| Literature DB >> 24953756 |
Birgit Braune1, John Chételat2, Marc Amyot3, Tanya Brown4, Meredith Clayden5, Marlene Evans6, Aaron Fisk7, Ashley Gaden8, Catherine Girard3, Alex Hare8, Jane Kirk9, Igor Lehnherr10, Robert Letcher2, Lisa Loseto11, Robie Macdonald12, Erin Mann13, Bailey McMeans7, Derek Muir9, Nelson O'Driscoll13, Alexandre Poulain14, Ken Reimer15, Gary Stern16.
Abstract
This review summarizes data and information which have been generated on mercury (Hg) in the marine environment of the Canadian Arctic since the previous Canadian Arctic Contaminants Assessment Report (CACAR) was released in 2003. Much new information has been collected on Hg concentrations in marine water, snow and ice in the Canadian Arctic. The first measurements of methylation rates in Arctic seawater indicate that the water column is an important site for Hg methylation. Arctic marine waters were also found to be a substantial source of gaseous Hg to the atmosphere during the ice-free season. High Hg concentrations have been found in marine snow as a result of deposition following atmospheric mercury depletion events, although much of this Hg is photoreduced and re-emitted back to the atmosphere. The most extensive sampling of marine sediments in the Canadian Arctic was carried out in Hudson Bay where sediment total Hg (THg) concentrations were low compared with other marine regions in the circumpolar Arctic. Mass balance models have been developed to provide quantitative estimates of THg fluxes into and out of the Arctic Ocean and Hudson Bay. Several recent studies on Hg biomagnification have improved our understanding of trophic transfer of Hg through marine food webs. Over the past several decades, Hg concentrations have increased in some marine biota, while other populations showed no temporal change. Marine biota also exhibited considerable geographic variation in Hg concentrations with ringed seals, beluga and polar bears from the Beaufort Sea region having higher Hg concentrations compared with other parts of the Canadian Arctic. The drivers of these variable patterns of Hg bioaccumulation, both regionally and temporally, within the Canadian Arctic remain unclear. Further research is needed to identify the underlying processes including the interplay between biogeochemical and food web processes and climate change. CrownEntities:
Keywords: Biogeochemical processes; Canadian Arctic; Food webs; Marine environment; Mercury; Temporal trends
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Year: 2014 PMID: 24953756 DOI: 10.1016/j.scitotenv.2014.05.133
Source DB: PubMed Journal: Sci Total Environ ISSN: 0048-9697 Impact factor: 7.963