Articles | Volume 12, issue 23
https://doi.org/10.5194/bg-12-7057-2015
https://doi.org/10.5194/bg-12-7057-2015
Research article
 | 
07 Dec 2015
Research article |  | 07 Dec 2015

Carbon dynamics in boreal peatlands of the Yenisey region, western Siberia

E. D. Schulze, E. Lapshina, I. Filippov, I. Kuhlmann, and D. Mollicone

Viewed

Total article views: 3,662 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,527 1,998 137 3,662 633 120 141
  • HTML: 1,527
  • PDF: 1,998
  • XML: 137
  • Total: 3,662
  • Supplement: 633
  • BibTeX: 120
  • EndNote: 141
Views and downloads (calculated since 17 Jul 2015)
Cumulative views and downloads (calculated since 17 Jul 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 06 Jul 2025
Download
Short summary
At the eastern border of the West Siberian Plain, south of permafrost, peat started to accumulate 15000 years ago. Peat accumulated as fen peat at a constant rate of 0.2 mm yr-1 and 0.01 kgC m-2 yr-1. Over the last 2000 years, the bogs have changed into Sphagnum mires, accumulating about 0.1 kgC m-2 yr-1 until the present. The high accumulation rate of peat in unfrozen mires indicates that thawing of permafrost peat may change northern peatlands into long-lasting carbon sinks.
Share
Altmetrics
Final-revised paper
Preprint