Parâmetros físicos pré-eruptivos do magmatismo ácido da província magmática do Paraná: Resultados preliminares

A set of 12 samples of acid rock types Palmas (ATP) and Chapecó (ATC) was used to determine the chemical composition of plagioclase and pyroxene by electron microprobe, with the purpose to get information about the pressure and temperature of crystallization of these rocks. The results show that the pyroxene of ATP rocks (3,2 ± 1,2 kbar, max = 5,1 kbar and 1028 ± 38°C) were formed under pressure conditions higher than those ATC (1,8 ± 0,9 kbar, max = 3,4 kbar and 995 ± 26oC). However, the pressures obtained from plagioclase showed higher pressures for ATC (3.2 ± 1 kbar, max = 6,4 kbar and 1033 ± 12°C) than ATP (1,9 ± 1 kbar, max = 4,8 kbar and 1043 ± 5°C), suggesting that the crystallization of rocktype ATP began with the formation of pyroxene and plagioclase almost simultaneously at a depth of around 17 km while the ATC, began with the crystallization of plagioclase at a depth of about 21 km (assuming a gradient of 3,3 kbar/km). The geothermometry of plagioclase allow us to calculate the concentration of water from about 1 ± 0,3% H2O for both acid rock types. Additional calculations allow us to get the depth of water exsolution of magmatic liquid at 30m below the surface. Although the data are still preliminary and insufficient to model the extrusion of these rocks, they point out to an effusion mechanism of a partially fluidized magma by volatile, which would spread to large areas with small friction with the surface that would increased with the increase of viscosity caused by the loss of volatile and decreasing of temperature, developing coherent structures as lava flows.

Spurious shifts in the pattern of diurnal variation of sea level pressure of reanalysis datasets

The main purpose of this work is to report the presence of spurious discontinuities in the pattern of diurnal variation of sea level pressure of the three reanalysis datasets from: the National Centers for Environmental Prediction (NCEP) and National Center for Atmospheric Science (R1), the NCEP and Department of Energy (R2), and the European Centre for Medium Range Weather Forecasting (ERA-40). Such discontinuities can be connected to the major changes in the global observing system that have occurred throughout reanalyses years. In the R1, the richest period in discontinuities is 1956-1958, coinciding with the start of modern radiosonde observation network. Rapid increase in the density of surface-based observations from 1967 also had an important impact on both R1 and ERA-40, with larger impact on R1. The reanalyses show discontinuities in the 1970s related to the assimilation of radiances measured by the Vertical Temperature Profile Radiometer and TIROS-N Operational Vertical Sounders onboard satellites. In the ERA-40, which additionally assimilated Special Sensor Microwave/Imager data, there are discontinuities in 1987-1989. The R1 also presents further discontinuities, in 1988-1993 likely connected to replacement/introduction of NOAA-series satellites with different biases, and to the volcanic eruption of Mount Pinatubo in June 1991, which is known to have severely affected measurements of infrared radiances for several years. The discontinuities in 1996-1998 might be partially connected to change in the type of radiosonde, from VIZ-B to VIZ-B2. The R2, which covers only satellite era (1979-on), shows discontinuities mainly in 1992, 1996-1997, and 2001. The discontinuities in 1992 and 2001 might have been caused by change in the satellite measurements and those in 1996-1997 by some changes in land-based observations network. © 2012 Springer-Verlag.

The emergence of Latin multinationals

Includes bibliography

Induction of ankylosis in the incisor for orthodontic tooth movement in rats

Background/Aim: The present research evaluated the induction of ankylosis and the eruption rate in rat incisors, with the aim of achieving stable anchorage for orthodontic tooth movement (OTM) of the molars. Material and methods: Fifteen male Wistar rats were used. In the Experimental group, the right superior incisor of each animal was extracted, denuded of the PDL and the dental papilla, and reimplanted. The Control group was the left superior incisors. The eruption rate was measured at 7, 10, 12, 14, and 16 days after replantation. NiTi closed springs with a 50cN release force were installed for additional 9 days, and the eruption rate was determined. Then, the rats were sacrificed, and ankylosis was examined by microscopic analysis. Differences with P < 0.01 were defined as statistically significant. Results: The eruption rates were 0 and 0.39 mm day-1 in the Experimental group and Control group, respectively. All incisors of the Experimental group showed ankylosis according to histological analysis. Conclusions: The methodology used to induce ankylosis in this study was effective for anchoring the incisors during the OTM of rat molars, eliminating the undesirable effects consequent to continuous eruption. © 2013 John Wiley & Sons A/S.

Class II malocclusion treatment using high-pull headgear with a splint: a systematic review

Objective: To systematically review the scientific evidence pertaining to the effectiveness of high-pull headgear in growing Class II subjects. Methods: A literature survey was performed by electronic database search. The survey covered the period from January 1966 to December 2008 and used Medical Subject Headings (MeSH). Articles were initially selected based on their titles and abstracts; the full articles were then retrieved. The inclusion criteria included growing subjects between 8 to 15 years of age, Class II malocclusion treatment with high-pull headgear, and a control group with Class II malocclusion. References from selected articles were hand-searched for additional publications. Selected studies were evaluated methodologically. Results: Four articles were selected; none were randomized controlled trials. All of the articles clearly formulated their objectives and used appropriate measures. The studies showed that high-pull headgear treatment improves skeletal and dental relationship, distal displacement of the maxilla, vertical eruption control and upper molars distalization. One of the studies showed a slight clockwise rotation of the palatal plane; the others showed no significant treatment effect. The mandible was not affected by the treatment. Conclusion: While there is still a lack of strong evidence demonstrating the effects of high-pull headgear with a splint, other studies indicate that the AP relations improve due to distalization of the maxilla and upper molars, with little or no treatment effects in the mandible. Greater attention to the design should be given to improve the quality of such trials. © 2013 Dental Press Journal of Orthodontics.

Organização e espontaneidade: a autonomia das massas no pensamento dialético de Rosa Luxemburg

Pós-graduação em Ciências Sociais - FFC

Efectos en El Salvador de las lluvias torrenciales, tormenta tropical Stan y erupción del volcán Ilamatepec (Santa Ana), octubre del 2005

Incluye Bibliografía

Distribuição dos mastócitos nas fases intra-óssea e submucosa na erupção dentária humana

Pós-graduação em Fisiopatologia em Clínica Médica - FMB

Avaliação da intrusão dos molares superiores pela técnica de ancoragem com miniplacas de titânio

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Identificação das atitudes dos pais e familiares frente ao uso da chupeta

Pós-graduação em Pediatria - FMB

An Assessment Of The Economic Impact Of Climate Change On The Transportation Sector In Montserrat

.--I. Introduction.--II. Literature review regarding climate change impacts on international transportation.--III. Economy of the Caribbean subregion and Monserrat.--IV. The international transportaion system in the Caribbean and in Monserrat.--V. Vulnerabilities of international transport system in Monserrat to climate change.--VI. Modelling.-- VII. Economic impact analysis of climate chage on the international transport.-- VIII. Approaches to mitigation and adaptation in the air and sea transportation sectors.-- IX. Conclusions

Avaliação do crescimento mandibular e desenvolvimento dentário em crianças com má oclusão de Classe II, Divisão 1, naturais e induzidos pelo tratamento ortopédico com o Bionator de Balters

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Desenvolvimento do dimorfismo sexual nos macacos-de-cheiro (Saimiri VOIGT, 1831)

Os macacos-de-cheiro, Saimiri Voigt, 1831 são primatas arbóreos e ágeis, com um corpo relativamente pequeno, se comparado a outros primatas do Novo Mundo. Distribuem-se por toda a Amazônia e parte da América Central. Vários estudos foram realizados com a finalidade de estabelecer grupos taxonômicos em Saimiri. No entanto, os resultados desses estudos mostraram uma série de divergências quanto à classificação, tanto em relação à validade dos táxons, como ao status taxonômico dos mesmos. Neste gênero, observa-se a existência de diferenças sexuais no padrão de coloração da pelagem, no tamanho e forma dos dentes caninos e, ainda, um ciclo espermatogênico anual nos machos, caracterizado pela aquisição de gordura subcutânea, denominada de "condição de engorda". Durante este período, os machos apresentam um aumento de peso variando de 15 a 20%. O presente estudo teve como objetivo investigar o dimorfismo sexual em Saimiri sciureus, comparando os resultados com os de cinco outras espécies de Saimiri (S. cassiquiarensis, S. juruanus, S. ustus, S. boliviensis e S. vanzolinii). Para tanto, foram analisados 610 espécimes pertencentes às coleções do Museu Paraense Emílio Goeldi (MPEG), Museu Nacional, Universidade Federal do Rio de Janeiro (MNRJ) e Museu de Zoologia da Universidade de São Paulo (MZUSP). As classes etárias foram determinadas de acordo com a morfologia da arcada, descrita com base na seqüência eruptiva dos dentes de leite e permanentes. Foram coletados dados sobre caracteres cromáticos, onde se analisou a coloração da mancha pré-auricular de fêmeas em relação ao processo de erupção dentária, morfologia craniana para verificação de diferenciação etária e sexual, além de vinte e uma medidas cranianas, analisadas através do Teste "t" de Student. A partir dos resultados obtidos, constatou-se que não existem diferenças na coloração da pelagem entre classes sexuais anteriores à idade adulta em nenhum dos sexos. Não foram observadas diferenças na coloração da pelagem entre classes de idade em machos. A mancha pré-auricular enegrecida é um caráter exclusivo de fêmeas adultas, mas não está estritamente relacionada à ontogenia. O aparecimento do dicromatismo sexual na pelagem não é sincronizado com o aparecimento do dimorfismo na morfologia do crânio, especialmente dos dentes. Diferenças sexuais visíveis macroscopicamente, como tamanho e forma da caixa craniana, forma da face, distância bi-zigomática e forma da mandíbula podem ser evidenciadas a partir da idade subadulta. Observou-se também que o dimorfismo sexual, para todas as espécies, é melhor evidenciado em variáveis relacionadas ao aparato mastigatório. Além disso, diferenças sexuais na morfologia dos ossos do crânio podem ser claramente observadas entre os indivíduos subadultos de qualquer táxon. Os machos se tornam maiores do que as fêmeas a partir da idade subadulta, e o caráter mais conspícuo do dimorfismo sexual é o comprimento do canino. Cada espécie difere das demais por apresentar exclusividade em alguma variável (ou conjunto de variáveis) morfométricas, evidenciando dimorfismo sexual.

Avaliação da microbiota bucal de mães e pares de crianças aos 6, 12, 18 e 24 meses de idade e sua relação com dieta alimentar, hábitos de higiene bucal, condição gengival, erupção dentária e prevalência de cárie dentária

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Avaliação histomorfométrica da movimentação dentária induzida em ratos com força contínua, contínua interrompida e intermitente

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)