Mercury is a globally distributed atmospheric pollutant, which travels long distances in the form of gaseous elemental mercury (Hg 0 ). Gaseous Hg 0 is removed from the atmosphere via the foliar uptake (Demers et al., 2013;Zhou et al., 2021) or via oxidation to Hg 2+ , which is readily deposited to the biosphere following sorption to particles (Hg P ) and/or precipitation (Selin, 2009). Since industrialization, anthropogenic activities alone have increased mercury emission by a factor of approximately 5 (Streets et al., 2017). Increased mercury loading to aquatic ecosystems can enhance microbial production of monomethylmercury (MeHg) (Benoit et al., 2003;Lindberg et al., 2007), which is a bioaccumulative toxin in food webs (Mergler et al., 2007). Humans are primarily exposed to MeHg via the consumption of fishery products (Sunderland, 2007).In 2017, the Minamata Convention on Mercury (MC), a multilateral agreement to mitigate anthropogenic mercury emissions and human health from mercury pollution, has entered into force (UNEP, 2019). As a part of the MC, provisions have been established for a global monitoring program and a convention effectiveness evaluation (Article 19, 22) to understand spatiotemporal changes in mercury levels as well as its sources, processes, and fate in various environmental media. Since then, numerous studies have assessed temporal trends of mercury in diverse atmospheric samples (Hg 0 , Hg 2+ , Hg P , precipitation) (Cheng et al., 2017;Dommergue et al., 2016) and biota (fish, bird eggs, polar bear) (Blukacz-Richards et al., 2017;Lee et al., 2016;McKinney et al., 2017) to gather insights on the changes in emissions, deposition, and ecosystem fate of mercury. Natural archives of sediment, peat, and ice cores have also been used to quantify long-term changes in the deposition of various atmospheric mercury species (Engstrom et al., 2014;Enrico