Phloem-xylem water flow in developing cladodes of Opuntia ficus-indica during sink-to-source transition

Phloem versus xylem water and carbon flow between a developingdaughter cladode (flattened stem segment) and the underlyingbasal cladode of Opuntia ficus-indica was assessed using netCO₂ uptake, transpiration, phloem sap concentration, and waterpotential of both organs as well as phloem and apoplastic tracers.A 14-d-old daughter cladode was a sink organ with a negativedaily net CO₂ uptake; its water potential was higher than thatof the underlying basal cladode, implicating a non-xylem pathwayfor the water needed for growth. Indeed, the relatively dilutephloem sap (7.44% dry weight) of a basal cladode can supplyall the water (7.1 gd^–1) along with photosynthate neededfor the growth of a 14-d-old daughter cladode; about 3% of theimported water flowed back to the basal cladode via the xylem.In contrast, a 28-d-old daughter cladode was a source organwhose water potential was lower than that of its basal cladode,so the xylem can supply the water needed (25.7 g d^–1)for its growth; about 6% of the imported water flowed back tothe basal cladode along with photosynthate via the phloem. Thephloem tracer carboxyfluorescein occurred in the phloem of 14-d-olddaughter cladodes after its precursor was applied to basal cladodes.When applied to basal cladodes, the apoplastic tracers sulphorhodamineG (SR) and trisodium 8-hydroxy-1,3,6-pyrenetrisulphonate (PTS)failed to move into 14-d-old daughter cladodes within 5 h, butmoved into 28-d-old daughter cladodes within 2 h. SR and PTSmoved into basal cladodes within 2 h when applied to 14-d-olddaughter cladodes, but not within 5-6 h when applied to 28-d-olddaughter cladodes. The tracer experiments therefore confirmedthe patterns of water flow determined using water and carbonbudgets. Key words: Carboxyfluorescein, phloem-xylem water flow, source-sink water relations, suiphorhodamine G, trisodium 8-hydroxy-1,3,6-pyrenetnsulphonate