Nocturnal sap flow in the C3-CAM species, Clusia minor
Clusia minor L. is a C 3-CAM species in which Crassulacean acid Metabolism (CAM) is
induced, among other factors, by water deficit. We propose that CAM induction by natural
drought in C. minor shifts the sap flow pattern from daytime to a night-time one, and that the
decreased osmotic potential due to increased malate content in droughted plants aids in the
increase in nocturnal sap flow. In order to test these hypotheses, we followed for 2 years the
seasonal changes in parameters of water relationships and sap flow velocity in one single …
induced, among other factors, by water deficit. We propose that CAM induction by natural
drought in C. minor shifts the sap flow pattern from daytime to a night-time one, and that the
decreased osmotic potential due to increased malate content in droughted plants aids in the
increase in nocturnal sap flow. In order to test these hypotheses, we followed for 2 years the
seasonal changes in parameters of water relationships and sap flow velocity in one single …
Abstract
Clusia minor L. is a C3-CAM species in which Crassulacean acid Metabolism (CAM) is induced, among other factors, by water deficit. We propose that CAM induction by natural drought in C. minor shifts the sap flow pattern from daytime to a night-time one, and that the decreased osmotic potential due to increased malate content in droughted plants aids in the increase in nocturnal sap flow. In order to test these hypotheses, we followed for 2 years the seasonal changes in parameters of water relationships and sap flow velocity in one single, freestanding tree growing in Caracas. Leaf water and osmotic potential were measured psychrometrically, nocturnal proton accumulation by titration of aqueous leaf extracts and sap flow density with thermal dissipation probes. Leaf water, osmotic and turgor potential remained relatively high throughout the seasons. Nocturnal proton accumulation was nil under extreme drought or after frequent and heavy rains, and high after moderate rainfall. Estimated malate and citrate concentrations contributed up to 80 and 60%, respectively, of the value of osmotic potential. The shape of the daily courses of sap flow velocity varied seasonally, from mostly diurnal during the dry season to mostly nocturnal after a short dry spell during the rainy season, when nocturnal acid accumulation attained high values. There was a strong positive relationship between the proportion of the integrated sap flow courses corresponding to the night and dawn [H+] (r 2 = 0.88). Increased nocturnal sap flow in the CAM stage of the tree of C. minor may be explained by a lower osmotic potential due to an increased acid concentration, together with increased stomatal aperture, as suggested by increased nocturnal acid accumulation probably due to nocturnal CO2 fixation.
Springer
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