Arctic mercury flux increased through the Last Glacial Termination with a warming climate

Mercury deposition onto the Greenland Ice Sheet increased from the Last Glacial Termination to early Holocene as the North Atlantic warmed and sea ice retreated, according to an ice-core mercury record and atmospheric chemistry modelling. Mercury is a pollutant of global concern, especially in the A...

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Bibliographic Details
Published in:Nature Geoscience
Main Authors: Segato, Delia, Saiz-Lopez, Alfonso, Mahajan, Anoop Sharad, Wang, Feiyue, Corella, Juan Pablo, Cuevas, Carlos Alberto, Erhardt, Tobias, Jensen, Camilla Marie, Zeppenfeld, Chantal, Kjaer, Helle Astrid, Turetta, Clara, Cairns, Warren Raymond Lee, Barbante, Carlo, Spolaor, Andrea
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
HIGH-RESOLUTION RECORD
SEA-ICE
ATMOSPHERIC MERCURY
FRAM STRAIT
HOLOCENE
GREENLAND
PEAT
ACCUMULATION
DEPOSITION
CHEMISTRY
Arctic
Greenland
East Greenland
East Greenland Ice-core Project
Fram Strait
Greenland ice core
Greenland Ice core Project
ice core
Ice Sheet
North Atlantic
Sea ice
Online Access:https://curis.ku.dk/portal/da/publications/arctic-mercury-flux-increased-through-the-last-glacial-termination-with-a-warming-climate(69f103b1-5458-4478-9201-84f4ebed4ddd).html
https://doi.org/10.1038/s41561-023-01172-9
Description
Summary:Mercury deposition onto the Greenland Ice Sheet increased from the Last Glacial Termination to early Holocene as the North Atlantic warmed and sea ice retreated, according to an ice-core mercury record and atmospheric chemistry modelling. Mercury is a pollutant of global concern, especially in the Arctic, where high levels are found in biota despite its remote location. Mercury is transported to the Arctic via atmospheric, oceanic and riverine long-range pathways, where it accumulates in aquatic and terrestrial ecosystems. While present-day mercury deposition in the Arctic from natural and anthropogenic emissions is extensively studied, the control of past climate changes on natural mercury variability remains unknown. Here we present an Arctic mercury record covering the Last Glacial Termination to the early Holocene epoch (15.7-9.0 thousand years before 2000 ce), collected as part of the East Greenland Ice-Core Project. We find a threefold increase in mercury depositional fluxes from the Last Glacial Termination into the early Holocene, which coincided with abrupt regional climate warming. Atmospheric chemistry modelling, combined with available sea-ice proxies, indicates that oceanic mercury evaporation and atmospheric bromine drove the increase in mercury flux during this climatic transition. Our results suggest that environmental changes associated with climate warming may contribute to increasing mercury levels in Arctic ecosystems.

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