1Present address: US Geological Survey, Forest and Rangeland Ecosystem Science Center, 3200 SW Jefferson Way, Corvallis, OR 97331, USA.
Effects of elevated CO2 on fine root dynamics in a Mojave Desert community: a FACE study
Article first published online: 1 DEC 2005
Global Change Biology
Volume 12, Issue 1, pages 61–73, January 2006
How to Cite
PHILLIPS, D. L., JOHNSON, M. G., TINGEY, D. T., CATRICALA, C. E., HOYMAN, T. L. and NOWAK, R. S. (2006), Effects of elevated CO2 on fine root dynamics in a Mojave Desert community: a FACE study. Global Change Biology, 12: 61–73. doi: 10.1111/j.1365-2486.2005.01085.x
- Issue published online: 1 DEC 2005
- Article first published online: 1 DEC 2005
- Received 31 March 2005; revised version received 2 September 2005; accepted 7 September 2005
- belowground standing crop;
- fine roots;
- turn over
Fine roots (≤1 mm diameter) are critical in plant water and nutrient absorption, and it is important to understand how rising atmospheric CO2 will affect them as part of terrestrial ecosystem responses to global change. This study's objective was to determine the effects of elevated CO2 on production, mortality, and standing crops of fine root length over 2 years in a free-air CO2 enrichment (FACE) facility in the Mojave Desert of southern Nevada, USA. Three replicate 25 m diameter FACE rings were maintained at ambient (∼370 μmol mol−1) and elevated CO2 (∼550 μmol mol−1) atmospheric concentrations. Twenty-eight minirhizotron tubes were placed in each ring to sample three microsite locations: evergreen Larrea shrubs, drought-deciduous Ambrosia shrubs, and along systematic community transects (primarily in shrub interspaces which account for ∼85% of the area). Seasonal dynamics were similar for ambient and elevated CO2: fine root production peaked in April–June, with peak standing crop occurring about 1 month later, and peak mortality occurring during the hot summer months, with higher values for all three measures in a wet year compared with a dry year. Fine root standing crop, production, and mortality were not significantly different between treatments except standing crop along community transects, where fine root length was significantly lower in elevated CO2. Fine root turnover (annual cumulative mortality/mean standing crop) ranged from 2.33 to 3.17 year−1, and was not significantly different among CO2 treatments, except for community transect tubes where it was significantly lower for elevated CO2. There were no differences in fine root responses to CO2 between evergreen (Larrea) and drought-deciduous (Ambrosia) shrubs. Combined with observations of increased leaf-level water-use efficiency and lack of soil moisture differences, these results suggest that under elevated CO2 conditions, reduced root systems (compared with ambient CO2) appear sufficient to provide resources for modest aboveground production increases across the community, but in more fertile shrub microsites, fine root systems of comparable size with those in ambient CO2 were required to support the greater aboveground production increases. For community transects, development of the difference in fine root standing crops occurred primarily through lower stimulation of fine root production in the elevated CO2 treatment during periods of high water availability.