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Title: Changes in peat chemistry associated with permafrost thaw increase greenhouse gas production

Journal Article · · Proceedings of the National Academy of Sciences of the United States of America
 [1];  [1];  [2];  [3];  [4];  [2];  [2];  [1]
  1. Florida State Univ., Tallahassee, FL (United States)
  2. Univ. of Arizona, Tucson, AZ (United States)
  3. Swedish Polar Research Secretariat, Abisko (Sweden). Abisko Scientific Research Station
  4. Stockholm Univ. (Sweden)

Carbon release due to permafrost thaw represents a potentially major positive climate change feedback. The magnitude of carbon loss and the proportion lost as methane (CH4) vs. carbon dioxide (CO2) depend on factors including temperature, mobilization of previously frozen carbon, hydrology, and changes in organic matter chemistry associated with environmental responses to thaw. While the first three of these effects are relatively well understood, the effect of organic matter chemistry remains largely unstudied. To address this gap, we examined the biogeochemistry of peat and dissolved organic matter (DOM) along a ~40-y permafrost thaw progression from recently- to fully thawed sites in Stordalen Mire (68.35°N, 19.05°E), a thawing peat plateau in northern Sweden. Thaw-induced subsidence and the resulting inundation along this progression led to succession in vegetation types accompanied by an evolution in organic matter chemistry. Peat C/N ratios decreased whereas humification rates increased, and DOM shifted toward lower molecular weight compounds with lower aromaticity, lower organic oxygen content, and more abundant microbially produced compounds. Corresponding changes in decomposition along this gradient included increasing CH4 and CO2 production potentials, higher relative CH4/CO2 ratios, and a shift in CH4 production pathway from CO2 reduction to acetate cleavage. These results imply that subsidence and thermokarst-associated increases in organic matter lability cause shifts in biogeochemical processes toward faster decomposition with an increasing proportion of carbon released as CH4. This impact of permafrost thaw on organic matter chemistry could intensify the predicted climate feedbacks of increasing temperatures, permafrost carbon mobilization, and hydrologic changes.

Research Organization:
Univ. of Arizona, Tucson, AZ (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
SC0004632; ER65245
OSTI ID:
1602275
Journal Information:
Proceedings of the National Academy of Sciences of the United States of America, Vol. 111, Issue 16; ISSN 0027-8424
Publisher:
National Academy of SciencesCopyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 232 works
Citation information provided by
Web of Science

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Dissolved organic matter and inorganic N jointly regulate greenhouse gases fluxes from forest soils with different moistures during a freeze-thaw period journal September 2019
Methane oxidation following submarine permafrost degradation: Measurements from a central Laptev Sea shelf borehole: METHANE IN THAWING SUBMARINE PERMAFROST journal May 2015
Vascular plant-mediated controls on atmospheric carbon assimilation and peat carbon decomposition under climate change journal April 2018
Methane emissions from Alaska in 2012 from CARVE airborne observations journal November 2014
Large carbon cycle sensitivities to climate across a permafrost thaw gradient in subarctic Sweden journal January 2019
Methane and Biogenic Volatile Organic Compound Emissions in Eastern Siberia book January 2019
Microbial Community Structure and Methane Cycling Potential along a Thermokarst Pond-Peatland Continuum journal October 2019
Reduced quantity and quality of SOM along a thaw sequence on the Tibetan Plateau journal October 2018
Peatland vascular plant functional types affect methane dynamics by altering microbial community structure journal May 2015
Persistent high temperature and low precipitation reduce peat carbon accumulation journal May 2016
Methanotrophy across a natural permafrost thaw environment journal June 2018
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Warmer temperature accelerates methane emissions from the Zoige wetland on the Tibetan Plateau without changing methanogenic community composition journal June 2015
Tropical peatland carbon storage linked to global latitudinal trends in peat recalcitrance journal September 2018
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Consortia of low-abundance bacteria drive sulfate reduction-dependent degradation of fermentation products in peat soil microcosms journal March 2016
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Organic-matter quality of deep permafrost carbon text January 2019
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Optimization of viral resuspension methods for carbon-rich soils along a permafrost thaw gradient journal January 2016
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