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. 2013 Aug 1;2:369. doi: 10.1186/2193-1801-2-369

Bias problems in culture-independent analysis of environmental bacterial communities: a representative study on hydrocarbonoclastic bacteria

Husain Al-Awadhi 1, Narjis Dashti 1, Majida Khanafer 1, Dina Al-Mailem 1, Nidaa Ali 1, Samir Radwan 1,✉
PMCID: PMC3769543  PMID: 24040582

Abstract

Culture-dependent methods for bacterial community analysis are currently considered obsolete; therefore, molecular techniques are usually used instead. The results of the current study on hydrocarbonoclastic bacteria in various oily habitats in Kuwait showed however, that the bacterial identities varied dramatically according to the analytical approach used. For six desert and six seawater samples used in this study, the culture-independent and culture-dependent techniques each led to a unique bacterial composition. Problems related to the culture-dependent technique are well known. The results of the current study highlighted bias problems other than those already recorded in the literature for the molecular approaches. Thus, for example, in contrast to the culture-dependent technique, the primers used in the molecular approach preferentially amplified the 16S rDNAs of hydrocarbonoclastic bacteria in total genomic DNAs of all the studied environmental samples, and in addition, failed to reveal in any environmental sample members of the Actinobacteria. The primers used in the molecular approach also amplified certain “pure” 16S rDNAs, but failed to do so when these DNAs were in mixture. In view of these results, it is recommended that the two analytical approaches should be used simultaneously because their combined results would reflect the bacterial community composition more precisely than either of them can do alone.

Introduction

The end of the 19th century witnessed the development of the well known and long adopted culture-dependent approach which is used for the study of the structure of the bacterial communities in various environments. This approach drove advances in microbiology, in spite of its well known, serious limitations (Amann et al. 1995; Jannasch & Jones 1959), mainly related to the selectivity of the nutrient media and culture conditions which lead to favoring only a fraction of the inhabiting bacterial community. The major limitation of this classical technique is thus, that it dramatically underestimates the microbial numbers and composition in the samples under study. On the other hand, the major advantage of this approach over the modern molecular techniques lies in that it provides the researcher with the microbial “material” that can be used in further studies.

Within the past few decades, molecular approaches have been developed (Head et al. 1998; Jannasch & Jones 1959; Muyzer & Smalla 1998) and used as alternative methods, neglecting in most studies the culture-depedent techniques, which are considered by most modern microbiologists as “obsolete”. The molecular methods “provide a new insight into microbial diversity and allow a more rapid, high resolution description of microbial communities than that provided by the traditional approach of isolation of microorganisms” (Dahllöf et al. 2000). Molecular approaches which comprise among others the combination of DGGE fingerprinting with sequencing of 16S rDNA bands to identify the species present in the environmental samples (Fuhrman & Davies 1997; Nielsen et al. 1999; Rölleke et al. 1999), and correlating the banding patterns and band numbers on DGGE gels with environmental variables (El Fantroussi et al. 1999; Nübel et al. 1999; Sievert et al. 1999; van Hannen et al. 1999a; van Hannen et al. 1999b) also have their limitations. Serious artifacts (Polz & Cavanaugh 1998; Sipos et al. 2007) do arise viz preferential amplification of upcoming species, inadequate specificity of primers used for DNA amplification, production of single bands by multiple strains and others.

During two decades of research on microorganisms in pristine and oily Kuwaiti areas that were polluted via the greatest man-made oil-pollution catastrophy in association with the second Gulf War, 1990/1991 (Al-Awadhi et al. 2012), we consistently noticed that microbial identities determined by using culture-dependent methods for analysis were dramatically, sometimes completely different from those determined using molecular approaches. Here, we demonstrate this in a microbiological study on hydrocarbon-utilizing bacterial community structures in seawater and desert samples with over 20 years history of heavy oil-pollution. We concluded from the results that the simultaneous use of the traditional culture-dependent methods, along with the modern molecular techniques is a must for obtaining precise findings from such studies.

Materials and methods

Oily and pristine seawater and desert soil samples were collected from various sites (Figure 1) along the Arabian Gulf coast, and from the desert of Kuwait, and processed the same day. As the culture-dependent method, we adopted the traditional dilution-plate method using a mineral medium with oil-vapor as the sole source of carbon and energy (Al-Awadhi et al. 2012). Representative colonies of oil vapor-utilizing bacteria were isolated and purified, their total DNA’s were extracted, the 16S rRNA genes were amplified using the universal primer pair GM5F and 907R, the amplicons were sequenced and the sequences compared with the nearest GenBank sequences (method details are available in reference (Al-Awadhi et al. 2012).

Figure 1.

Figure 1

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Kuwait map showing the coastal water (CW) and desert soil (DS) sampling sites.

For the molecular analysis of the environmental samples, the total genomic DNAs in the latter were extracted using Rapid Water DNA Isolation Kit (MO-BIO, Carlsbad, CA) for seawater samples and Fast DNA Spin for Soil Kit (MP Biomedicals, LLC., France) for desert soil samples. The extracts were stored at −80°C until used. The 16S rRNA-genes in the purified extracts were amplified as described earlier (Al-Awadhi et al. 2012). The 16S rDNA amplicons were subjected to parallel DGGE using Dcode Universal Mutation Detection System (Bio-Rad, California, USA). The denaturant concentrations were 45–55% for seawater samples and 45-60% for desert soil samples. DGGE was processed with the constant voltage of 50 V at 60°C for 16 h. Gels were stained with SYBR Green (Invitrogen, USA) in 1× TAE buffer (1:100000) for 30 min, and examined using a Dark Reader transilluminator (Clare Chemical Research, CO, USA). The bands were transformed into binary matrix; the presence of bands was given the weight of (1) and their absence (0). The binary matrix produced was analyzed using cluster analysis and dendrograms were plotted. For identification of individual bands; gel bands were excised, stored in 50 μl molecular water (Sigma, UK) at 4°C overnight to elute the DNA, 1 μl of the eluted DNA was amplified using the above primers, sequenced and the sequences were compared with the sequences in the GenBank database.

Results

The results of the culture-dependent analysis of the oil-polluted seawater and desert soil samples for the structure of their hydrocarbon-utilizing bacterial communities have been published before (Al-Awadhi et al. 2012), and are mentioned here only for comparison with the results of the current molecular analysis. The same environmental samples were used the same sampling day for total DNA extraction; the extracts were stored at −80°C and used in the current study. Details of environmental conditions that were prevailing during sampling have been described elsewhere in details (Al-Awadhi et al. 2012).

The results of the DGGE analysis of partially amplified 16S rDNA of the studied samples are presented in Figures 2 and 3. For the purpose of comparison, we also co-analyzed nearby, visually pristine samples. The DGGE profiles of the various seawater samples (Figure 2) showed a high degree of similarity as far as the 16S rDNA band numbers and migration patterns are concerned. This similarity was also valid for the profiles of the same sample irrespective of whether it was pristine or oil-polluted. In contrast, the DGGE profiles of the desert soil samples (Figure 3) exhibited dramatic variations, also depending on whether the sample was pristine or oil-polluted.

Figure 2.

Figure 2

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DGGE of 16S rDNA amplicons in total DNA extracts from six pristine (P) and nearby six oil-polluted (O) seawater samples collected from the Arabian Gulf coast of Kuwait. (a) DGGE gel; in contrast to the cases of the “closed” desert samples (Figure 3), the DGGE bands of the “open” seawater samples were similar as far as the band numbers and patterns are concerned. The total numbers of the bands for all samples were not much higher than the total number of species recorded in each sample using culture-based analysis (Al-Awadhi et al. 2012). DNAs in individual bands were amplified, sequenced and the sequences were compared with those (cultured and uncultured) of the closest species in the GenBank (results in Table 1, which presents also information related to the sequencing). (b) Cluster analysis of DGGE-results using Euclidean distances.

Figure 3.

Figure 3

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DGGE of 16S rDNA amplicons in total DNA extracts from six pristine (P) and nearby six oil-polluted (O) soil samples collected from the Kuwaiti desert. (a) DGGE gel, the 16S rDNA band numbers and patterns varied, not only according to the sampling sites, but also to whether the sample was pristine or oil-polluted. The bands were further processed as described in the legend to Figure 1, and the results are summarized in Table 2. (b) Cluster analysis of DGGE-results using Euclidean distances.

The 16S rDNA bands in Figures 2 and 3 were amplified, sequenced and the sequences were compared with the nearest sequences in the GenBank database. Like it was the case in many of our (and other) earlier reports, we failed to sequence many of the bands excised from the DGGE-gel. The results of this analysis (Tables 1 and 2) revealed only very little similarity but dramatic differences in comparison with the results previously obtained by the culture-dependent method (Al-Awadhi et al. 2012).

Table 1.

Results of 16S rDNA sequencing of DGGE-bands of seawater samples in Figure 2

Band no. Total bases Phylum Nearest GenBank match Similarity (%) Bases compared Accession number
1 446 α-Proteobacteria Candidatus Pelagibacter ubique clone fosmid 01-003783 97 466/482 KC147468
2 444 Bacteroidetes Uncultured Bacteroidetes* bacterium clone CB22B12 97 461/477 KC147469
3 455 γ-Proteobacteria Alteromonas macleodii strain CAIM 891 96 494/513 KC147470
4 402 γ-Proteobacteria Alteromonas macleodii strain CAIM 891 93 464/499 KC147471
5 442 γ-Proteobacteria Thalassolituus oleivorans isolate SLHC162b 96 490/513 KC147472
6 450 α-Proteobacteria Phaeobacter caeruleus strain UDC410 98 468/477 KC147473
7 447 α-Proteobacteria Phaeobacter caeruleus strain UDC410 98 465/474 KC147474
8 455 γ-Proteobacteria Alteromonas macleodii strain SWDOH3 97 488/504 KC147475
9 470 γ-Proteobacteria Pseudoalteromonas phenolica 97 504/521 KC147476
10 438 α-Proteobacteria Thalassobius mediterraneus strain D6064 95 466/489 KC147477
11 438 γ-Proteobacteria Alteromonas macleodii strain D7081 94 487/517 KC147478
12 405 γ-Proteobacteria Alteromonas macleodii strain CAIM 891 94 452/481 KC147479
13 430 γ-Proteobacteria Marinobacterium marisflavum strain IMCC4074 94 482/515 KC147480
14 438 γ-Proteobacteria Marinobacterium marisflavum strain IMCC4074 96 485/506 KC147481
15 440 γ-Proteobacteria Uncultured gammaproteobacterium clone OTU29 95 477/501 KC147482
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*Hydrocarbon-utilizers (Scherr et al. 2012; Jiménez et al. 2007).

Table 2.

Results of 16S rDNA sequencing of DGGE-bands of desert soil samples in Figure 3

Band no. Total bases Phylum Nearest GenBank match Similarity (%) Bases compared Accession number
1 462 Flavobacteriia Salinimicrobium xinjiangense strain BH206 98 486/498 KC147483
2 493 Sphingobacteriia Sediminibacterium sp. nju-T3 99 494/495 KC147484
3 423 Sphingobacteriia Segetibacter koreensis strain Gsoil 664 95 476/502 KC147485
4 500 β-proteobacteria Ralstonia solanacearum strain in4ss52 100 500/500 KC147486
5 512 β-proteobacteria Ralstonia solanacearum strain in4ss52 100 512/512 KC147487
6 493 β-proteobacteria Naxibacter alkalitolerans strain A12 99 503/510 KC147488
7 519 γ-Proteobacteria Acinetobacter junii strain OVC9 100 519/519 KC147489
8 502 Synergistetes Synergistaceae* bacterium enrichment culture clone B6_95 100 502/502 KC147490
9 510 γ-Proteobacteria Acinetobacter junii strain OVC9 100 510/510 KC147491
10 469 γ-Proteobacteria Uncultured Chromatiales† bacterium isolate DGGE gel band B16 98 491/502 KC147492
11 468 γ-Proteobacteria Uncultured Chromatiales bacterium isolate DGGE gel band B16 98 490/501 KC147493
12 501 Synergistetes Synergistaceae bacterium enrichment culture clone B6_95 99 504/505 KC147494
13 462 Cytophagia Pontibacter akesuensis strain AKS 1 96 503/523 KC147495
14 447 Cytophagia Pontibacter xinjiangensis strain: NBRC 107674 95 498/523 KC147496
15 376 Firmicutes Bacillales bacterium Mi4 91 457/503 KC147497
16 421 Firmicutes Firmicutes bacterium enrichment culture clone BSK_60 95 465/487 KC147498
17 463 β-proteobacteria Curvibacter delicatus strain: NBRC 14919 97 500/518 KC147499
18 513 Firmicutes Planomicrobium glaciei strain L25 99 515/516 KC147500
19 494 Firmicutes Planomicrobium alkanoclasticum strain QT3+ 99 498/502 KC147501
20 498 Firmicutes Bacillus niacini strain GYR1 99 502/506 KC147502
21 480 β-proteobacteria Burkholderia oxyphila clone: pCR2.1::OX-01_rDNA#7 97 499/512 KC147503
22 425 Firmicutes Bacillus selenatarsenatis strain NBSL41 96 458/475 KC147504
23 501 Firmicutes Planomicrobium glaciei strain GDM825 99 502/503 KC147505
24 493 Firmicutes Planomicrobium okeanokoites 99 494/495 KC147506
25 475 Firmicutes Planomicrobium okeanokoites strain QL-25 98 486/494 KC147507
26 514 Firmicutes Planomicrobium glaciei strain L25 99 516/517 KC147508
27 427 Firmicutes Uncultured Geobacillus sp. clone SHBZ1548 94 484/513 KC147509
28 464 Firmicutes Bacillus selenatarsenatis strain NBSL41 95 496/521 KC147510
29 505 Firmicutes Bacillus selenatarsenatis strain NBSL41 99 506/507 KC147511
30 475 γ-Proteobacteria Halomonas xinjiangensis strain YIM 91125 97 502/518 KC147512
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*Hydrocarbon-utilizers (Scherr et al. 2012).

† Hydrocarbon-utilizers (Jiménez et al. 2007).

The slight similarity was expressed in the predominance of the phylum Gammaproteobacteria in seawater and its relative rarity in the terrestrial samples. Assuming that each DGGE band on the gel represents one single species, as commonly accepted, our results demonstrate that the species numbers determined by using the molecular analysis for all the environmental samples were more than the numbers determined by using the culture-dependent method, and the differences were more pronounced for the desert than the seawater samples (Table 3). For the seawater samples, the differences ranged between about 1 and 4 fold, whereas for the desert samples, they ranged between about 1 and 12 fold more species counted by the molecular than by the culture-dependent methods.

Table 3.

Comparison between the composition of hydrocarbon-utilizing bacterial communities in seawater and desert soil-samples determined by the culture-based method versus that determined by a modern molecular approach

Sampling sites Culture-based analysis (using a mineral medium with oil vapor as sole source of carbon and energy, detailed results in Al-Awadhi et al. 2012) Combined DGGE and band amplification analysis
Total number of species Affiliated to the hydrocarbon-utilizing genera: Total number of DGGE bands Affiliated to the genera (hydrocarbon-utilizers are designated with the pertinent reference numbers):
Seawater
Doha 17 Psychrobacter, Oceanobacillus, Vibrio, Agarivorans,Alteromonas, Marinobacter, Stappia,Pseudoalteromonas, Microbacterium, Marinomonas, Nesiotobacter, Mycobacterium 18 Alteromonas, Candidatus1, Marinobacterium, Phaeobacter, Thalassobius2, Thalassolituus3
Sharq 5 Alcanivorax, Stappia, Thalassospira, Nitratireductor 20 Alteromonas, Candidatus, Marinobacterium, Phaeobacter,Pseudoalteromonas, Thalassobius, Thalassolituus
Salmiyah 15 Alteromonas, Echinicola, Klebsiella, Alcanivorax, Marinomonas, Gordonia, Pseudomonas, Rhodococcus, Microbacterium, Vibrio, Marinobacter, Kocuria 17 Alteromonas, Candidatus, Marinobacterium, Phaeobacter,Pseudoalteromonas, Thalassobius, Thalassolituus
Fahaheel 9 Pseudomonas, Dietzia, Shewanella, Arthrobacter,Pseudoalteromonas, Acinetobacter,Alteromonas 20 Alteromonas, Candidatus, Marinobacterium, Phaeobacter,Pseudoalteromonas, Thalassobius, Thalassolituus
Az Zour 4 Alcanivorax, Cobetia,Pseudoalteromonas 15 Alteromonas, Candidatus, Marinobacterium, Phaeobacter, Thalassobius, Thalassolituus
Al Khiran 6 Alcanivorax,Alteromonas,Pseudoalteromonas, Cobetia 15 Alteromonas, Candidatus, Marinobacterium, Phaeobacter*,Pseudoalteromonas, Thalassobius, Thalassolituus
Desert soil
Al Abdali 7 Arthrobacter, Dietzia, Microbacterium, Streptomyces, Agrococcus 30 Bacillus, Planomicrobium4, Ralstonia5, Salinimicrobium6, Segetibacter7
Sabiyah 8 Microbacterium, Dietzia, Pseudomonas, Bordetella, Roseomonas, 36 Acinetobacter, Bacillus, Burkholderia8, Geobacillus9, Halomonas10, Naxibacter11, Planomicrobium, Ralstonia
Kadma 4 Pseudomonas, Sphingomonas 47 Acinetobacter, Bacillus, Burkholderia, Curvibacter5, Sediminibacterium*, Halomonas, Naxibacter, Planomicrobium, Pontibacter12, Ralstonia, Segetibacter
Ahmadi 6 Cellulomonas, Pseudomonas, Arthrobacter, Sphingomonas 30 Acinetobacter, Bacillus, Burkholderia, Curvibacter, Naxibacter, Planomicrobium, Pontibacteter
Ash Shua’yba 12 Mycobacterium, Nocardia, Rhodococcus, Streptomyces,Bacillus 17 Bacillus, Planomicrobium, Pontibacter
Al Wafra 8 Kocuria, Streptomyces, Agrobacterium,Acinetobacter, Pseudomonas, Brevundimonas, Sphingobium 17 Acinetobacter,Bacillus, Halomonas, Naxibacter
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*No references were found on the hydrocarbon-degradation potential of Sediminibacterium or Phaeobacter. The superscript numbers are the reference numbers in the list recording hydrocarbonoclastic activity among species belonging to the given genera (1, Prabagaran et al. 2007;2, Teramoto et al. Teramoto et al. 2009; 3, Yakimov et al. Yakimov et al. 2004; 4, Yakimov et al. Yakimov et al. 2007; 5, Zhu et al. Zhu et al. 2010; 6, Yergeau et al. Yergeau et al. 2012; 7, Larentis et al. Larentis et al. 2009; 8; Morawski et al. 1997; 9, Arun et al. Arun et al. 2011; 10, Wang et al. Wang et al. 2007; 11, Kleinsteuber et al. Kleinsteuber et al. 2006; 12, Wan et al. Wan et al. 2011).

Genera that were revealed by both approaches are in bold.

In none of the six desert samples investigated could any single species be simultaneously recorded in the composition lists obtained by using the two techniques. Even the species belonging to the genera Bacillus and Acinetobacter in Ash Shua’yba and Al-Wafra samples, respectively varied according to the analytical approach. Using the culture-dependent method (Al-Awadhi et al. 2012), we recorded B. infantis and A. septicus, whereas by the molecular analysis, we recorded B. niacini, B. selenatarsenatis and A. junii. Basically, the same observation, albeit at a slightly less pronounced level, could be made for the open seawater samples. In two samples; Sharq and Az Zour the bacterial species lists were totally different depending on the analytical technique. In the other remaining seawater samples, the molecular approach revealed only two species, Alteromonas macleodii and Pseudoalteromonas phenolica, which were also recorded by the culture-dependent method (Al-Awadhi et al. 2012). The remaining species were totally different, as obvious in Table 3. The analytical technique-dependent differences of the bacterial community composition are also quite obvious in the phylogenetic trees based on the bacteria analyzed by the molecular approach in Figures 4 & 5 as compared with the corresponding trees based on bacteria analyzed by the traditional culture-deoendent method (Al-Awadhi et al. 2012).

Figure 4.

Figure 4

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Phylogenatic tree of 16S rRNA genes of bacteria from Kuwaiti oil polluted coastal water, as analyzed by the culture-independent method. Values shown in each node of the phylogenetic tree are bootstrap value; 2,000 bootstrap replicates were performed.

Figure 5.

Figure 5

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Phylogenatic tree of 16S rRNA genes of bacteria from Kuwaiti oil polluted desert soil, as analyzed by the culture-independent method. Values shown in each node of the phylogenetic tree are bootstrap value; 2,000 bootstrap replicates were performed.

For each of the 24 studied environmental samples, the bacterial community composition determined by using the culture-dependent method (Al-Awadhi et al. 2012) was dramatically, sometimes totally different from that determined by using the molecular approach. This implies that none of the two techniques can be used as a substitute of the other, since each of them favors bacterial taxa different from these favored by the other. Consequently, in order to limit the bias, both approaches should be adopted simultaneously, and the collective result would obviously reflect the “real bacterial composition” more precisely than that obtained using either of them alone, even though the bias problems are still not rased.

To provide a further evidence for the validity of the latter conclusion, the contribution of both techniques to the analysis of the group of the “obligate oil-degrading marine bacteria” in the seawater samples is highlighted. This is a new and ecophysiologically unusual group recently recognized and termed “the obligate hydrocarbonoclastic bacteria (OHCB)”; they repotedly play the major role in bioremediating oil in the marine ecosystem (Yakimov et al. 2007). The most common OHCB are species belonging to a few genera; Alcanivorax, Marinobacter, Thalassolituus, Cycloclasticus and Oleispira that occur in pristine seawater in minute numbers, but bloom immediately after oil-pollution. Our results show that Alcanivorax described as the “paradigm” of the OHCB (Yakimov et al. 2007), and Marinobacter were recorded, respectively, in 4 and 2 of the studied seawater sites, but only by using the culture-dependent analytical method (Al-Awadhi et al. 2012). The molecular approach we adopted failed to reveal any of the two OHCB genera in any of the six seawater samples. On the other hand, the genus Thalassolituus was recorded in all six sampling sites, but only when the molecular approach was adopted. By neither of the two techniques could Cycloclasticus and Oleispira be recorded in any of the six seawater samples. Probably, the two genera were not present in the studied samples. Interestingly however, using the molecular (but not the culture-dependent) approach, we recorded the former genus in biofilms on glass plates submerged in pristine and oily Gulf-water (Al-Bader et al. 2012).

Discussion

The DGGE profile similarities of the different seawater samples (Figure 1) should be expected, in view of that seawater in situ is an “open” environment in which the whole water body becomes mechanically mixed up to some extent. Remote samples would thus, show a degree of similarity in their microbial composition. Meanwhile, the DGGE dissimilarities of the different desert soil samples (Figure 2) may be explained on the basis that the processes regulating the bacterial species frequencies in various localities, the so-called patchiness operate at a very narrow, sometimes centimeter spacial scale (Duarte & Vaqué 1992; Long & Farooq 2001; Seuront et al. 2002; Seymour et al. 2000). Expectedly, this phenomenon should be more pronounced in the “closed”, terrestrial than the “open”, aquatic environments. The observed frequent occurrence of the Gammaproteobacteria in the Arabian Gulf water body has also often been recorded by earlier investigators (Al-Awadhi et al. 2012; Al-Sarawi et al. 2008) in the marine habitats.

An important and well known advantage of the culture-dependent approach is that it routinely analyses specific groups of bacteria (in this study oil-utilizers) via the use of selective nutrient media. Since this is not the case with the molecular analysis, we had to compare our results with literature reports. The comparison confirmed that all the bacterial genera listed in Table 3, with the only exception of Sediminibacterium and Phaeobacter, comprised hydrocarbon-utilizing species (see pertinent reference numbers in Table 3). This result demonstrates a serious bias, namely that the used molecular approach preferentially amplified the 16S rDNAs of hydrocarbon-utilizing bacteria in the total DNA extracts from the environmental samples and might have “neglected” others. Still another even more pronounced bias is that the molecular approach used did not reveal in any of the studied environmental samples any member of the phylum Actinobacteria. This was true although by using the culture-dependent method, many species belonging to this phylum were found (sometimes predominant) especially in the desert soil samples (Al-Awadhi et al. 2012). Obviously the technique successfully amplifies certain 16S rDNA’s only when in pure form, but not when mixed with others, as it is the case in the environmental samples. The molecular analysis of bacterial communities on biofilms that developed on glass plates submerged in pristine and oily seawater from the Arabian Gulf (samples similar to those used in this study) also did not reveal one single species belonging to the Actinobacteria (Al-Bader et al. 2012). The present state of knowledge about this subject in the literature is too limited to explain the reason for this latter bias of preferential amplification.

It should be expected that the molecular technique would reveal in every environmental sample most, if not all of the bacterial species that showed up in these samples using the culture-dependent method. Therefore, the most surprising result in our study was that the identities of the bacteria analyzed by both techniques for all the studied samples (and for samples analyzed earlier in our laboratory) were dramatically different. In this context, the assumption that each DGGE band represents one single species is not correct (Sekiguchi et al. 2001). It is established today that differential/preferential amplification of 16S rRNA-genes in environmental samples usually leads to serious bias regarding the actual composition of the bacterial communities (Polz & Cavanaugh 1998; Sipos et al. 2007). Again the results of the current study demonstrate that the technique-dependent differences in community composition are so dramatic that both techniques should necessarily complete, and not just substitute one another in every study. This is true although both approaches are associated with own bias problems. Based on our results, the molecular approach does not seem to reveal numerically much more bacterial species (even though it reveals different rather than the same species) in the environmental samples than the culture-dependent approach, as commonly believed, so far. As shown above, the differences were in all the studied samples only between about 1 and 12 fold, in favor of the molecular approach. This may appear to contradict the well known fact that direct microscopic counts give frequently up to 104 fold more bacterial cell numbers than those counted by the culture-dependent method. This implies that the cells counted microscopically are most probably members of “strains” or “varieties” belonging to a limited number of species, rather than to different species as frequently misunderstood.

As already mentioned, modern microbiologists tend to consider the traditional culture-dependent methods obsolete and prefer the use of the modern molecular approaches instead. However, this study surprisingly showed that the two approaches revealed distinctly different bacterial communities for each studied sample. This unexpected result consolidates that both techniques must not substitute one another, but should mutually complement each other, in order to gain a bacterial composition most close to reality.

Acknowledgements

This study has been supported by Kuwait University, research grant SL01/08.

Footnotes

Competing interests

The authors declare that they have no competing interests.

Authors’ contributions

HA, MK, DM participated in sample collection and DGGE analysis. ND, NA, MK, SR contributed to molecular analysis. SR suggested the research problem and finalized the manuscript. All authors read and approved the manuscript.

Contributor Information

Husain Al-Awadhi, Email: alawadhi@ku.edu.kw.

Narjis Dashti, Email: n.dashti@ku.edu.kw.

Majida Khanafer, Email: majida.khanafer@ku.edu.kw.

Dina Al-Mailem, Email: dina.almailem@ku.edu.kw.

Nidaa Ali, Email: ny.ali@ku.edu.kw.

Samir Radwan, Email: samir.radwan@ku.edu.kw.

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