resuspended in 1 ml of extraction buffer.
Enzymatic
lysis of microbial cells, as well as isolation and
purification
of total DNA, was performed using an extraction protocol
described
previously (
26).
Simultaneous extraction of total DNA and RNA.
Rice roots of
sample M70 were placed in a 2-ml reaction tube together with 1 g
of glass beads (diameter, 0.17 to 0.18 mm) and 700 µl of precooled
TPM buffer (50 mM Tris-HCl [pH 7.5], 1.7% [wt/vol]
polyvinylpyrrolidone, 10 mM MgCl2)
(18). This suspension was shaken for 60 s at maximum
speed in a bead beater (Dismembrator-S; B. Braun Biotech GmbH,
Melsungen, Germany). Glass beads, root particles, and cell debris were
pelleted by centrifugation for 5 min at 4°C, and the supernatant was
transferred to a new reaction tube. Seven hundred microliters of a
phenol-based lysis buffer was added to the pellet, and the bead-beating
procedure was repeated. After centrifugation, both supernatants were
pooled and extracted three times with cold phenol-chloroform (1:1,
vol/vol) followed by precipitation of total nucleic acids with 0.1 volume of sodium acetate (3 M; pH 5.2) and 2.5 volumes of ethanol. The
pellet was dried and suspended in 100 µl of Tris-EDTA buffer. For
subsequent DNA-based analyses a 50-µl aliquot was stored at
20°C.
For preparation of total RNA, the other 50-µl aliquot was mixed with
1 volume of TMC buffer (10 mM Tris-HCl [pH 7.5], 5 mM
MgCl2, 0.1 mM CsCl2) (18) and 5 U of RNase-free DNase (Promega, Madison, Wis.)
and incubated for 1 h at 37°C to remove the DNA. The reaction
was stopped by extraction with 1 volume of chloroform. Precipitation and resuspension of total RNA were performed as described above.
PCR amplification.
The primer sets used in this study are
listed in Table 1. For
pmoA-based T-RFLP analysis, the 5' primer A189 was labeled with the dye carboxyfluorescein. The reaction mixture contained 1 to 5 ng of DNA, 50 µl of MasterAmp PCR premix F (Epicentre Technologies, Madison, Wis.), 0.3 µM concentrations of each primer (MWG-Biotech, Ebersberg, Germany), and 2.5 U of Taq DNA polymerase
(AmpliTaq; PE Applied Biosystems, Foster City, Calif.). Amplification
was performed in a total volume of 100 µl in 0.2-ml reaction tubes, using a DNA thermal cycler (model 2400; PE Applied Biosystems). The
thermal PCR profile was as follows: initial denaturation for 2 min at
94°C and 30 cycles consisting of denaturation at 94°C for 45 s, primer annealing for 60 s (annealing temperature specific to
each target gene [Table 1]), and elongation at 72°C for 120 s.
The final elongation step was 6 min. Aliquots of the amplicons (10 µl) were checked by electrophoresis on a 1% agarose gel.
RT-PCR of 16S rRNA.
Ribosomal copy DNA (rcDNA) of type I
methanotrophs was synthesized from total RNA using primer MethT1cR
(Table 1), Moloney murine leukemia virus reverse transcriptase (RT)
(RNase H minus; Promega, Mannheim, Germany), and a previously described
protocol (38). PCR of 16S rcDNA was carried out as
described above.
pmoA-based T-RFLP analysis.
T-RFLP analysis
was performed for each total DNA extract in triplicate using a protocol
reported previously (38, 39). The pmoA was
amplified by PCR as described above. After purification with Qiaquick
spin columns (Qiagen, Hilden, Germany), approximately 100 ng of the
amplicons were digested with 10 U of the restriction endonuclease
MspI (Promega). The digestions were carried out in a total
volume of 10 µl for 3 h at 37°C. Aliquots (2.5 µl) of the
digested amplicons were mixed with 2.0 µl of formamide and 0.5 µl
of an internal lane standard (GeneScan-1000 ROX; PE Applied Biosystems). The mixtures were denatured at 100°C for 3 min and then
chilled on ice. Electrophoresis on a polyacrylamide gel (6%) was
performed using an automated DNA sequencer (model 373; PE Applied
Biosystems) for 6 h at the following settings: 2,500 V, 40 mA, and
27 W (24-cm gel length). After electrophoresis, the sizes of the
5'-terminal restriction fragments (T-RFs) and the intensities of their
fluorescence emission signals (i.e., signal intensities) were
automatically calculated by the GeneScan Analysis software, version 2.1 (PE Applied Biosystems). The accuracy of size estimation between
replicates was ±1 bp. The relative signal intensity of each T-RF was
calculated based on the signal intensity of the individual T-RF
in relation to the total signal intensity of all T-RFs (including the
531-bp fragment) detected in the respective T-RFLP community profile.
The 531-bp fragment corresponds to pmoA amplicons without
any restriction site for MspI.
pmoA-based DGGE.
PCR amplification of
pmoA and DGGE in the Dcode System (Bio-Rad, Munich, Germany)
were carried out as described by Henckel et al. (28). In
brief, PCR products were separated in 1-mm-thick polyacrylamide gels
(6.5% [wt/vol] acrylamide-bisacrylamide [37.5:1]) using a linear
denaturing gradient that ranged from 35 to 80%. A denaturing gradient
of 80% corresponded to 6.5% acrylamide, 5.6 M urea, and 32%
deionized formamide. The electrophoresis was performed in 0.5× TAE
buffer (0.04 M Tris-base, 0.02 M sodium acetate, 1 mM EDTA [pH 7.4])
for 15 h at a constant voltage of 74 V at 60°C. Gels were
stained with 1:10,000 (vol/vol) SYBR-Green I (Biozym,
Hessisch-Oldendorf, Germany) for 45 min and scanned with a Storm 860 Phosphorimager (Molecular Dynamics, Sunnyvale, Calif.).
Cloning and sequencing.
PCR products of pmoA,
mmoX, mxaF, 16S rDNA, and 16S rcDNA were cloned
using the TOPO TA cloning kit (Invitrogen Corp., San Diego, Calif.) as
recommended by the manufacturer. The preparation of plasmid DNA of
randomly selected clones, PCR amplification of cloned inserts, and
nonradioactive sequencing were carried out as described previously
(48). In addition, oligonucleotide primers targeting
internal regions of the cloned inserts were used for sequencing of
mmoX and 16S rDNA and rcDNA.
Phylogenetic analysis.
Based on sequence information
deposited either in public-domain databases or generated in the course
of this study, we established sequence databases for pmoA,
mxaF, and mmoX. Each of these sequence databases
was integrated into the ARB program package (developed by O. Strunk and
W. Ludwig; Technische Universität München
[http://www.arb-home.de]) and was manually put into an aligned
format. The 16S rDNA and rcDNA clone sequences were added to a database
of about 14,000 complete or partial bacterial 16S rRNA sequences.
Evolutionary distances (ARB and PHYLIP [17]) between
pairs of inferred amino acid sequences (pmoA,
mmoX, and mxaF) were calculated using various models (11, 36). Evolutionary-distance values between
pairs of 16S rDNA and rcDNA clone sequences were calculated by applying the Jukes-Cantor correction (35). The trees were
constructed using the neighbor-joining method (49). The
statistical significance levels of interior nodes were determined by
performing bootstrap analyses by the neighbor-joining method (500 data
resamplings). To exclude obvious chimeric primary structures from the
pmoA, mmoX, mxaF, and 16S rDNA and
rRNA sequence databases, separate treeing analyses of the 5' and 3'
halves of the respective sequence data sets were carried out.
Nucleotide sequence accession numbers.
The environmental
pmoA (plus amoA and sequence types of
uncertain affiliation), mmoX, mxaF, 16S
rDNA, and 16S rcDNA clone sequences recovered in this study from rice
roots of flooded rice microcosms have been deposited in the EMBL,
GenBank, and DDBJ nucleotide sequence databases under accession
no. AJ299946 to AJ299968, AJ299515 to AJ29953, AJ299504 to AJ299514, AJ299969 to AJ299983, and AJ299984 to AJ299989, respectively.
 |
RESULTS |
The use of PCR primer sets with intended-target specificity for
partial stretches of pmoA, mmoX, mxaF,
and 16S rDNA resulted in amplicons of the predicted sizes (Table 1).
Clone libraries were generated from the PCR products, and subsequently
individual clones were randomly selected for comparative sequence
analysis. In addition, methanotroph diversity was assessed by
pmoA-based T-RFLP analysis.
pmoA-based cloning approach.
One clone library
(each) was generated from samples M84 and M90. In total, 47 pmoA clones were randomly selected for comparative sequence analysis (28 and 19 clones from samples M84 and M90, respectively).
Thirty-six clones formed three distinct clusters within the
phylogenetic radiation of type I methanotrophs (Fig.
1A). Cluster
I (16 clones) was
affiliated with
Methylomonas methanica. Cluster
II (10 clones) formed a separate lineage without any clear affiliation
to any
of the known genera. Cluster III (10 clones) exhibited
a moderate
relationship to
Methylococcus capsulatus.

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FIG. 1.
(A) Distance dendrogram constructed for
partial pmoA and amoA gene sequences
based on 165 derived amino acid sites in relation to
pmoA-based T-RFLP (B) and DGGE (C) community patterns.
The two patterns and most of the pmoA clone sequences
were obtained from sample M84. (A) The dendrogram shows environmental
pmoA and amoA (plus other putative
monooxygenase) sequences retrieved from roots of submerged rice plants
(M84, M90) in relation to pmoA of cultured type I and
type II methanotrophs, environmental pmoA clone
sequences, and amoA sequences of the -proteobacterial
Nirosomonas and Nitrosospira group. The
environmental pmoA sequences used for reference were
retrieved from various habitats as follows: beech forest in Denmark
(RA14 [AF148521], RA21 [AF148522], Rold1 [AF148523], Rold4
[AF148526], Rold5 [AF148527]), rain forest in Brazil (Pantanal13
[AF148525]), mixed hardwood forest in the United States (Maine6
[AF148528], Maine9 [AF148531]) (33), deciduous forest
soil near Marburg, Germany (MR2 [AF200726], MR16 [AF 200729]
(29), MR1 [AF200729]) (29), rice soil
incubations (He-I [AF126908], He-II [AF126909], He-III
[AF126910], He-IV [AF126913], He-VI [AF126911])
(28), and blanket peat bog (PE9 [AF006050], PD2
[AF006047]) (41). The numbers I, II, and III refer to
three distinct pmoA sequence clusters of type I
methanotrophs, which have been retrieved from rice roots. The numbers
at the nodes indicate the percentage of recovery in 500 bootstrap
resamplings. Only bootstrap values 50 are shown. Scale bar, 0.1 substitution per amino acid site. Database accession numbers of
reference organisms are as follows: Methylocystis sp.
strain M, U81596; Methylocystis parvus, U31651;
Methylosinus trichosporium, U31550;
Methylobacter sp. strain BB5.1, AF016982;
Methylomicrobium album, U31654; Methylomicrobium
pelagicum, U31652; Methylomonas methanica,
U31653; Methylocaldum gracile, U89301;
Methylocaldum szegediense, U89303; Methylocaldum
tepidum, U89304; Methylococcus capsulatus,
L40804; strain HB, U89302; Nitrosospira
multiformis, U89833; and Nitrosomonas europaea,
AF037107. (B) pmoA-based T-RFLP profile. The
x axis shows the lengths (in base pairs) of the T-RFs,
and the y axis shows the intensities of the fragments in
arbitrary units. The numbers in boxes indicate the sizes of T-RFs which
could be assigned to phylogenetically defined methanotroph populations
or to autotrophic ammonia oxidizers (see arrows). (C)
pmoA-based DGGE pattern. For comparative sequence
analysis, predominant DGGE bands were excised, reamplified, and
reanalyzed by DGGE to verify band purity. Affiliation of these bands to
distinct pmoA clusters is indicated (compare with Fig.
1A).
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Only two
pmoA clones could be assigned to the
Methylocystis-
Methylosinus group (type II
methanotrophs). Four sequence types
grouped with ammonia
oxidizers of the

-proteobacterial
Nitrosomonas-
Nitrosospira group. Five sequences
formed the lineages A, B, and C (Fig.
1A),
which branched
distinctly from all currently known methanotrophs
or autotrophic
ammonia
oxidizers.
Separate treeing analysis of the 5' and 3' halves of the
respective sequence types suggested that the clone sequences assigned
to the lineages A, B, and C were of natural origin, i.e., separate
treeing analysis did not provide evidence that any of these clones
were
chimeric. We therefore determined amino acid signature residues
for the inferred peptide sequences of the lineages A, B, and
C
(Table
2) (
33). These are
either universal to PmoA (methanotrophs)
and AmoA (autotrophic ammonia
oxidizers) or specific for either
PmoA or AmoA
(substrate-diagnostic residues). Based on this approach,
Holmes et al. (
33) assigned a newly detected
cluster of sequence
types (forest clones) (Table
2) to an
uncharacterized group of
methanotrophs. The percentage distribution of
substrate-diagnostic
residues suggests that lineage A corresponds to a
novel
pmoA cluster
rather than to an
amoA
cluster. By contrast, due to the relatively
low number of conserved
substrate-diagnostic residues, sequence
types of the lineages B and C
could not be assigned to either
PmoA or AmoA.
pmoA-based T-RFLP analysis.
Based on our
pmoA sequence database derived from cultured methanotrophs
and environmental samples, we predicted that the tetrameric restriction
enzyme MspI would be the restriction enzyme most appropriate to analyze the genetic diversity of methanotrophic communities in
a single electrophoretic profile. Defined mixtures of genomic DNA from
cultured methanotrophs subjected to MspI-based
T-RFLP analysis exactly produced those T-RFs predicted based on our
pmoA sequence database (data not shown). Consequently,
MspI was used for pmoA-based T-RFLP
analysis of methanotrophic communities. Extraction of total DNA
from the same root sample in triplicate followed by PCR amplification
of pmoA and T-RFLP analysis produced highly similar T-RFLP
community profiles. The coefficients of variation of the relative
signal intensities between these profiles were between 5.4 and 12.3%
for the major peaks, i.e., those with sizes of 80, 245, 350, 440, 505, and 531 bp (Fig. 1B; see also Fig. 2). The coefficients of
variation for the major peaks between T-RFLP community profiles
generated in triplicate from individual DNA extracts ranged from 1.7 to
7.6%. This analysis showed that the T-RFLP technique was
reliable for a rapid PCR-based fingerprinting of
methanotrophic communities. High reproducibility of the T-RFLP technique has been reported previously (e.g., for 16S rDNA-based T-RFLP analysis [39, 44]).
The comparison of T-RFLP community profiles obtained from rice root
sample M84 with T-RFs of individual
pmoA and
amoA
sequence
types allowed the differentiation among type I methanotrophs,
type II methanotrophs, and autotrophic ammonia oxidizers (Fig.
1). Type
I methanotrophs were further differentiated into five
distinct T-RFs,
which correspond to phylogenetically distinct
sublineages affiliated
with the following: (i)
pmoA cluster III
plus members
of the genera
Methylococcus and
Methylocaldum
(80-bp
T-RF); (ii)
Methylomicrobium album (350-bp T-RF);
(iii)
pmoA cluster
I plus
Methylomonas
methanica (440-bp T-RF); (iv)
Methylobacter sp. strain
BB5.1 (505-bp T-RF); and (v)
pmoA cluster II (531-bp
peak;
no recognition site for
MspI). The type II methanotrophs
of
the
Methylocystis-Methylosinus group were characterized by
the 245-bp T-RF, while the 47-bp T-RF was indicative of
amoA
(
Nitrosomonas-
Nitrosospira group). Three further
minor peaks could be assigned to the lineages
A (280-bp T-RF), B
(228-bp T-RF), and C (113-bp T-RF). Several
peaks of mainly lower
relative signal intensity could be assigned
to none of the
pmoA or
amoA sequence types retrieved from rice
roots or deposited in public-domain databases. These T-RFs may
correspond to novel
pmoA or
amoA sequence
types.
Root-associated methanotroph diversity detectable by T-RFLP
analysis was compared to that detectable by DGGE using the same
extract
of total DNA as the starting material. DGGE revealed the
presence of
only
pmoA sequence types affiliated with type II
methanotrophs
and
pmoA cluster III (Fig.
1C).
The community profiles obtained by
pmoA-based T-RFLP
analysis from root samples M70, M84, and M90 showed similar relative
abundances of the major T-RFs, i.e., of T-RFs with sizes of 80,
245, 350, 440, 505, and 531 bp. The T-RFLP profiles generated
from the
anoxic bulk soil were characterized mainly by the 245-bp
T-RF of type
II methanotrophs, but minor peaks indicative of type
I methanotrophs
(80- and 350-bp T-RFs) and ammonia oxidizers (47-bp
T-RF) were also
present. The comparison of T-RFLP profiles obtained
from bulk soil
versus rice roots is shown for rice microcosm M84
(Fig.
2).

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FIG. 2.
Comparison of pmoA-based T-RFLP profiles
obtained from bulk soil (A) and rice roots (B) of the flooded rice
microcosm M84. See Fig. 1 for assignment of the major T-RFs to defined
methanotrophic populations and to autotrophic ammonia oxidizers.
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mmoX.
Five of 15 clones analyzed were closely
related to the mmoX of Methylocystis sp.
strain LR1 (Fig. 3). This type II
methanotroph was isolated in Canada (16). Three
mmoX clones were assigned to Methylocystis sp.
strain M. The treeing analysis suggested that clone M84-S38 was
affiliated to the mmoX of the acidophile Methylocella palustris (13, 14). However, the
dissimilarity values of the predicted peptide sequence of clone
M84-S38 with MmoX of Methylocella palustris
(15.7%), the Methylocystis-Methylosinus group
(17.1 to 18.5%), and Methylococcus capsulatus Bath (17.5%) were all similar. The MmoX sequence types of the phylogenetically distinct type I methanotrophs Methylomonas sp. strain KSWIII
and Methylococcus capsulatus Bath differ by 11.3%
(53). Taking into account these dissimilarity values, it
can only be speculated that clone M84-S38 corresponds to a novel
methanotrophic bacterium which harbors sMMO. The remaining six clones
were false positives containing non-mmoX sequence types.

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FIG. 3.
Distance dendrogram constructed for partial
mmoX sequences based on 286 derived amino acid sites.
The dendrogram shows environmental mmoX sequences
retrieved from roots of submerged rice plants (M84, M90) in relation to
mmoX sequences of representative type I and type II
methanotrophs. The environmental mmoX sequence
designated peat bog clone 24 (AF004555) was retrieved from an acidic
Sphagnum peat bog (12). The numbers at the
nodes indicate the percentage of recovery in 500 bootstrap resamplings.
Only bootstrap values 50 are shown. Scale bar, 0.1 substitution per
amino acid site. Database accession numbers of reference organisms are
as follows: Methylocystis sp. strain LR1, Y18440;
Methylocystis sp. strain M, U81594; Methylosinus
trichosporium, X55394; Methylocella palustris,
AF004554; Methylococcus capsulatus, M90050; and
Methylomonas sp. strain KSWIII, AB025022.
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mxaF.
Twenty-four of 50 clones analyzed formed
a coherent mxaF sequence cluster related to
Methylomonas methanica and Methylomicrobium album. One sequence type each could be assigned to
Methylocystis sp. strain LR1 (16), strain LK6
(Fig. 4), and
Hyphomicrobium sp. strain CM2 (data not shown). The
remaining 23 clones were false positives containing non-mxaF
sequence types.

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FIG. 4.
Distance dendrogram constructed for partial
mxaF sequences based on 172 derived amino acid sites.
The dendrogram shows environmental mxaF sequences
retrieved from roots of submerged rice plants (M84, M90) in relation to
mxaF sequences of representative type I and type II
methanotrophs, and Methylobacterium organophilum. The
mxaF sequence He-III [AF126296] was retrieved from
rice soil incubations (28), while Mo1 [AF283243] and Mo2
[AF283244] were detected in a methanotrophic consortium enriched with
a high CH4/low O2 mixing ratio
(31). The numbers at the nodes indicate the percentage of
recovery in 500 bootstrap resamplings. Only bootstrap values 50 are
shown. Scale bar, 0.1 substitution per amino acid site. Database
accession numbers of reference organisms are as follows:
Methylocystis sp. strain LR1, Y18441;
Methylocystis sp. strain M, U70517; Methylocystis
parvus, U70515; Methylosinus sporium, U70514;
Methylosinus trichosporium, U70516; Methylocella
palustris, AJ27831; Methylomicrobium album,
U70513; Methylomonas methanica, U70512;
Methylococcus capsulatus, U70511; strain LK6, U86503;
and Methylobacterium organophilum, M22629.
|
|
16S rDNA and 16S rRNA analysis of type I methanotrophs.
16S
rDNA clone libraries were generated from samples M70, M84, and M90. An
rcDNA clone library was created only from freshly prepared roots of
sample M70. Because RT-PCR was unsuccessful with the primer set
MethT1dF and MethT1bR, we replaced MethT1bR with primer MethT1cR (Table
1). The use of MethT1cR resulted in an amplicon of the predicted size
(556 bp). The retrieval of both 16S rDNA and 16S rRNA led to the
identification of a diverse community of type I methanotrophs (Fig.
5). No false-positive clone sequences
were detected in a set of 23 16S rDNA and 6 16S rcDNA clones randomly
selected for analysis. This underlines the target specificity of these
PCR primers for type I methanotrophs (57).

View larger version (28K):
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|
FIG. 5.
Distance dendrogram showing the 16S rDNA clone sequences
retrieved from roots of submerged rice plants (samples M70, M84, and
M90) in relation to type I methanotrophs and nonmethanotrophic
members of -Proteobacteria. The environmental 16S
rDNA sequences encompass the clones M70-D2 to M90-D34. Due to
limited sequence length (556 bp), the 16S rcDNA clones
M70-R5 to M70-R40 (R = 16S ribosomal copy DNA recovered from total RNA of sample M70) have
been inserted into the distance dendrogram using parsimony methods.
RRI1 (AF179603) was retrieved from rhizosphere soil of a flooded rice
microcosm (3). The 16S rDNA sequences of
-proteobacterial type II methanotrophs were used to root the tree.
The numbers at the nodes indicate the percentage of recovery in
500 bootstrap resamplings. Only bootstrap values 50 are
shown. Scale bar, 0.1 substitution per nucleotide sequence position.
Database accession numbers of reference organisms are as follows:
Methylocystis sp. strain M, U81595; Methylocystis
parvus, Y18945; Methylobacter sp. strain BB5.1,
AF016981; Methylobacter bovis, L20839;
Methylobacter capsulatus, L20843; Methylobacter
luteus, M95657; Methylobacter psychrophilus,
AF152597; Methylobacter vinelandii, L20841;
Methylobacter whittenburyi, X72773;
Methylomicrobium agile, X72767; Methylomicrobium
album, M95659; Methylomicrobium pelagicum,
L35540; Methylomonas aurantiaca, X72776;
Methylomonas methanica, AF50806; Methylomonas
fodinarum, X72778; Methylomonas rubra, M95662;
Methylosphaera hansonii, U77533; Methylocaldum
gracile, U89298; Methylocaldum szegediense,
U89300; Methylocaldum tepidum, U89297;
Methylococcus capsulatus, L20842;
Escherichia coli, V00348; Erwinia
carotovora, M59149; Vibrio cholerae,
O11197; Pseudomonas flavescens, U01916; and
Legionella steigerwaltii, X73400.
|
|
 |
DISCUSSION |
Root-associated methanotroph diversity assessed by
comparative analysis of pmoA, mmoX,
mxaF, and 16S rRNA and rDNA sequences.
The
branching pattern of the pmoA tree showed a remarkable
congruence with that of the 16S rDNA and rcDNA tree (Fig. 1A and 5).
Therefore, it is highly likely for example that pmoA cluster III corresponds to the 16S rDNA branch characterized by the clones M90-D37, M84-D38, and M84-D36. Although it is difficult to deduce a
close phylogenetic correspondence between distinct clusters of
environmental sequence types from two different gene markers, the
similarity in the tree topologies suggests that members of the same
type I sublineages were detected by both the pmoA and 16S
rDNA approaches. This finding agrees well with the results of a
cultivation-independent characterization of methanotrophic populations
in the sediment of Lake Washington (Seattle, Wash.) (10). The comparison of environmental libraries
constructed for methanotroph 16S rRNA and pmoA genes also
showed that the two different genes cover very similar ranges of diversity.
The
mxaF gene represents a universal marker for
methylotrophs. Its retrieval should allow detection of a range of
methanotroph
diversity similar to that detected by recovery of
pmoA and 16S
rRNA and rDNA. However, almost all
mxaF clones formed only one
distinct cluster which might
phylogenetically correspond to members
of
pmoA cluster I
(Fig.
1A and
4). This finding suggests that
the currently available
mxaF PCR assay is only of limited value
for the assessment
of methanotroph and methylotroph diversity
and should be applied only
in conjunction with other gene
markers.
Both the
pmoA-based T-RFLP profiles (Fig.
1 and
2) and the
retrieval of
mmoX confirmed the presence of type II
methanotrophs
on rice roots. The
mmoX-targeted primers used
in this study can
be considered to be complementary to primer sets
previously published
for the specific detection of
mmoX
(
2,
40,
43). Their applicability
in environmental studies
is demonstrated especially by the retrieval
of clone M84-S38 (Fig.
3).
This sequence type expands our current
knowledge about
mmoX-based methanotroph diversity. Overall, comparative
sequence analysis of cloned
pmoA,
mmoX,
mxaF, and 16S rDNA and
rcDNA revealed a genetically highly
diverse methanotrophic community
associated with rice
roots.
Comparison of various pmoA-based approaches to
assessing methanotroph diversity (cloning, DGGE, and T-RFLP
analysis).
The frequency distribution of methanotroph subgroups in
the clone library generated from sample M84 was not consistent with the
relative signal intensities of the corresponding T-RFs observed in the
T-RFLP community profiles (Fig. 1). For instance, pmoA sequence types affiliated with Methylomicrobium album
(350-bp T-RF) and Methylobacter sp. strain BB.1 (505-bp
T-RF) were not detected by the cloning approach. This finding might be
indicative of cloning bias and/or sampling error (i.e., analysis of too
few pmoA clones). Similarly, the proportion of type II
methanotroph pmoA sequence types in the clone library was
lower (2 of 28 clones analyzed) than one would expect based on the high
relative signal intensity of the 245-bp T-RF (35.4%). This
observation indicates either some bias against cloning of
pmoA genes from type II methanotrophs or errors in the
strict correlation of the 245-bp T-RF with type II methanotrophs of the
Methylocystis-Methylosinus group. However, both
T-RFLP analysis of individual pmoA clones retrieved from rice roots and a thorough in silico analysis of our current database of
approximately 130 pmoA sequences suggest such a strict
correlation of the 245-bp T-RF with type II methanotrophs.
The disparity between the frequency distribution of methanotroph
subgroups in the clone library and the relative signal intensities
of
the corresponding T-RFs stresses a major methodological advantage
of
MspI-based T-RFLP analysis

that it provides an exact
quantitative
measure of the T-RF composition of
pmoA PCR
products. Also,
pmoA-based
methanotroph diversity detectable
by T-RFLP analysis was clearly
higher than that detectable by
DGGE (Fig.
1B versus C). Explanations
for this finding might be
that sequence types are separated in
T-RFLP analysis and DGGE by
different methodological principles
and staining of DGGE gels is less
sensitive than fluorescence
detection in T-RFLP analysis. Taking
these observations together,
it can be concluded that for
cultivation-independent assessment
of methanotroph diversity
pmoA-based T-RFLP analysis represents
an important
tool to complement the
pmoA-based cloning approach
and
DGGE.
Ecological significance of root-associated methanotroph
diversity.
The analysis of phospholipid ester-linked fatty acids
(PLFA) recovered from rhizosphere soil of flooded rice microcosms
indicated an increased abundance of type I methanotrophs after
NH4+ fertilization (ninefold
increase in the type-I-specific PLFA biomarker), while the
type-II-specific PLFA biomarker increased only two- to threefold after
NH4+ fertilization
(3). These results led to the conclusion that a high
ammonium concentration is essential for growth of type I methanotrophs.
In a control experiment based on molecular retrieval of 16S rDNA and
DGGE, type I methanotrophs were also detected in rhizosphere soil of
unfertilized rice microcosms. However, type I methanotrophs were not
detected in the bulk soil of these microcosms. Based on these
preliminary data, it was concluded that the rice plant itself also
favors growth of type I methanotrophs (3).
The latter conclusion is clearly supported by this study. The T-RFLP
profiles suggest a substantially higher relative abundance
of type I
methanotrophs on rice roots than in the bulk soil (Fig.
2). The
detection of rRNA from type I methanotrophs (Fig.
5) provides
evidence that these species are metabolically active and thus
further
supports the idea that rice roots are an important habitat
for type I
methanotrophs. The promotion of methanotrophic activity
by rice plants
might be of twofold nature. The diffusional input
of oxygen into the
root environment directly affects the activities
of the obligately
aerobic methanotrophs. An indirect effect on
NH
4+ availability might be
mediated by the escape of oxygen from the
root tissue into the
rhizosphere soil, which can increase the
redox potential in the root
vicinity and, as a consequence, lead
to the desorption of fixed
NH
4+ ions from clay minerals
(
51). Increased availability of ammonium
should especially
favor proliferation of type I methanotrophs
(
3,
27).
The T-RFLP profiles obtained from rice roots and bulk soil are
characterized by high relative signal intensities of the type
II
methanotroph-specific 245-bp T-RF (35.4 and 67%,
respectively).
In the anoxic bulk soil, 16S rRNA genes
extracted from desiccation-resistant
exospores and lipid cysts
formed by
Methylosinus spp. and
Methylocystis spp. (
56), respectively, as well as from vegetative cells
present
in a stage of anaerobic dormancy (
46,
47), might
have contributed
to the high relative signal
intensity.
The cultivation-independent characterization of type I
methanotrophs in unfertilized rhizosphere soil by Bodelier et al.
(
3)
resulted in the detection of only one distinct cluster
of highly
similar 16S rDNA sequence types related to
Methylobacter spp.
(Fig.
5, sequence type RRI1). By
contrast, our results of comparative
sequence analysis of cloned
pmoA and T-RFLP community profiling
revealed a more complex
population structure encompassing type
I methanotrophs affiliated with
the genera
Methylomonas,
Methylobacter,
Methylomicrobium, and
Methylococcus and a novel
type I methanotroph
sublineage. The considerable number of distinct
methanotrophic
populations that colonized the root compartment is also
illustrated
by the recovery of various 16S rDNA sublineages of type I
methanotrophs.
The presence of such a highly diverse methanotrophic
community
might indicate that there are a large number of ecological
microniches
characterized by spatiotemporal variations in the mixing
ratios
of CH
4 and O
2
(
1,
30,
31) and in the availability of nitrogen
(
3,
24).
The hypothesis that the
CH
4/O
2 mixing ratio is an
important regulator of root-associated methanotroph diversity is
supported
by the close correspondence between
mxaF sequence
types obtained
in a previous study (clones Mo1/Mo2 [
31])
and the
mxaF cluster
detected on rice roots (Fig.
4). Mo1
and Mo2 were detected by
pmoA-based DGGE in a methanotrophic
consortium enriched from rice
field soil under a high
CH
4/low O
2 mixing ratio,
while enrichment
conditions using low CH
4/high
O
2 and low CH
4/low
O
2 mixing ratios
did not favor growth of these
type I
methanotrophs.
Final conclusions.
The comparison of data obtained by
retrieval of pmoA with those obtained by recovery of
mmoX, mxaF, and 16S rDNA and rRNA clearly
indicates that pmoA represents an excellent functional gene
marker for cultivation-independent analysis of methanotrophic diversity. However, the data also indicate that a comprehensive view of
methanotrophic diversity can be obtained only by a combined use of
various molecular techniques, i.e., by cloning and sequencing and by
cloning-independent fingerprinting. Within this framework, the
pmoA-based T-RFLP analysis proved to be a suitable tool to rapidly assess methanotrophic diversity. Taking all molecular data
together, a highly diverse community of type I and type II methanotrophs was detected. Except for Methylomicrobium
album, type I methanotroph populations were detected in the root
environment with clearly higher relative signal intensities than in the
bulk soil. Thus, the data as a whole agree well with the
hypothesis that type I methanotrophs are predominant in environments
that allow rapid growth of methanotrophic bacteria, while type II
methanotrophs are more abundant in environments where growth rates are
periodically restricted (27, 54).
 |
ACKNOWLEDGMENTS |
We are grateful to Sonja Fleissner for excellent technical assistance.
This work was supported by a grant from the European Community RTD
Programme Biotechnology (contract BIO-CT96-0419). M.T.Y. thanks the
Deutschen Akademischen Austauschdienst for financial support in the
form of a PhD scholarship.
 |
FOOTNOTES |
*
Corresponding author. Mailing address:
Max-Planck-Institut für terrestrische Mikrobiologie,
Karl-von-Frisch-Str., D-35043 Marburg, Germany. Phone: 49 (6421) 178 720. Fax: 49 (6421) 178 809. E-mail address:
liesack{at}mailer.uni-marburg.de.
 |
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Applied and Environmental Microbiology, September 2001, p. 4177-4185, Vol. 67, No. 9
0099-2240/01/$04.00+0 DOI: 10.1128/AEM.67.9.4177-4185.2001
Copyright © 2001, American Society for Microbiology. All rights reserved.
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