The Molten Globule of β2-Microglobulin Accumulated at pH 4 and Its Role in Protein Folding

The acid transition of β₂-microglobulin (β2m) was studied by tryptophan fluorescence, peptide circular dichroism, and NMR spectroscopy. The protein exhibits a three-state transition with an equilibrium intermediate accumulated at pH 4 (25 °C). The pH 4 intermediate has typical characteristics of the molten globule (MG) state; it showed a native-like secondary structure without specific side-chain tertiary structure, and the hydrodynamic radius determined by pulse field gradient NMR was only 20% larger than that of the native state. The accumulation of the pH 4 intermediate is very analogous to the behavior of apomyoglobin, for which the pH 4 MG has been well characterized, although β2m, a β-protein, is structurally very different from α-helical apomyoglobin. NMR pH titration of histidine residues of β2m has also indicated that His84 has an abnormally low pK_a value in the native state. From the pH dependence of the unfolding transition, the protonations of this histidine and 10 weakly abnormal carboxylates triggered the transition from the native to the MG state. This behavior is again analogous to that of apomyoglobin, suggesting a common mechanism of production of the pH 4 MG. In contrast to the folding of apomyoglobin, in which the MG was equivalent to the burst-phase kinetic folding intermediate, the burst-phase refolding intermediate of β2m, detected by stopped-flow circular dichroism, was significantly more structured than the pH 4 intermediate. It is proposed that the folding of β2m from its acid-denatured state takes place in the following order: denatured state → MG → burst-phase intermediate → native state.     

Could a strong alkali deproteinization replace the standard lysis step in alkaline single cell gel electrophoresis (comet) assay (pH > 13)?

The alkaline version of single cell gel electrophoresis (comet) assay is widely used for evaluating DNA damage at the individual cell level. The standard alkaline method of the comet assay involves deproteinization of cells embedded in agarose gel using a high salt–detergent lysis buffer, followed by denaturation of DNA and electrophoresis using a strong alkali at pH > 13 [N.P. Singh, M.T. McCoy, R.R. Tice, E.L. Schneider, A simple technique for quantitation of low levels of DNA damage in individual cells, Exp. Cell. Res. 175 (1988) 184–191]. However, a recent report showed that a strong alkali treatment results in simultaneous deproteinization of cells and denaturation of genomic DNA [P. Sestili, C. Martinelli, V. Stocchi, The fast halo assay: an improved method to quantify genomic DNA strand breakage at the single cell-level, Mutat. Res. 607 (2006) 205–214]. This study was carried out to test whether the strong alkali deproteinization of cells could replace the high salt–detergent lysis step used in the standard method of the alkaline comet assay. Peripheral blood lymphocytes from 3 healthy individuals were irradiated with gamma rays at doses varying between 0 and 10 Gy. Following irradiation, the comet assay was performed according to the standard alkaline method (pH > 13) and a modified method. In the modified method, agarose embedded cells were treated with a strong alkali (0.3 M NaOH, 0.02 M Trizma and 1 mM EDTA, pH > 13) for 20 min to allow deproteinization of cells and denaturation of DNA. This was followed by electrophoresis using the same alkali solution to obtain comets. DNA damage expressed in terms of comet tail length, percentage of DNA in comet tail and tail moment obtained by the standard alkaline method and the modified method were compared. In both methods, DNA damage showed a good correlation with the dose of gamma ray. The results indicate a satisfactory sensitivity of the modified method in detecting radiation-induced DNA damage in human peripheral blood lymphocytes.     

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.     

·遗传咨询·

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？     

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.     

L’art Paléolithique est-il un « art » ?: Réflexions autour d’une question d’actualité

During the last years, an international debate about the concept of “Palaeolithic art” has taken place. On one hand, several specialists have critiqued the use of the concept of “art” in naming the images created by Homo sapiens during the Palaeolithic era. They claim that the use of this term implies the projection of a modern category to a world - that of prehistoric humans - which is completely different from our own. On the other hand, some archaeologists consider that the term “Palaeolithic art” does not imply an anachronistic interpretation of prehistoric representations. In presenting the historical context, which has made such a discussion possible, we consider the causes and effects of this controversy. Firstly, we analyze the traditional interpretation, which considered Palaeolithic images as “works of art”. Secondly, we examine the connections, which can be found between the debate about “Palaeolithic art” and certain polemics, which have arisen from the history of art and anthropological frameworks. Thirdly, we consider the arguments utilized by those who are for and those who are against the term “Palaeolithic art”. Finally, we emphasize the importance of this debate to better understand the categories and the concepts, which determine the scientific practice.     

Determination of the lifetime of D<Stack><Subscript>2</Subscript><Superscript>−</Superscript></Stack> and HD<Superscript>−</Superscript> ions

A method for determining the lifetime of unstable ions is described. The method is based on measuring the decrease in the ion beam current onto a fixed detector with increasing path length of the ion beam from the ion source to the detector. The measurements performed for D^? ₂ and HD^? molecular ions have shown that their lifetimes are 3.5 ± 0.1 and 4.4 ± 0.1 μs, respectively.     

Au Gravettien, dans la grotte Cosquer (Marseille, Bouches-du-Rhône), l'Homme a-t-il compté sur ses doigts ?

Negative hands, occasionally with incomplete fingers, are often found in Paleolithic caves but so far have received no definitive explanation. Nowadays they are more commonly seen as the expression of a gestural language. In this paper, we suggest that the negative hands visible in the Cosquer cave and dating from around 27?000 BP could represent counting on fingers. Several arguments are developed to support this hypothesis. Furthermore we also suggest that the dots and dashes often associated with negative hands in numerous caves, might be another, more advanced way of representing numbers.     

Structures and stability of N<Subscript>13</Subscript><Superscript>+</Superscript> and N<Subscript>13</Subscript><Superscript>−</Superscript> clusters

The structures and stabilities of eleven N₁₃ ⁺ and N₁₃ ^– isomers have been investigated with second-order Møller–Plesset (MP2) and density functional theory (DFT) methods. Five N₁₃ ⁺ isomers and six N₁₃ ^– isomers are all reasonable local minima on their potential energy hypersurfaces. The most stable N₁₃ ⁺ cation is structure C-2 with C_2v symmetry, which contains a pentazole ring and two N₄ open chains. It is different from those of the N₇ ⁺ and N₉ ⁺ clusters, but similar to the N₁₁ ⁺ cluster. Meanwhile, the most stable N₁₃ ^– structure A-2 is composed of a pentazole ring and a six-membered ring connected by two nitrogen atoms. It is not only different from those of the N₇ ^– and N₉ ^– clusters, but also from the N₁₁ ^– cluster. The decomposition pathways of structures C-2 and A-2 were investigated at the B3LYP/(aug)-cc-pVDZ level. From the barrier heights of the structures C-2 and A-2 decomposition processes, it is suggested that C-2 is difficult to observe experimentally and A-2 may be observed as a short-lived species. Figure Optimized geometrical parameters of N₁₃ ⁺ isomer C-2      

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.     

Does Government Regulation Inhibit Embryonic Stem Cell Research and Can It Be Effective?

The UK was one of the first countries to introduce legislation regulating embryo research, and the British Parliament has taken a liberal view of the field. However, even in the UK, regulation of human embryonic stem cell (ESC) research has had drawbacks, and the regulatory framework is somewhat inconsistent and imposes considerable bureaucracy. There are around 33 countries that have broadly liberal legislation; each has a different view of what is permissible. Only about eight of these countries have contributed significantly to published research in the field. Paradoxically, in spite of tight federal restrictions, the USA remains the most productive country in terms of the number and quality of peer review research publications. But even in our increasingly global society, complex regulation will become progressively irrelevant and impossible to impose effectively because attitudes will continue to vary widely in different countries and because of international travel and trade. Consequently, there is a universal need for scientists to demonstrate their recognition of the ethical and commercial conflicts that may arise in their research and engage in public debate and dialogue to ensure responsible activity that benefits their research and reflects the values of society.     

Insight into π-hole interactions containing the inorganic heterocyclic compounds S<Subscript>2</Subscript>N<Subscript>2</Subscript>/SN<Subscript>2</Subscript>P<Subscript>2</Subscript>

Similar to σ-hole interactions, the π-hole interaction has attracted much attention in recent years. According to the positive electrostatic potentials above and below the surface of inorganic heterocyclic compounds S₂N₂ and three SN₂P₂ isomers (heterocyclic compounds 1–4), and the negative electrostatic potential outside the X atom of XH₃ (X = N, P, As), S₂N₂/SN₂P₂?XH₃ (X = N, P, As) complexes were constructed and optimized at the MP2/aug-cc-pVTZ level. The X atom of XH₃ (X = N, P, As) is almost perpendicular to the ring of the heterocyclic compounds. The π-hole interaction energy becomes greater as the trend goes from 1?XH₃ to 4?XH₃. These π-hole interactions are weak and belong to “closed-shell” noncovalent interactions. According to the energy decomposition analysis, of the three attractive terms, the dispersion energy contributes more than the electrostatic energy. The polarization effect also plays an important role in the formation of π-hole complexes, with the contrasting phenomena of decreasing electronic density in the π-hole region and increasing electric density outside the X atom of XH₃ (X = N, P, As).

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Graphical abstract Computed density difference plots for the complexes 3?NH ₃ (a ₁), 3?PH ₃ (b ₁), 3?AsH ₃ (c ₁) and electron density shifts for the complexes 3?NH ₃ (a ₂), 3?PH ₃ (b ₂),3?AsH ₃ (c ₂) on the 0.001 a.u. contour