Macroecology of Calanus finmarchicus and C. helgolandicus in the North Atlantic Ocean and adjacent seas

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The North Atlantic Ocean as habitat for Calanus finmarchicus: Environmental factors and life history traits (2014, methodology): “These temperature limits were chosen because based 13 on CPR observations (Helaouët and Beaugrand, 2007) that the optimal thermal habitat for C.”
Cod and climate in a latitudinal cline: physiological analyses of climate effects in marine fishes (2008, background): “More recently, the distribution shifts of the 2 copepod species themselves proved to be largely determined by warming effects (Helaouët & Beaugrand 2007), reflecting the different thermal windows of the 2 copepod species.”
Physiology, Ecological Niches and Species Distribution (2009, background): “Indeed, the spatial distribution of C. finmarchicus clearly matches the subpolar gyre and is limited by the Oceanic Polar Front (Dietrich 1964) and associated oceanic currents (Krauss 1986; Helaouët and Beaugrand 2007).”
Future climate‐driven shifts in distribution of Calanus finmarchicus (2011, methodology): “Helaouët & Beaugrand (2007) showed that SST was a controlling factor affecting the spatial distribution of the species.”
Rapid biogeographical plankton shifts in the North Atlantic Ocean (2009, background): “Providing that the thermal preferendum of a species is identified (Helaouët & Beaugrand, 2007; Beaugrand & Helaouët, 2008), forecasting might become possible.”