We have observed HCO+ J = 3-2 toward 16 class I sources and 18 class 0 sour
ces, many of which were selected from Mardones et al.'s recent observations
. Eight sources have profiles significantly skewed to the blue relative to
optically thin lines. We suggest six sources as new infall candidates. We f
ind an equal "blue excess" among class 0 and class I sources after combinin
g this sample with that of Gregersen et al. We used a Monte Carlo code to s
imulate the temporal evolution of line profiles of optically thick lines of
HCO+, CS, and H2CO in a collapsing cloud and found that HCO+ had the stron
gest asymmetry at late times. If a blue-peaked line profile implies infall,
then the dividing line between the two classes does not trace the end of t
he infall stage.