Aportaciones al conocimiento taxonomico de Verbascum blattaria L. y V. virgatum Stok.

Se estudia la variabilidad de los caracteres utilizados tradicionalmente en la taxonomía de los afínes Verbascum blattaria L. y V. virgatum Stokes, sobre la base de materiales procedentes de la Península Ibérica. El estudio comparado de ambas entidades ha comportado la creación de un nuevo taxon: V. virgatum Stokes subsp. dertosense Benedí and Rovira, restringido por ahora a las montañas tarraconenses de los Ports de Beseit (Horta de Sant Joan, Tarragona).

Noves aportacions sobre agricultura i alimentació durant la primera edat del ferro a Catalunya: dades de l'assentament de Sant Jaume/Mas d'en Serrà (Alcanar, Montsià)

Els resultats de l'estudi arqueobotànic realitzat sobre diferents àmbits de l'assentament de Sant Jaume aporta noves dades al coneixement de la gestió dels recursos vegetals de la protohistòria del nordest peninsular. El registre arqueològic constata una certa homogeneïtzació en la funcionalitat dels àmbits, que s'interpreten com a magatzems en el pis superior i espais d'estabulació a l'inferior. L'àmbit millor representat és l'A4, que conserva com a fet singular un elevat nombre de restes de llavors i fruits amb molt bon estat de conservació. Els tàxons conreats més importants són la pisana (Triticum dicoccum) i les guixes i guixols (Lathyrus sativus i Lathyrus cicera), seguits d¿una menor proporció d'ordi vestit (Hordeum vulgare), blat nu (comú/dur) (Triticum aestivum/durum), pèsol (Pisum sativum), llentia (Lens culinaris) i erb (Vicia ervilia). D'altra banda, el registre arqueobotànic del pis inferior de l'àmbit A4 sembla posar en evidència la presència de l¿associació de pisana i guixa, destinada a l'alim.

Archaeological and archaeomagnetic dating at a site from the ager Tarraconensis (Tarragona, Spain): El Vila-sec Roman pottery

A very accurate archaeological dating of a Roman site in NE Spain (El Vila-sec) was made based on the typology of pottery artifacts. Three different phases were identifi ed with activity ranging from the mid- 1st century BC to the early-3rd century AD. Analyses of bricks from kilns at El Vila-sec produced data on their stored archaeomagnetic vector. These data were compared with the secular variation curve for the Iberian Peninsula and the SCHA.DIF.3K regional archaeomagnetic model. Both, the reference curve and the model, produced probability distributions for the final period of use for two kilns from the second archaeological phase that were not used during the third phase. At a 95% con fidence level, both time distributions cover a wide chronological range including the presumed archaeological age. Both the Iberian secular variation curve and the SCHA.DIF.3K regional model proved to be suitable models for dating the site, although on their own they do not produce a single unambiguous solution. This archaeomagnetic approach could also be applied to neighbouring archaeological sites that have an imprecise archaeological age.

Feeding of nauplii, copepodites and adults of Calanipeda aquaedulcis (Calanoida) in Mediterranean salt marshes

Feeding of the different developmental stages of Calanipeda aquaedulcis on natural particles (bacterio-, phyto- and microzooplankton) was measured in a Mediterranean salt marsh (Empordà wetlands, NE Iberian Peninsula). Bottle incubations were performed in the field both in autumn and spring. The results showed differences in the diet of the different developmental stages due to both prey type and size. In general, the size of the ingested prey increased with increasing size of the C. aquaedulcis stage. While C. aquaedulcis adults had high ingestion rates and selection coefficients for large prey (micro- and nanoplankton), nauplii preferentially consumed smaller prey items (picoplankton). Copepodites showed the widest prey size range, including pico-, nano- and microplankton. Nevertheless, the lower size limit for particle capture was similar for all stages, i.e. between 1.7 and 2.1 μm. Omnivory was observed in all stages of C. aquaedulcis. Heterotrophic prey (picoplankton, dinoflagellates and ciliates) were the most ingested items. The ability to partition the available food among the different developmental stages could represent an advantage in times of ood scarcity because it may reduce intraspecific competition. This may explain how C. aquaedulcis is able to predominate in the zooplankton community for several weeks during spring and summer ven in situations of low food availability

Un clàssic del feminisme en català: La condició de la dona de Juliet Mitchell

Aquest article estudia la recepció a Catalunya d’una de les fundadores del pensament feminista contemporani: Juliet Mitchell. Les contribucions d’aquesta autora van ser fonamentals per a establir els límits de la relació entre el feminisme, el socialisme i la psicoanàlisi als anys setanta. Un dels seus llibres més importants, Woman’s State, es va publicar l’any 1971. En disposem d’una traducció catalana realitzada per Josep Vallverdú, sis anys després: La condició de la dona; el mateix any es va publicar La condición de la mujer, amb traducció de Julieta Diéguez Garza (es tracta d’una reedició per a la península d’una primera edició realitzada a Mèxic l’any 1974). En aquest estudi s’analitza la traducció catalana i es reflexiona sobre la seva importància en un context en què calia abastir de clàssics l’incipient teixit associatiu feminista.

La migració primaveral d'ocells als Aiguamolls de l'Empordà (Girona): primer anellament de Becadell Gros (Gallinago Media) a la Península Ibèrica

En aquest treball s'exposen els resultats obtinguts en la campanya 1994 d'anellament d'ocells inclosa dins del projecte italià Piccole Isole. Es demostra que el factor meteorològic afecta directament la fenologia migratòria de diferents espècies d'ocells. Es pretén també estudiar la influència dels diferents hàbitats en el nombre i en la diversitat de captures. Es recullen també en aquest treball les principals espècies visualitzades durant la campanya, com també l'elevat nombre de controls estrangers recuperats. Dintre de les captures i l'anellament posterior, destaca sobretot la d'un becadell gros (Gallinago media) fets per primera vegada a la peninsula Ibèrica

Scale effect in hazard assessment - application to daily rainfall

Daily precipitation is recorded as the total amount of water collected by a rain-gauge in 24h. Events are modelled as a Poisson process and the 24h precipitation by a Generalized Pareto Distribution (GPD) of excesses. Hazard assessment is complete when estimates of the Poisson rate and the distribution parameters, together with a measure of their uncertainty, are obtained. The shape parameter of the GPD determines the support of the variable: Weibull domain of attraction (DA) corresponds to finite support variables, as should be for natural phenomena. However, Fréchet DA has been reported for daily precipitation, which implies an infinite support and a heavy-tailed distribution. We use the fact that a log-scale is better suited to the type of variable analyzed to overcome this inconsistency, thus showing that using the appropriate natural scale can be extremely important for proper hazard assessment. The approach is illustrated with precipitation data from the Eastern coast of the Iberian Peninsula affected by severe convective precipitation. The estimation is carried out by using Bayesian techniques

The effect of scale in daily precipitation hazard assessment

Daily precipitation is recorded as the total amount of water collected by a rain-gauge in 24 h. Events are modelled as a Poisson process and the 24 h precipitation by a Generalised Pareto Distribution (GPD) of excesses. Hazard assessment is complete when estimates of the Poisson rate and the distribution parameters, together with a measure of their uncertainty, are obtained. The shape parameter of the GPD determines the support of the variable: Weibull domain of attraction (DA) corresponds to finite support variables as should be for natural phenomena. However, Fréchet DA has been reported for daily precipitation, which implies an infinite support and a heavy-tailed distribution. Bayesian techniques are used to estimate the parameters. The approach is illustrated with precipitation data from the Eastern coast of the Iberian Peninsula affected by severe convective precipitation. The estimated GPD is mainly in the Fréchet DA, something incompatible with the common sense assumption of that precipitation is a bounded phenomenon. The bounded character of precipitation is then taken as a priori hypothesis. Consistency of this hypothesis with the data is checked in two cases: using the raw-data (in mm) and using log-transformed data. As expected, a Bayesian model checking clearly rejects the model in the raw-data case. However, log-transformed data seem to be consistent with the model. This fact may be due to the adequacy of the log-scale to represent positive measurements for which differences are better relative than absolute

Rapid and sudden advection of warm and dry air in the Mediterranean Basin

Rapid advection of extremely warm and dry air is studied during two events in the Mediterranean Basin. On 27 August 2010 a rapid advection of extremely warm and dry air affected the northeast Iberian Peninsula during a few hours. At the Barcelona city center, the temperature reached 39.3 ° C, which is the maximum temperature value recorded during 230 yr of daily data series. On 23 March 2008 a rapid increase of temperature and drop of relative humidity were recorded for a few hours in Heraklion (Crete). During the morning on that day, the recorded temperature reached 34 °C for several hours on the northern coastline of this island.According to the World Meteorological Organization none of these events can be classified as a heat wave, which requires at least two days of abnormally high temperatures; neither are they a heat burst as defined by the American Meteorological Society, where abnormal temperatures take place during a few minutes. For this reason, we suggest naming this type of event flash heat. By using data from automatic weather stations in the Barcelona and Heraklion area and WRF mesoscale numerical simulations, these events are analyzed. Additionally, the primary risks and possible impacts on several fields are presented.

Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.

Deep incision in an Aptian carbonate succession indicates major sea-level fall in the Cretaceous

Long-term relative sea-level cycles (0 5 to 6 Myr) have yet to be fully understood for the Cretaceous. During the Aptian, in the northern Maestrat Basin (Eastern Iberian Peninsula), fault-controlled subsidence created depositional space, but eustasy governed changes in depositional trends. Relative sea-level history was reconstructed by sequence stratigraphic analysis. Two forced regressive stages of relative sea-level were recognized within three depositional sequences. The first stage is late Early Aptian age (intra Dufrenoyia furcata Zone) and is characterized by foreshore to upper shoreface sedimentary wedges, which occur detached from a highstand carbonate platform, and were deposited above basin marls. The amplitude of relative sea-level drop was in the order of tens of metres, with a duration of <1 Myr. The second stage of relative sea-level fall occurred within the Late Aptian and is recorded by an incised valley that, when restored to its pre-contractional attitude, was >2 km wide and cut 115 m down into the underlying Aptian succession. With the subsequent transgression, the incision was back-filled with peritidal to shallow subtidal deposits. The changes in depositional trends, lithofacies evolution and geometric relation of the stratigraphic units characterized are similar to those observed in coeval rocks within the Maestrat Basin, as well as in other correlative basins elsewhere. The pace and magnitude of the two relative sea-level drops identified fall within the glacio-eustatic domain. In the Maestrat Basin, terrestrial palynological studies provide evidence that the late Early and Late Aptian climate was cooler than the earliest part of the Early Aptian and the Albian Stage, which were characterized by warmer environmental conditions. The outcrops documented here are significant because they preserve the results of Aptian long-term sea-level trends that are often only recognizable on larger scales (i.e. seismic) such as for the Arabian Plate.

Forma Conventus Tarraconenesis I: Baetulo-Blanda. La primera carta arqueològica de la Península Ibèrica

Josep de Calasanç Serra i Ràfols va dedicar una part molt important de la seva vida professional a la topografia arqueològica, als arxius del Servei d’Investigacions Arqueològiques de l’Institut d’Estudis Catalans i a fer el seguiment de la descoberta i l’evolució dels jaciments arqueològics del país. En consonància amb aquesta labor, el 1928 va publicar la primera carta arqueològica de la península Ibèrica, una de les primeres corresponents al programa Forma Orbis Romani, de la Unió Acadèmica Internacional. Després de la Guerra Civil, proposem que fou el principal redactor de la Carta Arqueológica de España. Barcelona, que representa la tercera carta arqueològica publicada a la península Ibèrica.

La integración de Tarrakuna y su territorio en al-Andalus (s. VIII)

A inicios del siglo VIII, el antiguo regnum gothorum se vio fragmentado en diferentes territorios políticos, como muestra la simultaneidad de dos reyes (Rodrigo y Akhila) entre 710-711. Con la conquista islámica de la Península Ibérica y la formación de al-Andalus, las diversas regiones conocieron distintos destinos: algunas aristocracias pactaron con los conquistadores, otras se vieron sometidas por la fuerza. Pero la tradición historiográfica ha visto en la ciudad de Tarragona una excepción, un caso aislado. El objetivo de este artículo es plantear una nueva hipótesis, según la cual, durante todo el siglo VIII, madinat Tarrakuna formó parte del Estado andalusí de la misma forma que otras antiguas sedes episcopales visigodas.

Noves aportacions al coneixement florístic de l'Empordà - III

New records of some vascular plants in the Empordà (NE of Iberian Peninsula) are given. Some of them are new for this area. We make several annotations about chorology of these taxa. Coronilla repanda (Poir.) Guss. subsp. dura (Cav.) Cout. and Ranunculus nodiflorus L. are indicated for the first time in Catalonia

Hispania en las provincias occidentales del imperio durante la república y el alto imperio: una perspectiva arqueológica

El siguiente trabajo repasa los procesos y acontecimientos clave de la incidencia de Roma en la península Ibérica –en las denominadas «provincias hispanas»–, con especial atención al espacio comprendido entre el desembarco de Escipión en Emporion (218 a.C.) y el reinado de Adriano, por tanto, durante la República y el Alto Imperio. A partir de la documentación arqueológica y, en ocasiones, epigráfica, se esboza un panorama de la romanización peninsular partiendo de los acontecimientos más representativos de la misma y de sus huellas más evidentes. De igual modo, la bibliografía ofrecida pretende aportar la luz de las últimas novedades sobre la cuestión.