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A revised model for the last deglaciation of eastern Scotland.

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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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URL: http://jgs.geoscienceworld.org/cgi/content/abstract/164/2/313

DOI: 10.1144/0016-76492006-120


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
Faculty of Life and Health Sciences > School of Environmental Sciences
Research Institutes and Groups:Environmental Sciences Research Institute > Quaternary Environmental Change
ID Code:495
Deposited By:Dr Paul Dunlop
Deposited On:13 Nov 2009 08:56
Last Modified:15 Jun 2011 11:18

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