Geoquímica de elementos maiores e traços de granitoides neoproterozoicos da província Borborema e sua correlação com propriedades físicas de rochas

This paper discusses the correlation of thermal conductivity, density and magnetic susceptibility with composition of major and trace elements of Neoproterozoic igneous bodies from Borborema Province, Northeastern Brazil. These properties were used as potential markers among the studied magmatic suites. For the correlation between petrophysical and geochemical properties it was considered a set of 195 chemical analyzes of granitoid rocks, separated by the degree of acidity in basic, intermediate and acidic. Major (SiO2, Al2O3, Fe2O3, MgO, CaO, Na2O, K2O and TiO2) and some trace elements (Rb, Sr, Ba, Zr, Th and U) that are usually linked to the formation of the most common minerals of igneous rocks were used. The results show that SiO2 has the best positive correlation with the thermal conductivity, while Al2O3, CaO, Fe2O3, MgO and TiO2 exhibit negative correlation for the same property. The correlation with density is opposite to that one for these oxides with the thermal conductivity. The magnetic susceptibility did not correlate with the elements studied. The results for thermal conductivity and density indicate a tendency of SiO2 and oxides with higher affinity with mafic minerals (Al2O3, CaO, Fe2O3, TiO2 and MgO) in controlling these petrophysical parameters. The set of samples was divided into five different magmatic suites based on their lithogeochemical aspects into: i) peralkaline / alkaline; ii) alkaline; iii) calc-alkaline; iv) high potassium calcium alkaline; and v) shoshonitic. Data analysis showed that the thermal conductivity and density presented good results in the individualization of these suites, notably between peralkaline / alkaline, alkaline suites, calc-alkaline and shoshonitic. However, the high-K calc-alkaline suite overlapped with the other. In contrast, the magnetic susceptibility did not show effective results for separating the five chemical suites.

Extração, caracterização e prospecção de atividades farmacológicas de polissacarídeos sulfatados da macroalga verde Caulerpa prolifera

This study aimed to extract, characterize and conduct a prospective analysis of pharmacological activities of sulfated polysaccharides from green seaweed Caulerpa prolifera. Seven fractions (CP-0.3/CP-0.5/CP-0.7/CP-0.9/CP-1.1/CP-1.5/CP-2.0) were obtained from C. prolifera by alkaline proteolysis followed by sequential precipitation in acetone. The physicochemical analyzes indicated that C. prolifera synthesizes a homogalactan (CP-0.9) and different populations of sulfated heteropolysaccharides. In the analysis of anticoagulant activity, all fractions except CP-0.3, influenced the intrinsic coagulation pathway. All fractions showed antioxidant activity in six different assays being more pronounced in hydrogen peroxide scavenging assay, especially CP-0.3, CP-0.7 and CP-0.9 (which obtained 61% of hydrogen peroxide scavenging), in ferric chelation assay (especially CP-0.9 with 56% chelation) and cupric chelation assay (especially CP-2.0 with 78% chelation). With respect to immunomodulatory activity, the presence of CP-0.3, CP-0.7 and CP-0.9 showed an immunogenic potential, increasing the production of nitric oxide (NO) by 48, 142 and 163 times, respectively. Conversely, the NO synthesis fell 73% after the activation of macrophages by LPS, incubated concurrently with CP-2.0. The anti-adipogenic activity of the fractions was also evaluated and CP-1.5 was able to reduce the differentiation of pre-adipocytes (3T3-L1) into adipocytes by 60%, without affecting the cell viability. The fractions CP-0.3, CP-0.5 and CP-0.9 reduced the viability of the HeLa cells (human cervical adenocarcinoma) by 55% and CP-1.5 reduced the viability of the 786-0 cells (human renal adenocarcinoma) by 75%. Leishmanicidal activity and microbicide effect against Carbapenem-resistant Klebsiella pneumoniae (KPC) have not been identified. However, the viability of Staphylococcus epidermidis was reduced by 23.8% in the presence of CP -1.5. All fractions were able to change the formation of calcium oxalate crystals. CP-0.3, CP-0.5 and CP-1.1 only promoted the formation of COD type crystals with a very small size (1 μm). Confocal microscopy and zeta potential data of crystals formed in the presence of the samples showed that the polysaccharides present in the fractions must interact with calcium ions present throughout the crystal lattice, affecting the growth and morphology of crystals The results described herein indicate that the fractions rich in polysaccharides obtained from the green seaweed C. prolifera present a multi therapeutic potential, and subsequent purification steps, as well as research on the mechanisms of action by which these polymers act should be investigated.

Desenvolvimento e caracterização de um eco-compósito de poliuretano de mamona e fibra de lã canina

The Sustainability has been evidence in the world today; organizations have sought to be more and more into this philosophy in their processes, whether products or attendance. In the present work were manufactured eco-composites with animal fiber (dog wool) that is currently discarded into the environment without any use. Project phases consisted on the initial treatment of fibers with alkaline solution (NaOH) at 0.05 mols for removal of impurities, developing methods to convert these fibers (reinforcement) blended with castor oil polyurethane (matrix) in eco-composite with different proportions (5%, 10%, 15% and 20%). Fiber properties were evaluated by analysis of SEM, XRD and FTIR. The composites were produced by compression molding with dimensions 30x30x1cm. For characterization of the composites the following tests were performed: mechanical (tensile, compression, shore hardness A) according the standards and testing water absorption, moisture regain and biodegradation. The analysis of thermal properties on fibers and composites were by TG, DSC, thermal conductivity, resistivity, heat capacity and thermal resistance. Analyzing the results of these tests, it was observed that the composite reinforced with 20% showed a better thermal performance between others composites and dimensional stability when compared to commercial thermal insulation. Also is possible to observe a balance in moisture absorption of the composite being shown with its higher absorption rate in this same sample (20%). The micrographs show the fiber interaction regions with polyurethane to fill the empty spaces. In hardness and compression testing can identify that with increasing percentage of the fiber material acquires a greater stiffness by making a higher voltage is used for forming necessary. So by the tests performed in eco-composites, the highest percentage of fiber used as reinforcement in their composition obtained a better performance compared to the remaining eco-composites, reaching values very close to the PU.

Petrologia e geologia estrutural do plutão granítico Barcelona, província Borborema, NE do Brasil

The Dissertation aimed to advance the geological knowledge of the Barcelona Granitic Pluton (BGP). This body is located in the eastern portion of the Rio Grande do Norte Domain (RND), within the São José do Campestre subdomain (SJC), NE of the Borborema Province. The main goal was to understand the geological evolution of the rocks of the pluton and the tectonic setting of magma generation and its emplacement. The BGP has an assumed Ediacaran age and outcropping area of approximately 260 km2, being composed of three varied petrographic/textural facies: (a) porphyritic biotite monzogranite; (b) dykes and sheets of biotite microgranite; (c) dioritic to quartz-dioritic enclaves. The rocks of the BGP have the following structures: (i) a NE-SW and NW-SE directed magmatic fabric (Sγ), accompanied by a magmatic lineation (Lγ) with gentle dip to NE-SW and NW-SE. In the southern portion, there is the concentric pattern of this foliation with medium to high dip, and (ii) a solid state foliation, in part mylonitic (S3+), mainly on the eastern edge with slightly plunging to west. The integration of structural and gravity data permitted to interpret the emplacement of the BGP as controlled by the transcurrent shear zones systems Lajes Pintadas (LPSZ) and Sítio Novo (SNSZ), both of dextral strike-slip kinematics. Mineral chemistry data show that the amphibole form the porphyritic biotite monzogranite facies is hastingsite with moderate Mg / (Mg + Fe) ratios, indicating crystallization under moderate to high ƒO2 and cristallization pressure of around 5.0-6.0 kbar. The biotite tends to be slightly richer in annite molecule and plots in the transitional field from primary biotite to reequilibrated biotite. In discriminant diagrams of magmatic series, the biotite behave like those of subalkaline affinity, consistent with the potassium calc-alkaline / sub-alkaline geochemical affinity of the hosting rock. The opaque minerals are primarily magnetite, with some crystals martitized to hematite indicating relatively oxidizing conditions during magma evolution that originated the BGP. Zoning in plagioclase, K-feldspar and allanite crystals suggest fractional crystallization process. Lithogeochemical data suggest that the facies described for the BGP have similar magma source, usually plotting in the fields and trends of the subalkaline / high potassium calc-alkaline series.

Petrologia e geocronologia U-Pb do plúton granítico Serra da Rajada, porção central do domínio Rio Piranhas - Seridó, Província Borborema, NE do Brasil

The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

Petrologia e geocronologia U-Pb do plúton granítico Serra da Rajada, porção central do domínio Rio Piranhas - Seridó, Província Borborema, NE do Brasil

The ediacaran plutonic activity related to the Brasilian/Pan-African orogeny is one of the most important geological features in the Borborema Province, represented along its extension by numerous batholiths, stocks, and dikes.The object of this study, the Serra Rajada Granitic Pluton (SRGP), located in the central portion of the Piranhas-Seridó River Domain is an example of this activity. This pluton has been the subject of cartographic, petrographic, geochronological and lithogeochemical studies and its rocks were characterized by two facies. First, the granitic facies were described as monzogranites consisting of K-feldspar, plagioclase (oligoclase - An23-24%), quartz and biotite (main mafic) and opaque minerals such as titanite, allanite, apatite, and zircon as accessories. Alteration minerals are chlorite, white mica and carbonate. Second, the dioritic facies consist of rocks formed by quartz diorite containing plagioclase (dominant mineral phase), quartz and K-feldspar. Biotite and amphibole are the dominant mafic minerals; and titanite, opaque minerals, allanite, zircon and apatite are the accessories. However, previous geological mapping work in the region also identified the presence of other lithostratigraphic units. These were described as gneisses and migmatites with undifferentiated amphibolite lenses related to the Caicó Complex (Paleoproterozoic) and metasedimentary rocks of the Seridó Group (Neoproterozoic) composed of paragneiss with calc-silicate lenses, muscovite quartzite and biotite schist (respectively, the Jucurutu formations, Equador and Seridó), the host rocks for the SRGP rocks. Leucomicrogranite and pegmatite dikes have also been identified, both related to the end of the Ediacaran magmatism and colluvial- eluvial and alluvial deposits related to Neogene and Quaternary, respectively. Lithogeochemical data on the SRGP granite facies, highlighted quite evolved rocks (SiO2 69% to 75%), rich in alkalis (Na2O+K2O ≥ 8.0%), depleted of MgO (≤ 0.45%), CaO (≤ 1.42%) and TiO2 (≤ 0.36%) and moderate levels of Fe2O3t (2.16 to 3.53%). They display transitional nature between metaluminous and peraluminous (predominance of the latter) with sub-alkaline/monzonitic (High K calcium-alkali) affinity. Harker diagrams show negative correlations for Fe2O3t, MgO, and CaO, indicating mafic and plagioclase fractionation. REE spectrum shows enrichment of LREE relative to heavy REE (LaN/YbN = 23.70 to 10.13), with negative anomaly in the Eu (Eu/Eu* = 0.70 to 0.23), suggesting fractionation or accumulation in the feldspars source (plagioclase). Data integration allows to correlate the SRGP rocks with those described as Calcium-Alkaline Suite of equigranular High K. The crystallization conditions of the SRGP rocks were determined from the integration of petrographic and lithogeochemical data. These data indicated intermediate to high conditions of ƒO2 (mineral paragenesis titanite + magnetite + quartz), parent magma saturated in H2O (early biotite crystallization), tardi-magmatic processes of fluids rich in ƒCO2, H2O and O2 causing part of the mineral assembly to change (plagioclase carbonation and saussuritization, biotite chloritization and opaques Sphenitization). Thermobarometrical conditions were estimated based on geochemical parameters (Zr and P2O5) and CIPW normative minerals, with results showing the liquidus minimum temperature of about800°C and the solidus temperature of approximately 700°C. The final/minimum crystallization pressure are suggested to be between 3 and 5 Kbar. The presence of zoned minerals (plagioclase and allanite) associated with lithogeochemical data in bi-log diagrams for Rb vs. Ba and Rb vs. Sr suggest the role of fractional crystallization as the dominant process in the magmatic evolution of SRGP. U-Pb Geochronological and Sm-Nd isotope studies indicated, respectively, the crystallization age of biotite monzogranite as 557 ± 13 Ma, with TDM model age of 2.36 Ga, and εNd value of -20.10 to the crystallization age, allowing to infer paleoproterozoic crustal source for the magma.

Petrologia do Plutão Bom Jardim de Goiás (PBJG): implicação na evolução neoproterozoica da Província Tocantins

The Bom Jardim de Goiás Pluton (PBJG) is a semi-circular body, located in the central portion of the Tocantins Province, intrusive into orthogneisses and metassupracrustals of the Arenópolis Magmatic Arc. These metasupracrustals present a low to moderate dipping banding or schistosity, have a low to moderate angle of banding / foliation, defined by mica, andalusite and sillimanite and cordierite, which characterize an amphibolite facies metamorphism. This structure is crosscut by the emplacement of the PBJG rocks. The abrupt nature of the contacts and the absence of ductile structures indicate that the intrusion took place in a relatively cold crust. Under petrographic grounds, the pluton consists mainly of monzodiorites, tonalite and granodiorite, following the low to medium-K calk-alkaline alkaline trend. Rocks of the PBJG have hornblende and biotite as the main mafic phases, besides subordinate clinopyroxene, titanite, epidote and opaque. Late dikes of leucogranite contain only mineral biotite as relevant accessory mineral. One U-Pb zircon dating of a monzodiorite yielded an age of 550 ± 12 Ma (MSWD = 1.06). Whole-rock and mineral chemistry suggest that the studied rocks are calc-alkaline, having evolved by fractional crystallization of Ca- and Fe-Mg minerals under high oxygen fugacity. Using the amphibole-plagioclase geothermometer and the Al-in amphibole geobarometer, we calculate temperatures and pressures of, respectively, 692-791 °C e 2.4-5.0 kbar for the intrusion of the PBJG, which is corroborated by previous metamorphic assemblages in the country rocks. The geological, geochemical and geochronological features of PBJG demonstrate their post-tectonic or post-collisional nature, with emplacement into an already uplifted and relatively cool crust at the end of brasiliano orogeny in this portion of the Tocantins Province.

Petrologia do Plutão Bom Jardim de Goiás (PBJG): implicação na evolução neoproterozoica da Província Tocantins

The Bom Jardim de Goiás Pluton (PBJG) is a semi-circular body, located in the central portion of the Tocantins Province, intrusive into orthogneisses and metassupracrustals of the Arenópolis Magmatic Arc. These metasupracrustals present a low to moderate dipping banding or schistosity, have a low to moderate angle of banding / foliation, defined by mica, andalusite and sillimanite and cordierite, which characterize an amphibolite facies metamorphism. This structure is crosscut by the emplacement of the PBJG rocks. The abrupt nature of the contacts and the absence of ductile structures indicate that the intrusion took place in a relatively cold crust. Under petrographic grounds, the pluton consists mainly of monzodiorites, tonalite and granodiorite, following the low to medium-K calk-alkaline alkaline trend. Rocks of the PBJG have hornblende and biotite as the main mafic phases, besides subordinate clinopyroxene, titanite, epidote and opaque. Late dikes of leucogranite contain only mineral biotite as relevant accessory mineral. One U-Pb zircon dating of a monzodiorite yielded an age of 550 ± 12 Ma (MSWD = 1.06). Whole-rock and mineral chemistry suggest that the studied rocks are calc-alkaline, having evolved by fractional crystallization of Ca- and Fe-Mg minerals under high oxygen fugacity. Using the amphibole-plagioclase geothermometer and the Al-in amphibole geobarometer, we calculate temperatures and pressures of, respectively, 692-791 °C e 2.4-5.0 kbar for the intrusion of the PBJG, which is corroborated by previous metamorphic assemblages in the country rocks. The geological, geochemical and geochronological features of PBJG demonstrate their post-tectonic or post-collisional nature, with emplacement into an already uplifted and relatively cool crust at the end of brasiliano orogeny in this portion of the Tocantins Province.

Determinação voltamétrica de zinco empregando eletrodos quimicamente modificados com bismuto

This dissertation presents the development of voltammetric methods to zinc determination in multivitamin commercial samples, talc, and art materials for painting (soft pastel) combining an alkaline extraction with 1.0 mol L-1 NaOH aqueous solution and bismuth modified electrodes. Two electrodes were used to zinc quantification in the samples, bismuth film electrode (BiFE) plated in situ onto glassy carbon and carbon paste electrode chemically modified with strongly acidic ion exchange resin Amberlite® IR 120 and bismuth nanostructures (EPCAmbBi). It was verified that the best concentration of Bi3+ for Bi film deposition onto glassy carbon was 4.0 μmol L-1 using an 0.1 mol L-1 acetate buffer aqueous solution (pH = 4.5) as supporting electrolyte. The best condition to formation of Bi nanostructures in the EPC modified with 10 % Amberlite® IR 120 was the use of 30 s to pre-concentration (open circuit) in 0.5 mmol L-1 Bi3+ aqueous solution (pH 5.5) prepared with supporting electrolyte solution. The obtained analytical curve for Zn2+ using BiFE presented linear range from 0.5 to 5.0 μmol L-1, the limit of detection (LD) was 41 nmol L-1. For EPCAmbBi only one linear range was observed for the analytical curve varying the Zn2+ concentration from 0.05 to 8.2 μmol L-1, LD obtained in this curve it was equal to 10 nmol L-1. The EPCAmbBi presented the most intense and sharp anodic stripping peaks for Zn2+ presenting, therefore, a better voltammetric profile, with sensitivity higher than obtained with the BiFE. Moreover, the EPCAmbBi presented a LD lower than that obtained with the BiFE. Alkaline extraction was an efficient sample pretreatment to extract Zn2+ from solid samples, besides that, this procedure was less susceptible to interferences from Cu2+, since it remains at extracting vessel as insoluble Cu(OH)2. The combination of alkaline extraction with the EPCAmbBi is a simple, fast, efficient and low cost for the zinc determination in pharmaceutical formulations and art materials for painting (soft pastel) samples, which can be employed as a low-cost alternative method to the atomic absorption spectroscopy.

Papel biológico del diadenosin tetrafosfato en el ojo: efecto sobre la composición lacrimal e implicación en la función de barrera corneal

El Ap4A es una molécula con un amplio papel biológico en el ojo. Se ha descrito su implicación en procesos de secreción lagrimal, cicatrización epitelial, regulación de la presión intraocular, y presenta también un papel neuroprotector sobre los terminales simpáticos que inervan el cuerpo ciliar. El objetivo de este trabajo ha sido analizar la participación del Ap4A en otras posibles funciones a nivel ocular. En concreto se ha estudiado la capacidad de este dinucléotido para estimular la liberación de proteínas lagrimales de acción antibacteriana tales como la lisozima y la lactoferrina. Por otra parte se ha investigado su efecto como modulador de la función de barrera de la córnea a través de la regulación de los niveles de expresión de proteínas constituyentes de las tight junctions (TJ). Dicho efecto sobre la barrera puede tener una importante repercusión en la entrada de fármacos y en la consiguiente eficacia terapéutica de los mismos. Por último, se ha estudiado la posible implicación del dinucleótido en el proceso de edematización descrito en modelos animales glaucomatosos tales como el ratón DBA/2J. Con el objetivo de averiguar si la activación de Ap4A inducía un efecto sobre la producción de dos proteínas antimicrobianas relevantes de la lágrima (lisozima y lactoferrina) se realizaron ensayos en la lágrima de conejos albinos de Nueva Zelanda, mediante las técnicas de agar-agar y ELISA. Los resultados obtenidos demostraron que Ap4A produce un aumento en la concentración de lisozima y de lactoferrina del 93% y 24%, respectivamente, frente a valores basales, y este efecto está mediado por receptores de tipo P2...

Aplicación del sistema de recombinación específica de secuencia β-six al estudio de la regulación de la expresión génica en células eucariotas y modelos animales

Las recombinasas específicas de secuencia son herramientas muy valiosas en la generación de modificaciones génicas condicionales. Estos sistemas permiten controlar la recombinación de forma específica de tejido, temporalmente, o ambas, y sortean diversas limitaciones de los sistemas de knockout (KO) convencionales, como la letalidad embrionaria o la generación de mecanismos compensatorios. Actualmente los sistemas Cre/loxP y Flp/FRT son los más empleados tanto en modelos animales como vegetales. La necesidad de realizar modificaciones más complejas en un mismo organismo hace que sea primordial caracterizar otras recombinasas que complementen a las existentes. La b recombinasa (b-rec) es originaria del plásmido pSM19035 de Streptococcus pyogenes. A diferencia de Cre y Flp, que en ausencia de factores adicionales catalizan la integración en un nuevo sustrato, la b-rec necesita un sustrato superenrollado y un cofactor de la reacción, una proteína asociada a la cromatina (como la procariota Hbsu o la eucariota HMG1). Se ha demostrado que la b-rec cataliza de forma específicamente intramolecular (resolución o inversión) la recombinación en células eucariotas, tanto de sustratos episomales como integrados en la cromatina, lo que indica que el entorno eucariota es capaz de proveer del cofactor y del superenrollamiento necesarios para que la b-rec realice su función. En este trabajo hemos determinado que la tasa de recombinación mediada por la b-rec no se ve afectada en absoluto por la deficiencia en el cofactor HMG1, alcanzando el mismo valor de recombinación en MEF KO en HMG1 que en wt. Este y otros datos confirman que en el entorno eucariota hay otras proteínas accesorias que pueden actuar de cofactores y sugiere que estas reacciones pueden ocurrir en la mayor parte de tejidos y tipos celulares. Para estudiar detalladamente el potencial de la b-rec en eucariotas desarrollamos un sistema de RAGE (activación génica mediada por recombinación) dependiente de la actividad b-rec; este sistema ha resultado funcional tanto en sustratos episomales como en sustratos integrados en la cromatina. También hemos generado un vector retroviral que porta la proteína de fusión b-Egfp, permitiendo de forma rápida y eficiente la integración y expresión funcional de nuestra proteína...

Caracterización de un modelo murino de glaucoma: implicación funcional de la señalización del receptor P2X7 en procesos neurodegenerativos de la retina

El glaucoma es una de las causas más comunes de discapacidad visual y una de las enfermedades neurodegenerativas oculares más frecuentes de pérdida irreversible de visión. La afectación originada en la retina se caracteriza por la degeneración de las células ganglionares y la pérdida de axones. La presión intraocular es un factor de riesgo importante en el glaucoma, entre otros factores, implicando mecanismos bioquímicos que desencadenan la muerte de las células ganglionares. El ratón DBA/2J es un modelo de hipertensión ocular y de degeneración de las células ganglionares de la retina (CGR). Las características principales de éste son la dispersión del pigmento del iris (IPD) y la atrofia del estroma del iris (ISA) que conducen a la patogénesis del glaucoma. Los mecanismos bioquímicos que comprometen al sistema purinérgico en procesos patológicos como la degeneración glaucomatosa han sido estudiados en los últimos años, siendo de gran relevancia como posibles dianas farmacológicas para el tratamiento de diferentes neuropatías. Los receptores P2X comprenden una familia de siete canales iónicos de membrana activados por ligando (P2X1-7) que se activan por el ATP extracelular (ATPe). En particular, los receptores P2X7 podrían estar involucrados en la regulación de la transmisión sináptica y la muerte neuronal en la retina. Además, la excitotoxicidad mediada por ATP a través de la activación del receptor P2X7 sugiere su posible implicación en la degeneración neuronal y la pérdida de la función visual en las retinas glaucomatosas. Tan importante como la presencia de este receptor purinérgico es estudiar los niveles de ATP extracelular de la retina, así como evaluar los cambios en la expresión del transportador de nucleótidos vesicular (VNUT) y los niveles de ecto-nucleotidasa (E-NPP1) en este modelo murino de glaucoma durante el desarrollo de la enfermedad...

Papel del mecanismo de inmunoadherencia de "Leishmania" en la infección humana

La leishmaniosis es una enfermedad parasitaria causada por protozoos hemoflagelados del genero Leishmania que se transmite al hombre y a otros vertebrados a través de la picadura de un díptero de la familia Plebotominae. Cuando un flebótomo infectado pica al hospedador vertebrado, perfora la piel con su probóscide buscando las vénulas de la dermis, las lacera y provoca un pequeño hematoma donde deposita los promastigotes. Tras el contacto con la sangre tiene lugar la activación del complemento y deposición del C3 en la superficie del parásito. En primates, los promastigotes opsonizados se unen a eritrocitos y posteriormente son transferidos a las células aceptoras de la sangre: los leucocitos...

Impacto de los polimorfismos genéticos de las citoquinas en los resultados del trasplante renal

En el trasplante de órganos sólidos los factores que conducen a la pérdida del injerto son muy diversos. A pesar del avance en el diagnóstico y tratamiento de los pacientes trasplantados renales, el rechazo agudo sigue siendo una de las principales causas de deterioro progresivo de la función renal. La presencia de episodios de rechazo acorta la supervivencia del injerto e, incluso, la del paciente, dado que implica la activación de un proceso inflamatorio no sólo local, sino también sistémico y obliga al incremento de la carga de inmunosupresión a administrar. La detección de los pacientes con mayor grado de susceptibilidad al desarrollo de rechazo, puede ayudarnos a prevenirlo. No existe consenso sobre la definición de "riesgo inmunológico elevado" y que características tiene que cumplir un paciente para poder ser incluido dentro de este grupo de riesgo. Las citoquinas, moléculas inmunomoduladoras que actúan como mediadores de la inflamación y la respuesta inmune, son secretadas por células T y macrófagos. Participan activamente en todos los procesos de la respuesta inmune, desde la activación a la diferenciación y proliferación celular. La producción de estas citoquinas se encuentra, en muchas ocasiones, sometida a una regulación genética, de tal forma que polimorfismos a nivel de las regiones promotoras o codificadoras pueden alterar los niveles de las mismas y por tanto modificar la respuesta inflamatoria y/o inmunológica ante cualquier estímulo...

Mecanismos celulares activados por receptores P2Y₂ en los procesos ciliares: implicaciones en la hipertensión ocular y el glaucoma

El glaucoma es una neuropatía óptica crónica de etiología multifactorial, que provoca una pérdida progresiva e irreversible de la visión debida a la degeneración de los axones del nervio óptico y la muerte apoptótica de las células ganglionares de la retina (Downs et al., 2011; Quigley, 2011; Soto et al., 2014). Actualmente es la principal causa de ceguera irreversible en el mundo (Pascolini et al., 2012). Aunque su etiología aún no está clara, se sabe que el principal factor de riesgo para desarrollar la enfermedad es el aumento de la PIO debido a anomalías en la dinámica del humor acuoso (Casson et al., 2012). La presencia de receptores purinérgicos P2X y P2Y ha sido descrita en las principales estructuras oculares relacionadas con la producción y drenaje del humor acuoso, los procesos ciliares y la malla trabecular, que son bañadas por dicho fluido (Guzman-­‐Aranguez et al., 2013). Al mismo tiempo, se ha referido la presencia del dinucleótido Ap4A, agonista de dichos receptores, en el humor acuoso, y cómo sus niveles se veían significativamente incrementados en pacientes glaucomatosos (Castany et al., 2011). El objetivo de esta tesis ha sido evaluar la implicación de los receptores purinérgicos P2Y2 de los procesos ciliares en la hipertensión ocular. Más concretamente determinar el papel del Ap4A a través de la activación de dichos receptores sobre la movilización del ion cloruro y del agua a través de las proteínas acuaporinas (AQPs), principales componentes del humor acuoso. Por otra parte, se ha investigado el origen de los niveles incrementados de Ap4A debidos al aumento de la PIO, caracterizando uno de los posibles sensores celulares implicados en dicho proceso. Al mismo tiempo se han evaluado y caracterizado los diferentes mecanismos implicados en dicha liberación...