Dual Effects of Vegetation Restoration Patterns and Soil Depth on the Soil Microbial Residue Carbon Accumulation in a Red Soil Erosion Area of Southern China

IF 3.7 2区 农林科学 Q2 ENVIRONMENTAL SCIENCES Land Degradation & Development Pub Date : 2025-02-13 DOI:10.1002/ldr.5482
Mengqi Chang, Shengsheng Xiao, Fangchao Wang, Hongguang Liu, Haijin Zheng, Yunhua Liao, Fusheng Chen, G. Geoff Wang
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Abstract

Microbial residue carbon (MRC) is an important source of soil organic carbon (SOC) and plays a vital role in the accumulation and retention of SOC. Vegetation restoration is an effective strategy for restoring degraded lands. However, there are no studies on how the MRC in a profile changes with vegetation restoration. We evaluated MRC (using amino sugars) accumulation and its contribution to SOC at different soil depths (0–20, 20–50, and 50–100 cm) during vegetation restoration in a severely eroded forest (CK), a restored forest (ecological restoration management), an orchard (development management pattern), and a secondary forest (ideal control). Microbial biomarkers were extracted from the soil profiles and used to measure microbial diversity and microbial community composition (using 16S rRNA). Vegetation restoration, soil depth, and their interaction with each other significantly affected the MRC, fungal residue carbon (FRC), and bacterial residue carbon (BRC) contents. The MRC content tended to increase across the four vegetation restoration patterns in the following order: CK (323.25 mg kg−1) < orchard (1035.67 mg kg−1) < restored forest (2919.01 mg kg−1) < secondary forest (6556.72 mg kg−1). Furthermore, the contribution of MRC to SOC increased with increasing soil depth in the restored forest. The contributions of total MRC to the SOC content varied from 13.12% to 71.88%. The rapid accumulation of MRC was substantially influenced by the SOC content, total nitrogen content, soil pH, bacterial and fungal diversity, and bacterial and fungal phyla. In conclusion, the patterns of vegetation restoration and soil depth play important roles in the accumulation of soil MRC in red soil erosion areas. These findings are pivotal for improving our mechanistic understanding of the microbial regulation of SOC preservation during vegetation restoration of a degraded ecosystem.

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华南红壤侵蚀区植被恢复模式和土壤深度对土壤微生物残馀碳积累的双重影响
微生物残碳(MRC)是土壤有机碳(SOC)的重要来源,对土壤有机碳(SOC)的积累和保持起着至关重要的作用。植被恢复是恢复退化土地的有效策略。但是,目前还没有关于剖面MRC随植被恢复而变化的研究。研究了严重侵蚀林(CK)、恢复林(生态恢复管理)、果园(发展管理模式)和次生林(理想对照)植被恢复过程中不同土壤深度(0 - 20cm、20 - 50cm和50 - 100cm) MRC(氨基糖)积累及其对有机碳的贡献。从土壤剖面中提取微生物生物标志物,用于测量微生物多样性和微生物群落组成(使用16S rRNA)。植被恢复、土壤深度及其相互作用显著影响MRC、真菌残碳(FRC)和细菌残碳(BRC)含量。MRC含量在4种植被恢复模式中呈增加趋势,CK (323.25 mg kg−1)<;果园(1035.67 mg kg - 1);恢复森林(2919.01 mg kg−1)<;次生林(6556.72 mg kg−1)。土壤有机质对土壤有机碳的贡献随土壤深度的增加而增加。总MRC对有机碳含量的贡献在13.12% ~ 71.88%之间。土壤有机碳含量、全氮含量、土壤pH、细菌和真菌多样性以及细菌和真菌门类对MRC的快速积累有很大影响。综上所述,植被恢复模式和土壤深度对红壤侵蚀区土壤MRC的积累起重要作用。这些发现对于提高我们对退化生态系统植被恢复过程中有机碳保存的微生物调控机制的理解至关重要。
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来源期刊
Land Degradation & Development
Land Degradation & Development 农林科学-环境科学
CiteScore
7.70
自引率
8.50%
发文量
379
审稿时长
5.5 months
期刊介绍: Land Degradation & Development is an international journal which seeks to promote rational study of the recognition, monitoring, control and rehabilitation of degradation in terrestrial environments. The journal focuses on: - what land degradation is; - what causes land degradation; - the impacts of land degradation - the scale of land degradation; - the history, current status or future trends of land degradation; - avoidance, mitigation and control of land degradation; - remedial actions to rehabilitate or restore degraded land; - sustainable land management.
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