Submitted by Haroudo Xavier Filho (haroudo.xavierfo@ufpe.br) on 2016-07-01T12:51:52Z No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) TESE_Gaspar_FL_2015.pdf: 3846981 bytes, checksum: 5c71e8dea7a17180048b9ef119b20236 (MD5) / Made available in DSpace on 2016-07-01T12:51:52Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) TESE_Gaspar_FL_2015.pdf: 3846981 bytes, checksum: 5c71e8dea7a17180048b9ef119b20236 (MD5) Previous issue date: 2015-10-28 / CAPES / A plataforma continental Pernambucana é caracterizada pela oligotrofia e estabilidade térmica ao longo do ano influenciada pela corrente Norte do Brasil, que traz águas quentes e ricas em CO2 para a plataforma continental do nordeste brasileiro. Dentre os principais rios translitorâneos de Pernambuco estão os Rios Capibaribe e Jaboatão que recebem os efluentes domésticos do Recife e região metropolitana, o que causa alterações nos ciclos naturais do carbono. Desta maneira, foram avaliadas a variabilidade da pCO2 nos estuários do Capibaribe e de Barra de Jangadas assim como na plataforma continental interna do Estado de Pernambuco. Para análise nos estuários foram realizadas coletas durante a maré baixa, bimestralmente de Novembro de 2010 a Setembro de 2011. O estuário do Capibaribe apresentou os valores mais elevados de alcalinidade total (AT) e carbono inorgânico total (TCO2), com diferença significativa entre os dois rios. As médias anuais de alcalinidade encontradas foram 1649 ± 390 μmol kg-1 no Capibaribe e 1557±315 μmol kg-1 em Barra de Jangadas. Em relação a pCO2, os estuários apresentaram supersaturação de CO2 em relação a atmosfera durante todo o ano, com médias de 3317 ± 2034 μatm no Capibaribe e 6018 ± 4589 μatm em Barra de Jangadas. Estes valores durante o período chuvoso variaram entre os estuários, com diminuição na pCO2 no Capibaribe e aumentos de até 300% dos valores de pCO2 em Barra de Jangadas. A fim de se obter uma melhor avaliação da distribuição espacial da pCO2 na plataforma interna, foi construído um equipamento para a medição contínua e direta da pCO2 na água como alternativa de baixo-custo em relação aos fabricados importados. A primeira campanha realizada aconteceu em Dezembro de 2014, partindo do porto do Recife em direção ao estuário de Barra de Jangadas. Apesar de o período seco ser o de maior produtividade primária a região apresentou-se oligotrófica, com picos de chl-a (8.4 mg m3) próximo ao Capibaribe. Apenas uma pequena área apresentou subsaturação de CO2 em relação à atmosfera, com o valor mínimo registrado de 376,6 μatm. Foi identificada uma elevada fugacidade de CO2 (fCO2) na área da plataforma interna, com média de 474,33 ± 66,57 μatm, resultando em um fluxo médio para a atmosfera de 8,5 ± 6,82 mmol C m-2d-1. A partir dos resultados obtidos foi proposto um modelo para predizer a fCO2 a partir de valores de salinidade e temperatura para a plataforma interna durante o verão. Uma análise espacial e sazonal mais abrangente dos parâmetros do sistema carbonato na plataforma interna foi realizada utilizando-se dados de AT e TCO2 em áreas com e sem influência de rios entre os anos de 2013 e 2014. As médias da pCO2 e do pH na plataforma interna foram de 449 ± 45 μatm e 8,00 ± 0,03 respectivamente. Os parâmetros analisados foram influenciados pela distância da costa, o que resultou na elaboração de modelos para a predição de AT, TCO2, pCO2, pH, ΩCa e ΩAr a partir de dados de temperatura, salinidade e longitude. A região apresenta elevada alcalinidade inclusive na área influenciada por rios, onde foi encontrada a menor média de AT 2358 ± 28 μmol kg-1. A região apresenta, em curto prazo, baixa vulnerabilidade ao processo de acidificação oceânica. Os valores encontrados de pCO2 e fluxos de CO2 na plataforma continental de Pernambuco estão acima dos estimados nas médias globais para plataformas continentais abertas baseadas em modelos matemáticos. A variabilidade na pCO2 encontrada está ligada à própria característica da água tropical do Atlântico Sul, que cobre a rasa plataforma pernambucana com águas quentes. Onde a baixa solubilidade do CO2 devido à alta temperatura, associada à oligotrofia e aportes de matéria orgânica fazem com que a região da plataforma seja fonte de CO2 para atmosfera durante todo o ano. / The continental shelf of Pernambuco is characterized by oligotrophy and thermal stability throughout the year, influenced by the North Brazil current that brings warm water, rich in CO2 to the continental shelf of northeastern Brazil. The Capibaribe and Jaboatão rivers are one of the major rivers of Pernambuco. They receive a large input of domestic effluents from Recife and its metropolitan area, which causes changes in the natural carbon cycle. Here we evaluated the pCO2 variability in these two estuaries and in the inner shelf area of Pernambuco. To evaluate the role of the estuaries, samples were collected bimonthly during low tide, on a seasonal cycle from November 2010 to September 2011. The Capibaribe estuary presented the highest values of total alkalinity (TA) and total inorganic carbon (TCO2), with a significant difference between the two rivers. Both estuaries showed seasonal variation in TCO2 and TA values. The annual TA averages were 1649 ± 390 μmol kg-1 in the Capibaribe and 1557 ± 315 μmol kg-1 at Barra de Jangadas. Regarding the pCO2, the estuaries were saturated in CO2 throughout the year, with average for the dry season of 3317 ± 2034 μatm in the Capibaribe and 6018 ± 4589 μatm in Barra de Jangadas. These values varied seasonally between estuaries, with a pCO2 decrease during the rainy season in the Capibaribe, and an increase of up to 300% in the Barra de Jangadas estuary. In order to obtain a better evaluation of the spatial distribution of pCO2 over the shelf waters, it was developed an equipment for the continuous and direct measurement of sea surface pCO2 as low-cost alternative to the commercially manufactured ones. The first cruise took place in December 2014, starting from the port of Recife towards the Barra de Jangadas estuary. Even though the dry period has shown the highest primary productivity, the region presented itself as oligotrophic, with peaks of chl-a (8.4 mg m3) under influence of the Capibaribe plume. Only a small area showed CO2 subsaturation to the atmosphere, with the minimum value of 376.6 μatm. In general, a high CO2 fugacity (fCO2) was identified in the entire area of the inner shelf, with average of 474.33 ± 66.57 μatm, resulting in an mean flux to the atmosphere of 8.5 ± 6.82 mmol C m-2 d-1. It was proposed a model to predict the fCO2 using salinity and temperature values for inner the shelf during the summer. A more comprehensive spatial and seasonal distribution of the carbonate parameters was conducted by using values of TA TCO2 in areas subjected and non-subjected to riverine inputs during 2013 and 2014. The area presents a relative stability to what concerns the pCO2 and pH distribution, with overall average values of 449 ± 45 μatm and 8.00 ± 0,03 respectively. In general, the parameters analyzed were influenced by the distance from the coast, resulting in the development of prediction models for TA, TCO2, pCO2, pH, ΩCa and ΩAr using temperature, salinity and longitude data. The area has a low vulnerability to ocean acidification process, the TA is high even in the areas under riverine influence, where the lowest average values was registered 2358 ± 28 μmol kg-1. The values of pCO2 and CO2 fluxes found on the continental shelf of Pernambuco are above those expected on global averages estimated by mathematical models for open continental shelf. The variability in pCO2 found is linked to the own characteristic of the South Atlantic tropical water, which covers the shallow Pernambuco platform with warm waters. The low solubility of CO2 due to high temperature, combined with oligotrophy and the transport of organic matter to be respired outside the estuaries, turns the continental shelf into a source of CO2 to the atmosphere throughout the year.

Submitted by Fabio Sobreira Campos da Costa (fabio.sobreira@ufpe.br) on 2017-04-26T16:06:29Z No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Tese_Pinheiro_BR_2016_PPGO_UFPE.pdf: 4797187 bytes, checksum: 23d620ab5ad4e454bcb109d992f47da5 (MD5) / Made available in DSpace on 2017-04-26T16:06:29Z (GMT). No. of bitstreams: 2 license_rdf: 1232 bytes, checksum: 66e71c371cc565284e70f40736c94386 (MD5) Tese_Pinheiro_BR_2016_PPGO_UFPE.pdf: 4797187 bytes, checksum: 23d620ab5ad4e454bcb109d992f47da5 (MD5) Previous issue date: 2016-08-30 / O aumento da pressão parcial de dióxido de carbono (pCO2) na atmosfera, que passou de uma média de 280ppm antes da revolução industrial para acima de 400ppm nos dias atuais, é um dos principais responsáveis por uma série de mudanças globais. Entre elas, a elevação da temperatura superficial da água do mar (TSM), a elevação do nível do mar, e a acidificação oceânica (AO). Os ambientes recifais têm sido apontados como os mais vulneráveis a estas mudanças. Efeitos da elevação da pCO2 sob ambientes recifais no Atlântico Sul, são escassos e na sua maioria reportam apenas efeitos da elevação da TSM e eventos de branqueamento. O Atol das Rocas é a primeira Reserva Biológica marinha do Brasil e foi escolhido neste estudo por ser um exemplo de recife biogênico, oceânico e praticamente livre de impactos como sobrepesca, poluição, e turismo desordenado. Desta forma, o objetivo do presente estudo foi avaliar os efeitos da elevação da pCO2 atmosférica sob os organismos construtores do atol para estabelecer um ponto de referência para futuras comparações, devido a sua vulnerabilidade a estes processos. A pesquisa foi dividida em três etapas, sendo essas a caracterização, a avaliação do estado e a experimentação dos prováveis efeitos da acidificação nos organismos calcários. Inicialmente são apresentados dados sobre a cobertura bentônica e a sua interação com os parâmetros abióticos (temperatura, salinidade, disponibilidade de nutrientes dissolvidos, pH e alcalinidade total). Foi observada dominância de macro e tufos de algas em locais com maior disponibilidade de nutrientes dissolvidos, indicando que maiores concentrações de nutrientes inorgânicos na água do mar contribuem para a distribuição dos organismos no atol. E, além disso, ambientes com alta frequência de organismos carbonáticos foram associados com uma diminuição da concentração de alcalinidade. Em seguida, dados foram obtidos sobre reprodução, crescimento e distribuição de frequência da população da espécie de coral dominante nas piscinas do atol (Siderastrea stellata). Foi observado um evento de planulação e o crescimento inicial dos pólipos primários, os quais, após 3 meses mostraram uma média de diâmetro de 1,49±0,45 mm, variando entre 0,9 e 2,28 mm e 14,70% de taxa de mortalidade. A média da taxa de extensão anual das colônias adultas foi de 6,8 ± 0,7 mm. ano-1. Colônias com 4,1 a 10 cm de diâmetro também foram frequentes no atol (48,1±14,5%). A população de S. stellata no atol mostra-se com um alto potencial de manutenção e recuperação, embora tenha sido observado uma baixa taxa de recrutamento. Na outra etapa do estudo se fez uma caracterização do sistema carbonato no atol, avaliando a influência do metabolismo dos organismos sob as variações espaço-temporais observadas. Os resultados indicaram uma grande disponibilidade de carbonato dissolvido nas piscinas do atol. Os índices de saturação de aragonita não só suprem as necessidades metabólicas dos organismos, como estão acima dos observados para outros ambientes recifais. Desta forma, é possível que a intensa atividade biológica no atol das rocas possa servir como um tampão adicional para o equilíbrio do pH e mitigar alguns dos efeitos da acidificação oceânica localmente. Por fim, foi realizado um experimento com espécies que ocorrem no atol, o coral scleractíneo Porites astreoides e o zoantídeo Palythoa caribaeorum. Foram avaliadas as respostas fisiológicas (crescimento, respiração, fotossíntese, lipídios totais e clorofila a) desses organismos mediante condições de estresse térmico e acidificação. P. astreoides sofreu influência do aquecimento e da acidificação em todas as taxas metabólicas avaliadas, enquanto o P. caribaeorum teve um menor, ou nenhum impacto no seu metabolismo. / The increase in carbon dioxide partial pressure (pCO2) in the atmosphere, which rose from an average of 280 ppm before pre-industrial times to over 400 ppm today, it is one of the main responsible for a series of global changes. Among them, increasing sea surface temperature (SST), sea level rise and ocean acidification (OA). Coral reefs have been identified as the most vulnerable ecosystem to these changes. Investigations about the effects of elevated anthropogenic pCO2 on coral reef environments in the South Atlantic are scarce and mostly only effects of the increase of SST and bleaching events were reported. Rocas Atoll is the first Marine Biological Reserve in Brazil and was chosen in this study because it is an example of a oceanic biogenic reef, and virtually free from impacts such as overfishing, pollution, and unregulated tourism. Thus, the aim of this study was to evaluate the effects of increased atmospheric pCO2 on the atoll building organisms to establish a benchmark for future comparisons, because of their vulnerability to these processes. Initially are presented data on the benthic cover and its interaction with the abiotic parameters (temperature, salinity, availability of dissolved nutrients, pH and total alkalinity). It was observed a dominance of macro and tuff algae in places with higher availability of dissolved nutrients, indicating that higher concentrations of inorganic nutrients in seawater contribute to the spatial distribution of organisms on the atoll. And besides, environments with high frequency of carbonate organisms were associated with a decrease of alkalinity. Then, data were obtained on reproduction, growth and frequency distribution of the population of the dominant coral species in the atoll pools (Siderastrea stellata). A planulation event was observed and initial growth of primary polyps which, after 3 months showed 1.49 ± 0.45 mm average diameter ranging between 0.9 and 2.28 mm and 14.70% mortality rate. The average annual extension rate of adult colonies was 6.8 ± 0.7 mm. year-1. Colonies with 4.1 to 10 cm diameter were also common in the atoll (48.1 ± 14.5%). The population of S. stellata in the atoll shows a high potential for maintenance and recovery, although it was observed a low recruitment rate. In another stage of the study, a characterization of the carbonate system of the atoll was made, in order to assess the influence of the metabolism of organisms under spatio-temporal variations. The results indicated a large availability of dissolved carbonate in the atoll pools. The aragonite saturation rates not only supply the metabolic demands of the corals, but are above those observed for other coral reef environments. Thus, it is possible that the intense biological activity of the Rocas Atoll can serve as an additional buffer for the pH equilibrium and locally mitigate some of the effects of ocean acidification. Finally, an experiment was conducted with species that occur in the atoll, the scleractinian coral Porites astreoides and the zoanthid Palythoa caribaeorum. The physiological responses of these organisms were evaluated (growth, respiration, photosynthesis, total lipids and chlorophyll a) under conditions of heat stress and acidification. P. astreoides was influenced by warmer temperatures and acidification in all measured metabolic rates while P. caribaeorum showed a minor or no impact on your metabolism.

Submitted by Mario BC (mario@bc.ufrpe.br) on 2017-04-26T12:32:52Z No. of bitstreams: 1 Thiago Arcoverde Maciel.pdf: 2765936 bytes, checksum: b2a040b8c8b92a2259f8f141af305868 (MD5) / Made available in DSpace on 2017-04-26T12:32:52Z (GMT). No. of bitstreams: 1 Thiago Arcoverde Maciel.pdf: 2765936 bytes, checksum: b2a040b8c8b92a2259f8f141af305868 (MD5) Previous issue date: 2015-02-27 / Conselho Nacional de Pesquisa e Desenvolvimento Científico e Tecnológico - CNPq / Urolithiasis is a metabolic disease of complex and multifactorial etiology, characterized by uroliths formation in the urinary system. It becomes clinically important when obstruction occurs, with little chance of reversal, and prevention is the best option for maintaining the integrity of the reproductive capacity. For this, one must know the biochemical profile of animals and fix the possible factors that may be related to the formation of uroliths. Morphometric study in turn, enables the comparative observation and description of changes and can therefore be used as a method of diagnostic. Urinary acidification is cited as an efficient alternative for the prevention, so vitamin C was used. In this study, 20 healthy sheep, male (not neutered), Santa Ines breed, aged approximately 90 days, were divided into three groups (G1 n=7 - calculogenic diet without vitamin C, G2 n=7 - calculogenic diet with vitamin C and G3 n=6 - control). To analyze the biochemical profiles groups 1 and 2 were compared and the morphometric analysis the three groups were compared. Animals were examined weekly, allowing direct observation of clinical signs, such as prostration/restlessness, penile exposure, abdomen kicking, urethral process congestion, among others. Analysis of biochemical profiles of urine and serum revealed hyperproteinemia (8.99g/dL) and proteinuria (43.82g/dL) in 57.14% aciduria (G1) and 71.43% (G2) and the presence of erythrocytes, leukocytes, bacteria and sperm to the urinary sediment. There was an important increase of phosphorus and magnesium e there was a substantial decrease of calcium which was present in 50% of uroliths samples analyzed. At the end of the experimental time animals were slaughtered and necropsy of them was followed by morphometry of the organs of the urinary system. Necrosis of urethral process and bladder with extensive bleeding area were observed during the necropsy procedure. The width of the kidneys and ureters were higher in G2, which may have contributed to lower retention of uroliths on this site. / Urolitíase é uma doença metabólica de etiologia complexa e multifatorial, caracterizada pela formação de urólitos no sistema urinário. Torna-se clinicamente importante quando ocorre obstrução, havendo poucas chances de reversão do quadro, sendo a prevenção a melhor opção para manutenção da capacidade reprodutiva. Para isso, deve-se conhecer o perfil bioquímico dos animais e corrigir os possíveis fatores que estão relacionados à formação dos urólitos. O estudo morfométrico por sua vez, possibilita a observação comparativa e descrição de alterações podendo ser empregado como método de auxílio diagnóstico. A acidificação urinária é citada como alternativa eficiente para a prevenção, por isso a vitamina C foi utilizada. Nesse estudo foram utilizados 20 ovinos hígidos, da raça Santa Inês, machos (não castrados), com idade aproximada de 90 dias, distribuídos em três grupos (G1 n=7 – dieta calculogênica sem vitamina C, G2 n=7 – dieta calculogênica com vitamina C e G3 n=6 – controle). Para análise dos perfis bioquímicos foram confrontados os grupos 1 e 2, e para a morfometria foram comparados os três grupos. Os animais foram examinados semanalmente, permitindo a imediata observação dos sinais clínicos, como prostração/inquietação, exposição peniana, escoiceamento do abdômen, congestão de processo uretral. A bioquímica sérica e urinária revelou hiperproteinemia (8,99g/dL) e proteinúria (4,38g/dL), acidúria em 57,14% (G1) e 71,43% (G2) e presença de hemácias, leucócitos, bactérias e espermatozóides ao exame do sedimento urinário. Houve elevação expressiva do fósforo e do magnésio e diminuição substancial do cálcio que esteve presente em 50% das amostras de urólitos analisadas. Ao término do experimento foi realizado o abate e necropsia dos animais seguindo-se a morfometria dos órgãos do sistema urinário. Necrose de processo uretral e bexiga repleta com extensa área de hemorragia foram observados durante necropsia. Os rins e ureteres apresentaram valores morfométricos distintos entre os grupos, sendo maiores no G2, o que pode ter contribuído para uma menor retenção de cálculos neste local.

This thesis presents temporal perspectives of lake acidification in Sweden. Sediment records have been used to study timing, trends and causes of acidification, and two different techniques for assessing past lake-water acidity are presented. A new technique for pH prediction, based on near-infrared (NIR) spectroscopy of surface sediments, is developed. This study shows that there is a pH related fraction of lake sediments that can be recorded by NIR analysis. Relationships between NIR spectra of surface sediment samples and measured lake-water pH values, and between NIR spectra of sediment cores and historical pH values inferred by diatom analysis, are modelled by partial least squares regression. The prediction errors of the models are comparable to those obtained by modelling of diatom and lake-water pH data. By further development NIR spectroscopy can become useful for inferring past pH, as well as several other lake-water parameters, from sediment cores. Diatom-based predictive models, using multivariate calibration methods, are developed for inferences of lake-water pH, alkalinity and colour. These models are used to provide a regional assessment of recent lake acidification in the provinces of Västerbotten and Norrbotten, northern Sweden. The study shows that a pH decline has occurred in some southeastern lakes, but that most of the lakes have not faced significant changes in lake-water pH, alkalinity and colour. The inferred water chemistiy changes are discussed in relation to atmospheric deposition and land-use. In a study of eight acid-sensitive Swedish boreal-forest lakes a past-analogue approach is used to test whether contemporary expansion of conifers could cause lake acidification. Water chemistry changes associated with the natural pre-historic colonization and expansion of spruce in Sweden (≈3000 years B.P.), at times of background atmospheric acidity, are inferred to evaluate the acidification ability of spruce per se on surface waters. This study shows that under natural, unpolluted conditions spruce colonization and expansion did not cause lake acidification. In a synthesis of palaeolimnological acidification research in Sweden a general model for pH- development for acid clear-water lakes in southern Sweden is presented. The pH-development from the last deglaciation to present time can be divided into four different periods; (i) a natural long-term acidification period (12000 B.P. - 2300 B.P., or later), with a gradual decrease in pH resulting from declining fluxes of base cations from catchment soils; (ii) a human induced alkalization period (2300 B.P. - 1900 A.D.), with a pH increase due to human activities in the catchments; (iii) the recent acidification period (about 1900 A.D. - present), when pH decreased towards 4.5 due to acid deposition and possibly ceased land-use; and (iv) the liming period (1970s - present), when pH often increases to values above 7 following lime treatment to counteract acidification. The implications of these past pH changes for the concept of contemporary lake acidification and for liming policy are outlined. / digitalisering@umu

I explored the importance of decaying wood to survival and growth of trees in south coastal British Columbia, and the effect of decaying wood on the intensity of podzolization on mesic sites. A field pot study was carried out in both high light and low light conditions using woody and non-woody forest floor materials. After two growing seasons, Pseudotsuga menziesii, Tsuga heterophylla, and Abies amabilis seedlings growing in clearcuts had greater survival and growth in the non-woody substrate; however, in the understory, the effect was much less. The proliferation of western hemlock roots was used as an indicator of the value of decaying wood to trees. In both greenhouse trials (using seed sown on a series of planting pots with each half filled with either a woody substrate or a non-woody substrate), and in field sampling of woody and non-woody substrates in mature stands, the non-woody substrate had a larger density of fine and very fine roots compared to the woody substrates or mineral soil. Ten litres of concentrated solutions of non-woody humus substrate and woody substrates were leached through soil columns. Both the non-woody and woody solutions had similar mean pH but significantly different chemical properties. The non-woody solution leachate had greater net average output of dissolved organic C, Fe, and Mn. The mineral soil treated with the nonwoody solution had significantly greater concentrations of total N and pyrophosphate-extractable Fe. In the field, forest floor and soil samples were compared between pedons having large accumulation of decaying wood and pedons with non-woody humus forms. Despite large and significant differences in chemical properties between the two substrates, there were generally no significant differences between the chemical properties of the soils directly under these substrates. In most cases, the results of (3-analyses showed that the means were not pedologically different. Additionally, 18 pairs of zero tension plate lysimeters were installed under the two substrates. The lysimeter solutions showed no significant differences. I concluded that coarse woody debris appears not to have either a positive effect of increased productivity of trees or a negative effect of increased intensity of podzolization. / Forestry, Faculty of / Graduate

Made available in DSpace on 2016-01-26T18:55:44Z (GMT). No. of bitstreams: 1 Mozart Alves Goncalves Filho.pdf: 823168 bytes, checksum: 9a480c850a219c880f8d278e6850d549 (MD5) Previous issue date: 2015-06-26 / Cancer is a universal disease, with high mortality rates in some cases. It is the second leading cause of death in the Western world, and go to the first place around the year 2020. Cancer has genetic and environmental causes, one of them the ingestion of heavy metals such as cadmium. There are few studies evaluating the gastrointestinal toxicity of cadmium. There is no consensus in the literature on the treatment of cadmium toxicity. We need simple methods to avoid its effects. Objective: The objective of this study was to evaluate the lesions caused by cadmium poisoning in the digestive tract and the possible effect of the drinking water pH in the initiation of these lesions. Methods: For this study, 90 male Wistar rats were used, divided into 6 groups: A - 15 rats that received 400 mg / L cadmium chloride (CdCl2) in drinking water at a neutral pH of 7.0; B - 15 rats that received CdCl2 (400 mg / L) in drinking water at an acidic pH of 5.0; C - 15 rats that received CdCl2 (400 mg / L) in drinking water at a basic pH of 8.0; D - 15 rats that received water at an acidic pH of 5.0; E - 15 rats that received water at a basic pH of 8.0; and F - 15 rats that received water at a neutral pH of 7.0. All animals were euthanized after 6 months. Fragments of the esophagus, stomach, small intestine and large intestine of each rat were removed for microscopic analysis. Results: There were microscopic changes neither in the esophagus nor in the small and large intestine. Only cadmium exposed animals showed mild dysplasia of the gastric mucosa (p= 0.012), regardless of the pH (p> 0.05). Conclusion: The cadmium led to the formation of dysplastic lesions in the gastric glandular epithelium, regardless of water pH. / Câncer é uma doença universal, com taxa de mortalidade elevada em alguns casos. É a segunda causa de morte no mundo ocidental, e passará para primeiro lugar por volta do ano de 2020. Tem causas genéticas e ambientais, sendo uma delas a ingestão de metal pesado, como cádmio. Há poucos estudos avaliando a toxicidade gastrointestinal do cádmio. Não há consenso na literatura sobre o tratamento da toxicidade por cádmio. Há necessidade de métodos simples de evitar seus efeitos. Objetivo: O objetivo deste estudo foi avaliar as lesões causadas por intoxicação por cádmio no aparelho digestório e os possíveis efeitos do pH da água na gênese destas lesões. Material e métodos: Para este estudo, foram utilizados 90 ratos Wistar, machos. Os animais foram distribuídos em 6 grupos (n=15): A solução de cloreto de cádmio (400mg/L) na água de beber com pH neutro (pH 7,0); B solução de cloreto de cádmio (400mg/L) na água de beber com pH ácido (pH 5,0); C solução de cloreto de cádmio (400mg/L) na água com pH básico (pH 8,0). D água de beber com pH ácido (pH 5,0); E água de beber com pH básico (pH 8,0); F água com pH neutro (pH 7,0). Animais de todos os grupos foram eutanasiados após 6 meses. Foram retirados fragmentos do esôfago, estômago, intestino delgado e intestino grosso de cada rato para análise microscópica. Resultados: Não foram observadas alterações microscópicas no esôfago nem no intestino delgado e grosso. Somente animais expostos ao cádmio apresentaram displasia leve da mucosa gástrica (p= 0,012), porém sem diferença com relação aos diferentes pH da água (p>0,05). Conclusão: O cádmio levou a formação de lesões displásicas no epitélio glandular gástrico, independente do pH da água.

Made available in DSpace on 2016-07-18T17:53:15Z (GMT). No. of bitstreams: 1 Mozart Alves Goncalves Filho.pdf: 823168 bytes, checksum: 9a480c850a219c880f8d278e6850d549 (MD5) Previous issue date: 2015-06-26 / Cancer is a universal disease, with high mortality rates in some cases. It is the second leading cause of death in the Western world, and go to the first place around the year 2020. Cancer has genetic and environmental causes, one of them the ingestion of heavy metals such as cadmium. There are few studies evaluating the gastrointestinal toxicity of cadmium. There is no consensus in the literature on the treatment of cadmium toxicity. We need simple methods to avoid its effects. Objective: The objective of this study was to evaluate the lesions caused by cadmium poisoning in the digestive tract and the possible effect of the drinking water pH in the initiation of these lesions. Methods: For this study, 90 male Wistar rats were used, divided into 6 groups: A - 15 rats that received 400 mg / L cadmium chloride (CdCl2) in drinking water at a neutral pH of 7.0; B - 15 rats that received CdCl2 (400 mg / L) in drinking water at an acidic pH of 5.0; C - 15 rats that received CdCl2 (400 mg / L) in drinking water at a basic pH of 8.0; D - 15 rats that received water at an acidic pH of 5.0; E - 15 rats that received water at a basic pH of 8.0; and F - 15 rats that received water at a neutral pH of 7.0. All animals were euthanized after 6 months. Fragments of the esophagus, stomach, small intestine and large intestine of each rat were removed for microscopic analysis. Results: There were microscopic changes neither in the esophagus nor in the small and large intestine. Only cadmium exposed animals showed mild dysplasia of the gastric mucosa (p= 0.012), regardless of the pH (p> 0.05). Conclusion: The cadmium led to the formation of dysplastic lesions in the gastric glandular epithelium, regardless of water pH. / Câncer é uma doença universal, com taxa de mortalidade elevada em alguns casos. É a segunda causa de morte no mundo ocidental, e passará para primeiro lugar por volta do ano de 2020. Tem causas genéticas e ambientais, sendo uma delas a ingestão de metal pesado, como cádmio. Há poucos estudos avaliando a toxicidade gastrointestinal do cádmio. Não há consenso na literatura sobre o tratamento da toxicidade por cádmio. Há necessidade de métodos simples de evitar seus efeitos. Objetivo: O objetivo deste estudo foi avaliar as lesões causadas por intoxicação por cádmio no aparelho digestório e os possíveis efeitos do pH da água na gênese destas lesões. Material e métodos: Para este estudo, foram utilizados 90 ratos Wistar, machos. Os animais foram distribuídos em 6 grupos (n=15): A solução de cloreto de cádmio (400mg/L) na água de beber com pH neutro (pH 7,0); B solução de cloreto de cádmio (400mg/L) na água de beber com pH ácido (pH 5,0); C solução de cloreto de cádmio (400mg/L) na água com pH básico (pH 8,0). D água de beber com pH ácido (pH 5,0); E água de beber com pH básico (pH 8,0); F água com pH neutro (pH 7,0). Animais de todos os grupos foram eutanasiados após 6 meses. Foram retirados fragmentos do esôfago, estômago, intestino delgado e intestino grosso de cada rato para análise microscópica. Resultados: Não foram observadas alterações microscópicas no esôfago nem no intestino delgado e grosso. Somente animais expostos ao cádmio apresentaram displasia leve da mucosa gástrica (p= 0,012), porém sem diferença com relação aos diferentes pH da água (p>0,05). Conclusão: O cádmio levou a formação de lesões displásicas no epitélio glandular gástrico, independente do pH da água.

O palmito pode ser obtido a partir de várias espécies de palmeiras. Devido à alta taxa de exploração das palmeiras do gênero Euterpe e ao seu baixo poder de regeneração, no mercado consumidor há falta de produto de boa qualidade. Palmeiras mais precoces e que produzam bom palmito têm sido pesquisadas, uma delas é a pupunha (Bactris gasipaes), nativa da Amazônia que apresenta características de precocidade, rusticidade e perfilhamento, com palmito de ótima qualidade, diferindo dos demais pelo sabor adocicado e a coloração amarelada. O seu cultivo pode ser feito em grande parte do território brasileiro. A porção comestível do palmito de pupunha é dividida em três partes: a basal ou caulinar (coração), a apical, e a central ou foliar (creme ou tolete). O comércio de palmito privilegia a parte central da palmeira, vendendo o palmito basal como subproduto. O presente estudo tem como objetivo demonstrar a equivalência da qualidade do palmito basal e do foliar de pupunha, priorizando-se o tratamento adicional com ácido acético, que mascara o seu sabor adocicado, comparado com o ácido cítrico, largamente utilizado nas indústrias. As amostras de palmito de pupunha foram cultivadas em área experimental pertencente a ESALQ/USP; para o processamento foram cortadas 120 palmeiras em março de 2007. Foram analisadas características físicas, químicas, bioquímicas e sensoriais do palmito basal e foliar de pupunha em seis períodos de armazenamento (1, 15, 30, 60, 90, 120 dias). O controle das operações durante o processamento foi eficiente, pois o peso e o preenchimento dos vidros não variaram entre as unidades. Durante o período de armazenamento a coloração amarelada dos palmitos basal e foliar de pupunha se manteve constante. Embora as enzimas polifenoloxidase e peroxidase tenham sido detectadas nas análises bioquímicas, seus valores foram baixos, e como a coloração foi a mesma durante o armazenamento, considera-se que as enzimas foram inativadas. A composição centesimal das amostras (umidade, proteína, matéria graxa, fração cinza, fibras e carboidratos) indicou que ambos os produtos possuem as mesmas características, as quais se assemelham muito à da palmeira juçara. A análise sensorial não mostrou diferença significativa entre as amostras, porém as notas mais baixas foram atribuídas às conservas acidificadas com ácido acético. Com relação à freqüência de consumo, observou-se que o palmito de pupunha é pouco utilizado na alimentação humana, sendo a resposta às vezes predominante. Os resultados mostraram que o palmito basal e o foliar de pupunha têm as mesmas características físicas, químicas e sensoriais, indicando que o primeiro também pode ser comercializado como palmito de primeira qualidade; o período de armazenamento não alterou as principais características dos produtos. / The palm can be obtained from several palms trees. Besides of high rate of exploration of Euterpe palms trees and his low regeneration power, there is a lack of product in the consumer market. More precocious palms trees and which produce good palm heart have been investigated, one of them is the peach palm (Bactris gasipaes), native of Amazon region that presents characteristics of precociousness, rusticity and tillering with palm heart with good quality, differing of others for the slightly sweet taste and the yellowed coloration. His cultivation can be done in great part of the Brazilian territory. The edible portion of the palm is divided in three parts: basic one or caulinar (heart), apical and central or foliaceous (cream or thole). The commerce of palm privileges the central part of the palm tree, selling heart as by-product. The aim of this study was to demonstrate the equivalence of the quality of heart and thole of peach palm, acidified with citric acid, widely used in the industries, and with acetic acid that masks the slightly sweet taste. The samples of peach palm were cultivated in experimental area of ESALQ/USP and for the processing 120 palms trees were cut in march of 2007. Heart and thole of the palm were analysed by physical, chemical, biochemical and sensorial characteristics for six periods of storage (1, 15, 30, 60, 90, 120 days). The control of the operations on the processing was efficient, since the weight and the filling out from the glasses did not vary between the unities. During the period of storage the coloration of the tholes and hearts of palm peach was yellowed, characteristic that remained constant. Even though the enzymes polyphenol oxidase and peroxidase have appeared in the biochemical analyses, its values were low, and the coloration was the same during the storage. The centesimal composition of the samples (humidity, protein, oily matter, ash, fibers and carbohydrates) indicated heart and thole of peach palm have the same characteristics, which liken very much to that of the palm tree Euterpe edulis. The sensory analysis did not show significant difference between the samples, however the lowest notes were attributed to the pickles acidified with acetic acid. Regarding the frequency of consumption, it was noticed that the palm heart of peach palm is little used in the feeding of people, being the answer \"sometimes\" the one that had major constancy. Data showed that heart and the thole of peach palm have the same physical, chemical and sensory characteristics, indicating that the first one also can be marketed like palm heart of first quality; the period of storage did not change principal characteristics of the products.

The several million years preceding the Cretaceous/Paleogene (K/Pg) boundary has been the focus of many studies. Changes in ocean circulation and sea level, extinctions, and major volcanic events have all been documented for this interval. Important research questions these changes raise include the climate dynamics during the warm, but not hot, time after the decay of the Late Cretaceous greenhouse interval and the stability of ecosystems prior to the mass extinctions at the end-Cretaceous. I document several biotic perturbations as well as changes in ocean circulation during the Maastrichtian stage of the latest Cretaceous that question whether the biosphere was being preconditioned for the end-Cretaceous extinction. The first event at Shatsky Rise in the tropical North Pacific was the brief acme of inoceramid clams at ~71 Ma, followed by their abrupt extinction during the “mid-Maastrichtian event” at 70.1 Ma. The second is an intriguing dissolution event that began ~67.8 Ma at Ocean Drilling Program Site 1209 (2387 m). The dissolution event is marked by very poor planktic foraminiferal preservation and sharply reduced calcareous plankton diversity. The shift into the dissolution interval was initially gradual, then rapid. Within the late Maastrichtian dissolution interval, the planktic/benthic (P/B) ratio is low, planktic foraminifera are highly fragmented, larger taxa are mostly absent, small taxa are relatively abundant, and planktic foraminifera and nannofossil species richness are low. The event is followed by an abrupt recovery in carbonate preservation ~300 kyr prior to the K/Pg boundary. Was the dissolution event caused by a change in deep water circulation, migration of the site out of the high productivity tropical belt, or ocean acidification associated with Deccan Traps volcanism? Our data show that changing deep water masses, coupled with reduced productivity and associated decrease in pelagic carbonate flux was responsible for the dissolution interval, while Deccan Traps volcanism may have caused surface ocean acidification ~200-kyr prior to the K/Pg mass extinction event.

The aims of the thesis were to compare chemistry of the Černá Nisa stream in the Jizera Mountains (Northern Bohemia, Czech Republic) at the end of the era of strong anthropogenic acidification (in the mid-1990s) and in the period of the recent intensive chemical and biological recovery from acidification, and to study the present biota of the stream. During the year 2008, physical and chemical parameters of the water were studied, the species and age composition of ichthyofauna, and the quality and quantity of macrozoobenthos - the main component of the food for fish. Special attention was paid to the content of toxic metals (Be, Al, Cr, Mn, Fe, Co, Ni, Cu, Zn, As, Cd, Pb, Hg) in the water, main representatives of benthic organisms, and in selected tissues of brook charr. The comparison of the water chemistry with results from the years 1994, 1996, and 1997 showed a decrease in acidification, despite the unstable chemical climate during the seasons, and sulphate and nitrate concentrations still high. Since the mid 1990s, the stream has been inhabited by a stable population of brook charr (Salvelinus fontinalis), a non-native, highly acid-tolerant species, which is now dominating there. At present, also a stable population of a native species, common minnow (Phoxinus phoxinus), occurs in the stream....