Litter-mediated shifts in microbial communities along an altitudinal gradient enhance humification-driven soil organic carbon accumulation

IF 5 2区 农林科学 Q1 SOIL SCIENCE
Xiaojun Qi , Yiting Wang , Mengyao Zheng , Zhiyue Liu , Yanbo Ren , Yuan Li , Tong Jia
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Abstract

Humus constitutes the primary component of soil organic matter (SOM), while forest litter serves as a critical source of humus, driving the formation of soil organic carbon (SOC). However, the mechanisms through which litter inputs modulate humification and SOC sequestration remain elusive. In this study, amplicon sequencing of litter- and soil-associated bacteria and fungi was combined with biogeochemical analyses across an elevational gradient in the Zhongtiao Mountain forest ecosystem (Shanxi Province, China) to identify the drivers of humification and SOC accumulation. Results showed that while litter/soil nutrients increased with elevation, humus content declined. Microbial communities (including rare and abundant taxa) shifted with altitude, with pH, water content, total phosphorus, and microbial biomass nitrogen as key determinants. The Correlation analyses and Mantel tests further demonstrated that humus and SOC fractions were influenced not only by soil properties but also by the chemical properties of litter and the diversity and composition of microbial communities in litter. Notably, rare microbial taxa in the litter had greater impacts on humus and SOC accumulation compared to abundant taxa. Mixed-effects modeling validated that humus content was a significant predictor of SOC accumulation. In addition, structural equation modeling (SEM) indicated that early-stage litter-colonizing microorganisms directly enhanced humus and SOC storage and indirectly promoted humification by modifying soil microbial community structure. This study elucidates the mechanisms by which altitudinal variation in litter inputs regulates humification and SOC sequestration, quantifying the functional contributions of microbial communities to these processes. These findings advance understanding of forest SOM dynamics and provide scientific a basis for predicting soil carbon stabilization under environmental change.

Abstract Image

凋落物介导的微生物群落沿海拔梯度的变化增强了腐殖质化驱动的土壤有机碳积累
腐殖质是土壤有机质(SOM)的主要组成部分,而森林凋落物是腐殖质的重要来源,驱动土壤有机碳(SOC)的形成。然而,凋落物输入调节腐殖化和有机碳固存的机制尚不明确。本研究通过对山西中跳山森林生态系统中凋落物和土壤相关细菌和真菌的扩增子测序,结合生物地球化学分析,确定了腐殖化和有机碳积累的驱动因素。结果表明,凋落物/土壤养分随海拔升高而增加,腐殖质含量随海拔升高而下降。微生物群落(包括稀有和丰富的类群)随海拔高度的变化而变化,pH、含水量、总磷和微生物生物量氮是主要决定因素。相关分析和Mantel试验进一步表明,腐殖质和有机碳组分不仅受土壤性质的影响,还受凋落物化学性质和凋落物微生物群落多样性和组成的影响。值得注意的是,相对于丰富的微生物类群,凋落物中较少的微生物类群对腐殖质和有机碳积累的影响更大。混合效应模型验证了腐殖质含量是土壤有机碳积累的重要预测因子。此外,结构方程模型(SEM)表明,早期凋落物微生物通过改变土壤微生物群落结构,直接增加了腐殖质和有机碳的储量,并间接促进了腐殖化。本研究阐明了凋落物输入的海拔变化对腐殖化和有机碳吸收的调节机制,量化了微生物群落对这些过程的功能贡献。这些研究结果促进了对森林土壤有机质动态的认识,并为预测环境变化下土壤碳稳定提供了科学依据。
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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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