Increased belowground carbon inputs and warming promote loss of soil organic carbon through complementary microbial responses

• Published in: Soil biology & biochemistry Vol. 76; pp. 57 - 69
• Main Authors: Hopkins, Francesca M., Filley, Timothy R., Gleixner, Gerd, Lange, Markus, Top, Sara M., Trumbore, Susan E.
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier Ltd 01-09-2014; Elsevier
• Subjects: Agronomy. Soil science and plant productions; Biochemistry and biology; Biological and medical sciences; Carbon isotopes; Chemical, physicochemical, biochemical and biological properties; Elevated CO2; Fundamental and applied biological sciences. Psychology; Microbiology; Organic matter; Physics, chemistry, biochemistry and biology of agricultural and forest soils; PLFA; Priming effect; Soil organic matter decomposition; Soil science; Temperature response; Elevated CO2; Soil organic matter decomposition; PLFA; Priming effect; Carbon isotopes; Temperature response; Warming; Microbial activity; Organic carbon; Organic matter; Carbon dioxide; Temperature effect; Phospholipid; Increase; Decomposition; Fatty acids; Soils; Elevated CO; Soil science
• DOI: 10.1016/j.soilbio.2014.04.028
• EISSN: 1879-3428
• ISSN: 0038-0717

Current carbon cycle-climate models predict that future soil carbon storage will be determined by the balance between CO2 fertilization and warming. However, it is uncertain whether greater carbon inputs to soils with elevated CO2 will be sequestered, particularly since warming hastens soil carbon decomposition rates, and may alter the response of soils to new plant inputs. We studied the effects of elevated CO2 and warming on microbial soil carbon decomposition processes using laboratory manipulations of carbon inputs and soil temperature. We incubated soils from the Aspen Free Air CO2 Enrichment experiment, where no accumulation of soil carbon has been observed despite a decade of increased carbon inputs to soils under elevated CO2. We added isotopically-labeled sucrose to these soils in the laboratory to mimic and trace the effects of increased carbon inputs on soil organic carbon decomposition and its temperature sensitivity. Sucrose additions caused a positive priming of soil organic carbon decomposition, demonstrated by increased respiration derived from soil carbon, increased microbial abundance, and a shift in the microbial community towards faster growing microorganisms. Similar patterns were observed for elevated CO2 soils, suggesting that the priming effect was responsible for reductions in soil carbon accumulation at the site. Laboratory warming accelerated the rate of the priming effect, but the magnitude of the priming effect was not different amongst temperatures, suggesting that the priming effect was limited by substrate availability, not soil temperature. No changes in substrate use efficiency were observed with elevated CO2 or warming. The stimulatory effects of warming on the priming effect suggest that increased belowground carbon inputs from CO2 fertilization are not likely to be stored in mineral soils.
Effects of elevated CO2 and warming on the soil carbon cycle. [Display omitted]
•Increased carbon inputs in laboratory cause a positive priming of SOC decomposition.•Increased carbon inputs to soil from 10 y of eCO2 similarly altered SOC decomposition.•Warming increased the rate, not amount, of SOC primed by increased carbon inputs.•Microbial substrate use efficiency for added sucrose was unchanged by eCO2 or warming.•The priming effect did not change the proportion of different ages of C in respiration.