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 C-14 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. (c) 2013 Elsevier Ltd. All rights reserved.
| Original language | English |
|---|---|
| Pages (from-to) | 1-4 |
| Number of pages | 4 |
| Journal | Soil Biology and Biochemistry |
| Volume | 63 |
| DOIs | |
| Publication status | Published - Aug 2013 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 13 Climate Action
Keywords
- (CO2)-C-14
- Passive sampling
- Mountain birch
- Radiocarbon
- Tree-line
- Tundra-heath
- Winter respiration
- TEMPERATURE SENSITIVITY
- MOLECULAR-SIEVE
- VEGETATION TYPE
- ORGANIC-CARBON
- CLIMATE-CHANGE
- RESPIRATION
- DECOMPOSITION
- REGION
- TUNDRA
- STOCKS
Fingerprint
Dive into the research topics of 'The age of CO2 released from soils in contrasting ecosystems during the arctic winter'. Together they form a unique fingerprint.Cite this
- APA
- Author
- BIBTEX
- Harvard
- Standard
- RIS
- Vancouver