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. 2002 Aug 28;2:23. doi: 10.1186/1471-2180-2-23

Diversity and abundance of bacteria in an underground oil-storage cavity

Kazuya Watanabe 1,✉, Yumiko Kodama 1, Nobuo Kaku 1
PMCID: PMC126219  PMID: 12197947

Abstract

Background

Microorganisms inhabiting subterranean oil fields have recently attracted much attention. Since intact groundwater can easily be obtained from the bottom of underground oil-storage cavities without contamination by surface water, studies on such oil-storage cavities are expected to provide valuable information to understand microbial ecology of subterranean oil fields.

Results

DNA was extracted from the groundwater obtained from an oil-storage cavity situated at Kuji in Iwate, Japan, and 16S rRNA gene (16S rDNA) fragments were amplified by PCR using combinations of universal and Bacteria-specific primers. The sequence analysis of 154 clones produced 31 different bacterial sequence types (a unique clone or group of clones with sequence similarity of > 98). Major sequence types were related to Desulfotomaculum, Acetobacterium, Desulfovibrio, Desulfobacula, Zoogloea and Thiomicrospira denitrificans. The abundance in the groundwater of bacterial populations represented by these major sequence types was assessed by quantitative competitive PCR using specific primers, showing that five rDNA types except for that related to Desulfobacula shared significant proportions (more than 1%) of the total bacterial rDNA.

Conclusions

Bacteria inhabiting the oil-storage cavity were unexpectedly diverse. A phylogenetic affiliation of cloned 16S rDNA sequences suggests that bacteria exhibiting different types of energy metabolism coexist in the cavity.

Background

Underground cavities have been used for long-term storage of crude oil in several countries, and one of such facilities is situated at Kuji in Iwate, Japan. These cavities have been constructed in groundwater-rich rocky strata, where high groundwater pressure confines the stored oil in the cavities [1]. Consequently, groundwater migrates into and accumulates at the bottom of a cavity (cavity groundwater), and this cavity groundwater is discharged to maintain the oil storage capacity of the cavity (this system has been detailed in our previous study [1]). Our previous study [1] has also shown active growth of microorganisms in groundwater accumulating at the bottom of the cavities; the total count of microorganisms in the cavity groundwater was constantly more than 106 cells per ml (densities 100 times higher than those in groundwater around the cavities). This habitat can be characterized by (i) immediate contact with a large quantity of crude oil and (ii) an excess of electron donors for microbial growth (i.e., hydrocarbons) but a shortage of electron acceptors [1]. These characteristics may be similar to those of microbial habitats associated with subterranean oil reservoirs, which have recently attracted much attention in microbiology [2-6]. Since groundwater can easily be obtained from the bottom of the oil-storage cavities using standing sampling facilities without its contamination by surface water [1], studies on the oil-storage cavity are considered to provide valuable information to understand the microbial ecology of subterranean oil fields.

Our previous study applied rRNA approaches, namely cloning and sequencing of 16S rRNA gene fragments, denaturing gradient gel electrophoresis and fluorescent in situ hybridization (FISH), to analyze bacterial populations that occurred in the cavity groundwater obtained at Kuji [1]. As a result, a group of bacteria (called cluster-1 bacteria) affiliated with the Thiovulum subgroup in the ε subclass of the class Proteobacteria was consistently detected as a major population. Quantitative comparison of the results of these approaches, however, revealed a large bias associated with the cloning and sequencing approach; it was thus considered that the bacterial biodiversity has not sufficiently been assessed yet.

The present study was conducted to obtain a more reliable view on the bacterial biodiversity in the Kuji cavity groundwater. For this purpose, this study employed widely used universal primers [7] and a recently-modified Bacteria-specific primer [8] for PCR amplification of 16S rRNA gene (16S rDNA) fragments from the cavity groundwater, followed by cloning and sequencing. In addition, in order to quantitatively assess results of the cloning approach, competitive PCR (cPCR) assays were developed for some of abundantly obtained 16S rDNA types that were considered important for anaerobic petroleum degradation.

Results

FISH

In order to examine the abundance in the cavity groundwater of microorganisms affiliated with the Bacteria, FISH using probe EUB338 (Table 1) was carried out. The result was compared with that of FISH using an Archaea-specific probe, ARCH915 (Table 1). In the groundwater sample obtained in 1999, EUB338-labeled cells represented 53.5% ± 3.5% (mean ± standard deviation) of the DAPI-stained cells, while ARCH915-labeled cells represented 8.4% ± 1.8%. The FISH results for the cavity groundwater obtained in 2001 were almost the same. The result indicates that microorganisms affiliated with the Bacteria are the major constituents in the cavity groundwater.

Table 1.

Primers and probes used in this study.

Primer and probe Sequence Position (5' to 3')a Specificity Reference
EUB338 5'-GCTGCCTCCCGTAGGAGT-3' 355 to 338 Bacteria [9]
ARCH915 5'-GTGCTCCCCCGCCAATTCCT-3' 934 to 915 Archaea [10]
I-341f 5'-CCTACGGGIGGCIGCA-3' 341 to 356 Bacteria [8]
U515f 5'-GTGYCAGCMGCCGCGGTAA-3' 515 to 533 Universal [7]
U1492r 5'-GGTTACCTTGTTACGACTT-3' 1510 to 1492 Universal [7]
B341f 5'-CCTACGGGAGGCAGCAG-3' 341 to 357 Bacteria [11]
U533r 5'-TTACCGCGGCKGCTGRCAC-3' 533 to 515 Bacteria [11]
B968f 5'-AACGCGAAGAACCTTAC-3' 968 to 984 Bacteria [12]
DV387f 5'-CCTGACGCAGCGACG-3' 387 to 401 δ-Proteobacteria [13]
DV701r 5'-ACGGATTTCACTCCTACACC-3' 701 to 682 Desulfovibrio [14]
EP710r 5'-CAGTATCATCCCAGCAGA-3' 710 to 693 Cluster-1 bacteria [1]
DT1041r 5'-CACCCGAIGGTGAAAACGTAC-3' 1041 to 1021 Part of Desulfotomaculum This study
AB1173r 5'-GTGTTATCCACGGCAGTCTGCT-3' 1173 to 1152 Acetobacterium This study
AZ665r 5'-CTGCCGTACTCTAGTCATAC-3' 665 to 646 Parts of Azoarcus and Zoogloea This studyb
DB1286r 5'-AGGATTGGCTCCCCCTCACA-3' 1286 to 1267 Part of Desulfobacula This study
T7W 5'-TAATACGACTCACTATAGGGC-3' pGEM-T vector [1]
SP6W 5'-ATTTAGGTGACACTATAGAATACTC-3' pGEM-T vector [1]
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aCorresponding to the numbering in the sequence of the 16S rRNA gene of E. coli. bThis primer is a modified form of probe ZRA [38].

Analyses of cloned 16S rDNA fragments

The 16S rDNA fragments amplified by PCR from groundwater obtained in 1999 were cloned into E. coli, and two libraries of clones, namely 341/1492 and 515/1492 (designated according to the primers used, see Table 1), were constructed. Nucleotide sequences of a total of 154 clones were determined, which included 81 clones from library 341/1492 and 73 clones from 515/1492 (Table 2). Results of the sequence analysis are summarized in Table 2. As shown in this table, 31 different sequence types (a unique clones or group of clones with sequence similarity of > 0.98) affiliated with the Bacteria were obtained. The database search (Table 2) and phylogenetic analysis (Fig. 1) identified the phylogenetic positions of these sequence types. The sequence types containing more than several clones were related to Desulfotomaculum, Acetobacterium, Desulfovibrio, Desulfobacula, Zoogloea and Thiomicrospira denitrificans (this sequence type was affiliated with the cluster-1 bacteria [1]). Some sequence types showed homology to 16S rDNA clones obtained from contaminated groundwater and anaerobic consortia degrading petroleum constituents (Table 2).

Table 2.

16S rDNA sequence types obtained in this study.

Sequence type No of clones in each librarya,b Putative division Database match (> 90% identity)
341/1492 515/1492
KB20 2 (2.4) 0 (0) Actinobacteria No match
KB11 2 (2.4) 0 (0) Low-G+C gram positive 96% Syntrophomonas sp. MGB-C1 (AB021306)
KB32 1 (1.2) 0 (0) Low-G+C gram positive 91% Hydrocarbon-contaminated groundwater clone (AF050587)
KU26 1 (1.2) 24 (32.9) Low-G+C gram positive 90% Hydrocarbon-contaminated groundwater clone (AF050587)
90% Desulfotomaculum thermobenzoicum DSM 6193 (AJ294430)
KB13 17 (21.0) 2 (2.7) Low-G+C gram positive 94% Hydrocarbon-contaminated groundwater clone (AF050587)
91% Toluene-degrading methanogenic consortium clone Eub 1 (AF423181)
91% Desulfotomaculum thermobenzoicum DSM 6193 (AJ294430)
KU25 0 (0) 1 (1.4) Low-G+C gram positive 97% Acetobacterium paludosum DSM 8237 (X96958)
KU21 0 (0) 14 (19.2) Low-G+C gram positive 99% Groundwater clone Aspo4 (X95232)
99% Acetobacterium malicum DSM 4132 (X96957)
KU8 0 (0) 1 (1.4) Low-G+C gram positive No match
KB35 1 (1.2) 0 (0) CFB group 97% Marine clone agg32 (L10944)
KU30 0 (0) 1 (1.4) CFB group 90% Benzene mineralizing consortium clone SB-5 (AF029041)
KB43 2 (2.4) 0 (0) Spirochete-likec 94% Soil clone PBS-18 (AJ390485)
KU13 0 (0) 1 (1.4) Spirochete-likec No match
KU34 1 (1.2) 9 (12.3) β-Proteobacteria 96% Zoogloea ramigera ATCC 19544 (X74913)
KB17 1 (1.2) 0 (0) β-Proteobacteria 96% Hydrogenophaga palleronii DSM 63 (AF019073)
KB38 1 (1.2) 0 (0) β-Proteobacteria 97% Acidovorax defluvii BSB411 (Y18616)
KB1 11 (13.6) 1 (1.4) δ-Proteobacteria 98% Toluene-degrading methanogenic consortium clone Eub 5 (AF423185)
96% Desulfovibrio aminophilus ALA-3 (AF067964)
KB33 1 (1.2) 0 (0) δ-Proteobacteria 99% Desulfovibrio sp. Mlhm (AF193026)
KB47 8 (9.9) 0 (0) δ-Proteobacteria 91% Desulfovibrio sp. DR14 (Y17756)
KU12 0 (0) 2 (2.7) δ-Proteobacteria 97% Geobacter chapelleii 172 (U41561)
KU32 0 (0) 1 (1.4) δ-Proteobacteria 96% Chlorobenzene-contaminated groundwater clone GOUTB20 (AY050605)
KB14 6 (7.4) 0 (0) δ-Proteobacteria 94% Desulfobacula toluolica Tol2 (X70953)
KB16 1 (1.2) 0 (0) ε-Proteobacteria No match
KB36 2 (2.4) 0 (0) ε-Proteobacteria 99% Kuji groundwater clone 1070 (AB030590)
KB8 1 (1.2) 1 (1.4) ε-Proteobacteria 99% Kuji cluster-1 bacteria clone 1023 (AB030608)
KB2 7 (8.6) 2 (2.7) ε-Proteobacteria 99% Kuji cluster-1 bacteria clone 1033 (AB030608)
KB21 1 (1.4) 0 (0) ε-Proteobacteria 99% Kuji groundwater clone 1014 (AB030587)
99% Geospirillium sp. KoFum (Y18254)
KB49 1 (1.4) 0 (0) ε-Proteobacteria 99% Kuji groundwater clone 1065 (AB030598)
94% Arcobacter cryaerophilus CCUG 17801 (L14624)
KB19 2 (2.4) 0 (0) Chlamydia group No match
KB4 1 (1.2) 0 (0) Nitrospira group 94% Chlorobenzene-contaminated groundwater clone GOUTA19 (AY050588)
KB40 2 (2.4) 0 (0) Green nonsulfur bacteria 98% Hydrocarbon-contaminated groundwater clone WCHB1-44 (AF050565)
KB44 1 (1.2) 0 (0) Green nonsulfur bacteria 99% Trichlorobenzene-transforming consortium clone SJA-117 (AJ009488)
97% Toluene-degrading methanogenic consortium bacterium Eub 4 (AF423184)
Archaea 0 (0) 5 (6.8)
Chimera 1 (1.2) 0 (0)
Total 81 (100) 73 (100)
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aAccording to Hugenholtz et al. [22]. bA percent to the total clone number is presented in a parenthesis. cA lineage recently proposed by Derakshani et al. [23].

Figure 1.

Figure 1

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Neighbor-joining tree for rDNA sequences types. Sequences corresponding to nucleotide positions 515 to 1492 of the E. coli sequence were used for calculations. Sulfolobus acidocaldarius is used as the outgroup. Accession numbers of the sequences retrieved from the databases are indicated in parentheses. The numbers at the branch nodes are bootstrap values (per 100 trials); only values greater than 50 are shown. The scale bar indicates 0.044 substitution per site.

Quantification of rDNA copies by competitive PCR

It has been suggested that the PCR-amplification and cloning procedures may cause biases towards some specific 16S rDNA types [1,15]. In order to examine the abundance of bacteria represented by the major sequence types (those related to Desulfotomaculum, Acetobacterium, Desulfovibrio, Desulfobacula, Zoogloea and Thiomicrospira denitrificans), competitive PCR (cPCR) assays using specific primers were developed (Table 3). Fig. 2a shows that the PCR assays successfully amplified the target bands from the cavity groundwater. Results of cPCR for the groundwater obtained in 1999 and 2001 are shown in Fig. 2b. In the two groundwater samples, rDNA copies of the cluster-1 bacteria were most abundant, and those related to Desulfotomaculum, Acetobacterium, Desulfovibrio and Zoogloea also shared significant proportions (more than 1%) of the total bacterial rDNA copies.

Table 3.

Summary of cPCR assay.

cPCR type Primer used Annealing Tm (°C) Length of DNA fragment (bp) Specificity
Taget Competitor Sequence type Phylogenetic group
AB U515f and AB1173r 60 658 431 KU21, KU25 Acetobacterium
AZ B341f and AZ665r 55 324 437 KU34 Parts of Azoarcus and Zoogloea
BC B341f and U533r 55 170–210 336 All Bacteria
DB B968f and DB1286r 55 318 437 KB14 Part of Desulfobacula
DT U515f and DT1047r 60 526 340 KB13, KB32, KU26 Part of Desulfotomaculum
DV DV387f and DV701r 55 314 415 KB1, KB33, KB38 Desulfovibrio
EP B341f and EP710r 55 369 465 KB2, KB8 Cluster-1 bacteria
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Figure 2.

Figure 2

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cPCR assays for quantifying rDNA copies of major sequence types. The 6 cPCR systems used, namely AB, AZ, DB, DT, DV and EP, are explained in Table 3. (A) Target fragments amplified by PCR from the groundwater DNA (obtained in 1999) and competitor fragments. Lane 1, 50–2500 molecular size marker (FMC corp.); lanes 2, 4, 6, 8, 10, 12 and 14, target fragments; lanes 3, 5, 7, 9, 11, 13 and 15; competitor fragments. Lanes 2 and 3, DV; lanes 4 and 5, DB; lanes 6 and 7, AZ; lanes 8 and 9, EP; lanes 10 and 11, AB; lanes 12 and 13, DT; lanes 14 and 15, BC. (B) Rations of specific rDNA copies to the total bacterial rDNA copies (determined by the BC system in Table 3) in DNA extracted from the cavity groundwater. The total bacterial counts estimated by FISH were approximately 3 × 106 cells ml-1. The mean of three determinations is shown, and an error bar indicates a standard deviation.

Discussion

The present study used the two combinations of PCR primers for amplifying 16S rDNA fragments from the cavity groundwater. The sequence analysis of the amplified fragments suggests that the bacterial diversity in the cavity groundwater is much larger than the diversity found in our previous study [1]. The present study abundantly detected the sequence types related to Desulfotomaculum, Acetobacterium, Desulfovibrio, Desulfobacula, Zoogloea and Thiomicrospira denitificans, while major 16S rDNA sequences obtained in our previous study were solely affiliated with the ε-Proteobacteria. This comparison clearly indicates that methods employed in the molecular ecological approaches largely affect the results obtained. Differences in the methods employed in these two studies included primers used for PCR amplification of 16S rDNA fragments from the groundwater DNA and selection of E. coli clones harboring groundwater 16S rDNA fragments. The PCR primers used in our previous study were two Bacteria-specific primers (called 8f and 1546r [1]). We assume that organisms undetected in our previous study have 16S rDNA sequences that include mismatches to these primers, since this study did not determine sequences of the 5'- and 3'-end regions of 16S rDNA where 8f and 1546r exist. In addition to the primer selection, different from our previous study [1], the present study did not employ the β-galactosidase colony screening when selecting E. coli clones, because it has been reported that the vector containing a DNA fragment up to 2 kb in-frame produces a blue colony. These two modifications may have circumvented the bias toward the ε-Proteobacteria, which occurred in our previous study [1].

For estimating the abundance of bacterial populations represented by the major sequence types, this study employed cPCR assays. We did not use FISH, because a possible bias that causes the underestimation of slow-growing bacteria has been suggested [1]. Besides, in the present study, FISH with the Bacteria- and Archaea-specific probes detected only 60% in total of the DAPI-stained cells; in addition, a large portion of labeled cells exhibited weak signals. One possible explanation for this result would be that the probes used (e.g., EUB338) failed to detect some phylogenetic groups of microorganisms. The utility of cPCR for this purpose has been demonstrated in several studies [16,17], while attention should be paid to the variation in the number of 16S rDNA copies in a bacterial cell. For example, some Clostridium strains (affiliated with the low G+C gram positive bacteria) have been known to harbor more than 10 rDNA copies per cell [18,19], while the mean copy number in whole-genome-analyzed bacteria is 3.6 [20]. We assume that cPCR may have overestimated the Acetobacterium rDNA copies, since Acetobacterium belongs to the Clostridiaceae. In contrast, rDNA copy numbers per cell of bacteria related to the other major sequence types were not so different from the mean value for all bacteria [20]. We therefore consider that the results of cPCR reflected the abundance in the cavity groundwater of the cluster-1 bacteria and those related to Desulfotomaculum, Desulfovibrio and Zoogloea. Comparison of the cloning and cPCR results indicated that relative abundances determined by these two methods were inconsistent with each other in several cases (Table 2 and Figure 2). Furthermore, clones obtained in abundance in one library were minorities in another library in many cases (Table 2). These results suggest that the rDNA cloning approach employed in this study also included some biases.

Environmental rDNA sequencees have been used to infer some properties of the organisms that they represent [1,7,21], although this type of analysis is reliable only if some common properties can be recognized for phylogenetically related organisms. In the present study, we assume that the organism represented by sequence types KU21 and KU25 are acetogens [22], and those represented by KB1, KB14, KB33 and KB47 are likely sulfate-reducing bacteria [23]. KU34 is closely related to the genus Zoogloea that has been known to grow by denitrification under anaerobic conditions [24]. The Zoogloea belong to the Rhodocyclus group in the β subclass of the class Proteobacteria, which also includes the genera Rhodocyclus and Azoarcus[25]. Since organisms in these genera can commonly perform denitrification, organisms corresponding to clone KU34 are assumed to be capable of denitirfication. Sequence types KU26 and KB13 are related to the genus Desulfotomaculum that belongs to the Syntrophomonas/Thermoanaerobacter group in the low G+C gram-positive bacteria [25]. Typical members of this group are sulfate-reducing bacteria represented by Desulfotomaculum spp. [26], fermentative bacteria represented by Sporotomaculum hydroxybenzoicum[27] and acid-oxidizing syntrophs represented by Syntrophomonas spp. [28]. It is likely that organisms represented by KU26 and KB13 were engaged in some steps in organic compound decomposition. Similar types of bacteria, including δ-Proteobacteria, ε-Proteobacteria and low G+C gram-positive bacteria, have been detected by rDNA cloning analyses of mesophilic oil reservoirs in Canada [3], while β-Proteobacteria were not detected from there. We thus assume that understanding physiology of organisms represented by clone KU34 would provide valuable information regarding differences of ecosystem functions in these two subsurface oil fields.

We have recently isolated bacterial strains that belonged to the cluster-1 bacteria [Kodama, Y. and Watanabe, K. Unpublished results]. It has been found that these strains are capable of anaerobic chemolithotrophic growth by oxidizing reduced sulfur species (sulfide, elemental sulfur and thiosulfate) coupled to nitrate reduction. This finding suggests that this group of bacteria mainly consumed nitrate that was supplied by groundwater flowing into the oil-storage cavities.

Conclusions

The present study unveiled the large diversity of bacteria in the cavity groundwater. The phylogenetic affiliation of cloned 16S rDNA sequences suggests that bacteria exhibiting different types of energy metabolisms coexist as major proportions. This finding is considered interesting, because the chemical analyses of the groundwater have suggested that nitrate reduction is the major electron accepting process [1]. In particular, although sulfate was not significantly consumed [1] and sulfide was always undetectable (below 0.01 mg per liter [unpublished data]) in the cavity groundwater pool, the results of the present study indicate that sulfate-reducing bacteria were present at significant levels. One possible explanation for these findings would be the existence of a sulfur cycle in the cavity groundwater that involves sulfate reducers and anaerobic sulfur oxidizers that regenerated sulfate from sulfide. We assume that similar sulfur cycles may operate in subterranean oil fields, since sulfate-reducing bacteria have been isolated from subterranean oil fields whose formation water contained very low concentrations of sulfate [29,30]. In order to elucidate ecological niches and interactions among these bacteria, their isolation and physiological analyses in axenic cultures are needed. These studies will draw novel insights into the ecological interactions among microorganisms in subterranean oil fields.

Methods

Groundwater samples

The cavity groundwater was obtained in March 1999 and July 2001 from the TK101 underground crude oil storage cavity situated at Kuji in Iwate, Japan. Characteristics of the groundwater were reported previously [1].

Fluorescent in situ hybridization (FISH)

Rhodamine-labeled oligonucleotide probes, EUB338 and ARCH915 (Table 3) were used for fluorescence in situ hybridization (FISH). Microbial cells in groundwater were collected by centrifugation at 10,000 × g for 10 min, suspended in phosphate-buffered saline [31], and fixed in a 4% (wt/vol) paraformaldehyde solution for 5 h at 0°C. The cells were attached to gelatin-coated slides [31] and dehydrated by sequential washes in 50, 80, and 98% (vol/vol) ethanol (3 min each). Subsequently, 8 μl of hybridization solution (0.9 M NaCl, 20 mM Tris-HCl [pH 7.2], 0.01% [wt/vol] sodium dodecyl sulfate and formamide at a concentration [wt/vol] of 30% for EUB338 or 35% for ARCH915) containing 50 ng of probe was added to each hybridization well. It was incubated at 40°C (EUB338) or 46°C (ARCH915) for 3 h in a humid chamber. Slides were washed in the hybridization solution at 42°C (EUB338) or 48°C (ARCH915) for 20 min before all cells on the slide were stained with 4',6'-diamidino-2-phenylindole (DAPI) [1]. More than 1,000 DAPI-stained cells were counted to determine the ratio of probe-labeled cells to DAPI-stained cells. Slides were prepared in triplicate.

PCR amplification, cloning and sequencing of 16S rDNA fragments

DNA was extracted from the groundwater as described previously [1]. PCR amplification of 16S rDNA fragments was performed using either I-341f or 515f as a forward primer and 1492r as a reverse primer (Table 1). A PCR solution (50 μl) contained 1.25 U of Taq DNA polymerase (Amplitaq Gold; Applied Biosystems), 10 mM Tris-HCl (pH 8.3), 50 mM KCl, 1.5 mM MgCl2, 0.001% (wt/vol) gelatin, each deoxynucleoside triphosphate at a concentration of 200 μM, 50 pmol of each primer and 10 ng of DNA. The amplification conditions were as follows: 10 min of activation of the polymerase at 94°C, followed by 30 cycles consisting of 1 min at 94°C, 1 min at 50°C, and 2 min at 72°C, and finally 10 min of extension at 72°C. Amplified fragments were purified by electrophoresis, ligated into the pGEM-T vector (Promega) and cloned into Escherichia coli as described previously [1]. Vector-harboring clones were selected on Luria-Bertani plates [32] supplemented with ampicillin (50 μg ml-1). PCR-amplified 16S rDNA fragments were recovered from colonies by PCR using primers T7W and SP6W (the primers targeted the pGEM-T vector sequences flanking the insertion, see Table 1) as described previously [1]. Clones containing appropriate sizes of the insertion were selected by the electrophoresis analysis, and their nucleotide sequences were determined as described previously [1].

Sequence analysis

Database searches with 16S rDNA sequences were conducted by using the BLAST program [33] and the GenBank database. The profile alignment technique of ClustalW version 1.7 [34] was used to align the sequences, and the alignments were refined by visual inspection; secondary structures were considered for the refinement analysis [35]. A phylogenetic tree was constructed by the neighbor-joining method [36]using the njplot software in ClustalW, version 1.7. Nucleotide positions at which any sequence had an ambiguous base were not included in the phylogenetic calculations. Checks for chimeric sequences were conducted by using the chimera check in the RDP database [25].

cPCR

The primers used for cPCR (Table 1) were selected or designed by comparing the 16S rDNA sequences obtained in this study and those stored in the RDP database [25]. The specificity of the primers thus obtained was checked by using the probe match program in the RDP database [25]. Competitor fragments were produced by using a competitive DNA construction kit (Takara Shuzo). The composition of PCR solution was described above except for the competitor fragment being added at a known copy number. The PCR conditions used were as follows: 10 min of activation of the polymerase at 94°C, followed by 30 cycles consisting of 1 min at 94°C, 1 min at the annealing temperatures described Table 3, and 2 min at 72°C, and finally 10 min of extension at 72°C. Two microliters of the PCR product was electrophoresed through a 1.5% (wt/vol) agarose gel with TBE buffer, and the gel was photographed after it was stained with SYBR Gold (FMC Bioproducts). The band intensities of the target and competitor fragments were quantified by using the Multianalyst software supplied with Gel Doc 2000 (Bio-rad). A copy number of the target 16S rDNA fragment was estimated by considering the band intensity, length of the fragment and copy number of the competitor as described by Lee et al. [37].

Nucleotide sequence accession numbers

The nucleotide sequence data reported in this paper have been deposited in the GSDB, DDBJ, EMBL, and NCBI nucleotide sequence databases under accession no. AB074931 to AB074961.

Authors' contributions

KW carried out cloning and sequencing of 16S rDNA fragments and subsequent phylogenetic analyses. YK carried out sampling of groundwater and FISH analyses. NK participated in the design and coordination of this study.

Acknowledgments

Acknowledgements

We thank Yoichi Matsumura (Japan Under-ground Oil Storage Co.) for help in the groundwater sampling and Ikuko Hiramatsu for technical assistance. This work was supported in part by the New Energy and Industrial Technology Development Organization (NEDO).

Contributor Information

Kazuya Watanabe, Email: kazuya.watanabe@mbio.jp.

Yumiko Kodama, Email: yumiko.kodama@mbio.jp.

Nobuo Kaku, Email: nobuo.kaku@mbio.jp.

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