Deep peat warming increases surface methane and carbon dioxide emissions in a black spruce‐dominated ombrotrophic bog. (28th July 2017)

• Record Type: Journal Article
• Authors: Gill, Allison L.; Giasson, Marc‐André; Yu, Rieka; Finzi, Adrien C.
• Is Part Of: Global change biology. Volume 23:Number 12(2017)
• Page Start: 5398
• Page End: 5411
• Publication Date: 2017-07-28
• Subjects: bog -- climate change -- greenhouse gas flux -- Sphagnum -- warming experiment -- wetland; Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.13806
• Languages: English
• ISSNs: 1354-1013

Abstract

Abstract: Boreal peatlands contain approximately 500 Pg carbon (C) in the soil, emit globally significant quantities of methane (CH4 ), and are highly sensitive to climate change. Warming associated with global climate change is likely to increase the rate of the temperature‐sensitive processes that decompose stored organic carbon and release carbon dioxide (CO2 ) and CH4 . Variation in the temperature sensitivity of CO2 and CH4 production and increased peat aerobicity due to enhanced growing‐season evapotranspiration may alter the nature of peatland trace gas emission. As CH4 is a powerful greenhouse gas with 34 times the warming potential of CO2, it is critical to understand how factors associated with global change will influence surface CO2 and CH4 fluxes. Here, we leverage the Spruce and Peatland Responses Under Changing Environments (SPRUCE) climate change manipulation experiment to understand the impact of a 0–9°C gradient in deep belowground warming ("Deep Peat Heat", DPH) on peat surface CO2 and CH4 fluxes. We find that DPH treatments increased both CO2 and CH4 emission. Methane production was more sensitive to warming than CO2 production, decreasing the C‐CO2 :C‐CH4 of the respired carbon. Methane production is dominated by hydrogenotrophic methanogenesis but deep peat warming increased the δ 13 C of CH4 suggesting an increasing contribution of acetoclastic methanogenesis to total CH4 production with warming. Although the total quantity of C emitted from the SPRUCE Bog as CH4 is <2%, CH4 represents >50% of seasonal C emissions in the highest‐warming treatments when adjusted for CO2 equivalents on a 100‐year timescale. These results suggest that warming in boreal regions may increase CH4 emissions from peatlands and result in a positive feedback to ongoing warming. Abstract : Belowground warming increased both CO2 and CH4 emission, but CH4 production was more sensitive to warming which decreased the CO2 :CH4 of the respired C. Although the total quantity of C emitted from the bog as CH4 is small, CH4 represents >50% of seasonal C emissions in the highest warming treatments when adjusted for CO2 equivalents. These results suggest that high‐latitude warming may increase the contribution of CH4 to total ecosystem C losses and make peatlands a positive feedback to additional warming.