Does plant size affect growth responses to water availability at glacial, modern and future CO2 concentrations?

Plant responses to carbon (C) and water availability are strongly connected. Thus, we can learn much about the responses of modern plants to rising atmospheric carbon dioxide (CO₂) by studying their performance under a range of carbon and water availabilities, including very low CO₂ as in past glaci...

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Published in:Ecological research Vol. 31; no. 2; pp. 213 - 227
Main Authors: Liu, Jin-Chun, Temme, Andries A, Cornwell, William K, van Logtestijn, Richard S. P, Aerts, Rien, Cornelissen, Johannes H. C
Format: Journal Article
Language:English
Published: Tokyo Springer Japan 01-03-2016
Blackwell Publishing Ltd
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Summary:Plant responses to carbon (C) and water availability are strongly connected. Thus, we can learn much about the responses of modern plants to rising atmospheric carbon dioxide (CO₂) by studying their performance under a range of carbon and water availabilities, including very low CO₂ as in past glacial periods. We hypothesized that, especially in shallow soils, the positive effects of high CO₂ and the negative effects of low CO₂ on growth response to drought are moderated by plant size-driven feedbacks through transpiration and soil water depletion. We grew two temperate annual C₃ species, Avena sativa and Chenopodium album, in glacial (180 ppm), modern (400 ppm) and future (700 ppm) CO₂ levels and five soil water regimes in climate chambers. In both species, low CO₂ resulted in a much lower relative growth rate, biomass and total leaf area than at ambient CO₂ with higher water availability, but this difference disappeared steadily towards severe drought conditions. Elevated CO₂ increased relative growth rate, plant biomass and total leaf area of both species slightly compared with ambient CO₂. These results were especially pronounced under drought. Our results support the hypothesis that, in annuals, plant size modulates the negative drought effect at low CO₂. However, plant size-mediated effects of high CO₂ on growth response to drought were inconclusive. Further experiments should reveal the interactive effects of CO₂ and water regimes in environments closer to a field setting, both in shallow and in deep soils with unconstrained rooting, as well as in mixed communities.
Bibliography:http://dx.doi.org/10.1007/s11284-015-1330-y
Electronic supplementary material
The online version of this article (doi:10.1007/s11284‐015‐1330‐y) contains supplementary material, which is available to authorized users.
ISSN:0912-3814
1440-1703
DOI:10.1007/s11284-015-1330-y