Access

You are not currently logged in.

Access your personal account or get JSTOR access through your library or other institution:

login

Log in to your personal account or through your institution.

Restored Cut-Away Peatland as a Sink for Atmospheric CO₂

Eeva-Stiina Tuittila, Veli-Matti Komulainen, Harri Vasander and Jukka Laine
Oecologia
Vol. 120, No. 4 (1999), pp. 563-574
Published by: Springer in cooperation with International Association for Ecology
Stable URL: http://www.jstor.org/stable/4222423
Page Count: 12
  • Download ($43.95)
  • Cite this Item
Restored Cut-Away Peatland as a Sink for Atmospheric CO₂
Preview not available

Abstract

In a field study, we examined the relationship between vegetation, abiotic factors and the CO₂ exchange dynamics of a cut-away peatland 20 years after production had ended. The main objective was to determine the effect of rewetting on the CO₂ exchange dynamics, measured separately in Eriophorum vaginatum tussocks and intertussocks (almost non-vegetated surfaces) using closed-chamber techniques, one growing season before and three growing seasons after the rewetting treatment. Rewetting lowered total respiration ($R_{\text{TOT}}$) and increased gross photosynthesis ($P_{\text{G}}$), which resulted in a higher incorporation of CO₂ into the system. The seasonal CO₂ balance for the almost continuously submerged section of the rewetted site became positive 2 years after rewetting (9.1 g CO₂-C m-2), and it was still higher in the 3rd year (64.5 g CO₂-C m-2), i.e. the system accumulated carbon. In the driest section of the rewetted site the seasonal balance increased strongly, but the balance was still negative during the 3 years following rewetting with losses from the system of 44.1, 26.1, 38.3 g CO₂-C m-2 in 1995, 1996 and 1997 respectively. At the control site seasonal balance during 1995-1997 varied between ecosystem C losses of 41.8 and 95.3 in an area with high Eriophorum cover and between 52.1 and 109.9 g CO₂-C m-2 with lower cover. Simulation of a cut-away peatland with dense Eriophorum vegetation (Eriophorum cover 70%) showed that if the water level (WT) is low, the seasonal CO₂ balance of the ecosystem can reach the compensation point of no net C change ($P_{\text{G}}=R_{\text{TOT}}$) only if weather conditions are favourable, but with a high WT the seasonal CO₂ balance would be positive even under varying weather conditions. It can be concluded that with dense Eriophorum vegetation a restored cut-away peatland acts as a functional mire and becomes a sink for atmospheric CO₂.

Page Thumbnails

  • Thumbnail: Page 
[563]
    [563]
  • Thumbnail: Page 
564
    564
  • Thumbnail: Page 
565
    565
  • Thumbnail: Page 
566
    566
  • Thumbnail: Page 
567
    567
  • Thumbnail: Page 
568
    568
  • Thumbnail: Page 
569
    569
  • Thumbnail: Page 
570
    570
  • Thumbnail: Page 
571
    571
  • Thumbnail: Page 
572
    572
  • Thumbnail: Page 
573
    573
  • Thumbnail: Page 
574
    574