Published online by Cambridge University Press: 14 July 2015
Settling rates and behaviors of sediment grains are of particular interest as components in interpreting the hydrodynamics of skeletal carbonate sediments (Maiklem, 1968) and the deposition of skeletons of planktonic organisms (Bé, 1977; Casey and McMillen, 1977). Settling rates and behaviors also are important because even the disarticulated remains of benthic organisms may undergo repeated resuspension and differential settling prior to final burial.