996 resultados para Isolated carbonate platforms


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Signaling cascades initiated by Wnt lipoglycoproteins and their receptors of the Frizzled family regulate many aspects of animal development and physiology. Improper activation of this signaling promotes carcinogenic transformation and metastasis. Development of agents blocking the Wnt-Frizzled signaling is of prime interest for drug discovery. Despite certain progress no such agents are as yet brought to the market or even to clinical trials. One reason for these delays might be the use of suboptimal readout assays. In this article we overview existing and developing assay platforms to screen for Wnt-Frizzled antagonists. Among those, G protein-activating assays built on the emerging GPCR properties of Frizzleds are highlighted.

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The objective of this work was to characterize the genetic variability of phytoplasma and Spiroplasma kunkelii isolated from maize plants showing symptoms of stunt collected from different Brazilian geographic regions. A DNA fragment of 500 base pairs (bp) was amplified from the spiralin gene in S. kunkelii and one fragment of 1,200 bp was generated from 16S rDNA gene in phytoplasma. The partial sequences of the spiralin gene showed similarity of 98% among the isolates of S. kunkelii analyzed. These sequences were compared with the sequence of the spiralin gene from other Spiroplasma species deposited in the GenBank, resulting in a similarity varying from 76.9% to 88.1%. The 16S rDNA sequence from the phytoplasma were completely similar within the Brazilian isolates and showed up to 98% of the similarity with sequences already found from other phytoplasmas. A very narrow genetic variability was detected by these gene fragments within phytoplasma and Spiroplasma analyzed. However, other genomic regions with higher polymorphic levels shall be identified in order to better evaluate the genetic diversity within these microorganisms population.

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Atrial septal defects (ASDs) are typically asymptomatic in infancy and early childhood, and elective defect closure is usually performed at ages of 4 to 6 years. Severe pulmonary hypertension (PH) complicating an ASD is seen in adulthood and has only occasionally been reported in small children. A retrospective study was undertaken to evaluate the incidence of severe PH complicating an isolated ASD and requiring early surgical correction. During a 10-year period (1996 to 2006), 355 pediatric patients underwent treatment for isolated ASDs either surgically or by catheter intervention at 2 tertiary referral centers. Two hundred ninety-seven patients had secundum ASDs, and 58 had primum ASDs with mild to moderate mitral regurgitation. Eight infants were found with isolated ASDs (6 with secundum ASDs and 2 with primum ASDs) associated with significant PH, accounting for 2.2% of all patients with ASDs at the centers. These 8 infants had invasively measured pulmonary artery pressures of 50% to 100% of systemic pressure. They were operated in the first year of life and had complicated postoperative courses requiring specific treatment for PH for up to 16 weeks postoperatively. The ultimate outcomes in all 8 infants were good, with persistent normalization of pulmonary pressures during midterm follow-up of up to 60 months (median 28). All other patients with ASDs had normal pulmonary pressures, and the mean age at defect closure was significantly older, at 6.2 years for secundum ASDs and 3.2 years for primum ASDs. In conclusion, ASDs were rarely associated with significant PH in infancy but then required early surgery and were associated with excellent midterm outcomes in these patients.

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HR-116 is concerned with the relationship of carbonate aggregate to aging of highway concrete. The ultimate purpose of the research is to provide the Materials Department with better criteria for selection of carbonate aggregates for use in highway concrete. The research stems from the problem in Iowa which relates durability of highway concrete to use of certain aggregates. Service records of certain highways have shown that concrete deterioration is related to the source of coarse carbonate aggregate. Research on this problem in projects HR-15 and HR-86 helped define three broad areas of the problem in more detail: 1. The problem of evaluation of rocks which pass current specifications but have poor service records 2. The basic problem of how rocks contribute to distress in concrete 3. The problem of how concrete ages or weathers.

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The major objective of this research project was to use thermal analysis techniques in conjunction with x-ray analysis methods to identify and explain chemical reactions that promote aggregate related deterioration in portland cement concrete. Twenty-two different carbonate aggregate samples were subjected to a chemical testing scheme that included: • bulk chemistry (major, minor and selected trace elements) • bulk mineralogy (minor phases concentrated by acid extraction) • solid-solution in the major carbonate phases • crystallite size determinations for the major carbonate phases • a salt treatment study to evaluate the impact of deicer salts Test results from these different studies were then compared to information that had been obtained using thermogravimetric analysis techniques. Since many of the limestones and dolomites that were used in the study had extensive field service records it was possible to correlate many of the variables with service life. The results of this study have indicated that thermogravimetric analysis can play an important role in categorizing carbonate aggregates. In fact, with modern automated thermal analysis systems it should be possible to utilize such methods on a quality control basis. Strong correlations were found between several of the variables that were monitored in this study. In fact, several of the variables exhibited significant correlations to concrete service life. When the full data set was utilized (n = 18), the significant correlations to service life can be summarized as follows ( a = 5% level): • Correlation coefficient, r, = -0.73 for premature TG loss versus service life. • Correlation coefficient, r, = 0.74 for relative crystallite size versus service life. • Correlation coefficient, r, = 0.53 for ASTM C666 durability factor versus service life. • Correlation coefficient, r, = -0.52 for acid-insoluble residue versus service life. Separation of the carbonate aggregates into their mineralogical categories (i.e., calcites and dolomites) tended to increase the correlation coefficients for some specific variables (r sometimes approached 0.90); however, the reliability of such correlations was questionable because of the small number of samples that were present in this study.

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The distribution and diversity of acidophilic bacteria of a tailings impoundment at the La Andina copper mine, Chile, was examined. The tailings have low sulfide (1.7% pyrite equivalent) and carbonate (1.4% calcite equivalent) contents and are stratified into three distinct zones: a surface (0-70-80 cm) `oxidation zone' characterized by low-pH (2.5-4), a `neutralization zone' (70-80 to 300-400 cm) and an unaltered `primary zone' below 400 cm. A combined cultivation-dependent and biomolecular approach (terminal restriction enzyme fragment length polymorphism and 16S rRNA clone library analysis) was used to characterize the indigenous prokaryotic communities in the mine tailings. Total cell counts showed that the microbial biomass was greatest in the top 125 cm of the tailings. The largest numbers of bacteria (10(9) g(-1) dry weight of tailings) were found at the oxidation front (the junction between the oxidation and neutralization zones), where sulfide minerals and oxygen were both present. The dominant iron-/sulfur-oxidizing bacteria identified at the oxidation front included bacteria of the genus Leptospirillum (detected by molecular methods), and Gram-positive iron-oxidizing acidophiles related to Sulfobacillus (identified both by molecular and cultivation methods). Acidithiobacillus ferrooxidans was also detected, albeit in relatively small numbers. Heterotrophic acidophiles related to Acidobacterium capsulatum were found by molecular methods, while another Acidobacterium-like bacterium and an Acidiphilium sp. were isolated from oxidation zone samples. A conceptual model was developed, based on microbiological and geochemical data derived from the tailings, to account for the biogeochemical evolution of the Piuquenes tailings impoundment.

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The Iowa Pore Index (IPI) measures the pore system of carbonate (limestone and dolomite) rocks using pressurized water to infiltrate the pore system. This technique provides quantitative results for the primary and capillary (secondary) pores in carbonate rocks. These results are used in conjunction with chemical and mineralogical test results to calculate a quality number, which is used as a predictor of aggregate performance in Portland cement concrete (PCC) leading to the durability classification of the aggregate. This study had two main objectives: to determine the effect different aggregate size has on IPI test results and to establish the precision of IPI test and test apparatus. It was found that smaller aggregate size fractions could be correlated to the standard 1/2”-3/4” size sample. Generally, a particle size decrease was accompanied by a slight decrease in IPI values. The IPI testing also showed fairly good agreement of the secondary pore index number between the 1/2”-3/4”and the 3/8”-1/2” fraction. The #4-3/8” showed a greater difference of the secondary number from the 1/2”-3/4” fraction. The precision of the IPI test was established as a standard deviation (Sr) of 2.85 (Primary) and 0.87 (Secondary) with a repeatability limit (%r) of 8.5% and 14.9% for the primary and secondary values, respectively.

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Polyphosphate (iPOP) is a linear polymer of orthophosphate units linked together by high energy phosphoanhydride bonds. It is found in all organisms, localized in organelles called acidocalcisomes and ranges from a few to few hundred monomers in length. iPOP has been found to play a vast array of roles in all organisms, including phosphate and energy metabolism, regulation of enzymes, virulence, pathogenicity, bone remodelling and blood clotting, among many others. Recently it was found that iPOP levels were increased in myeloma cells. The growing interest in iPOP in human cell lines makes it an interesting molecule to study. However, not much is known about its metabolism in eukaryotes. Acidocalcisomes are electron dense, acidic organelles that belong to the group of Lysosome Related Organelles (LROs). The conservation of acidocalcisomes among all kingdoms of life is suggestive of their important roles for the organisms. However, they are difficult to analyse because of limited biochemical tools for investigation. Yeast vacuoles present remarkable similarities to acidocalcisomes in terms of their physiological and structural features, including synthesis and storage of iPOP, which make them an ideal candidate to study biological processes which are shared between vacuoles and acidocalcisomes. The availability of tools for genetic manipulation and isolation of vacuoles makes yeast a candidate of choice for the characterization of iPOP synthesis in eukaryotes. Our group has identified the Vacuolar Transporter Chaperone (VTC) complex as iPOP polymerase and identified the catalytic subunit (Vtc4). The goal of my study was to characterize the process of iPOP synthesis by isolated vacuoles and to reconstitute iPOP synthesis in liposomes. The first step was to develop a method for monitoring iPOP by isolated vacuoles over time and comparing it with previously known methods. Next, a detailed characterization was performed to determine the modulators of the process, both for intact as well as solubilized vacuoles. Finally, attempts were made to purify the VTC complex and reconstitute it in liposomes. A parallel line of study was the translocation and storage of synthesized iPOP in the lumen of the vacuoles. As a result of this study, it is possible to determine distinct pools of iPOP- inside and outside the vacuolar lumen. Additionally, I establish that the vacuolar lysate withstands harsh steps during reconstitution on liposomes and retains iPOP synthesizing activity. The next steps will be purification of the intact VTC complex and its structure determination by cryo-electron microscopy. - Les organismes vivants sont composés d'une ou plusieurs cellules responsables des processus biologiques élémentaires tels que la digestion, la respiration, la synthèse et la reproduction. Leur environnement interne est en équilibre et ils réalisent un très grand nombre de réactions chimiques et biochimiques pour maintenir cet équilibre. A différents compartiments cellulaires, ou organelles, sont attribuées des tâches spécifiques pour maintenir les cellules en vie. L'étude de ces fonctions permet une meilleure compréhension de la vie et des organismes vivants. De nombreux processus sont bien connus et caractérisés mais d'autres nécessitent encore des investigations détaillées. L'un de ces processus est le métabolisme des polyphosphates. Ces molécules sont des polymères linéaires de phosphate inorganique dont la taille peut varier de quelques dizaines à quelques centaines d'unités élémentaires. Ils sont présents dans tous les organismes, des bactéries à l'homme. Ils sont localisés principalement dans des compartiments cellulaires appelés acidocalcisomes, des organelles acides observés en microscopie électronique comme des structures denses aux électrons. Les polyphosphates jouent un rôle important dans le stockage et le métabolisme de l'énergie, la réponse au stress, la virulence, la pathogénicité et la résistance aux drogues. Chez l'homme, ils sont impliqués dans la coagulation du sang et le remodelage osseux. De nouvelles fonctions biologiques des polyphosphates sont encore découvertes, ce qui accroît l'intérêt des chercheurs pour ces molécules. Bien que des progrès considérables ont été réalisés afin de comprendre la fonction des polyphosphates chez les bactéries, ce qui concerne la synthèse, le stockage et la dégradation des polyphosphates chez les eucaryotes est mal connu. Les vacuoles de la levure Saccharomyces cerevisiae sont similaires aux acidocalcisomes des organismes supérieurs en termes de structure et de fonction. Les acidocalcisomes sont difficiles à étudier car il n'existe que peu d'outils génétiques et biochimiques qui permettent leur caractérisation. En revanche, les vacuoles peuvent être aisément isolées des cellules vivantes et manipulées génétiquement. Les vacuoles comme les acidocalcisomes synthétisent et stockent les polyphosphates. Ainsi, les découvertes faites grâce aux vacuoles de levures peuvent être extrapolées aux acidocalcisomes des organismes supérieurs. Le but de mon projet était de caractériser la synthèse des polyphosphates par des vacuoles isolées. Au cours de mon travail de thèse, j'ai mis au point une méthode de mesure de la synthèse des polyphosphates par des organelles purifés. Ensuite, j'ai identifié des composés qui modulent la réaction enzymatique lorsque celle-ci a lieu dans la vacuole ou après solubilisation de l'organelle. J'ai ainsi pu mettre en évidence deux groupes distincts de polyphosphates dans le système : ceux au-dehors de la vacuole et ceux en-dedans de l'organelle. Cette observation suggère donc très fortement que les vacuoles non seulement synthétisent les polyphosphates mais aussi transfère les molécules synthétisées de l'extérieur vers l'intérieur de l'organelle. Il est très vraisemblable que les vacuoles régulent le renouvellement des polyphosphates qu'elles conservent, en réponse à des signaux cellulaires. Des essais de purification de l'enzyme synthétisant les polyphosphates ainsi que sa reconstitution dans des liposomes ont également été entrepris. Ainsi, mon travail présente de nouveaux aspects de la synthèse des polyphosphates chez les eucaryotes et les résultats devraient encourager l'élucidation de mécanismes similaires chez les organismes supérieurs. - Les polyphosphates (iPOP) sont des polymères linéaires de phosphates inorganiques liés par des liaisons phosphoanhydres de haute énergie. Ces molécules sont présentes dans tous les organismes et localisées dans des compartiments cellulaires appelés acidocalcisomes. Elles varient en taille de quelques dizaines à quelques centaines d'unités phosphate. Des fonctions nombreuses et variées ont été attribuées aux iPOP dont un rôle dans les métabolismes de l'énergie et du phosphate, dans la régulation d'activités enzymatiques, la virulence, la pathogénicité, le remodelage osseux et la coagulation sanguine. Il a récemment été montré que les cellules de myélome contiennent une grande quantité de iPOP. Il y donc un intérêt croissant pour les iPOP dans les lignées cellulaires humaines. Cependant, très peu d'informations sur le métabolisme des iPOP chez les eucaryotes sont disponibles. Les acidocalcisomes sont des compartiments acides et denses aux électrons. Ils font partie du groupe des organelles similaires aux lysosomes (LROs pour Lysosome Related Organelles). Le fait que les acidocalcisomes soient conservés dans tous les règnes du vivant montrent l'importance de ces compartiments pour les organismes. Cependant, l'analyse de ces organelles est rendue difficile par l'existence d'un nombre limité d'outils biochimiques permettant leur caractérisation. Les vacuoles de levures possèdent des aspects structuraux et physiologiques très similaires à ceux des acidocalcisomes. Par exemple, ils synthétisent et gardent en réserve les iPOP. Ceci fait des vacuoles de levure un modèle idéal pour l'étude de processus biologiques conservés chez les vacuoles et les acidocalcisomes. De plus, la levure est un organisme de choix pour l'étude de la synthèse des iPOP compte-tenu de l'existence de nombreux outils génétiques et la possibilité d'isoler des vacuoles fonctionnelles. Notre groupe a identifié le complexe VTC (Vacuole transporter Chaperone) comme étant responsable de la synthèse des iPOP et la sous-unité Vtc4p comme celle possédant l'activité catalytique. L'objectif de cette étude était de caractériser le processus de synthèse des iPOP en utilisant des vacuoles isolées et de reconstituer la synthèse des iPOP dans des liposomes. La première étape a consisté en la mise au point d'un dosage permettant la mesure de la quantité de iPOP synthétisés par les organelles isolés en fonction du temps. Cette nouvelle méthode a été comparée aux méthodes décrites précédemment dans la littérature. Ensuite, la caractérisation détaillée du processus a permis d'identifier des composés modulateurs de la réaction à la fois pour des vacuoles intactes et des vacuoles solubilisées. Enfin, des essais de purification du complexe VTC et sa reconstitution dans des liposomes ont été entrepris. De façon parallèle, une étude sur la translocation et le stockage des iPOP dans le lumen des vacuoles a été menée. Il a ainsi été possible de mettre en évidence différents groupes de iPOP : les iPOP localisés à l'intérieur et ceux localisés à l'extérieur des vacuoles isolées. De plus, nous avons observé que le lysat vacuolaire n'est pas détérioré par les étapes de reconstitution dans les liposomes et conserve l'activité de synthèse des iPOP. Les prochaines étapes consisteront en la purification du complexe intact et de la détermination de sa structure par cryo-microscopie électronique.

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Aim:Isolated limb perfusion (ILP) is a technique consisting in administrating doses of chemotherapy up to 20 times higher than via systemic route in a limb affected by melanoma or sarcoma to maximise tumour reduction. ILP is performed in <50 centres worldwide and leads to partial or complete response, however without effect on overall survival. As an alternative to amputation, it improves patient quality of life. We report our >10-year single centre experience on the role of nuclear medicine in ILP. Material and method:From 2000 to 2012, we performed 77 ILP (45 women, 32 men; aged 62±16 years) for 49 melanoma (64%), 25 sarcoma (32%) and 3 others tumors (2 desmoid tumours and 1 aggressive fibromatosis) (3%). The affected limb vascularisation is isolated from the systemic circulation (SYS) using extracorporeal circulation, and chemotherapy (usually TNF and Melphalan) is administered. Peroperatively, limb isolation and eventual leakage from ILP to SYS are monitored by continuous measurement using a gamma-probe placed over the heart (150MBq of 99mTc-human serum albumin in ILP and 4MBq in SYS). The maximum acceptable leakage to the systemic circulation is 10% (maximum tolerated systemic TNF dose). Results:In total, 47 patients (61%) had positive leaks from the ILP to SYS of 4.1±14.5% (median 1% interquartile range 0.4% to 3.2%, range 0 to 100%) and 30 patients (39%) had negative leaks from the SYS to ILP of -0.9±1.2% (median -0.5%, interquartile range -0.8% to -0.2%, range -4.8% to -0.1%). In only 2 patients (2.6%), leaks >10% were observed leading to interrupting ILP. Conclusion:Nuclear Medicine has a crucial role for the safety and quality of ILP in monitoring leakage peroperatively and help deciding whether the procedure should be interrupted to minimize systemic toxicity.

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We report magnetic and magneto-optical measurements of two Mn12 single-molecule magnet derivatives isolated in organic glasses. Field-dependent magnetic circular dichroism (MCD) intensity curves (hysteresis cycles) are found to be essentially identical to superconducting quantum interference device magnetization results and provide experimental evidence for the potential of the optical technique for magnetic characterization. Optical observation of magnetic tunneling has been achieved by studying the decay of the MCD signal at weak applied magnetic field

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Organic geochemical and stable isotope investigations were performed to provide an insight into the depositional environments, origin and maturity of the organic matter in Jurassic and Cretaceous formations of the External Dinarides. A correlation is made among various parameters acquired from Rock-Eval, gas chromatography-mass spectrometry data and isotope analysis of carbonates and kerogen. Three groups of samples were analysed. The first group includes source rocks derived from Lower Jurassic limestone and Upper Jurassic ``Leme'' beds, the second from Upper Cretaceous carbonates, while the third group comprises oil seeps genetically connected with Upper Cretaceous source rocks. The carbon and oxygen isotopic ratios of all the carbonates display marine isotopic composition. Rock-Eval data and maturity parameter values derived from biomarkers define the organic matter of the Upper Cretaceous carbonates as Type I-S and Type II-S kerogen at the low stage of maturity up to entering the oil-generating window. Lower and Upper Jurassic source rocks contain early mature Type III mixed with Type IV organic matter. All Jurassic and Cretaceous potential source rock extracts show similarity in triterpane and sterane distribution. The hopane and sterane distribution pattern of the studied oil seeps correspond to those from Cretaceous source rocks. The difference between Cretaceous oil seeps and potential source rock extracts was found in the intensity and distribution of n-alkanes, as well as in the abundance of asphaltenes which is connected to their biodegradation stage. In the Jurassic and Cretaceous potential source rock samples a mixture of aromatic hydrocarbons with their alkyl derivatives were indicated, whereas in the oil seep samples extracts only asphaltenes were observed.

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The Jebel Ressas Pb-Zn deposits in North-Eastern Tunisia occur mainly as open-space fillings (lodes, tectonic breccia cements) in bioclastic limestones of the Upper Jurassic Ressas Formation and along the contact of this formation with Triassic rocks. The galena-sphalerite association and their alteration products (cerussite, hemimorphite, hydrozincite) are set within a calcite gangue. The Triassic rocks exhibit enrichments in trace metals, namely Pb, Co and Cd enrichment in clays and Pb, Zn, Cd, Co and Cr enrichment in carbonates, suggesting that the Triassic rocks have interacted with the ore-bearing fluids associated with the Jebel Ressas Pb-Zn deposits. The delta(18)O content of calcite associated with the Pb-Zn mineralization suggests that it is likely to have precipitated from a fluid that was in equilibrium with the Triassic dolostones. The delta(34)S values in galenas from the Pb-Zn deposits range from -1.5 to +11.4%, with an average of 5.9% and standard deviation of 3.9%. These data imply mixing of thermochemically-reduced heavy sulfur carried in geothermal- and fault-stress-driven deep-seated source fluid with bacterially-reduced light sulfur carried in topography-driven meteoric fluid. Lead isotope ratios in galenas from the Pb-Zn deposits are homogenous and indicate a single upper crustal source of base-metals for these deposits. Synthesis of the geochemical data with geological data suggests that the base-metal mineralization at Jebel Ressas was formed during the Serravallian-Tortonian (or Middle-Late Miocene) Alpine compressional tectonics.

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A geophysical and geochemical study has been conducted in a fractured carbonate aquifer located at Combioula in the southwestern Swiss Alps with the objective to detect and characterize hydraulically active fractures along a 260-m-deep borehole. Hydrochemical analyses, borehole diameter, temperature and fluid electrical conductivity logging data were integrated in order to relate electrokinetic self-potential signals to groundwater flow inside the fracture network. The results show a generally good, albeit locally variable correlation of variations of the self-potential signals with variations in temperature, fluid electrical conductivity and borehole diameter. Together with the hydrochemical evidence, which was found to be critical for the interpretation of the self-potential data, these measurements not only made it possible to detect the hydraulically active fractures but also to characterize them as zones of fluid gain or fluid loss. The results complement the available information from the corresponding litholog and illustrate the potential of electrokinetic self-potential signals in conjunction with temperature, fluid electrical conductivity and hydrochemical analyses for the characterization of fractured aquifers, and thus may offer a perspective for an effective quantitative characterization of this increasingly important class of aquifers and geothermal reservoirs.