A new Later Upper Palaeolithic open-air site with articulated horse bone in the Colne Valley, Berkshire
The end of the last Ice Age in Britain (c. 11500 BP) created major disruption to the biosphere. Open habitats were succeeded by more wooded landscapes, and changes occurred to the fauna following the abrupt disappearance of typical glacial herd species, such as reindeer and horse (Conneller & Hi...
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Veröffentlicht in: | Antiquity 2017-12, Vol.91 (360), p.1D-7D, Article e4 |
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