Objetivos de desarrollo del milenio y políticas de género en Marruecos (2008-2012)

El objetivo principal del presente trabajo es explicar de qué forma el Fondo para el Logro de los Objetivos de Desarrollo del Milenio (F-ODM) contribuyó al establecimiento de políticas de género en Marruecos. Como consecuencia de las dinámicas de interdependencia de los años 70, se hizo evidente que algunos estados no tenían la capacidad para proteger los Derechos Humanos, especialmente los derechos de las mujeres, por ésta razón las organizaciones supranacionales iniciaron lazos de cooperación con los estados para contribuir a la difusión y cumplimiento de los DD.HH. Tal es el caso de Marruecos, donde, entre el año 2008 y 2012, el F-ODM implementó un programa para promover el establecimiento de políticas de género a partir del empoderamiento de las mujeres, lo cual, contribuyó al proceso iniciado por el gobierno marroquí para fortalecer el marco normativo y mejorar la situación de las mujeres y niñas en el país.

(Table 1) Oxygen and carbon isotopic values of benthic foraminifera from the Upper Maastrichtian interval of various DSDP and ODP sites

Stable isotopic data from benthic foraminifera indicate the occurrence of at least three deepwater masses in the late Maastrichtian ocean. Given mean oceanic d18Ow of -1.0 per mil, the temperature of the coolest intermediate-depth waters was 5°-7°C, that of the deepest waters was 10°C, and that of the warmest intermediate waters was 13°-15°C. The cool intermediate-depth water mass probably originated in the high-latitude Southern Ocean. The deepest waters originated at least partly in the northern Atlantic. The source region for the warmest intermediate-depth water mass is unknown. Although much of the late Maastrichtian deep water was probably preconditioned for winter sinking by low- or middle-latitude evaporation, no more than ~11% of late Maastrichtian deep water could have been directly actuated by low-latitude sea surface evaporation. At least in the southern Atlantic and Indian Oceans, heat transport by upwelling of deep water was not the primary cause of mild sea surface and coastal temperatures.

Benthic foraminiferal number of specimens in Cretaceous samples of various DSDP and ODP Sites (Table 2)

Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the Cretaceous period. The samples analyzed are from the late Maastrichtian and within the planktic foraminiferal Abathomphus mayaroensis Zone from a wide range of oceans and paleolatitudes, including the low-latitude Sites 10 and 384 (Atlantic Ocean), 47, 171, 305, and 465 (Pacific Ocean), the mid-latitude Sites 20, 111, 356, 363, 516, 525, 527, 548, and 605 (Atlantic Ocean), 216, 217, and 758 (Indian Ocean), and the high-latitude Sites 208 (Pacific Ocean), 689,698,700,738 and 750 (Southern Ocean). Correspondence analysis, based on the 75 most common taxa, shows a clear biogeographic trend along the first correspondence axis by arranging the sites in paleolatitudinal order. The assemblages from the Tethyan Realm (i.e., low latitudes) are marked by abundant heavily calcified buliminids (such as Bulimina incisa, B. trinitatensis, B. velascoensis, and Reussella szajnochae) and Aragonia spp., whereas high-latitude faunas are characterized by abundant Alabamina creta, Gyroidinoides quadratus, and Pullenia coryelli. The results indicate that the faunas at low and high latitudes, respectively, were influenced by quite different environmental conditions. This is based on the much higher abundance of infaunal morphotypes at low and mid latitudes compared to high latitudes, suggesting that the biogeographic trend found in the data set coincides with the trophic regime at the various sites. The results also provide support for the hypothesis that postulates two simultaneous sources and mechanisms for deep-water formation during the Late Cretaceous, including warm, saline deep water produced by evaporation at low (equatorial) latitudes in contrast to the formation of cold deep waters at high (southern) latitudes.

Stable carbon and oxygen isotope ratios of foraminifera from Cretaceous and Paleocene sediments

Detailed analysis of over 200 samples of uppermost Cretaceous and Paleocene sediments from Atlantic Ocean DSDP Sites 384, 86, 95, 152, 144, 20C, 21, 356, 357, and 329 provides new information on the temperature stratification of Paleocene planktonic foraminifera, the temperature and carbon isotopic changes across the Cretaceous/Tertiary boundary, and the fluctuating temperature and carbon isotopic records through the Paleocene ~64.5-54 m.y.). There was a significant temperature rise across the Cretaceous/Tertiary boundary both at the surface and in deep waters of the Atlantic Ocean. This temperature rise occurred before the basal Tertiary 'Globigerina' eugubina Zone, so that in the oldest Paleocene sample yet analyzed from the deep sea (Site 356) temperatures are already three degrees higher at the bottom and at the surface than in the Cretaceous. The temperature rise across the boundaryis more pronounced on the bottom and in samples from higher latitudes. Accompanying the temperature rise across the boundary there is a significant shift in the carbon isotope profile. In the basal Paleocene the foraminifera of the surface zone demonstrate very negative carbon isotope values (unlike in the Cretaceous of today's ocean), while deeper dwelling species have more positive values which then decrease to the bottom. The unusual carbon isotope gradients persist through the first three million years of the Paleocene until towards the top of planktonic foraminiferal Zone P.1 (G. trinidadensis Zone) the foraminifera record a profile more positive at the surface and decreasing towards the bottom (as in today's ocean). During the Paleocene there are two noteworthy rises in surface water temperature; the first around 62-61 m.y. (G. trinidadensis Zone), and the second near the base of the Globorotalia angulata Zone, 60-59 m.y. At this time surface temperatures at low to mid latitudes reached values near 25°C, while at mid-latitude Site 384 temperature highs near 22°C were registered. At a sample spacing of around one per million years, we have only produced some of the detail of these temperature fluctuations. The later Paleocene is generally cooler and there do not seem to be any large variations either through time or latitude. Middle-latitude sites average temperatures near 15°C at the surface, while high lower latitude site temperatures range near 18°C. The most salient feature of the bottom temperature record (based on multispecific samples) through the Paleocene is its lack of fluctuations. There is an overall temperature range of 5°C at these intermediate depth sites (paleodepth estimates between 1500 and 3000 m). Higher values near 13°C accompany the surface temperature peaks around 62 and 60 m.y., while low values near 8°C occur in Zone P.2 (61-60 m.y.). We detected no change in bottom temperature across the paleocene/Eocene boundary in the few samples studied so far. While there are several fluctuations in the carbon isotope values through the early Paleocene, the general trend is one of increasingly positive values at the surface and at depth. This trend culminates in the late Paleocene (upper Zone P.4, about 56-57 m.y.) with a major excursion in the carbon isotope values. At low latitudes the range between the surface and the deepest planktonic foraminifera is a delta13C of 4 per mil as compared with a range of 2 per mil today. The carbon values drop off slightly, but remain strongly positive through the remainder of the Paleocene at most sites. Accompanying the carbon isotope excursion at Site 384 is a productivity increase and a proposed rise in the CCD.

Isolation of respiratory syncytial virus from nasopharyngeal aspirates stored at 20ºC from one to fifteen months after collection

Cell culture isolation is used for recovering respiratory syncytial virus (RSV) from respiratory specimens. As RSV is a thermolabile virus, specimens destined for inoculation into cell culture require special transport, handling, and storage. The isolation rate of RSV from nasopharyngeal aspirates (NPA) stored at 20ºC for one to 15 months after collection was investigated. A total of 126 samples considered positive for RSV by indirect fluorescence-antibody were tested by virus isolation in HEp-2 cell culture. RSV was isolated from 47/126 specimens (37.3%). These results show that RSV may be recovered from NPA stored at 20ºC by cell culture.

Avaliação da qualidade de polpa de goiaba 'Paluma' armazenada a -20ºC

Neste estudo, goiabas da cultivar 'Paluma' foram cortadas em duas partes e submetidas a diferentes processos de conservação antes do armazenamento a -20ºC. No primeiro processo a polpa dura foi triturada, acondicionada em sacos de polietileno, com espessura de 40 µm, congelada e armazenada a -20°C°, e no segundo processo a polpa dura foi cortada ao meio, branqueada em água quente a 98ºC por quatro minutos, seca e acondicionada em sacos de polietileno, com espessura de 40 µm, congelada e armazenada a -20ºC. A qualidade da polpa foi avaliada através do pH, teor de ácido ascórbico, sólidos solúveis totais, acidez total titulável, aparência, textura e coloração. As duas formas de conservação mostraram-se adequadas para preservação da polpa com boa aparência até 18 semanas. Houve redução no conteúdo de ácido ascórbico, principalmente na polpa triturada. A textura e o sabor da polpa foram afetados pelo tempo de armazenamento. Os dois procedimentos, como técnicas de preservação de goiabas pelas indústrias de alimentos, podem ser usados durante o período de safra, sendo uma boa alternativa para evitar perdas pós-colheita.

Estudo da sinterização do aço inox 316L reforçado com 3% Carbeto de Tântalo - TaC

The present work shows a contribution to the studies of development and solid sinterization of a metallic matrix composite MMC that has as starter materials 316L stainless steel atomized with water, and two different Tantalum Carbide TaC powders, with averages crystallite sizes of 13.78 nm and 40.66 nm. Aiming the metallic matrix s density and hardness increase was added different nanometric sizes of TaC by dispersion. The 316L stainless steel is an alloy largely used because it s high resistance to corrosion property. Although, its application is limited by the low wear resistance, consequence of its low hardness. Besides this, it shows low sinterability and it cannot be hardened by thermal treatments traditional methods because of the austenitic structure, face centered cubic, stabilized mainly in nickel presence. Steel samples added with TaC 3% wt (each sample with different type of carbide), following a mechanical milling route using conventional mill for 24 hours. Each one of the resulted samples, as well as the pure steel sample, were compacted at 700 MPa, room temperature, without any addictive, uniaxial tension, using a 5 mm diameter cylindrical mold, and quantity calculated to obtain compacted final average height of 5 mm. Subsequently, were sintered in vacuum atmosphere, temperature of 1290ºC, heating rate of 20ºC/min, using different soaking times of 30 and 60 min and cooled at room temperature. The sintered samples were submitted to density and micro-hardness analysis. The TaC reforced samples showed higher density values and an expressive hardness increase. The complementary analysis in optical microscope, scanning electronic microscope and X ray diffractometer, showed that the TaC, processed form, contributed with the hardness increase, by densification, itself hardness and grains growth control at the metallic matrix, segregating itself to the grain boarders

Avaliação da qualidade de polpa de goiaba 'Paluma' armazenada a -20ºC

Neste estudo, goiabas da cultivar 'Paluma' foram cortadas em duas partes e submetidas a diferentes processos de conservação antes do armazenamento a -20ºC. No primeiro processo a polpa dura foi triturada, acondicionada em sacos de polietileno, com espessura de 40 µm, congelada e armazenada a -20°C°, e no segundo processo a polpa dura foi cortada ao meio, branqueada em água quente a 98ºC por quatro minutos, seca e acondicionada em sacos de polietileno, com espessura de 40 µm, congelada e armazenada a -20ºC. A qualidade da polpa foi avaliada através do pH, teor de ácido ascórbico, sólidos solúveis totais, acidez total titulável, aparência, textura e coloração. As duas formas de conservação mostraram-se adequadas para preservação da polpa com boa aparência até 18 semanas. Houve redução no conteúdo de ácido ascórbico, principalmente na polpa triturada. A textura e o sabor da polpa foram afetados pelo tempo de armazenamento. Os dois procedimentos, como técnicas de preservação de goiabas pelas indústrias de alimentos, podem ser usados durante o período de safra, sendo uma boa alternativa para evitar perdas pós-colheita.

Efeito da duração do cio sobre a fertilidade de éguas inseminadas com sêmen eqüino diluído, resfriado a 20°C e transportado

The objective of this study was to evaluate the effect of different interval from the beginning of the heat to the ovulation on the fertility of inseminated mares with diluted equine semen, cooled at 20°C and transported. The mares were grouped with the following interval periods: T1 - period less than five days, T2 - period from five to seven days and T3 - period from 8 to 21 days. The conception rates in the first cycle were 53.85 (7/13), 52.17 (12/23) and 66.67% (10/15) for treatments 1, 2 and 3, respectively, and after three cycles, 50.00 (9/18), 48.15 (13/27) and 64.71% (11/17), in the same preceding order. The duration of heat, in the conditions of this experiment, did not influence the fertility of inseminated mares.

Efeito de diferentes concentrações espermáticas sobre a fertilidade de éguas inseminadas com sêmen eqüino diluído, resfriado a 20°C e transportado

One hundred and one estral cycles of 92 Mangalarga Marchador breed mares were analyzed to study the effect of different spermatic concentrations on different reproductive characteristics. The mares were inseminated with diluted equine semen, cooled at 20°C and transported: T1 - concentrations below 250×10 6 (177.58±41.74×10 6 viable spermatozoa per inseminate dose), T2 - concentrations between 250 and 350 10 6 sptz (315.51±20.78×106), and T3 - concentrations above 350×10 6 sptz (477.71±136.83×10 6). The conception rates in the first cycle were 43.75 (7/16), 57.89 (11/19) and 54.55% (18/33) for treatments 1, 2 and 3, respectively. After five cycles, the conception rates were 36.00 (9/25), 44.12 (15/34) and 54.76% (23/42) for treatments 1, 2 and 3, respectively. Concentrations of 177.58±41,74×10 6 viable spermatozoa per inseminate dose had moderate fertility index in a commercial program using cooled and transported semen.

Efeito antineoplásico do composto 4,2´,3´,4´-tetrametoxi chalcona em linhagem de neuroblastoma B103 de rato

Neuroblastoma é a neoplasia mais frequentemente diagnosticada na infância. O termo é comumente usado para se referir a uma ampla variedade de tumores neuroblásticos, incluindo os neuroblastomas, ganglioneuroblastomas e ganglioneuromas. Estimativas mostram que 8 milhões de crianças até 15 anos de idade por ano são atingidas por esta neoplasia, onde 80% dos casos são acometidos em até 4 anos de idade, o tumor é derivado de células malignas embrionárias advindas de células neuronais primordiais, desde gânglios simpáticos até medula adrenal e outros pontos. Neste estudo, foi avaliado o potencial citotóxico do composto 4,2´,3´,4´ tetrametoxi chalcona em modelo in vitro de neuroblastoma B103 de rato. Foram preparadas soluções estoques da droga a 50mM em dimetilsulfóxido (DMSO) e armazenadas a -20ºC para o preparo de novas concentrações (150μM, 100 μM, 75 μM e 50 μM). A viabilidade celular foi testada a partir de cultura de células da glia do córtex de rato e de neuroblastoma b103. Ensaios de migração celular e formação de colônias também foram realizados. Para a análise estatística foi realizado a análise de variância um critério (ANOVA) seguido pelo teste de Tukey, utilizando-se o programa BioEstat 5.0. Na avaliação do efeito citotóxico das chalconas, foi observado que o tratamento com o composto 4,2`3`4´- tetrametoxi chalcona não demonstrou nenhum efeito citotóxico contra células normais do córtex de rato para as concentrações testadas, enquanto que em culturas de células de neuroblastoma B103 foi demonstrado que esta droga promove a morte celular de forma significativa.

Stability of 3-bromotyrosine in serum and serum 3-bromotyrosine concentrations in dogs with gastrointestinal diseases

Abstract BACKGROUND: 3-Bromotyrosine (3-BrY) is a stable product of eosinophil peroxidase and may serve as a marker of eosinophil activation. A gas chromatography/mass spectrometry method to measure 3-BrY concentrations in serum from dogs has recently been established and analytically validated. The aims of this study were to determine the stability of 3-BrY in serum, to determine the association between peripheral eosinophil counts and the presence of an eosinophilic infiltrate in the gastrointestinal tract, and to compare serum 3-BrY concentrations in healthy dogs (n = 52) and dogs with eosinophilic gastroenteritis (EGE; n = 27), lymphocytic-plasmacytic enteritis (LPE; n = 25), exocrine pancreatic insufficiency (EPI; n = 26), or pancreatitis (n = 27). RESULTS: Serum 3-BrY concentrations were stable for up to 8, 30, and 180 days at 4°C, -20°C, and -80°C, respectively. There was no significant association between peripheral eosinophil count and the presence of eosinophils in the GI tissues (P = 0.1733). Serum 3-BrY concentrations were significantly higher in dogs with EGE (median [range] = 5.04 [≤0.63-26.26] μmol/L), LPE (median [range] = 3.60 [≤0.63-15.67] μmol/L), and pancreatitis (median [range] = 1.49 [≤0.63-4.46] μmol/L) than in healthy control dogs (median [range] = ≤0.63 [≤0.63-1.79] μmol/L; P < 0.0001), whereas concentrations in dogs with EPI (median [range] = 0.73 [≤0.63-4.59] μmol/L) were not different compared to healthy control dogs. CONCLUSIONS: The present study revealed that 3-BrY concentrations were stable in serum when refrigerated and frozen. No relationship between peripheral eosinophil count and the presence of eosinophils infiltration in the GI tissues was found in this study. In addition, serum 3-BrY concentrations were increased in dogs with EGE, but also in dogs with LPE and pancreatitis. Further studies are needed to determine whether measurement of 3-BrY concentrations in serum may be useful to assess patients with suspected or confirmed EGE or LPE.