Mercury (Hg) is a toxic metal released into the environment through human activities and natural processes and occurs in the atmosphere mainly as gaseous Hg 0 , which has a 0.5-to 1-year residence time (Amos et al., 2013;Lindberg et al., 2007). The present atmospheric Hg deposition has increased by 3-5 times compared to that during the preindustrial period due to the distinctly increasing anthropogenic Hg emissions since the 1850s (UN-Environment, 2019). To reduce anthropogenic Hg emissions across the globe, the Minamata Convention on Mercury, a legally binding international treaty, entered into force in August 2017. However, significant knowledge gaps in Hg cycling challenge our ability to assess the effectiveness of the Convention in reducing human and wildlife Hg exposure. Although the reduction of anthropogenic Hg emissions is expected to distinctly decrease the Hg concentration in the atmosphere, as has been observed at Northern Hemisphere remote sites (Tang et al., 2018;Zhang et al., 2016), it may take much longer for biotic Hg to decrease due to the complex processes associated with changes in climate and land use (