Landolfi Angela, Kähler Paul, Koeve Wolfgang, Oschlies Andreas
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany.
Front Microbiol. 2018 Sep 19;9:2112. doi: 10.3389/fmicb.2018.02112. eCollection 2018.
Fixed nitrogen (N) limits productivity across much of the low-latitude ocean. The magnitude of its inventory results from the balance of N input and N loss, the latter largely occurring in regionally well-defined low-oxygen waters and sediments (denitrification and anammox). The rate and distribution of N input by biotic N fixation, the dominant N source, is not well known. Here we compile N fixation estimates from experimental measurements, tracer-based geochemical and modeling approaches, and discuss their limitations and uncertainties. The lack of adequate experimental data coverage and the insufficient understanding of the controls of marine N fixation result in high uncertainties, which make the assessment of the current N-balance a challenge. We suggest that a more comprehensive understanding of the environmental and ecological interaction of marine N fixers is required to advance the field toward robust N fixation rates estimates and predictions.
固定氮(N)限制了低纬度大部分海洋的生产力。其储量大小取决于氮输入与氮损失的平衡,后者主要发生在区域界定明确的低氧水域和沉积物中(反硝化作用和厌氧氨氧化作用)。作为主要氮源的生物固氮作用的氮输入速率和分布情况尚不清楚。在此,我们汇总了基于实验测量、示踪地球化学和建模方法得出的固氮作用估算值,并讨论了它们的局限性和不确定性。由于缺乏足够的实验数据覆盖范围以及对海洋固氮作用控制因素的理解不足,导致不确定性较高,这使得评估当前的氮平衡成为一项挑战。我们建议,需要更全面地了解海洋固氮生物的环境与生态相互作用,以使该领域朝着可靠的固氮速率估算和预测方向发展。