skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Lower soil moisture and deep soil temperatures in thermokarst features increase old soil carbon loss after 10 years of experimental permafrost warming

Journal Article · · Global Change Biology
DOI:https://doi.org/10.1111/gcb.15481· OSTI ID:1834570

Abstract Almost half of the global terrestrial soil carbon (C) is stored in the northern circumpolar permafrost region, where air temperatures are increasing two times faster than the global average. As climate warms, permafrost thaws and soil organic matter becomes vulnerable to greater microbial decomposition. Long‐term soil warming of ice‐rich permafrost can result in thermokarst formation that creates variability in environmental conditions. Consequently, plant and microbial proportional contributions to ecosystem respiration may change in response to long‐term soil warming. Natural abundance δ 13 C and Δ 14 C of aboveground and belowground plant material, and of young and old soil respiration were used to inform a mixing model to partition the contribution of each source to ecosystem respiration fluxes. We employed a hierarchical Bayesian approach that incorporated gross primary productivity and environmental drivers to constrain source contributions. We found that long‐term experimental permafrost warming introduced a soil hydrology component that interacted with temperature to affect old soil C respiration. Old soil C loss was suppressed in plots with warmer deep soil temperatures because they tended to be wetter. When soil volumetric water content significantly decreased in 2018 relative to 2016 and 2017, the dominant respiration sources shifted from plant aboveground and young soil respiration to old soil respiration. The proportion of ecosystem respiration from old soil C accounted for up to 39% of ecosystem respiration and represented a 30‐fold increase compared to the wet‐year average. Our findings show that thermokarst formation may act to moderate microbial decomposition of old soil C when soil is highly saturated. However, when soil moisture decreases, a higher proportion of old soil C is vulnerable to decomposition and can become a large flux to the atmosphere. As permafrost systems continue to change with climate, we must understand the thresholds that may propel these systems from a C sink to a source.

Research Organization:
Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
Grant/Contract Number:
AC02-05CH11231; DE‐SC0006982; DE‐SC0014085
OSTI ID:
1834570
Alternate ID(s):
OSTI ID: 1804921
Journal Information:
Global Change Biology, Vol. 27, Issue 6; ISSN 1354-1013
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English

References (77)

Thermal Properties of Soils as affected by Density and Water Content journal September 2003
Temperature sensitivity of organic matter decomposition of permafrost-region soils during laboratory incubations journal June 2016
Vulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon Cycle journal September 2008
Plant species traits are the predominant control on litter decomposition rates within biomes worldwide journal October 2008
Advances in Thermokarst Research: Recent Advances in Research Investigating Thermokarst Processes journal April 2013
Inference from Iterative Simulation Using Multiple Sequences journal November 1992
The concentration and isotopic abundances of carbon dioxide in rural and marine air journal July 1961
Ecological Response to Permafrost Thaw and Consequences for Local and Global Ecosystem Services journal November 2018
Climate change and the permafrost carbon feedback journal April 2015
Beyond simple linear mixing models: process-based isotope partitioning of ecological processes journal January 2014
Decomposition of old organic matter as a result of deeper active layers in a snow depth manipulation experiment journal January 2010
Adding Depth to Our Understanding of Nitrogen Dynamics in Permafrost Soils journal August 2018
Dependence of the evolution of carbon dynamics in the northern permafrost region on the trajectory of climate change journal March 2018
Diurnal cycle of carbon isotope ratio in soil CO2 in various ecosystems journal January 1996
CLIMATE CHANGE: Permafrost and the Global Carbon Budget journal June 2006
Soil Thermal Conductivity journal January 2000
Divergent patterns of experimental and model-derived permafrost ecosystem carbon dynamics in response to Arctic warming journal October 2018
Experimental Warming Alters Productivity and Isotopic Signatures of Tundra Mosses journal May 2015
Permafrost Degradation and Ecological Changes Associated with a WarmingClimate in Central Alaska journal March 2001
Physical and ecological changes associated with warming permafrost and thermokarst in Interior Alaska journal July 2009
The amount and timing of precipitation control the magnitude, seasonality and sources ( 14 C) of ecosystem respiration in a polar semi-desert, northwestern Greenland journal January 2014
The Effects of Permafrost Thaw on Soil Hydrologic, Thermal, and Carbon Dynamics in an Alaskan Peatland journal November 2011
Holocene Carbon Stocks and Carbon Accumulation Rates Altered in Soils Undergoing Permafrost Thaw journal November 2011
Nitrogen availability increases in a tundra ecosystem during five years of experimental permafrost thaw journal February 2016
Drainage enhances modern soil carbon contribution but reduces old soil carbon contribution to ecosystem respiration in tundra ecosystems journal February 2019
R2WinBUGS : A Package for Running WinBUGS from R journal January 2005
Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire: an expert assessment journal March 2016
Permafrost thaw and resulting soil moisture changes regulate projected high-latitude CO 2 and CH 4 emissions journal September 2015
High Arctic wetting reduces permafrost carbon feedbacks to climate warming journal December 2013
The concentration and isotopic abundances of atmospheric carbon dioxide in rural areas journal January 1958
The BUGS project: Evolution, critique and future directions journal July 2009
Carbon Isotopic Fractionation Does Not Occur during Dark Respiration in C3 and C4 Plants journal May 1997
Isotope partitioning of soil respiration: A Bayesian solution to accommodate multiple sources of variability: Bayesian isotope partitioning of fluxes journal February 2015
Permafrost thaw and soil moisture driving CO 2 and CH 4 release from upland tundra journal March 2015
Carbon isotopes in terrestrial ecosystem pools and CO 2 fluxes journal April 2008
The effect of permafrost thaw on old carbon release and net carbon exchange from tundra journal May 2009
Fitting Linear Mixed-Effects Models Using lme4 journal January 2015
Direct observation of permafrost degradation and rapid soil carbon loss in tundra journal July 2019
Carbon Dioxide Capture Using a Zeolite Molecular Sieve Sampling System for Isotopic Studies ( 13 C and 14 C) of Respiration journal January 2005
Air permeability and trapped-air content in two soils journal September 1989
Using Stable Carbon Isotopes of Seasonal Ecosystem Respiration to Determine Permafrost Carbon Loss journal January 2019
Estimated stocks of circumpolar permafrost carbon with quantified uncertainty ranges and identified data gaps journal January 2014
sjmisc: Data and Variable Transformation Functions journal June 2018
Permafrost collapse after shrub removal shifts tundra ecosystem to a methane source journal November 2014
Isotopic composition of carbon dioxide from a boreal forest fire: Inferring carbon loss from measurements and modeling: ISOTOPIC COMPOSITION OF CARBON DIOXIDE FROM A BOREAL FOREST FIRE journal January 2003
Effects of experimental warming of air, soil and permafrost on carbon balance in Alaskan tundra: WARMING OF ALASKAN TUNDRA journal February 2011
Carbon Thaw Rate Doubles When Accounting for Subsidence in a Permafrost Warming Experiment journal June 2020
Carbon respired by terrestrial ecosystems - recent progress and challenges journal February 2006
Age of soil Organic Matter and soil Respiration: Radiocarbon Constraints on Belowground c Dynamics journal April 2000
Increasing rates of retrogressive thaw slump activity in the Mackenzie Delta region, N.W.T., Canada journal January 2008
TUNDRA CO 2 FLUXES IN RESPONSE TO EXPERIMENTAL WARMING ACROSS LATITUDINAL AND MOISTURE GRADIENTS journal May 2007
Factors Limiting Seasonal Growth and Peak Biomass Accumulation in Eriophorum Vaginatum in Alaskan Tussock Tundra journal March 1986
Radiocarbon Content of CO 2 Respired from High Arctic Tundra in Northwest Greenland journal August 2010
Plant Species Composition and Productivity following Permafrost Thaw and Thermokarst in Alaskan Tundra journal March 2007
A global relationship between the heterotrophic and autotrophic components of soil respiration? journal October 2004
THE RESPONSE OF TUNDRA PLANT BIOMASS, ABOVEGROUND PRODUCTION, NITROGEN, AND CO 2 FLUX TO EXPERIMENTAL WARMING journal July 1998
Long-term drainage reduces CO 2 uptake and increases CO 2 emission on a Siberian floodplain due to shifts in vegetation community and soil thermal characteristics journal January 2016
Evidence for warming and thawing of discontinuous permafrost in Alaska journal January 1999
Nonlinear CO 2 flux response to 7 years of experimentally induced permafrost thaw journal March 2017
14 C Background Levels in An Accelerator Mass Spectrometry System journal January 1987
Reconciling Carbon-cycle Concepts, Terminology, and Methods journal November 2006
Old soil carbon losses increase with ecosystem respiration in experimentally thawed tundra journal October 2015
Thawing permafrost increases old soil and autotrophic respiration in tundra: Partitioning ecosystem respiration using δ 13 C and ∆ 14 C journal November 2012
Thaw pond development and initial vegetation succession in experimental plots at a Siberian lowland tundra site journal August 2017
Respiration of aged soil carbon during fall in permafrost peatlands enhanced by active layer deepening following wildfire but limited following thermokarst journal August 2018
Bayesian measures of model complexity and fit
  • Spiegelhalter, David J.; Best, Nicola G.; Carlin, Bradley P.
  • Journal of the Royal Statistical Society: Series B (Statistical Methodology), Vol. 64, Issue 4 https://doi.org/10.1111/1467-9868.00353
journal October 2002
Responses of soil heterotrophic respiration to moisture availability: An exploration of processes and models journal April 2013
Feedback and Modularization in a Bayesian Meta–analysis of Tree Traits Affecting Forest Dynamics journal March 2013
Recovery of submilligram quantities of carbon dioxide from gas streams by molecular sieve for subsequent determination of isotopic carbon-13 and carbon-14 natural abundances journal April 1992
Increased plant productivity in Alaskan tundra as a result of experimental warming of soil and permafrost: Increased plant productivity in Alaskan tundra journal November 2011
Discussion Reporting of 14 C Data journal January 1977
Partitioning sources of soil respiration in boreal black spruce forest using radiocarbon journal February 2006
Radiocarbon Nomenclature, Theory, Models, and Interpretation: Measuring Age, Determining Cycling Rates, and Tracing Source Pools book January 2016
The effects of water table manipulation and elevated temperature on the net CO 2 flux of wet sedge tundra ecosystems journal January 1998
Carbon respiration from subsurface peat accelerated by climate warming in the subarctic journal July 2009
Soil moisture-temperature relationships: results from two field experiments journal January 2003
Soil organic carbon pools in the northern circumpolar permafrost region: SOIL ORGANIC CARBON POOLS journal June 2009