0
Article ? AI-assigned paper type based on the abstract. Classification may not be perfect — flag errors using the feedback button. Tier 2 ? Original research — experimental, observational, or case-control study. Direct primary evidence. Sign in to save

Estuarine plastisphere as an overlooked source of N2O production

Nature Communications 2022 199 citations ? Citation count from OpenAlex, updated daily. May differ slightly from the publisher's own count.
Xiaoxuan Su, Leyang Yang, Kai Yang, Yijia Tang, Teng Wen, Yingmu Wang, Matthias C. Rillig, Lena Rohe, Junliang Pan, Hu Li, Yong‐Guan Zhu

Summary

Researchers found that the "plastisphere" — the community of microbes that colonizes floating plastic debris in estuaries — produces more nitrous oxide (a potent greenhouse gas) than surrounding water, revealing that plastic pollution may be quietly contributing to climate change through altered microbial chemistry.

"Plastisphere", microbial communities colonizing plastic debris, has sparked global concern for marine ecosystems. Microbiome inhabiting this novel human-made niche has been increasingly characterized; however, whether the plastisphere holds crucial roles in biogeochemical cycling remains largely unknown. Here we evaluate the potential of plastisphere in biotic and abiotic denitrification and nitrous oxide (N2O) production in estuaries. Biofilm formation provides anoxic conditions favoring denitrifiers. Comparing with surrounding bulk water, plastisphere exhibits a higher denitrifying activity and N2O production, suggesting an overlooked N2O source. Regardless of plastisphere and bulk water, bacterial and fungal denitrifications are the main regulators for N2O production instead of chemodenitrification. However, the contributions of bacteria and fungi in the plastisphere are different from those in bulk water, indicating a distinct N2O production pattern in the plastisphere. These findings pinpoint plastisphere as a N2O source, and provide insights into roles of the new biotope in biogeochemical cycling in the Anthropocene.

Share this paper