1000 resultados para 191-1179
Resumo:
It is well known that exposure to low doses of lead causes long-lasting neurobehavioural deficits, but the cellular changes underlying these behavioural changes remain to be elucidated. A protective role of glial cells on neurons through lead sequestration by astrocytes has been proposed. The possible modulation of lead neurotoxicity by neuron-glia interactions was examined in three-dimensional cultures of foetal rat telencephalon. Mixed-brain cell cultures or cultures enriched in either neurons or glial cells were treated for 10 days with lead acetate (10(-6) m), a concentration below the limit of cytotoxicity. Intracellular lead content and cell type-specific enzyme activities were determined. It was found that in enriched cultures neurons stored more lead than glial cells, and each cell type alone stored more lead than in co-culture. Moreover, glial cells but not neurons were more affected by lead in enriched culture than in co-culture. These results show that neuron-glia interactions attenuate the cellular lead uptake and the glial susceptibility to lead, but they do not support the idea of a protective role of astrocytes.
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Annales très abrégées jusque vers le milieu du XVII e siècle, et plus développées ensuite. — On y a inséré un certain nombre de gravures et de pièces imprimées, parmi lesquelles : Épitaphe de Matthieu Molé, avec son portrait gravé par Robert Nanteuil, 1656, exemplaire sur vélin, placard grand in-folio (fol. 36) ; — Épitaphe de Pompone II de Bellièvre, avec son portrait en pied, gravé par J. Lenfant, 1657, placard grand in-folio (fol. 74) ; — Factums (fol. 43, etc.) ; — « Mausolée fait pour le service de la Reine dans l'église... de Saint-Germain-des-Prez..., 15 septembre 1683 », planches gravées (fol. 139 et 140) ; — Mandements impr. du cardinal de Furstemberg, abbé de Saint-Germain-des-???Prés, et autres (fol. 156, etc.) ; — Prospectus de l'édition de la Divina Bibliotheca de saint Jérôme, par les PP. Jean MARTIANAY et Antoine POUGET, 1693, in-8°, impr. (fol. 181) ; — « Lettre de M r PINSON, advocat en Parlement, adressée à M r Chassebras, escuyer, seigneur de Cramailles, du 1 er may 1692 », sur plusieurs religieux de l'abbaye de Saint-Germain-des-Prés, in-4°, impr. (fol. 191) ; — Planches gravées d'archéologie (fol. 247 et 248). — On remarque, en outre : Plans manuscrits de l'église de Saint-Germain-des-Prés, en 1644, « année de son rétablissement » (fol. 66), et en décembre 1656 (fol. 67), — et Plan des modifications introduites dans l'édifice entre ces deux dates (fol. 68) ; — Déclaration orig. de Robert « Audrenas » et d'« Anne Marcellin », sa femme, concernant une relique de saint Benoît, 1657 (fol. 70), — et Pièces, manuscrites et impr., concernant diverses reliques transférées à Saint-Germain-des-Prés (fol. 249) ; — « Livre des fondations faictes à l'abbaye de Sainct-Germain-des-Prez », 1613-1713 (fol. 229) ; — « Extraict du Registre des choses notables arrivées dans le monastère de Saint-Germain-des-Prez, à Paris », 1683, sur la mort de Louis-César de Bourbon, comte du Vexin, abbé de Saint-Germaindes-Prés (fol. 233). — Table des matières (fol. 253).
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Swiss national cancer mortality statistics from 1951 to 1984 and survival rates from the Vaud Cancer Registry datafile over the period 1974-1980 were considered in terms of sex ratios. Overall age-standardized cancer mortality for population aged 35-64 showed only a moderate decline in males (from 230 to 221/100,000), but a substantial one in females (from 191 to 152/100,000). Mortality from most cancer sites (except gallbladder and thyroid) was persistently higher in males, the male/female ratio ranging between 1.2 for intestines, skin, brain and lympho-reticular neoplasms to about 2 for stomach or pancreas, up to 7-10 for lung and cancers related to tobacco and alcohol (mouth or pharynx, oesophagus). The sex ratio for lung cancer increased between the early 1950's and the mid 1960's, but noticeably declined thereafter, probably reflecting trends in smoking prevalence among subsequent generations of Swiss males and females. Less obvious is the substantial increase in the sex ratio for liver cancer (from 1.6 to 5.7), which was evident in younger middle age, too. Population-based cancer survival statistics indicated that for most common sites rates were appreciably higher in females than in males. Thus, better survival explains part of the advantage in cancer mortality for women. This can be related to earlier diagnosis, better compliance or responsiveness to treatment, although there is no obvious single interpretation for this generalized more favourable pattern in females.
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We combined structural analysis, thermobarometry and oxygen isotope geochemistry to constrain the evolution of kyanite and/or andalusite-bearing quartz veins from the amphibolite facies metapelites of the Simano nappe, in the Central Alps of Switzerland. The Simano nappe records a complex polyphase tectonic evolution associated with nappe stacking during Tertiary Alpine collision (D1). The second regional deformation phase (132) is responsible for the main penetrative schistosity and mineral lineation, and formed during top-to-the-north thrusting. During the next stage of deformation (D3) the aluminosilicate-bearing veins formed by crystallization in tension gashes, in tectonic shadows of boudins, as well as along shear bands associated with top-to-the-north shearing. D2 and D3 are coeval with the Early Miocene metamorphic peak, characterised by kyanite + staurolite + garnet + biotite assemblages in metapelites. The peak pressure (P) and temperature (T) conditions recorded are constrained by multiple-equilibrium thermobarometry at 630 +/- 20 degrees C and 8.5 +/- 1 kbar (similar to 27 km depth), which is in agreement with oxygen isotope thermometry indicating isotopic equilibration of quartz-kyanite pairs at 670 +/- 50 degrees C. Quartz-kyanite pairs from the aluminosilicate-bearing quartz veins yield equilibration temperatures of 645 +/- 20 degrees C, confirming that the veins formed under conditions near metamorphic peak. Quartz and kyanite from veins and the surrounding metapelites have comparable isotopic compositions. Local intergranular diffusion in the border of the veins controls the mass-transfer and the growth of the product assemblage, inducing local mobilization of SiO2 and Al2O3. Andalusite is absent from the host rocks, but it is common in quartz veins, where it often pseudomorphs kyanite. For andalusite to be stable at T-max, the pressure in the veins must have been substantially lower than lithostatic. An alternative explanation consistent with structural observations would be inheritance by andalusite of the kyanite isotopic signature during polymorphic transformation after the metamorphic peak.
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Introduction : Les kystes intra-vitréens congénitaux sont rares et ne causent en général pas de complications oculaires. Objectifs et Méthodes : Nous rapportons le cas d'un kyste intra-vitréen non pigmenté que nous avons suivi pendant six ans pour analyser son comportement de croissance. Observation : Il s'agit d'un patient de 62 ans suivi pour un syndrome de Morbihan qui a consulté à cause d'une ombre aperçue dans le champ visuel de l'OD. L'AV était à 1,0 corrigée. L'examen à la lampe à fente a montré la présence d'un kyste transparent flottant dans le vitré. L'ultrason a confirmé l'existence d'un kyste avec un diamètre de 4,37 mm. Ce kyste était entouré d'un deuxième kyste plus grand de 7,15 mm de diamètre. Un contrôle clinique après six ans a montré que les diamètres des kystes ont augmenté à 6.20 mm pour le petit, et 7.95 mm pour le grand kyste. Les volumes des kystes ont augmenté de 43.70 mm3 à 124,97 mm3 pour le petit et de 191.39 mm3 à 263.09 mm3 pour le grand kyste. Discussion : Étant donné que les kystes n'avaient pas d'influence sur l'acuité visuelle, aucun traitement n'a été proposé. Conclusion : Un kyste intra-vitréen non pigmenté peut augmenter considérablement en volume durant six ans d'observation.
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In the Wadi Wasit area (Central Oman Mountains), Dienerian breccias are widespread. These breccias consist mostly of Guadalupian reefal blocks, often dolomitised, and some rare small-sized blocks of lowermost Triassic bivalve-bearing limestones. A unique block, with a size of about 200 m(3), including Permian and earliest Triassic faunas has been studied in detail. The so-called Wadi Wasit block consists of three major lithological units. A basal unstratified grey limestone is rich in various reef-building organisms (rugose corals, calcareous sponges, stromatoporoids) and has been dated as Middle Permian. It is disconformably overlain by well- and thin-bedded light grey to yellowish coloured limestones rich in molluscs. Two major lithologies (Coquina Limestone respectively Bioclastic Limestone unit) characterise the shelly limestones, their contact seems gradual. These two units are well-dated; they are of Griesbachian age and contain three conodont zones, the Parvus Zone, the Staeschei Zone and the Sosioensis Zone, and two ammonoid zones, the Ophiceras tibeticum Zone and an 'unnamed interval'. The third unit consists of a grey marly limestone containing Neospathodus kummeli (basal Dienerian). It is the first record of well-dated basal Triassic sediments in the Arabian Peninsula. The Coquina Limestone is dominated by the bivalve Promyalina with some Claraia and Eumorphotis. This bivalve association is interpreted as a pioneering opportunistic assemblage. Towards the top of the Bioclastic Limestone unit, the faunal diversity increases and contains probably more than 20 taxa of bivalves, microgastropods, crinoids, brachiopods, ammonoids, echinoid spines, ostracods and conodonts. The generic diversity of this biofacies exceeds by far any other Griesbachian assemblage known. Our data give new evidence for the geodynamical history for the distal carbonate shelf bordering the Hawasina Basin. A break in the sedimentation characterises the Late Permian. The basal Triassic shows a steady transgression and the breccias may record a distinct gravitational collapse of platform margins linked with sea-level low stand at the end of Induan time (late Dienerian-basal Smithian). delta(13)C(carb) isotopic analyses were performed and yield typical Permian values of around 4parts per thousand for the Reefal Limestone, with a strong negative shift across the Permian-Triassic boundary. During the Griesbachian values shift positively from 0.5 to 3.1parts per thousand parallel to an increase in faunal diversity and probably primary productivity. The detailed faunal analysis and the discovery of an unexpected diversity give,us a new understanding of the recovery of the Early Triassic marine ecosystem.
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O estudo do balanço de água no solo com cana-de-açúcar, cultivada em larga escala no Brasil, é essencial para o manejo agrícola, visando ao aumento de produtividade e à redução de riscos de poluição. Este estudo objetivou avaliar os componentes da equação do balanço de água em dois Latossolos cultivados com cana-de-açúcar (cana-planta), localizados nos Municípios de Jaboticabal e Pirassununga (São Paulo). Na área experimental de Jaboticabal, o estudo foi realizado entre os dias 30 de setembro de 2005 e 12 de julho de 2006, e constou de dois tratamentos: T1 (sem adubação nitrogenada) e T2 (120 kg ha-1 de N). Em Pirassununga, o estudo foi feito entre os dias 28 de setembro de 2005 e 08 de junho de 2006, mas apenas o tratamento T2. O delineamento experimental foi o de blocos aleatórios, com quatro repetições. O volume de controle utilizado para o balanço de água teve como limite superior a superfície do solo e como limite inferior outra paralela à primeira, localizada em profundidade de 0,90 m. As variações de armazenagem, as entradas (precipitação pluvial e ascensão capilar) e as saídas de água (evapotranspiração real e drenagem interna) nesse volume de solo, nas áreas experimentais de Jaboticabal e Pirassununga, foram determinadas em 13 e 10 períodos, respectivamente. Ambas as áreas estudadas eram planas e não irrigadas. Na área de Jaboticabal, em todo o período, tanto a perda de água por drenagem interna quanto o ganho por ascensão capilar foram maiores no tratamento T2 (-191,69 mm/5,33 mm e -238,37 mm/24,60 mm para T1 e T2, respectivamente); não houve diferença significativa de produtividade (145 e 146 t ha-1 para T1 e T2, respectivamente), nem de evapotranspiração real (1.058 mm para T1 e 1.028 mm para o T2) entre os tratamentos nesse ciclo de cana-planta, fazendo com que as plantas não adubadas apresentassem a mesma eficiência do uso da água (14 kg m-3) que as adubadas. Na área de Pirassununga, a drenagem interna e a ascensão capilar foram de -110,9 e 0,67 mm, respectivamente, e a eficiência de uso da água 13 kg m-3. Portanto, pode-se concluir que (a) nos períodos de alta pluviosidade, a drenagem interna foi significativa, alertando para possíveis problemas no manejo em relação a uma potencial de contaminação do lençol freático, e (b) tanto a evapotranspiração real quanto à eficiência do uso da água foram da mesma ordem de grandeza, independentemente da adubação nitrogenada, e a armazenagem de água no solo foi praticamente a mesma no início e no fim do ciclo estudado.
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Dispersed information on water retention and availability in soils may be compiled in databases to generate pedotransfer functions. The objectives of this study were: to generate pedotransfer functions to estimate soil water retention based on easily measurable soil properties; to evaluate the efficiency of existing pedotransfer functions for different geographical regions for the estimation of water retention in soils of Rio Grande do Sul (RS); and to estimate plant-available water capacity based on soil particle-size distribution. Two databases were set up for soil properties, including water retention: one based on literature data (725 entries) and the other with soil data from an irrigation scheduling and management system (239 entries). From the literature database, pedotransfer functions were generated, nine pedofunctions available in the literature were evaluated and the plant-available water capacity was calculated. The coefficient of determination of some pedotransfer functions ranged from 0.56 to 0.66. Pedotransfer functions generated based on soils from other regions were not appropriate for estimating the water retention for RS soils. The plant-available water content varied with soil texture classes, from 0.089 kg kg-1 for the sand class to 0.191 kg kg-1 for the silty clay class. These variations were more related to sand and silt than to clay content. The soils with a greater silt/clay ratio, which were less weathered and with a greater quantity of smectite clay minerals, had high water retention and plant-available water capacity.
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Este trabalho teve como objetivo estabelecer curvas de acúmulo de macronutrientes na cultura do girassol. Para isso, foi instalado um experimento em campo sobre Latossolo Vermelho distroférrico de textura muito argilosa, localizado na fazenda experimental da Embrapa Soja, em Londrina/PR. As parcelas foram constituídas de 14 linhas com 25 m de comprimento cada e espaçamento entrelinhas de 0,70 m, resultando em área total de 245 m². Cada parcela foi repetida quatro vezes. A adubação de semeadura foi de 300 kg ha-1 da fórmula 5-20-20, aplicada a lanço, antes do plantio. A adubação de cobertura foi parcelada em duas aplicações: 25 e 1 kg ha-1 de N e B, respectivamente, sendo a primeira aos 21 e a segunda aos 35 dias após a semeadura. O híbrido utilizado foi o BRS-191, e a densidade final de plantas foi de 40.000 plantas ha-1. Amostras de plantas foram coletadas em intervalos de 14 dias após a emergência e separadas em pecíolos, folhas, caules e, quando existentes, em capítulo e em aquênios. Após secagem, cada parte da planta foi pesada e moída para, em seguida, determinarem-se os teores de N, P, K, Ca, Mg e S. A partir desses nutrientes e da matéria seca de cada parte da planta, foram obtidas as curvas de acúmulo. Verificou-se que, para obtenção de produtividades superiores a 3.000 kg ha-1, o híbrido BRS 191 extrai aproximadamente 150, 24, 286, 116, 42 e 24 kg ha-1 de N, P, K, Ca, Mg e S, respectivamente, resultando na seguinte ordem de extração: K > N > Ca > Mg > P = S. Em relação à exportação, a ordem dos nutrientes foi a seguinte: N > P = K > Mg = S > Ca. Portanto, atenção especial deve ser dada à manutenção da adequada disponibilidade de N, K e Ca, devido à alta demanda da cultura por esses nutrientes.
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We analyzed the species distribution of Candida blood isolates (CBIs), prospectively collected between 2004 and 2009 within FUNGINOS, and compared their antifungal susceptibility according to clinical breakpoints defined by the European Committee on Antimicrobial Susceptibility Testing (EUCAST) in 2013, and the Clinical and Laboratory Standards Institute (CLSI) in 2008 (old CLSI breakpoints) and 2012 (new CLSI breakpoints). CBIs were tested for susceptiblity to fluconazole, voriconazole and caspofungin by microtitre broth dilution (Sensititre(®) YeastOne? test panel). Of 1090 CBIs, 675 (61.9%) were C. albicans, 191 (17.5%) C. glabrata, 64 (5.9%) C. tropicalis, 59 (5.4%) C. parapsilosis, 33 (3%) C. dubliniensis, 22 (2%) C. krusei and 46 (4.2%) rare Candida species. Independently of the breakpoints applied, C. albicans was almost uniformly (>98%) susceptible to all three antifungal agents. In contrast, the proportions of fluconazole- and voriconazole-susceptible C. tropicalis and F-susceptible C. parapsilosis were lower according to EUCAST/new CLSI breakpoints than to the old CLSI breakpoints. For caspofungin, non-susceptibility occurred mainly in C. krusei (63.3%) and C. glabrata (9.4%). Nine isolates (five C. tropicalis, three C. albicans and one C. parapsilosis) were cross-resistant to azoles according to EUCAST breakpoints, compared with three isolates (two C. albicans and one C. tropicalis) according to new and two (2 C. albicans) according to old CLSI breakpoints. Four species (C. albicans, C. glabrata, C. tropicalis and C. parapsilosis) represented >90% of all CBIs. In vitro resistance to fluconazole, voriconazole and caspofungin was rare among C. albicans, but an increase of non-susceptibile isolates was observed among C. tropicalis/C. parapsilosis for the azoles and C. glabrata/C. krusei for caspofungin according to EUCAST and new CLSI breakpoints compared with old CLSI breakpoints.