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首页> 外文期刊>Biogeosciences >High denitrification and anaerobic ammonium oxidation contributes to net nitrogen loss in a seagrass ecosystem in the central Red Sea
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High denitrification and anaerobic ammonium oxidation contributes to net nitrogen loss in a seagrass ecosystem in the central Red Sea

机译:高脱氮和厌氧铵氧化有助于中央红海的海草生态系统中的净氮气损失

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摘要

Nitrogen loads in coastal areas have increased dramatically, with detrimental consequences for coastal ecosystems. Shallow sediments and seagrass meadows are hotspots for denitrification, favoring N loss. However, atmospheric dinitrogen ( Nsub2/sub ) fixation has been reported to support seagrass growth. Therefore, the role of coastal marine systems dominated by seagrasses in the net Nsub2/sub flux remains unclear. Here, we measured denitrification, anaerobic ammonium oxidation (anammox), and Nsub2/sub fixation in a tropical seagrass (Enhalus acoroides) meadow and the adjacent bare sediment in a coastal lagoon in the central Red Sea. We detected high annual mean rates of denitrification ( 34.9±10.3 and 31.6±8.9 mg?N?m sup?2/sup d sup?1/sup ) and anammox ( 12.4±3.4 and 19.8±4.4 mg?N?m sup?2/sup d sup?1/sup ) in vegetated and bare sediments. The annual mean N loss was higher (between 8 and 63-fold) than the Nsub2/sub fixed (annual mean = 5.9±0.2 and 0.8±0.3 mg?N?m sup?2/sup d sup?1/sup ) in the meadow and bare sediment, leading to a net flux of Nsub2/sub from sediments to the atmosphere. Despite the importance of this coastal lagoon in removing N from the system, Nsub2/sub fixation can contribute substantially to seagrass growth since Nsub2/sub fixation rates found here could contribute up to 36?% of plant N requirements. In vegetated sediments, anammox rates decreased with increasing organic matter (OM) content, while Nsub2/sub fixation increased with OM content. Denitrification and anammox increased linearly with temperature, while Nsub2/sub fixation showed a maximum at intermediate temperatures. Therefore, the forecasted warming could further increase the Nsub2/sub flux from sediments to the atmosphere, potentially impacting seagrass productivity and their capacity to mitigate climate change but also enhancing their potential N removal.
机译:在沿海地区氮负荷急剧增加,与沿海生态系统有害后果。浅层沉积物和海草草场是脱硝的热点,有利于氮损失。然而,大气二氮(N <子> 2 )固定已报道支持海草增长。因此,沿海海洋系统通过在海草的网N为主的作用<子> 2 通量仍不清楚。在这里,我们测定脱硝,厌氧性氨氧化(厌氧氨氧化)和N <子> 2 固定在热带海草(海菖蒲属acoroides)草地和在红海中央沿海泻湖相邻裸沉积物。我们检测反硝化的高年平均速率(34.9±10.3和31.6±8.9毫克2 N?米?2 d λ1)和厌氧氨氧化(12.4±3.4和19.8± 4.4毫克2 N?米?2 d λ1)在植被和裸沉积物。年平均氮损失较高(8和63之间倍)比N <子> 2 固定的(年平均= 5.9±0.2和0.8±0.3毫克2 N?米?2 d λ1 2 从沉积物到大气SUP>)。尽管这样沿海泻湖在从系统中除去N个的重要性,N <子> 2 固定可以基本上由于N <子>有助于海草生长2 固定速率发现这里可能有助于多达36? %的植物氮要求。在植被沉积物,厌氧氨氧化速率随着有机物(OM)含量减少,而Ñ<子> 2 固定用OM含量增加。反硝化和厌氧氨氧化随温度线性增加,而Ñ<子> 2 固定显示在中间温度最大值。因此,预测的变暖可能进一步增加所述N个<子> 2 从沉积物通量到大气中,可能影响海草生产力和减缓气候变化,而且提高其潜在的N-去除能力。

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