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Title: 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 » 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.« less

Authors:
 [1];  [2];  [3];  [1];  [1];  [2];  [4];  [3];  [1];  [2];  [1]
  1. Univ. of Arizona, Tucson, AZ (United States)
  2. Univ. of Queensland, Brisbane, QLD (Australia)
  3. Florida State Univ., Tallahassee, FL (United States)
  4. 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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First evidence for cold-adapted anaerobic oxidation of methane in deep sediments of thermokarst lakes
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Host-linked soil viral ecology along a permafrost thaw gradient
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Genome-centric view of carbon processing in thawing permafrost
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Variation in Soil Methane Fluxes and Comparison between Two Forests in China
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Distinct microbial communities in the active and permafrost layers on the Tibetan Plateau
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Ecosystem carbon response of an Arctic peatland to simulated permafrost thaw
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Winter precipitation and snow accumulation drive the methane sink or source strength of Arctic tussock tundra
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Multi-omics of permafrost, active layer and thermokarst bog soil microbiomes
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The global methane budget 2000--2012
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Effect of permafrost thaw on plant and soil fungal community in a boreal forest: Does fungal community change mediate plant productivity response?
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Linking microbial communities to ecosystem functions: what we can learn from genotype–phenotype mapping in organisms
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Redox and temperature-sensitive changes in microbial communities and soil chemistry dictate greenhouse gas loss from thawed permafrost
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Molecular mechanisms of water table lowering and nitrogen deposition in affecting greenhouse gas emissions from a Tibetan alpine wetland
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Responses of tundra soil microbial communities to half a decade of experimental warming at two critical depths
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Incorporation of Microbial Functional Traits in Biogeochemistry Models Provides Better Estimations of Benthic Denitrification and Anammox Rates in Coastal Oceans
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Multi-year effect of wetting on CH4 flux at taiga–tundra boundary in northeastern Siberia deduced from stable isotope ratios of CH4
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Emissions of methane from northern peatlands: a review of management impacts and implications for future management options
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Co-cultivation of the strictly anaerobic methanogen Methanosarcina barkeri with aerobic methanotrophs in an oxygen-limited membrane bioreactor
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Diversity and abundance of microbial eukaryotes in stream sediments from Svalbard
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Methanotrophy across a natural permafrost thaw environment
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Landscape topography structures the soil microbiome in arctic polygonal tundra
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Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance
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Host-linked soil viral ecology along a permafrost thaw gradient
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Chemical Structure of the Lipid A component of Pseudomonas sp. strain PAMC 28618 from Thawing Permafrost in Relation to Pathogenicity
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Key evidence of the role of desertification in protecting the underlying permafrost in the Qinghai–Tibet Plateau
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Bridging the divide: a model-data approach to Polar & Alpine Microbiology
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Increases in temperature and nutrient availability positively affect methane‐cycling microorganisms in Arctic thermokarst lake sediments
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Metagenomics Reveals Pervasive Bacterial Populations and Reduced Community Diversity across the Alaska Tundra Ecosystem
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Implication of Viral Infections for Greenhouse Gas Dynamics in Freshwater Wetlands: Challenges and Perspectives
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Biotic and Environmental Drivers of Plant Microbiomes Across a Permafrost Thaw Gradient
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Toxic Algae Silence Physiological Responses to Multiple Climate Drivers in a Tropical Marine Food Chain
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Reviews and syntheses: Four decades of modeling methane cycling in terrestrial ecosystems
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Methane dynamics in the subarctic tundra: combining stable isotope analyses, plot- and ecosystem-scale flux measurements
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The ratio of methanogens to methanotrophs and water-level dynamics drive methane transfer velocity in a temperate kettle-hole peat bog
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Climate warming over the past half century has led to thermal degradation of permafrost on the Qinghai–Tibet Plateau
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