期刊
GLOBAL CHANGE BIOLOGY
卷 16, 期 1, 页码 454-468出版社
WILEY
DOI: 10.1111/j.1365-2486.2009.01975.x
关键词
atmospheric CO2; elevated CO2; grassland; root biomass; root lifespan; root respiration; roots; subambient CO2
资金
- DOE [64242-0012346]
- USDA-ARS
Atmospheric CO2 (C-a) concentration has increased significantly during the last 20 000 years, and is projected to double this century. Despite the importance of belowground processes in the global carbon cycle, community-level and single species root responses to rising C-a are not well understood. We measured net community root biomass over 3 years using ingrowth cores in a natural C-3-C-4 grassland exposed to a gradient of C-a from preglacial to future levels (230-550 mu mol mol(-1)). Root windows and minirhizotron tubes were installed below naturally occurring stands of the C-4 perennial grass Bothriochloa ischaemum and its roots were measured for respiration, carbohydrate concentration, specific root length (SRL), production, and lifespan over 2 years. Community root biomass increased significantly (P < 0.05) with C-a over initial conditions, with linear or curvilinear responses depending on sample date. In contrast, B. ischaemum produced significantly more roots at subambient than elevated C-a in minirhizotrons. The lifespan of roots with five or more neighboring roots in minirhizotron windows decreased significantly at high C-a, suggesting that after dense root growth depletes soil resource patches, plants with carbon surpluses readily shed these roots. Root respiration in B. ischaemum showed a curvilinear response to C-a under moist conditions in June 2000, with the lowest rates at C-a < 300 mu mol mol(-1) and peak activity at 450 mu mol mol(-1) in a quadratic model. B. ischaemum roots at subambient C-a had higher SRLs and slightly higher carbohydrate concentrations than those at higher C-a, which may be related to drier soils at low C-a. Our data emphasize that belowground responses of plant communities to C-a can be quite different from those of the individual species, and suggest that complex interactions between and among roots and their immediate soil environment influence the responses of root physiology and lifespan to changing C-a.
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