«S'ha de practicar, el problema és la solució» sense ús no hi ha prou aprenentatge: les pràctiques lingüístiques dels joves sabadellencs

El present article pretén conèixer les tries i els usos lingüístics dels joves de Sabadell. L'estudi se centra en els individus presents a l'escola secundària amb edats compreses entre 14 i 19 anys. En concret es basa a conèixer la importància de l'escola en l'adquisició de la segona llengua d'aquests joves, així com els factors que influencien en la tria i l'ús d'una llengua determinada en els diferents contextos. Donada la diversitat sociocultural actual de Catalunya els individus seleccionats representen les diverses tipologies principals existents segons el seu origen etnicolingüístic (català, castellà i bilingüe), combinat amb la composició del seu entorn bàsic de socialització (xarxes socials), i amb altres aspectes geogràfics, demogràfics i econòmics.

Marine and transitional Middle/Upper Eocenen units of the Southeastern Pyrenean Foreland Basin (NE Spain)

The stratigraphic basis of this work has allowed the use of larger foraminifers in the biostratigraphic characterisation of the new Shallow Benthic Zones (SBZ). This part of the volume presents a description of the sedimentary cycles formed by the transgressive-regressive systems of the Lutetian and Bartonian in the southeastern sector of the Ebro Foreland Basin. Concerning the Lutetian deposits studied in the Amer-Vic and Empordà areas, four sedimentary cycles have been characterised. The first and second are found within the Tavertet/Girona Limestone Formation (Reguant, 1967; Pallí, 1972), while the third and fourth cycles cover the Coll de Malla Marl Formation (Clavell et al., 1970), the Bracons Formation (Gich, 1969, 1972), the Banyoles Marl Formation (Almela and Ríos, 1943), and the Bellmunt Formation (Gich, 1969, 1972). In the Bartonian deposits studied in the Igualada area, two transgressive-regressive sedimentary cycles have been characterised in the Collbàs Formation (Ferrer, 1971), the Igualada Formation (Ferrer, 1971), and the Tossa Formation (Ferrer, 1971). The Shallow Benthic Zones (SBZs) recognised within the Lutetian are the following: SBZ 13, from the Early Lutetian, in the transgressive system of the first cycle; SBZ 14, from the Middle Lutetian, in the second cycle and the lower part of the transgressive system of the third cycle; SBZ 15, from the Middle Lutetian, in the remaining parts of the third system; SBZ 16, from the Late Lutetian, throughout the fourth cycle. The association of larger foraminifers in the first and second cycles of the Bartonian in the Igualada area has been used as the basis for the definition of SBZs 17 and 18 recognised in the Bartonian of the western Tethys.

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.

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.

Depositional models of lacustrine evaporites in the SE margin of the Ebro basin (Paleogene, NE Spain)

An important evaporitic sedimentation occurred during the Paleogene (Eocene to lower Oligocene) in the Barberà sector of the southeastern margin of the Tertiary Ebro Basin. This sedimentation took place in shallow lacustrine environments and was controlled by a number of factors: 1) the tectonic structuration of the margin; 2) the high calcium sulphate content in the meteoric waters coming from the marginal reliefs; 3) the semiarid climate; and 4) the development of large alluvial fans along the basin margin, which also conditioned the location of the saline lakes. The evaporites are currently composed of secondary gypsum in surface and anhydrite at depth. There are, however, vestiges of the local presence of sodium sulphates. The evaporite units, with individual thicknesses ranging between 50 and 100 m, are intercalated within various lithostratigraphic formations and exhibit a paleogeographical pattern. The units located closer to the basin margin are characterized by a massive gypsum lithofacies (originally, bioturbated gypsum) bearing chert, and also by meganodular gypsum locally (originally, meganodules of anhydrite) in association with red lutites and clastic intercalations (gypsarenites, sandstones and conglomerates). Chert, which is only linked to the thickest gypsum layers, seems to be an early diagenetic, lacustrine product. Cyclicity in these proximal units indicates the progressive development of lowsalinity, lacustrine bodies on red mud flats. At the top of some cycles, exposure episodes commonly resulted in dissolution, erosion, and the formation of edaphic features. In contrast, the units located in a more distal position with regard to the basin margin are formed by an alternation of banded-nodular gypsum and laminated gypsum layers in association with grey lutites and few clastic intercalations. These distal units formed in saline lakes with a higher ionic concentration. Exposure episodes in these lakes resulted in the formation of synsedimentary anhydrite and sabkha cycles. In some of these units, however, outer rims characterized by a lithofacies association similar to that of the proximal units occur (nodular gypsum, massive gypsum and chert nodules).

Foreword (2004)

This is the first issue of Geologica Acta dedicated to the memory of Professor Francesc Calvet, whose life was cut short in January 2002 when he was only 54. Francesc was a man with great human qualities, a distinguished scientist and an inspiring teacher who was held in high esteem by all those who knew him. His academic achievements, talent and friendly personality attracted numerous colleagues and students. Unfailingly courteous and polite, he was passionately committed to social justice and was a staunch defender of freedom of conscience and tolerance.

Coastal salina evaporites of the Triassic-Liassic boundary in the Iberian Peninsula: the Alacón borehole

The evaporite unit (the Lécera Formation), which was formed at the Triassic¿Liassic boundary in the Aragonian Branch of the Iberian Chain, was studied at the 01 Alacón borehole (Alacón village, Teruel province), where it is mainly constituted by a thick (>e and reflect deeper water settings, whereas in the upper part they correspond to shallower water settings. The evaporite sedimentation mainly occurred in a subsiding coastal basin of the salina or lagoon type. In this setting, the subaqueous precipitation of the carbonate and gypsum lithofacies was followed, in each cycle, by the interstitial growth of anhydrite in exposed conditions. As a whole, the evaporite succession reflects an infilling process. The conversion into anhydrite of the selenitic gypsum -probably also of the rest of depositional gypsum lithofaciesstarted under synsedimentary conditions and followed during shallow to moderate burial diagenesis.

Isotopic characterization of Jurassic evaporites. Aconcagua-Neuquén Basin, Argentina.

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Foreword (2007)

This is the second issue of Geologica Acta dedicated to the memory of Professor Francesc Calvet, who passed away in January 2002. Francesc was a man with great human qualities, a distinguished scientist and an inspiring teacher who was held in high esteem by all those who knew him. The first volume contained six papers on specific areas of research in which Francesc was engaged, and a biography (Geologica Acta, volume 2, Nº 4, 2004). This second volume is made up of contributions by colleagues and former students who wish to salute Francesc Calvet as an outstanding geologist and teacher. The papers included in this volume are also subjects in which Francesc was closely involved.

Fifth-order cyclicity and organic matter contents relationship (Lower Eocene, Pyrenees)

The Upper Limestone Member of the Corones Formation of the Spanish Pyrenees consists of various units (Lower and Upper Foraminifera Units, Shale Unit, Cherty-ostracode Unit, Ostracode Unit and Chara-ostracode Unit) and offers strong facies and lateral thickness (20 to 80 m) variations. Detailed facies analyses, fifth-order cycles and organic geochemical determinations in the central domain of the Corones platform carbonates (Cherty-ostracode Unit), lower Eocene in age, were carried out to establish a case of close relationship between variations in organic matter productivity and cyclicity with annual period. The Cherty-ostracode Unit displays a continuous and pervasive fifth-order cyclicity, represented by 5 cycles. Each cycle consists of a lower part (mollusc facies) and an upper part (laminated ostracode facies). The calculated fifth-order cycle period ranges from about 17,000 to 28,000 years, which falls within the Milankovitch Band. Variations in organic matter content related to these carbonate cycles have been established. The lower mollusc facies members show a low organic carbon content and Hydrogen Index (HI) below 0.6% in weight and 261, respectively. By contrast, the upper laminated ostracode facies members show high organic carbon contents (up to 2% in weight) and high HI (between 164 and 373), and are also characterized by important silicification processes (the content in chert is up to 30%). The organic geochemistry resulting from these organic rich levels reflects a contribution of algal marine input.

El català i els joves: propostes de política lingüística del Consell Social de la Llengua Catalana

Segons els estudis existents, en general, els joves són la franja més capacitada per utilitzar el català en tots els àmbits i contextos, però, en conjunt, són els que menys el fan servir. En l"àmbit metropolità, on resideix la majoria de la població de Catalunya, l"ús del català per part dels joves és encara més baix. Alhora, se sap que l"assoliment de la competència de l"expressió oral en català al final del primer cicle de l"ESo no és pas general, per la qual cosa tot sembla indicar que el model escolar actual no té gaire influència en els usos lingüístics més individualitzats. En el marc d"aquesta situació, el Govern de la Generalitat de Catalunya va encarregar al Consell Social de la Llengua Catalana un informe sobre les possibles mesures a prendre per tal d"intervenir-hi i potenciar més l"ús de la llengua. Les conclusions del Consell assenyalen que caldria actuar preferentment sobre els hàbits d"ús intergrupals i socials a través de la formació sociolingüística dels mestres i professors en general, i tot transformant els centres escolars que ho necessitin per la seva composició demolingüística en institucions molt conscients del seu paper en el desenvolupament eficaç d"una L2 (llengua segona). Igualment, es recomana que les polítiques lingüístiques no ignorin el pla cognitivoemotiu dels individus i que s"acompanyin de discursos legitimadors integradors. Per tal d"augmentar la percepció d"utilitat i funcionalitat del català, és imprescindible aconseguir que es converteixi en la llengua laboral més habitual, fet pel qual la intervenció sobre el món socioeconòmic té la màxima importància. En paral·lel, el Govern ha de procurar incidir en tot l"àmbit ludicomediàtic juvenil, ja que és una generació plenament integrada en aquest univers tecnològic.

El coral·ligen de les illes Medes: una comunitat fràgil amb un gran valor patrimonial

El coral·ligen ha estat definit com una bioconstrucció formada sobretot per algues calcàries de la família de les coral·linàcies, principalment dels gèneres Lithophyllum, Lithothamnion, Mesophyllum,Neogoniolithon, Peyssonnelia i Halimeda, que es desenvolupen entre 20 i 120 m de fondària, on la poca disponibilitat de llum limita el creixement de les algues fotofil·les (Ballesteros, 2006). En aquestescondicions, les espècies d’algues carbonatades passen a ser dominants i, juntament amb diferents espècies d’invertebrats, desenvolupen unes comunitats amb una forta complexitat estructural.Originalment, el coral·ligen es va descriure en el segle XIX a la zona de Marsella (Marion, 1833). El nom, coral·ligen, estava relacionat amb la “producció” de corall vermell Corallium rubrum per part deles bioconstruccions algals. De fet, a la zona de Marsella el corall vermell era un recurs pesquer molt important en aquella època i d’aquí, probablement, que s’emprès el terme. Tanmateix, el terme englobael conjunt de comunitats dominades per diferents algues calcàries i invertebrats que, independentment de la seva composició, estan caracterizades per desenvolupar importants bioconcrecions (fins a 2 m d’alçada) en diferents zones geogràfiques de la Mediterrània.