Microbial gene abundance mirrors soil nitrogen mineralization intensity across an age gradient in Chinese-fir plantations

IF 3.7 2区 农林科学 Q1 ECOLOGY European Journal of Soil Biology Pub Date : 2023-11-01 DOI:10.1016/j.ejsobi.2023.103570
Qingwu Zhan , Liang Chen , Huili Wu , Shuai Ouyang , Yelin Zeng , Xiangwen Deng , Yanting Hu , Wenhua Xiang
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Abstract

Stand development affects soil properties, nitrogen (N) dynamics, and soil microbial community composition, but the question remains whether differences in N mineralization rates are mirrored by the abundance of relevant functional genes. In this study, we used the 15N pool-dilution method to estimate N mineralization (i.e., ammonification and nitrification) rates across a Chinese fir (Cunninghamia lanceolata) chronosequence, with stands aged 7, 16, 29, 36, and >80 years. Gene copy numbers of bacteria (16S rRNA), fungi (ITS), ammonia-oxidizing archaea (AOA) and bacteria (AOB) (amoA), denitrifiers (nirS, nirK), N2 fixers (nifH) and organic N decomposers (chiA) were quantified by qPCR. Gross ammonification and nitrification rates increased linearly with stand age in the topsoil (0–5 cm depth) and were strongly positively correlated with the abundance of the bacterial 16S rRNA gene and AOA amoA, respectively. Higher net nitrification but lower NO3 immobilization rates in older stands (32 and > 80 years) drove higher N availability for vegetation than in young stands (7 years). Older stands also had higher rates of NH4+ consumption than younger stands due to the increased fungal ITS abundance and higher microbial biomass N (MBN), and AOA amoA was more abundant and active than AOB amoA due to the more acid conditions characteristic of mature forests. Redundancy analysis showed that functional gene abundance was strongly affected by soil properties such as pH, NH4+-N content, and MBN. We also found that microbial N storage potential was lower, and the NO3-N leaching and gaseous N loss potential were higher in older stands than in younger stands. Collectively, stand developmental stage gave rise to the observed spatial gradient of gross ammonification and nitrification rates by altering the abundance of microbial functional genes, which affected plantation productivity via its modulation of the supply of bioavailable N.

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微生物基因丰度反映了杉木人工林不同年龄梯度土壤氮矿化强度
林分发育影响土壤性质、氮动态和土壤微生物群落组成,但N矿化率的差异是否反映在相关功能基因的丰度上仍是一个问题。在这项研究中,我们使用15N池稀释法估算了杉木(杉木)林龄7、16、29、36和80年的N矿化(即氨化和硝化)速率。采用qPCR方法定量细菌(16S rRNA)、真菌(ITS)、氨氧化古菌(AOA)和细菌(AOB)、反硝化菌(nirS、nirK)、N2固定菌(nifH)和有机N分解者(chiA)的基因拷贝数。在表层土壤(0 ~ 5 cm深度),总氨化率和硝化率随林龄线性增加,分别与细菌16S rRNA基因丰度和AOA amoA丰度呈显著正相关。老林分净硝化作用较高,NO3−固定率较低(32和>80年)对植被氮有效性的影响高于幼林(7年)。由于真菌ITS丰度的增加和微生物生物量N (MBN)的增加,老林的NH4+消耗率也高于年轻林,而AOA amoA比AOB amoA更丰富和活跃,这是由于成熟林的酸性环境特征。冗余分析表明,功能基因丰度受pH、NH4+-N含量和MBN等土壤性质的强烈影响。微生物氮储存潜力较低,硝态氮淋失和气态氮损失潜力在老林分高于新林分。总体而言,林分发育阶段通过改变微生物功能基因丰度来影响总氨化和硝化速率的空间梯度,从而通过调节生物有效氮的供应来影响人工林生产力。
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来源期刊
European Journal of Soil Biology
European Journal of Soil Biology 环境科学-生态学
CiteScore
6.90
自引率
0.00%
发文量
51
审稿时长
27 days
期刊介绍: The European Journal of Soil Biology covers all aspects of soil biology which deal with microbial and faunal ecology and activity in soils, as well as natural ecosystems or biomes connected to ecological interests: biodiversity, biological conservation, adaptation, impact of global changes on soil biodiversity and ecosystem functioning and effects and fate of pollutants as influenced by soil organisms. Different levels in ecosystem structure are taken into account: individuals, populations, communities and ecosystems themselves. At each level, different disciplinary approaches are welcomed: molecular biology, genetics, ecophysiology, ecology, biogeography and landscape ecology.
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