Critical Behavior and Axis Defining Symmetry Breaking in Hydra Embryonic Development

The formation of a hollow cellular sphere is often one of the first steps of multicellular embryonic development. In the case of Hydra, the sphere breaks its initial symmetry to form a foot-head axis. During this process a gene, ks1, is increasingly expressed in localized cell domains whose size distribution becomes scale-free at the axis-locking moment. We show that a physical model based solely on the production and exchange of ks1-promoting factors among neighboring cells robustly reproduces the scaling behavior as well as the experimentally observed spontaneous and temperature-directed symmetry breaking.

Disseny i desenvolupament d’un joc de tauler per torns amb la plataforma Unity3D

Desenvolupament d’un videojoc per ordinador amb la possibilitat de tenir-lo també per dispositius mòbils

Vespignani, Giorgio, Iппoδρoμoς. Il circo di Costantinopoli nuova Roma dalla realtà alla storiografia, Fondazione Centro Italiano di Studi sull"Alto Medioevo, Spoleto, 2010, 303 páginas. ISBN: 978 88-7988-197-5

"El Circo Máximo es su templo, su hogar, su asamblea y la esperanza de todos sus deseos" (AmmiAnvs mArc., Res gest., XXVIII, 4, 29: eisque templum et habitaculum et contio et cupitorum spes omnis Circus est maximus). De este modo describió el historiador Amiano Marcelino, hacia el 382/397, la pasión que la plebe de Roma sentía hacia los espectáculos, especialmente hacia los ludi circenses. Se trata de una afición que se fue incrementando a lo largo de toda la historia del Imperio Romano, hasta el extremo que a mediados del siglo iv, según el calendario de Filócalo (CIL, I2, 1, p. 256-278), se alcanzaron los 177 días de juegos anuales. Y evidentemente tal apasionamiento no fue exclusivo de la ciudad de Roma, sino que se vivió de un modo común en todo el Imperio, sobre todo en las ciudades más grandes, entre las que destacó de una manera especial la capital de Oriente, Constantinopla, la nueva Roma fundada por Constantino I.

The provision of quality in a bilateral search market

We accomplish two goals. First, we provide a non-cooperative foundation for the use of the Nash bargaining solution in search markets. This finding should help to close the rift between the search and the matching-and-bargaining literature. Second, we establish that the diversity of quality offered (at an increasing price-quality ratio) in a decentralized market is an equilibrium phenomenon - even in the limit as search frictions disappear.

Information systems for water resources management improvement in developing countries

Water resources management, as also water service provision projects in developing countries have difficulties to take adequate decisions due to scarce reliable information, and a lack of proper information managing. Some appropriate tools need to be developed in order to improve decision making to improve water management and access of the poorest, through the design of Decision Support Systems (DSS). On the one side, a DSS for developing co-operation projects on water access improvement has been developed. Such a tool has specific context constrains (structure of the system, software requirements) and needs (Logical Framework Approach monitoring, organizational-learning, accountability and evaluation) that shall be considered for its design. Key aspects for its successful implementation have appeared to be a participatory design of the system and support of the managerial positions at the inception phase. A case study in Tanzania was conducted, together with the Spanish NGO ONGAWA – Ingeniería para el Desarrollo. On the other side, DSS are required also to improve decision making on water management resources in order to achieve a sustainable development that not only improves the living conditions of the population in developing countries, but that also does not hinder opportunities of the poorest on those context. A DSS made to fulfil these requirements shall be using information from water resources modelling, as also on the environment and the social context. Through the research, a case study has been conducted in the Central Rift Valley of Ethiopia, an endhorreic basin 160 km south of Addis Ababa. There, water has been modelled using ArcSWAT, a physically based model which can assess the impact of land management practices on large complex watersheds with varying soils, land use and management conditions over long periods of time. Moreover, governance on water and environment as also the socioeconomic context have been studied.

Proposta de criteris per la integració d¿alumnes amb NEE greus i permanents. Una distribució mes eficaç a les USEE com a eina d¿inclusió.

Les pràctiques desenvolupades a l¿EAP (Equip Assessorament Psicopedagògic) m¿han permès un apropament a les activitats que realitzen fora i dintre dels Centres Escolars i mes concretament la intervenció que es fa mitjançant les USEE (Unitats de Suport a l¿Educació Especial. Aquestes Unitats tenen com a finalitat afavorir la inclusió dels alumnes amb Necessitats Especials (NEE) amb dictamen. Mitjançant aquest treball podrem analitzar com la proposta de uns criteris clars i ben definits permet millorar la distribució d¿aquest alumnat i a la vegada aprofitar millor els recursos de suport dels Centres Educatius. De la mateixa manera aquesta proposta de criteris pot servir d¿oportunitat per establir nous escenaris de cooperació entre les unitats de suport i el sistema docent de l¿aula ordinària.

Modelo formativo y competencias transversales: una propuesta para el Grado en Educación Social

El objeto de esta comunicación es presentar el modelo formativo de los estudios de Grado de la Facultad de Educación Social y Trabajo Social Pere Tarrés de la Universidad Ramón Llull, una vez se han desplegado los tres primeros cursos de las titulaciones de Grado. Pretendemos dar a conocer las competencias transversales comunes en todas las asignaturas así como las metodologías y las actividades utilizadas para facilitar el proceso de aprendizaje de los estudiantes. Queremos constatar, por un lado, que nuestra propuesta avala la integración del nuevo modelo educativo, recogido en el Plan Bolonia, donde la actividad del estudiante es uno de los ejes centrales de su proceso formativo y, por el otro, que nos permita dar un salto cualitativo en la formación que ofrecemos a los futuros profesionales de la acción social. Pretendemos garantizar la coherencia entre los contenidos de las asignaturas que forman una misma materia y los niveles de consecución de las competencias a lo largo del período de formación. Esto implica una tarea de coordinación y de trabajo en equipo entre los profesores que garantice la consecución de los contenidos evitando vacíos o solapamientos entre asignaturas.

Simulation methods with extended stability for stiff biochemical kinetics

Background: With increasing computer power, simulating the dynamics of complex systems in chemistry and biology is becoming increasingly routine. The modelling of individual reactions in (bio)chemical systems involves a large number of random events that can be simulated by the stochastic simulation algorithm (SSA). The key quantity is the step size, or waiting time, τ, whose value inversely depends on the size of the propensities of the different channel reactions and which needs to be re-evaluated after every firing event. Such a discrete event simulation may be extremely expensive, in particular for stiff systems where τ can be very short due to the fast kinetics of some of the channel reactions. Several alternative methods have been put forward to increase the integration step size. The so-called τ-leap approach takes a larger step size by allowing all the reactions to fire, from a Poisson or Binomial distribution, within that step. Although the expected value for the different species in the reactive system is maintained with respect to more precise methods, the variance at steady state can suffer from large errors as τ grows. Results: In this paper we extend Poisson τ-leap methods to a general class of Runge-Kutta (RK) τ-leap methods. We show that with the proper selection of the coefficients, the variance of the extended τ-leap can be well-behaved, leading to significantly larger step sizes.Conclusions: The benefit of adapting the extended method to the use of RK frameworks is clear in terms of speed of calculation, as the number of evaluations of the Poisson distribution is still one set per time step, as in the original τ-leap method. The approach paves the way to explore new multiscale methods to simulate (bio)chemical systems.

Flank stability and processes off the western Canary Islands: a review from El Hierro and La Palma

The morphological characterisation of the western submarine island flanks of El Hierro and La Palma differentiates four type-zones that may give new insights into the evolution of oceanic island slopes. The different type-zones result from the interplay between constructive volcanic processes, hemipelagic settling and volcano collapses. The latter results in massive debris avalanche deposits, which form large volcaniclastic aprons. In most cases, the headwall scarps are clearly exposed on the emerged part of the islands. The events that occurred in the youngest and westernmost islands of El Hierro and La Palma have vertical runouts exceeding 6,000 m and volumes that can reach several hundred km3. The landslide frequency for the entire Canaries is one major event per 90 ka. Triggering mechanisms are closely related to magmatic processes. The increase in the shear stress is directly linked with the forceful intrusion of magma along ridge-rift systems, while in the western Canary Islands it seems that the main process reducing shear resistance may be related to the rise in pore pressure due to hydrothermal circulation.

The Upper Oligocene of Montgat (Catalan Coastal Ranges, Spain): new age constraints to the western Mediterranean Basin opening

The Oligocene deposits of Montgat are integrated in a small outcrop made up of Cenozoic and Mesozoic rocks located in the Garraf-Montnegre horst, close to the major Barcelona fault. The Oligocene of Montgat consists of detrital sediments of continental origin mainly deposited in alluvial fan environments; these deposits are folded and affected by thrusts and strike-slip faults. They can be divided in two lithostratigraphic units separated by a minor southwest-directed thrust: (i) the Turó de Montgat Unit composed of litharenites and lithorudites with high contents of quartz, feldspar, plutonic and limestone rock fragments; and (ii) the Pla de la Concòrdia Unit composed of calcilitharenites and calcilithorudites with high contents of dolosparite and dolomicrite rock fragments. The petrological composition of both units indicates that sediments were derived from the erosion of Triassic (Buntsandstein, Muschelkalk and Keuper facies), Jurassic and Lower Cretaceous rocks (Barremian to Aptian in age). Stratigraphic and petrological data suggest that these units correspond to two coalescent alluvial fans with a source area located northwestwards in the adjoining Collserola and Montnegre inner areas. Micromammal fossils (Archaeomys sp.) found in a mudstone layer of the Pla de la Concòrdia Unit assign a Chattian age (Late Oligocene) to the studied materials. Thus, the Montgat deposits are the youngest dated deposits affected by the contractional deformation that led to the development of the Catalan Intraplate Chain. Taking into account that the oldest syn-rift deposits in the Catalan Coastal Ranges are Aquitanian in age, this allows to precise that the change from a compressive to an extensional regime in this area took place during latest Oligocene-earliest Aquitanian times. This age indicates that the onset of crustal extension related to the opening of the western Mediterranean Basin started in southern France during latest Eocene-early Oligocene and propagated southwestward, affecting the Catalan Coastal Ranges and the northeastern part of the Valencia trough during the latest Chattian-earliest Aquitanian times.

Deep crustal electromagnetic structure of Bhuj earthquake region (India) and its implications

The existence of fluids and partial melt in the lower crust of the seismically active Kutch rift basin (on the western continental margin of India) owing to underplating has been proposed in previous geological and geophysical studies. This hypothesis is examined using magnetotelluric (MT) data acquired at 23 stations along two profiles across Kutch Mainland Uplift and Wagad Uplift. A detailed upper crustal structure is also presented using twodimensional inversion of MT data in the Bhuj earthquake (2001) area. The prominent boundaries of reflection in the upper crust at 5, 10 and 20 km obtained in previous seismic reflection profiles correlate with conductive structures in our models. The MT study reveals 1-2 km thick Mesozoic sediments under the Deccan trap cover. The Deccan trap thickness in this region varies from a few meters to 1.5 km. The basement is shallow on the northern side compared to the south and is in good agreement with geological models as well as drilling information. The models for these profiles indicate that the thickness of sediments would further increase southwards into the Gulf of Kutch. Significant findings of the present study indicate 1) the hypocentre region of the earthquake is devoid of fluids, 2) absence of melt (that is emplaced during rifting as suggested from the passive seismological studies) in the lower crust and 3) a low resistive zone in the depth range of 5-20 km. The present MT study rules out fluidsand melt (magma) as the causative factors that triggered the Bhuj earthquake. The estimated porosity value of 0.02% will explain 100-500 ohm·m resistivity values observed in the lower crust. Based on the seismic velocities and geochemical studies, presence of garnet is inferred. The lower crust consists of basalts - probably generated by partial melting of metasomatised garnet peridotite at deeper depths in the lithosphere - and their composition might be modified by reaction with the spinel peridotites.

The Upper Oligocene of Montgat (Catalan Coastal Ranges, Spain): new age constraints to the western Mediterranean Basin opening

The Oligocene deposits of Montgat are integrated in a small outcrop made up of Cenozoic and Mesozoic rocks located in the Garraf-Montnegre horst, close to the major Barcelona fault. The Oligocene of Montgat consists of detrital sediments of continental origin mainly deposited in alluvial fan environments; these deposits are folded and affected by thrusts and strike-slip faults. They can be divided in two lithostratigraphic units separated by a minor southwest-directed thrust: (i) the Turó de Montgat Unit composed of litharenites and lithorudites with high contents of quartz, feldspar, plutonic and limestone rock fragments; and (ii) the Pla de la Concòrdia Unit composed of calcilitharenites and calcilithorudites with high contents of dolosparite and dolomicrite rock fragments. The petrological composition of both units indicates that sediments were derived from the erosion of Triassic (Buntsandstein, Muschelkalk and Keuper facies), Jurassic and Lower Cretaceous rocks (Barremian to Aptian in age). Stratigraphic and petrological data suggest that these units correspond to two coalescent alluvial fans with a source area located northwestwards in the adjoining Collserola and Montnegre inner areas. Micromammal fossils (Archaeomys sp.) found in a mudstone layer of the Pla de la Concòrdia Unit assign a Chattian age (Late Oligocene) to the studied materials. Thus, the Montgat deposits are the youngest dated deposits affected by the contractional deformation that led to the development of the Catalan Intraplate Chain. Taking into account that the oldest syn-rift deposits in the Catalan Coastal Ranges are Aquitanian in age, this allows to precise that the change from a compressive to an extensional regime in this area took place during latest Oligocene-earliest Aquitanian times. This age indicates that the onset of crustal extension related to the opening of the western Mediterranean Basin started in southern France during latest Eocene-early Oligocene and propagated southwestward, affecting the Catalan Coastal Ranges and the northeastern part of the Valencia trough during the latest Chattian-earliest Aquitanian times.

Els nens i nenes amb “Dictamen d’escolarització” i amb suport del CDIAP: estudi de les dimensions de l’atenció a les necessitats especials de l’alumnat, entre tres i sis anys, escolaritzat en un centre públic de la comarca d’Osona

La meva recerca ha tingut com a punt de partida “Els nens i nenes amb “Dictamen d’escolarització” i amb suport del CDIAP: estudi de les dimensions de l’atenció a les necessitats especials de l’alumnat, entre tres i sis anys, escolaritzat en un centre públic de la comarca d’Osona”. A partir d’aquí, s’ha elaborat un marc teòric a partir de les lleis d’educació, decrets que regulen els diferents serveis i un seguit de conceptes bàsics. Un cop elaborat aquest marc teòric per tal de recollir les dades dels alumnes, de tres a sis anys, d’una escola en concret s’ha dissenyat un instrument de recollida de dades que li diem full resum de serveis (FRS). El FRS és un instrument que ens ha servit per recollir totes les dades d’alumnes amb necessitats específiques i, sobretot, per saber quin suport reben per part de l’escola i per part d’altres serveis. A més a més, per recollir informació sobre els diferents serveis que atenen aquesta diversitat s’ha elaborat un guió d’entrevistes (GE). Aquest GE serveix per recollir els aspectes més importants de les entrevistes realitzades a l’EAP (Equip d’Assessorament i Orientació Psicopedagògica), CDIAP (Centre de Desenvolupament Infantil i Atenció Precoç) i CSMIJ (Centre de Salut Mental Infantil i Juvenil). A partir de la informació extreta dels dos instruments, s’han elaborat unes conclusions respecte els objectius plantejats en aquest projecte i la pregunta plantejada a l’inici.

Stratigraphy and petrology of the Miocene Montjuic delta: (Barcelona, Spain).

The Neogene rift in the Catalan Coastal Ranges, which is located in the NE part of the Eastern Iberian Margin, corresponds to a system of grabens formed at the nort h - we s t e rn edge of the Valencia Trough. In the central part of the Catalan Coastal Ranges are the Valls - Peneds half-graben in the onshore and the Barcelona half-graben in the offshore, which are separated by the Garraf and the Collserola-Montnegre horsts. Montjuc hill is a tilted block, which is located to the S of the Barcelona city, between the Collserola-Montn egre horst and the Barcelona half-graben . The Middle Miocene section of Montjuc is constituted by an alternation of conglomerate, sandstone, mudstone and marlstone beds. The Montjuc section was divided into four lithostratigraphic units from base to top: (1) The Morrot conglomerate and sandstone Unit, interpreted as delta plain deposits; (2) the Castell conglomerate, sandstone and mudstone Unit considered as proximal delta front deposits; (3) the Miramar marlstone Unit attributed

Spain, Economic Crisis, and the New Enclosure of the Reproductive Commons

In the past f ew years numerous authors have examined how the current economic crisis in Spain has dif f erential impacts on women and men.1 While this is important to show, this article’s goal is to make the leap f rom a mere description of the gendered effects of the crisis, to an analysis of some of the very gendered processes that shape it at its core. In other words, the intent is to understand how both the crisis itself and the ways the state manages it are structurally shaped by gender.