RESUMEN
Biomass burning in the Brazilian Amazon is modulated by climate factors, such as droughts, and by human factors, such as deforestation, and land management activities. The increase in forest fires during drought years has led to the hypothesis that fire activity decoupled from deforestation during the twenty-first century. However, assessment of the hypothesis relied on an incorrect active fire dataset, which led to an underestimation of the decreasing trend in fire activity and to an inflated rank for year 2015 in terms of active fire counts. The recent correction of that database warrants a reassessment of the relationships between deforestation and fire. Contrasting with earlier findings, we show that the exacerbating effect of drought on fire season severity did not increase from 2003 to 2015 and that the record-breaking dry conditions of 2015 had the least impact on fire season of all twenty-first century severe droughts. Overall, our results for the same period used in the study that originated the fire-deforestation decoupling hypothesis (2003-2015) show that decoupling was clearly weaker than initially proposed. Extension of the study period up to 2019, and novel analysis of trends in fire types and fire intensity strengthened this conclusion. Therefore, the role of deforestation as a driver of fire activity in the region should not be underestimated and must be taken into account when implementing measures to protect the Amazon forest.
RESUMEN
Abstract This research evaluated the effect of flooding on the microphytobenthos community structure in a microbial mat from a tropical salt flat. Field samples were collected during four consecutive days: on the first three days the salt flat was dry, on the fourth day it was flooded by rain. In order to evaluate the community maintained in flood conditions, samples from this area were collected and kept in the laboratory for 10 days with sea water. The results of total abundance of microphytobenthos varied from 4.2 × 108 to 2.9 × 109 organisms L–1, total density increased one order of magnitude under the effect of water for both situations of precipitation in the salt flat and in experimental conditions, an increase due to the high abundance of Microcoleus spp. Shannon index (H’) was higher during the desiccation period. Our data suggest that changes in the abundance of organisms were due to the effect of water. The dominance of the most abundant taxa remained the same under conditions of desiccation and influence of water, and there is probably a consortium of microorganisms in the microbial mat that helps to maintain these dominances.
Resumo Esse trabalho avaliou os efeitos da inundação na estrutura da comunidade microfitobentônica de um tapete microbiano em uma planície hipersalina tropical. As amostragens foram realizadas no campo durante quatro dias consecutivos: nos três primeiros dias o local estava seco e no quarto dia foi inundando com chuva. Para avaliar a comunidade mantida em condições de inundação, foram coletadas amostras dessa região, sendo mantidas em laboratório por 10 dias com água do mar. Os resultados mostraram que a abundância total do microfitobentos variou de 4.2 × 108 a 2.9 × 109 organismos L–1, a densidade aumentou em uma ordem de grandeza com a influência da água, tanto na planície hipersalina como nas condições experimentais, um aumento que foi devido às maiores abundâncias de Microcoleus spp. O índice de Shannon (H’) foi mais elevado durante o período de dessecação. Nossos dados sugerem que as mudanças na abundância dos organismos foram devidas ao efeito da água, a dominância dos táxons mais abundantes permaneceu a mesma durante as condições de dessecação e inundação, e possivelmente existe um consórcio entre os microrganismos do tapete microbiano no qual eles ajudam a manter essa dominância.
Asunto(s)
Clima Tropical , Adaptación Fisiológica/fisiología , Monitoreo del Ambiente/métodos , Sedimentos Geológicos , Inundaciones , Microalgas/fisiología , Lluvia , Agua de Mar , Agua , Cloruro de Sodio , CianobacteriasRESUMEN
This research evaluated the effect of flooding on the microphytobenthos community structure in a microbial mat from a tropical salt flat. Field samples were collected during four consecutive days: on the first three days the salt flat was dry, on the fourth day it was flooded by rain. In order to evaluate the community maintained in flood conditions, samples from this area were collected and kept in the laboratory for 10 days with sea water. The results of total abundance of microphytobenthos varied from 4.2 × 108 to 2.9 × 109 organisms L-1, total density increased one order of magnitude under the effect of water for both situations of precipitation in the salt flat and in experimental conditions, an increase due to the high abundance of Microcoleus spp. Shannon index (H') was higher during the desiccation period. Our data suggest that changes in the abundance of organisms were due to the effect of water. The dominance of the most abundant taxa remained the same under conditions of desiccation and influence of water, and there is probably a consortium of microorganisms in the microbial mat that helps to maintain these dominances.
Asunto(s)
Adaptación Fisiológica/fisiología , Monitoreo del Ambiente/métodos , Inundaciones , Sedimentos Geológicos , Microalgas/fisiología , Clima Tropical , Cianobacterias , Lluvia , Agua de Mar , Cloruro de Sodio , AguaRESUMEN
Dredging is a catastrophic disturbance that directly affects key biological processes in aquatic ecosystems, especially in those small and shallow. In the tropics, metabolic responses could still be enhanced by the high temperatures and solar incidence. Here, we assessed changes in the aquatic primary production along a small section of low-flow tropical downstream (Imboassica Stream, Brazil) after dredging. Our results suggested that these ecosystems may show catastrophic shifts between net heterotrophy and autotrophy in waters based on three short-term stages following the dredging: (I) a strongly heterotrophic net primary production -NPP- coupled to an intense respiration -R- likely supported by high resuspended organic sediments and nutrients from the bottom; (II) a strongly autotrophic NPP coupled to an intense gross primary production -GPP- favored by the high nutrient levels and low solar light attenuation from suspended solids or aquatic macrophytes; and (III) a NPP near to the equilibrium coupled to low GPP and R rates following, respectively, the shading by aquatic macrophytes and high particulate sedimentation. In conclusion, changes in aquatic primary production could be an important threshold for controlling drastic shifts in the organic matter cycling and the subsequent silting up of small tropical streams after dredging events.
Asunto(s)
Ecosistema , Ríos , Calidad del Agua , BrasilRESUMEN
Abstract Dredging is a catastrophic disturbance that directly affects key biological processes in aquatic ecosystems, especially in those small and shallow. In the tropics, metabolic responses could still be enhanced by the high temperatures and solar incidence. Here, we assessed changes in the aquatic primary production along a small section of low-flow tropical downstream (Imboassica Stream, Brazil) after dredging. Our results suggested that these ecosystems may show catastrophic shifts between net heterotrophy and autotrophy in waters based on three short-term stages following the dredging: (I) a strongly heterotrophic net primary production -NPP- coupled to an intense respiration -R- likely supported by high resuspended organic sediments and nutrients from the bottom; (II) a strongly autotrophic NPP coupled to an intense gross primary production -GPP- favored by the high nutrient levels and low solar light attenuation from suspended solids or aquatic macrophytes; and (III) a NPP near to the equilibrium coupled to low GPP and R rates following, respectively, the shading by aquatic macrophytes and high particulate sedimentation. In conclusion, changes in aquatic primary production could be an important threshold for controlling drastic shifts in the organic matter cycling and the subsequent silting up of small tropical streams after dredging events.
Resumo Dragagem é um distúrbio catastrófico que afeta diretamente processos biológicos chave nos ecossistemas aquáticos, especialmente naqueles pequenos e rasos. Nos trópicos, as respostas metabólicas podem ser ainda mais intensificadas pelas altas temperaturas e incidência solar. No presente estudo, avaliamos mudanças na produção primária aquática ao longo de uma pequena seção de um riacho tropical após uma dragagem (riacho Imboassica, Brasil). Nossos resultados sugeriram que estes ecossistemas podem apresentar mudanças catastróficas desde heterotrofia à autotrofia líquida na água, baseadas em três etapas de curto prazo após a dragagem: (I) uma produção primária líquida -PPL- fortemente heterotrófica associada a uma intensa respiração -R-, provavelmente sustentada por sedimentos orgânicos e nutrientes advindos do fundo; (II) uma PPL fortemente autotrófica associada a uma intensa produção primária bruta -PPB- favorecida pelos elevados níveis de nutrientes e baixa atenuação da luz solar pelos sólidos em suspensão ou macrófitas aquáticas; e (III) uma PPL próxima ao equilíbrio associada às reduzidas taxas de PPB e R seguindo os sombreamento pelas macrófitas aquáticas e elevada sedimentação de particulados. Como conclusão, mudanças na produção primária aquática poderiam ser um importante limiar para controlar drásticas alterações na ciclagem da matéria orgânica e no subsequente assoreamento de pequenos riachos tropicais após eventos de dragagem.
Asunto(s)
Ecosistema , Ríos , Calidad del Agua , BrasilAsunto(s)
Conservación de los Recursos Naturales , Ecosistema , Ambiente , Ciclo del Nitrógeno , Agricultura , Biomasa , Actividades Humanas , Humanos , América Latina , Nitrógeno , Política , Salud Pública , Política PúblicaRESUMEN
Although only a small amount of the Earth's water exists as continental surface water bodies, this compartment plays an important role in the biogeochemical cycles connecting the land to the atmosphere. The territory of Brazil encompasses a dense river net and enormous number of shallow lakes. Human actions have been heavily influenced by the inland waters across the country. Both biodiversity and processes in the water are strongly driven by seasonal fluvial forces and/or precipitation. These macro drivers are sensitive to climate changes. In addition to their crucial importance to humans, inland waters are extremely rich ecosystems, harboring high biodiversity, promoting landscape equilibrium (connecting ecosystems, maintaining animal and plant flows in the landscape, and transferring mass, nutrients and inocula), and controlling regional climates through hydrological-cycle feedback. In this contribution, we describe the aquatic ecological responses to climate change in a conceptual perspective, and we then analyze the possible climate-change scenarios in different regions in Brazil. We also indentify some potential biogeochemical signals in running waters, natural lakes and man-made impoundments. The possible future changes in climate and aquatic ecosystems in Brazil are highly uncertain. Inland waters are pressured by local environmental changes because of land uses, landscape fragmentation, damming and diversion of water bodies, urbanization, wastewater load, and level of pollutants can alter biogeochemical patterns in inland waters over a shorter term than can climate changes. In fact, many intense environmental changes may enhance the effects of changes in climate. Therefore, the maintenance of key elements within the landscape and avoiding extreme perturbation in the systems are urgent to maintain the sustainability of Brazilian inland waters, in order to prevent more catastrophic future events.
Asunto(s)
Biota , Cambio Climático , Monitoreo del Ambiente/métodos , Ciclo Hidrológico , Animales , Brasil , Humanos , Lagos , Ríos , Estaciones del AñoRESUMEN
Although only a small amount of the Earth's water exists as continental surface water bodies, this compartment plays an important role in the biogeochemical cycles connecting the land to the atmosphere. The territory of Brazil encompasses a dense river net and enormous number of shallow lakes. Human actions have been heavily influenced by the inland waters across the country. Both biodiversity and processes in the water are strongly driven by seasonal fluvial forces and/or precipitation. These macro drivers are sensitive to climate changes. In addition to their crucial importance to humans, inland waters are extremely rich ecosystems, harboring high biodiversity, promoting landscape equilibrium (connecting ecosystems, maintaining animal and plant flows in the landscape, and transferring mass, nutrients and inocula), and controlling regional climates through hydrological-cycle feedback. In this contribution, we describe the aquatic ecological responses to climate change in a conceptual perspective, and we then analyze the possible climate-change scenarios in different regions in Brazil. We also indentify some potential biogeochemical signals in running waters, natural lakes and man-made impoundments. The possible future changes in climate and aquatic ecosystems in Brazil are highly uncertain. Inland waters are pressured by local environmental changes because of land uses, landscape fragmentation, damming and diversion of water bodies, urbanization, wastewater load, and level of pollutants can alter biogeochemical patterns in inland waters over a shorter term than can climate changes. In fact, many intense environmental changes may enhance the effects of changes in climate. Therefore, the maintenance of key elements within the landscape and avoiding extreme perturbation in the systems are urgent to maintain the sustainability of Brazilian inland waters, in order to prevent more catastrophic future events.
Embora apenas uma pequena quantidade de água da Terra esteja reservada em corpos d'água da superfície continental, esses ambientes desempenham papel importante nos ciclos biogeoquímicos, conectando a superfície à atmosfera. O território brasileiro é recortado por uma densa rede fluvial e exibe um enorme número de lagos rasos. Impactos de natureza humana têm sido intensos modificadores de ecossistemas límnicos. A biodiversidade e os processos ecossistêmicos são fortemente modulados por forças sazonais fluvial e/ou precipitação. Essas macroforçantes ecológicas respondem às mudanças climáticas. As águas interiores são ecossistemas com elevada biodiversidade, promovem transferências de energia dentro da paisagem, conectando os ecossistemas, e atuam na manutenção de fluxos de matérias - animais, vegetais, nutrientes e inóculos. Esses ecossistemas controlam o clima numa escala regional. Neste capítulo, são descritas algumas respostas dos ecossistemas aquáticos às alterações climáticas, tanto conceitualmente como analisando os possíveis cenários de mudanças climáticas em diferentes regiões no Brasil. Potenciais sinais biogeoquímicos em diferentes ecossistemas límnicos brasileiros foram identificados. Os ecossistemas límnicos são pressionados pelas atividades do uso do solo, pela fragmentação da paisagem, pelo represamento e pelo desvio de rios, pela urbanização, pela carga de águas residuais e do nível de poluentes. Essas ações perturbadoras podem alterar os padrões biogeoquímicos nas águas interiores numa escala temporal mais curta quando comparada às mudanças climáticas. A manutenção da sustentabilidade das ecossistemas aquáticos brasileiros é urgente de modo a prevenir futuros eventos catastróficos.
Asunto(s)
Animales , Humanos , Biota , Cambio Climático , Monitoreo del Ambiente/métodos , Ciclo Hidrológico , Brasil , Lagos , Ríos , Estaciones del AñoRESUMEN
Although only a small amount of the Earth's water exists as continental surface water bodies, this compartment plays an important role in the biogeochemical cycles connecting the land to the atmosphere. The territory of Brazil encompasses a dense river net and enormous number of shallow lakes. Human actions have been heavily influenced by the inland waters across the country. Both biodiversity and processes in the water are strongly driven by seasonal fluvial forces and/or precipitation. These macro drivers are sensitive to climate changes. In addition to their crucial importance to humans, inland waters are extremely rich ecosystems, harboring high biodiversity, promoting landscape equilibrium (connecting ecosystems, maintaining animal and plant flows in the landscape, and transferring mass, nutrients and inocula), and controlling regional climates through hydrological-cycle feedback. In this contribution, we describe the aquatic ecological responses to climate change in a conceptual perspective, and we then analyze the possible climate-change scenarios in different regions in Brazil. We also indentify some potential biogeochemical signals in running waters, natural lakes and man-made impoundments. The possible future changes in climate and aquatic ecosystems in Brazil are highly uncertain. Inland waters are pressured by local environmental changes because of land uses, landscape fragmentation, damming and diversion of water bodies, urbanization, wastewater load, and level of pollutants can alter biogeochemical patterns in inland waters over a shorter term than can climate changes. In fact, many intense environmental changes may enhance the effects of changes in climate. Therefore, the maintenance of key elements within the landscape and avoiding extreme perturbation in the systems are urgent to maintain the sustainability of Brazilian inland waters, in order to prevent more catastrophic future events.
Embora apenas uma pequena quantidade de água da Terra esteja reservada em corpos d'água da superfície continental, esses ambientes desempenham papel importante nos ciclos biogeoquímicos, conectando a superfície à atmosfera. O território brasileiro é recortado por uma densa rede fluvial e exibe um enorme número de lagos rasos. Impactos de natureza humana têm sido intensos modificadores de ecossistemas límnicos. A biodiversidade e os processos ecossistêmicos são fortemente modulados por forças sazonais fluvial e/ou precipitação. Essas macroforçantes ecológicas respondem às mudanças climáticas. As águas interiores são ecossistemas com elevada biodiversidade, promovem transferências de energia dentro da paisagem, conectando os ecossistemas, e atuam na manutenção de fluxos de matérias - animais, vegetais, nutrientes e inóculos. Esses ecossistemas controlam o clima numa escala regional. Neste capítulo, são descritas algumas respostas dos ecossistemas aquáticos às alterações climáticas, tanto conceitualmente como analisando os possíveis cenários de mudanças climáticas em diferentes regiões no Brasil. Potenciais sinais biogeoquímicos em diferentes ecossistemas límnicos brasileiros foram identificados. Os ecossistemas límnicos são pressionados pelas atividades do uso do solo, pela fragmentação da paisagem, pelo represamento e pelo desvio de rios, pela urbanização, pela carga de águas residuais e do nível de poluentes. Essas ações perturbadoras podem alterar os padrões biogeoquímicos nas águas interiores numa escala temporal mais curta quando comparada às mudanças climáticas. A manutenção da sustentabilidade das ecossistemas aquáticos brasileiros é urgente de modo a prevenir futuros eventos catastróficos.
RESUMEN
The aims of this research were to determine the main limiting nutrient to bacterial growth in Imboassica lagoon, southeastern Brazil, to estimate the percentage of dissolved organic carbon (DOC) available for bacterial growth, and to determine the bacterial growth efficiency (BGE) of natural assemblages. Bacterial growth and DOC consumption were determined in batch culture experiments, in which water samples were supplemented with nitrogen and phosphorus together or separately, or incubated without nutrient additions. When added together, N and P stimulated higher bacterial growth rates and production, as well as higher DOC consumption. The BGEs and DOC consumption rates were strongly dependent on the method used to determine bacterial production. The BGE ranged from 11 to 72%. However, only a minor fraction of bulk DOC was consumed by the planktonic bacteria (from 0.7 to 3.4%). The results suggest that low availability of phosphorus and nitrogen coupled with excess organic carbon was the main factor responsible for the relatively low bacterial utilization of DOC in Imboassica lagoon.
Asunto(s)
Bacterias/crecimiento & desarrollo , Biomasa , Carbono/metabolismo , Compuestos Orgánicos/metabolismo , Microbiología del Agua , Brasil , Agua DulceRESUMEN
The aim of this work was to study the effect of the herbicides glyphosate, nonanoic acid, and dichlorprop-P and the insecticides potassium oil, malation and Pyretrin and their combinations on nitrification. Nitrification was measured in slurries from the eutrophic and shallow Brabrand Lake (Aarhus, Denmark), by inhibiting oxidation of nitrite to nitrate with chloride. All herbicides and insecticides influenced nitrification. The No Observed Effect Concentration (NOEC) was assessed to be 30 microg.L-1 for glyphosate and nonanoic acid and 1 microg.L-1 for dichlorprop-P. The NOEC for malation and Pyretrin on nitrification was assessed to be 3 microg.L-1. No accumulation effect on nitrification of the insecticides malation and Pyretrin, or of the studied herbicides, was observed, indicating that their environmental impact is low at reduced concentrations, even in combination. The procedure used in this study can provide a useful tool for obtaining concentration limits for pesticides or other chemicals in a short period of time.
Asunto(s)
Sedimentos Geológicos , Herbicidas/farmacología , Insecticidas/farmacología , Nitritos/metabolismo , Nitrógeno/metabolismo , Agua DulceRESUMEN
Os objetivos desta pesquisa foram: determinar o principal nutriente limitante ao crescimento bacteriano na lagoa Imboassica, estimar a porcentagem de Carbono Orgânico Dissolvido (COD) disponível para o crescimento bacteriano e determinar a Eficiência de Crescimento Bacteriano (ECB) da comunidade bacteriana. O crescimento bacteriano e o consumo de COD foram avaliados em experimentos de culturas de diluição, nos quais nitrogênio e fósforo foram adicionados às amostras de água, juntos ou separadamente, e um controle foi preparado sem adições de nutrientes. Quando adicionados juntos, N e P estimularam um maior crescimento e produção bacterianos, assim como maiores taxas de consumo de COD. ECB e taxas de consumo de COD foram fortemente dependentes do método utilizado para determinar a produção bacteriana. ECB variou de 11% a 72%, porém apenas uma pequena fração do COD total foi consumida pelas bactérias planctônicas (de 0,7% a 3,4%). Sugere-se que as baixas disponibilidades de fósforo e nitrogênio são os principais fatores responsáveis pela baixa utilização de COD pelas bactérias na lagoa Imboassica.
Asunto(s)
Biomasa , Bacterias/crecimiento & desarrollo , Carbono/metabolismo , Compuestos Orgánicos/metabolismo , Microbiología del Agua , Brasil , Agua DulceRESUMEN
O objetivo desta pesquisa foi avaliar o efeito dos herbicidas "Glyphosate", Ácido Nonânico e "Dichlorprop-P" e dos insecticidas "Potassium oil", "Malation" e "Pyretrin" e da combinação destes compostos sobre o processo de nitrificação. As taxas de nitrificação foram mensuradas em uma mistura de água e sedimento do lago Brabrand, um lago raso e eutrófico (Aarhus, Dinamarca), por meio da inibição da oxidação do nitrito a nitrato por cloreto. Foi observada uma influência negativa de todos os herbicidas e inseticidas sobre o processo de nitrificação. A Concentração Sem Efeito Observado (CSEO) foi de 30 µg.L-1 para Glyphosate e Ácido Nonânico e 1 µg.L-1 para Dichlorprop-P. A CSEO para Malation e Pyretrin foi 3 µg.L-1. Não foi observado um efeito conjunto dos inseticidas Malation e Pyrethin e de todos os três herbicidas estudados, indicando que o impacto ambiental é baixo quando reduzidas concentrações destas substâncias estão presentes ao mesmo tempo no ambiente. O procedimento utilizado nesta pesquisa pode ser uma ferramenta útil para obtenção de limites nas concentrações de pesticidas ou outros produtos químicos em um curto período de tempo.
Asunto(s)
Sedimentos Geológicos , Herbicidas/farmacología , Insecticidas/farmacología , Nitritos/metabolismo , Nitrógeno/metabolismo , Agua DulceRESUMEN
The aims of this research were to determine the main limiting nutrient to bacterial growth in Imboassica lagoon, southeastern Brazil, to estimate the percentage of dissolved organic carbon (DOC) available for bacterial growth, and to determine the bacterial growth efficiency (BGE) of natural assemblages. Bacterial growth and DOC consumption were determined in batch culture experiments, in which water samples were supplemented with nitrogen and phosphorus together or separately, or incubated without nutrient additions. When added together, N and P stimulated higher bacterial growth rates and production, as well as higher DOC consumption. The BGEs and DOC consumption rates were strongly dependent on the method used to determine bacterial production. The BGE ranged from 11 to 72%. However, only a minor fraction of bulk DOC was consumed by the planktonic bacteria (from 0.7 to 3.4%). The results suggest that low availability of phosphorus and nitrogen coupled with excess organic carbon was the main factor responsible for the relatively low bacterial utilization of DOC in Imboassica lagoon.
Os objetivos desta pesquisa foram: determinar o principal nutriente limitante ao crescimento bacteriano na lagoa Imboassica, estimar a porcentagem de Carbono Orgânico Dissolvido (COD) disponível para o crescimento bacteriano e determinar a Eficiência de Crescimento Bacteriano (ECB) da comunidade bacteriana. O crescimento bacteriano e o consumo de COD foram avaliados em experimentos de culturas de diluição, nos quais nitrogênio e fósforo foram adicionados às amostras de água, juntos ou separadamente, e um controle foi preparado sem adições de nutrientes. Quando adicionados juntos, N e P estimularam um maior crescimento e produção bacterianos, assim como maiores taxas de consumo de COD. ECB e taxas de consumo de COD foram fortemente dependentes do método utilizado para determinar a produção bacteriana. ECB variou de 11% a 72%, porém apenas uma pequena fração do COD total foi consumida pelas bactérias planctônicas (de 0,7% a 3,4%). Sugere-se que as baixas disponibilidades de fósforo e nitrogênio são os principais fatores responsáveis pela baixa utilização de COD pelas bactérias na lagoa Imboassica.
RESUMEN
The aim of this work was to study the effect of the herbicides glyphosate, nonanoic acid, and dichlorprop-P and the insecticides potassium oil, malation and Pyretrin and their combinations on nitrification. Nitrification was measured in slurries from the eutrophic and shallow Brabrand Lake (Aarhus, Denmark), by inhibiting oxidation of nitrite to nitrate with chloride. All herbicides and insecticides influenced nitrification. The No Observed Effect Concentration (NOEC) was assessed to be 30 µg.L-1 for glyphosate and nonanoic acid and 1 µg.L-1 for dichlorprop-P. The NOEC for malation and Pyretrin on nitrification was assessed to be 3 µg.L-1. No accumulation effect on nitrification of the insecticides malation and Pyretrin, or of the studied herbicides, was observed, indicating that their environmental impact is low at reduced concentrations, even in combination. The procedure used in this study can provide a useful tool for obtaining concentration limits for pesticides or other chemicals in a short period of time.
O objetivo desta pesquisa foi avaliar o efeito dos herbicidas "Glyphosate", Ácido Nonânico e "Dichlorprop-P" e dos insecticidas "Potassium oil", "Malation" e "Pyretrin" e da combinação destes compostos sobre o processo de nitrificação. As taxas de nitrificação foram mensuradas em uma mistura de água e sedimento do lago Brabrand, um lago raso e eutrófico (Aarhus, Dinamarca), por meio da inibição da oxidação do nitrito a nitrato por cloreto. Foi observada uma influência negativa de todos os herbicidas e inseticidas sobre o processo de nitrificação. A Concentração Sem Efeito Observado (CSEO) foi de 30 µg.L-1 para Glyphosate e Ácido Nonânico e 1 µg.L-1 para Dichlorprop-P. A CSEO para Malation e Pyretrin foi 3 µg.L-1. Não foi observado um efeito conjunto dos inseticidas Malation e Pyrethin e de todos os três herbicidas estudados, indicando que o impacto ambiental é baixo quando reduzidas concentrações destas substâncias estão presentes ao mesmo tempo no ambiente. O procedimento utilizado nesta pesquisa pode ser uma ferramenta útil para obtenção de limites nas concentrações de pesticidas ou outros produtos químicos em um curto período de tempo.
RESUMEN
The aim of this research was to study the flood pulse influence and the anthropic impact caused by bauxite tailings on the chemical composition of O. glumaepatula in Batata lake (PA, Brazil). Sampling was carried out in stands of O. glumaepatula in the low-water, filling, high-water, and drawdown periods in impacted and natural areas of Batata lake. During the low-water and drawdown periods the stands of O. glumaepatula were exposed, and in the filling and high-water periods the water depth was respectively 1.4 and 3.8 m. The collected material was dried at 70 degrees C, ground, and concentrations of total phosphorus, total nitrogen, organic carbon, and energy content were determined. The results indicate that the biomass increase, caused by the rise in water level, has a dilution effect on nitrogen and phosphorus concentrations in O. glumaepatula. The energy contents did not present significant differences in any of the studied periods. The results suggest that from the low water to filling period, nitrogen becomes more limiting to O. glumaepatula in the impacted area, whereas phosphorus becomes more limiting in the natural area. The population of O. glumaepatula contributes to the recovery of the impacted area of Batata lake as the detritus from this species accumulates over the sediment. This accumulation impedes future re-suspension of the bauxite tailings and increases the organic matter and nutrient concentrations in the impacted sediment.
Asunto(s)
Monitoreo del Ambiente/métodos , Valor Nutritivo , Oryza/química , Contaminantes Químicos del Agua/metabolismo , Óxido de Aluminio/metabolismo , Biomasa , Brasil , Carbono/análisis , Agua Dulce , Nitrógeno/análisis , Oryza/metabolismo , Fósforo/análisisRESUMEN
O objetivo desta pesquisa foi estudar as influências do pulso de inundação e do impacto antrópico causado pelo rejeito de bauxita sobre a composição química de O. glumaepatula no lago Batata (PA, Brasil). As amostras foram realizadas em estandes de O. glumaepatula nos períodos de águas baixas, enchente, águas altas e vazante nas áreas natural e impactada desse ecossistema. Nos períodos de águas baixas e vazante, a área coletada encontrava-se exposta, enquanto nos períodos de enchente e águas altas, a profundidade da coluna d'água era de 1,4 e 3,8 m, respectivamente. O material coletado foi seco a 70ºC, moído e suas concentrações de fósforo total, nitrogênio total, carbono orgânico e conteúdo energético foram mensuradas. Os resultados indicaram que o aumento da biomassa causado pela elevação do nível d'água teve efeito diluidor sobre as concentrações de nitrogênio e fósforo em O. glumaepatula. O conteúdo energético não variou significativamente entre as áreas e os períodos estudados. Os resultados sugerem que, à medida que o nível d'água aumenta, O. glumaepatula torna-se limitada por nitrogênio na área impactada e por fósforo na área natural. A população de O. glumaepatula contribui para a recuperação da área impactada do lago Batata em decorrência do acúmulo de detritos dessa espécie sobre o sedimento, impedindo a resuspensão do rejeito de bauxita e promovendo aumento das concentrações de matéria orgânica e nutrientes.
Asunto(s)
Óxido de Aluminio/metabolismo , Biomasa , Monitoreo del Ambiente , Valor Nutritivo , Oryza/química , Contaminantes Químicos del Agua/metabolismo , Brasil , Carbono/análisis , Agua Dulce , Nitrógeno/análisis , Oryza/metabolismo , Fósforo/análisisRESUMEN
Lake Batata is a typical Amazonian clear water lake which has undergone anthropogenic impacts. Thirty percent of its total area has been covered with bauxite tailings. Thus, it is possible to distinguish two areas in this ecosystem: the impacted and the natural. The goal of this research was to study C, N, and P content variation and the values of biomass, length, density, and culm diameter of Oryza glumaepatula at different depths in the natural and impacted areas of Lake Batata. The results obtained in this research suggest that the availability of P and N, in both water and sediment, is lower at the shallow site when compared to the deeper sites. On the other hand, C concentrations decreased as P and N concentrations increased. This may be explained by the structural function of C in aquatic macrophytes. At shallower sites, due to the reduced water column, individuals invest in supporting structures that display high C concentrations. The higher density and biomass of O. glumaepatula at the intermediate site indicate that this area presents the best conditions for germination and establishment of individuals of this species. The chemical composition and biometric parameters of O. glumaepatula have shown that this population has higher spatial variation in the natural area. In the impacted area, the absence of significant variations in N and P concentrations in O. glumaepatula among the three sampled sites promotes higher homogeneity in the stands. The high C:P and N:P ratios indicate that, in the impacted area, P is more limiting to the development of O. glumaepatula than it is in the natural area. The reduced values of biomass and density of O. glumaepatula in the impacted area suggest that the bauxite tailings limit the development of this population.
Asunto(s)
Óxido de Aluminio/análisis , Ecosistema , Oryza/crecimiento & desarrollo , Contaminantes Químicos del Agua , Biomasa , Brasil , Carbono/análisis , Conservación de los Recursos Naturales , Agua Dulce , Nitrógeno/análisis , Fósforo/análisisRESUMEN
Lake Batata is a typical Amazonian clear water lake which has undergone anthropogenic impacts. Thirty percent of its total area has been covered with bauxite tailings. Thus, it is possible to distinguish two areas in this ecosystem: the impacted and the natural. The goal of this research was to study C, N, and P content variation and the values of biomass, length, density, and culm diameter of Oryza glumaepatula at different depths in the natural and impacted areas of Lake Batata. The results obtained in this research suggest that the availability of P and N, in both water and sediment, is lower at the shallow site when compared to the deeper sites. On the other hand, C concentrations decreased as P and N concentrations increased. This may be explained by the structural function of C in aquatic macrophytes. At shallower sites, due to the reduced water column, individuals invest in supporting structures that display high C concentrations. The higher density and biomass of O. glumaepatula at the intermediate site indicate that this area presents the best conditions for germination and establishment of individuals of this species. The chemical composition and biometric parameters of O. glumaepatula have shown that this population has higher spatial variation in the natural area. In the impacted area, the absence of significant variations in N and P concentrations in O. glumaepatula among the three sampled sites promotes higher homogeneity in the stands. The high C:P and N:P ratios indicate that, in the impacted area, P is more limiting to the development of O. glumaepatula than it is in the natural area. The reduced values of biomass and density of O. glumaepatula in the impacted area suggest that the bauxite tailings limit the development of this population
Asunto(s)
Óxido de Aluminio , Ecosistema , Oryza , Contaminantes Químicos del Agua , Biomasa , Brasil , Carbono , Conservación de los Recursos Naturales , Agua Dulce , Nitrógeno , FósforoRESUMEN
Lake Batata is a typical Amazonian clear water lake which has undergone anthropogenic impacts. Thirty percent of its total area has been covered with bauxite tailings. Thus, it is possible to distinguish two areas in this ecosystem: the impacted and the natural. The goal of this research was to study C, N, and P content variation and the values of biomass, length, density, and culm diameter of Oryza glumaepatula at different depths in the natural and impacted areas of Lake Batata. The results obtained in this research suggest that the availability of P and N, in both water and sediment, is lower at the shallow site when compared to the deeper sites. On the other hand, C concentrations decreased as P and N concentrations increased. This may be explained by the structural function of C in aquatic macrophytes. At shallower sites, due to the reduced water column, individuals invest in supporting structures that display high C concentrations. The higher density and biomass of O. glumaepatula at the intermediate site indicate that this area presents the best conditions for germination and establishment of individuals of this species. The chemical composition and biometric parameters of O. glumaepatula have shown that this population has higher spatial variation in the natural area. In the impacted area, the absence of significant variations in N and P concentrations in O. glumaepatula among the three sampled sites promotes higher homogeneity in the stands. The high C:P and N:P ratios indicate that, in the impacted area, P is more limiting to the development of O. glumaepatula than it is in the natural area. The reduced values of biomass and density of O. glumaepatula in the impacted area suggest that the bauxite tailings limit the development of this population.
O Lago Batata é um típico lago amazônico de águas claras que sofreu impactos antropogênicos. De sua área total, 30% foi recoberta com rejeito de bauxita. Desta forma, pode-se distinguir duas áreas nesse ecossistema: impactada e natural. O objetivo desta pesquisa foi estudar a variação de C, N e P e os valores de biomassa, comprimento, densidade e diâmetro do colmo de Oryza glumaepatula em diferentes profundidades, nas áreas impactada e natural, do Lago Batata. Os resultados obtidos na pesquisa sugerem que as disponibilidades de P e N, tanto na água como no sedimento, são menores no ponto raso quando comparado com os pontos mais profundos. Por outro lado, as concentrações de C diminuíram à medida que as concentrações de P e N aumentaram. Isto pode ser explicado pela função estrutural do C em macrófitas aquáticas. Nos pontos mais rasos, devido à reduzida coluna d'água, indivíduos investem em estruturas de suporte com elevadas concentrações de C. A elevada densidade e biomassa de O. glumaepatula no ponto intermediário indica que essa área apresenta as melhores condições para germinação e estabelecimento de indivíduos dessa espécie. A composição química e os parâmetros biométricos de O. glumaepatula mostraram que essa população possui elevada variação espacial na área natural. Na área impactada, a menor variação nas concentrações de N e P nos três pontos de amostragem promove alta homogeneidade nos estandes. As altas razões C:P e N:P indicam que, na área impactada, o P é mais limitante para o desenvolvimento de O. glumaepatula do que na área natural. Os reduzidos valores de biomassa e densidade de O. glumaepatula na área impactada sugerem que o rejeito de bauxita limita o desenvolvimento dessa população.