Glacial‐Interglacial Climate Cycles of Atmospheric Hg Deposition: Insights From Hg Isotopes in Loess‐Paleosol Sequences on the Chinese Loess Plateau

• Published in: Geophysical research letters Vol. 52; no. 7
• Main Authors: Xue, Wen, Xu, Zhidong, Cheng, Xing, Gou, Longfei, He, Maoyong, Jin, Zhangdong, Li, Miling, Fang, Linchuan, Yin, Runsheng
• Format: Journal Article
• Language: English
• Published: Washington John Wiley & Sons, Inc 16.04.2025; Wiley
• Subjects: Anthropogenic factors; Atmosphere; Climate control; Deposition; Dry deposition; Ecosystems; Emissions; Eolian deposits; Glacial deposits; Heavy metals; Interglacial periods; Isotope composition; Isotope ratios; Isotopes; Latitude; Loess; Mercury; Mercury (metal); Paleosols; Perturbation; Perturbations; Plateaus; Pollution dispersion; Soils; Wet deposition; Winter monsoon; Loess Plateau
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1029/2024GL113960

As a highly volatile heavy metal, Hg is transported over long distances in the atmosphere and enters global ecosystems via Hg(II) wet deposition and Hg(0) dry deposition. The Chinese Loess Plateau develops loess‐paleosol sequences (eolian deposits) reflecting glacial‐interglacial cycles. Here, we investigate the Hg concentration and isotopic composition of loess‐paleosol sequences covering three glacial‐interglacial cycles (spanning 350–80 ka). Paleosol layers display higher THg, Δ199Hg, and Δ200Hg values than loess layers, meaning enhanced Hg(II) wet deposition during interglacials. Based on a Δ200Hg‐based mixing model, Hg(II) wet and Hg(0) dry depositions account for 42% and 58% of Hg input into the Chinese Loess Plateau during interglacials but 21% and 79% during glacials, respectively. This work highlights a strong climatic control on atmospheric Hg deposition at glacial‐interglacial time scales, and suggests that atmospheric Hg deposition will likely increase in middle latitudes without considering perturbations of anthropogenic emissions. Plain Language Summary Mercury is a heavy metal pollutant that undergoes global transport in the atmosphere and enters global ecosystems via atmospheric deposition. This work for the first time observes glacial‐interglacial cycles of Hg concentration and Hg isotopic ratios in loess‐paleosol sequences on the Chinese Loess Plateau. The results provide strong evidence of climatic control on atmospheric Hg deposition. Variations in summer and winter monsoons during glacial‐interglacial cycles regulate the intensity of atmospheric Hg deposition on the Chinese Loess Plateau. This work predicts that atmospheric Hg deposition will likely increase in middle latitudes without considering perturbations of anthropogenic emissions. Key Points The atmospheric Hg deposition history was reconstructed using loess‐paleosol sequences on the Chinese Loess Plateau Glacial‐interglacial cycles of atmospheric Hg deposition were reported for the first time in eolian deposits Variations in summer and winter monsoons during glacial‐interglacial cycles control atmospheric Hg deposition