Resource-enhancing global changes shift soil multifunctionality towards faster cycling in arid grasslands

IF 5 2区 农林科学 Q1 SOIL SCIENCE Applied Soil Ecology Pub Date : 2025-04-01 Epub Date: 2025-02-24 DOI:10.1016/j.apsoil.2025.105987
Zhaobin Song , Xiaoan Zuo , Shaokun Wang , Xiangyun Li , Ya Hu , Jingjuan Qiao , Chao Wang , Ellen L. Fry , Jordi Sardans , Josep Peñuelas , Yann Hautier
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Abstract

Soil multifunctionality in terrestrial ecosystems plays a pivotal role in providing sustainable services to humanity. Resource-enhancing global changes, such as increased precipitation and nitrogen (N) deposition can accelerate the transformation of various aspects of ecosystem functions from slow to fast cycling. The difference in how these global change factors influence soil multifunctionality in arid grasslands remains unknown, limiting our ability to manage these ecosystems under anthropogenic changes. Using a framework recently developed to quantify slow-to-fast cycling transitions in ecosystem functions, we tested the impact of increased precipitation and N addition on soil slow-fast multifunctionality and its components related to soil carbon (C), N, and phosphorous (P) functions by conducting two separate manipulative experiments in arid grasslands. Additionally, we explored the contribution of plant diversity, microbial diversity and soil properties to the variations of soil multifunctionality. We found that increased precipitation and N addition drove shifts in soil multifunctionality towards faster cycling. However, such shifts resulted from different responses of soil C, N and P functions. Specifically, increased precipitation resulted in faster C, N and P cycling functions, while N addition led to faster N cycling functions. Although above- and below-ground diversity and soil properties were closely linked to soil N and P functions, increased precipitation did not affect these abiotic and biotic drivers. Therefore, the impacts of increased precipitation on soil C, N and P functions were direct. In contrast, the impact of N addition on soil N functions was mediated through changes in above- and below-ground community composition and soil properties. Our results provide deeper insights into the driving mechanisms by which increased precipitation and N addition affect soil multifunctionality, indicating that the drivers of multifunctionality are context-dependent. Therefore, we should develop corresponding strategies to mitigate the impacts of different global change factors on soil multifunctionality in arid grasslands.
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资源增强的全球变化将干旱草原土壤的多功能性转向更快的循环
陆地生态系统中的土壤多功能性在为人类提供可持续服务方面发挥着关键作用。资源增长型全球变化,如降水和氮沉降的增加,可以加速生态系统各方面功能由慢循环向快循环的转变。这些全球变化因素如何影响干旱草原土壤多功能性的差异仍然未知,限制了我们在人为变化下管理这些生态系统的能力。利用最近开发的一个框架来量化生态系统功能从慢到快的循环转变,我们通过在干旱草原上进行两个单独的操纵实验,测试了降水增加和氮添加对土壤慢-快多功能性及其与土壤碳(C)、氮和磷(P)功能相关的成分的影响。此外,我们还探讨了植物多样性、微生物多样性和土壤性质对土壤多功能性变化的贡献。我们发现,降水和氮添加的增加推动了土壤多功能性向更快循环的转变。然而,这种变化是由于土壤C、N、P功能的不同响应所致。具体而言,降水增加导致C、N、P循环函数加快,N添加导致N循环函数加快。虽然地上和地下多样性和土壤性质与土壤氮磷功能密切相关,但降水增加对这些非生物和生物驱动因素没有影响。因此,降水增加对土壤C、N、P功能的影响是直接的。施氮量对土壤氮功能的影响主要通过地上、地下群落组成和土壤性质的变化来调节。我们的研究结果为增加降水和氮添加影响土壤多功能性的驱动机制提供了更深入的见解,表明多功能性的驱动因素是上下文相关的。因此,我们应该制定相应的策略来缓解不同全球变化因子对干旱草原土壤多功能性的影响。
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来源期刊
Applied Soil Ecology
Applied Soil Ecology 农林科学-土壤科学
CiteScore
9.70
自引率
4.20%
发文量
363
审稿时长
5.3 months
期刊介绍: Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.
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