Anthropogenic activities release large quantities of
heavy metals
into the atmosphere. In China, the input of these heavy metals through
local and trans-boundary atmospheric deposition is poorly understood.
To assess this issue, herein, we use Pb and Zn isotopes to constrain
the sources of Pb and Zn in a 210Pb-dated sediment core
collected from the enclosed lake in South China. We observed a progressive
shift toward higher 208Pb/206Pb and Pb fluxes
(0.79–4.02 μg·cm–2·a–1) from 1850 to 1950 and a consistent decrease in δ66ZnIRMM (as low as −0.097 ± 0.030‰)
coupled with an increase in Pb (1.74–3.36 μg·cm–2·a–1) and Zn (8.07–10.44
μg·cm–2·a–1) fluxes
after 1980. These distinguished isotopic signals and flux variations
reveal the presence of trans-boundary Pb since 1900, with the addition
of local industrial Pb and Zn pollution after 1980. Up to 72.3% of
Pb deposited at our site can be attributed to long-distance transportation
from previously industrialized countries, resulting in a noteworthy
legacy of Pb in China since 1900. Despite the phasing out of leaded
gasoline, Chinese gasoline still contributes an average of 20.9%.
The contribution of China’s mining and smelting activities
to Pb has increased steadily since 1980 and remained stable at an
average of 25.1% since 2000.