

FOLLOWUS
1.Guangdong Basic Research Center of Excellence for Ecological Security and Green Development, Guangdong Provincial Key Laboratory of Water Quality Improvement and Ecological Restoration for Watersheds, School of Ecology, Environment and Ocean, Guangdong University of Technology, Guangzhou 510006, China
2.School of Environmental and Material Engineering, Yantai University, Yantai 264005, China
3.Guangdong Provincial Observation and Research Station for Social-Natural Complex Ecosystems in Haizhu Wetlands, Guangzhou 510399, China
qian_tan@gdut.edu.cn
Received:20 November 2025,
Online First:20 July 2026,
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LI Yingjie,ZHANG Sibo,LI Xiaoxiao,et al.Divergent environmental drivers for N2O and N2 dynamics along an urbanized river-estuary continuum[J].Journal of Oceanology and Limnology,DOI:. DOI: 10.1007/s00343-026-5468-y.
River-estuary continua are hotspots for nitrogen transformations; however
whether N
2
O and N
2
transformations vary in parallel in response to environmental variations along these continua remains poorly understood. This study compared spatial variations and environmental controls of excess N
2
O (ΔN
2
O) and excess N
2
(ΔN
2
) concentrations along an urban river-estuary continuum
combining multi-season measurements with metagenomic analysis of nitrogen-cycling functional genes. Both ΔN
2
O (-0.61–188.78 nmol/L) and ΔN
2
(-127.38–155.66 μmol/L) peaked in the river-estuary transition zone
coinciding with high nutrient inputs
and potentially prolonged water residence time. However
we found a clear decoupling between these two gases
evidenced by their insignificant correlation and spatially offset peaks. Machine learning analysis indicated their divergent environmental drivers; nitrate was more important for ΔN
2
O
while temperature and dissolved organic carbon (DOC) were more critical for ΔN
2
. DOC was positively correlated with the genetic potential ratio of N
2
production to fixation
and temperature was negatively linked to the genetic potential for N
2
O production relative to reduction. Furthermore
upon entering the estuary
ΔN
2
concentrations declined more sharply than ΔN
2
O
leading to widespread N
2
undersaturation (i.e.
ΔN
2
<
0). This undersaturation is consistent with reduced denitrification
reflected by decreased denitrifier abundance due to high salinity and sulfide levels
alongside persistent N
2
fixation. The slower decrease in ΔN
2
O is consistent with reduced N
2
O consumption and elevated ammonia-oxidizing archaea to ammonia-oxidizing bacteria ratio. Our findings highlight distinct biogeochemical controls on N
2
O and N
2
dynamics
providing insights for improving nitrogen removal and mitigating N
2
O emissions in aquatic ecosystems.
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