Department of Crop Sciences, Grassland Science, University of Goettingen, Goettingen, Germany.
Lehrstuhl für Grünlandlehre, Technische Universität München, Freising-Weihenstephan, Germany.
PLoS One. 2019 Jan 16;14(1):e0210623. doi: 10.1371/journal.pone.0210623. eCollection 2019.
Nitrogen stable isotope (15N) natural abundance is widely used to study nitrogen cycling. In grazed ecosystems, urine patches are hot-spots of nitrogen inputs, losses, and changes in δ15N. Understanding δ15N dynamics in urine-affected vegetation is therefore crucial for accurate inferences from 15N natural abundance in grasslands. We hypothesized that leaf δ15N following urine deposition varies with time and plant functional group. Specifically, we expected (i) short-term decreases in δ15N due to foliar absorption of 15N-depleted volatilized ammonia, (ii) followed by increases in δ15N due to uptake of 15N-enriched soil inorganic nitrogen, and (iii) that the magnitude of these changes is less in legumes than in grasses. The latter should be expected because ammonia absorption depends on leaf nitrogen concentration, which is higher in legumes than grasses, and because biological nitrogen fixation will modify the influence of urine-derived nitrogen on δ15N in legumes. We applied cattle urine to a mixture of Lolium perenne and Trifolium repens in a pot experiment. Nitrogen concentration and δ15N were determined for successive leaf cohorts and bulk biomass either 17 (early) or 32 (late) days after urine application. Early after urine application, leaves of L. perenne were 15N-depleted compared to control plants (δ15N 0.1 vs. 5.8‰, respectively), but leaves of T. repens were not (-1.1 vs. -1.1‰, respectively). Later, both species increased their δ15N, but T. repens (4.5‰) less so than L. perenne (5.9‰). Vegetation sampled within and outside urine patches in the field further supported these results. Our findings confirm that foliar ammonia uptake can substantially decrease grass foliar δ15N, and that in both grass and legume the direction of the δ15N response to urine changes over time. Temporal dynamics of plant δ15N at urine patches therefore need to be explicitly addressed when 15N natural abundance is used to study nitrogen cycling in grazed grasslands.
氮稳定同位素(15N)自然丰度被广泛用于研究氮循环。在放牧生态系统中,尿斑是氮输入、损失和 δ15N 变化的热点。因此,了解受尿影响的植被中 δ15N 的动态变化对于从草原 15N 自然丰度进行准确推断至关重要。我们假设,尿沉积后叶片 δ15N 随时间和植物功能群而变化。具体而言,我们预计(i)由于挥发氨中 15N 耗尽的叶吸收导致短期 δ15N 降低,(ii)随后由于吸收 15N 富集的土壤无机氮而导致 δ15N 增加,(iii)这些变化的幅度在豆科植物中比在禾本科植物中较小。这是因为氨吸收取决于叶片氮浓度,而豆科植物的氮浓度高于禾本科植物,并且因为生物固氮会改变尿源性氮对豆科植物 δ15N 的影响。我们在盆栽实验中将牛尿应用于黑麦草和三叶草的混合物中。在尿应用后 17(早期)或 32(晚期)天,分别为连续叶群和批量生物量确定氮浓度和 δ15N。在尿应用后的早期,黑麦草的叶片与对照植物相比,15N 含量降低(分别为 δ15N 0.1 和 5.8‰),但三叶草的叶片则没有(分别为-1.1 和-1.1‰)。后来,两种植物的 δ15N 都增加了,但三叶草(4.5‰)的增加幅度小于黑麦草(5.9‰)。田间尿斑内和尿斑外采集的植被进一步支持了这些结果。我们的研究结果证实,叶片氨吸收可显著降低草叶片 δ15N,并且在草和豆科植物中,随着时间的推移,尿对 δ15N 的影响方向发生变化。因此,在使用 15N 自然丰度研究放牧草地氮循环时,需要明确考虑尿斑处植物 δ15N 的时间动态变化。