Influência de alguns métodos de controle do escurecimento enzimático nas propriedades organoléticas da maçã Ohio Beauty conservada por congelação e liofilização

Foi estudada a influência de tres métodos de controle de escurecimento enzimático (branqueamento, ácido ascórbico e SO2) nas propriedades organoléticas da maçã em pedaços da variedade Ohio Beauty, conservada por congelação e liofilização. Imediatamente após seu recebimento, uma terça parte das frutas foi processada. Outra terça parte foi colocada em câmara fria a 1°C por tres semanas e a restante deixada sob as mesmas condições por seis semanas, sendo estas duas últimas processadas imediatamente após os respectivos tempos de armazenamento prévio. Os resultados mostraram que, para a congelação, o branqueamento foi o melhor tratamento para todos os atributos de qualidade, exceto para cor, em que o ácido ascórbico foi mais eficiente. Este último foi ligeiramente superior ao SO2 quanto à qualidade geral do produto. Para a liofilização, o tratamento com SO2 foi superior ao branqueamento quanto ao sabor e qualidade geral do produto, porém, foi inferior quanto à cor. Nenhum dos tratamentos, entretanto, controlou de maneira eficiente o escurecimento no produto liofilizado.

Estudo comparativo de três variedades de maçã para processamento

No presente trabalho foi feito um estudo comparativo entre as variedades de maçã Yellow Golden Delicious, Melrose e Rome Beauty, visando determinar para cada uma delas, o método mais adequado de processamento. Foram utilizados neste experimento, três tratamentos com a finalidade de evitar o escurecimento enzimático (branqueamento, ácido ascórbico e SO2) e três métodos de processamento (appertização, congelação e liofilização). Os resultados mostraram que a variedade mais adequada para processamento foi a Melrose, exceto para a combinação branqueamento-liofilização, em que as variedades Rome Beauty o Yellow Golden Delicious foram superiores. Esta última foi considerada a pior para processamento, exceto para a liofilização. A congelaçâo foi o método de processamento mais adequado para as três variedades de maçã estudadas.

Influência de alguns métodos de controle do escurecimento enzimático nas propriedades organoléticas da maçã Bruckner do Brasil conservada por congelação e liofilização

No presente trabalho foi estudada a influência de três métodos de controle do escurecimento enzimático (branqueamento, ácido ascórbico e SO2) nas propriedades organoléticas da maçã em pedaços da variedade Bruckner do Brasil, conservada por congelação e liofilização. Imediatamente após seu recebimento, uma terça parte das frutas foi processada. Outra terça parte foi colocada em câmara fria a 1°C por três semanas e a restante deixada sob as mesmas condições por seis semanas, sendo estas duas últimas processadas imediatamente após os respectivos tempos de armazenamento prévio. Para a congelação, o branqueamento foi considerado o melhor tratamento para todos os atributos de qualidade, exceto para cor, em que o SO2 e o ácido ascórbico foram superiores. Em termos de qualidade geral, o ácido ascórbico foi ligeiramente superior ao so2. Para a liofilização, o SO2 foi de um modo geral o melhor tratamento. Entretanto, nenhum dos tratamentos controlou de maneira eficiente o escurecimento no produto liofilizado.

Kabīr et la répétition du nom de Rāma, réalisation spirituelle et mémoire de Dieu

L'intention de l'A. est d'analyser la répétition du Nom de Rāma chez Kabīr. Cette technique prend un sens particulier chez ce poète, étroitement lié au souvenir constant de Dieu, à une vision imprégnée à la fois de spéculations métaphysiques et d'une profonde dévotion amoureuse. L'A. tente d'évaluer l'impact des différents courants qui ont forgé la pensée de Kabir et de démontrer leur importance dans l'oeuvre du poète. Par cet effort, il espère contribuer à éclairer l'atmosphère religieuse de l'époque et de situer une des pratiques très importantes de mantra dans le contexte de la bhakti médiévale

40Ar/39Ar dating of Penninic Front tectonic displacement (W Alps) during the Lower Oligocene (31-34 Ma)

Direct absolute dating of the Penninic Frontal Thrust tectonic motion is achieved using the Ar-40/Ar-39 technique in the Pelvoux Crystalline Massif (Western Alps). The dated phengites were formed syn-kinematically in shear zones. They underline the brittle-ductile stretching lineation, pressure-shadow fibres and slickensides consistent with underthrusting of the European continental slab below the propagating Penninic Thrust. Chlorite-phengite thermobarometry yields 10-15 km and T similar to 280 degrees C, while Ar-40/Ar-39 phengite ages mainly range between 34 and 30 Ma, with one younger age at 27 Ma. This Early Oligocene age range matches a major tectonic rearrangement of the Alpine chain. Preservation of prograde Ar-40/Ar-39 ages is ascribed to passive exhumation of the Pelvoux shear zone network, sandwiched between more external thrusts and the Penninic Front reactivated as an E-dipping detachment fault. Partial resetting in the Low Temperature part of argon spectra below 24 Ma is ascribed to brittle deformation and alteration of phengites.

Decrease in beta-Cell Proliferation Precedes Apoptosis during Diabetes Development in Bio-Breeding/Worcester Rat: Beneficial Role of Exendin-4

In autoimmune type 1 diabetes mellitus, proinflammatory cytokine-mediated apoptosis of beta-cells has been considered to be the first event directly responsible for beta-cell mass reduction. In the Bio-Breeding (BB) rat, an in vivo model used in the study of autoimmune diabetes, beta-cell apoptosis is observed from 9 wk of age and takes place after an insulitis period that begins at an earlier age. Previous studies by our group have shown an antiproliferative effect of proinflammatory cytokines on cultured beta-cells in Wistar rats, an effect that was partially reversed by Exendin-4, an analogue of glucagon-like peptide-1. In the current study, the changes in beta-cell apoptosis and proliferation during insulitis stage were also determined in pancreatic tissue sections in normal and thymectomized BB rats, as well as in Wistar rats of 5, 7, 9, and 11 wk of age. Although stable beta-cell proliferation in Wistar and thymectomized BB rats was observed along the course of the study, a decrease in beta-cell proliferation and beta-cell mass from the age of 5 wk, and prior to the commencement of apoptosis, was noted in BB rats. Exendin-4, in combination with anti-interferon-gamma antibody, induced a near-total recovery of beta-cell proliferation during the initial stages of insulitis. This highlights the importance of early intervention and, as well, the possibilities of new therapeutic approaches in preventing autoimmune diabetes by acting, initially, in the insulitis stage and, subsequently, on beta-cell regeneration and on beta-cell apoptosis.

The shift from low to high non-structural protein 1 expression in rotavirus-infected MA-104 cells

A hallmark of group/species A rotavirus (RVA) replication in MA-104 cells is the logarithmic increase in viral mRNAs that occurs four-12 h post-infection. Viral protein synthesis typically lags closely behind mRNA synthesis but continues after mRNA levels plateau. However, RVA non-structural protein 1 (NSP1) is present at very low levels throughout viral replication despite showing robust protein synthesis. NSP1 has the contrasting properties of being susceptible to proteasomal degradation, but being stabilised against proteasomal degradation by viral proteins and/or viral mRNAs. We aimed to determine the kinetics of the accumulation and intracellular distribution of NSP1 in MA-104 cells infected with rhesus rotavirus (RRV). NSP1 preferentially localises to the perinuclear region of the cytoplasm of infected cells, forming abundant granules that are heterogeneous in size. Late in infection, large NSP1 granules predominate, coincident with a shift from low to high NSP1 expression levels. Our results indicate that rotavirus NSP1 is a late viral protein in MA-104 cells infected with RRV, presumably as a result of altered protein turnover.

Early Variscan I-type pluton in the pre-Alpine basement of the Western Alps: The ca. 360 Ma Cogne diorite (NW-Italy)

Located at the internal border of the Grand-Saint-Bernard Zone, the diorite and its aureole lie on top of intensively studied Alpine eclogitic units but this pluton, poorly studied yet, has kept locally almost undeformed. The pluton intruded, at similar to 360 Ma, country-rocks mostly composed of dark shales with Na2O > K2O and minor mafic intercalations of tholeiitic basalt affinity. This association is characteristic of the Vanoise (France) basement series, where available age determinations suggest an Early Paleozoic age. Parts of the pluton, and of its hornfels aureole that is evidenced here for the first time, in the Punta Bioula section of Valsavaranche valley (NW-Italy), have been well-preserved from the Alpine deformation. Syn-emplacement hardening, dehydration-induced, probably prevented strain-enhanced Alpine recrystallization. Magmatic rock-types range continuously from subordinate mafic types at SiO2 similar to 48%, of hornblendite with cumulative or appinite affinities, to the main body of quartz diorite to quartz monzonite (SiO2 up to 62%). P-T estimates for the pluton emplacement, based on the abundance of garnet in the hornfelses, using also zircon and apatite saturation thermometry and Al-in-hornblende barometry, suggest T similar to 800-950 degrees C and minimum P in the 0.2-0.5 GPa range, with records of higher pressure conditions (up to 1-2 GPa?) in hornblendite phlogopite-cored amphibole. The high-K, Na > K, calcalkaline geochemistry is in line with a destructive plate-margin setting. Based on major element data and radiogenic isotope signature (epsilon Nd-360 Ma from -1.2 to + 0.9, Sr-87/Sr-86(360 MA) from 0.7054 to 0.7063), the parental magmas are interpreted in terms of deep-seated metabasaltic partial melts with limited contamination from shallower sources, the low radiogenic Nd-content excluding a major contribution from Vanoise tholeiites. There is no other preserved evidence for Variscan magmatism of similar age and composition in the Western Alps, but probable analogs are known in the western and northern parts of French Massif Central. Regarding the Alpine tectonics, not only the age of the pluton and its host-rocks (instead of the Permo-Carboniferous age previously believed), but also its upper mylonitic contact, suggest revisions of the Alpine nappe model. The Cogne diorite allegedly constituted the axial part of the E-verging ``pli en retour [backfold] du Valsavaranche'', a cornerstone of popular Alpine structural models: in fact, the alleged fold limbs, as attested here by field and geochemical data, do not belong to the same unit, and the backfold hypothesis is unfounded. (C) 2012 Elsevier B.V. All rights reserved.