847 resultados para Ecosystem functioning


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Studies on the effects of changes in biodiversity and ecosystem functioning have been a central theme in ecology over the past two decades. Several studies have showed that the diversity of plant debris differently affects the decomposition process in aquatic and terrestrial environments, but we know very about the effects of detritus diversity on decomposition under fluctuating environmental conditions. We tested whether and how the environmental contexts, as well as the dynamic of their alternation, influence the effects of detritus diversity on the decomposition process. We performed a field experiment where we manipulate the litter diversity of 8 species of terrestrial plants decomposing (litterbags) in single and in mixture containing the eight species together in three different environmental contexts: the terrestrial environment (T), aquatic (A) and interface (I) - experimental treatment that simulates variation in flooding regime. We measured the rate of decomposition through the loss of mass of the community and each individual detritus in monocultures and mixtures. Species richness and environmental variability had no effects on the magnitude and stability of the decomposition process. However, there were significant diversity effects on the decomposition of an individual alien species, F. benjamina. Environmental context had significant effects on the magnitude and variability of decomposition. Detritus decomposition was faster and more variable on aquatic, interface and terrestrial conditions, respectively. Our results demonstrate that the diversity of plant detritus has minor effects to the decomposition across disparate environmental conditions and suggest that it is necessary to consider the potential of other abiotic factors in affect the magnitude and variability of the decomposition processes

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A strategy to measure bacterial functional redundancy was developed and tested with soils collected along a soil reclamation gradient by determining the richness and diversity of bacterial groups capable of in situ growth on selected carbon substrates. Soil cores were collected from four sites along a transect from the Jamari tin mine site in the Jamari National Forest, Rondonia, RO, Brazil: denuded mine spoil, soil from below the canopy of invading pioneer trees, revegetated soil under new growth on the forest edge, and the forest floor of an adjacent preserved forest. Bacterial population responses were analyzed by amending these soil samples with individual carbon substrates in the presence of bromodeoxyuridine (BrdU), BrdU-labeled DNA was then subjected to a 16S-23S rRNA intergenic analysis to depict the actively growing bacteria from each site, the number and diversity of bacterial groups responding to four carbon substrates (L-serine, L-threonine, sodium citrate, and or-lactose hydrate) increased along the reclamation-vegetation gradient such that the preserved forest soil samples contained the highest functional redundancy for each substrate. These data suggest that bacterial functional redundancy increases in relation to the regrowth of plant communities and may therefore represent an important aspect of the restoration of soil biological functionality to reclaimed mine spoils. They also suggest that bacterial functional redundancy may be a useful indicator of soil quality and ecosystem functioning.

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Defaunation, the loss or population decline of medium and large native vertebrates represents a significant threat to the biodiversity of tropical ecosystems. Here we review the anthropogenic drivers of defaunation, provide a brief historical account of the development of this field, and analyze the types of biological consequences of this impact on the structure and functioning of tropical ecosystems. We identify how defaunation, operating at a variety of scales, from the plot to the global level, affects biological systems along a gradient of processes ranging from plant physiology (vegetative and reproductive performance) and animal behavior (movement, foraging and dietary patterns) in the immediate term; to plant population and community dynamics and structure leading to disruptions of ecosystem functioning (and thus degrading environmental services) in the short to medium term; to evolutionary changes (phenotypic changes and population genetic structure) in the long-term. We present such a synthesis as a preamble to a series of papers that provide a compilation of our current understanding of the impact and consequences of tropical defaunation. We close by identifying some of the most urgent needs and perspectives that warrant further study to improve our understanding of this field, as we confront the challenges of living in a defaunated world. © 2013 Elsevier Ltd.

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Os artrópodes possuem uma importante função no ecossistema, pois participam da ciclagem de nutrientes, decomposição, trituração e mistura da serrapilheira. Os incêndios florestais, cada vez mais freqüentes na Amazônia, destroem a camada de serrapilheira e os artrópodes que nela vivem. O objetivo desta tese é investigar como o fogo recorrente atua sobre este processo, investigando a abundância e densidade de artrópodes de serrapilheira e as taxas de decomposição da matéria orgânica e a mineralização de C e N em uma floresta de transição da Amazônia no município de Querência, estado do Mato Grosso. Para tanto, uma parcela de 50 ha de floresta primária (500 x 1000 m) foi queimada experimentalmente a cada ano a partir de 2004, e outra área de mesmo tamanho foi mantida intacta para controle. Os artrópodes foram coletados aleatoriamente em 40 pontos distribuídos dentro da parcela, por meio de armadilhas de solo (“pitfalls”) e em 40 pontos sendo extraídos da serrapilhaira através de funis de Berlese. As coletas foram realizadas em fevereiro, abril (estação chuvosa), junho e agosto (estação seca) de 2007, após a terceira queima experimental anual. Os artrópodes foram analisados até o nível taxonômico de ordem e as formigas foram identificadas até gênero. O estudo de decomposição foi feito com 480 bolsas se serrapilheira distribuídas aleatoriamente, com 240 em cada parcela, quatro meses após a última queimada. As bolsas foram confeccionadas com malhas de nylon com aberturas de 2 mm (malha fina), e em metade delas foram feitos três orifícios de 1 cm² de cada lado, permitindo a entrada de macroartrópodes (malha grossa). Em cada bolsa foi inserido cerca de 10 g de folhas secas. A cada dois meses 30 bolsas de cada tipo de malha foi retirada de cada parcela, totalizando duas retiradas na estação seca e duas na estação chuvosa. As bolsas foram secas em estufa e pesadas novamente. A diferença entre peso seco inicial e final representou a taxa de decomposição. A cada retirada de um lote de bolsas de cada tipo de malha e de cada parcela, uma subamostra (10) destas bolsas foram selecionadas aleatoriamente para análises de análise de C e N das folhas. Os artrópodes apresentaram fortes diferenças sazonais. Na estação seca os colêmbolas ocorreram em menor abundância e as formigas ocorreram em maior abundância. Concomitantemente aos efeitos de sazonalidade, os artrópodes apresentaram diversas respostas ao fogo, com alguns grupos apresentando aumento e outros redução em abundância e densidade em diferentes datas pós-fogo, em comparação a floresta controle. Os ortópteros se destacaram por terem apresentado maior abundância em todas as datas pós-fogo em comparação a floresta controle. Em geral os macropredadores freduziram sua abundância e densidade após o fogo (formigas, besouros, dentre outros) e os engenheiros de ecossistema e decompositores foram mais abundantes (baratas, ácaros, dentre outros) em relação à floresta controle. As formigas também apresentaram diferenças entre as parcelas: maior diversidade e modificações na composição de gêneros durante a estação seca, pois o fogo favoreceu o aumento em abundância de formigas generalistas. As taxas de decomposição na parcela queimada foram menores do que na parcela controle, e as bolsas de malha fina com menores taxas de decomposição do que as bolsas de malha grossa. As taxas de C e N também foram diferentes entre as parcelas, e a razão C/N, na parcela queimada se manteve estável em todas as datas pós-fogo, enquanto na parcela controle houve declínio gradual durante o experimento seguindo as estações. Estes resultados indicam que o fogo modifica a fauna de serrapilheira, reduzindo diversas populações de artrópodes e modificando a composição deste grupo. As bolsas de malha fina indicam que a exclusão de macroartrópodes reduzem a taxa de decomposição da matéria orgânica e que os microartrópodes são mais prejudicados. O fogo também reduz o processo de mineralização de C e N já que a razão C/N se manteve estável na parcela queimada. Este estudo demonstra que o fogo recorrente tem forte efeito sobre artrópodes de serrapilheira e ciclagem de nutrientes em florestas de transição da Amazônia.

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

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The Large Scale Biosphere Atmosphere Experiment in Amazonia (LBA) is a long-term (20 years) research effort aimed at the understanding of the functioning of the Amazonian ecosystem. The strong biosphere-atmosphere interaction is a key component of the ecosystem functioning. Two aerosol components are the most visible: The natural biogenic emissions of particles and VOCs, and the biomass burning emissions. Two aerosol and trace gases monitoring stations were operated for 4 years in Manaus and Porto Velho, two very distinct sites, with different land use change. Manaus is a very clean and pristine site and Porto Velho is representative of heavy land use change in Amazonia. Aerosol composition, optical properties, size distribution, vertical profiling and optical depth were measured from 2008 to 2012. Aerosol radiative forcing was calculated over large areas. It was observed that the natural biogenic aerosol has significant absorption properties. Organic aerosol dominates the aerosol mass with 80 to 95%. Light scattering and light absorption shows an increase by factor of 10 from Manaus to Porto Velho. Very few new particle formation events were observed. Strong links between aerosols and VOC emissions were observed. Aerosol radiative forcing in Rondonia shows a high -15 watts/m² during the dry season of 2010, showing the large impacts of aerosol loading in the Amazonian ecosystem. The increase in diffuse radiation changes the forest carbon uptake by 20 to 35%, a large increase in this important ecosystem.

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Atmospheric nitrogen (N) and phosphorus (P) depositions are expected to increase in the tropicsrnas a consequence of increasing human activities in the next decades. Furthermore, a possiblernshortened El Niño Southern Oscillation cycle might come along with more frequent calcium (Ca)rndepositions on the eastern slope of the Ecuadorian Andes originating from Saharan dust. It isrncrucial to understand the response of the old-growth montane forest in Ecuador to increasedrnnutrient deposition to predict the further development of this megadiverse ecosystem.rnI studied experimental additions of N, P, N+P and Ca to the forest and an untreatedrncontrol, all in a fourfold replicated randomized block design. These experiments were conductedrnin the framework of a collaborative research effort, the NUtrient Manipulation EXperimentrn(NUMEX). I collected litter leachate, mineral soil solution (0.15 and 0.30 m depths), throughfallrnand fine litterfall samples and determined N, P and Ca concentrations and fluxes. This approachrnalso allowed me to assess whether N, P and/or Ca are limiting nutrients for forest growth.rnFurthermore, I evaluated the response of fine root biomass, leaf area index, leaf area and specificrnleaf area, tree diameter growth and basal area increment contributed from a cooperating group inrnthe Ca applied and control treatments.rnDuring the observation period of 16 months after the first fertilizer application, less thanrn10, 1 and 5% of the applied N, P and Ca, respectively, leached below the organic layer whichrncontained almost all roots but no significant leaching losses occurred to the deeper mineral soil.rnDeposited N, P and Ca from the atmosphere in dry and wet form were, on balance, retained in therncanopy in the control treatment. Retention of N, P and Ca in the canopy in their respectiverntreatments was reduced resulting in higher concentrations and fluxes of N, P and Ca inrnthroughfall and litterfall. Up to 2.5% of the applied N and 2% of the applied P and Ca werernrecycled to the soil with throughfall. Fluxes of N, P and Ca in throughfall+litterfall were higher inrnthe fertilized treatments than in the control; up to 20, 5 and 25% of the applied N, P and Ca,rnrespectively, were recycled to the soil with throughfall+litterfall.rnIn the Ca-applied plots, fine root biomass decreased significantly. Also the leaf area of thernfour most common tree species tended to decrease and the specific leaf area increasedrnsignificantly in Graffenrieda emarginata Triana, the most common tree species in the study area.rnThese changes are known plant responses to reduced nutrient stress. Reduced aluminium (Al)rntoxicity as an explanation of the Ca effect was unlikely, because of almost complete organocomplexationrnof Al and molar Ca:Al concentration ratios in solution above the toxicity threshold.rnThe results suggest that N, P and Ca co-limit the forest ecosystem functioning in thernnorthern Andean montane forests in line with recent assumptions in which different ecosystemrncompartments and even different phenological stages may show different nutrient limitationsrn(Kaspari et al. 2008). I conclude that (1) the expected elevated N and P deposition will bernretained in the ecosystem, at least in the short term and hence, quality of river water will not bernendangered and (2) increased Ca input will reduce nutrient stress of the forest.

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So far, seed limitation as a local process, and dispersal limitation as a regional process have been largely neglected in biodiversity-ecosystem functioning research. However, these processes can influence both local plant species diversity and ecosystem processes, such as biomass production. We added seeds of 60 species from the regional species pool to grassland communities at 20 montane grassland sites in Germany. In these sites, plant species diversity ranged from 10 to 34 species m(-2) and, before manipulation, diversity was not related to aboveground biomass, which ranged from 108 to 687 g m(-2). One year after seed addition, local plant species richness had increased on average by six species m(-2) (29%) compared with control plots, and this increase was highest in grasslands with intermediate productivity. The increased diversity after adding seeds was associated with an average increase of aboveground biomass of 36 g m(-2) (14.8%) compared with control plots. Thus, our results demonstrate that a positive relationship between changes in species richness and productivity, as previously reported from experimental plant communities, also holds for natural grassland ecosystems. Our results show that local plant communities are dispersal limited and a hump-shaped model appears to be the limiting outline of the natural diversity-productivity relationship. Hence, the effects of dispersal on local diversity can substantially affect the functioning of natural ecosystems.