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| 论文摘要： | Anthropogenic activities have introduced substantial quantities of carbon and nitrogen into aquatic system, which are hotspots for nitrous oxide emissions and play multiple roles in the global biogeochemical cycle. We characterized the seasonal variation of DOM by employing a comprehensive approach incorporating absorption spectroscopy, excitation-emission matrix fluorescence and Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS). Results revealed that DOM seasonal variation could be the main factor driven lake N2O emission alteration. In warm seasons, lakes are predominant with recalcitrant aromatic compounds DOM released by phytoplankton, such as highly unsaturated and phenolic compounds, polyphenols., and lignin, accompanied by low N2O concentrations (0.03+0.02 mu mol/L). In cold seasons, bioavailable components (Aliphatic, Sugar-like, Peptide-like) are dominated in lakes, the increased abundance of S-containing compounds and low aromaticity compounds largely influenced by anthropogenic emissions, leads to elevated N2O concentrations (1.91+0.06 mu mol/L). The DOM with high bioavailable components promotes sediment N2O production (nir/nosZ (I+II)-type denitrifiers) (n = 678). Recalcitrant DOM reduced sediment nirK and nirS-type denitrifiers, and increased nosZ (I+II)-type denitrifiers, enhance the N2O reduction and led to a lower N2O emission. This study advances the understanding of the microbial mechanisms that DOM regulates N2O emissions in lakes. |
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