The morphology of leaf venation has been studied repeatedly and variou
s systems have been proposed for the classification of the observed le
af venation patterns. Almost nothing is known, however, about the func
tional properties of the various venation types. Using a computer mode
lling approach we analysed the water transport properties of typical c
raspedodromous and brochidodromous venation patterns. The water transp
ort through the leaf and the veins was modelled as a fluid flow throug
h a porous medium and the mathematical model was solved with the Finit
e Element Method. The simulations illustrate that the leaf margin repr
esents a critical region in terms of water supply. The results provide
a plausible functional explanation for three well known phenomena: 1)
the correlation between craspedodromous venation and the formation of
leaf teeth; 2) the fact that craspedodromous venation is more common
in temperate than in tropical regions and 3) the fact that xeromorphic
leaves tend to have more closed venation.