Seasonal variations in the soil microbiota of a temperate wetland in Northeast China in response to nitrogen deposition

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Catena Pub Date : 2025-02-03 DOI:10.1016/j.catena.2025.108794
Rong-Tao Zhang , Shen-Zheng Wang , Hai-Xiu Zhong , Xin Sui , Ying-Nan Liu
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Abstract

Purpose

China has recently witnessed a significant rise in nitrogen (N) deposition associated with human activities, especially in temperate regions. Although much research has been conducted on aboveground biodiversity, the effects of long-term N deposition on the composition, function and variety of the soil microbiota (especially across seasons) have received less attention.

Methods

We investigated the effects of varying levels of nitrogen deposition on the composition, function and diversity of soil microbiota (bacteria and fungi) in temperate natural wetlands in summer and winter using Illumina sequencing. N deposition are categorized into low N addition (LN: 40 kg N/ha yr−1) and high N addition (HN: 80 kg N/ha yr−1).

Results

In both summer and winter, N deposition had a significant effect on bacterial α diversity. In contrast, fungal α diversity exhibited no significant change in either of the two seasons. Additionally, the diversity of the soil microbiota exhibited higher sensitivity to N deposition in winter compared to summer. During the summer months, nitrogen deposition significantly altered the relative abundance of bacterial phyla such as Acidobacteria, Myxococcota, Verrucomicrobia and Actinobacteria. In winter, bacterial phyla in the surface soil exhibited distinct changes in their relative abundance. Relative abundance of Epsilonbacteraeota was highest in plots without added nitrogen, whereas the N-treated plots exhibited the lowest abundances. In addition, the relative abundance of Ascomycota was significantly increased by the addition of N, whereas Mortierellomycota exhibited a significant decrease, with Basidiomycota exhibiting no significant effect. The results from the structural equation model (SEM) revealed that soil organic carbon (SOC) and total nitrogen (TN) exerted a significant influence on the composition of both bacterial and fungal communities in the soil, regardless of the season. Specifically, in the summer season, SOC and TN account for 87 % of the variation observed in bacterial diversity and 83 % of the variation in fungal diversity. Likewise, during the winter season, these factors explain 91 % of the changes in bacterial diversity and 88 % of the changes in fungal diversity.

Conclusion

Our research findings have unveiled that bacterial communities display a heightened sensitivity to nitrogen (N) deposition compared to their fungal counterparts. This discovery emphasizes the crucial need to concurrently evaluate the responses of the soil microbiome to global changes across various seasons, highlighting the intricate interplay between microbial dynamics and environmental factors.
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东北温带湿地土壤微生物群对氮沉降的季节变化响应
目的近年来,由于人类活动,中国特别是温带地区的氮素沉降显著增加。虽然对地上生物多样性的研究较多,但长期氮沉降对土壤微生物群组成、功能和多样性(特别是跨季节)的影响较少。方法采用Illumina测序技术,研究了不同氮沉降水平对温带自然湿地夏冬土壤微生物群(细菌和真菌)组成、功能和多样性的影响。N沉积分为低N添加量(LN: 40 kg N/ha yr - 1)和高N添加量(HN: 80 kg N/ha yr - 1)。结果在夏季和冬季,氮沉降对细菌α多样性均有显著影响。真菌α多样性在两个季节均无显著变化。此外,冬季土壤微生物多样性对氮沉降的敏感性高于夏季。夏季,氮沉降显著改变了酸性菌门、黏液菌门、Verrucomicrobia和放线菌门等细菌门的相对丰度。冬季土壤表层细菌门类相对丰度变化明显。未施氮处理的样地Epsilonbacteraeota相对丰度最高,而施氮处理的样地相对丰度最低。此外,添加N显著提高了子囊菌门的相对丰度,而Mortierellomycota则显著降低,担子菌门则无显著影响。结构方程模型(SEM)结果表明,土壤有机碳(SOC)和全氮(TN)对土壤细菌和真菌群落的组成有显著影响,而不受季节的影响。具体而言,在夏季,SOC和TN分别占细菌多样性变化的87%和真菌多样性变化的83%。同样,在冬季,这些因素解释了91%的细菌多样性变化和88%的真菌多样性变化。结论与真菌相比,细菌群落对氮沉降具有更高的敏感性。这一发现强调了同时评估土壤微生物组对不同季节全球变化的响应的关键需求,强调了微生物动力学与环境因素之间复杂的相互作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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