Señal salud

Señal Salud es un programa radial dedicado a la promoción de hábitos y conductas saludables, que nació en el 2003. Este espacio, desarrollado desde entonces por el Departamento de Educación y Comunicación para la Salud, es conducido por Sergio Gras y producido por Leonardo Rearte, Licenciado en Comunicación graduado en la Universidad Nacional de Cuyo. El programa producido en el Centro de Comunicación e Información de la UNCuyo fue emitido por FM Universidad (95.3) también al resto de la provincia a través de más de 15 radios. Señal Salud tiene una agenda temática, destinando a cada emisión el tratamiento de un tema en particular (diabetes, salud bucal, sida, accidentes, etc.). El programa, durante sus diez minutos, plantea mitos, presenta a un especialista, abre el micrófono al público, repasa el tratamiento del tema en los medios masivos y entrega cinco soluciones.Considerando que toda información tiene potencialmente la capacidad de ser entendida como una fuerza transformadora, facilita procesos cognoscitivos y atiende necesidades de un grupo determinado de personas. Así es como Señal Salud busca mejorar la calidad de vida todos los mendocinos.

Trombolisis en el tromboembolismo de pulmón

Fil: Valdivieso, W.. Universidad Nacional de Cuyo. Facultad de Ciencias Médicas. Área de Cardiología

Manejo del bajo gasto cardíaco en el posoperatorio cardiovascular pediátrico

Fil: Grzona, María Estela. Universidad Nacional de Cuyo. Facultad de Ciencias Médicas. Departamento de Pediatría, Gineco-Obstetricia y Salud Pública

Tratamiento de úlceras venosas de piernas : revisión bibliográfica

Fil: Vidal, Jorgelina Natalí. Hospital Luis Lagomaggiore (Mendoza, Argentina). Servicio de Dermatología

Factores trombogénicos sistémicos en paciente con síndrome coronario agudo con cinecoronariografía normal y patológica

En la fisiopatología del síndrome coronario agudo (SCA) sin evidencia de lesión ateromatosa oclusiva, podría participar un estado de hipertrombogenicidad sanguínea, generado por factores trombogénicos sistémicos, como los factores de riesgo cardiovascular y los que intervienen en el balance coagulación-anticoagulación, fibrinolisis y formación de fibrina. Objetivo: Estudiar y comparar los factores trombogénicos sistémicos en pacientes con SCA y cinecoronariografía (CCG) normal y patológica.

Succession of benthic hard-bottom communities in the shallow sublitoral of Comau Fjord, Chile

Succession was already studied over decades. The present thesis investigated the succession on hard substrate at two different study sites within the fjord Comau, Chile. Nine plates were installed at both sites (mouth of fjord and inner fjord) and photographed over three years. Additionally the natural community was recorded and a ground truthing was carried out to verify the analyzed species. Respectively at both sites over 50 different species were identified. Abundance data decreased with only one exception continuously, whereas the percentage cover increased. But the communities on the recruitment plates do still not reach the community structure of the natural environment. The present data showed that the hard-bottom succession in the fjord Comau is best described by the TOLERANCE MODEL (Connell & Slatyer, 1977). An important species of the natural community is the stony coral Desmophyllum dianthus, which normally (outside the fjord) grows beneath 1000 m water depth. The results of this work indicate that the mature community is not reached after 36 months.

Miozene larger foraminifera in ODP Leg 133 holes

The Marion Plateau is a large carbonate platform off northeastern Queensland. Three sites (815, 816, and 826) were drilled on this platform and form the basis for this study. Larger benthic foraminifers, together with rare planktonic forms from the shallow-water carbonates that form the main part of the platform sequence, were studied to establish a biostratigraphy. The presence of Lepidocyclina (Nephrolepidiná) howchini sensu lato and Ladoronia vermicularis, together with Globorotalia (Globorotalia) praemenardii and Orbulina, indicate an early middle Miocene (N9-N12) age (i.e., lower Tf stage) for these carbonates. Dolomitization has destroyed much of the original fabric of these carbonates, making study of the larger foraminifers difficult. Sites 815 (forereef location) and 826 (backreef, lagoonal setting) provide the best faunas. However, at all sites nodular coralline algae and Halimeda are the major bioclasts; coral fragments form a major component at Sites 816 and 826. The middle Miocene neritic sequence is separated from the overlying hemipelagic sequence by an unconformity that spans much of the middle and late Miocene. At Site 815, which is in a forereef situation, the overlying hemipelagic sequence contains a Zone N17A fauna, but at Site 816, higher on the platform, a similar sequence contains a Zone N19 fauna. The faunas indicate that the platform was built up during the early middle Miocene and remained at fairly constant water depths and temperatures during this period. It was then exposed prior to subsiding rapidly during the late Miocene and Pliocene to depths similar to those of the present day.

Bivalve mollusks in the sediments of the Anapa Bay Bar (Black Sea) in October 2010

Sandy beaches of the Anapa Bay Bar are a unique natural resource, but they are gradually being degrade under both natural and anthropogenic factors. Emissions of sand and shelly ground from the adjacent sea bottom partly compensate for this process. Concentration of carbonates may reach up to 50% in beach sands, and most of these carbonates are of mollusk origin. The major deposit formation role belongs to the key bivalve species: Chamelea gallina (Linnaeus, 1758). Average biomass of this mollusk species reaches up to 450 g/m**2 at depths 5-10 m. The other two subdominating mollusk species, bivalve Donax trunculus (Linnaeus, 1758) and gastropod Rapana venosa (Valenciennes, 1846), may impact as 16 g/m**2 and 6 g/m**2, respectively. Annually, 350 kg of shelly ground per running meter are newly deposited on the Anapa beach.