985 resultados para nitrogen metabolism
Resumo:
Sediments off northwest Africa were assayed for activities of the respiratory electron transport system (ETS) and for primary amino nitrogen. ETS activities were used to compute respiratory oxygen consuption, carbon oxidation, and nitrate reduction rates. Activities were correlated with depth of the water column, and their longshore distribution resembled that of euphotic zone phytoplankton productivity. Protein concentrations were closely correlated with ETS activities. Carbon biomass was calculated from protein and compared with other computed values. The carbon oxidation rate accounted for 13 % of the region's primary production.
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With each cellular generation, oxygenic photoautotrophs must accumulate abundant protein complexes that mediate light capture, photosynthetic electron transport and carbon fixation. In addition to this net synthesis, oxygenic photoautotrophs must counter the light-dependent photoinactivation of Photosystem II (PSII), using metabolically expensive proteolysis, disassembly, resynthesis and re-assembly of protein subunits. We used growth rates, elemental analyses and protein quantitations to estimate the nitrogen (N) metabolism costs to both accumulate the photosynthetic system and to maintain PSII function in the diatom Thalassiosira pseudonana, growing at two pCO2 levels across a range of light levels. The photosynthetic system contains c. 15-25% of total cellular N. Under low growth light, N (re)cycling through PSII repair is only c. 1% of the cellular N assimilation rate. As growth light increases to inhibitory levels, N metabolite cycling through PSII repair increases to c. 14% of the cellular N assimilation rate. Cells growing under the assumed future 750 ppmv pCO2 show higher growth rates under optimal light, coinciding with a lowered N metabolic cost to maintain photosynthesis, but then suffer greater photoinhibition of growth under excess light, coincident with rising costs to maintain photosynthesis. We predict this quantitative trait response to light will vary across taxa.
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A complex study of influence of various environmental factors on rates of oxygen (M_O2 ), ammonium (M_NH4), and phosphate (M_PO4) metabolism in Ahnfeltia tobuchiensis has been carried out in situ in the Izmena Bay of the Kunashir Island. The following environmental factors have been included into the investigation: photosynthetically active radiation (PAR); ammonium (NH4); phosphate (PO4); and contents of carbon (C), nitrogen (N), phosphorus (P), and chlorophyll a (Chl) in tissue. Population of agar-containing seaweed A. tobuchiensis forms a layer with thickness up to 0.5 m, which occupies about 23.3 km**2; biomass is equal to 125000 tons. Quantitative assessment of organic matter production and nutrient consumption during oxygen metabolism has been carried out for the whole population. It has been shown that daily oxygen metabolism depends on PAR intensity, concentrations of PO4 and NH4 in seawater, and contents of N and P in tissues (r**2=0.78, p<0.001). Average daily NH4 consumption is 0.21 µmol/g of dry weight/hour and depends on NH4 and O2 concentrations in seawater and on ? and Chl a contents in algal tissues (r**2=0.64, p<0.001). Average daily PO4 consumption is 0.01 µmol/g of dry weight/hour and depends on NH4 concentrations in seawater and on P contents in algal tissues (r**2=0.40, p<0.001).
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The sediments penetrated on Leg 58 of the Deep Sea Drilling Project in the Philippine Sea represent long periods of geologic time during which depositional conditions apparently remained very constant. Organic carbon and nitrogen contents of the sediments decrease with increasing depth of burial, before leveling off at minimum values of about 0.05 to 0.10 per cent and 0.01 per cent, respectively. The depth at which the minimum values are reached varies from site to site, but ages of sediments corresponding to the minima are all about 5 m.y. We infer that slow bacterial diagenesis is responsible for the gradual depletion of organic carbon and nitrogen. It is likely that the rate of bacterial metabolism is controlled by the rate of diffusion of electron acceptors within the sediments. These results suggest that bacterial ecosystems in deep-water sediments play a much more important role in diagenesis than has previously been thought.
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Myora Springs is one of many groundwater discharge sites on North Stradbroke Island (Queensland, Australia). Here spring waters emerge from wetland forests to join Moreton Bay, mixing with seawater over seagrass meadows dominated by eelgrass, Zostera muelleri. We sought to determine how low pH / high CO2 conditions near the spring affect these plants and their interactions with the black rabbitfish (Siganus fuscescens), a co-occurring grazer. In paired-choice feeding trials S. fuscescens preferentially consumed Z. muelleri shoots collected nearest to Myora Springs. Proximity to the spring did not significantly alter the carbon and nitrogen contents of seagrass tissues but did result in the extraordinary loss of soluble phenolics, including Folin-reactive phenolics, condensed tannins, and phenolic acids by ?87%. Conversely, seagrass lignin contents were, in this and related experiments, unaffected or increased, suggesting a shift in secondary metabolism away from the production of soluble, but not insoluble, (poly)phenolics. We suggest that groundwater discharge sites such as Myora Springs, and other sites characterized by low pH, are likely to be popular feeding grounds for seagrass grazers seeking to reduce their exposure to soluble phenolics.
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Photosynthesis, biological nitrogen fixation, and carbon dioxide assimilation are three fundamental biological processes catalyzed by photosynthetic bacteria. In the present study, it is shown that mutant strains of the nonsulfur purple photosynthetic bacteria Rhodospirillum rubrum and Rhodobacter sphaeroides, containing a blockage in the primary CO2 assimilatory pathway, derepress the synthesis of components of the nitrogen fixation enzyme complex and abrogate normal control mechanisms. The absence of the Calvin–Benson–Bassham (CBB) reductive pentose phosphate CO2 fixation pathway removes an important route for the dissipation of excess reducing power. Thus, the mutant strains develop alternative means to remove these reducing equivalents, resulting in the synthesis of large amounts of nitrogenase even in the presence of ammonia. This response is under the control of a global two-component signal transduction system previously found to regulate photosystem biosynthesis and the transcription of genes required for CO2 fixation through the CBB pathway and alternative routes. In addition, this two-component system directly controls the ability of these bacteria to grow under nitrogen-fixing conditions. These results indicate that there is a molecular link between the CBB and nitrogen fixation process, allowing the cell to overcome powerful control mechanisms to remove excess reducing power generated by photosynthesis and carbon metabolism. Furthermore, these results suggest that the two-component system integrates the expression of genes required for the three processes of photosynthesis, nitrogen fixation, and carbon dioxide fixation.
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Gene homologs of GlnK PII regulators and AmtB-type ammonium transporters are often paired on prokaryotic genomes, suggesting these proteins share an ancient functional relationship. Here, we demonstrate for the first time in Archaea that GlnK associates with AmtB in membrane fractions after ammonium shock, thus, providing a further insight into GlnK-AmtB as an ancient nitrogen sensor pair. For this work, Haloferax mediterranei was advanced for study through the generation of a pyrE2-based counterselection system that was used for targeted gene deletion and expression of Flag-tagged proteins from their native promoters. AmtB1-Flag was detected in membrane fractions of cells grown on nitrate and was found to coimmunoprecipitate with GlnK after ammonium shock. Thus, in analogy to bacteria, the archaeal GlnK PII may block the AmtB1 ammonium transporter under nitrogen-rich conditions. In addition to this regulated protein–protein interaction, the archaeal amtB-glnK gene pairs were found to be highly regulated by nitrogen availability with transcript levels high under conditions of nitrogen limitation and low during nitrogen excess. While transcript levels of glnK-amtB are similarly regulated by nitrogen availability in bacteria, transcriptional regulators of the bacterial glnK promoter including activation by the two-component signal transduction proteins NtrC (GlnG, NRI) and NtrB (GlnL, NRII) and sigma factor σN (σ54) are not conserved in archaea suggesting a novel mechanism of transcriptional control.
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In plant cells, as in all other cells, proteins are submitted to permanent turnover, and the intracellular content of a given protein depends on its rate of both synthesis and degradation. The life time of most proteins is shorter than that of the cell. Thus, in young leaves of Lemna minor, the average half-life of protein was estimated to be 7 days, and it was shorter under stress conditions (Davies 1982). Such observations mean that nitrogen and amino acid fluxes are both cylic and permanent. Although protein turnover may appear wasteful, in terms of energy, numerous studies have shown that proteolysis provides multiple functions in cell physiology, and is an essential regulatory mechanism of cell metabolism and development.
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Warming and acidification of the oceans as a consequence of increasing CO2-concentrations occur at large scales. Numerous studies have shown the impact of single stressors on individual species. However, studies on the combined effect of multiple stressors on a multi-species assemblage, which is ecologically much more realistic and relevant, are still scarce. Therefore, we orthogonally crossed the two factors warming and acidification in mesocosm experiments and studied their single and combined impact on the brown alga Fucus vesiculosus associated with its natural community (epiphytes and mesograzers) in the Baltic Sea in all seasons (from April 2013 to April 2014). We superimposed our treatment factors onto the natural fluctuations of all environmental variables present in the Benthocosms in so-called delta-treatments. Thereby we compared the physiological responses of F. vesiculosus (growth and metabolites) to the single and combined effects of natural Kiel Fjord temperatures and pCO2 conditions with a 5 °C temperature increase and/or pCO2 increase treatment (1100 ppm in the headspace above the mesocosms). Responses were also related to the factor photoperiod which changes over the course of the year. Our results demonstrate complex seasonal pattern. Elevated pCO2 positively affected growth of F. vesiculosus alone and/or interactively with warming. The response direction (additive, synergistic or antagonistic), however, depended on season and daylength. The effects were most obvious when plants were actively growing during spring and early summer. Our study revealed for the first time that it is crucial to always consider the impact of variable environmental conditions throughout all seasons. In summary, our study indicates that in future F. vesiculosus will be more affected by detrimental summer heat-waves than by ocean acidification although the latter consequently enhances growth throughout the year. The mainly negative influence of rising temperatures on the physiology of this keystone macroalga may alter and/or hamper its ecological functions in the shallow coastal ecosystem of the Baltic Sea.
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The rms2 and rms4 pea ( Pisum sativum L.) branching mutants have higher and lower xylem-cytokinin concentration, respectively, relative to wild type (WT) plants. These genotypes were grown at two levels of nitrogen (N) supply for 18 - 20 d to determine whether or not xylem-cytokinin concentration (X-CK) or delivery altered the transpiration and leaf growth responses to N deprivation. Xylem sap was collected by pressurising de-topped root systems. As sap-flow rate increased, X-CK declined in WT and rms2, but did not change in rms4. When grown at 5.0 mM N, X-CKs of rms2 and rms4 were 36% higher and 6-fold lower, respectively, than WT at sap-flow rates equivalent to whole-plant transpiration. Photoperiod cytokinin (CK) delivery rates ( the product of transpiration and X-CK) decreased more than 6-fold in rms4. Growth of plants at 0.5 mM N had negligible (< 10%) effects on transpiration rates expressed on a leaf area basis in WT and rms4, but decreased transpiration rates of rms2. The low-N treatment decreased leaf expansion by 20 - 25% and expanding leaflet N concentration by 15%. These changes were similar in all genotypes. At sap-flow rates equivalent to whole-plant transpiration, the low N treatment decreased X-CK in rms2 but had no discernible effect in WT and rms4. Since the low N treatment decreased transpiration of all genotypes, photoperiod CK delivery rates also decreased in all genotypes. The similar leaf growth response of all genotypes to N deprivation despite differences in both absolute and relative X-CKs and deliveries suggests that shoot N status is more important in regulating leaf expansion than xylem-supplied cytokinins. The decreased X-CK and transpiration rate of rms2 following N deprivation suggests that changes in xylem-supplied CKs may modify water use.
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The effect of cancer cachexia on protein metabolism has been studied in mice transplanted with the MAC16 adenocarcinoma. The progressive cachexia induced by the MAC16 tumour was characterised by a reduction in carcass nitrogen between 16-30% weight loss and a reciprocal increase in tumour nitrogen content. Carcass nitrogen loss was accompanied by a concomitant decrease in gastrocnemius muscle weight and nitrogen content and also by a decrease in liver nitrogen content. The loss of gastrocnemius muscle throughout the progression of cachexia was attributable to a 60% decrease in the rate of protein synthesis and a 240% increase in the rate of protein degradation. The loss of skeletal muscle protein that may be partially mediated by an increased rate of protein degradation has been correlated with a circulatory catabolic factor present only in cachectic tumour-bearing animals, that degrades host muscle in vitro. The proteolysis-inducing factor was found to be heat stable, not a serine protease and was inhibited by indomethacin and eicosapentaenoic acid (EPA) in a dose-related manner. The proteolytic factor induced prostaglandin E2 formation in the gastrocnemius muscle of non tumour-bearing animals and this effect was inhibited by indomethacin and EPA. In vivo studies show EPA (2.0g/kg-1 by gavage) to effectively reverse the decrease in body weight in animals bearing the MAC16 tumour with a concomitant reduction in tumour growth. Muscle from animals treated with EPA showed a decrease (60%) in protein degradation without an effect on protein synthesis. In vivo studies show branched chain amino acid treatment to be ineffective in moderating the cachectic effect of the MAC16 tumour. The action of the factor was largely mimicked by triarachidonin and trilinoleia. The increased serum levels of arachidonic acid in cachectic tumour-bearing animals may thus be responsible for increased protein degradation through prostanoid metabolism. The understanding of protein metabolism and catabolic factors in the cachectic animal may provide future avenues for the reversal of cachexia and the treatment of cancer.metabolism and catabolicmetabolism and cat
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Adaptive mechanisms involving upregulation of cytoprotective genes under the control of transcription factors such as Nrf2 exist to protect cells from permanent damage and dysfunction under stress conditions. Here we explore of the hypothesis that Nrf2 activation by reactive oxygen and nitrogen species modulates cytotoxicity during hypoxia (H) with and without reoxygenation (H/R) in H9C2 cardiomyoblasts. Using MnTBap as a cell permeable superoxide dismutase (SOD) mimetic and peroxynitrite scavenger and L-NAME as an inhibitor of nitric oxide synthase (NOS), we have shown that MnTBap inhibited the cytotoxic effects of hypoxic stress with and without reoxygenation. However, L-NAME only afforded protection during H. Under reoxygenation, conditions, cytotoxicity was increased by the presence of L-NAME. Nrf2 activation was inhibited independently by MnTBap and L-NAME under H and H/R. The increased cytotoxicity and inhibition of Nrf2 activation by the presence of L-NAME during reoxygenation suggests that NOS activity plays an important role in cell survival at least in part via Nrf2-independent pathways. In contrast, O2 -• scavenging by MnTBap prevented both toxicity and Nrf2 activation during H and H/R implying that toxicity is largely dependent on O2 -.To confirm the importance of Nrf2 for myoblast metabolism, Nrf2 knockdown with siRNA reduced cell survival by 50% during 4h hypoxia with and without 2h of reoxygenation and although cellular glutathione (GSH) was depleted during H and H/R, GSH loss was not exacerbated by Nrf2 knockdown. These data support distinctive roles for ROS and RNS during H and H/R for Nrf2 induction which are important for survival independently of GSH salvage. © 2013 The Authors.
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Compared to phosphorus (P), nitrogen (N) has received little attention across the Everglades landscape. Despite this lack of attention, N plays important roles in many Everglades systems, including being a significant pollutant in Florida Bay and the Gulf of Mexico, the limiting nutrient in highly P-impacted areas, and an important substrate for microbial metabolism. Storage and transport of N throughout the Everglades is dominated by organic forms, including peat soils and dissolved organic N in the water column. In general, N sources are highest in the northern areas; however, atmospheric deposition and active N2 fixation by the periphyton components are a significant N source throughout most systems. Many of the processes involved in the wetland N cycle remain unmeasured for most of the Everglades systems. In particular, the lack of in situ rates for N2 fixation and denitrification prevent the construction of system-level budgets, especially for the Southern mangrove systems where N export into Florida Bay is critical. There is also the potential for several novel N processes (e.g., Anammox) with an as yet undetermined importance for nitrogen cycling and function of the Everglades ecosystem. Phosphorus loading alters the N cycle by stimulating organic N mineralization with resulting flux of ammonium and DON, and at elevated P concentrations, by increasing rates of N2 fixation and N assimilation. Restoration of hydrology has a potential for significantly impacting N cycling in the Everglades both in terms of affecting N transport, but also by altering aerobic-anaerobic transitions at the soil-water interface or in areas with seasonal drawdowns (e.g., marl prairies). Based on the authors’ understanding of N processes, much more research is necessary to adequately predict potential impacts from hydrologic restoration, as well as the function of Everglades systems as sinks, sources, and transformers of N in the South Florida landscape.
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Les dinoflagellés sont des eucaryotes unicellulaires retrouvés dans la plupart des écosystèmes aquatiques du globe. Ces organismes amènent une contribution substantielle à la production primaire des océans, soit en tant que membre du phytoplancton, soit en tant que symbiontes des anthozoaires formant les récifs coralliens. Malheureusement, ce rôle écologique majeur est souvent négligé face à la capacité de certaines espèces de dinoflagellés à former des fleurs d'eau, parfois d'étendue et de durée spectaculaires. Ces floraisons d'algues, communément appelées "marées rouges", peuvent avoir de graves conséquences sur les écosystèmes côtiers, sur les industries de la pêche et du tourisme, ainsi que sur la santé humaine. Un des facteurs souvent corrélé avec la formation des fleurs d'eau est une augmentation dans la concentration de nutriments, notamment l’azote et le phosphore. Le nitrate est un des composants principaux retrouvés dans les eaux de ruissellement agricoles, mais également la forme d'azote bioaccessible la plus abondante dans les écosystèmes marins. Ainsi, l'agriculture humaine a contribué à magnifier significativement les problèmes associés aux marées rouges au niveau mondial. Cependant, la pollution ne peut pas expliquer à elle seule la formation et la persistance des fleurs d'eau, qui impliquent plusieurs facteurs biotiques et abiotiques. Il est particulièrement difficile d'évaluer l'importance relative qu'ont les ajouts de nitrate par rapport à ces autres facteurs, parce que le métabolisme du nitrate chez les dinoflagellés est largement méconnu. Le but principal de cette thèse vise à remédier à cette lacune. J'ai choisi Lingulodinium polyedrum comme modèle pour l'étude du métabolisme du nitrate, parce que ce dinoflagellé est facilement cultivable en laboratoire et qu'une étude transcriptomique a récemment fourni une liste de gènes pratiquement complète pour cette espèce. Il est également intéressant que certaines composantes moléculaires de la voie du nitrate chez cet organisme soient sous contrôle circadien. Ainsi, dans ce projet, j'ai utilisé des analyses physiologiques, biochimiques, transcriptomiques et bioinformatiques pour enrichir nos connaissances sur le métabolisme du nitrate des dinoflagellés et nous permettre de mieux apprécier le rôle de l'horloge circadienne dans la régulation de cette importante voie métabolique primaire. Je me suis tout d'abord penché sur les cas particuliers où des floraisons de dinoflagellés sont observées dans des conditions de carence en azote. Cette idée peut sembler contreintuitive, parce que l'ajout de nitrate plutôt que son épuisement dans le milieu est généralement associé aux floraisons d'algues. Cependant, j’ai découvert que lorsque du nitrate était ajouté à des cultures initialement carencées ou enrichies en azote, celles qui s'étaient acclimatées au stress d'azote arrivaient à survivre près de deux mois à haute densité cellulaire, alors que les cellules qui n'étaient pas acclimatées mourraient après deux semaines. En condition de carence d'azote sévère, les cellules arrivaient à survivre un peu plus de deux semaines et ce, en arrêtant leur cycle cellulaire et en diminuant leur activité photosynthétique. L’incapacité pour ces cellules carencées à synthétiser de nouveaux acides aminés dans un contexte où la photosynthèse était toujours active a mené à l’accumulation de carbone réduit sous forme de granules d’amidon et corps lipidiques. Curieusement, ces deux réserves de carbone se trouvaient à des pôles opposés de la cellule, suggérant un rôle fonctionnel à cette polarisation. La deuxième contribution de ma thèse fut d’identifier et de caractériser les premiers transporteurs de nitrate chez les dinoflagellés. J'ai découvert que Lingulodinium ne possédait que très peu de transporteurs comparativement à ce qui est observé chez les plantes et j'ai suggéré que seuls les membres de la famille des transporteurs de nitrate de haute affinité 2 (NRT2) étaient réellement impliqués dans le transport du nitrate. Le principal transporteur chez Lingulodinium était exprimé constitutivement, suggérant que l’acquisition du nitrate chez ce dinoflagellé se fondait majoritairement sur un système constitutif plutôt qu’inductible. Enfin, j'ai démontré que l'acquisition du nitrate chez Lingulodinium était régulée par la lumière et non par l'horloge circadienne, tel qu'il avait été proposé dans une étude antérieure. Finalement, j’ai utilisé une approche RNA-seq pour vérifier si certains transcrits de composantes impliquées dans le métabolisme du nitrate de Lingulodinium étaient sous contrôle circadien. Non seulement ai-je découvert qu’il n’y avait aucune variation journalière dans les niveaux des transcrits impliqués dans le métabolisme du nitrate, j’ai aussi constaté qu’il n’y avait aucune variation journalière pour n’importe quel ARN du transcriptome de Lingulodinium. Cette découverte a démontré que l’horloge de ce dinoflagellé n'avait pas besoin de transcription rythmique pour générer des rythmes physiologiques comme observé chez les autres eukaryotes.