832 resultados para Arca zebra, d13C
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Oxygen and carbon isotope analyses have been carried out on calcareous skeletons of important recent groups of organisms. Annual temperature ranges and distinct developmental stages can be reconstructed from single shells with the aid of the micro-sampling technique made possible by modern mass-spectrometers. This is in contrast to the results of earlier studies which used bulk sampIes. The skeletons analysed are from Bermuda, the Philippines, the Persian Gulf and the continental margin off Peru. In these environments, seasonal salinity ranges and thus annual variations in the isotopic composition of the water are small. In addition, environmental parameters are weIl documented in these areas. The recognition of seasonal isotopic variations is dependant on the type of calcification. Shells built up by carbonate deposition at the margin, such as molluscs, are suitable for isotopic studies. Analysis is more difficult where chambers are added at the margin of the shell but where older chambers are simultaneously covered by a thin veneer of carbonate e. g. in rotaliid foraminifera. Organisms such as calcareous algae or echinoderms that thicken existing calcareous parts as weIl as growing in length and breadth are the most difficult to analyse. All organisms analysed show temperature related oxygen-isotope fractionation. The most recent groups fractionate oxygen isotopes in accordance with established d18O temperature relationships (Tab. 18, Fig. 42). These groups are deep-sea foraminifera, planktonic foraminifera, serpulids, brachiopods, bryozoa, almost all molluscs, sea urchins, and fish (otoliths). A second group of organisms including the calcareous algae Padina, Acetabularia, and Penicillus, as weIl as barnacles, cause enrichment of the heavy isotope 18O. Finally, the calcareous algae Amphiroa, Cymopolia and Halimeda, the larger foraminifera, corals, starfish, and holothurians cause enrichment of the lighter isotope 16O. Organisms causing non-equilibrium fractionation also record seasonal temperature variations within their skeletons which are reflected in stable-oxygen-isotope patterns. With the exception of the green algae Halimeda and Penicillus, all organisms analysed show lower d13C values than calculated equilibrium values (Tab. 18, Fig. 42). Especially enriched with the lighter isotope 12C are animals such as hermatypic corals and larger foraminifera which exist in symbiosis with other organisms, but also ahermatypic corals, starfish, and holothurians. With increasing age of the organisms, seven different d13C trends were observed within the skeletons. 1) No d13C variations are observed in deep-sea foraminifera presumably due to relatively stable environmental conditions. 2) Lower d13C values occur in miliolid larger foraminifera and are possibly related to increased growth with increasing age of the foraminifera. 3) Higher values are found in planktonic foraminifera and rotaliid larger foraminifera and can be explained by a slowing down of growth with increasing age. 4) A sudden change to lower d13C values at a distinct shell size occurs in molluscs and is possibly caused by the first reproductive event. 5) A low-high-Iow cycle in calcareous algae is possibly caused by variations in the stage of calcification or growth. 6) A positive correlation between d18O and d13C values is found in some hermatypic corals, all ahermatypic corals, in the septa of Nautilus and in the otoliths of fish. In hermatypic corals from tropical areas, this correlation is the result of the inverse relationship between temperature and light caused by summer cloud cover; in other groups it is inferred to be due to metabolic processes. 7) A negative correlation between d18O and d13C values found in hermatypic corals from the subtropics is explained by the sympathetic relationship between temperature and light in these latitudes. These trends show that the carbon isotope fractionation is controlled by the biology of the respective carbonate producing organisms. Thus, the carbon isotope distribution can provide information on the symbiont-host relationship, on metabolic processes and calcification and growth stages during ontogenesis of calcareous marine organisms.
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Hemorrhage in regions remote from the site of initial intracranial operations is rare, but may be fatal. Postoperative cerebellar hemorrhage as a complication of supratentorial surgery, with a radiological appearance known as zebra sign, is an increasingly recognized clinical entity and is associated mainly with vascular neurosurgery or temporal lobe resection. The pathophysiology remains unclear. Three cases of remote cerebellar hematoma occurred after neck clipping of anterior communicating artery aneurysms. All patients had similar clinical findings and underwent pterional craniotomy with the head in accentuated extension. One patient died and the two were discharged without symptoms. Cerebellar hemorrhage probably has a multifactorial origin involving positioning associated with abundant cerebrospinal fluid drainage causing cerebellar sag with resultant vein stretching and bleeding, and use of aspirin or other antiplatelet agents.
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Pholeohedra overstreeti n. g., n. sp. (Digenea: Haploporidae) is described from Girella zebra (Kyphosidae) in South Australia. The new genus is compared with all genera of Haploporidae sensu late (including Atractotrematidae, Megasolenidae and Waretrematidae) and has a unique bell-shaped concavity at its posterior end. The genus otherwise resembles Hapladena in the arrangement of the testis, vitellarium and gut but also resembles Megasolena, Metamegasolena and Vitellibaculum except in having a single testis. This is the first haploporid reported from kyphosid fishes in Australia.
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Mestrado em Engenharia Geotécnica e Geoambiente
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Este trabalho pretende enfatizar a importância da elaboração de uma base de dados extensa e robusta para o melhoramento da cartografia geotécnica subterrânea do maciço granítico do sector de Carvalhido–Burgães (Porto). Este estudo envolveu a análise e o refinamento das principais características geomecânicas ao longo de um traçado com cerca de 1220 m, para a caracterização do maciço rochoso da galeria subterrânea Carvalhido–Burgães. Para esta caracterização foram coligidos e uniformizados dados geológicos, geotécnicos e geomecânicos relativos a várias campanhas de campo, realizadas entre 2005 e 2011, tendo estado a técnica da amostragem linear aplicada ao grau de compartimentação do maciço rochoso na base do seu estudo. Além disso, procedeu‐se a um tratamento estatístico das descontinuidades, bem como dos parâmetros geológico‐geotécnicos e geomecânicos a estas associados. O zonamento geotécnico do maciço granítico foi realizado sempre em estreita ligação com o conhecimento das características do maciço in situ. Pretende‐se que esta metodologia contribua para um melhor conhecimento da compartimentação dos maciços rochosos em geral e, em particular, do modelo geomecânico comportamental do maciço rochoso do Porto.
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O peixe-zebra é utilizado como modelo vertebrado para estudos in vivo de diversas patologias de origem genética. Neste trabalho pretendeu-se estudar a discinesia ciliar primária através do estudo in vivo do organizador da esquerda-direita destes peixes, conhecido por vesícula de Kupffer. Em particular, após análise de sequências de imagens captadas a alta velocidade, avaliou-se o com-portamento dinâmico de cílios normais e comparou-se com o de cílios com alte-rações genéticas com o objectivo de melhor compreender os processos que in-fluenciam a localização assimétrica dos órgãos internos, associados a esta doen-ça. De vídeos obtidos por microscopia de alta velocidade do interior da vesí-cula de Kupffer foram analisados 32 cílios, sendo 8 normais e os restantes cílios pertencentes a três alterações genéticas diferentes: subexpressão de Pkd2, so-brexpressão de Arl13b e mutação no gene deltaD. Para cada cílio calculou-se a frequência de batimento e caracterizou-se quantitativamente o movimento. Esta última análise teve como base a segmentação manual do cílio em quatro pontos definindo a base, o meio e a ponta. De seguida, estudou-se a dinâmica de cada uma das rectas constituídas por estas três estruturas ao longo do tempo. Com recurso à análise estatística ANOVA podemos comprovar diferenças no movi-mento entre os cílios alterados quando comparados com os normais. A análise da frequência demonstrou que todos os cílios estudados possu-em uma frequência média 34,9 Hz. Demonstrou-se ainda que, quando compa-rados com cílios normais, os cílios Pkd2 possuem um movimento 60% mais rí-gido, os Alr13b são caracterizados por amplitudes angulares 26% superiores no seu movimento e, por fim, a relação entre as amplitudes base/meio é 23% supe-rior nos cílios Delta D. Para implementar estes estudos, desenvolveu-se uma ferramenta baseada num plugin para ImageJ conjuntamente com códigos em R, que poderá vir a ser utilizada em investigações da discinesia ciliar primária em peixes-zebra.
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Abstract: Birds harbor a variety of bacteria on their plumage, some of which can degrade feathers in vitro. Whether these keratinolytic bacteria are active on live birds and can effect feather degradation on birds is debatable. The effect of such bacteria on the body condition and behavior of birds, is unknown. Using a community of feather-degrading bacteria (EB), we investigate the interaction between the activity and load of such bacteria, on the morphology, body condition, and behavior of zebra finches (Taeniopygia guttata). In Chapter 2, we find that the elevated loads of such microbes lead to a reduction in the expression of morphological traits, such as male bill color (a sexually selected trait) and uropygial gland volume, without reducing body mass, or evoking a cellular immune response. We also suggest the presence of a carotenoid based defense response in hosts, to such elevated loads of microbes and document a sex-based difference in the source of carotenoids used for such a response. In Chapter 3, we investigated the effect of EB loads on male mate choice of zebra finches, wherein male choice of females with elevated and un-altered bacterial loads, varied with male size. We found that larger males preferred females with higher bacterial load and smaller males preferred females with lower bacterial load. Chapter 4 demonstrates that the presence of melanin in feathers reduces the growth and activity of the community of feather-degrading bacteria (EB) and that the EB community can effect feather degradation in humid conditions, without broth. Additional results also demonstrate that the EB community consists of bacteria that can attach themselves to feathers on live birds and those that can live freely on avian plumage. Finally, chapter 5 demonstrates that the self-maintenance, social and sexual behaviors of birds are implicated in the infection and horizontal transmission of bacteria. It also suggests a linked oral - faecal - genital mode of transmission of pathogens in birds. These results demonstrate that differential loads of normal flora of vertebrate hosts can effect changes in their morphology and behavior. They also shed light on the role of feather-degrading bacteria in the evolution of melanin polymorphism in birds and suggest that bacteria can be active on live birds. This thesis also highlights the importance of social and, sexual behaviors of birds, in epidemiology. Résumé: Les Oiseaux ont dans leur plumage diverses bactéries dont certaines dégradent les plumes in vitro, néanmoins. Il n'est pas clair, au vu de précédentes études, si ces bactéries kératinolytiques sont actives sur des oiseaux vivants, et si celles-ci dégradent effectivement le plumage de leur hôte, L'effet de ces bactéries sur la condition corporelle ainsi que le comportement des oiseaux n'est pas connu. A l'aide d'une communauté de bactéries dégradant les plumes (EB), non pathogènes, nous examinons les interactions entre l'activité et la charge bactérienne sur la morphologie, la condition corporelle et le comportement du diamant mandarins (Taeniopygia guttata). Dans le chapitre 2, nous montrons qu'une charge élevée de ces microbes mène à une réduction de l'expression de certains traits morphologiques, tels que la couleur du bec chez le mâle (un trait soumis à sélection sexuelle), ainsi que le volume de la glande uropygienne, sans qu'il y ait une réduction de la masse corporelle, ni déclenchement d'une réponse immune cellulaire. Nos données suggèrent la présence d'une défense chez l'hôte à des charges élevées de bactéries basée sur la présence de caroténoïdes. Nous montrons, de plus une différence liée au sexe dans la source des caroténoïdes utilisé pour cette réponse. Dans le chapitre 3 nous examinons l'influence de la charge bactérienne EB sur le choix des mâles chez le diamant mandarins. Des femelles avec une charge bactérienne normale et augmentée sont choisies par les mâles et ce choix varie avec la taille des mâles. Nous avons mis en évidence que les grands mâles préfèrent les femelles avec une charge bactérienne plus élevée. Les petits mâles préfèrent les femelles avec une charge bactérienne réduite. Le chapitre 4 démontre que la présence de mélanine dans les plumes réduit la croissance et l'activité de la communauté de bactéries dégradant le plumage (EB), et que cette communauté EB peut dégrader les plumes dans des conditions humides, sans milieu de culture liquide. De plus nous montrons que cette communauté consiste en des bactéries qui peuvent s'attacher sur les plumes d'oiseaux vivants ainsi que des bactéries libres. Pour finir nous montrons dans le chapitre 5 que la maintenance corporelle, l'interaction sociale et le comportement sexuel de ces oiseaux sont impliqués dans l'infection et la transmission horizontale de ces bactéries. Nos données suggèrent une transmission orale-fécale-génitale des pathogènes chez les oiseaux. Ces résultats montrent que des charges différentes de la flore bactérienne habituelle et non pathogène de vertébrés peuvent affecter leur morphologie et leur comportement. Ils éclaircissent également le rôle des bactéries dégradant les plumes dans l'évolution du polymorphisme mélanique chez les oiseaux et suggèrent que ces bactéries peuvent être actives sur des oiseaux vivants. Cette thèse souligne également l'importance du comportement social et sexuel des oiseaux dans l'épidémiologie.
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Mitochondria have a fundamental role in the transduction of energy from food into ATP. The coupling between food oxidation and ATP production is never perfect, but may nevertheless be of evolutionary significance. The 'uncoupling to survive' hypothesis suggests that 'mild' mitochondrial uncoupling evolved as a protective mechanism against the excessive production of damaging reactive oxygen species (ROS). Because resource allocation and ROS production are thought to shape animal life histories, alternative life-history trajectories might be driven by individual variation in the degree of mitochondrial uncoupling. We tested this hypothesis in a small bird species, the zebra finch (Taeniopygia guttata), by treating adults with the artificial mitochondrial uncoupler 2,4-dinitrophenol (DNP) over a 32-month period. In agreement with our expectations, the uncoupling treatment increased metabolic rate. However, we found no evidence that treated birds enjoyed lower oxidative stress levels or greater survival rates, in contrast to previous results in other taxa. In vitro experiments revealed lower sensitivity of ROS production to DNP in mitochondria isolated from skeletal muscles of zebra finch than mouse. In addition, we found significant reductions in the number of eggs laid and in the inflammatory immune response in treated birds. Altogether, our data suggest that the 'uncoupling to survive' hypothesis may not be applicable for zebra finches, presumably because of lower effects of mitochondrial uncoupling on mitochondrial ROS production in birds than in mammals. Nevertheless, mitochondrial uncoupling appeared to be a potential life-history regulator of traits such as fecundity and immunity at adulthood, even with food supplied ad libitum.
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The dolomite veins making up rhythmites common in burial dolomites are not cement infillings of supposed cavities, as in the prevailing view, but are instead displacive veins, veins that pushed aside the host dolostone as they grew. Evidence that the veins are displacive includes a) small transform-fault-like displacements that could not have taken place if the veins were passive cements, and b) stylolites in host rock that formed as the veins grew in order to compensate for the volume added by the veins. Each zebra vein consists of crystals that grow inward from both sides, and displaces its walls via the local induced stress generated by the crystal growth itself. The petrographic criterion used in recent literature to interpret zebra veins in dolomites as cements - namely, that euhedral crystals can grow only in a prior void - disregards evidence to the contrary. The idea that flat voids did form in dolostones is incompatible with the observed optical continuity between the saddle dolomite euhedra of a vein and the replacive dolomite crystals of the host. The induced stress is also the key to the self-organization of zebra veins: In a set of many incipient, randomly-spaced, parallel veins just starting to grow in a host dolostone, each vein¿s induced stress prevents too-close neighbor veins from nucleating, or redissolves them by pressure-solution. The veins that survive this triage are those just outside their neighbors¿s induced stress haloes, now forming a set of equidistant veins, as observed.