Abstract
Prior geophysical surveys provided evidence for a hypersaline subglacial lake complex beneath the center of Devon Ice Cap, Canadian Arctic; however, the full extent and characteristics of the hydrological system remained unknown due to limited data coverage. Here, we present results from a new, targeted aerogeophysical survey that provides evidence (i) supporting the existence of a subglacial lake complex and (ii) for a network of shallow brine/saturated sediments covering ∼170 km2. Newly resolved lake shorelines indicate three closely spaced lakes covering a total area of 24.6 km2. These results indicate the presence of a diverse hypersaline subglacial hydrological environment with the potential to support a range of microbial habitats, provide important constraints for future investigations of this compelling scientific target, and highlight its relevance as a terrestrial analog for aqueous systems on other icy worlds.
| Original language | English |
|---|---|
| Pages (from-to) | 379-395 |
| Number of pages | 17 |
| Journal | The Cryosphere |
| Volume | 16 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 2 Feb 2022 |
Programme Area
- Programme Area 5: Nature and Climate
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