Abstract
In arctic ecosystems, winter soil respiration can contribute substantially to annual CO2 release, yet the source of this C is not clear. We analysed the 14C content of C released from plant-free plots in mountain birch forest and tundra-heath. Winter-respired CO2 was found to be a similar age (tundra) or older (forest) than C released during the previous autumn. Overall, our study demonstrates that the decomposition of older C can continue during the winter, in these two contrasting arctic ecosystems. copy; 2013 Elsevier Ltd.
| Original language | English |
|---|---|
| Pages (from-to) | 1-4 |
| Number of pages | 4 |
| Journal | Soil Biology and Biochemistry |
| Volume | 63 |
| DOIs | |
| Publication status | Print publication - Aug 2013 |
| Externally published | Yes |
Keywords
- CO
- Mountain birch
- Passive sampling
- Radiocarbon
- Tree-line
- Tundra-heath
- Winter respiration