Impacts of temperature and soil characteristics on methane production and oxidation in Arctic tundra
Rapid warming of Arctic ecosystems accelerates microbial decomposition of soil organic matter and leads to increased production of carbon dioxide (CO 2 ) and methane (CH 4 ). CH 4 oxidation potentially mitigates CH 4 emissions from permafrost regions, but it is still highly uncertain whether soils i...
| Published in: | Biogeosciences |
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| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Copernicus Publications
2018
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/bg-15-6621-2018 https://doaj.org/article/807822e9bb714a2d99f9b847bbd6ceaf |
| Summary: | Rapid warming of Arctic ecosystems accelerates microbial decomposition of soil organic matter and leads to increased production of carbon dioxide (CO 2 ) and methane (CH 4 ). CH 4 oxidation potentially mitigates CH 4 emissions from permafrost regions, but it is still highly uncertain whether soils in high-latitude ecosystems will function as a net source or sink for CH 4 in response to rising temperature and associated hydrological changes. We investigated CH 4 production and oxidation potential in permafrost-affected soils from degraded ice-wedge polygons on the Barrow Environmental Observatory, Utqiaġvik (Barrow), Alaska, USA. Frozen soil cores from flat and high-centered polygons were sectioned into organic, transitional, and permafrost layers, and incubated at −2, +4 and +8 °C to determine potential CH 4 production and oxidation rates. Significant CH 4 production was only observed from the suboxic transition layer and permafrost of flat-centered polygon soil. These two soil sections also exhibited highest CH 4 oxidation potentials. Organic soils from relatively dry surface layers had the lowest CH 4 oxidation potential compared to saturated transition layer and permafrost, contradicting our original assumptions. Low methanogenesis rates are due to low overall microbial activities measured as total anaerobic respiration and the competing iron-reduction process. Our results suggest that CH 4 oxidation could offset CH 4 production and limit surface CH 4 emissions, in response to elevated temperature, and thus must be considered in model predictions of net CH 4 fluxes in Arctic polygonal tundra. Future changes in temperature and soil saturation conditions are likely to divert electron flow to alternative electron acceptors and significantly alter CH 4 production, which should also be considered in CH 4 models. |
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