2010/01/18 by Nicole S. Nowinski, L. Taneva, Susan Trumbore +1 · 1 citation
Earth and Planetary Sciences · Chemistry · #Climate change and permafrost #Geology and Paleoclimatology Research #Cryospheric studies and observations #Snow #Permafrost #Tundra #Organic matter #Radiocarbon dating #Soil water #Soil respiration #Autotroph #Soil horizon #Snow removal #Heterotroph #Carbon cycle #Total organic carbon #Environmental chemistry #Soil science #Atmospheric sciences #Environmental science #Geology #Ecology #Biology #Arctic #Ecosystem #Chemistry #Geomorphology #Paleontology
paper · pdf · doi:10.1007/s00442-009-1556-x
openalex publication_date 2010/01/18 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/01
A snow addition experiment in moist acidic tussock tundra at Toolik Lake, Alaska, increased winter snow depths 2-3 m, and resulted in a doubling of the summer active layer depth. We used radiocarbon (Delta(14)C) to (1) determine the age of C respired in the deep soils under control and deepened active layer conditions (deep snow drifts), and (2) to determine the impact of increased snow and permafrost thawing on surface CO(2) efflux by partitioning respiration into autotrophic and heterotrophic components. Delta(14)C signatures of surface respiration were higher in the deep snow areas, reflecting a decrease in the proportion of autotrophic respiration. The radiocarbon age of soil pore CO(2) sampled near the maximum mid-July thaw depth was approximately 1,000 years in deep snow treatment plots (45-55 cm thaw depth), while CO(2) from the ambient snow areas was approximately 100 years old (30-cm thaw depth). Heterotrophic respiration Delta(14)C signatures from incubations were similar between the two snow depths for the organic horizon and were extremely variable in the mineral horizon, resulting in no significant differences between treatments in either month. Radiocarbon ages of heterotrophically respired C ranged from <50 to 235 years BP in July mineral soil samples and from 1,525 to 8,300 years BP in August samples, suggesting that old soil C in permafrost soils may be metabolized upon thawing. In the surface fluxes, this old C signal is obscured by the organic horizon fluxes, which are significantly higher. Our results indicate that, as permafrost in tussock tundra ecosystems of arctic Alaska thaws, carbon buried up to several thousands of years ago will become an active component of the carbon cycle, potentially accelerating the rise of CO(2) in the atmosphere.