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首页> 外文期刊>Global change biology >Stream metabolism controls diel patterns and evasion of CO2 in Arctic streams
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Stream metabolism controls diel patterns and evasion of CO2 in Arctic streams

机译:流代谢控制北极流中二氧化碳模式和避难

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Streams play an important role in the global carbon (C) cycle, accounting for a large portion of CO2 evaded from inland waters despite their small areal coverage. However, the relative importance of different terrestrial and aquatic processes driving CO2 production and evasion from streams remains poorly understood. In this study, we measured O-2 and CO2 continuously in streams draining tundra-dominated catchments in northern Sweden, during the summers of 2015 and 2016. From this, we estimated daily metabolic rates and CO2 evasion simultaneously and thus provide insight into the role of stream metabolism as a driver of C dynamics in Arctic streams. Our results show that aquatic biological processes regulate CO2 concentrations and evasion at multiple timescales. Photosynthesis caused CO2 concentrations to decrease by as much as 900 ppm during the day, with the magnitude of this diel variation being strongest at the low-turbulence streams. Diel patterns in CO2 concentrations in turn influenced evasion, with up to 45% higher rates at night. Throughout the summer, CO2 evasion was sustained by aquatic ecosystem respiration, which was one order of magnitude higher than gross primary production. Furthermore, in most cases, the contribution of stream respiration exceeded CO2 evasion, suggesting that some stream reaches serve as net sources of CO2, thus creating longitudinal heterogeneity in C production and loss within this stream network. Overall, our results provide the first link between stream metabolism and CO2 evasion in the Arctic and demonstrate that stream metabolic processes are key drivers of the transformation and fate of terrestrial organic matter exported from these landscapes.
机译:溪流在全球碳(C)周期中发挥着重要作用,尽管处于面积覆盖率,但占从内陆水域逃离的大部分二氧化碳。然而,不同陆地和水生过程的相对重要性驾驶二氧化碳的生产和逃离流的逃避仍然清晰。在这项研究中,我们在2015年和2016年夏季的夏季地区,在瑞典北部的溪流排放潮流统治集水区的溪流中持续测量O-2和CO2。从这一点,我们同时估计了日常代谢率和二氧化碳救济,从而提供了对角色的见解流代谢作为北极流中C动力学的驾驶员。我们的结果表明,水生生物过程调节CO2浓度和多个时间尺寸的逃避。光合作用在白天引起CO2浓度降低多达900ppm,该二极管变化的大小在低湍流流处最强。二氧化碳浓度的二极形模式反过来影响逃避,夜间速度高达45%。在整个夏天,CO2逃避受水生生态系统呼吸持续的,这是一个高于初级生产的数量级。此外,在大多数情况下,流呼吸的贡献超过了二氧化碳逃避,这表明一些流达到CO2的净来源,从而在该流网络中产生C生产和损失中的纵向异质性。总体而言,我们的结果提供了北极流代谢和二氧化碳逃避之间的第一个联系,并证明了物流代谢过程是从这些景观出口的陆地有机物的转化和命运的关键驱动因素。

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