Manganese and iron porphyrins catalyze peroxynitrite decomposition and simultaneously increase nitration and oxidant yield: implications for their use as peroxynitrite scavengers in vivo.

Twelve substituted metalloporphyrins (MPs), some of which have been previously characterized with respect to superoxide dismutase and peroxynitrite decomposing activities, were evaluated for their ability to scavenge peroxynitrite in vitro at 37 degrees C. Because the overall effectiveness of MPs as catalytic peroxynitrite scavengers is a function of (1) how fast they react with peroxynitrite, (2) how fast they cycle back to the starting compound, and (3) how well they contain or quench the reactive intermediates generated, all of these properties were evaluated and compared directly under the same conditions. Of the various MPs tested, only the iron and manganese porphyrins showed significant reactivity with peroxynitrite. The Mn(IV) intermediates resulting from oxidation by peroxynitrite were relatively stable and rereduction to the Mn(III) forms was rate-limiting to catalytic decomposition of peroxynitrite. However, in the presence of oxidizeable substrates like phenolics, rereduction of Mn(IV) forms occurred very rapidly and both the Mn- and Fe-porphyrins catalyzed nitration and oxidation by peroxynitrite. Mn- and Fe-porphyrins enhanced the yield of nitrated phenolics by peroxynitrite as much as 5-fold at pH 7.4 and up to 12-fold at pH 9. 1, while total oxidative yield was more than doubled. Nitration enhancement by MPs was effectively inhibited by ascorbate, glutathione, or serum, although much higher concentrations of ascorbate were required to inhibit nitration catalyzed by either Mn or Fe tetramethylpyridyl porphyrin. Catalysis of peroxynitrite nitration by MPs appears to proceed via a radical-mediated reaction mechanism whereby the phenolic substrate rapidly reduces Mn(IV) = O or Fe[IV] = O to the +3 state to yield phenoxyl radical which then combines with the other primary product, nitrogen dioxide. Based on the rate constants and the proposed reaction mechanism, it is reasonable to suggest that Mn and Fe porphyrins could detoxify peroxynitrite in vivo by efficiently trapping the relatively unreactive peroxynitrite anion and, in effect, channeling it into a single reaction pathway which could then be more effectively scavenged by cellular reductants like ascorbate.     

Rapid and irreversible inactivation of protein tyrosine phosphatases PTP1B, CD45, and LAR by peroxynitrite.

Protein tyrosine phosphatases (PTPs) contain an essential thiol in the active site which may be susceptible to attack by nitric oxide-derived biological oxidants. We assessed the effects of peroxynitrite, nitric oxide, and S-nitrosoglutathione on the activity of three human tyrosine phosphatases in vitro. The receptor-like T-cell tyrosine phosphatase (CD45), the non-receptor-like tyrosine phosphatase PTP1B, and leukocyte-antigen-related (LAR) phosphatase were all irreversibly inactivated by peroxynitrite in less than 1 s with IC(50) values of 相似文献   

Mutation Rate and Dominance of Genes Affecting Viability in DROSOPHILA MELANOGASTER

Spontaneous mutations were allowed to accumulate in a second chromosome that was transmitted only through heterozygous males for 40 generations. At 10-generation intervals the chromosomes were assayed for homozygous effects of the accumulated mutants. From the regression of homozygous viability on the number of generations of mutant accumulation and from the increase in genetic variance between replicate chromosomes it is possible to estimate the mutation rate and average effect of the individual mutants. Lethal mutations arose at a rate of 0.0060 per chromosome per generation. The mutants having small effects on viability are estimated to arise with a frequency at least 10 times as high as lethals, more likely 20 times as high, and possibly many more times as high if there is a large class of very nearly neutral mutations.-The dominance of such mutants was measured for chromosomes extracted from a natural population. This was determined from the regression of heterozygous viability on that of the sum of the two constituent homozygotes. The average dominance for minor viability genes in an equilibrium population was estimated to be 0.21. This is lower than the value for new mutants, as expected since those with the greatest heterozygous effect are most quickly eliminated from the population. That these mutants have a disproportionately large heterozygous effect on total fitness (as well as on the viability component thereof) is shown by the low ratio of the genetic load in equilibrium homozygotes to that of new mutant homozygotes.     

Serum T(4) and serum T(3) concentrations in immature captive whitetip reef sharks, Triaenodon obesus.

Serum T(3) (3,5,3' triiodothyronine) and serum T(4) (thyroxine) concentrations were repetitively assayed by radioimmunoassay over a three-year period in two male and two female immature captive whitetip reef sharks, Triaenodon obesus. These sharks were maintained at the Waikiki Aquarium, Honolulu, Hawaii, in an open system holding pool receiving 568 liters per minute of water from a saltwater well with an iodide concentration of 0.076 mg/liter. No significant male-female difference was observed for either serum T(3) or serum T(4). No seasonal pattern of serum T(3) was detected (P = 0.07). Serum T(3) concentrations ranged (mean +/- SEM) from 0. 52 to 0.83 ng/mL (0.67 +/- 0.01; n = 64). A significant seasonal difference was observed for serum T(4) (P < 0.001). Serum T(4) concentration was higher in winter (October-January) with a mean (range +/- SEM) of 6.58 ng/mL (1.48-8.77 +/- 0.35; n = 24) and lower in summer (May-August) with a mean of 3.62 ng/mL (1.34-5.71 +/- 0. 22; n = 24). The thyroid hormone T(4) has a seasonal rhythm even in immature sharks and may have an important role in physiology. J. Exp. Zool. 284:500-504, 1999.     

Interactive biotic and abiotic regulators of soil carbon cycling: evidence from controlled climate experiments on peatland and boreal soils

Partially decomposed plant and animal remains have been accumulating in organic soils (i.e. >40% C content) for millennia, making them the largest terrestrial carbon store. There is growing concern that, in a warming world, soil biotic processing will accelerate and release greenhouse gases that further exacerbate climate change. However, the magnitude of this response remains uncertain as the constraints are abiotic, biotic and interactive. Here, we examined the influence of resource quality and biological activity on the temperature sensitivity of soil respiration under different soil moisture regimes. Organic soils were sampled from 13 boreal and peatland ecosystems located in the United Kingdom, Ireland, Spain, Finland and Sweden, representing a natural resource quality range of C, N and P. They were incubated at four temperatures (4, 10, 15 and 20 °C) at either 60% or 100% water holding capacity (WHC). Our results showed that chemical and biological properties play an important role in determining soil respiration responses to temperature and moisture changes. High soil C : P and C : N ratios were symptomatic of slow C turnover and long‐term C accumulation. In boreal soils, low bacterial to fungal ratios were related to greater temperature sensitivity of respiration, which was amplified in drier conditions. This contrasted with peatland soils which were dominated by bacterial communities and enchytraeid grazing, resulting in a more rapid C turnover under warmer and wetter conditions. The unexpected acceleration of C mineralization under high moisture contents was possibly linked to the primarily role of fermented organic matter, instead of oxygen, in mediating microbial decomposition. We conclude that to improve C model simulations of soil respiration, a better resolution of the interactions occurring between climate, resource quality and the decomposer community will be required.     

Chronic nitrogen additions suppress decomposition and sequester soil carbon in temperate forests

The terrestrial biosphere sequesters up to a third of annual anthropogenic carbon dioxide emissions, offsetting a substantial portion of greenhouse gas forcing of the climate system. Although a number of factors are responsible for this terrestrial carbon sink, atmospheric nitrogen deposition contributes by enhancing tree productivity and promoting carbon storage in tree biomass. Forest soils also represent an important, but understudied carbon sink. Here, we examine the contribution of trees versus soil to total ecosystem carbon storage in a temperate forest and investigate the mechanisms by which soils accumulate carbon in response to two decades of elevated nitrogen inputs. We find that nitrogen-induced soil carbon accumulation is of equal or greater magnitude to carbon stored in trees, with the degree of response being dependent on stand type (hardwood versus pine) and level of N addition. Nitrogen enrichment resulted in a shift in organic matter chemistry and the microbial community such that unfertilized soils had a higher relative abundance of fungi and lipid, phenolic, and N-bearing compounds; whereas, N-amended plots were associated with reduced fungal biomass and activity and higher rates of lignin accumulation. We conclude that soil carbon accumulation in response to N enrichment was largely due to a suppression of organic matter decomposition rather than enhanced carbon inputs to soil via litter fall and root production.     

Inhibition of a malaria host–pathogen interaction by a computationally designed inhibitor

Malaria is a substantial global health burden with 229 million cases in 2019 and 450,000 deaths annually. Plasmodium vivax is the most widespread malaria-causing parasite putting 2.5 billion people at risk of infection. P. vivax has a dormant liver stage and therefore can exist for long periods undetected. Its blood-stage can cause severe reactions and hospitalization. Few treatment and detection options are available for this pathogen. A unique characteristic of P. vivax is that it depends on the Duffy antigen/receptor for chemokines (DARC) on the surface of host red blood cells for invasion. P. vivax employs the Duffy binding protein (DBP) to bind to DARC. We first de novo designed a three helical bundle scaffolding database which was screened via protease digestions for stability. Protease-resistant scaffolds highlighted thresholds for stability, which we utilized for selecting DARC mimetics that we subsequentially designed through grafting and redesign of these scaffolds. The optimized design small helical protein disrupts the DBP:DARC interaction. The inhibitor blocks the receptor binding site on DBP and thus forms a strong foundation for a therapeutic that will inhibit reticulocyte infection and prevent the pathogenesis of P. vivax malaria.