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Applied and Environmental Microbiology, May 2000, p. 1814-1817, Vol. 66, No. 5
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Quantification of phnAc and
nahAc in Contaminated New Zealand Soils by
Competitive PCR
Andrew D.
Laurie
and
Gareth
Lloyd-Jones*
Landcare Research, Hamilton, New Zealand
Received 7 September 1999/Accepted 7 February 2000
 |
ABSTRACT |
Unculturable polycyclic aromatic hydrocarbon (PAH)-degrading
bacteria are a significant reservoir of the microbial potential to
catabolize low-molecular-weight PAHs. The population of these bacteria
is larger than the population of nah-like bacteria that are
the dominant organisms in culture-based studies. We used the recently
described phn genes of Burkholderia sp. strain
RP007, which feature only rarely in culture-based studies, as an
alternative genotype for naphthalene and phenanthrene degradation and
compared this genotype with the genotypically distinct but ubiquitous
nah-like class in different soils. Competitive PCR
quantification of phnAc and nahAc, which encode
the iron sulfur protein large (
) subunits of PAH dioxygenases in
nah-like and phn catabolic operons, revealed that the phn genotype can have a greater ecological
significance than the nah-like genotype.
 |
INTRODUCTION |
It could mistakenly be inferred from
available nucleotide sequence data that highly conserved
nah-like gene clusters, which are isolated from polycyclic
aromatic hydrocarbon (PAH)-degrading pseudomonads obtained from diverse
geographic areas, are the dominant gene clusters involved in
degradation of the low-molecular-weight PAHs naphthalene and
phenanthrene. The results of probing and PCR amplification of
nah sequences from contaminated soils and sediments also
indicate that these sequences are ubiquitous (7, 17).
Although PAH degraders with nah genotypes are easily
isolated, it has been acknowledged that the nah catabolic
cluster and closely related homologues may be present in only a small
part of the PAH-degrading bacterial population (1, 4, 12,
20). Recently, the phn genes of
Burkholderia sp. strain RP007 provided evidence that there
is a different genotype that exhibits a low level of sequence homology
with nah and has a different gene order yet encodes enzymes
for an identical PAH degradation pathway (9, 10).
As increasingly diverse genes that encode enzymes for PAH catabolism
are characterized (4-6, 14, 20), it is important not only
to understand the function of these genes but also to determine their
ecological significance in the context of environmental pollution. The
objective of this study was, therefore, to compare the prevalence in
aromatic hydrocarbon-contaminated soils of two distinct PAH catabolic
genotypes. These genotypes were the divergent phn genes
(9, 10), which are difficult to isolate by conventional microbiological methods (12), and the easily isolated
nah-like genes (1, 7, 17). It has been shown that
culture-based methods overemphasize nah-like genes and fail
to detect bacteria with phn genotypes in contaminated soils
in which both nahAc and phnAc are detected by PCR
amplification and DNA hybridization (12). A molecular
biological approach was required to overcome the disparity in the ease
of culturing of host bacteria harboring these two genotypes. Highly
specific primer combinations, which targeted genes that encode the iron
sulfur protein large (
) subunits of the nah-like and
phn PAH initial dioxygenases, allowed us to determine the
number of copies of phnAc and nahAc present in
soil by a quantitative competitive PCR (QC-PCR) technique (3, 11, 19). Although this approach did not allow us to determine
relative activity or fluxes through nah-like and
phn pathways, it did reveal the relative enrichment of
populations after they were exposed to PAHs and allowed us to
demonstrate that the phn genotype was enriched in response
to the selective pressures exerted by specific PAHs in a range of soils.
 |
MATERIALS AND METHODS |
Soil samples and analysis.
Two soils from the Waikato region
of New Zealand (38°S, 175°E) containing different levels of PAHs
were selected for analysis. One soil (soil A) was obtained from the
site of a former town gas-generating plant and was severely
contaminated with PAHs; the other soil (soil B) was contaminated with
petroleum fuels. The PAH content of each sample was determined
commercially by using U.S. Environmental Protection Agency methods
3545, 3540, and 3630. The number of culturable heterotrophs present in
each sample was determined on R2A plates (Difco Laboratories, Detroit, Mich.) by spreading dilutions of a soil suspension that was prepared by
shaking 10 g of soil in 90 ml of 0.1% pyrophosphate along with 30 g of glass beads for 1 h at 25°C. The R2A plates were
incubated at 25°C for 48 h. Noncontaminated (pristine) soils
from central Siberia (61°N, 89°E), Ross Island in the Antarctic
(77°S, 166°E), and a native New Zealand forest (38°S, 175°E)
were used to assess the ubiquity of the phn genes in
different environments.
Development of QC-PCR protocol.
The PCR primers used for
specific probing of the nahAc and phnAc sequences
were designed during a previous study (12). Primer nahAcfor
(5'-TGGCGATGAAGAACTTTTCC) and primer nahAcrev
(5'-AACGTACGCTGAACCGAGTC) amplify a 992-bp region
encompassing nucleotides 63 to 1055 of Pseudomonas putida G7
nahAc (GenBank accession no. M83949). Primer P8073
(5'-TTCGAGCTGGAATGTGAGC) and primer P9047
(5'-AATAACCGGCGATTCCAAAC) amplify a 993-bp region
encompassing nucleotides 82 to 1075 of Burkholderia sp.
strain RP007 phnAc (GenBank accession no. AF061751). Since
in this study we relied on accurate relative quantification of specific
DNA templates, it was important that only homologous sequences were
amplified. Therefore, an annealing temperature of 65°C was used; this
temperature was determined empirically to be near the maximum optimum
annealing temperature for the two primer sets. PCR amplification was
carried out in 50-µl reaction mixtures that contained 20 mM Tris-HCl
(pH 8.4), 50 mM KCl, 1.25 mM MgCl2, each deoxynucleoside
triphosphate at a concentration of 200 µM, 2.5 U of PLATINUM
Taq DNA polymerase (Gibco BRL, Gaithersburg, Md.), 0.2 µM
forward primer, 0.2 µM reverse primer, and 0.1 µg of template DNA.
The following PCR cycling conditions (Techne Cyclogene thermal cycler)
were used: 94°C for 5 min; 35 cycles consisting of 94°C for 45 s, 65°C for 30 s, and 72°C for 60 s; 72°C for 10 min;
and finally, cooling to 4°C. Maximum ramp rates were used throughout.
Each QC-PCR titration was performed by using six dilutions of standard
DNA (prepared as described below), which resulted in a series of
reaction mixtures that contained 10, 1, 0.1, 0.01, 0.001, and 0.0001 amol of pN
STD and pP
STD (equivalent to 6 × 106
to 60 copies of standard DNA template per reaction mixture). To each
reaction mixture we added a known volume of target DNA that was
extracted from 0.5 g of soil by the method of Berthelet et al.
(2). Each QC-PCR preparation contained 25 to 125 ng of DNA
based on spectrophotometric determination of absorbance at 260 nm. The
DNA extract volume, which included the aqueous phase added plus the
soil moisture, was recorded in order to obtain an accurate dilution
factor for subsequent calculation of the gene copy number per gram (dry
weight) in each soil. Standard and target amplicons generated during
the QC-PCR experiment were quantified by electrophoresing 10 µl of
each reaction mixture through a 1% agarose gel in Tris-borate-EDTA
buffer. After electrophoresis, the DNA was stained for 3 h with
SYBR Gold (FMC Bioproducts, Rockland, Maine), and the gel was
photographed. The intensities of the target and standard amplicons were
then determined by processing images of scanned photographs with Scion
Image software (Scion Corp., Frederick, Md.). A regression analysis,
based on the amplicon intensities and sizes of target and standard DNAs
and the initial concentration of standard DNA, was used to calculate
the concentration of nahAc or phnAc genes present
in each soil DNA extract; this concentration was subsequently adjusted
to obtain a gene copy value on a soil dry weight basis. QC-PCR
titrations for the contaminated soil samples were replicated with
aliquots of each soil DNA extract; mean values and standard errors are reported.
Construction of standard templates.
Deletion derivatives of
the G7 nahAc and RP007 phnAc genes were
constructed and used as standards for QC-PCR. Klenow fragment-treated nahAc and phnAc amplicons were ligated into the
SmaI site of pUC18 to form pNTGT and pPTGT, and restriction
fragments situated between the primer binding sites were then removed
before religation of constructs following S1 nuclease treatment. Thus,
a 351-bp HpaI-NsiI deletion of the G7
nahAc amplicon was used to generate pN
STD, and a 324-bp
NsiI-ApaI deletion of the RP007 phnAc
amplicon was used to generate pP
STD. The construct pN
STD yielded
a 637-bp PCR product with primers nahAcfor and nahAcrev, and pP
STD
yielded a 665-bp PCR product with primers P8073 and P9047. Each primer set exhibited identical amplification kinetics with the specific target
and standard DNAs; therefore, an equimolar ratio of target and standard
DNAs was used to calculate the QC-PCR titration. This ratio was
determined by comparing the concentrations of the two PCR products in
aliquots taken from PCR over a number of cycles (data not shown).
Accurate standard solutions of pP
STD and pN
STD were prepared, and
equimolar amounts based on a molecular mass of 660 Da/bp
(15) were combined and diluted to obtain a stock preparation
which contained 20 amol of both standard templates per µl. Tenfold
dilutions of this mixture were used as standards in the QC-PCR
experiments. Mixing the phn and nah templates
ensured consistent dilution and did not interfere with subsequent PCR amplification.
Establishment of microcosms.
Enrichment for nahAc
and phnAc was evaluated in microcosms containing pristine
soil amended with different PAHs. The soil was collected from a native
New Zealand forest. Ten-gram samples of soil and 1-ml portions of basal
salts [4 g of Na2HPO4 per liter, 2 g of
KH2PO4 per liter, 1 g of
(NH4)2SO4 per liter] were placed in 100-ml glass flasks. Preparations were subjected to the following four treatments before they were incubated in the dark at 20°C for 60 days: no additional carbon source (blank); naphthalene supplied as a
vapor from a vapor tube suspended above the soil; phenanthrene supplied
as a vapor (as routinely used in our laboratory [9, 10,
12]); and 50 mg of fluoranthene added directly to the soil.
Soil samples obtained from Siberia and Antarctica were also enriched in
microcosms by using naphthalene and phenanthrene as supplementary
carbon sources.
Sequencing of phnAc amplicons.
Amplicons of
phnAc derived from PAH- and petroleum-contaminated soils
were cloned into the SmaI site of pUC18 by using a SureClone ligation kit (Amersham Pharmacia Biotech Inc., Piscataway, N.J.). The
nucleotide sequences of selected amplification products were determined
in both orientations by using the universal primers and a PRISM Ready
Reaction DNA terminator cycle sequencing kit (Perkin-Elmer, Inc.,
Wellesley, Mass.). The Reaction mixtures were resolved by using an ABI
model 377 sequencer at the Waikato DNA Sequencing Facility, and the
sequences were analyzed by using Omiga 1.0 sequence analysis software
(Oxford Molecular Group Ltd., Oxford, United Kingdom).
 |
RESULTS AND DISCUSSION |
QC-PCR analysis of phnAc and nahAc from
contaminated soils.
The two contaminated New Zealand soils used in
this study were selected to represent high and low levels of PAH
contamination and are described in Table
1. Figure 1
shows representative photographs of QC-PCR titration of
phnAc and nahAc for the two soils (Fig. 1a), as
well as an example of a QC-PCR calibration curve for phnAc (Fig. 1b). The lower limit of the QC-PCR titration series was 0.0001 amol of standard template (approximately 60 copies), which was
equivalent to a detection limit of 2 × 105 copies of
a given gene per gram (dry weight) of soil. By using PCR primers that
were specific for a gene that encodes the iron sulfur protein large
(
) subunit of the PAH dioxygenase from the recently described
phn type of catabolic operon (10), we found that
cells harboring phn genes are not as rare as microbiological culture techniques might lead us to believe (10, 12).

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|
FIG. 1.
(a) QC-PCR of phnAc and nahAc
amplified from two contaminated soils. Soil A was derived from a former
town gas-generating site and contained high levels of PAHs. Soil
B was contaminated with petrochemicals and contained low levels
of PAHs. The upper band in each QC-PCR titration series contained the
target amplicon (unknown); the lower band consisted of amplicons
derived from the standard DNA. The amounts of standard DNA used (10 to
0.0001 amol) are indicated above the lanes. (b) Representative plot of
the ratio of target DNA intensity to standard DNA intensity plotted
against the initial concentration of standard DNA on logarithmic
scales. Band intensities were quantified by processing images of
Polaroid photographs of SYBR Gold-stained gels. The plot is not a
representation of panel a.
|
|
Replicate QC-PCR experiments (
n = 3) revealed that the
PAH-contaminated soil (soil A) contained 1.0 × 10
8 ± 0.3 × 10
8 copies of
phnAc per g of soil and 2.0 × 10
8 ± 0.9 × 10
8 copies of
nahAc per g of soil,
while the petroleum-contaminated
soil (soil B) contained 6.2 × 10
7 ± 1.3 × 10
7 copies of
phnAc per g of soil and 1.3 × 10
6 ± 0.9 × 10
6 copies of
nahAc per g of soil.
The numbers of copies of both
phnAc and
nahAc in
these contaminated soils were significantly
greater than the numbers of
copies in a pristine soil, which did
not contain detectable levels of
either gene (i.e., less than
2 × 10
5 copies per g).
The greater numbers of copies in the PAH-contaminated
soil than in the
petroleum-contaminated soil may reflect higher
naphthalene and
phenanthrene levels. Similar observations have
been made in previous
studies of the molecular ecology of
nah-like
genotypes in
PAH-contaminated soil (
16,
17). For the two contaminated
New
Zealand soils that we analyzed, the
phn and
nah-like genotypes
were present (assuming that there was one
copy of each gene per
cell) at levels that were greater than or equal
to the total numbers
of heterotrophs determined for the same soil
samples by culture
techniques (Table
1). Although the presence of
phnAc or
nahAc genes in a soil does not a priori
indicate that PAH-degrading
activity is present, our data revealed
elevated levels of the
phnAc and
nahAc genes in
soils in which it can reasonably be expected
that selection pressures
exerted by PAHs would enrich populations
able to degrade these
substrates.
Diversity of phnAc amplicons.
Previous studies
have shown that primers based on nah-like genes target a
group of sequences that exhibit more than 75% sequence homology and
form the phylogenetically distinct nah-like and
dnt-ntd groups (7, 12, 18). We sequenced both
strands of phnAc amplicons to determine the diversity of
homologous sequences targeted in soil DNA by primers P8073 and P9047.
The phn primers P8073 and P9047 amplified a very highly
conserved group of phnAc genes that exhibit more than 98%
sequence identity with the RP007 phnAc sequence. In this
study two sequences derived from petroleum-contaminated soil and one
sequence derived from PAH-contaminated soil were identical to the RP007
phnAc sequence, while an additional three sequences derived
from PAH-contaminated soil samples differed at only 2, 12, and 15 nucleotide positions. Similarly high levels of sequence conservation
were also found for six phnAc amplicons derived from two
other contaminated soils in a previous study, which also exhibited more
than 98% nucleotide homology with the RP007 phnAc sequence
(9). Sequence errors due to Taq DNA polymerase or
PCR amplicon contamination during cloning were statistically improbable
since the majority of base substitutions (24 of 29 substitutions;
>80%) resulted in synonymous (silent) substitutions. In addition, the
Taq DNA polymerase error rate, <0.05%, as determined by
sequencing two cloned phnAc amplicons derived from the
Burkholderia sp. wild-type strain RP007, was also too low to
account for these substitutions.
The highly conserved nature of the
phnAc amplicons obtained
with primers P8073 and P9047 may be an artifact of the high degree
of
primer specificity and stringent amplification conditions.
We have not
determined whether this observation is a true reflection
of the
diversity of
phn genes in the environment, which would
require the use of degenerate primers allied with less stringent
annealing conditions during PCR amplification. What is certain
is that
the original isolation of the
phn genes was fortuitous
since
bacteria harboring this genotype appear to be very difficult
to isolate
yet are ubiquitously distributed and may be present
in relatively high
numbers in PAH-contaminated
soils.
Distribution of phn genes.
Having determined that
phn genes were enriched in PAH-contaminated New Zealand
soils, we were also interested in evaluating whether the phn
genes are ubiquitous. Noncontaminated (pristine) soils obtained from
central Siberia (61°N, 89°E), Ross Island in the Antarctic (77°S,
166°E), and a native New Zealand forest (38°S, 175°E) were used
to assess the ubiquity of the phn genes in different
environments. Enrichment of the PAH-degrading populations in these
uncontaminated soils was necessary before we screened for the
phnAc genotype since the levels of analogues of
phnAc were initially below the limits of detection (i.e.,
less than 2 × 105 copies per g of soil) in these
soils. Soil microcosms were therefore established, and PAH-degrading
bacteria were enriched by using the low-molecular-weight PAHs
naphthalene and phenanthrene. The broad geographic distribution of the
phn genotype was confirmed when phnAc was
amplified from a central Siberian soil, from an Antarctic soil from
Ross Island, and from various New Zealand soils. The phn
genes were enriched in soil microcosms that were incubated for 1 week
in the presence of either naphthalene or phenanthrene, and after
enrichment the levels were above our limit of detection (2 × 105 copies of phnAc per g [dry weight] of
soil). Again it is particularly interesting that we detected
phn genes in soils from areas as far afield as Siberia,
Antarctica, and New Zealand and yet to our knowledge only one confirmed
strain with a phn genotype has been isolated from the
environment (9, 10, 12).
In situ specificity of the phn genes.
We also
examined the effects of the selection pressures exerted by different
low-molecular-weight PAHs on the phnAc and nahAc genotypes in an uncontaminated New Zealand soil. The levels of both
nahAc and phnAc were initially below the
detection limit (2 × 106 copies of phnAc
per g [dry weight] of soil) in subsamples of this soil. This
detection limit was higher than the detection limit for the
contaminated soils due to the higher humic content of this soil, which
required greater dilution of target DNA to a level which did not
inhibit PCR amplification. As expected, selection pressures within the
microcosms enriched for a PAH-degrading phenotype (8, 13)
but interestingly favored the phn genotype and not the
nah-like genotype, which we were not able to detect in any
microcosm (Table 2). These findings imply
that the nah-like genotype is not always ecologically
dominant and confirm that it is not always realistic to represent PAH
degradation by one genotype, as this genotype may not be present at a
detectable (or significant) level in all environments (1,
12).
Enrichment of
phnAc from uncontaminated soils appeared to be
greatest with naphthalene (nine times greater than enrichment
in the
control microcosm), which has the greatest volatility,
solubility, and,
hence, availability of the three PAH substrates
used for enrichment.
Since previous studies have shown that the
phn genes are
induced by both naphthalene and phenanthrene (
10),
it is
likely that phenanthrene also enriches for the
phn genotype.
Although the QC-PCR data for phenanthrene enrichment of
phnAc may not be conclusive in the New Zealand soil
microcosm (the level
was only two to three times the level observed in
the control
microcosm), we have demonstrated that
phnAc was
enriched in both
Siberian and Antarctic soils when they were exposed to
phenanthrene.
It remains to be established whether fluoranthene is
degraded
in situ by
phn gene products or is able to induce
transcription
of the
phn genes, since the evidence for
enrichment in response
to fluoranthene was not conclusive. Whether the
increase observed
in the control microcosm was real or due to
variability and biases
inherent in using small soil samples was not
determined. A real
increase may have occurred in response to natural
soil substrates
as a consequence of moisture, temperature, and
inorganic nutrient
level adjustments made while the control microcosm
was being
established.
 |
ACKNOWLEDGMENTS |
This work was supported by grant C09810 from the Foundation for
Research Science and Technology, New Zealand.
We thank R. Fraser and D. W. F. Hunter for technical
assistance and colleagues at Landcare Research for providing soil samples.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Landcare
Research, Private Bag 3127, Hamilton, New Zealand. Phone: (64) 7 858 3700. Fax: (64) 7 858 4964. E-mail:
lloyd-jonesg{at}landcare.cri.nz.
Present address: Department for Cell and Molecular Biology, Umeå
University, Umeå, Sweden.
 |
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Applied and Environmental Microbiology, May 2000, p. 1814-1817, Vol. 66, No. 5
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
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