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首页> 外文期刊>Aquatic Sciences >Burrowing macroinvertebrates alter phosphorus dynamics in drainage ditch sediments
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Burrowing macroinvertebrates alter phosphorus dynamics in drainage ditch sediments

机译:挖洞Macroinvertebres在排水沟沉积物中的磷动力学

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摘要

Consumptive and nonconsumptive interactions of benthic organisms play important roles in regulating rates of ecosystem services such as nutrient cycling in freshwater ecosystems. Studies of macroinvertebrate communities in drainage ditches have focused on documenting the biodiversity supported by these human-altered environments, but none have explored the ecosystem functions provided by those biological communities in ditches. Bioturbation by burrowing benthic invertebrates in ditch sediments may change rates of biogeochemical processes controlling fluxes of nutrients across the sediment-water interface. We used microcosms to test the effect of four species of burrowing invertebrates (Naididae: Ilyodrilus templetoni, Naididae: Limnodrilus hoffmeisteri, Gammaridae: Crangonyx sp., Chironomidae: Chironomus decorus S.G.) on exchanges of phosphorus between sediment and water from a drainage ditch. These effects were measured across a range of sediment and water characteristics, representing variability within ditches. All species reduced concentrations of P (as molybdenum-reactive phosphorus) in the surface water relative to controls under conditions were sediment porewater was not likely to contain higher concentrations of P than surface water. Decreases in P concentration were linked to changes in the sediment redox potential and water pH. Two species (L. hoffmeisteri and C. decorus) increased P concentrations under conditions where sediment porewater likely had higher concentrations of P than surface water. Increases in P concentrations were likely due to physical changes to the sediment from burrowing, and increased transport of dissolved P from sediment porewater to surface waters. Management of ditches should consider effects of burrowing benthic invertebrates on physical and biogeochemical processes at the sediment-water interface. Habitat manipulation in ditches could lead to unpredicted changes in nutrient dynamics mediated by changes to the burrowing benthic invertebrate community.
机译:底栖生物的消耗和非承认相互作用在淡水生态系统中的营养循环等生态系统服务率中起重要作用。在排水沟中的大型脊椎动物社区的研究侧重于记录这些人类改变环境支持的生物多样性,但没有探索这些生物社区提供的生态系统职能。通过在沟槽沉积物中挖洞底栖无脊椎动物的生物扰动可能会改变控制沉积物水界面营养素势态的生物地球化学过程的速率。我们使用微观来测试四种穴居无脊椎动物的效果(Naididae:Ilyodrilus Templetoni,Naididae:Limnodrilus Hoffmeisteri,Gammaridae:Cranononyx Sp。,Chironomidae:ChironomiDae:ChironomiDae:ChironomiDae:Chironomus Decorus S.G.)在排水沟中沉积物和水之间的磷交换。这些效果在一系列沉积物和水特征上测量,代表了沟渠内的可变性。所有物种相对于条件下的对照,所有物种在地表水中的浓度降低(作为钼 - 反应性磷)是沉积物沉淀水的沉积物,不太可能含有较高浓度的P比地表水。 P浓度的降低与沉积物氧化还原潜力和水pH的变化有关。在沉积物沉淀水可能比地表水浓度较高的条件下,两种物种(L. hoffmeisteri和C. dectus)增加了P浓度。 P浓度的增加可能是由于穴居沉积物的物理变化,以及从沉积物沉淀物到表面水的溶解P的运输增加。沟渠的管理应考虑挖洞肉体无脊椎动物对沉积物 - 水界面的物理和生物地球化学过程的影响。栖息地在沟渠中操纵可能导致营养动态的未预测变化,由挖洞底栖无脊椎动物群落的变化介导。

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