“…Over the last few decades, sea surface temperatures (SST) have significantly increased along this coastline, while five interspersed upwelling areas (west coast of Portugal, Strait of Gibraltar, Cape Ghir, Cape Juby and north of Cape Blanc) show lower or non‐significant temperature increase and rather, in some cases, cooling trends (Lima & Wethey, ), offering natural experimental replicates. Importantly, these shores are a biogeographical transition region where several warm‐ and cold‐water species reach their northern or southern range limits (Lima et al ., ; Lourenço et al ., ; Rubal et al ., ), therefore offering the opportunity for early identification of distributional expansions and contractions (Lima et al ., , ; Nicastro et al ., ; Neiva et al ., ).…”