Juan Ignacio Morales

First fossil evidence of an “interglacial refugium” in the Pyrenean region

A refugium is generally understood as an area where temperate species survive cold periods, such as the Iberian, Italian, or Balkan Peninsulas in Europe. Strictly speaking, this definition refers to what is known as a glacial refugium. However, there are various types of lesser-known refugia such as the interglacial refugium, which denotes a mountainous region at low latitudes, such as the Pyrenees, where species adapted to the cold survive during interstadial periods. The small-vertebrate association from the sequence of Cova Colomera, which is located on the southern face of the Pyrenees and contains the final cold spell of the Late Pleistocene and the beginnings of the temperate period in which we currently find ourselves (the Holocene), could constitute the first fossil evidence of such an interglacial refugium, thus providing new paleoecological data on the phenomenon.

Small-mammal diversity in Spain during the late Pleistocene to early Holocene: Climate, landscape, and human impact

We investigate changes in small-mammal richness and diversity in southwestern Europe (Iberian Peninsula) during the late Pleistocene–Holocene transition in order to evaluate whether they follow a climatic pattern or are predominantly determined by human impact, especially after the emergence of agriculture in the Neolithic period. We selected 6 late Pleistocene and Holocene sites that correspond to 18 different layers dated to between ca. 22 and 3 kyr B.P. Using indices of species richness and evenness diversity, we show that climate played an important role at some sites during the late Pleistocene and at the beginning of the Holocene, in that the richness and diversity of small mammals were closely related to the mean annual temperatures and landscape changes, and varied according to the different climatic fluctuations detected (Heinrich Event 1, Bolling-Allerod, and Preboreal-Boreal). However, at the beginning of the mid-Holocene, the small-mammal richness and diversity no longer seem to follow any kind of climatic pattern, and the observed changes in some studied sites are more closely related to human activities. By contrast with similar studies carried out in other parts of the world, the changes in diversity in the Iberian Peninsula do not seem to follow a constant pattern during the late Pleistocene and beginning of the Holocene. Some of the changes detected appear to be related to climate (late Pleistocene), and others appear to be related to human influence (Holocene) on the landscape.

The gigapixel image concept for graphic SEM documentation. Applications in archeological use-wear studies

In this paper, we propose a specific procedure to create gigapixel-like images from SEM (scanning electron microscope) micrographs. This methodology allows intensive SEM observations to be made for those disciplines that require of large surfaces to be analyzed at different scales once the SEM sessions have been completed (e.g., stone tools use-wear studies). This is also a very useful resource for academic purposes or as a support for collaborative studies, thus reducing the number of live observation sessions and the associated expense.

La malacofauna marina de las fases holocenas en la Cueva del Toll (Moià, Barcelona): nuevas aportacionespara el Neolítico nororiental

Factores que afectan a la densidad reproductora del Quebrantahuesos, el Buitre Leonado y el Alimoche comun en Cataluna (NE de Espana): implicaciones para su gestion.- Utilizando analisis multivariantes examinamos las diferencias en la densidad reproductora del Quebrantahuesos Gypaetus barbatus, el Buitre Leonado Gyps fulvus y el Alimoche comun Neophron percnopterus en el NE de Espana (Cataluna), de acuerdo con diferentes variables troficas, orografico-paisajisticas y antropicas, y tomando la division comarcal como unidad de estudio. Los modelos sugieren que la alta densidad de Quebrantahuesos esta principalmente relacionada con la superficie de terreno no arbolado y poco humanizado. Por otro lado, las altas densidad de Alimoches comunes y Buitres Leonados se asocian a la alta disponibilidad de recursos alimenticios (ovejas y cabras), y ademas a una escasa densidad de habitantes en el caso del Alimoche comun y con la altitud (rango entre 1.000 y 2.000 m) y la ausencia de superficie arbolada en el caso del Buitre Leonado. El Quebrantahuesos parece la especie mas selectiva con las caracteristicas del medio, mientras que el Buitre Leonado y el Alimoche comun muestran una mayor plasticidad ecologica. Las medidas de conservacion futuras deberian tener en cuenta estos resultados de cara a optimizar su gestion. En este sentido, la importancia del alimento proporcionado por el ganado no estabulado parece fundamental para la conservacion de las aves carroneras. Las comarcas con mayor densidad poblacional (Alta Ribagorca, Pallars Jussa y Alt Urgell) son en las que deberian invertirse mayores medidas de control y proteccion puesto que albergan un porcentaje muy importante de la poblacion de estas especies. Por otro lado, las comarcas con menor densidad poblacional deberian ser administradas de manera que su gestion y las acciones de conservacion favorezcan la expansion geografica y los procesos de recolonizacion de zonas no ocupadas por estas especies. Las prioridades de conservacion deberian basarse en favorecer la ganaderia extensiva y, como una alternativa a la creacion de muladares, permitir a los ganaderos dejar las carcasas de animales en el campo, teniendo en cuenta la compatibilidad con las politicas sanitarias.[eng] In this work we present a geophysical study of three Western Mediterranean basins: Valencia Trough, Gulf of Lions and Algero-Balearic Basin. The work aims to define the tectonic structure, nature of the basement, and to discuss the age, kinematics and mechanisms involved in basin formation. To study the basins we have gathered all deep penetrating seismic data available in the region consisting on several academic and industry data reprocessed and interpreted for this work. To study the Valencia Trough Basin structure, we reprocessed from field data the 400 km-long multichannel seismic line ESCI-Valencia acquired in 1992 by Geco-Prakla’s survey vessel M.V. Bin Hai supported by the Spanish “Plan Nacional de I+D” with reference projects GEO89-0858 and GEO90-0733. We reprocessed the stack of the 170 km-long VALSIS-819 multichannel seismic line acquired in 1988 by the Lamont- Doherty Earth Observatory Research Vessel (R/V) Robert D. Conrad. We have also interpreted an industry seismic grid SGV01 acquired in 2001 by the Fugro-Geoteam vessel R.V. Geo Baltic. To study the Gulf of Lions Basin formation we interpreted an industry dataset SPBAL01 acquired in 2001 by Spectrum Energy with the Polar Princes vessel. Some amount of post-migration cosmetic processing was done on some of the lines of this data set for presentation purposes. To study the tectonic structure of the Algero-Balearic Basin we processed a 97 km- long multichannel seismic line TOPOMED-26 acquired by our group and with my participation in 2011 on-board the Spanish R/V Sarmiento de Gamboa. In order to discuss the nature of the basement of the Algero-Balearic Basin, we also used the Vp model of the wide-angle seismic profile P03 from the WESTMED project. Moreover we have done “mirror imaging” with Ocean Bottom Seismometers along line P04 of WESTMED, and integrated the results of line ESCI-Valencia across the south-Balearic margin. The analysis, processing and interpretation of all this dataset allows us to a novel interpretation of a series of aspects regarding the structure and nature of the crust, and to discuss some new proposals for the tectonic processes that have led to the current configuration of the main Western Mediterranean basins. Seismic interpretation of the Valencia Trough reveals that this basin is possibly floored by continental crust and it is possibly the oldest Western Mediterranean basin. Contrary to what it is typically interpreted; we propose that the present day configuration of the Valencia Trough is strongly dominated by the tectonic activity of Mesozoic structures. During Mesozoic times occurred the greatest thinning of the crust yielding a minimum crustal thickness of ~4.5 km under the Columbretes Basin (SW Valencia Trough). Multichannel seismic sections show that the main tectonic structures are Mesozoic in age and reveal that the Neogene extensional event is very limited comparatively and has had a minor influence in the formation of the current crustal structure of the Valencia Trough. We also found no evidence of any relevant crustal thickening during Paleogene times. Thus our interpretation supports that the extension leading to the crustal configuration of the Valencia Trough was largely formed during Mesozoic times. Interpretation of a grid of multichannel seismic profiles in the Gulf of Lions supports the existence of three geological domains that are: 1) a continental domain formed by normal faults that tilted the continental basement with syn-rift sediment infill. 2) a ~100 km wide transition domain between continental and clear oceanic domain, characterized by a thin anomalous layer with high velocity (7.5 km s-1) that has been debated in the literature and that we interpret as exhumed and serpentinized mantle peridotite and 3) an oceanic domain characterized by thin oceanic crust (~5 km) with little evidence of important faulting. Multichannel seismic results from Algero-Balearic Basin have been complemented with information provided by a Vp wide-angle tomographic model coincident with one of the seismic reflection lines. A comparison of depth-velocity profiles of the tomographic model with existing 1D velocity-depth compilations of continental and oceanic crust (e.g. White et al., 1992; Christensen and Mooney, 1995) gives clues on the nature of the basement. The results reveal the existence of three main geological and geophysical domains: 1) a continental domain, with little evidence of faulted and tilted blocks (which are common features on extensional margins), although the vertical velocity structure matches well the Vp compilation for continental crust (Christensen and Mooney, 1995). The Vp data, seismic images and previous works on the region available in literature support abundant magmatism (with volcanism) during extension of soon after. 2) A narrow continent-ocean domain with vertical velocities neither typically continental crust nor oceanic crust and 3) a clear oceanic domain characterized by 6 km thick oceanic crust, with a vertical velocity gradient of oceanic layer 2 and 3, even though in this case formed in a back-arc context. A new kinematic model for the opening of the Western Mediterranean basins is beyond the scope of our work, and requires integration with other datasets from Tyrrhenian and Alboran Basins, and an extended study of the West Sardinia and Corsica margins. Also, to advance in such model, it requires a detailed reconstruction of submarine volcanic activity, imaged in the seismic data in all three basins but inadequately studied in available literature. Nonetheless, the results of this work should be considered in the future for new reconstructions that we propose need to be reviewed. [cat] Aquesta tesi te com a objectiu descriure l’estructura tectonica i la naturalesa del basament de les principals conques de la Mediterrania occidental: Solc de Valencia, Golf de Lleo i conca algerina-balear i discutir l’edat i els mecanismes de formacio que han donat lloc a la configuracio actual. Per aixo, s’han utilitzat tot un seguit de dades geofisiques tant d’industria com academiques. S’ha dut a terme el processat i la interpretacio de diversos perfils de sismica multicanal situats a l’area d’estudi i la interpretacio de dos perfils de sismica de gran angle de la conca algerina-balear. A mes a mes, en aquest cas s’ha utilitzat una nova tecnica coneguda com “Mirror Imaging” per a processar el senyal dels multiples en sismica de gran angle i que dona uns resultats equiparables als de sismica multicanal. La interpretacio sismica dels diferents perfils mostra com el Solc de Valencia presenta un basament de naturalesa continental al llarg de tota la conca i com la seva configuracio esta lligada als processos i les estructures que van tenir lloc durant el Mesozoic. Per altre banda, la interpretacio sismica dels perfils situats al Golf de Lleo han permes definir el limit entre 3 dominis amb un tipus de naturalesa del basament diferent: 1) Domini continental, 2) domini de transicio entre escorca continental i oceanica i 3) Domini oceanic. Finalment, la interpretacio dels resultats de sismica multicanal de la conca algerina-balear juntament amb un estudi exhaustiu de les velocitats obtingudes a traves de la tomografia de gran angle a permes comparar el model de velocitats obtingut per aquets zona amb els models de referencia per escorca continental (Christensen and Mooney, 1995) i escorca oceanica (White et al., 1992), definint aixi 3 dominis diferents: 1) Domini continental, 2) domini de transicio entre escorca continental i escorca oceanica i 3) domini oceanic. Els resultats obtinguts en aquesta tesi intenten donar resposta a diverses questions encara obertes avui en dia, com son l’edat d’obertura de les diferents conques i la cinematica que ha donat lloc a llur formacio, aixi com discutir la validesa dels diferents models establerts per a la formacio de les conques de rere arc a la Mediterrania occidental.Cerquides and Rodriguez-Aguilar are funded by projects COR (TIN2012-38876-C02-01), AT (CSD2007-0022), and the Generalitat of Catalunya grant 2009-SGR-1434. This work was supported by the EPSRC-Funded ORCHID Project EP/I011587/1In the present work, a dynamic lumped parameter model of the electrochemical and thermal behavior of a Solid Oxide Fuel Cell (SOFC) has been developed. The model is implemented in the MATLAB-Simulink visual programming software. The model was calibrated using experimental data. A strategy is proposed for the thermal management of the stack and a controller is designed to keep the operating temperature of the system constant. This implemented strategy and controller is evaluated through simulation.Here we present an overview on the results of eight years of research line devoted to the organisation, expression and evolution of rRNA genes in plant genomes. We describe how we discovered a new rDNA arrangement in genus Artemisia, which includes all rRNA genes in a single unit (L-type). This was the first time that such organisation was found in seed plants. We further explored family Asteraceae in depth, to which Artemisia belongs, to find that the L-type arrangement may be present in about 25% of its species. Later on we move to gymnosperms to describe the landscape of rRNA arrangements in a representative sample of its diversity. We assess the expression rate of the L-type rRNA in several L-type species, which is comparable to that of species with separated arrangement of rRNA genes (S-type). Finally, we present the resource www.plantrdnadatabase.com which includes information on type of rDNA arrangement, number and position of rDNA loci in plants. Correspondence/Reprint request: Dr. Sònia Garcia, Institut Botànic de Barcelona (IBB-CSIC-ICUB), Passeig del Migdia s/n, 08038 Barcelona, Spain. E-mail: soniagarcia@ibb.csic.es Sònia Garcia et al. 50Trabajo presentado en el Seminaris de recerca Facultat de Farmacia, Universitat de Barcelona, celebrado en Barcelona el 15 de marzo de 2016.Over the past years different activities related on marine ecosystems monitoring techniques have been carried out at OBSEA observatory. The OBSEA is a cabled observatory placed at 4 km from the coast of Vilanova i la Geltru, Barcelona (Spain), and at 20 m depth, which has been in operation for more than 10 years. The special characteristics of the OBSEA platform (e.g. unlimited power supply, high bandwidth communication, and easy access) offers an extraordinary opportunity to develop and test different acoustic monitoring techniques. In this framework, many methods have been deployed and tested on target monitoring techniques, which goes from hydrophones surveillance, to target tracking using acoustic range-only methods by the use of autonomous underwater vehicles.La financiacion para este trabajo proviene del Ministerio de Economia mediante los proyectos CGL2009-09727 (RIFSIS), CSD 2006-00041 (TopoIberia), CGL2007-63889 (SIMA), CGL2008-3474 (TopoMed) y de la subvencion de la Generalitat de Catalunya 2009SGR996. Hemos utilizado tambien datos del proyecto PICASSO, financiado por el proyecto EAR0808939 de la NSF de Estados UnidosRodriguez Gonzalez, A., Perez Torrado, F.J., Fernandez Turiel, J. L., Carracedo, J.C., Gimeno, D., Guillou, H., Paris, R., Hansen, A., Aulinas, M. Modelizacion morfologica y morfometrica de erupciones volcanicas recientes generando plataformas costeras: caso estudio del volcan de Montana del Tesoro (El Hierro, Islas Canarias). En: El Cuaternario en Espana y Areas Afines, Avances en 2011 (Eds. V. Turu, Constante, A.), pp. 105-108. Fecha: 4/7/2011. Editorial: Asociacion Espanola para el Estudio del Cuaternario (AEQUA), Andorra la Vella, Andorra. ISBN 978-99920-1-856-9.Gisbert Pinto G., Gimeno Torrente D., Aulinas Junca M., Fernandez–Turiel J. L., Gasperini D., Fernandez De La Cruz A. Origin of clinopyroxene cores of lavas from the Garrotxa Volcanic Field (Spain). Macla, ISSN 2659-9864, 2011, 15, 101-102.Funding for the research was provided by Departament de Medi Ambient of Generalitat de Catalunya and Fundacio Territori i PaisatgeTrabajo presentado en el XI Simposi de Neurobiologia: Future technical advances, organizado por la Socitat Catalana de Biologia, en Barcelona, los dias 12 y 13 de noviembre de 2018A thesis submitted to the Universitat Politecnica de Catalunya to obtain the degree of Doctor of Philosophy. Doctoral programme: Automatic Control, Robotics and Computer Vision. This thesis was completed at: Institut de Robotica i Informatica Industrial, CSIC-UPC.The third author is partially supported by Catalan grant 2000FI00100 and by Spanish grant 2000SGR00007.Just as conventional institutions are organisational structures for coordinating the activities of multiple interacting individuals, electronic institutions provide a computational analogue for coordinating the activities of multiple interacting software agents. In this paper, we argue that open multi-agent systems can be effectively designed and implemented as electronic institutions, for which we provide a comprehensive computational model. More specifically, the paper provides an operational semantics for electronic institutions, specifying the essential data structures, the state representation and the key operations necessary to implement them.Ajuts a les universitats i centres publics de recerca de Catalunya per a accions integrades amb centres de recerca de les regions i entitats associades amb Catalunya (ACI) - Pla de Recerca de Catalunya 1993-1996, Accion Integrada con la Universidad de Buenos Aires, ArgentinaThis research has been supported by MICINN-Spain under contracts TIN2011-28689-C02-01, TIN2012-38876-C02-01 and the Generalitat of Catalunya (2009-SGR-1434)Intentional and accidental poisoning of wild and domestic animals in Spain: differences between regions. In this study we have analyzed 1,157 suspected cases of poisoning of wild and domestic animals in the natural environment (1,800 animals and 340 baits) from different Spanish regions during the period 2004- 2010. We detected 41.2% of positive cases (40.8% of animals and 52.6% of baits). In domestic carnivores detection of toxic compounds reached 71.4%, indicating its usefulness as sentinels of the use of poison in the environment. In those animals positive for toxicological analysis, 78.3% have been considered as intentional poisonings. The diurnal raptors were most affected by poisoning (43.6% of positives), followed by carnivorous mammals (27.1%). The most frequently detected toxicants were anticholinesterase insecticides (baits/animals: 80.4%/65.8%), followed by anticoagulant rodenticides (5%/19.6%), strychnine (2.2%/6.5%) and arsenic (4.5%/2.3%). The differences observed between regions underlines the dominance in the use of strychnine in Asturias, anticoagulant rodenticides in Castilla y Leon, organophosphate insecticides in Aragon, carbamate insecticides in Castilla-La Mancha and Madrid, and the emergence of other poisons, such as a-chloralose or barbiturates, in Catalonia. In summary, 82.3% of intentional poisonings were due to anticholinesterase pesticides and 85.5% of accidental anticoagulant rodenticides. Future regulations of pesticides and biocides should take into account the risk of illegal use in the preparation of poisoned baits which involves the marketing of formulations with high richness of active ingredients with low LD . 50Second Symposium on Fishery-Dependent Information, 3-6 March 2014, Rome, Italy.-- 1 page, 7 figuresVI Simposio Internacional de Ciencias del Mar - VI International Symposium of Marine Sciences (ISMS 2018), 20- 22 June 2018, Vigo.-- 2 pagesALC acknowledges the Xunta de Galicia for a postdoctoral contract funded by the ‘Programa de axudas a etapa posdoutoral da Xunta de Galicia’ (Conselleria de Cultura, Educacion e Ordenacion Universitaria). This work was carried out jointly within the ‘Grup de Recerca Consolidat de la Generalitat de Catalunya’ B-CSI (2014SGR940) and the Geologia Marina y Ambiental (Geoma-XM2) GroupA thesis submitted to the Universitat Politecnica de Catalunya to obtain the degree of Doctor of Philosophy. Doctoral programme: Automatic Control, Robotics and Computer Vision. This thesis was completed at: Institut de Robotica i Informatica Industrial, CSIC-UPC.Trabajo presentado en el XI Simposi de Neurobiologia: Future technical advances, organizado por la Socitat Catalana de Biologia, en Barcelona, los dias 12 y 13 de noviembre de 2018Hogan recently provided an heuristic technique called family of modes (FOM) to solve model predictive control (MPC) problems under hybrid constraints and underactuation. The goal of this study is to further develop this new method and to expand its usage in the robotics manipulation community. With that objective in mind, we address some of the methods weaknesses, we provide comparison tools to try to compare the method with traditional MPC solving techniques and we provide a simple and systematic technique to set-up the methods parameters. We conclude the study by presenting our the future lines of research, which consist in generalizing the method for more complex systems and testing its robustness.Este trabajo ha recibido financiacion procedente proviene del Ministerio de Economia y Competitividad (MINECO) mediante los proyectos CSD 2006-00041 (TopoIberia), Red TopoIberia-Iberarray CGL2014-54582-REDC] y de la subvencion de la Generalitat de Catalunya 2009SGR996.Farias S., Fernandez-Turiel J. L., Gimeno D. Arsenico en aguas superficiales y subterraneas del Partido de Villarino, Provincia de Buenos Aires, Argentina. En: Galindo G., Fernandez-Turiel J. L., Storniolo A. (eds.), Presencia de fluor y arsenico en aguas subterraneas. Grupo Argentino de la Asociacion Internacional de Hidrogeologos y Ediciones Amerindia., pp. 23-32. 2009. ISBN 978-987-1082-35-3.O.D. acknowledges funding from the Israel Science Foundation through Grants No. 1814/14 and No. 2143/14. Work in Bellaterra was supported by MINECO (Spain) through Grant No. FIS2015-64886-C5-3-P as well as the Severo Ochoa Centers of Excellence Programs under Grant No. SEV-2015- 0496, and by Generalitat de Catalunya (2017SGR1506). J.I. was supported by the Luxembourg National Research Fund through Grant No. P12/4853155 COFERMAT.Papastergios G., Filippidis A., Fernandez–Turiel J.L., Gimeno D., Sikalidis C. Environmental assessment of potentially toxic trace elements in sediments of Filippos B Port, Northern Aegean Sea – a comparison with other national and international coastal regions. Scientific Annals, School of Geology, Faculty of Sciences, Aristotle University of Thessaloniki, Proceedings XIX Carpathian-Balkan Geological Association Congress, 23-26, 2010, Thessaloniki, Greece, Special Volume 100, 113-120.Global concerns about nowadays’ energy shortage problems as well as climate change eects have encouraged alternatives to classical energy sources such as fossil fuels and nuclear power plants. In this context, combined heat and power is presented as a useful option due to its ability of generating both electrical and thermal energy more eciently than conventional methods. Regarding this, high temperature proton exchange membrane fuel cells are not only a reliable way of implementing combined heat and power systems, but also a better solution in terms of energy conversion eciency and greenhouse gases emissions reduction. Therefore, high temperature proton exchange membrane fuel cells are being installed around the world and policies encouraging its utilisation are being promoted.Memoria de tesis doctoral presentada por Rosana Arizmendi Mejia para optar al grado de Doctora por la Universitat de Barcelona (UB), realizada bajo la direccion de la Dra. Cristina Linares Prats de la Universitat de Barcelona (UB) y del Dr. Jean-Baptiste Ledoux del Institut de Ciencies del Mar (ICM-CSIC).-- 148 pagesProjects 2014-100575 from Departament de Cultura de and SGR2014-901 from AGAUR (both from Generalitat de Catalunya) financed the drilling campaigns.Dellunde and Garca-Cerda~na are supported by EdeTRI (TIN2012-39348-C02-01); Garca-Cerda~na is also supported by the Spanish MICINN project MTM 201125745 and the grant 2009SGR 1433 from the Generalitat de Catalunya;Noguera is supported by the project GA13-14654S of the Czech Science Foundation and by the FP7-PEOPLE-2009-IRSES project MaToMUVI (PIRSES-GA-2009-247584)This study was supported by the Departament de Medi Ambient de la Generalitat de Catalunya and Direccion General de Conservacion de la Naturaleza (Ministerio de Medio Ambiente).ENGLISH: In this PhD thesis we present a geophysical study of the westernmost Mediterranean basin: the Alboran Basin. This basin is located between the Iberian Peninsula and North Africa, and it is surrounded by the Betics and Rif orogenic ranges. Along the Alboran basin, runs the plate boundary between Iberia and Africa tectonic plates. The processes that led to the basin formation in this compressive setting, and the later processes that controlled the basin deformation, remain unclear, as well as the deep structure of the basin. This study aims to: 1) characterize the crust and the basement of the basin, 2) define a seismostratigraphy coherent for the entire basin and analyse the basin evolution in the basis of the sedimentary record, 3) characterize the northeaster transition between the Alboran Basin and the Algero-Balearic Basin through the study of the Palomares Margin and 4) characterize the two most prominent tectonic structures in the area, the Yusuf Fault and the Alboran Ridge front fault. The results of this thesis have been integrated in a geodynamic model of the area, and will help to improve the regional seismic and tsunami hazard assessment model. In order to perform a regional scale study of the Alboran Basin, we have a wide Multichannel Seismic reflection (MCS) profiles grid acquired during different projects (including TOPOMED, EVENTDEEP, CAB, ESCI, CONRAD and IMPULS projects). Our results reveal that three different crusts are coexisting in the Alboran Basin: a thinned continental crust below the West Alboran and Malaga basins, a magmatic arc crust in the central and eastern parts, and the North African continental crust, below the Pytheas and Habibas basins. The basin is configured in a fore-arc basin an magmatic arc, being the back-arc basin of the system the Algero-Balearic Basin. The seismostratigraphy study supported and early Miocene initiation of the extension in the West Alboran and Malaga basins, followed by a Langhian-Serravallian extension in the North African margin. At the Tortonian, magmatic activity linked to the subduction system led to the volcanic arc formation. At the Messinian, extensional processes ended and the contractive reorganization of the basin occurred. The geomorphology study of the Palomares margin support that this contractive reorganization is not a widespread processed, as only few minor faults are reactivated. This hypothesis is confirmed by the characterizations of the Yusuf Fault and the Alboran Ridge front fault. Results in both fault systems are coherent, and point out a minimum total slip of ~20 km in a SE-NW direction since the Messinian top (5.3 Ma). Taking into account the plate convergence rates, the total convergence since the Messinian top is ~24 km, supporting that most of the strain is accommodated by these two faults. These results highlight the importance of a further seismic characterization of the area. The integration of the results presented in this thesis, together with the most recent tomographic studies (i.e., TOPOIBERIA project), bring to light the necessity of review the geodynamic models of the area. We conclude that the Alboran basin formation took place during the Miocene. The extensional processes were controlled by the geodynamics of the subduction system evolution, including westward slab roll-back and lithosphere tearing. At the ended of the Messinian, extension in the basin finished as a consequence of the ceased of the subduction. The Plio-Quaternary represented the deformational stage of the basin, led by the Iberian – African plate convergence. The distribution of the tectonic structures active in this compressive setting was defined by the inherited lithospheric structure that defined the weakness areas were these faults were developed. CASTELLANO La presente Tesis Doctoral se fundamenta en un estudio basado esencialmente en perfiles de sismica de reflexion (mayormente adquiridos durante los proyectos TOPOMED, EVENT-DEEP y ESCI) de la Cuenca de Alboran, situada entre las cordilleras Beticas (Sur de la Penisula Iberica) y Rif (Norte de Marruecos). El proceso de formacion de la cuenca es aun discutido, al igual que los posteriores procesos de deformacion. He centrado el presente estudio en: 1) caracterizar la estructura cortical de la cuenca, 2) definir su evolucion, basandome en el estudio del registro sedimentario, y 3) estudiar la reorganizacion contractiva de la cuenca. El estudio de la reorganizacion contractiva lo he centrado en tres zonas: el margen de Palomares, la falla de Yusuf y el cabalgamiento frontal de la Cresta de Alboran. Los resultados revelan tres tipos de corteza que coexisten a lo largo de la cuenca: a) corteza continental adelgazada, b) corteza de arco magmatico y por ultimo, c) corteza continental del Norte de Africa. Las primeras evidencias de la fase extensional se localizan en la cuenca oriental de Alboran y en la cuenca de Malaga de edad Burdigaliense, seguidas por la creacion de un segundo depocentro en el norte de Africa durante el periodo Languiense-Serravaliense. El arco magmatico se formo durante el Tortoniense. Los procesos extensionales en la cuenca ocurren hasta el Mesiniense, y a partir del Mioceno tardio-Plioceno temprano, cesa la extension y comienza la fase de deformacion compresiva de la cuenca. El estudio de las estructuras activas confirma que la inversion tectonica se focaliza en unas pocas fallas que marcan los limites entre dominios corticales. El desplazamiento acumulado desde el Plioceno Inferior de dos de las principales fallas de la Cuenca de Alboran, Yusuf y el cabalgamiento frontal de la Cresta de Alboran, es como minimo de 20 km. Este valor es cercano al valor total de la convergencia entre las placas de Iberia y Africa, y por tanto confirma que actualmente la deformacion se concentra principalmente en unas pocas estructuras. Dada su importancia, es necesario realizar un estudio de la peligrosidad de estas fallas para evaluar su potencial sismico y tsunamogenico e incluirlas en las bases de datos nacionales y europeas de riesgos geologicos.When people need help with day-to-day tasks they turn to family, friends or neighbours to help them out. Despite an increasingly networked world, technology falls short in supporting such daily tasks. u-Help provides a platform for building a community of helpful people and supports them in finding volunteers for day-to-day tasks. It relies on three techniques that allow a requester and volunteer to find one another easily, and build up a community around such provision of services. First, we use an ontology to distinguish between the various tasks that u-Help allows people to provide. Second, a computational trust model is used to aggregate feedback from community members and allows people to discover who are good or bad at performing the various tasks. Last, a flooding algorithm quickly disseminates requests for help through the community.Trabajo presentado en la 84th Annual Meeting of the American Assocition of Physical Anthropologists (AAPA 2015), celebrada en San Luis (US) del 25 al 28 de marzo de 2015.Memoria de tesis doctoral presentada por Melissa Judith Acevedo Dudley para obtener el titulo de Doctora en Ciencias del Mar por la Universitat Politecnica de Catalunya (UPC), realizada bajo la direccion del Dr. Albert Calbet Fabregat y la Dra. Veronica Fuentes del Institut de Ciencies del Mar (ICM-CSIC).-- 129 pagesThe diversification of Cheirolophus in Macaronesian archipelagos constitutes a paradigmatic example of radiation on oceanic islands. Phylogenetic and molecular dating analyses indicate an extraordinarily fast process, showing one of the highest speciation rates ever found on plants from oceanic islands. Such radiation has been recently studied employing phylogeographic, population genetic and molecular cytogenetic approaches. Here, the main potential patterns and processes involved in the diversification of the genus in the Canary Islands and Madeira are reviewed and discussed as a whole.This research has been partially supported by the 2014-SGR-118 grant from the Generalitat de Catalunya.Oxydromus humesi is an annelid polychaete living as a strict bivalve endosymbiont (likely parasitic) of Tellina nymphalis in Congolese mangrove swamps and of Scrobicularia plana and Macomopsis pellucida in Iberian saltmarshes. The Congolese and Iberian polychaete populations were previously considered as belonging to the same species, the latter showing regular distribution, intra-specific aggressive behaviour, and complex hostentering behaviour. The fresh Iberian samples enabled us to undertake consistent morphometric analyses, as well as to further analyse the characteristics of the association and the population dynamics of the Iberian population hosted by S. plana. Among the morphological differences between the Congolese and Iberian specimens, leading to the description of the latter as Oxydromus okupa sp. nov., the most important are: 1) longer cephalic appendages, 2) greater distance between the eyes, 3) larger dorsal cirrostyle in relation to the corresponding dorsal lobe and cirrophore. Moreover, dorsal and ventral lobes are similar in length, with the tip of the former reaching the tip of the latter in O. okupa sp. nov., while the dorsal lobe is much shorter than the ventral one in O. humesi. Mature adults of O. okupa sp. nov. occurred during the whole study period, with a higher percentage of ripe females in spring and, particularly, in summer. Numerous host specimens showed the symbiont’s most preferred shell length (>26 36 mm). However, the prevalence was very low (usually <5%) and showed a clear seasonal pattern, being lower during spring/summer. This suggests that males are able to leave their hosts during this period, most likely to improve fertilization by directly entering or approaching a host occupied by a ripe female, while females usually remain inside. Based on the new results, the current knowledge of symbiotic Hesionidae and their relationships with invertebrate hosts is updated and discussed.

Human impact on small-mammal diversity during the middle- to late-Holocene in Iberia: The case of El Mirador cave (Sierra de Atapuerca, Burgos, Spain):

The human impact on the environment in the Holocene has usually been characterized on the basis of palaeobotanical records, but attempts to distinguish the anthropogenic impact from natural events in landscape evolution have been the subject of much debate in recent years. The aim of this paper is to analyse small-mammal diversity and the presence of synanthropic species, whose small size makes them more sensitive to any changes in their environment that may occur. This study has allowed us to characterize palaeoclimatic and palaeoenvironmental changes, recording small changes whether resulting from a human influence or otherwise. Our object of study is El Mirador cave, which has a sequence with a well-documented human occupation extending from 7200 to 3000 cal. BP. The study has led us to differentiate two phases. In one phase, we can see small changes in diversity related to climatic oscillations from ca. 7200 to 6800 cal. BP, while in the second phase, lasting from ca. 6800 to 3000 cal. BP, the changes in diversity and in the assemblage of synanthropic species are associated with human economic strategies. Moreover, we distinguish which kinds of economic activity (crop and livestock farming) have influenced these changes, because some small-mammal species are influenced, positively or negatively, by environmental changes based on crop farming and animal husbandry. All this information is contrasted with other archaeological proxies, such as the large-mammal and palaeobotanical assemblages from El Mirador cave. Furthermore, this integrative analysis has made it possible to identify the existence of altered environments more generally throughout the Iberian Peninsula from ca. 6000 cal. BP. It additionally confirms the theory of low human occupation intensity in the northern Meseta and in high mountainous areas during the early Neolithic.

Métodos de talla y estrategias de reducción en la fabricación de foliáceos en el III milenio A.N.E. [Knapping methods and reduction strategies in leaf-like projectile production in the 3rd millennia B.C.E.]

In this paper we present a technological study of leaf-like arrow points recovered in an open-air site from the 3th millennium B.C., named El Tossal de La Munda (Vistabella del Maestrazgo, Castellon). It is located at the central east of Spain, in the southern part of Iberian range in a mountainous area about 100 km far from the coast. The site is on a small flat-topped hill of about 5000 m² and it is 820 m.a.s.l. The upper surface has been strongly eroded and the lithic material has been found directly on the bedrock or over the dissolution clays. We recovered close to 5000 lithic remains, offering an assemblage mainly produced in the 3rd millennia BC: retouched blades and flakes as main groups, leaf-like arrow points, in addition to some other retouched tools as segments (one triangle, one bifacial circle and a trapezoid), scrapers, end-scrapers, denticulate and notches, one raclette and one drill. We also found two small adzes. The cores were intensively exhausted. Just some of them show bladelet scars but most of them are small discoid and irregular shaped cores for the production of small flakes. Few of them show marks of bipolar flaking on anvil. Within the lithic assemblage there is a sample of 73 bifacial rough-outs and projectile points at different reduction stages, from initial blanks to finished and used ones. In addition, we found one refit and one conjoint. All of them are leaf-like arrow points except a fragment showing shoulders as an exception. We have identified some typical accidents in bifacial reduction: fractured rough-outs, overshot flakes, overshot negatives and another accident that we named “bending notches”, linked principally to the pressure technique (two positives and two negatives). We analysed both preforms and finished leaf-like arrow points from a technological point of view, first trying to identify the blank type and shape, and secondly trying to distinguish knapping methods and techniques. We have divided the methods in three main types: parallels (adjacent and contiguous), alternating, and independent method. We have identified the strategies according to edges and blank faces management. In our case, only simple combinations has been detected, mainly alternate (first one face, after the other side on the same edge). We have divided leaf-like production in five technical stages, and we described the identified knapping methods and strategies used at the site according to the reduction stage. In order to show this, we describe in the paper the most significant cases of the site. The identification of blanks has been possible in most of the rough-outs, verifying that the blanks used at the site were irregular and cortical flakes, chunks, fissure slabs and small cores. Despite this, leaf-like production at the site was really homogeneous, applying the same methods and also managing the blank faces similarly. Alternate strategy is completely dominant, firstly removing the ventral face, secondly the dorsal part. The main knapping method used at the site is the independent method, removing consecutively the most highlighted ridges. When the sketch is advanced and reaches a regular shape, the application of parallel method series is common. Technically we have observed two phases: first direct percussion (mainly with stone hammer); second, pressure technique. Heat modifications have been detected in 20 rough-outs and projectiles but most of them seem to be non-intentional, exhibiting cupules and cracks. Most of the finished ones do not show double shine (heat patina). According to this, we state that leaf-like production at the site was not a specialized process but it recovers to use as blanks previously discarded flakes, chunks and exhausted cores, part of them recycled before burning. The elaboration of leaf-like arrow points was embedded in the laminar production, and it played a marginal role within a lithic reduction system that is focused on blade and bladelet production. They used mainly cortical and non-cortical flakes, that seem to be by-products of blade core preparation, or exhausted cores that were reused for this purpose. Despite most of the arrow points result in crude and thick foliated shapes, we argue that in this technological context, the use of waste as blanks constrains the knapping reduction, and lead to rude shapes. Derived from this, we discuss on the leaf-like arrow point morphology and its profitability, the resistance of thick-elliptical tips and their role in the technological framework of the site and its landscape. We also discuss about the visibility of the skilled knapping in this context, when small, irregular and cortical flakes, burned chunks and exhausted cores were used as a blank to make leaf-like projectiles.