Abstract
Abstract Soils in hyper-arid climates, such as the Chilean Atacama Desert, show indications of past and present forms of life despite extreme water limitations. We hypothesize that fog plays a key role in sustaining life. In particular, we assume that fog water is incorporated into soil nutrient cycles, with the inland limit of fog penetration corresponding to the threshold for biological cycling of soil phosphorus (P). We collected topsoil samples (0?10?cm) from each of 54 subsites, including sites in direct adjacency (
| Original language | English |
|---|---|
| Pages (from-to) | e17068 |
| Journal | Global Change Biology |
| Volume | 30 |
| Issue number | 1 |
| Early online date | 8 Dec 2023 |
| DOIs | |
| Publication status | Published - 1 Jan 2024 |
Keywords
- Atacama Desert
- fog
- hyper-aridity
- oxygen isotopes ratio in phosphates
- soil P cycle
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