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. 2018 Jul 6;111(12):2323–2347. doi: 10.1007/s10482-018-1123-8

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© The Author(s) 2018

Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.

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Fig. 1 — Origin of isolates used in this study: 1—Bardufoss, Målselv, Norway (69°4′5.54″N, 18°28′46.01″E); 2—Rudda, Kvæfjord, Norway (68°42′14.36″N, 16°18′33.53″E); 3—Syverud, Ås, Norway (59°41′20.79″N, 10°45′10.18″E); 4—Tagtvedt, Larvik, Norway (59°3′37.00″N 10°4′6.68″)E; 5—Resko, Poland (53°45′56.18″N, 15°25′19.25″E); 6—Babimost, Poland (52°10′23.42″N, 15°48′37.38″E); 7—Sopotnia, Poland (49°35′39.54″N, 19°16′39.02″E) 8—Zabierzów, Poland (50°6′26.01″N, 19°46′11.71″E); 9—Ispina, Poland (50°6′20.61″N, 20°22′11.85″E); 10—Wierzchosławice, Poland, 50°2′21.06″N, 20°48′49.32″E, 11—Rozpucie, Poland (49°34′59.71″N, 22°24′19.38″E)