Faunes ichthyologiques du Néogène Supérieur d’Angola, leur âge, remarques sur le Pliocène marin en Afrique Australe

This note is concerned with fish remains from Upper Neogene beds at Farol das Lagostas (and nearby quarry of SECIL) and Baía Farta, mainly recovered by the author in 1960, 1961, 1963 and 1967. For further data see ANTUNES, 1964, pp. 213-215. All the forms identified until now (many of them for the first time) are show in «tableau I». Smaller ones are poorly represented. I. benedeni is provisorily accepted as a distinct species, though it may correspond to a dental morphotype that does exist equally in the extant I. oxyrhinchus (see text): therefore I. benedeni from Farol das Lagostas may after all represent only some dental variations that really belong in the form described as I. cf. oxyrhinchus. The presence of Aprionodon and Hypoprion could not be ascertained: Procarcharodon megalodon, Carcharodon carcharias, Isurus benedeni. Galeocerdo cuvieri, and Carcharhinus sp. I and sp. II are specially discussed. The whole fauna does not correspond either to a very shallow and coastal environment, or to deep waters far away from the coast. It clearly points out to warm waters: an acceptable model would be the fauna from the tropical Atlantic between Northern Angola and Senegal-Cape Verde. The age of this fauna was long regarded as Burdigalian. The data formerly presented (ANTUNES, 1963) that allowed us to ascribe a pliocene age to the uppermost Neogene beds of Farol das Lagostas (Neogene III, ANTUNES, 1964) are reviewed and developed in this paper. This view is corroborated by planctonic foraminifera and stratigraphical data which provide further evidence to prove the presence of miocene beds much younger than Burdigalian, and that some deposits previously correlated to this stage have instead a Plio-Pleistocene age. Fish fauna from Farol das Lagostas is very characteristic, with giant P. megalodon in association with C. carcharias (which predominates, and whose stratigraphical distribution is particularly discussed), and with other very advanced forms like the extant tiger shark, G. cuvieri, enormous I. Benedeni, Hemipristis, and Carcharhinus (whose size largely exceeds the maximum observed with miocene material). With the exception of P. megalodon (extinct) all the other forms show very close affinities, or even identity with modern species. Comparisons with very similar faunas from some South African localities that may also have a Pliocene age are also presented.

Faunes ichthyologiques du Néogène Supérieur d’Angola, leur âge, remarques sur le Pliocène marin en Afrique Australe

This note is concerned with fish remains from upper Neogene beds at Farol das Lagostas (and nearby quarry of SECIL) and Baía Farta, mainly recovered by the author in 1960, 1961, 1963 and 1967. For further data see ANTUNES, 1964, pp. 213-215. All the forms identified until now (many of them for the first time) are show in «tableau I». Smaller ones are poorly represented. I. benedeni is provisorily accepted as a distinct species, though it may correspond to a dental morphotype that does exist equally in the extant I. oxyrhinchus (see text): therefore I. benedeni from Farol das Lagostas may after all represent only some dental variations that really belong in the form described as I. cf. oxyrhinchus. The presence of Aprionodon and Hypoprion could not be ascertained: Procarcharodon megalodon, Carcharodon carcharias, Isurus benedeni. Galeocerdo cuvieri, and Carcharhinus sp. I and sp. II are specially discussed. The whole fauna does not correspond either to a very shallow and coastal environment, or to deep waters far away from the coast. It clearly points out to warm waters: an acceptable model would be the fauna from the tropical Atlantic between Northern Angola and Senegal-Cape Verde. The age of this fauna was long regarded as Burdigalian. The data formerly presented (ANTUNES, 1963) that allowed us to ascribe a pliocene age to the uppermost Neogene beds of Farol das Lagostas (Neogene III, ANTUNES, 1964) are reviewed and developed in this paper. This view is corroborated by planctonic foraminifera and stratigraphical data which provide further evidence to proove the presence of miocene beds much younger than Burdigalian, and that some deposits previously correlated to this stage have instead a Plio-Pleistocene age. Fish fauna from Farol das Lagostas is very characteristic, with giant P. megalodon in association with C. carcharias (which predominates, and whose stratigraphical distribution is particularly discussed), and with other very advanced forms like the extant tiger shark, G. cuvieri, enormous I. Benedeni, Hemipristis, and Carcharhinus (whose size largely exceeds the maximum observed with miocene material). With the exception of P. megalodon (extinct) all the other forms show very close affinities, or even identity with modern species. Comparisons with very similar faunas from some South African localities that may also have a Pliocene age are also presented.

Caracterização de um mamógrafo Senographe 600T Senix da GE com ânodo de Mo. dosimetria das qualidades de radiação

Dissertação para obtenção do Grau de Mestre em Engenharia Biomédica

Héraldique des sceaux du clergé séculier portugais au Moyen Âge

Ce n’est que dans les dernières années que l’héraldique au Portugal a entamé le processus de rénovation qui, en France, a commencé il y a déjà quelques décennies. Dans ce processus, l’étude de l’héraldique médiévale a été peu contemplé, restant pratiquement à faire, en bonne partir dû à l’absence d’armoriaux antérieurs au XVe siècle qui permettent de connaître les armes utilisées par les familles et les diverses entités portugaises. Pour cette raison, les sceaux portant des représentations héraldiques ont une importance extrême, car ils constituent très fréquemment la seule source pour l’étude des armoiries, ayant en plus l’avantage d’être datés avec précision et liées à des personnages ou entités qui sont connues. Cependant, la sigillographie portugaise se trouve aussi dans une phase de son évolution qui, n’étant plus embryonnaire, est encore une phase de formation. Il nous manque des catalogues, des dépouillages systématiques, des études approfondies qui permettent aux héraldistes de faire leurs recherches. C’est dans ce contexte qui est née ce partenariat entre deux médiévalistes très intéressés à la sigillographie et un spécialiste d’héraldique, qui ensemble ont décidé d’entamer l’étude des origines des représentations héraldiques dans les sceaux portugais, en commençant par les sceaux du clergé séculier, qui constitue le sujet par excellence de la recherche des deux historiens. Dans ce vaste univers sigillaire, qui concerne des personnes d’une grande variété d’origines sociales, y compris la noblesse et la riche bourgeoisie urbaine, les éléments héraldiques semblent avoir émergé seulement à partir de la fin du XIIIe siècle, et d’une façon timide. Le XIVe siècle assiste à sa diffusion dans les sceaux d’évêques, dignités et chanoines, mais ce n’est qu’au XVe siècle que l’héraldique s’impose, gagnant même une place primordiale dans quelques représentations sigillographiques. Le but de cette communication sera donc l’analyse du processus d’héraldisation des sceaux du clergé séculier portugais, entre les dernières décennies du XIIIe et le XVe siècle, pour évaluer comme s’est procédé, dans le cas portugais, le phénomène d’«acculturation héraldique» de l’emblématique épiscopale et cléricale.

Petites villes européenes au bas Moyen Âge: perspectives de recherche

Fundação para a Ciência e Tecnologia,

BÉRIOU, Nicole, JOSSERAND, Philippe (coord.), Prier et Combattre – Dictionnaire européen des ordres militaires au Moyen Âge, Fayard, 2009

Medievalista [Em linha]. Nº10, (Julho 2011). Direc. José Mattoso. Lisboa: IEM.