NADH-Linked oxidative phosphorylation inNitrobacter agilis

A particulate cell-free fraction (144,000-X-g pellet) fromNitrobacter agilis catalyzes the acrobic or anaerobic oxidation of NADH. Phosphorylation coupled to the aerobic oxidation of NADH yields P/O ratios of 1.1. The net formation of ATP coupled to the anaerobic oxidation of NADH by nitrate yields P/NO₃ ratios of 0.7. Phosphate esterification is uncoupled by carbonylcyanide-m-chlorophenyl-hydrozone and is sensitive to inhibitors of the electron transport system.     

Energy-coupling mechanisms under aerobic and anaerobic conditions in autotrophically grown Pseudomonas saccharophila

The cell-free preparations from autotrophieally grown Pseudomonas saccharophila catalyzed the process of electron transport from H₂ or various other organic electron donors to either O₂ or NO₃^? with concomitant ATP generation. The respective $\text{P}\text{O}$ ratios with H₂ and NADH were 0.63 and 0.73, the respective $\text{P}\text{NO}{}_3{}^{\mathrm{?}}$ ratios were 0.57 and 0.54. In contrast, the $\text{P}\text{O}$ and $\text{P}\text{NO}{}_3{}^{\mathrm{?}}$ ratios with succinate were 0.18 and 0.11, respectively. ATP formation coupled to the oxidation of ascorbate, in the absence or presence of added N,N,N′,N′-tetramethyl-p-phenylenediamine or cytochrome c, could not be detected. Various uncouplers inhibited phosphorylation with either O₂ or NO₃^? as terminal electron acceptors without affecting the oxidation of H₂ or other substrates. The NADH oxidation at the expense of O₂ or NO₃^? reduction as well as the associated phosphorylation were inhibited by rotenone and amytal. The aerobic and anaerobic H₂ oxidation and coupled ATP synthesis, on the other hand, was unaffected by the flavoprotein inhibitors as well as by the NADH trapping system. The NADH, H₂, and succinate-linked electron transport to O₂ or NO₃^? and the associated phosphorylations were sensitive, however, to antimycin A or 2-n-nonyl-4-hydroxyquino-line-N-oxide, and cyanide or azide. The data indicated that although the phosphorylation sites 1 and II were associated with NADH oxidation by O₂ or NO₃^?, the energy conservation coupled to H₂ oxidation under aerobic or anaerobic conditions appeared to involve site II only.     

Isotopic signature of nitrate in two contrasting watersheds of Brush Brook,Vermont, USA

We used the dual isotope method to study differences in nitrate export in two subwatersheds in Vermont, USA. Precipitation, soil water and streamwater samples were collected from two watersheds in Camels Hump State Forest, located within the Green Mountains of Vermont. These samples were analyzed for the δ¹⁵N and δ¹⁸O of NO₃⁻. The range of δ¹⁵N–NO₃⁻ values overlapped, with precipitation −4.5‰ to +2.0‰ (n = 14), soil solution −10.3‰ to +6.2‰ (n = 12) and streamwater +0.3‰ to +3.1‰ (n = 69). The δ¹⁸O of precipitation NO₃⁻ (mean 46.8 ± 11.5‰) was significantly different (P < 0.001) from that of the stream (mean 13.2 ± 4.3‰) and soil waters (mean 14.5 ± 4.2‰) even during snowmelt periods. Extracted soil solution and streamwater δ¹⁸O of NO₃⁻ were similar and within the established range of microbially produced NO₃⁻, demonstrating that NO₃⁻ was formed by microbial processes. The δ¹⁵N and δ¹⁸O of NO₃⁻ suggests that although the two tributaries have different seasonal NO₃⁻ concentrations, they have a similar NO₃⁻ source.     

Iron interference in the quantification of nitrate in soil extracts and its effect on hypothesized abiotic immobilization of nitrate

Human alteration of the nitrogen cycle has stimulated research on nitrogen cycling in many aquatic and terrestrial ecosystems, where analyses of nitrate (NO₃ ⁻) by standard laboratory methods are common. A recent study by Colman et al. (Biogeochemistry 84:161–169, 2007) identified a potential analytical interference of soluble iron (Fe) with NO₃ ⁻ quantification by standard flow-injection analysis of soil extracts, and suggested that this interference may have led Dail et al. (Biogeochemistry 54:131–146, 2001) to make an erroneous assessment of abiotic nitrate immobilization in prior ¹⁵N pool dilution studies of Harvard Forest soils. In this paper, we reproduce the Fe interference problem systematically and show that it is likely related to dissolved, complexed-Fe interfering with the colorimetric analysis of NO₂ ⁻. We also show how standard additions of NO₃ ⁻ and NO₂ ⁻ to soil extracts at native dissolved Fe concentrations reveal when the Fe interference problem occurs, and permit the assessment of its significance for past, present, and future analyses. We demonstrate low soluble Fe concentrations and good recovery of standard additions of NO₃ ⁻ and NO₂ ⁻ in extracts of sterilized Harvard Forest soils. Hence, we maintain that rapid NO₃ ⁻ immobilization occurred in sterilized samples of the Harvard Forest O horizon in the study by Dail et al. (2001). Furthermore, additional evidence is accumulating in the literature for rapid disappearance of NO₃ ⁻ added to soils, suggesting that our observations were not the result of an isolated analytical artifact. The conditions for NO₃ ⁻ reduction are likely to be highly dependent on microsite properties, both in situ and in the laboratory. The so-called “ferrous wheel hypothesis” (Davidson et al., Glob Chang Biol 9:228–236, 2003) remains an unproven, viable explanation for published observations.     

Yield response and nitrate accumulation in rhodes grass (Chloris gayana Kunth) grown in high-nitrate-content solutions

The effect of nitrate concentration in the nutrient solution, on yields and nitrate accumulation in the plant, was studied in Rhodes grass grown in sand culture. The results showed that optimal yield was achieved in the 7.5meq.L⁻¹ N solution. The optimal NO₃−N concentration in the plant canopy may be an indicator of effective N fertilizer use. Increasing N fertilization will only increase the NO₃−N concentration in the plant. A.R.O. Contribution no. 2244-E, 1987 series.     

Light dependent reduction of nitrate by pea chloroplasts in the presence of nitrate reductase and C4-dicarboxylic acids

In the presence of purified nitrate reductase (NR) and 1 mM NADH, illuminated pea chloroplasts catalysed reduction of NO₃^? to NH₃ with the concomitant evolution of O₂. The rates were slightly less than those for reduction of NO₂^? to NH₃ and O₂, evolution by chloroplasts in the absence of NR and NADH (ca 6 μg atoms N/mg Chl/hr). Illuminated chloroplasts quantitatively reduced 0.2 mM oxaloacetate (OAA) to malate. In the presence of an extrachloroplast malate-oxidizing system comprised of NAD-specific malate dehydrogenase (NAD-MDH), NAD, NR and NO₃^?, illuminated chloroplasts supported OAA-dependent reduction of NO₃^? to NH₃ with the evolution of O₂. The reaction did not proceed in the absence of any of these supplements or in the dark but malate could replace OAA. The results are consistent with the reduction of NO₃^?by reducing equivalents from H₂O involving a malate/OAA shuttle. The ratios for O₂, evolved: C₄-acid supplied and N reduced: C₄-acid supplied in certain experiments imply recycling of the C₄-acids.     

Salinity affects indirectly nitrate acquisition associated with glutamine accumulation in cowpea roots

The aim of this study was to test the hypothesis that salinity can affect indirectly the nitrate acquisition by a negative modulation triggered by glutamine accumulation. Cowpea plants were exposed to a mild NaCl concentration (50 mM) in order to restrict growth and N-demand. After 21 d, pretreated plants and control plants were supplied with 0, 5 and 10 mM of Ca(NO₃)₂ for 3 d in absence of NaCl. Salt pretreated plants showed a great limitation in acquisition of NO₃ ⁻, indicated by decline in the nitrate uptake rate, NO₃ ⁻ accumulation, nitrate reductase activity and protein content. The restriction of NO₃ ⁻ utilization was positively associated with increased glutamine synthetase activity and glutamine accumulation, especially in roots.     

Influence of hydrogen acceptors on growth and energy production ofProteus mirabilis

The generation time ofP. mirabilis in defined and in complex medium is shorter in the presence of hydrogen acceptors than in their absence. In the presence of hydrogen acceptors the molar growth yield for glucose and the acetate production are strongly increased. From the molar growth yield and the acetate production Y_ATP in defined medium was calculated as 5.5 g/mole, whereas in complex medium a value of 12.6 g/mole was obtained. The molar growth yield, the acetate production, the amount of hydrogen acceptor reduced and Y_ATP were used to calculate P/2e⁻ratios for phosphorylation coupled to electron transfer to oxygen, nitrate and tetrathionate as respectively 2.80; 1.48 and 1.23 in defined medium. Under anaerobic conditions in the presence of nitrate or tetrathionate as hydrogen acceptor in complex medium a bend in the growth curve is observed. In the period of rapid growth the P/2e⁻ratio for nitrate reduction is of the same magnitude as that in defined medium, however much lower P/2e⁻ratios are found during the subsequent period of slow growth. The P/2e⁻ratios for tetrathionate reduction in complex medium for both growth periods are lower than those in defined medium. Most probably these results indicate that during this period growth and energy production are uncoupled. Under aerobic conditions in complex medium a constant Y_O value of 32.2 g/atom O is found during a short period of the growth curve. Afterwards when the cell density increases a steady decrease of Y_O is observed.     

Response of nodulating and non-nodulatingPisum sativum L. to nitrate

This study examined whether ‘Risnod2’ and ‘Risnod27’ non-nodulating mutants of pea (Pisum sativum L.) provided with increasing concentrations of nitrate could achieve a growth and nitrogen accumulation comparable to their parental N₂-fixing cv. Finale. In the cv. Finale, nodule number, nodule dry mass accumulation, total C₂H₂-reducing activity of nodulated roots (TAR) and estimated N₂ fixation were considerably inhibited at 5.0 and 10.0 mM root medium NO₃ ⁻ concentrations. In contrast a 0.63 mM level stimulated both the nodule dry mass and TAR. The cv. Finale N₂-fixing plants grown on 0 to 2.5 mM NO₃ ⁻ levels had higher shoot N concentrations than the Nod⁻ mutants, but within the 5.0 to 10.0 mM levels the Nod⁻ mutants approached or even overtopped the N concentration of the cv. Finale plants. Compared with a high positive correlation found in the Nod⁻ mutants, shoot N concentration in the cv. Finale was negatively correlated with the root medium NO₃ ⁻ concentration. The pattern of nitrogen content in shoot dry mass was very similar to that seen in the shoot dry mass accumulation. The Nod⁻ mutants grown on the 5.0 and/or 10.0 mM NO₃ ⁻ level had plant dry mass, shoot nitrogen concentration, shoot nitrogen content, and root/shoot dry mass ratio comparable with those of the nodulating cv. Finale grown on the same nitrate levels.     

Succinate is the controller of O<Stack><Subscript>2</Subscript><Superscript>−</Superscript></Stack>/H<Subscript>2</Subscript>O<Subscript>2</Subscript> release at mitochondrial complex I : negative modulation by malate,positive by cyanide

Mitochondrial production of H₂O₂ is low with NAD substrates (glutamate/pyruvate, 3 and 2 mM) (G/P) and increases over ten times upon further addition of succinate, with the formation of a sigmoidal curve (semimaximal value at 290 μM, maximal H₂O₂ production at 600 μM succinate). Malate counteracts rapidly the succinate induced increased H₂O₂ release and moves the succinate dependent H₂O₂ production curve to the right. Nitric oxide (NO) and carbon monoxide (CO) are cytochrome c oxidase inhibitors which increase mitochondrial ROS production. Cyanide (CN⁻) was used to mimic NO and CO. In the presence of G/P and succinate (300 μM), CN⁻ progressively increased the H₂O₂ release rate, starting at 1.5 μM. The succinate dependent H₂O₂ production curve was moved to the left by 30 μM CN⁻. The V_max was little modified. We conclude that succinate is the controller of mitochondrial H₂O₂ production, modulated by malate and CN⁻. We propose that succinate promotes an interaction between Complex II and Complex I, which activates O₂⁻ production.     

Some Reactions of Isolated Corn Mitochondria Influenced by Juglone

The effects of juglone on the uptake of O₂ by excised corn roots (Zea mays L., Wf9 cms- T × M14) and isolated corn mitochondria arc reported. The O₂ uptake by excised corn roots, as measured by an O₂ electrode, was inhibited more than 90% after a one-hour treatment of 500 μM juglone. Lesser inhibitions were observed with 50 μM and 250 μM juglone. In a KC1 reaction medium in the absence of inorganic phosphate (Pi), juglone stimulated the rate of O₂ uptake by isolated mitochondria oxidizing NADH, succinate, or malate + pyruvate. In the presence of Pi, juglone concentrations of 3 μM and greater inhibited the state 3 oxidation rates of succinate and malate + pyruvate, lowered respiratory control and ADP/O ratios obtained from the oxidation of NADH, malate + pyruvate, or succinate, and reduced the coupled deposition of calcium phosphate within isolated mitochondria driven, by the oxidation of malate + pyruvate. The inhibition of state 3 O₂ uptake by isolated mitochondria, an oxidative state in which electron transfer is coupled to ATP production, is seen to correlate with the inhibition affected by juglone when applied to tissues in vivo.     

Denitrification,dissimilatory nitrate reduction to ammonium,and nitrogen fixation along a nitrate concentration gradient in a created freshwater wetland

Wetlands are often highly effective nitrogen (N) sinks. In the Lake Waco Wetland (LWW), near Waco, Texas, USA, nitrate (NO₃⁻) concentrations are reduced by more than 90% in the first 500 m downstream of the inflow, creating a distinct gradient in NO₃⁻ concentration along the flow path of water. The relative importance of sediment denitrification (DNF), dissimilatory NO₃⁻ reduction to ammonium (DNRA), and N₂ fixation were examined along the NO₃⁻ concentration gradient in the LWW. “Potential DNF” (hereafter potDNF) was observed in all months and ranged from 54 to 278 μmol N m⁻² h⁻¹. “Potential DNRA” (hereafter potDNRA) was observed only in summer months and ranged from 1.3 to 33 μmol N m⁻² h⁻¹. Net N₂ flux ranged from 184 (net denitrification) to −270 (net N₂ fixation) μmol N m⁻² h⁻¹. Nitrogen fixation was variable, ranging from 0 to 426 μmol N m⁻² h⁻¹, but high rates ranked among the highest reported for aquatic sediments. On average, summer potDNRA comprised only 5% (±2% SE) of total NO₃⁻ loss through dissimilatory pathways, but was as high as 36% at one site where potDNF was consistently low. Potential DNRA was higher in sediments with higher sediment oxygen demand (r ² = 0.84), and was related to NO₃⁻ concentration in overlying water in one summer (r ² = 0.81). Sediments were a NO₃⁻ sink and accounted for 50% of wetland NO₃⁻ removal (r ² = 0.90). Sediments were an NH₄⁺ source, but the wetland was often a net NH₄⁺ sink. Although DNRA rates in freshwater wetlands may rival those observed in estuarine systems, the importance of DNRA in freshwater sediments appears to be minor relative to DNF. Furthermore, sediment N₂ fixation can be extremely high when NO₃⁻ in overlying water is consistently low. The data suggest that newly fixed N can support sustained N transformation processes such as DNF and DNRA when surface water inorganic N supply rates are low.     

Role of nitrite reductase in the ammonia-oxidizing pathway of <Emphasis Type="Italic">Nitrosomonas europaea</Emphasis>

Metabolism of ammonia (NH₃) and hydroxylamine (NH₂OH) by wild-type and a nitrite reductase (nirK) deficient mutant of Nitrosomonas europaea was investigated to clarify the role of NirK in the NH₃ oxidation pathway. NirK-deficient N. europaea grew more slowly, consumed less NH₃, had a lower rate of nitrite (NO₂ ⁻) production, and a significantly higher rate of nitrous oxide (N₂O) production than the wild-type when incubated with NH₃ under high O₂ tension. In incubations with NH₃ under low O₂ tension, NirK-deficient N. europaea grew more slowly, but had only modest differences in NH₃ oxidation and product formation rates relative to the wild-type. In contrast, the nirK mutant oxidized NH₂OH to NO₂ ⁻ at consistently slower rates than the wild-type, especially under low O₂ tension, and lost a significant pool of NH₂OH–N to products other than NO₂ ⁻ and N₂O. The rate of N₂O production by the nirK mutant was ca. three times higher than the wild-type during hydrazine-dependent NO₂ ⁻ reduction under both high and low O₂ tension. Together, the results indicate that NirK activity supports growth of N. europaea by supporting the oxidation of NH₃ to NO₂ ⁻ via NH₂OH, and stimulation of hydrazine-dependent NO₂ ⁻ reduction by NirK-deficient N. europaea indicated the presence of an alternative, enzymatic pathway for N₂O production.     

The effect of the osmotic potential and specific ion concentration of the nutrient solution on the uptake and reduction of nitrate by barley seedlings

Summary Short-term absorption experiments were conducted with intact barley (Hordeum vulgare L.) seedlings to observe the effects of the osmotic potential (Ψ^π) and salt species on nitrate uptake andin vivo nitrate reduction. The experiments consisted of growing barley seedlings for 5 days in complete nutrient solutions salinized to (Ψ^π) levels of −0.6, −1.8, −3.0, −4.2, and −5.4 bars with NaCl, CaCl₂ or Na₂SO₄. After the absorption period, the seedlings were separated into shoots and roots, weighed, then analyzed for NO₃. The nutrient solutions were sampled for NO₃ analysis each day immediately before renewing the solutions. The accumulative loss of NO₃ from the solutions was considered to be uptake whereas NO₃ reduction was the difference between uptake and seedling content. Lowering the (Ψ^π) of the nutrient solutions resulted in decreased concentrations of NO₃ in the plant, little or no effect (except at the lowest (Ψ^π) level) on uptake, and increased nitrate reductase activity. Increased rates of NO₃ reduction were in particular associated with the Cl concentration of the nutrient solution.     

Bioaugmented sulfur-oxidizing denitrification system with <Emphasis Type="Italic">Alcaligenes defragrans</Emphasis> B21 for high nitrate containing wastewater treatment

The performance of enriched sludge augmented with the B21 strain of Alcaligenes defragrans was compared with that of enriched sludge, as well as with pure Alcaligenes defragrans B21, in the context of a sulfur-oxidizing denitrification (SOD) process. In synthetic wastewater treatment containing 100–1,000 mg NO₃⁻-N/L, the single strain-seeded system exhibited superior performance, featuring higher efficiency and a shorter startup period, provided nitrate loading rate was less than 0.2 kg NO₃⁻-N/m³ per day. At nitrate loading rate of more than 0.5 kg NO₃⁻-N/m³ per day, the bioaugmented sludge system showed higher resistance to shock loading than two other systems. However, no advantage of the bioaugmented system over the enriched sludge system without B21 strain was observed in overall efficiency of denitrification. Both the bioaugmented sludge and enriched sludge systems obtained stable denitrification performance of more than 80% at nitrate loading rate of up to 2 kg NO₃⁻-N/m³ per day.     

Dual isotope analyses indicate efficient processing of atmospheric nitrate by forested watersheds in the northeastern U.S.

Nitrogen from atmospheric deposition serves as the dominant source of new nitrogen to forested ecosystems in the northeastern U.S. By combining isotopic data obtained using the denitrifier method, with chemical and hydrologic measurements we determined the relative importance of sources and control mechanisms on nitrate (NO₃ ⁻) export from five forested watersheds in the Connecticut River watershed. Microbially produced NO₃ ⁻ was the dominant source (82–100%) of NO₃ ⁻ to the sampled streams as indicated by the δ¹⁵N and δ¹⁸O of NO₃ ⁻. Seasonal variations in the δ¹⁸O–NO₃ ⁻ in streamwater are controlled by shifting hydrologic and temperature affects on biotic processing, resulting in a relative increase in unprocessed NO₃ ⁻ export during winter months. Mass balance estimates find that the unprocessed atmospherically derived NO₃ ⁻ stream flux represents less than 3% of the atmospherically delivered wet NO₃ ⁻ flux to the region. This suggests that despite chronically elevated nitrogen deposition these forests are not nitrogen saturated and are retaining, removing, and reprocessing the vast majority of NO₃ ⁻ delivered to them throughout the year. These results confirm previous work within Northeastern U.S. forests and extend observations to watersheds not dominated by a snow-melt driven hydrology. In contrast to previous work, unprocessed atmospherically derived NO₃ ⁻ export is associated with the period of high recharge and low biotic activity as opposed to spring snowmelt and other large runoff events.     

Anaerobic ammonia oxidation with nitrogen dioxide by Nitrosomonas eutropha

Nitrosomonas eutropha, an obligately lithoautotrophic bacterium, was able to nitrify and denitrify simultaneously under anoxic conditions when gaseous nitrogen dioxide (NO₂) was supplemented to the atmosphere. In the presence of gaseous NO₂, ammonia was oxidized, nitrite and nitric oxide (NO) were formed, and hydroxylamine occurred as an intermediate. Between 40 and 60% of the produced nitrite was denitrified to dinitrogen (N₂). Nitrous oxide (N₂O) was shown to be an intermediate of denitrification. Under an N₂ atmosphere supplemented with 25 ppm NO₂ and 300 ppm CO₂, the amount of cell protein increased by 0.87 mg protein per mmol ammonia oxidized, and the cell number of N. eutropha increased by 5.8 × 10⁹ cells per mmol ammonia oxidized. In addition, the ATP and NADH content increased by 4.3 μmol ATP (g protein)^–1 and 6.3 μmol NADH (g protein)^–1 and was about the same in both anaerobically and aerobically grown cells. Without NO₂, the ATP content decreased by 0.7 μmol (g protein)^–1, and the NADH content decreased by 1.2 μmol (g protein)^–1. NO was shown to inhibit anaerobic ammonia oxidation. Received: 9 October 1996 / Accepted: 5 December 1996     

Whole-stream nitrate addition affects litter decomposition and associated fungi but not invertebrates

We assessed the effect of whole-stream nitrate enrichment on decomposition of three substrates differing in nutrient quality (alder and oak leaves and balsa veneers) and associated fungi and invertebrates. During the 3-month nitrate enrichment of a headwater stream in central Portugal, litter was incubated in the reference site (mean NO₃-N 82 μg l⁻¹) and four enriched sites along the nitrate gradient (214–983 μg NO₃-N l⁻¹). A similar decomposition experiment was also carried out in the same sites at ambient nutrient conditions the following year (33–104 μg NO₃-N l⁻¹). Decomposition rates and sporulation of aquatic hyphomycetes associated with litter were determined in both experiments, whereas N and P content of litter, associated fungal biomass and invertebrates were followed only during the nitrate addition experiment. Nitrate enrichment stimulated decomposition of oak leaves and balsa veneers, fungal biomass accrual on alder leaves and balsa veneers and sporulation of aquatic hyphomycetes on all substrates. Nitrate concentration in stream water showed a strong asymptotic relationship (Michaelis–Menten-type saturation model) with temperature-adjusted decomposition rates and percentage initial litter mass converted into aquatic hyphomycete conidia for all substrates. Fungal communities did not differ significantly among sites but some species showed substrate preferences. Nevertheless, certain species were sensitive to nitrogen concentration in water by increasing or decreasing their sporulation rate accordingly. N and P content of litter and abundances or richness of litter-associated invertebrates were not affected by nitrate addition. It appears that microbial nitrogen demands can be met at relatively low levels of dissolved nitrate, suggesting that even minor increases in nitrogen in streams due to, e.g., anthropogenic eutrophication may lead to significant shifts in microbial dynamics and ecosystem functioning. Electronic Supplementary Material Supplementary material is available to authorised users in the online version of this article at .     

Effect of nitrate concentration and UVR on photosynthesis,respiration, nitrate reductase activity,and phenolic compounds in <Emphasis Type="Italic">Ulva rigida</Emphasis> (Chlorophyta)

Seaweeds growing in the intertidal zone are exposed to fluctuating nitrate and ultraviolet radiation (UVR) levels. While it has been shown that elevated UVR levels and the decrease of nitrate concentration can reduce photosynthetic levels in seaweeds, less is known about the combined effect of nitrate levels and UVR on metabolism and photoprotection mechanisms of intertidal species. Consequently, the objective of this study was to evaluate the effect of nitrate concentration and UVR treatments on photosynthesis, respiration, nitrate reductase activity and phenolic compound levels of Ulva rigida (Chlorophyta). There was a two- to threefold increase in maximal gross photosynthesis (GP_max) and respiration rates, as nitrate increased from 0 to 50 μM NO₃⁻. Similarly, nitrate reductase activity increased linearly from low values in algae incubated at 0 μM NO₃ to high values in tissue incubated at 50 μM NO₃⁻. Phenolic compounds in the tissue of U. rigida increased approximately 60% under 50 μM NO₃⁻ relative to those incubated at 0 μM NO₃⁻. Algae exposed to UVR (8 h) showed a significant decrease in the effective quantum yield and respiration, however, no effect was observed in the phenolic compounds levels. Full recovery of effective quantum yield was observed after U. rigida was transferred for 48 h to low PAR. Nitrate reductase also decreased after an 8-h UVR exposure, but no differences were observed among the nitrate treatments. This study shows that high nitrate levels reduced the negative effect of UVR on the effective quantum yield and increased the recovery of key metabolic enzymes. It is possible that the increase of phenolic compounds in the thallus of U. rigida under high nitrate levels provide a photoprotective mechanism when exposed to high UV levels during low tides.     

NADH oxidase activity of rat and human liver xanthine oxidoreductase: potential role in superoxide production

To characterise the NADH oxidase activity of both xanthine dehydrogenase (XD) and xanthine oxidase (XO) forms of rat liver xanthine oxidoreductase (XOR) and to evaluate the potential role of this mammalian enzyme as an O₂ ^•− source, kinetics and electron paramagnetic resonance (EPR) spectroscopic studies were performed. A steady-state kinetics study of XD showed that it catalyses NADH oxidation, leading to the formation of one O₂ ^•− molecule and half a H₂O₂ molecule per NADH molecule, at rates 3 times those observed for XO (29.2 ± 1.6 and 9.38 ± 0.31 min⁻¹, respectively). EPR spectra of NADH-reduced XD and XO were qualitatively similar, but they were quantitatively quite different. While NADH efficiently reduced XD, only a great excess of NADH reduced XO. In agreement with reductive titration data, the XD specificity constant for NADH (8.73 ± 1.36 μM⁻¹ min⁻¹) was found to be higher than that of the XO specificity constant (1.07 ± 0.09 μM⁻¹ min⁻¹). It was confirmed that, for the reducing substrate xanthine, rat liver XD is also a better O₂ ^•− source than XO. These data show that the dehydrogenase form of liver XOR is, thus, intrinsically more efficient at generating O₂ ^•− than the oxidase form, independently of the reducing substrate. Most importantly, for comparative purposes, human liver XO activity towards NADH oxidation was also studied, and the kinetics parameters obtained were found to be very similar to those of the XO form of rat liver XOR, foreseeing potential applications of rat liver XOR as a model of the human liver enzyme.