Biogeosciences
Biogeosciences
BG
Articles | Volume 13, issue 15
Articles | Volume 13, issue 15
https://doi.org/10.5194/bg-13-4315-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-4315-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 13, issue 15
Research article
 | 
01 Aug 2016
Research article |  | 01 Aug 2016

Decadal and long-term boreal soil carbon and nitrogen sequestration rates across a variety of ecosystems

Kristen L. Manies, Jennifer W. Harden, Christopher C. Fuller, and Merritt R. Turetsky

Viewed

Total article views: 2,281 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,357 828 96 2,281 330 89 109
  • HTML: 1,357
  • PDF: 828
  • XML: 96
  • Total: 2,281
  • Supplement: 330
  • BibTeX: 89
  • EndNote: 109
Views and downloads (calculated since 27 Jan 2016)
Cumulative views and downloads (calculated since 27 Jan 2016)

Cited

Saved (preprint)

Latest update: 22 Feb 2025
Download
Short summary
Boreal soils are important to the global C cycle. We need to understand what controls how C accumulates and is lost from this soil. To help we examined C & N accumulation rates for five boreal ecosystems. Most ecosystems were similar. But the rich fen had higher long-term C & N accumulation rates, likely due to differences in nutrient cycling & because it burns less. Therefore, shifts among ecosystems will not change regional C & N dynamics much, unless there is a shift to or from a rich fen.
Read more
Share
Altmetrics
Final-revised paper
Preprint