Chemistry of interstitial waters of ODP Leg 112 samples

Two distinct hydrogeochemical regimes currently dominate the Peruvian continental margin. One, in shallower water (150-450 m) shelf to upper-slope regions, is characterized by interstitial waters with strong positive chloride gradients with depth. The maximum measured value of 1043 mM chloride at Site 680 at ITS corresponds to a degree of seawater evaporation of ~2 times. Major ion chemistry and strontioum isotopic composition of the interstitial waters suggest that a subsurface brine that has a marine origin and is of pre-early Miocene "age," profoundly influences the chemistry and diagenesis of this shelf environment. Site 684 at ~9°S must be closest to the source of this brine, which becomes diluted with seawater and/or interstitial water as it flows southward toward Site 686 at ~13?S (and probably beyond) at a rate of approximately 3 to 4 cm/yr, since early Miocene time. The other regime, in deep water (3000-5000 m) middle to lower-slope regions, is characterized by interstitial waters with steep negative and nonsteady-state chloride gradients with depth. The minimum measured value of 454 mM chloride, at Site 683 at ITS, corresponds to ~20% dilution of seawater chloride The most probably sources of these low-chloride fluids are gas hydrate dissociation and mineral (particularly clay) dehydration reactions. Fluid advection is consistent with (1) the extent of dilution shown in the chloride profiles, (2) the striking nonsteady-state depth profiles of chlorides at Sites 683 and 688 and of 87Sr/86Sr ratios at Site 685, and (3) the temperatures resulting from an average geothermal gradient of 50°C/km and required for clay mineral dehydration reactions. Strontium isotope data reveal two separate fluid regimes in this slope region: a more northerly one at Sites 683 and 685 that is influenced by fluids with a radiogenic continental strontium signature, and a southerly one at Sites 682 and 688 that is influenced by fluids with a nonradiogenic oceanic signatures. Stratigraphically controlled fluid migration seems to prevail in this margin. Because of its special tectonic setting, Site 679 at ITS is geochemically distinct. The interstitial waters are characterized by seawater chloride concentrations to -200 mbsf and deeper by a significantly lower chloride concentration of about two-thirds of the value in seawater, suggesting mixing with a meteoric water source. Regardless of the hydrogeochemical regime, the chemistry and isotopic compositions of the interstitial waters at all sites are markedly modified by diagenesis, particularly by calcite and dolomite crystallization.

Evaluation of Postpolymerization as a Function of the Storage Time of Triethylene Glycol Dimethacrylate/2,2-Bis[4-(2-Hydroxy-3-Methacryloxy-Prop-1-Oxy)-Phenyl]-propane Bisphenyl-alpha-Glycidyl Ether Dimethacrylate Copolymers Used in Dental Resins by Differential Scanning Calorimetry and Dynamic Mechanical Analysis

The aim of this work was to evaluate the effect of the storage time on the thermal properties of triethylene glycol dimethacrylate/2,2-bis[4-(2-hydroxy-3-methacryloxy-prop-1-oxy)-phenyl]propane bisphenyl-alpha-glycidyl ether dimethacrylate (TB) copolymers used in formulations of dental resins after photopolymerization. The TB copolymers were prepared by photopolymerization with an Ultrablue IS light-emitting diode, stored in the dark for 160 days at 37 degrees C, and characterized with differential scanning calorimetry (DSC), dynamic mechanical analysis (DMA), and Fourier transform infrared spectroscopy with attenuated total reflection. DSC curves indicated the presence of an exothermic peak, confirming that the reaction was not completed during the photopolymerization process. This exothermic peak became smaller as a function of the storage time and was shifted at higher temperatures. In DMA studies, a plot of the loss tangent versus the temperature initially showed the presence of two well-defined peaks. The presence of both peaks confirmed the presence of residual monomers that were not converted during the photopolymerization process. (C) 2009 Wiley Periodicals, Inc. J Appl Polym Sci 112: 679-684, 2009

Carbon and Sulphur concentrations of sediments from Peru, Oman and Benguela upwelling environments

Abundances of organic carbon, sulfur, and reactive iron in sediments of three upwelling environments (Peru, Oman and Benguela) suggest that organic carbon/reduced sulfur ratios (C/S-ratios) in this category of marine sediments deviate considerably from previously established empirical ratios in normal marine sediments. To clarify the discrepancies, we investigated those components of the diagenetic system that limit the formation of pyrite: sulfate concentrations and reduction rates in pore waters, availability of reactive iron, and the quantity and quality of organic matter. All three limitations are evident in our sample pools. The results suggest that C/S-ratios in recent and fossil marine sediments rich in organic matter may be unsuitable as paleoenvironmental indicators.

Hydrocarbon gases in Tertiary and Quaternary sediments offshore Peru

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.

Malasseziose Auricular Canina : estudo de Prevalência em 112 cães num hospital Veterinário em Almada

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.

Tratamiento de la toxoplasmosis, observaciones en 112 pacientes

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.

Estudo retrospectivo terapêutico da neurocriptococose em 112 aidéticos ou não

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