Plasma cell polyp of the vocal fold

Plasma cell polyps of the vocal fold (plasma cell granulomas) are rare inflammatory polyps of the larynx. They should be included in the clinical and histological differential diagnosis of laryngeal polyps. Histologically they are polyclonal aggregates of plasma cells. It is essential to distinguish them from monoclonal, neoplastic plasma cell proliferations. The treatment of choice is surgical resection, although radiotherapy, laser ablation, antibiotics and steroids have been used successfully. We present a case of plasma cell granuloma presenting as a vocal fold polyp, treated surgically.

k-fold Subsampling based Sequential Backward Feature Elimination

We present a new wrapper feature selection algorithm for human detection. This algorithm is a hybrid featureselection approach combining the benefits of filter and wrapper methods. It allows the selection of an optimalfeature vector that well represents the shapes of the subjects in the images. In detail, the proposed featureselection algorithm adopts the k-fold subsampling and sequential backward elimination approach, while thestandard linear support vector machine (SVM) is used as the classifier for human detection. We apply theproposed algorithm to the publicly accessible INRIA and ETH pedestrian full image datasets with the PASCALVOC evaluation criteria. Compared to other state of the arts algorithms, our feature selection based approachcan improve the detection speed of the SVM classifier by over 50% with up to 2% better detection accuracy.Our algorithm also outperforms the equivalent systems introduced in the deformable part model approach witharound 9% improvement in the detection accuracy

An 40Ar/39Ar, Rb/Sr, and stable isotope study of micas in low-grade fold-and-thrust belt: An example from the Swiss Helvetic Alps

White micas in carbonate-rich tectonites and a few other rock types of large thrusts in the Swiss Helvetic fold-and-thrust belt have been analyzed by Ar-40/Ar-39 and Rb/Sr techniques to better constrain the timing of Alpine deformation for this region. Incremental Ar-40/Ar-39 heating experiments of 25 weakly metamorphosed (anchizone to low greenschist) samples yield plateau and staircase spectra. We interpret most of the staircase release spectra result from variable mixtures of syntectonic (neoformed) and detrital micas. The range in dates obtained within individual spectra depends primarily on the duration of mica nucleation and growth, and relative proportions of neoformed and detrital mica. Rb/Sr analyses of 12 samples yield dates of ca. 10-39 Ma (excluding one anomalously young sample). These dates are slightly younger than the Ar-40/Ar-39 total gas dates obtained for the same samples. The Rb/ Sr dates were calculated using initial Sr-87/Sr-86 ratios obtained from the carbonate-dominated host rocks, which are higher than normal Mesozoic carbonate values due to exchange with fluids of higher Sr-87/Sr-86 ratios (and lower O-18/O-16 ratios). Model dates calculated using Sr-87/Sr-86 values typical of Mesozoic marine carbonates more closely approximate the Ar-40/Ar-39 total gas dates for most of the samples. The similarities of Rb/Sr and Ar-40/Ar-39 total gas dates are consistent with limited amounts of detrital mica in the samples. The delta(18)O values range from 24-15%. (VSMOW) for 2-6 mum micas and 27-16parts per thousand for the carbonate host rocks. The carbonate values are significantly lower than their protolith values due to localized fluid-rock interaction and fluid flow along most thrust surfaces. Although most calcite-mica pairs are not in oxygen isotope equilibrium at temperatures of ca. 200-400 degreesC, their isotopic fractionations are indicative of either 1) partial exchange between the minerals and a common external fluid, or 2) growth or isotopic exchange of the mica with the carbonate after the carbonate had isotopically exchanged with an external fluid. The geological significance of these results is not easily or uniquely determined, and exemplifies the difficulties inherent in dating very fine-grained micas of highly deformed tectonites in low-grade metamorphic terranes. Two generalizations can be made regarding the dates obtained from the Helvetic thrusts: 1) samples from the two highest thrusts (Mt. Gond and Sublage) have all of their Ar-40/Ar-39 steps above 20 Ma, and 2) most samples from the deepest Helvetic thrusts have steps (often accounting for more than 80% of Ar-39 release) between 15 and 25 Ma. These dates are consistent with the order of thrusting in the foreland-imbricating system and increase proportions of neoformed to detrital mica in the more metamorphosed hinterland and deeply buried portions of the nappe pile. Individual thrusts accommodated the majority of their displacement during their initial incorporation into the foreland-imbricating system, and some thrusts remained active or were reactivated down to 15 Ma.

Caractérisation de l’ubiquitin-fold modifier (UFM1) dans un modèle C. elegans

L’ubiquitin-fold modifier (UFM1) fait partie de la classe 1 de la famille de protéine ubiquitin-like (Ubl). UFM1 et Ub ont très peu d’homologie de séquence, mais partagent des similarités remarquables au niveau de leur structure tertiaire. Tout comme l’Ub et la majorité des autres Ubls, UFM1 se lie de façon covalente à ses substrats par l’intermédiaire d’une cascade enzymatique. Il est de plus en plus fréquemment rapporté que les protéines Ubls sont impliquées dans des maladies humaines. Le gène Ufm1 est surexprimé chez des souris de type MCP développant une ischémie myocardique et dans les îlots de Langerhans de patients atteints du diabète de type 2. UFM1 et ses enzymes spécifiques, UBA5, UFL1 et UFC1, sont conservés chez les métazoaires et les plantes suggérant un rôle important pour les organismes multicellulaires. Le Caenorhabditis elegans est le modèle animal le plus simple utilisé en biologie. Sa morphologie, ses phénotypes visibles et ses lignées cellulaires ont été décrits de façon détaillée. De plus, son cycle de vie court permet de rapidement observer les effets de certains gènes sur la longévité. Ce modèle nous permet de facilement manipuler l’expression du gène Ufm1 et de mieux connaître ses fonctions. En diminuant l’expression du gène ufm-1 chez le C.elegans, par la technique de l’ARN interférence par alimentation, nous n’avons observé aucun problème morphologique grave. Les vers ressemblaient aux vers sauvages et possédaient un nombre de progéniture normal. Cependant, les vers sauvage exposés à l’ARNi d’ufm-1 vivent significativement moins longtemps que les contrôles et ce, de façon indépendante de la voie de signalisation de l’insuline/IGF. Chez le C. elegans la longévité et la résistance au stress cellulaire sont intimement liées. Nous n’avons remarqué aucun effet d’ufm-1 sur le stress thermal, osmotique ou oxydatif, mais il est requis pour la protection contre le stress protéotoxique. Il est également nécessaire au maintien de l’intégrité neuronale au cours du vieillissement des animaux. L’ensemble de nos données nous renseigne sur les fonctions putatives du gène Ufm1.

Alps Workshop 4 p6 Fold your arms

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Singularización de la intervención educativa en educación infantil. 'Singularity of educational intervention in primary school'.

Resumen tomado del autor

On the time for fold surfaces to order during the crystallization of polyethylene from the melt and its dependence on molecular parameters

New experiments underpin the interpretation of the basic division in crystallization behaviour of polyethylene in terms of whether or not there is time for the fold surface to order before the next molecular layer is added at the growth front. For typical growth rates, in Regime 11, polyethylene lamellae form with disordered {001} fold surfaces then transform, with lamellar thickening and twisting, towards the more-ordered condition found for slower crystallization in Regime 1, in which lamellae form with and retain {201} fold surfaces. Several linear and linear-low-density polyethylenes have been used to show that, for the same polymer crystallized alone or in a blend, the growth rate at which the change in initial lamellar condition occurs is reasonably constant thereby supporting the concept of a specific time for surfaces to attain the ordered {201}) state. This specific time, in the range from milliseconds to seconds, increases with molecular length, and in linear-low-density polymer, for higher branch contents. (c) 2006 Elsevier Ltd. All rights reserved.