Low-Concentration Kinetics of Atmospheric CH4 Oxidation in Soil and Mechanism of NH4+ Inhibition

NH₄⁺ inhibition kinetics for CH₄ oxidation were examined at near-atmospheric CH₄ concentrations in three upland forest soils. Whether NH₄⁺-independent salt effects could be neutralized by adding nonammoniacal salts to control samples in lieu of deionized water was also investigated. Because the levels of exchangeable endogenous NH₄⁺ were very low in the three soils, desorption of endogenous NH₄⁺ was not a significant factor in this study. The K_m(app) values for water-treated controls were 9.8, 22, and 57 nM for temperate pine, temperate hardwood, and birch taiga soils, respectively. At CH₄ concentrations of ≤15 μl liter⁻¹, oxidation followed first-order kinetics in the fine-textured taiga soil, whereas the coarse-textured temperate soils exhibited Michaelis-Menten kinetics. Compared to water controls, the K_m(app) values in the temperate soils increased in the presence of NH₄⁺ salts, whereas the V_max(app) values decreased substantially, indicating that there was a mixture of competitive and noncompetitive inhibition mechanisms for whole NH₄⁺ salts. Compared to the corresponding K⁺ salt controls, the K_m(app) values for NH₄⁺ salts increased substantially, whereas the V_max(app) values remained virtually unchanged, indicating that NH₄⁺ acted by competitive inhibition. Nonammoniacal salts caused inhibition to increase with increasing CH₄ concentrations in all three soils. In the birch taiga soil, this trend occurred with both NH₄⁺ and K⁺ salts, and the slope of the increase was not affected by the addition of NH₄⁺. Hence, the increase in inhibition resulted from an NH₄⁺-independent mechanism. These results show that NH₄⁺ inhibition of atmospheric CH₄ oxidation resulted from enzymatic substrate competition and that additional inhibition that was not competitive resulted from a general salt effect that was independent of NH₄⁺.Atmospheric CH₄ contributes substantially to the greenhouse effect, and the concentration of atmospheric CH₄ has increased dramatically in the past century because of human activity associated with agriculture, land use changes, and industry (34, 35). Bacterial oxidation of atmospheric CH₄ in well-drained soils is an important regulator of atmospheric CH₄ concentration, yet the organisms responsible remain unidentified and the physiology of the process is poorly understood (9, 35, 36). Although soil CH₄ consumption is inhibited by a wide variety of anthropogenic disturbances, such as agriculture, N deposition, and forestry (12, 17, 22, 23, 32, 43, 44), predictable inhibition patterns have failed to emerge, which has made it difficult to predict the effects of disturbance on soil CH₄ flux in various ecosystems. The most commonly reported disturbance effect is that of NH₄⁺ fertilizers, which can suppress soil CH₄ consumption by up to 70% (1, 8, 10, 17, 22, 32, 33, 37, 38, 43). In the field, inhibition may occur immediately following fertilization, may be delayed for months to years, or may never occur despite years of chronic fertilization (9, 17). This variety of responses may stem at least in part from the distribution of physiologically diverse methane oxidizer populations across sites (17, 18, 20).Of the various NH₄⁺ inhibition patterns, immediate inhibition is the best documented. As in field studies, however, physiological laboratory studies have produced variable results, suggesting that there may be multiple inhibition mechanisms (15, 17, 26–28, 36, 39). Physicochemical similarities between CH₄ and NH₃ may permit these two compounds to compete for enzyme active sites so that fortuitous NH₃ oxidation competitively inhibits CH₄ oxidation (38). Although this mechanism has been demonstrated to occur in pure cultures of methanotrophic bacteria (6) and in a CH₄-producing agricultural soil (15), it has not been demonstrated to occur in well-drained, nonagricultural mineral soils, which comprise the dominant terrestrial sink for atmospheric CH₄ (14, 38, 45), nor has it been demonstrated to occur at near-atmospheric CH₄ concentrations. In many cases, the kinetics of immediate NH₄⁺ inhibition in soil cannot be reconciled easily with substrate competition (15, 16, 26–28, 39). An alternative mechanism has been proposed, whereby the toxicity of NO₂⁻ or NH₂OH produced by fortuitous NH₄⁺ oxidation suppresses methanotrophic activity (26, 27, 39). Hence, multiple inhibition mechanisms may be involved, and these mechanisms may vary with the physiology of different CH₄ oxidizer populations (17).Two physiologically distinct communities of CH₄ oxidizers apparently exist in soil. One group, generally associated with atmospheric CH₄ consumption, exhibits an extremely high affinity for CH₄. Representatives of this group have yet to be cultivated or otherwise identified (9). The second group exhibits a much lower affinity for CH₄ and is generally associated with common methanotrophs, such as those that have been studied in pure culture for many years (2, 9). In upland mineral soils, only high-affinity activity is usually detectable without artificial enrichment with high CH₄ concentrations in the laboratory. However, the only prior study in which kinetic constants for NH₄⁺ inhibition of soil CH₄ oxidation were reported was conducted in a periodically moist, organic matter-rich agricultural soil with demonstrable methanogenesis (15, 16). Such a soil potentially harbors a rich community of CH₄ oxidizers representing a continuum from low-affinity organisms to high-affinity organisms. Although this important investigation demonstrated that NH₄⁺ inhibits CH₄ oxidation via enzymatic substrate competition in an agricultural humisol, it is unclear to what extent its results apply to well-drained mineral soils lacking endogenous CH₄ sources. Physiological studies of soil CH₄ oxidation typically derive kinetic constants from oxidation rates at CH₄ concentrations ranging from atmospheric levels (∼1.7 μl liter⁻¹) to ≫K_m for high-affinity CH₄ oxidizers. Even in soil in which only high-affinity organisms are active, the CH₄-oxidizing enzyme(s) could respond differently to NH₄⁺ at high CH₄ concentrations than at near-atmospheric concentrations (15, 39). Thus, to study NH₄⁺ inhibition of high-affinity CH₄ oxidizers per se, it would be preferable to examine inhibition kinetics at near-atmospheric CH₄ concentrations in a soil with no apparent endogenous CH₄ source.A common shortcoming of NH₄⁺ inhibition studies, regardless of the organisms involved, has been a lack of attention to nonammoniacal salt effects despite numerous reports of substantial inhibition by such salts (1, 10, 15, 17, 24). King and Schnell (28) examined the effects of several Cl⁻ and SO₄²⁻ salts and concluded that nonammoniacal salts indirectly inhibit CH₄ oxidation by desorbing endogenous NH₄⁺ from cation exchange sites in the soil, which then directly inhibit CH₄ oxidation. Many N-limited soils, however, have extremely low concentrations of exchangeable NH₄⁺, yet are substantially inhibited by nonammoniacal salts (17), suggesting that these salts have NH₄⁺-independent effects on atmospheric CH₄ oxidizers. Additional mechanisms may alter inhibition kinetics, thus hindering the diagnosis of NH₄⁺-specific inhibition.With the limitations described above in mind, we used a simple steady-state kinetics approach to assess the mechanism of NH₄⁺ inhibition of CH₄ oxidation at near-atmospheric concentrations (1.8 to 15 μl liter⁻¹) in three well-drained, N-limited forest soils that lack known endogenous CH₄ sources. In addition, we examined the effects of nonammoniacal salts in parallel samples to judge the utility of these salts as experimental controls for neutralizing NH₄⁺-independent salt effects.     

Contribution of Methanotrophic and Nitrifying Bacteria to CH4 and NH4+ Oxidation in the Rhizosphere of Rice Plants as Determined by New Methods of Discrimination

Methanotrophic and nitrifying bacteria are both able to oxidize CH₄ as well as NH₄⁺. To date it is not possible to estimate the relative contribution of methanotrophs to nitrification and that of nitrifiers to CH₄ oxidation and thus to assess their roles in N and C cycling in soils and sediments. This study presents new options for discrimination between the activities of methanotrophs and nitrifiers, based on the competitive inhibitor CH₃F and on recovery after inhibition with C₂H₂. By using rice plant soil as a model system, it was possible to selectively inactivate methanotrophs in soil slurries at a CH₄/CH₃F/NH₄⁺ molar ratio of 0.1:1:18. This ratio of CH₃F to NH₄⁺ did not affect ammonia oxidation, but methane oxidation was inhibited completely. By using the same model system, it could be shown that after 24 h of exposure to C₂H₂ (1,000 parts per million volume), methanotrophs recovered within 24 h while nitrifiers stayed inactive for at least 3 days. This gave an “assay window” of 48 h when only methanotrophs were active. Applying both assays to model microcosms planted with rice plants demonstrated a major contribution of methanotrophs to nitrification in the rhizosphere, while the contribution of nitrifiers to CH₄ oxidation was insignificant.     

The High Salt Requirement of the Moderate Halophile Chromohalobacter salexigens DSM3043 Can Be Met Not Only by NaCl but by Other Ions

The growth rate of Chromohalobacter salexigens DSM 3043 can be stimulated in media containing 0.3 M NaCl by a 0.7 M concentration of other salts of Na⁺, K⁺, Rb⁺, or NH₄⁺, Cl⁻, Br⁻, NO₃⁻, or SO₄²⁻ ions. To our knowledge, growth rate stimulation by a general high ion concentration has not been reported for any organism previously.     

Influence of Starvation on Potential Ammonia-Oxidizing Activity and amoA mRNA Levels of Nitrosospira briensis

The effect of short-term ammonia starvation on Nitrosospira briensis was investigated. The ammonia-oxidizing activity was determined in a concentrated cell suspension with a NO_x biosensor. The apparent half-saturation constant [K_m(app)] value of the NH₃ oxidation of N. briensis was 3 μM NH₃ for cultures grown both in continuous and batch cultures as determined by a NO_x biosensor. Cells grown on the wall of the vessel had a lower K_m(app) value of 1.8 μM NH₃. Nonstarving cultures of N. briensis showed potential ammonia-oxidizing activities of between 200 to 250 μM N h⁻¹, and this activity decreased only slowly during starvation up to 10 days. Within 10 min after the addition of fresh NH₄⁺, 100% activity was regained. Parallel with activity measurements, amoA mRNA and 16S rRNA were investigated. No changes were observed in the 16S rRNA, but a relative decrease of amoA mRNA was observed during the starvation period. During resuscitation, an increase in amoA mRNA expression was detected simultaneously. The patterns of the soluble protein fraction of a 2-week-starved culture of N. briensis showed only small differences in comparison to a nonstarved control. From these results we conclude that N. briensis cells remain in a state allowing fast recovery of ammonia-oxidizing activity after addition of NH₄⁺ to a starved culture. Maintaining cells in this kind of active state could be the survival strategy of ammonia-oxidizing bacteria in nature under fluctuating NH₄⁺ availability.     

Effects of Hypoxia on 13NH4+ Fluxes in Rice Roots : Kinetics and Compartmental Analysis

Techniques of compartmental (efflux) and kinetic influx analyses with the radiotracer ¹³NH₄⁺ were used to examine the adaptation to hypoxia (15, 35, and 50% O₂ saturation) of root N uptake and metabolism in 3-week-old hydroponically grown rice (Oryza sativa L., cv IR72) seedlings. A time-dependence study of NH₄⁺ influx into rice roots after onset of hypoxia (15% O₂) revealed an initial increase in the first 1 to 2.5 h after treatment imposition, followed by a decline to less than 50% of influx in control plants by 4 d. Efflux analyses conducted 0, 1, 3, and 5 d after the treatment confirmed this adaptation pattern of NH₄⁺ uptake. Half-lives for NH₄⁺ exchange with subcellular compartments, cytoplasmic NH₄⁺ concentrations, and efflux (as percentage of influx) were unaffected by hypoxia. However, significant differences were observed in the relative amounts of N allocated to NH₄⁺ assimilation and the vacuole versus translocation to the shoot. Kinetic experiments conducted at 100, 50, 35, and 15% O₂ saturation showed no significant change in the K_m value for NH₄⁺ uptake with varying O₂ supply. However, V_max was 42% higher than controls at 50% O₂ saturation, unchanged at 35%, and 10% lower than controls at 15% O₂. The significance of these flux adaptations is discussed.     

Platinum cross-linking of adenines and guanines on the quadruplex structures of the AG3(T2AG3)3 and (T2AG3)4 human telomere sequences in Na+ and K+ solutions

The quadruplex structures of the human telomere sequences AG₃(T₂AG₃)₃ I and (T₂AG₃)₄ II were investigated in the presence of Na⁺ and K⁺ ions, through the cross-linking of adenines and guanines by the cis- and trans-[Pt(NH₃)₂(H₂O)₂](NO₃)₂ complexes 1 and 2. The bases involved in chelation of the cis- and trans-Pt(NH₃)₂ moieties were identified by chemical and 3′-exonuclease digestions of the products isolated after denaturing gel electrophoresis. These are the four adenines of each sequence and four out of the 12 guanines. Two largely different structures have been reported for I: A from NMR data in Na⁺ solution and B from X-ray data of a K⁺-containing crystal. Structure A alone agrees with our conclusions about the formation of the A1–G10, A13–G22, A1–A13 platinum chelates at the top of the quadruplex and A7–A19, G4–A19 and A7–G20 at the bottom, whether the Na⁺ or K⁺ ion is present. At variance with a recent proposal that structures A and B could be the major species in Na⁺ and K⁺ solutions, respectively, our results suggest that structure A exists predominantly in the presence of both ions. They also suggest that covalent platinum cross-linking of a human telomere sequence could be used to inhibit telomerase.     

Properties of an Inwardly Rectifying ATP-sensitive K+ Channel in the Basolateral Membrane of Renal Proximal Tubule

The potassium conductance of the basolateral membrane (BLM) of proximal tubule cells is a critical regulator of transport since it is the major determinant of the negative cell membrane potential and is necessary for pump-leak coupling to the Na⁺,K⁺-ATPase pump. Despite this pivotal physiological role, the properties of this conductance have been incompletely characterized, in part due to difficulty gaining access to the BLM. We have investigated the properties of this BLM K⁺ conductance in dissociated, polarized Ambystoma proximal tubule cells. Nearly all seals made on Ambystoma cells contained inward rectifier K⁺ channels (γ_{slope, in} = 24.5 ± 0.6 pS, γ_{chord, out} = 3.7 ± 0.4 pS). The rectification is mediated in part by internal Mg²⁺. The open probability of the channel increases modestly with hyperpolarization. The inward conducting properties are described by a saturating binding–unbinding model. The channel conducts Tl⁺ and K⁺, but there is no significant conductance for Na⁺, Rb⁺, Cs⁺, Li⁺, NH₄⁺, or Cl⁻. The channel is inhibited by barium and the sulfonylurea agent glibenclamide, but not by tetraethylammonium. Channel rundown typically occurs in the absence of ATP, but cytosolic addition of 0.2 mM ATP (or any hydrolyzable nucleoside triphosphate) sustains channel activity indefinitely. Phosphorylation processes alone fail to sustain channel activity. Higher doses of ATP (or other nucleoside triphosphates) reversibly inhibit the channel. The K⁺ channel opener diazoxide opens the channel in the presence of 0.2 mM ATP, but does not alleviate the inhibition of millimolar doses of ATP. We conclude that this K⁺ channel is the major ATP-sensitive basolateral K⁺ conductance in the proximal tubule.     

Different transport mechanisms in plant and human AMT/Rh-type ammonium transporters

The conserved family of AMT/Rh proteins facilitates ammonium transport across animal, plant, and microbial membranes. A bacterial homologue, AmtB, forms a channel-like structure and appears to function as an NH₃ gas channel. To evaluate the function of eukaryotic homologues, the human RhCG glycoprotein and the tomato plant ammonium transporter LeAMT1;2 were expressed and compared in Xenopus oocytes and yeast. RhCG mediated the electroneutral transport of methylammonium (MeA), which saturated with K_m = 3.8 mM at pH_o 7.5. Uptake was strongly favored by increasing the pH_o and was inhibited by ammonium. Ammonium induced rapid cytosolic alkalinization in RhCG-expressing oocytes. Additionally, RhCG expression was associated with an alkali-cation conductance, which was not significantly permeable to NH₄⁺ and was apparently uncoupled from the ammonium transport. In contrast, expression of the homologous LeAMT1;2 induced pH_o-independent MeA⁺ uptake and specific NH₄⁺ and MeA⁺ currents that were distinct from endogenous currents. The different mechanisms of transport, including the RhCG-associated alkali-cation conductance, were verified by heterologous expression in appropriate yeast strains. Thus, homologous AMT/Rh-type proteins function in a distinct manner; while LeAMT1;2 carries specifically NH₄⁺, or cotransports NH₃/H⁺, RhCG mediates electroneutral NH₃ transport.     

Purification and Characterization of Monovalent Cation-Activated Levodione Reductase from Corynebacterium aquaticum M-13

(6R)-2,2,6-Trimethyl-1,4-cyclohexanedione (levodione) reductase was isolated from a cell extract of the soil isolate Corynebacterium aquaticum M-13. This enzyme catalyzed regio- and stereoselective reduction of levodione to (4R,6R)-4-hydroxy-2,2,6-trimethylcyclohexanone (actinol). The relative molecular mass of the enzyme was estimated to be 142,000 Da by high-performance gel permeation chromatography and 36,000 Da by sodium dodecyl sulfate-polyacrylamide gel electrophoresis. The enzyme required NAD⁺ or NADH as a cofactor, and it catalyzed reversible oxidoreduction between actinol and levodione. The enzyme was highly activated by monovalent cations, such as K⁺, Na⁺, and NH₄⁺. The NH₂-terminal and partial amino acid sequences of the enzyme showed that it belongs to the short-chain alcohol dehydrogenase/reductase family. This is the first report of levodione reductase.     

The bulge region of HIV-1 TAR RNA binds metal ions in solution

Binding of Mg²⁺, Ca²⁺ and Co(NH₃)₆³⁺ ions to the HIV-1 TAR RNA in solution was analysed by ¹⁹F NMR spectroscopy, metal ion-induced RNA cleavages and Brownian dynamics (BD) simulations. Chemically synthesised 29mer oligoribonucleotides of the TAR sequence labelled with 5-fluorouridine (FU) were used for ¹⁹F NMR-monitored metal ion titration. The chemical shift changes of fluorine resonances FU-23, FU-25 and FU-40 upon titration with Mg²⁺ and Ca²⁺ ions indicated specific, although weak, binding at the bulge region with the dissociation constants (K_d) of 0.9 ± 0.6 and 2.7 ± 1.7 mM, respectively. Argininamide, inducing largest ¹⁹F chemical shifts changes at FU-23, was used as a reference ligand (K_d = 0.3 ± 0.1 mM). In the Pb²⁺-induced TAR RNA cleavage experiment, strong and selective cleavage of the C24-U25 phosphodiester bond was observed, while Mg²⁺ and Ca²⁺ induced cuts at all 3-nt residues of the bulge. The inhibition of Pb²⁺-specific TAR cleavage by di- and trivalent metal ions revealed a binding specificity [in the order Co(NH₃)₆³⁺ > Mg²⁺ > Ca²⁺] at the bulge site. A BD simulation search of potential magnesium ion sites within the NMR structure of HIV-1 TAR RNA was conducted on a set of 20 conformers (PDB code 1ANR). For most cases, the bulge region was targeted by magnesium cations.     

The external K+ concentration and mutations in the outer pore mouth affect the inhibition of kv1.5 current by Ni2+

By examining the consequences both of changes of [K⁺]_o and of point mutations in the outer pore mouth, our goal was to determine if the mechanism of the block of Kv1.5 ionic currents by external Ni²⁺ is similar to that for proton block. Ni²⁺ block is inhibited by increasing [K⁺]_o, by mutating a histidine residue in the pore turret (H463Q) or by mutating a residue near the pore mouth (R487V) that is the homolog of Shaker T449. Aside from a slight rightward shift of the Q-V curve, Ni²⁺ had no effect on gating currents. We propose that, as with H_o⁺, Ni²⁺ binding to H463 facilitates an outer pore inactivation process that is antagonized by K_o⁺ and that requires R487. However, whereas H_o⁺ substantially accelerates inactivation of residual currents, Ni²⁺ is much less potent, indicating incomplete overlap of the profiles of these two metal ions. Analyses with Co²⁺ and Mn²⁺, together with previous results, indicate that for the first-row transition metals the rank order for the inhibition of Kv1.5 in 0 mM K_o⁺ is Zn²⁺ (K_D ~ 0.07 mM) ≥ Ni²⁺ (K_D ~ 0.15 mM) > Co²⁺ (K_D ~ 1.4 mM) > Mn²⁺ (K_D > 10 mM).     

Source and Magnitude of Ammonium Generation in Maize Roots

Studies with ¹⁵N indicate that appreciable generation of NH₄⁺ from endogenous sources accompanies the uptake and assimilation of exogenous NH₄⁺ by roots. To identify the source of NH₄⁺ generation, maize (Zea mays L.) seedlings were grown on ¹⁴NH₄⁺ and then exposed for 3 d to highly labeled ¹⁵NH₄⁺. More of the entering ¹⁵NH₄⁺ was incorporated into the protein-N fraction of roots in darkness (approximately 25%) than in the light (approximately 14%). Although the ¹⁴NH₄⁺ content of roots declined rapidly to less than 1 μmol per plant, efflux of ¹⁴NH₄⁺ continued throughout the 3-d period at an average daily rate of 14 μmol per plant. As a consequence, cumulative ¹⁴NH₄⁺ efflux during the 3-d period accounted for 25% of the total ¹⁴N initially present in the root. Although soluble organic ¹⁴N in roots declined during the 3-d period, insoluble ¹⁴N remained relatively constant. In shoots both soluble organic ¹⁴N and ¹⁴NH₄⁺ declined, but a comparable increase in insoluble ¹⁴N was noted. Thus, total ¹⁴N in shoots remained constant, reflecting little or no net redistribution of ¹⁴N between shoots and roots. Collectively, these observations reveal that catabolism of soluble organic N, not protein N, is the primary source of endogenous NH₄⁺ generation in maize roots.     

P-Loop Residues Critical for Selectivity in K+ Channels Fail to Confer Selectivity to Rabbit HCN4 Channels

HCN channels are thought to be structurally similar to K_v channels, but show much lower selectivity for K⁺. The ∼3.3 Å selectivity filter of K⁺ channels is formed by the pore-lining sequence XT(V/I)GYG, with X usually T, and is held stable by key residues in the P-loop. Differences in the P-loop sequence of HCN channels (eg. the pore-lining sequence L₄₇₈C₄₇₉IGYG) suggest these residues could account for differences in selectivity between these channel families. Despite being expressed, L478T/C479T HCN4 channels did not produce current. Since threonine in the second position is highly conserved in K⁺ channels, we also studied C479T channels. Based on permeability ratios (P_X/P_K), C479T HCN4 channels (K⁺(1)>Rb⁺(0.85)>Cs⁺(0.59)>Li⁺(0.50)≥Na⁺(0.49)) were less selective than WT rabbit HCN4 (K⁺(1)>Rb⁺(0.48)>Cs⁺(0.31)≥Na⁺(0.29)>Li⁺(0.03)), indicating that the TIGYG sequence is insufficient to confer K⁺ selectivity to HCN channels. C479T HCN4 channels had an increased permeability to large organic cations than WT HCN4 channels, as well as increased unitary K⁺ conductance, and altered channel gating. Collectively, these results suggest that HCN4 channels have larger pores than K⁺ channels and replacement of the cysteine at position 479 with threonine further increases pore size. Furthermore, selected mutations in other regions linked previously to pore stability in K⁺ channels (ie. S475D, S475E and F471W/K472W) were also unable to confer K⁺ selectivity to C479T HCN4 channels. Our findings establish the presence of the TIGYG pore-lining sequence does not confer K⁺ selectivity to rabbit HCN4 channels, and suggests that differences in selectivity of HCN4 versus K⁺ channels originate from differences outside the P-loop region.     

Varied Diazotrophies, Morphologies, and Toxicities of Genetically Similar Isolates of Cylindrospermopsis raciborskii (Nostocales, Cyanophyceae) from Northern Australia

The potentially toxic freshwater cyanobacterium Cylindrospermopsis raciborskii has become increasingly prevalent in tropical and temperate water bodies worldwide. This paper investigates the effects of different nitrogen sources (NO₃⁻, NH₄⁺, and omission of a fixed form of nitrogen) on the growth rates, morphologies, and cylindrospermopsin (CYL) concentrations (expressed as a percentage of the freeze-dried weight) of seven C. raciborskii isolates obtained from a range of water bodies in northern Australia and grown in batch culture. In general, growth rates were lowest in the absence of a fixed-nitrogen source and highest with NH₄⁺ as the nitrogen source. Conversely, the highest concentrations of CYL were recorded in cultures grown in the absence of a fixed-nitrogen source and the lowest were found in cultures supplied with NH₄⁺. Cultures supplied with NO₃⁻ were intermediate with respect to both CYL concentration and growth rate. Different nitrogen sources resulted in significant differences in the morphology of C. raciborskii trichomes. Most notable were the loss of heterocysts and the tapering of end cells in cultures supplied with NH₄⁺ and the statistically significant increase in vegetative cell length (nitrogen depleted < NO₃⁻ < NH₄⁺). The morphological changes induced by different nitrogen sources were consistent for all isolates, despite measurable differences in vegetative-cell and heterocyst dimensions among isolates. Such induced morphological variation has implications for Cylindrospermopsis taxonomy, given that distinctions between species are based on minor and overlapping differences in cell lengths and widths. The close phylogenetic association among all seven isolates was confirmed by the high level (>99.8%) of similarity of their 16S rRNA gene sequences. Another genetic technique, analysis of the HIP1 octameric-palindrome repeated sequence, showed greater heterogeneity among the isolates and appears to be a useful method for distinguishing among isolates of C. raciborskii.     

Structural basis of polyamine-DNA recognition: spermidine and spermine interactions with genomic B-DNAs of different GC content probed by Raman spectroscopy

Four genomic DNAs of differing GC content (Micrococcus luteus, 72% GC; Escherichia coli, 50% GC; calf thymus, 42% GC; Clostridium perfringens, 27% GC) have been employed as targets of interaction by the cationic polyamines spermidine {[H₃N(CH₂)₃NH₂(CH₂)₄NH₃]³⁺} and spermine {[(CH₂)₄(NH₂(CH₂)₃NH₃)₂]⁴⁺}. In solutions containing 60 mM DNA phosphate (~20 mg DNA/ml) and either 1, 5 or 60 mM polyamine, only Raman bands associated with the phosphates exhibit large spectral changes, demonstrating that B-DNA phosphates are the primary targets of interaction. Phosphate perturbations, which are independent of base composition, are consistent with a model of non-specific cation binding in which delocalized polyamines diffuse along DNA while confined by the strong electrostatic potential gradient perpendicular to the helix axis. This finding provides experimental support for models in which polyamine-induced DNA condensation is driven by non-specific electrostatic binding. The Raman spectra also demonstrate that major groove sites (guanine N7 and thymine C5H₃) are less affected than phosphates by polyamine–DNA interactions. Modest dependence of polyamine binding on genome base composition suggests that sequence context plays only a secondary role in recognition. Importantly, the results demonstrate that polyamine binding has a negligible effect on the native B-form secondary structure. The capability of spermidine or spermine to bind and condense genomic B-DNA without disrupting the native structure must be taken into account when considering DNA organization within bacterial nucleoids or cell nuclei.     

Nitrate-ammonium synergism in rice. A subcellular flux analysis

Many reports have shown that plant growth and yield is superior on mixtures of NO₃⁻ and NH₄⁺ compared with provision of either N source alone. Despite its clear practical importance, the nature of this N-source synergism at the cellular level is poorly understood. In the present study we have used the technique of compartmental analysis by efflux and the radiotracer ¹³N to measure cellular turnover kinetics, patterns of flux partitioning, and cytosolic pool sizes of both NO₃⁻ and NH₄⁺ in seedling roots of rice (Oryza sativa L. cv IR72), supplied simultaneously with the two N sources. We show that plasma membrane fluxes for NH₄⁺, cytosolic NH₄⁺ accumulation, and NH₄⁺ metabolism are enhanced by the presence of NO₃⁻, whereas NO₃⁻ fluxes, accumulation, and metabolism are strongly repressed by NH₄⁺. However, net N acquisition and N translocation to the shoot with dual N-source provision are substantially larger than when NO₃⁻ or NH₄⁺ is provided alone at identical N concentrations.     

The Na+-Responsive ntp Operon Is Indispensable for Homeostatis of K+ and Na+ in Enterococcus hirae at Limited Proton Potential

Enterococcus hirae ATCC 9790 grew well in Na⁺-deficient, low-K⁺ medium, but growth was inhibited by carbonylcyanide m-chlorophenylhydrazone (CCCP). Growth inhibition and decrease of cellular K⁺ levels in the presence of CCCP were relieved by the addition of Na⁺ and a high concentration of K⁺. In contrast, in the mutant defective in Na⁺-ATPase or the NtpJ component of the KtrII K⁺ uptake system, CCCP-induced growth inhibition was rescued by a high concentration of K⁺ but not of Na⁺. These transporters are thus indispensable for homeostatis of K⁺ and Na⁺ at low proton potential.     

Purification, Characterization, and Gene Cloning of Purine Nucleosidase from Ochrobactrum anthropi

A bacterium, Ochrobactrum anthropi, produced a large amount of a nucleosidase when cultivated with purine nucleosides. The nucleosidase was purified to homogeneity. The enzyme has a molecular weight of about 170,000 and consists of four identical subunits. It specifically catalyzes the irreversible N-riboside hydrolysis of purine nucleosides, the K_m values being 11.8 to 56.3 μM. The optimal activity temperature and pH were 50°C and pH 4.5 to 6.5, respectively. Pyrimidine nucleosides, purine and pyrimidine nucleotides, NAD, NADP, and nicotinamide mononucleotide are not hydrolyzed by the enzyme. The purine nucleoside hydrolyzing activity of the enzyme was inhibited (mixed inhibition) by pyrimidine nucleosides, with K_i and K_i′ values of 0.455 to 11.2 μM. Metal ion chelators inhibited activity, and the addition of Zn²⁺ or Co²⁺ restored activity. A 1.5-kb DNA fragment, which contains the open reading frame encoding the nucleosidase, was cloned, sequenced, and expressed in Escherichia coli. The deduced 363-amino-acid sequence including a 22-residue leader peptide is in agreement with the enzyme molecular mass and the amino acid sequences of NH₂-terminal and internal peptides, and the enzyme is homologous to known nucleosidases from protozoan parasites. The amino acid residues forming the catalytic site and involved in binding with metal ions are well conserved in these nucleosidases.     

Effects of Ammonium and Non-Ammonium Salt Additions on Methane Oxidation by Methylosinus trichosporium OB3b and Maine Forest Soils

Additions of ammonium and non-ammonium salts inhibit atmospheric methane consumption by soil at salt concentrations that do not significantly affect the soil water potential. The response of soils to non-ammonium salts has previously raised questions about the mechanism of ammonium inhibition. Results presented here show that inhibition of methane consumption by non-ammonium salts can be explained in part by ion-exchange reactions: cations desorb ammonium, with the level of desorption varying as a function of both the cation and anion added; differential desorption results in differential inhibition levels. Differences in the extent of inhibition among ammonium salts can also be explained in part by the effects of anions on ammonium exchange. In contrast, only minimal effects of cations and anions are observed in liquid cultures of Methylosinus trichosporium OB3b. The comparable level of inhibition by equinormal concentrations of NH₄Cl and (NH₄)₂SO₄ and the insensitivity of salt inhibition to increasing methane concentrations (from 10 to 100 ppm) are of particular interest, since both of these patterns are in contrast to results for soils. The greater inhibition of methane consumption for NH₄Cl than (NH₄)₂SO₄ in soils can be attributed to increased ammonium adsorption by sulfate; increasing inhibition by non-ammonium salts with increasing methane concentrations can be attributed to desorbed ammonium and a physiological mechanism proposed previously for pure cultures.     

Change of RNase P RNA function by single base mutation correlates with perturbation of metal ion binding in P4 as determined by NMR spectroscopy

The solution structures of two 27 nt RNA hairpins and their complexes with cobalt(III)-hexammine [Co(NH₃)₆³⁺] were determined by NMR spectroscopy. The RNA hairpins are variants of the P4 region from Escherichia coli RNase P RNA: a U-to-A mutant changing the identity of the bulged nucleotide, and a U-to-C, C-to-U double mutant changing only the bulge position. Structures calculated from NMR constraints show that the RNA hairpins adopt different conformations. In the U-to-C, C-to-U double mutant, the conserved bulged uridine in the P4 wild-type stem is found to be shifted in the 3′-direction by one nucleotide when compared with the wild-type structure. Co(NH₃)₆³⁺ is used as a spectroscopic probe for Mg(H₂O)₆²⁺ binding sites because both complexes have octahedral symmetry and have similar radii. Intermolecular NOE crosspeaks between Co(NH₃)₆³⁺ and RNA protons were used to locate the site of Co(NH₃)₆³⁺ binding to both RNA hairpins. The metal ion binds in the major groove near a bulge loop in both mutants, but is shifted 3′ by about one base pair in the double mutant. The change of the metal ion binding site is compared with results obtained on corresponding mutant RNase P RNA molecules as reported by Harris and co-workers (RNA, 1, 210–218).