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Understanding the relative contribution of environmental and substrate controls on rice paddy methanogenesis is critical for developing mechanistic models of landscape‐scale methane (CH 4 ) flux. A diurnal pattern in observed rice paddy CH 4 flux has been attributed to fluctuations in soil temperature physically driving diffusive CH 4 transport from the soil to atmosphere. Here we make direct landscape‐scale measurements of carbon dioxide and CH 4 fluxes and show that gross ecosystem photosynthesis (GEP) is the dominant cause of the diurnal pattern in CH 4 flux, even after accounting for the effects of soil temperature. The time series of GEP and CH 4 flux show strong spectral coherency throughout the rice growing season at the diurnal timescale, where the peak in GEP leads that of CH 4 flux by 1.3 ± 0.08 hours. By applying the method of conditional Granger causality in the spectral domain, we demonstrated that the diurnal pattern in CH 4 flux is primarily caused by GEP.
An entry from the Cambridge Structural Database, the world’s repository for small molecule crystal structures. The entry contains experimental data from a crystal diffraction study. The deposited dataset for this entry is freely available from the CCDC and typically includes 3D coordinates, cell parameters, space group, experimental conditions and quality measures.