Capelin (Mallotus villosus) spawning behaviour in Newfoundland waters-the interaction between beach and demersal spawning

By B. Nakashima, J. Wheeler. 2002

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Capelin (Mallotus villosus) distribution and climate: a sea “canary” for marine ecosystem change (2005, unknown): “…Spawning ReferencesDepth Temperature Start End Depth Temperature Salinity NL coastal 1 to 450 1.5 to 6 ( 1 to 2) 6 7 0 to 10 3.5 to 10 14 to 33 Nakashima and Wheeler, 2002; unpubl. data Grand Bank 1 to 250 1.5 to 6 ( 1 to 2) 6 7 40 to 50 2 to 5 34 to 35 Carscadden et al., 1989; unpubl. data…”
Shoal behaviour and maturity relations of spawning capelin (Mallotus villosus )o ff Newfoundland: demersal spawning and diel vertical movement patterns (2006, methodology): “Additionally, determining the potential spatial extent of demersal spawning in coastal Newfoundland is important and may be possible using available data on bathymetry, historical temperature, and substrate types and distribution in coastal Newfoundland.”
Comparative ecology of widely distributed pelagic fish species in the North Atlantic: Implications for modelling climate and fisheries impacts (2014, background): “Spawning mainly occurs in March–April in the Barents Sea and around Iceland and in May–July in the NW Atlantic stocks (Vilhjálmsson, 1994; Nakashima and Wheeler, 2002).”
Consequences of foraging trip duration on provisioning behaviour and fledging condition of common murres Uria aalgae (2003, background): “Nakashima and Wheeler 2002 ) and provide dense aggregations of prey for breeding seabirds, large piscivorous fishes and marine mammals.”