“…Both palaeobotanical and molecular data have provided evidence that southern margins of the European continent acted as refugia for many European tree species in Late Pleniglacial (LPG; 24–14.6 ka) during which the most extreme glacial conditions prevailed and the Scandinavian Ice Sheet (SIS) attained its maximal size. However, in the case of some species, a specific set of life history traits may have enabled them to maintain additional refugial populations sparsely distributed closer to the ice margins (Bhagwat & Willis, ; Dering, Latałowa, Boratyńska, Kosiński, & Boratyński, ). This idea of northern refugia has been a subject of vivid debate for over a decade, during which supporting arguments of enthusiasts and doubts of sceptics have been colliding (de Lafontaine, Amasifuen Guerra, Ducousso, & Petit, ; Parducci et al., ; Tzedakis, Emerson, & Hewitt, ; Willis & van Andel, ).…”