Gradual drying of permafrost peat decreases carbon dioxide production in drier peat plateaus but not in wetter fens and bogs
<p>Permafrost thawing of northern peatlands can cause the local collapse of peat plateaus into much wetter thermokarst bogs and fens, dominated by <i>Sphagnum</i> mosses and graminoids, respectively. However, permafrost thaw can also improve landscape drainage and, thus, lead to th...
Saved in:
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-05-01
|
| Series: | SOIL |
| Online Access: | https://soil.copernicus.org/articles/11/371/2025/soil-11-371-2025.pdf |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|