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The water–water cycle in leaves is not a major alternative electron sink for dissipation of excess excitation energy when CO 2 assimilation is restricted
Author(s) -
DRIEVER STEVEN M.,
BAKER NEIL R.
Publication year - 2011
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.1365-3040.2011.02288.x
Subject(s) - photosynthesis , chemistry , photosystem ii , water cycle , sink (geography) , electron transport chain , biology , ecology , biochemistry , cartography , geography
Electron flux from water via photosystem II (PSII) and PSI to oxygen (water–water cycle) may provide a mechanism for dissipation of excess excitation energy in leaves when CO 2 assimilation is restricted. Mass spectrometry was used to measure O 2 uptake and evolution together with CO 2 uptake in leaves of French bean and maize at CO 2 concentrations saturating for photosynthesis and the CO 2 compensation point. In French bean at high CO 2 and low O 2 concentrations no significant water–water cycle activity was observed. At the CO 2 compensation point and 3% O 2 a low rate of water–water cycle activity was observed, which accounted for 30% of the linear electron flux from water. In maize leaves negligible water–water cycle activity was detected at the compensation point. During induction of photosynthesis in maize linear electron flux was considerably greater than CO 2 assimilation, but no significant water–water cycle activity was detected. Miscanthus × giganteus grown at chilling temperature also exhibited rates of linear electron transport considerably in excess of CO 2 assimilation; however, no significant water–water cycle activity was detected. Clearly the water–water cycle can operate in leaves under some conditions, but it does not act as a major sink for excess excitation energy when CO 2 assimilation is restricted.