Efecto de las tetraciclinas sobre la quimiotaxis leucocitaria : estudio doble ciego en pacientes con acné vulgaris

Tesis (Maestría en Ciencias con Especialidad en Microbiología Médica) UANL

Characterization of Adult Stem/Progenitor Cell Populations From Bone Marrow in a Three-Dimensional Collagen Gel Culture System.

Stem cell transplantation therapy using mesenchymal stem cells (MSCs) is considered a useful strategy. Although MSCs are commonly isolated by exploiting their plastic adherence, several studies have suggested that there are other populations of stem and/or osteoprogenitor cells which are removed from primary culture during media replacement. Therefore, we developed a three-dimensional (3D) culture system in which adherent and non-adherent stem cells are selected and expanded. Here, we described the characterization of 3D culture-derived cell populations in vitro and the capacity of these cells to differentiate into bone and/or cartilage tissue when placed inside of demineralized bone matrix (DBM) cylinders, implanted subcutaneously into the backs of rat for 2, 4 and 8 weeks. Our results demonstrates that 3D culture cells were a heterogeneous population of uncommitted cells that express pluripotent, hematopoietic, mesenchymal and endothelial specific markers in vitro and can undergo osteogenic differentiation in vivo.

Capacidad pronóstica del eje SDF-1/CXCR4 en pacientes con carcinomas escamosos de cabeza y cuello

Introducció: El Stromal Derived Factor 1 (SDF-1) és una quimioquina que compta amb la capacitat de modular en la proliferació, supervivència, angiogènesi, quimiotaxi i metàstasi de les cèl•lules tumorals actuant a través del seu receptor: CXCR4. L'objectiu d'aquest estudi és valorar la relació en l'expressió dels gens de SDF-1 i CXCR4 comparant-los amb l'expressió en mucosa sana i determinar l'impacte en la supervivència en pacients amb Carcinoma escamós de cap i coll. Material i mètodes: Es va dur a terme una determinació de l'expressió de SDF-1 i CXCR4 en mostres de biòpsies prèvies al tractament i de mucosa sana en 76 pacients amb carcinoma escamós de cap i coll mitjançant una tècnica de PCR quantitativa. Es va determinar la supervivència ajustada mitjançant una tècnica d'arbres de classificació. Resultats: Van existir diferències significatives en la supervivència en funció dels nivells d'expressió de SDF-1 i CXCR4 (p = 0,004). Conclusions: L'expressió dels gens que codifiquen l'eix SDF-1 / CXCR4 té capacitat pronòstica significativa en pacients amb Carcinoma escatós de cap i coll.

Evaluación y comparación del potencial de osteoinducción de la combinación de rhPDGF-BB y rhBMP-2 en regeneración ósea

Introducción. Los factores de crecimiento polipéptidos son una clase de mediadores biológicos naturales que regulan los eventos celulares clave en la reparación tisular, incluyendo la proliferación celular, quimiotaxis, diferenciación y síntesis de la matriz mediante la union a receptores de superficie específicos. El hueso es una fuente rica en factores de crecimiento con acciones importantes en la regulación de la formación y reabsorción ósea, entre los que se encuentran, las proteinnas morfogenéticas óseas (BMPs), el factor de crecimiento derivado de plaquets (PDGF), entre otros. El objetivo de esta investigación fue evaluar el potencial de regeneración ósea (osteoide) y osteoinducción (factores de mineralización) del rhPDGF-BB y rhBMP-2 en defectos de tamaño crítico en el cráneo de ratas Sprague-Dawley a las 4 semanas de cicatrización Materiales y Métodos. El diseño de esta investigación fue comparativo, abierto, experimental y longitudinal. La mustra consistió en 16 ratas Sprague-Dawley, las cuales se dividieron en grupos de 4, conformando así un grupo Control, un grupo Experimental 1 al cual se le colocó esponja de colágeno + 30μl a una concentración de 100 μg/ml de rhPDGFBB; un grupo Experimental 2 al que se le colocó esponja de colágeno + 30μl a una concentración de 100 μg/ml de rhBMP-2; y un grupo Experimental 3, cual cual consistió en la colocación de esponja de colágeno + 30μl a una concentración de 100 μg/ml de rhPDGF-BB + 30μl a una concentración de 100 μg/ml de rhBMP-2. Se dejó un período de cicatrización de 4 semanas y posteriormente se sacrificaron los especímenes. Resultados Resultados. Tanto rhPDGF-BB como rhBMP-2 incrementaron la producción de osteoprotegerina y de osteopontina (p<0.05). La combinación de ambos factores de crecimiento también incremento la producción de ambos factores de mineralización (p<0.01). Resultados semejantes fueron encontrados en la producción de osteoide por ambos factores. Conclusión. La combinación de ambos factores de crecimiento aumenta la regeneración ósea demostrado por el incremento en la producción de osteoide y de los factores de mineralización osteopontina y osteoprotegerina.

Devoções e diversões em São João del-Rei : um estudo sobre as festas do Bom Jesus de Matosinhos 1884-1924

Universidade Estadual de Campinas . Faculdade de Educação Física

Propiedades termofísicas del jugo concentrado de lulo a temperaturas por encima del punto de congelación

En este trabajo fueron determinados experimentalmente el calor específico, conductividad térmica, difusividad térmica y densidad del jugo de lulo en el rango de contenido de agua de 0.55 a 0.90 (p/p en base húmeda) y en temperaturas variando de 4 a 78.6 °C. La conductividad térmica y el calor específico fueron obtenidos utilizando el mismo aparato - una célula constituida de dos cilindros concéntricos - operando en estado estacionario y no- estacionario, respectivamente. La difusividad térmica fue obtenida a través del método de Dickerson y la densidad determinada por picnometria. Tanto la temperatura como el contenido de agua presentaron una fuerte influencia en los datos experimentales de las propiedades termofísicas del jugo de lulo. Los resultados obtenidos fueron utilizados para obtener modelos matemáticos y predecir estas propiedades en función de la concentración y la temperatura.

HR Del REMNANT ANATOMY USING TWO-DIMENSIONAL SPECTRAL DATA AND THREE-DIMENSIONAL PHOTOIONIZATION SHELL MODELS

The HR Del nova remnant was observed with the IFU-GMOS at Gemini North. The spatially resolved spectral data cube was used in the kinematic, morphological, and abundance analysis of the ejecta. The line maps show a very clumpy shell with two main symmetric structures. The first one is the outer part of the shell seen in H alpha, which forms two rings projected in the sky plane. These ring structures correspond to a closed hourglass shape, first proposed by Harman & O'Brien. The equatorial emission enhancement is caused by the superimposed hourglass structures in the line of sight. The second structure seen only in the [O III] and [N II] maps is located along the polar directions inside the hourglass structure. Abundance gradients between the polar caps and equatorial region were not found. However, the outer part of the shell seems to be less abundant in oxygen and nitrogen than the inner regions. Detailed 2.5-dimensional photoionization modeling of the three-dimensional shell was performed using the mass distribution inferred from the observations and the presence of mass clumps. The resulting model grids are used to constrain the physical properties of the shell as well as the central ionizing source. A sequence of three-dimensional clumpy models including a disk-shaped ionization source is able to reproduce the ionization gradients between polar and equatorial regions of the shell. Differences between shell axial ratios in different lines can also be explained by aspherical illumination. A total shell mass of 9 x 10(-4) M(circle dot) is derived from these models. We estimate that 50%-70% of the shell mass is contained in neutral clumps with density contrast up to a factor of 30.

Matrix elements of U(2n) generators in a multishell spin-orbit basis. I. The del-operator MEs in a two-shell composite Gelfand-Paldus basis

This is the first in a series of three articles which aimed to derive the matrix elements of the U(2n) generators in a multishell spin-orbit basis. This is a basis appropriate to many-electron systems which have a natural partitioning of the orbital space and where also spin-dependent terms are included in the Hamiltonian. The method is based on a new spin-dependent unitary group approach to the many-electron correlation problem due to Gould and Paldus [M. D. Gould and J. Paldus, J. Chem. Phys. 92, 7394, (1990)]. In this approach, the matrix elements of the U(2n) generators in the U(n) x U(2)-adapted electronic Gelfand basis are determined by the matrix elements of a single Ll(n) adjoint tensor operator called the del-operator, denoted by Delta(j)(i) (1 less than or equal to i, j less than or equal to n). Delta or del is a polynomial of degree two in the U(n) matrix E = [E-j(i)]. The approach of Gould and Paldus is based on the transformation properties of the U(2n) generators as an adjoint tensor operator of U(n) x U(2) and application of the Wigner-Eckart theorem. Hence, to generalize this approach, we need to obtain formulas for the complete set of adjoint coupling coefficients for the two-shell composite Gelfand-Paldus basis. The nonzero shift coefficients are uniquely determined and may he evaluated by the methods of Gould et al. [see the above reference]. In this article, we define zero-shift adjoint coupling coefficients for the two-shell composite Gelfand-Paldus basis which are appropriate to the many-electron problem. By definition, these are proportional to the corresponding two-shell del-operator matrix elements, and it is shown that the Racah factorization lemma applies. Formulas for these coefficients are then obtained by application of the Racah factorization lemma. The zero-shift adjoint reduced Wigner coefficients required for this procedure are evaluated first. All these coefficients are needed later for the multishell case, which leads directly to the two-shell del-operator matrix elements. Finally, we discuss an application to charge and spin densities in a two-shell molecular system. (C) 1998 John Wiley & Sons.

Petrology and geochemistry of the Bandas del Sur Formation, Las Canadas Edifice, Tenerife (Canary Islands)

The Bandas del Sur Formation preserves a Quaternary extra-caldera record of central phonolitic explosive volcanism of the Las Canadas volcano at Tenerife. Volcanic rocks are bimodal in composition, being predominantly phonolitic pyroclastic deposits, several eruptions of which resulted in summit caldera collapse, alkali basaltic lavas erupted from many fissures around the flanks. For the pyroclastic deposits, there is a broad range of pumice glass compositions from phonotephrite to phonolite. The phonolite pyroclastic deposits are also characterized by a diverse, 7-8-phase phenocryst assemblage (alkali feldspar + biotite + sodian diopside + titanomagnetite + ilmenite + nosean-hauyne + titanite + apatite) with alkali feldspar dominant, in contrast to interbedded phonolite lavas that typically have lower phenocryst contents and lack hydrous phases. Petrological and geochemical data are consistent with fractional crystallization (involving the observed phenocryst assemblages) as the dominant process in the development of phonolite magmas. New stratigraphically constrained data indicate that petrological and geochemical differences exist between pyroclastic deposits of the last two explosive cycles of phonolitic volcanism. Cycle 2 (0.85-0.57 Ma) pyroclastic fall deposits commonly show a cryptic compositional zonation indicating that several eruptions tapped chemically, and probably thermally stratified magma systems. Evidence for magma mixing is most widespread in the pyroclastic deposits of Cycle 3 (0.37-0.17 Ma), which includes the presence of reversely and normally zoned phenocrysts, quenched mafic glass blebs in pumice, banded pumice, and bimodal to polymodal phenocryst compositional populations. Syn-eruptive mixing events involved mostly phonolite and tephriphonolite magmas, whereas a pre-eruptive mixing event involving basaltic magma is recorded in several banded pumice-bearing ignimbrites of Cycle 3. The periodic addition and mixing of basaltic magma ultimately may have triggered several eruptions. Recharge and underplating by basaltic magma is interpreted to have elevated sulphur contents (occurring as an exsolved gas phase) in the capping phonolitic magma reservoir. This promoted nosean-hauyne crystallization over nepheline, elevated SO3 contents in apatite, and possibly resulted in large, climatologically important SO2 emissions.