Índice de expansão florística na floresta equatorial de terra-firme

Analisa as variações florísticas em uma floresta equatorial de terra-firme, próximo de Manaus, através do índice de Expansão Florística (IEF), obtido através da taxa de regeneração natural, ponderada pela abundância relativa das espécies, concluindo que existe um grupo de cinqüenta e quatro espécies que ampliaram sua representatividade na composição florística, ocupando os espaços deixados por outro grupo de cinqüenta e uma espécies que reduziram sua representatividade florística. Sendo esses dois grupos responsáveis pelas variações florísticas na área, estudada. Um outro grupo de cento e vinte e três espécies, representando cerca de 30% dos indivíduos e mais 50% das espécies, é responsável pela manutenção da fisionomia estrutural da floresta.

Distribuição espacial das espécies arbóreas da floresta equatorial de terra-firme

RESUMOAnalisa a distribuição espacial das espécies arbóreas com DAP maior ou igual a 20 cm em uma floresta equatorial de terra-firme, propondo um novo índice de dispersão ID = FrAB%, onde ID é o índice de dispersão, Fr é a frequência absoluta e AB% é a abundância relativa das espécies, concluindo que existem 39 espécies com distribuição aleatória e 108 espécies com distribuição regular, o que contraria alguns autores que afirmam ser muito rara a ocorrência desse último tipo de distribuição em florestas naturais.

A relação entre abundância e frequência na floresta equatorial de terra firme

Analisa a relação entre a abundância e a frequência absoluta através de análise de regressão a partir dos resultados de Jardim Hosohawa (1986/87), concluindo que existe uma proporcionalidade direta entre as duas variáveis, expressa pela equação Y = 3,14785 X 1,12292 onde Y é a abundância relativa e X é a frequência absoluta, de cada espécie.

Mosaic maternal ancestry in the Great Lakes region of East Africa

The Great Lakes lie within a region of East Africa with very high human genetic diversity, home of many ethno-linguistic groups usually assumed to be the product of a small number of major dispersals. However, our knowledge of these dispersals relies primarily on the inferences of historical, linguistics and oral traditions, with attempts to match up the archaeological evidence where possible. This is an obvious area to which archaeogenetics can contribute, yet Uganda, at the heart of these developments, has not been studied for mitochondrial DNA (mtDNA) variation. Here, we compare mtDNA lineages at this putative genetic crossroads across 409 representatives of the major language groups: Bantu speakers and Eastern and Western Nilotic speakers. We show that Uganda harbours one of the highest mtDNA diversities within and between linguistic groups, with the various groups significantly differentiated from each other. Despite an inferred linguistic origin in South Sudan, the data from the two Nilotic-speaking groups point to a much more complex history, involving not only possible dispersals from Sudan and the Horn but also large-scale assimilation of autochthonous lineages within East Africa and even Uganda itself. The Eastern Nilotic group also carries signals characteristic of West-Central Africa, primarily due to Bantu influence, whereas a much stronger signal in the Western Nilotic group suggests direct West-Central African ancestry. Bantu speakers share lineages with both Nilotic groups, and also harbour East African lineages not found in Western Nilotic speakers, likely due to assimilating indigenous populations since arriving in the region ~3000 years ago.

A influência do evento El Niño - Oscilação Sul e Atlântico Equatorial na precipitação sobre as regiões norte e nordeste da América do Sul

Os impactos de eventos anômalos no oceano Pacífico associados ao El Niño-Oscilação Sul (ENOS) na precipitação da região norte e nordeste da América do Sul foram avaliados para o período de 1900 a 2007, fazendo-se uso de análise de composições. Os eventos El Niño (La Niña) no Pacífico que juntamente com um Modo Equatorial no Atlântico (MEA) frio (quente) formam um gradiente interbacias entre o Pacífico e Atlântico foram analisados considerando, separadamente, aqueles para os quais o gradiente se forma na fase inicial do ENOS daqueles em que o gradiente se forma na fase de decaimento do ENOS. Os resultados mostram que o padrão de precipitação na região norte e nordeste da América do Sul é reforçado mediante a configuração do gradiente interbacias durante a fase inicial do ENOS. Nesse caso, uma possível explicação é que o MEA de sinal contrário ao ENOS durante sua fase inicial cria condições favoráveis para o desenvolvimento de um gradiente inter-hemisférico no Atlântico Tropical atuando no mesmo sentido do gradiente interbacias, e colaborando para fortalecer o efeito do El Niño (La Niña) na precipitação. Por outro lado, para os eventos ENOS em que o gradiente se forma em sua fase de decaimento, o impacto na precipitação é mais significativo na região norte e centro-oeste da bacia. Uma possível explicação para essas diferenças está associada às mudanças que ocorrem na circulação atmosférica leste-oeste associada ao gradiente leste-oeste de anomalias da TSM. Os resultados deste estudo podem ser úteis, principalmente, para fins de monitoramento climático.

60,000 years of interactions between Central and Eastern Africa documented by major African mitochondrial haplogroup L2

Mitochondrial DNA (mtDNA) haplogroup L2 originated in Western Africa but is nowadays spread across the entire continent. L2 movements were previously postulated to be related to the Bantu expansion, but L2 expansions eastwards probably occurred much earlier. By reconstructing the phylogeny of L2 (44 new complete sequences) we provide insights on the complex net of within-African migrations in the last 60 thousand years (ka). Results show that lineages in Southern Africa cluster with Western/Central African lineages at a recent time scale, whereas, eastern lineages seem to be substantially more ancient. Three moments of expansion from a Central African source are associated to L2: (1) one migration at 70-50 ka into Eastern or Southern Africa, (2) postglacial movements (15-10 ka) into Eastern Africa; and (3) the southward Bantu Expansion in the last 5 ka. The complementary population and L0a phylogeography analyses indicate no strong evidence of mtDNA gene flow between eastern and southern populations during the later movement, suggesting low admixture between Eastern African populations and the Bantu migrants. This implies that, at least in the early stages, the Bantu expansion was mainly a demic diffusion with little incorporation of local populations.

Female gender but not season of birth is associated with mood seasonality in a near-equatorial Brazilian city

OBJECTIVE: Studies conducted mainly in countries located in the Northern Hemisphere have shown that season of birth influences mood seasonality. Greater mood seasonality has been observed for individuals born during spring/summer months than those born during autumn/winter months. Expanding past research to the Southern Hemisphere, in this study we examine the influence of season of birth on mood seasonality in a sample of 1,247 healthy young Brazilians. METHOD: The Seasonal Pattern Assessment Questionnaire was used to compute a global seasonality score as a measure of mood seasonality in a cross-sectional study. RESULTS: Analysis of covariance was conducted to examine the effects of month of birth and gender on mood seasonality, with age entered as a covariate. A main effect of gender was observed, F (1, 1197) = 17.86, p < .01; partial Eta-squared = .02, with mood seasonality being higher for females (M = 8) than for males (M = 7). Contradicting previous findings, no significant main effect for month of birth was observed, F (1, 1197) = 0.65, p > .05. CONCLUSION: The unexpected finding is tentatively explained by differences in geographic location and weather fluctuations between the sampling location in Brazil and other countries where season of birth has been found to influence mood seasonality. Additional studies with larger samples from the Southern Hemisphere are necessary to shed additional light on the possible significant influence of season of birth on mood.

Diversity of non-clinical Acinetobacter species in a sub-saharan Africa region: evidence of carbapenem-hydrolysing class D-β-lactamase producers

[Excerpt] Although Acinetobacter baumannii has been the main agent for healthcare infections, recent reports suggest that some Acinetobacter environmental species should be considered as a potential cause of disease. In Angola, there are no previous data on its environmental reservoirs and resistance features. We aimed to unveil the occurrence and diversity of Acinetobacter species and the presence of resistance mechanisms in different non-clinical settings in Angola.

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 1 1868 - Ranuncul-Connar

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 2 1871 - Leguminosae-Ficoideae

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 3 1877 - Umbelliferae-Eben

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 4 (1-4) 1902-04 - Ola-Gentianeae

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 4 (1-3) 1905-06 - Hydrophyll-Pedalineae

Flora of tropical Africa /by Daniel Oliver ... assisted by other botanists.

v. 5 (1-3) 1899-1900 - Acanth-Plantagineae