Late Pleistocene chronostratigraphy and ice sheet limits, southern Ireland

The morpho-stratigraphic subdivision of the surficial glacial drifts of Ireland into \'Older Drift\' and \'Younger Drift\' is a long-standing convention in Irish Quaternary studies. Across southern Ireland a broad swath of terrain has traditionally been interpreted as Munsterian (penultimate glaciation) in age and large end moraine complexes bordering this zone of \'Older Drift\' such as the \'South Ireland End Moraine\' have long been regarded as marking the limit of the Late Midlandian (last glaciation) ice sheet. Sedimentary sequences exposed along the south coast of Ireland provide a window into the stratigraphy of the \'Older Drift\' and have been studied for over a century. The present paper supports a fundamental revision of the traditional interpretation of ice sheet limits in southern Ireland and argues for an extensive last Irish Ice Sheet which covered much of the area of the Older Drift at the Last Glacial Maximum. The basis for this revision is threefold. Firstly, nineteen new optically stimulated luminescence (OSL) dates on the Courtmacsherry Raised Beach and overlying shallow marine sands demonstrate that on the south coast the beach and shallow marine sands formed during marine isotope stages 4-3. Secondly, AMS radiocarbon dates on reworked shells from the \'Irish Sea Till\', demonstrate that this till and overlying \'inland\' tills from central and SW Ireland were formed after ~24. cal. ka. BP. Thirdly, new OSL dates of 24-21. ka. BP from deglacial outwash overlying the Irish Sea Till. Collectively these data are consistent with a last glaciation age for the glacigenic sequence along the south coast of Ireland, thus supporting a fundamental revision of the age of the Older (Munsterian) Drifts of southern Ireland. Most of southern Ireland was glaciated during the LGM and the moraine belts which have traditionally been interpreted as marking the last glacial limit such as the South Ireland End Moraine are reinterpreted here as recessional features formed during ice sheet retreat. © 2010 Elsevier Ltd.