Competitive equilibrium between carbon loss and sequestration driven by erosion: Stratified responses of microbial metabolism and mineral protection - 2026
[en] Soil erosion drives the redistribution of soil organic carbon (SOC) through transportation and deposition processes, yet its underlying mechanisms in shaping the carbon source/sink patterns on slopes remain inadequately understood. Prevailing studies have predominantly focused on the physical translocation effects of erosion, overlooking the biologically-driven priming mineralization. The differential transport and burial of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) induced by erosion may form a physical carbon sink; however, the synergistic mechanisms between physical protection and biological metabolic processes are still unclear. To address this critical knowledge gap, this study investigated a gentle slope in the Black Soil Region of Northeast China. We measured the contents of SOC fractions (SOC, POC, and MAOC), soil extracellular enzyme activities (BG, and NAG+LAP), and microbial carbon use efficiency (CUE) in topsoil (0–20 cm) and subsoil (20–40 cm) layers along typical upper and lower slope positions. Partial least squares path modeling (PLS-PM) analysis results indicated that the upper zones suffered from a loss of labile POC due to selective erosion, leading to microbial substrate scarcity and a decline in CUE, thereby exacerbating carbon loss. In contrast, lower zones facilitated the enrichment of stable MAOC through mineral protection mechanisms, concomitant with an increase in CUE, creating a local carbon sink. Simultaneously, the vertical migration of carbon contributed to the formation of a relatively stable MAOC pool in the subsoil, partially offsetting erosion-induced carbon release. This study reveals that the redistribution of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) across eroded landscapes, coupled with microbial metabolic adaptation, governs the carbon source/sink dynamics along the slope. Future assessments of the carbon budget under soil erosion must concurrently quantify the losses from physical translocation and the sequestration driven by mineral-biological synergy to systematically decipher the response pathways of the carbon cycle to erosion.
Li, Mengni; Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Agricultural and Rural Eco-Environment, Ministry of Agriculture and Rural Affairs, Beijing, China
Shi, Yulong; Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Agricultural and Rural Eco-Environment, Ministry of Agriculture and Rural Affairs, Beijing, China
Xue, Runyu; Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Agricultural and Rural Eco-Environment, Ministry of Agriculture and Rural Affairs, Beijing, China ; College of Resources and Environment, Qingdao Agricultural University, Qingdao, China
Meersmans, Jeroen ; Université de Liège - ULiège > Département GxABT > Echanges Eau - Sol - Plantes
Zhang, Qingwen; Agricultural Clean Watershed Research Group, Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences/Key Laboratory of Agricultural and Rural Eco-Environment, Ministry of Agriculture and Rural Affairs, Beijing, China
Language :
English
Title :
Competitive equilibrium between carbon loss and sequestration driven by erosion: Stratified responses of microbial metabolism and mineral protection
CAAS - Chinese Academy of Agricultural Sciences NSCF - National Natural Science Foundation of China
Funding text :
This work was supported by the Innovation Program of Chinese Academy of Agricultural Sciences (CAAS-CSAL-202302), and the National Natural Science Foundation of China (No. 41977072).
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