“…Once released into the water column, sperm and ova may coalesce as a result of passive transport by turbulence, or by active sperm swimming. Models and experiments suggest that a combination of large, pheromoneproducing eggs and small, motile sperm increases gamete encounter rates (Dusenbery, 2000;Dusenbery, 2002;Podolsky, 2001;Podolsky, 2002). Turbulent stirring and mixing produces long-term dilution of gamete concentrations (Csanady, 1973;Denny et al, 1992), but the dilution may be mitigated by releasing gametes in a viscous matrix (Thomas, 1994a;Marshall, 2002;Yund and Meidel, 2003), or through gamete sequestration in surge channels (Denny et al, 1992) and tide pools (Pearson and Brawley, 1996).…”