Iniciativas para el desarrollo sostenible del Área de Conservación Arenal- Huetar Norte, Costa Rica

El presente proyecto tiene como zona de estudio el Área de Conservación Arenal- Huetar Norte (ACA-HN), concretamente los cantones de Upala, Los Chiles y Guatuso. El propósito del proyecto es promover el desarrollo sostenible de la zona mediante los pilares de la educación y la economía. Para ello se elabora un manual de educación ambiental de la cuenca de río Frío y así poder solventar algunas de las carencias en educación que tienen los docentes de las escuelas de la cuenca hidrográfica. Por otro lado, se diagnostica la cadena de valor sobre usos alternativos de la biodiversidad, específicamente zoocriaderos de mariposas diurnas, en los cantones de Upala y Los Chiles. Por último, se trata la información de la zona de estudio con Sistemas de Información Geográfica (SIG) para elaborar mapas que ilustren los proyectos anteriores y el proyecto sobre el diagnóstico de la industria de turismo local.

Visor Web de les Normes subsidiàries i el cadastre de l’Ajuntament de Campos

El Visor Web de Cartografia de les Normes Subsidiàries i el Cadastre de Campos és un sistema, basat en la tecnologia WMS, que està desenvolupat emprant programari lliure i s’ha fet seguint els estàndards de l’OGC. El servidor és MapServer instal•lat sobre una plataforma Linux distribució openSUSE 10.1. La base de dades és PostgreSQL-PostGIS. S’ha emprat l’entorn Ka-Map que consisteix en una tecnologia que combina l’ús de la capacitat del servidor amb la de l’ordinador del client, cosa que fa que la visualització sigui més ràpida i ens permet que el mapa pugui emprar tota la pantalla de l’ordinador.

Analog Modelling of N-S anticlines of the External Sierras (Jaca basin, Southern Pyrenees)

Report for the scientific sojourn carried out at the Uppsala Universitet, Sweden, from April to July the 2007. Two series of analogue models are used to explore ductile-frictional contrasts of the basal décollement in the development of oblique and transverse structures simultaneously to thin-skinned shortening. These models simulate the evolution of the Central External Sierras (Southern Pyrenees, Spain), which constitute the frontal emerging part of the southernmost Pyrenean thrust sheet. They are characterized by the presence of transverse N-S to NW-SE anticlines, which are perpendicular to the Pyrenean structural trend and developed in the hangingwall of the Santo Domingo thrust system, detaching on an unevenly distributed Triassic materials (evaporitic-dolomitic interfingerings). Model setup performs a décollement made by three patches of silicone neighbouring pure brittle sand. Model series A test the thickness ratio between overburden and décollement. Model series B test the width of frictional detachment areas. Model results show how deformation reaches further in areas detached on ductile layer whereas frictional décollement areas assimilate the strain by means of an additional uplift. This replicates the structural style of Central External Sierras: higher structural relief of N-S anticlines with regard to orogen-parallel structures, absence of a representative ductile décollement in the core, tilting towards the orogen and foreland-side closure not thrusted by the frontal emerging South-Pyrenean thrust.

Condicions socioecològiques de la riera d'Arbúcies pel retorn de la llúdriga (Lutra lutra)

La llúdriga (Lutra lutra) va desaparèixer de la conca de la Tordera a causa de la pressió humana sobre ella i el seu hàbitat. Recentment les seves poblacions s’estan recuperant a las conques nord de Catalunya. En aquest context es presenta els resultats dels anàlisis dels requeriments socioecològics de la llúdriga en l’afluent del riu Tordera de la riera d’Arbúcies: qualitat del bosc de ribera, valoració de la contaminació de l’aigua i l’anàlisi de les poblacions d’ictiofauna, a més de l’estimació de l’espècie més abundant. L’evolució de l’ús i cobertes del sòl del sòl mostren que existeix una tendència augment en las masses forestals, zones urbanitzades i infraestructures; també una disminució del camps de cultiu, fruiters i vinyes. La qualitat del bosc de ribera es va valorar a partir del l’índex QBR, obtenint que la màxima qualitat es localitza en el tram alt, disminuint a mesura que s’apropa a la desembocadura al Tordera. La contaminació de l’aigua a estat valorada, per una banda analitzant la qualitat biològica a partir dels índexs IPS i BMWPC, obtenint que la qualitat de l’aigua disminueix a mesura que transcorre riu avall, segons l’IPS. Amb el BMWPC es troba que existeix una recuperació de la qualitat de l’aigua en l’últim tram. Per altra banda s’han analitzat el compostos químics que afecten a la llúdriga, obtenint que les concentracions d’aquest no són rellevants a l’aigua. S’ha analitzat l’estructura de la població d’ictiofauna present, trobant que el Barbus meridionalis és l’espècie més abundant en tots el trams, a més d’augmentar en captures a mesura que l’aigua s’apropa al aiguabarreig amb la Tordera. S’ha estimat la biomassa present d’aquesta espècie, concloent que es suficient per mantenir una població no gaire densa de llúdrigues, inferior a 0,15 individus per kilòmetre de riu.

El Estado en los campos. La regulación del cultivo del arroz en la España del siglo XIX

El papel desempeñado por el Estado en la economía española del siglo XIX ha sido muy controvertido y, en general, ha recibido juicios negativos. Este artículo trata de evaluar la intervención pública en el ámbito de la regulación del cultivo del arroz. Justificada frente al paludismo, esta reglamentación encontró grandes dificultades para ser aplicada hasta que se consolidó el nuevo aparato estatal salido de la revolución liberal, a causa de las resistencias locales y las limitaciones administrativas. En la segunda mitad del siglo XIX, sin embargo, el Estado estableció una legislación que perviviría en el tiempo y fue ampliamente respetada. De ese modo el Estado mostró una cierta autonomía respecto a intereses sociales muy arraigados y materializó medidas que tenían un impacto sobre la mejora sanitaria de la población.

Analysis of Pleistocene paleodrainage evolution in the Po Basin (Italy) by multivariate statistical techniques

In order to obtain a high-resolution Pleistocene stratigraphy, eleven continuouslycored boreholes, 100 to 220m deep were drilled in the northern part of the PoPlain by Regione Lombardia in the last five years. Quantitative provenanceanalysis (QPA, Weltje and von Eynatten, 2004) of Pleistocene sands was carriedout by using multivariate statistical analysis (principal component analysis, PCA,and similarity analysis) on an integrated data set, including high-resolution bulkpetrography and heavy-mineral analyses on Pleistocene sands and of 250 majorand minor modern rivers draining the southern flank of the Alps from West toEast (Garzanti et al, 2004; 2006). Prior to the onset of major Alpine glaciations,metamorphic and quartzofeldspathic detritus from the Western and Central Alpswas carried from the axial belt to the Po basin longitudinally parallel to theSouthAlpine belt by a trunk river (Vezzoli and Garzanti, 2008). This scenariorapidly changed during the marine isotope stage 22 (0.87 Ma), with the onset ofthe first major Pleistocene glaciation in the Alps (Muttoni et al, 2003). PCA andsimilarity analysis from core samples show that the longitudinal trunk river at thistime was shifted southward by the rapid southward and westward progradation oftransverse alluvial river systems fed from the Central and Southern Alps.Sediments were transported southward by braided river systems as well as glacialsediments transported by Alpine valley glaciers invaded the alluvial plain.Kew words: Detrital modes; Modern sands; Provenance; Principal ComponentsAnalysis; Similarity, Canberra Distance; palaeodrainage

A Factor analysis of hidrochemical composition of Llobregat river basin

Hydrogeological research usually includes some statistical studies devised to elucidate mean background state, characterise relationships among different hydrochemical parameters, and show the influence of human activities. These goals are achieved either by means of a statistical approach or by mixing modelsbetween end-members. Compositional data analysis has proved to be effective with the first approach, but there is no commonly accepted solution to the end-member problem in a compositional framework.We present here a possible solution based on factor analysis of compositions illustrated with a case study.We find two factors on the compositional bi-plot fitting two non-centered orthogonal axes to the most representative variables. Each one of these axes defines a subcomposition, grouping those variables thatlay nearest to it. With each subcomposition a log-contrast is computed and rewritten as an equilibrium equation. These two factors can be interpreted as the isometric log-ratio coordinates (ilr) of three hiddencomponents, that can be plotted in a ternary diagram. These hidden components might be interpreted as end-members.We have analysed 14 molarities in 31 sampling stations all along the Llobregat River and its tributaries, with a monthly measure during two years. We have obtained a bi-plot with a 57% of explained totalvariance, from which we have extracted two factors: factor G, reflecting geological background enhanced by potash mining; and factor A, essentially controlled by urban and/or farming wastewater. Graphicalrepresentation of these two factors allows us to identify three extreme samples, corresponding to pristine waters, potash mining influence and urban sewage influence. To confirm this, we have available analysisof diffused and widespread point sources identified in the area: springs, potash mining lixiviates, sewage, and fertilisers. Each one of these sources shows a clear link with one of the extreme samples, exceptfertilisers due to the heterogeneity of their composition.This approach is a useful tool to distinguish end-members, and characterise them, an issue generally difficult to solve. It is worth note that the end-member composition cannot be fully estimated but only characterised through log-ratio relationships among components. Moreover, the influence of each endmember in a given sample must be evaluated in relative terms of the other samples. These limitations areintrinsic to the relative nature of compositional data

ClubMed? Cyclical fluctuations in the Mediterranean basin

We investigate macroeconomic fluctuations in the Mediterranean basin, their similarities and convergence. A model with four indicators, roughly covering theWest, the East and the Middle East and the North Africa portions of theMediterranean, characterizes well the historical experience since the early 1980.Idiosyncratic causes still dominate domestic cyclical fluctuations in many countries. Convergence and divergence coexist are local and transitory. The cyclicaloutlook for the next few years is rosier for the East than for the West.

On the spread of the European catfish (Silurus glanis) in the Iberian Peninsula: first record in the Llobregat river basin

The first record of the European catfish (Silurus glanis L. 1758) introduced to the Llobregat river basin (NE Spain) is reported. We captured one individual of this silurid fish species (of a total of 541 fish) in La Baells reservoir on 30 August 2006. Given the low catchability of this fish species, the popularity among some anglers, and old rumours on this introduction, we hypothesize that this species has been present in the reservoir since a few years ago, despite we did not capture it in two previous surveys. The illegal introduction of this and other exotic species to other Iberian river basins should be prevented by the Spanish administration

Magnetostratigraphy of the Miocene continental deposits of the Montes de Castejón (central Ebro basin, Spain): geochronological and paleoenvironmental implications

A detailed magnetostratigraphic study has been carried out in the early to middle Miocene distal alluvial and lacustrine sediments of the Montes de Castejón (central Ebro Basin). The study was based on the analysis of 196 magnetostratigraphic sites sampled along a stratigraphic interval of about 240 meters. Local magnetostratigraphy yielded a sequence of 12 magnetozones (6 normal and 6 reverse) which could be correlated with the Geomagnetic Polarity Time Scale (GPTS) interval C5Cr to C5AD (between 17 and 14.3 Ma.). The sampled sedimentary sequences include the boundary between two tectosedimentary units (TSU, T5 and T6) already defined in the Ebro Basin. The magnetostratigraphy of the Montes de Castejón allows to date the T5/T6 TSU boundary at 16.14 Ma, within chron C5Cn.1n. This magnetostratigraphy also allows us to analyse in detail as well as to discuss the variations in sedimentation rates through space and time between different lacustrine environments: Outer carbonate lacustrine fringes and distal alluvial plains (Montes de Castejón sections) show higher sedimentation rates than offshore lacustrine areas (San Caprasio section, 50 km east of Montes de Castejón).

Sedimentological and palaeohydrological responses to tectonics and climate in a small, closed lacustrine system: Oligocene As Pontes Basin (Spain)

A small, closed, lacustrine system developed during the restraining overstep stages of the Oligocene As Pontes strike-slip basin (Spain). The increase in basin accommodation and the headward spread of the drainage, which increased the water input, triggered a change from shallow, holomictic to deeper, meromictic conditions.

Late Neogene lacustrine record and paleogeography in the Quillagua-Llamara basin, Central Andean fore-arc (Northern Chile)

The Cenozoic QuillaguaLlamara basin (northern Chile, Central Andes) is an asymmetrical, intramassif fore-arc basin with a relatively wide northern sector separated from a narrower southward extension by a basement threshold. The north- ern sector was characterised by a noticeable Oligocene?late Neogene alluvial-fan and lacustrine dominated deposition which resulted in sequences up to 900 m thick, whereas the southern sector was often a bypass zone with thinner fluvial and lacustrine sediment accumulation.

An inventory of the marine and transitional Middle/Upper Eocene deposits of the Southeastern Pyrenean Foreland Basin (NE Spain)

In the southeastern Ebro Foreland Basin, the marine deposits of Lutetian and Bartonian age show excellent outcrop conditions, with a great lateral and horizontal continuity of lithostratigraphic units. In addition, the rich fossil record -mainly larger foraminifers-, provides biostratigraphic data of regional relevance for the whole Paleogene Pyrenean Basin, that can be used for the Middle Eocene biocorrelation of the western Tethys. This contribution is a sedimentary and biostratigraphic synthesis of the basic outcrops and sections of the Lutetian andBartonian marine and transitional deposits in the southeastern sector of the Ebro Foreland Basin.