Resumé
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.
| Originalsprog | Engelsk |
|---|---|
| Sider (fra-til) | 379-395 |
| Antal sider | 17 |
| Tidsskrift | The Cryosphere |
| Vol/bind | 16 |
| Udgave nummer | 2 |
| DOI | |
| Status | Udgivet - 2 feb. 2022 |
Programområde
- Programområde 5: Natur og klima
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