Land-use change (LUC) and salinization interact synergistically to regulate depth-dependent fractionation and biological mediation of soil organic carbon (SOC) in vulnerable agroecosystems. Unlike previous syntheses addressing these drivers separately, the present review integrates them within a depth-resolved biological framework to reveal their combined effects on fraction-specific distribution under contrasting anthropogenic and ionic regimes. In the topsoil (0–30 cm), LUC and salinity synergistically collapse fungal networks, suppress carbon use efficiency, and restructure microbial communities to accelerate particulate organic matter (POM) turnover and impair mineral-associated organic matter (MAOM) formation. In the subsoil (>30 cm), salinity-driven clay dispersion and pore occlusion restrict oxygen diffusion and carbon accessibility, while LUC-induced loss of deep-rooting vegetation reduces carbon supply to mineral-associated pools. These depth-decoupled mechanisms render subsoil MAOM relatively resilient to direct ionic stress but highly vulnerable to land-use legacy, a distinction rarely represented in existing conceptual models. The evidence highlights key management implications, including restoring biological complexity in topsoil through reduced tillage, mycorrhizal re-establishment, and osmotic stress alleviation; conserving subsoil carbon by restoring deep-rooting vegetation and maintaining favorable ionic conditions for organo-mineral stabilization; and using depth-specific biomarkers, including enzymatic stoichiometry, fungal-to-bacterial ratios to detect SOC vulnerability before measurable losses occur. Future research should prioritize depth-explicit monitoring and integrated biological–physicochemical approaches to improve predictions of SOC dynamics. The resulting framework provides a mechanistic basis for depth-differentiated carbon management in salinizing landscapes.
The temperature sensitivity of soil carbon (C) and nitrogen (N) mineralization commonly expressed as the Q
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coefficient, plays a pivotal role in regulating soil–atmosphere greenhouse gas exchanges in temperate ecosystems. This review synthesizes findings from 181 peer-reviewed studies (1960–2025) to evaluate ho...
K. N. Sheuly, Khalid Syfullah, Z. Solaiman· Biogeochemistry· 0 citations
Changes in temperature and nitrogen deposition associated with altered climatic conditions are likely to significantly alter rates of soil organic matter decomposition. However, our current knowledge about how warming and nitrogen deposition interactively alter mineralization of soil organic carbon is largely lim...
Wen-Jun Zhang, Yuan-Hang Hua, Ping Quan et al.· Journal of Plant Nutrition A...· 0 citations
Microplastics (MPs) pollution in agricultural soils alters global carbon cycling, yet the underlying mechanisms remain poorly understood. Through a global meta-analysis of 1230 observations from 89 studies, we show that MPs exposure increased soil organic carbon (SOC) by 27.1%, dissolved organic carbon (DOC) by 16.3%,...
Bing-Yu Zhu, Xiao-Bo Gu, Ya-Dan Du et al.· Journal of Hazardous Materia...· 0 citations
Microbial carbon use efficiency (CUE) has been proposed as a critical determinant of soil organic carbon (SOC) dynamics, yet its relative importance compared with plant carbon inputs, edaphic conditions, microbial attributes, and physicochemical protection remains poorly understood. Here, we conducted large‐scale soil...
Jun-Xiao Pan, Xian-Jin He, Jin-Song Wang et al.· Global Change Biology· 0 citations
Ecological restoration in arid and semi-arid regions plays a vital role in maintaining regional carbon balance under global change. Although water management and vegetation composition regulate soil carbon cycling, their combined effects on greenhouse gas source/sink dynamics in sandy ecosystems and the underlying micr...
Hai-Fu Fang, Xiang Chen, Jian Zhang et al.· Journal of Environmental Man...· 0 citations
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