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Preliminary estimates of the contribution of Arctic nitrogen fixation to the global nitrogen budget

机译:北极固氮对全球氮预算的贡献的初步估计

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Dinitrogen (N2) fixation is the source of all biologically available nitrogen on earth, and its presence or absence impacts net primary production and global biogeochemical cycles. Here, we report rates of 3.5–17.2 nmol N L?1 d?1 in the ice‐free coastal Alaskan Arctic to show that N2 fixation in the Arctic Ocean may be an important source of nitrogen to a seasonally nitrogen‐limited system. If widespread in surface waters over ice‐free shelves throughout the Arctic, N2 fixation could contribute up to 3.5 Tg N yr?1 to the Arctic nitrogen budget. At these rates, N2 fixation occurring in ice‐free summer waters would offset up to 27.1% of the Arctic denitrification deficit and contribute an additional 2.7% to N2 fixation globally, making it an important consideration in the current debate of whether nitrogen in the global ocean is in steady state. Additional investigations of high‐latitude marine diazotrophic physiology are required to refine these N2 fixation estimates.
机译:固氮是地球上所有生物可用氮的来源,其存在与否都会影响净初级生产和全球生物地球化学循环。在这里,我们报告在无冰的沿海阿拉斯加北极地区3.5-17.2 nmol N L?1 d?1的比率表明,北冰洋中的N2固定可能是季节性氮限制系统的重要氮源。如果在整个北极的无冰架上的地表水中广泛分布,则固氮可能会为北极的氮预算贡献高达3.5 Tg N yr?1。以这样的速度,在无冰的夏季水中进行的N2固定将抵消高达27.1%的北极反硝化赤字,并为全球范围内的N2固定额外贡献2.7%,这使其成为当前关于全球是否存在氮的辩论中的重要考虑因素。海洋处于稳定状态。需要进一步研究高纬度海洋重氮营养生理,以完善这些N2固定估计值。

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