Ángela Sierra González (ed.) Discursos políticos, identidades y nuevos paradigmas de gobernanza en América Latina. Barcelona, Laertes, 2015. 264 pp.

Fil: Bolla, Luisina. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación. Instituto de Investigaciones en Humanidades y Ciencias Sociales (UNLP-CONICET); Argentina.

PLAN DE GESTIÓN COMUNITARIA DEL TURISMO PARA LA SIERRA DE TEPEQUEM, MUNICIPIO AMAJARI - RORAIMA - BRASIL

Esto trabajo objetiva diseñar un plan de gestión comunitaria del turismo para la Sierra de Tepequem, localizada en el Municipio Amajari, Estado de Roraima, Brasil. Se utilizó el método cualitativo y cuantitativo. Se hizo uso de instrumentos como: entrevistas grabadas con informantes clave de la referida comunidad; cuestionarios aplicado a los turista para determinar el perfil de los mismo; cuestionario a la comunidad para determinar su opinión sobre el desarrollo del turismo y su participación en la gestión comunitaria; cuestionario a los actores privados y públicos para obtener su opinión sobre el desarrollo del turismo en el sitio y el rol de responsabilidad de cado actor involucrado en la actividad turística; observación de campo para diagnosticar la situación actual de los recursos naturales, culturales, la gestión comunitaria y el desarrollo turístico en el sitio; además de recolectar informaciones en documentos publicados anteriormente. Los instrumentos aplicados facilitaron la realización del diagnóstico, pronóstico, el análisis DOFA y la formulación de las políticas prioritarias para que el éxito del plan. Con base en los estudios anteriormente expuestos se desarrollo el Plan de Gestión Comunitaria del Turismo para la Sierra de Teqpequem.

ENTRE AGRICULTURA COMERCIAL Y SOBERANÍA ALIMENTARIA: LOS RETOS DEL CAMPESINADO EN LA SIERRA ECUATORIANA

En Ecuador, la migración campesina es el motor principal de las recomposiciones actuales del medio rural andino. En la provincia del Azuay, el corazón histórico de la dinámica migratoria nacional, la disminución de la mano de obra en los últimos años provocó una desestructuración de los hogares campesinos y una reorganización lógica de las tareas agrícolas. La desaparición progresiva de los cultivos de ciclo largo, como el maíz, se hizo al inverso del aumento de las superficies de pasto, cuyo resultado fue la « pecuarización » de la economía campesina. No obstante, desde hace diez años, la utilización más racional de la mano de obra y la intensificación del trabajo sobre micro-huertos participan al renacimiento de la agricultura familiar local. Gracias a la cercanía de la ciudad de Cuenca, los grupos campesinos han desarrollado redes comerciales dinámicas al cultivar hortalizas y frutales. Actualmente, son más de 350 familias que viven principalmente de la agricultura, con ingresos regulares, y todas pertenecen a diferentes asociaciones de productores agroecológicos cuya visibilidad es cada vez más importante en los mercados urbanos. A través de esta ponencia, nos proponemos mostrar como los grupos campesinos se han vuelto los actores claves del aprovisionamiento urbano regional, desarrollando un agricultura sustentable capaz de responder al reto de la seguridad alimentaria en la región andina.

ACTORES SOCIALES EN LA GESTIÓN DEL TERRITORIO Y RIESGOS AMBIENTALES EN LA SIERRA NORTE DE PUEBLA

Esta ponencia tiene como objetivo analizar, en el contexto de la descentralización del Estado y recorte del gasto público que enfrenta México desde1982, la participación de actores sociales en la gestión del territorio y riesgos ambientales en la Sierra Norte de Puebla; área agrícola, sujeta al impacto de amenazas naturales que impactan negativamente en la calidad de vida de la población de la región, predominantemente indígena en condiciones de marginalidad. En particular se analiza el caso de la Cooperativa Agropecuaria Regional Tosepan-Titataniske, organización con presencia en la sierra, que en las últimas décadas ha realizado actividades exitosas para elevar la calidad de vida de los habitantes de la región; entre ellas la organización comunitaria en torno a los cultivos de café y pimienta, la gestión de recursos para dotar de infraestructura a las localidades, y la gestión de riesgos y prevención de desastres.

AVALANCHAS EN LA SIERRA VOLCANICA CENTRAL. EL CASO DE RIO CIRUELAS

El dia 20 de julio de 1988, en la tarde, se produjo una avalancha considerable en el rio Ciruelas, localizado en la ladera suroeste del volcán Barva, Heredia, Costa Rica, causando daños enormes en la población de San Bosco de Santa Bárbara.  El área afectada se dividió en tres grandes sectores, descritos a continuación: I.        SECTOR SUPERIOR (DESLIZAMIENTOS)Comprendido entre las cotas de 2.600m y 2.800 m, o sea cerca de la cima del Barva, caracterizado por desprendimientos de materiales poco consolidados (cenizas gruesas) con un ancho de aproximadamente 30m-40m y una profundidad de aproximadamente 4m-5m en casi todos los afluentes del rio Ciruelas. II.      SECTOR INTERMEDIO (TRANSITO)Comprendido entre las cotas de 2.600m y 1.600m, caracterizado por profundización erosiva del cauce en areas de materiales poco resistentes y por la ocurrencia de pequeños deslizamientos secundarios causados por la profundización del cauce. III.    SECTOR BAJO ( SEDIMENTACION)De 1.600m hasta 950m, caracterizado por la sedimentación en los primeros kilómetros de material grueso(bloques mayores de 2m). El pueblo de San Bosco esta situado sobre un abanico aluvial de materiales de eventos similares. En lo9s siguientes kilómetros se presenta la sedimentación de materiales mas finos.  La causa de esta desastre es únicamente la presencia de lluvias de alta intensidad provocadas por un frente de brisa, que en este dia ocurrieron en el sector I, provocando los deslizamientos y por ende las avalanchas de rocas y lodo que llegaron a los lugares mas bajos. Por estar el sector superior totalmente y el sector intermedio parcialmente en la selva virgen del Parque Nacional Braulio Carrillo se puede excluir definitivamente algún impacto humano que haya causado la desestabilización de las laderas. Por los vestigios de eventos antiguos de este tipo( acumulaciones cerca de San Bosco) se puede derivar que estos fenómenos también ocurrieron en tiempos pasados , sin embargo, se estima la probabilidad de una repetición pronta como muy baja. SUMMARYA big avalanche  that occurred the 20 th of july in the afternoon in the (rio ciruelas) watershed situated on the sowthwestern slope of the Volcano Barva, Costa Rica, caused big losses in the village of San Bosco de Santa Barbarbara. Based on field observations we distinguished three sectors analysed below: I.                    SUPERIOR SECTOR (LAND SLIDES)Localed in altitude between 2.600m and 2.800m near the peak of the volcano, characterized by landslides of poorly consolidated ashes, with a  width of between 30m-40m and a depth of about 4m to 5m, found in nearly and all of the affluents of the (Rio Ciruelas). II.                  MEDIUM SECTOR (TRANSIT)Between 2.600m and 1.600m, characterized by deep erosion in area of materials of low resistivity and by secondary(small) landslides provoked by the destruction of the support. III.                LOWER SECTOR ( SEDIMENTATION)Between 1.600m and 950m, characterized by sedimentation, in the first kilometers of coarse material (sometimes<2m).The village of San Bosco was constructed exactly above the detrictic cone of anterior events. In the subsequent kilometers we found the sedimentation of fine materials. As the cause of this desastre we analysed high intensity rainfalls provoked by a local front in the zone of the firt sector, causing landslides and then avalanches in the lower part of the primary forest of the national park <<Braulio Carrillo>>.The sediments of older events(the San Bosco cone) prove that avalanches ocurr in this area with a certain frecuency, but with relatively long recurrence intervals.   

A longitudinal study of mental health in refugees from Burma : the impact of therapeutic interventions

Objective: The present study seeks to examine the impact of therapeutic interventions for people from refugee backgrounds within a naturalistic setting. Method: Sixty-two refugees from Burma were assessed soon after arriving in Australia. All participants received standard interventions provided by a resettlement organisation which included therapeutic interventions, assessment, social assistance, and referrals where appropriate. At the completion of service provision a follow-up assessment was conducted. Results: Over the course of the intervention, participants experienced a significant decrease in symptoms of post-traumatic stress disorder, anxiety, depression and somatisation. Pre-intervention symptoms predicted symptoms post-intervention for post-traumatic stress, anxiety, and somatisation. Post-migration living difficulties, the number of traumas experienced, and the number of contacts with the service agency were unrelated to all mental health outcomes. Conclusions: In the first Australian study of its kind, reductions in mental health symptoms post-intervention were significantly linked to pre-intervention symptomatology and the number of therapy sessions predicted post-intervention symptoms of post-traumatic stress. Future studies need to include larger samples and control groups to verify findings.

Pulling apart the mid to late Cenozoic magmatic record of the Gulf of California : no room for the Comondú Arc

Understanding the link between tectonic-driven extensional faulting and volcanism is crucial from a hazard perspective in active volcanic environments, while ancient volcanic successions provide records on how volcanic eruption styles, compositions, magnitudes and frequencies can change in response to extension timing, distribution and intensity. Significantly, incorrect tectonic interpretations can be made when the spatial-temporal-compositional trends of, and source contributions to magmatism are not properly considered. This study draws on intimate relationships of volcanism and extension preserved in the Sierra Madre Occidental (SMO) and Gulf of California (GoC) regions of western Mexico. Here, a major Oligocene rhyolitic ignimbrite “flare-up” (>300,000 km3) switched to a dominantly bimodal and mixed effusive-explosive volcanic phase in the Early Miocene (~100,000 km3), associated with distributed extension and opening of numerous grabens. Rhyolitic dome fields were emplaced along graben edges and at intersections of cross-graben and graben-parallel structures during early stages of graben development. Concomitant with this change in rhyolite eruption style was a change in crustal source as revealed by zircon chronochemistry with rapid rates of rhyolite magma generation due to remelting of mid- to upper crustal, highly differentiated igneous rocks emplaced during earlier SMO magmatism. Extension became more focused ~18 Ma resulting in volcanic activity being localised along the site of GoC opening. This localised volcanism (known as the Comondú “arc”) was dominantly effusive and andesite-dacite in composition. This compositional change resulted from increased mixing of basaltic and rhyolitic magmas rather than fluid flux melting of the mantle wedge above the subducting Guadalupe Plate. A poor understanding of space-time relationships of volcanism and extension has thus led to incorrect past tectonic interpretations of Comondú-age volcanism.

25 million years to break a continent : early to middle Miocene rifting and syn-extensional magmatism in the southern Gulf of California

Cenozoic extension in western Mexico has been divided into two episodes separated by the change from convergence to oblique divergence at the plate boundary. The Gulf Extensional Province is thought to have started once subduction ended at ~12.5 Ma whereas early extension is classified as Basin and Range. Mid-Miocene volcanism of the Comondú group has been considered as a subduction-related arc, whereas post ~12.5 Ma volcanism would be extension-related. Our new integration of the continental onshore and offshore geology of the south-east Gulf region, backed by tens of Ar-Ar and U-Pb ages and geochemical studies, document an early-mid Miocene rifting and extension-related bimodal to andesitic magmatism prior to subduction termination. Between ~21 and 11 Ma a system of NNW-SSE high-angle extensional faults rifted the western side of the Sierra Madre Occidental (SMO) ignimbrite plateau. In Nayarit, rhyolitic domes and some basalts were emplaced along this extensional belt at 18-17 Ma. These rocks show strong antecrystic inheritance but an absence of Mesozoic and older xenocrysts, suggesting a genesis in the mid-upper crust triggered by extension-induced basaltic influx. In Sinaloa, large grabens were floored by huge dome complexes at ~21-17 Ma and filled by continental sediments with interlayered basalts dated at 15 Ma. Mid-Miocene volcanism, including the largely volcaniclastic Comondú strata in Baja California, was thus emplaced in rift basins and appears associated to decompression melting rather than subduction. Along the coast, flat-lying basaltic lava flows dated at 11-10 Ma are exposed just above the present sea level. Here crustal thickness is 25-20 Km, almost half that in the core of the SMO, implying significant lithosphere stretching before ~11 Ma. This mafic pulse, with relatively high Ti but still clear Nb-Ta negative spikes, may be related to the detachment of the lower part of the subducted slab, allowing asthenosphere to flow into parts of the mantle previously fluxed by subduction fluids. Very uniform OIB-like lavas appear in late Pliocene and Pleistocene, only 18 m.y. after the onset of rifting and ~9 m.y. after the end of subduction. Our study shows that rifting began much earlier than Late Miocene and progressively overwhelmed subduction in generating magmatism.

How do supercontinents break up? — assessing the continental large igneous province (LIP) record of the break-up of Pangea

LIP emplacement is linked to the timing and evolution of supercontinental break-up. LIP-related break-up produces volcanic rifted margins, new and large (up to 108 km2) ocean basins, and new, smaller continents that undergo dispersal and potentially reassembly (e.g., India). However, not all continental LIPs lead to continental rupture. We analysed the <330 Ma continental LIP record(following final assembly of Pangea) to find relationships between LIP event attributes (e.g., igneous volume, extent, distance from pre-existing continental margin) and ocean basin attributes (e.g., length of new ocean basin/rifted margin) and how these varied during the progressive break up of Pangea. No correlation exists between LIP magnitude and size of the subsequent ocean basin or rifted margin. Our review suggests a three-phased break-up history of Pangea: 1) “Preconditioning” phase (∼330–200 Ma): LIP events (n=7) occurred largely around the supercontinental margin clustering today in Asia, with a low (<20%) rifting success rate. The Panjal Traps at ∼280 Ma may represent the first continental rupturing event of Pangea, resulting in continental ribboning along the Tethyan margin; 2) “Main Break-up” phase (∼200–100 Ma): numerous large LIP events(n=10) in the supercontinent interior, resulting in highly successful fragmentation (90%) and large, new ocean basins(e.g., Central/South Atlantic, Indian, >3000 km long); 3) “Waning” phase (∼100–0 Ma): Declining LIP magnitudes (n=6), greater proximity to continental margins (e.g., Madagascar, North Atlantic, Afro-Arabia, Sierra Madre) producing smaller ocean basins (<2600 km long). How Pangea broke up may thus have implications for earlier supercontinent reconstructions and LIP record.

A systematic review of naturalistic interventions in refugee populations

Naturalistic interventions with refugee populations examine outcomes following mental health interventions in existing refugee service organisations. The current review aimed to examine outcomes of naturalistic interventions and quality of the naturalistic intervention literature in refugee populations with the view to highlight the strengths and limitations of naturalistic intervention studies. Database search was conducted using the search terms ‘refugee’, ‘asylum seeker’, ‘treatment’, ‘therapy’ and ‘intervention. No date limitations were applied, but searches were limited to articles written in English. Seven studies were identified that assessed the outcome of naturalistic interventions on adult refugees or asylum seekers in a country of resettlement using quantitative outcome measures. Results showed significant variation in the outcomes of naturalistic intervention studies, with a trend towards showing decreased symptomatology at post-intervention. However, conclusions are limited by methodological problems of the studies reviewed, particularly poor documentation of intervention methods and lack of control in the design of naturalistic intervention studies. Further examination of outcomes following naturalistic interventions is needed with studies which focus on increasing the rigour of the outcome assessment process.

The influence of atmospheric conditions on the leakage current of ceramic insulators on the Colombian Caribbean coast

The contamination of electrical insulators is one of the major contributors to the risk of operation outages in electrical substations, especially in coastal zones with high salinity levels and atmospheric pollution. By using the measurement of leakage-currents, which is one of the main indicators of contamination in insulators, this work seeks to the determine the correlation with climatic variables, such as ambient temperature, relative humidity, solar irradiance, atmospheric pressure, and wind speed and direction. The results obtained provide an input to the behaviour of the leakage current under atmospheric conditions that are particular to the Caribbean coast of Colombia. Spearman’s rank correlation coefficients and principal component analysis are utilised to determine the significant relationships among the different variables under consideration. The necessary information for the study was obtained via historical databases of both atmospheric variables and the leakage current measured in over a period of one year in a 220-kV potential transformer insulator. We identified the influencing factors of temperature, humidity, radiation, wind speed and direction on the magnitude of the leakage current as the most relevant.

An SECM study on the influence of cationic, membrane-active peptides on a gold-supported self-assembled monolayer

The influence of the membrane active peptides, Tat44–57 (activator in HIV-1) and melittin (active content of bee venom), on self-assembled monolayers of 6-mercaptohexanoic acid (MHA) on gold electrodes has been studied with scanning electrochemical microscopy (SECM). It was found that MHA, when deprotonated at physiological pH, significantly affected the relative rates of electron transfer between the [Fe(CN)6]4− solution based mediator and the underlying gold electrode, predominantly by the electrostatic interaction between the mediator and MHA. Upon the introduction of Tat44–57 ormelittin to the electrolyte, the relative rate of electron transfer through the MHA layer could be increased or decreased depending on the mediator used. However, in all cases it was found that these peptides have the ability to be incorporated into synthetic SAMs, which has implications for future electrochemical studies carried out using cell mimicking membranes immobilised on such layers.

Therapeutic practice with refugee clients: a qualitative study of therapist experience

Background There is limited research on the subjective experience of therapists and their understanding of therapeutic process when working with people from refugee backgrounds. Objective The present study provides a qualitative account of therapists’ conceptions of therapeutic practice and experiences of working therapeutically with refugee clients. Method Participants were 12 mental health workers who had worked therapeutically with people from refugee backgrounds, with an average of 7.6 years (range 1.5-16 years) experience in this field. Participants completed a semi-structured interview and completed a brief quantitative survey. Findings Thematic analysis revealed a number of super-ordinate themes. Four key themes are explored in the current study: principles of therapeutic practice; therapy as a relational experience; the role of context in informing therapeutic work with refugee clients; and the impact of therapeutic work on the therapist. Discussion The results revealed the complexity and demands of working with people from refugee backgrounds. Further, the lack of research evidence for the methods of therapeutic practice described in the current study highlights the distinction between naturalistic therapeutic practice and the current state of the evidence regarding therapeutic interventions for refugee clients. The findings have important implications for training and supporting therapists to work with people who have fled their countries of origin and who have often been exposed to highly traumatic events.

Mechanistic details of the membrane perforation and passive translocation of TAT peptides

The trans-activator of transcription (TAT) peptide is regarded as the “gold standard” for cell-penetrating peptides, capable of traversing a mammalian membrane passively into the cytosolic space. This characteristic has been exploited through conjugation of TAT for applications such as drug delivery. However, the process by which TAT achieves membrane penetration remains ambiguous and unresolved. Mechanistic details of TAT peptide action are revealed herein by using three complementary methods: quartz crystal microbalance with dissipation (QCM-D), scanning electrochemical microscopy (SECM) and atomic force microscopy (AFM). When combined, these three scales of measurement define that the membrane uptake of the TAT peptide is by trans-membrane insertion using a “worm-hole” pore that leads to ion permeability across the membrane layer. AFM data provided nanometre-scale visualisation of TAT punctuation using a mammalian-mimetic membrane bilayer. The TAT peptide does not show the same specificity towards a bacterial mimetic membrane and QCM-D and SECM showed that the TAT peptide demonstrates a disruptive action towards these membranes. This investigation supports the energy-independent uptake of the cationic TAT peptide and provides empirical data that clarify the mechanism by which the TAT peptide achieves its membrane activity. The novel use of these three biophysical techniques provides valuable insight into the mechanism for TAT peptide translocation, which is essential for improvements in the cellular delivery of TAT-conjugated cargoes including therapeutic agents required to target specific intracellular locations.