Complejo granuloma eosinofílico

El complejo granuloma eosinofílico agrupa tres entidades clínico/histológicas denominadas granuloma colagenolítico, placa eosinofílica y úlcera indolente. En el presente artículo se describe su etiología y sus aspectos clínicos y terapéuticos.The eosinophilic granuloma complex is comprised of three clinical/histological entities: collagenolytic granuloma, eosinophilic plaque and indolent ulcer. In this article, its etiology, clinical aspects and therapy are discussed

Síndrome uveodermatológico en el perro

Se describe un caso de síndrome uveodermatológico en un perro Mastín español, macho, de 2 años. Los signos clínicos observados eran similares al síndrome de Vogt- Koyanagi-Harada humano y se caracterizaban por una uveitis asociada a una despigmentación y erosión cutánea y mucocutánea en cara, escroto, región perianal y almohadillas plantares. El estudio histopatológico reveló una dermatitis liquenoide, en la que predominaban los macrófagos. El tratamiento se basó en la administración oral de prednisona asociada a una terapia ocular tópica a base de atropina y corticosteroides. Al cabo de 8 meses las lesiones cutáneas y mucosas remitieron completamente.A case of uveodermatologic syndrome in a male 2 year old, Spanish Mastiff is described. The clinical signs found, namely uvezitis associated with cutaneus and mucocutaneous depigmentation and erosions of the face, scrotum, perianal region and footpads, were similar to those of the human Vogt-Koyanagi-Harada syndrome. The histopathological study showed a lichenoid dermatitis with prevalence of macrophages. The treatment encompassed the administration of prednisone per os and topical ocular therapy with corticosteroids associated with atropin e. After 8 months the cutaneous and mucosal Iesions had completely remitted

Emissions of Fe(II) and its kinetic of oxidation at Tagoro submarine volcano, El Hierro

The eruptive process that took place in October 2011 in the submarine volcano Tagoro off the Island of El Hierro and the subsequent degasification stage, five months later, have increased the concentration of TdFe(II) (Total dissolved iron(II)) in thewaters nearest to the volcanic edifice. In order to detect any variation in concentrations of TdFe(II) due to hydrothermal emissions, three cruiseswere carried out two years after the eruptive process in October 2013,March 2014 andMay 2015. The results fromthese cruises confirmed important positive anomalies in TdFe(II), which coincided with negatives anomalies in pHF,is (pH in free scale, at in situ conditions) located in the proximity of themain cone. Maximumvalues in TdFe(II) both at the surface, associated to chlorophyll a maximum, and at the sea bottom, were also observed, showing the important influence of organic complexation and particle re-suspension processes. Temporal variability studies were carried out over periods ranging from hours to days in the stations located over themain and two secondary cones in the volcanic edifice with positive anomalies in TdFe(II) concentrations and negative anomalies in pHF,is values. Observations showed an important variability in both pHF,is and TdFe(II) concentrations, which indicated the volcanic area was affected by a degasification process that remained in the volcano after the eruptive phase had ceased. Fe(II) oxidation kinetic studies were also undertaken in order to analyze the effects of the seawater properties in the proximities of the volcano on the oxidation rate constants and t1/2 (half-life time) of ferrous iron. The increased TdFe(II) concentrations and the low associated pHF,is values acted as an important fertilization event in the seawater around the Tagoro volcano at the Island of El Hierro providing optimal conditions for the regeneration of the area.En prens

Search for shape-coexisting 0(+) states in Ni-66 from lifetime measurements

The lifetime of the 0(3)(+) state in Ni-66, two neutrons below the N = 40 subshell gap, has been measured. The transition B(E2; 0(3)(+) -> 2(1)(+)) is one of the most hindered E2 transitions in the Ni isotopic chain and it implies that, unlike Ni-68, there is a spherical structure at low excitation energy. We have performed extensive shell-model calculations that correctly predict this result, obtaining a spherical 0(+) state at the correct energy and with an extremely low B(E2; 0(3)(+)-> 2(1)(+)) value

The natural ocean acidification and fertilization event caused by the submarine eruption of El Hierro

Versión del edito

Comparison of Maldi-Tof with gene sequencing in bacteria isolates from plants belonging to family Rhizobiaceae

Comunicaciones a congreso

Reconstrucción paleoclimática y paleoambiental de la Península Ibérica durante el Cuaternario, aplicación de modelos geoprospectivos para la evaluación de escenarios futuros

Esta comunicación trata de resumir el trabajo realizado por el ITGE, BRGM, CCMA, IPE, ETSIMM y ENRESA en el proyecto titulado "Paleoclimatological Revision of Climate Evolution and Environment in Western Mediterranean Region. Evaluation of future evolution scenarios in the Iberian Peninsula", en el marco del Programa de la Comisión de las Comunidades Europeas sobre Gestión y Almacenamiento de Residuos Radioactivos (contrato CEC FI2WCT91- 0075)

Severe Deoxygenation Event Caused by the 2011 Eruption of the Submarine Volcano Tagoro (El Hierro, Canary Islands)

The shallow, near-shore submarine volcano Tagoro erupted in October 2011 at the Mar de las Calmas marine reserve, south of El Hierro island. The injection of lava into the ocean had its strongest episode during November 2011 and lasted until March 2012. During this time, in situ measurements of dissolved oxygen were carried out, using a continuous oxygen sensor constantly calibrated with water samples. A severe deoxygenation was observed in the area, particularly during October-November 2011, which was one of the main causes of the high mortality observed among the local marine ecosystem. The measured O2 concentrations were as low as 7.71 µmol kg-1, which represents a -96% decrease with respect to unaffected waters. The oxygen depletion was found in the first 250 m of the water column, with peaks between 70-120 m depth. The deoxygenated plume covered an area of at least 464 km2, distributed particularly south and south-west of the volcano, with occasional patches found north of the island. The oxygen levels were also monitored through the following years, during the degassing stage of the volcano, when oxygen depletion was no longer observed. Additionally, during the eruption, an island-generated anticyclonic eddy interacted with the volcanic plume and transported it for at least 80 km, where the O2 measurements still showed a -8% decrease after mixing and dilution. This feature draws attention to the permanence and transport of volcanic plumes far away from their source and long after the emission.En prens

Significant Release of Dissolved Inorganic Nutrients From the Shallow Submarine Volcano Tagoro (Canary Islands) Based on Seven-Year Monitoring

Tagoro, the shallow submarine volcano that erupted south of El Hierro (Canary Islands, Spain) in October 2011, has been intensely monitored for over 7 years, from the early eruptive stage to the current degassing stage characterized by moderate hydrothermal activity. Here, we present a detailed study of the emissions of inorganic macronutrients (NO2– + NO3–, PO4, and Si(OH)4) comprising a dataset of over 3300 samples collected through three different sampling methodologies. Our results show a significant nutrient enrichment throughout the whole studied period, up to 8.8-fold (nitrate), 4.0-fold (phosphate), and 16.3-fold (silicate) in the water column, and larger enrichments of phosphate (10.5-fold) and silicate (325.4-fold), but not of nitrate, in the samples collected directly from the vents. We also provide some preliminary results showing ammonium (NH4+) concentrations up to 1.97 μM in the vent fluids as compared to 0.02 μM in the surrounding waters. Nutrient fluxes from the volcano during the degassing stage were estimated as 3.19 ± 1.17 mol m–2 year–1 (NO2– + NO3–), 0.02 ± 0.01 mol m–2 year–1 (PO4), and 0.60 ± 1.35 mol m–2 year–1 (Si(OH)4), comparable to other important nutrient sources in the region such as fluxes from the NW-African upwelling. Nutrient ratios were affected, with a minimum (NO3– + NO2–):PO4 ratio of 2.36:1; moreover, a linear correlation between silicate and temperature enabled the use of this nutrient as a mixing tracer. This study sheds light on how shallow hydrothermal systems impact the nutrient-poor upper waters of the ocean.En prens

Viabilidad del uso de fotodetectores SiPM en sistemas PET/IRM

Actas de: XXVIII Congreso Anual de la Sociedad Española de Ingeniería Biomédica (CASEIB 2010). Madrid, 24-26 de noviembre de 2010.El fotomultiplicador de silicio (SiPM) es un detector compuesto por una matriz de fotodiodos funcionando en modo avalancha, también conocido como modo Geiger. Se trata de un dispositivo de alta eficiencia en la detección de fotones que, por tratarse de un semiconductor, es compacto, teóricamente insensible a campos magnéticos, y de bajo coste. Además, la electrónica asociada es sencilla y podría integrarse en el mismo dispositivo. Estas características hacen de este componente un buen candidato para construir detectores de rayos gamma para imagen médica nuclear (PET y SPECT). En este trabajo se evalúan las prestaciones de tres detectores diferentes de 1 x 1 mm2 y una matriz de 2 x 2 SiPMs (6 x 6 mm² área activa total). Se ha analizado la dependencia de los parámetros operacionales del dispositivo en presencia de campos magnéticos estáticos intensos y de los campos de radiofrecuencia generados por un sistema de IRM preclínico, en condiciones extremas de trabajo en cuanto a intensidad y frecuencia de conmutación de los gradientes de campo. Al mismo tiempo se ha verificado que la presencia de estos dispositivos en la zona de imagen de la RM no afecta a la calidad de la misma.Este trabajo ha sido financiado por los proyectos TEC2007-64731, TEC 2008-06715-C02-1 del Ministerio de Ciencia e Innovación, por la RETIC-RECAVA del Ministerio de Sanidad y Consumo, por el programa ARTEMIS S2009/DPI-1802 de la Comunidad de Madrid, por el proyecto europeo FMT-XCT FP7-201792, los programas FPA2007-62216, TEC2008-06715-C02-01, UCM (Grupos UCM; 910059), CPAN (Consolider-Ingenio 2010) y CSPD-2007-00042. Parte de los cálculos realizados en este trabajo se han hecho en el ‘‘High Capacity Cluster for Physical Techniques’’ de la UCM, financiados en parte por la UE bajo el programa FEDER, y en otra parte por la UCM.Publicad