Isotopic signatures and mercury content of arctic char and their prey, and water chemistry of 18 arctic Canadian lakes

• Main Authors: Gantner, Nikolaus, Power, Michael, Iqaluk, Deborah, Meili, Markus, Borg, Hans, Sundbom, Marcus, Solomon, Keith R, Lawson, Greg, Muir, Derek C G
• Format: Other/Unknown Material
• Language: English
• Published: PANGAEA 2010
• Subjects: International Polar Year (2007-2008); IPY; Arctic; International Polar Year; Zooplankton
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.810149; https://doi.org/10.1594/PANGAEA.810149

Concentrations of mercury (Hg) have increased slowly in landlocked Arctic char over a 10- to 15-year period in the Arctic. Fluxes of Hg to sediments also show increases in most Arctic lakes. Correlation of Hg with trophic level (TL) was used to investigate and compare biomagnification of Hg in food webs from lakes in the Canadian Arctic sampled from 2002 to 2007. Concentrations of Hg (total Hg and methylmercury [MeHg]) in food webs were compared across longitudinal and latitudinal gradients in relation to d13C and d15N in periphyton, zooplankton, benthic invertebrates, and Arctic char of varying size-classes. Trophic magnification factors (TMFs) were calculated for the food web in each lake and related to available physical and chemical characteristics of the lakes. The relative content of MeHg increased with trophic level from 4.3 to 12.2% in periphyton, 41 to 79% in zooplankton, 59 to 72% in insects, and 74 to 100% in juvenile and adult char. The d13C signatures of adult char indicated coupling with benthic invertebrates. Cannibalism among char lengthened the food chain. Biomagnification was confirmed in all 18 lakes, with TMFs ranging from 3.5 ± 1.1 to 64.3 ± 0.8. Results indicate that TMFs and food chain length (FCL) are key factors in explaining interlake variability in biomagnification of [Hg] among different lakes.