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[Nitrogen fixation productivity in the plant phyllosphere].

The dynamics of nitrogen fixation was studied in the phyllosphere of birch and timothy, and the productivity of the process within the vegetation period was determined on the basis of the study. The activity of nitrogen fixation was measured under natural conditions using the acetylene technique. A proportion is suggested which makes it possible to determine the actual activity of nitrogen fixation in the phyllosphere from the potential one. The productivity of nitrogen fixation was 7 and 10 kg of nitrogen per hectare per season for birch and timothy respectively.

Nitrogen Fixation↗

Reduced nitrogen fixation in the glacial ocean inferred from changes in marine nitrogen and phosphorus inventories.

To explain the lower atmospheric CO2 concentrations during glacial periods, it has been suggested that the productivity of marine phytoplankton was stimulated by an increased flux of iron-bearing dust to the oceans. One component of this theory is that iron-an essential element/nutrient for nitrogen-fixing organisms-will increase the rate of marine nitrogen fixation, fuelling the growth of other marine phytoplankton and increasing CO2 uptake. Here we present data that questions this hypothesis. From a sediment core off the northwestern continental margin of Mexico, we show that denitrification and phosphorite formation-processes that occur in oxygen-deficient upwelling regions, removing respectively nitrogen and phosphorus from the ocean-declined in glacial periods, thus increasing marine inventories of nitrogen and phosphorus. But increases in phosphorus were smaller and less rapid, leading to increased N/P ratios in the oceans. Acknowledging that phytoplankton require nitrogen and phosphorus in constant proportions, the Redfield ratio, and that N/P ratios greater than the Redfield ratio are likely to suppress nitrogen fixation, we suggest therefore that marine productivity did not increase in glacial periods in response to either increased nutrient inventories or greater iron supply.

Atmosphere↗

Traffic lights in trichodesmium. Regulation of photosynthesis for nitrogen fixation studied by chlorophyll fluorescence kinetic microscopy.

We investigated interactions between photosynthesis and nitrogen fixation in the non-heterocystous marine cyanobacterium Trichodesmium IMS101 at the single-cell level by two-dimensional (imaging) microscopic measurements of chlorophyll fluorescence kinetics. Nitrogen fixation was closely associated with the appearance of cells with high basic fluorescence yield (F(0)), termed bright cells. In cultures aerated with normal air, both nitrogen fixation and bright cells appeared in the middle of the light phase. In cultures aerated with 5% oxygen, both processes occurred at a low level throughout most of the day. Under 50% oxygen, nitrogen fixation commenced at the beginning of the light phase but declined soon afterwards. Rapid reversible switches between fluorescence levels were observed, which indicated that the elevated F(0) of the bright cells originates from reversible uncoupling of the photosystem II (PSII) antenna from the PSII reaction center. Two physiologically distinct types of bright cells were observed. Type I had about double F(0) compared to the normal F(0) in the dark phase and a PSII activity, measured as variable fluorescence (F(v) = F(m) - F(0)), similar to normal non-diazotrophic cells. Correlation of type I cells with nitrogen fixation, oxygen concentration, and light suggests that this physiological state is connected to an up-regulation of the Mehler reaction, resulting in oxygen consumption despite functional PSII. Type II cells had more than three times the normal F(0) and hardly any PSII activity measurable by variable fluorescence. They did not occur under low-oxygen concentrations, but appeared under high-oxygen levels outside the diazotrophic period, suggesting that this state represents a reaction to oxidative stress not necessarily connected to nitrogen fixation. In addition to the two high-fluorescence states, cells were observed to reversibly enter a low-fluorescence state. This occurred mainly after a cell went through its bright phase and may represent a fluorescence-quenching recovery phase.

Chlorophyll↗

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 N(2) gas species ((28)N(2), (29)N(2), and (30)N(2)) were monitored during incubation experiments after the addition of (15)NO(3)(-). Formulas were developed to estimate the production (denitrification) and consumption (N(2) fixation) of N(2) gas from the fluxes of the different isotopic forms of N(2). Proportions of the three isotopic forms produced from (15)NO(3)(-) and (14)NO(3)(-) 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 microg-atoms of N m(-2) h(-1). They were enhanced by light and organic matter enrichment. In this environment of high nitrogen fixation, low N(2) production rates due to denitrification could be separated from high N(2) 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 microg-atoms of N m(-2) h(-1)) were lower than nitrogen fixation rates (average, 60 microg-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 N(2) isotope capability, it was possible to do isotope-pairing experiments with the MIMS system.

Geologic Sediments↗

Regulation of nitrogen fixation in Rhizobium sp.

Regulation of nitrogen fixation by ammonium and glutamate was examined in Rhizobium sp. 32H1 growing in defined liquid media. Whereas nitrogenase synthesis in Klebsiella pneunoniae is normally completely repressed during growth on NH4+, nitrogenase activity was detected in cultures of Rhizobium sp. grown with excess NH4+. However, an "ammonium effect" on activity was invariably observed in cultures grown on NH4+ as sole nitrogen source; the nitrogenase activity was, depending on conditions, 14 to 36% of that of comparable glutamate-grown cultures. Glutamate inhibited utilization of exogenous NH4+ and, in one of two procedures described, glutamate partially alleviated the ammonium effect on nitrogenase activity. NH4+, apparently produced from N2, was excreted into the culture medium when growth was initiated on glutamate, but not when NH4+ was thesole source of fixed nitrogen for growth. These findings are discussed in relation to nitrogen fixation by Rhizobium bacteroids.

Ammonium Sulfate↗

The natural history of nitrogen fixation.

In recent years, our understanding of biological nitrogen fixation has been bolstered by a diverse array of scientific techniques. Still, the origin and extant distribution of nitrogen fixation has been perplexing from a phylogenetic perspective, largely because of factors that confound molecular phylogeny such as sequence divergence, paralogy, and horizontal gene transfer. Here, we make use of 110 publicly available complete genome sequences to understand how the core components of nitrogenase, including NifH, NifD, NifK, NifE, and NifN proteins, have evolved. These genes are universal in nitrogen fixing organisms-typically found within highly conserved operons-and, overall, have remarkably congruent phylogenetic histories. Additional clues to the early origins of this system are available from two distinct clades of nitrogenase paralogs: a group composed of genes essential to photosynthetic pigment biosynthesis and a group of uncharacterized genes present in methanogens and in some photosynthetic bacteria. We explore the complex genetic history of the nitrogenase family, which is replete with gene duplication, recruitment, fusion, and horizontal gene transfer and discuss these events in light of the hypothesized presence of nitrogenase in the last common ancestor of modern organisms, as well as the additional possibility that nitrogen fixation might have evolved later, perhaps in methanogenic archaea, and was subsequently transferred into the bacterial domain.

Amino Acid Motifs↗

Nitrogen fixation. Endocrine disrupters and flavonoid signalling.

Nitrogen fixation is a symbiotic process initiated by chemical signals from legumes that are recognized by soil bacteria. Here we show that some endocrine-disrupting chemicals (EDCs), so called because of their effect on hormone-signalling pathways in animal cells, also interfere with the symbiotic signalling that leads to nitrogen fixation. Our results raise the possibility that these phytochemically activated pathways may have features in common with hormonal signalling in vertebrates, thereby extending the biological and ecological impact of EDCs.

Hormones↗

How many metals does it take to fix N2? A mechanistic overview of biological nitrogen fixation.

During the process of biological nitrogen fixation, the enzyme nitrogenase catalyzes the ATP-dependent reduction of dinitrogen to ammonia. Nitrogenase consists of two component metalloproteins, the iron (Fe) protein and the molybdenum-iron (MoFe) protein; the Fe protein mediates the coupling of ATP hydrolysis to interprotein electron transfer, whereas the active site of the MoFe protein contains the polynuclear FeMo cofactor, a species composed of seven iron atoms, one molybdenum atom, nine sulfur atoms, an interstitial light atom, and one homocitrate molecule. This Perspective provides an overview of biological nitrogen fixation and introduces three contributions to this special feature that address central aspects of the mechanism and assembly of nitrogenase.

Adenosine Triphosphate↗

Boron requirement in the Discaria trinervis (Rhamnaceae) and Frankia symbiotic relationship. Its essentiality for Frankia BCU110501 growth and nitrogen fixation.

The essentiality of boron (B) for nitrogen fixation in heterocystous cyanobacteria and rhizobial symbioses has been widely established. However, nothing is known about the possible involvement of the micronutrient in actinorhizal symbioses. Therefore, the effect of boron (B) deficiency on the establishment of the Discaria trinervis-Frankia BCU110501 symbiosis was investigated. Nodulation was diminished in B-deficient D. trinervis or in plants inoculated with Frankia grown in the absence of B. These poorly nodulated plants showed a reduction of shoot and root weight and small size. Because depletion of the micronutrient during growth of the actinomycete altered the infection capacity of Frankia, we also studied growth, structure and nitrogen fixation of free-living Frankia BCU110501. Growth was delayed in B-deficient BAP media (+N cultures), and completely inhibited in B-deprived N-free BAP media (-N cultures), suggesting that B is required to enhance growth of Frankia and essential for the development of nitrogen fixing activity. Ultrastructural study of B-deficient cells showed an alteration of filament walls both in +N and especially in -N cultures, indicating a possible role of the microelement in the maintenance of these structures. Moreover, the stability of vesicle envelopes was impaired in the absence of B and, hence, nitrogenase occurrence and nitrogen fixation were totally absent. The results show that B is required for both partners to establish an effective symbiosis.

Journal Article↗

Effect of certain herbicides on survival, growth, and nitrogen fixation of blue-green alga Anabaena doliolum Bharadwaja.

Growth and fixation of nitrogen were retarded in Anabaena doliolum when grown on elemental nitrogen in presence of four different herbicides. The alga was found to be intolerant to these chemicals under nitrogen fixing conditions even in low concentrations. An inhibition of photosynthesis has been regarded as the main basis of herbicidal activity besides other interactions.

Cyanobacteria↗

The evolutionary history of nitrogen fixation, as assessed by NifD.

The evolutionary history of nitrogen fixation has been vigorously debated for almost two decades. Previous phylogenetic analyses of nitrogen fixation genes (nif) have shown support for either evolution by vertical descent or lateral transfer, depending on the specific nif gene examined and the method of analyses used. The debate centers on the placement and monophyly of the cyanobacteria, proteobacteria, and Gram-positive bacteria (actinobacteria and firmicutes). Some analyses place the cyanobacteria and actinobacteria within the proteobacteria, which suggests that the nif genes have been laterally transferred since this topology is incongruent with ribosomal phylogenies, the standard marker for comparison. Other nif analyses resolve and support the monophyly of the cyanobacteria, proteobacteria, and actinobacteria, supporting vertical descent. We have revisited these conflicting scenarios by analyzing nifD from an increased number of cyanobacteria, proteobacteria, and Gram-positive bacteria. Parsimony analyses of amino acid sequences and maximum likelihood analysis of nucleic acid sequences support the monophyly of the cyanobacteria and actinobacteria but not the proteobacteria, lending support for vertical descent. However, distance analysis of nucleic acid sequences placed the actinobacteria within the proteobacteria, supporting lateral transfer. We discuss evidence for both vertical descent and lateral transfer of nitrogen fixation.

Bacteria↗

Nitrogen fixation in the Rhode River estuary of Chesapeake Bay.

The distribution, seasonal variation, origin, and significance of biological nitrogen fixation has been determined for a Chesapeake Bay estuary using the acetylene reduction technique. Studies over a 15-month period have shown that nitrogen fixation occurs predominantly in the surface intertidal (marsh) and subtidal sediments. Negligible activity was found in surface waters. A marked seasonal variation in nitrogen fixation was observed for intertidal sediments incubated at a standard 20 degrees C. Average rates of about 37 and 12 ng N/g dry sediment per hour were observed in the late fall months of 1972 and 1973, respectively, and less than or equal to 5 ng N/g dry sediment per hour during other seaons. Peaks of activity were lowered considerably when samples were incubated at ambient temperatures (in situ). Activity in the subtidal sediments was low (less than or equal to 6.8 ng N/g dry sediment per hour but showed a similar (approximately twofold) seasonal variation in nitrogen fixation potential. Light-dark and substrate addition experiments suggest that heterotrophic bacteria are the principal agents for nitrogen fixation in sediments. Integrated estimates of nitrogen fixation in the estuary indicate that biological fixation probably accounts for less than 5% of the total influx of nitrogen into the system. Rates of activity in the intertidal sediments are insufficient to account for the high productivity of marine angiosperms found in the marsh.

Acetylene↗

Biological nitrogen fixation: recent advances and future prospects.

Current research on nitrogen fixation is basic to finding the knowledge needed for agriculture research in the future. Genetic engineering is the best approach to increase biological nitrogen fixation and recent developments hold promise for this technology. This concept employing atmospheric nitrogen fixation instead of fertilizer to grow food and feed crops, while a complex engineering task, is possible. The opportunities and difficulties are discussed.

Agriculture↗

Nitrogen fixation in methanogens: the archaeal perspective.

The methanogenic Archaea bring a broadened perspective to the field of nitrogen fixation. Biochemical and genetic studies show that nitrogen fixation in Archaea is evolutionarily related to nitrogen fixation in Bacteria and operates by the same fundamental mechanism. At least six nif genes present in Bacteria (nif H, D, K, E, N and X) are also found in the diazotrophic methanogens. Most nitrogenases in methanogens are probably of the molybdenum type. However, differences exist in gene organization and regulation. All six known nif genes of methanogens, plus two homologues of the bacterial nitrogen sensor-regulator glnB, occur in a single operon in Methanococcus maripaludis. nif gene transcription in methanogens is regulated by what appears to be a classical prokaryotic repression mechanism. At least one aspect of regulation, post-transcriptional ammonia switch-off, involves novel members of the glnB family. Phylogenetic analysis suggests that nitrogen fixation may have originated in a common ancestor of the Bacteria and the Archaea.

Amino Acid Sequence↗

Diel nitrogen fixation by cyanobacterial surface blooms in sanctuary lake, pennsylvania.

Diel nitrogen fixation studies were conducted with assemblages of cyanobacteria sampled from surface blooms on Sanctuary Lake, Pa. The studies were conducted between July and September of 1982 to 1985 by using the acetylene reduction technique. Assemblages with the lowest cell concentrations (0.9 x 10 to 1.0 x 10 cells per liter) exhibited nitrogen fixation activity throughout the day, with maximum fixation rates occurring in mid to late afternoon; fixation proceeded throughout the night at rates equivalent to 23 to 28% of the afternoon maximum. In studies conducted with the highest cell concentrations (3.7 x 10 to 6.7 x 10 cells per liter), fixation rates reached maximum values in mid to late morning. The rates declined rapidly throughout the midday period and subsequently ceased from late afternoon until sunrise on the following day. The afternoon decline and cessation of fixation exhibited by high cell concentrations correlated with photosynthetically induced low total CO(2) and supersaturating O(2) concentrations. The midday decline could be prevented and partially reversed by experimentally lowering O(2) and increasing total CO(2) concentrations. Under experimental conditions which simultaneously prevented supersaturating O(2) concentrations and maintained high total CO(2) availability, nitrogen fixation continued throughout the solar day, with maximum rates occurring at midday. These observations indicate that temporal changes in photosynthetic activity may affect diel fluctuations in nitrogen fixation.

Journal Article↗

Transcriptional regulatory cascade of nitrogen-fixation genes in anoxygenic photosynthetic bacteria: oxygen- and nitrogen-responsive factors.

Many photosynthetic bacteria from aquatic and terrestrial habitats reduce atmospheric dinitrogen to ammonia. The synthesis of proteins required for nitrogen fixation in these microorganisms is repressed by fixed nitrogen or oxygen. Studies on the purple non-sulphur phototroph Rhodobacter capsulatus have helped to clarify this transcriptional control and to define the factors involved in this regulation. The molecular mechanisms by which the nitrogen and oxygen status of the cell are relayed into nif gene expression or repression involve many trans- and cis-acting factors. The roles of these factors in the nif regulatory cascade of R. capsulatus are summarized. Two levels of control are present. The first level of control involves the nitrogen sensing circuitry in which at least four proteins act in a cascade. Upon nitrogen deficiency, genes involved in the second level of control are transcriptionally activated. These genes encode regulatory proteins that subsequently activate transcription of all other nif genes under anaerobic conditions. The R. capsulatus cascade is compared to the nif regulatory cascade in Klebsiella pneumoniae, highlighting both common and unique aspects.

Bacteria↗

[Nitrogen fixation and primary production in Western Mediterranean].

Nitrogen fixation, nitrate assimilation and primary production ((13)C/(15)N method) were investigated during one year and half in the northwestern Mediterranean Sea. Nitrogen fixation was detectable all over the year with rates ranged from 2 to 17 nmol N l(-1) d(-1)(d). Highest values being obtained during spring associated with the phytoplankton bloom. High rates (4-8 nmol N l(-1) d(-1)(d)) were also measured during summer, when primary productivity was very low. Then, diazotrophy process supplies significant new nitrogen during summer oligotrophic periods. This new nitrogen input can balance the annual nitrogen biogeochemical budget in the Mediterranean Sea and should explain the high nitrate/phosphate ratio observed in deep waters.

Mediterranean Sea↗