Soils of the Jurassic formations in the central Algarve; their occurrence, distribution, genesis and site qualities

In the central Algarve different soils have developed dependent on petrography of the parent material, slope position and recent erosion. The general patterns of occurence and distribution of different soils are described. The age of an eutric Nitosol is estimated and the relation between the soil and the parent material is investigated. Some different soils are described as examples with their chemical and physical properties. The water budget of soils is described in general with considerations concerning ground water recharge and run-off as well as in dependence of climate and of different site conditions.

On the fractional central differences and derivatives

Fractional central differences and derivatives are studied in this article. These are generalisations to real orders of the ordinary positive (even and odd) integer order differences and derivatives, and also coincide with the well known Riesz potentials. The coherence of these definitions is studied by applying the definitions to functions with Fourier transformable functions. Some properties of these derivatives are presented and particular cases studied.

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-EfE-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing oeean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

Índice de distorção, parâmetros celulares e composição química de cordierite de granitóides e corneanas da região de Tondela - Oliveira do Hospital (Portugal Central)

Memórias e Noticias, PubI. Mus. Lab. Mineral. Geol., Univ. Coimbra, n.O 116, 1993

Fractional central differences and derivatives

Journal of Vibration and Control, Vol. 14, Nº 9-10

Aplicação de um SIG no ordenamento do território para a implantação de uma central de ciclo combinado

Dissertação apresentada por Elisabete de Jesus Barrelas Lopes Raimundo à Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa, para obtenção do grau de Mestre em Ordenamento do Território e Planeamento Ambiental

Análise do balanço entre sequestro e emissão de CO2 resultante do circuito de produção e consumo de biomassa florestal numa central de co-geração

Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Bioenergia

Contributo para o estudo da influência do stress na resposta imunitária à vacina contra a gripe em profissionais de saúde

Resumo: Os profissionais de saúde podem estar expostos a vários factores indutores de stress crónico nomeadamente de natureza profissional destacando-se, entre os seus possíveis efeitos, a diminuição da resposta de anticorpos após administração de vacinas, entre as quais, a vacina contra a gripe. Uma vez que os trabalhadores da saúde estão expostos a factores indutores de stress e, simultaneamente, a agentes biológicos cujos efeitos poderão ser prevenidos pela vacinação, é pertinente estudar a influência do stress na resposta imunitária à vacina contra a gripe em enfermeiros. Constituíram objectivos deste trabalho: (1) estudar a associação entre a presença de stress crónico em enfermeiros hospitalares e a “insuficiente” resposta imunitária à vacina contra a gripe, avaliada um mês após a vacinação (T1); (2) estudar a associação entre a presença de stress crónico em enfermeiros hospitalares e a redução dos títulos de anticorpos dirigidos às hemaglutininas seis meses após a vacinação (T6) e (3) identificar algumas características das unidades de internamento e do trabalho dos participantes que possam estar associadas à presença de stress crónico e estudar a sua possível associação com a resposta imunitária à vacina contra a gripe. Realizou-se um estudo caso-controlo incorporado num estudo de coortes e a amostra em estudo foi constituída por 136 enfermeiros saudáveis (83,8% sexo feminino; média de idades de 33anos) de um hospital universitário. Realizaram-se entrevistas individuais e aplicaram-se as versões portuguesas dos questionários The General Health Questionnaire (GHQ12) e Maslach Burnout Inventory – Human Services Survey (MBI-HSS) para determinação da presença de stress crónico pelo método da triangulação, no início do estudo (T0) e realizou-se a recolha de dados relativos à caracterização de elementos de trabalho nas unidades de internamento. Foi administrada a vacina contra a gripe e determinou-se os títulos de anticorpos dirigidos às hemaglutininas de cada estirpe componentes da vacina contra a gripe utilizada em 2007, antes da vacinação, um mês e seis meses após a vacinação. Não se encontrou associação, ao nível de significância de 5%, entre a presença de stress e a “insuficiente” resposta à vacina contra a gripe, avaliada pela taxa de indivíduos que apresentaram um aumento, ao fim de um mês, inferior a quatro vezes os títulos de anticorpos antes da vacinação. No entanto, encontrou-se uma maior proporção de indivíduos com stress no grupo de participantes em que ocorreu uma diminuição do título de anticorpos dirigidos à hemaglutinina AH1 (ac AH1) em T6, quando comparado com o respectivo grupo controlo. A diferença entre grupos foi estatisticamente significativa, quando se avaliou a presença de stress pelo método da triangulação usando a entrevista (p=0,006), pelo método da triangulação usando o GHQ12 (p=0,045) e ainda usando a combinação dos três critérios (p=0,001). Após análise multivariada, verificou-se que a associação entre a presença de XXVI stress e a redução dos ac AH1 em T6 manteve significado estatístico (respectivamente, p= 0,010, p= 0,042 e p=0,002) e apresentou odds ratio ajustados, em função de cada um dos métodos de avaliação da presença de stress, de 3,643, de 2,733 e de 5,223. A quantidade de trabalho percepcionada como sobrecarga constituiu o factor indutor de stress mais vezes referido (58,8% da amostra e 61,8% dos enfermeiros de unidades de internamento), seguida dos conflitos entre profissionais. O contacto com o sofrimento e a morte de doentes foram identificados em quarto lugar pela amostra, mas em segundo pelos enfermeiros de unidades de internamento. Nesses, verificou-se uma associação positiva entre trabalhar em Serviços onde o número de doentes falecidos foi muito elevado e a presença de stress, medido pelo método da triangulação usando a entrevista (p=0,039), usando o GHQ12 (p=0,019), usando a escala de exaustão emocional do MBI-HSS (p=0,012) e pela combinação dos três métodos (p=0,014). Verificou-se também uma associação positiva entre a presença de stress, identificada pelo método da triangulação usando a escala de exaustão emocional do MBI-HSS, e o trabalho em serviços de internamento onde a percentagem de doentes idosos (p=0,025) e a taxa de letalidade (p=0,036) foram elevadas. Contudo, não se encontrou associação entre a exposição muito frequente ao sofrimento e à morte de doentes e a redução do título de ac AH1 em T6. Possivelmente, a exposição a esse factor indutor de stress, apesar de estar relacionada com a presença de stress nos enfermeiros de serviços de internamento, não foi suficientemente intenso para, por si só, estar associada à redução do título de ac AH1 em T6. A associação encontrada entre a presença de stress crónico e a redução do título de anticorpos AH1 em T6 vem apoiar a resposta à questão de investigação inicialmente colocada de que o stress poderá influenciar negativamente a manutenção dos títulos de anticorpos, mesmo em indivíduos adultos não idosos. Assim, o risco de um enfermeiro com stress apresentar redução do título de anticorpos dirigidos à hemaglutinina da estirpe AH1N1 – A/Solomon Islands/3/2006 ao fim dos seis meses do estudo, foi 3,6, 2,7 ou 5,2 vezes superior ao de um enfermeiro sem stress, consoante o critério de stress ter sido determinado, respectivamente, pelo método da triangulação usando a entrevista, pelo método da triangulação utilizando o GHQ12 ou pela combinação dos três critérios. Summary: Health workers may be exposed to various factors causing chronic stress namely those related directly to their activity, in particular the decrease in the capacity of the response of antibodies after the administration of the vaccines, amongst others the Influenza vaccine. Since health workers are exposed to factors causing stress and at the same time biological agents, whose effects may be prevented through vaccination, it is important to study the influence of stress in the immunity response to the Influenza vaccine on nurses. The aims of this study are: (1) to examine the relation between chronic stress in hospital nurses and the “insufficient” immunity response to the Influenza vaccine, assessed at one month after vaccination (T1); (2) to examine the relation between chronic stress in hospital nurses and the decrease of the hemagglutinin titles of antibodies six months after vaccination (T6); (3) to identify some characteristics of internment units and the work of the participants that may be related to the presence of chronic stress and to study its possible relation with the immunity response to the Influenza vaccine. A control-case study, integrated in a coortes study, was carried out and the sample under analysis consisted of 136 healthy nurses (83,8% female; average age 33 years old) from a university hospital. Several individual interviews were conducted and the portuguese versions of General Health Questionnaire (GHQ12) and Maslach Burnout Inventory – Human Services Survey (MBI-HSS) was applied in order to determine the presence of chronic stress, using the triangulation method at the beginning of the study (T0). Data concerning the particular features of the internment units was collected. The Influenza vaccine was administered and the titles of hemagglutinin antibodies of each strain composing the Influenza vaccine used in 2007, before vaccination, and a month and six months after vaccination, were determined. There was no statistically relevant (5%) relation between stress and the “insufficient” immune response to the Influenza vaccine, according to the rate of individuals that showed, after a month, a level of antibodies concentration lower than four times the level prior to the vaccination. Nevertheless, there was a greater number of individuals with stress in the group of participants in which there was a decrease of the hemagglutinin titles of antibodies AH1 (ac AH1) in T6, when compared to the control group under study. The difference between groups was statistically relevant when assessing the presence of stress by triangulation method using the interview (p=0,006), by triangulation method using the GHQ12 (p=0,045) and by the combination of the three criteria (p=0,001). After multivariate analysis, it was verified that the XXVIII relation between the presence of stress and the reduction of the ac AH1 in T6 was statistically relevant (respectively, p= 0,010, p= 0,042 and p=0,002) and the odds ratio were, according to each of the methods used to assess the presence of stress, 3,643, 2,733 and 5,223. Overwork was the most emphasised stress-causing factor (58,8% of the sample and 61,8% of the nurses working in the Internment Units), followed by conflicts arousing among co-workers. Witnessing the suffering and death of patients was ranked as the fourth cause of stress, but the second by the nurses of the internment units. The former revealed a positive connection between working in the services, where there was a high rate of deaths, and the presence of stress, when assessing the presence of stress by triangulation method using the interview (p=0,039), the GHQ12 (p=0,019), the MBI-HSS emotional exhaustion scale (p=0,012) and by the combination of the three criteria (p=0,014).There was also a connection between the presence of stress, identified by the method of triangulation using the MBI-HSS emotional exhaustion scale, and working in the internment units, where the percentage of elderly people (p=0,025) and the mortality rate (p=0,036) were high. However, there was no connection between frequent exposure to suffering and death in patients and the reduction of ac AH1 titles, in T6. Although one can establish a connection between stress in nurses working in the internment units and the aforementioned stress-causing factor, the exposure to that factor was not, per se, intense enough to reduce the ac AH1 title in T6. The relation found between the presence of chronic stress and the reduction of AH1 antibodies titles in T6, corroborates the hypothesis that stress can negatively influence the title of antibodies, even in non-elderly adults. Thus, and according to the criteria used to define stress, by the triangulation method using the interview, by the triangulation method using the GHQ12 or the combination of the three criteria respectively, the risk of a nurse suffering from stress showing a reduction in the title of hemagglutinin antibodies for the strain AH1N1 – A/Solomon Islands/3/2006 six-month after Influenza vaccine was 3,6, 2,7 or 5,2 times greater than on a nurse suffering from no stress at all. Résumé: Les professionnels de la santé peuvent être exposés à différents facteurs inducteurs de stress chronique de nature professionnelle. On remarque, parmi les effets possibles, une baisse de la réponse des anticorps après l´administration de vaccins, comme en particulier, le vaccin de la grippe. Lorsque les professionnels de la santé ont été exposés à des facteurs inducteurs de stress, et de manière simultanée, à des agents biologiques dont les effets pourront être prévenus par la vaccination, il est pertinent d´étudier l´influence du stress dans la réponse immunitaire au vaccin de la grippe chez les infirmiers. Ils ont constitué des objectifs d´études et de discussion : (1) étudier l´association entre la présence de stress chronique chez les infirmiers, en milieu hospitalier, et la “insuffisant” réponse immunitaire au vaccin de la grippe, vérifiée à un mois après la vaccination (T1); (2) étudier l´association entre la présence de stress chronique chez les infirmiers, en milieu hospitalier, et la réduction de la teneur des anticorps dirigé à la hémaglutinina six mois après la vaccination (T6) (3) identifier certaines caractéristiques des unités d´internement, et étudier les aspects du travail des participants, qui puissent être associée à la présence de stress chronique et étudier sa possible association avec la réponse immunitaire au vaccin de la grippe. Une étude cas-contrôle incorporée dans une étude de groupe a été réalisée et un échantillon, pour étude, a été constitué par 136 infirmiers sains (83,8% de sexe féminin, âge moyen 33 ans) travaillant dans un hôpital universitaire. Des entretiens individuels ont été réalisés et les versions portugaises des questionnaires de General Health Questionnaire (GHQ12) et Maslach Burnout Inventory- Human Service Survey (MBI-HSS) ont été utilisés pour déterminer la présence de stress chronique grâce à la méthode de triangulation, au début de l´étude (T0) et un relevé de données relatives à la caractérisation d´éléments de travail dans les unités d´internement a été fait. Le vaccin de la grippe a été administré et les teneurs en anticorps dirigés aux hémaglutininas de chaque composant du vaccin de la grippe pour 2007 ont été déterminés, avant la vaccination et un mois et six mois après. On n´a pas trouvé d´association, à un niveau significatif de au moins 5%, entre la présence de stress et la “insuffisant” réponse au vaccin de la grippe, évaluée par le taux d´individus qui ont présenté une augmentation, à la fin du mois, inférieur à quatre fois la teneur des anticorps par rapport à avant la vaccination. Cependant , on a trouvé une plus grande proportion d´individus victimes de stress dans le groupe des participants où il y a eu une baisse de la teneur des anticorps dirigé à la hémaglutinina AH1 (ac AH1) en T6, après comparaison avec le respectif groupe de contrôle. La différence entre les groupes a été statistiquement significative lorsqu´on a vérifié la présence de stress grâce à la méthode de triangulation, en utilisant l´entretien (p=0,006), par la méthode de triangulation en utilisant le GHQ12 (p=0,045) et en utilisant aussi la combinaison des trois critères (p=0,001). Après une analyse XXX multivariée, on a vérifié que l´association entre la présence de stress et la réduction des ac AH1 en T6 a conservé un signifié statistique (respectivement, p=0,010, p=0,042 et p=0,002) et a présenté des odds ratio ajustés, en fonction de chacune des méthodes de vérification de la présence de stress de 3,643, de 2,733 et de 5,223. La quantité de travail perçue comme une surcharge constitue le facteur inducteur de stress le plus souvent cité (58,8% de l´échantillon et 61,8% des infirmiers des unités d´internement), suivi par les conflits entre professionnels. Le contact avec la souffrance et la mort des patients a été placé en quatrième position par l´échantillon, mais en deuxième position par les infirmiers des unités d´internement. Dans ces cas, on a vérifié une association évidente entre le fait de travailler dans des services où le nombre de patients décédés a été très élevé et la présence de stress, identifiée par la méthode de triangulation, en utilisant l´entretien (p=0,039), le GHQ12 (p=0,019), l´échelle de fatigue émotionnelle du MBI-HSS (p=0,012) et en utilisant aussi la combinaison des trois critères (p=0,014). On a aussi vérifié une association positive entre la présence de stress, identifiée par la méthode de triangulation, en utilisant l´échelle de fatigue émotionnelle du MBI-HSS et le travail dans des services d´internement où le pourcentage de malade âgés (p=0,025) et le taux de mortalité ont été élevés (p=0,036). Malgré tout, on n´a pas trouvé d´association entre l´exposition très fréquente à la souffrance et à la mort des patients et la réduction de la teneur de ac AH1 en T6. Probablement l´exposition à ce facteur inducteur de stress, bien qu´elle soit liée à la présence de stress chez les infirmiers des services d´internement, n´a pas été suffisamment intense pour, en elle-même, être associée à la réduction de la teneur ac AH1 enT6. L´association trouvée entre la présence de stress chronique et la réduction de la teneur des anticorps AH1 en T6 vient renforcer l´hypothèse que le stress pourra influencer négativement la manutention des teneurs en anticorps même chez les individus adultes jeunes. Donc le risque qu´un infirmier stressé présente une réduction de la teneur en anticorps dirigés à la hémaglutinina de le composant AH1N1-A/Solomon Island/3/2006 à la fin des six mois d´études a été 3,6, 2,7 ou 5,2 fois supérieure à celui d´un infirmier sans stress, après avoir déterminé le critère de stress, respectivement par la méthode de triangulation utilisant l´entretien, par la méthode de triangulation utilisant le GHQ12 ou par la combinaison des trois critères.

Fractional central differences and derivatives

Journal of Vibration and Control, 14(9–10): 1255–1266, 2008

The Transversarium-Bifurcatus Zone boundary at Rocha (Peral area, East-Central Algarve, Portugal)

This paper represents the first detailed study of the Transversarium-Bifurcatus Zone boundary in the Algarve. The boundary studied in the Peral area is associated with a stratigraphic discontinuity, whose hiatus partially affects the Transversarium-Bifurcatus Zones. A discontinuity was also recognized in the Bifurcatus-Birnammatum Zone boundary, which can be correlated with the traces of a Type II unconformity, which separates cycles 4.3-4.4 in HAQ et al. (1987), present on the South Iberian palaeomargin. An analysis was made of the ecostratigraphic evolution in the interval between the uppermost Transversarium Zone and the lower part of the Bimammatum Zone on the basis of the faunal spectra obtained. We conclude that ammonites are the most tolerant cephalopods to the ecological stress caused by the increase of inflows and the decrease of the shelf's ecospace. Benthic fauna decreased considerably in these conditions. A relatively abundant and diversified fauna ofDichotomoceras is noteworthy among the ammonites collected, as this genus was previously little known in the Algarve.

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-E/E-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing ocean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.

Paleoalterações e cimentações nos depósitos continentais terciários de Portugal central: importância na interpretação de processos antigos

This paper describes the palaeoweathering, cementation, clay minerals association and other closely related characteristics of central Portugal allostratigraphic Tertiary units (SLD's), that can be used for palaeoclimatic interpretation and palaeoenvironmental reconstruction. Lateral and vertical changes in palaeosols are of value for improving our understanding of the autocyclic and allocyclic controls on sediment acumulation in an alluvial basin, but they can also have stratigraphic importance. In some cases it is concluded that the geomorphological setting may have been more decisive than climatic conditions to the production of the palaeoweathering. During late Palaeogene (SLD7-8), surface and near-surface silicification were developed on tectonically stable land surfaces of minimal local relief under a semi-arid climate; groundwater flow was responsible for some eodiagenesis calcareous accumulations, with the neoformation of palygorskite. Conditions during the Miocene (SLD9-11) were favourable for the smectization of the metamorphic basement and arenization of granites. Intense rubefaction associated with basement conversion into clay (illite and kaolinite), is ascribed to internal drainage during late Messinian-Zanclean (SLD12). During Piacenzian (SLD13) intense kaolinization and hydromorphism are typical, reflecting a more humid and hot temperate climate and important Atlantic fluvial drainage. Later on (Gelasian-early Pleistocene ?; SLD14). more cold and dry conditicns are interpreted, at the beginning of the fluvial incision sage. Silica cementation is identified in the upper Eocence-Oligocene ? (SLD18; the major period of silicification), middle to upper Miocene (SLD10)and upper Tortonian-Messinian (SLD11); these occurrences are compatible with either arid or semi-arid conditions and the establishment of a flat landscape upon which a silcrete was developed.

Significado regional dos depósitos neogénicos continentais da área de Vila de Rei (Portugal Central)

In the Vila de Rei area (Central Portugal) the continental deposits of the Lower Tagus Tertiary Basin lay upon the pediment of the Portuguese Central Chain. Three conglomerate units are recorded from the base upwards, separated by regional or basinal unconformities; Conglomerados de Rio de Moinhos (RM); Conglomerados de Serra de Almeirim (SA) and Conglomerados de Vila de Rei (VR). The first two units (RM and SA) have been sites of gold exploitation in huge open pit mines probably during Roman colonisation times. The contact of this units, on the Paleozoic basement or on the Paleogene unit Grés de Monsanto, is unconform, defining in both limits a large nondepositional and/or erosional hiatus. Those conglomerates seal the sedimentation of the Lower Tagus Tertiary Basin along its northern border. Taking into account the significance assigned to their basinal unconformity limits, the uplift of the Portuguese Central Chain, and the fact of this continental units yielded no fossils with chronostratigraphic significance, they have been considered ranging from Upper Miocene to the beginning of the Quaternary. Finally, a lithostraligraphic equivalence with the Neogenic units of the Bierzo and Duerna basins (NW of the Iberian Peninsula), where exploitations from Roman times are also evident, is presented.

High-resolution correlation of coastal cliff sections in the Lagos- Portimao Formation (Lower - Middle Miocene, central Algarve, Portugal)

This paper describes a high-resolution stratigraphic correlation scheme for the early to middle Miocene Lagos-Portimão Formation of central Algarve, southern Portugal. The Lagos Portimão-Formation of central Algarve is a 60 m thick package of horizontally bedded siliciclastics and carbonates. The bryozoan and mollusc dominated biofacies is typical of a shallow marine, warm-temperate climatic environment. We define four stratigraphic marker beds based on biofacies, lithology, and gamma-ray signatures. Marker bed 1 is a reddish shell bed composed predominantly of bivalve shells in various stages of fragmentation. Marker bed 2 is a fossiliferous sandstone / sandy rudstone characterized by bryozoan masses. Marker bed 3 is also a fossiliferous sandstone with abundant larger foraminifers and foliate bryozoans. Marker bed 4 is composed of three distinct layers; two fossiliferous sandstones with an intercalated shell bed. The upper sandstone unit displays thickets of the bryozoan Celleporaria palmate associated with the coral Culizia parasitica. This stratigraphic framework allows to correlate isolated outcrops within the stratigraphic context of the Lagos-Portimão Formation and to establish high resolution chronostratigraphic Sr-isotopic dating.

The Cenomanian-Turonian transition in West Central Portugal: ammonites and biostratigraphy

The Upper Cenomanian and Lower Turonian ammonite assemblages from the onshore sectors of the West Portuguese Margin are reviewed after new studies on the type section of Figueira da Foz, and correlative sections of Baixo Mondego. The faunal succession shows a strong contribution of vascoceratids and other ammonites with North African and Tethyan affinities. Euomphaloceras septemseriatum (Cragin, 1893), Kamerunoceras douvillei (Pervinquere, 1907), Fagesia catinus (Mantell, 1822), Neoptychites cephalotus (Courtiller, 1860), and Thomasites rollandi (Thomas & Peron, 1889) are for the first time mentioned to Portugal. The Upper Cenomanian is recognised after a set of 3 assemblage zones: Neolobites vibrayeanus z., Euomphaloceras septemseriatum z ., and Pseudaspidoceras pseudonodosoides z. The carbonate succession shows an important unconformity across the Cenomanian-Turonian boundary, associated to subaerial exposure, and to the development of a palaeokarst over Upper Cenomanian units. The first Lower Turonian carbonates are yielded a single but diverse ammonite assemblage of middle Lower Turonian age (Thomasites rollandi z.). This biozone was previously recognised in Central Tunisia by G. Chancellor et al. (1994).