U.S. Department of Energy Office of Biological and Environmental Research

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Warming Increases Carbon Losses in Biocrust Soils
Published: November 26, 2015
Posted: May 06, 2016

Many arid and semiarid ecosystems have soils covered with well-developed biological soil crust communities (biocrusts) made up of mosses, lichens, cyanobacteria, and heterotrophs living at the soil surface. These communities are a fundamental component of dryland ecosystems and are critical to dryland carbon cycling. To examine the effects of warming temperatures on soil carbon balance in a dryland ecosystem, a recent study used infrared heaters to warm biocrust-dominated soils to 2°C above control conditions at a field site on the Colorado Plateau. The researchers monitored net soil exchange (NSE) of carbon dioxide (CO2) every hour for 21 months using automated flux chambers (5 control and 5 warmed chambers), which included the CO2 fluxes of the biocrusts and the soil beneath them. They observed measurable photosynthesis in biocrust soils on 12 percent of measurement days, which correlated well with precipitation events and soil wet-up. These days included several snow events, providing what is believed to be the first evidence of substantial photosynthesis underneath snow by biocrust organisms in drylands. Overall, biocrust soils in both the control and warmed plots were net CO2 sources to the atmosphere, with control plots losing 62 ± 8 g carbon m-2 (mean ± SE) over the first year of measurement and warmed plots losing 74 ± 9 g carbon m-2. Between the control and warmed plots, the difference in soil carbon loss was uncertain over the course of the entire year due to large and variable rates in spring, but on days during which soils were wet and crusts were actively photosynthesizing, biocrusts that were warmed by 2 oC had a substantially more negative carbon balance (i.e., biocrust soils took up less carbon and/or lost more carbon in warmed plots). Taken together, these data suggest a substantial risk of increased carbon loss from biocrust soils with higher future temperatures, and highlight a robust capacity to predict CO2 exchange in biocrust soils using easily measured environmental parameters.

Reference: Darrouzet-Nardi, A., S. C. Reed, E. E. Grote, and J. Belnap. 2015. “Observations of Net Soil Exchange of CO2 in a Dryland Show Experimental Warming Increases Carbon Losses in Biocrust Soils,” Biogeochemistry 126, 366-78. DOI: 10.1007/s10533-015-0163-7. (Reference link)

Contact: Jared DeForest, SC-23, (301) 903-3251, Daniel Stover, SC-23.1, (301) 903-0289
Topic Areas:

  • Research Area: Terrestrial Ecosystem Science
  • Research Area: Carbon Cycle, Nutrient Cycling
  • Research Area: Microbes and Communities

Division: SC-23.1 Climate and Environmental Sciences Division, BER

 

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