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Volume 14, issue 9
Biogeosciences, 14, 2481–2494, 2017
https://doi.org/10.5194/bg-14-2481-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 14, 2481–2494, 2017
https://doi.org/10.5194/bg-14-2481-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 May 2017

Research article | 17 May 2017

Long-term carbon and nitrogen dynamics at SPRUCE revealed through stable isotopes in peat profiles

Erik A. Hobbie et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (27 Dec 2016) by Paul Stoy
AR by Erik Hobbie on behalf of the Authors (15 Feb 2017)  Author's response
ED: Referee Nomination & Report Request started (18 Feb 2017) by Paul Stoy
RR by Tim Moore (13 Mar 2017)
RR by Anonymous Referee #4 (23 Mar 2017)
ED: Publish subject to technical corrections (28 Mar 2017) by Paul Stoy
AR by Erik Hobbie on behalf of the Authors (07 Apr 2017)  Author's response    Manuscript
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Short summary
We measured carbon and nitrogen isotope ratios (13C : 12C and 15N : 14N) in peat cores in a northern Minnesota bog to understand how climate, vegetation type, and decomposition affected C and N budgets over the last 9000 years. 13C : 12C patterns were primarily influenced by shifts in temperature, peatland vegetation and atmospheric CO2, whereas tree colonization and upland N influxes affected 15N : 14N ratios. Isotopic markers provided new insights into long-term patterns of CO2 and nitrogen losses.
We measured carbon and nitrogen isotope ratios (13C : 12C and 15N : 14N) in peat cores in a...
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