Methane dynamics regulated by microbial community response to permafrost thaw
Abstract
Permafrost contains about 50% of the global soil carbon. It is thought that the thawing of permafrost can lead to a loss of soil carbon in the form of methane and carbon dioxide emissions. The magnitude of the resulting positive climate feedback of such greenhouse gas emissions is still unknown and may to a large extent depend on the poorly understood role of microbial community composition in regulating the metabolic processes that drive such ecosystem-scale greenhouse gas fluxes. Here we show that changes in vegetation and increasing methane emissions with permafrost thaw are associated with a switch from hydrogenotrophic to partly acetoclastic methanogenesis, resulting in a large shift in the δ13C signature (10–15‰) of emitted methane. We used a natural landscape gradient of permafrost thaw in northern Sweden as a model to investigate the role of microbial communities in regulating methane cycling, and to test whether a knowledge of community dynamics could improve predictions of carbon emissions under loss of permafrost. Abundance of the methanogen Candidatus ‘Methanoflorens stordalenmirensis’ is a key predictor of the shifts in methane isotopes, which in turn predicts the proportions of carbon emitted as methane and as carbon dioxide, an important factor for simulating the climatemore »
- Authors:
-
- Univ. of Arizona, Tucson, AZ (United States)
- Univ. of Queensland, Brisbane, QLD (Australia)
- Florida State Univ., Tallahassee, FL (United States)
- Stockholm Univ. (Sweden)
- Publication Date:
- Research Org.:
- Univ. of Arizona, Tucson, AZ (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- OSTI Identifier:
- 1776499
- Grant/Contract Number:
- SC0004632
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Nature (London)
- Additional Journal Information:
- Journal Name: Nature (London); Journal Volume: 514; Journal Issue: 7523; Journal ID: ISSN 0028-0836
- Publisher:
- Nature Publishing Group
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Biogeochemistry; Microbial ecology; Stable isotope analysis
Citation Formats
McCalley, Carmody K., Woodcroft, Ben J., Hodgkins, Suzanne B., Wehr, Richard A., Kim, Eun-Hae, Mondav, Rhiannon, Crill, Patrick M., Chanton, Jeffrey P., Rich, Virginia I., Tyson, Gene W., and Saleska, Scott R. Methane dynamics regulated by microbial community response to permafrost thaw. United States: N. p., 2014.
Web. doi:10.1038/nature13798.
McCalley, Carmody K., Woodcroft, Ben J., Hodgkins, Suzanne B., Wehr, Richard A., Kim, Eun-Hae, Mondav, Rhiannon, Crill, Patrick M., Chanton, Jeffrey P., Rich, Virginia I., Tyson, Gene W., & Saleska, Scott R. Methane dynamics regulated by microbial community response to permafrost thaw. United States. https://doi.org/10.1038/nature13798
McCalley, Carmody K., Woodcroft, Ben J., Hodgkins, Suzanne B., Wehr, Richard A., Kim, Eun-Hae, Mondav, Rhiannon, Crill, Patrick M., Chanton, Jeffrey P., Rich, Virginia I., Tyson, Gene W., and Saleska, Scott R. Wed .
"Methane dynamics regulated by microbial community response to permafrost thaw". United States. https://doi.org/10.1038/nature13798. https://www.osti.gov/servlets/purl/1776499.
@article{osti_1776499,
title = {Methane dynamics regulated by microbial community response to permafrost thaw},
author = {McCalley, Carmody K. and Woodcroft, Ben J. and Hodgkins, Suzanne B. and Wehr, Richard A. and Kim, Eun-Hae and Mondav, Rhiannon and Crill, Patrick M. and Chanton, Jeffrey P. and Rich, Virginia I. and Tyson, Gene W. and Saleska, Scott R.},
abstractNote = {Permafrost contains about 50% of the global soil carbon. It is thought that the thawing of permafrost can lead to a loss of soil carbon in the form of methane and carbon dioxide emissions. The magnitude of the resulting positive climate feedback of such greenhouse gas emissions is still unknown and may to a large extent depend on the poorly understood role of microbial community composition in regulating the metabolic processes that drive such ecosystem-scale greenhouse gas fluxes. Here we show that changes in vegetation and increasing methane emissions with permafrost thaw are associated with a switch from hydrogenotrophic to partly acetoclastic methanogenesis, resulting in a large shift in the δ13C signature (10–15‰) of emitted methane. We used a natural landscape gradient of permafrost thaw in northern Sweden as a model to investigate the role of microbial communities in regulating methane cycling, and to test whether a knowledge of community dynamics could improve predictions of carbon emissions under loss of permafrost. Abundance of the methanogen Candidatus ‘Methanoflorens stordalenmirensis’ is a key predictor of the shifts in methane isotopes, which in turn predicts the proportions of carbon emitted as methane and as carbon dioxide, an important factor for simulating the climate feedback associated with permafrost thaw in global models. By showing that the abundance of key microbial lineages can be used to predict atmospherically relevant patterns in methane isotopes and the proportion of carbon metabolized to methane during permafrost thaw, we establish a basis for scaling changing microbial communities to ecosystem isotope dynamics. Here, our findings indicate that microbial ecology may be important in ecosystem-scale responses to global change.},
doi = {10.1038/nature13798},
journal = {Nature (London)},
number = 7523,
volume = 514,
place = {United States},
year = {Wed Oct 22 00:00:00 EDT 2014},
month = {Wed Oct 22 00:00:00 EDT 2014}
}
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