98 resultados para Zonotrichia-capensis


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There are two major groups of ticks: soft ticks and hard ticks. The hard ticks comprise the prostriate ticks and the metastriate ticks. The mitochondrial (mt) genomes of one species of prostriate tick and two species of metastriate ticks had been sequenced prior to our study. The prostriate tick has the ancestral arrangement of mt genes of arthropods, whereas the two metastriate ticks have rearrangements of eight genes and duplicate control regions. However, the arrangement of genes in the mt genomes of soft ticks had not been studied. We sequenced the mt genomes of two species of soft ticks, Carios capensis and Ornithodoros moubata, and a metastriate tick, Haemaphysalis flava. We found that the soft ticks have the ancestral arrangement of mt genes of arthropods, whereas the metastriate tick, H. flava, shares the rearrangements of mt genes and duplicate control regions with the other two metastriate ticks that have previously been studied. Our study indicates that gene rearrangements and duplicate control regions in mt genomes occurred once in the most recent common ancestor of metastriate ticks, whereas the ancestral arrangement of arthropods has remained unchanged for over 400 million years in the lineages leading to the soft ticks and the prostriate ticks.

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La trazabilidad y el correcto etiquetado de los piensos y sus ingredientes son factores esenciales para prevenir fraudes y garantizar la seguridad alimentaria. En el ámbito de la lucha contra las Encefalopatías Espongiformes Transmisibles (EETs), la prohibición de la Unión Europea (UE) de alimentar a rumiantes y otros animales de granja con harinas de carne y huesos derivadas de animales, hace necesaria la disponibilidad de metodologías que permitan identificar el origen de las materias primas e ingredientes presentes en los piensos. El método oficial de análisis microscópico tradicionalmente empleado para este fin presenta limitaciones a la hora de diferenciar entre los huesos de mamíferos y de aves, así como para determinar el origen animal específico de las partículas detectadas. Por ello, una de las prioridades de la UE en los últimos años ha sido potenciar la búsqueda y desarrollo de técnicas analíticas alternativas que permitan la detección específica de todos los componentes que integran los piensos. Teniendo en cuenta estos aspectos, en esta Tesis Doctoral se han desarrollado técnicas de PCR en tiempo real con sondas TaqMan® para el control de autenticidad y trazabilidad de ingredientes de origen animal utilizados en la fabricación de los piensos. Las especies objeto de este trabajo han sido: vaca (Bos taurus), oveja (Ovis aries), cabra (Capra hircos), grupo rumiante, cerdo (Sus scrofa), pollo (Gallus gallos), pavo (Meleagris g-allopavo), pato (Anal platyrhynchos x Cairina moschata), oca (Anser anser), grupo aviar, caballo (Equus caballus), conejo (Oryctolagus cuniculus), liebre (Lepus capensis), grupo lepórido (conejo y liebre) y pescados...

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Sporomorphs and dinoflagellate cysts from site GIK16867 in the northern Angola Basin record the vegetation history of the West African forest during the last 700 ka in relation to changes in salinity and productivity of the eastern Gulf of Guinea. During most cool and cold periods, the Afromontane forest, rather than the open grass-rich dry forest, expanded to lower altitudes partly replacing the lowland rain forest of the borderlands east of the Gulf of Guinea. Except in Stage 3, when oceanic productivity was high during a period of decreased atmospheric circulation, high oceanic productivity is correlated to strong winds. The response of marine productivity in the course of a climatic cycle, however, is earlier than that of wind vigour and makes wind-stress-induced oceanic upwelling in the area less likely. Monsoon variation is well illustrated by the pollen record of increased lowland rain forest that is paired to the dinoflagellate cyst record of decreased salinity forced by increased precipitation and run-off.

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Palynological investigation of the marine core, GeoB1008-3, from near the mouth of the Congo river (6°35.6'S/10°19.1'E), provides information about the changes in vegetation and climate in West Equatorial Africa during the last 190 ka. The pollen diagram is divided into zones 1-6 which are considered to correspond in time with the marine isotope stages 1-6. Oscillations in temperature and moisture are indicated during the cold stage 6. During stage 5, two cooler periods (5d and 5b) can be shown with an expansion of Podocarpus forests to lower elevations on the expense of lowland rain forest. Extended mangrove swamps existed along the coast in times of high sea level (stages 5 and 1).