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The full programme book (PDF) - Royal Geographical Society

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T9<br />

Island Evolution: a ‘front-line’ biotic response to sea-level change<br />

Victoria Herridge 1 , David Richards 2 , Jean-Luc Schwenninger 3 , Ed Rhodes 4 , Kirsty<br />

Penkman 5 and Adrian Lister 1 .<br />

1 Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD<br />

2 School of <strong>Geographical</strong> Sciences, University of Bristol, University Road, Bristol, BS8 1SS<br />

3 Research Laboratory of Archaeology and the History of Art, University of Oxford, South Parks Road,<br />

Oxford, OX1 3QY<br />

4 Department of Earth and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA<br />

5 Department of Chemistry, University of York, York, YO10 5DD<br />

Island biodiversity is closely related to island area and distance from the mainland two<br />

characters unquestionably linked with eustatic sea level. Additionally, island populations<br />

typically have high evolutionary rates and are characterized by endemic and often unusual<br />

flora and fauna that are vulnerable to extinction. Thus we might expect island faunas to be<br />

affected to a greater extent, and at a faster rate, than those of the mainland – forming the<br />

‘front-line’ of biotic response to global sea-level change. Quaternary island systems show<br />

great potential for quantifying the evolutionary response of faunas to climatically driven<br />

environmental and associated sea-level changes characteristic of that period (Siddall et al<br />

2003). A widespread evolutionary response of insular Quaternary large mammals is<br />

extreme body size reduction (e.g. 100 kg elephant Palaeoloxodon falconeri on Sicily and<br />

Malta descended from 10,000 kg mainland species, P. antiquus). This phenomenon is<br />

usually ‘explained’ by the ‘Island Rule’, whereby small mammals become large and large<br />

mammals dwarf on islands. A paucity of geochronological information has hampered the<br />

consideration of insular body-size change within the context of the climatic fluctuations of<br />

the Quaternary, despite the fact that island conditions are significantly affected by climate<br />

and sea-level changes. Using new evidence, we make a preliminary assessment of the<br />

role that sea-level change may have played in driving the evolution of Mediterranean<br />

dwarf elephant and dwarf deer.

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