Articles | Volume 16, issue 21
Biogeosciences, 16, 4261–4275, 2019
https://doi.org/10.5194/bg-16-4261-2019
Biogeosciences, 16, 4261–4275, 2019
https://doi.org/10.5194/bg-16-4261-2019

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 et al.

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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.
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