Alimentação, composição corporal e cancro da mama

Introdução – A nível mundial, o cancro da mama é o tipo de cancro mais frequente nas mulheres. Estudos têm sugerido que os fatores de estilo de vida (alimentação, consumo de álcool, atividade física) e a adiposidade corporal estão implicados na sua etiologia, sobretudo nos tumores diagnosticados após a menopausa. O objetivo deste artigo foi o de identificar quais os fatores nutricionais e de composição corporal implicados na etiologia da doença e qual a sua relação. Metodologia – Foi realizada uma revisão da literatura referente a estudos de revisão, de coorte e experimentais, de acordo com a temática em estudo. Resultados – As mulheres obesas têm maior risco de desenvolver cancro da mama após a menopausa e a adiposidade corporal, localizada na região abdominal, é também fator de risco. A obesidade, além de fator promotor, relaciona-se inversamente com o prognóstico da doença. Relativamente ao padrão alimentar, a ingestão de ácidos gordos saturados confere risco, ainda que com uma associação fraca e, com uma associação modesta, a dieta mediterrânica parece estar associada a um menor risco de cancro da mama pós-menopausa. Conclusão – A adoção de um estilo de vida saudável (alimentação e atividade física) e a obtenção/manutenção de um peso corporal saudável devem ser encorajados para prevenir o cancro da mama. Mais estudos devem ser realizados no futuro para consolidar a associação com outras variáveis dietéticas. ABSTRACT - Background – Breast cancer is worldwide the most common cancer in women. Studies have suggested that lifestyle such as nutrition, alcohol intake and physical activity are enrolled in aetiology, especially in postmenopausal tumours. This review aimed to investigate the relationship between nutritional factors and body composition with the disease. Methods – A selective review of the literature for recent studies and meta-analyses on this topic. Results – Obese women have higher risk to develop breast cancer after menopause. Abdominal adiposity is also a risk factor. Obesity, beside of promote the disease, is also a negative factor of prognoses. In respect to dietary pattern, the intake of saturated fatty acids seems to attribute risk, even if with a weak association. Although with a modest association, Mediterranean diet may be associated with lower breast cancer risk among postmenopausal women. Conclusion – Adopt a healthy lifestyle (nutrition and physical activity) and maintain a healthy body weight should be encouraged to prevent breast cancer. Future research should focus other dietary variables already investigated but still with no clear evidence.

Magma flow pattern in dykes of the Azores revealed by ansiotropy of magnetic susceptibility

The localization of magma melting areas at the lithosphere bottom in extensional volcanic domains is poorly understood. Large polygenetic volcanoes of long duration and their associated magma chambers suggest that melting at depth may be focused at specific points within the mantle. To validate the hypothesis that the magma feeding a mafic crust, comes from permanent localized crustal reservoirs, it is necessary to map the fossilized magma flow within the crustal planar intrusions. Using the AMS, we obtain magmatic flow vectors from 34 alkaline basaltic dykes from São Jorge, São Miguel and Santa Maria islands in the Azores Archipelago, a hot-spot related triple junction. The dykes contain titanomagnetite showing a wide spectrum of solid solution ranging from Ti-rich to Ti-poor compositions with vestiges of maghemitization. Most of the dykes exhibit a normal magnetic fabric. The orientation of the magnetic lineation k1 axis is more variable than that of the k3 axis, which is generally well grouped. The dykes of São Jorge and São Miguel show a predominance of subhorizontal magmatic flows. In Santa Maria the deduced flow pattern is less systematic changing from subhorizontal in the southern part of the island to oblique in north. These results suggest that the ascent of magma beneath the islands of Azores is predominantly over localized melting sources and then collected within shallow magma chambers. According to this concept, dykes in the upper levels of the crust propagate laterally away from these magma chambers thus feeding the lava flows observed at the surface.