Articles | Volume 14, issue 18
Biogeosciences, 14, 4341–4354, 2017
https://doi.org/10.5194/bg-14-4341-2017
Biogeosciences, 14, 4341–4354, 2017
https://doi.org/10.5194/bg-14-4341-2017

Research article 28 Sep 2017

Research article | 28 Sep 2017

Soil respiration across a permafrost transition zone: spatial structure and environmental correlates

James C. Stegen et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Jun 2017) by Edzo Veldkamp
AR by James Stegen on behalf of the Authors (12 Jun 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (16 Jun 2017) by Edzo Veldkamp
RR by Alfred Stein (20 Jun 2017)
RR by Anonymous Referee #2 (08 Jul 2017)
ED: Publish subject to technical corrections (04 Aug 2017) by Edzo Veldkamp
AR by James Stegen on behalf of the Authors (15 Aug 2017)  Author's response    Manuscript
Download
Short summary
CO2 loss from soil to the atmosphere (soil respiration) is a key ecosystem function, especially in systems with permafrost. We find that soil respiration shows a non-linear threshold at permafrost depths > 140 cm and that the number of large trees governs soil respiration. This suggests that remote sensing could be used to estimate spatial variation in soil respiration and (with knowledge of key thresholds) empirically constrain models that predict ecosystem responses to permafrost thaw.
Altmetrics
Final-revised paper
Preprint