Abstract

To better understand zooplankton dynamics in Lake Ontario’s Toronto Harbour and adjacent coastal area (CA), we sampled zooplankton, phytoplankton, nutrients and physical parameters on six dates in 2016. Despite higher levels of nutrients, chlorophyll and primary production in the inner harbor (IH), the areas supported similar May to November zooplankton biomass (IH = 32 ± 7 and CA = 42 ± 10 mg/m3).IHvalues weremuch lowerthanother nutrient-enriched embayments in Lake Ontario, yet CA biomass was twice that of nearshore sites away from Toronto.Smallzooplanktonsuch as rotifers andBosminadominated IH; and large taxa (Daphnia, calanoids and predatory cladocerans) weremore important in the CA. Daphnia, Bosmina, cyclopoids and calanoids were larger in the CA, and adult cyclopoids had higher egg ratios.This led to low annual IH production estimates for both cyclopoid and calanoid copepods.Total phosphorus and chlorophyll did not appear to regulate zooplankton biomass, but positive relationships were found with bacterial biomass in the IH and with temperature in the cool season. Atypically high fish planktivory rates likely suppressed larger IH zooplankton in 2016, allowingsmall,resilient Bosmina to flourish and contribute 84% of total production in the IH. Comparing 2016 data to previous zooplankton surveys revealed considerable inter-annual variation in proportions of Daphnia, Bosmina and predatory cladocerans over the 1994 to 2016 period, and the strong top-down controls observed in2016were not typical.Elevated microbial production may serve as an important alternate trophic pathway supporting cladoceran populations in Toronto Harbour.

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