Plant-Mediated Iron–Carbon Interactions: Microbial Drivers of Soil Organic Carbon Sequestration in the Caohai Wetland, Guizhou Province, China

Unofficial AI-generated summary based on the public title and abstract. Not an official translation.

🔬研究者:Provides mechanistic insights into microbial drivers of SOC sequestration in wetlands, useful for carbon cycle modeling.

🏢実務担当者:May inform wetland management and restoration practices to enhance carbon storage.

🏛政策担当者:Supports evidence for wetland conservation as a climate mitigation strategy.

Iron oxides are crucial to soil organic carbon (SOC) sequestration in wetland ecosystems. Whether vegetation drives soil microorganisms to regulate iron–carbon interactions and influence SOC sequestration capacity remains controversial. Thus, this study investigated iron–carbon coupling processes and their microbial drivers in the Caohai alpine freshwater closed wetland, Guizhou Province, China. Using metagenomic sequencing and physicochemical analyses, we compared vegetated areas (Phragmites australis and Scirpus tabernaemontani) with bare flats (BF). Levels of SOC, microbial necromass carbon (MNC), and plant-derived carbon (PC) in vegetated soils were significantly higher than those in BF (p < 0.05). In all study regions, the PC/SOC ratio (PA: 27.89 ± 3.59 %; ST: 24.58 ±1.86 %; BF: 24 ±2.82 %) exceeded the MNC/SOC ratio (PA: 15.58 ± 0.94 %; ST: 15.95 ± 0.73 %; BF: 13.06 ±1.30 %). The PC/SOC and MNC/SOC ratios were higher in vegetated areas than in BF areas. Compared with BF, vegetation enhanced wetland SOC stability and promoted carbon sequestration. Iron-bound organic carbon (Fed–OC) content was substantially greater in vegetated soils (PA:0.34 ± 0.08 g/kg; ST:1.07 ± 0.58 g/kg) than in BF (0.14 ± 0.08 g/kg) (p < 0.05). Based on the Fed–OC/Fed ratio (PA: 22.87 ± 14.00 %; ST: 23.00 ± 13.90%; BF: 5.36 ± 3.40 %), Fed–OC associations in vegetated soils were dominated by stable coprecipitation, whereas unstable adsorption prevailed in BF. In all study regions, the abundances of iron-reducing bacteria (FeRB) and iron-oxidizing bacteria (FeOB) peaked in BF. Several FeRB genera, including Thiobacillus, Intrasporangium, Gallionella, and Nocardioides, were significantly and positively correlated with Fed (p < 0.05). Conversely, Geobacter and Nitrospira exhibited significant negative correlations with Fed–OC and PC (p < 0.05). The FeOB genera—Thioalkalivibrio, Thiohalobacter, and Pseudomonas—were negatively correlated with Fed. Vegetation presence appears to influence microbial metabolic potentials through the provision of rhizodeposits and the modulation of rhizosphere conditions, thereby affecting Fed–OC associations and contributing to SOC sequestration in wetland soils to some extent. These findings provide critical insights into plant–microbe–mineral interactions and a scientific framework for predicting carbon sink dynamics in wetland ecosystems.

• openalex https://doi.org/10.3390/ecologies7030077first seen 2026-08-05 04:59:54