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Climate warming and agricultural stressors interact to determine stream periphyton community composition

机译:气候变暖和农业压力因素相互作用,确定溪流附近植物群落组成

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Lack of knowledge about how the various drivers of global climate change will interact with multiple stressors already affecting ecosystems is the basis for great uncertainty in projections of future biological change. Despite concerns about the impacts of changes in land use, eutrophication and climate warming in running waters, the interactive effects of these stressors on stream periphyton are largely unknown. We manipulated nutrients (simulating agricultural runoff), deposited fine sediment (simulating agricultural erosion) (two levels each) and water temperature (eight levels, 0-6 degrees C above ambient) simultaneously in 128 streamside mesocosms. Our aim was to determine the individual and combined effects of the three stressors on the algal and bacterial constituents of the periphyton. All three stressors had pervasive individual effects, but in combination frequently produced synergisms at the population level and antagonisms at the community level. Depending on sediment and nutrient conditions, the effect of raised temperature frequently produced contrasting response patterns, with stronger or opposing effects when one or both stressors were augmented. Thus, warming tended to interact negatively with nutrients or sediment by weakening or reversing positive temperature effects or strengthening negative ones. Five classes of algal growth morphology were all affected in complex ways by raised temperature, suggesting that these measures may prove unreliable in biomonitoring programs in a warming climate. The evenness and diversity of the most abundant bacterial taxa increased with temperature at ambient but not with enriched nutrient levels, indicating that warming coupled with nutrient limitation may lead to a more evenly distributed bacterial community as temperatures rise. Freshwater management decisions that seek to avoid or mitigate the negative effects of agricultural land use on stream periphyton should be informed by knowledge of the interactive effects of multiple stressors in a warming climate.
机译:缺乏对全球气候变化的各种驱动因素将如何与已经影响生态系统的多种压力因素相互作用的知识,是对未来生物变化的预测存在很大不确定性的基础。尽管担心自来水的土地利用变化,富营养化和气候变暖的影响,但这些压力源对溪流附生植物的交互作用仍是未知的。我们在128个河边的中层环境中同时处理了营养物(模拟了农业径流),沉积的细小沉积物(模拟了农业侵蚀)(每个水平两个)和水温(八个水平,高于环境温度0-6摄氏度)。我们的目的是确定这三种应激因素对附生植物的藻类和细菌成分的单独影响和综合影响。所有这三种压力源均具有普遍的个体效应,但结合起来常常在人群一级产生协同作用,在社区一级产生拮抗作用。取决于沉积物和养分条件,升高温度的影响通常会产生相反的响应模式,当增加一个或两个压力源时,会产生较强或相反的影响。因此,变暖往往会通过减弱或逆转正温度效应或增强负温度效应而与养分或沉积物产生不利的相互作用。温度升高会以复杂的方式影响五种藻类的生长形态,这表明这些措施在变暖的气候下的生物监测程序中可能不可靠。最丰富的细菌类群的均匀度和多样性随环境温度的升高而增加,但不随营养水平的升高而增加,这表明随着温度升高,变暖加上营养物质的限制可能导致分布更均匀的细菌群落。旨在避免或减轻农业用地对河流水生植物的不利影响的淡水管理决定,应在变暖的气候条件下了解多种胁迫因素的相互作用。

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