The swimming behaviour of settling larvae of the bivalve Cerastodenna edule (L.) was studied in still water and in a flume boundary-layer flow.In still water and slow flow the larvae swam upward in helices with high directionality, which is interpreted as morphological geotaxis By reducing velar propulsion larvae regularly descended towards the bottom due to gravity.In moderate and fast flow (5 to 10 cm s l ) the larvae became confined to the viscous sublayer, where they slowly drifted in the streamwise direction at 0.45 to 1.6 mm s l , less than 1 mm above the sediment surface, periodically making contact with the bottom.At flow velocities exceeding 15 cm s 1 the steady near-bottom drift changed to bed-load transport of tumbling larvae with high probability of resuspension.Based on kinematic and force analysis of swimming behaviour we suggest that boundary-shear induced torque restricts the settling larvae to the viscous sublayer.This near-bottom confinement may explain how habitat selection in benthic bivalves is realized under natural flow regimes.
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Jonsson et al. (1991) studied this question.
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