Faunule ichthyologique du Lias inférieur de S. Pedro de Muel, Portugal

The material collected in the Lower Liassic beds of S. Pedro de Muel (Portugal) contains some remains of actinopterygian fishes. The most significant elements have been described, and two genera have been recognized. One of them, Furo, is a halecomorph of the Caturidae family, the other one, Proleptolepis, is a teleostean genus belonging to the family Leptolepidae s. str. It is the first record of these two genera in Portugal. This discovery gives new data on the geographical distribution of Furo and Proleptolepis. In the present state of our knowledge, this last genus seems to be restricted to the Sinemurian - Lotharingian.

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, S��o Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

Sobre a ocorrência de copiapite na orla meso-cenozóica occidental de Portugal

The occurrence of a copiapite in the Paleogenic (?) formations of Vale Furado (South of S. Pedro de Muel, Portugal) is described, X-ray, DTA and TGA data and a chemical analysis of this mineral are presented.

Sobre a ocorrência de copiapite na orla meso-cenozóica ocidental de Portugal

The occurrence of a copiapite in the Paleogenic (?) formations of Vale Furado (South of S. Pedro de Muel, Portugal) is described, X-ray, DTA and TGA data and a chemical analysis of this mineral are presented.

Essai de biozonation du Domérien portugais

The biozonation of the portuguese Domerian is presented. This biozonation is based essentially on fauna from the following sections: S. Pedro de Muel, Peniche (Stokesi zone and lower part of the Margaritatus zone) and Brenha (Margaritatus and Spinatum zones). The distribution of the main fossil groups enabled an accurate division of the Stokesi zone into three horizons: Occidentale, Monestieri-Nitescens and Lusitanicum. In the Middle Domerian, the extension of the Ragazzonii horizon was reduced. An Elisa horizon was individualized at the top of the Upper Domerian.

Sedimentation pelagique et encroûtements cryptalgaires: les calcaires gremeleux du Carixien portugais

In Portugal, Carixian is generally represented by alternative layers of marly limestones characterized by nodule and lumpy levels. These layers are particularly developped [show preferential development] on passage areas to a sedimentary basin, particularly along the slope of tilted blocks between the Meseta and Berlenga's horst. This facies is included in the range of the «nodular limestone» and of the «ammonitico-rosso». Limestones are radiolaria micrites with fragments of pelagic organisms (ammonoids, thin shelled gastropods). These layers can be affected by intensive bioturbation (Brenha) which is responsible for dismantlement, specially where the initial thickness does not exceed a few centimetres. This process can lead to the isolation of residual nodules (Brenha, S��o Pedro de Muel, Peniche) which can be mobilised by massive sliding (Peniche). The isolated elements, shell fragments or residual nodules, can also be incrustated, thus developing oncolitic cryptalgal structures. At Brenha the lump structure developed progressively into a sequence overlapping the normal sedimentary one (thick limestone beds alternating with bituminous shales). Cryptalgal structures correspond to rather unstable environment conditions on mobile margins. These structures are known in deep pelagic sediments corresponding to well defined events of the geodynamic evolution (end of the initial rifting). Cryptalgal accretions disappear towards the sedimentary basin, and the nodular levels are less important. In the articulation areas with the Tomar platform, small mounds and cupules (Alcabideque) developed within the alternating marly-limestone levels. They represent the so called «mud mounds�� of metric dimensions. The upper part of these «mud mounds�� is hardened, showing track remains and supporting some brachiopods and pectinids. Hence the lumpy facies of Portugal is included among the range of sedimentaty environments and can be used as «geodynamic tracer».

Biostratigraphie et paléoécologie des peuplements d'ostracodes dans le Domérien du Bassin Lusitanien, Portugal

The Domerian sections from the Lusitanian Basin of S��o Pedro de Muel, Rabaçal and Tomar have provided us with more than 1100 Ostracods belonging from 18 genus and about 48 species. The faunal diversity and density of the associations decrease in space (from Tomar to Rabaçal and S��o Pedro de Muel) and time, with favourable environments for the proliferation of Ostracods at the lower part of the sections (Stokesi subzone) and more hostile at the upper part (Ragazzonii subzone). The Monestieri and Nitescens horizons and the Subnodosus subzone are characterized by a typical assemblage of Ostracods. The palaeoecological Ostracod indexes reveal the fluctuations of the oxygenation, temperature, depth and hydrodynamism of the water, on the different sections and on the whole platform. They display a diachronous cooling in the Lower Domerian series. In the upper part of the Middle and in the Upper Domerian, the deeper, less oxygenated and cooler waters prevent the development of the Ostracod faunas.

The Sinemurian ammonites of the Lusitanian Basin (Portugal): an example of complex endemic evolutioin

Palaeodiversity 3: 59–87; Stuttgart 30 December 2010

Investigando a financeirização pelos seus teóricos / Pedro Rozales Rodero Dominczak

Partimos do fato de que, nas últimas décadas, em especial a partir da década de 1980, o capital retoma parte da lucratividade perdida na década anterior. Essa retomada da lucratividade, contudo, se dá sobre características fortemente diferenciadas da acumulação que marcou o crescimento do período conhecido como os “30 anos dourados��� do capitalismo (sobretudo para a perspectiva das classes dominantes dos países centrais). Nesse sentido, nosso pressuposto é que, desde a virada operada pela crise estrutural da década de 1970, a esfera financeira ganhou autonomia em relação ao ciclo global da reprodução capitalista. E, decorrente dessa autonomia, a esfera financeira salta à condição de dominância em relação ao ciclo global. Assim, o objetivo geral desta dissertação é analisar os trabalhos que, pela perspectiva crítica, têm como objeto a esfera financeira. E nosso objetivo específico é compreender como a esfera financeira se relaciona com o ciclo global da reprodução capitalista. Dessa forma, quais seriam as principais características deste novo momento? Quais as causas que teriam impulsionado um crescimento tão acelerado da esfera financeira? Se vivemos em uma fase do capitalismo com forte influência financeira, em que consiste a financeirização, termo que aqui adotamos? E, principalmente, qual o seu relacionamento com o ciclo global do capital? Ela contribuiu para o desenvolvimento da acumulação capitalista ou pode ser considerada como refratária ao desenvolvimento e à expans��o do capitalismo? Estas serão as questões que serão trabalhadas ao longo da dissertação.

O isolamento no Hospital Colônia Pedro Fontes, Itanhenga/ES e a caracterização da população do Educandário Alzira Bley no período de 1937 a 1979

Caracteriza e analisa a população do Educandário, com as informações provenientes de uma fonte de dados documental e histórica contida nos dois livros de registros do Educandário e seus arquivos fotográficos. As informações sobre as 3.432 pessoas compõem um banco de dados que foi construído durante a realização desta pesquisa e as fotografias foram digitalizadas. O Educandário Alzira Bley, localiza-se na BR 101 - km 9, bairro de Itanhenga - Cariacica/ES. No estudo foram realizadas entrevistas semiestruturadas com funcionários e ex-internos do Educandário, que deram vida e movimento às análises dos gráficos e tabelas elaborados a partir do banco de dados. Para o embasamento teórico do estudo da população s��o empregados conceitos pertinentes à transição demográfica e à transição epidemiológica, às migrações forçadas, às redes migratórias e às características da população (sexo, idade, cor, origem e suas variações) que forneceram os elementos para a análise do estado da população em diferentes momentos históricos. A Geografia Histórica completa os referenciais teóricos desta investigação, pois muitas características geográficas requerem estudos históricos para uma explicação satisfatória de como chegaram ao que s��o hoje. As fotografias, os depoimentos e livros de registros do Educandário propiciaram a caracterização da população que passou e/ou viveu no Educandário Alzira Bley ao longo do período das internações compuls��rias no Hospital Colônia Pedro Fontes (1937-1979). Com a realização desta investigação chegamos às seguintes conclus��es: a) cada geração é vítima do conhecimento científico do seu tempo; b) a transição demográfica encontrava-se em sua primeira fase nos meados do s��culo XX, e os índices elevados de mortalidade e de fecundidade eram observados na população estudada; c) a transição epidemiológica, também em curso no Espírito Santo era caracterizada por elevada incidência das doenças infectocontagiosas, dentre as quais a hanseníase era ainda uma doença sem cura. d) o isolamento dos hansenianos em hospitais colônias, bem como seus filhos em preventórios foram movimentos de migração forçada; e) a internação compuls��ria dos hansenianos em hospitais colônias desencadeava uma migração em rede de familiares e demais parentes e amigos que pudessem estar com a doença.

O caráter político-pedagógico dos movimentos populares de bairro da Grande S��o Pedro: avanços e recuos sob o imperativo da ordem capitalista

Este trabalho tem como objeto de estudo as ações organizativas dos movimentos populares de bairro, enquanto práticas político-pedagógicas. Tomamos como foco, as associações de moradores da região da Grande S��o Pedro. Apesar de ter ficado conhecida na década de 1980 pela situação de mis��ria, os moradores dessa região, historicamente perpassada pelo fenômeno da segregação socioespacial, encontraram nas adversidades motivação para a organização do movimento popular como forma de construir sua história e afirmar sua cidadania. Totalmente transformada no que tange à sua urbanização, a região ainda hoje apresenta um cenário adverso para os moradores. Nesse sentido, a importância da organização dos moradores na atualidade é fundamental para lutar contra as situações de opressão que se impõem sobre os mesmos. Entretanto, o quadro que os atuais movimentos populares de bairro desta região apresenta é de reprodução de um modelo político-cultural marcado pelo individualismo, com traços peculiares da formação social brasileira - caracterizada por práticas de centralização, dependência e clientelismo político. Deve-se registrar que apesar de também trazerem traços de lutas e resistência, a forma como atualmente acontecem, com ações em níveis imediatos, esvaziadas de conteúdo político mais amplo, sem articulação com movimentos mais abrangentes, acabam se expressando em um “associativismo individualizado”. Desta feita, reiteramos neste trabalho a necessidade de a classe trabalhadora brasileira retomar, reconstruir espaços que contribuam com a formação de lideranças, com a qualificação das bases desses movimentos, para que seus protagonistas possam consolidar uma prática político-pedagógica fundamentada na educação popular e com isso venham adensar as lutas da classe trabalhadora e somar ao projeto de construção da contra-hegemonia, visando à transformação social. Buscar-se-ia neste sentido, a consolidação de um projeto social mais igualitário, justo e verdadeiramente democrático, no qual seja possível a emancipação humana.

Use of biofilm in the postharvest conservation of 'Pedro Sato' guava

This present work aimed to assess the effect of different concentrations of cassava starch, associated or not with prochloraz fungicide, on the postharvest conservation of 'Pedro Sato' guavas. Physiologically mature fruits were immersed in a solution of prochloraz (49.5 g/100 liters of water) for 5 min. Fruit treated with distilled water and air dried were used as control. They were immersed in cassava starch suspension at concentrations of 0, 20, 30 and 40 g/L, plus 0.5 mL/L of mineral oil. The fruits were stored at 21.0 ± 1.0 ºC and relative humidity of 85 ± 5%, for 12 days, and were examined at every three days. The combination of prochloraz and cassava starch resulted in delayed loss of firmness and yellowness and inhibited the incidence of lesions caused by Colletotrichum gloeosporioides during the 12 days of storage. Fruits treated with 40 g/L of starch, whether containing prochloraz or not, had unpleasant taste and odor, which suggests the occurrence of fermentation. Control fruits, with and without prochloraz, and those treated with starch with no prochloraz, had nearly 100% lesion occurrence within the 12 days. Starch suspension of 30 g/L, containing prochloraz, was the most effective in maintaining fruit quality.