Niños "vergonzantes" y "pequeños rojos". La población marginal infantil en la Cataluña interior del primer franquismo

En el imaginario colectivo de la sociedad de posguerra siempre están presentes las duras condiciones de la vida cotidiana. La población infantil fue especialmente sensible a esta situación debido al alto índice de enfermedades infecciosas, el racionamiento dietético y las angustias derivadas del conflicto bélico. En estas condiciones, el Auxilio Social de la Falange fue el encargado de administrar la beneficencia y, a su vez, resocializar la población, en este caso, la infantil, dentro de los valores nacionalsindicalistas y nacionalcatólicos. Ello le permitió no sólo controlar la política social sino también criminalizar a los vencidos en el momento de administrarla. En definitiva, fue uno de los pilares fundamentales en el proceso de construcción del edificio franquista.

A Potential Contributory Role for Ciliary Dysfunction in the 16p11.2 600 kb BP4-BP5 Pathology.

The 16p11.2 600 kb copy-number variants (CNVs) are associated with mirror phenotypes on BMI, head circumference, and brain volume and represent frequent genetic lesions in autism spectrum disorders (ASDs) and schizophrenia. Here we interrogated the transcriptome of individuals carrying reciprocal 16p11.2 CNVs. Transcript perturbations correlated with clinical endophenotypes and were enriched for genes associated with ASDs, abnormalities of head size, and ciliopathies. Ciliary gene expression was also perturbed in orthologous mouse models, raising the possibility that ciliary dysfunction contributes to 16p11.2 pathologies. In support of this hypothesis, we found structural ciliary defects in the CA1 hippocampal region of 16p11.2 duplication mice. Moreover, by using an established zebrafish model, we show genetic interaction between KCTD13, a key driver of the mirrored neuroanatomical phenotypes of the 16p11.2 CNV, and ciliopathy-associated genes. Overexpression of BBS7 rescues head size and neuroanatomical defects of kctd13 morphants, whereas suppression or overexpression of CEP290 rescues phenotypes induced by KCTD13 under- or overexpression, respectively. Our data suggest that dysregulation of ciliopathy genes contributes to the clinical phenotypes of these CNVs.

Zone indécise. Périphéries urbaines et voyage de proximité dans la littérature contemporaine

Depuis les années 1980, les périphéries urbaines sont très fortement investies par les écrivains. Six d'entre eux sont étudiés dans ce livre: François Bon, François Maspero, Jacques Réda, Jean Rolin, Denis Tillinac et Philippe Vasset. Ils "voyagent" sur le pourtour parisien, parfois plus loin, là où, dit-on, la ville est moins ville que la ville, dans des espaces qui souffriraient d'un déficit d'urbanité. Ce faisant, ils en éprouvent la consistance paysagère, compliquent l'opposition facile entre Paris et sa banlieue, apparaissent, de fait, comme les agents d'une requalification symbolique de la ville contemporaine. La démarche de l'auteur se situe ici au confluent d'un corpus particulier, circonscrit dans le temps - les textes retenus ont paru entre 1990 et 2007 - et d'une question de grande ampleur historique, culturelle et esthétique: le paysage. Tout en plaçant les oeuvres commentées dans la lumière où elles trouvent leur relief spécifique, sa réflexion, associant ponctuellement l'analyse littéraire à d'autres disciplines (géographie, sociologie, philosophie), apporte, sur un champ peu exploré de la littérature vivante, un éclairage neuf et original qui s'adresse aux spécialistes du contemporain, ou de l'extrême contemporain, mais aussi à tous les lecteurs intéressés par les pratiques et les savoirs de la ville.

The Sottunga-Jurmo shear zone : structure and deformation history of a crustal-scale ductile shear zone in SW Finland

The aim of this study is to gain a better understanding of the structure and the deformation history of a NW-SE trending regional, crustal-scale shear structure in the Åland archipelago, SW Finland, called the Sottunga-Jurmo shear zone (SJSZ). Approaches involving e.g. structural geology, geochronology, geochemistry and metamorphic petrology were utilised in order to reconstruct the overall deformation history of the study area. The study therefore describes several features of the shear zone including structures, kinematics and lithologies within the study area, the ages of the different deformation phases (ductile to brittle) within the shear zone, as well as some geothermobarometric results. The results indicate that the SJSZ outlines a major crustal discontinuity between the extensively migmatized rocks NE of the shear zone and the unmigmatised, amphibolite facies rocks SW of the zone. The main SJSZ shows overall dextral lateral kinematics with a SW-side up vertical component and deformation partitioning into pure shear and simple shear dominated deformation styles that was intensified toward later stages of the deformation history. The deformation partitioning resulted in complex folding and refolding against the SW margin of the SJSZ, including conical and sheath folds, and in a formation of several minor strike-slip shear zones both parallel and conjugate to the main SJSZ in order to accommodate the regional transpressive stresses. Different deformation phases within the study area were dated by SIMS (zircon U-Pb), ID-TIMS (titanite U-Pb) and 40Ar/39Ar (pseudotachylyte wholerock) methods. The first deformation phase within the ca. 1.88 Ga rocks of the study area is dated at ca. 1.85 Ga, and the shear zone was reactivated twice within the ductile regime (at ca. 1.83 Ga and 1.79 Ga), during which the strain was successively increasingly partitioned into the main SJSZ and the minor shear zones. The age determinations suggest that the orogenic processes within the study area did not occur in a temporal continuum; instead, the metamorphic zircon rims and titanites show distinct, 10-20 Ma long breaks in deformation between phases of active deformation. The results of this study further imply slow cooling of the rocks through 600-700ºC so that at 1.79 Ga, 2 the temperature was still at least 600ºC. The highest recorded metamorphic pressures are 6.4-7.1 kbar. At the late stages or soon after the last ductile phase (ca. 1.79 Ga), relatively high-T mylonites and ultramylonites were formed, witnessing extreme deformation partitioning and high strain rates. After the rocks reached lower amphibolite facies to amphibolite-greenschist facies transitional conditions (ca. 500-550ºC), they cooled rapidly, probably due to crustal uplift and exhumation. The shear zone was reactivated at least once within the semi-brittle to brittle regime between ca. 1.79 Ga and 1.58 Ga, as evidenced by cataclasites and pseudotachylytes. In summary, the results of this study suggest that the Sottunga-Jurmo shear zone (and the South Finland shear zone) defines a major crustal discontinuity, and played a central role in accommodating the regional stresses during and after the Svecofennian orogeny.