To amplify grain production capacity, a global trend is emerging in which many regions are transitioning from dependence on rainfall to irrigated agriculture. An illustrative example of this form of land consolidation is the conversion from dryland to paddy fields, which has changed the ecological environment of farmlands, resulting in significant effects on carbon fixation and emissions. However, there currently exists a deficiency in essential understanding regarding the short-term effects of dryland-to-paddy conversion on ecological processes tied to soil carbon-fixation bacteria and carbon emission efficiency (CEE). Therefore, field monitoring and high-throughput sequencing were carried out to monitor the changes in soil carbon emission efficiency and carbon-fixation bacteria before and after the conversion. Our results indicate that while conversion from dryland to paddy fields can boost grain yield, it also results in an increase in soil carbon emissions and a consequent decrease of 25.78% in carbon emission efficiency. This transition has resulted in an increased soil carbon-fixing bacterial alpha diversity index and enhanced network complexity. The structural equation model indicates that changes in soil environmental factors, especially soil moisture, soil organic carbon (SOC), readily oxidizable carbon (ROC), and carbon-fixing bacteria, are the primary drivers of CEE variation (p < 0.05). Given the critical role that the soil carbon cycle plays in global climate change, there is a pressing need for increased global attention towards the carbon emissions triggered by the transition from rainfed to irrigated agriculture.

Fusarium wilt is a devastating soilborne disease that significantly reduces watermelon production worldwide. This disease is caused by Fusarium oxysporum subsp. niveum (E.F.Sm.) W.C. Snyder & H.N.Hansen. Earthworms can influence fungal populations either by consuming or dispersing fungal propagules, making them a promising candidate for the biological control of Fusarium wilt. However, the underlying mechanisms remain poorly understood. In this study, we investigated the effects of adding the local earthworm species Metaphire guillelmi (Michaelsen, 1895) on Fusarium wilt in watermelon under field conditions, laboratory pot experiments, and laboratory pot experiments with sterilized soil. The results demonstrated that, compared to the control, the earthworm addition reduced the population of F. oxysporum by approximately 10⁵ copies/mg and suppressed the incidence of Fusarium wilt by 84.4%. A correlation analysis revealed that the abundance of F. oxysporum was negatively correlated with soil organic matter (SOM), available nitrogen (AN), and available phosphorus (AP). The relative interaction index values indicated that earthworms could enhance SOM and AN levels in the soil. A two-factor network relationship analysis showed that the earthworm addition could inhibit bacteria and fungi to stimulate growth of F. oxysporum while restraining them. A metabolomics analysis revealed that most differential metabolites associated with F. oxysporum were upregulated in the presence of earthworms. Overall, M. guillelmi can reduce the occurrence of Fusarium wilt by improving soil fertility, the relationship of F. oxysporum and microorganisms, and may influence the metabolic process, which need further exploration. It is a potential pathway for the biocontrol of Fusarium wilt.

Coastal reclamation reshapes both soils and vegetation, yet their coupled trajectories remain poorly understood. Here we investigated soil–vegetation co-evolution across a 15-year chronosequence on Hengsha Island in the Yangtze River estuary. The reclaimed soils were formed primarily from dredged estuarine silt and clay slurry deposited during hydraulic filling. Four representative sites were studied, spanning 3 (Y3), 7 (Y7), 10 (Y10), and 15 (Y15) years since reclamation. Soil physicochemical properties (pH, electrical conductivity, salinity, nitrogen, phosphorus, potassium) were measured, while vegetation cover was quantified using NDVI and fractional vegetation cover (FVC) derived from satellite data. Soil conditions improved markedly with reclamation age: pH, conductivity, and salinity declined, whereas nitrogen, phosphorus, and potassium accumulated significantly (p < 0.001). Vegetation shifted from salt-tolerant pioneers (e.g., Suaeda salsa, Phragmites australis) to mixed communities and cultivated rice fields (Oryza sativa), reflecting progressive improvements in soil quality. Vegetation cover increased in parallel, with NDVI rising from 0.12 ± 0.05 (Y3) to 0.35 ± 0.09 (Y15), reflecting a shift from salt-tolerant pioneers to structurally complex communities. Mantel tests revealed strong positive associations of NDVI with organic matter, nitrogen, and phosphorus, and negative associations with pH, conductivity, and salinity. Structural equation modeling identified organic matter and nitrogen enrichment, along with declining pH and dissolved salts, as dominant drivers of vegetation recovery. These results highlight a co-evolutionary process in which soil improvement and vegetation succession reinforce one another, offering insights for ecological restoration and sustainable management in coastal reclamation landscapes.

To improve the degradation rate of sulfamethoxazole (SMX) under hypoxic conditions in paddy fields during the flooding period, a laboratory microcosm experiment was established in this study to investigate the regulatory effect of straw return on the hypoxic degradation of SMX and its underlying microbial mechanisms. The results demonstrated that straw addition significantly promoted the hypoxic degradation of SMX. By the 10th day of the experiment, the residual SMX content in the straw-amended group was only 11.3% of that in the non-straw control group, and the average degradation rate throughout the experimental period was increased by 85.7%. Straw provided complex carbon sources, including organic carbon (e.g., starch, sugars, and humus) and cellulose, which not only reshaped the microbial community structure and created new ecological niches but also increased the microbial network density under SMX stress from 0.010 to 0.024. Acinetobacter, Bacillus, and Pseudomonas, which possess both straw decomposition and SMX degradation capabilities, sequentially became the dominant bacterial taxa. These dominant taxa can adapt to hypoxic fermentation in the flooded environment and co-metabolize SMX by activating the metabolic pathways of aromatic compounds and sugars. This study is expected to open up a novel approach for the remediation of SMX-contaminated flooded paddy fields and provide valuable innovative insights for technological breakthroughs and practical applications in related fields.

Continuous greenhouse watermelon cultivation is widely constrained by declining soil function, impaired nutrient cycling, and increasing soil-borne disease pressure. Developing biologically driven strategies to restore soil–crop coupling is therefore critical for sustainable protected horticulture. Here, we conducted a two-year field experiment (2024–2025) using a randomized block design with three treatments (CK, ST, and STE), three replicates per treatment, and a plot area of 22.5 m² to evaluate how straw application alone and in combination with earthworms regulate soil processes and crop performance in a continuous greenhouse watermelon system. Compared with CK and ST, earthworm–straw co-application (STE) exerted stronger effects, particularly during the mid-to-late growth stages. In 2024, STE increased soil organic matter by 25.34% and 30.28% relative to CK at the fruiting and harvest stages, respectively; in 2025, the corresponding increases were 25.22% and 27.62%. STE also significantly increased total nitrogen at nearly all growth stages, with the maximum increase reaching 67.23% relative to CK at harvest. In 2025, total phosphorus under STE was significantly higher than under CK and ST across all growth stages, with increases of 75.82% and 79.63%, respectively, at the fruiting stage. Neutral phosphatase activity was markedly enhanced, increasing by 292.24% at the fruiting stage in 2025. These improvements were accompanied by higher plot yield and lower wilt disease incidence, with yield increasing by 34.00% in 2024 and 21.29% in 2025 relative to CK, while disease incidence decreased by 41.46% and 56.06%, respectively. Integrative Mantel tests showed that total nitrogen was the factor most strongly associated with watermelon yield, with the correlation coefficient increasing from r = 0.490 (p = 0.001) in 2024 to r = 0.662 (p = 0.001) in 2025. Co-occurrence network analysis further revealed a strong positive correlation between yield and total nitrogen (r = 0.848 in 2024; r = 0.673 in 2025) and a negative correlation between disease incidence and total nitrogen (r = −0.661 in 2024; r = −0.822 in 2025), indicating progressively strengthened soil–plant functional coupling over time. Our findings demonstrate that earthworm–straw co-application strengthened soil nutrient transformation capacity and enhanced soil suppressiveness against wilt disease, thereby providing an effective ecology-based strategy for alleviating continuous-cropping constraints in greenhouse watermelon systems.