Stable isotope signatures of Holocene syngenetic permafrost trace seabird presence in the Thule District (NW Greenland)

Wetterich, Sebastian; Davidson, Thomas A.; Bobrov, Anatoly; Opel, Thomas; Windirsch, Torben; Johansen, Kasper L.; González-Bergonzoni, Ivan; Mosbech, Anders; Jeppesen, Erik

doi:https://doi.org/10.5194/bg-16-4261-2019

Articles | Volume 16, issue 21

https://doi.org/10.5194/bg-16-4261-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/bg-16-4261-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 16, issue 21

Research article

|

11 Nov 2019

Research article |

| 11 Nov 2019

Stable isotope signatures of Holocene syngenetic permafrost trace seabird presence in the Thule District (NW Greenland)

Sebastian Wetterich, Thomas A. Davidson, Anatoly Bobrov, Thomas Opel, Torben Windirsch, Kasper L. Johansen, Ivan González-Bergonzoni, Anders Mosbech, and Erik Jeppesen

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Final revised paper (published on 11 Nov 2019)
Supplement to the final revised paper
Preprint (discussion started on 10 Apr 2019)

Interactive discussion

Status: closed

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

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RC1: 'minor revision', Anonymous Referee #1, 30 Apr 2019
- AC1: 'Responses from the authors to comments of anonymous Referee #1 - bg-2019-71', Sebastian Wetterich, 12 Sep 2019
RC2: 'Referee comments', Anonymous Referee #2, 06 Jul 2019
- AC2: 'Responses from the authors to comments of anonymous Referee #2 - bg-2019-71', Sebastian Wetterich, 12 Sep 2019

Peer-review completion

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

ED: Reconsider after major revisions (16 Sep 2019) by Anja Rammig

AR by Sebastian Wetterich on behalf of the Authors (17 Sep 2019) Author's response Manuscript

ED: Publish as is (30 Sep 2019) by Anja Rammig

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Short summary

The effects of seabird presence on permafrost peat evolution in NW Greenland were studied by tracing changes in stable C and N isotope composition along the path from bird sources into permafrost peat. The permafrost growth was triggered by organic matter and nutrient input since the neoglacial cooling and concurrent polynya establishment. The study deals with the complex response of biologic and permafrost dynamics to High Arctic climatic and oceanographic conditions of the Late Holocene.