ABSTRACT
BACKGROUND AND OBJECTIVES: The red blood cell Le(a-b-) phenotype was proposed as risk factor for type 1 diabetes, but contradictory results were published elsewhere. This study re-examined the potential association between Lewis histo-blood group system and type 1 diabetes. MATERIAL AND METHODS: Patients and controls of both sexes, Caucasians and non-Caucasians, matched by sex, geographical origin and ethnicity were evaluated. The red blood cell Lewis phenotypes were identified by gel column agglutination and also inferred from the FUT2 and FUT3 genotyping. RESULTS: The Le(a-b-) phenotype was prevalent in patients with type 1 diabetes, and the Le(a-b+) phenotype was prevalent in controls when both were determined by gel columns agglutination. No differences were observed in the frequencies of the Le(a-b-) phenotype inferred from the FUT2 and FUT3 genotyping between patients and controls. CONCLUSIONS: The Lewis red blood cell phenotyping and genotyping reveal divergence in the association of Le(a-b-) phenotype and type 1 diabetes.
Subject(s)
Diabetes Mellitus, Type 1/blood , Genotype , Lewis Blood Group Antigens/genetics , Phenotype , Adolescent , Adult , Case-Control Studies , Child , Child, Preschool , Female , Fucosyltransferases/genetics , Humans , Male , Middle Aged , Galactoside 2-alpha-L-fucosyltransferaseABSTRACT
As queimadas que ocorrem majoritariamente em áreas tropicais do planeta, são fontes importantes de poluentes para a atmosfera. Na América do Sul, durante os meses de inverno, uma área, principalmente de ecossistemas de cerrado e floresta, da ordem de 40 mil km² é queimada anualmente. Estas queimadas ocorrem primariamente nas regiões Amazônica e do Brasil Central, porém, através do transporte atmosférico de suas emissões resulta uma distribuição espacial de fumaça sobre uma extensa área, ao redor de 4-5 milhões de km², em muito superior a área onde estão concentradas as queimadas. Durante a combustão de biomassa são emitidos para a atmosfera gases poluentes e partículas de aerossol que interagem eficientemente com a radiação solar e afetam os processos de microfísica e dinâmica de formação de nuvens e a qualidade do ar. Os efeitos destas emissões excedem, portanto, a escala local e afetam regionalmente a composição e propriedades físicas e químicas da atmosfera na América do Sul e áreas oceânicas vizinhas, com potencial impacto em escala global.
Subject(s)
South America , Ecosystem , Biomass , Air Pollution , Environmental Pollutants , Particulate Matter , Fires , GasesABSTRACT
Heavy smoke from forest fires in the Amazon was observed to reduce cloud droplet size and so delay the onset of precipitation from 1.5 kilometers above cloud base in pristine clouds to more than 5 kilometers in polluted clouds and more than 7 kilometers in pyro-clouds. Suppression of low-level rainout and aerosol washout allows transport of water and smoke to upper levels, where the clouds appear "smoking" as they detrain much of the pollution. Elevating the onset of precipitation allows invigoration of the updrafts, causing intense thunderstorms, large hail, and greater likelihood for overshooting cloud tops into the stratosphere. There, detrained pollutants and water vapor would have profound radiative impacts on the climate system. The invigorated storms release the latent heat higher in the atmosphere. This should substantially affect the regional and global circulation systems. Together, these processes affect the water cycle, the pollution burden of the atmosphere, and the dynamics of atmospheric circulation.
