Detection,Distribution, and Organohalogen Compound Discovery Implications of the Reduced Flavin Adenine Dinucleotide-Dependent Halogenase Gene in Major Filamentous Actinomycete Taxonomic Groups

Halogenases have been shown to play a significant role in biosynthesis and introducing the bioactivity of many halogenated secondary metabolites. In this study, 54 reduced flavin adenine dinucleotide (FADH₂)-dependent halogenase gene-positive strains were identified after the PCR screening of a large collection of 228 reference strains encompassing all major families and genera of filamentous actinomycetes. The wide distribution of this gene was observed to extend to some rare lineages with higher occurrences and large sequence diversity. Subsequent phylogenetic analyses revealed that strains containing highly homologous halogenases tended to produce halometabolites with similar structures, and halogenase genes are likely to propagate by horizontal gene transfer as well as vertical inheritance within actinomycetes. Higher percentages of halogenase gene-positive strains than those of halogenase gene-negative ones contained polyketide synthase genes and/or nonribosomal peptide synthetase genes or displayed antimicrobial activities in the tests applied, indicating their genetic and physiological potentials for producing secondary metabolites. The robustness of this halogenase gene screening strategy for the discovery of particular biosynthetic gene clusters in rare actinomycetes besides streptomycetes was further supported by genome-walking analysis. The described distribution and phylogenetic implications of the FADH₂-dependent halogenase gene present a guide for strain selection in the search for novel organohalogen compounds from actinomycetes.It is well known that actinomycetes, notably filamentous actinomycetes, have a remarkable capacity to produce bioactive molecules for drug development (4, 6). However, novel technologies are demanded for the discovery of new bioactive secondary metabolites from these microbes to meet the urgent medical need for drug candidates (5, 9, 31).Genome mining recently has been used to search for new drug leads (7, 20, 42, 51). Based on the hypothesis that secondary metabolites with similar structures are biosynthesized by gene clusters that harbor certain homologous genes, such homologous genes could serve as suitable markers for distinct natural-product gene clusters (26, 51). A wide range of structurally diverse bioactive compounds are synthesized by polyketide synthase (PKS) and nonribosomal peptide synthetase (NRPS) systems in actinomycetes, therefore much attention has been given to revealing a previously unrecognized biosynthetic potential of actinomycetes through the genome mining of these genes (2, 3, 22). However, the broad distribution of PKS and NRPS genes and their high numbers even in a single actinomycete complicate their use (2, 3). To rationally exploit the genetic potential of actinomycetes, more and more special genes, such as tailoring enzyme genes, are being utilized for this sequence-guided genetic screening strategy (20, 38).Tailoring enzymes, which are responsible for the introduction and generation of diversity and bioactivity in several structural classes during or after NRPS, PKS, or NRPS/PKS assembly lines, usually include acyltransferases, aminotransferases, cyclases, glycosyltransferases, halogenases, ketoreductases, methyltransferases, and oxygenases (36, 45). Halogenation, an important feature for the bioactivity of a large number of distinct natural products (16, 18, 30), frequently is introduced by one type of halogenase, called reduced flavin adenine dinucleotide (FADH₂)-dependent (or flavin-dependent) halogenase (10, 12, 35). More than 4,000 halometabolites have been discovered (15), including commercially important antibiotics such as chloramphenicol, vancomycin, and teicoplanin (43).Previous investigations of FADH₂-dependent halogenase genes were focused largely on related gene clusters in the genera Amycolatopsis (33, 44, 53) and Streptomyces (8, 10, 21, 27, 32, 34, 47-49) and also on those in the genera Actinoplanes (25), Actinosynnema (50), Micromonospora (1), and Nonomuraea (39); however, none of these studies has led to the rest of the major families and genera of actinomycetes. In addition, there is evidence that FADH₂-dependent halogenase genes of streptomycetes usually exist in halometabolite biosynthetic gene clusters (20), but we lack knowledge of such genes and clusters in other actinomycetes.In the present study, we show that the distribution of the FADH₂-dependent halogenase gene in filamentous actinomycetes does indeed correlate with the potential for halometabolite production based on other genetic or physiological factors. We also showed that genome walking near the halogenase gene locus could be employed to identify closely linked gene clusters that likely encode pathways for organohalogen compound production in actinomycetes other than streptomycetes.     

Phylogenetic Analysis Indicates Evolutionary Diversity and Environmental Segregation of Marine Podovirus DNA Polymerase Gene Sequences

The distribution of viral genotypes in the ocean and their evolutionary relatedness remain poorly constrained. This paper presents data on the genetic diversity and evolutionary relationships of 1.2-kb DNA polymerase (pol) gene fragments from podoviruses. A newly designed set of PCR primers was used to amplify DNA directly from coastal sediment and water samples collected from inlets adjacent to the Strait of Georgia, British Columbia, Canada, and from the northeastern Gulf of Mexico. Restriction fragment length polymorphism analysis of 160 cloned PCR products revealed 29 distinct operational taxonomic units (OTUs), with OTUs within a site typically being more similar than those among sites. Phylogenetic analysis of the DNA pol gene fragments demonstrated high similarity between some environmental sequences and sequences from the marine podoviruses roseophage SIO1 and cyanophage P60, while others were not closely related to sequences from cultured phages. Interrogation of the CAMERA database for sequences from metagenomics data demonstrated that the amplified sequences were representative of the diversity of podovirus pol sequences found in marine samples. Our results indicate high genetic diversity within marine podovirus communities within a small geographic region and demonstrate that the diversity of environmental polymerase gene sequences for podoviruses is far more extensive than previously recognized.Marine viruses are the most abundant (41) and diverse (2, 6) biological entities in the ocean. They affect community composition by causing the lysis of specific subsets of the microbial community (22, 28, 46, 47) and, by killing numerically dominant host taxa, may influence species evenness and richness (24, 28, 43, 50). Despite the abundance of bacteriophages in marine systems and their important roles in marine microbial composition, little is known about the distribution and diversity of specific groups of marine viruses. However, most marine bacteriophage isolates are tailed phages (3) belonging to the order Caudovirales (27), which comprises the families Myoviridae, Podoviridae, and Siphoviridae.Podoviruses are classified into several groups (e.g., T7-like, P22-like, and phi-29-like) based on genome size, genome arrangement, and shared genes and can be readily isolated from seawater (11, 16, 42, 45). Genomic analysis of roseophage SIO1 (33), cyanophage P60 (7), vibriophage VpV262 (21), and cyanophage PSSP7 (40) suggests that many of the isolates are T7-like. Despite the apparently wide distribution of podoviruses in the sea, and their potential importance as agents of microbial mortality, there has been little effort to explore their diversity.Sequence analysis of representative genes is one approach that has been used to examine the genetic diversity of specific groups of marine viruses. For example, homologues for structural genes (g20 and g23) found in T4-like phages are found in some marine myoviruses (18, 20) and have been used to examine the distribution, diversity, and evolutionary relationships among marine myoviruses (12, 14, 17, 37, 38, 49). Other studies have used DNA polymerase (pol) to examine the diversity of viruses infecting eukaryotic phytoplankton (8, 38) and have shown that phylogenies constructed with this gene are congruent with established viral taxonomy (9, 36, 37).Although it is not universally present, family A DNA pol is a good target for examining the diversity of podoviruses (4). Our study presents a newly designed set of PCR primers that amplify a longer fragment of the DNA polymerase from a much larger suite of podoviruses and shows that the diversity within marine podoviruses as revealed by DNA pol sequences is far greater than previously realized.     

Inactivation of Vibrio anguillarum by Attached and Planktonic Roseobacter Cells

The purpose of the present study was to investigate the inhibition of Vibrio by Roseobacter in a combined liquid-surface system. Exposure of Vibrio anguillarum to surface-attached roseobacters (10⁷ CFU/cm²) resulted in significant reduction or complete killing of the pathogen inoculated at 10² to 10⁴ CFU/ml. The effect was likely associated with the production of tropodithietic acid (TDA), as a TDA-negative mutant did not affect survival or growth of V. anguillarum.Antagonistic interactions among marine bacteria are well documented, and secretion of antagonistic compounds is common among bacteria that colonize particles or surfaces (8, 13, 16, 21, 31). These marine bacteria may be interesting as sources for new antimicrobial drugs or as probiotic bacteria for aquaculture.Aquaculture is a rapidly growing sector, but outbreaks of bacterial diseases are a limiting factor and pose a threat, especially to young fish and invertebrates that cannot be vaccinated. Because regular or prophylactic administration of antibiotics must be avoided, probiotic bacteria are considered an alternative (9, 18, 34, 38, 39, 40). Several microorganisms have been able to reduce bacterial diseases in challenge trials with fish or fish larvae (14, 24, 25, 27, 33, 37, 39, 40). One example is Phaeobacter strain 27-4 (17), which inhibits Vibrio anguillarum and reduces mortality in turbot larvae (27). The antagonism of Phaeobacter 27-4 and the closely related Phaeobacter inhibens is due mainly to the sulfur-containing tropolone derivative tropodithietic acid (TDA) (2, 5), which is also produced by other Phaeobacter strains and Ruegeria mobilis (28). Phaeobacter and Ruegeria strains or their DNA has been commonly found in marine larva-rearing sites (6, 17, 28).Phaeobacter and Ruegeria (Alphaproteobacteria, Roseobacter clade) are efficient surface colonizers (7, 11, 31, 36). They are abundant in coastal and eutrophic zones and are often associated with algae (3, 7, 41). Surface-attached Phaeobacter bacteria may play an important role in determining the species composition of an emerging biofilm, as even low densities of attached Phaeobacter strain SK2.10 bacteria can prevent other marine organisms from colonizing solid surfaces (30, 32).In continuation of the previous research on roseobacters as aquaculture probiotics, the purpose of this study was to determine the antagonistic potential of Phaeobacter and Ruegeria against Vibrio anguillarum in liquid systems that mimic a larva-rearing environment. Since production of TDA in liquid marine broth appears to be highest when roseobacters form an air-liquid biofilm (5), we addressed whether they could be applied as biofilms on solid surfaces.     

Alignment of the c-Type Cytochrome OmcS along Pili of Geobacter sulfurreducens

Immunogold localization revealed that OmcS, a cytochrome that is required for Fe(III) oxide reduction by Geobacter sulfurreducens, was localized along the pili. The apparent spacing between OmcS molecules suggests that OmcS facilitates electron transfer from pili to Fe(III) oxides rather than promoting electron conduction along the length of the pili.There are multiple competing/complementary models for extracellular electron transfer in Fe(III)- and electrode-reducing microorganisms (8, 18, 20, 44). Which mechanisms prevail in different microorganisms or environmental conditions may greatly influence which microorganisms compete most successfully in sedimentary environments or on the surfaces of electrodes and can impact practical decisions on the best strategies to promote Fe(III) reduction for bioremediation applications (18, 19) or to enhance the power output of microbial fuel cells (18, 21).The three most commonly considered mechanisms for electron transfer to extracellular electron acceptors are (i) direct contact between redox-active proteins on the outer surfaces of the cells and the electron acceptor, (ii) electron transfer via soluble electron shuttling molecules, and (iii) the conduction of electrons along pili or other filamentous structures. Evidence for the first mechanism includes the necessity for direct cell-Fe(III) oxide contact in Geobacter species (34) and the finding that intensively studied Fe(III)- and electrode-reducing microorganisms, such as Geobacter sulfurreducens and Shewanella oneidensis MR-1, display redox-active proteins on their outer cell surfaces that could have access to extracellular electron acceptors (1, 2, 12, 15, 27, 28, 31-33). Deletion of the genes for these proteins often inhibits Fe(III) reduction (1, 4, 7, 15, 17, 28, 40) and electron transfer to electrodes (5, 7, 11, 33). In some instances, these proteins have been purified and shown to have the capacity to reduce Fe(III) and other potential electron acceptors in vitro (10, 13, 29, 38, 42, 43, 48, 49).Evidence for the second mechanism includes the ability of some microorganisms to reduce Fe(III) that they cannot directly contact, which can be associated with the accumulation of soluble substances that can promote electron shuttling (17, 22, 26, 35, 36, 47). In microbial fuel cell studies, an abundance of planktonic cells and/or the loss of current-producing capacity when the medium is replaced is consistent with the presence of an electron shuttle (3, 14, 26). Furthermore, a soluble electron shuttle is the most likely explanation for the electrochemical signatures of some microorganisms growing on an electrode surface (26, 46).Evidence for the third mechanism is more circumstantial (19). Filaments that have conductive properties have been identified in Shewanella (7) and Geobacter (41) species. To date, conductance has been measured only across the diameter of the filaments, not along the length. The evidence that the conductive filaments were involved in extracellular electron transfer in Shewanella was the finding that deletion of the genes for the c-type cytochromes OmcA and MtrC, which are necessary for extracellular electron transfer, resulted in nonconductive filaments, suggesting that the cytochromes were associated with the filaments (7). However, subsequent studies specifically designed to localize these cytochromes revealed that, although the cytochromes were extracellular, they were attached to the cells or in the exopolymeric matrix and not aligned along the pili (24, 25, 30, 40, 43). Subsequent reviews of electron transfer to Fe(III) in Shewanella oneidensis (44, 45) appear to have dropped the nanowire concept and focused on the first and second mechanisms.Geobacter sulfurreducens has a number of c-type cytochromes (15, 28) and multicopper proteins (12, 27) that have been demonstrated or proposed to be on the outer cell surface and are essential for extracellular electron transfer. Immunolocalization and proteolysis studies demonstrated that the cytochrome OmcB, which is essential for optimal Fe(III) reduction (15) and highly expressed during growth on electrodes (33), is embedded in the outer membrane (39), whereas the multicopper protein OmpB, which is also required for Fe(III) oxide reduction (27), is exposed on the outer cell surface (39).OmcS is one of the most abundant cytochromes that can readily be sheared from the outer surfaces of G. sulfurreducens cells (28). It is essential for the reduction of Fe(III) oxide (28) and for electron transfer to electrodes under some conditions (11). Therefore, the localization of this important protein was further investigated.     

A New Borrelia Species Defined by Multilocus Sequence Analysis of Housekeeping Genes

Analysis of Lyme borreliosis (LB) spirochetes, using a novel multilocus sequence analysis scheme, revealed that OspA serotype 4 strains (a rodent-associated ecotype) of Borrelia garinii were sufficiently genetically distinct from bird-associated B. garinii strains to deserve species status. We suggest that OspA serotype 4 strains be raised to species status and named Borrelia bavariensis sp. nov. The rooted phylogenetic trees provide novel insights into the evolutionary history of LB spirochetes.Multilocus sequence typing (MLST) and multilocus sequence analysis (MLSA) have been shown to be powerful and pragmatic molecular methods for typing large numbers of microbial strains for population genetics studies, delineation of species, and assignment of strains to defined bacterial species (4, 13, 27, 40, 44). To date, MLST/MLSA schemes have been applied only to a few vector-borne microbial populations (1, 6, 30, 37, 40, 41, 47).Lyme borreliosis (LB) spirochetes comprise a diverse group of zoonotic bacteria which are transmitted among vertebrate hosts by ixodid (hard) ticks. The most common agents of human LB are Borrelia burgdorferi (sensu stricto), Borrelia afzelii, Borrelia garinii, Borrelia lusitaniae, and Borrelia spielmanii (7, 8, 12, 35). To date, 15 species have been named within the group of LB spirochetes (6, 31, 32, 37, 38, 41). While several of these LB species have been delineated using whole DNA-DNA hybridization (3, 20, 33), most ecological or epidemiological studies have been using single loci (5, 9-11, 29, 34, 36, 38, 42, 51, 53). Although some of these loci have been convenient for species assignment of strains or to address particular epidemiological questions, they may be unsuitable to resolve evolutionary relationships among LB species, because it is not possible to define any outgroup. For example, both the 5S-23S intergenic spacer (5S-23S IGS) and the gene encoding the outer surface protein A (ospA) are present only in LB spirochete genomes (36, 43). The advantage of using appropriate housekeeping genes of LB group spirochetes is that phylogenetic trees can be rooted with sequences of relapsing fever spirochetes. This renders the data amenable to detailed evolutionary studies of LB spirochetes.LB group spirochetes differ remarkably in their patterns and levels of host association, which are likely to affect their population structures (22, 24, 46, 48). Of the three main Eurasian Borrelia species, B. afzelii is adapted to rodents, whereas B. valaisiana and most strains of B. garinii are maintained by birds (12, 15, 16, 23, 26, 45). However, B. garinii OspA serotype 4 strains in Europe have been shown to be transmitted by rodents (17, 18) and, therefore, constitute a distinct ecotype within B. garinii. These strains have also been associated with high pathogenicity in humans, and their finer-scale geographical distribution seems highly focal (10, 34, 52, 53).In this study, we analyzed the intra- and interspecific phylogenetic relationships of B. burgdorferi, B. afzelii, B. garinii, B. valaisiana, B. lusitaniae, B. bissettii, and B. spielmanii by means of a novel MLSA scheme based on chromosomal housekeeping genes (30, 48).     

Cultivation of Fastidious Bacteria by Viability Staining and Micromanipulation in a Soil Substrate Membrane System

Soil substrate membrane systems allow for microcultivation of fastidious soil bacteria as mixed microbial communities. We isolated established microcolonies from these membranes by using fluorescence viability staining and micromanipulation. This approach facilitated the recovery of diverse, novel isolates, including the recalcitrant bacterium Leifsonia xyli, a plant pathogen that has never been isolated outside the host.The majority of bacterial species have never been recovered in the laboratory (1, 14, 19, 24). In the last decade, novel cultivation approaches have successfully been used to recover “unculturables” from a diverse range of divisions (23, 25, 29). Most strategies have targeted marine environments (4, 23, 25, 32), but soil offers the potential for the investigation of vast numbers of undescribed species (20, 29). Rapid advances have been made toward culturing soil bacteria by reformulating and diluting traditional media, extending incubation times, and using alternative gelling agents (8, 21, 29).The soil substrate membrane system (SSMS) is a diffusion chamber approach that uses extracts from the soil of interest as the growth substrate, thereby mimicking the environment under investigation (12). The SSMS enriches for slow-growing oligophiles, a proportion of which are subsequently capable of growing on complex media (23, 25, 27, 30, 32). However, the SSMS results in mixed microbial communities, with the consequent difficulty in isolation of individual microcolonies for further characterization (10).Micromanipulation has been widely used for the isolation of specific cell morphotypes for downstream applications in molecular diagnostics or proteomics (5, 15). This simple technology offers the opportunity to select established microcolonies of a specific morphotype from the SSMS when combined with fluorescence visualization (3, 11). Here, we have combined the SSMS, fluorescence viability staining, and advanced micromanipulation for targeted isolation of viable, microcolony-forming soil bacteria.     

Proteorhodopsin-Bearing Bacteria in Antarctic Sea Ice

Proteorhodopsins (PRs) are widespread bacterial integral membrane proteins that function as light-driven proton pumps. Antarctic sea ice supports a complex community of autotrophic algae, heterotrophic bacteria, viruses, and protists that are an important food source for higher trophic levels in ice-covered regions of the Southern Ocean. Here, we present the first report of PR-bearing bacteria, both dormant and active, in Antarctic sea ice from a series of sites in the Ross Sea using gene-specific primers. Positive PR sequences were generated from genomic DNA at all depths in sea ice, and these sequences aligned with the classes Alphaproteobacteria, Gammaproteobacteria, and Flavobacteria. The sequences showed some similarity to previously reported PR sequences, although most of the sequences were generally distinct. Positive PR sequences were also observed from cDNA reverse transcribed from RNA isolated from sea ice samples. This finding indicates that these sequences were generated from metabolically active cells and suggests that the PR gene is functional within sea ice. Both blue-absorbing and green-absorbing forms of PRs were detected, and only a limited number of blue-absorbing forms were found and were in the midsection of the sea ice profile in this study. Questions still remain regarding the protein''s ecological functions, and ultimately, field experiments will be needed to establish the ecological and functional role of PRs in the sea ice ecosystem.Proteorhodopsins (PRs) are retinal binding bacterial integral membrane proteins that function as light-driven proton pumps (9, 10) and belong to the microbial rhodopsin superfamily of proteins (54). Since the first reported PR sequence from members of SAR86 clade marine (class Gammaproteobacteria) in 2000 (9), many other PR-bearing bacteria have been identified in a range of marine habitats (5, 18, 20, 24, 25, 46, 62). In the recent Global Ocean Sampling (GOS) expedition, almost 4,000 PR sequences from 41 distinct surface marine environments were acquired, demonstrating that these PR genes are extremely abundant in the genomes of ocean bacterioplankton (46). In fact, PR-containing bacteria account for 13% of the community in the Mediterranean Sea and Red Sea and 70% of the community in the Sargasso Sea (18, 46, 49, 60). These light-harvesting bacteria are present in three major marine classes of bacteria: the Alphaproteobacteria, Gammaproteobacteria, and Flavobacteria. In addition, two distinct PR genes encode pigments with “blue-absorbing” and “green-absorbing” properties, which is achieved by a substitution at a single amino acid position, which thereby functions as a spectral tuning switch (10, 37, 48).Sea ice represents a complex physicochemical environment in polar regions and covers up to 13% of the Earth''s surface (59). Although extreme gradients of temperature, salinity, nutrient availability, and light stratify the ice matrix from the surface to the ice-water interface (41), the sea ice habitat nevertheless supports a diverse microbial community of phytoplankton, Bacteria, Archaea, viruses, and protists that grow in liquid brine channels within the ice (14, 35, 56). This sea ice microbial community (SIMCO) is highly metabolically active despite being unable to avoid the extreme environmental conditions that they experience (39). In fact, very-high-standing stocks of the SIMCO exist in many regions of the Southern Ocean. For example, the concentration of chlorophyll a, a proxy for microalgal biomass, typically reaches 200 mg m⁻² in the Ross Sea, while the concentration of chlorophyll a in the water column below is approximately 2 orders of magnitude less (47), and the percentage of metabolically active bacteria (32% [39]) is significantly higher than the 10% observed for temperate marine systems (36). The SIMCO is thus a major source of biomass in ice-covered regions of the Southern Ocean (59), providing a critical food source for grazing zooplankton (and, consequently, also for higher trophic levels) for much of the year (3, 59). This biomass is of particular importance during the darkness of the polar winter, where the bottom-ice community is the only available food source for juvenile krill. These grazers absolutely rely on the sea ice microbial community to survive, as the water lacks other food sources (6, 28).In the past decade, reports of the widespread occurrence of bacteriochlorophyll and PR pigments in planktonic marine bacteria have challenged the assumption that chlorophyll a is the only principal light-capturing pigment in ocean surface waters. These alternative pigments may in fact play a critical role in light energy harvesting for microbial metabolism in various aquatic ecosystems (5, 10, 25, 40, 49). It has been proposed that energy, rather than nutrient conservation, is important for the regulation of productivity (7). PR-containing phototrophic eubacteria could play a significant role in the energy budget of cells in the photic zone in marine environments (15). PR sequences have been detected in the Southern Ocean (9), but to our knowledge, there have been no reports of PR-bearing bacteria within the sea ice matrix.The majority of the microbial rhodopsin genes found in oceanic samples have been detected by environmental sequencing (30, 46, 48, 60). We have used degenerate PR gene primers (5) in this study to positively identify PR-bearing operational taxonomic units (OTUs) from sea ice. Also, specific bacterial mRNA can now be detected from extracted nucleic acids and used to examine gene expression and, thus, infer metabolic activity (8). With this in mind, we have generated cDNA from RNA extracted from sea ice samples. From these observations, we deduce that PR-bearing bacteria are present in sea ice and may be actively contributing to the ecosystem within this extreme microenvironment.     

Population Structure of the Lyme Borreliosis Spirochete Borrelia burgdorferi in the Western Black-Legged Tick (Ixodes pacificus) in Northern California

Factors potentially contributing to the lower incidence of Lyme borreliosis (LB) in the far-western than in the northeastern United States include tick host-seeking behavior resulting in fewer human tick encounters, lower densities of Borrelia burgdorferi-infected vector ticks in peridomestic environments, and genetic variation among B. burgdorferi spirochetes to which humans are exposed. We determined the population structure of B. burgdorferi in over 200 infected nymphs of the primary bridging vector to humans, Ixodes pacificus, collected in Mendocino County, CA. This was accomplished by sequence typing the spirochete lipoprotein ospC and the 16S-23S rRNA intergenic spacer (IGS). Thirteen ospC alleles belonging to 12 genotypes were found in California, and the two most abundant, ospC genotypes H3 and E3, have not been detected in ticks in the Northeast. The most prevalent ospC and IGS biallelic profile in the population, found in about 22% of ticks, was a new B. burgdorferi strain defined by ospC genotype H3. Eight of the most common ospC genotypes in the northeastern United States, including genotypes I and K that are associated with disseminated human infections, were absent in Mendocino County nymphs. ospC H3 was associated with hardwood-dominated habitats where western gray squirrels, the reservoir host, are commonly infected with LB spirochetes. The differences in B. burgdorferi population structure in California ticks compared to the Northeast emphasize the need for a greater understanding of the genetic diversity of spirochetes infecting California LB patients.In the United States, Lyme borreliosis (LB) is the most commonly reported vector-borne illness and is caused by infection with the spirochete Borrelia burgdorferi (3, 9, 52). The signs and symptoms of LB can include a rash, erythema migrans, fever, fatigue, arthritis, carditis, and neurological manifestations (50, 51). The black-legged tick, Ixodes scapularis, and the western black-legged tick, Ixodes pacificus, are the primary vectors of B. burgdorferi to humans in the United States, with the former in the northeastern and north-central parts of the country and the latter in the Far West (9, 10). These ticks perpetuate enzootic transmission cycles together with a vertebrate reservoir host such as the white-footed mouse, Peromyscus leucopus, in the Northeast and Midwest (24, 35), or the western gray squirrel, Sciurus griseus, in California (31, 46).B. burgdorferi is a spirochete species with a largely clonal population structure (14, 16) comprising several different strains or lineages (8). The polymorphic ospC gene of B. burgdorferi encodes a surface lipoprotein that increases expression within the tick during blood feeding (47) and is required for initial infection of mammalian hosts (25, 55). To date, approximately 20 North American ospC genotypes have been described (40, 45, 49, 56). At least four, and possibly up to nine, of these genotypes are associated with B. burgdorferi invasiveness in humans (1, 15, 17, 49, 57). Restriction fragment length polymorphism (RFLP) and, subsequently, sequence analysis of the 16S-23S rRNA intergenic spacer (IGS) are used as molecular typing tools to investigate genotypic variation in B. burgdorferi (2, 36, 38, 44, 44, 57). The locus maintains a high level of variation between related species, and this variation reflects the heterogeneity found at the genomic level of the organism (37). The IGS and ospC loci appear to be linked (2, 8, 26, 45, 57), but the studies to date have not been representative of the full range of diversity of B. burgdorferi in North America.Previous studies in the northeastern and midwestern United States have utilized IGS and ospC genotyping to elucidate B. burgdorferi evolution, host strain specificity, vector-reservoir associations, and disease risk to humans. In California, only six ospC and five IGS genotypes have been described heretofore in samples from LB patients or I. pacificus ticks (40, 49, 56) compared to approximately 20 ospC and IGS genotypes identified in ticks, vertebrate hosts, or humans from the Northeast and Midwest (8, 40, 45, 49, 56). Here, we employ sequence analysis of both the ospC gene and IGS region to describe the population structure of B. burgdorferi in more than 200 infected I. pacificus nymphs from Mendocino County, CA, where the incidence of LB is among the highest in the state (11). Further, we compare the Mendocino County spirochete population to populations found in the Northeast.     

Vertical Distribution of Ammonia-Oxidizing Crenarchaeota and Methanogens in the Epipelagic Waters of Lake Kivu (Rwanda-Democratic Republic of the Congo)

Four stratified basins in Lake Kivu (Rwanda-Democratic Republic of the Congo) were sampled in March 2007 to investigate the abundance, distribution, and potential biogeochemical role of planktonic archaea. We used fluorescence in situ hybridization with catalyzed-reported deposition microscopic counts (CARD-FISH), denaturing gradient gel electrophoresis (DGGE) fingerprinting, and quantitative PCR (qPCR) of signature genes for ammonia-oxidizing archaea (16S rRNA for marine Crenarchaeota group 1.1a [MCG1] and ammonia monooxygenase subunit A [amoA]). Abundance of archaea ranged from 1 to 4.5% of total DAPI (4′,6-diamidino-2-phenylindole) counts with maximal concentrations at the oxic-anoxic transition zone (∼50-m depth). Phylogenetic analysis of the archaeal planktonic community revealed a higher level of richness of crenarchaeal 16S rRNA gene sequences (21 of the 28 operational taxonomic units [OTUs] identified [75%]) over euryarchaeotal ones (7 OTUs). Sequences affiliated with the kingdom Euryarchaeota were mainly recovered from the anoxic water compartment and mostly grouped into methanogenic lineages (Methanosarcinales and Methanocellales). In turn, crenarchaeal phylotypes were recovered throughout the sampled epipelagic waters (0- to 100-m depth), with clear phylogenetic segregation along the transition from oxic to anoxic water masses. Thus, whereas in the anoxic hypolimnion crenarchaeotal OTUs were mainly assigned to the miscellaneous crenarchaeotic group, the OTUs from the oxic-anoxic transition and above belonged to Crenarchaeota groups 1.1a and 1.1b, two lineages containing most of the ammonia-oxidizing representatives known so far. The concomitant vertical distribution of both nitrite and nitrate maxima and the copy numbers of both MCG1 16S rRNA and amoA genes suggest the potential implication of Crenarchaeota in nitrification processes occurring in the epilimnetic waters of the lake.Lake Kivu is a meromictic lake located in the volcanic region between Rwanda and the Democratic Republic of the Congo and is the smallest of the African Great Rift Lakes. The monimolimnion of the lake contains a large amount of dissolved CO₂ and methane (300 km³ and 60 km³, respectively) as a result of geological and biological activity (24, 73, 85). This massive accumulation converts Lake Kivu into one of the largest methane reservoirs in the world and into a unique ecosystem for geomicrobiologists interested in the methane cycle and in risk assessment and management (34, 71, 72, 85). Comprehensive studies on the diversity and activity of planktonic populations of both large and small eukaryotes and their trophic interplay operating in the epilimnetic waters of the lake are available (33, 39, 49). Recent surveys have also provided a deeper insight into the seasonal variations of photosynthetic and heterotrophic picoplankton (67, 68), although very few data exist on the composition, diversity, and spatial distribution of bacterial and archaeal communities. In this regard, the studies conducted so far of the bacterial/archaeal ecology in Lake Kivu have been mostly focused on the implications on the methane cycle (34, 73), but none have addressed the presence and distribution of additional archaeal populations in the lake.During the last few years, microbial ecology studies carried out in a wide variety of habitats have provided compelling evidence of the ubiquity and abundance of mesophilic archaea (4, 10, 13, 19). Moreover, the discovery of genes encoding enzymes related to nitrification and denitrification in archaeal metagenomes from soil and marine waters (29, 86, 88) and the isolation of the first autotrophic archaeal nitrifier (40) demonstrated that some archaeal groups actively participate in the carbon and nitrogen cycles (56, 64, 69). In relation to aquatic environments, genetic markers of ammonia-oxidizing archaea (AOA) of the marine Crenarchaeota group 1.1a (MCG1) have consistently been found in water masses of several oceanic regions (6, 14, 17, 26, 28, 30, 37, 42, 51, 52, 89), estuaries (5, 9, 26, 53), coastal aquifers (26, 66), and stratified marine basins (15, 41, 44). Although less information is available for freshwater habitats, recent studies carried out in oligotrophic high-mountain and arctic lakes showed an important contribution of AOA in both the planktonic and the neustonic microbial assemblages (4, 61, 89).The oligotrophic nature of Lake Kivu and the presence of a well-defined redoxcline may provide an optimal niche for the development of autotrophic AOA populations. Unfortunately, no studies of the involvement of microbial planktonic populations in cycling nitrogen in the lake exist, and only data on the distribution of dissolved inorganic nitrogen species in relation to phytoplankton ecology (67, 68) and nutrient loading are available (54, 58). Our goals here were to ascertain whether or not archaeal populations other than methane-related lineages were relevant components of the planktonic microbial community and to determine whether the redox gradient imposed by the oxic-anoxic interphase acts as a threshold for their vertical distribution in epipelagic waters (0- to 100-m depth). To further explore the presence and potential activity of nitrifying archaeal populations in Lake Kivu, samples were analyzed for the abundance and vertical distribution of signature genes for these microorganisms, i.e., the 16S rRNA of MCG1 and the ammonia monooxygenase subunit A (amoA) gene by quantitative PCR.     

High Abundance of Ammonia-Oxidizing Archaea in Coastal Waters,Determined Using a Modified DNA Extraction Method

Molecular characterizations of environmental microbial populations based on recovery and analysis of DNA generally assume efficient or unbiased extraction of DNA from different sample matrices and microbial groups. Appropriate controls to verify this basic assumption are rarely included. Here three different DNA extractions, performed with two commercial kits (FastDNA and UltraClean) and a standard phenol-chloroform method, and two alternative filtration methods (Sterivex and 25-mm-diameter polycarbonate filters) were evaluated, using the addition of Nitrosopumilus maritimus cells to track the recovery of DNA from marine Archaea. After the comparison, a simplified phenol-chloroform extraction method was developed and shown to be significantly superior, in terms of both the recovery and the purity of DNA, to other protocols now generally applied to environmental studies. The simplified and optimized method was used to quantify ammonia-oxidizing Archaea at different depth intervals in a fjord (Hood Canal) by quantitative PCR. The numbers of Archaea increased with depth, often constituting as much as 20% of the total bacterial community.Efficient DNA extraction from environmental samples is fundamental to many culture-independent characterizations (10). Thus, there was an early and concerted effort to establish appropriate methods of DNA extraction from different types of environmental samples (14, 19, 25, 30, 34, 43, 47). DNA extraction efficiency is particularly important for quantitative PCR (qPCR), because poor DNA extraction efficiency results in the underestimation of gene copy numbers in the samples examined (6, 42).Most methodological developments addressed DNA extraction from soil and sediment samples, with fewer comparative studies of the efficiency of collection and extraction from water samples (4, 13, 40). In part, a methodological focus on soils reflected the simplicity of filtration to collect aquatic populations and the generally good recovery of DNA from the Gram-negative bacteria making up a significant fraction of aquatic communities. However, small Archaea are now known to constitute a substantial fraction of the prokaryotic populations in marine and terrestrial systems (2, 7, 9, 20, 26, 31, 33, 45). Since the archaeal cell wall and membrane structures are distinct from those of bacteria, there is no assurance that commonly used extraction methods are adequate. With increasing reliance on commercially available bead-beating-type DNA extraction kits, these methods are now often used for different water samples (1, 5-7, 14, 19, 36). Although most protocols incorporate mechanical disruption to ensure more-uniform extraction than is possible by using methods that rely entirely on enzymatic digestion and/or chemical disruption (4, 13, 40), the suitability of these protocols for the concerted analysis of archaeal and bacterial populations has not been fully evaluated.In the studies reported here, the recently isolated marine archaeon Nitrosopumilus maritimus strain SCM1 (22) was therefore used as a reference standard for evaluation of the commonly employed DNA extraction methods by using qPCR. This archaeon was then used as a reference for the development of a simple, rapid, and efficient method of extracting DNA from both archaeal and bacterial cells. The modified protocol was subsequently employed to characterize the vertical distribution of ammonia-oxidizing Archaea in a fjord (Hood Canal) in Puget Sound (Washington State), revealing a high fractional representation of Archaea relative to Bacteria not observed previously in coastal waters.     

mcrA-Targeted Real-Time Quantitative PCR Method To Examine Methanogen Communities

Methanogens are of great importance in carbon cycling and alternative energy production, but quantitation with culture-based methods is time-consuming and biased against methanogen groups that are difficult to cultivate in a laboratory. For these reasons, methanogens are typically studied through culture-independent molecular techniques. We developed a SYBR green I quantitative PCR (qPCR) assay to quantify total numbers of methyl coenzyme M reductase α-subunit (mcrA) genes. TaqMan probes were also designed to target nine different phylogenetic groups of methanogens in qPCR assays. Total mcrA and mcrA levels of different methanogen phylogenetic groups were determined from six samples: four samples from anaerobic digesters used to treat either primarily cow or pig manure and two aliquots from an acidic peat sample stored at 4°C or 20°C. Only members of the Methanosaetaceae, Methanosarcina, Methanobacteriaceae, and Methanocorpusculaceae and Fen cluster were detected in the environmental samples. The three samples obtained from cow manure digesters were dominated by members of the genus Methanosarcina, whereas the sample from the pig manure digester contained detectable levels of only members of the Methanobacteriaceae. The acidic peat samples were dominated by both Methanosarcina spp. and members of the Fen cluster. In two of the manure digester samples only one methanogen group was detected, but in both of the acidic peat samples and two of the manure digester samples, multiple methanogen groups were detected. The TaqMan qPCR assays were successfully able to determine the environmental abundance of different phylogenetic groups of methanogens, including several groups with few or no cultivated members.Methanogens are integral to carbon cycling, catalyzing the production of methane and carbon dioxide, both potent greenhouse gases, during organic matter degradation in anaerobic soils and sediment (8). Methanogens are widespread in anaerobic environments, including tundra (36), freshwater lake and wetland sediments (9, 12), estuarine and marine sediments (2), acidic peatlands (4, 14), rice field soil (10, 16), animal guts (41), landfills (30), and anaerobic digesters treating animal manure (1), food processing wastewater (27), and municipal wastewater and solid waste (37, 57). Methane produced in anaerobic digesters may be captured and used for energy production, thus offsetting some or all of the cost of operation and reducing the global warming potential of methane release to the atmosphere.Methanogens are difficult to study through culture-based methods, and therefore many researchers have instead used culture-independent techniques to study methanogen populations. The 16S rRNA gene is the most widely used target for gene surveys, and a number of primers and probes have been developed to target methanogen groups (9, 11, 31, 36, 38, 40, 46, 48, 57). To eliminate potential problems with nonspecific amplification, some researchers have developed primers for the gene sequence of the α-subunit of the methyl coenzyme M reductase (mcrA) (17, 30, 49). The Mcr is exclusive to the methanogens with the exception of the methane-oxidizing Archaea (18) and shows mostly congruent phylogeny to the 16S rRNA gene, allowing mcrA analysis to be used in conjunction with, or independently of, that of the 16S rRNA gene (3, 30, 49). A number of researchers have examined methanogen communities with mcrA and have found uncultured clades quite different in sequence from cultured methanogen representatives (9, 10, 12, 14, 17, 22, 28, 47).Previous studies described methanogen communities by quantitation of different clades through the use of rRNA-targeted or rRNA gene-targeted probes with techniques such as dot blot hybridization (1, 27, 37, 38, 48) and fluorescent in situ hybridization (11, 40, 44, 57). Real-time quantitative PCR (qPCR) is an alternate technique capable of determining the copy number of a particular gene present in the DNA extracted from an environmental sample. Only a few studies have used qPCR to quantitatively examine different clades within methanogen communities, and most of these studies have exclusively targeted the 16S rRNA gene (19, 41, 42, 54-56). Far fewer researchers have used qPCR to quantify methanogen clades by targeting the mcrA (21, 34, 45), and these studies were limited to only a few phylogenetic groups.In this paper we present a methodology for determining methanogen gene copy numbers through the use of qPCR targeting the mcrA. Methanogens were quantified in total using methanogen-specific primers in SYBR green assays and also as members of nine different phylogenetic groups using TaqMan probes targeting specific subsets of methanogens.     

Cultivation of Autotrophic Ammonia-Oxidizing Archaea from Marine Sediments in Coculture with Sulfur-Oxidizing Bacteria

The role of ammonia-oxidizing archaea (AOA) in nitrogen cycling in marine sediments remains poorly characterized. In this study, we enriched and characterized AOA from marine sediments. Group I.1a crenarchaea closely related to those identified in marine sediments and “Candidatus Nitrosopumilus maritimus” (99.1 and 94.9% 16S rRNA and amoA gene sequence identities to the latter, respectively) were substantially enriched by coculture with sulfur-oxidizing bacteria (SOB). The selective enrichment of AOA over ammonia-oxidizing bacteria (AOB) is likely due to the reduced oxygen levels caused by the rapid initial growth of SOB. After biweekly transfers for ca. 20 months, archaeal cells became the dominant prokaryotes (>80%), based on quantitative PCR and fluorescence in situ hybridization analysis. The increase of archaeal 16S rRNA gene copy numbers was coincident with the amount of ammonia oxidized, and expression of the archaeal amoA gene was observed during ammonia oxidation. Bacterial amoA genes were not detected in the enrichment culture. The affinities of these AOA to oxygen and ammonia were substantially higher than those of AOB. [¹³C]bicarbonate incorporation and the presence and activation of genes of the 3-hydroxypropionate/4-hydroxybutyrate cycle indicated autotrophy during ammonia oxidation. In the enrichment culture, ammonium was oxidized to nitrite by the AOA and subsequently to nitrate by Nitrospina-like bacteria. Our experiments suggest that AOA may be important nitrifiers in low-oxygen environments, such as oxygen-minimum zones and marine sediments.Archaea have long been known as extremophiles, since most cultivated archaeal strains were cultivated from extreme environments, such as acidic, hot, and high-salt environments. The view of archaea as extremophiles (i.e., acidophiles, thermophiles, and halophiles) has radically changed by the application of molecular technologies, including PCR in environmental microbiology. Using Archaea-specific PCR primers, novel archaeal 16S rRNA gene sequences were discovered in seawater (23, 27). Following these discoveries, an ever-increasing and unexpectedly high variety of archaeal 16S rRNA gene sequences has been reported from diverse “nonextreme” environments (67). This indicates that archaea are, like bacteria, ubiquitous in the biosphere rather than exclusively inhabiting specific extreme niches. Archaea are abundant in water columns of some oceanic provinces (33, 36) and deep-subsea floor sediments (11, 12, 48). Despite the increasing number of reports of the diversity and abundance of these nonextreme archaea by molecular ecological studies, their physiology and ecological roles have remained enigmatic.Oxidation of ammonia, a trait long thought to be exclusive to the domain Bacteria (13), was recently suggested to be a trait of archaea of the crenarchaeal groups I.1a and I.1b, based on a metagenome analysis (79) and supported by the discovery of archaeal amoA-like genes in environmental shotgun sequencing studies of Sargasso Sea water (80) and genomic analysis of “Candidatus Cenarchaeum symbiosum,” a symbiont of a marine sponge (30). Molecular ecological studies indicated that these ammonia-oxidizing archaea (AOA) are often predominant over ammonia-oxidizing bacteria (AOB) in ocean waters (9, 53, 87), soils (17, 47), and marine sediments (61). Critical evidence for autotrophic archaeal ammonia oxidation was obtained by the characterization of the first cultivated mesophilic crenarchaeon (group I.1a), “Candidatus Nitrosopumilus maritimus SCM1,” from an aquarium (38), and a related archaeon from North Sea water (87) and subsequently by enrichment of thermophilic AOA (22, 31). Whole-genome-based phylogenetic studies recently indicated that the nonthermophilic crenarchaea, including the AOA, likely form a phylum separate from the Crenarchaeota and Euryarchaeota phyla (15, 16, 72). This proposed new phylum was called Thaumarchaeota (15).Microorganisms in marine sediments contribute significantly to global biogeochemical cycles because of their abundance (85). Nitrification is essential to the nitrogen cycle in marine sediments and may be metabolically coupled with denitrification and anaerobic ammonium oxidation, resulting in the removal of nitrogen as molecular nitrogen and the generation of greenhouse gases, such as nitrous oxide (19, 75). Compared with studies on archaeal nitrification in the marine water column, only limited information on archaeal nitrification in marine sediments is available so far. Archaeal amoA genes have been retrieved from marine and coastal sediments (8, 26, 61), and the potentially important role of AOA in nitrification has been suggested based on the abundance of archaeal amoA genes relative to that of bacterial amoA genes in surface marine sediments from Donghae (South Korea) (61). Cultivation of AOA, although difficult (38), remains essential to estimating the metabolic potential of archaea in environments such as soils (47) and marine sediments (61). Here, we report the successful enrichment of AOA of crenarchaeal group I.1a from marine sediments by employing a coculture with sulfur-oxidizing bacteria (SOB) which was maintained for ca. 20 months with biweekly transfers. In this way, we were able to characterize AOA from marine sediments, providing a clue for the role of AOA in the nitrogen cycle of marine sediments.     

Cell-to-Cell Spread of the RNA Interference Response Suppresses Semliki Forest Virus (SFV) Infection of Mosquito Cell Cultures and Cannot Be Antagonized by SFV

In their vertebrate hosts, arboviruses such as Semliki Forest virus (SFV) (Togaviridae) generally counteract innate defenses and trigger cell death. In contrast, in mosquito cells, following an early phase of efficient virus production, a persistent infection with low levels of virus production is established. Whether arboviruses counteract RNA interference (RNAi), which provides an important antiviral defense system in mosquitoes, is an important question. Here we show that in Aedes albopictus-derived mosquito cells, SFV cannot prevent the establishment of an antiviral RNAi response or prevent the spread of protective antiviral double-stranded RNA/small interfering RNA (siRNA) from cell to cell, which can inhibit the replication of incoming virus. The expression of tombusvirus siRNA-binding protein p19 by SFV strongly enhanced virus spread between cultured cells rather than virus replication in initially infected cells. Our results indicate that the spread of the RNAi signal contributes to limiting virus dissemination.In animals, RNA interference (RNAi) was first described for Caenorhabditis elegans (27). The production or introduction of double-stranded RNA (dsRNA) in cells leads to the degradation of mRNAs containing homologous sequences by sequence-specific cleavage of mRNAs. Central to RNAi is the production of 21- to 26-nucleotide small interfering RNAs (siRNAs) from dsRNA and the assembly of an RNA-induced silencing complex (RISC), followed by the degradation of the target mRNA (23, 84). RNAi is a known antiviral strategy of plants (3, 53) and insects (21, 39, 51). Study of Drosophila melanogaster in particular has given important insights into RNAi responses against pathogenic viruses and viral RNAi inhibitors (31, 54, 83, 86, 91). RNAi is well characterized for Drosophila, and orthologs of antiviral RNAi genes have been found in Aedes and Culex spp. (13, 63).Arboviruses, or arthropod-borne viruses, are RNA viruses mainly of the families Bunyaviridae, Flaviviridae, and Togaviridae. The genus Alphavirus within the family Togaviridae contains several mosquito-borne pathogens: arboviruses such as Chikungunya virus (16) and equine encephalitis viruses (88). Replication of the prototype Sindbis virus and Semliki Forest virus (SFV) is well understood (44, 71, 74, 79). Their genome consists of a positive-stranded RNA with a 5′ cap and a 3′ poly(A) tail. The 5′ two-thirds encodes the nonstructural polyprotein P1234, which is cleaved into four replicase proteins, nsP1 to nsP4 (47, 58, 60). The structural polyprotein is encoded in the 3′ one-third of the genome and cleaved into capsid and glycoproteins after translation from a subgenomic mRNA (79). Cytoplasmic replication complexes are associated with cellular membranes (71). Viruses mature by budding at the plasma membrane (35).In nature, arboviruses are spread by arthropod vectors (predominantly mosquitoes, ticks, flies, and midges) to vertebrate hosts (87). Little is known about how arthropod cells react to arbovirus infection. In mosquito cell cultures, an acute phase with efficient virus production is generally followed by the establishment of a persistent infection with low levels of virus production (9). This is fundamentally different from the cytolytic events following arbovirus interactions with mammalian cells and pathogenic insect viruses with insect cells. Alphaviruses encode host response antagonists for mammalian cells (2, 7, 34, 38).RNAi has been described for mosquitoes (56) and, when induced before infection, antagonizes arboviruses and their replicons (1, 4, 14, 15, 29, 30, 32, 42, 64, 65). RNAi is also functional in various mosquito cell lines (1, 8, 43, 49, 52). In the absence of RNAi, alphavirus and flavivirus replication and/or dissemination is enhanced in both mosquitoes and Drosophila (14, 17, 31, 45, 72). RNAi inhibitors weakly enhance SFV replicon replication in tick and mosquito cells (5, 33), posing the questions of how, when, and where RNAi interferes with alphavirus infection in mosquito cells.Here we use an A. albopictus-derived mosquito cell line to study RNAi responses to SFV. Using reporter-based assays, we demonstrate that SFV cannot avoid or efficiently inhibit the establishment of an RNAi response. We also demonstrate that the RNAi signal can spread between mosquito cells. SFV cannot inhibit cell-to-cell spread of the RNAi signal, and spread of the virus-induced RNAi signal (dsRNA/siRNA) can inhibit the replication of incoming SFV in neighboring cells. Furthermore, we show that SFV expression of a siRNA-binding protein increases levels of virus replication mainly by enhancing virus spread between cells rather than replication in initially infected cells. Taken together, these findings suggest a novel mechanism, cell-to-cell spread of antiviral dsRNA/siRNA, by which RNAi limits SFV dissemination in mosquito cells.     

Effects of Ammonium and Nitrite on Growth and Competitive Fitness of Cultivated Methanotrophic Bacteria

The effects of nitrite and ammonium on cultivated methanotrophic bacteria were investigated. Methylomicrobium album ATCC 33003 outcompeted Methylocystis sp. strain ATCC 49242 in cultures with high nitrite levels, whereas cultures with high ammonium levels allowed Methylocystis sp. to compete more easily. M. album pure cultures and cocultures consumed nitrite and produced nitrous oxide, suggesting a connection between denitrification and nitrite tolerance.The application of ammonium-based fertilizers has been shown to immediately reduce the uptake of methane in a number of diverse ecological systems (3, 5, 7, 8, 11-13, 16, 27, 28), due likely to competitive inhibition of methane monooxygenase enzymes by ammonia and production of nitrite (1). Longer-term inhibition of methane uptake by ammonium has been attributed to changes in methanotrophic community composition, often favoring activity and/or growth of type I Gammaproteobacteria methanotrophs (i.e., Gammaproteobacteria methane-oxidizing bacteria [gamma-MOB]) over type II Alphaproteobacteria methanotrophs (alpha-MOB) (19-23, 25, 26, 30). It has been argued previously that gamma-MOB likely thrive in the presence of high N loads because they rapidly assimilate N and synthesize ribosomes whereas alpha-MOB thrive best under conditions of N limitation and low oxygen levels (10, 21, 23).Findings from studies with rice paddies indicate that N fertilization stimulates methane oxidation through ammonium acting as a nutrient, not as an inhibitor (2). Therefore, the actual effect of ammonium on growth and activity of methanotrophs depends largely on how much ammonia-N is used for assimilation versus cometabolism. Many methanotrophs can also oxidize ammonia into nitrite via hydroxylamine (24, 29). Nitrite was shown previously to inhibit methane consumption by cultivated methanotrophs and by organisms in soils through an uncharacterized mechanism (9, 17, 24), although nitrite inhibits purified formate dehydrogenase from Methylosinus trichosporium OB3b (15). Together, the data from these studies show that ammonium and nitrite have significant effects on methanotroph activity and community composition and reveal the complexity of ammonia as both a nutrient and a competitive inhibitor. The present study demonstrates the differential influences of high ammonium or nitrite loads on the competitive fitness of a gamma-MOB versus an alpha-MOB strain.     

High Ratio of Bacteriochlorophyll Biosynthesis Genes to Chlorophyll Biosynthesis Genes in Bacteria of Humic Lakes

Recent studies highlight the diversity and significance of marine phototrophic microorganisms such as picocyanobacteria, phototrophic picoeukaryotes, and bacteriochlorophyll- and rhodopsin-holding phototrophic bacteria. To assess if freshwater ecosystems also harbor similar phototroph diversity, genes involved in the biosynthesis of bacteriochlorophyll and chlorophyll were targeted to explore oxygenic and aerobic anoxygenic phototroph composition in a wide range of lakes. Partial dark-operative protochlorophyllide oxidoreductase (DPOR) and chlorophyllide oxidoreductase (COR) genes in bacteria of seven lakes with contrasting trophic statuses were PCR amplified, cloned, and sequenced. Out of 61 sequences encoding the L subunit of DPOR (L-DPOR), 22 clustered with aerobic anoxygenic photosynthetic bacteria, whereas 39 L-DPOR sequences related to oxygenic phototrophs, like cyanobacteria, were observed. Phylogenetic analysis revealed clear separation of these freshwater L-DPOR genes as well as 11 COR gene sequences from their marine counterparts. Terminal restriction fragment length analysis of L-DPOR genes was used to characterize oxygenic aerobic and anoxygenic photosynthesizing populations in 20 lakes differing in physical and chemical characteristics. Significant differences in L-DPOR community composition were observed between dystrophic lakes and all other systems, where a higher proportion of genes affiliated with aerobic anoxygenic photosynthetic bacteria was observed than in other systems. Our results reveal a significant diversity of phototrophic microorganisms in lakes and suggest niche partitioning of oxygenic and aerobic anoxygenic phototrophs in these systems in response to trophic status and coupled differences in light regime.Recent studies have discovered novel phototrophic organisms and pointed us to their diversity in the oceans (1, 2, 3, 27, 39, 47, 50). Microorganisms such as picocyanobacteria, picoeukaryotes, and bacteriochlorophyll- and rhodopsin-containing bacteria use diverse photopigments to photosynthesize. These organisms represent a significant fraction of marine microbial communities and are likely to be ecologically and biogeochemically significant (1, 2, 13, 27, 28, 35, 39, 47). Several molecular studies based on genes of the puf operon, coding for the bacteriochlorophyll subunits, have shown that Roseobacter and Roseobacter-like bacteria constitute a significant portion of the aerobic anoxygenic photosynthetic bacteria (AAnPB) in marine waters (37). Microscopic counts have revealed that AAnPB contribute 1 to 16% to the total marine bacterioplankton in the euphotic zone and that there are regional and temporal differences in their abundances (see, for example, references 28, 41, and 50). Still, the global significance of this functional group and the role of, for example, AAnPB in the oceanic flow of energy and carbon are controversial (13, 20, 27, 28, 41, 48). Most AAnPB isolated so far have been described as photoorganoheterotrophs that rely primarily on organic substrates for growth but can derive a significant portion of their energy requirements from solar radiation (references 13 and 26 and references therein).AAnPB have been isolated from various freshwater habitats, ranging from cyanobacterial mats (49) to the pelagic zone of oligotrophic lakes (19, 38), but there are so far no studies of freshwater AAnPB diversity and community composition based on culture-independent techniques. A recent survey revealed some first patterns in the distribution of bacteriochlorophyll a-containing cells as well as the concentrations of the pigments in lakes ranging from oligotrophic to eutrophic. Infrared epifluorescence microscopy, fluorescence emission spectroscopy, and high-performance liquid chromatography were used to demonstrate that AAnPB may constitute up to 80% of total bacterial biomass in some low-productive lakes, implying that they are an important component of many lake ecosystems (33). In addition, genes encoding proteins for light harvesting (bacteriochlorophyll pufL and pufM gene clusters) have been identified in fosmid libraries from bacteria of the Delaware River (48) and in a functional gene survey of an Antarctic lake (24).In the present study, we used a specific primer set that amplifies the L subunit of the dark-operative protochlorophyllide oxidoreductase (L-DPOR) and its homologs (nitrogenase and chlorophyllide oxidoreductase [COR]). The dark-operative protochlorophyllide oxidoreductase (DPOR) is encoded by three genes (chlN-bchN, chlB-bchB, and chlL-bchL) and catalyzes the reductive formation of chlorophyllide from protochlorophyllide during biosynthesis of chlorophylls (chl) and bacteriochlorophylls (bch) in the dark (see reference 7 for more detail). Analysis of the deduced amino acid sequences indicated the presence of significant sequence dissimilarity in DPOR between oxygenic and anoxygenic photosynthetic organisms (5, 8, 16, 17, 18). Molecular studies have shown that AAnPB contain only DPOR (15) but that cyanobacteria, algae, and gymnosperms (nonflowering plants) contain both DPOR and a light-dependent protochlorophyllide oxidoreductase (POR) which carries one of the only two known enzymes other than photochemical reaction centers with light-driven catalysis (7).Despite the lack of POR, AAnPB are able to modify their chlorophyllide so that their absorption spectrum is broadened to span from <350 to <1,050 nm (usually 365 to 770 nm) in the UV and near-infrared ranges. This spectral characteristic allows AAnPB to utilize light at a wavelength other than that utilized by chlorophyll-containing cyanobacteria and algae. The first step in a series of modifications is performed by COR, an enzyme that is found in anoxygenic phototrophic bacteria and that transforms chlorophyllide to bacteriochlorophyll (7).In the present study, we assessed the diversity of L-DPOR, COR, and the coamplified homolog nifH genes in bacteria of seven different lakes by using PCR-based clone libraries parallel to a molecular fingerprinting technique to study L-DPOR gene composition in a larger data set (comprising 20 Swedish lakes). By using L-DPOR genes as our target, we simultaneously assessed the compositions of both AAnPB and oxygenic phototrophs in freshwater ecosystems and their distributions along trophic gradients.