Swimming Motility Mutants of Marine Synechococcus Affected in Production and Localization of the S-Layer Protein SwmA

The S-layer protein SwmA is required for nonflagellar swimming in marine Synechococcus. An analysis of mutations in seven genes at two loci in the Synechococcus sp. strain WH8102 genome indicates that a multicomponent transporter and glycosyltransferases are required for the production and proper localization of SwmA.The mechanism of nonflagellar motility by which certain strains of marine Synechococcus swim in the absence of any extracellular organelle remains mysterious. The cell surface itself is predicted to produce thrust (11), and to date, two cell surface proteins required for swimming have been characterized (7, 14). SwmA is a 130-kDa glycoprotein that forms a paracrystalline surface layer (S-layer) (16). Whether the S-layer plays a direct role in motility or a more indirect role, e.g., being required for the proper placement and functioning of other components of the motility apparatus, remains unclear. SwmB is a highly repetitive, 1.12-MDa protein which is also required for motility and is similarly localized near the cell surface where it is arranged in a punctate manner (14).Transposon mutagenesis identified three separate chromosomal regions required for swimming motility in Synechococcus sp. strain WH8102 (15). In addition to the genes coding for SwmA and SwmB, two separate multicomponent ABC transporter genes, several putative glycosyltransferase genes, and various conserved and hypothetical genes of unknown function comprise the remaining genes present in these motility loci (15). We show here that mutations in several of these open reading frames (ORFs; SYNW0079, SYNW0087 to SYNW0089, and SYNW0192 to SYNW0195) affect the production and cellular localization of SwmA, and in the case of SYNW0087 and SYNW0195, that of a 70-kDa outer membrane protein (OMP).     

Structural and Genetic Basis for the Serological Differentiation of Pasteurella multocida Heddleston Serotypes 2 and 5

Pasteurella multocida is classified into 16 serotypes according to the Heddleston typing scheme. As part of a comprehensive study to define the structural and genetic basis of this scheme, we have determined the structure of the lipopolysaccharide (LPS) produced by P. multocida strains M1404 (B:2) and P1702 (E:5), the type strains for serotypes 2 and 5, respectively. The only difference between the LPS structures made by these two strains was the absence of a phosphoethanolamine (PEtn) moiety at the 3 position of the second heptose (Hep II) in M1404. Analysis of the lpt-3 gene, required for the addition of this PEtn residue, revealed that the gene was intact in P1702 but contained a nonsense mutation in M1404. Expression of an intact copy of lpt-3 in M1404 resulted in the attachment of a PEtn residue to the 3 position of the Hep II residue, generating an LPS structure identical to that produced by P1702. We identified and characterized each of the glycosyltransferase genes required for assembly of the serotype 2 and 5 LPS outer core. Monoclonal antibodies raised against serotype 2 LPS recognized the serotype 2/5-specific outer core LPS structure, but recognition of this structure was inhibited by the PEtn residue on Hep II. These data indicate that the serological classification of strains into Heddleston serotypes 2 and 5 is dependent on the presence or absence of PEtn on Hep II.Pasteurella multocida is a gram-negative pathogen that causes serious diseases in animals and humans. It is the causative agent of fowl cholera (7), hemorrhagic septicemia in cattle (9), atrophic rhinitis in pigs (6), and dog and cat bite infections in humans (28).P. multocida isolates may be grouped serologically based on capsular antigens into five serogroups—A, B, D, E, and F—using a passive hemagglutination test with erythrocytes sensitized with capsular antigen. Structural information is available for the capsular polysaccharides synthesized by serogroups A (hyaluronic acid) (22), D (heparin) (10), and F (chondroitin) (10). The genes involved in biosynthesis of the capsules have been identified for all five serogroups (27), and capsule is a critical virulence factor for serogroups A (8) and B (3).Lipopolysaccharide (LPS) is also an important virulence factor in P. multocida (13) and can be used for the identification of strains, with two main somatic typing systems reported (14, 17). The Namioka system is based on a tube agglutination test and is able to recognize 11 serotypes (17), whereas the Heddleston system uses a gel diffusion precipitation test and can recognize 16 serotypes; the Heddleston system is currently the preferred method (14). Current classification of P. multocida strains combines capsular typing with Heddleston somatic typing. Strains are given a designation in which the first letter indicates the capsular group and the number designates the Heddleston LPS serotype (e.g., A:1 indicates a strain that is capsular group A and LPS serotype 1). LPS produced by each of the 16 Heddleston serotype strains has been examined previously for sugar content and reactivity with LPS antisera (21). The LPS isolated from serotype 2 and 5 strains was virtually identical in sodium dodecyl sulfate-polyacrylamide gel electrophoresis migration profile (19), sugar composition, and serological reactivity with anti-LPS antibodies (21). Interestingly, serotypes 2 and 5 were the only serotypes found to elaborate two isomers of heptose in their LPS, namely l-glycero-d-manno-heptose (ld-Hep) and d-glycero-d-manno-heptose (dd-Hep) (21). The aims of this study were to determine whether the LPS molecules made by these two serotypes were structurally distinct and to compare the LPS structures with those previously determined for P. multocida serotypes 1 and 3 (24-26). Furthermore, we identified the transferase genes responsible for the assembly of the outer core LPS structure in each of these strains and characterized the function of each glycosyltransferase.     

Isolation of Novel Extreme-Tolerant Cyanobacteria from a Rock-Dwelling Microbial Community by Using Exposure to Low Earth Orbit

Many cyanobacteria are known to tolerate environmental extremes. Motivated by an interest in selecting cyanobacteria for applications in space, we launched rocks from a limestone cliff in Beer, Devon, United Kingdom, containing an epilithic and endolithic rock-dwelling community of cyanobacteria into low Earth orbit (LEO) at a height of approximately 300 kilometers. The community was exposed for 10 days to isolate cyanobacteria that can survive exposure to the extreme radiation and desiccating conditions associated with space. Culture-independent (16S rRNA) and culture-dependent methods showed that the cyanobacterial community was composed of Pleurocapsales, Oscillatoriales, and Chroococcales. A single cyanobacterium, a previously uncharacterized extremophile, was isolated after exposure to LEO. We were able to isolate the cyanobacterium from the limestone cliff after exposing the rock-dwelling community to desiccation and vacuum (0.7 × 10⁻³ kPa) in the laboratory. The ability of the organism to survive the conditions in space may be linked to the formation of dense colonies. These experiments show how extreme environmental conditions, including space, can be used to select for novel microorganisms. Furthermore, it improves our knowledge of environmental tolerances of extremophilic rock-dwelling cyanobacteria.The surface and interior of rocks is a ubiquitous environment for microorganisms. Comprehensive culturing and culture-independent analyses of endolithic (interior of rocks) and epilithic (on the surface of rocks) microbial communities have been conducted. The primary producers in these environments are phototrophs, such as cyanobacteria, that are either free living or endosymbionts in lichens (16).Epilithic microorganisms are often an important part of rock-dwelling communities. The characterization of the epilithic cyanobacteria from natural environments, such as beach rock and caves, and from human-made environments, such as hypogea and buildings, has identified a variety of cyanobacteria. This includes both unicellular and filamentous forms, for example, Lyngbya-related species and Chroococcidiopsis (5, 14, 37, 47).Many microorganisms also inhabit the interior of rocks as endoliths. The endolithic environment provides protection from environmental stresses such as desiccation, extreme temperature, UV radiation, and high photosynthetically active radiation (400 to 700 nm) (6, 16, 25, 32). Endolithic communities are often the dominant form of life in extreme environments such as hot and cold deserts (15-17), savannahs, and semideserts (3, 6, 15, 48). In these extreme environments, the endolithic cyanobacteria are mainly unicellular cyanobacteria, for example, Chroococcidiopsis, Myxosarcina, and Gloeocapsa species (11, 46, 50). Conversely, in nondesert environments, such as dolomitic rocks in Switzerland (41), the limestone of the Niagara Escarpment (19, 20), and travertine deposits in Yellowstone National Park, the endolithic communities are more diverse and include both filamentous and unicellular types of cyanobacteria, such as Leptolyngbya, Nostoc, and Synechocystis (34).Although rock-dwelling cyanobacteria communities are diverse, there has been limited, if any, use of artificial extreme conditions to select for novel extremophilic cyanobacteria from these environments. Such an investigation could have implications for understanding the physiological requirements of life in extreme environments.The work described in this paper was motivated by an interest in understanding the physiological tolerance of cyanobacteria to space conditions and their potential use in space applications, such as oxygen and feedstock provision, which are crucial for extraterrestrial settlements (23, 29). In this work, we exposed samples of a coastal limestone cliff in Beer, Devon, United Kingdom, which is inhabited by a diverse cyanobacterial community, to low Earth orbit (LEO) to isolate novel extreme-tolerant cyanobacteria.     

Photoheterotrophic Microbes in the Arctic Ocean in Summer and Winter

Photoheterotrophic microbes, which are capable of utilizing dissolved organic materials and harvesting light energy, include coccoid cyanobacteria (Synechococcus and Prochlorococcus), aerobic anoxygenic phototrophic (AAP) bacteria, and proteorhodopsin (PR)-containing bacteria. Our knowledge of photoheterotrophic microbes is largely incomplete, especially for high-latitude waters such as the Arctic Ocean, where photoheterotrophs may have special ecological relationships and distinct biogeochemical impacts due to extremes in day length and seasonal ice cover. These microbes were examined by epifluorescence microscopy, flow cytometry, and quantitative PCR (QPCR) assays for PR and a gene diagnostic of AAP bacteria (pufM). The abundance of AAP bacteria and PR-containing bacteria decreased from summer to winter, in parallel with a threefold decrease in the total prokaryotic community. In contrast, the abundance of Synechococcus organisms did not decrease in winter, suggesting that their growth was supported by organic substrates. Results from QPCR assays revealed no substantial shifts in the community structure of AAP bacteria and PR-containing bacteria. However, Arctic PR genes were different from those found at lower latitudes, and surprisingly, they were not similar to those in Antarctic coastal waters. Photoheterotrophic microbes appear to compete successfully with strict heterotrophs during winter darkness below the ice, but AAP bacteria and PR-containing bacteria do not behave as superior competitors during the summer.Photoheterotrophy, which is the ability to utilize organic substrates and to harvest light energy, occurs in a broad range of microbes (14). Phototrophic microbes should be included in models of carbon cycling and food web dynamics, which now typically include only photoautotrophs, which produce organic carbon and oxygen, and heterotrophs, which consume organic matter and oxygen via aerobic respiration (55). Photoheterotrophy is potentially an important competitive adaptation, enabling microbes to survive adverse conditions or to outgrow competitors. Photoheterotrophic microbes include proteorhodopsin (PR)-containing bacteria, aerobic anoxygenic phototrophic (AAP) bacteria, and cyanobacteria.PR is a membrane protein that binds retinal and functions as a light-driven proton pump that can have several physiological functions, including ATP generation (15). The actual role of PR in the environment is uncertain, however. Light enhances the growth of some PR-containing bacteria, such as Dokdonia sp. (17), but has no effect on the growth of others, including Pelagibacter ubique (16) and the SAR92-like strain HTCC2207 (44). Similarly, Campbell et al. (4) found no significant correlation with light intensity for three of four PR gene types examined in the North Atlantic Ocean. Nevertheless, emerging biogeographic patterns of PR genes are providing clues about what controls the distribution and abundance of PR-containing photoheterotrophs in oceanic systems. One of the first oceanic environments to be examined for PR was the coastal waters near Palmer Station, Antarctica (2). Sequence analysis revealed that the Antarctic PRs differed from those isolated from Monterey Bay and surface waters in the central North Pacific (2). In spite of this early report, there has been no work on PR-containing bacteria in Arctic waters. PR-containing bacteria may have unique responses to the continuous summer light, winter darkness, and shading by seasonal ice cover that occur in high-latitude environments.The diversity and abundance of AAP bacteria have been examined by sequencing of the pufM gene (20, 51, 58), which is involved in bacteriochlorophyll (BChl a) synthesis, and by counting of BChl a-fluorescing cells by infrared fluorescence microscopy (14). Enumeration by infrared epifluorescence microscopy indicates that the abundance of AAP bacteria in environments such as the North Pacific Gyre and the Northeast Atlantic Ocean ranges from 1% to 10% (12, 13, 42) and can exceed 10% of the total prokaryotic community in estuaries (41, 50). AAP bacteria have been found in freshwater high-latitude waters (20, 35), but sequence analysis of pufM genes indicates that these AAP bacteria are distinct from those found in marine systems (50). The abundance of AAP bacteria decreases with latitude within the North Atlantic Ocean, from the central gyre to the waters near Greenland (13). Although these photoheterotrophic microbes are still present at 65°N, extrapolation of the trend suggests that AAP bacteria might be absent from the high-latitude waters of the Arctic Ocean.Polar waters appear to be an exception to the otherwise widespread distribution of coccoid cyanobacteria in the world oceans (33, 54). The abundance of Synechococcus and Prochlorococcus decreases with latitude, as exemplified by the 4-orders-of-magnitude decline in abundance between 44°S and 62°S in the South Atlantic Ocean (25). The abundance of Synechococcus also decreases with latitude in the North Atlantic Ocean, between the central gyre and the waters near Greenland, to a low level at 65°N (13). The strong correlation between abundance and temperature (25) suggests that coccoid cyanobacteria are not important at high latitudes, although there are scattered reports of Prochlorococcus in waters as far north as 60°N, near Iceland (27), and of Synechococcus in Antarctic coastal waters (53). However, more data are needed on the abundance of Synechococcus and Prochlorococcus in polar waters such as the Arctic Ocean.The goal of this study was to explore the abundance and diversity of photoheterotrophic microbes in the Arctic Ocean in order to develop a better picture of the biogeographic range of these biogeochemically important microbes and to gain insights into their ecology. Coastal waters of the Chukchi Sea and the Beaufort Sea were sampled in summer at the end of 24-h daylight and in winter following the period of 24-h darkness. The abundances of cyanobacteria, PR-containing bacteria, and AAP bacteria were monitored using flow cytometry, infrared epifluorescence microscopy, and real-time quantitative PCR (QPCR). These data provide a unique perspective on the potential impact of photoheterotrophic microbes on food webs and carbon cycling in this high-latitude aquatic system.     

The Biosynthetic Pathway for Myxol-2′ Fucoside (Myxoxanthophyll) in the Cyanobacterium Synechococcus sp. Strain PCC 7002

Synechococcus sp. strain PCC 7002 produces a variety of carotenoids, which comprise predominantly dicylic β-carotene and two dicyclic xanthophylls, zeaxanthin and synechoxanthin. However, this cyanobacterium also produces a monocyclic myxoxanthophyll, which was identified as myxol-2′ fucoside. Compared to the carotenoid glycosides produced by diverse microorganisms, cyanobacterial myxoxanthophyll and closely related compounds are unusual because they are glycosylated on the 2′-OH rather than on the 1′-OH position of the ψ end of the molecule. In this study, the genes encoding two enzymes that modify the ψ end of myxoxanthophyll in Synechococcus sp. strain PCC 7002 were identified. Mutational and biochemical studies showed that open reading frame SynPCC7002_A2032, renamed cruF, encodes a 1′-hydroxylase and that open reading frame SynPCC7002_A2031, renamed cruG, encodes a 2′-O-glycosyltransferase. The enzymatic activity of CruF was verified by chemical characterization of the carotenoid products synthesized when cruF was expressed in a lycopene-producing strain of Escherichia coli. Database searches showed that homologs of cruF and cruG occur in the genomes of all sequenced cyanobacterial strains that are known to produce myxol or the acylic xanthophyll oscillaxanthin. The genomes of many other bacteria that produce hydroxylated carotenoids but do not contain crtC homologs also contain cruF orthologs. Based upon observable intermediates, a complete biosynthetic pathway for myxoxanthophyll is proposed. This study expands the suite of enzymes available for metabolic engineering of carotenoid biosynthetic pathways for biotechnological applications.A wide variety of organisms produce carotenoid glycosides, which act as natural surfactants, stabilize membranes, and possibly contribute to regulating the permeability of membranes to oxygen (4, 41, 51). The first carotenoid glycosides were isolated from saffron in 1818 (6). However, the structures of the glycosylated carotenoids phleixanthophyll and 4-keto-phleixanthophyll were the first to be completely determined, in 1967, after their isolation from Mycobacterium phlei (15, 34). Tertiary glycosides are relatively rare in nature but seem to be common in carotenoid biosynthesis (34). These include the glycosylated carotenoids of the myxobacteria, which have characteristic C-3′,4′ desaturation and C-1′ glycosylation (18, 19). Acylated carotenoid C-1′-glycosides are broadly distributed among bacteria, including Salinibacter ruber and members of the Chloroflexi and Chlorobi (24, 46, 47).The glycosylated carotenoids of cyanobacteria differ from the examples mentioned above in that glycosylation characteristically occurs on the C-2′-hydroxyl group rather than that at the C-1′ position of the ψ end of myxol (3′,4′-didehydro-1′,2′-dihydro-β,ψ-carotene-3,1′,2′-triol) or oscillol (3,4,3′,4′-tetradehydro-1,2,1′,2′-ψ,ψ-carotene-1,2,1′,2′-tetrol) to form myxoxanthophyll or oscillaxanthin, respectively (16, 17). Myxoxanthophyll is thus far found uniquely in members of the phylum Cyanobacteria, and this compound is named after the synonym for this group of organisms, i.e., Myxophyceae (14, 42). As carotenoids from increasingly diverse bacteria are characterized, the apparent uniqueness of myxoxanthophyll to cyanobacteria will probably not persist. For example, the aglycone myxol occurs in marine flavobacteria, along with saporaxanthin (38, 49). Oscillaxanthin, which was once thought to be unique to the Nostophyceae, was recently identified as the major pigment of three strains of Methylobacterium spp. (20). Moreover, oscillol appears to be a precursor of the glycosylated and acylated carotenoids of Thermomicrobium roseum (52).Several variations on the myxoxanthophyll pathway, which lead to a variety of possible compounds, are known to occur in cyanobacteria. A number of different sugars commonly occur in myxoxanthophyll derivatives found in different strains. Strains of Oscillatoria and Spirulina spp. produce compounds that are chinovosides, fucosides, or methylfucosides (1, 7). Derivatives containing fucose have been found in Nostoc punctiforme strain PCC 73102 and Nostoc sp. strain PCC 7120 (45), whereas myxoxanthophyll dimethylfucoside has been found in Synechocystis sp. strain PCC 6803 (42). Variations in the ring oxidation level of the basal compound, with the addition of a keto group at the C-4 position or of an additional hydroxyl group at the C-2 or C-4 position, may also lead to several related compounds.Myxol is presumably synthesized from lycopene, the acyclic precursor of all carotenoids in cyanobacteria (see Fig. ​Fig.1)1) (27). Because of the occurrence of a β-ionone ring in the final product, monocyclic γ-carotene is also presumed to be an intermediate in this pathway (21, 41). The question of what enzyme is responsible for the formation of the β-ionone ring from the linear ψ end of γ-carotene has been contentious but has recently been resolved. Although CrtL-type lycopene cyclases occur in some cyanobacteria, genes for lycopene cyclases of this family do not occur in the genomes of sequenced cyanobacteria that produce myxoxanthophyll (11, 26). Mohamed and Vermaas reported that the open reading frame (ORF) sll0254 encodes an enzyme thought to be involved simultaneously in the cyclization and ψ-end hydroxylation of lycopene in Synechocystis sp. strain PCC 6803 (31). However, subsequent studies of both Synechococcus sp. strain PCC 7002 and Synechocystis sp. strain PCC 6803 showed that this is not the case (11, 26). Like nearly all other cyanobacteria lacking CrtL homologs, both of these cyanobacteria contain two genes, cruA and cruP, which encode lycopene cyclases (26). A third class of organisms, which so far includes only Synechococcus sp. strains PCC 7942 and PCC 6301, have CrtL and CruP homologs.Open in a separate windowFIG. 1.HPLC elution profiles for pigments from two cyanobacteria. (A) HPLC elution profiles (obtained by the jegpsu method) for pigments extracted from the wild type (solid line) and the slr1293 mutant (dotted line) of Synechocystis sp. strain PCC 6803. (B) HPLC elution profiles (obtained by the jegpsu method) for pigments extracted from the wild type (solid line) and SynPCC7002_A1623 mutant (dotted line) of Synechococcus sp. strain PCC 7002. Peak identities: s, synechoxanthin; md, myxol-2′ dimethylfucoside; mf, myxol-2′ fucoside; z, zeaxanthin; c, cryptoxanthin; e, echinenone; and b, β-carotene.The well-conserved β-hydroxylase CrtR functions in the C-3 hydroxylation of myxoxanthophyll, and CrtR also functions in the synthesis of zeaxanthin, cryptoxanthin, and 3′-hydroxy-echinenone (11, 21, 27, 28). CrtR seems to be responsible for all C-3 hydroxylation reactions in Synechocystis sp. strain PCC 6803, and it is notable that CrtR seems to be extremely highly conserved among cyanobacteria (11, 27). Considerable confusion has existed concerning the remaining reactions of this biosynthetic pathway. Mohamed and Vermaas reported that ORF slr1293 encodes the 3′,4′ desaturase in Synechocystis sp. strain PCC 6803 (30). Furthermore, Mohamed and Vermaas additionally reported that the product of ORF sll0254 plays a dual role as a lycopene cyclase and a mediator of ψ-end hydroxylation during myxoxanthophyll biosynthesis in Synechocystis sp. strain PCC 6803 (31). However, subsequent studies have shown that the sll0254 product and its orthologs, renamed CruE, are carotene desaturases/methyltransferases that participate in the synthesis of the aromatic carotenoid synechoxanthin (12, 13).In this study, we identified two genes, cruF and cruG, which encode the C-1′-hydroxylase and 2′-O-glycosyltransferase, respectively, that are uniquely required for mxyoxanthophyll biosynthesis in Synechococcus sp. strain PCC 7002. Orthologs of these genes are found in all sequenced genomes of cyanobacteria that synthesize myxoxanthophyll. Additionally, in contrast to the data in a previous report (30), we show that ORF slr1293 of Synechocystis sp. strain PCC 6803 and its ortholog SynPCC7002_A2031 in Synechococcus sp. strain PCC 7002 do not play an essential role in myxoxanthophyll biosynthesis.     

Residues of Heat-Labile Enterotoxin Involved in Bacterial Cell Surface Binding

Enterotoxigenic Escherichia coli (ETEC) is a leading cause of traveler''s diarrhea worldwide. One major virulence factor released by this pathogen is the heat-labile enterotoxin LT, which upsets the balance of electrolytes in the intestine. After export, LT binds to lipopolysaccharide (LPS) on the bacterial surface. Although the residues responsible for LT''s binding to its host receptor are known, the portion of the toxin which mediates LPS binding has not been defined previously. Here, we describe mutations in LT that impair the binding of the toxin to the external surface of E. coli without altering holotoxin assembly. One mutation in particular, T47A, nearly abrogates surface binding without adversely affecting expression or secretion in ETEC. Interestingly, T47A is able to bind mutant E. coli expressing highly truncated forms of LPS, indicating that LT binding to wild-type LPS may be due primarily to association with an outer core sugar. Consequently, we have identified a region of LT distinct from the pocket involved in eukaryotic receptor binding that is responsible for binding to the surface of E. coli.Enterotoxigenic Escherichia coli (ETEC), a common etiologic agent behind traveler''s diarrhea, is also a significant cause of mortality worldwide (38). Many strains of ETEC elaborate a virulence factor called heat-labile enterotoxin or LT (34). LT is an AB₅ toxin, consisting of a single A subunit, LTA, and a ring of five B subunits, LTB (33). LTB mediates the toxin''s binding properties, and LTA ADP ribosylates host G proteins, increasing levels of cyclic AMP and causing the efflux of electrolytes and water into the intestinal lumen (27, 35). Each subunit of LT is translated separately from a bicistronic message and then transported to the periplasm, where holotoxin assembly spontaneously occurs (16). Subsequent export into the extracellular milieu is carried out by the main terminal branch of the general secretory pathway (31, 36).LT binds eukaryotic cells via an interaction between LTB and host gangliosides, primarily the monosialoganglioside GM₁ (35). The binding site for GM₁, situated at the interface of two B subunits, has been identified by crystallography (26). GM₁ binding can be strongly impaired by a point mutation in LTB that converts Gly-33 to an aspartic acid residue (37). LT is highly homologous to cholera toxin (CT), both in sequence and structure (7, 35), contributing to ETEC''s potentially cholera-like symptoms (39).Previous work in our lab has demonstrated that LT possesses an additional binding capacity beyond its affinity for host glycolipids: the ability to associate with lipopolysaccharide (LPS) on the surface of E. coli (20). LPS, the major component of the outer leaflet of the gram-negative outer membrane, consists of a characteristic lipid moiety, lipid A, covalently linked to a chain of sugar residues (30). In bacteria like E. coli, this sugar chain can be further divided into an inner core oligosaccharide of around five sugars, an outer core of four to six additional sugars, and in some cases a series of oligosaccharide repeats known as the O antigen. Lipid A itself cannot inhibit binding of soluble LT to cells containing full-length or truncated LPS, indicating that the LT-LPS interaction involves sugar residues on the surface of E. coli (19). The addition of the inner core sugar 3-deoxy-d-manno-octulosonic acid (Kdo) is the minimal lipid A modification required for LT binding, although longer oligosaccharide chains are preferred, and expression of a kinase that phosphorylates Kdo abrogates binding by LT (19). Competitive binding assays and microscopy with fluorescently labeled ETEC vesicles show that binding to GM₁ and LPS can occur at the same time, revealing that the binding sites are distinct (20, 23). In contrast to LT''s ability to bind to the surface of ETEC, CT (or LT, when expressed heterologously) cannot bind Vibrio cells, presumably because Kdo is phosphorylated in Vibrio spp. (5).As a result of the LT-LPS surface interaction, over 95% of secreted LT is found associated with E. coli outer membrane vesicles (OMVs), rather than being secreted solubly (20). OMVs are spherical structures, 50 to 200 nm in diameter, that are derived from the outer membrane but also enclose periplasmic components (24). As such, active LT is found both on the surface of an OMV and within its lumen (21). ETEC releases a large amount of OMVs (40), and these vesicles may serve as vehicles for delivery of LT to host cells.Recent work by Holmner et al. has uncovered a third binding substrate for LT: human blood group A antigen (17, 18). This interaction was noted previously as a novel binding characteristic of artificially constructed CT-LT hybrid molecules, but it has now been shown to occur with wild-type LT as well (17, 18). LTB binding to sugar residues in the receptor molecule occurs at a site that is separate from the GM₁-binding pocket, in the same region we proposed was involved in LPS binding (17, 19). While the severity of cholera disease symptoms has been linked to blood type (14), the effects of blood type on ETEC infection are less clear. However, it has been demonstrated that LT can use A antigen as a functional receptor in cultured human intestinal cells (11, 12), and one recent cohort study found an increased prevalence of ETEC-based diarrhea among children with A or AB blood type (29).We set out to generate a mutation in LT that reduces its LPS binding without adversely affecting its expression, secretion, or toxicity. In this work, we present the discovery of point mutations in LTB that impair its interactions with the bacterial surface. Examination of these mutations reveals an LPS binding pocket which shares residues with the blood sugar pocket. Binding studies of mutants to bacteria with truncated LPS provide a better understanding of the roles that inner and outer core sugars play in toxin binding, and expression, secretion, and toxicity studies demonstrate which mutant is a particularly good candidate for future research. These binding mutants may lead to further discovery of the role that surface binding plays in the pathogenesis associated with ETEC infection.     

Characterization of the FtsZ-Interacting Septal Proteins SepF and Ftn6 in the Spherical-Celled Cyanobacterium Synechocystis Strain PCC 6803

Assembly of the tubulin-like cytoskeletal protein FtsZ into a ring structure at midcell establishes the location of the nascent division sites in prokaryotes. However, it is not yet known how the assembly and contraction of the Z ring are regulated, especially in cyanobacteria, the environmentally crucial organisms for which only one FtsZ partner protein, ZipN, has been described so far. Here, we characterized SepF and Ftn6, two novel septal proteins, in the spherical-celled strain Synechocystis PCC 6803. Both proteins were found to be indispensable to Synechocystis sp. strain PCC 6803. The depletion of both SepF and Ftn6 resulted in delayed cytokinesis and the generation of giant cells but did not prevent FtsZ polymerization, as shown by the visualization of green fluorescent protein (GFP)-tagged FtsZ polymers. These GFP-tagged Z-ring-like structures often appeared to be abnormal, because these reporter cells respond to the depletion of either SepF or Ftn6 with an increased abundance of total, natural, and GFP-tagged FtsZ proteins. In agreement with their septal localization, we found that both SepF and Ftn6 interact physically with FtsZ. Finally, we showed that SepF, but not Ftn6, stimulates the formation and/or stability of FtsZ polymers in vitro.Binary fission of a mother cell to form two daughter cells is a widely conserved cell proliferation mechanism. In nearly all bacteria, cell division is initiated by the polymerization into a ring-like structure at midcell of the tubulin homolog GTPase protein FtsZ, which is also found in some archae, as well as in plastids and some mitochondria (for reviews, see references 7, 21, and 33). The Z-ring is subsequently used as a scaffold for recruitment of downstream factors that execute the synthesis of the division septum. The assembly of this complex, also referred to as the divisome, has been thoroughly investigated in studies of the rod-shaped model organisms Escherichia coli and Bacillus subtilis) (for reviews, see references 3, 4, 7, 9, 11, 19, and 21). In E. coli, more than 10 different proteins are required for the progression and completion of cell division. They are designated Fts proteins because their depletion leads to filamentation of the bacteria, and they are recruited to the division site in the following sequential order: FtsZ→FtsA/ZipA/ZapB→FtsK→FtsQ and FtsL/FtsB→FtsW→FtsI and FtsN.The stability of the FtsZ protofilaments is thought to be important for assembly of the septal Z ring. Four FtsZ-interacting proteins have been shown to promote FtsZ polymerization and/or Z-ring stabilization, namely, ZapA and ZipA (found only in gammaproteobacteria), FtsA (an actin-like protein), and SepF (not found in gammaproteobacteria) (10, 31). Both FtsA and ZipA assemble at the Z-ring early and participate in its anchorage to the inner face of the cytoplasmic membrane of the cell. They also participate in the recruitment of the downstream cytokinetic factor FtsK. Subsequently, the recruitment of FtsQ and the FtsB/FtsL complex allow the progressive assembly of downstream factors (FtsW, FtsI, and FtsN) involved in synthesis of the septal cell wall (7).By contrast, the negative regulatory proteins MinCDE, DivIVA, EzrA, SulA, and Noc operate in the destabilization and positioning of the Z-ring at midcell (7, 21, 30), sometimes through a direct interaction with FtsZ (SulA, MinC, and ErzA).Little is known concerning cell division in cyanobacteria, in spite of their crucial importance to the biosphere (5, 27, 34) and their interest for biotechnologists (1, 6, 32). Cyanobacteria are also attractive because many species (such as E. coli and B. subtilis) exhibit a cylindrical morphology with a well-defined middle, whereas many others have a spherical shape (29) and thus possess an infinite number of potential division planes at the point of greatest cell diameter. Furthermore, as the progenitor of the chloroplasts (8), cyanobacteria can be of help for deciphering the stromal chloroplastic division machinery (33). Interestingly, several cell division factors occurring in E. coli and B. subtilis have been shown (FtsZ, MinCDE, and SulA) or proposed (FtsE, FtsI, FtsQ, and FtsW) to be conserved in cyanobacteria (23, 26) and chloroplasts (which lack MinC) (33). In contrast, ftsA, ftsB, zipA, ftsK, ftsL, ftsN, and zapA have not been detected in cyanobacteria.So far, cyanobacterial cytokinesis has mainly been investigated using the two unicellular species Synechococcus sp. strain PCC 7942 (rod shaped; hereafter S. elongatus) and Synechocystis sp. strain PCC 6803 (spherical-celled; hereafter Synechocystis sp.) and the filamentous strain Anabaena PCC 7120, all of which possess a fully sequenced genome (http://genome.kazusa.or.jp/cyanobase/) that is easily manipulated (16). Both FtsZ and ZipN/Ftn2/Arc6, a protein occurring only in cyanobacteria (ZipN [alternative name, Ftn2]) and plant chloroplasts (Arc6), were found to be crucial for cytokinesis (17, 23, 26) and to physically interact with each other (20, 23). We also reported that the MinCDE system participates in determining the correct positioning of the septal Z ring at midcell (23). In addition, it has recently been shown in studies of Synechococcus sp. that inactivation of both the cdv2 gene (an orthologue of the gene encoding B.subtilis sepF) and the ftn6 gene (present in only some cyanobacteria) promotes filamentation, though their role in cell division has yet to be characterized (16, 26).In a continuous effort to characterize the divisome machine of Synechocystis sp., we have used a combination of in vivo and in vitro techniques for thorough analysis of the SepF and Ftn6 proteins. We report here that both SepF and Ftn6 are crucial cytokinetic proteins that localize at the division site at midcell and whose depletion leads to the formation of giant cells that remain spherical. In agreement with their septal localization, both SepF and Ftn6 were found to interact physically with FtsZ; also, SepF, but not Ftn6, was found to stimulate the formation and/or stability of FtsZ polymers.     

Polyphasic Characterization of a Thermotolerant Siderophilic Filamentous Cyanobacterium That Produces Intracellular Iron Deposits

Despite the high potential for oxidative stress stimulated by reduced iron, contemporary iron-depositing hot springs with circum-neutral pH are intensively populated with cyanobacteria. Therefore, studies of the physiology, diversity, and phylogeny of cyanobacteria inhabiting iron-depositing hot springs may provide insights into the contribution of cyanobacteria to iron redox cycling in these environments and new mechanisms of oxidative stress mitigation. In this study the morphology, ultrastructure, physiology, and phylogeny of a novel cyanobacterial taxon, JSC-1, isolated from an iron-depositing hot spring, were determined. The JSC-1 strain has been deposited in ATCC under the name Marsacia ferruginose, accession number BAA-2121. Strain JSC-1 represents a new operational taxonomical unit (OTU) within Leptolyngbya sensu lato. Strain JSC-1 exhibited an unusually high ratio between photosystem (PS) I and PS II, was capable of complementary chromatic adaptation, and is apparently capable of nitrogen fixation. Furthermore, it synthesized a unique set of carotenoids, but only chlorophyll a. Strain JSC-1 not only required high levels of Fe for growth (≥40 μM), but it also accumulated large amounts of extracellular iron in the form of ferrihydrite and intracellular iron in the form of ferric phosphates. Collectively, these observations provide insights into the physiological strategies that might have allowed cyanobacteria to develop and proliferate in Fe-rich, circum-neutral environments.Cyanobacteria inhabiting ferrous iron-rich hot springs with circum-neutral pH represent unique models for examining the mechanisms by which early organisms evolved to cope with such habitats common on early Earth. Such organisms have previously been shown to be resistant to Fe²⁺ (37) or Fe³⁺ (6, 7) at concentrations in the micromolar to millimolar range. Moreover, high Fe concentrations (apparent optimum of ∼0.5 mM) stimulated the growth of these cyanobacteria, which were described as siderophilic (having an affinity for iron) cyanobacteria (7).The cyanobacteria inhabiting the Chocolate Pots hot springs in Yellowstone National Park, Wyoming, were shown to have played at least a passive role in contributing to iron deposition by serving as nucleation sites for the accumulation of iron minerals and associated silica deposits (36, 38). The precipitation of external iron that encrusts the cyanobacterial cells inhabiting this hot spring appears to be dependent on the species composition and chemistry of the mat (36, 38); however, multiple anoxygenic phototrophs found in the Chocolate Pots hot springs (8) could also contribute to the formation of Fe oxides (21, 49). Therefore, only iron mineralization experiments with model cyanobacterial strains can demonstrate the role of siderophilic cyanobacteria in the formation of specific, iron-bearing minerals.An additional common feature of circum-neutral iron-depositing hot springs is elevated concentrations of hydrogen peroxide (50). Shcolnick and coauthors (41) showed that a wild type of Synechococcus sp. PCC 6803 was resistant to 8 mM H₂O₂ if grown with 0.3 μM Fe³⁺, while the same concentration of hydrogen peroxide completely inhibited the growth of this cyanobacterium if it was grown with 10 μM Fe³⁺. If a similar correlation between iron concentration and the magnitude of an externally applied oxidative stress were the case for siderophilic cyanobacteria, iron-depositing hot springs should be free of cyanobacteria. However, such springs are very rich with cyanobacteria (38, 7, 36), which suggests that siderophilic cyanobacteria may possess unusual mechanisms of iron homeostasis maintenance and oxidative stress mitigation. Additionally, understanding iron tolerance and phenomena associated with siderophily in oxygenic prokaryotes is also important because such siderophilic organisms might help us find applications for bioremediation of waters polluted with iron.The current work describes the morphology, ultrastructure, physiology, and phylogeny of a previously undescribed, siderophilic cyanobacterium. The results of this polyphasic characterization led to the conclusion that strain JSC-1 represents a new operational taxonomic unit (OTU). (The epithet for JSC-1, Marsacia ferruginose, was chosen in honor of Nicole Tandeau de Marsac.) Additionally, biomineralization of intracellular iron by a cyanobacterium is demonstrated for the first time.     

Highly Diverse Cyanobactins in Strains of the Genus Anabaena

Cyanobactins are small, cyclic peptides recently found in cyanobacteria. They are formed through proteolytic cleavage and posttranslational modification of short precursor proteins and exhibit antitumor, cytotoxic, or multi-drug-reversing activities. Using genome project data, bioinformatics, stable isotope labeling, and mass spectrometry, we discovered novel cyclic peptides, anacyclamides, in 27 Anabaena strains. The lengths of the anacylamides varied greatly, from 7 to 20 amino acids. Pronounced sequence variation was also detected, and only one amino acid, proline, was present in all anacyclamides. The anacyclamides identified included unmodified proteinogenic or prenylated amino acids. We identified an 11-kb gene cluster in the genome of Anabaena sp. 90, and heterologous expression in Escherichia coli confirmed that this cluster was responsible for anacyclamide production. The discovery of anacyclamides greatly increases the structural diversity of cyanobactins.Cyanobacteria are a prolific source of secondary metabolites with potential as drug leads or useful probes for cell biology studies (23). They include biomedically interesting compounds, such as the anticancer drug lead cryptophycin (15), and environmentally problematic hepatotoxic peptides, such as microcystins and nodularins produced by bloom-forming cyanobacteria (23). Many of these compounds contain nonproteinogenic amino acids and modified peptides and are produced by nonribosomal peptide synthesis (23, 26).The cyanobactins are a new group of cyclic peptides recently found in cyanobacteria (4). They are assembled through posttranslational proteolytic cleavage and head-to-tail macrocyclization of short precursor proteins. The cyanobactins are low-molecular-weight cyclic peptides that contain heterocyclized amino acids and can be prenylated or contain d-amino acids (3, 4). The cyanobactins that contain heterocyclized amino acids include patellamides, ulithiacyclamides, trichamide, tenuecyclamides, trunkamides, patellins, and microcyclamides and are synthesized in this manner (3, 4, 20, 24, 28). They possess antitumor, cytotoxic, and multi-drug-reversing activities and have potential as drug leads (4, 18, 20).Cyanobactins containing heterocyclized amino acids are found in a variety of cyanobacteria (4). A recent study demonstrated that the cyanobactin biosynthetic pathway is prevalent in planktonic bloom-forming cyanobacteria (14). However, the products of these gene clusters encoding new cyanobactins are unknown. Here we report discovery of a novel family of low-molecular-weight cyanobactins and show that these compounds are common in strains of the genus Anabaena. These anacyclamides exhibit pronounced length and sequence variation and contain unmodified or prenylated amino acids.     

Bar-Coded Pyrosequencing Reveals Shared Bacterial Community Properties along the Temperature Gradients of Two Alkaline Hot Springs in Yellowstone National Park

An understanding of how communities are organized is a fundamental goal of ecology but one which has historically been elusive for microbial systems. We used a bar-coded pyrosequencing approach targeting the V3 region of the bacterial small-subunit rRNA gene to address the factors that structure communities along the thermal gradients of two alkaline hot springs in the Lower Geyser Basin of Yellowstone National Park. The filtered data set included a total of nearly 34,000 sequences from 39 environmental samples. Each was assigned to one of 391 operational taxonomic units (OTUs) identified by their unique V3 sequence signatures. Although the two hot springs differed in their OTU compositions, community resemblance and diversity changed with strikingly similar dynamics along the two outflow channels. Two lines of evidence suggest that these community properties are controlled primarily by environmental temperature. First, community resemblance decayed exponentially with increasing differences in temperature between samples but was only weakly correlated with physical distance. Second, diversity decreased with increasing temperature at the same rate along both gradients but was uncorrelated with other measured environmental variables. This study also provides novel insights into the nature of the ecological interactions among important taxa in these communities. A strong negative association was observed between cyanobacteria and the Chloroflexi, which together accounted for ∼70% of the sequences sampled. This pattern contradicts the longstanding hypothesis that coadapted lineages of these bacteria maintain tightly cooccurring distributions along these gradients as a result of a producer-consumer relationship. We propose that they instead compete for some limiting resource(s).Elucidating how biodiversity is distributed and the mechanisms underlying those patterns is a central goal of ecology. Although microorganisms make critical contributions to ecosystem function through their participation in biogeochemical cycles, we still have only a limited understanding of the factors that control the spatial structure and diversity of microbial communities (37). For example, although it is clear that microbial community composition is influenced by environmental variation (11, 17, 18, 28), the question of how diversity changes along environmental gradients remains generally unresolved. Of particular interest is the relationship between microbial diversity and temperature, as this environmental variable is strongly correlated with diversity over a broad range of spatial scales for many plant and animal taxa in terrestrial, freshwater, and marine ecosystems (1, 12, 36, 39, 43). In addition, because spatially resolved abundance data for individual microbial taxa are scarce, we have only limited information regarding the patterns of association among microorganisms. Consequently, microbial ecology has developed with little clarity regarding the potential roles of either negative or positive biotic interactions for structuring communities or whether microbial community organization along environmental gradients conforms to either individualistic (e.g., see references 13 and 20) or organismal (e.g., see reference 9) community ecology paradigms developed for macroscopic organisms.Hot spring microbial ecosystems present an excellent opportunity to investigate fundamental questions regarding community organization. Steep temperature gradients enable the explicit investigation of the importance of environmental variation for structuring diversity while controlling for other factors that typically vary across sampling locations on larger geographic scales, such as solar energy availability and geological history. Decades of biological research on the alkaline-silica hot springs of Yellowstone National Park (reviewed in reference 49) further inform predictions regarding the nature of the ecological interactions among abundant community members.These systems are particularly notable for the presence of ecologically diverse groups of cyanobacteria and photosynthetic green nonsulfur bacteria (i.e., the Chloroflexi). The former group includes lineages of Synechococcus, the most thermotolerant of which delimits the thermal maximum for photosynthesis, whereas the latter includes divergent “green” (the genus Chloroflexus and relatives) and “red” (the genus Roseiflexus) clades. The conventional view is that interactions among cyanobacteria and the Chloroflexi are generally positive. Specifically, it has been proposed that coadapted lineages of Synechococcus and Chloroflexi maintain tightly cooccurring distributions due to a producer-consumer relationship in which the Chloroflexi grow as photoheterotrophs on low-molecular-weight organic compounds excreted by the cyanobacteria (48, 49). In turn, the filamentous Chloroflexi were previously suggested to provide a matrix within which Synechococcus cells become stably embedded (5). According to this model, we would expect to observe coincident peaks in abundance between coadapted lineages of cyanobacteria and Chloroflexi along alkaline hot spring gradients as well as a general positive correlation between the abundances of both groups. However, other evidence raises the possibility that these groups may not share a strict cross-feeding relationship. The genus Chloroflexus is metabolically flexible in laboratory culture, and certain strains have been grown as photoautotrophs with hydrogen sulfide or hydrogen as an electron donor (16, 26, 30). Although Roseiflexus is yet to be grown autotrophically in the laboratory, comparative genomics of laboratory strains and metagenomic data from microbial mat communities have also revealed the presence of Roseiflexus genes involved in the autotrophic hydroxypropionate pathway (24). In addition, stable carbon isotope data (46, 47) suggest that certain members of the Chloroflexi may have the capacity to grow autotrophically in situ. The issue of the nature of the ecological interactions between cyanobacteria and the Chloroflexi therefore requires clarification.In the present study, we investigated the patterns of distribution of bacteria along the temperature gradients of two alkaline-silica hot springs in Yellowstone National Park to determine how community properties changed in response to temperature and whether the realized distributions of cyanobacteria and the Chloroflexi meet the prediction of the coadaptation hypothesis. To do so, we used bar-coded mass parallel pyrosequencing of the V3 variable region of the bacterial small-subunit (SSU) rRNA gene to simultaneously interrogate the sequence diversity of environmental samples from multiple locations along both hot springs. This strategy is distinct from recent applications of next-generation DNA sequencing technology for investigating microbial diversity, as previous efforts focused principally on the deep sampling of one or a few discrete habitats for the purpose of quantifying the magnitude of diversity (e.g., see references 21, 38, and 41). We report that community properties changed with similar dynamics in response to temperature despite differences between hot springs in water chemistries and taxon composition, and we reject the coadaptation hypothesis for these communities based on a strong negative association in abundances of cyanobacteria and Chloroflexi.     

Catabolic Function of Compartmentalized Alanine Dehydrogenase in the Heterocyst-Forming Cyanobacterium Anabaena sp. Strain PCC 7120

In the diazotrophic filaments of heterocyst-forming cyanobacteria, an exchange of metabolites takes place between vegetative cells and heterocysts that results in a net transfer of reduced carbon to the heterocysts and of fixed nitrogen to the vegetative cells. Open reading frame alr2355 of the genome of Anabaena sp. strain PCC 7120 is the ald gene encoding alanine dehydrogenase. A strain carrying a green fluorescent protein (GFP) fusion to the N terminus of Ald (Ald-N-GFP) showed that the ald gene is expressed in differentiating and mature heterocysts. Inactivation of ald resulted in a lack of alanine dehydrogenase activity, a substantially decreased nitrogenase activity, and a 50% reduction in the rate of diazotrophic growth. Whereas production of alanine was not affected in the ald mutant, in vivo labeling with [¹⁴C]alanine (in whole filaments and isolated heterocysts) or [¹⁴C]pyruvate (in whole filaments) showed that alanine catabolism was hampered. Thus, alanine catabolism in the heterocysts is needed for normal diazotrophic growth. Our results extend the significance of a previous work that suggested that alanine is transported from vegetative cells into heterocysts in the diazotrophic Anabaena filament.Cyanobacteria such as those of the genera Anabaena and Nostoc grow as filaments of cells (trichomes) that, when incubated in the absence of a source of combined nitrogen, present two cell types: vegetative cells that perform oxygenic photosynthesis and heterocysts that perform N₂ fixation. Heterocysts carry the oxygen-labile enzyme nitrogenase, and, thus, compartmentalization is the way these organisms separate the incompatible activities of N₂ fixation and O₂-evolving photosynthesis (9). In Anabaena and Nostoc, heterocysts are spaced along the filament so that approximately 1 in 10 to 15 cells is a heterocyst. Heterocysts differentiate from vegetative cells in a process that involves execution of a specific program of gene expression (12, 15, 39). In the N₂-fixing filament, the heterocysts provide the vegetative cells with fixed nitrogen, and the vegetative cells provide the heterocysts with photosynthate (38). Two important aspects of the diazotrophic physiology of heterocyst-forming cyanobacteria that are still under investigation include the actual metabolites that are transferred intercellularly and the mechanism(s) of transfer (10).Because the ammonium produced by nitrogenase is incorporated into glutamate to produce glutamine in the heterocyst and because the heterocyst lacks the main glutamate-synthesizing enzyme, glutamine(amide):2-oxoglutarate amino transferase (GOGAT; also known as glutamate synthase), a physiological exchange of glutamine and glutamate resulting in a net transfer of nitrogen from the heterocysts to the vegetative cells has been suggested (21, 36, 37). On the other hand, a sugar is supposed to be transferred from vegetative cells to heterocysts. Because high invertase activity levels are found in the heterocysts (34) and because overexpression of sucrose-degrading sucrose synthase in Anabaena sp. impairs diazotrophic growth (4), it is possible that sucrose is a transferred carbon source. Indeed, determination of ¹⁴C-labeled metabolites in heterocysts isolated from filaments incubated for short periods of time with [¹⁴C]bicarbonate identified sugars and glutamate as possible compounds transferred from vegetative cells to heterocysts (13). However, this study also identified alanine as a metabolite possibly transported from vegetative cells to heterocysts.The cyanobacteria bear a Gram-negative type of cell envelope, carrying an outer membrane (OM) outside the cytoplasmic membrane (CM) and the peptidoglycan layer (9, 15). In filamentous cyanobacteria, whereas the CM and peptidoglycan layer surround each cell, the OM is continuous along the filament, defining a continuous periplasmic space (10, 19). In Anabaena sp. strain PCC 7120, the OM is a permeability barrier for metabolites such as glutamate and sucrose (27). Two possible pathways for intercellular molecular exchange in heterocyst-forming cyanobacteria have been discussed: the periplasm (10, 19) and cell-to-cell-joining proteinaceous structures (11, 22, 25). Whereas the latter would mediate direct transfer of metabolites between the cytoplasm of adjacent cells, the former would require specific CM permeases to mediate metabolite transfer between the periplasm and the cytoplasm of each cell type (10).In Anabaena sp. strain PCC 7120, two ABC-type amino acid transporters have been identified that are specifically required for diazotrophic growth (29, 30). The N-I transporter (NatABCDE), which shows preference for neutral hydrophobic amino acids, is present exclusively in vegetative cells (30). The N-II transporter (NatFGH-BgtA), which shows preference for acidic and neutral polar amino acids, is present in both vegetative cells and heterocysts (29). A general phenotype of mutants of neutral amino acid transporters in cyanobacteria is release into the culture medium of some hydrophobic amino acids, especially alanine (16, 23, 24), which is accumulated at higher levels in the extracellular medium of cultures incubated in the absence than in the presence of a source of combined nitrogen (30).Thus, alanine is a conspicuous metabolite in the diazotrophic physiology of heterocyst-forming cyanobacteria, and the possibility that it moves in either direction between heterocysts and vegetative cells has been discussed (13, 29, 30). Alanine dehydrogenase, which catalyzes the reversible reductive amination of pyruvate, has been detected in several cyanobacteria (8). In Anabaena spp., alanine dehydrogenase has been found at higher levels or exclusively in diazotrophic cultures (26), and in the diazotrophic filaments of Anabaena cylindrica it is present at higher levels in heterocysts than in vegetative cells (33). Open reading frame (ORF) alr2355 of the Anabaena sp. strain PCC 7120 genome is predicted to encode an alanine dehydrogenase (14). In this work we addressed the expression and inactivation of alr2355, identifying it as the Anabaena ald gene and defining an important catabolic role for alanine dehydrogenase in diazotrophy.     

Identifying the Source of Unknown Microcystin Genes and Predicting Microcystin Variants by Comparing Genes within Uncultured Cyanobacterial Cells

While multiple phylogenetic markers have been used in the culture-independent study of microcystin-producing cyanobacteria, in only a few instances have multiple markers been studied within individual cells, and in all cases these studies have been conducted with cultured isolates. Here, we isolate and evaluate large DNA fragments (>6 kb) encompassing two genes involved in microcystin biosynthesis (mcyA2 and mcyB1) and use them to identify the source of gene fragments found in water samples. Further investigation of these gene loci from individual cyanobacterial cells allowed for improved analysis of the genetic diversity within microcystin producers as well as a method to predict microcystin variants for individuals. These efforts have also identified the source of the novel mcyA genotype previously termed Microcystis-like that is pervasive in the Laurentian Great Lakes and they predict the microcystin variant(s) that it produces.Microcystin-producing cyanobacteria are common nuisance organisms in harmful algal blooms in freshwaters around the world (4). This genetically diverse group (based on 16S rRNA, mcyA, mcyD, and mcyE gene sequences [6, 10, 15, 16, 22]) ranges in morphology from unicellular and colonial cocci to large filamentous strands. Many species can produce a variety of secondary metabolites that can act as hepatatoxins upon ingestion by animals (e.g., variants of microcystin) (4, 33). Microcystin production reduces the water quality in reservoirs used by human populations and fishery resources, and production of these toxins by this group of cyanobacteria makes them important organisms for continued observation and study (4, 33, 36). Much effort has been expended over the past 15 years to characterize the genomic and structural components of the microcystin (mcy) synthetase operon responsible for the production of microcystins. Several complete DNA sequences of the mcy synthetase operon are currently available in GenBank (3, 11, 29, 31).Although the mechanisms of microcystin production are now better understood, recent analyses of mcyA gene fragments from Lakes Erie and Ontario indicated a microcystin toxin producer of unknown phylogeny (7, 28). This discrepancy suggested a need for improved molecular characterization of naturally occurring microcystin producers, which spurred our research to identify the source of several unusual mcyA fragments from the cyanobacterial community (7, 28). It was apparent from initial sequence data that these mcyA gene fragments, termed Microcystis-like, were highly similar to those from Microcystis spp. (colonial or unicellular cocci). However, they contained a 6-nucleotide insert consistent with mcyA genes from filamentous cyanobacteria (e.g., Anabaena, Nostoc, and Planktothrix) (28). These preliminary findings suggested that these unusual mcyA fragments either came from (i) a novel species or strain, (ii) an ancestral Microcystis, (iii) the highly unlikely hybridization of colonial cocci and filamentous cyanobacteria, or (iv) a chimera of cocci and filamentous PCR products. To identify the source of these mcyA gene fragments from uncultured cyanobacteria, we used culture-independent methods to amplify and isolate long regions of the mcy synthetase operon for the simultaneous analysis of two genes, mcyA and mcyB, in one individual from a population. This approach ensures that both genes are contained on the same DNA molecule, thus allowing for more continuous sequence information to use in comparative phylogenetic analyses than previously described. We also envisioned that this mcy gene combination would provide an improved diagnostic tool for determining the genetic potential of naturally occurring cyanobacteria to produce specific microcystin variants by comparing the phylogenetic marker in mcyA to the predictor of amino acid incorporation (via an adenylation domain) in mcyB1.