Expresión diferencial del gen CsGH3-1 y su relación con la formación de raíces adventicias en los brotes de castaño.

Peer reviewe

Análisis por qPCR de la respuesta a P. cinnamomi en clones de castaño in vitro con diferente nivel de resistencia

Peer reviewe

Descripción de una especie nueva de Melanips Walker (Hymenoptera: Figitidae), primer registro del género para la región neotropicaL

A new species of Melanips Walker (Hymenoptera: Figitidae) from Mexico, Melanips lomeyva sp. nov. is described. This species represents the first record of the genus Melanips from Mexico and to the Neotropical region. Diagnostic characters of the new species are illustrated and discussed. The adults were obtained from pupae of Leucopis bellula (Chamaemyiidae) natural enemy of wild cochineal of prickly pear Dactylopius opuntiae (Dactylopiidae). Biological data and hosts of this new species are commented

Caracterização bioquímica e molecular de doentes com diagnóstico clínico de Dislipidemia Familiar Combinada

A Dislipidemia Familiar Combinada (FCHL) é uma doença poligénica caracterizada por hiperlipidemia simples ou combinada, variabilidade intra-individual e intra-familiar do perfil lipídico, ApoB elevada (> 120 mg/dL) e risco elevado de doença cardiovascular (DCV). A sua causa é desconhecida mas alterações nos genes LPL, APOAIV, APOAV, APOCIII e USF1 parecem contribuir para o seu fenótipo. O objectivo deste estudo é caracterizar bioquímica e molecularmente doentes com diagnóstico clínico de FCHL. Todos os exões e promotor dos genes LPL, APOAIV, APOAV, APOCIII e regiões do gene USF1 (s1,s2) de 41 doentes foram amplificados por PCR e sequenciados. O colesterol total (CT), c-LDL, c-HDL, sdLDL, trigliceridos (TG), apoB e apoCIII foram determinados num aparelho automatizado. Em alguns doentes as sdLDL foram também analisadas por electroforese de lipoproteínas. A ApoAIV e ApoAV foram quantificadas por ELISA. Foram encontradas alterações genéticas em 37 doentes, 3 não descritas (APOAIV Q359_E362, APOAV D332fsX336 e APOCIII 3269C>A). O índex com a alteração Q359_E362del apresentou valores normais de apo AIV (15.5 mg/dL) e o índex com a alteração D332fsX336 apresentou valores baixos de apo AV (74.5 ng/mL). Os doentes estudados apresentam valores elevados de CT (285 ± 83 mg/dL), c-LDL (189 ± 85 mg/dL), TG (310 ± 253 mg/dL), e apo CIII (15 ± 4 mg/dL) e valores reduzidos de c-HDL (45 ± 11 mg/dL), sem medicação. Os valores de apoAIV (17,5 ± 10,4 mg/dL) e apoAV (150 ± 135 ng/mL) encontram-se, na maioria dos casos, no intervalo normal assim como os valores de sdLDL (35 ± 18 mg/dL), no entanto alguns casos apresentam valores acima do cut-off para DCV (35 mg/dL). A análise de sdLDL por electroforese foi realizada em 11 doentes, 9 dos quais apresentaram um perfil aterogénico. O valor médio de ApoB destes doentes era de 94 ± 43 mg/dL, mas aproximadamente 70% dos doentes estavam medicados com terapêutica hipolimiante (estatinas e/ou fibratos). Cerca de 30% dos doentes apresentavam DCV prematura. Os resultados obtidos parecem indicar que alterações nos genes estudados influenciam o fenótipo da FCHL. Os níveis séricos de apo CIII encontram-se alterados nesta dislipidemia. Doentes com FCHL, apesar de estarem medicados, apresentam valores elevados de sdLDL, evidenciando o seu elevado risco cardiovascular. A caracterização bioquímica complementa a identificação genética e permite uma melhor avaliação do risco cardiovascular do doente bem como a escolha de uma terapêutica adequada

Un texto inédito de Quevedo: "Memorial de don Francisco de Quevedo Villegas dado a la Inquisición General sobre los libros del Monte Santo de Granada"

This article presents an unknown and unpublished text written by Quevedo, the Memorial de don Francisco de Quevedo Villegas dado a la Inquisición General sobre los libros del Monte Santo de Granada, with an annotated edition and preceded by an introductory study. The study shows evidence for Quevedo’s authorship of the text and suggests an approximate date of composition. In the Memorial, Quevedo defends the fake nature of the texts and relics found in the Sacromonte de Granada and urges the Inquisition to burn them down instead of sending them to Rome for further examination, as Pope Urban VIII had requested. The text confirms Quevedo’s inclination to influence issues of government as well as his adhesion to Catholic orthodoxy and his aspiration to historiographical rigour.Este trabajo presenta un texto desconocido e inédito de Quevedo, el Memorial de don Francisco de Quevedo Villegas dado a la Inquisición General sobre los libros del Monte Santo de Granada, en una edición anotada y precedida de un estudio introductorio. El estudio determina la autoría de Quevedo y propone una fecha aproximada de composición. En el Memorial, Quevedo considera falsos los textos y reliquias encontrados en el Sacromonte granadino, y propone a la Inquisición que estos sean quemados ya en España y no enviados a Roma para su examen, como había solicitado el papa Urbano VIII. El memorial muestra la tendencia de Quevedo a influir en los asuntos de gobierno, así como su ortodoxia católica y su pretensión de rigor historiográfico

Photorefractive nonlinear propagation of single beams in undoped LiNbO3: Self-defocusing and beam break-up

Beam propagation in photorefractive LiNbO3 planar waveguides has been studied at different beam intensities and propagation lengths. Self-defocusing and beam break-up have been observed and explained using BPM simulations under a 2-centre band transport model

High selectivity of TiC-CDC for CO2/N2 separation

A series of carbide-derived carbons (CDC) have been prepared starting from TiC and using different chlorine treatment temperatures (500–1200 °C). Contrary to N2 adsorption measurements at −196 °C, CO2 adsorption measurements at room temperature and high pressure (up to 1 MPa) together with immersion calorimetry measurements into dichloromethane suggest that the synthesized CDC exhibit a similar porous structure, in terms of narrow pore volume, independently of the temperature of the reactive extraction treatment used (samples synthesized below 1000 °C). Apparently, these carbide-derived carbons exhibit narrow constrictions were CO2 adsorption under standard conditions (0 °C and atmospheric pressure) is kinetically restricted. The same accounts for a slightly larger molecule as N2 at a lower adsorption temperature (−196 °C), i.e. textural parameters obtained from N2 adsorption measurements on CDC must be underestimated. Furthermore, here we show experimentally that nitrogen exhibits an unusual behavior, poor affinity, on these carbide-derived carbons. CH4 with a slightly larger diameter (0.39 nm) is able to partially access the inner porous structure whereas N2, with a slightly smaller diameter (0.36 nm), does not. Consequently, these CDC can be envisaged as excellent sorbent for selective CO2 capture in flue-gas streams.This work was supported by the National Science Centre under the Grant No. DEC–2011/01/N/ST5/05595. Rafał Janus wishes to thank the Foundation for Polish Science MPD Programme co-financed by the EU European Regional Development Fund for the financial support. The research was carried out with the equipment purchased thanks to the financial support of the European Regional Development Fund in the framework of the Polish Innovation Economy Operational Program (contract No. POIG.02.01.00-12-023/08)

A Mobility Determination Method for Parallel Platforms Based on the Lie Algebra of SE(3) and Its Subspaces

This contribution presents a screw theory-based method for determining the mobility of fully parallel platforms. The method is based on the application of three stages. The first stage involves the application of the intersection of subalgebras of Lie algebra, se(3), of the special Euclidean group, SE(3), associated with the legs of the platform. The second stage analyzes the possibility of the legs of the platform generating a sum or direct sum of two subalgebras of the Lie algebra, se(3). The last stage, if necessary, considers the possibility of the kinematic pairs of the legs satisfying certain velocity conditions; these conditions reduce the platform’s mobility analysis to one that can be solved using one of the two previous stages. Several examples are illustrated

Thinning of the Monte Perdido Glacier in the Spanish Pyrenees since 1981

This paper analyzes the evolution of the Monte Perdido Glacier, the third largest glacier in the Pyrenees, from 1981 to the present. We assessed the evolution of the glacier''s surface area by analysis of aerial photographs from 1981, 1999, and 2006, and changes in ice volume by geodetic methods with digital elevation models (DEMs) generated from topographic maps (1981 and 1999), airborne lidar (2010) and terrestrial laser scanning (TLS, 2011, 2012, 2013, and 2014) data. We interpreted the changes in the glacier based on climate data from nearby meteorological stations. The results indicate that the degradation of this glacier accelerated after 1999. The rate of ice surface loss was almost three times greater during 1999-2006 than during earlier periods. Moreover, the rate of glacier thinning was 1.85 times faster during 1999-2010 (rate of surface elevation change = -8.98 ± 1.80 m, glacier-wide mass balance = -0.73 ± 0.14 m w.e. yr-1) than during 1981-1999 (rate of surface elevation change = -8.35 ± 2.12 m, glacier-wide mass balance = -0.42 ± 0.10 m w.e. yr-1). From 2011 to 2014, ice thinning continued at a slower rate (rate of surface elevation change = -1.93 ± 0.4 m yr-1, glacier-wide mass balance = -0.58 ± 0.36 m w.e. yr-1). This deceleration in ice thinning compared to the previous 17 years can be attributed, at least in part, to two consecutive anomalously wet winters and cool summers (2012-2013 and 2013-2014), counteracted to some degree by the intense thinning that occurred during the dry and warm 2011-2012 period. However, local climatic changes observed during the study period do not seem sufficient to explain the acceleration of ice thinning of this glacier, because precipitation and air temperature did not exhibit statistically significant trends during the study period. Rather, the accelerated degradation of this glacier in recent years can be explained by a strong disequilibrium between the glacier and the current climate, and likely by other factors affecting the energy balance (e.g., increased albedo in spring) and feedback mechanisms (e.g., heat emitted from recently exposed bedrock and debris covered areas)