Abstract
Tree stems from wetland, floodplain and upland forests can produce and emit methane (CH 4 ). Tree CH 4 stem emissions have high spatial and temporal variability, but there is no consensus on the biophysical mechanisms that drive stem CH 4 production and emissions. Here, we summarize up to 30 opportunities and challenges for stem CH 4 emissions research, which, when addressed, will improve estimates of the magnitudes, patterns and drivers of CH 4 emissions and trace their potential origin. We identified the need: (1) for both long-term, high-frequency measurements of stem CH 4 emissions to understand the fine-scale processes, alongside rapid large-scale measurements designed to understand the variability across individuals, species and ecosystems; (2) to identify microorganisms and biogeochemical pathways associated with CH 4 production; and (3) to develop a mechanistic model including passive and active transport of CH 4 from the soil–tree–atmosphere continuum. Addressing these challenges will help to constrain the magnitudes and patterns of CH 4 emissions, and allow for the integration of pathways and mechanisms of CH 4 production and emissions into process-based models. These advances will facilitate the upscaling of stem CH 4 emissions to the ecosystem level and quantify the role of stem CH 4 emissions for the local to global CH 4 budget.
Original language | English |
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Pages (from-to) | 18-28 |
Number of pages | 11 |
Journal | New Phytologist |
Volume | 222 |
Issue number | 1 |
DOIs | |
State | Published - Apr 2019 |
Funding
We acknowledge the feedback and comments from Zhi-Ping Wang while developing the manuscript and the insights from two anonymous reviewers. We also acknowledge support from Oak Spring Garden Foundation. RV acknowledges support from the National Science Foundation (grant 1652594). ZZ and BP acknowledge support from the Gordon and Betty Moore Foundation (grant GBMF5439). CWS acknowledges support from the US Department of Energy, Office of Science, Biological and Environmental Sciences Office. JvH acknowledges support from the National Science Foundation (grants 1355066 and 1442152). MP thanks the Academy of Finland Research Fellow project (288494) and the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (grant agreement no. 757695). AR-U acknowledges Pacific Northwest National Laboratory (PNNL), operated for the DOE by Battelle Memorial Institute under contract DE-AC06-76RL0. We acknowledge the feedback and comments from Zhi-Ping Wang while developing the manuscript and the insights from two anonymous reviewers. We also acknowledge support from Oak Spring Garden Foundation. RV acknowledges support from the National Science Foundation (grant 1652594). ZZ and BP acknowledge support from the Gordon and Betty Moore Foundation (grant GBMF5439). CWS acknowledges support from the US Department of Energy, Office of Science, Biological and Environmental Sciences Office. JvH acknowledges support from the National Science Foundation (grants 1355066 and 1442152). MP thanks the Academy of Finland Research Fellow project (288494) and the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement no. 757695). AR-U acknowledges Pacific Northwest National Laboratory (PNNL), operated for the DOE by Battelle Memorial Institute under contract DE-AC06-76RL0.
Keywords
- CH transport
- methane emissions
- methanogenesis
- spatial variability
- temporal variability
- tree stems
- upland forests
- wetland forests