nitrogenase inhibition
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2019 ◽  
Vol 24 (11) ◽  
pp. 1022-1031 ◽  
Author(s):  
John F. Allen ◽  
Brenda Thake ◽  
William F. Martin

2019 ◽  
Vol 20 (20) ◽  
pp. 5099 ◽  
Author(s):  
David Soba ◽  
Bangwei Zhou ◽  
Cesar Arrese-Igor ◽  
Sergi Munné-Bosch ◽  
Iker Aranjuelo

Alfalfa (Medicago sativa L.) is frequently constrained by environmental conditions such as drought. Within this context, it is crucial to identify the physiological and metabolic traits conferring a better performance under stressful conditions. In the current study, two alfalfa cultivars (San Isidro and Zhong Mu) with different physiological strategies were selected and subjected to water limitation conditions. Together with the physiological analyses, we proceeded to characterize the isotopic, hormone, and metabolic profiles of the different plants. According to physiological and isotopic data, Zhong Mu has a water-saver strategy, reducing water lost by closing its stomata but fixing less carbon by photosynthesis, and therefore limiting its growth under water-stressed conditions. In contrast, San Isidro has enhanced root growth to replace the water lost through transpiration due to its more open stomata, thus maintaining its biomass. Zhong Mu nodules were less able to maintain nodule N2 fixing activity (matching plant nitrogen (N) demand). Our data suggest that this cultivar-specific performance is linked to Asn accumulation and its consequent N-feedback nitrogenase inhibition. Additionally, we observed a hormonal reorchestration in both cultivars under drought. Therefore, our results showed an intra-specific response to drought at physiological and metabolic levels in the two alfalfa cultivars studied.


2018 ◽  
Author(s):  
John F. Allen ◽  
Brenda Thake ◽  
William F. Martin

Cyanobacteria produced the atmospheric O2that began accumulating 2.4 billion years ago1, leading to Earth’s Great Oxidation Event (GOE)2. For nearly 2 billion years following the GOE, O2production was restricted and atmospheric oxygen remained low2–5. Oxygen rose again sharply with the advent of land plants roughly 450 million years ago, which increased atmospheric O2through carbon burial4–5. Why did the O2content of the atmosphere remain constant and low for more than a billion years despite the existence of O2-producing cyanobacteria? While geological limitations have been explored2–7, the limiting factor may have been biological, and enzymatic. Here we propose that O2was kept low by oxygen inhibition of nitrogenase activity. Nitrogenase is the sole N2-fixing enzyme on Earth, and is inactive in air containing 2% or more O2by volume8. No O2-resistant nitrogenase enzyme is known9–12. We further propose that nitrogenase inhibition by O2kept atmospheric O2low until upright terrestrial plants physically separated O2production in aerial photosynthetic tissues from N2fixation in soil, liberating nitrogenase from inhibition by atmospheric O2.


2010 ◽  
Vol 192 (10) ◽  
pp. 835-841 ◽  
Author(s):  
Sylvia M. C. Alquéres ◽  
Jose Henrique M. Oliveira ◽  
Eduardo M. Nogueira ◽  
Helma V. Guedes ◽  
Pedro L. Oliveira ◽  
...  

2008 ◽  
Vol 54 (3) ◽  
pp. 235-239 ◽  
Author(s):  
Claudio L. Gusso ◽  
Emanuel M. de Souza ◽  
Liu Un Rigo ◽  
Fábio de Oliveira Pedrosa ◽  
M.G. Yates ◽  
...  

Herbaspirillum seropedicae is a nitrogen-fixing bacterium that grows well with ammonium chloride or sodium nitrate as alternative single nitrogen sources but that grows more slowly with l-alanine, l-serine, l-proline, or urea. The ntrC mutant strain DCP286A was able to utilize only ammonium or urea of these nitrogen sources. The addition of 1 mmol·L–1ammonium chloride to the nitrogen-fixing wild-type strain inhibited nitrogenase activity rapidly and completely. Urea was a less effective inhibitor; approximately 20% of nitrogenase activity remained 40 min after the addition of 1 mmol·L–1urea. The effect of the ntrC mutation on nitrogenase inhibition (switch-off) was studied in strain DCP286A containing the constitutively expressed gene nifA of H. seropedicae. In this strain, nitrogenase inhibition by ammonium was completely abolished, but the addition of urea produced a reduction in nitrogenase activity similar to that of the wild-type strain. The results suggest that the NtrC protein is required for assimilation of nitrate and the tested amino acids by H. seropedicae. Furthermore, NtrC is also necessary for ammonium-induced switch-off of nitrogenase but is not involved in the mechanism of nitrogenase switch-off by urea.


2006 ◽  
Vol 280 (1-2) ◽  
pp. 135-142 ◽  
Author(s):  
Luis Bolaños ◽  
Marta Martín ◽  
Abdelaziz El-Hamdaoui ◽  
Rafael Rivilla ◽  
Ildefonso Bonilla

1990 ◽  
Vol 92 (4) ◽  
pp. 1101-1107 ◽  
Author(s):  
David B. Layzell ◽  
Stephen Hunt ◽  
Gerald R. Palmer

1987 ◽  
Vol 247 (3) ◽  
pp. 547-554 ◽  
Author(s):  
G A Ashby ◽  
M J Dilworth ◽  
R N F Thorneley

Ethylene (C2H4) inhibited H2 evolution by the Mo-containing nitrogenase of Klebsiella pneumoniae. The extent of inhibition depended on the electron flux determined by the ratio of Fe protein (Kp2) to MoFe protein (Kp1) with KiC2H4 = 409 kPa ([Kp2]/[Kp1] = 22:1) and KC2H4i = 88 kPa ([Kp1]/[Kp2] = 21:1) at 23 degrees C at pH 7.4. At [Kp2]/[Kp1] = 1:1, inhibition was minimal with C2H4 (101 kPa). Extrapolation of data obtained when C2H4 was varied from 60 to 290 kPa indicates that at infinite pressure of C2H4 total inhibition of H2 evolution should occur. C2H4 inhibited concomitant S2O4(2-) oxidation to the same extent that it inhibited H2 evolution. Although other inhibitors of total electron flux such as CN- and CH3NC uncouple MgATP hydrolysis from electron transfer, C2H4 did not affect the ATP/2e ratio. Inhibition of H2 evolution by C2H4 was not relieved by CO. C2H4 was reduced to C2H6 at [Kp2]/[Kp1] ratios greater than or equal to 5:1 in a reaction that accounted for no more than 1% of the total electron flux. These data are discussed in terms of the chemistry of alkyne and alkene reduction on transition-metal centres.


1987 ◽  
Vol 42 (7-8) ◽  
pp. 902-906 ◽  
Author(s):  
Sabine Reich ◽  
Helmar Almon ◽  
Peter Böger

Cyanobacterium . Anabaena variabilis, Nitrogenase Regulation, Ammonia, Methylamine Using the heterocystous cyanobacterium A nabaena variabilis (ATCC 29413) in an alkaline environment its nitrogenase activity is rapidly inhibited by ammonia and methylamine. Nitro­genase inhibition by ammonia is probably caused by a mechanism comparable to the switch-off effect, which has been described for several species of the Rhodospirillaceae, whereas methyl-amine-induced inhibition is caused by an uncoupling effect only. Evidence for these different effects is obtained by comparing nitrogenase activity in cell-free extracts of filaments pretreated by ammonia or methylamine. In addition, ammonia-dependent nitrogenase inhibition is shown to be dependent on protein synthesis and on light intensity.


1977 ◽  
Vol 23 (11) ◽  
pp. 1548-1553 ◽  
Author(s):  
Alfred G. Buchanan

Nitrogenase in Azotobacter chroococcum whole cells was inhibited by enzymically generated superoxide anion (O2−), hydrogen peroxide, and ethyl hydrogen peroxide. The degree of inhibition produced by O2− was related to the quantity of oxygen supplied to the organisms in continuous cultures. O2− also inhibited oxygen uptake by whole cells. These O2−-mediated inhibitions were prevented by bovine superoxide dismutase. The quantities of superoxide dismutase (SOD), and catalase associated with cells grown under varying oxygen concentrations were determined. The role of hydrogen peroxide, and of the hydroxyl radical (∙OH) in nitrogenase inhibition was examined. The response of Azotobacter chroococcum to oxygen was evaluated with respect to the observed effects of O2− on the organism, and some explanation is given to account for nitrogenase sensitivity to oxygen.


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