Settlement of ophiuroids (Ophiopholis aculeata, Ophiura spp.) was measured
using artificial collectors at 3-day intervals during their annual 2-week s
ettlement period in July-August 1993 in St. Margaret's Bay, Nova Scotia. Hy
drographic (temperature, salinity, current velocity, wave height and period
) and meteorologic conditions (atmospheric pressure and wind velocity) were
recorded concurrently at the site or at nearby locations. A major settleme
nt pulse occurred over one 3-day period, with declining settlement over the
following 6 days. This pulse was associated with a shift in current direct
ion and preceded by rapid temperature and salinity fluctuations. Similar ch
anges in temperature occurred at a second site (4.5 km away), indicating at
least bay-scale forcing. This period was characterised by the passage of w
eak atmospheric pressure gradients and a low-energy sea state. These meteor
ologic and oceanographic fluctuations were within the normal range for this
time of year, indicating that major settlement events can occur at scales
of days in association with minor fluctuations in the physical environment.