Assinatura estrutural e geofísica da porção norte (fronteira Ceará-Piauí) no lineamento transbrasiliano: reativação na bacia do Parnaíba

The Transbrasiliano Lineament is a major shear zone trending NE-SW, related to the Brasiliano orogeny and evolved through high to low temperature stages. In this study, the structural and geophysical signature of the northern segment of Transbrasiliano Lineament was studied in its northern border, between Ceará and Piauí states, involving the Brasiliano mylonite zone, the Jaibaras Graben and reactivations affecting the sedimentary sequences post-ordovician of Parnaíba Basin. In the literature, is commonly the phanerozoic reactivation of this structure referred, generating several late Brasiliano grabens predating the paleozoic Parnaíba syneclises, like the Jaibaras Graben. Faults that cut the stratigraphic units of the Parnaíba Basin along the entire length of the Transbrasiliano Lineament express its reactivation during younger events. The magnetic anomaly field reduced to the pole map exhibit anomalies NE-trending, interpreted as the signature of the Transbrasiliano Lineament (and Brasiliano structures of the Borborema Province) in its high-temperature expression. The Jaibaras Graben is marked by a straight anomalous track with high magnetic susceptibility (interpreted as a prevalence of ferromagnesian rocks, probably volcanic), apparently without significant continuity in the substrate of Parnaíba Basin. The geometric and kinematic analysis of the structures in the study area, using remote sensing and field data, led to the characterization of four deformation phases brittle the ductilebrittle Dn, D1, D2 and D3. The Dn deformation phase of ediacaran-cambrian age, occurs exclusively in the Jaibaras Graben, with the development of comparatively higher temperature (as regards to younger events) ductile-brittle structures. D1, D2 and D3 deformation phases affect both the Jaibaras Graben as well as the paleozoic sequences of the northeastern edge of Parnaíba Basin, generating structures developed at lower temperatures, basically brittle/cataclastic. The SRTM image analysis allowed mapping different NE, NW and E-W trending lineaments in Parnaíba Basin, whose correlation with mesoscopic structures is discussed in terms of the reactivation of Transbrasiliano Lineament in association with the stages of general Atlantic opening and separation between South America and Africa, or even the distal orogenic events in Paleozoic.

Estudo da sismicidade na barragem do Açu no período de 2012 a 2013

The seismic activity in the Northeastern of Brazil has been a constant target of study, since it is the most active region of the country. However, some areas have their earthquakes related to human action, what means they are induced. The Açu dam is a classic example of reservoir-induced seismicity and it has been the subject of several studies. Recently, after a considerable period of inactivity, the LabSis / UFRN recorded events related to the dam, which led to the installation of a network around the reservoir. From the data provided by this network, it was observed that the seismic activity is related to a new epicental area inside the lake. The epicentral parameters and the focal mechanism were determined. It was found that the events were related to the reactivation of a basement structure in a new seismogenic subvertical fault with NE-SW-striking subparallel to the São Rafael Fault. These results were used in the preparation of a scientific paper, which discussed the relationship between this seismicity with the geology of the region and with the reservoir water level. The paper showed that the diffusion of pore pressure was the main mechanism that controlled the triggering of the induced seismicity at the reservoir.

Estudo da sismicidade na barragem do Açu no período de 2012 a 2013

The seismic activity in the Northeastern of Brazil has been a constant target of study, since it is the most active region of the country. However, some areas have their earthquakes related to human action, what means they are induced. The Açu dam is a classic example of reservoir-induced seismicity and it has been the subject of several studies. Recently, after a considerable period of inactivity, the LabSis / UFRN recorded events related to the dam, which led to the installation of a network around the reservoir. From the data provided by this network, it was observed that the seismic activity is related to a new epicental area inside the lake. The epicentral parameters and the focal mechanism were determined. It was found that the events were related to the reactivation of a basement structure in a new seismogenic subvertical fault with NE-SW-striking subparallel to the São Rafael Fault. These results were used in the preparation of a scientific paper, which discussed the relationship between this seismicity with the geology of the region and with the reservoir water level. The paper showed that the diffusion of pore pressure was the main mechanism that controlled the triggering of the induced seismicity at the reservoir.

Evolução morfotectônica da porção centro-sul da Bacia Paraíba

Recent endogenous processes provide dynamic movements in the lithosphere and generate the varied forms of relief, even in areas of passive continental margins, such as the research area of this work located in northeastern Brazil. The reactivation of Precambrian basement structures, after the breakup between South America and Africa in the Cretaceous played an important role in the evolution of basins, which provided generated forms of relief. These morphodynamic characteristics can be easily observed in marginal basins that exhibit strong evidence fault reactivations. The purpose of this study is to investigate the influence of morphotectonic processes in the landscape structuring of Paraíba Basin. Therefore, we used aeromagnetic, high–resolution images of the Shuttle Radar Topographic Mission–SRTM, structural geological data, deep well data and geological field data. Based on the results of the data was observed that some preexisting structures in the crystalline basement coincide with magnetic and topographic lineaments interpreted as fault reactivation of the Post–Miocene units in the Paraíba Basin. Faults that offset lithostratigraphic units provided evidence that tectonic activity associated with the deposition and erosion in the Paraíba Basin occurred from Cretaceous to the Quaternary. The neotectonic activity that occurred in Paraíba Basin was able to influence the deposition of sedimentary units and landforms. It indicates that the deposition of post–Cretaceous units was influenced by reactivation of Precambrian basement structures in this part of the Brazilian continental margin.

(Table S1) Age determination of Atlantic Ocean sediment cores

Well-dated benthic foraminifer oxygen isotopic records (d18O) from different water depths and locations within the Atlantic Ocean exhibit distinct patterns and significant differences in timing over the last deglaciation. This has two implications: on the one hand, it confirms that benthic d18O cannot be used as a global correlation tool with millennial-scale precision, but on the other hand, the combination of benthic isotopic records with independent dating provides a wealth of information on past circulation changes. Comparing new South Atlantic benthic isotopic data with published benthic isotopic records, we show that (1) circulation changes first affected benthic d18O in the 1000-2200 m range, with marked decreases in benthic d18O taking place at ~17.5 cal. kyr B.P. (ka) due to the southward propagation of brine waters generated in the Nordic Seas during Heinrich Stadial 1 (HS1) cold period; (2) the arrival of d18O-depleted deglacial meltwater took place later at deeper North Atlantic sites; (3) hydrographic changes recorded in North Atlantic cores below 3000 m during HS1 do not correspond to simple alternations between northern- and southern-sourced water but likely reflect instead the incursion of brine-generated deep water of northern as well as southern origin; and (4) South Atlantic waters at ~44°S and ~3800 m depth remained isolated from better-ventilated northern-sourced water masses until after the resumption of North Atlantic Deep Water (NADW) formation at the onset of the Bølling-Allerod, which led to the propagation of NADW into the South Atlantic.

Pedagogía y política. La campaña de alfabetización CREAR en la historia reciente de la educación de adultos en la Argentina de los '70

La tesis que presentamos es el resultado de un trabajo de investigación sobre la campaña de alfabetización CREAR realizada entre 1973 y 1975. La Campaña de Reactivación de la Educación del Adulto para la Reconstrucción, estuvo dirigida por la Dirección Nacional de Educación de Adultos (DINEA) en la etapa de la recuperación democrática luego de dieciocho años de gobiernos autoritarios combinados con la proscripción de la fuerza política mayoritaria. Apoyada en el registro testimonial de quienes fueron sus inspiradores, conductores, coordinadores, alfabetizadores, la investigación se propone analizar la articulación entre pedagogía y política durante la realización de la campaña. Los testimonios rescatados en la presente investigación, representan figuras destacadas de la campaña de alfabetización en su doble dimensión de pedagogos y militantes políticos. En esta dirección, la presente tesis se propone recuperar los principales debates y discusiones que se generaron en torno a su desarrollo a partir de quienes fueron sus testigos. ¿Qué sueños proyectaban en la alfabetización? ¿Qué formas de imbricación entre lo político y lo pedagógico se produjo en su desarrollo? ¿Cómo se plasmó dicha articulación? ¿Sobre qué ejes vertebraron su discurso? Entre la pedagogía de la liberación y la doctrina del peronismo ¿qué lectura predominó? El desarrollo de este trabajo de investigación se propone invitar a recorrer este camino cargado de tensiones y contradicciones que, esperamos, se convierta en una contribución al campo de la historia de la educación reciente de la Argentina

Pedagogía y política. La campaña de alfabetización CREAR en la historia reciente de la educación de adultos en la Argentina de los '70

La tesis que presentamos es el resultado de un trabajo de investigación sobre la campaña de alfabetización CREAR realizada entre 1973 y 1975. La Campaña de Reactivación de la Educación del Adulto para la Reconstrucción, estuvo dirigida por la Dirección Nacional de Educación de Adultos (DINEA) en la etapa de la recuperación democrática luego de dieciocho años de gobiernos autoritarios combinados con la proscripción de la fuerza política mayoritaria. Apoyada en el registro testimonial de quienes fueron sus inspiradores, conductores, coordinadores, alfabetizadores, la investigación se propone analizar la articulación entre pedagogía y política durante la realización de la campaña. Los testimonios rescatados en la presente investigación, representan figuras destacadas de la campaña de alfabetización en su doble dimensión de pedagogos y militantes políticos. En esta dirección, la presente tesis se propone recuperar los principales debates y discusiones que se generaron en torno a su desarrollo a partir de quienes fueron sus testigos. ¿Qué sueños proyectaban en la alfabetización? ¿Qué formas de imbricación entre lo político y lo pedagógico se produjo en su desarrollo? ¿Cómo se plasmó dicha articulación? ¿Sobre qué ejes vertebraron su discurso? Entre la pedagogía de la liberación y la doctrina del peronismo ¿qué lectura predominó? El desarrollo de este trabajo de investigación se propone invitar a recorrer este camino cargado de tensiones y contradicciones que, esperamos, se convierta en una contribución al campo de la historia de la educación reciente de la Argentina

Pedagogía y política. La campaña de alfabetización CREAR en la historia reciente de la educación de adultos en la Argentina de los '70

La tesis que presentamos es el resultado de un trabajo de investigación sobre la campaña de alfabetización CREAR realizada entre 1973 y 1975. La Campaña de Reactivación de la Educación del Adulto para la Reconstrucción, estuvo dirigida por la Dirección Nacional de Educación de Adultos (DINEA) en la etapa de la recuperación democrática luego de dieciocho años de gobiernos autoritarios combinados con la proscripción de la fuerza política mayoritaria. Apoyada en el registro testimonial de quienes fueron sus inspiradores, conductores, coordinadores, alfabetizadores, la investigación se propone analizar la articulación entre pedagogía y política durante la realización de la campaña. Los testimonios rescatados en la presente investigación, representan figuras destacadas de la campaña de alfabetización en su doble dimensión de pedagogos y militantes políticos. En esta dirección, la presente tesis se propone recuperar los principales debates y discusiones que se generaron en torno a su desarrollo a partir de quienes fueron sus testigos. ¿Qué sueños proyectaban en la alfabetización? ¿Qué formas de imbricación entre lo político y lo pedagógico se produjo en su desarrollo? ¿Cómo se plasmó dicha articulación? ¿Sobre qué ejes vertebraron su discurso? Entre la pedagogía de la liberación y la doctrina del peronismo ¿qué lectura predominó? El desarrollo de este trabajo de investigación se propone invitar a recorrer este camino cargado de tensiones y contradicciones que, esperamos, se convierta en una contribución al campo de la historia de la educación reciente de la Argentina

Progressive Multifocal Leukoencephalopathy and Systemic Lupus Erythematosus: Focus on Etiology

Progressive multifocal leukoencephalopathy (PML) caused by reactivation of the JC virus (JCV), a human polyomavirus, occurs in autoimmune disorders, most frequently in systemic lupus erythematosus (SLE). We describe a HIV-negative 34-year-old female with SLE who had been treated with immunosuppressant therapy (IST; steroids and azathioprine) since 2004. In 2011, she developed decreased sensation and weakness of the right hand, followed by vertigo and gait instability. The diagnosis of PML was made on the basis of brain MRI findings (posterior fossa lesions) and JCV isolation from the cerebrospinal fluid (700 copies/ml). IST was immediately discontinued. Cidofovir, mirtazapine, mefloquine and cycles of cytarabine were sequentially added, but there was progressive deterioration with a fatal outcome 1 year after disease onset. This report discusses current therapeutic choices for PML and the importance of early infection screening when SLE patients present with neurological symptoms. In the light of recent reports of PML in SLE patients treated with rituximab or belimumab, we highlight that other IST may just as well be implicated. We conclude that severe lymphopenia was most likely responsible for JCV reactivation in this patient and discuss how effective management of lymphopenia in SLE and PML therapy remains an unmet need.

Étude de la reconstitution de l’immunité spécifique au cytomégalovirus et au virus de la varicelle suite à la transplantation de sang de cordon ombilical

La transplantation de sang de cordon ombilical (TSCO) constitue un traitement de choix pour une multitude de pathologies hématologiques malignes et non malignes chez l’enfant et dans certains cas l’adulte. La TSCO est associée à certaines complications, dont une reconstitution immunitaire plus lente et une incidence élevée d’infections opportunistes, notamment celles reliées au cytomégalovirus (CMV) et au virus varicella-zoster (VZV). Dans le cadre de ce travail, nous nous sommes intéressés dans un premier temps à la caractérisation de la reconstitution immunitaire spécifique au CMV et au VZV. Nos résultats ont démontré que la reconstitution de l’immunité cellulaire ne requiert ni un statut séropositif pré-transplantation ni le développement de la maladie. De plus, des reconstitutions spontanées ont été détectées chez certains patients séronégatifs vis-à-vis du CMV ou du VZV. Outre le fait qu’elle se manifeste surtout à partir de 6 mois post-transplantation, ladite reconstitution mérite le qualificatif de « protectrice » en termes de réactivations virales et du développement de signes cliniques lorsqu’une fréquence de 150 cellules produisant l’IFN-γ/million est dépassée. Toutefois, moins de 5% des patients développent une réponse T anti-VZV et anti-CMV au cours 100 premiers jours suivant la TSCO. Il est donc possible que les lymphocytes CD8+ T provenant du SCO, comparativement à leurs homologues provenant de la moelle osseuse (MO), présentent un défaut de fonctionnalité, communément appelé « épuisement clonal ». La caractérisation du répertoire de récepteurs inhibiteurs exprimés par les cellules T CD8+ suivant la TSCO ou la transplantation de moelle osseuse (TMO) a révélé une augmentation significative de la fréquence des cellules exprimant PD-1 tôt suivant la transplantation. Cette population, caractérisée majoritairement par un phénotype effecteur-mémoire (EM), démontre une perte significative de la capacité proliférative et exprime moins d'IFN-γ, d'IL-2, de TNF-α et de CD107a. Une meilleure caractérisation de la reconstitution immunitaire après TSCO permettrait, d'une part de sélectionner des biomarqueurs en vue d’une meilleure gestion des patients à risques de développer des infections virales et/ou de rechuter, et d'autre part d'améliorer leur pronostic.

Agrandissement des feuillets mitraux en insuffisance aortique : un mécanisme actif pouvant prévenir l’insuffisance mitrale dans le ventricule dilaté

L’insuffisance mitrale (IM) fonctionnelle est une complication fréquente des cardiopathies, causée par la dilatation du ventricule gauche (VG) qui empêche la valve de se fermer. L’insuffisance aortique (IA) est une condition associée à des valves mitrales (VM) inhabituellement grandes, et relativement peu d’IM malgré des VG très dilatés. Cet élargissement de la VM a le potentiel de prévenir l’IM dans les VG dilatés. Les mécanismes sont cependant peu compris : il n’est pas clair s’il s’agit d’une croissance active ou d’un étirement passif des feuillets. Également, le timing de l’adaptation valvulaire n’est pas connu. Notre hypothèse est que l’agrandissement de la valve mitrale en IA est un phénomène actif avec réactivation des mécanismes de croissance embryonnaire. Cent-onze rats ont été divisés en deux groupes : IA (perforation aortique) et contrôle. Les animaux ont été sacrifiés à 48 h, 1 semaine et 3 mois après la création du modèle. Des échocardiographies ont évalué la sévérité de l’IA, la présence d’IM et les dimensions du VG. Les valves ont été prélevées pour analyses microscopiques et moléculaires. La création de l’insuffisance aortique a entrainé une dilatation et une hypertrophie du VG. Malgré cette dilatation rapide du VG, aucun animal n’a développé de l’IM fonctionnelle. À l’échographie, le feuillet antérieur mitral était significativement plus long dans les groupes IA. Par microscopie, les feuillets étaient plus épais dés la première semaine. L’IA était associée à une surexpression de collagène α-SMA (un marqueur de myofibroblastes), TGF-β1 et MMP-2 dans le tissu valvulaire dès la première semaine. Les valves exposées à l’IA étaient également positives pour ces différents facteurs dés les premiers jours. L’agrandissement de la VM est un phénomène actif qui survient rapidement après la création de l’IA, en parallèle de la dilatation du VG. La stimulation de cette croissance dans d’autres pathologies pourrait contribuer à prévenir l’IM fonctionnelle.

New morpho-bathymetric and tectono-stratigraphic data on Naples and Salerno gulfs (southern tyrrhenian sea, Italy) derived from bathymetric and seismic data analysis and integrated geological interpretation

New morpho-bathymetric and tectono-stratigraphic data on Naples and Salerno Gulfs, derived from bathymetric and seismic data analysis and integrated geologic interpretation are here presented. The CUBE(Combined Uncertainty Bathymetric Estimator) method has been applied to complex morphologies, such as the Capri continental slope and the related geological structures occurring in the Salerno Gulf.The bathymetric data analysis has been carried out for marine geological maps of the whole Campania continental margin at scales ranging from 1:25.000 to 1:10.000, including focused examples in Naples and Salerno Gulfs, Naples harbour, Capri and Ischia Islands and Salerno Valley. Seismic data analysis has allowed for the correlation of main morpho-structural lineaments recognized at a regional scale through multichannel profiles with morphological features cropping out at the sea bottom, evident from bathymetry.Main fault systems in the area have been represented on a tectonic sketch map, including the master fault located northwards to the Salerno Valley half graben. Some normal faults parallel to the master fault have been interpreted from the slope map derived from bathymetric data. A complex system of antithetic faults bound two morpho-structural highs located 20km to the south of the Capri Island. Some hints of compressional reactivation of normal faults in an extensional setting involving the whole Campania continental margin have been shown from seismic interpretation.

Quantifying uplift and denudation of a thermally heterogeneous crust: a detailed multi-thermochronometeric study of central west Britain

Topography is often thought as exclusively linked to mountain ranges formed by plates collision. It is now, however, known that apart from compression, uplift and denudation of rocks may be triggered by rifting, like it happens at elevated passive margins, and away from plate boundaries by both intra-plate stress causing reactivation of older structures, and by epeirogenic movements driven by mantle dynamics and initiating long-wavelength uplift. In the Cenozoic, central west Britain and other parts of the North Atlantic margins experienced multiple episodes of rock uplift and denudation that have been variable both at spatial and temporal scales. The origin of topography in central west Britain is enigmatic, and because of its location, it may be related to any of the processes mentioned above. In this study, three low temperature thermochronometers, the apatite fission track (AFT) and apatite and zircon (U-Th-Sm)/He (AHe and ZHe, respectively) methods were used to establish the rock cooling history from 200◦C to 30◦C. The samples were collected from the intrusive rocks in the high elevation, high relief regions of the Lake District (NW England), southern Scotland and northern Wales. AFT ages from the region are youngest (55–70 Ma) in the Lake District and increase northwards into southern Scotland and southwards in north Wales (>200 Ma). AHe and ZHe ages show no systematic pattern; the former range from 50 to 80 Ma and the latter tend to record the post-emplacement cooling of the intrusions (200–400 Ma). The complex, multi-thermochronometric inverse modelling suggests a ubiquitous, rapid Late Cretaceous/early Palaeogene cooling event that is particularly marked in Lake District and Criffell. The timing and rate of cooling in southern Scotland and in northern Wales is poorly resolved as the amount of cooling was less than 60◦C. The Lake District plutons were at >110◦C prior to the early Palaeogene; cooling due to a combined effect of high heat flow, from the heat producing granite batholith, and the blanketing effect of the overlying low conductivity Late Mesozoic limestones and mudstones. Modelling of the heat transfer suggests that this combination produced an elevated geothermal gradient within the sedimentary rocks (50–70◦C/km) that was about two times higher than at the present day. Inverse modelling of the AFT and AHe data taking the crustal structure into consideration suggests that denudation was the highest, 2.0–2.5 km, in the coastal areas of the Lake District and southern Scotland, gradually decreasing to less than 1 km in the northern Southern Uplands and northern Wales. Both the rift-related uplift and the intra-plate compression poorly correlate with the timing, location and spatial distribution of the early Palaeogene denudation. The pattern of early Palaeogene denudation correlates with the thickness of magmatic underplating, if the changes of mean topography, Late Cretaceous water depth and eroded rock density are taken into consideration. However, the uplift due to underplating alone cannot fully justify the total early Palaeogene denudation. The amount that is not ex- plained by underplating is, however, roughly spatially constant across the study area and can be referred to the transient thermal uplift induced by the mantle plume arrival. No other mechanisms are required to explain the observed pattern of denudation. The onset of denudation across the region is not uniform. Denudation started at 70–75 Ma in the central part of the Lake District whereas the coastal areas the rapid erosion appears to have initiated later (65–60 Ma). This is ~10 Ma earlier than the first vol- canic manifestation of the proto-Iceland plume and favours the hypothesis of the short period of plume incubation below the lithosphere before the volcanism. In most of the localities, the rocks had cooled to temperatures lower than 30◦C by the end of the Palaeogene, suggesting that the total Neogene denudation was, at a maximum, several hundreds of metres. Rapid cooling in the last 3 million years is resolved in some places in southern Scotland, where it could be explained by glacial erosion and post-glacial isostatic uplift.

Beebe House

The Beebe House was one of the first hotels built on South Bass Island. Constructed in the 1860s, it was expanded by Henry Beebe in 1869. Situated on Main Street in Put-in-Bay, the hotel accommodated 400 guests. It housed a billiard room, bowling alley, and dance hall. Rates were $14,00 per week and $2.50 per day. Servants and children were half price.