Objective: To evaluate the effect of pasteurization on antioxidant and oxidant properties of human milk. Methods: 42 samples of milk before and after pasteurisation were used to evaluate the antioxidant activity by the ferric reducing capacity and by scavenging the 2,2’-azino-bis 3-ethylbenzthiazoline-6-sulfonic acid radical. Lipid peroxidation was estimated by the concentration of malondialdehyde product using the thiobarbituric acid reactive substances assay and by the evaluation of advanced oxidation protein products. Results: No significant difference was observed in fresh human milk and after pasteurization in relation to antioxidant properties determined by the ferric reducing capacity (50.0±3.4% and 48.8±3.0%, respectively) and by scavenging the 2,2’-azino-bis 3-ethylbenzthiazoline-6-sulfonic acid radical (28.9±1.5% and 31.2±1.3%, respectively). The results of malondialdehyde (62.6±4.1 and 64.3±3.6 µM/mg) and protein oxidation products (59.4±3.4 and 54.2±3.8 µM/L) of fresh and pasteurized milk, respectively, did not exhibited any significant difference. Conclusions: This data showed that human milk has an important antioxidant activity and that the pasteurizing process does not influence the antioxidant capacity, avoiding the peroxidation of breast milk lipids and the formation of advanced protein oxidation products.
Brazil has always been one of the most important coffee producing countries. Lately, there has equally been a renewed interest in alternative coffee production systems. The state of Espírito Santo is the second greatest coffee producer in Brazil; so, we used local coffee plantations to evaluate the relations between soil macrofauna and chemical and microbiological soil properties to identify which of these properties discriminate more effectively between the organic management system (OS) and the conventional management system (CS) of coffee plantations. For each of these two cultivation systems we chose three coffee farms who employed both cultivation systems and picked out the most similar fields from each property. At each site, first we sampled the litter at the soil surface. Afterwards, we sampled nine soil monoliths to evaluate the macrofauna, in summer and winter. We also collected nine supplemental soil samples, taken at a few centimeters from the soil monoliths, for chemical and microbiological analyses. Macrofauna density was evaluated by ANOVA and multivariate analysis. The chemical and microbiological properties are environmental variables, while the data on macrofauna are the explanatory variables. The total number of individuals recovered in this study was 3,354, and the climate, identified by the sampling season, was a great modulator of macrofauna, with higher numbers in winter. The principal components analysis showed that soil moisture, organic matter, nitrogen, phosphorus, boron, copper, pH, acid and alkaline phosphatases and microbial biomass carbon, were the most outstanding ones to discriminate both cultivation systems. We found no statistical significant differences in macrofauna density between OS and CS, probably due to a general great variability, since there was a tendency for much greater values in OS. We detected the interference of chemical and microbiological soil properties on the macrofauna community in both systems of coffee cultivation, and some results clearly correlated much better with climate data than with other factors. To our knowledge, this is the first time in which the data point to a clear separation between the more numerous and diversified soil macrofauna in coffee with organic cultivation from that with a conventional cultivation system.
O objetivo deste estudo foi analisar possíveis influências do local da desova no sucesso da eclosão e na duração da incubação de Caretta caretta (Linnaeus, 1758) no sul do estado do Espírito Santo. Geomorfologicamente a área da desova na praia da Guanabara, em Anchieta (ES), pode ser dividida em praia aberta e berma. Durante quatro estações reprodutivas foram coletados dados sobre o tamanho dos sedimentos, a altura dos ninhos em relação ao nível do mar, a compartimentação geomorfológica da praia, a data da desova, o número de filhotes vivos e o tamanho da ninhada. Os resultados mostraram variações dos principais parâmetros sedimentológicos entre os anos, indicando que as temporadas reprodutivas devem ser analisadas individualmente. O sucesso da eclosão não foi afetado pelas características geológicas do local da desova. A duração da incubação não variou entre a praia e a berma, apesar das diferenças significativas no tamanho do sedimento, na profundidade dos ninhos e na altura em relação ao nível do mar. A duração da incubação se correlacionou positivamente ao tamanho dos sedimentos, com ninhos em sedimentos mais grossos eclodindo mais cedo que os ninhos localizados em sedimentos mais finos. Como as características dos ninhos influenciam a duração da incubação, recomenda-se que a transferência de ninhos, quando inevitável, respeite as diferenças entre os locais de desova, principalmente, quanto à profundidade da câmara de ovos.
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