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Geological Society, London, Special Publications; 1995; v. 96; p. NP;
DOI: 10.1144/GSL.SP.1995.096.01.17
© 1995 Geological Society of London

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About this title

It is generally believed that Britain last became separated from mainland Europe about 8500 years ago, although earlier stages of the Quaternary are also considered in this book. The evidence for insularity, or otherwise, of both Britain and Ireland is based on a wide range of data, reflecting the multidisciplinary nature of Quaternary research.

This volume provides up-to-date reviews of this evidence: physical or geological, and palaeontological data, as well as marine and non-marine organisms, are examined. Also evaluated are the possible biological repercussions of insularity: the fauna and flora of Britain and Ireland are certainly impoverished when compared with neighbouring mainland European countries - see, for example, the spectacular ecological and evolutionary consequences on the red deer populations of Jersey.