Stable Isotope Probing with 15N2 Reveals Novel Noncultivated Diazotrophs in Soil

Biological nitrogen fixation is a fundamental component of the nitrogen cycle and is the dominant natural process through which fixed nitrogen is made available to the biosphere. While the process of nitrogen fixation has been studied extensively with a limited set of cultivated isolates, examinations of nifH gene diversity in natural systems reveal the existence of a wide range of noncultivated diazotrophs. These noncultivated diazotrophs remain uncharacterized, as do their contributions to nitrogen fixation in natural systems. We have employed a novel ¹⁵N₂-DNA stable isotope probing (⁵N₂-DNA-SIP) method to identify free-living diazotrophs in soil that are responsible for nitrogen fixation in situ. Analyses of 16S rRNA genes from ¹⁵N-labeled DNA provide evidence for nitrogen fixation by three microbial groups, one of which belongs to the Rhizobiales while the other two represent deeply divergent lineages of noncultivated bacteria within the Betaproteobacteria and Actinobacteria, respectively. Analysis of nifH genes from ¹⁵N-labeled DNA also revealed three microbial groups, one of which was associated with Alphaproteobacteria while the others were associated with two noncultivated groups that are deeply divergent within nifH cluster I. These results reveal that noncultivated free-living diazotrophs can mediate nitrogen fixation in soils and that ¹⁵N₂-DNA-SIP can be used to gain access to DNA from these organisms. In addition, this research provides the first evidence for nitrogen fixation by Actinobacteria outside of the order Actinomycetales.     

Characterization of growing microorganisms in soil by stable isotope probing with H218O

A new approach to characterize growing microorganisms in environmental samples based on labeling microbial DNA with H(2)(18)O is described. To test if sufficient amounts of (18)O could be incorporated into DNA to use water as a labeling substrate for stable isotope probing, Escherichia coli DNA was labeled by cultivating bacteria in Luria broth with H(2)(18)O and labeled DNA was separated from [(16)O]DNA on a cesium chloride gradient. Soil samples were incubated with H(2)(18)O for 6, 14, or 21 days, and isopycnic centrifugation of the soil DNA showed the formation of two bands after 6 days and three bands after 14 or 21 days, indicating that (18)O can be used in the stable isotope probing of soil samples. DNA extracted from soil incubated for 21 days with H(2)(18)O was fractionated after isopycnic centrifugation and DNA from 17 subsamples was used in terminal restriction fragment length polymorphism (TRFLP) analysis of bacterial 16S rRNA genes. The TRFLP patterns clustered into three groups that corresponded to the three DNA bands. The fraction of total fluorescence contributed by individual terminal restriction fragments (TRF) to a TRFLP pattern varied across the 17 subsamples so that a TRF was more prominent in only one of the three bands. Labeling soil DNA with H(2)(18)O allows the identification of newly grown cells. In addition, cells that survive but do not divide during an incubation period can also be characterized with this new technique because their DNA remains without the label.     

Using Stable Isotope Probing to Characterize Differences Between Free-Living and Sediment-Associated Microorganisms in the Subsurface

Aquifers are subterranean reservoirs of freshwater with heterotrophic bacterial communities attached to the sediments and free-living in the groundwater. In the present study, mesocosms were used to assess factors controlling the diversity and activity of the subsurface bacterial community. The assimilation of ¹³C, derived from ¹³C-acetate, was monitored to determine whether the sediment-associated and free-living bacterial community would respond similarly to the presence of protozoan grazers. We observed a dynamic response in the sediment-associated bacterial community and none in the free-living community. The disparity in these observations highlights the importance of the sediment-associated bacterial community in the subsurface carbon cycle.     

Characterization of para-Nitrophenol-Degrading Bacterial Communities in River Water by Using Functional Markers and Stable Isotope Probing

Microbial degradation is a major determinant of the fate of pollutants in the environment. para-Nitrophenol (PNP) is an EPA-listed priority pollutant with a wide environmental distribution, but little is known about the microorganisms that degrade it in the environment. We studied the diversity of active PNP-degrading bacterial populations in river water using a novel functional marker approach coupled with [¹³C₆]PNP stable isotope probing (SIP). Culturing together with culture-independent terminal restriction fragment length polymorphism analysis of 16S rRNA gene amplicons identified Pseudomonas syringae to be the major driver of PNP degradation in river water microcosms. This was confirmed by SIP-pyrosequencing of amplified 16S rRNA. Similarly, functional gene analysis showed that degradation followed the Gram-negative bacterial pathway and involved pnpA from Pseudomonas spp. However, analysis of maleylacetate reductase (encoded by mar), an enzyme common to late stages of both Gram-negative and Gram-positive bacterial PNP degradation pathways, identified a diverse assemblage of bacteria associated with PNP degradation, suggesting that mar has limited use as a specific marker of PNP biodegradation. Both the pnpA and mar genes were detected in a PNP-degrading isolate, P. syringae AKHD2, which was isolated from river water. Our results suggest that PNP-degrading cultures of Pseudomonas spp. are representative of environmental PNP-degrading populations.     

Stable Isotope Ratios and Forensic Analysis of Microorganisms

In the aftermath of the anthrax letters of 2001, researchers have been exploring various analytical signatures for the purpose of characterizing the production environment of microorganisms. One such signature is stable isotope ratios, which in heterotrophs, are a function of nutrient and water sources. Here we discuss the use of stable isotope ratios in microbial forensics, using as a database the carbon, nitrogen, oxygen, and hydrogen stable isotope ratios of 247 separate cultures of Bacillus subtilis 6051 spores produced on a total of 32 different culture media. In the context of using stable isotope ratios as a signature for sample matching, we present an analysis of variations between individual samples, between cultures produced in tandem, and between cultures produced in the same medium but at different times. Additionally, we correlate the stable isotope ratios of carbon, nitrogen, oxygen, and hydrogen for growth medium nutrients or water with those of spores and show examples of how these relationships can be used to exclude nutrient or water samples as possible growth substrates for specific cultures.     

Nutrient Amendments in Soil DNA Stable Isotope Probing Experiments Reduce the Observed Methanotroph Diversity

Stable isotope probing (SIP) can be used to analyze the active bacterial populations involved in a process by incorporating ¹³C-labeled substrate into cellular components such as DNA. Relatively long incubation times are often used with laboratory microcosms in order to incorporate sufficient ¹³C into the DNA of the target organisms. Addition of nutrients can be used to accelerate the processes. However, unnatural concentrations of nutrients may artificially change bacterial diversity and activity. In this study, methanotroph activity and diversity in soil was examined during the consumption of ¹³CH₄ with three DNA-SIP experiments, using microcosms with natural field soil water conditions, the addition of water, and the addition of mineral salts solution. Methanotroph population diversity was studied by targeting 16S rRNA and pmoA genes. Clone library analyses, denaturing gradient gel electrophoresis fingerprinting, and pmoA microarray hybridization analyses were carried out. Most methanotroph diversity (type I and type II methanotrophs) was observed in nonamended SIP microcosms. Although this treatment probably best reflected the in situ environmental conditions, one major disadvantage of this incubation was that the incorporation of ¹³CH₄ was slow and some cross-feeding of ¹³C occurred, thereby leading to labeling of nonmethanotroph microorganisms. Conversely, microcosms supplemented with mineral salts medium exhibited rapid consumption of ¹³CH₄, resulting in the labeling of a less diverse population of only type I methanotrophs. DNA-SIP incubations using water-amended microcosms yielded faster incorporation of ¹³C into active methanotrophs while avoiding the cross-feeding of ¹³C.     

Biphenyl-Metabolizing Bacteria in the Rhizosphere of Horseradish and Bulk Soil Contaminated by Polychlorinated Biphenyls as Revealed by Stable Isotope Probing

DNA-based stable isotope probing in combination with terminal restriction fragment length polymorphism was used in order to identify members of the microbial community that metabolize biphenyl in the rhizosphere of horseradish (Armoracia rusticana) cultivated in soil contaminated with polychlorinated biphenyls (PCBs) compared to members of the microbial community in initial, uncultivated bulk soil. On the basis of early and recurrent detection of their 16S rRNA genes in clone libraries constructed from [¹³C]DNA, Hydrogenophaga spp. appeared to dominate biphenyl catabolism in the horseradish rhizosphere soil, whereas Paenibacillus spp. were the predominant biphenyl-utilizing bacteria in the initial bulk soil. Other bacteria found to derive carbon from biphenyl in this nutrient-amended microcosm-based study belonged mostly to the class Betaproteobacteria and were identified as Achromobacter spp., Variovorax spp., Methylovorus spp., or Methylophilus spp. Some bacteria that were unclassified at the genus level were also detected, and these bacteria may be members of undescribed genera. The deduced amino acid sequences of the biphenyl dioxygenase α subunits (BphA) from bacteria that incorporated [¹³C]into DNA in 3-day incubations of the soils with [¹³C]biphenyl are almost identical to that of Pseudomonas alcaligenes B-357. This suggests that the spectrum of the PCB congeners that can be degraded by these enzymes may be similar to that of strain B-357. These results demonstrate that altering the soil environment can result in the participation of different bacteria in the metabolism of biphenyl.Polychlorinated biphenyls (PCBs) are very stable chloroorganic compounds with the general formula C₁₂H_10-xCl_x. Mixtures of PCBs have been used as coolants and lubricants in transformers, capacitors, and other electrical equipment as they do not burn easily and are good insulators. It is estimated that some 1.5 million tons of PCBs were produced up to 1988 worldwide (11; http://www.atsdr.cdc.gov/cercla; http://www.epa.gov/epawaste/hazard/tsd/pcbs/pubs/about.htm). Although production of these compounds was stopped, due to their long-term persistence, many sites all over the world are still contaminated with PCBs. Moreover, not only do PCBs threaten human health in the vicinity of the contaminated area, but lower PCB congeners volatilize and migrate to places far from where they were originally released (2, 3, 16). Also, their metabolic products have environmental significance; activities of both plants and microorganisms result in formation of different intermediates and final products whose toxicity can in some cases be even higher than that of the original toxicant (24, 26; http://www.atsdr.cdc.gov/cercla).Physical-chemical methods used for the removal of PCBs often cause further natural disturbance and pollution; in contrast, biological methods of removal (i.e., bioremediation) are less expensive and more environmentally sound and thus have aroused much interest (7). These methods include the use of microorganisms and also exploitation of plants (i.e., phytoremediation) (19) and the cooperation of plants with microorganisms in the rhizosphere (i.e., rhizoremediation) (21). These bioremediation options also include the use of genetically modified bacteria (6) and/or plants (18, 23). PCBs were only recently introduced into the environment, and no completely efficient pathways for the aerobic bacterial degradation of all of these compounds have evolved (34); however, lower chlorinated PCB congeners can be degraded via the pathway that is used by aerobic bacteria to degrade biphenyl (35). Therefore, metabolism of biphenyl as a potential cometabolite of PCBs was the subject of this study.The biphenyl degradation pathway is the same in all aerobic bacteria, and enzymes of this pathway degrade biphenyl in four steps into benzoate and 2-hydroxypenta-2,4-dienoate (21). The first enzyme of the pathway, biphenyl dioxygenase, has broad substrate specificity and thus permits degradation of biphenyl-related compounds (9). Substrates for biphenyl dioxygenase comprise, in addition to biphenyl itself, other diphenyl or benzene skeletons with several substituents, including halogens and bicyclic or tricyclic fused heterocyclic aromatics (35). These substrates also include certain natural compounds, including some plant flavonoids, phenols, or terpenes (10). Bacteria capable of metabolizing biphenyl are thus pervasive members of many microbial communities in vegetated soil.As reported previously (20), there are two main problems with introduction of a new population of degrading or genetically modified microorganisms to enhance the biodegradation of PCBs in a contaminated environment: legislative barriers and the inability of strains added to the soil to survive. Therefore, the use of microorganisms for bioremediation of contaminated sites is not likely to be successful. Hence, understanding the biodegradative processes in the natural communities is necessary for planning remediation strategies. Identification of members of the community potentially responsible for the degradative process has recently been enabled by DNA-based stable isotope probing (SIP), as reviewed previously; therefore, this technique has become an efficient tool in microbial ecology (33). In this study, by tracking the transfer of ¹³C from [¹³C]biphenyl into bacterial DNA, it was possible to identify biphenyl-metabolizing bacteria in PCB-contaminated soil. To analyze how the bacterial diversity can be changed by introduction of a plant and subsequent cultivation in a greenhouse, bacteria in the rhizosphere of horseradish (Armoracia rusticana) cultivated in a contaminated soil were studied.     

Stable Isotope Probing Analysis of Interactions between Ammonia Oxidizers

The response of natural microbial communities to environmental change can be assessed by determining DNA- or RNA-targeted changes in relative abundance of 16S rRNA gene sequences by using fingerprinting techniques such as denaturing gradient gel electrophoresis (DNA-DGGE and RNA-DGGE, respectively) or by stable isotope probing (SIP) of 16S rRNA genes following incubation with a ¹³C-labeled substrate (DNA-SIP-DGGE). The sensitivities of these three approaches were compared during batch growth of communities containing two or three Nitrosospira pure or enriched cultures with different tolerances to a high ammonia concentration. Cultures were supplied with low, intermediate, or high initial ammonia concentrations and with ¹³C-labeled carbon dioxide. DNA-SIP-DGGE provided the most direct evidence for growth and was the most sensitive, with changes in DGGE profiles evident before changes in DNA- and RNA-DGGE profiles and before detectable increases in nitrite and nitrate production. RNA-DGGE provided intermediate sensitivity. In addition, the three molecular methods were used to follow growth of individual strains within communities. In general, changes in relative activities of individual strains within communities could be predicted from monoculture growth characteristics. Ammonia-tolerant Nitrosospira cluster 3b strains dominated mixed communities at all ammonia concentrations, and ammonia-sensitive strains were outcompeted at an intermediate ammonia concentration. However, coexistence of ammonia-tolerant and ammonia-sensitive strains occurred at the lowest ammonia concentration, and, under some conditions, strains inhibited at high ammonia in monoculture were active at high ammonia in mixed cultures, where they coexisted with ammonia-tolerant strains. The results therefore demonstrate the sensitivity of SIP for detection of activity of organisms with relatively low yield and low activity and its ability to follow changes in the structure of interacting microbial communities.Molecular characterization of natural microbial communities has demonstrated the existence of novel high-level taxonomic groups with no cultured representatives and with significant diversity within phylogenetic and functional groups already established through analysis of organisms in laboratory culture. Autotrophic ammonia-oxidizing bacteria (AOB) exemplify the latter situation. Their low growth rates and the limited number of readily measured phenotypic characteristics available for identification of these organisms necessitate the use of molecular techniques for characterization of their diversity in natural environments. Phylogenetic analysis of 16S rRNA gene sequences places the majority of cultivated autotrophic bacterial ammonia oxidizers in a monophyletic group within the Betaproteobacteria (8, 26). Amplification and phylogenetic analysis of 16S rRNA gene sequences from enrichment cultures of ammonia oxidizers and sequences of environmental clones (31) suggest the existence of novel groups with no cultivated representative and considerable diversity within those represented by pure cultures.Increased awareness of microbial diversity has raised questions regarding links between species diversity and functional diversity, functional redundancy, and the influence of environmental conditions on the activities of representatives of different phylotypes. For ammonia-oxidizing bacteria, relationships exist between broad phylogenetic groups and the environments from which laboratory isolates were obtained, which are linked, in some cases, to differences in physiological characteristics (11). There is also evidence of links between the relative abundance of different ammonia oxidizer groups and environmental conditions (1, 13, 14, 18, 21, 23, 34), suggesting selection for organisms with particular physiological characteristics. In one study (36), a combination of molecular and physiological studies has demonstrated links between species diversity, functional diversity, and soil nitrification kinetics. However, for ammonia oxidizers and other groups, there is little direct evidence about which strains within diverse communities are active under particular conditions or the extent of competition for substrates.Stable isotope probing (SIP) (24, 27) of nucleic acids provides direct evidence of which members of mixed communities are active. This involves addition of substrates labeled with a stable isotope (most commonly ¹³C), extraction of nucleic acids, separation of ¹²C- and ¹³C-labeled nucleic acids by density gradient centrifugation, and subsequent molecular analysis. Sequences amplified from ¹³C-labeled DNA or RNA are derived from organisms actively assimilating the substrate. This approach has been used to identify organisms that utilize methane or methanol (4, 19), organic compounds (15, 20), or CO₂ (6, 9) in microcosms and those that assimilate plant root exudates in the field (28). SIP therefore links phylogeny to ecosystem function and has identified established and novel groups by utilizing labeled compounds in complex soil communities. The technique also enables in situ physiological studies and investigation of interactions between organisms in mixed cultures belonging to the same functional group. For autotrophic betaproteobacterial ammonia oxidizers, amplification of 16S rRNA genes from ¹³C-labeled DNA during incubation with [¹³C]CO₂ has the potential for discriminating which strains are active under specific conditions. Assessment of the discriminatory ability of this approach in complex natural environments requires studies under controlled and well-characterized conditions. The first aim of this study was, therefore, to assess the ability of SIP to discriminate activities of different members of simple mixed communities in comparison with direct measurement of product concentration and DNA- and RNA-denaturing gradient gel electrophoresis (DGGE). The second was to determine whether the activities of members of mixed communities of ammonia-oxidizing bacteria, in particular, their ability to grow at high ammonia concentrations, could be predicted from their physiological characteristics in monoculture. Of particular interest was whether strains with low ammonia tolerance are competitive at low ammonia concentrations. Mixed cultures were assembled from pure culture representatives of Nitrosospira clusters 0, 3a, and 3b (26, 36), which are frequently found in soil environments, and from enrichment cultures containing representatives of these clusters with heterotrophic contaminants. Other criteria for choice of community members were similarities in specific growth rate and cultivation conditions to enable meaningful competition experiments.     

Methodological Considerations for the Use of Stable Isotope Probing in Microbial Ecology

Stable isotope probing (SIP) is a method used for labeling uncultivated microorganisms in environmental samples or directly in field studies using substrate enriched with stable isotope (e.g., ¹³C). After consumption of the substrate, the cells of microorganisms that consumed the substrate become enriched in the isotope. Labeled biomarkers, such as phospholipid-derived fatty acid (PLFA), ribosomal RNA, and DNA can be analyzed with a range of molecular and analytical techniques, and used to identify and characterize the organisms that incorporated the substrate. The advantages and disadvantages of PLFA-SIP, RNA-SIP, and DNA-SIP are presented. Using examples from our laboratory and from the literature, we discuss important methodological considerations for a successful SIP experiment.     

Identification of Ciliate Grazers of Autotrophic Bacteria in Ammonia-Oxidizing Activated Sludge by RNA Stable Isotope Probing

It is well understood that protozoa play a major role in controlling bacterial biomass and regulating nutrient cycling in the environment. Little is known, however, about the movement of carbon from specific reduced substrates, through functional groups of bacteria, to particular clades of protozoa. In this study we first identified the active protozoan phylotypes present in activated sludge, via the construction of an rRNA-derived eukaryote clone library. Most of the sequences identified belonged to ciliates of the subclass Peritrichia and amoebae, confirming the dominance of surface-associated protozoa in the activated sludge environment. We then demonstrated that ¹³C-labeled protozoan RNA can be retrieved from activated sludge amended with ¹³C-labeled protozoa or ¹³C-labeled Escherichia coli cells by using an RNA stable isotope probing (RNA-SIP) approach. Finally, we used RNA-SIP to track carbon from bicarbonate and acetate into protozoa under ammonia-oxidizing and denitrifying conditions, respectively. RNA-SIP analysis revealed that the peritrich ciliate Epistylis galea dominated the acquisition of carbon from bacteria with access to CO₂ under ammonia-oxidizing conditions, while there was no evidence of specific grazing on acetate consumers under denitrifying conditions.Protozoa are the main consumers of bacteria in the environment, and as such they play a major role in controlling bacterial biomass (33) and regulating nutrient recycling (14). Therefore, being able to study the flow of carbon in food webs involving bacteria and protozoa can provide an insight into how protozoan grazing affects bacterial function in a wide range of systems.Protozoan grazing has the potential to alter the genotypic and phenotypic composition of bacterial communities (15, 17, 18, 35). Perhaps as a result of this, protozoan grazing has also been found to have an effect on the function of activated sludge systems, including nitrogen removal processes. Studies using eukaryotic inhibitors to remove grazers from activated sludge have reported a wide range of effects following reduced grazing pressure. These effects include an increase in turbidity or planktonic cell densities, and either no effect (21, 32), higher nitrification rates (16, 20), or lower (29, 30) rates of nitrification in the absence of grazers. These conflicting reports on the effect of predation on nitrification might be due to protozoa displaying feeding preferences or to the indirect ways in which protozoan grazing can affect bacterial processes. For example, it has been shown that the release of substances, such as vitamins and nucleotides, secreted by protozoa as metabolic by-products, can act as growth factors, which enhance bacterial activity, including nitrification (31). In addition, the presence of some types of grazers, particularly ciliates, has been shown to be closely related to a decrease in biochemical oxygen demand (27), and it has been reported that ciliates can alter water flux and help redistribute nutrients in flocs (8), which in turn might have an impact on nitrification rates.Although the data presented in the literature suggest that protozoan grazing is an important factor for activated sludge processes, there are still many questions as to whether its effects are directly linked to predation and possibly feeding preferences. In the present study we sought to identify protozoa assimilating carbon from autotrophic bacteria under ammonia-oxidizing conditions and acetate-consuming bacteria under denitrifying conditions using RNA-stable isotope probing (RNA-SIP).Since it was first developed, RNA-SIP has been successfully used to identify functional groups of bacteria responsible for different processes, including denitrification and benzene and phenol degradation (9, 10, 19, 25, 26). In these studies, the flow of carbon was tracked from soluble labeled substrates into the bacteria consuming it. However, recent studies have shown that it is possible to use this technique to track the flow of carbon across more than one trophic level, unraveling some of the interactions observed in microbial food webs (11, 13, 23, 24). These studies exemplify the broad range of questions that can be addressed with SIP and have begun to define the boundaries beyond which SIP has limited utility.     

Stable Isotope Probing with 15N Achieved by Disentangling the Effects of Genome G+C Content and Isotope Enrichment on DNA Density

Stable isotope probing (SIP) of nucleic acids is a powerful tool that can identify the functional capabilities of noncultivated microorganisms as they occur in microbial communities. While it has been suggested previously that nucleic acid SIP can be performed with ¹⁵N, nearly all applications of this technique to date have used ¹³C. Successful application of SIP using ¹⁵N-DNA (¹⁵N-DNA-SIP) has been limited, because the maximum shift in buoyant density that can be achieved in CsCl gradients is approximately 0.016 g ml⁻¹ for ¹⁵N-labeled DNA, relative to 0.036 g ml⁻¹ for ¹³C-labeled DNA. In contrast, variation in genome G+C content between microorganisms can result in DNA samples that vary in buoyant density by as much as 0.05 g ml⁻¹. Thus, natural variation in genome G+C content in complex communities prevents the effective separation of ¹⁵N-labeled DNA from unlabeled DNA. We describe a method which disentangles the effects of isotope incorporation and genome G+C content on DNA buoyant density and makes it possible to isolate ¹⁵N-labeled DNA from heterogeneous mixtures of DNA. This method relies on recovery of “heavy” DNA from primary CsCl density gradients followed by purification of ¹⁵N-labeled DNA from unlabeled high-G+C-content DNA in secondary CsCl density gradients containing bis-benzimide. This technique, by providing a means to enhance separation of isotopically labeled DNA from unlabeled DNA, makes it possible to use ¹⁵N-labeled compounds effectively in DNA-SIP experiments and also will be effective for removing unlabeled DNA from isotopically labeled DNA in ¹³C-DNA-SIP applications.     

Use of Field-Based Stable Isotope Probing To Identify Adapted Populations and Track Carbon Flow through a Phenol-Degrading Soil Microbial Community

The goal of this field study was to provide insight into three distinct populations of microorganisms involved in in situ metabolism of phenol. Our approach measured ¹³CO₂ respired from [¹³C]phenol and stable isotope probing (SIP) of soil DNA at an agricultural field site. Traditionally, SIP-based investigations have been subject to the uncertainties posed by carbon cross-feeding. By altering our field-based, substrate-dosing methodologies, experiments were designed to look beyond primary degraders to detect trophically related populations in the food chain. Using gas chromatography-mass spectrometry (GC/MS), it was shown that ¹³C-labeled biomass, derived from primary phenol degraders in soil, was a suitable growth substrate for other members of the soil microbial community. Next, three dosing regimes were designed to examine active members of the microbial community involved in phenol metabolism in situ: (i) 1 dose of [¹³C]phenol, (ii) 11 daily doses of unlabeled phenol followed by 1 dose of [¹³C]phenol, and (iii) 12 daily doses of [¹³C]phenol. GC/MS analysis demonstrated that prior exposure to phenol boosted ¹³CO₂ evolution by a factor of 10. Furthermore, imaging of ¹³C-treated soil using secondary ion mass spectrometry (SIMS) verified that individual bacteria incorporated ¹³C into their biomass. PCR amplification and 16S rRNA gene sequencing of ¹³C-labeled soil DNA from the 3 dosing regimes revealed three distinct clone libraries: (i) unenriched, primary phenol degraders were most diverse, consisting of α-, β-, and γ-proteobacteria and high-G+C-content gram-positive bacteria, (ii) enriched primary phenol degraders were dominated by members of the genera Kocuria and Staphylococcus, and (iii) trophically related (carbon cross-feeders) were dominated by members of the genus Pseudomonas. These data show that SIP has the potential to document population shifts caused by substrate preexposure and to follow the flow of carbon through terrestrial microbial food chains.     

Ubiquitous Dissolved Inorganic Carbon Assimilation by Marine Bacteria in the Pacific Northwest Coastal Ocean as Determined by Stable Isotope Probing

In order to identify bacteria that assimilate dissolved inorganic carbon (DIC) in the northeast Pacific Ocean, stable isotope probing (SIP) experiments were conducted on water collected from 3 different sites off the Oregon and Washington coasts in May 2010, and one site off the Oregon Coast in September 2008 and March 2009. Samples were incubated in the dark with 2 mM ¹³C-NaHCO₃, doubling the average concentration of DIC typically found in the ocean. Our results revealed a surprising diversity of marine bacteria actively assimilating DIC in the dark within the Pacific Northwest coastal waters, indicating that DIC fixation is relevant for the metabolism of different marine bacterial lineages, including putatively heterotrophic taxa. Furthermore, dark DIC-assimilating assemblages were widespread among diverse bacterial classes. Alphaproteobacteria, Gammaproteobacteria, and Bacteroidetes dominated the active DIC-assimilating communities across the samples. Actinobacteria, Betaproteobacteria, Deltaproteobacteria, Planctomycetes, and Verrucomicrobia were also implicated in DIC assimilation. Alteromonadales and Oceanospirillales contributed significantly to the DIC-assimilating Gammaproteobacteria within May 2010 clone libraries. 16S rRNA gene sequences related to the sulfur-oxidizing symbionts Arctic96BD-19 were observed in all active DIC assimilating clone libraries. Among the Alphaproteobacteria, clones related to the ubiquitous SAR11 clade were found actively assimilating DIC in all samples. Although not a dominant contributor to our active clone libraries, Betaproteobacteria, when identified, were predominantly comprised of Burkholderia. DIC-assimilating bacteria among Deltaproteobacteria included members of the SAR324 cluster. Our research suggests that DIC assimilation is ubiquitous among many bacterial groups in the coastal waters of the Pacific Northwest marine environment and may represent a significant metabolic process.     

Identification of Novel Methane-, Ethane-, and Propane-Oxidizing Bacteria at Marine Hydrocarbon Seeps by Stable Isotope Probing

Marine hydrocarbon seeps supply oil and gas to microorganisms in sediments and overlying water. We used stable isotope probing (SIP) to identify aerobic bacteria oxidizing gaseous hydrocarbons in surface sediment from the Coal Oil Point seep field located offshore of Santa Barbara, California. After incubating sediment with ¹³C-labeled methane, ethane, or propane, we confirmed the incorporation of ¹³C into fatty acids and DNA. Terminal restriction fragment length polymorphism (T-RFLP) analysis and sequencing of the 16S rRNA and particulate methane monooxygenase (pmoA) genes in ¹³C-DNA revealed groups of microbes not previously thought to contribute to methane, ethane, or propane oxidation. First, ¹³C methane was primarily assimilated by Gammaproteobacteria species from the family Methylococcaceae, Gammaproteobacteria related to Methylophaga, and Betaproteobacteria from the family Methylophilaceae. Species of the latter two genera have not been previously shown to oxidize methane and may have been cross-feeding on methanol, but species of both genera were heavily labeled after just 3 days. pmoA sequences were affiliated with species of Methylococcaceae, but most were not closely related to cultured methanotrophs. Second, ¹³C ethane was consumed by members of a novel group of Methylococcaceae. Growth with ethane as the major carbon source has not previously been observed in members of the Methylococcaceae; a highly divergent pmoA-like gene detected in the ¹³C-labeled DNA may encode an ethane monooxygenase. Third, ¹³C propane was consumed by members of a group of unclassified Gammaproteobacteria species not previously linked to propane oxidation. This study identifies several bacterial lineages as participants in the oxidation of gaseous hydrocarbons in marine seeps and supports the idea of an alternate function for some pmoA-like genes.Hydrocarbon seeps are widespread along continental margins and emit large amounts of oil and gas into the surrounding environment. This gas is primarily composed of methane, a powerful greenhouse gas, and marine hydrocarbon seeps are estimated to contribute 20 Tg year⁻¹ methane to the atmosphere, representing about 5% of the total atmospheric flux (21, 39). Seeps of thermogenic gas also release an estimated 0.45 Tg year⁻¹ ethane and 0.09 Tg year⁻¹ propane to the atmosphere (20). Each of these three fluxes would be substantially larger if not for microbial oxidation in the sediments and water column (68). Methane, ethane, and propane are subject to anaerobic oxidation in anoxic sediments and water columns (44, 53, 68) or to aerobic oxidation in oxic and suboxic water columns and oxygenated surface sediment (10, 47, 53, 80). We focus here on aerobic oxidation.The majority of known aerobic methane-oxidizing bacteria are members of either Gammaproteobacteria (type I) or Alphaproteobacteria (type II) (29), though several strains of highly acidophilic methanotrophic Verrucomicrobia have also been recently isolated (63). Most methanotrophs are capable of growth only on methane or other one-carbon compounds (17, 29), using a methane monooxygenase (MMO) enzyme to oxidize methane to methanol. There are two known forms of this enzyme: soluble methane monooxygenase (sMMO) and particulate methane monooxygenase (pMMO). sMMO is a soluble, di-iron-containing monooxygenase found only in certain methanotrophs and typically expressed only under low-copper conditions (57). In contrast, pMMO is a membrane-bound enzyme believed to contain copper and iron (26). It is found in all known methanotrophs, with the exception of species of the genus Methylocella (16). pmoA, the gene encoding the α subunit of pMMO, is often used to identify methanotrophic bacteria (54). Very few methanotrophs from marine environments have been cultured (22, 49, 72, 74), but several previous studies of marine methanotrophs (35, 62, 77, 82, 85) have been performed with culture-independent methods and have almost exclusively detected type I methanotrophs. Many of the pmoA sequences from methane seep sites are quite different from those of cultured organisms, suggesting that these environments may contain many novel methanotrophs (77, 82, 85).Even less is known about the organisms that oxidize ethane or propane in marine environments. The number of such isolates, which primarily represent high G+C Gram-positive bacteria (Nocardia, Pseudonocardia, Gordonia, Mycobacterium, and Rhodococcus) or Pseudomonas species, is limited (70). Nearly all of these strains were isolated from soil and selected for their ability to grow on propane or n-butane as the sole carbon source. Most propane-oxidizing strains can oxidize butane, as well as a range of longer chain n-alkanes, but differ in the ability to oxidize ethane. These strains show little, if any, ability to oxidize methane, and none have been shown to grow with methane as the sole carbon source (13, 27, 38, 45, 65). As with methane metabolism, the first step in aerobic ethane and propane metabolism is the oxidation of the alkane to an alcohol (70). Several different enzymes are known to catalyze this step. Thauera butanivorans uses a soluble di-iron butane monooxygenase related to sMMO to oxidize C₂ through C₉ n-alkanes (18, 73). Gordonia sp. strain TY-5, Mycobacterium sp. strain TY-6, and Pseudonocardia sp. strain TY-7 contain soluble di-iron propane monooxygenases that are capable of both terminal and subterminal propane oxidation and differ in their substrate ranges (45, 46). Nocardioides sp. strain CF8 is believed to possess a copper-containing monooxygenase similar to pMMO and ammonia monooxygenase (27, 28). An alkane hydroxylase typically used to oxidize longer-chain n-alkanes has also shown some ability to oxidize propane and butane but not ethane (38). The variety of enzymes and their substrate ranges make it difficult to identify ethane or propane oxidizers with a single functional gene.In order to identify the organisms responsible for methane, ethane, and propane oxidation at hydrocarbon seeps, we used stable isotope probing (SIP). SIP allows the identification of organisms actively consuming a ¹³C-labeled substrate of interest, based on the incorporation of ¹³C into biomass, including DNA and lipids (67). We collected sediment from the Coal Oil Point seep field and incubated sediment-seawater slurries with ¹³C methane, ethane, or propane. Samples were removed at three time points, chosen to ensure sufficient ¹³C incorporation into DNA while minimizing the spread of ¹³C through the community as a result of cross-feeding on metabolic byproducts. ¹³C-DNA was separated from ¹²C-DNA by CsCl density gradient ultracentrifugation, and we used the fractionated DNA for terminal restriction fragment length polymorphism (T-RFLP) and clone library analysis. We also measured ¹³C incorporation into fatty acids in order to confirm significant ¹³C enrichment in membrane lipids, to determine the carbon labeling pattern for each substrate and lipid, and to further characterize the composition of the microbial community.     

Sorption of Cadmium by Microorganisms in Competition with Other Soil Constituents

The fate of cadmium in soil is influenced to a great extent by microbial activity. Microorganisms were compared with abiotic soil components for their ability to sorb Cd from a liquid medium. When the same amount (on a dry weight basis) of bacterial cells (Serratia marcescens and Paracoccus sp.), clay (montmorillonite), or sand was separately incubated in 0.05 M phosphate buffer, pH 7.2, containing 10 ppm of Cd (10 μg/ml), bacterial cells removed the largest quantity of Cd. Dead cells sorbed much more Cd from the medium than live cells. A comparative study of Cd removal from the medium by seven soil bacteria and four fungi did not indicate appreciable differences. With increasing microbial biomass, the relative efficiency of 0.1 M NaOH as an extractant of sorbed Cd increased, whereas the extraction efficiency of 0.005 M DTPA (diethylenetriaminepentaacetic acid) decreased. It appeared that NaOH and DTPA extracted different chemical forms of Cd. This assumption was supported by vastly different correlation coefficients in the relative amount of Cd extracted by the two solvents.