Deep ice as a geochemical reactor: insights from iron speciation and mineralogy of dust in the Talos Dome ice core (East Antarctica)
Thanks to its insolubility, mineral dust is considered a stable proxy in polar ice cores. With this study we show that below an ice-depth of 1000 m, the Talos Dome ice core (Ross Sea sector of East Antarctica) presents evident and progressive signs of post-depositional processes affecting the minera...
Main Authors: | , , , , , , , , , |
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Format: | Text |
Language: | English |
Published: |
2021
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-2021-162 https://tc.copernicus.org/preprints/tc-2021-162/ |