“…Environmental variability associated with the glacial‐interglacial cycles of the Late Quaternary predating the appearance of modern climatic conditions (~11.5 ky before present) have been recurrently invoked to explain present‐day phylogeographic patterns in a variety of living organisms (e.g., Maggs et al., ; Randi, ). For instance, colder water conditions around the tip of South Africa during glacial periods, and the presence of the cold Benguela current during warm interglacial periods have been proposed to explain Atlantic versus Indo‐Pacific isolation and mitochondrial lineage divergence in warm‐temperate and tropical sharks, such as in cosmopolitan oceanic epipelagic species (e.g., R. typus, Vignaud et al., ; C. falciformis, Clarke et al., ) and in many cosmopolitan coastal pelagic carcharhinoids (e.g., C. limbatus, Keeney & Heist, ; Keeney, Heupel, Hueter, & Heist, ; Carcharhinus obscurus (Lesueur, 1818) Benavides et al., ; Carcharhinus plumbeus (Nardo, 1827) , Portnoy, McDowell, Heist, Musick, & Graves, ; Carcharhinus brachyurus (Günther, 1870), Benavides et al., ; Benavides et al., ; Galeocerdo cuvier (Péron & Lesuer, 1822) Bernard et al., ; Sphyrna lewini (Griffith & Smith, 1834), Duncan, Martin, Bowen, & De Couet, ; Daly‐Engel et al., ). Lineage divergence associated with between‐ocean cessation of gene flow in temperate species with wide temperature ranges, such as the blue shark, may also have occurred during periods when water temperatures around South Africa went below their thermal tolerance limit.…”