资源环境科技发展态势分析平台

Ice core measurements of the concentration and stable isotopic composition of atmospheric nitrous oxide (N₂O) 74,000‐59,000 years ago constrain marine and terrestrial emissions. The data include two major Dansgaard‐Oeschger (D‐O) events and the N₂O decrease during global cooling at the Marine Isotope Stage (MIS) 5a‐4 transition. The N₂O increase associated with D‐O 19 (~73‐71.5 ka) was driven by equal contributions from marine and terrestrial emissions. The N₂O decrease during the transition into MIS 4 (~71.5‐67.5 ka) was caused by gradual reductions of similar magnitude in both marine and terrestrial sources. A 50 ppb increase in N₂O concentration at the end of MIS 4 was caused by gradual increases in marine and terrestrial emissions between ~64‐61 ka, followed by an abrupt increase in marine emissions at the onset of D‐O 16/17 (59.5 ka). This suggests that the importance of marine versus terrestrial emissions in controlling millennial‐scale N₂O fluctuations varied in time.