Peatlands play an important role in boreal ecosystems, storing a large amount of soil organic carbon. In northern ecosystems, collapse-scar bogs (also known as thermokarst bogs) often form as the result of ground subsidence following permafrost thaw. To examine how ecosystem carbon balance changes with the loss of permafrost, we measured carbon and nitrogen storage within a thermokarst bog and the surrounding forest, which continues to have permafrost. These sites are a part of the Bonanza Creek Long Term Ecological Research (LTER) site and are located within Interior Alaska. Here, we report on methods used for core collection analysis as well as the cores’ physical, chemical, and descriptive properties.
Citation Information
| Publication Year | 2017 |
|---|---|
| Title | Soil data for a thermokarst bog and the surrounding permafrost plateau forest, located at Bonanza Creek Long Term Ecological Research Site, Interior Alaska |
| DOI | 10.3133/ofr20161173 |
| Authors | Kristen L. Manies, Christopher C. Fuller, Miriam C. Jones, Mark P. Waldrop, John P. McGeehin |
| Publication Type | Report |
| Publication Subtype | USGS Numbered Series |
| Series Title | Open-File Report |
| Series Number | 2016-1173 |
| Index ID | ofr20161173 |
| Record Source | USGS Publications Warehouse |
| USGS Organization | Volcano Science Center |
Related Content
Mark P Waldrop, Ph.D.
Research Soil Scientist
Research Soil Scientist
Email
Related Content
- Connect
Mark P Waldrop, Ph.D.
Research Soil ScientistEmail