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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.

Delia Segato
Alfonso Saiz-Lopez
Andrea Spolaor
Research04 May 2023
Nature Geoscience

Volume: 16, P: 439-445

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