We conducted discrete-depth, hourly sampling for larval weakfish Cynos
cion regalis at a station in southern Delaware Bay, USA, during the sp
awning seasons of 1988 (131 h) and 1989 (150 h). During both years, co
incident measurements of current velocity, salinity, and temperature w
ere made at 2 depths in the water column and tidal-height data were ob
tained from a nearby NOAA tide gauge. Results of nonparametric analysi
s of variance showed that larvae were significantly more abundant at d
epth than at the surface. Post-yolksac larvae were significantly more
abundant during flood tides, but there was no effect of tidal stage on
the abundance of yolksac larvae. Cross-correlation analysis indicated
that post-yolksac larvae showed a periodicity in abundance around 12
h, which is similar to the period of the semidiurnal tide in the Bay.
This indicates that post-yolksac larvae may utilize selective tidal st
ream transport to effect retention in the estuary. Results of autocorr
elation indicate that larval-patch diameter was approximately 3 km. Re
sults of both cross-correlation and spectral analysis suggest that nei
ther salinity nor sea level height serves as a cue for vertical migrat
ion. Rather, some aspect of the tidal-velocity field appears to be imp
ortant.