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.

Le gisement pleistocène de Morgadinho, en Algarve

Small mammals from a water well near Morgadinho indicate an age comprised between Middle Villafranchian, MN 17 zone and lowermost Middle Pleistocene, MN 20. This fauna corresponds to an humid region under a possibly temperate (certainly not cool) climate. Nearly all Gastropoda have quaternary affinities. Most are freshwater dwellers. Ostracoda lived in lacustrine or extensive swamp enviromnents rich in plants. They also point out to fresh waters (eventually oligohaline; this may suggest some kind of communication with the sea, which would not be very close by), and to water temperatures over 10.5°C. Charophyta thrive in fresh, carbonate-rich waters. Cyprinid fishes are also freshwater dwellers, and amphibians exclude any significant salinity. Palynological analysis shows climate should be warm and rather humid. Near Morgadinho there was a mixte mesophytic forest (and perhaps a sempervirent, large leave type forest at Algoz). Morgadinho and Algoz (this locality being dated MN 20, lowermost Middle Pleistocene) are probably correlative, and this may also be true for lacustrine limestones at Ponte das Lavadeiras, near Faro.

Goldra: premier gisement karstique en Algarve, faune et industries

A bone breccia from Goldra, near Loulé, is studied. It corresponds to the infilling of a karst depression, consisting of: rather worn and probably transported dolomite pebbles at the bottom; accumulations of frequently burnt bone scraps, much broken and with acute edges (no transport), certainly debris of human food, suggesting habitat level (s); in association with the former, stone (flint, quartz, quartzite, graywacke) rather uncharacteristic artifacts that seem compatible with middle and upper Paleolithic, or with Epipaleolithic; and small mammal teeth and bones. Fauna includes an extinct species, Microtus brecciensis recognized for the first time in Portugal. It is not older than Riss-Wiirm interglacial, and may be of this age or later, maybe that of one of wurm's first interstades. Fauna points out to a varied landscape with open country and woods; and to a rather warm and dry temperate, or dry subtropical mediterranean climate. Climate differences should not be significant in comparison with the extant situation. The presence of the mammal species found so far is consistent with modern distribution.

Mammifères pleistocènes de Algoz, en Algarve: une revision

At Algoz, Algarve, some mammals were found. The fauna, as revised here, corresponds to lowermost Middle Pleistocene (Biharian), just before the first glacial advance of Gunz glaciation. It is much older than it was previously regarded (Riss-Wurm interglacial). Evidence indicates an humid, swampy, riparian environment rich in plant life, and a nearby forest. Climate seems to have been rather warm (see ANTUNES et al., 1985). Age and ecology suggest that Algoz and Morgadinho, also in Algarve, are correlative (Morgadinho's age is from Villanyian to Biharian, and is thus compatible with that from Algoz). Lithology and palynological analysis corroborate this view. Algoz is the first locality of this age known in Portugal. Morgadinho and perhaps lacustrine limestones at Ponte das Lavadeiras (Faro) are more or less the same age.

Conocimientos acerca de plantas en la nueva ruralidad. Cambio social e agro ecología en en Parque Natural de Montesinho (Portugal)

Perifèria. Revista de recerca i formació en antropologia, N.10

L'émigration en tant que processus de déplacement et de recomposition de l'habitat

Sociedade e Território - Enjeux sociaux et transformations du territoire, Nº Especial, Lisboa, p. 53-56

Société rurale, société urbaine: espaces en interaction

La sociologie et les nouveaux défis de la modernisation, Porto, pp. 315-326

Difficultés d'adaptation de questionaire sur les transmissions entre famille et écoles en contextes linguistiques et culturels différents

Les résultats des études PISA – aussi bien en ce qui concerne celle de 2000 comme celle de 2003 - n’ont guêre été satisfaisants pour de nombreux pays de l’OCDE (ce n’est pas le cas pour la Belgique!). Par exemple Portugal, s’il présente des résultats comparables à la moyenne des pays européens ou même supérieurs pour la région de Lisbonne et la vallée du Tage, présente des résultats inférieurs pour l’ensemble du territoire. La Suisse est, curieusement, un autre pays qui se situe en deçà des expectatives. Selon le rapport 2003 (Ramalho, 2004 :50), les études comparatives en littéracie (lecture) et en numéracie n’ont pas démontré de différence significative par rapport aux résultats de 2000. Nous avons pris connaissance d’une étude suisse qui avait pris pour point de départ des résultats également défavorables, pour ce pays, au même rapport PISA : cette recherche analyse l’insertion socio-économique des familles comme également l’influence des transmissions familiales sur les parcours scolaires des élèves.

Télédetection en milieu périurbain. Détection et localisation du changement de l'occupation du sol par intégration des donnés-satellite SPOT HRV dans un système d'information géographique

Thèse pour obtenir le grade de DOCTEUR DE L' UNIVERSITÉ PARIS XII, Discipline: Urbanisme Aménagement

Invertebrados y micropaleontología en la evolución de la Cuenca del Guadalquivir (España) y la Plataforma del Algarve (Portugal)

Based upon the depositional sequences in the Guadalquivir basin and the bio-events defined (foraminifera and nanoplancton) we present the synthesis of the paleontological results in correlation with the Neogene of Algarve (Portugal). We present the most representative outcrops for micropaleonlologic results, as well as paleoenvironmental correlations between Algarve and the Guadalquivir basin.

Reflexiones en torno a María Zambrano

Seminario María Zambrano», n.º 9, Novembro-Dezembro, 2008, Barcelona, pp. 91-94. Tradutora Mercedes López Quintela

La nueva flora medicinal mejicana en Europa del siglo XVI

41º Congresso Internacional de História da Medicina (Societé Internationale d´Histoire de la Médecine), México, 2008

L’instabilité dynamique pendant le Toarcien dans le Moyen Atlas (Maroc): mise en évidence de glissements synsédimentaires dans le synclinal de Bou Angar

During the Toarcian, shelves undergo block-faulting with mechanisms of tilting. It results the break up of the Middle Atlas basin in subsident sectors separated by resistant ridges. This device is highlighted by strong variations of facies, more or less extended lacunar zones, reefs aligned on the ridges and of synsedimentary tectonics structures. Within the framework of mapping survey carried out in the south-west of Middle Atlas, a meticulous prospection of Bou Angar synclinal allowed the description of a new outcrop of Toarcian. This one offers good examples of extensional structures and bio-accumulations. These data, supplemented by other witnesses of the dynamic instability in the rest of the Middle Atlas, permit to propose a paleogeographic map of the Middle Atlas basin during the Toarcian.

Implicações imunobiológicas da infecção a herpesvirus em tumores malignos : pesquisa e análise quantitativa de herpesvirus humanos no astrocitoma pilocítico

RESUMO: As infecções virais podem contribuir para o desenvolvimento do cancro, estando vários tumores malignos associados aos Herpesvirus (HHV). O vírus de Epstein-Barr (EBV) e o Herpesvirus 8, dois Herpesvirus, foram reconhecidos como agentes etiológicos de várias neoplasias. O astrocitoma pilocítico do cerebelo é um dos tumores cerebrais mais frequentes na criança, adolescentes e jovens adultos e a proliferação astrocitária ocorre geralmente após vários tipos de agressão, nomeadamente a infecção viral. Para investigar esta eventual interligação, estudámos 35 astrocitomas pilocíticos, pesquisando a presença dos 8 Herpesvirus. Neste estudo, foram utilizadas 10 amostras de biópsias do cerebelo de doentes que faleceram por doenças não relacionadas com infecção ou patologia tumoral. A maioria dos astrocitomas (33) eram tumores de baixa malignidade. As amostras foram analisadas por PCR (Polymerase Chain Reaction) quantitativa em tempo real (qPCR), com amplificação do gene da DNA polimerase viral. Treze astrocitomas e 7 controles revelaram pequenas quantidades de DNA viral (1-100 cópias/100ng DNA) de todos os Herpesvirus, com excepção do HHV6 A e B que estava ausente nas amostras. O EBV foi identificado em 9 dos 35 astrocitomas (26%) e em 7 dos 10 controles (70%) estando muito mais presente nos controles. As amostras positivas para o EBV foram também analisadas por imunohistoquímica, não tendo sido imunoreactivas para os anticorpos utilizados. A PCR com CODEHOP (consensus-degenerated hybrid oligonucleotide primers) foi utilizada para investigar a presença de um eventual Herpesvirus novo nestas amostras. Não foi identificada nenhuma sequência indicativa de um novo HHV por este método. 24. Em conclusão, os dados apontam para a presença de Herpesvirus, com particular relevância para o EBV, em tecido de cerebelo normal e em tumores cerebrais, embora em níveis demasiado baixos para poderem ser responsabilizados pela indução tumoral. A presença de sequências de DNA de Herpesvirus, nomeadamente do EBV, no Sistema Nervoso Central vem enriquecer a discussão sobre o significado da infecção viral na oncogénese humana, particularmente na neuro-oncogénese. ABSTRACT: Viral infections can contribute to the development of human cancer. Several human malignancies are linked with Human Herpesviruses (HHVs). Epstein-Barr virus and HHV8, two hHerpesvirus, have been recognized as etiologic agents of several neoplasms. Pilocytic astrocytoma of the cerebellum is one of the most common brain tumour in children, adolescents and young adults and astrocytary proliferation generally occurs after several types of injury, namely viral infection. To further explore this association, we have searched the tissue from 35 pilocytic astrocytoma, for all the 8 HHV. In this study, ten brain biopsies (cerebellum) from patients who died of unrelated diseases were used as controls. Most of the astrocytomas (33) were of low grade malignity. Samples were assessed by Real-time quantitative Polymerase Chain Reaction (q PCR) amplification of viral DNA polymerase gene. Thirteen astrocytoma and 7 controls showed low viral DNA levels (1-100 copies/100ng DNA) for all HHVs, with the exception of HHV6 that was absent. EBV was identified in 9 of the 35 astrocytoma (26 %) and in 7 of the 10 controls (70%) being more present in controls. EBV positive samples were also assessed by Immunohistochemistry (IHC) but none showed immunoreactivity for the antibodies used. PCR with consensus-degenerated hybrid oligonucleotide primers (CODEHOP) were also used to look for novel HHVs in these samples and no sequence indicative of a new HHV was detected. 26 Altogether the data indicate the presence of HHVs, with relevance for EBV in normal cerebellum tissue and also in brain tumours but at too low levels to be considered responsible for tumour induction. The presence of HHV DNA sequences, particularly EBV, in the studied brain tumours and control samples, further enriches the discussion about the relevance of viral infection in human oncogenesis, particularly neuro-oncogenesis.RÉSUMÉ: Les infections virales peuvent contribuer au développement du cancer. Les vírus de type Herpès sont associés à plusieurs néoplasies. Il est par exemple établi que les vírus Epstein-Barr et « human Herpesvirus 8 » (HHV-8) sont responsables de plusieurs tumeurs malignes. L´astrocytome pilocitique du cervelet est l’une des tumeurs les plus fréquentes chez les enfants, adolescents et adultes jeunes. En général la prolifération des astrocytes se produit en réponse à une agression. Posant l’hypothèse d’une agression d’origine virale, nous avons recherché la présence des 8 vírus Herpès dans les tissus de 35 astrocytomes. Dans cette étude, 10 échantillons de biopsie de cervelet de patients décédés suite à d’autres pathologies, ont été utilisés comme contrôles. La majorité des astrocytomes étaient de très basse malignité. Les échantillons ont été étudiés par PCR quantitative en temps réel, en amplifiant le gène de l’ADN-polymérase virale. Treize astrocytomes sur 35 (37%) et 7 contrôles sur 10 (70%) ont été trouvés positifs pour tous les HHV sauf l´HHV6, toujours avec un nombre de copies de polymérase virale bas (< 100 copies/100 ng d’ADN). Notamment l’EBV a été identifié 7 fois dans les contrôles (70%) et 9 fois dans les astrocytomes (26%). Les échantillons positifs pour l`EBV ont aussi été étudiés par immuno-histochimie. Aucun signal n’a été observé avec les anticorps utilisés. Enfin, une technique de PCR avec oligonucléotides dégénérés (CODEHOP ou consensus degenerated hybrid oligonucleotide primers) a été utilisée pour rechercher la présence d´un éventuel nouveau vírus Herpès dans les échantillons d’astrocytome. Aucun nouveau vírus n’a été identifié. 28 En résumé, nous avons établi la présence de vírus Herpès, en particulier l´EBV, dans le cervelet normal et dans les tumeurs du cerveau. Les quantités d’ADN viral retrouvées sont faibles et ne permettent pas d’attribuer à ces vírus la responsabilité de l’induction des tumeurs. Cependant, la présence d’ADN de vírus Herpès dans le cerveau sain ou pathologique vient enrichir la discussion sur le signification de l´infection virale dans les processus d´oncogenèse en général, et dans la neuroonco-genèse en particulier.