Environmental correlates of peatland carbon fluxes in a thawing landscape: do transitional thaw stages matter?

Malhotra, A.; Roulet, N. T.

doi:https://doi.org/10.5194/bg-12-3119-2015

Articles | Volume 12, issue 10

https://doi.org/10.5194/bg-12-3119-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Freshwater ecosystems in changing permafrost landscapes

https://doi.org/10.5194/bg-12-3119-2015

© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 12, issue 10

Research article

|

29 May 2015

Research article |

| 29 May 2015

Environmental correlates of peatland carbon fluxes in a thawing landscape: do transitional thaw stages matter?

A. Malhotra and N. T. Roulet

Download

Final revised paper (published on 29 May 2015)
Preprint (discussion started on 08 Jan 2015)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC C16: 'Referee comments', Anonymous Referee #1, 20 Jan 2015
RC C243: 'Anonymous referee', Anonymous Referee #2, 17 Feb 2015
AC C1192: 'Author response', Avni Malhotra, 13 Apr 2015
AC C1215: 'Tracked changes version of manuscript', Avni Malhotra, 15 Apr 2015

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Avni Malhotra on behalf of the Authors (15 Apr 2015) Author's response Manuscript

ED: Publish as is (04 May 2015) by Jorien Vonk

Short summary

We found that the dominant abiotic and biotic correlates of CO2 and CH4 fluxes change in strength and interactions as permafrost thaw progresses in a sub-arctic peatland. Our results emphasize the importance of incorporating transitional stages of thaw in landscape-level C budgets and highlight that end-member thaw stages do not adequately describe the variability in structure-function relationships present along a thaw gradient.