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Massive nitrous oxide emissions from the tropical South Pacific Ocean

机译:来自热带南太平洋的大量一氧化二氮排放

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Nitrous oxide is a potent greenhouse gas(1) and a key compound in stratospheric ozone depletion(2). In the ocean, nitrous oxide is produced at intermediate depths through nitrification and denitrification, in particular at low oxygen concentrations(3). Although a third of natural emissions of nitrous oxide to the atmosphere originate from the ocean(1), considerable uncertainties in the distribution and magnitude of the emissions still exist(4). Here we present high-resolution surface measurements and vertical profiles of nitrous oxide that include the highest reported nitrous oxide concentrations in marine surface waters, suggesting that there is a hotspot of nitrous oxide emissions in high-productivity upwelling ecosystems along the Peruvian coast. We estimate that off Peru, the extremely high nitrous oxide supersaturations we observed drive a massive efflux of 0.2-0.9 Tg of nitrogen emitted as nitrous oxide per year, equivalent to 5-22% of previous estimates of global marine nitrous oxide emissions. Nutrient and gene abundance data suggest that coupled nitrification-denitrification in the upper oxygen minimum zone and transport of resulting nitrous oxide to the surface by upwelling lead to the high nitrous oxide concentrations. Our estimate of nitrous oxide emissions from the Peruvian coast surpasses values from similar, highly productive areas.
机译:一氧化二氮是一种有力的温室气体(1),是平流层臭氧消耗的关键化合物(2)。在海洋中,一氧化二氮是通过硝化和反硝化作用在中等深度产生的,特别是在低氧浓度下(3)。尽管排放到大气中的一氧化二氮自然排放量的三分之一来自海洋(1),但排放的分布和大小仍然存在相当大的不确定性(4)。在这里,我们提供高分辨率的地面测量结果和一氧化二氮的垂直剖面图,其中包括海洋表层水中报告的最高一氧化二氮浓度,这表明秘鲁沿海高生产力上升流生态系统存在一氧化二氮排放热点。我们估计,在秘鲁以外,我们观察到的极高的一氧化二氮过饱和度会导致每年大量排放0.2-0.9 Tg的氮作为一氧化二氮排放,相当于先前全球海洋一氧化二氮排放量的5-22%。营养和基因丰度数据表明,在最小氧上限区域中硝化-反硝化作用耦合,以及通过上升流将生成的一氧化二氮运输到表面,导致一氧化二氮浓度较高。我们对秘鲁海岸一氧化二氮排放量的估算超过了类似的高产地区的排放量。

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