PHOTOSYNTHETIC AND WATER RELATIONS RESPONSES TO ELEVATED CO-2 IN THE C-4 GRASS ANDROPOGON-GERARDII

Citation
Ak. Knapp et al., PHOTOSYNTHETIC AND WATER RELATIONS RESPONSES TO ELEVATED CO-2 IN THE C-4 GRASS ANDROPOGON-GERARDII, International journal of plant sciences, 154(4), 1993, pp. 459-466
Citations number
27
Categorie Soggetti
Plant Sciences
ISSN journal
10585893
Volume
154
Issue
4
Year of publication
1993
Pages
459 - 466
Database
ISI
SICI code
1058-5893(1993)154:4<459:PAWRRT>2.0.ZU;2-P
Abstract
Undisturbed tallgrass prairie, dominated by the C-4 grass Andropogon g erardii, was exposed to ambient and elevated (double ambient) levels o f atmospheric CO2 in large open-top chambers throughout the 1991 and 1 992 growing seasons. Responses in leaf xylem pressure potential (psi), net photosynthesis (A), and stomatal conductance (g) were measured in both years for A. gerardii grown within chambers and from adjacent fi eld plots. In 1992, maximum photosynthetic capacity (A(max)), apparent quantum requirement (Q(r)), the photosynthetic light compensation poi nt (LCP), and dark respiration (R(d)) were also measured. Midday psi w as significantly higher in plants grown at elevated CO2 in both years, and seasonally averaged psi was 0.48-0.70 MPa lower in 1991 (a dry ye ar) than 1992 (a wet year). In 1991, A and g were significantly higher (regardless of measurement CO2 level) in plants grown at elevated vs. ambient CO2. These increases were measured in well-watered plants ins uring that these plants differed only in CO2 growth conditions and pre vious exposure to low psi. Increased A at elevated CO2 occurred (as mu ch as 7.1 mu mol m(-2) s(-1)) over a broad range of temperatures (17-3 5 C), but the temperature optimum for A was similar at both 350 and 70 0 mu L L(-1) CO2. In 1992, no differences in A, A(max), Q(r), LCP, or R(d) were detected when ambient and elevated CO2 plants were compared. In plants collected from field plots, R(d), LCP, and leaf N were sign ificantly higher than in plants within the chambers indicating that a chamber effect exists for these parameters. In both years, g was signi ficantly reduced (21%-51%) when measured at 700 vs. 350 mu L L(-1) CO2 . Peak aboveground biomass was increased at elevated CO2 in 1991 but n ot in 1992. These data indicate that for C-4 grasses, effects of eleva ted CO2 may only be detectable in years with significant water stress, a common occurrence in the central North American tallgrass prairies.