2008
DOI: 10.1111/j.1365-2907.2008.00137.x
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Quaternary history of the European roe deer Capreolus capreolus

Abstract: 1. The European roe deer Capreolus capreolus is a typical faunal element of the Holocene. It was already present in Europe at least 600 000 years ago and it has been known from both glacial and interglacial phases since then. With nearly 3000 fossil and subfossil records, it is one of the most frequent mammals in the Late Quaternary.

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Cited by 68 publications
(57 citation statements)
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“…2010 for a detailed discussion). Nevertheless, it is safe to say that most of Europe was recolonized from the west after the last glaciation (in contrast, the roe deer Capreolus capreolus seems to have recolonized large European regions from the east; Sommer et al. 2009).…”
Section: Intraspecific Taxonomy and Phylogeographymentioning
confidence: 99%
“…2010 for a detailed discussion). Nevertheless, it is safe to say that most of Europe was recolonized from the west after the last glaciation (in contrast, the roe deer Capreolus capreolus seems to have recolonized large European regions from the east; Sommer et al. 2009).…”
Section: Intraspecific Taxonomy and Phylogeographymentioning
confidence: 99%
“…However, in contrast to mammals (e.g. Sommer et al, 2008Sommer et al, , 2009aSommer et al, , 2011 or the European pond turtle (Sommer et al, 2009b), the fossil record is not helpful for determining the arrival date of grass snakes in Fennoscandia. There are only few Holocene records in Denmark and Sweden.…”
mentioning
confidence: 93%
“…Several lines of evidence suggest that populations of European temperate species went extinct in the northern regions of Europe and survived in southern areas that served as refugia during the Last Glacial Maximum (LGM), followed by northward range expansions back into Europe during the interglacial warmer periods (Hewitt, 1999). The southern European peninsulas of Iberia, Italy and the Balkans (and also Turkey), as well as smaller regions such as the Carpathians and southern France, played host to those ice age refugia, and the populations in them eventually recolonized Europe, although there was probably an important inflow from eastern regions near the Caspian Sea during the recolonization process (Sommer & Benecke, 2005; Sommer & Nadachowski, 2006; Schmitt, 2007; Sommer et al. , 2008, 2009; Sommer & Zachos, 2009).…”
Section: Introductionmentioning
confidence: 99%