Sobre la publicació "Los Fenicios en Cataluña".

En aquesta important comunicació al Simposi de Jerez de la Frontera que ell mateix havia organitzat, el Dr. Maluquer assenyalava amb proves arqueologiques la presencia del comer~ fenici a Catalunya. De fet, era la primera vegada que es parlava de la presencia fenícia a Catalunya amb dades concretes, i d'aquí la importancia cabdal d'aquesta comunicació per a la historia de la recerca arqueologica. Cal tenir en compte que la presencia fenícia a les costes catalanes és silenciada per les fonts escrites, contrariament al que succeeix amb la presencia rOdia o focea posem per cas, de manera que es pot dir que la descoberta de l'element fenici va ser una descoberta exclusivament arqueologica, i que va causar la natural sorpresa al Dr. Maluquer, el seu descobridor.

Grau Mira, Ignacio: La organización del territorio en el área central de la 'Contestania' Ibérica, Anejo de la revista Lucentum, 12, Publicaciones de la Universidad de Alicante, Alacant, 2002

Els estudis sobre territoris iberics -no sobre arees territorials més o menys coherents, com l'estudi classic de Llobregat (1972) sobre la Contestania o el de Lillo (1981) sobre l'area murciana, que són una altra COsa- compten ja amb una tradició relativament llarga, des deis primers treballs de F. Burillo (1982) sobre la val! mitjana de l'Ebre i els d' A. Ruiz i M. Molinos (1984) al' Alt Guadalquivir, posteriorment els de J. Bernabeu, H. Bonet, P. Guerin i C. Mata a l'Edetania (en particular, Bonet, 1995) i els que diferents autors han realitzat a les arees costaneres de Catalunya (Martín i Plana, 2001). El trebal! d'Ignacio Grau Mira s'insereix plenament dins d'aquesta tradició i, com és lógic, se'n beneficia en gran mesura.

Reply to Pierre Moret

I would like to thank Pierre Moret for his praises -which I certainly do not deserve- as well as for his valuable comments and criticisms. An intellectual discussion with such a prominent scholar is a satisfying experience, even if I do not wholly agree with his opinions. His reactions are related to three different topics: the definition of the geographical area covered in my article; the role of population increase in social evolution and the role of migrations.

En torno al paralelo de una placa-fíbula

La invención de la fíbula se ongmo sin duda por la necesidad de poseer un útil capaz de lograr entera seguridad en el abrochado de los vestidos. Una vez creada la fíbula no podía quedar relegada al simple papel de un objeto útil, su misma posición en lugares visibles y bien destacables del vestido, sobre todo en el femenino, hizo que el artesano desde un primer momento pensase en conferirle mayor belleza. Ambas funciones de útil y adorno se cumplen a la perfección en un ejemplar que, procedente de la necrópolis de Mas de Mussols, en La Palma, Tortosa, tuve ya ocasión de dar a conocer en mi anterior trabajo sobre las fíbulas en Cataluña. Se trata de una placa circular de bronce a cuyo reverso hay inserta una fibulita. De las tres placas halladas en la necrópolis la más representativa es una que pertenece a la colección municipal de Amposta.

Inclusió i segregació a l'escola: pràctiques inclusives i excloents amb l'alumnat vulnerable

El present article aborda l'anàlisi dels components inclusius dels centres educatius que es plantegen una educació de qualitat per a tot l'alumnat, posant especial atenció en l'alumnat de grups socialment vulnerables. Es basa en les dades qualitatives d¿una part del projecte integrat INCLUD-ED, que estudià 20 casos de centres educatius d'èxit en diferents països de la Unió Europea. Tots els centres atenien alumnat de baix nivell socioeconòmic i havien demostrat tenir més èxit escolar que el conjunt de centres situats en contextos similars. L'article revisa altres investigacions afins i exposa els resultats agrupats en quatre tòpics: l'agrupament de l'alumnat; les expectatives; el suport; i la participació de les famílies i la comunitat. Les conclusions se sotmeten a discussió.

Consumption of macrophytes by invertebrates in Tancada lagoon (NE Spain)

Gammarus aequicauda and Sphaeroma hookeri are the most abundant macroinvertebrates on Ruppia cirrhosa (1275 and 1290 individuals.m-2) and Potamogeton pectinatus (140 and 680 individuals. m-2) in Tancada lagoon, a Mediterranean coastal lagoon in the Ebro Delta (NE Spain). Consumption and assimilation efficiencies were calculated from bell jar experiments. Gammarus grazing effects are higher than Sphaeroma on both Ruppia cirrhosa and Potamogeton pectinatus. Green Ruppia leaves lost 0.3 mg per mg Gammarus per day, while Potamogeton leaves lost 0.2 mg per mg Gammarus per day. Decomposing Ruppia leaves lost 0.35-0.54 mg per mg Gammarus per day. Losses of weight by both Ruppia and Potamogeton due to Sphaeroma feeding were less than half those by Gammarus. Assimilation efficiencies are higher for Gammarus (44-78% feeding on Ruppia 2% feeding on Potamogeton) than for Sphaeroma (26-48%) feeding on Ruppia). These assimilation efficiencies were higher than those reported by other authors working at higher latitudes perhaps because of the higher temperature under which the experiments were carried out.

Seasonal patterns op biomass variation of Ruppia cirrhosa (Petagna) Grande and Potamageton pectinatus L. in a coastal logoon

Coastal lagoons where salinity varies within a wide range during the year are colonized by euryhaline macrophytes which can develop extensive beds. Seasonal changes in biomass of Ruppia cirrhosa and Potamogeton pectinatus were studied in Tancada Lagoon (Ebro Delta, NE Spain) in order to reveal the environmental factors controlling their population development. Ruppia cirrhosa occupy a larger area of the lagoon than Potarnogeton pectinatus. Their maximum above ground biomasses are also different (495 g m-2 and 351 g m-2 ash free dry weight, respectively). Below ground biomass of Ruppia cirrhosa is between 9 and 53 % of the above ground biomass, while it is 3-40 % for Potamogeton pectinatus. Chlorophyll a contents show fluctuations similar to biomass. Low salinity and high turbidity caused by freshwater inflows favour Potamogeton expansion, while Ruppia development is favoured by high salinity and transparent water.

Decomposition of Ruppia cirrhosa (Petagna) Grande in the sediment of a coastal lagoon

The decomposition process of Ruppia cirrhosa was studied in a Mediterranean coastal lagoon in the Delta of the River Ebro (NE Spain). Leaves and shoots of Ruppia were enclosed in 1 mm-mesh and 100 pm-mesh litter bags to ascertain the effect of detritivores, macroinvertebrates, and bacteria and fungi, respectively. Changes in biomass and carbon, and, nitrogen and phosphorus concentrations in the detritus were studied at the sediment-water interface and in the sediment. Significant differences in biomass decay were observed between the two bag types. Significant differences in decomposition were observed between the two experimental conditions studied using 100 pm-mesh bags. These differences were not significant when using the 1 mm-mesh bags. The carbon content in the detritus remained constant during the decomposition process. The percentage of nitrogen increased progressively from an initial 2.4 % to 3 %. The percentage of phosphorus decreased rapidly during the first two days of decomposition from an initial 0.26 % to 0.17 %. This loss is greater in the sediment than in the water column or at the sediment-water interface. From these results we deduce that the activity of microorganisms seems to be more important in the sediment than in the water-sediment interface, and that grazing by macroinvertebrates has less importance in the sediment than in the water column.

Sedimen-water nutrient fluxes: Preliminary results of in situ measurements in Alfaques Bay, Ebro River Delta.

Sediment-water exchanges of oxygen, ammonium, nitrate, total dissolved nitrogen, phosphate and total dissolved phosphorus were measured by means of an in situ incubator of 7 1 volume and 700 cm2 base area. The incubations lasted for three hours and were done over a whole season on different kinds of sediments in Alfaques Bay. We present some preliminary results on: i) methodological aspects, ii) spatial and temporal variability of fluxes, and iii) estimates of contribution of benthic nutrient regeneration relative to total nutrient loading of the Bay. Oxygen uptake averaged 1700 mmo1 m-2 h-1 (range 200-3500); no differences were found between sandy and muddy sediments. The release of ammonia from the sediment averaged 70 mmo1 m-2 h-1 and was higher in muddy sediments than in sandy ones. Very low to null nitrate and nitrite fluxes and only small fluxes of organic nitrogen were detected. We conclude that ammonium release from sediment is the major path of nitrogen regeneration. Some sediments removed dissolved reactive phosphorus (DRP) from the water and released dissolved organic phosphorus (DOP). Additional manipulative experiments revealed DRP release under particular conditions (turbulence, anoxia). From these data, we estimate that at least 50% of the nitrogen requirements of phytoplankton in the area may be supplied by benthic remineralization.

Aportacions a la Flora de les comarques transiberiques, II.

Presentem un recull de novetats corològiques i taxonòmiques per a les comarques catalanes situades al sud de l'Ebre. Es descriuen dos tàxons nous: Brassica repanda (Willd.) DC. subsp. dertosensis Molero i Rovira i Helianthemum pilosum (L.) Pers. var. pseudoasperum Molero i Rovira. S'estableix una nova combinació nomenclatural: Reseda lutea L. subsp. vivantii (P. Montserrat) A. Rovira. En l'aspecte corologie, Euphorbia lagascae Sprengel representa una novetat per a Catalunya. La majoria de les altres citacions representen novetats pel conjunt d'aquestes comarques catalanes meridio-occidentals.

Stellario pallidae-Chenopodietum exsuccii Molero et Blanche, nueva asociacion de la comarca de los Monegros (Valle del Ebro).

Los montes de la Retuerta de Pina, situados en el corazón de los Monegros, entre Pina y Bujaraloz, constituyen una suave elevación que se alza ligeramente (417 m s.m. en Purburell) sobre la plataforma de Bujaraloz (300 m de altitud media). Información sobre los suelos, clima general y vegetación de este enclave puede encontrarse en los trabajos especializados de BRAUN BLANQUET & O. BOLOS (Anales Est. Exp. Aula Dei 5. 1957) y TERRADAS (Orsis 2: 71-95.1986). En las estribaciones septentrionales más abruptas de estos montes, se abren una serie de valles de dirección SE-NW, algunos con desniveles relativamente pronunciados (30-50 m) entre las crestas y los fondos. La maquia arbolada del Rhamno-Quercetum cocciferae subas, thuriferetosum está, en las vertientes de umbría, magníficamente representada. Su relativa frondosidad, así como el tamaño y buena conservación de los árboles /. thuriferay P. halepensis, atestiguan la escasa manipulación humana.

De Vegetatio notulae, II

161 . Arenarietum viridis. Los inventarios fueron efectuados en la Cova deis Angels, del valle de la Fou (término de la Sénia), en los Ports de Tortosa, a unos 550 m. de altitud.

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).

L'avançament de la introducció d'una llengua estrangera: un fugida cap enrera?

The age at which school children begin instruction in the foreign language has been brought forward on two main grounds: (1) young children are better language learners than older children, and (2) bilingualism brings cognitive advantages to children. Both statements are critically analysed in this paper. First of all, recent research findings show that the advantage that younger learners show in a naturalistic language learning situation (or through school immersion) disappears in a formal language learning situation with very limited exposure to the target language. Secondly, the positive effects on cognitive development that have been revealed through research correspond to situations of balanced bilingualism, that is, situations in which children have a high command of the two languages. In contrast, children¿s command of the foreign language in our context is very limited and hence far from the situation of balanced bilingualism (or trilingualism) that is said to bring positive cognitive effects.

La dimensión afectiva de la competencia comunicativa intercultural en la Educación Secundaria Obligatoria: escala de sensibilidad intercultural

Dialogar de forma enriquecedora, apreciando las diferencias culturales, supone disponer de cierta competencia comunicativa intercultural que tiene una especial importancia en la educación secundaria obligatoria. Para ello, proponemos evaluar las necesidades del alumnado en este periodo educativo a través de la escala de sensibilidad intercultural. Esta escala ha sido adaptada tanto a nivel lingüístico cultural, como también de nivel madurativo. Los resultados obtenidos en este diagnóstico de la comarca del Baix Llobregat, ponen de manifiesto la necesidad de desarrollar competencias de tipo afectivo en esta etapa educativa. Diversas diferencias estadísticamente significativas también nos indican la relevancia de desarrollar estas competencias en la totalidad del alumnado adolescente.