993 resultados para Wattenberg, Martin P


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UANL

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F1651, les pili Pap et l’antigène CS31A associé aux antigènes de surface K88 sont tout trois des membres de la famille de type P des facteurs d’adhérence jouant un rôle ppondérant lors de l’établissement d’une maladie causée par des souches Escherichia coli pathogènes, en particulier des souches d’E. coli pathogènes extra-intestinales (ExPEC, Extra-intestinal pathogenic E. coli). Leur expression est sous le contrôle d’un mécanisme de régulation transcriptionnel dépendant de l’état de méthylation de l’ADN, résultant dans l’existence de deux populations définies, l’une exprimant l’adhésine (population ON) et l’autre ne l’exprimant pas (population OFF). Malgré de fortes identités de séquences, ces trois systèmes diffèrent l’un de l’autre, principalement par le pourcentage de cellules ON rencontrées. Ainsi, quand CS31A est systématiquement orienté vers un état considéré comme OFF, F1651 présente une phase ON particulièrement élevée et Pap montre deux états OFF et ON bien distincts, selon le phénotype de départ. La protéine régulatrice sensible à la leucine (Lrp, Leucine-responsive regulatory protein) joue un rôle essentiel dans la réversibilité de ce phénomène épigénétique et il est supposé que les différences de séquences au niveau de la région régulatrice modifient la localisation à ces sites de fixation de Lrp; ce qui résulte, en final, aux différences de phase existant entre CS31A, F1651 et Pap.À l’aide de divers techniques parmi lesquelles l’utilisation de gènes rapporteurs, mutagénèses dirigées et d’analyse des interactions ADN-protéines in vitro, nous montrons dans ce présent projet que la phase OFF prédominante chez CS31A est principalement due à une faible interaction de Lrp avec la région distale de l’opéron clp, et que la présence d’un homologue du régulateur local PapI joue un rôle également clef dans la production de CS31A. Dans le cas de F1651, nous montrons dans cette étude que le taux élevé de cellules en phase ON est dû à une altération dans le maintien de Lrp sur les sites répresseurs 1-3. Ceci est dû à la présence de deux nucléotides spécifiques, situé de part et d’autre du site répresseur 1, qui défavorisent la fixation de Lrp sur ce site précis. Tout comme dans le cas de CS31A, la formation d’un complexe, activateur ou répresseur de la phase ON, dépend également de l’action de du régulatuer local FooI, qui favorise alors le déplacement de Lrp des sites répresseurs 1-3 vers les sites activateurs 4-6.

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Nota biogràfica sobre el filòsof Martin Heidegger on es fa, per una banda, un breu repàs dels principals fets de la seva vida com a filòsof i, per una altra banda, un breu repàs de la seva obra

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"análisis de la trayectoria organizacional y de servicios de estas entidades, para así entrar a valorar la evolución y comportamiento de estas corporaciones, y determinar la existencia de economías o deseconomías de escala."

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Resumen basado en el de la publicaci??n

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The low availability of zinc (Zn) in soils and crops affects dietary Zn intake worldwide. This study sought to determine if the natural genetic variation in shoot Zn concentrations (Zn(shoot)) is sufficient to pursue a crop improvement breeding strategy in a leafy vegetable crop. The gene-pool of Brassica oleracea L. was sampled using a large (n = 376) diversity foundation set (DFS), representing almost all species-wide common allelic variation, and 74 commercial varieties (mostly F(1)). The DFS genotypes were grown at low and high soil phosphorus (P) levels under glasshouse and field conditions, and also in a Zn-deficient soil, with or without Zn-fertilisation, in a glasshouse. Despite the large variation in Zn(shoot) among genotypes, environment had a profound effect on Zn(shoot) The heritability of Zn(shoot) was significant, but relatively low, among 90 doubled-haploid (DH) lines from a mapping population. While several quantitative trait loci (QTL) associated with Zn(shoot) occurred on chromosomes C2, C3, C5, C7, and C9, these were generally weak and conditional upon growth conditions. Breeding for Zn(shoot) in B. oleracea is therefore likely to be challenging. Shoot P concentrations increased substantially in all genotypes under low soil Zn conditions. Conversely, only some genotypes had increased Zn(shoot) at low soil P levels. Sufficient natural genetic variation may therefore exist to study some of the interactions between Zn and P nutrition.

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Aim  This paper documents reconstructions of the vegetation patterns in Australia, Southeast Asia and the Pacific (SEAPAC region) in the mid-Holocene and at the last glacial maximum (LGM). Methods  Vegetation patterns were reconstructed from pollen data using an objective biomization scheme based on plant functional types. The biomization scheme was first tested using 535 modern pollen samples from 377 sites, and then applied unchanged to fossil pollen samples dating to 6000 ± 500 or 18,000 ± 1000 14C yr bp. Results  1. Tests using surface pollen sample sites showed that the biomization scheme is capable of reproducing the modern broad-scale patterns of vegetation distribution. The north–south gradient in temperature, reflected in transitions from cool evergreen needleleaf forest in the extreme south through temperate rain forest or wet sclerophyll forest (WSFW) and into tropical forests, is well reconstructed. The transitions from xerophytic through sclerophyll woodlands and open forests to closed-canopy forests, which reflect the gradient in plant available moisture from the continental interior towards the coast, are reconstructed with less geographical precision but nevertheless the broad-scale pattern emerges. 2. Differences between the modern and mid-Holocene vegetation patterns in mainland Australia are comparatively small and reflect changes in moisture availability rather than temperature. In south-eastern Australia some sites show a shift towards more moisture-stressed vegetation in the mid-Holocene with xerophytic woods/scrub and temperate sclerophyll woodland and shrubland at sites characterized today by WSFW or warm-temperate rain forest (WTRF). However, sites in the Snowy Mountains, on the Southern Tablelands and east of the Great Dividing Range have more moisture-demanding vegetation in the mid-Holocene than today. South-western Australia was slightly drier than today. The single site in north-western Australia also shows conditions drier than today in the mid-Holocene. Changes in the tropics are also comparatively small, but the presence of WTRF and tropical deciduous broadleaf forest and woodland in the mid-Holocene, in sites occupied today by cool-temperate rain forest, indicate warmer conditions. 3. Expansion of xerophytic vegetation in the south and tropical deciduous broadleaf forest and woodland in the north indicate drier conditions across mainland Australia at the LGM. None of these changes are informative about the degree of cooling. However the evidence from the tropics, showing lowering of the treeline and forest belts, indicates that conditions were between 1 and 9 °C (depending on elevation) colder. The encroachment of tropical deciduous broadleaf forest and woodland into lowland evergreen broadleaf forest implies greater aridity. Main conclusions  This study provides the first continental-scale reconstruction of mid-Holocene and LGM vegetation patterns from Australia, Southeast Asia and the Pacific (SEAPAC region) using an objective biomization scheme. These data will provide a benchmark for evaluation of palaeoclimate simulations within the framework of the Palaeoclimate Modelling Intercomparison Project.