Articles | Volume 22, issue 9
https://doi.org/10.5194/cp-22-1655-2026
https://doi.org/10.5194/cp-22-1655-2026
Research article
 | 
08 Sep 2026
Research article |  | 08 Sep 2026

Quantifying Southern Hemisphere dust sources during the Last Glacial-Interglacial Transition using rare earth elements in the EPICA Dome C ice core

Sibylle Boxho, Aubry Vanderstraeten, Nadine Mattielli, Goulven G. Laruelle, Aloys Bory, Paolo Gabrielli, and Steeve Bonneville

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Short summary
We present a high-resolution, quantitative reconstruction of dust provenance in the EPICA Dome C ice core (33.7–2.8 kyr BP) using Rare Earth Elements (REE). Dust was mainly sourced from Patagonia during glacial periods, shifting toward Australia, Southern Africa, and the Puna-Altiplano after 14.5 kyr BP due to sea-level rise and hydrological rearrangement in Patagonia. These changes also reflect major reorganizations of Southern Hemisphere atmospheric circulation.
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