Anti-Candida activity of the water-soluble lectin from Moringa oleifera seeds (WSMoL).

This work reports the effects of the water-soluble lectin from Moringa oleifera seeds (WSMoL) on growth and survival of Candida species. In addition, cellular alterations linked to the antifungal effect were investigated. The minimal inhibitory (MIC) and fungicidal (MFC) concentrations were determined and 24-h growth curves in absence and presence of lectin were established. Flow cytometry was used to evaluate the induction of apoptosis/necrosis, alterations in mitochondrial membrane potential (ΔΨm), and occurrence of lysosomal damage. WSMoL inhibited the growth of C. albicans, C. glabrata, C. krusei and C. parapsilosis with MIC of 20µg/mL. The lowest MFC (20µg/mL) was detected for C. glabrata and the highest (80µg/mL) for C. albicans and C. parapsilosis. The inhibitory effect started from the ninth to nineteenth hour of incubation depending on the fungal species. Incubation with the lectin at the MIC for 24h increased the number of cells undergoing apoptosis and necrosis. Hyperpolarization of the mitochondrial membrane was detected after 12-h treatment, followed by reduction of ΔΨm or depolarization after 24h. No lysosomal damage was detected in treated cells. In conclusion, WSMoL is a fungistatic and fungicide agent against Candida with differential effects depending on the species.

Soil chemical factors and grassland species density in Emas National Park (central Brazil).

Studies of grasslands on specific soil types suggest that different nutrients can limit biomass production and, hence, species composition and number. The Brazilian cerrado is the major savanna region in America and once covered about 2 million km(2), mainly in the Brazilian Central Plateau, under seasonal climate, with wet summer and dry winter. In view of the importance of soil chemical factors in the distribution of the vegetation forms within the Cerrado domain and which may influence the number of species, we analyzed some soil characteristics in three herbaceous vegetation forms -- hyperseasonal cerrado, seasonal cerrado, and wet grassland -- in Emas National Park, a core cerrado site, to investigate the relationship between number of species and soil characteristics. We collected vegetation and soil samples in these three vegetation forms and submitted the obtained data to multiple linear regression. We found out that aluminum and pH were the best predictors of species density, the former positively related to species density and the latter negatively related. Since the predictable variation in species density is important in determining areas of conservation, we can postulate that these two soil factors are indicators of high species density areas in tropical grasslands, which could be used in selecting priority sites for conservation.

Soil chemical factors and grassland species density in Emas National Park (central Brazil) / Características químicas do solo e densidade de espécies em comunidades herbáceas no Parque Nacional das Emas (Brasil central)

Studies of grasslands on specific soil types suggest that different nutrients can limit biomass production and, hence, species composition and number. The Brazilian cerrado is the major savanna region in America and once covered about 2 million km², mainly in the Brazilian Central Plateau, under seasonal climate, with wet summer and dry winter. In view of the importance of soil chemical factors in the distribution of the vegetation forms within the Cerrado domain and which may influence the number of species, we analyzed some soil characteristics in three herbaceous vegetation forms - hyperseasonal cerrado, seasonal cerrado, and wet grassland - in Emas National Park, a core cerrado site, to investigate the relationship between number of species and soil characteristics. We collected vegetation and soil samples in these three vegetation forms and submitted the obtained data to multiple linear regression. We found out that aluminum and pH were the best predictors of species density, the former positively related to species density and the latter negatively related. Since the predictable variation in species density is important in determining areas of conservation, we can postulate that these two soil factors are indicators of high species density areas in tropical grasslands, which could be used in selecting priority sites for conservation.

Estudos em comunidades herbáceas em tipos específicos de solos sugerem que diferentes nutrientes podem limitar a produção de biomassa e, também, a composição e o número de espécies. O cerrado brasileiro é a maior região de savana na América e ocupava, originalmente, cerca de 2 milhões de km², principalmente no Planalto Central Brasileiro. Encontra-se sob clima estacional, com verão chuvoso e inverno seco. Como as variáveis químicas do solo são importantes na distribuição das formas de vegetação no domínio do Cerrado e podem influenciar no número de espécies, analisamos algumas variáveis edáficas em três formas vegetacionais herbáceas - cerrado hiperestacional, cerrado estacional e campo úmido - no Parque Nacional das Emas, uma região nuclear de cerrado, para investigar quais seriam as relações entre o número de espécies e as características do solo. Coletamos amostras de solo e vegetação nesses três ambientes e submetemos os dados obtidos a uma análise de regressão múltipla linear. Encontramos que o alumínio e o pH foram os melhores previsores da densidade de espécies, sendo o primeiro relacionado positivamente com a densidade de espécies, e o último, negativamente. Já que a variação previsível na densidade de espécies é importante para se determinar áreas de conservação, podemos postular que esses dois fatores do solo podem ser indicadores de áreas com alta densidade de espécies em comunidades herbáceas tropicais, que poderiam ser usados para a escolha de locais prioritários para conservação.

Soil characteristics of a hyperseasonal cerrado compared to a seasonal cerrado and a floodplain grassland: implications for plant community structure.

Savannas may be divided according to their seasonality into semi-seasonal, seasonal, hyperseasonal, or marshy savannas. Hyperseasonal savannas are characterized by the alternation of two contrasting stresses during each annual cycle, one induced by drought and fire and the other, by waterlogging. In South America, the largest savanna region is the Brazilian cerrado, in which there are few hyperseasonal areas that become waterlogged in the rainy season. The cerrado soils are generally well drained, but in central Brazil there is a small cerrado area in which the soil is poorly drained and which becomes waterlogged in the middle of the rainy season, allowing the appearance of a hyperseasonal cerrado. As long as soil is important in the ecology of the cerrado vegetation, we asked whether the waterlogging in this hyperseasonal cerrado implied that there were differences in soil characteristics in relation to a seasonal cerrado, which is not waterlogged in the rainy season, and to a floodplain grassland, which remains waterlogged throughout the year. In each environment, we randomly selected ten points, in which we collected soil samples in the mid-rainy season for chemical and granulometric analyses. For all variables, we found significant differences among the three environments, at least at one of the depths. Nevertheless, when we took into account all the variables together, we observed that the soils under the hyperseasonal and seasonal cerrados were similar and both were different to the soil under the floodplain grassland. The soil under the floodplain grassland was related to larger amounts of clay, silt, organic matter, phosphorus, aluminium, aluminium saturation, cation exchange capacity, and sum of bases, whereas soils under hyperseasonal and seasonal cerrados were related to higher pH values, base saturation, calcium, magnesium, and sand. As long as the soil under both cerrados was chemically and physically similar, the duration of waterlogging in the hyperseasonal cerrado is not long enough to alter its soil characteristics. Limitations to the plants growing on the hyperseasonal cerrado soil must be a consequence of the direct effects of flooding. Since cerrado plant species are dryland ones, the hypoxia caused by waterlogging may limit the number of cerrado species able to withstand these conditions.

Soil characteristics of a hyperseasonal cerrado compared to a seasonal cerrado and a floodplain grassland: implications for plant community structure

As savanas podem ser divididas de acordo com a sua estacionalidade em savanas semi-estacionais, savanas estacionais, savanas hiperestacionais ou esteros. Savanas hiperestacionais são caracterizadas pela alternância de dois estresses contrastantes durante cada ciclo anual, um induzido pela seca e fogo e outro, pelo alagamento. A maior região de savana na América do Sul é o cerrado brasileiro, que apresenta poucas áreas hiperestacionais, que se tornam alagadas durante a estação chuvosa. Os solos de cerrado são geralmente bem drenados, mas há, no Brasil central, uma pequena área de cerrado em que o solo é pobremente drenado e que se torna alagada no meio da estação úmida, possibilitando o aparecimento de um cerrado hiperestacional. Como o solo é importante para a ecologia da vegetação do cerrado, nós nos perguntamos se o alagamento no cerrado hiperestacional implicava diferenças nas características edáficas em relação ao cerrado estacional, que não alaga durante a estação chuvosa, e ao campo úmido, que permanece alagado durante o ano todo. Em cada ambiente, nós sorteamos dez pontos, em que coletamos amostras de solo, no meio da estação chuvosa, para análises químicas e granulométricas. Para todas as variáveis, encontramos diferenças significativas entre os três ambientes, ao menos em uma profundidade. Não obstante, quando analisamos todas as variáveis edáficas conjuntamente, observamos que os solos sob os cerrados hiperestacional e estacional foram semelhantes e ambos foram diferentes do solo sob o campo úmido. O solo sob campo úmido relacionou-se a maiores quantidades de argila, silte, matéria orgânica, fósforo, alumínio, saturação por alumínio, capacidade de troca catiônica e soma de bases, enquanto que os solos sob cerrados hiperestacional e estacional relacionaram-se a maiores valores de pH, areia, saturação por bases, cálcio e magnésio. Uma vez que os solos sob os dois tipos de cerrado foram similares química e fisicamente, a duração do alagamento no cerrado hiperestacional não é suficiente para alterar as suas características edáficas. Limitações para as plantas crescendo no cerrado hiperestacional devem ser conseqüência dos efeitos diretos do alagamento. Como as espécies vegetais de cerrado são espécies de áreas secas, a hipoxia causada pelo alagamento pode limitar o número de espécies de cerrado que são capazes de suportar essa condição.