Effect of the Spartina alterniflora Root-Rhizome System on Salt Marsh Soil Denitrifying Bacteria

Nitrous oxide (N₂O) reductase activity was used as an index of the denitrification potential in salt marsh soils. In a short Spartina alterniflora marsh, the seasonal distribution of N₂O reductase activity indicated a causal relationship between S. alterniflora root-rhizome production and the denitrification potential of the soil system. The relationship was not discerned in samples from a tall S. alterniflora marsh. To further examine the in situ plant-denitrifier interaction in the short S. alterniflora marsh, plots with and without living S. alterniflora were established and analyzed for N₂O reductase activity 5 and 18 months later. In the plots without living Spartina there was a significant reduction in the soil denitrification potential after 18 months, indicating that in the SS marsh the denitrifiers are tightly coupled to the seasonal production of below-ground Spartina macroorganic matter. In plots with intact Spartina, the soil denitrification potential was not altered by NH₄NO₃ or glucose enrichment. However, in plots without living Spartina, there were significant changes in soil N₂O reductase activity, thus indicating that the plants can serve as a “buffer” against this form of pulse perturbation.     

Molecular Analysis of Diazotroph Diversity in the Rhizosphere of the Smooth Cordgrass, Spartina alterniflora

N₂ fixation by diazotrophic bacteria associated with the roots of the smooth cordgrass, Spartina alterniflora, is an important source of new nitrogen in many salt marsh ecosystems. However, the diversity and phylogenetic affiliations of these rhizosphere diazotrophs are unknown. Denaturing gradient gel electrophoresis (DGGE) of PCR-amplified nifH sequence segments was used in previous studies to examine the stability and dynamics of the Spartina rhizosphere diazotroph assemblages in the North Inlet salt marsh, near Georgetown, S.C. In this study, plugs were taken from gel bands from representative DGGE gels, the nifH amplimers were recovered and cloned, and their sequences were determined. A total of 59 sequences were recovered, and the amino acid sequences predicted from them were aligned with sequences from known and unknown diazotrophs in order to determine the types of organisms present in the Spartina rhizosphere. We recovered numerous sequences from diazotrophs in the γ subdivision of the division Proteobacteria (γ-Proteobacteria) and from various anaerobic diazotrophs. Diazotrophs in the α-Proteobacteria were poorly represented. None of the Spartina rhizosphere DGGE band sequences were identical to any known or previously recovered environmental nifH sequences. The Spartina rhizosphere diazotroph assemblage is very diverse and apparently consists mainly of unknown organisms.     

Nitrogen Fixation (Acetylene Reduction) in a Salt Marsh Amended with Sewage Sludge and Organic Carbon and Nitrogen Compounds

Seasonal distribution of nitrogen fixation by Spartina alterniflora epiphytes and in surface and soil samples was investigated in a Georgia salt marsh which was amended with sewage sludge or with glucose and/or ammonium nitrate. There was no significant difference between the rates of fixation in the unamended and sewage sludge plots. Additional perturbation experiments suggested that nitrogen addition indirectly stimulates nitrogen fixation by enhancing Spartina production and root exudation. Glucose additions, on the other hand, suppressed nitrogen fixation on a long-term basis. It is suggested that the microbial population in the soil out-competed the plants for the available nitrogen and in turn suppressed plant production and possibly root exudation. A comparison of nitrogen fixation in clipped and unclipped Spartina plots substantiated the suggestion that root exudation probably supports nitrogen fixation. Fixation in the clipped plots was significantly lower (P < 0.05) than the rates in the unclipped plots.     

Seasonal patterns of daily net photosynthesis,transpiration and net primary productivity of Juncus roemerianus and Spartina alterniflora in a Georgia salt marsh

Summary Studies of the seasonal CO₂ and water vapor exchange patterns of Juncus roemerianus and Spartina alterniflora were conducted in an undisturbed marsh community on Sapelo Island, Georgia. Daily patterns of net photosynthesis, transpiration, leaf diffusive conductance and water-use efficiency in response to ambient conditions were monitored on intact, in situ plants. Net primary productivity was calculated from the daytime CO₂ fixation totals, nighttime CO₂ loss, leaf standing stock and aboveground to belowground biomass ratios for each plant type.The tall form of S. alterniflora had higher rates of photosynthesis and higher water-use efficiency values which, in conjunction with low respiratory losses and large leaf standing crop, results in high values of net primary productivity. The environmental factors in the marsh which permit these physiological responses occur in less than 10% of the marsh. Overall, the physiological capabilities of the short form of S. alterniflora were reduced in comparison to the tall form, but the combination of environmental factors which determine the physiological responses of this form occur in a much greater portion of the marsh, and the short form of S. alterniflora dominates the Sapelo Island marshes.The response patterns of the C₃ species, J. roemerianus, differed somewhat from the height forms of S. alterniflora. A large, seasonally constant leaf standing crop coupled with moderate rates of photosynthesis resulted in a net primary productivity value which was between the tall and short height forms of S. alterniflora. However, as with the tall S. alterniflora, the environmental conditions under which this high productivity and high water loss rate can be sustained are restricted to specific regions of the environmental gradient in the marsh.Contribution No. 435 from the University of Georgia Marine Institute     

Populations of Methane-Producing Bacteria and In Vitro Methanogenesis in Salt Marsh and Estuarine Sediments

Most probable numbers (MPNs) of methanogens in various salt marsh and estuarine sediments were determined with an anaerobic, habitat-simulating culture medium with 80% H₂ plus 20% CO₂ as substrate. Average MPNs for the short Spartina (SS) marsh sediments of Sapelo Island, Ga., were maximal at the 5- to 7-cm depth (1.2 × 10⁷/g of dry sediment). Populations decreased to approximately 880/g of dry sediment at the 34- to 36-cm depth. There was no significant difference between summer and winter populations. In tall Spartina (TS) marsh sediments, average populations were maximal (1.2 × 10⁶/g of dry sediment) in the upper 0- to 2-cm zone; populations from the 5- to 36-cm zones were similar (average of 9 × 10⁴/g of dry sediment). Methanogenic populations for TS sediments of James Island Creek marsh, Charleston, S.C., were similar (average of 3 × 10⁶/g of dry sediment) for all depths tested (0 to 22 cm), which was comparable to the trend observed for TS sediments at Sapelo Island, Ga. Sediment grab samples collected along a transect of James Island Creek and its adjacent Spartina marsh had MPNs that were approximately 20 times greater for the region of Spartina growth (average of 10⁶/g of dry sediment) compared with the channel (approximately 5 × 10⁴ methanogens per g of dry sediment). A similar trend was found at Pawley's Island marsh, S.C., but populations were approximately one order of magnitude lower. In vitro rates of methanogenesis with SS sediments incubated under 80% H₂-20% CO₂ showed that the 5- to 7-cm region exhibited maximal activity (51 nmol of CH₄ g⁻¹ h⁻¹), which was greater than rates for sediments above and below this depth. SS sediment samples (5 to 7 cm) incubated under 100% N₂ and supplemented with formate exhibited rates of methanogenesis similar to those generated by samples under 80% H₂-20% CO₂. Replacing the N₂ atmosphere with H₂ resulted in an eightfold decrease in the rate of methanogenesis. In vitro methanogenic activity by TS salt marsh sediments, incubated under 80% H₂-20% CO₂, was similar for all depths tested (0 to 22 cm). TS sediment samples (0 to 7 cm) supplemented with formate and incubated under 100% N₂ had greater rates of methanogenesis compared with unsupplemented samples.     

Enumeration and Localization of N2-Fixing Bacteria Associated with Roots of Spartina alterniflora Loisel

Numbers and possible locations of N₂-fixing bacteria were investigated in roots of Spartina alterniflora Loisel, which support nitrogenase activity in the undisturbed native habitat. N₂-fixing bacteria were recovered in cultures both from S. alterniflora roots and from the surrounding sediment, and they formed a greater proportion of the bacteria recovered from root homogenates than from salt-marsh sediment. N₂-fixing bacteria were recovered in high numbers from the rhizoplane of S. alterniflora after roots were treated with 1 or 5% chloramine-T for 1 h or with 1% NaOCl for 1 or 2 h. Immersing S. alterniflora roots in 5% NaOCl for 1 h was more effective in distinguishing bacteria inside the roots since this treatment nearly eliminated N₂-fixing bacteria recoverable from the rhizoplane, although high numbers of N₂-fixing bacteria were recovered from homogenates of roots treated with 5% NaOCl for 1 h. However, this treatment was less effective with roots of Zea mays L. (Funks G4646) and Sorghum bicolor (L.) Moench (CK-60 A), indicating that techniques to surface sterilize roots should be evaluated for different plants. Bacteria were observed by light and electron microscopy inter- and intracellularly in the cortex and in the aerenchyma of S. alterniflora roots. This study clearly shows that bacteria, including N₂ fixers, colonize the interior of roots of S. alterniflora growing in a Chesapeake Bay, Maryland, salt marsh.     

Interactions among nitrogen fixation and soil phosphorus acquisition strategies in lowland tropical rain forests

Paradoxically, symbiotic dinitrogen (N₂) fixers are abundant in nitrogen (N)‐rich, phosphorus (P)‐poor lowland tropical rain forests. One hypothesis to explain this pattern states that N₂ fixers have an advantage in acquiring soil P by producing more N‐rich enzymes (phosphatases) that mineralise organic P than non‐N₂ fixers. We assessed soil and root phosphatase activity between fixers and non‐fixers in two lowland tropical rain forest sites, but also addressed the hypothesis that arbuscular mycorrhizal (AM) colonisation (another P acquisition strategy) is greater on fixers than non‐fixers. Root phosphatase activity and AM colonisation were higher for fixers than non‐fixers, and strong correlations between AM colonisation and N₂ fixation at both sites suggest that the N–P interactions mediated by fixers may generally apply across tropical forests. We suggest that phosphatase enzymes and AM fungi enhance the capacity of N₂ fixers to acquire soil P, thus contributing to their high abundance in tropical forests.     

Effect of Sulfide on Nitrogen Fixation in a Stream Sediment-Water System

Nitrogen fixation (C₂H₂ reduction) in a sediment-water system was studied under anaerobic incubation conditions. Sodium sulfide at low concentrations stimulated activity, with a twofold increase in C₂H₄ production occurring in the presence of 8 μmol of S²⁻ per ml of stream water. Sodium sulfide at concentrations of 16 μmol of S²⁻ per ml or greater inhibited nitrogen fixation, with 64 μmol of S²⁻ per ml being completely inhibitory. Sulfide at levels of 16 μmol/ml or above inhibited CO₂ production, and the degree of inhibition increased with increasing concentration of sulfide. Titanium (III) citrate (used to modify Eh levels) stimulated both nitrogen fixation and CO₂ production, but could not duplicate, at any concentration tested, the twofold increase in nitrogen fixation caused by 8 μmol of S²⁻ per ml. Sulfide additions caused pH changes in the sediment, and when the sediment was adjusted and maintained at pH 7.0 all concentrations of sulfide inhibited nitrogen fixation activity. From considerations of the redox equilibria of H₂, H₂S, and other sulfur species at various pH values, it appeared that H₂S was the toxic entity and that HS⁻ was less toxic. The observed stimulation of activity was apparently due to a pH change coupled with the concurrent production of HS⁻ from H₂S.     

Nitrogen Transfer from Four Nitrogen-Fixer Associations to Plants and Soils

Nitrogen (N) fixation is the main source of ‘new’ N for N-limited ecosystems like subarctic and arctic tundra. This crucial ecosystem function is performed by a wide range of N₂ fixer (diazotroph) associations that could differ fundamentally in their timing and amount of N release to the soil. To assess the importance of different associative N₂ fixers for ecosystem N cycling, we tracked ¹⁵N-N₂ into four N₂-fixer associations (with a legume, lichen, free-living, moss) and into soil, microbial biomass and non-diazotroph-associated plants 3 days and 5 weeks after in situ labelling. In addition, we tracked ¹³C from ¹³CO₂ labelling to assess if N and C fixation are linked. Three days after labelling, half of the fixed ¹⁵N was recovered in the legume soils, indicating a fast release of fixed N₂. Within 5 weeks, the free-living N₂ fixers released two-thirds of the fixed ¹⁵N into the soil, whereas the lichen and moss retained the fixed ¹⁵N. Carbon and N₂ fixation were linked in the lichen shortly after labelling, in free-living N₂ fixers 5 weeks after labelling, and in the moss at both sampling times. The four investigated N₂-fixer associations released fixed N₂ at different rates into the soil, and non-diazotroph-associated plants have no access to ‘new’ N within several weeks after N₂ fixation. Although legumes and free-living N₂ fixers are immediate sources of ‘new’ N for N-limited tundra ecosystems, lichens and especially mosses, do not contribute to increase the N pool via N₂ fixation in the short term.     

Co-Regulations of Spartina alterniflora Invasion and Exogenous Nitrogen Loading on Soil N2O Efflux in Subtropical Mangrove Mesocosms

Both plant invasion and nitrogen (N) enrichment should have significant impact on mangrove ecosystems in coastal regions around the world. However, how N₂O efflux in mangrove wetlands responds to these environmental changes has not been well studied. Here, we conducted a mesocosm experiment with native mangrove species Kandelia obovata, invasive salt marsh species Spartina alterniflora, and their mixture in a simulated tide rotation system with or without nitrogen addition. In the treatments without N addition, the N₂O effluxes were relatively low and there were no significant variations among the three vegetation types. A pulse loading of exogenous ammonium nitrogen increased N₂O effluxes from soils but the stimulatory effect gradually diminished over time, suggesting that frequent measurements are necessary to accurately understand the behavior of N-induced response of N₂O emissions. With the N addition, the N₂O effluxes from the invasive S. alterniflora were lower than that from native K. obovata mesocosms. This result may be attributed to higher growth of S. alterniflora consuming most of the available nitrogen in soils, and thus inhibiting N₂O production. We concluded that N loading significantly increased N₂O effluxes, while the invasion of S. alterniflora reduced N₂O effluxes response to N loading in this simulated mangrove ecosystem. Thus, both plant invasion and excessive N loading can co-regulate soil N₂O emissions from mangrove wetlands, which should be considered when projecting future N₂O effluxes from this type of coastal wetland.     

Seasonal patterns of CO2 and water vapor exchange of the tall and short height forms of Spartina alterniflora Loisel in a Georgia salt marsh

Summary Seasonal patterns of the responses of net photosynthesis, transpiration, leaf diffusive conductance, water-use efficiency and respiration to temperature, light and CO₂ concentration were determined on intact plants of the short and tall height forms of Spartina alterniflora. The studies were conducted on in situ plants in an undisturbed marsh community on Sapelo Island, Ga. Net photosynthesis of the tall form at full sunlight was significantly higher than the short form except during the winter months. Tall S. alterniflora did not light saturate during any season, whereas the short form tended to saturate during all seasons except the summer. The temperature optima of photosynthesis of both forms were similar and showed acclimation to prevailing seasonal temperatures. Leaf conductances to water vapor decreased with increasing temperature and were significantly different between the height forms only at higher temperatures. Dark respiration was relatively low at seasonal temperatures, but increased with temperature. Dark respiration and the respiratory Q₁₀ of the short form tended to be slightly higher than those of the tall form during all seasons. Transpiration rates and water-use efficiency of the tall form were generally higher than the short form.The seasonal response patterns showed intrinsic differences in the capacities of the height forms to metabolize CO₂ and respond to prevailing environmental parameters. Analyses of the components of the CO₂ diffusion pathway suggested that metabolic or internal components were more important than stomatal factors in determining the photosynthetic patterns of the short height form. It is suggested that the observed differences in the physiological responses of the height forms of the C₄ species are due to micro-habitat differences between the low and high marsh. Higher salinity, lower nitrogen availability and other soil factors may limit the CO₂ and water vapor exchange capacity of the short form compared to the tall.Contribution No. 401 from the University of Georgia Marine Institute     

Effect of Altered pO(2) in the Aerial Part of Soybean on Symbiotic N(2) Fixation

Dry matter accumulation, nitrogen content and N₂ fixation rates of soybean (Glycine max [L.] Merr. cv. Wye) plants grown in chambers in which the aerial portion was exposed to a pO₂ of 5, 10, 21, or 30% and a pCO₂ of 300 μl CO₂/l or a pO₂ of 21% and a pCO₂ of 1200 μl CO₂/l during the complete growth cycle were measured. Total N₂[C₂H₂] fixed was increased by CO₂/O₂ ratios greater than those in air and was decreased by ratios smaller than those in air; the effects on N₂ fixation of decreased pO₂ or elevated pCO₂ were quantitatively similar during the period of vegetative growth. Decreased pO₂ produced a smaller increase then elevated pCO₂ during the reproductive period, presumably because of the decreased sink activity of the arrested reproductive growth under subambient pO₂. At a pO₂ of 5% and a pCO₂ of 300 μl CO₂/l total N₂ fixed was increased 125% and per cent nitrogen content in the vegetative parts was increased relative to air while that in the seed was decreased. Dry matter production was increased and reproductive growth was arrested as previously reported for plants receiving only fertilizer nitrogen. At a pO₂ of 30% and a pCO₂ of 300 μl CO₂/l total N₂ fixed was decreased 50% and per cent nitrogen content in the vegetative part was increased relative to air while that in the reproductive structures was unaffected. Dry matter production was similarly decreased in both vegetative and reproductive structures. These effects of altered pO₂ in the aerial part on N₂ fixation are consistent with the hypothesis that the amount of photosynthate available to the nodule may be the most significant primary factor limiting N₂ fixation while sink activity of the reproductive structures may be a secondary factor.     

Accumulation of proline and glycinebetaine in Spartina alterniflora Loisel. in response to NaCl and nitrogen in the marsh

Summary The possible interaction of high soil salinity and low soil nitrogen content in affecting the growth of Spartina alterniflora Loisel in the high and low marshes of the Eastern U.S. was explored. Throughout the whole growing season, the short plants growing in the high marsh, where there was a higher soil salinity and lower available soil nitrogen, contained more proline and glycinebetaine and showed a lower leaf water potential than the tall plants growing in the low marsh. In both short and tall plants, the growing season, with the highest content occurring in spring and fall. In contrast, the glycinebetaine content in both short and tall plants remained fairly constant throughout the growing season, and was consistently at least 10 fold higher than the proline content. It is estimated that 19–30% of the total leaf nitrogen was in the form of proline and glycinebetaine in the short plants, and 14–27% in the tall plants. Ammonium nitrate fertilization in the field resulted in increased growth, higher proline and glycinebetaine contents, and lower water potentials in the short plants, but had little effect on these parameters in the tall plants. We suggest that in the low marsh, the plants can obtain sufficient nitrogen for osmoregulation and other metabolism. In the high marsh with higher soil salinity and lower nitrogen content, the plants have to allocate a even greater proportion of the already limited nitrogen supply for osmoregulation. Thus, nitrogen available for osmoregulation and other nitrogen-requiring metabolism is insufficient, resulting in reduced growth.     

Measurement of Nitrous Oxide Reductase Activity in Aquatic Sediments

Denitrification in aquatic sediments was measured by an N₂O reductase assay. Sediments consumed small added quantities of N₂O over short periods (a few hours). In experiments with sediment slurries, N₂O reductase activity was inhibited by O₂, C₂H₂, heat treatment, and by high levels of nitrate (1 mM) or sulfide (10 mM). However, ambient levels of nitrate (<100 μM) did not influence activity, and moderate levels (about 150 μM) induced only a short lag before reductase activity began. Moderate levels of sulfide (<1 mM) had no effect on N₂O reductase activity. Nitrous oxide reductase displayed Michaelis-Menten kinetics in sediments from freshwater (K_m = 2.17 μM), estuarine (K_m = 14.5 μM), and alkaline-saline (K_m = 501 μM) environments. An in situ assay was devised in which a solution of N₂O was injected into sealed glass cores containing intact sediment. Two estimates of net rates of denitrification in San Francisco Bay under approximated in situ conditions were 0.009 and 0.041 mmol of N₂O per m² per h. Addition of chlorate to inhibit denitrification in these intact-core experiments (to estimate gross rates of N₂O consumption) resulted in approximately a 14% upward revision of estimates of net rates. These results were comparable to an in situ estimate of 0.022 mmol of N₂O per m² per h made with the acetylene block assay.     

Simultaneous Measurement of Denitrification and Nitrogen Fixation Using Isotope Pairing with Membrane Inlet Mass Spectrometry Analysis

A method for estimating denitrification and nitrogen fixation simultaneously in coastal sediments was developed. An isotope-pairing technique was applied to dissolved gas measurements with a membrane inlet mass spectrometer (MIMS). The relative fluxes of three N₂ gas species (²⁸N₂, ²⁹N₂, and ³⁰N₂) were monitored during incubation experiments after the addition of ¹⁵NO₃⁻. Formulas were developed to estimate the production (denitrification) and consumption (N₂ fixation) of N₂ gas from the fluxes of the different isotopic forms of N₂. Proportions of the three isotopic forms produced from ¹⁵NO₃⁻ and ¹⁴NO₃⁻ agreed with expectations in a sediment slurry incubation experiment designed to optimize conditions for denitrification. Nitrogen fixation rates from an algal mat measured with intact sediment cores ranged from 32 to 390 μg-atoms of N m⁻² h⁻¹. They were enhanced by light and organic matter enrichment. In this environment of high nitrogen fixation, low N₂ production rates due to denitrification could be separated from high N₂ consumption rates due to nitrogen fixation. Denitrification and nitrogen fixation rates were estimated in April 2000 on sediments from a Texas sea grass bed (Laguna Madre). Denitrification rates (average, 20 μg-atoms of N m⁻² h⁻¹) were lower than nitrogen fixation rates (average, 60 μg-atoms of N m⁻² h⁻¹). The developed method benefits from simple and accurate dissolved-gas measurement by the MIMS system. By adding the N₂ isotope capability, it was possible to do isotope-pairing experiments with the MIMS system.     

Mineralization of Detrital Lignocelluloses by Salt Marsh Sediment Microflora

Specifically radiolabeled ¹⁴C-(cellulose)-lignocellulose and ¹⁴C-(lignin)-lignocellulose were isolated from labeled cuttings of Spartina alterniflora (cordgrass) and Pinus elliottii (slash pine). These were used to estimate the rates of mineralization to CO₂ of lignocelluloses of estuarine and terrestrial origin in salt marsh estuarine sediments. The lignin moiety of pine lignocellulose was mineralized 10 to 14 times more slowly than that of Spartina lignocellulose, depending on the source of inoculum. Average values for percent mineralization after 835 h of incubation were 1.4 and 13.9%, respectively. For Spartina lignocellulose, mineralization of the cellulose moiety was three times faster than that of the lignin moiety. Average values for percent mineralization after 720 h of incubation were 32.1 and 10.6%, respectively. Lignocellulose and lignin contents of live pine and Spartina plants were analyzed and found to be 60.7 and 20.9%, respectively, for pine and 75.6 and 15.1%, respectively, for Spartina.     

Impacts of an alien species (Spartina alterniflora) on the macrobenthos community of Jiangsu coastal inter-tidal ecosystem

Spartina alterniflora, a species vegetating on inter-tidal flats that was introduced from the eastern coast of United States, has become a hot topic, focusing on its invasion within local species in the coastal zone of China. Impacts of S. alterniflora on the inter-tidal macrobenthos community in the Jiangsu coastland are addressed by comparing the macrobenthos characteristics in a mudflat and in a four-year-old Spartina salt marsh that had earlier been a mudflat. During the period October 2002–July 2003, we studied the distribution pattern and diversity of macrobenthos, and discussed their correlation with environmental factors caused by Spartina vegetation. The results showed that a total of 43 macrobenthos species were found, mainly consisting of Mollusca, Crustacea, and Annelida. Ten macrobenthos species were found in the Spartina salt marsh, and 36 species were found in the mudflat. Life forms and functional groups of macrobenthos in the Spartina salt marsh were obviously distrinct from that of the mudflat. The study showed that macrobenthos diversity in the Spartina salt marsh decreased, and the community structure altered obviously, whereas the biomass showed no differences in different seasons. Statistical analysis demonstrated that seasonal change of macrobenthos diversity in the Spartina salt marsh negatively related to content of sediment organic matter, total N, bulk density, height and biomass of Spartina vegetation, and positively related to the density of Spartina. All these differences suggested the obvious effects of the Spartina vegetation on the Jiangsu inter-tidal benthic macroinvertebrate ecology. Furthermore, the investigation also showed that the niche of the native macrobenthos living in the mudflat has been transferred down, seaward, due to the invasion of Spartina in our study site.     

EFFECT OF AN AMMONIUM NITRATE PULSE ON THE GROWTH AND ELEMENTAL COMPOSITION OF NATURAL STANDS OF SPARTINA ALTERNIFLORA AND JUNCUS ROEMERIANUS

A nitrogen (ammonium nitrate) pulse of 200 kg ha“¹ was added to stands of tall (1.0–1.5 m) Spartina alterniflora, short (< 0.5 m) Spartina alterniflora, and Juncus roemerianus in a Georgia salt marsh in July. The major response ten weeks later was an increase in the aerial biomass and a sharp reduction in the C/N ratio in short Spartina alterniflora. One year after the treatment the difference between the biomass in enriched and control plots was greater than ten weeks after treatment, but the C/N ratio in the plants in the treated plots had risen to that of the controls. The availability of nitrogen appears to limit growth in the middle elevation Georgia salt marsh (short S. alterniflora), but not in the lower (tall S. alterniflora) or higher (J. roemerianus) portions.     

Physiological Diversity of the Rhizosphere Diazotroph Assemblages of Selected Salt Marsh Grasses

Rhizosphere diazotroph assemblages of salt marsh grasses are thought to be influenced by host plant species and by a number of porewater geochemical parameters. Several geochemical variables can adversely affect plant productivity and spatial distributions, resulting in strong zonation of plant species and growth forms. This geochemically induced stress may also influence the species compositions and distributions of rhizosphere diazotroph assemblages, but little is currently known about these organisms. The diversity and key physiological features of culturable, O₂-tolerant rhizosphere diazotrophs associated with the tall and short growth forms of Spartina alterniflora and with Juncus roemerianus were examined. A total of 339 gram-negative strains were isolated by a root stab culture approach and morphologically and physiologically characterized by using API and BIOLOG tests. Eighty-six distinct groups composed of physiologically similar strains were identified. Of these groups, 72% were shown to be capable of N₂ fixation through molecular analyses, and a representative strain was chosen from each diazotroph group for further characterization. Cluster and principal-components analysis of BIOLOG data allowed the designation of physiologically distinct strain groupings. Most of these groups were dominated by strains that were not identifiable to species on the basis of API or BIOLOG testing. Representatives of several families including the Enterobacteriaceae, Vibrionaceae, Azotobacteraceae, Spirillaceae, Pseudomonadaceae, and Rhizobiaceae were recovered, as well as strains with no clear taxonomic affiliations. This study identifies numerous potentially important physiological groups of the salt marsh diazotroph assemblage.     

Subunit Composition Determines the Single Channel Kinetics of the Epithelial Sodium Channel

We have further characterized at the single channel level the properties of epithelial sodium channels formed by coexpression of α with either wild-type β or γ subunits and α with carboxy-terminal truncated β (β_T) or γ (γ_T) subunits in Xenopus laevis oocytes. αβ and αβ_T channels (9.6 and 8.7 pS, respectively, with 150 mM Li⁺) were found to be constitutively open. Only upon inclusion of 1 μM amiloride in the pipette solution could channel activity be resolved; both channel types had short open and closed times. Mean channel open probability (P _o) for αβ was 0.54 and for αβ_T was 0.50. In comparison, αγ and αγ_T channels exhibited different kinetics: αγ channels (6.7 pS in Li⁺) had either long open times with short closings, resulting in a high P _o (0.78), or short openings with long closed times, resulting in a low P _o (0.16). The mean P _o for all αγ channels was 0.48. αγ_T (6.6 pS in Li⁺) behaved as a single population of channels with distinct kinetics: mean open time of 1.2 s and closed time of 0.4 s, with a mean P _o of 0.6, similar to that of αγ. Inclusion of 0.1 μM amiloride in the pipette solution reduced the mean open time of αγ_T to 151 ms without significantly altering the closed time. We also examined the kinetics of amiloride block of αβ, αβ_T (1 μM amiloride), and αγ_T (0.1 μM amiloride) channels. αβ and αβ_T had similar blocking and unblocking rate constants, whereas the unblocking rate constant for αγ_T was 10-fold slower than αβ_T. Our results indicate that subunit composition of ENaC is a main determinant of P _o. In addition, channel kinetics and P _o are not altered by carboxy-terminal deletion in the β subunit, whereas a similar deletion in the γ subunit affects channel kinetics but not P _o.