Historical
records of mercury (Hg) deposition in lake sediments
have commonly been used to monitor historic atmospheric concentrations.
In the Australian environment, however, freshwater lakes are limited,
restricting the region for which depositional archives of Hg can be
derived. In this study we show that dendrochemistry can provide a
record of atmospheric concentrations at very high resolution. We measured
Hg concentrations in growth rings of two tree species from a site
in western in Tasmania-Huon Pine (Lagarostrobus franklinii) and Celery Top Pine (Phyllocladus aspleniifolius). This region has been heavily mined over the past 150 years. Although
much previous work has linked atmospheric Hg to gold mining, the evidence
in this study suggests that copper smelters in Queenstown and Zeehan,
not gold mining activities, were the main sources of Hg emissions
to the atmosphere in this location. Huon Pine had significantly higher
background Hg concentrations (x̅ = 5.62
ng/g) than Celery Top Pine (x̅ = 2.95
ng/g). No significant increase in Hg concentration during the peak
copper smelting phase (1896 to 1935) was observed in Celery Top Pine,
while a significant 1.4 fold-increase was observed in Huon Pine. Our
results show that of species examined across the globe, Huon Pine
is one of the most efficient bioaccumulators of Hg, making it a good
proxy for tracking historical Hg emissions in western Tasmania. This
ability to measure Hg in the environment is essential if Australia
ratifies the Minamata Convention.