“…These species might benefit from nutrient incorporation (200–400 km out at sea) through advection processes (cyclone gyres or jets) and subarctic flow at large scales (Bernal & Chelton, ; Chelton, , ), as has been suggested to explain zooplankton biomass increases in oceanic zones (Bernal, , ; Bernal & McGowan, ; Chelton, , ). In the oceanic area of the southern part of the CCS, assemblage structures of mesopelagic larvae are highly variable and influenced by cold and warm conditions associated with La Niña and El Niño events, but these structures principally varied on a seasonal basis (Funes‐Rodríguez, Hinojosa‐Medina, Aceves‐Medina, Jiménez‐Rosenberg, & Bautista‐Romero, ; Funes‐Rodríguez, Zárate‐Villafranco, Hinojosa‐Medina, & González‐Armas, ; Funes‐Rodríguez et al., ). In the present study, a large amount of data were used, and these were sampled over a wide spatiotemporal range.…”