Consanguinidade e efeito fundador da mutação G377S da doença de Gaucher em população de Tabuleiro do Norte – Ceará – Brasil

Gaucher’s disease (GD) is caused by a β-glucocerebrosidase deficiency, leading to the accumulation of glucocerebroside in the reticuloendothelial system. The prevalence of GD in Tabuleiro do Norte (TN) (1:4000) is the highest in Brazil. The purpose of this study was to present evidence of consanguinity and founder effect for the G377S mutation (c.1246G>A) among GD patients in TN based on enzyme, molecular and genealogical studies. Between March 2009 and December 2010, 131 subjects at risk for GD (GC in dried blood ≤2.19 nmol/h/ml) and 5 confirmed GD patients from the same community were submitted for molecular analysis to characterize the genetic profile of the population. Based on the enzymatic and molecular analysis, the subjects were classified into three categories: affected (n=5), carrier (n=20) and non-carrier (n=111). All carriers were (G377S/wt). Affected subjects were homozygous (G377S/G377S). The identification of a single mutation in carriers and homozygotes from different generations, the history of the community and the genealogy study suggest that the high prevalence of GD in this population may be due to a combination of consanguinity and founder effect for the G377S mutation

High-pressure experiments on a natural olivine gabbro from ODP Hole 176-735B

We have conducted high-pressure experiments on a natural oceanic gabbro composition (Gb108). Our aim was to test recent proposals that Sr-enrichment in rare primitive melt inclusions from Mauna Loa, Hawaii, may have resulted from melting of garnet pyroxenite formed in the magma source regions by reaction of peridotite with siliceous, Sr-enriched partial melts of eclogite of gabbroic composition. Gb108 is a natural, Sr-enriched olivine gabbro, which has a strong positive Sr anomaly superimposed on an overall depleted incompatible trace element pattern, reflecting its origin as a plagioclase-rich cumulate. At high pressures it crystallises as a coesite eclogite assemblage, with the solidus between 1,300 and 1,350°C at 3.5 GPa and 1,450 and 1,500°C at 4.5 GPa. Clinopyroxenes contain 4-9% Ca-eskolaite component, which varies systematically with pressure and temperature. Garnets are almandine and grossular-rich. Low degree partial melts are highly siliceous in composition, resembling dacites. Coesite is eliminated between 50 and 100°C above the solidus. The whole-rock Sr-enrichment is primarily hosted by clinopyroxene. This phase dominates the mode (>75 wt%) at all investigated PT conditions, and is the major contributor to partial melts of this eclogite composition. Hence the partial melts have trace element patterns sub-parallel to those of clinopyroxene with ~10* greater overall abundances and with strong positive Sr anomalies. Recent studies of primitive Hawaiian volcanics have suggested the incorporation into their source regions of eclogite, formerly gabbroic material recycled through the mantle at subduction zones. The models suggest that formerly gabbroic material, present as eclogite in the Hawaiian plume, partially melted earlier than surrounding peridotite (i.e. at higher pressure) because of the lower solidus temperature of eclogite compared with peridotite. This produced highly siliceous melts which reacted with surrounding peridotite producing hybrid pyroxene + garnet lithologies. The Sr-enriched nature of the formerly plagioclase-rich gabbro was present in the siliceous partial melts, as demonstrated by these experiments, and was transferred to the reactive pyroxenite. These in turn partially melted, producing Sr-enriched picritic liquids which mixed with normal picritic partial melts of peridotite before eruption. On rare occasions these mixed, relatively Sr-rich melts were trapped as melt inclusions in primitive olivine phenocrysts.Yaxley-Sobolev

Geochemistry of ODP Leg 135 igneous rock samples

Ocean Drilling Program Leg 135 provided igneous rock cores from six sites drilled on a transect across the Lau Basin between the Lau Ridge remnant arc and the modem spreading ridges of the Central and Eastern Lau Spreading Centers. The drill cores sampled crust from the earliest stage of backarc extension (latest Miocene time, about 6 Ma), and younger crust (late Pliocene, about 3.8-2 Ma, and middle Pleistocene, about 0.64-0.8 Ma). Nearly all of the igneous samples are from tholeiitic basalt flows; many of them are interbedded with arc-composition volcaniclastic sediments. Rock compositions range from olivine-plagioclase-clinopyroxene basalt, with up to 8% MgO, to oceanic andesites with less than 3.2% MgO and silica contents as high as 56%. The oldest rocks recovered are close in composition to rocks formed at the modern Central and Eastern Lau Spreading Centers and have MORB-like characteristics. Generation of the oldest units was coeval with arc-tholeiitic volcanism on the Lau Ridge less than 100 km to the west. The arc and backarc melts came from different mantle sources. At three sites near the center of the basin, the crust is arc-tholeiitic basalt, two-pyroxene basaltic-andesite, and two-pyroxene andesite. These rocks have many similarities to modem Tofua Arc lavas yet they were drilled within 70 km of the MORB-like Eastern Lau Spreading Center. Estimates of the minimum age for these arc-like rocks indicate that they are late Pliocene (about 2 Ma). These ages overlap the age of the nearby Eastern Lau Spreading Center. The heterogeneous crust of the Lau Basin carries many of the signatures of supra-subduction zone (SSZ) melts but also has a distinct MORB-like component. Mixing between SSZ and MORB mantle sources may explain the variations and the spatial distribution of magma types.

Geochemistry of ODP Hole 176-735B igneous and hydrothermal veins

During Legs 118 and 176, Ocean Drilling Program Hole 735B, located on Atlantis Bank on the Southwest Indian Ridge, was drilled to a total depth of 1508 meters below seafloor (mbsf) with nearly 87% recovery. The recovered core provides a unique section of oceanic Layer 3 produced at an ultraslow spreading ridge. Metamorphism and alteration are extensive in the section but decrease markedly downward. Both magmatic and hydrothermal veins are present in the core, and these were active conduits for melt and fluid in the crust. We have identified seven major types of veins in the core: felsic and plagioclase rich, plagioclase + amphibole, amphibole, diopside and diopside + plagioclase, smectite ± prehnite ± carbonate, zeolite ± prehnite ± carbonate, and carbonate. A few epidote and chlorite veins are also present but are volumetrically insignificant. Amphibole veins are most abundant in the upper 50 m of the core and disappear entirely below 520 mbsf. Felsic and plagioclase ± amphibole ± diopside veins dominate between ~50 and 800 mbsf, and low-temperature smectite, zeolite, and prehnite veins are present in the lower 500 m of the core. Carbonate veinlets are randomly present throughout the core but are most abundant in the lower portions. The amphibole veins are closely associated with zones of intense crystal plastic deformation formed at the brittle/ductile boundary at temperatures above 700°C. The felsic and plagioclase-rich veins were formed originally by late magmatic fluids at temperatures above 800°C, but nearly all of these have been overprinted by intense hydrothermal alteration at temperatures between 300° and 600°C. The zeolite, prehnite, and smectite veins formed at temperatures <100°C. The chemistry of the felsic veins closely reflects their dominant minerals, chiefly plagioclase and amphibole. The plagioclase is highly zoned with cores of calcic andesine and rims of sodic oligoclase or albite. In the felsic veins the amphibole ranges from magnesio-hornblende to actinolite or ferro-actinolite, whereas in the monomineralic amphibole veins it is largely edenite and magnesio-hornblende. Diopside has a very narrow range of composition but does exhibit some zoning in Fe and Mg. The felsic and plagioclase-rich veins were originally intruded during brittle fracture at the ridge crest. The monomineralic amphibole veins also formed near the ridge axis during detachment faulting at a time of low magmatic activity. The overprinting of the igneous veins and the formation of the hydrothermal veins occurred as the crustal section migrated across the floor of the rift valley over a period of ~500,000 yr. The late-stage, low-temperature veins were deposited as the section migrated out of the rift valley and into the transverse ridge along the margin of the fracture zone.

Geochemistry of sheeted dike complex minerals of ODP Hole 140-504B

Diabases were recovered during Legs 137 and 140 at Hole 504B from depths between 1621.5 and 2000.4 meters below seafloor in the lower sheeted dike complex. The samples contain multiple generations of millimetric to centimetric veins. The orientation of the measured veins suggests that two main vein sets exist: one characterized by shallow dipping and the other by random trend. Thermal contraction during rock cooling is considered the main mechanism responsible for fracture formation. Vein infill is related to the circulation of hydrothermal fluids near the spreading axis. Some veins are surrounded by millimeter-sized alteration halos due to fluid percolation from the fractures through the host rock. Vein-filling minerals are essentially amphibole, chlorite, and zeolites. Amphibole composition is controlled by the microstructural site of the rock. Actinolite is the main amphibole occurring in the veins and also in the groundmass away from the halos. In the alteration halos, amphibole shows composition of actinolitic hornblende and Mg-hornblende. Late-stage tension gashes and interstitial spaces in some amphibole-bearing veins are filled with zeolites, suggesting that the veins likely suffered multiple opening stages that record the cooling history of the circulating fluids. Evidence of deformation recorded by the recovered samples seems to be restricted to veins that clearly represent elements of weakness of the rock. On the basis of vein geometry and microstructure we infer structural interpretations for the formation mechanism and for deformation of veins.

Geochemical composition of minerals obtained from ODP Sites 180-1109, 180-1117 and 180-1118

During the last 8 m.y. the Papuan Peninsula region of Papua New Guinea has been affected by extension which opened the Woodlark Basin. The present-day spreading tip is located at the foot of the Moresby Seamount, a crustal block whose northern flank is an active low-angle normal fault related to this extension. During Ocean Drilling Program Leg 180 (7 June-11 August 1998), 11 sites (1108-1118) were drilled along a north-south-trending transect across the Woodlark Basin just ahead of the spreading tip. Four of these sites (1118, 1109, 1114, and 1117) reached the crystalline basement, which is composed of diabase and gabbro. Sites 1118 and 1109, located on the Woodlark Rise, belong to the hanging wall block, and Sites 1114 and 1117, located on the crest of the Moresby Seamount, belong to the footwall block and the fault zone itself. Most of the basalt, diabase, and gabbro that were recovered show a well-preserved magmatic texture. The diabase, which is the most abundant rock type, has a coarse-grained ophitic texture composed of poikilitic clinopyroxene including radiating, locally skeletal plagioclase laths with interstitial iron oxide grains. Secondary mineralogy consists of chlorite, zeolite, calcite, albite, and quartz. The gabbro shows a medium-grained granular texture. The magmatic mineralogy consists of euhedral laths of plagioclase and anhedral interstitial clinopyroxene. Secondary mineralogy consists of a magnesio to actinolitic hornblende, chlorite, clinozoisite, zeolite, quartz, and calcite. The retrograde metamorphic evolution of both gabbro and diabase occurred under low amphibolite to subgreenschist facies conditions associated mainly with brittle deformation and the development of a local low-temperature shear zone. This shows no evidence for high thermal gradient in the crust during the continental rifting.

Major element compositions, minerals and trace elements at DSDP Leg 67 Holes

Mineralogical (microprobe) and geochemical (X-ray fluorescence, neutron activation analyses) data are given for 18 samples of volcanic rocks from the Guatemala Trench area (Deep Sea Drilling Project Leg 67). Typical fresh oceanic tholeiites occur in the trench itself (Hole 500) and in its immediate vicinity on the Cocos Plate (Site 495). Several samples (often reworked) of "spilitic" oceanic tholeiites are also described from the Trench: their mineralogy (greenschist facies association - actinolite + plagioclase + chlorite) and geochemistry (alteration, sometimes linked to manganese and zinc mineralization) are shown to result from high-temperature (300°-475°C) hydrothermal sea water-basalt interactions. The samples studied are depleted in light rare-earth elements (LREE), with the exception of the slightly LREE-enriched basalts from Hole 500. The occurrence of such different oceanic tholeiites in the same area is problematic. Volcanic rocks from the Guatemala continental slope (Hole 494A) are described as greenschist facies metabasites (actinolite + epidote + chlorite + plagioclase + calcite + quartz), mineralogically different from the spilites exposed on the Costa Rica coastal range (Nicoya Peninsula). Their primary magmatic affinity is uncertain: clinopyroxene and plagioclase compositions, together with titanium and other hygromagmaphile element contents, support an "active margin" affinity. The LREE-depleted patterns encountered in the present case, however, are not frequently found in orogenic samples but are typical of many oceanic tholeiites.

The activity of the feminist online publications: challenges for the transmission of the feminist culture in Spain

Traditionally, big media corporations have contributed to hiding the women’s movement itself, as well as its main claims and topics of discussion (Marx, Myra y Hess, 1995; Rhode, 1995; Mendes, 2011). This has led the feminist movement to develop its own media generally print publications, usually, with a very specialized character and reduced audience. This is similar to what has occurred with quality main stream media, asthese publications have had to adapt themselves to a new communicatiion context, because of the financial crisis and  technological evolution. Feminist media has found in the Internet an excellent opportunity to access citizens and communicate their messages. , In view of this scene of change and renovation,  this article offers the results of a qualitative analysis focused on the experiences of four feminist online media sites edited in Spain: Pikaramagazine.com, Proyecto-kahlo.com, Mujeresenred.net and Laindependent.cat. Besides exploring the characteristics and content of these sites, the article pays attention to the virality of their contents spread through Facebook and Twitter. The onclusion estimates their social impact, insofar as they symbolize the specialization, diversification and dialogue promoted by the Web.

Módulo de comunicación y creatividad: taller conversacional. Orientaciones didácticas

Este ‘Taller conversacional’ tiene como objetivo desarrollar habilidades que faciliten una inclusión total en el entorno. Se contempla la conversación como una manifestación de comunicación entre las personas, pero también como un proceso de conocimiento de uno mismo y de los que participan en la conversación, así como una estrategia de adquisición de conocimientos sobre los diferentes temas que se abordan. El taller se desarrolló en una muestra de jóvenes con síndrome de Down y con otras discapacidades intelectuales de 15 a 20 años y también en una muestra de adultos con edades comprendidas entre los 21 y 35 años. La guía didáctica que aquí se presenta (junto con el resto de materiales didácticos de apoyo) es el resultado de este trabajo llevado a cabo entre octubre de 2011 y mayo de 2014. En ella se explica el modo en que se desarrollaron las actividades a través de un modelo didáctico mediacional; no pretende ser un conjunto de orientaciones estáticas e inflexibles, sino más bien, la descripción didáctica de una experiencia desarrollada con una muestra limitada de jóvenes y adultos con síndrome de Down. Cada profesor sabrá adaptar lo que aquí se propone a su caso particular. Esta guía se estructura en los siguientes elementos: objetivos y contenido, actividades organizadas en niveles, orientaciones didácticas, desarrollo metodológico de las actividades, evaluación y seguimiento, materiales didácticos de apoyo, organización de las sesiones, y actividades con las familias.

Aplicación de la filtración gruesa para diseño de una planta de tratamiento de aguas de alto riesgo mediante filtración gruesa

Mediante filtración gruesa se puede tratar agua efectivamente aún siendo de alto riesgo, para esto se recomienda el uso de filtro grueso dinámico, filtro grueso ascendente en capas y filtro lento de arena. Este proceso es efectivo para zonas rurales y de escasos recursos, pues el costo de mantenimiento y uso de químicos es bajo y de fácil manejo. Su dificultad radica en el extenso espacio físico y con gradientes efectivos que favorezcan el proceso por fuerzas gravitatorias. En general es un método práctico, lógico, materiales del lugar y de fácil operación.

Alternativas de uso da borra de café através de hidrólise ácida, enzimática, ou como substrato para a produção das enzimas: lacase e celulase

In the industrial production of soluble coffee, huge amounts of extracted coffee residues are generated; onaverage, for eachtonne of green coffee extracted, 480 kg of coffee ground waste is produced. This is a solid residue currently used to generate energy at the steam boilers from the soluble coffee industry. Some is also used or as fertilizer on agriculture fields. Seeking a better end use, the work reported here aimed to study the viability of hydrolyzing the coffee ground residue for the production of carbohydrates. Hydrolysis was undertaken with hydrochloric acid at different temperatures and pressures, using a water bath or autoclave.An enzymatic hydrolysis with Viscozyme Lwas developed using Whatman filter paper No1 and the optimal conditions were determined using a rotational central composite experimental design (DCCR).The best conditions to hydrolyze filter paper cellulose were 50 FBG (Fungal β-glucanase) of Viscozyme L at pH 4.0 for 1.0 h and 45 ºC. The ground coffee was hydrolyzed under the same conditions as described above for filter paper, however this enzymatic hydrolysis was not efficient. A combination of enzymatic hydrolysis as a pre-treatment for the ground coffee followed by acid hydrolysis using HCl conducted in an autoclave (120 C for 2.0 h) resulted in higher production of glucose as analyzed by HPLC. Another end use of the ground coffee evaluated was as source of substrate in the culture medium to grow Botryosphaeria rhodina MAMB-05 to produce the enzymes laccase and cellulase. Highest enzyme titres obtained were with 8% (w/v) coffee grounds to which was added a minimum salts medium(Vogel), under agitation conditions (180 rpm) at 28ºC. The phenolic compounds present in the coffee grounds appear to have induced laccase by Botryosphaeria rhodina.

Impact de la lumière sur la production de protéines recombinantes chez Nicotiana benthamiana

La moléculture végétale est une approche prometteuse pour la production de protéines d’intérêt médical ou industriel. Considérant les variations de rendement possibles dans une plante soumise à différentes conditions culturales, nos objectifs étaient : (i) de cartographier l’accumulation d’un antigène viral d’intérêt clinique dans les feuilles du tabac sauvage Nicotiana benthamiana utilisé comme bio-usine, et (ii) d’évaluer l’impact de la lumière en période de croissance sur le rendement total en antigène. Nous avons étudié les relations entre l’âge foliaire, le régime lumineux, l’expression du transgène et le rendement final en antigène dans les feuilles. Nos données confirment l’influence de l’âge sur les variations de rendement d’une feuille à l’autre, et l’impact positif de l’intensité lumineuse sur le rendement par plante. Elles mettent aussi en relief l’importance des tiges secondaires sur le rendement et le rôle clé de la transcription du transgène sur la teneur en antigène à l’échelle cellulaire.

Las carencias de la prensa tradicional, un lastre para el periodismo emprendedor

Introducción: La prensa tradicional ha heredado a la digital cuatro retos; cada uno de ellos es objeto de análisis en esta investigación: atraer nuevos lectores con narrativas informativas multimedia, generar estrategias de proximidad con sus usuarios, crear nuevos modelos de negocio y proyectarse como espacio profesional que refleje la feminización de la carrera de periodismo. Metodología: Este artículo presenta los resultados de un análisis de contenido aplicado a 281 medios creados por el periodismo emprendedor. Resultados y conclusiones: Los resultados de este estudio constatan que el periodismo emprendedor no ha innovado en la presentación de la información (utiliza como principal reclamo la imagen fija). Adoptan el mismo modelo de negocio basado en la publicidad. Carecen de canales para establecer feedbacks con los usuarios. Por último, igual que el medio en papel, no es un espacio para el empoderamiento femenino.

Adaptación argentina del Inventario Psicológico de Ejecución Deportiva (IPED): validez, fiabilidad y precisión

El objetivo de este trabajo es presentar el proceso de adaptación del Inventario Psicológico de Ejecución Deportiva (IPED) para su uso con deportistas argentinos. En primer lugar, se estudió la equivalencia lingüística y conceptual mediante la evaluación de jueces expertos y la aplicación de una primera versión a deportistas de diferentes edades (población diana). Posteriormente, se aplicó la versión modificada de la escala a 664 deportistas de ambos géneros, entre 10 y 67 años de edad (M = 25,31; DT = 10,35) en dos formas de evaluación: en papel (n = 309) y online (n = 355), mediante una plataforma de evaluación informatizada. Se estudió la estructura de la escala mediante análisis factorial confirmatorio en las diferentes muestras de participantes, calculando los índices de validez y confiabilidad. Asimismo, se estudió la consistencia interna, las diferencias en las dos modalidades de evaluación y diferencias entre grupos (por género y nivel de competición). Los resultados mostraron que la escala en su versión adaptada para su uso con deportistas argentinos, logra evaluar de forma válida y fiable las habilidades psicológicas asociadas al rendimiento deportivo.

FUNGOS ASSOCIADOS ÀS SEMENTES DE Enterolobium contortisiliquum : ANÁLISE DA INCIDÊNCIA, CONTROLE E EFEITOS NA QUALIDADE FISIOLÓGICA COM O USO DE EXTRATOS VEGETAIS

Os fungos são os principais micro-organismos associados às sementes, podendo causar danos, tanto na fase de campo, como também na pós-colheita e durante o armazenamento. Nesta última fase, a deterioração pode ocorrer pela ação específica de fungos, afetando a qualidade fisiológica das sementes. A utilização de extratos de plantas com propriedades antimicrobianas são alternativas ecológicas e promissoras para substituir a proteção promovida pela aplicação de fungicidas. Objetivou-se nesta pesquisa avaliar a eficiência dos extratos de Allamanda blanchetti e Momordica charantia nas concentrações de 10, 100, 500 e 1000 ppm sobre a micoflora e germinação em sementes de Enterolobium contortisiliquum . As sementes foram coletadas em diferentes municípios do estado da Paraíba (Areia, Arara, Conde e Sobrado). Os lotes foram submetidos a testes de sanidade e de germinação. A avaliação da incidência de fungos foi feita a partir da visualização dos fungos através do método de papel de filtro. Utilizaram-se no teste de sanidade 100 sementes por tratamento, as quais foram imersas em 20 mL dos extratos por cinco minutos, em seguida incubadas em placas de Petri sobre dupla camada de papel de filtro. No teste de germinação utilizaram-se 200 sementes, distribuídas em papel germitest e germinadas à temperatura de 30 ± 2°C. O delineamento experimental utilizado foi o inteiramente casualizado. Constatou-se nas sementes de Enterolobium contortisiliquum os fungos: Aspergillus niger , Aspergillus flavus , Rhizopus stolonifer , Penicillium sp., Curvularia lunata , Nigrospora sp. e Cladosporium sp. Os extratos de Allamanda blanchetti e Momordica charantia nas concentrações de 500 e 1000 ppm causaram redução da frequência dos fungos. O extrato de Momordica charantia nas concentrações de 500 e 1000 ppm proporcionou o aumento na germinação e primeira contagem, além de reduzir o percentual de sementes mortas.