Aspectos clínico-laboratoriais da infecção natural por Trypanosoma cruzi em cães de Mato Grosso do Sul

A doença de Chagas causada pelo T. cruzi é transmitida, principalmente, por insetos vetores e está distribuída na Argentina, no Chile, na Venezuela e no Brasil. O cão, além de ser um importante reservatório, também é vítima da doença e a única espécie capaz de desenvolver manifestações clínicas iguais a do homem. O presente trabalho teve como objetivo descrever as alterações clínicas encontradas em quatro cães infectados naturalmente pelo T. cruzi e alertar para a possibilidade de que a ocorrência dessa enfermidade em cães de Mato Grosso do Sul possa estar sendo subestimada. Os animais foram selecionados a partir de exames sorológicos de reação de imunofluorescência indireta (RIFI), ensaio imunossorvente ligado à enzima (ELISA) e immunoblotting com antígeno secretado e excretado da forma tripomastigota do T. cruzi (TESA-blot) e submetidos a xenodiagnóstico, exame físico, radiografia torácica, eletrocardiografia, ecocardiografia e bioquímica sérica. As alterações encontradas foram aumento de ventrículo direito, presença de arritmias do tipo bloqueio átrio ventricular, sinus arrest e bloqueio de ramo direito, além de disfunção sistólica e diastólica. Três animais apresentaram hiperproteinemia e as dosagens das enzimas CK e CK-MB revelaram valores indicativos de uma miocardite ativa. Esses são os primeiros casos descritos de cães com evidências consistentes de infecção natural pelo T. cruzi em Mato Grosso do Sul e ressalta-se o alerta aos médicos veterinários para a importância clínica e o papel dessa espécie como reservatório da doença.

Miocardite chagásica em caninos no Estado do Rio Grande do Sul

Neste trabalho, são relatados dois casos de morte súbita por doença de Chagas aguda em caninos da zona rural de Porto Alegre, Rio Grande do Sul, Brasil. Os cães, um macho Pit Bull com nove meses (canino 1) e uma fêmea Labrador Retriever com dois anos (canino 2), morreram em janeiro de 2005 e maio de 2008, respectivamente. As necropsias revelaram aumento cardíaco em ambos os casos. O coração do canino 2 apresentou formato globoso com múltiplas áreas pálidas na musculatura cardíaca, mais evidentes no ventrículo direito e câmaras cardíacas dilatadas, principalmente as da direita. Ao exame histológico, ambos os casos apresentaram alterações semelhantes caracterizadas por infiltrado inflamatório difuso não-purulento acentuado, predominantemente linfocitário intersticial. Nas fibras miocárdicas, havia grande número de pseudocistos, repletos de formas amastigotas do Trypanosoma cruzi. Ao teste sorológico TESA-blot, amostra do canino 2 foi positiva para anticorpos IgM e IgG anti-T.cruzi, achado característico da fase aguda da miocardite chagásica. Os resultados indicam que a doença de Chagas deve ser investigada em casos de morte súbita em cães na região Sul do Brasil e que a espécie pode servir como reservatório e sentinela da doença em humanos.

Metodologia para determinar parâmetros petrofísicos de corte em um campo de petróleo: o caso Socororo, bacia do Oriente, Venezuela

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Paracoccidioides brasiliensis: a mycologic and immunochemical study of a sample isolated from an armadillo (Dasipus novencinctus)

Amostra de Paracoccidioides brasiliensis isolada de vísceras (baço e fígado) de um tatu (Dasipus novencinctus) foi estudada do ponto de vista micológico e imunoquímico. O tatu havia sido capturado em área da usina hidroelétrica de Tucuruí (Estado do Pará). Este já havia sido considerado como reservatório enzoótico do Paracoccidioides brasiliensis naquela região. Esta amostra, conservada na Micoteca do Instituto de Medicina Tropical de São Paulo sob o número 135, apresenta todas as características de Paracoccidioides brasiliensis, com elevado poder antigênico e baixa virulência para cobaios e ratos Wistar. A demonstração do exo-antígeno específico do P. brasiliensis, representado pela glicoproteína de peso molecular 43 kDa, foi evidente através das técnicas de Imunodifusão Dupla, Imunoeletroforese, SDS-PAGE e Imunoblotting.

The role of organic matter on the adsorption of mercury in sediments from Amazon lakes, Brazil

Gold has been exploited intensively in the Brazilian Amazon during the past 20 years, and the elemental mercury (Hg) used in amalgamating the gold has caused abnormal Hg concentrations in waterways. Since 1986 particular attention has been given to the Madeira River because it is the largest tributary of the Amazon River and gold mining was officially allowed on a 350-km sector of the river. In this paper, samples of sediments from nine lakes located in the Madeira River basin, Rondonia State, Brazil, were analysed for mercury and organic matter. The average Hg content ranged between 33 and 157 ppb, which is about 8-40 times higher than the average value corresponding to 4.4 ppb for rocks occurring in the area (regional background). Significant correlation was found between the Hg content and organic matter in the sediments, indicating its importance on the retention of this heavy metal.

Floodplain construction in an anastomosed river

Fluvial environments and sedimentary facies involved in the floodplain (C2a type) construction of an anastomosed river system (Upper Parana River, Brazil) were studied. Sediment volume of floodplain deposits and sedimentation rate of each environment were obtained: channel (51.56%; 8.5 mm/yr), splay (33.85%; 1.27 mm/yr), pond (8.60%; 1.0 mm/yr), abandonment (3.64%; 3.87 mm/yr) and natural levee (3.41%; 2.34 mm/yr), reaching a total sedimentation rate average of 5.07 mm/yr. The causes of abandonment are also discussed. (C) 2003 Elsevier B.V. Ltd and INQUA. All rights reserved.

PALEOCLIMATIC CONTROLS ON STABLE OXYGEN AND CARBON ISOTOPES IN CALICHE OF THE ABO FORMATION (PERMIAN), SOUTH-CENTRAL NEW-MEXICO, USA

The stable oxygen and carbon isotopic composition of caliche in fluvial and supratidal rocks of the Abo Formation (Permian), south-central New Mexico, is controlled by palecoclimate and depositional environment. Fluvial caliche consists of low-Mg calcite nodules and vertically oriented tubules that display stage II texture. Micrite matrix support, brecciation, ooids/pisoliths, aveolar-septal texture, and peloids are common in the fluvial caliche and, along with red color and slickensides in the host shale, indicate pedogenesis in a well-oxidized vadose zone. In contrast, periodic waterlogging of the supratidal paleosols, probably due to high water table, is indicated by drab colors, carbonaceous flecks, horizontal rhizoliths, and the paucity of vadose textures in the stage II caliche nodules.Stable oxygen isotopes are similar in the fluvial and supratidal caliches and range from 21.6 to 30.5 parts per thousand (SMOW). The data exhibit a crude bimodality and delta-O-18 enrichment with a decrease in age (higher in the section). Consideration of these data in the context of delta-temperature relations suggests that 1) surface waters responsible for caliche formation increased in delta-O-18 (from roughly -8 to + 1 parts per thousand) over the 18 m.y. time interval that separated the lowest stratigraphic nodule horizon from the highest, 2) the increasing delta-O-18 values also reflect a warming trend (approximately 15-degrees to nearly 30-degrees-C) in the mean monthly temperature over this same time period, with perhaps an associated increase in Permian ocean temperatures, and 3) the significant variation in delta-O-18 from oldest to youngest caliche was probably enhanced by the amount effect, such that as the temperature increased, the amount of precipitation decreased, resulting in high delta-O-18 values.Caliches in the Abo are enriched in heavy carbon (-7.2 to -1.5 part per thousand PDB) compared to that of soil carbonate derived exclusively from C3 plants (-12 part per thousand PDB), and the supratidal caliches contain somewhat heavier carbon compared to the fluvial caliche. The delta-C-13 values for both environments increase with a decrease in caliche age. These results indicate that as the temperature increased and rainfall decreased with time, the level of C3 plant productivity apparently declined, allowing a greater influx of atmospheric CO2 into the soil. This can only occur when soil respiration rates are quite low or at very shallow depths (less than 10 cm), or both. Atmospheric CO2 seems to have invaded the supratidal soils to a somewhat greater extent than the fluvial soils.

A QUANTITATIVE APPROACH TO SUBSIDIZE THE PRECAUTIONARY MANAGEMENT of THE SMALL-SCALE FISHERIES IN ITAIPU RESERVOIR, BRAZIL

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

A stratigraphic chart of the Late Carboniferous/Permian succession of the eastern border of the Parana Basin, Brazil, South America

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Drenagem e traces tectonicos na Regiao Norte-Ocidental de Estado de Sao Paulo.

A detailed statistical study of the drainage was made as an indirect means for interpreting the modern tectonic traits of the area. Over 1000 measurements of direction of fluvial courses were made from maps and air photos. These data allowed the diagnosis of the existence of a regional tectonic pattern, printed on the basaltic rocks, and its influence on the drainage adjustment as well as a more local control exerted by structures present in the Bauru Group rocks. -from English summary

Aspectos morfologicos da Planicie Amazonica na Ilha de Tupinambarana (Amazonia-Brasil).

The Island is bordered by Amazon and Madeira rivers and by Uraria furo. The alluvial bars show the evolution phases of these big rivers on the fluvial plain. The lacustrine deltas are another morphologic feature. Within the lakes it is possible to observe streams with great density of sediments, when the flood phases of the Amazon create internal deltas and lake bedforms.-from English summary

Aspectos fisico-geograficos da Regiao Administrativa de Aracatuba.

In this region there are exposures of sandstones, siltstones, and argillites of the Adamantina Formation, belonging to the Bauru Group. Using satellite and radar images, superposition of drainage maps, toposheets geologic and pedologic maps and field trips, it was possible to discern (three geomorphological domains; a) hilly and interfluvial plateau in the divisories areas of Tiete - Aguapei and Tiete - Sao Jose dos Dourados mainrivers; b) colluvial surfaces located around the interfluvial plateau; and c) fluvial terraces and floodplains. The indiscriminant use of the soils is accelerating the erosive process, increasing the sedimentation of the river beds, the size of the floodplains and prejudicing the water quality, used to supply the rural and urban population. -from English summary

Influencia do soerguimento do alto Paranaiba na sedimentacao pos- basaltica na area do Triangulo Mineiro (MG), borda NNE da Bacia do Parana

Faciologic analysis method was applied to after-basaltic sedimentary deposits in Triangulo Mineiro (MG) area. Faciologic association 1 (Adamantina formation) and unities 1 to 5 (Uberaba formation) are related to the fluvial and lake deposits: faciologic association 3 (Ponte Alta Member) and 2 (Sierra da Galga Member) represent the sedimentary deposits associated to the alluvial fans conditions. With faciologic association and unities it could be to recognize the paleogeografic and tectonic conditions in sedimentation time of that depositional tract. -English summary

Comparing river basins world-wide and contrasting inland fisheries in Africa and Central Amazonia

An analysis of covariance relating basin area (A, km2) to river length (L, km) and discharge rate (D, m3 s-1) was performed for two continents and showed that the two covariates (L and D) were highly significant and that the strength of the relationship changed between continents. For comparison, D was excluded but the result remained the same. Although geomorphological models are useful for establishing global levels of production, these regressions should be applied with caution. Historically, simple statistical models were developed to predict fish catches in rivers. These, based upon regression of catches on channel length or basin area for Africa and Central Amazonia, are contrasted in this paper because of their generally similar approach.

Modelo para o estudo da dinâmica evolutiva dos aspectos fisiográficos dos pantanais

This paper studies the applicability of a model to the evolutive dynamics of Pantanal physiography. The Miranda-Aquidauana Pantanal has developed as a pre-existent fluvial plain in the beginning, from Paraguay river, whose ancient marks, recognized by weathering alteration volumes, show components that make possible its relative age determination and consequently permit the comprehension of the ancient and recent dynamic evolutions, that are responsible for the present physiographic form.