999 resultados para 112-681B


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Detailed petrographical and bulk geochemical investigations of organic matter (OM) have been performed on sediments deposited below or close to upwelling areas offshore Peru (ODP-Leg 112; Sites 679, 681, 688) and Oman (ODP-Leg 117; Sites 720, 723, 724) in order to obtain a quantitative understanding of its accumulation and degradation. Microscopical as well as nanoscopical investigations reveal that the OM in sediments affected by upwelling mechanisms mainly (up to 98%) consists of unstructured (amorphous) organic aggregates without any apparent biological structures. In sediments which are not or to a lesser extent affected by upwelling (Site 720) terrestrial OM predominates. Organic carbon (TOC) contents are highly variable and range between 9.8% in sediments deposited below upwelling cells and 0.2% in sediments outside the upwelling zone. The TOC/sulphur ratios of the sediments scatter widely. The samples from the deep-water locations (Sites 688 and 720), show C/S-ratios of "normal" marine sediments, whereas at the other locations no correlation or even a negative correlation between sulphur and TOC concentration exists. In most of the upwelling-influenced sediments OM contains a significant amount of sulphur. The incorporation of sulphur into the OM followed microbial sulphate reduction and occurred in the upper meters of the sedimentary column. Below, OM is still present in vast amounts and relatively hydrogen-rich, but is nevertheless non-metabolizable and becomes the limiting factor for bacterial sulphate reduction. According to mass balance calculations 90-99% of the OM produced in the photic zone was remineralized and 1-3% was consumed by microbial sulphate reduction. The aerobic and anaerobic processes have greatly affected degradation and conservation of OM.

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Hydrocarbon gases (methane, ethane, propane, isobutane, n-butane, ethene, and propene) are present in Tertiary and Quaternary shelf, upper-slope, and lower-slope deposits of the Peruvian continental margin. Methane dominates the composition of the hydrocarbon gas at all 10 sites examined during Ocean Drilling Program (ODP) Leg 112. Generation of methane is regulated by the amount of sulfate in pore water. Wherever sulfate concentrations approach or equal zero, methane concentrations increase rapidly, reaching values near 100,000 µL/L of wet sediment at eight of the 10 sites. Methane at all 10 sites results from methanogenesis, which is inhibited where sulfate is present and microbial reduction of sulfate occurs. Hydrocarbon gases heavier than methane also are present, but at much lower concentrations than methane. These hydrocarbons are thought to result from early thermal and microbial diagenesis, based on relative gas compositions and trends of concentrations with depth. With few exceptions, the results obtained in the shipboard and shore-based laboratories are comparable for methane and ethane in sediments of Leg 112. Reanalyses of canned sediments from ODP Leg 104 and from Deep Sea Drilling Project (DSDP) Legs 76 and 84 show that gas samples can be stored for as long as 8 yr, but the amounts of individual hydrocarbon gases retained vary. Nevertheless, the trends of the data sets with depth are similar for fresh and stored samples.

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Planktonic foraminifers were studied from 213 samples collected during Leg 112 at 10 sites located on the continental shelf and slope off Peru. Because planktonic foraminifers occur discontinuously downcore, detailed biostratigraphic zonation was not defined. However, it was possible to distinguish early and middle Eocene, early and late Miocene, Pliocene, and Pleistocene sediments on the basis of the planktonic foraminifers. The oldest sediments of Zone P6 of early Eocene age were obtained from the basal part of Hole 688E, which was penetrated to 779.0 m below seafloor (bsf). A biosiliceous facies of the area predominates above the N6-N7 zonal interval of early Miocene age. All sites are within the present coastal upwelling area off Peru, and many of the late Pliocene and Pleistocene assemblages are similar to those that are characteristic of modern upwelling areas. The core samples differ, however, by having a predominance of cold-water elements, such as Neogloboquadrina incompta and N. pachyderma. Warm-water species are prevalent at some horizons in the cores, suggesting shifts of the coastal upwelling centers or warmer climatic events.

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Com este trabalho pretendeu contribuir-se para o conhecimento sobre a otite causada por Malassezia pachydermatis através de um estudo de prevalência de malasseziose auricular em cães. Esta dissertação foi desenvolvida no âmbito do estágio curricular do Mestrado Integrado de Medicina Veterinária da Universidade Lusófona de Humanidades e Tecnologias que se realizou entre Setembro de 2009 e Fevereiro de 2010 no Hospital Veterinário SOSVET em Almada. As percentagens de presença de Malassezia, independentemente do tamanho da população fúngica, em animais saudáveis (36,11%) e em animais com otite externa (85,29%) estão em concordância com estudos anteriores. A maior prevalência de malasseziose (em termos de sobrecrescimento de Malassezia) em animais com sinais de otite (79,41%) e animais com orelhas pendulares (31,65%), assim como a aparente susceptibilidade da raça Cocker spaniel também são aspectos referidos em estudos anteriores. O estudo permitiu evidenciar uma relação estatisticamente relevante entre a presença de otite e o sobrecrescimento de Malassezia, porém não ficou provada a relação entre a ocorrência de sobrecrescimento de Malassezia com a idade, sexo, tipo de orelha ou história clínica. Este estudo permitiu verificar que nenhum dos dois ouvidos estava particularmente predisposto ao sobrecrescimento, que 35,42% dos animais com presença de Malassezia auricular tinham tamanhos de população diferentes entre ouvidos e que os cocos eram as principais bactérias associadas a Malassezia nos ouvidos. O estudo também deixou perceber como pode ser complicada e subjectiva a avaliação de citologias auriculares face à ausência de consenso sobre valores de referência.

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En los últimos 5 anos hemos tratado 112 casos de toxoplasmosis. La mayor parte presentaba abortos o coriorretinitis; algunos presentaban meningo-encefalitis, miocarditis y otras formas. Ocho por ciento de los pacientes presentaban dos cuadros anatomoclínicos de toxoplasmosis. Se administro en forma alterna pirimetamina, sulfametopirazina o espiramicina durante períodos prolongados, practicando reacción de Sabin y Feldman cada tres meses. La meta es negativizar la prueba serológica, la cual generalmente logramos. Clinicamente se aprecia curación al observar la desaparición de los fenômenos inflamatorios en el fondo del ojo, la desaparición de adenopatías u otros signos clínicos, ó el desarrollo de embarazos normales con productos normales en mujeres abortadoras. Considerando los graves problemas que hemos visto en hijos de madres con toxoplasmosis, preferimos tratar a éstas antes de nuevos embarazos.

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Cento e doze aidéticos ou não com neurocriptococose, admitidos no Hospital Emílio Ribas - São Paulo, Brasil, receberam anfotericina B (AMB) - grupo III ou a associação AMB/ 5 fluorcitosina (5FC): grupos I e II. Testes de Goodman aplicados revelaram: 1. leuco e glicorraquia semelhantes nos três grupos eproteinorraquia inferior a 85mg/dlapós 1, 5g/AMB; 1. a coloração pelo método da tinta da China e a cultura para Cryptococcus neoformans, positivas até l,Og/AMB; 3. hipocalemia na monoterapia, hipo e hipercalemia durante a associação; 4. as reações adversas mais evidentes a > 0,7gAMB/250g 5FC; 5. óbitos (precoce e tardio) frequentes no grupo 1 e nos grupos I e III entre 2,5 a 4,0g de AMB; 6. remissão e morte semelhantes nos grupos. A associação terapêutica iniciale amanutençãopelo AMB conduziram à recaída tardia

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L’objectiu principal d’aquest estudi consisteix a determinar quines implicacions té en l’ordenament jurídic civil català l’aprovació de la Directiva 2008/122, del Parlament Europeu i del Consell, 14.1.2009, relativa a la protecció dels consumidors respecte a determinats aspectes dels contractes d’aprofitament per torn de béns d’ús turístic, d’adquisició de productes de vacances de llarga durada, de revenda i d’intercanvi.