Mapeamento da Responsabilidade Social em Portugal (The Mapping of Social Responsibility in Portugal)

Conferência multidisciplinar e multicultural.

Tchekov em Portugal, um caminho

Este artigo analisa a presença da dramaturgia de Anton Tchekov no teatro em Portugal (de 1936 a 2005).

Samuel Beckett em Portugal: imagens roubadas ao tempo: 1959-2006

Este artigo analisa a presença da dramaturgia de Samuel Beckett no teatro em Portugal (de 1959 a 2006).

Contributo para o estudo do tempo de espera para radioterapia em Portugal : adaptação de um instrumento de recolha de dados

RESUMO - É reconhecido o impacto negativo e prejudicial que o tempo de espera tem para radioterapia sobre o controlo tumoral e a taxa de sobrevida, bem como a importância de estabelecer tempos máximos para o início do tratamento, de forma a garantir o cumprimento de uma boa prática. O presente projecto de investigação tem o objectivo de construir e validar uma grelha de observação, como instrumento de recolha de dados, que se pretende no futuro aplicar, de forma a poder contribuir para o estudo sobre o tempo de espera para radioterapia em Portugal. Para alcançar o objectivo proposto, optou-se pela metodologia usada por Drinkwater e Williams na re-auditoria efectuada no Reino Unido pelo Royal College of Radiologists, em 2007, sobre os tempos de espera para radioterapia. A grelha de observação elaborada foi baseada na grelha utilizada por Drinkwater e Williams, na revisão da literatura, e tendo em consideração a realidade portuguesa. Após a análise das respostas dos peritos, ao questionário de avaliação e adequação do instrumento à realidade portuguesa, parece existir concordância na adequação do instrumento, o que nos permite afirmar a possibilidade da aplicação do mesmo nos centros de radioterapia de Portugal. --- --------------------------------ABSTRACT - It is recognized the negative impact that radiotherapy waiting time have in tumour control and survival, as well the importance of establish maximum waiting times for the start of the treatment, in the sense to guarantee a good practice. The present investigation project aim is to build and validates a data collection tool, which pretends to apply in the future, in the sense to contribute for the study of the radiotherapy waiting time in Portugal. To accomplish the project aim, we chose the method used by Drinkwater and Williams in the re-audit performed in United Kingdom for the Royal College of Radiologists, in 2007, about the radiotherapy waiting time. The data collection tool built was based on the data collection tool used by Drinkwater and Williams, on the literature review and taking in account the Portuguese reality. After the analyse of the experts answers, it seems to exist agreement about the adequacy of the data collection tool, which allow us to claim the possibility of the tool application at radiotherapy centres, in Portugal.

Le Crétacé terminal de Beira Litoral, Portugal: remarques stratigraphiques et écologiques, étude complémentaire de Rosasia soutoi (Cbelonii, Bothremydidae)

The synthetic study of the uppermost Cretaceous of the Beira Litoral (fauna, floral confirms its upper Campanian-Maastrichtian age. It shows the presence of a tropical to subtropical climate in an area constituted by a low coastal plain only occasionally linked to the sea, saturared with fresh water and possessing accordingly, a predominantely freshwater fauna (Viso, Aveiro); this plain changed towards the interior into a drier more forested zone with a more abundant terrestrial fauna which includes mammals (Taveiro). A thorough study of the chelonian Rosasia, abundant on the coastal plain, was made possible thanks to the discovery of a skull: it demonstrates that the genus belongs to the family Bothremydidae, revalided here. The composition of this family is presented, its phylogenetic and paleobiogeographic relation with the other pleurodires are analyzed, and its diagnosis established. The family is constituted of three groups; Rosasia belongs to one of rhese, the Bothremys group.

Castor fiber na gruta do Caldeirão Existência, distribuição e extinção do castor em Portugal

Beaver only had been found in Portugal in a Chalcolithic locality, the Vila Nova de S. Pedro castrum. It has now been idenrified in the Upper Paleolithic (Solurrean) from Gruta do Caldeirão, near Tomar. The species has been found recently at «Gruta do Almonda»; 4 teeth were collected in bed C, older than a Solutrean sequence (see Anexo for details). The species seems to have been rare, as it was also the case with portuguese miocene Castoridae Enroxenomys minutus and Chalicomys jaegeri. If account is taken of the presence in the Middle Ages until Castille of words meaning beaver (related to the popular latin Fiber/Biber), it is obvious that these animals still existed then. Such nouns were largely predominant over the rather erudite larin (greek derived) words as Castor, -óris and derived ones, as it could be expected. This allowed us to recognize that veiro should be the corresponding word with Fiber affinities in archaic portuguese. It was previously supposed to mean only expensive furs then imported into Portugal. Indeed it was also a zoonym. Anyway, beaver should be scarce by XIIIth century since it is not included in the quite detailed price list imposed by the «Lei da Almotaçaria» from December 26, 1253 (see Quadro II). Toponyms in veiro and derived words (fig. 2; Quadro III) (plural, feminines, diminutives, inhabited places) give a restrictive view of the Middle Age distribution. Some of them are certainly older than Portugal itself (first half of XIIth century); others existed by the XIVth century but were probably older. Some rare toponyms seem to be derived from rhe erudite latin Castor, -óris. Nothing suggests that these words were still in use as zoonyms during the Middle Ages. All toponyms are located in regions near rivers and other freshwaters ecologically suitable for beavers, so wecan approximately retrace irs former, Middle Age distribution in Portugal (fig. 2; Quadro III). Most of them are located in the Center-West and Northwest of Portugal, with a suitable c1imate (rainfall in general over 800 milimeters per year); the only sure geographical exception is Veiros, in Alto Alentejo province, in a region with comparable precipitations and less dry climare conditions than most of the territories South of the Tagus. There are less and less of these toponyms towards the South and the inner part of the country, and they are enrirely lacking in ali drier regions from Trás-os-Montes, Beira, Alentejo beyond Tagus' basin, and in Algarve. Nothing suggests beavers lived there, No pose-medieval toponym is known, nor any reference after middle XVth century. No such locality was at, or close by to, any frontier. Hence the hypothesis of veiro (e: al.) as meaning but points where expensive furs(supposedly known as veiros in general but without clearly saying from what animal they were obtained from) is to be discarded. During the Middle Ages, beaver distribution concerned all the main river basins from Minho to Tagus ones. Quice racefied in the XIIIth, the beavers may have disappeared from Portugal during the XVth century. Ecological requirements restricted their former distribution. Vulnerability to natural causes (i.e., severe drought) and to human pressure may have accounted heavily for this species extinction. Last (1446) reference for Portugal known to us suggests the species was by then almost extinct.

Palinomorfos ante-cenomanianos do «Grés do Buçaco» (Lousã, Portugal) *

The palynological study of sediments from lower levels of Lousã basin (Lomba do Alveite Arkoses). is presented. The palynological association includes several species of Appendicisporites and Cicatricosisporites, Costatoperforosporites sp., Ischyosporites teixeirae, Pattelasporites tavaredensis, Echinatisporis sp., Spheripollenites perinatus, Tricolpopollenites sp. and Retitricolpites maximus. The presence of the last two forms, and the absence of Normapolles, suggest an ante-Cenomanian, most probably Albian age for the assemblage. From these results, the begining of the infilling of the Lousã basin, is, at least in part, synchronous with the deposition of the «Grés Grosseiro Inferior» from the Occidental portuguese Basin. The presence of Lower Cretaceous sediments directly overlying the Paleozoic basement, hence outside of the Occidental Portuguese Basin,is shown for the first time.

Rupicapra rupicapra (Mammalia) In the Late Pleistocene of Portugal

The presence of the genus Rupicapra in Portugal is shown for the first time, on some dental and skeletal remains from the upper Pleistocene (Solutrean) of Salemas cave. The fossil material may be ascribed to R. rupicapra pyrenaica.