4.6 Article

Soybean leaf hydraulic conductance does not acclimate to growth at elevated [CO2] or temperature in growth chambers or in the field

Journal

ANNALS OF BOTANY
Volume 112, Issue 5, Pages 911-918

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/aob/mct143

Keywords

Leaf hydraulic conductance; elevated CO2; temperature; climate change; water potential; soybean; Glycine max

Categories

Funding

  1. United States Department of Agriculture (USDA) Agriculture Research Service (ARS)
  2. Office of Science (BER), US Department of Energy through the Midwestern Center of the National Institute for Climate Change Research (NICCR)

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Leaf hydraulic properties are strongly linked with transpiration and photosynthesis in many species. However, it is not known if gas exchange and hydraulics will have co-ordinated responses to climate change. The objective of this study was to investigate the responses of leaf hydraulic conductance (K-leaf) in Glycine max (soybean) to growth at elevated [CO2] and increased temperature compared with the responses of leaf gas exchange and leaf water status. Two controlled-environment growth chamber experiments were conducted with soybean to measure K-leaf, stomatal conductance (g(s)) and photosynthesis (A) during growth at elevated [CO2] and temperature relative to ambient levels. These results were validated with field experiments on soybean grown under free-air elevated [CO2] (FACE) and canopy warming. In chamber studies, K-leaf did not acclimate to growth at elevated [CO2], even though stomatal conductance decreased and photosynthesis increased. Growth at elevated temperature also did not affect K-leaf, although g(s) and A showed significant but inconsistent decreases. The lack of response of K-leaf to growth at increased [CO2] and temperature in chamber-grown plants was confirmed with field-grown soybean at a FACE facility. Leaf hydraulic and leaf gas exchange responses to these two climate change factors were not strongly linked in soybean, although g(s) responded to [CO2] and increased temperature as previously reported. This differential behaviour could lead to an imbalance between hydraulic supply and transpiration demand under extreme environmental conditions likely to become more common as global climate continues to change.

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