Unexpected early extinction of the European pond turtle (Emys orbicularis) in Sweden and climatic impact on its Holocene range |
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Authors: | ROBERT S. SOMMER&Dagger &Dagger ,CHARLOTTE LINDQVIST&dagger § § ,ARNE PERSSON&Dagger ,HENRIK BRINGSØ E§ ,ERS G. J. RHODIN¶ ,NORBERT SCHNEEWEISS,PAVEL IROKÝ &dagger &dagger ,LUTZ BACHMANN&dagger , UWE FRITZ |
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Affiliation: | Museum of Zoology, Natural History State Collections Dresden, A. B. Meyer Building, D-01109 Dresden, Germany;, Natural History Museum, University of Oslo, Blindern, N-0317 Oslo, Norway;, Department of Geology, GeoBiosphere Science Centre, Lund University, Sölvegatan 12, S-223 62 Lund, Sweden;, Irisvej 8, DK-4600 Køge, Denmark;, Chelonian Research Foundation, Lunenburg, MA 01462, USA;, Landesumweltamt Brandenburg, Naturschutzstation Rhinluch, D-16833 Linum, Germany;, Department of Biology and Wildlife Diseases, Faculty of Veterinary Hygiene and Ecology, University of Veterinary and Pharmaceutical Sciences, Palackého 1-3, CZ-612 42 Brno, Czech Republic |
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Abstract: | Using ancient DNA sequences of subfossil European pond turtles ( Emys orbicularis ) from Britain, Central and North Europe and accelerator mass spectrometry radiocarbon dating for turtle remains from most Swedish sites, we provide evidence for a Holocene range expansion of the pond turtle from the southeastern Balkans into Britain, Central Europe and Scandinavia, according to the 'grasshopper pattern' of Hewitt. Northeastern Europe and adjacent Asia were colonized from another refuge located further east. With increasing annual mean temperatures, pond turtles reached southern Sweden approximately 9800 years ago. Until approximately 5500 years ago, rising temperatures facilitated a further range expansion up to Östergötland, Sweden (approximately 58°30'N). However, around 5500 years ago pond turtle records suddenly terminate in Sweden, some 1500 years before the Holocene thermal maximum ended in Scandinavia and distinctly earlier than previously thought. This extinction coincides with a temporary cooling oscillation during the Holocene thermal maximum and is likely related to lower summer temperatures deteriorating reproductive success. Although climatic conditions improved later again, recolonization of Sweden from southern source populations was prevented by the Holocene submergence of the previous land connection via the Danish Straits that occurred approximately 8500 years ago. |
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Keywords: | ancient DNA climate Holocene phylogeography radiocarbon dating |
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