The development of an 191Os →191mIr generator using an osmium chelate parent complex—I. Trans-dioxobismalonatoosmate(VI)

A ¹⁹¹Os→ ^191mIr generator has been developed that has higher ^191mIr yield and lower ¹⁹¹Os breakthrough than previous designs. These improvements have been realized through the use of the osmium chelate complex trans-dioxobismalonatoosmate(VI) as the parent species on the generator. The new generator provides an initial ^191mIr yield of 40%/mL and ¹⁹¹Os breakthrough of 2–3 × 10⁻³% when eluted with a solution of 0.05 M malonic acid/0.10 M sodium chloride at pH 4. Other advantages of the new design include faster clearance of the ¹⁹¹Os breakthrough products and simpler assembly.     

Spectroscopic and reactivity comparison of pentacyanonitrosylruthenate(2-) with pentacyanonitrosylferrate(2-), nitroprusside

Lithium penta(cyano-¹³C)nitrosylruthenate (2-), Li₂[Ru(¹³CN)₅NO], in which the anion is the ruthenium analogue of the nitroprusside ion, has been synthesized at 90% isotopic enrichment, and characterized spectroscopically. Despite the very high level of ¹³C enrichment, no two-bond coupling ²J(¹³C_ax-Ru¹³C_eq) was detected in the high-frequency ¹³C NMR spectrum of Li₂[Ru(¹³CN)₅NO], nor was any such coupling observed in Li₄[Ru(¹³CN)₅(¹⁵NO₂)] although both two-bond couplings to ¹⁵N, ²J(¹³C_ax-Ru¹⁵NO₂) and ²J(¹³C_eqRu¹⁵N) were observed. Li₂[Ru(¹³CN)₅(¹⁴NO)] reacted with excess of Li[¹⁵NO₂] to yield Li₄[Ru(¹³CN)₅(¹⁵NO₂)] only: no Li₂[Ru(¹³CN)₅(¹⁵NO)] was observed. Li₄[Ru(¹³CN)₅(¹⁴NO₂)] however showed no exchange with Li[¹⁵NO₂]. While [Ru(CN)₅NO]²⁻ reacted with both OH⁻ and SH⁻ in reactions similar to those of [Fe(CN)₅NO]²⁻, no reactions were detected between [Ru(CN)₅NO]²⁻ and piperidine, [CH(CN)₂]⁻, [CH(COCH₃)₂]⁻, MeS⁻, or [S₂O₄]²⁻, all of which are known to react readily with [Fe(CN)₅NO]²⁻     

Mechanism of nitrate uptake into Chara corallina cells: lack of evidence for obligatory coupling to proton pump and a new NO3−/NO3− exchange model

Abstract. Nitrate uptake into Chara corallina cells at different external pH (pH_o) after different NO₃⁻ pretreatment conditions has been investigated. Following NO₃⁻ pretreatment (0.2 mol m⁻³ NO₃⁻) there was little effect of pH_o on subsequent net NO₃⁻ uptake into Chara cells. After N deprivation (2 mmol m⁻³ NO₃⁻) there was a pronounced effect of pH_o on nitrate uptake, the maximum rate occurring at pH_o 4.7. There was no consistent relationship between OH⁻ efflux and NO₃⁻ uptake in short term experiments (< 1 h). NO₃⁻ efflux was also sensitive to pH_o, the maximum rate occurring at ∼ pH_o 5.0. An inhibitor of the proton pump, DES, immediately stimulated NO₃⁻ uptake into cells pretreated with NO₃⁻ and prevented the time-dependent decrease in NO₃⁻, uptake into Chara cells that had been previously treated with low N (2 mmol m⁻³ NO₃⁻). NO₃⁻ efflux was found to be very sensitive to DES with K_i= 0.7 mmol m⁻³. At the optimum pH_o for NO₃⁻ uptake the effect of DES on membrane potential (ψ_m) were slight, and only apparent after 30 min. The results are interpreted in context of current models relating NO₃⁻ uptake and H⁺ pump activity. A new model for NO₃⁻ uptake is proposed which involves NO₃⁻/NO₃⁻ exchange at steady state.     

The binding of metal Ions by mercaptoacids. II. Formation constants for the complexes of mercaptosuccinate with Cd(II) and computer simulation of its ability to mobilize the low molecular weight fraction of Cd(II) in blood plasma

Formation constants for cadmium(II) complexes of mercaptosuccinate in aqueous solution have been determined at 37 °C and 150 mmol dm⁻³ chloride medium by potentiometric titrations using a glass electrode. The emf data obtained have been analyzed using the ESTA computer program library. The experimental data can be explained by the formation of the complexes Cd₃(MSA)₂, Cd₂(MSA)₂H⁻, Cd₂- (MSA)₂²⁻, Cd₂(MSA)₂OH³⁻ and Cd(MSA)₂⁴⁻. The formation constants obtained have been used in a simulation model of blood plasma to investigate the mobilization of cadmium(II) by mercaptosuccinate in normal plasma. It is shown that mobilization is unlikely at pharmacological levels of the drug.     

Complexes of magnesium(II) and other divalent metal ions with adenosine 5′-triphosphate and 2,2′-dipyridylamine in aqueous solution

Binary and ternary systems involving adenosine 5′-triphosphate (ATP), 2,2′-dipyridylamine (DPA) and magnesium, calcium, strontium, manganese, cobalt, copper, and zinc(II) metal ions have been investigated in aqueous media by potentiometric titrations. The analysis of the titration curves shows the existence of M(ATP)²⁻, M(ATP)(H)⁻, and M(ATP)₂(H)₂⁴⁻ species for alkaline-earth metal ions, while no ternary complex can be detected. For transition metal ions both binary and ternary species are found. Binary M(ATP)₂(H)₂⁴⁻ complexes are present in solutions containing manganese and cobalt(II) metal ions but these species cannot be revealed in the case of copper and zinc(II). Ternary complexes as M(ATP)(DPA)²⁻ and M(ATP)(DPA)(H)⁻ are common to all transition metals. Binuclear and hydroxo complexes as M₂(ATP)(OH)⁻ and M(ATP)(OH)³⁻ are found only for copper and zinc(II). A hypothesis on the possible role of the species M-ATP in 1:2 ratio in the dephosphorylation mechanism is advanced on the basis of a comparison between the equilibrium data in the solution phase and the solid state structures of the magnesium, calcium, and manganese(II)- ATP-DPA systems.     

An integrated network analysis reveals that nitric oxide reductase prevents metabolic cycling of nitric oxide by Pseudomonas aeruginosa

Nitric oxide (NO) is a chemical weapon within the arsenal of immune cells, but is also generated endogenously by different bacteria. Pseudomonas aeruginosa are pathogens that contain an NO-generating nitrite (NO₂⁻) reductase (NirS), and NO has been shown to influence their virulence. Interestingly, P. aeruginosa also contain NO dioxygenase (Fhp) and nitrate (NO₃⁻) reductases, which together with NirS provide the potential for NO to be metabolically cycled (NO→NO₃⁻→NO₂⁻→NO). Deeper understanding of NO metabolism in P. aeruginosa will increase knowledge of its pathogenesis, and computational models have proven to be useful tools for the quantitative dissection of NO biochemical networks. Here we developed such a model for P. aeruginosa and confirmed its predictive accuracy with measurements of NO, O₂, NO₂⁻, and NO₃⁻ in mutant cultures devoid of Fhp or NorCB (NO reductase) activity. Using the model, we assessed whether NO was metabolically cycled in aerobic P. aeruginosa cultures. Calculated fluxes indicated a bottleneck at NO₃⁻, which was relieved upon O₂ depletion. As cell growth depleted dissolved O₂ levels, NO₃⁻ was converted to NO₂⁻ at near-stoichiometric levels, whereas NO₂⁻ consumption did not coincide with NO or NO₃⁻ accumulation. Assimilatory NO₂⁻ reductase (NirBD) or NorCB activity could have prevented NO cycling, and experiments with ΔnirB, ΔnirS, and ΔnorC showed that NorCB was responsible for loss of flux from the cycle. Collectively, this work provides a computational tool to analyze NO metabolism in P. aeruginosa, and establishes that P. aeruginosa use NorCB to prevent metabolic cycling of NO.     

Synthesis,characterization and DNA-binding properties of novel dipyridophenazine complex of ruthenium (II) : [Ru(IP)2(DPPZ)]2+

A novel ruthenium(II) complex of dipyridophenazine (DPPZ) with the ancillary ligand imidazole[4,5-f] [1,10]phenanthroline (IP), [Ru(IP)₂(DPPZ)] (PF₆)₂, has been synthesized and characterized by elemental analysis, 1D and 2D ¹H NMR, fast-atom bombardment mass spectra (FABMS), electronic spectroscopy and cyclic voltammetry. The DNA-binding properties of the complex were studied by spectroscopic methods. The intrinsic binding constant, K =2.1 × 10⁷M⁻¹, of the complex to calf thymus DNA has been determined by absorption titration in 5 mmol dm⁻³ Tris-HCl, 50 mmol dm⁻³ NaCl buffer (pH 7.0). The excited state lifetimes and luminescence quenching with [Fe(CN)₆]⁴⁻ as the quencher in the presence of DNA were also tested and mono-exponentiality was observed for the emission decay curves. Viscosity measurements together with the optical titrations unambiguously proved that the complex bound with DNA intercalatively and that the binding affinity to DNA was several times larger than that of the parent complex [Ru(bpy)₂(DPPZ)]²⁺.     

The high-affinity binding site for manganese on the oxidizing side of Photosystem II

Electron donation to Photosystem II (PS II) by diphenylcarbazide (DPC) is interrupted by the presence of endogenous Mn in PS II particles. Removal of this Mn by Tris treatment greatly stimulates the electron transport with DPC as donor. Binding of low concentration of exogenous Mn(II) to Tris-treated PS II particles inhibits DPC photooxidation competitively with DPC. This phenomenon was used to locate a highly specific Mn(II) binding site on the oxidizing side of Photosystem II with dissociation constant about 0.15 μM. The binding of Mn(II) is electrostatic in nature. Its affinity depends not only on the ionic strength, but also on the anion species of the salt in the medium. The effectiveness in decreasing the affinity follows the order F⁻ > SO²⁻₄ > CH₃COO⁻ > CI⁻ > Br⁻ > NO₃⁻. This observation is interpreted as follows: smaller ions, like F⁻, CH₃COO⁻, and larger ions, like SO²⁻₄, have inhibitory effects on Mn(II) binding, whereas ions with optimal size, like Cl⁻, Br⁻ and NO₃⁻, can stabilize the binding, resembling the anion requirement for reactivation of Cl⁻-depleted chloroplasts. We suggest that the binding site for Mn(II) we observed is the site for the endogenous Mn in the O₂-evolving complex of PS II. This site remains after Tris treatment, which removes all the endogenous Mn as well as the three extrinsic proteins, indicating that it is on the intrinsic component(s) of PS II reaction centers. Furthermore, the Cl⁻ requirement for O₂ evolution may be attributed, at least partly to its stabilizing effect on Mn binding.     

Electron-acceptor loadings affect chloroform dechlorination in a hydrogen-based membrane biofilm reactor

Chloroform (CF) can undergo reductive dechlorination to dichloromethane, chloromethane, and methane. However, competition for hydrogen (H₂), the electron-donor substrate, may cause poor dechlorination when multiple electron acceptors are present. Common acceptors in anaerobic environments are nitrate (NO₃⁻), sulfate (SO₄²⁻), and bicarbonate (HCO₃⁻). We evaluated CF dechlorination in the presence of HCO₃⁻ at 1.56 e⁻ Eq/m²-day, then NO₃⁻ at 0.04–0.15 e⁻ Eq/m²-day, and finally NO₃⁻ (0.04 e⁻ Eq/m²-day) along with SO₄²⁻ at 0.33 e⁻ Eq/m²-day in an H₂-based membrane biofilm reactor (MBfR). When the biofilm was initiated with CF-dechlorination conditions (no NO₃⁻ or SO₄²⁻), it yielded a CF flux of 0.14 e⁻ Eq/m²-day and acetate production via homoacetogenesis up to 0.26 e⁻ eq/m²-day. Subsequent addition of NO₃⁻ at 0.05 e⁻ Eq/m²-day maintained full CF dechlorination and homoacetogenesis, but NO₃⁻ input at 0.15 e⁻ Eq/m²-day caused CF to remain in the reactor's effluent and led to negligible acetate production. The addition of SO₄²⁻ did not affect CF reduction, but SO₄²⁻ reduction significantly altered the microbial community by introducing sulfate-reducing Desulfovibrio and more sulfur-oxidizing Arcobacter. Dechloromonas appeared to carry out CF dechlorination and denitrification, whereas Acetobacterium (homoacetogen) may have been involved with hydrolytic dechlorination. Modifications to the electron acceptors fed to the MBfR caused the microbial community to undergo changes in structure that reflected changes in the removal fluxes.     

Blue-light-induced pH changes associated with NO3−, NO2− and Cl− uptake by the green alga Monoraphidium braunii

In M. braunii, the uptake of NO₃⁻ and NO₂⁻ is blue-light-dependent and is associated with alkalinization of the medium. In unbuffered cell suspensions irradiated with red light under a CO₂-free atmosphere, the pH started to rise 10s after the exposure to blue light. When the cellular NO₃⁻ and NO₂⁻ reductases were active, the pH increased to values of around 10, since the NH₄⁺ generated was released to the medium. When the blue light was switched off, the pH stopped increasing within 60 to 90s and remained unchanged under background red illumination. Titration with H₂SO₄ of NO₃⁻ or NO₂⁻ uptake and reduction showed that two protons were consumed for every one NH₄⁺ released. The uptake of Cl⁻ was also triggered by blue light with a similar 10 s time response. However, the Cl⁻ -dependent alkalinization ceased after about 3 min of blue light irradiation. When the blue light was turned off, the pH immediately (15 to 30 s) started to decline to the pre-adjusted value, indicating that the protons (and presumably the Cl⁻) taken up by the cells were released to the medium. When the cells lacked NO₃⁻ and NO₂⁻ reductases, the shape of the alkalinization traces in the presence of NO₃⁻ and NO₂⁻ was similar to that in the presence of Cl⁻, suggesting that NO₃⁻ or NO₂⁻ was also released to the medium. Both the NO₃⁻ and Cl⁻-dependent rates of alkalinization were independent of mono- and divalent cations.     

Characterization of a proton pump from pea stem microsomes

Abstract The present work deals with the characterization of an ATP-dependent proton translocation monitored by the ΔpH probe acridine orange. The ATP-dependent proton translocation has an optimum activity at pH 6.5 and is substrate specific for ATP. It is stimulated by Cl⁻, HCO₃⁻ and Br⁻, but is insensitive to several monovalent cations. Divalent cations (Mg²⁺ or Mn²⁺) are required for proton translocation, while in the presence of Ca²⁺ no uptake is observed. NO₃⁻, NO₂⁻ and citrate strongly inhibit proton uptake. On the contrary, F⁻, SO₄²⁻, malate, pyruvate, succinate, oxalate and acetate have no inhibitory effect. Proton uptake is stimulated by valinomycin and unaffected by molybdate. Two thiols, dithioerythritol and dithiothreitol, are able partially to prevent the FCCP-abolished proton uptake or partially restore the ATP-dependent proton translocation in FCCP-collapsed vesicles. It is suggested that pea stem microsomes possess an electrogenic ATPase, acting as a proton pump, which, on the basis of its characteristics, can be tentatively associated with membranes of tonoplast origin.     

[RuIII(medtra)(H2O)] (medtra = N-methylethylenediaminetriacetate) complex – A highly efficient NO inhibitor with low toxicity

Stopped-flow kinetic measurements were used to compare the reactivities of [Ru(medtra)(H₂O)] (medtra³⁻ = N-methylethylenediaminetriacetate) (1) and [Ru(hedtra)(H₂O)] (2) (hedtra³⁻ = N-hydroxyethylethylenediaminetriacetate) with NO in aqueous solution at 15 °C, pH 7.2 (phosphate buffer). The measured second-order rate constants (3 × 10³ and 6 × 10⁴ M⁻¹ s⁻¹ for 1 and 2, respectively) are three to four order of magnitudes lower than that for the reaction between [Ru^III(edta)(H₂O)]⁻ (3) with NO. However, NO scavenging studies of complexes 1–3, conducted by measuring the difference in nitrite production between treated and untreated murine macrophage cells, revealed that despite being less kinetically reactive toward NO, the [Ru(medtra)(H₂O)] complex exhibited the highest NO scavenging ability and lowest toxicity of compounds 1–3.     

CoX2(NO)(PMe3)2 Complexes: an example of the influence of X (X = CI,Br, I,NO2) on the stereochemistry and electronic structure of the five-coordinate {CoNO}8 complexes

CoX₂(NO)(PMe₃)₂ complexes (X = Cl, Br, I, NO₂) exhibit markedly different ν(NO) stretching frequencies and different geometries. The structure of CoI₂(NO)(PMe₃)₂ (1) and CoCl₂(NO)(PMe₃)₂ (2) have been determined by X-ray diffraction. Both crystallize in the orthorhombic system, Pnma space group with four molecules in a cell of the following dimensions: for 1, a = 10.497(2), b = 10.694(2), c = 13.975(2) Å, ν= 1568.8, ų; for 2, a = 9.607(2), b = 10.689(2), c = 13.512(3) Å, ν= 1387.5 ų. The structures were refined to conventional R values of R = 0.040 from 1630 reflections for 1 and R = 0.033 from 976 reflections for 2. In both cases, the coordination geometry about the five-coordinate cobalt atom is approximately trigonal bipyramidal, with the NO group sharing the equatorial positions with the halide ligands. Structure 2 is disordered, which prevents any precise structural characterization. In (1), the CoNO angle is 179.2(19)° and the Co NO distance is 1.728(23) Å; v(NO) is 1753 cm⁻¹. CoCl₂(NO)(PMe₃)₃ shows a v(NO) vibration at 1637 cm⁻¹. Co(NO₂)₂(NO)(PMe₃)₂ with v(NO) = 1658 cm⁻¹ has been proposed as a square pyramidal structure with a bent apical CoNO. These differences in NO stretching frequencies and geometries are discussed.     

Terrestrial nitrogen cycle simulation with a dynamic global vegetation model

A global scale Dynamic Nitrogen scheme (DyN) has been developed and incorporated into the Lund–Posdam–Jena (LPJ) dynamic global vegetation model (DGVM). The DyN is a comprehensive process‐based model of the cycling of N through and within terrestrial ecosystems, with fully interactive coupling to vegetation and C dynamics. The model represents the uptake, allocation and turnover of N in plants, and soil N transformations including mineralization, N₂ fixation, nitrification and denitrification, NH₃ volatilization, N leaching, and N₂, N₂O and NO production and emission. Modelled global patterns of site‐scale nitrogen fluxes and reservoirs are highly correlated to observations reported from different biomes. The simulation of site‐scale net primary production and soil carbon content was improved relative to the original LPJ, which lacked an interactive N cycle, especially in the temporal and boreal regions. Annual N uptake by global natural vegetation was simulated as 1.084 Pg N yr⁻¹, with lowest values <1 g N m⁻² yr⁻¹ (polar desert) and highest values in the range 24–36.5 g N m⁻² yr⁻¹ (tropical forests). Simulated global patterns of annual N uptake are consistent with previous model results by Melillo et al. The model estimates global total nitrogen storage potentials in vegetation (5.3 Pg N), litter (4.6 Pg N) and soil (≥67 Pg as organic N and 0.94 Pg as inorganic N). Simulated global patterns of soil N storage are consistent with the analysis by Post et al. although total simulated N storage is less. Deserts were simulated to store 460 Tg N (up to 0.262 kg N m⁻²) as NO₃⁻, contributing 80% of the global total NO₃⁻ inventory of 580 Tg N. This model result is in agreement with the findings of a large NO₃⁻ pool beneath deserts. Globally, inorganic soil N is a small reservoir, comprising only 1.6% of the global soil N content to 1.5 m soil depth, but the ratio has a very high spatial variability and in hot desert regions, inorganic NO₃⁻ is estimated to be the dominant form of stored N in the soil.     

Synthesis and spectroscopic studies of platinum(II) complexes of N,N′-dicyclohexylethylenediamine

The platinum(II) complexes of the formula [Pt(DCHEDA)X₂], where DCHEDA is N,N′-dicyclohexylethylenediamine and X⁻ is CL⁻, Br⁻, I⁻, 0.5C₂O₄²⁻ (oxalate), 0.5C₃H₂O₄²⁻ (malonate), 0.5C₉H₄O₆²⁻ (4-carboxyphthalate), 0.5S₂O₃²⁻ or 0.5SO₄²⁻, have been synthesized and characterized by UVVis, IR, and ¹H NMR spectral techniques. All the above complexes are non-electrolytes in DMF/H₂O, except the sulphate complex which becomes a 1:1 electrolyte after incubation for 24 h at 28 °C. The halide complexes were also studied by X-ray photoelectron spectroscopy and these data suggest that there is π-bonding from platinum to halide in these complexes. The oxalate, malonate and sulphate bind in their complexes as bidentate ligands to platinum through two oxygen atoms whereas the thiosulphate in its complex binds as a bidentate ligand to platinum through one oxygen atom and one sulphur atom.     

Hydrologic regulation of gross methyl chloride and methyl bromide uptake from Alaskan Arctic tundra

The Arctic tundra has been shown to be a potentially significant regional sink for methyl chloride (CH₃Cl) and methyl bromide (CH₃Br), although prior field studies were spatially and temporally limited, and did not include gross flux measurements. Here we compare net and gross CH₃Cl and CH₃Br fluxes in the northern coastal plain and continental interior. As expected, both regions were net sinks for CH₃Cl and CH₃Br. Gross uptake rates (−793 nmol CH₃Cl m⁻² day⁻¹ and −20.3 nmol CH₃Br m⁻² day⁻¹) were 20–240% greater than net fluxes, suggesting that the Arctic is an even greater sink than previously believed. Hydrology was the principal regulator of methyl halide flux, with an overall trend towards increasing methyl halide uptake with decreasing soil moisture. Water table depth was one of the best predictors of net and gross uptake, with uptake increasing proportionately with water table depth. In drier areas, gross uptake was very high, averaging −1201 nmol CH₃Cl m⁻² day⁻¹ and −34.9 nmol CH₃Br m⁻² day⁻¹; in flooded areas, gross uptake was significantly lower, averaging −61 nmol CH₃Cl m⁻² day⁻¹ and −2.3 nmol CH₃Br m⁻² day⁻¹. Net and gross uptake was greater in the continental interior than in the northern coastal plain, presumably due to drier inland conditions. Within certain microtopographic features (low‐ and high‐centered polygons), uptake rates were positively correlated with soil temperature, indicating that temperature played a secondary role in methyl halide uptake. Incubations suggested that the inverse relationship between water content and methyl halide uptake was the result of mass transfer limitation in saturated soils, rather than because of reduced microbial activity under anaerobic conditions. These findings have potential regional significance, as the Arctic is expected to become warmer and drier due to anthropogenic climate forcing, potentially enhancing the Arctic sink for CH₃Cl and CH₃Br.     

Metal Ion-Biomolecule Interactions. VIII: Methylmercury(II) Complexes of 8-Thioguanosine. Synthesis and Spectroscopic Investigations

The reaction of 8-thioguanosine (8-thioGuo^H₂ with methylmercury(II) has been shown to give rise to 1:1 (neutral and cationic), 1:2 (neutral and cationic), and 1:3 (cationic) complexes of the type [CH₃Hg(8-thioGuoH)], [(CH₃Hg(8-thioGuoH₂)]NO₃, [(CH₃Hg)₂(8-thioGuo)], [(CH₃Hg)₂(8-thioGuoH)]NO₃ and [(CH₃Hg)₃(8-thioGuo)]NO₃, depending upon the reactant stoichiometry and pH. ¹H NMR, ¹³C NMR, and IR, as well as analytical data were used to characterize the complexes. Coupling of methylmercury(II)-protons to mercury-199 has been observed in all compounds. The magnitude of the coupling, ²J(¹H-¹⁹⁹Hg), is strongly dependent on the nature of the ligand bonded to the methylmercury(II) group and correlates with the ¹³C chemical shifts of coordinated CH₃Hg(II) at the different binding sites.     

The Cu/ligand stoichiometry effect on the coordination behavior of aroyl hydrazone with copper(II): Structure,anticancer activity and anticancer mechanism

In an effort to better understand the biological efficacy of the tridentate aroyl hydrazone Cu(II) complexes, three Cu(II) complexes of acetylpyridine benzoyl hydrazone (HL), [Cu(L)(NO₃) (H₂O)]·H₂O (C1), [Cu(L)₂] (C2) and [Cu(L)(HL)]·(NO₃)(Sas) (C3) (Sas = salicylic acid) were synthesized and characterized. X-ray crystal structures and infrared (IR) spectra of the complexes reveal that the L⁻ ligand of C1 and C2 are predominantly in the enolate resonance form, while one L⁻ ligand in C3 is represented enolate resonance form and the other HL ligand exhibits keto resonance form. All Cu(II) complexes showed significantly more anticancer activity than the ligand alone. Interestingly, the Cu complexes where the ligand/metal ratio was 1:1 (C1) rather than 2:1 (C2 and C3) had higher antitumor efficacy. Moreover, the 1:1 Cu/ligand complex, C1, promotes A549 cell apoptosis possibly through the intrinsic reactive oxygen species (ROS) mediated mitochondrial pathway, accompanied by the regulation of Bcl-2 family proteins.     

The effect of nutrient concentrations,nutrient ratios and temperature on photosynthesis and nutrient uptake by Ulva prolifera: implications for the explosion in green tides

The green-tide macroalga, Ulva prolifera, was tested in the laboratory to determine its nutrient uptake and photosynthesis under different conditions. In the nutrient concentration experiments U. prolifera showed a saturated uptake for nitrate but an escalating uptake in the tested range for phosphorus. Both N/P and NO₃ ^?/NH₄ ⁺ ratios influenced nutrient uptake significantly (p?<?0.05) while the PSII quantum yield [Y(II)] (p?>?0.05) remained unaffected. The maximum N uptake rate (33.9?±?0.8 μmol g^?1 DW h^?1) and P uptake rate (11.1?±?4.7) was detected at N/P ratios of 7.5 and 2.2, respectively. U. prolifera preferred NH₄ ⁺-N to NO₃ ^?-N when the NO₃ ^?-N/NH₄ ⁺-N ratio was less than 2.2 (p?<?0.05). But between ratios of 2.2 and 12.9, the uptake of NO₃ ^?-N surpassed that of NH₄ ⁺-N. In the temperature experiments, the highest N uptake rate and [Y(II)] were observed at 20 °C, while the lowest rates were detected at 5 °C. P uptake rates were correlated with increasing temperature.     

Effect of lipophilicity of amylamine and amylglycine ligands on biological activity of new anticancer cisplatin analog

Investigation of side effects and solubility of anticancer drugs is a major challenge in chemotherapy science. Thus, design and synthesis of cisplatin analogs with higher lipophilicity as novel water-soluble anticancer drugs is valuable. In this work, two new Pt(II) complexes were synthesized with formula cis-[Pt(NH₃)₂(amylgly)]NO₃ and cis-[Pt(amylamine)₂(amylgly)]NO₃, where gly is penthyl glycine as an amino acid. The new compounds were synthesized and extensively characterized using analytical techniques; spectroscopic methods, and conductivity measurement. The anticancer activity of synthesized complexes was investigated against colon cancer cell line HCT116 using MTT assay and results showed excellent anticancer activity with Cc₅₀ values of 36 and 270 M after 24-h incubation time for cis-[Pt(NH₃)₂(amylgly)]NO₃ and cis-[Pt(NH₂-amyl)₂(amylgly)]NO₃, respectively; which is lower than that for cisplatin. These complexes were also interacted with highly polymerized calf thymus DNA and the binding mode of the complexes to CT-DNA was evaluated by fluorescence, circular dichroism, and UV spectroscopy. The calculation of binding and thermodynamic of Pt(II) complexes with CT-DNA can provide deeper insight into mechanism of the action of these types of complexes with nucleic acids. So, thermodynamic parameters were also determined according to isothermal titration. In comparison with cis-[Pt(NH₃)₂(amylgly)]NO₃ in DNA interaction, the result show that cis-[Pt(NH₂-amyl)₂(amylgly)]NO₃ has higher affinity with binding constant K_f = 8.72 mM to CT-DNA. The results indicate that cis-[Pt(amylamine)₂(amylgly)]NO₃ with large and bulky aliphatic group bind to CT-DNA by different modes and covalent and groove bindings were preferred mode of interaction with DNA.