Contributions of Plant- and Microbial-Derived Carbon to Soil Organic Carbon Across a Grassland Restoration Chronosequence in a Semi-Arid Typical Steppe of Inner Mongolia

作者：Yiming Liu, Wenjun Li, Sihan Yang, Petri Nummi, Jiazheng Xu, Deli Wang · 发表于：Agronomy · 年份：2026 · DOI：10.3390/agronomy16111102 · 研究领域：Soil Carbon and Nitrogen Dynamics、Remote Sensing in Agriculture、Mycorrhizal Fungi and Plant Interactions

Grassland restoration through grazing exclusion is a key strategy for enhancing soil organic carbon (SOC) sequestration, yet the dynamic contributions of plant- versus microbial-derived carbon (C) remain incompletely understood. We hypothesized that with increasing restoration duration, microbial-derived C would become a major contributor to SOC relative to plant-derived C, and that the relative proportion of bacterial necromass would increase compared to fungal necromass. To explore this, we investigated a 25-year restoration chronosequence (3, 10, 19, 25 years) of a degraded typical steppe on Kastanozem soil in Inner Mongolia, China. While acknowledging the inherent limitations of a space-for-time substitution approach, such as potential unquantified variations in initial pre-enclosure soil conditions and plant species composition, we used lignin phenols, amino sugars, and PLFA analysis to estimate the dynamics of plant- and microbial-derived C. Grassland restoration was associated with significant increases in total PLFAs (15.4–58.8%), bacterial PLFAs (14.5–82.4%), lignin phenols (16.9–91.8%), and estimated microbial-derived C (5.0–8.8 g kg−1). Based on these specific biomarker estimates, which track only a subset of total C and do not equal 100% of the SOC pool, microbial-derived C accounted for 52.8–63.3% of SOC, compared to 10.1–15.5% for plant-derived C. Within the estimated microbial-derived C, the bacterial fraction increased over the restoration chronosequence, whil...