Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia

Walz, Josefine; Knoblauch, Christian; Tigges, Ronja; Opel, Thomas; Schirrmeister, Lutz; Pfeiffer, Eva-Maria

doi:https://doi.org/10.5194/bg-15-5423-2018

Articles | Volume 15, issue 17

https://doi.org/10.5194/bg-15-5423-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/bg-15-5423-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 15, issue 17

Research article

|

13 Sep 2018

Research article |

| 13 Sep 2018

Greenhouse gas production in degrading ice-rich permafrost deposits in northeastern Siberia

Josefine Walz, Christian Knoblauch, Ronja Tigges, Thomas Opel, Lutz Schirrmeister, and Eva-Maria Pfeiffer

Download

Final revised paper (published on 13 Sep 2018)
Preprint (discussion started on 14 May 2018)

Interactive discussion

Status: closed

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

- Printer-friendly version

- Supplement

RC1: 'Review Walz et al.', Anonymous Referee #1, 20 Jun 2018
- AC1: 'Response to RC1', Josefine Walz, 14 Aug 2018
RC2: 'I recommend to accept the paper of J. Walz for publication with technical corrections. See my suggestions below.', Anonymous Referee #2, 25 Jul 2018
- AC2: 'Response to RC2', Josefine Walz, 14 Aug 2018

Peer-review completion

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

ED: Publish subject to minor revisions (review by editor) (14 Aug 2018) by Alexey V. Eliseev

AR by Josefine Walz on behalf of the Authors (14 Aug 2018) Author's response Manuscript

ED: Publish as is (21 Aug 2018) by Alexey V. Eliseev

Short summary

We investigate potential CO₂ and CH₄ production in degrading ice-rich permafrost in northeastern Siberia, deposited under different climatic conditions. With laboratory incubations, it could be shown that Late Pleistocene yedoma deposits generally produced more CO₂ than Holocene deposits. Thus, OM decomposability needs to be interpreted against the paleoenvironmental background. However, OM decomposability cannot be generalized solely based on the stratigraphic position.