Estuarine plastisphere as an overlooked source of N2O production

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作者
Xiaoxuan Su
Leyang Yang
Kai Yang
Yijia Tang
Teng Wen
Yingmu Wang
Matthias C. Rillig
Lena Rohe
Junliang Pan
Hu Li
Yong-guan Zhu
机构
[1] Chinese Academy of Sciences,Key Laboratory of Urban Environment and Health, Institute of Urban Environment
[2] Southwest University,Interdisciplinary Research Center for Agriculture Green Development in Yangtze River Basin, College of Resources and Environment
[3] University of the Chinese Academy of Sciences,School of Life and Environmental Sciences
[4] The University of Sydney,School of Geography
[5] Nanjing Normal University,College of Civil Engineering
[6] Fuzhou University,School of Electrical Engineering
[7] Freie Universität Berlin,State Key Laboratory of Urban and Regional Ecology, Research Center for Eco
[8] Institute of Biology,Environmental Sciences
[9] Berlin-Brandenburg Institute of Advanced Biodiversity Research,undefined
[10] Thünen Institute of Climate-Smart Agriculture,undefined
[11] Chongqing University,undefined
[12] Chinese Academy of Sciences,undefined
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摘要
“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.
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