“…During the late Pleistocene, when American and Northwestern mtDNA are estimated to have diverged ~ 443,000 years ago, North America was undergoing extensive glacial advances and retreats at regular ~ 100,000‐year Croll‐Milankovich intervals (Clark et al, 2009; Muller & MacDonald, 1997). Much of the Pacific Northwest was covered in ice sheets during the glacial periods, isolating terrestrial organisms south of the ice sheets or in ice‐free northern refugia such as Beringia, Haida Gwaii, or the Alexander Archipelago (Anderson, Hu, Nelson, Petit, & Paige, 2006; Burg, Gaston, Winker, & Friesen, 2006; Galbreath & Cook, 2004; Geraldes et al, 2019; Godbout, Fazekas, Newton, Yeh, & Bousquet, 2008; Shafer, Cullingham, Côté, & Coltman, 2010). During the interglacial periods, terrestrial organisms expanded from refugial populations into newly ice‐free habitats, leading to secondary contact and potentially renewed gene flow between closely related, previously allopatric forms (Shafer et al, 2010).…”