Articles | Volume 14, issue 6
https://doi.org/10.5194/bg-14-1593-2017
© 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-14-1593-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
28 Mar 2017
Research article |
| 28 Mar 2017
Estimating global nitrous oxide emissions by lichens and bryophytes with a process-based productivity model
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, 10691 Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Ulrich Pöschl
Max Planck Institute for Chemistry, P.O. Box 3060, 55020 Mainz, Germany
Axel Kleidon
Max Planck Institute for Biogeochemistry, P.O. Box 10 01 64, 07701 Jena, Germany
Christian Beer
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, 10691 Stockholm, Sweden
Bolin Centre for Climate Research, Stockholm University, 10691 Stockholm, Sweden
Bettina Weber
Max Planck Institute for Chemistry, P.O. Box 3060, 55020 Mainz, Germany
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- Canopy structure affects temperature distributions and free convection in moss shoot systems S. Rice et al. 10.1002/ajb2.1145
- Environmental effects of ozone depletion, UV radiation and interactions with climate change: UNEP Environmental Effects Assessment Panel, update 2017 A. Bais et al. 10.1039/c7pp90043k
- Hydration status and diurnal trophic interactions shape microbial community function in desert biocrusts M. Kim & D. Or 10.5194/bg-14-5403-2017
- Utilization of deep learning tools to map and monitor biological soil crusts S. Herdy et al. 10.1016/j.ecoinf.2023.102417
- Global NO and HONO emissions of biological soil crusts estimated by a process-based non-vascular vegetation model P. Porada et al. 10.5194/bg-16-2003-2019
- Effect of climate and moss vegetation on ground surface temperature and the active layer among different biogeographical regions in Antarctica F. Hrbáček et al. 10.1016/j.catena.2020.104562
- Effects of short-term variability of meteorological variables on soil temperature in permafrost regions C. Beer et al. 10.5194/tc-12-741-2018
- Effects of climate change and land use intensification on regional biological soil crust cover and composition in southern Africa E. Rodríguez-Caballero et al. 10.1016/j.geoderma.2021.115508
- Cryptogamic organisms are a substantial source and sink for volatile organic compounds in the Amazon region A. Edtbauer et al. 10.1038/s43247-021-00328-y
- Changes in fluxes of carbon dioxide and methane caused by fire in Siberian boreal forest with continuous permafrost E. Köster et al. 10.1016/j.jenvman.2018.09.051
- Bryophytes impact the fluxes of soil non-carbon dioxide greenhouse gases in a subalpine coniferous forest A. Li et al. 10.1007/s00374-020-01483-8
- Lachgasbildung durch Mikroalgen J. Sander 10.1002/biuz.202070206
- How do forest fires affect soil greenhouse gas emissions in upland boreal forests? A review C. Ribeiro-Kumara et al. 10.1016/j.envres.2020.109328
- Significant contribution of non-vascular vegetation to global rainfall interception P. Porada et al. 10.1038/s41561-018-0176-7
- Contrasting effects of reindeer grazing on CO2, CH4, and N2O fluxes originating from the northern boreal forest floor K. Köster et al. 10.1002/ldr.2868
- Bark Water Storage Plays Key Role for Growth of Mediterranean Epiphytic Lichens P. Porada & P. Giordani 10.3389/ffgc.2021.668682
22 citations as recorded by crossref.
- Desiccation and rehydration of mosses greatly increases resource fluxes that alter soil carbon and nitrogen cycling M. Slate et al. 10.1111/1365-2745.13162
- When time is not of the essence: constraints to the carbon balance of bryophytes A. Perera-Castro et al. 10.1093/jxb/erac104
- Ecophysiological properties of three biological soil crust types and their photoautotrophs from the Succulent Karoo, South Africa A. Tamm et al. 10.1007/s11104-018-3635-4
- N<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N<sub>2</sub>O emissions and carbon–nitrogen cycle interactions F. Joos et al. 10.5194/bg-17-3511-2020
- The Ecology of Subaerial Biofilms in Dry and Inhospitable Terrestrial Environments F. Villa & F. Cappitelli 10.3390/microorganisms7100380
- Towards a Systems Biology Approach to Understanding the Lichen Symbiosis: Opportunities and Challenges of Implementing Network Modelling H. Nazem-Bokaee et al. 10.3389/fmicb.2021.667864
- Dryland photoautotrophic soil surface communities endangered by global change E. Rodriguez-Caballero et al. 10.1038/s41561-018-0072-1
- Canopy structure affects temperature distributions and free convection in moss shoot systems S. Rice et al. 10.1002/ajb2.1145
- Environmental effects of ozone depletion, UV radiation and interactions with climate change: UNEP Environmental Effects Assessment Panel, update 2017 A. Bais et al. 10.1039/c7pp90043k
- Hydration status and diurnal trophic interactions shape microbial community function in desert biocrusts M. Kim & D. Or 10.5194/bg-14-5403-2017
- Utilization of deep learning tools to map and monitor biological soil crusts S. Herdy et al. 10.1016/j.ecoinf.2023.102417
- Global NO and HONO emissions of biological soil crusts estimated by a process-based non-vascular vegetation model P. Porada et al. 10.5194/bg-16-2003-2019
- Effect of climate and moss vegetation on ground surface temperature and the active layer among different biogeographical regions in Antarctica F. Hrbáček et al. 10.1016/j.catena.2020.104562
- Effects of short-term variability of meteorological variables on soil temperature in permafrost regions C. Beer et al. 10.5194/tc-12-741-2018
- Effects of climate change and land use intensification on regional biological soil crust cover and composition in southern Africa E. Rodríguez-Caballero et al. 10.1016/j.geoderma.2021.115508
- Cryptogamic organisms are a substantial source and sink for volatile organic compounds in the Amazon region A. Edtbauer et al. 10.1038/s43247-021-00328-y
- Changes in fluxes of carbon dioxide and methane caused by fire in Siberian boreal forest with continuous permafrost E. Köster et al. 10.1016/j.jenvman.2018.09.051
- Bryophytes impact the fluxes of soil non-carbon dioxide greenhouse gases in a subalpine coniferous forest A. Li et al. 10.1007/s00374-020-01483-8
- Lachgasbildung durch Mikroalgen J. Sander 10.1002/biuz.202070206
- How do forest fires affect soil greenhouse gas emissions in upland boreal forests? A review C. Ribeiro-Kumara et al. 10.1016/j.envres.2020.109328
- Significant contribution of non-vascular vegetation to global rainfall interception P. Porada et al. 10.1038/s41561-018-0176-7
- Contrasting effects of reindeer grazing on CO2, CH4, and N2O fluxes originating from the northern boreal forest floor K. Köster et al. 10.1002/ldr.2868
1 citations as recorded by crossref.
Latest update: 19 Apr 2024
Short summary
Lichens and bryophytes have been shown to release nitrous oxide, which is a strong greenhouse gas and atmospheric ozone-depleting agent. Here we apply a process-based computer model of lichens and bryophytes at the global scale, to estimate growth and respiration of the organisms. By relating respiration to nitrous oxide release, we simulate global nitrous oxide emissions of 0.27 (0.19–0.35) Tg yr−1. Moreover, we quantify different sources of uncertainty in nitrous oxide emission rates.
Lichens and bryophytes have been shown to release nitrous oxide, which is a strong greenhouse...
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