Late Quaternary distribution dynamics and phylogeography of the red deer (Cervus elaphus) in Europe
Late Quaternary distribution dynamics and phylogeography of the red deer (Cervus elaphus) in Europe
复制标题
欧洲马鹿晚第四纪分布动态和系统发育地理学
DOI:
10.1016/j.quascirev.2007.11.016
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发表时间:
2008
影响因子:
4
通讯作者:
N. Benecke
中科院分区:
文献类型:
--
作者:
R. Sommer;F. Zachos;M. Street;O. Jöris;Anna Skog;N. Benecke
Here we present spatial–temporal patterns for European late Quaternary red deer (Cervus elaphus), based on radiocarbon-supported evidence derived mainly from archaeological sites. This is followed by an overview of the recent phylogeography of this species using haplogroup studies of recent molecular data. The implications of the synthesis of palaeontological and genetic data are discussed and we propose that present day European red deer haplogroup distributions are best explained against the history of late Quaternary population contractions into and expansions from glacial refugia. Around 800 records of Cervus elaphus were assigned to the period covering the later part of the Last Glacial and the Early to Middle Holocene. Red deer becomes increasingly visible in faunal assemblages dated to late OIS-3 (<40.0ka14CBP). The species persisted throughout the LGM on the Iberian Peninsula, in adjacent regions of South-Western France (Gascony, Dordogne, Languedoc), on the Italian Peninsula, in the Balkans and Greece, and east of the Carpathians in Moldavia. We suggest that genetic exchange between the populations of the Balkans and the East of the Carpathians remained uninterrupted during the LGM. The expansion of red deer from its southern refugia into Central and Northern Europe begins rapidly at 12,50014CBP. The expansion of red deer coincides with the sudden rise in temperature at the onset of Greenland Interstadial 1e and the dispersion of open birch woodland into the northern half of Europe. Radiocarbon supported records show a more or less universal distribution of Cervus elaphus across Europe following the Pleistocene/Holocene climatic change at 10.0ka14CBP for the first time. Molecular data and fossil record combined provide a clearer temporal and spatial pattern for the Lateglacial recolonisation process of the northern part of Europe.