Abstract
Several experiments were conducted with tropical tree and liana seedlings in which transpiration ratio and leaf phosphorus to carbon ratio (P:C) were measured. Transpiration ratio was expressed as kg H 2O transpiredg -1 C incorporated into plant biomass, and leaf P:C as mg Pg -1 C. Leaf P:C was positively correlated with transpiration ratio across 19 species for plants grown under similar conditions (R 2=0.35, P<0.01, n=19). For five species in the dataset, multiple treatments were imposed to cause intra-specific variation in transpiration ratio. Within four of these five species, leaf P:C correlated positively with transpiration ratio. The slope and strength of the correlation varied among species. In one experiment, whole-plant P:C was measured in addition to leaf P:C. Patterns of correlation between whole-plant P:C and transpiration ratio were similar to those between leaf P:C and transpiration ratio. Together, these observations suggest that transpiration can influence the rate of P uptake from soil in tropical tree and liana seedlings. We suggest that this occurs through transport of inorganic phosphate and organic P compounds to root surfaces by transpiration-induced mass flow of the soil solution. The positive correlation between leaf P:C and transpiration ratio suggests that leaf P:C could decline in tropical forests as atmospheric CO 2 concentration rises, due to decreasing transpiration ratios.
Original language | English |
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Pages (from-to) | 878-885 |
Number of pages | 8 |
Journal | Tree Physiology |
Volume | 31 |
Issue number | 8 |
DOIs | |
Publication status | Published - Aug 2011 |