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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 14
Biogeosciences, 14, 3561–3584, 2017
https://doi.org/10.5194/bg-14-3561-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Changing Permafrost in the Arctic and its Global Effects in...

Biogeosciences, 14, 3561–3584, 2017
https://doi.org/10.5194/bg-14-3561-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 27 Jul 2017

Research article | 27 Jul 2017

Dissolved organic carbon and major and trace elements in peat porewater of sporadic, discontinuous, and continuous permafrost zones of western Siberia

Tatiana V. Raudina et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (15 May 2017) by Susan Natali
AR by O.S. Pokrovsky on behalf of the Authors (15 May 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (22 May 2017) by Susan Natali
RR by Anonymous Referee #2 (19 Jun 2017)
ED: Publish subject to technical corrections (27 Jun 2017) by Susan Natali
AR by O.S. Pokrovsky on behalf of the Authors (03 Jul 2017)  Author's response    Manuscript
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Short summary
We collected peat porewaters across a 640 km latitudinal transect of sporadic to continuous permafrost zone and analyzed organic carbon and trace metals. There was no distinct decrease in concentration along the latitudinal transect from 62.2° N to 67.4° N. The northward migration of the permafrost boundary or the change of hydrological regime is unlikely to modify chemical composition of peat porewater fluids larger than their natural variation within different micro-landscapes.
We collected peat porewaters across a 640 km latitudinal transect of sporadic to continuous...
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