Nonactin,monactin, dinactin,trinactin, and tetranactin. A Raman spectroscopic study

Raman spectra are reported for crystalline nonactin, monactin, dinactin, trinactin, and tetranactin and their solutions in CCl₄, CHCl₃, CH₃OH, and 4:1 (v/v) CH₃OH:CHCl₃. The macrotetrolide nactins selectively bind a wide variety of cations, and are important model compounds for the study of ion complexation. The conformations of nonactin, monactin, and dinactin in solution are similar. Their conformations are found to be sufficiently open to permit the ester carbonyl groups to form hydrogen bonds with CH₃OH; this gives rise to characteristic changes in the vibration frequencies associated with the ester groups. Nonactin, which is the least soluble of the nactins in CH₃OH, is also the least effective at forming hydrogen bonds with CH₃OH. The greater ability of the higher nactins to form hydrogen bonds with CH₃OH may be due to the increased inductive effect of ethyl over methyl side chains, which may increase the dipole moment of the ester carbonyl groups. Spectra of crystalline nonactin, monactin, and tetranactin are fairly similar, while the spectra of dinactin and trinactin comprise a second, distinct family. This is consistent with X-ray crystallographic studies, which show that nonactin and tetranactin form monoclinic crystals, while trinactin is triclinic.     

PYRUVATE KINASE ISOZYMES IN NEURONS, GLIA, NEUROBLASTOMA, AND GLIOBLASTOMA

Abstract– The distribution of pyruvate kinase isozymes (EC 2.7.1.40) was examined in cells and tissues from the central and peripheral nervous system of the rat. Most tissues contain significant quantities of both the K₄ (fetal type) and M₄ (skeletal muscle type) isozymes plus tetrameric hybrids comprised of various combination of the type M and type K subunits. Retina, for example, contains a five-mem-bered hybrid set weighted toward K₄, while sciatic nerve and spinal cord have patterns very similar to that of adult brain, consisting predominantly of M₄ with small amounts of K₄ and K-M hybrids. This adult pattern is achieved by a gradual shift from a hybrid set dominated by K₄ in fetal life, to the pattern at birth at which time the two most prominent bands were M₄ and K₂M₂, and finally to the adult pattern by about 28 days after birth. Neurons and glial cells were isolated from rat and mouse brains at the various developmental levels. The pyruvate kinase isozyme patterns in the two cell types were similar to each other and to the patterns seen in whole brain homogenates at all ages, indicating similar rates of isozymic maturation in the two cell types. The correlation of maturation with pyruvate kinase isozyme patterns was further tested in cultures of malignant cell lines. A K-M hybrid set, weighted toward K₄, was seen in two clonal lines of mouse neuroblastoma under normal culture conditions. However, lowering the serum concentration in the culture medium or adding bromodeoxyuridine caused a shift in the patterns toward type M as the cells differentiated, mimicking in part the in vivo maturation of normal cells. On the other hand, a rapidly growing and poorly differentiated line of rat glioblastoma had only K₄ under all conditions examined.     

C4 photosynthesis, atmospheric CO2, and climate

The objectives of this synthesis are (1) to review the factors that influence the ecological, geographical, and palaeoecological distributions of plants possessing C₄ photosynthesis and (2) to propose a hypothesis/model to explain both the distribution of C₄ plants with respect to temperature and CO₂ and why C₄ photosynthesis is relatively uncommon in dicotyledonous plants (hereafter dicots), especially in comparison with its widespread distribution in monocotyledonous species (hereafter monocots). Our goal is to stimulate discussion of the factors controlling distributions of C₄ plants today, historically, and under future elevated CO₂ environments. Understanding the distributions of C₃/C₄ plants impacts not only primary productivity, but also the distribution, evolution, and migration of both invertebrates and vertebrates that graze on these plants. Sixteen separate studies all indicate that the current distributions of C₄ monocots are tightly correlated with temperature: elevated temperatures during the growing season favor C₄ monocots. In contrast, the seven studies on C₄ dicot distributions suggest that a different environmental parameter, such as aridity (combination of temperature and evaporative potential), more closely describes their distributions. Differences in the temperature dependence of the quantum yield for CO₂ uptake (light-use efficiency) of C₃ and C₄ species relate well to observed plant distributions and light-use efficiency is the only mechanism that has been proposed to explain distributional differences in C₃/C₄ monocots. Modeling of C₃ and C₄ light-use efficiencies under different combinations of atmospheric CO₂ and temperature predicts that C₄-dominated ecosystems should not have expanded until atmospheric CO₂ concentrations reached the lower levels that are thought to have existed beginning near the end of the Miocene. At that time, palaeocarbonate and fossil data indicate a simultaneous, global expansion of C₄-dominated grasslands. The C₄ monocots generally have a higher quantum yield than C₄ dicots and it is proposed that leaf venation patterns play a role in increasing the light-use efficiency of most C₄ monocots. The reduced quantum yield of most C₄ dicots is consistent with their rarity, and it is suggested that C₄ dicots may not have been selected until CO₂ concentrations reached their lowest levels during glacial maxima in the Quaternary. Given the intrinsic light-use efficiency advantage of C₄ monocots, C₄ dicots may have been limited in their distributions to the warmest ecosystems, saline ecosystems, and/or to highly disturbed ecosystems. All C₄ plants have a significant advantage over C₃ plants under low atmospheric CO₂ conditions and are predicted to have expanded significantly on a global scale during full-glacial periods, especially in tropical regions. Bog and lake sediment cores as well as pedogenic carbonates support the hypothesis that C₄ ecosystems were more extensive during the last glacial maximum and then decreased in abundance following deglaciation as atmospheric CO₂ levels increased. Received: 12 February 1997 / Accepted: 20 June 1997     

The geochemistry of methane in Lake Fryxell,an amictic,permanently ice-covered,antarctic lake

The abundance and distribution of dissolved CH₄ were determined from 1987–1990 in Lake Fryxell, Antarctica, an amictic, permanently ice-covered lake in which solute movement is controlled by diffusion. CH₄ concentrations were < 1 υM in the upper oxic waters, but increased below the oxycline to 936 μM at 18 m. Sediment CH₄ was 1100 μmol (1 sed)⁻¹ in the 0–5 cm zone. Upward flux from the sediment was the source of the CH₄, NH₄ ⁺, and DOC in the water column; CH₄ was 27% of the DOC+CH₄ carbon at 18 m. Incubations with surficial sediments indicated that H¹⁴CO₃ ⁻ reduction was 0.4 μmol (1 sed)⁻¹ day⁻¹ or 4× the rate of acetate fermentation to CH₄. There was no measurable CH₄ production in the water column. However, depth profiles of CH₄, NH₄, and DIC normalized to bottom water concentrations demonstrated that a significant CH₄ sink was evident in the anoxic, sulfate-containing zone of the water column (10–18 m). The δ¹³CH₄ in this zone decreased from −72 % at 18 m to −76% at 12 m, indicating that the consumption mechanism did not result in an isotopic enrichment of ¹³CH₄. In contrast, δ¹³CH₄ increased to −55 % at 9 m due to aerobic oxidation, though this was a minor aspect of the CH₄ cycle. The water column CH₄ profile was modeled by coupling diffusive flux with a first order consumption term; the best-fit rate constant for anaerobic CH₄ consumption was 0.012 yr⁻¹. On a total carbon basis, CH₄ consumption in the anoxic water column exerted a major effect on the flux of carbonaceous material from the underlying sediments and serves to exemplify the importance of CH₄ to carbon cycling in Lake Fryxell.     

Quantification of GA1, GA3, GA4, GA7, GA8, GA9, GA19 and GA20; and GA20 metabolism in dormant and non-dormant beechnuts

The endogenous levels of GA₁, GA₃, GA₄, GA₇, GA₈, GA₉, GA₁₉ and GA₂₀ were determined in beech seeds (Fagus sylvatica L.) treated with different dormancy breaking treatments. Gibberellins were analysed separately in cotyledons and embryo axes. After purification of the extracts, GAs were quantified by GC-MS-selected ion monitoring (GC-MS-SIM) with deuterated GAs as internal standards. The results showed that GAs corresponding to the 13-OH pathway seemed to be involved in dormancy breaking. Strong differences in GA₁, GA₃, GA₈, GA₁₉ and GA₂₀ levels between embryo axes and cotyledons of dormant and non-dormant beechnuts were detected with less pronounced differences for GA₄, GA₇ and GA₉ levels. Both the quantitative differences between dormant and non-dormant seeds in the analysed GAs corresponding to the 13-OH pathway, and the capacity of non-dormant seeds to carry out metabolic conversions when labelled GA₂₀ was injected into the seeds, reveal a dynamic role of GAs in dormancy release.     

Synthesis,characterization, and biological activity of platinum II,III, and IV pivaloamidine complexes

Imino ligands have proven to be able to activate the trans geometry of platinum(II) complexes towards antitumor activity. These ligands, like aromatic N-donor heterocycles, have a planar shape but, different from the latter, have still an H atom on the coordinating nitrogen which can be involved in H-bond formation. Three classes of imino ligands have been extensively investigated: iminoethers (HN=C(R)OR′), ketimines (HN=CRR′), and amidines (HN=C(R)NR′R″). The promising efficacy of the platinum compounds with amidines (activity comparable to that of cisplatin for cis complexes and much greater than that of transplatin for trans complexes) prompted us to extend the investigation to amidine complexes with a bulkier organic residue (R = t-Bu). The tert-butyl group can confer greater affinity for lipophilic environments, thus potentiating the cellular uptake of the compound. In the present study we describe the synthesis and characterization of pivaloamidine complexes of platinum(II), (cis and trans-[PtCl₂(NH₃){Z-HN=C(t-Bu)NH₂}] and cis and trans-[PtCl₂{Z-HN=C(t-Bu)NH₂}₂]), platinum(III) ([Pt₂Cl₄{HN=C(t-Bu)NH}₂(NH₃)₂]), and platinum(IV) (trans-[PtCl₄(NH₃){Z-HN=C(t-Bu)NH₂}] and trans-[PtCl₄{Z-HN=C(t-Bu)NH₂}₂]). The cytotoxicity of all new Pt complexes was tested toward a panel of cultured cancer cell lines, including cisplatin and multidrug resistant variants. In addition, cellular uptake and DNA binding, perturbations of cell cycle progression, induction of apoptosis, and p53 activation were investigated for the most promising compound trans-[PtCl₂(NH₃){Z-HN=C(t-Bu)NH₂}]. Remarkably, the latter complex was able to overcome both acquired and intrinsic cisplatin resistance.     

Twenty-four-hour variations in activity,core temperature,metabolic rate,and respiratory quotient in captive chinese pangolins

The circadian rhythms in activity, core temperature (T_c), O₂ consumption, CO₂ production, and respiratory quotient (RQ) were monitored in four captive Chinese pangolins (Manis pentadactyla). The pangolins were strictly nocturnal, never emerging from their nest before 1600 h, and their intermittent activity continued no later than 0230. As is usual in nocturnal mammals, the highest values observed in T_c, O₂ consumption, and CO₂ production occurred during the night; the lowest values occurred during the day. The magnitude of the variation in T_c, O₂ consumption, CO₂ production, and RQ averaged 1.2°C, 1.3 ml O₂ kg^?1 min^?1, 1.2 ml CO₂ kg^?1 min^?1, and 0.24, respectively. The circadian pattern in RQ was independent of activity, T_c, and the metabolic parameters and was of a different character than the patterns exhibited in the other variables. RQ remained constant at either a high or low level for long periods (8–10 h) and then increased or decreased relatively rapidly (1–2h) to the other level as in a square wave, whereas the rhythms in the other variables are similar to sine waves. The sharp increase in RQ was followed by a slow decline in T_c, and the sharp decline in RQ was followed by a slow increase in T_c.     

Quantification of GA1, GA3, GA4, GA7, GA9, and GA20 in vegetative and male cone buds from juvenile and mature trees of Pinus radiata

The gibberellins GA₁, GA₃, GA₄, GA₇, GA₉ and GA₂₀ were quantified in vegetative and pollen cone buds of juvenile and mature trees of Pinus radiata by combined gas chromatography-mass spectrometry and selected ion monitoring (GC-MS-SIM) using deuterated GAs as internal standards. Higher levels of GA₇ and GA₉ and lower levels of GA₄ were detected in juvenile vegetative buds compared to mature buds, and there were no differences in relation to age for GA₁, GA₃ and GA₂₀. Conversely, when differences between vegetative and pollen cone buds from a mature tree were studied, the highest levels of GA₁ and GA₄ were found in pollen cone buds, similar levels of GA₃, GA₇ and GA₉ were observed in both, and ten fold lower levels of GA₂₀ were found in pollen cone buds as compared with vegetative buds. These results indicate a difference in GA metabolism in relation to both the tree age as well as the physiological status of buds: vegetative or reproductive in this conifer.     

Electronic, magnetic and optical properties of Cu, Ag, Au-doped Si clusters

The structural, optical and magnetic properties of Cu, Ag, Au-doped Si₇ Clusters have been systematically investigated using density functional theory calculations. The global optimized structures of Cu, Ag, Au-doped Si clusters are predicted to have a lower HOMO–LUMO gap and higher magnetic moment. M-doping (M?=?Cu, Ag, Au) in Si cluster widens a range of adsorption wavelength, especially Au-doping. The characteristics in electronic density of states (DOSs) show that C_5v-Si₆Cu has a big asymmetrical spin-up and spin-down. The average atomic moment is 0.428 mμ_B per atom for the Si₆Cu cluster with C_5v symmetry, while the average paramagnetic moment is 0.143 mμ_B per atom for other M-doped (M?=?Cu, Ag, Au) Si₇ clusters.     

Hydrogen exchange of rhenium(VII) heptahydridobis(triphenylphosphine) with water, aniline, methanol, and itself

The hydride ligands of ReH₇(PPh₃)₂ undergo fast hydrogen exchange with water at room temperature while exchanging with the hydrogen atoms of aromatic solvent molecules at a slower rate. The amount of time required for isotopomer peaks to appear in the ¹H NMR hydride resonance of ReH₇(PPh₃)₂ was used to distinguish fast hydrogen exchange from slow hydrogen exchange. The room temperature ¹H NMR T₁ values of adventitious water resonances were used to distinguish two rhenium heptahydride compounds that participate in fast hydrogen exchange with water, ReH₇(PPh₃)₂ and ReH₇(AsPh₃)₂, from one compound that does not participate, ReH₇(PCy₃)₂. Fast hydrogen exchange between ReH₇(PPh₃)₂ and water is greatly slowed or stopped when the compound is dissolved in a solution that contains DMSO. The compound ReH₆D(PPh₃)₂, an isotopomer of ReH₇(PPh₃)₂ that was prepared in situ, exhibited an isotopomer shift in its ³¹P-{¹H} NMR spectrum as well as D-P coupling when measured in the solvent anisole. In a solvent system containing deuteroaniline, nearly all of the hydride ligands were exchanged with deuterium, from aniline, in less than 2 h. Hydrogen exchange between the hydride ligands of ReH₇(PPh₃)₂ and deuteroaniline was found to be reversible upon the addition of normal aniline. The distribution of hydrogen isotopes in the rhenium coordination spheres reflected the overall composition of the exchangeable hydrogen isotopes present in the bulk sample. In a deuteromethanol-containing solvent system, the exchange of hydride ligands between separate ReH₇(PPh₃)₂ isotopomers was evident. The presumed hydrogen exchange intermediate, [ReH₆(H₂)(PPh₃)₂]⁺, may be responsible for the evident exchange of hydride ligands and may also be important to the thermal loss of dihydrogen from ReH₇(PPh₃)₂.     

The chemical reactivity of tetraisobutyldialuminum towards ethers,nitrogen lewis bases,aluminumtrimethyl, borontrichloride and ethylene

Treatment of Al₂ⁱBu₄ with THF and Et₂O results in partial decomposition to afford Al metal while reaction with γ-picoline products a bis-adduct of limited stability. Reactions with AlMe₃ and BCl₃, separately, involves ligand exchange with accompanying disproportionation to yield Al metal. Dimethylamine induces disproportionation to afford AlⁱBu₃·HNMe₂ and an intemediate trialuminum species. The latter undergoes AlAl bond cleavage with formation of H₂, _iBu₂AlNMe₂, and [Me₂N- (ⁱBu)AlAlⁱBu₂]₂· Al₂iBu₄ eliminates Me₂CCH₂ in solution at 80 °C, and the catenated AlH intermediate reacts with ethylene to afford AlEt and AlCH₂CH₂CH₂CH₃ moieties.     

Methanotrophy in a Paleoproterozoic oil field ecosystem,Zaonega Formation,Karelia, Russia

Organic carbon rich rocks in the c. 2.0 Ga Zaonega Formation (ZF), Karelia, Russia, preserve isotopic characteristics of a Paleoproterozoic ecosystem and record some of the oldest known oil generation and migration. Isotopic data derived from drill core material from the ZF show a shift in δ¹³C_org from c. ?25‰ in the lower part of the succession to c. ?40‰ in the upper part. This stratigraphic shift is a primary feature and cannot be explained by oil migration, maturation effects, or metamorphic overprints. The shift toward ¹³C‐depleted organic matter (δ¹³C_org < ?25‰) broadly coincides with lithological evidence for the generation of oil and gas in the underlying sediments and seepage onto the sea floor. We propose that the availability of thermogenic CH₄ triggered the activity of methanotrophic organisms, resulting in the production of anomalously ¹³C‐depleted biomass. The stratigraphic shift in δ¹³C_org records the change from CO₂‐fixing autotrophic biomass to biomass containing a significant contribution from methanotrophy. It has been suggested recently that this shift in δ¹³C_org reflects global forcing and progressive oxidation of the Earth. However, the lithologic indication for local thermogenic CH₄, sourced within the oil field, is consistent with basinal methanotrophy. This indicates that regional/basinal processes can also explain the δ¹³C_org negative isotopic shift observed in the ZF.     

Iron and nickel complexes with heterocyclic ligands: Stability,synthesis, spectral characterization,antimicrobial activity,acute and subacute toxicity

The synthesis and characterization by elemental analysis, emission atomic spectroscopy, TG measurements, magnetic measurements, FTIR, ¹H NMR, UV–visible spectra and conductivity of a series of iron (II) and nickel (II) complexes with two heterocyclic ligands (L¹(SMX): sulfamethoxazole and L²(MIZ): metronidazole) used in pharmaceutical field and with a new ligand derived benzoxazole (L³(MPBO): 2-(5-methylpyridine-2-yl)benzoxazole), were reported. The formulae obtained for the complexes are: [M(L¹)₂ Cl₂]·nH₂O, [M(L²)₂Cl₂(H₂O)₂]·H₂O and [M(L³)₂(OH)₂]·nH₂O. Stability constants of these complexes have been determined by potentiometric methods in water–ethanol (90:10, v/v) mixture at a 0.2 mol L^?1 ionic strength (NaCl) and at 25.0 ± 0.1 °C. Sirko program was used to determine the protonation constants as well as the binding constants of three species [ML₂H₂]²⁺, [ML₂] and [ML]²⁺. The antimicrobial activity of the ligands and complexes was evaluated in vitro against different human bacteria and fungi using agar diffusion method.Iron sulfamethoxazole complex showed a remarkable inhibition of bacteria growth especially on Staphylococcus aureus and P. aeruginosa. The iron metronidazole complex is active against yeasts especially on Candida tropicalis strain. Nickel complexes presented different antibacterial and antifungal behavior's against bacteria and fungal.The acute toxicity study revealed that the iron complexes are not toxic at 2000 mg/kg dose orally administrated.LD₅₀ for nickel complexes was determined using graphical method.No significant differences in the body weights between the control and the treated groups of both rat sexes in subacute toxicity study using for iron complexes. Hematological and clinical blood chemistry analysis revealed no toxicity effects of the iron complexes. Pathologically, neither gross abnormalities nor histopathological changes were observed for these complexes.     

Water-energy dynamics,habitat heterogeneity,history, and broad-scale patterns of mammal diversity

Numerous hypotheses on diversity patterns are often presented as if they were mutually exclusive. However, because of multicollinearity, correlational analyses are not able to distinguish the causal effects of different factors on these patterns. For this reason, we examine the interrelationships among current climate, habitat heterogeneity and evolutionary history by partitioning the variation in both total and non-volant mammal species richness in the Iberian Peninsula. Thus, it is possible to determine the variation accounted for by each one of these three components that is not shared by the others, and the respective overlaps. More specifically, we hypothesize that (H₁) in warm temperate zones, a small increase in the available energy has strong negative effects on mammal richness if water availability is limiting; (H₂) there are functional relationships between woody plant species richness (WOOD) and the richness of mammal species; (H₃) there is a signal of evolutionary history in contemporary patterns of species richness, and (H₄) mammal richness and the historical variable mean root distance (MRD) respond to the same driving forces. Additionally, we also test for spatial autocorrelation. We found a sharp nonlinear decrease in mammal richness with increasing energy and a monotonic increase with increasing water availability. Moreover, an interaction term between these two climate factors appeared to be statistically significant, so H₁ could not be rejected. WOOD remained significant after partialling out both current climate and MRD at the family level (MRDf), supporting H₂. The relationship between mammal diversity and MRD averaged by species richness was found to be spurious, but there appeared a significant historical signal using MRDf (this supports H₃). The overlaps among these factors are consistent with H₄ and suggest that water-energy dynamics have probably been active drivers throughout evolutionary history with habitat heterogeneity, and biotic interactions playing an important role.     

Aerobic Biotransformation of N-Nitrosodimethylamine and N-Nitrodimethylamine by Benzene-, Butane-, Methane-, Propane-, and Toluene-Fed Cultures

N-Nitrosodimethylamine (NDMA) is an emerging contaminant of concern. N-nitrodimethylamine (DMNA) is a structural analog to NDMA. NDMA and DMNA have been found in drinking water, groundwater, and other media and are of concern due their toxicity. The authors evaluated biotransformation of NDMA and DMNA by cultures enriched from contaminated groundwater growing on benzene, butane, methane, propane, or toluene. Maximum specific growth rates of enriched cultures on butane (μ_max = 1.1 h^?1) and propane (μ_max = 0.65 h^?1) were 1 to 2 orders of magnitude higher than those presented in the literature. Growth rates of mixed cultures grown on benzene (μ_max = 1.3 h^?1), methane (μ_max = 0.09 h^?1), and toluene (μ_max = 0.99 h^?1) in these studies were similar to those presented in the literature. NDMA biotransformation rates for methane oxidizers (υ_max = 1.4 ng min^?1 mg^?1) and toluene oxidizers (υ_max = 2.3 ng min^?1 mg^?1) were comparable to those presented in the literature, whereas the biotransformation rate for propane oxidizers (υ_max = 0.37 ng min^?1 mg^?1) was lower. NDMA biotransformation rates for benzene oxidizers (υ_max = 1.02 ng min^?1 mg^?1) and butane oxidizers (υ_max = 1.2 ng min^?1 mg^?1) were comparable to those reported for other primary substrates. These studies showed that DMNA biotransformation rates for benzene (υ_max = 0.79 ng min^?1 mg^?1), butane (υ_max = 1.0 ng min^?1 mg^?1), methane (υ_max = 2.1 ng min^?1 mg^?1), propane (υ_max = 1.46 ng min^?1 mg^?1), and toluene (υ_max = 0.52 ng min^?1 mg^?1) oxidizers were all comparable. These studies highlight potential bioremediation methods for NDMA and DMNA in contaminated groundwater.     

Effects of Metals on Methanogenesis, Sulfate Reduction, Carbon Dioxide Evolution, and Microbial Biomass in Anoxic Salt Marsh Sediments

The effects of several metals on microbial methane, carbon dioxide, and sulfide production and microbial ATP were examined in sediments from Spartina alterniflora communities. Anaerobically homogenized sediments were amended with 1,000 ppm (ratio of weight of metal to dry weight of sediment) of various metals. Time courses in controls were similar for CH₄, H₂S, and CO₂, with short initial lags (0 to 4 h) followed by periods of constant gas production (1 to 2 days) and declining rates thereafter. Comparisons were made between control and experimental assays with respect to initial rates of production (after lag) and overall production. Methane evolution was inhibited both initially and overall by CH₃HgCl, HgS, and NaAsO₂. A period of initial inhibition was followed by a period of overall stimulation with Hg, Pb, Ni, Cd, and Cu, all as chlorides, and with ZnSO₄, K₂CrO₄, and K₂Cr₂O₇. Production of CO₂ was generally less affected by the addition of metals. Inhibition was noted with NaAsO₂, CH₃HgCl, and Na₂MoO₄. Minor stimulation of CO₂ production occurred over the long term with chlorides of Hg, Pb, and Fe. Sulfate reduction was inhibited in the short term by all metals tested and over the long term by all but FeCl₂ and NiCl₂. Microbial biomass was decreased by FeCl₂, K₂Cr₂O₇, ZnSO₄, CdCl₂, and CuCl₂ but remained generally unaffected by PbCl₂, HgCl₂, and NiCl₂. Although the majority of metals produced an immediate inhibition of methanogenesis, for several metals this was only a transient phenomenon followed by an overall stimulation. The initial suppression of methanogenesis may be relieved by precipitation, complexation, or transformation of the metal (possibly by methylation), with the subsequent stimulation resulting from a sustained inhibition of competing organisms (e.g., sulfate-reducing bacteria). For several environmentally significant metals, severe metal pollution may substantially alter the flow of carbon in sediments.     

Modeled production,oxidation, and transport processes of wetland methane emissions in temperate,boreal, and Arctic regions

Wetlands are the largest natural source of methane (CH₄) to the atmosphere. The eddy covariance method provides robust measurements of net ecosystem exchange of CH₄, but interpreting its spatiotemporal variations is challenging due to the co-occurrence of CH₄ production, oxidation, and transport dynamics. Here, we estimate these three processes using a data-model fusion approach across 25 wetlands in temperate, boreal, and Arctic regions. Our data-constrained model—iPEACE—reasonably reproduced CH₄ emissions at 19 of the 25 sites with normalized root mean square error of 0.59, correlation coefficient of 0.82, and normalized standard deviation of 0.87. Among the three processes, CH₄ production appeared to be the most important process, followed by oxidation in explaining inter-site variations in CH₄ emissions. Based on a sensitivity analysis, CH₄ emissions were generally more sensitive to decreased water table than to increased gross primary productivity or soil temperature. For periods with leaf area index (LAI) of ≥20% of its annual peak, plant-mediated transport appeared to be the major pathway for CH₄ transport. Contributions from ebullition and diffusion were relatively high during low LAI (<20%) periods. The lag time between CH₄ production and CH₄ emissions tended to be short in fen sites (3 ± 2 days) and long in bog sites (13 ± 10 days). Based on a principal component analysis, we found that parameters for CH₄ production, plant-mediated transport, and diffusion through water explained 77% of the variance in the parameters across the 19 sites, highlighting the importance of these parameters for predicting wetland CH₄ emissions across biomes. These processes and associated parameters for CH₄ emissions among and within the wetlands provide useful insights for interpreting observed net CH₄ fluxes, estimating sensitivities to biophysical variables, and modeling global CH₄ fluxes.     

Synthesis, characterization, spectroscopy, electronic and redox properties of a new nickel dithiolene system

A new dithiolene ligand with 3,5-dibromo substituted phenyl groups was designed and synthesized. The protected form of the ligand was reacted with a nickel salt providing neutral Ni(S₂C₂(3,5-C₆H₃Br₂)₂)₂ and anionic [Ni(S₂C₂(3,5-C₆H₃Br₂)₂)₂]⁻ isolated as a Bu₄N⁺ salt. Both were characterized by UV-Vis and IR spectroscopy and compared with the similar known molecular systems. They exhibit intense low energy transitions that are characteristic of such systems. The electrochemical behavior of these molecules was investigated by cyclic voltammetry.     

Sarcoplasmic reticulum calcium ATPase interactions with decaniobate, decavanadate, vanadate, tungstate and molybdate

Over the last few decades there has been increasing interest in oxometalate and polyoxometalate applications to medicine and pharmacology. This interest arose, at least in part, due to the properties of these classes of compounds as anti-cancer, anti-diabetic agents, and also for treatment of neurodegenerative diseases, among others. However, our understanding of the mechanism of action would be improved if biological models could be used to clarify potential toxicological effects in main cellular processes. Sarcoplasmic reticulum (SR) vesicles, containing a large amount of Ca^2 +-ATPase, an enzyme that accumulates calcium by active transport using ATP, have been suggested as a useful model to study the effects of oxometalates on calcium homeostasis. In the present article, it is shown that decavanadate, decaniobate, vanadate, tungstate and molybdate, all inhibited SR Ca²⁺-ATPase, with the following IC₅₀ values: 15, 35, 50, 400 μM and 45 mM, respectively. Decaniobate (Nb₁₀), is the strongest P-type enzyme inhibitor, after decavanadate (V₁₀). Atomic-absorption spectroscopy (AAS) analysis, indicates that decavanadate binds to the protein with a 1:1 decavanadate:Ca^2 +-ATPase stoichiometry. Furthermore, V₁₀ binds with similar extension to all the protein conformations, which occur during calcium translocation by active transport, namely E1, E1P, E2 and E2P, as analysed by AAS. In contrast, it was confirmed that the binding of monomeric vanadate (H₂VO₄^2 −; V₁₎ to the calcium pump is favoured only for the E2 and E2P conformations of the ATPase, whereas no significant amount of vanadate is bound to the E1 and E1P conformations. Scatchard plot analysis, confirmed a 1:1 ratio for decavanadate-Ca^2 +-ATPase, with a dissociation constant, k_d of 1 μM^− 1. The interaction of decavanadate V₁₀O₂₈^6 − (V₁₀) with Ca^2 +-ATPase is prevented by the isostructural and isoelectronic decaniobate Nb₁₀O₂₈^6 − (Nb₁₀), whereas no significant effects were detected with ATP or with heparin, a known competitive ATP binding molecule, suggesting that V₁₀ binds non-competitively, with respect to ATP, to the protein. Finally, it was shown that decaniobate inhibits SR Ca^2 +-ATPase activity in a non competitive type of inhibition, with respect to ATP. Taken together, these data demonstrate that decameric niobate and vanadate species are stronger inhibitors of the SR calcium ATPase than simple monomeric vanadate, tungstate and molybdate oxometalates, thus affecting calcium homeostasis, cell signalling and cell bioenergetics, as well many other cellular processes. The ability of these oxometalates to act either as phosphate analogues, as a transition-state analogue in enzyme-catalysed phosphoryl group transfer processes and as potentially nucleotide-dependent enzymes modulators or inhibitors, suggests that different oxometalates may reveal different mechanistic preferences in these classes of enzymes.