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Applied and Environmental Microbiology, August 1999, p. 3319-3324, Vol. 65, No. 8
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Anaerobic Mineralization of Quaternary Carbon
Atoms: Isolation of Denitrifying Bacteria on Dimethylmalonate
Olaf
Kniemeyer,1
Christina
Probian,1
Ramon
Rosselló-Mora,2 and
Jens
Harder1,*
Department of
Microbiology1 and Molecular Ecology
Group,2 Max-Planck-Institute for Marine
Microbiology, D-28359 Bremen, Germany
Received 19 January 1999/Accepted 18 May 1999
 |
ABSTRACT |
The microbial capacity to degrade simple organic compounds with
quaternary carbon atoms was demonstrated by enrichment and isolation of
five denitrifying strains on dimethylmalonate as the sole electron
donor and carbon source. Quantitative growth experiments showed a
complete mineralization of dimethylmalonate. According to phylogenetic
analysis of the complete 16S rRNA genes, two strains isolated from
activated sewage sludge were related to the genus
Paracoccus within the
-Proteobacteria (98.0 and 98.2% 16S rRNA gene similarity to Paracoccus
denitrificansT), and three strains isolated from
freshwater ditches were affiliated with the
-Proteobacteria (97.4 and 98.3% 16S rRNA gene
similarity to Herbaspirillum seropedicaeT and
Acidovorax facilisT, respectively).
Most-probable-number determinations for denitrifying populations in
sewage sludge yielded 4.6 × 104
dimethylmalonate-utilizing cells ml
1, representing up to
0.4% of the total culturable nitrate-reducing population.
 |
INTRODUCTION |
Quaternary carbon atoms bind with
all four single
bonds to carbon atoms. This structural motif is
found in many isoprenoic compounds, e.g., the monoterpenes pinene and
carene, cholesterol, and carotene. The biosynthetic pathway involves an
irreversible cationic polymerization of alkene bonds to newly formed
carbon-carbon single bonds. As a result, quaternary carbon atoms are
formed from tertiary carbon atoms (9).
The microbial degradation of compounds with quaternary C atoms has not
been studied thoroughly. Already-discovered mineralization pathways in
aerobic microorganisms often involve molecular oxygen as a cosubstrate.
Camphor and eucalyptol feature a ketone in an
position with respect
to a quaternary C-atom. This functional group enables a biological
Baeyer-Villiger oxygenation to a lactone that yields, after hydrolysis,
a tertiary alcohol (31). A second pathway is provided by
Candida albicans sterol 14
-demethylase, a cytochrome P450
monooxygenase. This enzyme catalyzes the oxidation of a methyl group
adjacent to a quaternary C atom to an aldehyde that is oxidized in a
third monooxygenation reaction and is eliminated as formate. Thus, the
quaternary C atom is changed via radical intermediates into a tertiary
C atom with an alkene bond (27). This aldehyde lyase
reaction was first described for aromatase, which catalyzes the C-19
removal of androgens, leading to the formation of estrogens (2,
32). Another pathway present in aerobic bacteria involves an
oxygenation of the C-9 atom of cholesterol. The
9
-hydroxy-androsta-1,4-dien-2,17-dione formed is labile and reacts
nonenzymatically to produce
9,10-seco-androsta-1,3,5(10)-trien-3-ol-9,17-dione. The spontaneous
carbon-carbon cleavage obliterates a quaternary C atom and a tertiary
alcohol (16).
One example of an oxygen-independent pathway is the cleavage of
-pinene oxide by a lyase. Three rings are opened in an isomerization reaction, and at the same time a quaternary C atom is transformed into
a tertiary C atom (11). This rather unusual intramolecular depolymerization reaction can be perceived as the reverse of the biosynthetic pathway.
Research on the fate of quaternary carbon atoms in anoxic habitats
advanced with the recent report of denitrifying
-Proteobacterium strain 72Chol, that anaerobically
mineralizes cholesterol (14). In a theoretical analysis, we
developed a plausible pathway for the degradation of cholesterol via
carboxy-methylmalonates as possible intermediates (17).
Hence, dimethylmalonate was chosen for enrichment and isolation of
denitrifying bacteria to verify the existence of the physiological
capacity to mineralize a small compound with a quaternary carbon atom
in the absence of molecular oxygen.
 |
MATERIALS AND METHODS |
Sources of organisms.
Enrichment cultures were inoculated
with activated sludge obtained from a local wastewater treatment plant
(Lintel, Osterholz-Scharmbeck, Germany) or with a water-mud mixture
obtained from freshwater ditches located in Bremen, Germany.
Most-probable-number (MPN) counts were performed with the activated
sludge. Alcaligenes defragrans strains (8),
Azoarcus sp. strain 22Lin (12), and Thauera linaloolentis and Thauera terpenica strains
(7) were maintained in our laboratory since their isolation.
Media and culture conditions.
Anoxic media and cultivation
techniques were used in this study (33). The basic medium
contained (per liter of distilled water) 0.5 g of
MgSO4 · 7H2O, 0.5 g of
NH4Cl, 0.5 g of KH2PO4, 0.1 g of CaCl2, and 0.85 g of NaNO3
(10 mM). After autoclaving, 2 ml of a chelated trace element mixture (1 liter of distilled water contained 2,100 mg of FeSO4
· 7H2O, 30 mg of H3BO3, 100 mg of
MnCl2 · 4H2O, 190 mg of
CoCl2 · 6H2O, 24 mg of
NiCl2 · 6H2O, 29 mg of
CuSO4 · 5H2O, 144 mg of
ZnSO4 · 7H2O, 36 mg of
NaMoO4 · 7H2O, and 5.2 g of EDTA,
pH 6.5), 2 ml of selenite-tungstate solution (0.4 g of NaOH
liter
1, 8 mg of Na2WO4 · 2H2O liter
1, and 6 mg of
Na2SeO3 · 5H2O liter
1)
(33), 1 ml of vitamin solution (4 mg of 4-aminobenzoic acid, 2 mg of D-(+)-biotin, 10 mg of nicotinic acid, 5 mg of
calcium D-(+)-pantothenate, 15 mg of pyridoxin
hydrochloride, 4 mg of folic acid, and 1 mg of lipoic acid in 100 ml of
10 mM NaH2PO4, pH 7.1), 1 ml of cyanocobalamin
solution (50 mg liter
1), 1 ml of thiamine solution (10 mg
of thiamine hydrochloride in 100 ml of 25 mM
NaH2PO4, pH 3.4), 1 ml of riboflavin solution (2.5 mg in 100 ml of 25 mM NaH2PO4, pH 3.2)
(1), and 50 ml of NaHCO3 solution (1 M) were
added, and the pH was adjusted to 7.2. N2-CO2
(90:10, vol/vol) was used as the gas phase for all anoxic cultures.
Electron donors were added from sterile stock solutions prior to
inoculation. All incubations were performed at 28°C in the dark.
Enrichment and isolation of denitrifying bacteria on
dimethylmalonate.
Enrichment cultures contained 330 ml of medium
with 5 mM dimethylmalonate and 20 ml of sewage sludge or 250 ml of
medium and 100 ml of a water-mud mixture in 0.5-liter bottles that were
sealed with thick butyl rubber stoppers. Control enrichments were
prepared in parallel without dimethylmalonate to account for
endogeneous carbon sources of the inoculate. Overpressure due to gas
formation and the amounts of nitrate and nitrite in the culture were
determined regularly, and 10 mM nitrate was added when the electron
acceptor was depleted. Transfer of the enrichment cultures involved an anaerobically performed serial dilution prior to inoculation to obtain
an inoculation size of 1.0 × 10
6 (vol/vol) for a
medium volume of 150 ml. After three passages, bacteria were isolated
via repeated dilution in agar with 5 mM dimethylmalonate and 10 mM
nitrate (33). Isolated colonies were pure strains according
to microscopic observations of cultures grown on AC broth (Difco,
Detroit, Mich.), yeast extract (0.5 g liter
1), glucose (5 mM), or pyruvate (10 mM) under fermenting or denitrifying conditions
and according to the formation of homogenous colonies on oxic agar
plates containing either AC broth or dimethylmalonate.
Strain maintenance and growth tests.
Isolated strains were
kept in culture tubes (21 ml) with 15 ml of anoxic medium under
selective growth conditions (5 mM dimethylmalonate and 10 mM nitrate).
Transfer of an inoculum of 5% (vol/vol) into freshly prepared culture
medium was done every second month. Grown cultures were transferred to
a refrigerator and kept at 8°C until the next transfer. Growth
experiments were performed in duplicate with culture tubes with an
inoculum of 2% (vol/vol). Growth was monitored by turbidimetry at 660 nm, and nitrate and nitrite were analyzed in the late stationary phase.
Control experiments demonstrated that the carbon sources present in the
vitamin solutions and the inoculate did not support observable
microbial growth.
The quantification of dimethylmalonate degradation was done by
inoculating a 1- or 5-ml portion of a recently grown culture into 200 ml of medium in a 250-ml Erlenmeyer flask with a depressed sidearm for
turbidimetric determinations and a threaded neck to hold the butyl
rubber stopper with a screw cap against the overpressure that is build
up by denitrification. The culture was regularly sampled with sterile,
nitrogen-flushed syringes for analyses of organic acids, nitrite, and
nitrate. Nitrogen formation was measured in cultures containing an
He-CO2 (90:10, vol/vol) atmosphere. Formation of carbon
dioxide was assayed in cultures that were made without bicarbonate and
carbon dioxide and were buffered by potassium phosphate (20 mM, pH
7.0).
Denitrifying growth on dimethylmalonate occurred not only in
oxygen-free media but also in chemically reduced media. Anoxic
media
were prereduced in control experiments with 4 mM ascorbate.
The strains
did not utilize ascorbate as a carbon and energy source.
Thus,
ascorbate could routinely be added to ensure anoxic conditions
in the
culture.
Enumeration of dimethylmalonate-utilizing denitrifying
bacteria.
The size of the denitrifying population in sewage sludge
was estimated with MPN dilutions in liquid medium (3). MPN
counts were performed with the medium described above and either 5 mM dimethylmalonate or a mixture of fatty acids (acetate, propionate, and
butyrate [2 mM each compound] and succinate, valerate, isovalerate,
-methylbutyrate, and isobutyrate [50 µM each compound]) as the sole electron donor. A 10-fold dilution was used, with three portions per dilution. The MPN culture tubes were incubated in the dark at
20°C for 18 weeks.
Chemical analyses.
Biomass formation was measured
turbidimetrically at 660 nm. Cell dry weight determinations were
performed as described previously (12). Qualitative
measurements of nitrate consumption were performed with an indicator
strip (Merck, Darmstadt, Germany). Nitrate and nitrite were determined
quantitatively by high-pressure liquid chromatography (13),
and gases (dinitrogen oxide, dinitrogen, and carbon dioxide) were
determined by packed-column gas chromatography as described previously
(14). Ammonium was measured photometrically by the
indophenol method (14). Organic acids were quantified by ion
exclusion chromatography on a WA1 column (7.8 by 300 mm; Sarasep, San
Jose, Calif.) with a high-pressure liquid chromatography system (Sykam,
Garching, Germany) equipped with a UV detector (Linear Instruments,
Fremont, Calif.). Culture samples of 950 µl were acidified with 50 µl of 1 M H2SO4 and clarified by
centrifugation. Subsamples of 50 µl were separated with 5 mM
H2SO4 as the liquid phase at a flow rate of 0.6 ml min
1 at 35°C. Organic acids were detected at 210 nm.
Net retention times for dimethylmalonate, acetate, and propionate were
5.09, 9.23, and 11.97 min, respectively.
Cells were observed with a standard phase-contrast microscope (Zeiss,
Oberkochen, Germany) with an oil immersion objective
(100/1.6). Dense
cultures were wet mounted on glass slides coated
with 2% washed agar
(
26) and photographed by using Ortho 25
film (Agfa-Gevaert,
Leverkusen,
Germany).
16S rRNA gene sequence and data analysis.
In vitro
amplification of the 16S rRNA gene and direct sequencing were performed
as previously described (29). Sequencing reactions were
performed with a Taq Dyedeoxy Terminator Cycle Sequencing kit (Applied
Biosystems, Foster City, Calif.) and were run on an Applied Biosystems
373S DNA sequencer. The obtained sequences were added to an alignment
of about 5,300 homologous bacterial 16S rRNA primary structures
(22), applying the aligning tool of the ARB program package
(30). Phylogenetic trees were constructed by using subsets
of data that included sequences from outgroup reference organisms as
well as representative and genealogically related sequences of members
of the alpha and beta subclasses of Proteobacteria
(22). Topologies were evaluated by using distance matrix,
maximum-parsimony, and maximum-likelihood methods as implemented in the
ARB software to elaborate a consensus tree (21).
Whole-cell in situ hybridization.
Microbes that were grown
in highly diluted MPN tubes were analyzed by whole-cell in situ
hybridization for the presence of
- and
-Proteobacteria as described by Manz et al.
(23). Probes EUB338 (23) and ALF968
(24) were used to detect Eubacteria and
-Proteobacteria, respectively. For
-Proteobacteria, CY3-labelled probe BET42a was used with
a nonlabelled competitor probe, GAM42a (23).
Nucleotide sequences accession numbers.
The sequences
determined in this work have been deposited under EMBL accession
numbers AJ012067 to AJ012071.
 |
RESULTS |
Enrichment and isolation.
The capacity of nitrate-reducing
microorganisms to degrade dimethylmalonate was investigated with
activated sludge and a water-mud mixture from freshwater ditches. A
small inoculum of the former was used to reduce the amount of
endogenous electron donors. The enrichment containing 5 mM
dimethylmalonate and 10 mM nitrate consumed all nitrate within 9 days
and formed 30 ml of gas. After nitrate addition, the gas formation
continued to a total volume of 47 ml on day 16. A control experiment
without dimethylmalonate produced only 8 ml of gas in this time. The
freshwater enrichment contained a significant amount of endogenous
electron donors for nitrate reduction. The control consumed nearly 30 mM nitrate in 20 days and formed 89 ml of gas. Gas formation in the
enrichment culture started to exceed that in the control on day 14 and
accumulated to 116 ml on day 20, when 40 mM nitrate was consumed. Small
inocula of these enrichment cultures (150 nl obtained by serial
dilution) were transferred, resulting in a dilution of 1 ppm to select
for bacteria that were probably present in larger amounts in the
enrichment. Two additional passages with small inocula (1 ppm) ensured
a selection for bacteria that grew well on dimethylmalonate. Isolation
by agar dilution series was then successfully attempted. Two strains, B8B1 and B8B2, originated from activated sludge, and three strains, G7A1, G8A1, and G8B1, originated from the freshwater ditches.
Characterization of the isolated strains.
Strains B8B1 and
B8B2 were nonmotile spherical cells or short rods with dimensions of
0.7 to 1.0 by 1.0 to 2.0 µm, resembling Paracoccus.
Strains G7A1 and G8B1 were Pseudomonas-like motile straight
rods with sizes of 0.5 to 0.7 by 1.5 to 2.5 µm. The motile strain
G8A1 was a small spirillum, 0.3 to 0.5 by 1.0 to 2.0 µm in size (Fig.
1). The microorganisms grew on several
organic acids, including isobutyrate. Strains G7A1 and G8B1 did not
utilize methylsuccinate. Sugars were utilized only by strains B8B1 and
B8B2 (Table 1).

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FIG. 1.
Phase-contrast photomicrographs of new denitrifying
isolates grown with dimethylmalonate (5 mM) and nitrate (10 mM). Bar,
10 µm.
|
|
Carbon limitation was achieved with 2 mM dimethylmalonate in the
presence of 10 mM nitrate. Grown cultures of all strains
contained
nitrate and dinitrogen oxide but no nitrite. Nitrate-limited
cultures
were obtained with 5 mM dimethylmalonate and 10 mM nitrate.
Nitrate and
nitrite were depleted under these conditions. Nitrogen
formation was
observed in cultures with a helium atmosphere. Ammonium
present in the
medium was assimilated during denitrifying growth,
excluding
ammonification as a catabolic
process.
Different biomass yields were observed for the strains in
carbon-limited cultures and in nitrate-limited cultures; i.e., strains
B8B1 and B8B2 produced an optical density (OD) at 660 nm of 0.6
on 10 mM nitrate, whereas strains G7A1, G8A1, and G8B1 produced
an OD of only
0.3. Koch showed that, in the absence of pigments,
cells with a volume
range of 0.4 to 2 µm
3 had an average dry weight/OD ratio
of 371 mg (dry weight) liter
1 OD at 660 nm
1
(
18). To account for the smaller size of strain G8A1 cells,
we determined the dry weight formed in nitrate-limited denitrifying
cultures: strain B8B2 formed 21.4 g (dry weight) mol of
nitrate
1, whereas strains G8A1 and G8B1 formed only 10.3 and 10.8 g (dry
weight) mol of nitrate
1,
respectively.
All strains grew aerobically on nitrate-free agar plates with
dimethylmalonate.
Quantification of denitrifying growth on dimethylmalonate.
Strain B8B2 was used to determine quantitatively dimethylmalonate and
nitrate consumption (Fig. 2). A biomass
of 32.6 mg was formed based on a measured correlation of 427.6 mg (dry
mass) liter
1 to 1 liter of culture with an OD of 1.0. According to the assimilation equation
17C5H8O4 + 2H2O
20C4H7O3 + 5CO2, this corresponds to a consumption of 269 µmol of
dimethylmalonate. Since 870 µmol of dimethylmalonate disappeared
during growth, complete mineralization of the calculated amount of
dissimilated dimethylmalonate (601 µmol) would provide a total of 12 mmol of electrons for denitrification. Ten millimoles of electrons is
required to account for a reduction of nitrate (2 mmol consumed) to
dinitrogen. In separate experiments, the nitrogen and carbon balances
were analyzed. In nitrate-limited cultures grown under a helium
atmosphere, nitrate consumption of 2.56 mmol of nitrogen atoms occurred
with the synthesis of 160 µmol of dinitrogen oxide N and 2.13 mmol of
nitrogen N. Carbon dioxide formation correlated with the amount of
dimethylmalonate supplied. In grown carbon-limited cultures (2 mmol of
C as dimethylmalonate), we detected 1.35 mmol of carbon dioxide; the
increase in biomass represented, according to the aforementioned
equation, an assimilation of 776 µmol of C. Thus, the electron,
nitrogen, and carbon balances support within experimental uncertainties
the complete mineralization of dimethylmalonate according to the
catabolic reaction C5H8O4 + 4H+ + 4NO3
5CO2 + 2N2 + 6H2O.
Phylogenetic affiliations of the isolated strains.
Almost-complete 16S rRNA gene sequences from the isolates were obtained
by in vitro amplification and direct sequencing. The sequences of
strains B8B1 and B8B2 were nearly identical, with a similarity of
99.8%, and strains G7A1 and G8B1 had identical sequences. Sequence
analysis showed that both activated-sludge strains B8B1 and B8B2 were
affiliated with the genus Paracoccus of the
-Proteobacteria (Fig. 3).
Their closest relative was P. denitrificans, with a sequence
similarity of 98.0%. Similarities of this strains to one group of
Paracoccus species (P. alcaliphilus, P. aminophilus, P. aminovorans, P. thiocyanatus, and P. versutus) ranged from 96.8 to
97.5%, and those to a second group of Paracoccus species
(P. alkenifer, P. marcusii, P. solventivorans, and P. kocurii) ranged from 94.9 to
95.4%. In contrast, all three ditch isolates were affiliated with the
-Proteobacteria. Strains G7A1 and G8B1 were affiliated
with the genus Acidovorax, having 98.3% sequence similarity
with the type strains of Acidovorax facilis. The closest
relative to both ditch isolates, with a similarity of 99.3%, was the
activated-sludge clone sequence T20 (28). Strain G8A1 was
affiliated with the same branch as Herbaspirillum seropedicae (97.4% similarity) and a soil ultramicrobacterium, strain MY14, (97.0% similarity) within the
Oxalobacter-Telluria-Duganella lineage. Based on these
phylogenetic affiliations and the consistent cell morphologies, three
isolated strains were selected for deposition at the German Collection
of Microorganisms and Cell Cultures, Braunschweig (8a), as
Acidovorax sp. strain G8B1 (DSM 12578), Herbaspirillum sp. strain G8A1 (DSM 12579), and
Paracoccus sp. strain B8B2 (DSM 12584).

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FIG. 3.
16S rRNA-based tree reflecting the phylogenetic
relationships of (i) strains B8B1 and B8B2 and a selection of
Proteobacteria from the alpha subclass and (ii) strains
G7A1, G8B1, and G8A1 and a selection of Proteobacteria of
the beta subclass. The tree is based on the results of a distance
matrix analysis including complete or almost-complete 16S rRNA
sequences from representative bacteria of the , , and subclasses (22). The topology of the tree was evaluated and
corrected according to the results of distance matrix,
maximum-parsimony, and maximum-likelihood analyses of various data
sets. The phylogenetic positions of the analyzed strains did not differ
in any of the treeing approaches. Multifurcations indicate topologies
that could not be unambiguously resolved. The bar indicates 5%
estimated sequence divergence. The P. denitrificans group
comprises the species P. denitrificans (GenBank accession
no. X69159) and P. versutus (D32243 and D32244) and
Paracoccus sp. strains KL1, KS1, and KS2 (U58017, U58016,
and U58015). The P. aminovorans group comprises the species
P. aminovorans (D32240), P. alcaliphilus
(D32238), and P. thiocyanatus (D32242). The A. delafieldii group comprises the species A. delafieldii
(AF078764), A temperans (AF078766), and A. facilis (AF078765) and Acidovorax sp. strain 7078 (AF078767). The A. avenae group comprises A. anthurii (AJ007013), A. konjaci (AF078760), A. avenae subsp. avena (AF078759), A. avenae
subsp. citrulli (AF078761), A. avenae subsp.
cattleyae (AF078762), and Acidovorax sp. strain
IMI 357678 (AF078763). Accession numbers of other bacterial 16S rRNA
gene sequences are U00006 (Escherichia coli), D13429
(Bradyrhizobium japonicum), D32239 (P. aminophilus), D32241 (P. kocurii), X53855
(Rhodobacter sphaeroides), D16211 (Rhodoferax
fermentans), D30793 (Variovorax paradoxus), Z93964
(unidentified bacterium clone T20), M11224 (Comamonas
testosteroni), AB008503 (ultramicrobacterium strain MY14), Y10146
(H. seropedicae), X65590 (Telluria
chitinolytica), U49757 (Oxalobacter formigenes), X74914
(Duganella zoogloeoides), and X07714 (Neisseria
gonorrhoeae).
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Population sizes of denitrifying bacteria.
Volatile fatty
acids are major primary fermentation products and may as such be
important carbon sources and electron donors for denitrifying bacteria
in sewage plants. The population size of nitrate-reducing bacteria was
determined by MPN counts with either a defined mixture of fatty acids
or AC broth as an electron donor. Both measurements yielded the same
population size (data not shown). Thus, we now routinely use a defined
mixture of fatty acids as a carbon source for MPN counts of
nitrate-reducing bacteria in order to avoid the growth of fermentative bacteria.
Clarification of the wastewater at the plant in Lintel involved a
limited aeration to introduce early a sequential
nitrification-denitrification.
MPN counts on samples from the first and
third basins indicated
a population of 4.6 × 10
4
bacteria ml
1 that were capable of denitrifying growth on
dimethylmalonate.
The total denitrifying population decreased from the
first basin
(1.1 × 10
8 bacteria ml
1) to
the third basin (1.1 × 10
7 bacteria
ml
1). In situ hybridization of cells was performed on the
highest-diluted
MPN tubes exhibiting growth. The
Bacteria-specific probe EUB338
visualized 75% ± 24% of
DAPI (4',6-diamidino-2-phenylindole)-stained
cells from the fatty
acid-utilizing, nitrate-reducing microorganisms
with a statistical
population size of greater than 10
5 bacteria
ml
1. None of the cells hybridized with the

-
Proteobacteria-specific
probe, but the probe for the
beta subclass detected 52% ± 18%
of DAPI-stained cells. Major
contributions to the dimethylmalonate-degrading
denitrifying
subpopulation within the sludge were made by

-
Proteobacteria.
In MPN tubes representing greater than
10
3 cells ml
1, the EUB338 and BET42a probes
indicated a relative abundance
of 71% ± 24% of
Bacteria
and of 52% ± 18% of members of the beta
subclass. A small
contribution of

-
Proteobacteria (3% of DAPI-stained
cells) was found in a single MPN tube that represented a statistical
population density of greater than 10
3 cells
ml
1.
Some

-
Proteobacteria that were recently isolated
anaerobically on a comparable minimal medium with a single carbon and
electron
source and nitrate as an acceptor were tested for denitrifying
growth on dimethylmalonate.
Azoarcus sp. strain 22Lin and
Alcaligenes defragrans 51Men and 65Phen mineralized
dimethylmalonate. No utilization
was observed in cultures of
A. defragrans 54Pin
T and 62Car,
Thauera
linaloolentis 47Lol
T, and
Thauera terpenica
21Mol and 58Eu
T.
 |
DISCUSSION |
In this study we isolated, for the first time to our knowledge,
bacteria that are able to grow on dimethylmalonate as a carbon source
and electron donor. The anoxic culture conditions were chosen to select
for an oxygen-independent degradation pathway. In addition, aerobic
growth of the isolated microorganisms on dimethylmalonate demonstrated
the presence of dimethylmalonate-degrading capacities in
oxygen-respiring bacteria. The observation of quantitative dimethylmalonate oxidation attests to the capacity of microorganisms to
mineralize simple compounds with quaternary carbon atoms. The presence
of the dimethylmalonate-degrading capacity in a medium-sized population
of bacteria in sewage sludge suggests that dimethylmalonate and related
disubstituted malonates may be intermediates of the microbial
degradation of organic matter.
The enrichment procedure, with inocula sizes of 10
6
(vol/vol), allows the isolation of a probably abundant bacterium with
efficient growth on dimethylmalonate and nitrate. The isolation of
related strains B8B1 and B8B2 from sewage sludge and G7A1 and G8B1 from freshwater ditches reflects the high selection pressure during enrichment. The isolation of Paracoccus sp. strains B8B1 and
B8B2 from sewage sludge corresponds to the general methylotrophic
physiology of members of the genus Paracoccus
(20); e.g., Paracoccus cells constituted 3.5% of
the total population in a denitrifying sand filter fed with methanol
(25). Denitrification is also widespread among
Paracoccus species (20). However, analysis of the
dimethylmalonate-degrading bacteria grown in highly diluted MPN tubes
with oligodeoxynucleotide probes indicated a predominance of
-Proteobacteria. Hence, the Paracoccus strains
B8B1 and B8B2 had successfully competed with the
-Proteobacteria during the enrichment. The key advantage of the nitrate-limited enrichment was probably the higher biomass yield
of the Paracoccus strains. The partition of
-Proteobacteria in dimethylmalonate degradation was
confirmed by the freshwater isolates and by denitrifying growth of
Azoarcus sp. strain 22Lin and A. defragrans 51Men
and 65Phen on dimethylmalonate.
The isolates from freshwater ditches are
-Proteobacteria
related to the genera Acidovorax and
Herbaspirillum. The presence of
-Proteobacteria in highly diluted MPN tubes is in
agreement with in situ investigations of activated sludge that found a
dominance of
-Proteobacteria (28). Curiously,
a cloned 16S rRNA gene sequence obtained in that study (28),
clone T20, has the highest 16S rRNA gene sequence similarity (98.3%)
to the isolated strains G7A1 and G8B1. Members of Acidovorax
can denitrify (34, 35), but the described H. rubrisubalbicans and H. seropedicae are only able to
reduce nitrate to nitrite (4). Dinitrogen formation did not
occur. Phylogenetically related ultramicrobacteria were not tested for
the capacity to denitrify (15). Isolate G8A1 is the first
isolate in the phylogenetic group that reduces nitrate to dinitrogen
oxide and further to dinitrogen.
Two pathways for dimethylmalonate degradation can be considered. In
model studies for the mechanism of the coenzyme
B12-dependent methylmalonyl-coenzyme A (CoA) mutase,
dimethylmalonate derivatives of organocobalamin were found to decompose
spontaneously in neutral aqueous solutions. The products formed
included methylsuccinate derivatives (10). A similar
enzymatic rearrangement based on radical intermediates seems feasible,
especially because of the utilization of methylsuccinate by strains
G8A1, B8B1, and B8B2. The alternative is a decarboxylation yielding
isobutyrate derivatives. During incubation with
14CO2, Mn2+, ATP, and
isobutyryl-CoA, enzyme fractions of Mycobacterium sp. strain
IBS-M formed two labelled acids that were identified as succinate and
dimethylmalonate (19). Besides this observation, a
decarboxylase entity is imaginable based on the knowledge of methylmalonyl-CoA and malonyl-CoA decarboxylases (5, 6). We
will investigate these possibilities in future research.
 |
ACKNOWLEDGMENT |
This study was supported by the Max-Planck-Gesellschaft.
 |
ADDENDUM IN PROOF |
Acidovorax sp. strains G7A1 and G8B1 belong to the
recently established species Acidovorax defluvii
(26a) on the basis of 16S rRNA sequences.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Abteilung
Mikrobiologie, Max-Planck-Institut für marine Mikrobiologie,
Celsiusstr. 1, D-28359 Bremen, Germany. Phone: 49-421-2028-750. Fax:
49-421-2028-580. E-mail: jharder{at}mpi-bremen.de.
 |
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Applied and Environmental Microbiology, August 1999, p. 3319-3324, Vol. 65, No. 8
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