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Anoxia decreases the magnitude of the carbon, nitrogen, and phosphorus sink in freshwaters

机译:缺氧会降低淡水中碳、氮和磷汇的大小

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Abstract Oxygen availability is decreasing in many lakes and reservoirs worldwide, raising the urgency for understanding how anoxia (low oxygen) affects coupled biogeochemical cycling, which has major implications for water quality, food webs, and ecosystem functioning. Although the increasing magnitude and prevalence of anoxia has been documented in freshwaters globally, the challenges of disentangling oxygen and temperature responses have hindered assessment of the effects of anoxia on carbon, nitrogen, and phosphorus concentrations, stoichiometry (chemical ratios), and retention in freshwaters. The consequences of anoxia are likely severe and may be irreversible, necessitating ecosystem‐scale experimental investigation of decreasing freshwater oxygen availability. To address this gap, we devised and conducted REDOX (the Reservoir Ecosystem Dynamic Oxygenation eXperiment), an unprecedented, 7‐year experiment in which we manipulated and modeled bottom‐water (hypolimnetic) oxygen availability at the whole‐ecosystem scale in a eutrophic reservoir. Seven years of data reveal that anoxia significantly increased hypolimnetic carbon, nitrogen, and phosphorus concentrations and altered elemental stoichiometry by factors of 2–5× relative to oxic periods. Importantly, prolonged summer anoxia increased nitrogen export from the reservoir by six‐fold and changed the reservoir from a net sink to a net source of phosphorus and organic carbon downstream. While low oxygen in freshwaters is thought of as a response to land use and climate change, results from REDOX demonstrate that low oxygen can also be a driver of major changes to freshwater biogeochemical cycling, which may serve as an intensifying feedback that increases anoxia in downstream waterbodies. Consequently, as climate and land use change continue to increase the prevalence of anoxia in lakes and reservoirs globally, it is likely that anoxia will have major effects on freshwater carbon, nitrogen, and phosphorus budgets as well as water quality and ecosystem functioning.
机译:摘要 全球许多湖泊和水库的氧气供应量正在下降,这增加了了解缺氧(低氧)如何影响耦合生物地球化学循环的紧迫性,这对水质、食物网和生态系统功能具有重大影响。尽管全球淡水中缺氧的程度和患病率都在增加,但解开氧气和温度响应的挑战阻碍了对缺氧对碳、氮和磷浓度、化学计量(化学比率)和淡水中保留的影响的评估。缺氧的后果可能是严重的,可能是不可逆转的,因此有必要对淡水氧气供应的减少进行生态系统规模的实验研究。为了解决这一差距,我们设计并进行了 REDOX(储层生态系统动态氧合实验),这是一项史无前例的 7 年实验,我们在富营养化储层中操纵和模拟了整个生态系统尺度的底水(低limnetic)氧气可用性。七年的数据显示,与含氧期相比,缺氧显著增加了低浸泡碳、氮和磷浓度,并使元素化学计量改变了 2×-5 倍。重要的是,长期的夏季缺氧使储层的氮输出增加了六倍,并将储层从净汇转变为下游磷和有机碳的净源。虽然淡水中的低氧被认为是对土地利用和气候变化的反应,但REDOX的结果表明,低氧也可能是淡水生物地球化学循环发生重大变化的驱动因素,这可能是一种强化反馈,增加下游水体的缺氧。因此,随着气候和土地利用的变化继续增加全球湖泊和水库缺氧的患病率,缺氧可能会对淡水碳、氮和磷收支以及水质和生态系统功能产生重大影响。

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