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Comparing ecosystem gaseous elemental mercury fluxes over a deciduous and coniferous forest

Jun Zhou, Silas W. Bollen, Eric M. Roy, David Y. Hollinger, Ting Wang, John T. Lee and Daniel Obrist ()
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Jun Zhou: University of Massachusetts
Silas W. Bollen: University of Massachusetts
Eric M. Roy: University of Massachusetts
David Y. Hollinger: Northern Research Station
Ting Wang: University of Massachusetts
John T. Lee: University of Maine
Daniel Obrist: University of Massachusetts

Nature Communications, 2023, vol. 14, issue 1, 1-9

Abstract: Abstract Sources of neurotoxic mercury in forests are dominated by atmospheric gaseous elemental mercury (GEM) deposition, but a dearth of direct GEM exchange measurements causes major uncertainties about processes that determine GEM sinks. Here we present three years of forest-level GEM deposition measurements in a coniferous forest and a deciduous forest in northeastern USA, along with flux partitioning into canopy and forest floor contributions. Annual GEM deposition is 13.4 ± 0.80 μg m−2 (coniferous forest) and 25.1 ± 2.4 μg m−2 (deciduous forest) dominating mercury inputs (62 and 76% of total deposition). GEM uptake dominates in daytime during active vegetation periods and correlates with CO2 assimilation, attributable to plant stomatal uptake of mercury. Non-stomatal GEM deposition occurs in the coniferous canopy during nights and to the forest floor in the deciduous forest and accounts for 24 and 39% of GEM deposition, respectively. Our study shows that GEM deposition includes various pathways and is highly ecosystem-specific, which complicates global constraints of terrestrial GEM sinks.

Date: 2023
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DOI: 10.1038/s41467-023-38225-x

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