Articles | Volume 14, issue 9
https://doi.org/10.5194/bg-14-2481-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-14-2481-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
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
Earth Systems Research Center, University of New Hampshire, Durham,
New Hampshire, 03824, USA
Janet Chen
Earth Systems Research Center, University of New Hampshire, Durham,
New Hampshire, 03824, USA
Soil and Water Management & Crop Nutrition Laboratory, FAO/IAEA
Agriculture & Biotechnology Laboratories, Seibersdorf, Austria
Paul J. Hanson
Climate Change Science Institute and Environmental Sciences Division,
Oak Ridge National Laboratory, Oak Ridge, Tennessee, 37831, USA
Colleen M. Iversen
Climate Change Science Institute and Environmental Sciences Division,
Oak Ridge National Laboratory, Oak Ridge, Tennessee, 37831, USA
Karis J. McFarlane
Center for Accelerator Mass Spectrometry, Lawrence Livermore National
Laboratory, Livermore, California, 94551, USA
Nathan R. Thorp
Earth Systems Research Center, University of New Hampshire, Durham,
New Hampshire, 03824, USA
Kirsten S. Hofmockel
Department of Ecology, Evolution and Organismal Biology, Iowa State
University, Ames, Iowa, 50011, USA
Pacific Northwest National Laboratory, Richland, Washington, 99354, USA
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Cited
31 citations as recorded by crossref.
- Stable carbon isotopic composition of peat columns, subsoil and vegetation on natural and forestry-drained boreal peatlands H. Nykänen et al. 10.1080/10256016.2018.1523158
- Soil Microbiomes Under Climate Change and Implications for Carbon Cycling D. Naylor et al. 10.1146/annurev-environ-012320-082720
- Plant communities control long term carbon accumulation and biogeochemical gradients in a Patagonian bog P. Mathijssen et al. 10.1016/j.scitotenv.2019.05.310
- Climate drivers alter nitrogen availability in surface peat and decouple N2 fixation from CH4 oxidation in the Sphagnum moss microbiome C. Petro et al. 10.1111/gcb.16651
- Rewetting and Drainage of Nutrient-Poor Peatlands Indicated by Specific Bacterial Membrane Fatty Acids and a Repeated Sampling of Stable Isotopes (δ15N, δ13C) M. Groß-Schmölders et al. 10.3389/fenvs.2021.730106
- Temporal and Spatial Variation in Peatland Carbon Cycling and Implications for Interpreting Responses of an Ecosystem‐Scale Warming Experiment N. Griffiths et al. 10.2136/sssaj2016.12.0422
- Isotope composition of dissolved organic carbon in runoff and peat leachates from a Central European wetland: Temporal and spatial variability in DOC sources M. Novak et al. 10.1016/j.catena.2018.10.011
- Stable isotopes (δ13C, δ15N) and biomarkers as indicators of the hydrological regime of fens in a European east–west transect M. Groß-Schmölders et al. 10.1016/j.scitotenv.2022.156603
- Research challenges and opportunities for using big data in global change biology J. Xia et al. 10.1111/gcb.15317
- Distinctions in heterotrophic and autotrophic-based metabolism as recorded in the hydrogen and carbon isotope ratios of normal alkanes B. Tipple & J. Ehleringer 10.1007/s00442-018-4189-0
- Natural abundance of 13C and 15N provides evidence for plant–soil carbon and nitrogen dynamics in a N‐fertilized meadow R. Wang et al. 10.1002/ecy.3348
- Plant succession and geochemical indices in immature peatlands in the Changbai Mountains, northeastern region of China: Implications for climate change and peatland development L. Zhang et al. 10.1016/j.scitotenv.2020.143776
- Divergent biotic and abiotic filtering of root endosphere and rhizosphere soil fungal communities along ecological gradients C. Lumibao et al. 10.1093/femsec/fiaa124
- Can plant or lichen natural abundance 15N ratios indicate the influence of oil sands N emissions on bogs? R. Wieder et al. 10.1016/j.ejrh.2022.101030
- Water Table Drawdown Alters Soil and Microbial Carbon Pool Size and Isotope Composition in Coastal Freshwater Forested Wetlands K. Minick et al. 10.3389/ffgc.2019.00007
- Draining Effects on Recent Accumulation Rates of C and N in Zoige Alpine Peatland in the Tibetan Plateau C. Li et al. 10.3390/w10050576
- Peatland warming strongly increases fine-root growth A. Malhotra et al. 10.1073/pnas.2003361117
- Minnesota peat viromes reveal terrestrial and aquatic niche partitioning for local and global viral populations A. ter Horst et al. 10.1186/s40168-021-01156-0
- Carbon and nitrogen accumulation rates in ombrotrophic peatlands of central and northern Alberta, Canada, during the last millennium S. van Bellen et al. 10.1007/s10533-020-00724-0
- Microbial abundances and carbon use under ambient temperature or experimental warming in a southern boreal peatland M. Felice et al. 10.1007/s10533-024-01129-z
- Plant and Soil Nitrogen in an Ombrotrophic Peatland, Southern Canada T. Moore & J. Bubier 10.1007/s10021-019-00390-w
- Depth trends of δ13C and δ15N values in peatlands in aeolian environments of Iceland S. Möckel et al. 10.1007/s13157-024-01796-6
- Atmospheric nitrogen enrichment changes nutrient stoichiometry and reduces fungal N supply to peatland ericoid mycorrhizal shrubs R. Vesala et al. 10.1016/j.scitotenv.2021.148737
- Biochemical components of Sphagnum and persistence in peat soil G. Pipes & J. Yavitt 10.1139/cjss-2021-0137
- Different leaf carbon, nitrogen, and phosphorus stoichiometry and carbon and nitrogen isotopes among peatland plants in northeastern China C. Chen et al. 10.1007/s11104-021-05085-7
- Local Spatial Heterogeneity of Holocene Carbon Accumulation throughout the Peat Profile of an Ombrotrophic Northern Minnesota Bog K. McFarlane et al. 10.1017/RDC.2018.37
- δ15N systematics in two minerotrophic peatlands in the eastern U.S.: Insights into nitrogen cycling under moderate pollution M. Novak et al. 10.1016/j.gecco.2019.e00571
- Effects of peat decomposition on δ13C and δ15N depth profiles of Alpine bogs S. Drollinger et al. 10.1016/j.catena.2019.02.027
- Climate warming and elevated CO2 alter peatland soil carbon sources and stability N. Ofiti et al. 10.1038/s41467-023-43410-z
- Switch of fungal to bacterial degradation in natural, drained and rewetted oligotrophic peatlands reflected in <i>δ</i><sup>15</sup>N and fatty acid composition M. Groß-Schmölders et al. 10.5194/soil-6-299-2020
- Effects of long-term nitrogen addition on the δ15N and δ13C of Larix gmelinii and soil in a boreal forest G. Liu et al. 10.1186/s13717-022-00382-0
30 citations as recorded by crossref.
- Stable carbon isotopic composition of peat columns, subsoil and vegetation on natural and forestry-drained boreal peatlands H. Nykänen et al. 10.1080/10256016.2018.1523158
- Soil Microbiomes Under Climate Change and Implications for Carbon Cycling D. Naylor et al. 10.1146/annurev-environ-012320-082720
- Plant communities control long term carbon accumulation and biogeochemical gradients in a Patagonian bog P. Mathijssen et al. 10.1016/j.scitotenv.2019.05.310
- Climate drivers alter nitrogen availability in surface peat and decouple N2 fixation from CH4 oxidation in the Sphagnum moss microbiome C. Petro et al. 10.1111/gcb.16651
- Rewetting and Drainage of Nutrient-Poor Peatlands Indicated by Specific Bacterial Membrane Fatty Acids and a Repeated Sampling of Stable Isotopes (δ15N, δ13C) M. Groß-Schmölders et al. 10.3389/fenvs.2021.730106
- Temporal and Spatial Variation in Peatland Carbon Cycling and Implications for Interpreting Responses of an Ecosystem‐Scale Warming Experiment N. Griffiths et al. 10.2136/sssaj2016.12.0422
- Isotope composition of dissolved organic carbon in runoff and peat leachates from a Central European wetland: Temporal and spatial variability in DOC sources M. Novak et al. 10.1016/j.catena.2018.10.011
- Stable isotopes (δ13C, δ15N) and biomarkers as indicators of the hydrological regime of fens in a European east–west transect M. Groß-Schmölders et al. 10.1016/j.scitotenv.2022.156603
- Research challenges and opportunities for using big data in global change biology J. Xia et al. 10.1111/gcb.15317
- Distinctions in heterotrophic and autotrophic-based metabolism as recorded in the hydrogen and carbon isotope ratios of normal alkanes B. Tipple & J. Ehleringer 10.1007/s00442-018-4189-0
- Natural abundance of 13C and 15N provides evidence for plant–soil carbon and nitrogen dynamics in a N‐fertilized meadow R. Wang et al. 10.1002/ecy.3348
- Plant succession and geochemical indices in immature peatlands in the Changbai Mountains, northeastern region of China: Implications for climate change and peatland development L. Zhang et al. 10.1016/j.scitotenv.2020.143776
- Divergent biotic and abiotic filtering of root endosphere and rhizosphere soil fungal communities along ecological gradients C. Lumibao et al. 10.1093/femsec/fiaa124
- Can plant or lichen natural abundance 15N ratios indicate the influence of oil sands N emissions on bogs? R. Wieder et al. 10.1016/j.ejrh.2022.101030
- Water Table Drawdown Alters Soil and Microbial Carbon Pool Size and Isotope Composition in Coastal Freshwater Forested Wetlands K. Minick et al. 10.3389/ffgc.2019.00007
- Draining Effects on Recent Accumulation Rates of C and N in Zoige Alpine Peatland in the Tibetan Plateau C. Li et al. 10.3390/w10050576
- Peatland warming strongly increases fine-root growth A. Malhotra et al. 10.1073/pnas.2003361117
- Minnesota peat viromes reveal terrestrial and aquatic niche partitioning for local and global viral populations A. ter Horst et al. 10.1186/s40168-021-01156-0
- Carbon and nitrogen accumulation rates in ombrotrophic peatlands of central and northern Alberta, Canada, during the last millennium S. van Bellen et al. 10.1007/s10533-020-00724-0
- Microbial abundances and carbon use under ambient temperature or experimental warming in a southern boreal peatland M. Felice et al. 10.1007/s10533-024-01129-z
- Plant and Soil Nitrogen in an Ombrotrophic Peatland, Southern Canada T. Moore & J. Bubier 10.1007/s10021-019-00390-w
- Depth trends of δ13C and δ15N values in peatlands in aeolian environments of Iceland S. Möckel et al. 10.1007/s13157-024-01796-6
- Atmospheric nitrogen enrichment changes nutrient stoichiometry and reduces fungal N supply to peatland ericoid mycorrhizal shrubs R. Vesala et al. 10.1016/j.scitotenv.2021.148737
- Biochemical components of Sphagnum and persistence in peat soil G. Pipes & J. Yavitt 10.1139/cjss-2021-0137
- Different leaf carbon, nitrogen, and phosphorus stoichiometry and carbon and nitrogen isotopes among peatland plants in northeastern China C. Chen et al. 10.1007/s11104-021-05085-7
- Local Spatial Heterogeneity of Holocene Carbon Accumulation throughout the Peat Profile of an Ombrotrophic Northern Minnesota Bog K. McFarlane et al. 10.1017/RDC.2018.37
- δ15N systematics in two minerotrophic peatlands in the eastern U.S.: Insights into nitrogen cycling under moderate pollution M. Novak et al. 10.1016/j.gecco.2019.e00571
- Effects of peat decomposition on δ13C and δ15N depth profiles of Alpine bogs S. Drollinger et al. 10.1016/j.catena.2019.02.027
- Climate warming and elevated CO2 alter peatland soil carbon sources and stability N. Ofiti et al. 10.1038/s41467-023-43410-z
- Switch of fungal to bacterial degradation in natural, drained and rewetted oligotrophic peatlands reflected in <i>δ</i><sup>15</sup>N and fatty acid composition M. Groß-Schmölders et al. 10.5194/soil-6-299-2020
1 citations as recorded by crossref.
Latest update: 25 Apr 2024
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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