Nitrogen isotope effects in the assimilation of inorganic nitrogenous compounds by marine diatoms

Nitrogen isotope fractionation in the assimilation of inorganic nitrogenous compounds was studied using marine diatoms (Phaeodactylum tricornutum and Chaetoceros sp.). The isotopic composition (δ¹⁵N) of the diatoms ranged from 7 to ‐18‰ relative to that of the nitrogen source, i.e., ammonium, nitrite, or nitrate. When the growth was light‐limited, the isotope fractionation in nitrate assimilation was inversely correlated with the growth rate. The highest fractionation factor of 1.016 was obtained when the growth rate was as low as 0.025 day^‐1. Fractionation was negligible when the growth, rate was higher than 1 day^‐1. A steady‐state kinetic model was applied to explain the isotope fractionation in nitrate assimilation. The nitrogen isotope fractionation primarily takes place at the step of N‐O bond breaking in nitrate reduction to nitrite. The extent of the isotope fractionation associated with the nitrate uptake is very small, and barely exceeds the limit of detection.     

INFLUENCE OF LOW LIGHT AND A LIGHT: DARK CYCLE ON NO3– UPTAKE,INTRACELLULAR NO3–, AND NITROGEN ISOTOPE FRACTIONATION BY MARINE PHYTOPLANKTON1

The nitrogen isotope enrichment factor (ɛ) of four species of marine phytoplankton grown in batch cultures was determined during growth in continuous saturating light, continuous low light, and a 12:12‐h light:dark cycle, with nitrate as a nitrogen source. The low growth rate that resulted from low irradiance caused an increased accumulation of the intracellular nitrate pool and/or a reduction in cell volume and was correlated to a species‐specific increase in the measured ɛ value, compared with the saturating light conditions. The largest response was in the diatom Thalassiosira weissflogii (Grun.) Fryxell et Hasle, which showed a nearly 3‐fold increase between high and low light conditions (6.2–15.2‰). The smallest response was in T. pseudonana (Hustedt) Hasle et Heimdal, which showed no change in the ɛ value of approximately 5‰ in both high and low light conditions. There was significant but smaller increases in the ɛ value for the diatom T. rotula Meunier (2.7–5.6‰) and the prymnesiophyte Emiliania huxleyi (Lohm.) Hay et Mohler (4.5–9.4‰) between high and low light levels. In the light:dark experiments, all three diatoms but not the prymnesiophyte exhibited an increase in ɛ. This increase was linked to the ability of diatoms to assimilate nitrate at night. The results of the these experiments suggest that the light regime influences the relative uptake, assimilation, and efflux rates of nitrate and results in differences in the expression of the isotope effect by the enzyme nitrate reductase. Therefore, variations in nitrate isotope fractionation in nature can be more accurately interpreted when the light regime and species composition are taken into consideration.     

Metabolic origin of δ15N values in nitrogenous compounds from Brassica napus L. leaves

Nitrogen isotope composition (δ¹⁵N) in plant organic matter is currently used as a natural tracer of nitrogen acquisition efficiency. However, the δ¹⁵N value of whole leaf material does not properly reflect the way in which N is assimilated because isotope fractionations along metabolic reactions may cause substantial differences among leaf compounds. In other words, any change in metabolic composition or allocation pattern may cause undesirable variability in leaf δ¹⁵N. Here, we investigated the δ¹⁵N in different leaf fractions and individual metabolites from rapeseed (Brassica napus) leaves. We show that there were substantial differences in δ¹⁵N between nitrogenous compounds (up to 30‰) and the content in (¹⁵N enriched) nitrate had a clear influence on leaf δ¹⁵N. Using a simple steady‐state model of day metabolism, we suggest that the δ¹⁵N value in major amino acids was mostly explained by isotope fractionation associated with isotope effects on enzyme‐catalysed reactions in primary nitrogen metabolism. δ¹⁵N values were further influenced by light versus dark conditions and the probable occurrence of alternative biosynthetic pathways. We conclude that both biochemical pathways (that fractionate between isotopes) and nitrogen sources (used for amino acid production) should be considered when interpreting the δ¹⁵N value of leaf nitrogenous compounds.     

Daily changes in nitrate influx,efflux and metabolism in maize and pearl millet

Maize (Zea mays L.) and pearl millet (Pennisetum americanum (L.) Leeke) seedlings were exposed to [¹⁵N]nitrate for 1-h periods at eight times during a 24-h period (16–8 h light-dark for maize; 14–10 h for millet). Influx of [¹⁵N]nitrate as well as its reduction and translocation were determined during each period. The efflux of previously absorbed [¹⁴N]nitrate to the uptake solution was also estimated. No marked diurnal changes in [¹⁴N]nitrate efflux or [¹⁵N]nitrate influx were evident in maize. In contrast, [¹⁴N]nitrate efflux from millet increased and eventually exceeded [¹⁵N]nitrate influx during the late dark and early light periods, resulting in net nitrate efflux from the roots. The dissimilarity of their diurnal patterns indicates that influx and efflux are independently regulated. In both species, [¹⁵N]nitrate reduction and ¹⁵N translocation to shoots were curtailed more by darkness than was [¹⁵N]nitrate influx. In the light, maize reduced 15% and millet 24% of the incoming [¹⁵N]nitrate. In darkness, reduction dropped to 11 and 17%, respectively. Since the accumulation of reduced-¹⁵N in shoots declined abruptly in darkness, whereas that in roots was little affected, it is suggested that in darkness [¹⁵N]nitrate reduction occurred primarily in roots. The decrease in nitrate uptake and reduction in darkness was not related to efflux, which remained constant in maize and did not respond immediately to darkness in pearl millet.Paper No. 6722 of the Journal Series of the North Carolina Agricultural Research Service, Raleigh     

Box-modeling of 15N/14N in mammals

The ¹⁵N/¹⁴N signature of animal proteins is now commonly used to understand their physiology and quantify the flows of nutrient in trophic webs. These studies assume that animals are predictably ¹⁵N-enriched relative to their food, but the isotopic mechanism which accounts for this enrichment remains unknown. We developed a box model of the nitrogen isotope cycle in mammals in order to predict the ¹⁵N/¹⁴N ratios of body reservoirs as a function of time, N intake and body mass. Results of modeling show that a combination of kinetic isotope fractionation during the N transfer between amines and equilibrium fractionation related to the reversible conversion of N-amine into ammonia is required to account for the well-established ≈4‰ ¹⁵N-enrichment of body proteins relative to the diet. This isotopic enrichment observed in proteins is due to the partial recycling of ¹⁵N-enriched urea and the urinary excretion of a fraction of the strongly ¹⁵N-depleted ammonia reservoir. For a given body mass and diet δ¹⁵N, the isotopic compositions are mainly controlled by the N intake. Increase of the urea turnover combined with a decrease of the N intake lead to calculate a δ¹⁵N increase of the proteins, in agreement with the observed increase of collagen δ¹⁵N of herbivorous animals with aridity. We further show that the low δ¹⁵N collagen values of cave bears cannot be attributed to the dormancy periods as it is commonly thought, but inversely to the hyperphagia behavior. This model highlights the need for experimental investigations performed with large mammals in order to improve our understanding of natural variations of δ¹⁵N collagen.     

Ectomycorrhizal impacts on plant nitrogen nutrition: emerging isotopic patterns,latitudinal variation and hidden mechanisms

Ectomycorrhizal (EcM)‐mediated nitrogen (N) acquisition is one main strategy used by terrestrial plants to facilitate growth. Measurements of natural abundance nitrogen isotope ratios (denoted as δ¹⁵N relative to a standard) increasingly serve as integrative proxies for mycorrhiza‐mediated N acquisition due to biological fractionation processes that alter ¹⁵N:¹⁴N ratios. Current understanding of these processes is based on studies from high‐latitude ecosystems where plant productivity is largely limited by N availability. Much less is known about the cause and utility of ecosystem δ¹⁵N patterns in the tropics. Using structural equation models, model selection and isotope mass balance we assessed relationships among co‐occurring soil, mycorrhizal plants and fungal N pools measured from 40 high‐ and 9 low‐latitude ecosystems. At low latitudes ¹⁵N‐enrichment caused ecosystem components to significantly deviate from those in higher latitudes. Collectively, δ¹⁵N patterns suggested reduced N‐dependency and unique sources of EcM ¹⁵N‐enrichment under conditions of high N availability typical of the tropics. Understanding the role of mycorrhizae in global N cycles will require reevaluation of high‐latitude perspectives on fractionation sources that structure ecosystem δ¹⁵N patterns, as well as better integration of EcM function with biogeochemical theories pertaining to climate‐nutrient cycling relationships.     

The 15N isotope effect in Escherichia coli: A neutron can make the difference

Several techniques based on stable isotope labeling are used for quantitative MS. These include stable isotope metabolic labeling methods for cells in culture as well as live organisms with the assumption that the stable isotope has no effect on the proteome. Here, we investigate the ¹⁵N isotope effect on Escherichia coli cultures that were grown in either unlabeled (¹⁴N) or ¹⁵N‐labeled media by LC‐ESI‐MS/MS‐based relative protein quantification. Consistent protein expression level differences and altered growth rates were observed between ¹⁴N and ¹⁵N‐labeled cultures. Furthermore, targeted metabolite analyses revealed altered metabolite levels between ¹⁴N and ¹⁵N‐labeled bacteria. Our data demonstrate for the first time that the introduction of the ¹⁵N isotope affects protein and metabolite levels in E. coli and underline the importance of implementing controls for unbiased protein quantification using stable isotope labeling techniques.     

Assimilation of [N]Nitrate and [N]Nitrite in Leaves of Five Plant Species under Light and Dark Conditions

Light dependency of nitrate and nitrite assimilation to reduced-N in leaves remains a controversial issue in the literature. With the objective of resolving this controversy, the light requirement for nitrate and nitrite assimilation was investigated in several plant species. Dark and light assimilation of [¹⁵N]nitrate and [¹⁵N]nitrite to ammonium and amino-N was determined with leaves of wheat, corn, soybean, sunflower, and tobacco. In dark aerobic conditions, assimilation of [¹⁵N]nitrate as a percentage of the light rate was 16 to 34% for wheat, 9 to 16% for tobacco, 26% for corn, 35 to 76% for soybean, and 55 to 63% for sunflower. In dark aerobic conditions, assimilation of [¹⁵N]nitrite as a percentage of the light rate was 11% for wheat, 7% for tobacco, 13% for corn, 28 to 36% for soybeans, and 12% for sunflower. It is concluded that variation among plant species in the light requirement for nitrate and nitrite assimilation explains some of the contradictory results in the literature, but additional explanations must be sought to fully resolve the controversy.

In dark anaerobic conditions, the assimilation of [¹⁵N]nitrate to ammonium and amino-N in leaves of wheat, corn, and soybean was 43 to 58% of the dark aerobic rate while dark anaerobic assimilation of [¹⁵N]nitrite for the same species was 31 to 41% of the dark aerobic rate. In contrast, accumulation of nitrite in leaves of the same species in the dark was 2.5-to 20-fold higher under anaerobic than aerobic conditions. Therefore, dark assimilation of nitrite cannot alone account for the absence of nitrite accumulation in the in vivo nitrate reductase assay under aerobic conditions. Oxygen apparently inhibits nitrate reduction in the dark even in leaves of plant species that exhibit a relatively high dark rate of [¹⁵N]nitrite assimilation.

     

Nitrogen‐isotope fractionation in the nitrate respiration by the marine bacterium Serratia marinorubra

Abstract

The isotopic composition (δ¹⁵N) of nitrite produced during nitrate respiration by both growing and washed cells of the marine bacterium, Serratia marinorubra, was determined. In both the growing and washed cells, δ¹⁵N of the nitrite changed considerably with time. At least two reaction steps, producing different isotope effects (active transport of nitrate across membranes and reduction of nitrate to nitrite), appear to be involved. With washed cells, a fractionation factor as high as 1.039 was obtained—the highest ever reported for biologicalnitrate reduction. The physiological state of nitrate‐respiring bacteria in oxygen‐depleted subsurface waters of the sea is discussed from the viewpoint of isotope fractionation.     

STIMULATION OF NITRATE NET UPTAKE AND REDUCTION BY RED AND BLUE LIGHT AND REVERSION BY FAR-RED LIGHT IN THE GREEN ALGA ULVA RIGIDA1

The steady-state levels of nitrate, nitrite, and ammonium were estimated in the green alga Ulva rigida C. Agardh in darkness after addition of 0.5 mM KNO₃ and irradiation with red (R) and blue (B) light pulses of different duration (5 and 30 min). The net uptake of nitrate was very rapid. Seventy-five percent of the nitrate added was consumed after 60 min in darkness. Although uptake was stable after R or B, efflux of nitrate occurred within 3 h in the dark control and when R or B were followed by far-red (FR) irradiation. The internal nitrate concentration after 3 h in darkness was similar after R and B light pulses; however, the intracellular ammonium was higher after R than after B. The intracellular nitrate and ammonium decreased when FR tight pulses were applied immediately after R or B. Thus, the involvement of phytochrome in the transport of nitrate and ammonium is proposed. Nitrate reductase activity, measured by the in situ method, was increased by both R and B light pulses. The effect was partially reversed by FR light. Nitrate reductase activity was higher after 5 min of R light than after 5 min of B. However, after 30-min light pulses, the relative increase in activity was reversed for R and B. We propose that phytochrome and a blue-light photoreceptor are involved in regulation of nitrogen metabolism. Nitrate uptake and reduction correlates with previously detected light-regulated accumulation of protein in Ulva rigida under the same experimental conditions.     

Nitrate influx and efflux by intact wheat seedlings: Effects of prior nitrate nutrition

Summary Wheat (Triticum vulgare L., cv. Blueboy) seedlings, grown with 0.25, 1.0 and 15 mM nitrate in complete nutrient solutions, were transferred 10 days after germination to 1.0 mM K¹⁵NO₃ (99 A% ¹⁵N) plus 0.1 mM CaSO₄ at pH 6.0. The solutions were replaced periodically over a 6-h period (5 mW cm^-2; 23°). Changes in the [¹⁵N]- and [¹⁴N]nitrate in the solution were determined by nitrate reductase and mass-spectrometric procedures and potassium by flame photometry. Influx of [¹⁵N]nitrate was depressed in plants grown at 1.0 mM nitrate relative to those grown at 0.25 mM, but there was no appreciably difference in [¹⁴N]nitrate efflux. Prior growth at 15 mM further restricted [¹⁵N]nitrate influx which, together with a substantial increase in [¹⁴N]nitrate efflux, resulted in no net nitrate uptake during the course of the experiment. Efflux of [¹⁴N]nitrate occurred to solutions containing no nitrate but it was significantly enhanced upon exposure to [¹⁵N]nitrate in the external solution. Influx of [¹⁵N]nitrate was more restricted at 5°, relative to 23°, than was [¹⁴N]nitrate efflux. The nitrate concentrations of the root tissue immediately before exposure to the K¹⁵NO₃ solutions did not give a precise indication of the subsequent [¹⁵N]nitrate influx rates nor of the [¹⁴N]nitrate efflux rates. Net K⁺ uptake was related to the magnitude of the net nitrate uptake, not to the initial K⁺ concentration in the roots. The data are interpreted as indicating that [¹⁵N]nitrate influx and [¹⁴N]nitrate efflux are largely independent processes, subject to different controls, and that net nitrate uptake provides the driving force for net potassium uptake.Paper No. 4884 of the Journal Series of the North Carolina Agricultural Experiment Station, Raleigh, NC, USA. This investigation was supported in part by the U.S. Energy Research and Development Administration, Contract No. AT-(40-1)-2410     

15N MEASUREMENTS OF AMMONIUM AND NITRATE UPTAKE BY ULVA FENESTRATA (CHLOROPHYTA) AND GRACILARIA PACIFICA (RHODOPHYTA): COMPARISON OF NET NUTRIENT DISAPPEARANCE,RELEASE OF AMMONIUM AND NITRATE,AND 15N ACCUMULATION IN ALGAL TISSUE 1

Ammonium and nitrate uptake rates in the macroalgae Ulva fenestrata (Postels and Ruprecht) (Chlorophyta) and Gracilaria pacifica (Abbott) (Rhodophyta) were determined by ¹⁵N accumulation in algal tissue and by disappearance of nutrient from the medium in long‐term (4–13 days) incubations. Nitrogen‐rich algae (total nitrogen> 4% dry weight [dw]) were used to detect isotope dilution by release of inorganic unlabeled N from algal thalli. Uptake of NH₄ ⁺ was similar for the two macroalgae, and the highest rates were observed on the first day of incubation (45 μmol N·g dw ^{? 1}·h ^{? 1} in U. fenestrata and 32 μmol N·g dw ^{? 1}·h ^{? 1} in G. pacifica). A significant isotope dilution (from 10 to 7.9 atom % enrichment) occurred in U. fenestrata cultures during the first day, corresponding to a NH₄ ⁺ release rate of 11 μmol N·g dw ^{? 1}·h ^{? 1}. Little isotope dilution occurred in the other algal cultures. Concurrently to net NH₄ ⁺ uptake, we observed a transient free amino acid (FAA) release on the first day in both macroalgal cultures. The uptake rates estimated by NH₄ ⁺ disappearance and ¹⁵N incorporation in algal tissue compare well (82% agreement, defined as the percentage ratio of the lower to the higher rate) at high NH₄ ⁺ concentrations, provided that isotope dilution is taken into account. On average, 96% of added ¹⁵NH₄ ⁺ was recovered from the medium and algal tissue at the end of the incubation. Negligible uptake of NO₃ ^? was observed during the first 2–3 days in both macroalgae. The lag of uptake may have resulted from the need for either some N deprivation (use of NO₃ ^? pools) or physiological/metabolic changes required before the uptake of NO₃ ^? . During the subsequent days, NO₃ ^? uptake rates were similar for the two macroalgae but much lower than NH₄ ⁺ uptake rates (1.97–3.19 μmol N·g dw ^{? 1}·h ^{? 1}). Very little isotope dilution and FAA release were observed. The agreement between rates calculated with the two different methods averaged 91% in U. fenestrata and 95% in G. pacifica. Recovery of added ¹⁵NO₃ ^? was virtually complete (99%). These tracer incubations show that isotope dilution can be significant in NH₄ ⁺ uptake experiments conducted with N‐rich macroalgae and that determination of ¹⁵N atom % enrichment of the dissolved NH₄ ⁺ is recommended to avoid poor isotope recovery and underestimation of uptake rates.     

PHOSPHORUS LIMITATION AND CARBON METABOLISM IN A UNICELLULAR ALGA: INTERACTION BETWEEN GROWTH RATE AND THE MEASUREMENT OF NET AND GROSS PHOTOSYNTHESIS1

Chlamydomonas reinhardii Dangeard was grown in continuous culture under P limitation at a range of dilution rates. Carbon uptake measurements were performed using double isotope (¹²C/¹⁴C) techniques and the fluxes of carbon in the light and dark were analysed over the range of growth rates. ¹⁴C uptake was shown to be equal to gross photosynthesis only at maximum relative growth rates; at low relative growth rates ¹⁴C uptake approximated net photosynthesis. The altered pattern of C uptake was found to be due to the suppression of dark respiration in the light and the release of ¹⁴C0₂ from respiratory pathways at low relative growth rates. Metabolic channelling of ¹⁴C from photosynthetic pathways to respiratory pathways occurred at low growth rates as the specific activity of the respired CO₂ reached 45% of the input gas mixture. These data are discussed in the light of the controversy concerning the measurement of gross and net photosynthesis in natural populations and in the light of models of ¹⁴C uptake in single celled algae. Existing models are shown to be adequate for high relative growth rates but not for low relative growth rates under P limitation.     

Light-mediated 15N fractionation in Caribbean gorgonian octocorals: implications for pollution monitoring

The stable nitrogen isotope ratio (?? ¹⁵N) of coral tissue is a useful recorder of anthropogenic pollution in tropical marine ecosystems. However, little is known of the natural environmentally induced fractionations that affect our interpretation of coral ?? ¹⁵N values. In symbiotic scleractinians, light affects metabolic fractionation of N during photosynthesis, which may confound the identification of N pollution between sites of varied depth or turbidity. Given the superiority of octocorals for ?? ¹⁵N studies, our goal was to quantify the effect of light on gorgonian ?? ¹⁵N in the context of monitoring N pollution sources. Using field collections, we show that ?? ¹⁵N declined by 1.4?? over 20?m depth in two species of gorgonians, the common sea fan, Gorgonia ventalina, and the slimy sea plume, Pseudopterogorgia americana. An 8-week laboratory experiment with P. americana showed that light, not temperature causes this variation, whereby the lowest fractionation of the N source was observed in the highest light treatment. Finally, we used a yearlong reciprocal depth transplant experiment to quantify the time frame over which ?? ¹⁵N changes in G. ventalina as a function of light regime. Over the year, ?? ¹⁵N was unchanged and increased slightly in the deep control colonies and shallow colonies transplanted to the deep site, respectively. Within 6?months, colonies transplanted from deep to shallow became enriched by 0.8??, mirroring the enrichment observed in the shallow controls, which was likely due to the combined effect of an increase in the source ?? ¹⁵N and reduced fractionation. We conclude that light affects gorgonian ?? ¹⁵N fractionation and should be considered in sampling designs for N pollution monitoring. However, these fractionations are small relative to differences observed between natural and anthropogenic N sources.     

Tracing the Sources of Exported Nitrate in the Turkey Lakes Watershed Using 15N/14N and 18O/16O isotopic ratios

Nitrate produced by bacterially mediated nitrification in soils is isotopically distinct from atmospheric nitrate in precipitation. ¹⁵N/¹⁴N and ¹⁸O/¹⁶O isotopic ratios of nitrate can therefore be used to distinguish between these two sources of nitrate in surface waters and groundwaters. Two forested catchments in the Turkey Lakes Watershed (TLW) near Sault Ste. Marie, Ontario, Canada were studied to determine the relative contributions of atmospheric and microbial nitrate to nitrate export. The TLW is reasonably undisturbed and receives a moderate amount of inorganic nitrogen bulk deposition (8.7 kg N · ha⁻¹· yr⁻¹) yet it exhibits unusually low inorganic nitrogen retention (average = 65% of deposition). The measured isotopic ratios for nitrate in precipitation ranged from +35 to +59‰ (VSMOW) for δ¹⁸O and −4 to +0.8‰ (AIR) for δ¹⁵N. Nitrate produced from nitrification at the TLW is expected to have an average isotope value of approximately −1.0‰ for δ¹⁸O and a value of about 0 to +6‰ for δ¹⁵N, thus, the isotopic separation between atmospheric and soil sources of nitrate is substantial. Nitrate produced by nitrification of ammonium appears to be the dominant source of the nitrate exported in both catchments, even during the snowmelt period. These whole catchment results are consistent with the results of small but intensive plot scale studies that have shown that the majority of the nitrate leached from these catchments is microbial in origin. The isotopic composition of stream nitrate provides information about N-cycling in the forested upland and riparian zones on a whole catchment basis. Received 5 October 1999; accepted 18 August 2000     

Variation in fluxes estimated from nitrogen isotope discrimination corresponds with independent measures of nitrogen flux in Populus balsamifera L.

Acquisition of mineral nitrogen by roots from the surrounding environment is often not completely efficient, in which a variable amount of leakage (efflux) relative to gross uptake (influx) occurs. The efflux/influx ratio (E/I) is, therefore, inversely related to the efficiency of nutrient uptake at the root level. Time‐integrated estimates of E/I and other nitrogen‐use traits may be obtainable from variation in stable isotope ratios or through compartmental analysis of tracer efflux (CATE) using radioactive or stable isotopes. To compare these two methods, Populus balsamifera L. genotypes were selected, a priori, for high or low nitrogen isotope discrimination. Vegetative cuttings were grown hydroponically, and E/I was calculated using an isotope mass balance model (IMB) and compared to E/I calculated using ¹⁵N CATE. Both methods indicated that plants grown with ammonium had greater E/I than nitrate‐grown plants. Genotypes with high or low E/I using CATE also had similarly high or low estimates of E/I using IMB, respectively. Genotype‐specific means were linearly correlated (r = 0.77; P = 0.0065). Discrepancies in E/I between methods may reflect uncertainties in discrimination factors for the assimilatory enzymes, or temporal differences in uptake patterns. By utilizing genotypes with known variation in nitrogen isotope discrimination, a relationship between nitrogen isotope discrimination and bidirectional nitrogen fluxes at the root level was observed.     

A non‐lethal approach to estimate whole‐body 13C and 15N stable isotope ratios of freshwater amphipods using walking legs

To analyze the stable isotope ratios of small‐bodied invertebrates, the entire animal is typically sacrificed and processed, which is problematic for threatened or endangered species. Appendages which are regenerated could be used to infer whole‐body isotope ratios, but differences in turnover rates and isotopic signatures among tissues may confound such an approach. We tested the hypothesis that the δ¹³C and δ¹⁵N of whole‐body tissue for freshwater amphipods could be predicted from the δ¹³C and δ¹⁵N of walking legs, with the goal of estimating body δ¹³C and δ¹⁵N of Gammarus acherondytes, a United States federally endangered species. To test this, we analyzed the δ¹³C and δ¹⁵N of walking legs and bodies of five species of amphipods from geographically distant areas (Idaho, Illinois, and Washington) in the United States. The general relationships of whole‐body isotope ratios of C and N as a function of leg isotope ratios were linear and had slopes of one. In the range of the data, leg δ¹³C was slightly lower than body δ¹³C, indicating some tissue‐specific fractionation, while δ¹⁵N was similar for legs and bodies. Our data suggest that legs can be used to predict body isotope ratios in freshwater amphipods. This approach provides an additional tool to help researchers understand the biology of small, endangered invertebrates without sacrificing individuals. This is especially useful in cave ecosystems where populations are naturally sparse.     

NITRATE REDUCTASE IN PHOTOSYNTHETIC BACTERIUM, RHODOSPIRILLUM RUBRUM. ADAPTIVE FORMATION OF NITRATE REDUCTASE

1. A method was discovered for adapting the cells of Rhodospirillumrubrum to grow on a nitrate medium, a capacity initially lackingin the organism. The adapted cells were able to grow with nitrateas the sole source of nitrogen. The growth responses of theadapted cells towards various nitrogenous sources were investigatedunder various conditions of incubation (aero- and anaerobiosis,light and dark).
2. The adapted cells were found to have simultaneouslyacquiredthe capacity for reducing nitrite and hydroxylamineas wellas nitrate. The path of nitrogen in the adapted cellswas assumedto be as follows: NO₃^– NO₂^– NH₂OH CellularNitrogen.
3. Nitrate metabolism of the adapted cells was investigatedundervarious conditions. In the light, nitrate was reducedand furtherassimilated, leaving insignificant amounts of nitritein themedium. In this case, consumption of nitrate was markedlyinhibitedby other forms of nitrogen (e.g., nitrite, hydroxylamine,aminoacids and ammonium salts). In the dark, nitrate was reducedas the terminal hydrogen acceptor in the oxidative breakdownof organic substances (e.g., malate) in the medium (i.e., nitraterespiration). More nitrite was accumulated in this case thanin the light. Molecular oxygen inhibited the reduction of, aswell as the growth on, nitrate in any of the above cases.
4. Theeffects on the rate of nitrate reduction (and respiratoryoxygenuptake) caused by various experimental factors (pH, nitrateconcentration, electron donors, and addition of hydroxylamine)were investigated, using the resting cells of the adapted organism.

¹ This paper was submitted to the University of Tokyo to fulfillthe requirement for the author's doctorate. ² Present Address: Botanical Institute, Kyoto University, Sakyo-ku,Kyoto. (Received February 14, 1963; )     

The relationship between N isotopic fractionation within soybean and N2 fixation during soybean development

The contribution of N₂ fixation to overall soybean N uptake has most commonly been quantified by N isotope‐based methods, which rely on isotopic differences in plant N between legumes and non‐fixing reference plants. The choice of non‐fixing reference plants is critical for the accuracy of isotope‐based methods, and mismatched reference plants remain a potential source of error. Accurate estimates of soybean N₂ fixation also require information on N isotopic fractionation within soybean. On the basis of a previous observation of a close correlation between an expression of N fractionation within soybean and the proportion of plant N derived from atmosphere (%Ndfa) determined by ¹⁵N natural abundance, this field study aimed at assessing the relationship between various expressions describing intraplant ¹⁵N or N partitioning and %Ndfa during soybean development. Starting from a late vegetative stage until beginning senescence, the N content and N isotopic composition of shoots, roots and nodules of nodulated and non‐nodulated soybeans was determined at eight different developmental stages. Regression analysis showed that %Ndfa most closely correlated with the difference in the N isotopic composition of shoot N minus that of root including nodule N, and that this relationship was similar to that obtained in a previous multi‐site field study. We therefore consider this expression to hold promise as a means of quantifying %Ndfa independent of a reference plant, which would avoid some of the external sources of error introduced by the use of reference plants in determining %Ndfa.     

Do cyanobacteria dominate in eutrophic lakes because they fix atmospheric nitrogen?

1. The sources of nitrogen for phytoplankton were determined for a bloom‐prone lake as a means of assessing the hypothesis that cyanobacteria dominate in eutrophic lakes because of their ability to fix nitrogen when the nitrogen : phosphorous (N : P) supply ratio is low and nitrogen a limiting resource. 2. Nitrogen fixation rates, estimated through acetylene reduction with ¹⁵N calibration, were compared with ¹⁵N‐tracer estimates of ammonium and nitrate uptake monthly during the ice‐free season of 1999. In addition, the natural N stable isotope composition of phytoplankton, nitrate and ammonium were measured biweekly and the contribution of N₂ to the phytoplankton signature estimated with a mixing model. 3. Although cyanobacteria made up 81–98% of phytoplankton biomass during summer and autumn, both assays suggested minimal N acquisition through fixation (<9% for the in‐situ incubations; <2% for stable isotope analysis). Phytoplankton acquired N primarily as ammonium (82–98%), and secondarily as nitrate (15–18% in spring and autumn, but <5% in summer). Heterocyst densities of <3 per 100 fixer cells confirmed low reliance on fixation. 4. The lake showed symptoms of both light and nitrogen limitation. Cyanobacteria may have dominated by monopolizing benthic sources of ammonium, or by forming surface scums that shaded other algae.