@article {3141, title = {When is a microbial culture "pure"? Persistent cryptic contaminant escapes detection even with deep genome sequencing.}, journal = {mBio}, volume = {4}, year = {2013}, month = {2013 Mar 12}, pages = {e00591-12}, abstract = {

UNLABELLED: Geobacter sulfurreducens strain KN400 was recovered in previous studies in which a culture of the DL1 strain of G. sulfurreducens served as the inoculum in investigations of microbial current production at low anode potentials (-400 mV versus Ag/AgCl). Differences in the genome sequences of KN400 and DL1 were too great to have arisen from adaptive evolution during growth on the anode. Previous deep sequencing (80-fold coverage) of the DL1 culture failed to detect sequences specific to KN400, suggesting that KN400 was an external contaminant inadvertently introduced into the anode culturing system. In order to evaluate this further, a portion of the gene for OmcS, a c-type cytochrome that both KN400 and DL1 possess, was amplified from the DL1 culture. HiSeq-2000 Illumina sequencing of the PCR product detected the KN400 sequence, which differs from the DL1 sequence at 14 bp, at a frequency of ca. 1 in 10(5) copies of the DL1 sequence. A similar low frequency of KN400 was detected with quantitative PCR of a KN400-specific gene. KN400 persisted at this frequency after intensive restreaking of isolated colonies from the DL1 culture. However, a culture in which KN400 could no longer be detected was obtained by serial dilution to extinction in liquid medium. The KN400-free culture could not grow on an anode poised at -400 mV. Thus, KN400 cryptically persisted in the culture dominated by DL1 for more than a decade, undetected by even deep whole-genome sequencing, and was only fortuitously uncovered by the unnatural selection pressure of growth on a low-potential electrode.

IMPORTANCE: Repeated streaking of isolated colonies on solidified medium remains a common strategy for obtaining pure cultures, especially of difficult-to-cultivate microorganisms such as strict anaerobes. The results presented here demonstrate that verifying the purity of cultures obtained in this manner may be difficult because extremely rare variants can persist, undetectable with even deep genomic DNA sequencing. The only way to ensure that a culture is pure is to cultivate it from an initial single cell, which may be technically difficult for many environmentally significant microbes.

}, keywords = {Coinfection, Electrodes, Genes, Bacterial, Genotype, Geobacter, High-Throughput Nucleotide Sequencing, Microbial Interactions, Polymerase Chain Reaction}, issn = {2150-7511}, doi = {10.1128/mBio.00591-12}, author = {Shrestha, Pravin Malla and Nevin, Kelly P and Shrestha, Minita and Lovley, Derek R} } @article {443, title = {De Novo assembly of the complete genome of an enhanced electricity-producing variant of Geobacter sulfurreducens using only short reads.}, journal = {PLoS One}, volume = {5}, year = {2010}, month = {2010}, pages = {e10922}, abstract = {State-of-the-art DNA sequencing technologies are transforming the life sciences due to their ability to generate nucleotide sequence information with a speed and quantity that is unapproachable with traditional Sanger sequencing. Genome sequencing is a principal application of this technology, where the ultimate goal is the full and complete sequence of the organism of interest. Due to the nature of the raw data produced by these technologies, a full genomic sequence attained without the aid of Sanger sequencing has yet to be demonstrated.We have successfully developed a four-phase strategy for using only next-generation sequencing technologies (Illumina and 454) to assemble a complete microbial genome de novo. We applied this approach to completely assemble the 3.7 Mb genome of a rare Geobacter variant (KN400) that is capable of unprecedented current production at an electrode. Two key components of our strategy enabled us to achieve this result. First, we integrated the two data types early in the process to maximally leverage their complementary characteristics. And second, we used the output of different short read assembly programs in such a way so as to leverage the complementary nature of their different underlying algorithms or of their different implementations of the same underlying algorithm.The significance of our result is that it demonstrates a general approach for maximizing the efficiency and success of genome assembly projects as new sequencing technologies and new assembly algorithms are introduced. The general approach is a meta strategy, wherein sequencing data are integrated as early as possible and in particular ways and wherein multiple assembly algorithms are judiciously applied such that the deficiencies in one are complemented by another.}, keywords = {Algorithms, Electricity, Genome, Bacterial, Geobacter, Polymerase Chain Reaction}, issn = {1932-6203}, doi = {10.1371/journal.pone.0010922}, author = {Nagarajan, Harish and Butler, Jessica E and Klimes, Anna and Qiu, Yu and Zengler, Karsten and Ward, Joy and Young, Nelson D and Meth{\'e}, Barbara A and Palsson, Bernhard {\O} and Lovley, Derek R and Barrett, Christian L} } @article {488, title = {Gene transcript analysis of assimilatory iron limitation in Geobacteraceae during groundwater bioremediation.}, journal = {Environ Microbiol}, volume = {10}, year = {2008}, month = {2008 May}, pages = {1218-30}, abstract = {Limitations on the availability of Fe(III) as an electron acceptor are thought to play an important role in restricting the growth and activity of Geobacter species during bioremediation of contaminated subsurface environments, but the possibility that these organisms might also be limited in the subsurface by the availability of iron for assimilatory purposes was not previously considered because copious quantities of Fe(II) are produced as the result of Fe(III) reduction. Analysis of multiple Geobacteraceae genomes revealed the presence of a three-gene cluster consisting of homologues of two iron-dependent regulators, fur and dtxR (ideR), separated by a homologue of feoB, which encodes an Fe(II) uptake protein. This cluster appears to be conserved among members of the Geobacteraceae and was detected in several environments. Expression of the fur-feoB-ideR cluster decreased as Fe(II) concentrations increased in chemostat cultures. The number of Geobacteraceae feoB transcripts in groundwater samples from a site undergoing in situ uranium bioremediation was relatively high until the concentration of dissolved Fe(II) increased near the end of the field experiment. These results suggest that, because much of the Fe(II) is sequestered in solid phases, Geobacter species, which have a high requirement for iron for iron-sulfur proteins, may be limited by the amount of iron available for assimilatory purposes. These results demonstrate the ability of transcript analysis to reveal previously unsuspected aspects of the in situ physiology of microorganisms in subsurface environments.}, keywords = {Bacterial Proteins, Biodegradation, Environmental, Culture Media, Ferric Compounds, Ferrous Compounds, Fresh Water, Gene Expression Regulation, Bacterial, Geobacter, Iron, Multigene Family, Phylogeny, Polymerase Chain Reaction, Repressor Proteins, Reverse Transcriptase Polymerase Chain Reaction, Transcription, Genetic, Uranium, Water Pollution, Radioactive}, issn = {1462-2920}, doi = {10.1111/j.1462-2920.2007.01537.x}, author = {O{\textquoteright}Neil, Regina A and Holmes, Dawn E and Coppi, Maddalena V and Adams, Lorrie A and Larrahondo, M Juliana and Ward, Joy E and Nevin, Kelly P and Woodard, Trevor L and Vrionis, Helen A and N{\textquoteright}guessan, Lucie A and Lovley, Derek R} } @article {493, title = {Subsurface clade of Geobacteraceae that predominates in a diversity of Fe(III)-reducing subsurface environments.}, journal = {ISME J}, volume = {1}, year = {2007}, month = {2007 Dec}, pages = {663-77}, abstract = {There are distinct differences in the physiology of Geobacter species available in pure culture. Therefore, to understand the ecology of Geobacter species in subsurface environments, it is important to know which species predominate. Clone libraries were assembled with 16S rRNA genes and transcripts amplified from three subsurface environments in which Geobacter species are known to be important members of the microbial community: (1) a uranium-contaminated aquifer located in Rifle, CO, USA undergoing in situ bioremediation; (2) an acetate-impacted aquifer that serves as an analog for the long-term acetate amendments proposed for in situ uranium bioremediation and (3) a petroleum-contaminated aquifer in which Geobacter species play a role in the oxidation of aromatic hydrocarbons coupled with the reduction of Fe(III). The majority of Geobacteraceae 16S rRNA sequences found in these environments clustered in a phylogenetically coherent subsurface clade, which also contains a number of Geobacter species isolated from subsurface environments. Concatamers constructed with 43 Geobacter genes amplified from these sites also clustered within this subsurface clade. 16S rRNA transcript and gene sequences in the sediments and groundwater at the Rifle site were highly similar, suggesting that sampling groundwater via monitoring wells can recover the most active Geobacter species. These results suggest that further study of Geobacter species in the subsurface clade is necessary to accurately model the behavior of Geobacter species during subsurface bioremediation of metal and organic contaminants.}, keywords = {Biodegradation, Environmental, Ecosystem, Ferric Compounds, Geobacter, Hydrocarbons, Aromatic, Molecular Sequence Data, Oxidation-Reduction, Petroleum, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Uranium}, issn = {1751-7362}, doi = {10.1038/ismej.2007.85}, author = {Holmes, Dawn E and O{\textquoteright}Neil, Regina A and Vrionis, Helen A and N{\textquoteright}guessan, Lucie A and Ortiz-Bernad, Irene and Larrahondo, Maria J and Adams, Lorrie A and Ward, Joy A and Nicoll, Julie S and Nevin, Kelly P and Chavan, Milind A and Johnson, Jessica P and Long, Philip E and Lovley, Derek R} } @article {515, title = {c-Type cytochromes in Pelobacter carbinolicus.}, journal = {Appl Environ Microbiol}, volume = {72}, year = {2006}, month = {2006 Nov}, pages = {6980-5}, abstract = {Previous studies failed to detect c-type cytochromes in Pelobacter species despite the fact that other close relatives in the Geobacteraceae, such as Geobacter and Desulfuromonas species, have abundant c-type cytochromes. Analysis of the recently completed genome sequence of Pelobacter carbinolicus revealed 14 open reading frames that could encode c-type cytochromes. Transcripts for all but one of these open reading frames were detected in acetoin-fermenting and/or Fe(III)-reducing cells. Three putative c-type cytochrome genes were expressed specifically during Fe(III) reduction, suggesting that the encoded proteins may participate in electron transfer to Fe(III). One of these proteins was a periplasmic triheme cytochrome with a high level of similarity to PpcA, which has a role in Fe(III) reduction in Geobacter sulfurreducens. Genes for heme biosynthesis and system II cytochrome c biogenesis were identified in the genome and shown to be expressed. Sodium dodecyl sulfate-polyacrylamide gel electrophoresis gels of protein extracted from acetoin-fermenting P. carbinolicus cells contained three heme-staining bands which were confirmed by mass spectrometry to be among the 14 predicted c-type cytochromes. The number of cytochrome genes, the predicted amount of heme c per protein, and the ratio of heme-stained protein to total protein were much smaller in P. carbinolicus than in G. sulfurreducens. Furthermore, many of the c-type cytochromes that genetic studies have indicated are required for optimal Fe(III) reduction in G. sulfurreducens were not present in the P. carbinolicus genome. These results suggest that further evaluation of the functions of c-type cytochromes in the Geobacteraceae is warranted.}, keywords = {Bacterial Proteins, Cytochromes c, Deltaproteobacteria, Heme, Polymerase Chain Reaction, Proteomics, Reverse Transcriptase Polymerase Chain Reaction, RNA, Messenger}, issn = {0099-2240}, doi = {10.1128/AEM.01128-06}, author = {Haveman, Shelley A and Holmes, Dawn E and Ding, Yan-Huai R and Ward, Joy E and Didonato, Raymond J and Lovley, Derek R} } @article {538, title = {DNA microarray analysis of nitrogen fixation and Fe(III) reduction in Geobacter sulfurreducens.}, journal = {Appl Environ Microbiol}, volume = {71}, year = {2005}, month = {2005 May}, pages = {2530-8}, abstract = {A DNA microarray representing the genome of Geobacter sulfurreducens was constructed for use in global gene expression profiling of cells under steady-state conditions with acetate as the electron donor and Fe(III) or fumarate as the electron acceptor. Reproducible differences in transcript levels were also observed in comparisons between cells grown with ammonia and those fixing atmospheric nitrogen. There was a high correlation between changes in transcript levels determined with microarray analyses and an evaluation of a subset of the genome with quantitative PCR. As expected, cells required to fix nitrogen had higher levels of transcripts of genes associated with nitrogen fixation, further demonstrating that the microarray approach could reliably detect important physiological changes. Cells grown with Fe(III) as the electron acceptor had higher levels of transcripts for omcB, a gene coding for an outer membrane c-type cytochrome that is essential for Fe(III) reduction. Several other c-type cytochrome genes also appeared to be up-regulated. An unexpected result was significantly higher levels of transcripts for genes which have a role in metal efflux, potentially suggesting the importance of maintaining metal homeostasis during release of soluble metals when reducing Fe(III). A substantial proportion (30\%) of significantly expressed genes during Fe(III) reduction were genes of unknown function or hypothetical proteins, suggesting differences in Fe(III) reduction physiology among microorganisms which perform this metabolic process.}, keywords = {Ferric Compounds, Fumarates, Geobacter, Microarray Analysis, Nitrogen Fixation, Oxidation-Reduction, Polymerase Chain Reaction}, issn = {0099-2240}, doi = {10.1128/AEM.71.5.2530-2538.2005}, author = {Meth{\'e}, Barbara A and Webster, Jennifer and Nevin, Kelly and Butler, Jessica and Lovley, Derek R} } @article {526, title = {Microbial incorporation of 13C-labeled acetate at the field scale: detection of microbes responsible for reduction of U(VI).}, journal = {Environ Sci Technol}, volume = {39}, year = {2005}, month = {2005 Dec 1}, pages = {9039-48}, abstract = {A field-scale acetate amendment experiment was performed in a contaminated aquifer at Old Rifle, CO to stimulate in situ microbial reduction of U(VI) in groundwater. To evaluate the microorganisms responsible for microbial uranium reduction during the experiment, 13C-labeled acetate was introduced into well bores via bio-traps containing porous activated carbon beads (Bio-Sep). Incorporation of the 13C from labeled acetate into cellular DNA and phospholipid fatty acid (PLFA) biomarkers was analyzed in parallel with geochemical parameters. An enrichment of active sigma-proteobacteria was demonstrated in downgradient monitoring wells: Geobacter dominated in wells closer to the acetate injection gallery, while various sulfate reducers were prominent in different downgradient wells. These results were consistent with the geochemical evidence of Fe(III), U(VI), and SO(4)2- reduction. PLFA profiling of bio-traps suspended in the monitoring wells also showed the incorporation of 13C into bacterial cellular lipids. Community composition of downgradient monitoring wells based on quinone and PLFA profiling was in general agreement with the 13C-DNA result. The direct application of 13C label to biosystems, coupled with DNA and PLFA analysis,}, keywords = {Acetates, Biodegradation, Environmental, Carbon Isotopes, Electrophoresis, Polyacrylamide Gel, Geobacter, Phylogeny, Polymerase Chain Reaction, Proteobacteria, Uranium}, issn = {0013-936X}, author = {Chang, Yun-Juan and Long, Philip E and Geyer, Roland and Peacock, Aaron D and Resch, Charles T and Sublette, Kerry and Pfiffner, Susan and Smithgall, Amanda and Anderson, Robert T and Vrionis, Helen A and Stephen, John R and Dayvault, Richard and Ortiz-Bernad, Irene and Lovley, Derek R and White, David C} } @article {530, title = {Microbiological and geochemical heterogeneity in an in situ uranium bioremediation field site.}, journal = {Appl Environ Microbiol}, volume = {71}, year = {2005}, month = {2005 Oct}, pages = {6308-18}, abstract = {The geochemistry and microbiology of a uranium-contaminated subsurface environment that had undergone two seasons of acetate addition to stimulate microbial U(VI) reduction was examined. There were distinct horizontal and vertical geochemical gradients that could be attributed in large part to the manner in which acetate was distributed in the aquifer, with more reduction of Fe(III) and sulfate occurring at greater depths and closer to the point of acetate injection. Clone libraries of 16S rRNA genes derived from sediments and groundwater indicated an enrichment of sulfate-reducing bacteria in the order Desulfobacterales in sediment and groundwater samples. These samples were collected nearest the injection gallery where microbially reducible Fe(III) oxides were highly depleted, groundwater sulfate concentrations were low, and increases in acid volatile sulfide were observed in the sediment. Further down-gradient, metal-reducing conditions were present as indicated by intermediate Fe(II)/Fe(total) ratios, lower acid volatile sulfide values, and increased abundance of 16S rRNA gene sequences belonging to the dissimilatory Fe(III)- and U(VI)-reducing family Geobacteraceae. Maximal Fe(III) and U(VI) reduction correlated with maximal recovery of Geobacteraceae 16S rRNA gene sequences in both groundwater and sediment; however, the sites at which these maxima occurred were spatially separated within the aquifer. The substantial microbial and geochemical heterogeneity at this site demonstrates that attempts should be made to deliver acetate in a more uniform manner and that closely spaced sampling intervals, horizontally and vertically, in both sediment and groundwater are necessary in order to obtain a more in-depth understanding of microbial processes and the relative contribution of attached and planktonic populations to in situ uranium bioremediation.}, keywords = {Acetates, Biodegradation, Environmental, Deltaproteobacteria, DNA, Bacterial, DNA, Ribosomal, Ferric Compounds, Fresh Water, Geologic Sediments, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sulfates, Uranium, Water Pollution}, issn = {0099-2240}, doi = {10.1128/AEM.71.10.6308-6318.2005}, author = {Vrionis, Helen A and Anderson, Robert T and Ortiz-Bernad, Irene and O{\textquoteright}Neill, Kathleen R and Resch, Charles T and Peacock, Aaron D and Dayvault, Richard and White, David C and Long, Philip E and Lovley, Derek R} } @article {548, title = {Direct correlation between rates of anaerobic respiration and levels of mRNA for key respiratory genes in Geobacter sulfurreducens.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Sep}, pages = {5183-9}, abstract = {The predominance of Geobacter species in environments in which Fe(III) reduction is important has suggested that Fe(III) reduction rates might be estimated in Geobacter-dominated environments by assessing in situ activity with molecular techniques. To determine whether mRNA levels of key respiratory genes might be correlated with respiration rates in Geobacter sulfurreducens, studies were conducted with fumarate as the electron acceptor and acetate as the limiting electron donor in anaerobic continuous cultures. Levels of mRNA for a fumarate reductase gene, frdA, quantified by real-time reverse transcription-PCR were directly correlated with fumarate reduction rates. In similar studies with Fe(III) as the electron acceptor, mRNA levels for omcB, a gene for an outer membrane c-type cytochrome involved in Fe(III) reduction, were positively correlated with Fe(III) reduction rates. Levels of mRNA for frdA and omcB were also positively correlated with fumarate and Fe(III) reduction rates, respectively, when growth was limited by the availability of fumarate or Fe(III), but mRNA levels were higher than in acetate-limited cultures. Levels of mRNA for omcC, which encodes a c-type cytochrome highly similar to OmcB but not necessary for Fe(III) reduction, followed patterns different than those of omcB. This agrees with the previous finding that OmcC is not involved in Fe(III) reduction and suggests that changes in mRNA levels of omcB are related to its role in Fe(III) reduction. These results demonstrate that mRNA levels for respiratory genes might be used to estimate in situ Fe(III) reduction rates in Geobacter-dominated environments but suggest that information on environmental conditions and/or the metabolic state of Geobacter species is also required for accurate rate estimates.}, keywords = {Anaerobiosis, Base Sequence, DNA Primers, Geobacter, Kinetics, Oxygen Consumption, Polymerase Chain Reaction, RNA, Messenger}, issn = {0099-2240}, doi = {10.1128/AEM.70.9.5183-5189.2004}, author = {Chin, Kuk-Jeong and Esteve-N{\'u}{\~n}ez, Abraham and Leang, Ching and Lovley, Derek R} } @article {543, title = {In situ expression of nifD in Geobacteraceae in subsurface sediments.}, journal = {Appl Environ Microbiol}, volume = {70}, year = {2004}, month = {2004 Dec}, pages = {7251-9}, abstract = {In order to determine whether the metabolic state of Geobacteraceae involved in bioremediation of subsurface sediments might be inferred from levels of mRNA for key genes, in situ expression of nifD, a highly conserved gene involved in nitrogen fixation, was investigated. When Geobacter sulfurreducens was grown without a source of fixed nitrogen in chemostats with acetate provided as the limiting electron donor and Fe(III) as the electron acceptor, levels of nifD transcripts were 4 to 5 orders of magnitude higher than in chemostat cultures provided with ammonium. In contrast, the number of transcripts of recA and the 16S rRNA gene were slightly lower in the absence of ammonium. The addition of acetate to organic- and nitrogen-poor subsurface sediments stimulated the growth of Geobacteraceae and Fe(III) reduction, as well as the expression of nifD in Geobacteraceae. Levels of nifD transcripts in Geobacteraceae decreased more than 100-fold within 2 days after the addition of 100 microM ammonium, while levels of recA and total bacterial 16S rRNA in Geobacteraceae remained relatively constant. Ammonium amendments had no effect on rates of Fe(III) reduction in acetate-amended sediments or toluene degradation in petroleum-contaminated sediments, suggesting that other factors, such as the rate that Geobacteraceae could access Fe(III) oxides, limited Fe(III) reduction. These results demonstrate that it is possible to monitor one aspect of the in situ metabolic state of Geobacteraceae species in subsurface sediments via analysis of mRNA levels, which is the first step toward a more global analysis of in situ gene expression related to nutrient status and stress response during bioremediation by Geobacteraceae.}, keywords = {Acetates, Biodegradation, Environmental, Culture Media, DNA, Ribosomal, Fresh Water, Gene Expression Regulation, Bacterial, Geobacter, Geologic Sediments, Nitrogenase, Petroleum, Phylogeny, Polymerase Chain Reaction, Quaternary Ammonium Compounds, Rec A Recombinases, RNA, Ribosomal, 16S, Water Pollutants, Chemical}, issn = {0099-2240}, doi = {10.1128/AEM.70.12.7251-7259.2004}, author = {Holmes, Dawn E and Nevin, Kelly P and Lovley, Derek R} } @article {568, title = {Microorganisms associated with uranium bioremediation in a high-salinity subsurface sediment.}, journal = {Appl Environ Microbiol}, volume = {69}, year = {2003}, month = {2003 Jun}, pages = {3672-5}, abstract = {Although stimulation of dissimilatory metal reduction to promote the reductive precipitation of uranium has been shown to successfully remove uranium from some aquifer sediments, the organisms in the family Geobacteraceae that have been found to be associated with metal reduction in previous studies are not known to grow at the high salinities found in some uranium-contaminated groundwaters. Studies with a highly saline uranium-contaminated aquifer sediment demonstrated that the addition of acetate could stimulate the removal of U(VI) from the groundwater. This removal was associated with an enrichment in microorganisms most closely related to Pseudomonas and Desulfosporosinus species.}, keywords = {Acetates, Biodegradation, Environmental, DNA, Ribosomal, Fresh Water, Geologic Sediments, Peptococcaceae, Polymerase Chain Reaction, Pseudomonas, RNA, Ribosomal, 16S, Sodium Chloride, Uranium, Water Pollution}, issn = {0099-2240}, author = {Nevin, Kelly P and Finneran, Kevin T and Lovley, Derek R} } @article {582, title = {Specific 16S rDNA sequences associated with naphthalene degradation under sulfate-reducing conditions in harbor sediments.}, journal = {Microb Ecol}, volume = {43}, year = {2002}, month = {2002 Jan}, pages = {134-45}, abstract = {Previous studies have demonstrated that naphthalene and other polycyclic aromatic hydrocarbons (PAHs) can be anaerobically oxidized with the reduction of sulfate in PAH-contaminated marine harbor sediments, including those in San Diego Bay. In order to learn more about the microorganisms that might be involved in anaerobic naphthalene degradation, the microorganisms associated with naphthalene degradation in San Diego Bay sediments were evaluated. A dilution-to-extinction enrichment culture strategy, designed to recover the most numerous culturable naphthalene-degrading sulfate reducers, resulted in the enrichment of microorganisms with 16S rDNA sequences in the d-Proteobacteria, which were closely related to a previously described pure culture of a naphthalene-degrading sulfate reducer, NaphS2, isolated from sediments in Germany. A more traditional enrichment culture approach, expected to enrich for the fastest-growing naphthalene-degrading sulfate reducers, yielded 16S rDNA sequences closely related to those found in the dilution-to-extinction enrichments and NaphS2. Analysis of 16S rDNA sequences in sediments from two sites in San Diego Bay that had been adapted for rapid naphthalene degradation by continual amendment with low levels of naphthalene suggested that the microbial community composition in the amended sediments differed from that present in the unamended sediments from the same sites. Most significantly, 6-8\% of the sequences recovered from 100 clones of each of the naphthalene-amended sediments were closely related to the 16S rDNA sequences in the enrichment cultures as well as the sequence of the pure culture, NaphS2. No sequences in this NaphS2 phylotype were recovered from the sediments that were not continually exposed to naphthalene. A PCR primer, which was designed based on these phylotype sequences, was used to amplify additional 16S rDNA sequences belonging to the NaphS2 phylotype from PAH-degrading sediments from Island End River (Boston), MA, and Liepaja Harbor, Latvia. Closely related sequences were also recovered from highly contaminated sediment from Tampa Bay, FL. These results suggest that microorganisms closely related to NaphS2 might be involved in naphthalene degradation in harbor sediments. This finding contrasts with the frequent observation that the environmentally relevant microorganisms cannot be readily recovered in pure culture and suggests that further study of the physiology of NaphS2 may provide insights into factors controlling the rate and extent of naphthalene degradation in marine harbor sediments.}, keywords = {Biodegradation, Environmental, DNA Primers, DNA, Bacterial, Geologic Sediments, Naphthalenes, Oxidation-Reduction, Phylogeny, Polymerase Chain Reaction, RNA, Ribosomal, 16S, Sequence Analysis, DNA, Sulfur-Reducing Bacteria, Water Pollutants, Chemical}, issn = {0095-3628}, doi = {10.1007/s00248-001-1055-z}, author = {Hayes, L A and Lovley, Derek R} }