Department of Ecology, Evolution, Behavior, University of Minnesota, Saint Paul, MN, 55108, USA.
Department of Biology, Williams College, Williamstown, MA, 01267, USA.
Ecol Lett. 2021 Apr;24(4):802-811. doi: 10.1111/ele.13700. Epub 2021 Feb 14.
Plant litter decomposition is a central process in the carbon (C) cycle and sensitive to ongoing anthropogenic nitrogen (N) fertilisation. Previous syntheses evaluating the effect of N fertilisation on litter decomposition relied largely on models that define a constant rate of mass loss throughout decomposition, which may mask hypothesised shifts in the effect of N fertilisation on litter decomposition dynamics. In this meta-analysis, we compared the performance of four empirical decomposition models and showed that N fertilisation consistently accelerates early-stage but slows late-stage decomposition when the model structure allows for flexibility in decomposition rates through time. Within a particular substrate, early-stage N-stimulation of decomposition was associated with reduced rates of late-stage decay. Because the products of early- vs. late-stage decomposition are stabilised in soils through distinct chemical and physical mechanisms, N-induced changes in the litter decomposition process may influence the formation and cycling of soil C, the largest terrestrial C pool.
植物凋落物分解是碳(C)循环的核心过程,对正在进行的人为氮(N)施肥敏感。以前评估 N 施肥对凋落物分解影响的综合研究主要依赖于定义整个分解过程中质量损失恒定速率的模型,这可能掩盖了对 N 施肥对凋落物分解动力学影响的假设变化。在这项荟萃分析中,我们比较了四种经验分解模型的性能,并表明当模型结构允许通过时间灵活调整分解速率时,N 施肥会一致加速早期分解但减缓晚期分解。在特定基质中,分解的早期 N 刺激与晚期衰减速率降低有关。由于早期与晚期分解产物通过不同的化学和物理机制稳定在土壤中,凋落物分解过程中的 N 诱导变化可能会影响土壤 C 的形成和循环,土壤 C 是最大的陆地 C 库。