Photosynthetic rates of aquatic macrophytes are affected by the diffus
ion of carbon through the boundary layer which decreases with increasi
ng flow velocities. This is shown by a significant increase in photosy
nthetic rates of Ulva lactuca fronds exposed to friction velocities (u
) between 0.0 and 0.3 cm s-1. No further increase in photosynthetic r
ates is observed at u values between 0.3 and 1.0 cm s-1. Stagnating f
low conditions at saturating light levels caused a 29 % reduction in p
hotosynthetic rates. Experiments in a closed system indicate that Ulva
may, utilize internal carbon sources during periods of stagnation. On
a subtidal rock directly exposed to wave action, Ulva lactuca is not
exposed to such conditions while in a wave flushed intertidal pool sta
gnation occurs during very short time intervals based on in situ measu
rements of u levels on fronds of this species using a microprocessor-
controlled, autonomous recorder and hot-film sensors.