Assessing the Potential for Mobilization of Old Soil Carbon After Permafrost Thaw: A Synthesis of 14C Measurements From the Northern Permafrost Region. Issue 9 (14th September 2020)

• Record Type: Journal Article
• Authors: Estop‐Aragonés, Cristian; Olefeldt, David; Abbott, Benjamin W.; Chanton, Jeffrey P.; Czimczik, Claudia I.; Dean, Joshua F.; Egan, Jocelyn E.; Gandois, Laure; Garnett, Mark H.; Hartley, Iain P.; Hoyt, Alison; Lupascu, Massimo; Natali, Susan M.; O'Donnell, Jonathan A.; Raymond, Peter A.; Tanentzap, Andrew J.; Tank, Suzanne E.; Schuur, Edward A. G.; Turetsky, Merritt; Anthony, Katey Walter
• Is Part Of: Global biogeochemical cycles. Volume 34:Issue 9(2020:Sep.)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-09-14
• Subjects: permafrost thaw -- radiocarbon -- carbon dioxide -- methane -- dissolved organic carbon -- particulate organic carbon; Biogeochemical cycles -- Periodicals; Electronic journals; 577.1405
• DOI: 10.1029/2020GB006672
• Languages: English
• ISSNs: 0886-6236

Abstract

Abstract: The magnitude of future emissions of greenhouse gases from the northern permafrost region depends crucially on the mineralization of soil organic carbon (SOC) that has accumulated over millennia in these perennially frozen soils. Many recent studies have used radiocarbon ( 14 C) to quantify the release of this "old" SOC as CO2 or CH4 to the atmosphere or as dissolved and particulate organic carbon (DOC and POC) to surface waters. We compiled ~1, 900 14 C measurements from 51 sites in the northern permafrost region to assess the vulnerability of thawing SOC in tundra, forest, peatland, lake, and river ecosystems. We found that growing season soil 14 C‐CO2 emissions generally had a modern (post‐1950s) signature, but that well‐drained, oxic soils had increased CO2 emissions derived from older sources following recent thaw. The age of CO2 and CH4 emitted from lakes depended primarily on the age and quantity of SOC in sediments and on the mode of emission, and indicated substantial losses of previously frozen SOC from actively expanding thermokarst lakes. Increased fluvial export of aged DOC and POC occurred from sites where permafrost thaw caused soil thermal erosion. There was limited evidence supporting release of previously frozen SOC as CO2, CH4, and DOC from thawing peatlands with anoxic soils. This synthesis thus suggests widespread but not universal release of permafrost SOC following thaw. We show that different definitions of "old" sources among studies hamper the comparison of vulnerability of permafrost SOC across ecosystems and disturbances. We also highlight opportunities for future 14 C studies in the permafrost region. Key Points: We compiled ~1, 900 14 C measurements of CO2, CH4, DOC, and POC from the northern permafrost region Old carbon release increases in thawed oxic soils (CO2 ), thermokarst lakes (CH4 and CO2 ), and headwaters with thermal erosion (DOC and POC) Simultaneous and year‐long 14 C analyses of CO2, CH4, DOC, and POC are needed to assess the vulnerability of permafrost carbon across ecosystems