McCabe, AM and OCofaigh, C (1996) Upper pleistocene facies sequences and relative sea-level trends along the south coast of Ireland. JOURNAL OF SEDIMENTARY RESEARCH, 66 (2, Par). pp. 376-390. [Journal article]
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Upper Pleistocene sequences, deposited around 20 ka provide a record of sedimentation during the last glacial/deglacial cycle along the south coast of Ireland. A stratigraphy based on eight lithofacies associations is recognized. Typically, the facies sequences overlie a glaciated shore platform furrowed by subglacial meltwaters. Elements within the stratigraphy comprise: (1) ice advance southwards onto the continental shelf; (2) stagnation-zone retreat triggered by rising sea level related to isostatic depression coupled with subglacial meltwater events that furrowed the platform; (3) progressive rise in relative sea level recorded by a submergent facies sequence on an isostatically depressed slope (beach gravels -->2 subaqueous jet afflux sediments -->2 wave-influenced sands -->2 glaciomarine mud drape); ice-marginal oscillation is recorded by glaciotectonically deformed gravels, sands, and foliated diamict; (4) terrestrial emergence is marked by angular breccias derived from local slopes by periglacial weathering. There is a clear facies transition between the breccias and underlying wave-influenced sands. Facies sequences suggest that the local deglacial cycle was out of phase with the global eustatic cycle along the south coast of Ireland. Stagnation-zone retreat was largely dependent on magnitudes of isostatic depression, high relative sea level, and meltwater events, and not on climatic 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|
Environmental Sciences Research Institute
|Deposited By:||Mrs Linda Allen|
|Deposited On:||04 Sep 2012 11:07|
|Last Modified:||04 Sep 2012 11:07|
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