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Higher daytime leaf temperatures contribute to lower freeze tolerance under elevated CO 2
Author(s) -
LOVEYS BETH R.,
EGERTON JOHN J. G.,
BALL MARILYN C.
Publication year - 2006
Publication title -
plant, cell and environment
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.646
H-Index - 200
eISSN - 1365-3040
pISSN - 0140-7791
DOI - 10.1111/j.1365-3040.2005.01482.x
Subject(s) - daytime , stomatal conductance , evergreen , acclimatization , frost (temperature) , photosynthesis , horticulture , snow , chemistry , zoology , botany , atmospheric sciences , biology , meteorology , physics , geology
Elevated atmospheric CO 2 adversely affects freezing tolerance in many evergreens, but the underlying mechanism(s) have been elusive. We compared effects of elevated CO 2 with those of daytime warming on acclimation of snow gum ( Eucalyptus pauciflora ) to freezing temperatures under field conditions. Reduction in stomatal conductance g c under elevated CO 2 was shown to cause leaf temperature to increase by up to 3 °C. In this study, this increase in leaf temperature was simulated under ambient CO 2 conditions by using a free air temperature increase (FATI) system to warm snow gum leaves during daytime, thereby increasing the diurnal range in temperature without affecting temperature minima. Acclimation to freezing temperatures was assessed using measures of electrolyte leakage and photosynthetic efficiency of leaf discs exposed to different nadir temperatures. Here, we show that both elevated CO 2 and daytime warming delayed acclimation to freezing temperatures for 2–3 weeks after which time freeze tolerance of the treated plants in both the FATI and open top chamber (OTC) experiments did not differ from control plants. Our results support the hypothesis that delayed development of freezing tolerance under elevated CO 2 is because of higher daytime leaf temperatures under elevated CO 2 . Thus, potential gains in productivity in response to increasing atmospheric CO 2 and prolonging the growing season may be reduced by an increase in freezing stress in frost‐prone areas.