Alder and lupine enhance nitrogen cycling in a degraded forest soil in Northern Sweden

Positive effects of legumes and actinorhizal plants on N-poor soils have been observed in many studies but few have been done at high latitudes, which was the location of our study. We measured N₂ fixation and several indices of soil N at a site near the Arctic Circle in northern Sweden. More than 20 years ago lupine (Lupinus nootkatensis Donn) and gray alder (Alnus incana L. Moench) were planted on this degraded forest site. We measured total soil N, net N mineralization and nitrification with a buried bag technique, and fluxes of NH⁺ ₄ and NO^– ₃ as collected on ion exchange membranes. We also estimated N₂ fixation activity of the N₂-fixing plants by the natural abundance of ¹⁵N of leaves with Betula pendula Roth. as reference species. Foliar nitrogen in the N₂-fixing plants was almost totally derived from N₂ fixation. Plots containing N₂-fixing species generally had significantly higher soil N and N availability than a control plot without N₂-fixing plants. Taken together, all measurements indicated that N₂-fixing plants can be used to effectively improve soil fertility at high latitudes in northern Sweden.     

Effect of nitrogen starvation on ammonium-inhibition of nitrogenase activity in Azotobacter chroococcum

When Azotobacter chroococcum cells grown in batch culture under N₂-fixing conditions were transferred to a medium lacking a nitrogen source, the cellular C/N ratio, the amount of alginic acid released into the external medium and the rate of endogenous respiration increased appreciably after 6 h to the exclusion of dinitrogen, whereas nitrogenase activity did not undergo any significant change. Nitrogen deficiency caused a decrease in the ammonium inhibition of nitrogenase activity from 95% inhibition at zero time to 14% after 6 h incubation under dinitrogen starvation, with no difference in the rate of ammonium utilization by N₂-fixing and N₂-starved cells being observed. This suggests that a balance of nitrogen and carbon assimilation is necessary for the ammonium inhibition of nitrogenase activity in A. chroococcum to take place.     

Facultative nitrogen fixation by canopy legumes in a lowland tropical forest

Symbiotic dinitrogen (N₂) fixation is often invoked to explain the N richness of tropical forests as ostensibly N₂-fixing trees can be a major component of the community. Such arguments assume N₂ fixers are fixing N when present. However, in laboratory experiments, legumes consistently reduce N₂ fixation in response to increased soil N availability. These contrasting views of N₂ fixation as either obligate or facultative have drastically different implications for the N cycle of tropical forests. We tested these models by directly measuring N₂-fixing root nodules and nitrogenase activity of individual canopy-dominant legume trees (Inga sp.) across several lowland forest types. Fixation was substantial in disturbed forests and some gaps but near zero in the high N soils of mature forest. Our findings suggest that canopy legumes closely regulate N₂ fixation, leading to large variations in N inputs across the landscape, and low symbiotic fixation in mature forests despite abundant legumes.     

Sugar beet and barley yields in relation to inoculation with N2-fixing and phosphate solubilizing bacteria

Recently, there has been a resurgence of interest in bioorganic fertilizers as part of sustainable agricultural practices to alleviate drawbacks of intensive farming practices. N₂-fixing and P-solubilizing bacteria are important in plant nutrition increasing N and P uptake by the plants, and playing a significant role as plant growth-promoting rhizobacteria in the biofertilization of crops. A study was conducted in order to investigate the effects of two N₂-fixing (OSU-140 and OSU-142) and a strain of P-solubilizing bacteria (M-13) in single, dual and three strains combinations on sugar beet and barley yields under field conditions in 2001 and 2002. The treatments included: (1) Control (no inoculation and fertilizer), (2) Bacillus OSU-140, (3) Bacillus OSU-142, (4) Bacillus M-13, (5) OSU-140 + OSU-142, (6) OSU-140 + M-13, (7) OSU-142 + M-13, (8) OSU-140 + OSU-142 + M-13, (9) N, (10) NP. N and NP plots were fertilized with 120 kg N ha^–1 and 120 kg N ha^–1 + 90 kg P ha^- for sugar beet and 80 kg N ha^–1 and 80 kg N ha^–1 + 60 kg P ha^–1 for barley. The experiments were conducted in a randomized block design with five replicates. All inoculations and fertilizer applications significantly increased leaf, root and sugar yield of sugar beet and grain and biomass yields of barley over the control. Single inoculations with N₂-fixing bacteria increased sugar beet root and barley yields by 5.6–11.0% depending on the species while P-solubilizing bacteria alone gave yield increases by 5.5–7.5% compared to control. Dual inoculation and mixture of three bacteria gave increases by 7.7–12.7% over control as compared with 20.7–25.9% yield increases by NP application. Mixture of all three strains, dual inoculation of N₂-fixing OSU-142 and P-solubilizing M-13, and/or dual inoculation N₂-fixing bacteria significantly increased root and sugar yields of sugar beet, compared with single inoculations with OSU-140 or M-13. Dual inoculation of N₂-fixing Bacillus OSU-140 and OSU-142, and/or mixed inoculations with three bacteria significantly increased grain yield of barley compared with single inoculations of OSU-142 and M-13. In contrast with other combinations, dual inoculation of N₂-fixing OSU-140 and P-solubilizing M-13 did not always significantly increase leaf, root and sugar yield of sugar beet, grain and biomass yield of barley compared to single applications both with N₂-fixing bacteria. The beneficial effects of the bacteria on plant growth varied significantly depending on environmental conditions, bacterial strains, and plant and soil conditions.     

Inoculation of forage grasses with N2-fixing Enterobacteriaceae

Summary Previous investigations indicated some forage grass roots in Texas are heavily colonized with N₂-fixing bacteria. The most numerous N₂-fixing bacteria were in the genera Klebsiella and Enterobacter. In the present investigation inoculation experiments were conducted using 18 isolates of these bacteria to determine if a N₂-fixing association could be established between the bacteria and the grassesCynodon dactylon andPanicum coloratum. Plants were grown in soil for approximately 5 months in a greenhouse and were measured periodically for dry matter, nitrogen accumulation, and acetylene reduction activity. Results of the investigation indicated that 25% of the plant-soil systems were active in acetylene reduction and the activity was high enough to indicate agronomically significant quantities of N₂ were being fixed (>8kg N ha⁻¹). However, plant systems extrapolated to fix>8 kg N ha⁻¹ contained less nitrogen and accumulated less dry matter than plants less active in acetylene reduction. Inocula could not be re-isolated from healthy grass roots indicating that the N₂-fixing activity may have not have been closely assiciated with plant roots. Future research is needed to determine factors limiting colonization of grass roots.     

Effect of Inoculation with N2-Fixing Spirilla and Azotobacter on Nitrogenase Activity on Roots of Maize Grown Under Subtropical Conditions

Inoculated and non-inoculated seedlings of maize were grown in fertile clayloam soils of Egypt and Belgium under subtropical conditions provided in a greenhouse. Acetylene-reducing activity and microbial counts were determined during a period ranging from 6 to 12 weeks after sowing. Irrespective of soil origin, N₂-fixing spirilla and Azotobacter were common under maize cultivation. Inoculation resulted in a transitional increase in their numbers at early stages of growth. Nitrogenase activity was not detected in the rhizosphere of young plants. The maximum activities measured (81 to 1,436 nmol of C₂H₄ g⁻¹ h⁻¹) occurred close to the 50 to 70% silking stage. Inoculation with N₂-fixing spirilla, particularly in Nile Delta soil, doubled the amount of N₂ fixed in a late period of growth (12 weeks), whereas inoculation with Azotobacter had no noticeable effect.     

Survival and colonization of inoculated bacteria in kallar grass rhizosphere and quantification of N2-fixation

Two experiments have been conducted, one in semi-solid Hoagland nutrient medium and the other in shallow pots containing saline soil. N₂-fixing bacteria belonging toAzospirillum, Azotobacter, Klebsiella andEnterobacter were inoculated separately on kallar grass grown in semi-solid nutrient medium. It was shown that inoculation affects root proliferation and also results in¹⁵N isotopic dilution. The % Ndfa ranged from 47–70 whereas no significant effect on the total nitrogen uptake was observed. The bacterial colonization of the root surface and the presence of enteric bacteria inside the root hair cells is reported. In a soil pot experiment, non-N₂-fixingPolypogon monspeliensis was used as a reference plant (control). A treatment receiving a high rate of nitrogen was also used as a non-N₂-fixing control.¹⁵N-labelled ammonium sulphate at 20 kg N ha^–1 and 90 kg N ha^–1 was used. The % Ndfa in the aerial parts of kallar grass was 12–15 whenP. monspeliensis was used as reference plant whereas 37–39% Ndfa was estimated when the treatment receiving high nitrogen fertilizer was used as a non-N₂-fixing control. These investigations revealed some problems of methodology which are discussed.     

Utilization of amino acids by Frankia sp. strain CpI1

The utilization of some amino acids, added at 1 mM and 10 mM concentrations, as the sole combined nitrogen sources by Frankia sp. strain CpI1, has been investigated. Glutamine, like NH ₄ ⁺ , provided rapid growth without N₂ fixation. Histidine at 1 mM yielded poor N₂-fixing activity but better cell growth than N₂. Aspartate, glutamate, alanine, proline, each at 1 mM concentration, supported similar levels of N₂ fixation and growth. Growth on 10 mM glutamate, proline, or histidine resulted in poor N₂-fixing activity and poor cell growth. Cells grown on 10 mM alanine had about half the N₂-fixing activity of cells grown on N₂ but growth was good. Aspartate at 10 mM concentration, however, stimulated N₂-fixing activity dramatically and promoted faster growth. Enzyme analysis suggested that asparate is catabolized by glutamate-oxaloacetate transaminase (GOT), since GOT specific activity was induced, and aspartase activity was not detected, in cells grown on aspartate as the sole combined nitrogen source. Thinlayer chromatography (TLC) of metabolites extracted from N₂-grown cells fed with [¹⁴C]-aspartate showed that label was rapidly accumulated mainly on aspartate and/or glutamate, depending on the cells' physiological state, without detectable labeling on fumarate or oxaloacetate (OAA). These findings provide evidence that aspartate is catabolized by GOT to OAA which, in turn, is rapidly converted to -ketoglutarate through the TCA cycle and then to glutamate by GOT or by glutamate synthase (GOGAT). The stimulation of N₂ fixation and growth by aspartate is probably caused by an increased intracellular glutamate pool.     

Seasonal accumulation and partitioning of nitrogen by lentil

Although wheat (Triticum aestivum L.) is the dominant crop of the semi-arid plains of Canada and the western United States, lentil (Lens culinaris Medik.) has become an important alternative crop. Sources and seasonal accumulation of N must be understood in order to identify parameters that can lead to increased N₂-fixing activity and yield. Inoculated lentil was grown in a sandy-loam soil at an irrigated site in Saskatchewan, Canada. Wheat was used as the reference crop to estimate N₂ fixation by the A-value approach. Lentil and wheat received 10 and 100 kg N ha⁻¹ of ammonium nitrate, respectively. Crops were harvested six times during the growing season and plant components analyzed. During the first 71 days after planting the wheat had a higher daily dry matter and N accumulation compared to lentil. However, during the latter part of the growing season, daily dry matter and N accumulation were greater for lentil. The maximum total N accumulation for lentil at maturity was 149 kg ha⁻¹. In contrast, wheat had a maximum N accumulation of 98 kg ha⁻¹ in the Feekes 11.1 stage, or 86 days after planting. The maximum daily rates of N accumulation were 3.82 kg N ha⁻¹ day⁻¹ for lentil and 2.21 kg N ha⁻¹ day⁻¹ for wheat. The percentage of N derived from N₂ fixation (% Ndfa) ranged from 0 at the first harvest to 92 % at final harvest. Generative plant components had higher values for % Ndfa than the vegetative components which indicates that N in the reproductive plant parts was derived largely from current N₂ fixation and lentil continued to fix N until the end of the pod fill stage. At final harvest, lentil had derived 129 kg N ha⁻¹ from N₂ fixation with maximum N₂-fixing activity (4.4 kg N ha⁻¹ day⁻¹) occurring during the early stages of pod fill. Higher maximum rates of N₂-fixing activity than net N accumulation (3.82 kg N ha⁻¹ day⁻¹) may have been caused by N losses like volatilization. In addition, lentil provided a net N contribution to the soil of 59 kg ha⁻¹ following the removal of the grain.     

Natural 15N abundance of presumed N2-fixing and non-N2-fixing plants from selected ecosystems

Summary The ¹⁵N/¹⁴N ratios of plant and soil samples from Northern California ecosystems were determined by mass spectrometry. The ¹⁵N abundance of 176 plant foliar samples averaged 0.0008 atom % ¹⁵N excess relative to atmospheric N₂ and ranged from-0.0028 to 0.0064 atom % ¹⁵N excess relative to atmospheric N₂. Foliage from reported N₂-fixing species had significantly lower mean ¹⁵N abundance (relative to atmospheric N₂ and total soil N) and significantly higher N concentration (% N dry wt.) than did presumed non-N₂-fixing plants growing on the same sites. The mean difference between N₂-fixing species and other plants was 0.0007 atom % ¹⁵N. N₂-fixing species had lower ¹⁵N abundance than the other plants on most sites examined despite large differences between sites in vegetation, soil, and climate. The mean ¹⁵N abundance of N₂-fixing plants varied little between sites and was close to that of atmospheric N₂. The ¹⁵N abundance of presumed non-N₂-fixing species was highest at coastal sites and may reflect an input of marine spray N having relatively high ¹⁵N abundance. The ¹⁵N abundance of N₂-fixing species was not related to growth form but was for other plants. Annual herbaceous plants had highest ¹⁵N abundance followed in decreasing order by perennial herbs, shrubs, and trees. Several terrestrial ferns (Pteridaceae) had ¹⁵N abundances comparable to N₂-fixing legumes suggesting N₂-fixation by these ferns. On sites where the ¹⁵N abundance of soil N differs from that of the atmosphere, N₂-fixing plants can be identified by the natural ¹⁵N abundance of their foliage. This approach can be useful in detecting and perhaps measuring N₂-fixation on sites where direct recovery of nodules is not possible.     

Nitrogen fixation associated with roots of Kallar grass (Leptochloa fusca L. Kunth)

Summary An ecological survey was made to measure the N₂-fixing activity in the rhizosphere of a salt-tolerant grass,Leptochloa fusca (L.) Kunth. Samples were obtained every month at two sites over a period of one year. Soil cores, unwashed, washed and surface-sterilized roots were subjected to acetylene reduction assay (ARA). ARA values up to 50 nmoles h^–1 for soil cores, 1095 nmoles g dry root^–1 h^–1 for unwashed roots, 4929 nmoles g dry root^–1 h^–1 for washed roots and 2494 nmoles g dry root^–1 h^–1 for surface-sterilized roots were observed but for most samples the range was 1–200 nmoles g dry root^–1 h^–1. A lag period of 5–7 h was observed before the onset of N₂-fixing activity by excised roots and O₂ levels had no effect on this lag. Values for roots incubated without preincubation were similar to those for unwashed preincubated roots. Activity was highest in September, October and November when the temperature is not very high and photosynthetic activity is reasonably good. N₂-fixing-bacteria were counted on the same samples by plate count and MPN methods, the latter being estimated on the basis of ARA and pellicle formation. Fairly high numbers of bacteria (10⁴–10⁷) were recorded in the histoplane fraction which indicates the presence of diazotrophs in the inner cells of grass roots.     

An assessment of soil enrichment by actinorhizal N2 fixation using δ15N values in a chronosequence of deglaciation at Glacier Bay,Alaska

The extent of transfer of fixed N between N₂-fixing and non-N₂-fixing plant species is largely unknown in successional studies. In order to redress this deficiency at a locale intensively studied ecologically, leaf tissue samples were collected from actinorhizal N₂-fixing (Alnus, Shepherdia, and Dryas) and two non-N₂-fixing (Salix) woody species within research plots located along a chronosequence of deglaciated fjord in Glacier Bay National Park, Alaska. The tissue samples were analyzed for ¹⁵N content, and the resulting data analyzed for trends in plant tissue N. Among the non-N₂-fixing Salix species, ¹⁵N values increased from the most recently deglaciated sites to converge with the temporally more-stable values for the symbiotic N₂-fixing species on sites at about 40 years after deglaciation. The lower ¹⁵N values of sequestered N in plant tissues suggested that N derived from N₂-fixing plants accounts for the major portion of N in associated plants up to 40 years after deglaciation. The ¹⁵N isotopic data also suggested that Shepherdia canadensis depends least on soil N, D. drummondii the most, and A. viridis ssp. sinuata somewhere between those two species. The presence of a sere dominated by dense thickets of A. viridis ssp. sinuata at the convergence of ¹⁵N values for the N₂-fixing and non-N₂-fixing species indicated that this species is most responsible for accumulation of fixed N in soil at Glacier Bay. This paper is dedicated to the memory of Steven J. Kohls who died prior to publication of this research.     

Seasonal fluctuations in the population of denitrifying and N2-fixing bacteria in an acid soil of a Norway spruce forest

The seasonal fluctuations in the concentration of cultured denitrifying and N₂-fixing bacteria were followed in an ammonium fertilised and a control soil of a Norway spruce forest near Villingen/Black Forest from December 1994 to August 1998. The horizontal distribution of bacteria in three layers was determined by the MPN-method and by molecular probing (colony hybridisation) using specific 0.4–0.7 kb DNA probes for denitrification steps (narG, nirS, nirK and nosZ) and for N₂-fixation (nifH). The data showed that highest bacterial counts and higher numbers of denitrifying and N₂-fixing bacteria were generally detectable in the upper (= 5 cm) soil layer and that their amount decreased with soil depth. The concentration of these cultured bacteria showed seasonal fluctuations with highest numbers in autumn/winter/early spring and with low counts in summer. Denitrifying and N₂-fixing bacteria amounted to less than 10% of the total number of cultured bacteria determined by the MPN-method. Fertilisation with ammonium did not cause a shift in the population of these bacteria. These findings were corroborated by hybridisation experiments with genomic DNA isolated from the different layers. Strongest DNA–DNA hybridisation band intensities were obtained in the upper soil layer and their intensities decreased with soil depth. Soil samples from Villingen assayed in the laboratory produced N₂O (in dependence of nitrate and C₂H₂ added to the vessels) and utilised this gas with higher activities in the assays with the fertilised soil. It is concluded that molecular techniques can successfully be applied for assessing seasonal fluctuations of bacterial populations in soil. Relative abundance of denitrifying and N₂-fixing bacteria can be determined from experiments with DNA isolated from soils. Attempts to transform these results to the total population of soil bacteria on a single cell basis are faced with many uncertainties.     

PHOTOAUTOTROPHIC GROWTH OF A RECENTLY ISOLATED N2-FIXING MARINE NON-HETEROCYSTOUS FILAMENTOUS CYANOBACTERIUM, SYMPLOCA SP. (CYANOBACTERIA)

Photoautotrophic growth of a marine non-heterocystous filamentous cyanobacterium, Symploca sp. strain S84, was examined under nitrate-assimilating and N₂-fixing conditions. Under continuous light, photon flux density of 55 μmol photons·m⁻² ·s⁻¹ was at a saturating level for growth, and light did not inhibit the growth rate under N₂-fixing conditions even when the photon flux density was doubled (110 μmol photons·m⁻² ·s⁻¹). Doubling times of the N₂-fixing cultures under 55 and 110 μmol photons·m⁻² ·s⁻¹ were about 30 and 31 h, respectively. Under 110 μmol photons·m⁻² ·s⁻¹ during the light phase of an alternating 12:12-h light:dark (L:D) cycle, the doubling time of the N₂-fixing culture was also about 30 h. When grown diazotrophically under a 12:12-h L:D regime, C₂H₂ reduction activity was observed mainly during darkness. In continuous light, relatively large cyclic fluctuations in C₂H₂ reduction were observed during growth. The short-term (<4 h) effect of 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU; 5 μM) indicated that C₂H₂ reduction activity was not influenced by photosynthetic O₂ evolution. Long-term (24 h) effects of DCMU indicated that photosynthesis and C₂H₂ reduction activity occur simultaneously. These results indicate that strain S84 grows well under diazotrophic conditions when saturating light is supplied either continuously or under a 12:12-h L:D diel light regime.     

Neotropical Legume Tree Inga edulis Forms N2-fixing Symbiosis with Fast-growing Bradyrhizobium Strains

Inga edulis Mart. is a tropical legume tree used for shade in coffee and cacao plantations and as a hedgerow in alley-cropping practices. Little information can be found concerning N₂ fixation in this species. This study was conducted to characterize the rhizobia of I. edulis and determine if it is capable of fixing substantial amounts of N₂. Four strains of fast-growing, Gram-negative rhizobia-type bacteria were isolated from I. edulis nodules. The strains were identified by sequencing of partial 16S–23S rDNA internal spacer region. Nitrogenase activity was determined using acetylene reduction assay (ARA). Dinitrogen fixation was measured under controlled conditions by the ¹⁵N isotope dilution technique using two non-N₂-fixing reference species, Vochysia guatemalensis Donn. Sm, and Gmelina arborea Roxb. ex. Sm. Seedlings were grown in three growth media: native soil and naturally N-depleted sand amended to a low and high N level. The four strains of symbiotic bacteria were closely related to Bradyrhizobium japonicum and to Bradyrhizobium liaoningense. Nodules demonstrated nitrogenase activity as measured by ARA. Vochysia guatemalensis was a better non-N₂-fixing reference than G. arborea. When V. guatemalensis was used as the non-N₂-fixing reference, the estimate of the percentage of N fixed from atmosphere out of total N in I. edulis seedlings was ca. 40 in the two sand media treatments and 10 in the native soil.     

Nitrogen fixation associated with non-legumes in agriculture

Summary This review examines the nitrogen cycle in upland agricultural situations where nonlegume N₂-fixation is likely to be important for crop growth. Evidence for associative fixation is adduced from accumulation of N in the top 15 cm soil under grasses, from N balances for crop production obtained from both pot and field experiments, in tropical and temperate environments, measurements of nitrogen (C₂H₂ reduction) activity, uptake of¹⁵N₂ by plants and¹⁵N isotope dilution. Factors influencing the activity such as the provision of carbon substrate by the plant and the efficiency of its utilisation by the bacteria, plant cultivar, soil moisture and N levels, and inoculation with N₂-fixing bacteria are discussed. Crop responses to inoculation withAzospirillum are detailed. The breakdown of crop residues, particularly straw, can support large levels of N₂-fixation. Cyanobacteria as crusts on the soil surface also fix nitrogen actively in many environments. Fixation by the nodulated, non-legume treesCasuarina andParasponia has beneficial effects in some cropping systems in Asia. I conclude that nonlegume N₂-fixation makes a significant contribution to the production of some major cereal crops in both temperate and tropical environments.     

Natural15N abundance as a method of estimating the contribution of biologically fixed nitrogen to N2-fixing systems: Potential for non-legumes

The¹⁵N abundance of plants usually closely reflects the¹⁵N abundance of their major immediate N source(s); plant-available soil N in the case of non-N₂-fixing plants and atmospheric N₂ in the case of N₂ fixing plants. The¹⁵N abundance values of these sources are usually sufficiently different from each other that a significant and systematic difference in the¹⁵N abundance between the two kinds of plants can be detected. This difference provides the basis for the natural¹⁵N abundance method of estimating the relative contribution of atmospheric N₂ to N₂-fixing plants growing in natural and agricultural settings. The natural¹⁵N abundance method has certain advantages over more conventional methods, particularly in natural ecosystems, since disturbance of the system is not required and the measurements may be made on samples dried in the field. This method has been tested mainly with legumes in agricultural settings. The tests have demonstrated the validity of this method of arriving at semi-quantitative estimates of biological N₂-fixation in these settings. More limited tests and applications have been made for legumes in natural ecosystems. An understanding of the limits and utility of this method in these systems is beginning to emerge. Examples of systematic measurements of differences in¹⁵N abundance between non-legume N₂-fixing systems and neighbouring non-fixing systems are more unusual. In principle, application of the method to estimate N₂-fixation by nodulated non-legumes, using the natural¹⁵N abundance method, is as feasible as estimating N₂-fixation by legumes. Most of the studies involving N₂-fixing non-legumes are with this type of system (e.g., Ceanothus, Chamabatia, Eleagnus, Alnus, Myrica, and so forth). Resuls of these studies are described. Applicability for associative N₂-fixation is an empirical question, the answer to which probably depends upon the degree to which fixed N goes predominantly to the plant rather than to the soil N pool. The natural¹⁵N abundance method is probably not well suited to assessing the contribution of N₂-fixation by free-living microorganisms in their natural habitat, particularly soil microorganisms.This work was supported in part by subcontracts under grants from the US National Science Foundation (DEB79-21971 and BSR821618)     

Influence of pH,exchangeable aluminium and 0.02M CaCl2-extractable aluminium on the growth and nitrogen-fixing activity of white clover (Trifolium repens) in some New Zealand soils

The effects of soil acidity on the growth and N₂-fixing activity of white clover in seven acid topsoils and subsoils of New Zealand were investigated using a glasshouse experiment.The application of phosphate (Ca(H₂PO₄)₂) to the soils resulted in very large increases in white clover growth on all soils. The application of phosphate, as well as increasing P supply, also decreased 0.02M CaCl₂-extractable Al levels, but had little effect on exchangeable Al levels.Where adequate phosphate was applied, increasing rates of lime (CaCO₃) resulted in increased plant growth on most soils. N₂[C₂H₂]-fixing activity was increased by the first level of lime for one soil, but generally remained approximately constant or declined slightly at higher rates of lime. Up to the point of maximum yield, white clover top weight was more highly correlated with 0.02M CaCl₂-extractable soil Al than with exchangeable Al or pH. At pH values greater than 5.5, plant yield declined on some soils, apparently because of Zn deficiency. The data suggest that white clover is unlikely to be affected by Al toxicity at 0.02M CaCl₂-extractable Al levels of less than about 3.3 g g^–1. However, there were differences between soils in apparent plant tolerance to 0.02M CaCl₂-extractable Al, which appeared to be caused by differing C levels in the 0.02M CaCl₂ extracts.     

Nitrogen fixation in the sub-Antarctic Macquarie Island

Summary The N₂-fixing biota of Macquarie Island are dominated by cyanobacteria growing epiphytically or symbolically with plants or lichens. Highest rates of C₂H₂-reducing activity were found in the leafy lichen Peltigera sp. colonizing herbfields and short grasslands and in the coastal angiosperm Colobanthus muscoides. Significant rates of C₂H₂ reduction were also found to be associated with the liverwort Jamesoniella colorata, commonly occurring in coastal and plateau mires, in a mossbed of Dicranella cardotii colonizing a land-slip face on the grassland slopes at 100 m altitude and within polsters of the mosses Ditrichum strictum and Andreaea sp. found in exposed localities on the plateau at 200–300 m altitude. It was concluded that the common feature of plants supporting active N₂ fixation in dry habitats was the dense packing of stems and leaves, enabling water translocation to the cyanobacterial zone by wick action. Epiphytic cyanobacterial C₂H₂ reduction in wet habitats was widespread and not restricted to any particular plant species. Notable N₂-fixing lichens of the plateau were Pseudocyphellaria delisea and Stereocaulon sp., although both were also occasionally found in coastal herbfields. No significant N₂-fixing activity was associated with any of the dominant grasses tested. Heterotrophic N₂ fixation was also found to be insignificant in the various habitats tested, however N₂-fixing Bacillus (B. macerans or B. polymyxa) were universally present in coastal, grassland slope, or plateau samples, including moss polster samples. A N₂fixing Clostridium sp. was isolated in only one instance, from soil in the vicinity of a seal wallow on the coast.     

Ecogenomic sensor reveals controls on N2-fixing microorganisms in the North Pacific Ocean

Nitrogen-fixing microorganisms (diazotrophs) are keystone species that reduce atmospheric dinitrogen (N₂) gas to fixed nitrogen (N), thereby accounting for much of N-based new production annually in the oligotrophic North Pacific. However, current approaches to study N₂ fixation provide relatively limited spatiotemporal sampling resolution; hence, little is known about the ecological controls on these microorganisms or the scales over which they change. In the present study, we used a drifting robotic gene sensor to obtain high-resolution data on the distributions and abundances of N₂-fixing populations over small spatiotemporal scales. The resulting measurements demonstrate that concentrations of N₂ fixers can be highly variable, changing in abundance by nearly three orders of magnitude in less than 2 days and 30 km. Concurrent shipboard measurements and long-term time-series sampling uncovered a striking and previously unrecognized correlation between phosphate, which is undergoing long-term change in the region, and N₂-fixing cyanobacterial abundances. These results underscore the value of high-resolution sampling and its applications for modeling the effects of global change.