McCabe, M, Clark, P.U, Smith, D.E and Dunlop, P (2007) A revised model for the last deglaciation of eastern Scotland. Journal of the Geological Society, 164 (2). pp. 313-316. [Journal article]
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Accelerator mass spectrometry 14C ages on monospecific marine microfauna from raised mud record initial deglaciation of the eastern coast of Scotland before 21.0 cal ka bp. Two subsequent ice-margin readvances occurred prior to the Loch Lomond Advance and are identified from ice-contact deposits overlying marine mud. The Lunan Bay Readvance dates to <20.2 cal ka bp, and possibly <18.2 cal ka bp. The younger Perth Readvance occurred between c. 17.5 cal ka bp and 14.5 10Be ka. Within dating uncertainties, these readvances are similar in age to ice-margin fluctuations documented from the Irish Sea Basin and northwestern Ireland and record three near-synchronous fluctuations of much of the British–Irish Ice Sheet margin during the last deglaciation, suggesting a common response to regional climate forcing.
|Item Type:||Journal article|
|Faculties and Schools:||Faculty of Life and Health Sciences > School of Geography and Environmental Sciences|
Faculty of Life and Health Sciences
|Research Institutes and Groups:||Environmental Sciences Research Institute > Quaternary Environmental Change|
|Deposited By:||Dr Paul Dunlop|
|Deposited On:||13 Nov 2009 08:56|
|Last Modified:||15 Jun 2011 10:18|
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