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Microplastics Modulate Carbon Sequestration in PaddyFields by Regulating Rhizosphere Silicon Mobility

Figshare 2025
Linan Liu (715375), Xinzuo Yang (22430399), Qiang Li (8118), Jingmin Sun (20285180), Xin He (48101), Han Wu (218687), Robert Mark Ellam (6941357), Zhaoliang Song (459006), Zimin Li (6034085), Jingchun Tang (7440344)

Summary

Researchers investigated how biodegradable PLA and non-degradable PE microplastics alter rhizosphere silicon dynamics, carbon metabolism, and soil carbon storage in a rice paddy growth-cycle microcosm experiment. PLA transiently boosted grain carbon accumulation by 33% via altered silicon translocation, while PE reduced accumulation by 26-40%; both types ultimately disrupted long-term silicon bioavailability and carbon-silicon biogeochemical cycling in paddy fields.

Polymers

Although microplastics (MPs)-induced alterations in microbial carbon (C) and nitrogen (N) cycling have been increasingly documented, their integrated effects on silicon (Si)-mediated C sequestration in paddy ecosystems remain poorly understood. Using a rice (Oryza sativa L.) growth-cycle microcosm experiment, this study investigated how biodegradable (poly(lactic acid), PLA) and nondegradable (polyethylene, PE) MPs alter rhizosphere Si dynamics, microbial C/N metabolism, and soil C storage. PLA treatment increased C accumulation in grains (+33%) and shoots (+10%) relative to the control, whereas PE reduced both by 26–40%, coinciding with divergent Si uptake patterns. Transient stimulation of Si translocation (up to 2-fold under PLA) was associated with short-term mitigation of microbial-driven C losses. However, both MP types progressively reduced rhizosphere Si bioavailability and disrupted aggregate stability, indicating long-term depletion of labile Si pools. Moreover, PLA enhanced N mineralization via enriching Chloroflexi and Actinobacteriota, elevated labile organic C, and downregulated key genes involved in C fixation (e.g., korA/B), thereby undermining persistent C storage. These findings reveal a MPs-induced dual role of short-term elevated C accumulation via rhizosphere Si uptake by plants versus long-term disruption of C–Si coupled biogeochemical cycle in paddy fields.

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