The protein amide <Superscript>1</Superscript>H<Superscript>N</Superscript> chemical shift temperature coefficient reflects thermal expansion of the N–H···O=C hydrogen bond

The protein amide ¹H^N chemical shift temperature coefficient can be determined with high accuracy by recording spectra at different temperatures, but the physical mechanism responsible for this temperature dependence is not well understood. In this work, we find that this coefficient strongly correlates with the temperature coefficient of the through-hydrogen-bond coupling, ^3hJ_NC′, based on NMR measurements of protein GB3. Parallel tempering molecular dynamics simulation suggests that the hydrogen bond distance variation at different temperatures/replicas is largely responsible for the ¹H^N chemical shift temperature dependence, from which an empirical equation is proposed to predict the hydrogen bond thermal expansion coefficient, revealing responses of individual hydrogen bonds to temperature changes. Different expansion patterns have been observed for various networks formed by β strands.     

Theoretical study of noncovalent interactions in XCN···YO<Subscript>2</Subscript>H (X = F,Cl, Br,I; Y = P,As, Sb) complexes

Noncovalent interactions in XCN···YO₂H (X = F, Cl, Br, I; Y = P, As, Sb) complexes were investigated using ab initio calculations at the MP2/aug-cc-pVDZ level of theory. There are four different configurations of these complexes, and the complexes are formed via hydrogen bonds, halogen bonds, π-hole interactions, or dual interactions. An examination of binding distances and interaction energies suggested that π-hole bonds are more stable than the other interactions. Molecular electrostatic potentials, electron densities, second-order stabilization energies, and electron density differences were computed to study the character of these interactions.     

Synthesis,characterization, and studies on DNA binding of the complex Fe(Sal<Subscript>2</Subscript>dienNO<Subscript>3</Subscript>·H<Subscript>2</Subscript>O)

A new metal complex, Fe(Sal₂dienNO₃·H₂O) (where Sal is salicylaldehyde and dien is diethylenetriamine), has been synthesized and characterized. The interactions between the Fe(III) complex and calf thymus DNA has been investigated using UV and fluorescence spectra, viscosity, thermal denaturation, and molecular modeling. The cleavage reaction on plasmid DNA has been monitored by agarose gel electrophoresis. The experimental results show that the mode of binding of the complex to DNA is classical intercalation and the complex can cleave pBR322 DNA.     

Spectroscopic Behavior and Biological Activity of K<Subscript>2</Subscript>[VO(O<Subscript>2</Subscript>)NTA]·2H<Subscript>2</Subscript>O

The dihydrated potassium salt of the complex anion [VO(O₂)NTA]²⁻ (NTA = nitrilotriacetate anion, [N(CH₂-COO)₃]³⁻) was thoroughly characterized by electronic and vibrational (infrared and Raman) spectroscopies. The bioactivity of the complex on the cell proliferation was tested on three cell lines in culture (UMR106 rat osteosarcoma-derived cells, Caco-2 derived from a human colon adenocarcinoma, and RAW 264.7, a macrophage murine cell line).     

On the generation of OH<Superscript>·</Superscript> radical species from H<Subscript>2</Subscript>O<Subscript>2</Subscript> by Cu(I) amyloid beta peptide model complexes: a DFT investigation

According to different studies, the interaction between amyloid β-peptide (Aβ) and copper ions could yield radical oxygen species production, in particular the highly toxic hydroxyl radical OH^· that is suspected to contribute to Alzheimer’s disease pathogenesis. Despite intensive experimental and computational studies, the nature of the interaction between copper and Aβ peptide, as well as the redox reactivity of the system, are still matter of debate. It was proposed that in Cu(II) → Cu(I) reduction the complex Cu(II)–Aβ could follow a multi-step conformational change with redox active intermediates that may be responsible for OH^· radical production from H₂O₂ through a Fenton-like process. The purpose of this work is to evaluate, using ab initio Density Functional Theory computations, the reactivity of different Cu(I)–Aβ coordination modes proposed in the literature, in terms of OH^· production. For each coordination model, we considered the corresponding H₂O₂ adduct and performed a potential energy surface scan along the reaction coordinate of O–O bond dissociation of the peroxide, resulting in the production of OH^· radical, obtaining reaction profiles for the evaluation of the energetic of the process. This procedure allowed us to confirm the hypothesis according to which the most populated Cu(I)–Aβ two-histidine coordination is not able to perform efficiently H₂O₂ reduction, while a less populated three-coordinated form would be responsible for the OH^· production. We show that coordination modes featuring a third nitrogen containing electron-donor ligand (an imidazole ring of an histidine residue is slightly favored over the N-terminal amine group) are more active towards H₂O₂ reduction.     

Competition and interplay between the lithium bonding and hydrogen bonding: R3C···HY···LiY and R3C···LiY···HY triads as a working model (R=H, CH3; Y=CN, NC)

UMP2 calculations with aug-cc-pVDZ basis set were used to analyze intermolecular interactions in R₃C···HY···LiY and R₃C···LiY···HY triads (R=H, CH₃; Y=CN, NC), which are connected via lithium and hydrogen bonds. To better understand the properties of these systems, the corresponding dyads were also studied. Molecular geometries and binding energies of dyads, and triads were investigated at the UMP2/aug-cc-pVDZ computational level. Particular attention was paid to parameters such as cooperative energies, and many-body interaction energies. All studied complexes, with the simultaneous presence of a lithium bond and a hydrogen bond, showed cooperativity with energy values ranging between ?1.71 and ?9.03 kJ mol^?1. The electronic properties of the complexes were analyzed using parameters derived from atoms in molecules (AIM) methodology. Energy decomposition analysis revealed that the electrostatic interactions are the major source of the attraction in the title complexes.     

Interplay between halogen bonds and hydrogen bonds in OH/SH···HOX···HY (X = Cl, Br; Y = F, Cl, Br) complexes

The character of the cooperativity between the HOX···OH/SH halogen bond (XB) and the Y―H···(H)OX hydrogen bond (HB) in OH/SH···HOX···HY (X = Cl, Br; Y = F, Cl, Br) complexes has been investigated by means of second-order Møller?Plesset perturbation theory (MP2) calculations and “quantum theory of atoms in molecules” (QTAIM) studies. The geometries of the complexes have been determined from the most negative electrostatic potentials (V _S,min) and the most positive electrostatic potentials (V _S,max) on the electron density contours of the individual species. The greater the V _S,max values of HY, the larger the interaction energies of halogen-bonded HOX···OH/SH in the termolecular complexes, indicating that the ability of cooperative effect of hydrogen bond on halogen bond are determined by V _S,max of HY. The interaction energies, binding distances, infrared vibrational frequencies, and electron densities ρ at the BCPs of the hydrogen bonds and halogen bonds prove that there is positive cooperativity between these bonds. The potentiation of hydrogen bonds on halogen bonds is greater than that of halogen bonds on hydrogen bonds. QTAIM studies have shown that the halogen bonds and hydrogen bonds are closed-shell noncovalent interactions, and both have greater electrostatic character in the termolecular species compared with the bimolecular species.

Australopithecus afarensis : bipédie stricte ou associée à une composante arboricole ? Critiques et révision du matériel fémoral

Although much research has been carried out on Australopithecus afarensis locomotion, no consensus has yet been reached. Our new critic study on femoral material brings to the fore a strictly bipedal behaviour within this taxon. Our results are based on the pertinence of human anatomical characteristics among A. afarensis and on the absence of characteristics revealing arboreal displacement. These results have emerged from our different observation and interpretation of some preceding authors concerning the anatomy of these fossil hominids. It is important to underline that apomorphic characteristics of this species are difficult to interpret. They must not however be used to support the idea of arboreal displacement simply based on the fact of a no totally human morphe. We believe that present day humans do not necessarily reflect the earliest strict bipedal anatomic model. An the other hand, it appears that the disagreement between the two locomotor hypothesis for A. afarensis that are bipedalism and arboreal displacement, facing the possibility of bipedalism associated with negligible arboreal displacement, results more from an evolutionary fact than from a real scientific conflict.     

&#183;遗传咨询&#183;

1．多囊肾的遗传 问：我有家族多囊肾遗传史,自己双肾有囊肿,现在怀孕29周,胎儿彩超双肾大,有回声,医生判定为多囊肾,我如果不要这胎,再怀孕,有不遗传的可能吗？     

Mg<Superscript>2+ </Superscript> modulation of EMCV IRES key activity fragment equilibria and r(G·C) base-pair kinetics

NMR magnetization transfer from water and ammonia-catalyzed exchange of the imino proton have been used to probe enhanced thermostability and conformational rearrangements induced by Mg^2 + in two key activity fragments r(CACCUGGCGACAGGUG) and r(GGCCAAAAGCC) of the encephalomyocarditis virus (EMCV) picornavirus internal ribosome entry site (IRES). We have measured some of their r(G·C) base-pair lifetimes and dissociation constants under different MgCl₂ conditions, and we compare them with those of other short RNA duplexes. The RNA fragment r(CACCUGGCGACAGGUG) adopts two topologies, a palindromic duplex with two conformations and a hairpin, whose equilibrium can be monitored: the duplex form is destabilized by Mg^2 + and temperature, a delicate balance wherein the entropic contribution of the free energy helps populate the hairpin state. For both fragments, the opening rates of the r(G·C) pairs are lower in the presence of Mg^2 + and their dissociation constants are smaller or comparable. Analysis of the results suggests that Mg^2 + has a preferential and specific effect on the r(CACCUGGCGACAGGUG) hairpin in the region close to the r(G·C) closing pair of the GCGA tetraloop, and the ion moves diffusively around r(GGCCAAAAGCC), thereby differentiating the GNRA and RAAA hairpin motifs that are both involved in the biological regulation functions of the EMCV IRES.     

Chronic Atmospheric NO<Stack><Subscript>3</Subscript><Superscript>−</Superscript></Stack> Deposition Does Not Induce NO<Stack><Subscript>3</Subscript><Superscript>−</Superscript></Stack> Use by <Emphasis Type="Italic">Acer saccharum</Emphasis> Marsh.

The ability of an ecosystem to retain anthropogenic nitrogen (N) deposition is dependent upon plant and soil sinks for N, the strengths of which may be altered by chronic atmospheric N deposition. Sugar maple (Acer saccharum Marsh.), the dominant overstory tree in northern hardwood forests of the Lake States region, has a limited capacity to take up and assimilate NO₃⁻. However, it is uncertain whether long-term exposure to NO₃⁻ deposition might induce NO₃⁻ uptake by this ecologically important overstory tree. Here, we investigate whether 10 years of experimental NO₃⁻ deposition (30 kg N ha⁻¹ y⁻¹) could induce NO₃⁻ uptake and assimilation in overstory sugar maple (approximately 90 years old), which would enable this species to function as a direct sink for atmospheric NO₃⁻ deposition. Kinetic parameters for NH₄⁺ and NO₃⁻ uptake in fine roots, as well as leaf and root NO₃⁻ reductase activity, were measured under conditions of ambient and experimental NO₃⁻ deposition in four sugar maple-dominated stands spanning the geographic distribution of northern hardwood forests in the Upper Lake States. Chronic NO₃⁻ deposition did not alter the V _max or K _m for NO₃⁻ and NH₄⁺ uptake nor did it influence NO₃⁻ reductase activity in leaves and fine roots. Moreover, the mean V _max for NH₄⁺ uptake (5.15 μmol ¹⁵N g⁻¹ h⁻¹) was eight times greater than the V _max for NO₃⁻ uptake (0.63 μmol ¹⁵N g⁻¹ h⁻¹), indicating a much greater physiological capacity for NH₄⁺ uptake in this species. Additionally, NO₃⁻ reductase activity was lower than most values for woody plants previously reported in the literature, further indicating a low physiological potential for NO₃⁻ assimilation in sugar maple. Our results demonstrate that chronic NO₃⁻ deposition has not induced the physiological capacity for NO₃⁻ uptake and assimilation by sugar maple, making this dominant species an unlikely direct sink for anthropogenic NO₃⁻ deposition.     

Negative molecular ion of deuterium D<Stack><Subscript>2</Subscript><Superscript>−</Superscript></Stack>

D₂⁻ ions produced in collisions of D⁻ ions with relative energies of 2.5–9.2 eV were detected for the first time. It is shown that the effective cross section for this reaction is no less than 1.5 × 10⁻¹⁴ cm². Along with the theoretically predicted short-lived state of negative molecular deuterium ions, a state existing for more than 1 μs was observed.     

Flow of Deposited Inorganic N in Two Gleysol-dominated Mountain Catchments Traced with <Superscript>15</Superscript>NO<Subscript>3</Subscript><Superscript>−</Superscript> and <Superscript>15</Superscript>NH<Subscript>4</Subscript><Superscript>+</Superscript>

In two mountain ecosystems at the Alptal research site in central Switzerland, pulses of ¹⁵NO₃ and ¹⁵NH₄ were separately applied to trace deposited inorganic N. One forested and one litter meadow catchment, each approximately 1600 m², were delimited by trenches in the Gleysols. K¹⁵NO₃ was applied weekly or fortnightly over one year with a backpack sprayer, thus labelling the atmospheric nitrate deposition. After the sampling and a one-year break, ¹⁵NH₄Cl was applied as a second one-year pulse, followed by a second sampling campaign. Trees (needles, branches and bole wood), ground vegetation, litter layer and soil (LF, A and B horizon) were sampled at the end of each labelling period. Extractable inorganic N, microbial N, and immobilised soil N were analysed in the LF and A horizons. During the whole labelling period, the runoff water was sampled as well. Most of the added tracer remained in both ecosystems. More NO₃⁻ than NH₄⁺ tracer was retained, especially in the forest. The highest recovery was in the soil, mainly in the organic horizon, and in the ground vegetation, especially in the mosses. Event-based runoff analyses showed an immediate response of ¹⁵NO₃⁻ in runoff, with sharp ¹⁵N peaks corresponding to discharge peaks. NO₃⁻ leaching showed a clear seasonal pattern, being highest in spring during snowmelt. The high capacity of N retention in these ecosystems leads to the assumption that deposited N accumulates in the soil organic matter, causing a progressive decline of its C:N ratio.     

Estimation of denitrification potential in a karst aquifer using the <Superscript>15</Superscript>N and <Superscript>18</Superscript>O isotopes of NO<Stack><Subscript>3</Subscript><Superscript>−</Superscript></Stack>

A confined aquifer in the Malm Karst of the Franconian Alb, South Germany was investigated in order to understand the role of the vadose zone in denitrifiaction processes. The concentrations of chemical tracers Sr²⁺ and Cl^– and concentrations of stable isotope ¹⁸O were measured in spring water and precipitation during storm events. Based on these measurements a conceptual model for runoff was constructed. The results indicate that pre-event water, already stored in the system at the beginning of the event, flows downslope on vertical and lateral preferential flow paths. Chemical tracers used in a mixing model for hydrograph separation have shown that the pre-event water contribution is up to 30%. Applying this information to a conceptual runoff generation model, the values of ¹⁵N and ¹⁸O in nitrate could be calculated. Field observations showed the occurence of significant microbial denitrification processes above the soil/bedrock interface before nitrate percolates through to the deeper horizon of the vadose zone. The source of nitrate could be determined and denitrification processes were calculated. Assuming that the nitrate reduction follows a Rayleigh process one could approximate a nitrate input concentration of about 170 mg/l and a residual nitrate concentration of only about 15%. The results of the chemical and isotopic tracers postulate fertilizers as nitrate source with some influence of atmospheric nitrate. The combined application of hydrograph separation and determination of isotope values in ¹⁵N and ¹⁸O of nitrate lead to an improved understanding of microbial processes (nitrification, denitrification) in dynamic systems.     

Delimiting a rice wide-compatibility gene <Emphasis Type="Italic">S</Emphasis><Stack><Subscript>5</Subscript><Superscript><Emphasis Type="Italic">n</Emphasis></Superscript></Stack> to a 50 kb region

Wide-compatibility (WC) is one of the most important traits in rice, which can overcome the fertility barrier in the indica/japonica hybrids, and hence to make it possible to utilize the higher yield potential of inter-subspecific hybrids. The S ₅ ⁿ gene located on chromosome 6 has been previously reported to be responsible for the wide-compatibility in rice. Here we report the precise location of the S ₅ ⁿ gene. In the first-pass mapping, the S ₅ ⁿ gene was restricted within a 200 kb region by using a population of 242 isogenic lines in combination with high-density markers developed in the S ₅ region. In the fine mapping, the S ₅ region was further saturated with newly developed markers and more isogenic lines (549 in total) were investigated. Eventually, the S ₅ ⁿ gene was mapped within a 50 kb region delimited by the left marker J13 and the right marker J17. One BAC clone screened from the BAC library of the WC rice variety 02428 covered the whole S ₅ region. Sequence analysis of the 50 kb region revealed two candidate genes, coding an aspartyl protease and a hypothetical protein. This result would greatly accelerate both cloning and marker-assisted selection of this important S ₅ ⁿ gene. Qing Ji and Jufei Lu have contributed equally to this paper.     

Different effects of SNP and GSNO on mitochondrial O<Stack><Subscript>2</Subscript><Superscript>.−</Superscript></Stack>/H<Subscript>2</Subscript>O<Subscript>2</Subscript> production

Sodium Nitroprusside (SNP) and S-Nitrosoglutathione (GSNO) differently affect mitochondrial H₂O₂ release at Complex-I. mM SNP increases while GSNO decreases the release induced by succinate alone or added on top of NAD-linked substrates. Stimulation likely depends on Nitric Oxide ( ^. NO) (released by SNP but not by GSNO) inhibiting cytochrome oxidase and mitochondrial respiration. Preincubations with SNP or high GSNO (10 mM plus DTE to increases its ^. NO release) induces an inhibition of the succinate dependent H₂O₂ production consistent with a ^. NO dependent covalent modification. However maximal inhibition of the succinate dependent H₂O₂ release is obtained in the presence of low GSNO (20–100 μM), but not with SNP. This inhibition appears independent of ^. NO release since μM GSNO does not affect mitochondrial respiration, or the H₂O₂ detection systems and its effect is very rapid. Inhibition may be partly due to an increased removal of O₂^.− since GSNO chemically competes with NBT and cytochrome C in O₂^.− detection.     

A <Superscript>13</Superscript>C-detected <Superscript>15</Superscript>N double-quantum NMR experiment to probe arginine side-chain guanidinium <Superscript>15</Superscript>N<Superscript>η</Superscript> chemical shifts

Arginine side-chains are often key for enzyme catalysis, protein–ligand and protein–protein interactions. The importance of arginine stems from the ability of the terminal guanidinium group to form many key interactions, such as hydrogen bonds and salt bridges, as well as its perpetual positive charge. We present here an arginine ¹³C^ζ-detected NMR experiment in which a double-quantum coherence involving the two ¹⁵N^η nuclei is evolved during the indirect chemical shift evolution period. As the precession frequency of the double-quantum coherence is insensitive to exchange of the two ¹⁵N^η; this new approach is shown to eliminate the previously deleterious line broadenings of ¹⁵N^η resonances caused by the partially restricted rotation about the C^ζ–N^ε bond. Consequently, sharp and well-resolved ¹⁵N^η resonances can be observed. The utility of the presented method is demonstrated on the L99A mutant of the 19 kDa protein T4 lysozyme, where the measurement of small chemical shift perturbations, such as one-bond deuterium isotope shifts, of the arginine amine ¹⁵N^η nuclei becomes possible using the double-quantum experiment.