Late‐glacial recolonization and phylogeography of E uropean red deer ( C ervus elaphus L .)
Abstract The Pleistocene was an epoch of extreme climatic and environmental changes. How individual species responded to the repeated cycles of warm and cold stages is a major topic of debate. For the European fauna and flora, an expansion–contraction model has been suggested, whereby temperate spec...
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Published in | Molecular ecology Vol. 22; no. 18; pp. 4711 - 4722 |
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Main Authors | , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
01.09.2013
|
Online Access | Get full text |
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Summary: | Abstract
The Pleistocene was an epoch of extreme climatic and environmental changes. How individual species responded to the repeated cycles of warm and cold stages is a major topic of debate. For the European fauna and flora, an expansion–contraction model has been suggested, whereby temperate species were restricted to southern refugia during glacial times and expanded northwards during interglacials, including the present interglacial (
H
olocene). Here, we test this model on the red deer (
C
ervus elaphus
) a large and highly mobile herbivore, using both modern and ancient mitochondrial
DNA
from the entire European range of the species over the last
c
. 40 000 years. Our results indicate that this species was sensitive to the effects of climate change. Prior to the
L
ast
G
lacial
M
aximum (
LGM
) haplogroups restricted today to
S
outh‐
E
ast
E
urope and
W
estern Asia reached as far west as the
UK
. During the
LGM
, red deer was mainly restricted to southern refugia, in Iberia, the Balkans and possibly in Italy and
S
outh‐
W
estern
A
sia. At the end of the
LGM
, red deer expanded from the Iberian refugium, to
C
entral and
N
orthern
E
urope, including the
UK
,
B
elgium,
S
candinavia,
G
ermany,
P
oland and
B
elarus. Ancient
DNA
data cannot rule out refugial survival of red deer in
N
orth‐
W
est
E
urope through the
LGM
. Had such deer survived, though, they were replaced by deer migrating from Iberia at the end of the glacial. The Balkans served as a separate
LGM
refugium and were probably connected to
W
estern
A
sia with genetic exchange between the two areas. |
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ISSN: | 0962-1083 1365-294X |
DOI: | 10.1111/mec.12420 |