Sandfly fauna in an area endemic for visceral leishmaniasis in Aracaju, State of Sergipe, Northeast Brazil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

The venomous toadfish Thalassophryne nattereri (niquim or miquim): report of 43 injuries provoked in fishermen of Salinópolis (Pará State) and Aracaju (Sergipe State), Brazil

Os peixes da família Batrachoididae causam um grande número de acidentes em pescadores das regiões Norte e Nordeste do Brasil. O gênero Thalassophryne apresenta várias espécies no Brasil e a espécie Thalassophryne nattereri é a mais comum, todas apresentando veneno. O veneno é inoculado por duas espículas ocas na nadadeira dorsal e duas nas regiões pré-operculares, ligadas a uma glândula de veneno na base. Os envenenamentos causaram dor intensa, edema e eritema iniciais em 43 pescadores observados em Salinópolis (Pará) e Aracaju (Sergipe). em todos os casos, não ocorreram fenômenos sistêmicos dignos de nota, mas ocorreu necrose local em oito pacientes e infecção bacteriana em dez. As circunstâncias dos acidentes são comentadas, assim como aspectos terapêuticos. Nossa conclusão foi que o envenenamento por Thalassophryne é importante e freqüente e deve ser considerado de média gravidade, em função de não haverem fenômenos sistêmicos, como observado nos acidentes por peixes-escorpião (Scorpaena) ou arraias marinhas e fluviais.

Carboxylic acids of marine evaporitic oils from Sergipe-Alagoas Basin, Brazil

A. suite of 10 different marine evaporitic oil samples from Sergipe-Alagoas Basin, Brazil was studied for its biomarker content, in particular its acidic constituents. The oils showed different molecular distributions and relative abundances of n-alkanoic, isoprenoid and hopanoic acids. The observed differences were assigned to the incorporation of immature organic matter in the oils and fractionation along the migration pathway. The diagenetic precursor functionality (alcohol/ether or acid) was proposed based on the comparison of the relative abundances of the neutral and acidic biomarkers (hopanoids, isoprenoids, alkyl-steranes, monoaromatic alkyl-steroids). In the acidic fraction, 3 series of steroid-alkanoic acids and monoaromatic steroid-alkanoic acids (steroid-methanoic, ethanoic and propanoic acids and monoaromatic steroid-methanoic, ethanoic and propanoic acids) were detected, while in the neutral fraction only 2 series of each corresponding class could be observed (methyl and ethyl-steranes and monoaromatic methyl and ethyl-steroids). These carbon shifts suggest that decarboxylation is an important process in the formation of the alkyrsteranes and monoaromatic alkyl-steroids, and we infer that carboxylic acids are the diagenetic precursors of these classes of compounds. When alcohol or ether are the diagenetic precursors (isoprenoids and hopanoids), no significant differences in the molecular distributions between neutral and acidic fractions were observed. (C) 2000 Elsevier B.V. Ltd. All rights reserved.

Evidence for euphotic zone anoxia during the deposition of Aptian source rocks based on aryl isoprenoids in petroleum, Sergipe-Alagoas Basin, northeastern Brazil

Four crude oil samples from the Sergipe-Alagoas Basin, northeastern Brazil, were analyzed using full scan gas chromatography-quadrupole mass spectrometry (GC-qMS) for biomarkers, in order to correlate them using aromatic carotenoids thereby enhancing knowledge about the depositional environment of their source rocks. The geochemical parameters derived from saturated fractions of the oils show evidence of little or no biodegradation and similar thermal maturation (Ts/(Ts+Tm) for terpanes, C29 αββ/(αββ+ααα), C27, and C29 20S/(20S+20R) for steranes). Low pristane/phytane ratios and the abundance of gammacerane and β-carotane are indicative of an anoxic and saline depositional environment for the source rocks. Moreover, we identified a large range of diagenetic and catagenetic products of the aromatic carotenoid isorenieratene, including C40, C33, and C32 diaryl isoprenoids and aryl isoprenoid derivatives with short side chains and/or additional rings. These results indicate anoxia in the photic zone during the deposition of the source rocks. © 2013 The Authors.

A independência do solo que habitamos: autonomia, poder e cultura política na construção do império brasileiro. Sergipe (1750-1831)

Pós-graduação em História - FCHS

A independência do solo que habitamos: poder, autonomia e cultura política na construção do império brasileiro - Sergipe (1750-1831)

A Província de Sergipe ganhou autonomia em relação à Província da Bahia em 1820, por decisão de D. João VI, que então já havia transferido a Corte portuguesa para o Brasil. Dois anos depois o Brasil se tornava uma nação soberana, separando-se de Portugal. Esses dois acontecimentos, que guardam proximidade temporal e política, instigaram a historiadora Edna Maria Matos Antônio a estudar a presença da corte portuguesa no Brasil e os significados das transformações institucionais aplicadas pelo governo joanino às regiões distantes do Rio de Janeiro, então sede política da nação. A autora aborda as reformas econômicas e administrativas promovidas pelo estado metropolitano, iniciadas na fase pombalina em meados do século XVIII e continuadas com a chegada de D. João VI ao Rio de Janeiro. E avalia as distintas conseqüências de tais reformas para o desenvolvimento regional do Brasil, além da influência que teriam exercido sobre o movimento da independência brasileira. Tomando como referência a Revolução Pernambucana de 1817, que ao contestar a política joanina e exigir reformas recebeu adesão de parte das elites locais e desencadeou conflitos na relação com o poder monárquico, o livro analisa o processo de independência da capitania de Sergipe. A autonomia teria sido concedida em reconhecimento da Coroa à participação dos representantes do poder sergipano no combate à revolta de Pernambuco. A investigação desses fatos permitiu à autora expor a natureza desses conflitos e seus desdobramentos dentro da crise do colonialismo em terras brasileiras. O momento exigia que os grupos sociais e políticos da Colônia tomassem decisões sobre formatos políticos institucionais vistos como soluções para melhorar e modificar a realidade. De acordo com a autora, Diferentes concepções e perspectivas sobre Estado e sociedade acabaram por definir os rumos da configuração governativa e estrutura política da nação...

Perfil, concepções e práticas pedagógicas de professores que atuam em turmas multisseriadas de escolas públicas de Sergipe

This article examines some aspects of the organization of multigrade schooling, taking as reference the state of Sergipe. It describes the profile, the conceptions and pedagogical practices of teachers working in multigrade classes in public schools. The data presented result from a statistical analysis of information collected by Instituto Nacional de Estudos e Pesquisas Educacionais Anísio Teixiera (Inep) and from researches realized with public school teachers of Sergipe. The research has shown that the organization of multigrade schooling has different patterns and its central premise is the junction of years/grades, disregarding the age factor and inhibiting a possible pedagogical intervention, which considers the diversity of subjects and their lifetime. Therefore, it is necessary that teachers have a closer look at subjects of education in rural areas and build an educational intervention that goes beyond administrative aspects of formation of classes. The analysis of conceptions and practices of the teachers working in multigrade classes showed that the teaching work is obstructed by external determinations and by administrative barriers, inhibiting new reflections and practices that break up with the traditional logic of grades, permeated of excluding elements. The article aims to contribute to the dissemination of reflections and policies in the area of country education, especially for schools organized by multigrade schooling.

Mapeando a Situação Educacional no estado de Sergipe

This article examines historical and legal aspects of educational policy in Brazil, presenting the main challenges for the consolidation of the new National Education Plan, currently under construction. From this, the article focuses on the description of some educational indicators, describing the educational reality in the state of Sergipe. The study focuses on indicators for early childhood education, to primary education and teacher training, showing historical deficits in basic education. In describing data on education in the state of Sergipe, contextualizing it within the framework and illustrates some national educational policies implemented in the state. As a result of the study is intended to show the importance of research into the educational policy in the state of Sergipe, in order to contribute to improving the quality of educational provision.

Aspectos petrográficos dos carbonatos da Formação Riachuelo - Albiano, bacia de Sergipe

The carbonatic rocks have great importance in petroleum geology, since most hydrocarbons reservoirs in the world are associated to this kind of rock. The new giant petroleum fields discovered in the Brazilian southeast Atlantic margin are directly connected to calcareous rocks, which are subjacent to the Aptian evaporite pack. This demand an increase in the number of geologists able to study such deposits. The Aptian carbonatic platform is completely exposed only in the Sergipe-Alagoas Basin. Therefore, it works as a natural laboratory to the study and understanding of this kind of rock. The Sergipe Basin is situated in the east Brazilian coast, and has its evolutional history is intimately related to the formation of the South Atlantic Ocean, through the break-up of the Gondwana supercontinent. The marine sequence of the Brazilian marginal basins is of Albian age and is marked by the development of carbonatic platforms. In doing so, this paper aims to analyze the Albian limestones from Riachuelo Formation of the Sergipe Basin. The project gave to the student the opportunity to increase his knowledge in carbonates, due to the laboratory and outdoor activities. The studied deposits, within a regional outline, were petrografically described, allowing interpretations about the evolution of the former South Atlantic Ocean. Ten points were visited where samples were collected for making of thin sheets. In this work several carbonatic facies were identified totaling 116 laminates described.

Caracterização epidemiológica de brucelose e leptospirose de pequenos ruminantes dos estados do Sergipe, Bahia, Ceará e Paraíba

Pós-graduação em Medicina Veterinária - FCAV

Biosorption of Cr(III) using in natura and chemically treated tropical peats

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Abarema cochliacarpos: Gastroprotective and ulcer-healing activities

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Burial history and porosity evolution of Brazilian upper Jurassic to tertiary sandstone reservoirs

The parameter time-depth index (TDI) is applied in this study to quantify empirically the influence of burial history on sandstone porosity evolution. The TDI, expressed in kilometers per million years of age, is defined as the area in the burial history diagram enclosed by the burial curve of the reservoir and the axes of the diagram. In practice, reservoir depths during burial history are integrated at regular time intervals of 1 m.y. The calculations exclude present-day bathymetry or paleobathymetry. Sandstone reservoirs from several sedimentary basins along the Brazilian continental margin (Santos, Campos, Espírito Santo, Cumuruxatiba, Recôncavo, Sergipe, Alagoas, and Potiguar) were analyzed to investigate the evolution of porosity against TDI. These Upper Jurassic to Tertiary sandstones lie in depths of 700 to 4900 m, and are hydrocarbon charged (oil or gas). Average porosities of most of these reservoirs were obtained from core analysis, and a few porosity data were taken from well log interpretations. Detrital constituents of the sandstones are mainly quartz, feldspar, and granitic/gneissic rock fragments. Sandstones were grouped into three main reservoir types, based on composition (detrital quartz content) and grain sorting: Type I (average quartz content <50%) are very coarse grained to conglomeratic, poorly to very poorly sorted lithic arkoses. Rock fragments are mainly granitic/gneissic and coarse grained. Type II (average quartz content ranging from 50% to 70%) are fine- to coarse-grained (pebbles absent or occurring in small percentages), moderately sorted arkoses. Type III (average quartz content >80%) are fine to coarse, moderately to poorly sorted quartz arenites or subarkoses. Plots of average porosity against depth show great dispersion in porosity values; such dispersion is mostly due to differences in the reservoir burial histories. However, plotting porosity values against the TDI for individual reservoir types produces well-defined trends. The decrease in porosity is less marked in Type III reservoirs, intermediate in Type II, and faster in Type I. Such plots suggest that it is possible to make relatively accurate porosity predictions based on reservoir TDI, texture, and composition,: within the constraints of reservoir depth/age and basin tectonics analyzed in this study.

Structure and properties of Brazilian peat: Analysis by spectroscopy and microscopy

Peat was taken from the Sergipe State, Brazil and characterized by several techniques: elemental and thermal analyses; Fourier infrared (FTIR) and solid state 13C nuclear magnetic resonance (NMR) spectroscopies; scanning electron microscopy (SEM), environmental scanning electron microscopy (ESEM) and X-ray diffractometry (XRD). Also, the Sergipe State peat samples were compared with other peat sample from later from Sao Paulo State, Brazil. The lowest O/C and E 4/E 6 ratios and differential thermal analysis (DTA) curves of the Santo Amaro (SAO) sample indicated that this sample had the highest degree of decomposition. FTIR results showed that Itabaiana (ITA) and São Paulo (SAP) samples presented more prominent peak at 1086 cm -1 attributed the presence of Si-O than SAO sample spectra. The SAO sample showed two more intense peaks at 2920 cm -1 and 2850 cm -1. These results were corroborated by 13C NMR and thermal gravimetric (TG) where the relative abundance of the alkyl-C groups was greater in the SAO sample. The X-ray diffractometry (XRD) of SAO sample is characteristic of amorphous matter however, the SAP and ITA samples revealed the large presence of quartz mineral. The scanning electron microscopy (SEM) and environmental scanning electron microscopy (ESEM) showed that the surface of peat samples have porous granules of organic material. The ITA and SAP peat samples are alike while SAO peat sample is richer in organic material. Only the SAO sample has truthful characteristics of peat. The results of this study showed that the samples are very different due to variable inorganic and organic material contents. ©2007 Sociedade Brasileira de Química.