Nitrate reductase and its role in nitrate assimilation in plants

Nitrate reductase (EC 1.6.6.1) is an enzyme found in most higher plants and appears to be a key regulator of nitrate assimilation as a result of enzyme induction by nitrate. The biochemistry of nitrate reductase has been elucidated to a great extent and the role that nitrate reductase plays in regulation of nitrate assimilation is becoming understood.     

Regulation of nitrate reductase activity in higher plants

Nitrate reductase is one of the most important enzymes in the assimilation of exogenous nitrate—the predominant form of nitrogen available to green plants growing in soil. Activity of this enzyme in plants gives a good estimate of the nitrogen status of the plant and is very often correlated with growth and yield. Although it is difficult to explain the physiological significance and the mechanism of effects of several factors on the enzyme activity, in some cases suitable postulates have been advanced. In general, the enzyme activity in a plant tissue is a balance between its relative rates of synthesis/degradation and activation/inactivation. Factors may affect the overall activity by interfering with either of these processes.     

植物中硝酸还原酶和亚硝酸还原酶的作用

植物通过硝酸盐同化途径以硝酸盐和氨的形式吸收氮元素。硝酸盐的同化是一个受到严格控制的过程,其中两个先后参加反应的酶——硝酸还原酶(NR)和亚硝酸还原酶(NiR)对初级氮的同化起主要调控。在高等植物中,NR和NiR基因的转录及转录后加工受到各种内在和外在因素的影响,翻译后调控是消除亚硝酸盐积累的重要机制。随着分子生物学技术的发展,可以更容易地通过突变体和转基因方式来研究NR和NiR基因的调控。     

The partitioning of nitrate assimilation between root and shoot of higher plants

Abstract The partitioning of nitrate assimilation between root and shoot of higher plant species is indicated by the relative proportions of total plant nitrate reductase activity (NRA) in the two plant parts and the relative concentrations of nitrate and reduced N in the xylem sap. These have been collated here from the literature and temperate and tropical species compared. Both the distribution of NRA and xylem sap nitrate: reduced N indicate that the following four generalizations can be made.

• 1 Temperate, perennial species growing in low external nitrate concentrations (about 1 mol m^?3) carry out most of their nitrate assimilation in the root. As external nitrate concentration increases (in the range found in agricultural soils, 1–20 mol m^?3), shoot nitrate assimilation becomes increasingly important.
• 2 Temperate, annual legume species growing in low external nitrate concentrations carry out most of their nitrate assimilation in the root. Shoot nitrate assimilation increases in importance as external nitrate concentration is increased.
• 3 Temperate, annual non-legume species vary greatly in their partitioning of nitrate assimilation between root and shoot when growing in low external nitrate concentrations. Regardless of the proportion carried out in the root at low external nitrate concentrations, nitrate assimilation in the shoot becomes increasingly important as external nitrate concentration is increased.
• 4 Tropical and subtropical species, annual and perennial, carry out a substantial proportion of their nitrate assimilation in the shoot when growing in low external nitrate concentrations. The partitioning of nitrate assimilation between root and shoot remains constant as external nitrate concentration increases.

It is proposed that a greater proportion of nitrate assimilation occurs in the shoot when an increase in the rate of nitrate uptake does not induce an increase in NR level in the root. Thus, a greater proportion of the nitrate taken up remains unassimilated and is passed into the xylem. A constant partitioning of nitrate assimilation between root and shoot is achieved by balancing NR levels in the root with rates of nitrate uptake. The advantages and disadvantages of assimilating nitrate in either the root or shoot are discussed in relation to temperate and tropical habitats.     

Nitrate uptake and reduction in higher and lower plants

The nitrogen compounds nitrate and ammonium are the minerals that plants need in large quantities and which limit their growth in temperate zones. The nitrate assimilation pathway starts with nitrate uptake followed by nitrate reduction resulting in ammonium which is fixed into the amino acids glutamine and glutamate in most plants. This review concentrates on nitrate uptake and nitrate reduction with respect to higher and lower plants. The physiology and the progress in molecular approaches of both processes are considered. For nitrate uptake the well‐established uptake systems are discussed and special attention is drawn to nitrate sensing and the nitrate carrier. Knowledge, particularly on nitrate sensing is rare, but it seems to be the first step in a signal transduction chain triggered by nitrate. Therefore further work should consider this topic more frequently. For nitrate reductase the focus is on the post‐translational modification as a regulatory tool for nitrate assimilation, on the intersections of carbon and nitrogen metabolism and on the molecular approaches. A few remarks on how environmental conditions affect nitrate assimilation are also included. Further progress is needed to understand the transduction of positive and negative signals from the environment affecting the expression of genes coding for the nitrate assimilating pathway.     

Inorganic nitrogen assimilation in plants of Austrlian rainforest communities

In a study of the plant communities of two Australian rainforests, it was found that pioner species had high levels of nitrate reductase (EC 1.6.6.1) and were predominantly leaf nitrate assimilators. Under- and over-storey species had low levels of shoot and root nitrate reductase activity, and many of them showed little capacity for nitrate reduction even when nitrate ions were freely available. Although closed-forest species have lower levels of nitrate reductase than those of gaps and forest margins, their total nitrogen contents were similar, suggesting the former utilize nitrogen sources other than nitrate ions. Glutamine synthetase (EC 6.3.1.2) was present in the leaves of all species examined. In the leaves of pioneer species the chloroplastic isoform of glutamine synthetase predominted, while in most of the species typical of closed-forest the cytosolic isoform accounted for at least 40% of total leaf activity. Low levels of chloroplastic glutamine synthetase were correlated with a low capacity for leaf nitrate reduction, and both are characteristic of many species that regenerate and grow for some time in shade. Low levels of chloroplastic glutamine synthetase imply that, in some of these woody plants, photorespiratory ammonia is re-assimilated via cytosolic glutamine synthetase.     

植物氮代谢硝酸还原酶水平调控机制的研究进展

氮代谢是植株体内最基本的物质代谢之一,硝酸还原酶是植物氮代谢的关键酶。主要对植物氮代谢在硝酸还原酶水平上调控的研究新进展,尤其是其合成／降解及活性调控机制进行了较为系统的综述。硝酸还原酶合成的调控主要发生在转录水平和翻译水平上,硝酸还原酶降解的调控主要发生在翻译后水平上,同时NO3^-及光在硝酸还原酶转录水平调控上的作用重大,硝酸还原酶编码基因转录的mRNA的稳定性强弱影响植物的氮代谢,而影响mRNA稳定性的因素很多,机理复杂;磷酸化／去磷酸化在硝酸还原酶活性调控中占举足轻重的地位,研究也比较深入。钝化蛋白也能够影响硝酸还原酶活性,许多小分子物质对硝酸还原酶活性有影响。     

Nitrate reductase is not accumulated in chloroplast-ribosome-deficient mutants of higher plants

The activities of nitrite reductase (EC 1.7.7.1) are 60–70% of wild-type activity in pigment-deficient leaves of the chloroplast-ribosomedeficient mutants albostrians (Hordeum vulgare) and iojap (Zea mays). The activity and apoprotein of nitrate reductase (EC 1.6.6.1.) are lacking in the barley mutant. Only very low activities of nitrate reductase can be extracted from leaves of the maize mutant. The molybdenum cofactor of nitrate reductase and xanthine dehydrogenase (EC 1.2.3.2) is present in maize and barley mutant plants. However, it is not inducible by nitrate in pigment-deficient leaves of albostrians. From these results we conclude: (i) Nitrite reductase (a chloroplast enzyme) is synthesized in the cytoplasm and does not need the presence of nitrate reductase for the induction and maintenance if its activity. (ii) The loss or low activity of nitrate reductase is a consequence of the inability of the mutants to accumulate the apoprotein of this enzyme. (iii) The chloroplasts influence the accumulation (i.e. most probably the synthesis) of the nonchloroplast enzyme, nitrate reductase. The accumulation of nitrate reductase needs a chloroplast factor which is not provided by mutant plastids blocked at an early stage of their development.Abbreviations CRM cross-reacting material - Mo-co molybdenum cofactor - NiR nitrite reductase - NR nitrate reductase     

Nitrate reductase and nitrate accumulation in relation to nitrate toxicity in Boronia megastigma

Moderate levels of N were toxic to the native Australian plant boronia (Boronia megastigma Nees). As NO^-₃ is the major N form available for plants under cultivated conditions, NO^-₃ reduction and accumulation patterns in boronia were examined following the supply of various levels of NO^-₃ to understand the physiological basis of this toxicity. At a low level of supplied NO^-₃ [15 mmol (plant)^-1], NO^-₃ was reduced without any detectable accumulation and without nitrate reductase activity (NRA) reaching its maximum capacity. When higher NO^-₃ levels [≥25 mmol (plant)^-1] were supplied, both NRA and NO^-₃ accumulation increased further. However, NRA increased to a maximum of ca 500 nmol NO^-₃ (g fresh weight)^-1 h^-1, both in the roots and leaves, irrespective of a 4-fold difference in the levels of supplied NO^-₃, whereas NO^-₃ continued to accumulate in proportion to the level of supplied NO^-₃. Chlorotic toxicity symptoms appeared on the leaves at an accumulation of ca 32 μmol NO^-₃ (g fresh weight)^-1. High endogenous NO^-₃ concentrations inhibited NRA. The low level of NRA in boronia was not limited by NO^-₃ or electron donor availability. It is concluded that the low NR enzyme activity is a genetic adaptation to the low NO^-₃ availability in the native soils of boronia. Thus, when NO^-₃ supply is high, the plat cannot reduce it at high rates, leading to large and toxic accumulations of the ion in the leaf tissues.     

The role of glutamine synthetase in regulation of nitrogen metabolism within the soil microbial community

Recent advances in our understanding of the enzymology and regulatory systems involved in microbial metabolism of N hold promise to elucidate some of the underlying factors controlling metabolism of N in soil ecosystems. A review of recent work is used to construct a paradigm for N metabolism regulation in soil based on the central role of glutamine synthetase (GS) in such regulation within the soil microbial community. The studies involved use of GS inhibitors to elucidate the role of GS activity in regulation of soil N metabolism. Such studies have shown that the glutamine formed by microbial assimilation of NH₄ ⁺ via GS activity influences the regulatory mechanisms controlling both the production and activity of enzymes involved in N metabolism. For example, these studies showed that the inhibition of GS activity within the soil microbial community relieved the repression of urease production caused by microbial assimilation of inorganic N and blocked the short-term regulation of assimilatory nitrate reductase (ANR) by NH₄ ⁺ assimilation. Other studies have indicated that common environmental factors in soil may influence GS activity in microorganisms and thereby may influence metabolism of N within the soil microbial community. The paradigm for N metabolism regulation in soil that has emerged from such studies should lead to a better understanding of the mechanisms controlling fate of N in soil ecosystems.     

The pathway of nitrogen assimilation in plants

The major route of nitrogen assimilation has been considered for many years to occur via the reductive amination of α-oxoglutarate, catalysed by glutamate dehydrogenase. However, recent work has shown that in most bacteria an alternative route via glutamine synthetase and glutamine: 2-oxoglutarate aminotransferase (glutamate synthase) operates under conditions of ammonia limitation. Subsequently the presence of a ferredoxin-dependent glutamate synthase in green leaves and green and blue-green algae, and a NAD(P)H and ferredoxin-dependent enzyme in roots and other non-green plant tissues, has suggested that this route may also function in most members of the plant kingdom. The only exceptions are probably the majority of the fungi, where so far most organisms studied do not appear to contain glutamate synthase. Besides the presence of the necessary enzymes there is other evidence to support the contention that the assimilation of ammonia into amino acids occurs via glutamine synthetase and glutamate synthase, and that it is unlikely that glutamate dehydrogenase plays a major role in nitrogen assimilation in bacteria or higher plants except in circumstances of ammonia excess.     

Alterations in nitrogen assimilation and partitioning in nitrogen stressed plants

Although nutrient stress is known to alter partitioning between shoots and roots, the physiological basis for the phenomenon is unresolved. Experiments were conducted to examine assimilation of ¹⁵NO₃ by N-stressed plants and to determine whether apparent changes in assimilation in the root contributed to alterations in whole-plant partitioning of reduced-N. Tobacco plants (Nicotiana tabacum L. cv. NC 2326) were exposed to a low concentration of NO₃^? in solution (80 μM) for 9 days to effect a N-stress response. Exposure of plants to 1000 μM¹⁵NO₃^? for 12 h on selected days revealed that roots of N-stressed plants developed an increased capacity to absorb NO₃^?, and accumulation of reduced-¹⁵N in the root increased to an even greater extent. When plants were exposed to 80 or 1000 μM¹⁵NO₃^? in steady-state, ¹⁵NO₃^? uptake over a 12 h period was noticeably restricted at the lower concentration, but a larger proportion of the absorbed ¹⁵N still accumulated as reduced-¹⁵N in the root. The alteration in reduced-¹⁵N partitioning was maintained in N-stressed plants during the subsequent 3-day “chase” period when formation of insoluble reduced-¹⁵N in the root was quantitatively related to the disappearance of ¹⁵NO₃^? and soluble reduced-¹⁵N. The results indicate that increased assimilation of absorbed NO₃^?, in the root may contribute significantly to the altered reduced-N partitioning which occurs in N-stressed plants.     

Partitioning of inorganic nitrogen assimilation between the roots and shoots of cerrado and forest trees of contrasting plant communities of South East Brasil

Summary Woody plants growing in cerrado and forest communities of south-east Brasil were found to have low levels of nitrate reductase activity in their leaves suggesting that nitrate ions are not an important nitrogen source in these communities. Only in the leaves of species growing in areas of disturbance, such as gaps and forest margins, were high levels of nitrate reductase present. When pot-grown plants were supplied with nitrate, leaves and roots of almost all species responded by inducing increased levels of nitrate reductase. Pioneer or colonizing species exhibited highest levels of nitrate reductase and high shoot: root nitrate reductase activities. Glutamine synthetase, glutamate synthase and glutamate dehydrogenase were present in leaves and roots of the species examined.¹⁵N-labelled nitrate and ammonium were used to compare the assimilatory characteristics of two species:Enterolobium contortisiliquum, with a high capacity to reduce nitrate, andCalophyllum brasiliense, of low capacity. The rate of nitrate assimilation in the former was five times that of the latter. Both species had similar rates of ammonium assimilation. Results for eight species of contrasting habitats showed that leaf nitrogen content increased in parallel with xylem sap nitrogen concentrations, suggesting that the ability of the root system to acquire, assimilate or export nitrate determines shoot nitrogen status. These results emphasise the importance of nitrogen transport and metabolism in roots as determinants of whole plant nitrogen status.     

Reassessing the nitrogen relations of Arctic plants: a mini-review

The Arctic is often assumed to be an NH₄⁺-dominated ecosystem. This review assesses the validity of this assumption. It also addresses the question of whether Arctic plant growth is limited by the ability to use the forms of nitrogen that are available. The review demonstrates that several sources of soil nitrogen are available to Arctic plants, including soluble organic nitrogen (e.g. glycine, aspartic acid and glutamic acid), NH₄⁺ and NO^?₃. In mesic Arctic soils, soluble organic nitrogen is potentially more important than either NH⁺₄ or NO^?₃. Many Arctic species are capable of taking up soluble organic nitrogen (either directly and/or in association with ectomycorrhizae), with the greatest potential for soluble organic nitrogen uptake being exhibited by deciduous species. The ability to take up soluble organic nitrogen may enable some Arctic plants to avoid nitrogen limitations imposed by the slow rate of organic matter decomposition. NO^?₃ is also present in many Arctic soils, especially calcareous soils and soils near flowing water, animal burrows and bird cliffs. Arctic species characteristic of mesic and xeric habitats are capable of taking up and assimilating NO^?₃. Even when present in lower concentrations in soils than NH⁺₄, NO^?₃ is still an important source of nitrogen for some Arctic plants. Arctic-plants therefore have a variety of nitrogen sources available to them, and are capable of using those nitrogen sources. Taken together, these findings demonstrate that the Arctic is not an NH⁺₄dominated ecosystem. Symbiotic fixation of atmospheric N₂ does not appear to be an important source of nitrogen for Arctic plants. The reliance of Arctic plants on internal recycling of nitrogen substantially reduces their dependence on soil nitrogen uptake (this is particularly the case for slow-growing evergreens). Despite the high level of internal nitrogen recycling, Arctic plant growth remains limited by the low levels of available soil nitrogen. However, Arctic plant growth is not limited by an inability to utilize any of the available forms of nitrogen. The potential effects of climatic warming on nitrogen availability and use are discussed. The question of whether the Arctic ecosystem is uniquely different from temperate nitrogen-deficient ecosystems is also assessed.     

Light and dark assimilation of nitrate in plants

Abstract. Heterotrophic assimilation of nitrate in roots and leaves in darkness is closely linked with the oxidative pentose phosphate pathway. The supply of glucose-6-phosphate to roots and chloroplasts in leaves in darkness is essential for assimilation of nitrite into amino acids. When green leaves are exposed to light, the key enzyme, glucoses-phosphate dehydrogenase, is inhibited by reduction with thioredoxin. Hence the dark nitrate assimilatory pathway is inhibited under photoautotrophic conditions and replaced by regulatory reactions functioning in light. On account of direct photo-synthetic reduction of nitrite in chloroplasts and availability of excess NADH for nitrate reduclase, the rate of nitrate assimilation is extremely rapid in light. Under dark anaerobic conditions also nitrate is equally rapidly reduced to nitrite on account of abolition of competition for NADH between nitrate reductase and mitochondrial oxidation.     

施氮对不同品种冬小麦植株硝态氮和硝酸还原酶活性的影响

以黄土高原南部半湿润区土垫旱耕人为土为供试土壤进行盆栽试验,以NR 9405、9430、偃师9号、小偃6号、陕229号和西农2208冬小麦品种为供试材料,研究施氮对不同品种冬小麦植株硝态氮含量和硝酸还原酶活性(NRA)的影响.结果表明,施氮能明显增加叶片NRA.不施氮时除小偃6号和偃师9号外,其余品种NRA在全生育时期的动态变化均呈双峰曲线,2个高峰期分别在返青期和开花期,且开花期高峰值(36.17 NO2-μg.-g 1FW.h-1)明显比返青期峰值(15.407 NO2-μg.-g 1FW.h-1)大;施氮时不同品种叶片NRA在全生育期呈单峰曲线变化,最高峰在开花期,平均峰值为80.93 NO2-μg.-g 1FW.h-1),比同期不施氮处理增加1倍以上.施氮后地上部硝态氮含量在各时期均显著提高,在小麦生育前期(出苗到拔节)表现最为显著.氮肥对不同品种硝态氮含量的影响程度基本上与对NRA的影响程度相反,即施氮后硝态氮增加幅度小的品种,NRA却增加幅度大.