945 resultados para Meiofauna, substrato secondario algale, acidificazione, vent, Ischia


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Mirocaris fortunata were sampled from the Lucky Strike hydrothermal vent area (Eiffel Tower site) on the mid-Atlantic ridge during the French DIVA 2 cruise (June 1994). Small adults (17 to 22 mm total length), although morphologically identical, could be divided into 2 categories on the basis of pigmentation, lipid composition and C-13/C-12 stable isotope ratios of fatty acids. Highly pigmented small adults (8.6 to 9.2 mu g carotenoid shrimp(-1)) contained higher levels of total lipid than similar-sized individuals containing lower levels of pigment (0.9 to 2.9 mu g carotenoid shrimp(-1)). Lipid class analysis indicated that wax esters comprised 62.5% of total lipid in the former group. These pigmented shrimp also contained high proportions of polyunsaturated fatty acids (PUFA), particularly the phototrophic microplanktonic markers 20:5(n-3) and 22:6(n-3) (14.0 and 33.5% respectively). By contrast small adults (22 mm) and adult shrimp (25 to 26 mm) with low levels of carotenoid pigmentation contained lower amounts of total lipid, little or no wax ester and low levels of 20:5(n-3) and 22:6(n-3), but did contain 16:2(n-4) and 18:2(n-4) and the non-methylene interrupted dienes 20:2 Delta 5,13 and 22:2 Delta 7,15. GC-IRMS analysis of all fatty acids and fatty alcohols in the pigmented small adults indicated delta(13)C values of -18.2 to -27.7 parts per thousand, which is consistent with a photosynthetic carbon source for these compounds. The C-13/C-12 isotope composition of fatty acids from low-pigmented small adults and adults was more variable (-12.5 to -33.1 parts per thousand) and suggests a bimodal distribution which may be attributable to differing nutritional sources or the physiological/reproductive status of these shrimp. Samples of eggs, which are carried by the female on the pleopods, represented approximately 57% of total somatic lipid which indicates a substantial reproductive investment by this species. The egg lipids comprised high proportions of triacylglycerols (64.4 to 78.0% of total lipid) whilst the fatty acid composition was dominated by the monounsaturated fatty acids 16:1(n-7), 18:1(n-7) and 18:1(n-9), which accounted for 65.7 to 33.5% of total fatty acids. By contrast, PUFA were relatively minor components of egg lipids, particularly 20:5(n-3) and 22:6(n-3), which accounted for only 1.1 and 2.9% of total egg fatty acids respectively. This indicates that the reproductive investment by this species is supported mainly by material derived from bacterial chemosynthesis. The potential for M. fortunata hedge betting by producing larvae which either metamorphose at the vent site or adopt a bathypelagic lifestyle and delay metamorphosis to facilitate more widespread dispersal is discussed.

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Tem sido relatado que as estacas de Camellia sinensis possuem baixa capacidade de emitir raízes, motivando assim a realização de estudos básicos para otimização do processo de propagação por estacas. Assim sendo, o presente trabalho objetivou quantificar o potencial rizogênico de diferentes genótipos e o efeito da posição da estaca no ramo e incisão na base, do substrato, tamanho do recipiente e ácido indolbutírico no enraizamento de estacas semi-lenhosas dessa espécie. Para tal, foram coletados ramos dos genótipos IAC 259, F15 e Comum, em Pariquera-Açu-SP, no inverno de 2010. em seguida, preparadas as estacas, contendo uma gema e uma folha, foram mantidas em viveiro com 70% de sombreamento. Estacas da posição basal e mediana dos ramos são as mais adequadas para estaquia devido a menor mortalidade e maior enraizamento. A injúria na base da estaca não afeta a mortalidade e o enraizamento das estacas, porém induz à formação de calo. Também não houve diferenças na mortalidade e no enraizamento das estacas quando as mesmas foram mantidas em recipiente de 50, 90 e 120 cm³. Comparado com vermiculita, areia e casca de arroz carbonizada, o solo foi o melhor substrato para estaquia, que na presença do ferimento, juntamente com o tratamento das estacas com 10 g L-1 de AIB promoveu a maior porcentagem de enraizamento. Todavia, ainda nessa condição a mortalidade média das estacas foi de 42%. O potencial de enraizamento do genótipo Comum foi superior ao do IAC 259 e F15.

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Metal substrates were coated by thermal spraying plasma torch, they were positioned at a distance of 4 and 5 cm from the nozzle exit of the plasma jet. The starting materials were used for deposition of tantalum oxide powder and aluminium. These two materials were mixed and ground into high-energy mill, then immersed in the torch for the production of alumina coating infused with particles of tantalum with nano and micrometric size. The spraying equipment used is a plasma torch arc not transferred, which operating in the range of 250 A and 80 V, was able to produce enough heat to ignite aluminothermic between Ta2O5 and aluminum. Upon reaching the plasma jet, the mixing powders react with the heat of the blaze, which provides sufficient energy for melting aluminum particles. This energy is transferred through mechanisms of self-propagating to the oxide, beginning a reduction reaction, which then hits on the surface of the substrate and forms a coating on which a composite is formed by a junction metal - ceramic (Ta +Al2O3). The phases and quantification of each were obtained respectively by X-ray diffraction and the Rietveld method. Morphology by scanning electron microscopy and chemical analysis by energy dispersive spectroscopy EDS. It was also performed measurements of the substrate roughness, Vickers microhardness measurements in sprays and determination of the electron temperature of the plasma jet by optical emission spectroscopy EEO. The results confirmed the expectation generated around the end product of spraying the mixture Ta2O5 + Al, both in the formation of nano-sized particles and in their final form. The electron excitation temperature was consistent with the purpose of work, in addition, the thermodynamic temperature was efficient for the reduction process of Ta2O5. The electron excitation temperature showed values of 3000, 4500 and 8000 K for flows10, 20 and 30 l / min respectively, these values were taken at the nozzle exit of the plasma jet. The thermodynamic temperature around 1200 ° C, was effective in the reduction process of Ta2O5

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Dissertação de Mestrado, Engenharia Biológica, Faculdade de Ciências e Tecnologia, Universidade do Algarve, 2014

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In light of deep-sea mining industry development, particularly interested in massive-sulphide deposits enriched in metals with high commercial value, efforts are increasing to better understand potential environmental impacts to local fauna. The aim of this study was to assess the natural background levels of biomarkers in the hydrothermal vent shrimp Rimicaris exoculata and their responses to copper exposure at in situ pressure (30MPa) as well as the effects of depressurization and pressurization of the high-pressure aquarium IPOCAMP. R. exoculata were collected from the chimney walls of the hydrothermal vent site TAG (Mid Atlantic Ridge) at 3630m depth during the BICOSE cruise in 2014. Tissue metal accumulation was quantified in different tissues (gills, hepatopancreas and muscle) and a battery of biomarkers was measured: metal exposure (metallothioneins), oxidative stress (catalase, superoxide dismutase, glutathione-S-transferase and glutathione peroxidase) and oxidative damage (lipid peroxidation). Data show a higher concentration of Cu in the hepatopancreas and a slight increase in the gills after incubations (for both exposed groups). Significant induction of metallothioneins was observed in the gills of shrimps exposed to 4μM of Cu compared to the control group. Moreover, activities of enzymes were detected for the in situ group, showing a background protection against metal toxicity. Results suggest that the proposed method, including a physiologically critical step of pressurizing and depressurizing the test chamber to enable the seawater exchange during exposure to contaminants, is not affecting metal accumulation and biomarkers response and may prove a useful method to assess toxicity of contaminants in deep-sea species.

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A aqüicultura é uma atividade que tem evoluído muito nos últimos anos. Para avaliar a qualidade da água na aqüicultura, o biomonitoramento por macroinvertebrados bentônicos tem sido cada vez mais utilizado, porém ainda é incipiente. Há diversas formas de coleta desses organismos, como pegadores de fundo e coletores com substrato artificial.O objetivo deste trabalho foi avaliar a eficiência de diferentes coletores com substrato artificial para o biomonitoramento de um reservatório rural utilizado para a produção de tilápias em tanques-rede. Foram avaliados dois tipos de coletores contendo taboa e pedra brita, fixados à meia água e rente ao fundo, por períodos de 30, 60 e 90 dias. Durante esse período também foram coletadas amostras de sedimento do fundo com uma draga tipo Petit Ponar. Ao final do experimento foram identificadas onze famílias de macroinvertebrados, sendo que a maior riqueza foi observada nas amostras coletadas com a draga. Os dados indicam uma diminuição da diversidade biológica ao longo do tempo nos coletores que continham folhas de taboa, e um pico de colonização aos 60 dias para os coletores com pedra. Apesar das amostras coletadas com a draga terem apresentado a maior riqueza de famílias, esse equipamento apresentou algumas desvantagens como o difícil manuseio, enquanto que os coletores com substratos artificiais são facilmente manuseados, além de garantir uma maior uniformidade das amostras, o que é muito vantajoso no monitoramento de pontos espacialmente distribuídos no interior dos reservatórios e viveiros utilizados pela aqüicultura.

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O bagaço de cana-de-açúcar (BCA), possui em sua composição principalmente celulose e hemicelulose que podem ser hidrolisadas para produção de etanol de segunda geração. O objetivo deste trabalho foi verificar se o BCA hidrolisado quimicamente poderia ser utilizado como substrato para a caracterização de enzimas lignocelulolíticas.

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A murcha de Fusarium spp. em crisântemo é responsável por sérios prejuízos à cultura no Brasil. Uma alternativa para o seu controle é o uso de substrato supressivo, o qual pode ser obtido pela adição de fontes de matérias orgânicas. Dessa forma, o presente trabalho teve por objetivo desenvolver um substrato supressivo à murcha do Fusarium em crisântemo com a introdução de matéria orgânica aos substratos padrões. Para tanto, lodo de esgoto e lodo de esgoto compostado; torta de mamona; esterco suíno; cama aviária; compostos comerciais LanziC); casca de camarão, biofertilizante e hidrolisado de peixe foram incorporados a substratos à base de casca de Pinus e de turfa em diferentes concentrações e combinações. Os experimentos foram realizados em propriedade produtora de crisântemo Bola-belga com problemas de Fusarium. Em todos os experimentos o número mínimo de repetições foi de 20 vasos por tratamento. Transcorridas 8, 12, 15 e 20 semanas do transplantio foi avaliada a severidade da doença por uma escala de notas de O para planta sadia a 5 para planta morta. Com os dados foram calculadas as áreas abaixo da curva de progresso da severidade da murcha de Fusarium. Além disso, foram realizadas análises dos atributos químicos e da atividade microbiana dos substratos bem como do desenvolvimento das plantas. O lodo de esgoto, lodo de esgoto compostado e a cama aviária induziram a supressividade do substrato à base de casca se Pinus e de turfa, controlando a murcha de Fusarium. O Lanzi®, também foi supressivo ao patógeno. A casca de camarão e o composto Lanzi® também induziram a supressividade dos substratos. Por outro lado, esterco suíno, torta de mamona, hidrolisado de peixe, quitosana e Trichoderma asperellum não interferiu na supressividade à doença. Substratos obtidos com lodo de esgoto e cama aviária, em mistura ou não, nas concentrações de 10, 20 e 30% (v/v) foram os mais adequados do ponto de vista de indução de supressividade e qualidade do produto, sendo os substratos recomendados para uso pelo agricultor. A supressividade observada nos substratos foi devido à união de características químicas e biológicas obtidas com a introdução das matérias orgânicas.

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A produção de mudas vigorosas é um dos primeiros passos para o sucesso do cultivo de olerícolas. Os adubos orgânicos e biofertilizantes auxiliam no suprimento nutricional das plantas e tem menor custo quando obtidos na propriedade. Foi avaliado o uso de biofertilizante e esterco de aves sobre a produção de mudas de pimentão (cv. Dhara R, Sakata®).

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Large igneous provinces (LIPs) are sites of the most frequently recurring, largest volume basaltic and silicic eruptions in Earth history. These large-volume (N1000 km3 dense rock equivalent) and large-magnitude (NM8) eruptions produce areally extensive (104–105 km2) basaltic lava flow fields and silicic ignimbrites that are the main building blocks of LIPs. Available information on the largest eruptive units are primarily from the Columbia River and Deccan provinces for the dimensions of flood basalt eruptions, and the Paraná–Etendeka and Afro-Arabian provinces for the silicic ignimbrite eruptions. In addition, three large-volume (675– 2000 km3) silicic lava flows have also been mapped out in the Proterozoic Gawler Range province (Australia), an interpreted LIP remnant. Magma volumes of N1000 km3 have also been emplaced as high-level basaltic and rhyolitic sills in LIPs. The data sets indicate comparable eruption magnitudes between the basaltic and silicic eruptions, but due to considerable volumes residing as co-ignimbrite ash deposits, the current volume constraints for the silicic ignimbrite eruptions may be considerably underestimated. Magma composition thus appears to be no barrier to the volume of magma emitted during an individual eruption. Despite this general similarity in magnitude, flood basaltic and silicic eruptions are very different in terms of eruption style, duration, intensity, vent configuration, and emplacement style. Flood basaltic eruptions are dominantly effusive and Hawaiian–Strombolian in style, with magma discharge rates of ~106–108 kg s−1 and eruption durations estimated at years to tens of years that emplace dominantly compound pahoehoe lava flow fields. Effusive and fissural eruptions have also emplaced some large-volume silicic lavas, but discharge rates are unknown, and may be up to an order of magnitude greater than those of flood basalt lava eruptions for emplacement to be on realistic time scales (b10 years). Most silicic eruptions, however, are moderately to highly explosive, producing co-current pyroclastic fountains (rarely Plinian) with discharge rates of 109– 1011 kg s−1 that emplace welded to rheomorphic ignimbrites. At present, durations for the large-magnitude silicic eruptions are unconstrained; at discharge rates of 109 kg s−1, equivalent to the peak of the 1991 Mt Pinatubo eruption, the largest silicic eruptions would take many months to evacuate N5000 km3 of magma. The generally simple deposit structure is more suggestive of short-duration (hours to days) and high intensity (~1011 kg s−1) eruptions, perhaps with hiatuses in some cases. These extreme discharge rates would be facilitated by multiple point, fissure and/or ring fracture venting of magma. Eruption frequencies are much elevated for large-magnitude eruptions of both magma types during LIP-forming episodes. However, in basaltdominated provinces (continental and ocean basin flood basalt provinces, oceanic plateaus, volcanic rifted margins), large magnitude (NM8) basaltic eruptions have much shorter recurrence intervals of 103–104 years, whereas similar magnitude silicic eruptions may have recurrence intervals of up to 105 years. The Paraná– Etendeka province was the site of at least nine NM8 silicic eruptions over an ~1 Myr period at ~132 Ma; a similar eruption frequency, although with a fewer number of silicic eruptions is also observed for the Afro- Arabian Province. The huge volumes of basaltic and silicic magma erupted in quick succession during LIP events raises several unresolved issues in terms of locus of magma generation and storage (if any) in the crust prior to eruption, and paths and rates of ascent from magma reservoirs to the surface.