Floral induction of mango 'Tommy Atkins' at submedio São Francisco Region, Brazil

Irregular production is a major problem in mango. In an attempt to overcome irregular bearing, effects of two antigibberellins on flowering were evaluated, uniconazole (0.25 g of active ingredient per meter of canopy tree diameter) and paclobutrazol (1.0 g of active ingredient per meter of canopy tree diameter). Treatments were applied as a soil drench using 2 L of solution per tree, in a commercial orchard of 'Tommy Atkins' mango. Treatments were applied after the second vegetative flush commenced, subsequent to pruning. Branch growth was evaluated every 30 days after treatment application up to a maximum period of 90 days. The flowering percentage was recorded at 130 days. Ammonium nitrate (NH4NO3) as a foliar spray (concentration of 0.75%) was applied five times at seven day intervals from 95 to 100 days after treatment application as a dormancy breaking treatment. It was found that both paclobutrazol (PBZ) and uniconazole (UCZ) significantly inhibited the development of vegetative growth compared to the control. Both treatments resulted in identical rates of flowering shoots, 87%; based on results, it can be concluded that the application of antigibberellins (PBZ and UCZ) inhibit vegetative development in mango 'Tommy Atkins', and promote high levels of flowering. Additional tests are being carried out in other farms to confirm these findings, for different cultivars and seasons. © ISHS 2013.

Plant regulators on vegetative growth of 'Tommy Atkins' mangoes

Paclobutrazol applied to the soil is used for the production management of mango in most of orchards on the semiarid region. However, it is necessary to identify other plant growth regulators that might be applied to the leaves, so as to minimize the risk of residues in the soil and plant. The present paper has the purpose to evaluate the effect of plant regulators in the management of vegetative growth on mangoes 'Tommy Atkins'. Three plant growth regulators, sprayed to the leaves, were evaluated: prohexadione-Ca, ethyl-trinexapac and chlormequat chloride, applied in two dosages, and compared to paclobutrazol applied to the soil. In order to compare the effects of the treatment, data were recorded on the vegetative growth (number and length of the shoots). Furthermore, the levels of gibberellins in the apical area of the shoots of 'Tommy Atkins' were quantified, from the beginning of the experiment until the beginning of floral induction. The results showed that sprayings with prohexadione-Ca, trinexapac-ethyl and chlormequat chloride in a dosage of 1.5 g a.i. plant-1 plant was as efficient as a dose of 4.0 g a.i. plant-1 of paclobutrazol applied to the soil, regarding the regulation of vegetative growth of 'Tommy Atkins'. © ISHS 2013.

Temario provisional = Provisional agenda

Incluye Bibliografía

Avaliação colostral e de níveis séricos imunes de bezerros holandezes oriundos de vacas acometidas ou não por mastite

Pós-graduação em Ciência Animal - FMVA

La evolución reciente de los procesos de integración en América Latina y el Caribe

Incluye Bibliografía

Panamá: evolución económica durante 2010

Incluye Bibliografía

An assessment of the economic impact of climate change on the coastal and human settlements, tourism and transport sectors in Barbados

This report analyses the coastal and human settlements, tourism and transport sectors in Barbados to assess the potential economic impact of climate change on the sectors. The fundamental aim of this report is to assist with the development of strategies to deal with the potential impact of climate change on Barbados. Some of the key anticipated manifestations of climate change for the Caribbean include elevated air and sea-surface temperatures, sea-level rise, possible changes in extreme events and a reduction in freshwater resources. The economic impact of climate change on the three sectors was estimated for the A2 and B2 IPCC scenarios until 2050 (tourism and transport sectors) and 2100 (coastal and human settlements sector). An exploration of various adaptation strategies was also undertaken for each sector using standard evaluation techniques. The analysis has shown that based upon exposed assets and population, SLR can be classified as having the potential to create potential catastrophe in Barbados. The main contributing factor is the concentration of socioeconomic infrastructure along the coastline in vulnerable areas. The A2 and B2 projections have indicated that the number of catastrophes that can be classified as great is likely to be increased for the country. This is based upon the possible effects of the projected unscheduled impacts to the economy both in terms of loss of life and economic infrastructure. These results arise from the A2 and B2 projections, thereby indicating that growth in numbers and losses are largely due to socioeconomic changes over the projection period and hence the need for increased adaptation strategies. A key adaptation measure recommended is for the government of Barbados to begin reducing the infrastructure deficit by continuously investing in protective infrastructure to decrease the country’s vulnerability to changes in the climate. With regard to the tourism sector, it was found that by combining the impacts due to a reduction in tourist arrivals, coral reef loss and SLR, estimated total economic impact of climate change is US $7,648 million (A2 scenario) and US $5,127 million (B2 scenario). An economic analysis of the benefits and costs of several adaptation options was undertaken to determine the cost effectiveness of each one and it was found that four (4) out of nine (9) options had high cost-benefit ratios. It is therefore recommended that the strategies that were most attractive in terms of the cost-benefit ratios be pursued first and these were: (1) enhanced reef monitoring systems to provide early warning alerts of bleaching events; (2) artificial reefs or fish-aggregating devices; (3) development of national adaptation plans (levee, sea wall and boardwalk); (4) revision of policies related to financing carbon neutral tourism; and (5) increasing recommended design wind speeds for new tourism-related structures. The total cost of climate change on international transportation in Barbados aggregated the impacts of changes in temperature and precipitation, new climate policies and SLR. The impact for air transportation ranges from US$10,727 million (B2 scenario) to US$12,279 million (A2 scenario) and for maritime transportation impact estimates range from US$1,992 million (B2 scenario) to US$2,606 million (A2 scenario). For international transportation as a whole, the impact of climate change varies from US$12,719 million under the B2 scenario to US$14,885 million under the A2 scenario. Barbados has the institutions set up to implement adaptive strategies to strengthen the resilience of the existing international transportation system to climate change impacts. Air and sea terminals and facilities can be made more robust, raised, or even relocated as need be, and where critical to safety and mobility, expanded redundant systems may be considered.

Investigação de conhecimento teórico: aceitação/rejeição ao behaviorismo radical entre professores

Pós-graduação em Educação - FFC

Associação entre indicadores do ambiente construído e variáveis individuais com atividade física no lazer e no transporte em adultos do município de Rio Claro - SP

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Efeito agudo dos exercícios com pesos sobre os níveis de leptina, adiponectina e fator de necrose tumoral alfa em adultos não treinados

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Avaliação do bem-estar durante o pré-abate e abate e condição sanitária de diferentes segmentos da produção avícola

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Paleoambiente e proveniência da formação cabeças da bacia do Parnaíba: evidências da glaciação famenniana e implicações na potencialidade do reservatório

O histórico de prospecção de hidrocarbonetos da Bacia Paleozoica do Parnaíba, situada no norte-nordeste do Brasil, sempre foi considerado desfavorável quando comparado aos super-reservatórios estimados do Pré-Sal das bacias da Margem Atlântica e até mesmo interiores, como a Bacia do Solimões. No entanto, a descoberta de gás natural em depósitos da superseqüência mesodevoniana-eocarbonífera do Grupo Canindé, que incluem as formações Pimenteiras, Cabeças e Longá, impulsionou novas pesquisas no intuito de refinar a caracterização paleoambiental, paleogeográfica, bem como, entender o sistema petrolífero, os possíveis plays e a potencialidade do reservatório Cabeças. A avaliação faciológica e estratigráfica com ênfase no registro da tectônica glacial, em combinação com a geocronologia de zircão detrítico permitiu interpretar o paleoambiente e a proveniência do reservatório Cabeças. Seis associações de fácies agrupadas em sucessões aflorantes, com espessura máxima de até 60m registram a evolução de um sistema deltaico Devoniano influenciado por processos glaciais principalmente no topo da unidade. 1) frente deltaica distal, composta por argilito maciço, conglomerado maciço, arenito com acamamento maciço, laminação plana e estratificação cruzada sigmoidal 2) frente deltaica proximal, representada pelas fácies arenito maciço, arenito com laminação plana, arenito com estratificação cruzada sigmoidal e conglomerado maciço; 3) planície deltaica, representada pelas fácies argilito laminado, arenito maciço, arenito com estratificação cruzada acanalada e conglomerado maciço; 4) shoreface glacial, composta pelas fácies arenito com marcas onduladas e arenito com estratificação cruzada hummocky; 5) depósitos subglaciais, que englobam as fácies diamictito maciço, diamictito com pods de arenito e brecha intraformacional; e 6) frente deltaica de degelo, constituída pelas fácies arenito maciço, arenito deformado, arenito com laminação plana, arenito com laminação cruzada cavalgante e arenito com estratificação cruzada sigmoidal. Durante o Fammeniano (374-359 Ma) uma frente deltaica dominada por processos fluviais progradava para NW (borda leste) e para NE (borda oeste) sobre uma plataforma influenciada por ondas de tempestade (Formação Pimenteiras). Na borda leste da bacia, o padrão de paleocorrente e o espectro de idades U-Pb em zircão detrítico indicam que o delta Cabeças foi alimentado por áreas fonte situadas a sudeste da Bacia do Parnaíba, provavelmente da Província Borborema. Grãos de zircão com idade mesoproterozóica (~ 1.039 – 1.009 Ma) e neoproterozóica (~ 654 Ma) são os mais populosos ao contrário dos grãos com idade arqueana (~ 2.508 – 2.678 Ma) e paleoproterozóica (~ 2.054 – 1.992 Ma). O grão de zircão concordante mais novo forneceu idade ²⁰⁶Pb/²³⁸U de 501,20 ± 6,35 Ma (95% concordante) indicando idades de áreas-fonte cambrianas. As principais fontes de sedimentos do delta Cabeças na borda leste são produto de rochas do Domínio Zona Transversal e de plútons Brasilianos encontrados no embasamento a sudeste da Bacia do Parnaíba, com pequena contribuição de sedimentos oriundos de rochas do Domínio Ceará Central e da porção ocidental do Domínio Rio Grande do Norte. No Famenniano, a movimentação do supercontinente Gondwana para o polo sul culminou na implantação de condições glaciais concomitantemente com o rebaixamento do nível do mar e exposição da região costeira. O avanço das geleiras sobre o embasamento e depósitos deltaicos gerou erosão, deposição de diamictons com clastos exóticos e facetados, além de estruturas glaciotectônicas tais como plano de descolamento, foliação, boudins, dobras, duplex, falhas e fraturas que refletem um cisalhamento tangencial em regime rúptil-dúctil. O substrato apresentava-se inconsolidado e saturados em água com temperatura levemente abaixo do ponto de fusão do gelo (permafrost quente). Corpos podiformes de arenito imersos em corpos lenticulares de diamicton foram formados pela ruptura de camadas pelo cisalhamento subglacial. Lentes de conglomerados esporádicas (dump structures) nos depósitos de shoreface sugere queda de detritos ligados a icebergs em fases de recuo da geleira. A elevação da temperatura no final do Famenniano reflete a rotação destral do Gondwana e migração do polo sul da porção ocidental da América do Sul e para o oeste da África. Esta nova configuração paleogeográfica posicionou a Bacia do Parnaíba em regiões subtropicais iniciando o recuo de geleiras e a influência do rebound isostático. O alívio de pressão é indicado pela geração de sills e diques clásticos, estruturas ball-and-pillow, rompimento de camadas e brechas. Falhas de cavalgamento associadas à diamictitos com foliação na borda oeste da bacia sugerem que as geleiras migravam para NNE. O contínuo aumento do nível do mar relativo propiciou a instalação de sedimentação deltaica durante o degelo e posteriormente a implantação de uma plataforma transgressiva (Formação Longá). Diamictitos interdigitados com depósitos de frente deltaica na porção superior da Formação Cabeças correspondem a intervalos com baixo volume de poros e podem representar trapas estratigráficas secundárias no reservatório. As anisotropias primárias subglaciais do topo da sucessão Cabeças, em ambas as bordas da Bacia do Parnaíba, estende a influência glacial e abre uma nova perspectiva sobre a potencialidade efetiva do reservatório Cabeças do sistema petrolífero Mesodevoniano-Eocarbonífero da referida bacia.

Potential of adjuvants to reduce drift in agricultural spraying

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Contribuição da amplitude de movimento articular do joelho na marcha de crianças com paralisia cerebral espástica

Individuals with spastic cerebral palsy show muscle weakness, difficulties in the control of agonist and antagonist muscles, decreased range of motion and tonus and sensibility alterations, especially in knee joint. These problems can interfere on the performance of functional activities such gait. The aim of this study was to analyze the contribution of knee range of motion on gait of hemiplegic and diplegic children considering their asymmetries. Twelve children, 6 hemiplegics e 6 diplegics from 7 to 12 years of age (age average= 9,5 ± 1,93) took part. Spasticity was assessed by the Ashworth’s Modified Scale and the passive knee range of motion by an eletrogoniometer. The task was to walk on a walkway of 8m long, in their preferred speed, in 6 attempts, been 3 on right and 3 on left sagital planes. Eigth passive markers were bilaterally fixed for the kinematic record. Orthogonally to the walkway, two digital camcorders were assembled on the sagital plane. The fotogrametric procedures were performed by the Dvideow 6.3 software. The Matlab 7.0.1 software was used to filter and to calculate the dependent variables. The U test of Mann- Whitney found differences to the cerebral palsy type for knee extension/hiperextension (U = - 2.943; p= 0.003), knee relative angle at heel contact (U = - 5.992; p= 0.001) and knee range during stride (U = - 4.099; p= 0.001). The Wilcoxon’s test revealed differences according to the asymmetries for the hemiplegics only for the knee relative angle at heel contact (T= - 2.635; p<0.008). The contributions of passive knee range of motion, revealed by the Spearman correlations, for the more afected limb of the diplegics, showed that the knee extension/hiperextension interfere on the cadence, stride duration and step width; the knee relative angle at heel contact change the stride length and duration and cadence; and the...(Complete abstract click electronic access below)