Published March 9, 2020 | Version v1
Journal article Open

Diverse responses of common vole (Microtus arvalis) populations to Late Glacial and Early Holocene climate changes - Evidence from ancient DNA

  • 1. Centre of New Technologies, University of Warsaw, S. Banacha 2c, 02-097, Warsaw, Poland
  • 2. Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Sławkowska 17, 31-016, Krakow, Poland
  • 3. Museum and Institute of Zoology, Polish Academy of Sciences, Wilcza 64, 00-679, Warsaw, Poland
  • 4. Department of Zoology, Charles University, Vinicna 7, 128 44, Prague, Czech Republic
  • 5. IPHES, Institut Catala de Paleoecologia Humana i Evolucio Social, Zona Educacional, 4 e Campus Sescelades URV (Edifici W3), 43007, Tarragona, Spain
  • 6. MTA-MTM-ELTE Research Group for Palaeontology, Ludovika ter 2, 1083, Budapest, Hungary
  • 7. Laboratoire departemental de Prehistoire du Lazaret, CEPAM, UMR 7264 CNRS, 24, Avenue des Diables Bleus F - 06357 Nice Cedex 4, France
  • 8. TRACES, UMR 5608 (CNRSdUniversite Toulouse le Mirail), 5, Allees Antonio Machado, F 31058, Toulouse cedex 9, France
  • 9. Institute of Archaeology, University of Warsaw, Krakowskie Przedmiescie 26/28, 00-927, Warsaw, Poland
  • 10. Institute for Quaternary Palaeontology and Geology, Croatian Academy of Sciences and Arts, Ante Kovacica 5, 10000, Zagreb, Croatia
  • 11. Dept. Estratigrafía y Paleontología, Facultad de Ciencias, Universidad del País Vasco, Barrio de Sarriena, s/n 48940 Leioa (Bizkaia), Apdo. 644, 48080, Bilbao, Spain
  • 12. Aragosaurus-IUCA-Earth Sciences Dpt, University of Zaragoza, C/Pedro Cerbuna 12, 50009, Zaragoza, Spain
  • 13. Institute of Archaeology, Faculty of History, Nicolaus Copernicus University, Szosa Bydgoska 44/48, 87-100, Torun, Poland
  • 14. Natural History Museum, Njegoseva 51, 11000, Belgrade, Serbia
  • 15. Institute of Speleology "E. Racovitza", 13 Septembrie 13, 050711, Sector 5, Bucharest, Romania
  • 16. Department of Archaeology, Anthropology and Geography, University of Winchester, Winchester, SO22 4NR, United Kingdom
  • 17. Faculty of Science and Technology, Bournemouth University, Fern Barrow, Poole, Dorset, BH12 5BB, United Kingdom

Description

The harsh climatic conditions during the Last Glacial Maximum (LGM) period have been considered the cause of local extinctions and major faunal reorganizations that took place at the end of the Pleistocene. Recent studies have shown, however, that in addition many of these ecological events were associated with abrupt climate changes during the so-called Late Glacial and the Pleistocene/Holocene transition. Here we used ancient DNA to investigate the impact of those changes on European populations of
temperate vole species (Microtus arvalis). The genetic diversity of modern populations and the fossil record suggests that the species may have survived cold episodes, like LGM, not only in the traditional Mediterranean glacial refugia but also at higher latitudes in cryptic northern refugia located in Central France, the northern Alps as well as the Carpathians. However, the details of the post-glacial recolonization and the impact of the Late Glacial and Early Holocene climate changes on the evolutionary history
of the common vole remains unclear. To address this issue, we analysed mtDNA cytochrome b sequences from more than one hundred common vole specimens from 36 paleontological and archaeological sites scattered across Europe. Our data suggest that populations from the European mid- and high latitudes suffered a local population extinction and contraction as a result of Late Glacial and Early Holocene climate and environmental changes. The recolonization of earlier abandoned areas took place in the Mid to Late Holocene. In contrast, at low latitudes, in Northern Spain there was a continuity of common vole populations. This indicates different responses of common vole populations to climate and environmental changes across Europe and corroborates the hypothesis that abrupt changes, like those associated with Younger Dryas and the Pleistocene/Holocene transition, had a significant impact on populations at the mid- and high latitudes of Europe.

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