Family- and population-level responses to atmospheric CO2 concentration: gas exchange and the allocation of C, N, and biomass in Plantago lanceolata (Plantaginaceae)

To ascertain the inheritance of responses to changing atmospheric CO2 content, we partitioned response to elevated CO2 in Plantago lanceolata between families and populations in 18 families in two populations. Plants were grown in 35 Pa and 71 Pa partial pressure of CO2 (pCO2) in open‐top chambers....

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Published inAmerican journal of botany Vol. 88; no. 6; pp. 1080 - 1087
Main Authors Jenkins Klus, Dawn, Kalisz, Susan, Curtis, Peter S, Teeri, James A, Tonsor, Stephen J
Format Journal Article
LanguageEnglish
Published United States Botanical Soc America 01.06.2001
Botanical Society of America
Botanical Society of America, Inc
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Summary:To ascertain the inheritance of responses to changing atmospheric CO2 content, we partitioned response to elevated CO2 in Plantago lanceolata between families and populations in 18 families in two populations. Plants were grown in 35 Pa and 71 Pa partial pressure of CO2 (pCO2) in open‐top chambers. We measured above‐ and belowground mass, carbon (C), nitrogen (N), hexose sugar, and gas exchange properties in both CO2 treatments. Families within populations differed in mass, mass allocation, root : shoot ratios, aboveground percentage N, C : N ratio, and gas exchange properties. The CO2 × family interaction is the main indicator of potential evolutionary responses to changing CO2. Significant CO2 × family interactions were observed for N content, C : N ratio, and photosynthetic rate (A: instantaneous light‐saturated carbon assimilation capacity), intercellular CO2 concentration, transpiration rate (E), and water use efficiency (WUE = A/E), but not for stomatal conductance. Families differed significantly in acclimation across time. The ratio of A in elevated vs. ambient growth CO2, when measured at a common internal CO2 partial pressure was 0.79, indicating down‐regulation of A under CO2 enrichment. Mass, C : N ratio, percentage, C (%C), and soluble sugar all increased significantly but overall %N did not change. Increases in %C and sugar were significant and were coincident with redistribution of N aboveground. The observed variation among populations and families in response to CO2 is evidence of genetic variation in response and therefore of the potential for novel evolutionary trajectories with rising atmospheric CO2.
Bibliography:Author for reprint requests (e‐mail
tonsor@pitt.edu
The authors thank Jon Ervin, Pam Woodruff, Nina Consolatti, Chris Vogel, Sandy Halstead, Hal Collins, R. Kelman Wieder, Brenda Casper, Phillip Brautigam, and Kim Hollingshead for technical help and the graduate students at W.K. Kellogg Biological Station for discussions on this topic. DJK gives most special thanks to John and Nicholas Klus. Mark Vandermeulen and the Tonsor lab group at The University of Pittsburgh provided useful comments on the manuscript. This project was supported by a Grant‐in‐Aid of Research through Sigma Xi and an NSF Predoctoral Fellowship to DJK, an NSF Research Training Group at Kellogg Biological Station (CIR‐9113598), NSF grant BSR 8906283 to SJT, a Michigan State All University Research Initiation Grant to SK, the University of Michigan Biological Station, and the University of Michigan Global Change Project.
Current address: A234 Langley Hall, The University of Pittsburgh, Department of Biological Sciences, Pittsburgh Pennsylvania 15260 USA.
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ISSN:0002-9122
1537-2197
DOI:10.2307/2657091