A 5-and a-half-year-experiment shows precipitation thresholds in litter decomposition and nutrient dynamics in arid and semi-arid regions

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
Hao Qu, Eduardo Medina-Roldán, Shaokun Wang, Xujun Ma, Xinyuan Wang, Xia Tang, Liangxu Liu
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Abstract

Precipitation is a key driver of litter decomposition in arid/semiarid regions; where soils are poor in organic matter, and thus re-incorporation of litter is key for soil nutrient accumulation and soil structure. It remains unclear, though, whether litter decomposition responds symmetrically to precipitation variation (e.g., if precipitation surpluses produce a stimulatory effect of a similar magnitude, but opposite direction to inhibitory effects of precipitation deficits), and whether litter decomposition and litter nutrient dynamics in arid and semiarid ecosystems that differ in climate show similar responses to precipitation. We set up a 5-and-a-half-year experiment that manipulated rainfall along a gradient (7 treatments): increases by 20%, 40%, and 60%, background precipitation, and reductions by the same 3 percentages. We applied such experiment in two sites with different pattens of precipitation (Urat: arid; and Naiman: semiarid) in Inner Mongolia to elucidate our questions. Litter mass loss and all nutrients that we measured (carbon, nitrogen, phosphorous, potassium, plus lignin) decomposed faster at the highest level of surplus precipitation, and more slowly in the two largest precipitation reductions. This indicates that these levels of precipitation constitute thresholds (value of precipitation beyond which ecosystem function is critically altered). Litter decomposition in the semiarid site was faster and more complete, but decomposition in the direr Urat was more efficient per unit cumulative rainfall. Thus, site specific effects played an important role in decomposition. Reductions in precipitation decreased the loss of C, N, P, K, and lignin from litter; and clear precipitation thresholds in the dynamic of these nutrients in litter were observed. Overall, this indicated the importance of precipitation limitation at controlling nutrient release. Our study highlights the importance of long-term studies on litter decomposition in environments with slow decomposition rates, and the importance of taking into account mechanistic effects of water availability on decomposition.

Abstract Image

5年半试验揭示了干旱半干旱区凋落物分解和养分动态的降水阈值
降水是干旱/半干旱区凋落物分解的关键驱动因素;在土壤有机质缺乏的地方,凋落物的重新结合是土壤养分积累和土壤结构的关键。然而,目前尚不清楚凋落物分解是否对降水变化有对称的响应(例如,降水盈余是否产生与降水不足抑制效应相似但方向相反的刺激效应),以及不同气候的干旱和半干旱生态系统中凋落物分解和凋落物营养动态是否对降水有类似的响应。我们设置了一个5年半的实验,沿着梯度(7个处理)控制降雨量:增加20%,40%和60%,背景降水,减少同样的3个百分比。我们在两个不同降水模式的站点(乌拉特:干旱;和内蒙古的奈曼(半干旱)来阐明我们的问题。我们测量的凋落物质量损失和所有营养物质(碳、氮、磷、钾和木质素)在剩余降水的最高水平分解得更快,而在两个最大的降水减少中分解得更慢。这表明这些降水水平构成了阈值(超过该值,生态系统功能就会发生严重改变)。半干旱区凋落物分解速度更快、更彻底,而乌拉尔地区单位累积雨量分解效率更高。因此,位点特异性效应在分解中起着重要作用。降水的减少减少了凋落物中C、N、P、K和木质素的损失;在凋落物中这些养分的动态中观察到明显的降水阈值。综上所述,这表明限制降水对控制养分释放的重要性。我们的研究强调了在分解速率缓慢的环境中对凋落物分解进行长期研究的重要性,以及考虑水分有效性对分解的机制影响的重要性。
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来源期刊
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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