Mercury,
a neurotoxic substance, circulates globally,
significantly
stored in soils through atmospheric deposition and plant decay. Despite
being deposited, mercury can be remobilized and released into the
atmosphere and water, enhancing its global cycle. Recent research
suggests that climate warming may amplify the remobilization of soil
mercury, facilitating its incorporation into food webs that humans
exploit. However, the potential geospatial feedback of soil mercury
levels in response to warming remains unclear. By leveraging up-to-date
soil measurements and observation-driven models, we determined the
amount of mercury stored in global 0–100 cm soils to be 4.3
Tg (interquartile range: 2.5–6.3 Tg). Furthermore, our analysis
indicates that warming likely aggravates global soil mercury levels,
particularly in many temperate areas in East Asia, North Europe, and
North America (>20 ng g–1 increase by 2100) due
to warming-induced vegetation greening. Critically, observation-driven
models raise the possibility that implementing ambitious mercury-emission-control
schemes alone may be insufficient to counterbalance the positive feedback
of soil mercury concentration, while process-based biogeochemical
modeling demonstrates consistent patterns that reinforce this concern.
These findings hold broad implications; for example, such feedback
may catalyze mercury remobilization in land-ocean continuums and exacerbate
human risks, stressing the necessity for continued reductions in greenhouse
gas and mercury emissions.