Articles | Volume 16, issue 2
https://doi.org/10.5194/bg-16-541-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-541-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Jan 2019
Research article |
| 31 Jan 2019
| 31 Jan 2019
Zero to moderate methane emissions in a densely rooted, pristine Patagonian bog – biogeochemical controls as revealed from isotopic evidence
Wiebke Münchberger
CORRESPONDING AUTHOR
Ecohydrology and Biogeochemistry Research Group, Institute of
Landscape Ecology, University of Münster, Heisenbergstraße 2, 48149
Münster, Germany
Biodiversity and Ecosystem Research Group, Institute of Landscape
Ecology, University of Münster, Heisenbergstraße 2, 48149 Münster,
Germany
Klaus-Holger Knorr
CORRESPONDING AUTHOR
Ecohydrology and Biogeochemistry Research Group, Institute of
Landscape Ecology, University of Münster, Heisenbergstraße 2, 48149
Münster, Germany
Christian Blodau
Ecohydrology and Biogeochemistry Research Group, Institute of
Landscape Ecology, University of Münster, Heisenbergstraße 2, 48149
Münster, Germany
deceased, July 2016
Verónica A. Pancotto
Centro Austral de Investigaciones Científicas (CADIC-CONICET), B.
Houssay 200, 9410 Ushuaia, Tierra del Fuego, Argentina
Instituto de Ciencias Polares y Ambiente (ICPA-UNTDF), Fuegia Basket,
9410 Ushuaia, Tierra del Fuego, Argentina
Till Kleinebecker
Biodiversity and Ecosystem Research Group, Institute of Landscape
Ecology, University of Münster, Heisenbergstraße 2, 48149 Münster,
Germany
Institute of Landscape Ecology and Resources Management, Justus Liebig University Giessen, Heinrich-Buff-Ring 26, 35392 Gießen, Germany
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Cited
19 citations as recorded by crossref.
- Cushion bogs are stronger carbon dioxide net sinks than moss-dominated bogs as revealed by eddy covariance measurements on Tierra del Fuego, Argentina D. Holl et al. 10.5194/bg-16-3397-2019
- Methane fluxes but not respiratory carbon dioxide fluxes altered under Si amendment during drying – rewetting cycles in fen peat mesocosms A. Hömberg et al. 10.1016/j.geoderma.2021.115338
- Limited Potential for Mineralization of Permafrost Peatland Soil Carbon Following Thermokarst: Evidence From Anoxic Incubation and Priming Experiments C. Estop‐Aragonés et al. 10.1029/2022JG006910
- Element mobility related to rock weathering and soil formation at the westward side of the southernmost Patagonian Andes B. Klaes et al. 10.1016/j.scitotenv.2022.152977
- Spatial and temporal patterns of methane emissions from mountain peatlands in the northern Andes across a disturbance gradient J. Benavides et al. 10.3389/feart.2023.1078830
- Divergent effect of silicon on greenhouse gas production from reduced and oxidized peat organic matter A. Hömberg et al. 10.1016/j.geoderma.2020.114916
- Technical note: Skirt chamber – an open dynamic method for the rapid and minimally intrusive measurement of greenhouse gas emissions from peatlands F. Thalasso et al. 10.5194/bg-20-3737-2023
- Influence of land-use change and season on soil greenhouse gas emissions from a tropical wetland: A stepwise explorative assessment R. Ondiek et al. 10.1016/j.scitotenv.2021.147701
- Control of carbon and nitrogen accumulation by vegetation in pristine bogs of southern Patagonia W. Schuster et al. 10.1016/j.scitotenv.2021.151293
- Influence of the microtopography of patagonian peatbogs on the fluxes of greenhouse gasses and dissolved carbon in porewater M. Iseas et al. 10.1016/j.ecohyd.2024.01.013
- Fine-Scale Spatial Variability of Greenhouse Gas Emissions From a Subantarctic Peatland Bog B. Riquelme del Río et al. 10.1021/acs.est.3c10746
- Plant-mediated CH4 exchange in wetlands: A review of mechanisms and measurement methods with implications for modelling M. Ge et al. 10.1016/j.scitotenv.2023.169662
- Carbon dynamics in high‐Andean tropical cushion peatlands: A review of geographic patterns and potential drivers M. García Lino et al. 10.1002/ecm.1614
- Plant mediated methane efflux from a boreal peatland complex A. Korrensalo et al. 10.1007/s11104-021-05180-9
- A 14,000 year peatland record of environmental change in the southern Gutland region, Luxembourg K. Schittek et al. 10.1177/0959683621994645
- Cushion bog plant community responses to passive warming in southern Patagonia V. Pancotto et al. 10.5194/bg-18-4817-2021
- 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
- Controlled soil monolith experiment for studying the effects of waterlogging on redox processes R. Kronberg et al. 10.1016/j.geoderma.2024.117110
- A combined microbial and biogeochemical dataset from high-latitude ecosystems with respect to methane cycle M. Barret et al. 10.1038/s41597-022-01759-8
18 citations as recorded by crossref.
- Cushion bogs are stronger carbon dioxide net sinks than moss-dominated bogs as revealed by eddy covariance measurements on Tierra del Fuego, Argentina D. Holl et al. 10.5194/bg-16-3397-2019
- Methane fluxes but not respiratory carbon dioxide fluxes altered under Si amendment during drying – rewetting cycles in fen peat mesocosms A. Hömberg et al. 10.1016/j.geoderma.2021.115338
- Limited Potential for Mineralization of Permafrost Peatland Soil Carbon Following Thermokarst: Evidence From Anoxic Incubation and Priming Experiments C. Estop‐Aragonés et al. 10.1029/2022JG006910
- Element mobility related to rock weathering and soil formation at the westward side of the southernmost Patagonian Andes B. Klaes et al. 10.1016/j.scitotenv.2022.152977
- Spatial and temporal patterns of methane emissions from mountain peatlands in the northern Andes across a disturbance gradient J. Benavides et al. 10.3389/feart.2023.1078830
- Divergent effect of silicon on greenhouse gas production from reduced and oxidized peat organic matter A. Hömberg et al. 10.1016/j.geoderma.2020.114916
- Technical note: Skirt chamber – an open dynamic method for the rapid and minimally intrusive measurement of greenhouse gas emissions from peatlands F. Thalasso et al. 10.5194/bg-20-3737-2023
- Influence of land-use change and season on soil greenhouse gas emissions from a tropical wetland: A stepwise explorative assessment R. Ondiek et al. 10.1016/j.scitotenv.2021.147701
- Control of carbon and nitrogen accumulation by vegetation in pristine bogs of southern Patagonia W. Schuster et al. 10.1016/j.scitotenv.2021.151293
- Influence of the microtopography of patagonian peatbogs on the fluxes of greenhouse gasses and dissolved carbon in porewater M. Iseas et al. 10.1016/j.ecohyd.2024.01.013
- Fine-Scale Spatial Variability of Greenhouse Gas Emissions From a Subantarctic Peatland Bog B. Riquelme del Río et al. 10.1021/acs.est.3c10746
- Plant-mediated CH4 exchange in wetlands: A review of mechanisms and measurement methods with implications for modelling M. Ge et al. 10.1016/j.scitotenv.2023.169662
- Carbon dynamics in high‐Andean tropical cushion peatlands: A review of geographic patterns and potential drivers M. García Lino et al. 10.1002/ecm.1614
- Plant mediated methane efflux from a boreal peatland complex A. Korrensalo et al. 10.1007/s11104-021-05180-9
- A 14,000 year peatland record of environmental change in the southern Gutland region, Luxembourg K. Schittek et al. 10.1177/0959683621994645
- Cushion bog plant community responses to passive warming in southern Patagonia V. Pancotto et al. 10.5194/bg-18-4817-2021
- 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
- Controlled soil monolith experiment for studying the effects of waterlogging on redox processes R. Kronberg et al. 10.1016/j.geoderma.2024.117110
Latest update: 14 Dec 2024
Short summary
Processes governing CH4 dynamics have been scarcely studied in southern hemispheric bogs. These can be dominated by cushion-forming plants with deep and dense roots suppressing emissions. Here we demonstrate how the spatial distribution of root activity drives a pronounced pattern of CH4 emissions, likewise also possible in densely rooted northern bogs. We conclude that presence of cushion vegetation as a proxy for negligible CH4 emissions from cushion bogs needs to be interpreted with caution.
Processes governing CH4 dynamics have been scarcely studied in southern hemispheric bogs. These...
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