“…Previous studies have demonstrated the importance of oceanographic structures to these spawning activities, as well as the direct effects of temperature, salinity and other abiotic factors (Bakun, 2006; Brunel et al., 2017; Kloppmann et al., 2001; Lough et al., 1996). For example, most of the intense spawning areas of SPF appear within regions of high zooplankton productivity, which are associated with the main upwelling areas or meso‐scale hydrodynamic structures such as eddies and ocean fronts (Aceves‐Medina et al., 2009; Baldé et al., 2019; Peck et al., 2013; Somarakis & Nikolioudakis, 2007). However, some SPF use different spawning strategies to avoid the strong passive transport of their eggs and larvae or the strong turbulence and instability of the water column in some intense upwelling systems (Dias et al., 2014; Lluch‐Belda et al., 1991; Parrish et al., 1981; Tiedemann et al., 2017), suggesting that SPF show adaptive phenotypic characteristics in different oceanographic systems.…”