Mercury Accumulation and Sequestration in a Deglaciated Forest Chronosequence: Insights from Particulate and Mineral-Associated Forms of Organic Matter

Abstract

Understanding mercury (Hg) complexation with soil organic matter is important in assessing atmospheric Hg accumulation and sequestration processes in forest ecosystems. Separating soil organic matter into particulate organic matter (POM) and mineral-associated organic matter (MAOM) can help in the understanding of Hg dynamics and cycling due to their very different chemical constituents and associated formation and functioning mechanisms. The concentration of Hg, carbon, and nitrogen contents and isotopic signatures of POM and MAOM in a deglaciated forest chronosequence were determined to construct the processes of Hg accumulation and sequestration. The results show that Hg in POM and MAOM are mainly derived from atmospheric Hg0 deposition. Hg concentration in MAOM is up to 76% higher than that in POM of broadleaf forests and up to 60% higher than that in POM of coniferous forests. Hg accumulation and sequestration in organic soil vary with the vegetation succession. Variations of δ202Hg and Δ199Hg are controlled by source mixing in the broadleaf forest and by Hg sequestration processes in the coniferous forest. Accumulation of atmospheric Hg and subsequent microbial reduction enrich heavier Hg isotopes in MAOM compared to POM due to the specific chemical constituents and nutritional role of MAOM.

Fate and Transport of Mercury through Waterflows in a Tropical Rainforest

“…One is that geogenic Hg is mainly fixed in the soil minerals and hardly dissolves into water. 59 The other is that much more negative signatures of δ 202 Hg and Δ 199 Hg in runoff water than the isotopic features in bedrock (δ 202 Hg = −0.42 ± 0.19‰ and Δ 199 Hg = −0.09 ± 0.03‰) 50 also confirm negligible contribution from geogenic Hg. Hg in throughfall and surface runoff comes primarily from atmospheric Hg 0 and Hg 2+ .…”