A. Marshall McCabe's research while affiliated with Ulster University and other places

... Glacial landforms deposited in the Late Pleistocene potentially continued to evolve for some time during the Early Holocene, as observed in Carrawaystick cirque (Kelly's Lough) beneath Corrigasleggaun (794 m) in the Wicklow Mountains. Early Holocene 10 Be exposure ages from an inner cirque moraine (n 5 2; c.9.6 ka; Barth et al., 2018) indicate a c.1À2 ka period of moraine stabilisation following initial ice-free conditions (n 5 3; c.11.7 ka), consistent with wider evidence from unconsolidated glacial landforms (Putkonen and Swanson, 2003;Briner et al., 2005;Dortch et al., 2010). Other landscape elements may have adjusted even more rapidly to nonglacial conditions (10 1 À10 2 years; Ballantyne, 2002), as indicated by low rates of rockfall (Ballantyne and Kirkbride, 1987;Ballantyne and Harris, 1994) and rock slope failure activity in the Holocene when compared to the Late-glacial period (Ballantyne et al., 2014). ...

... Up-ice of the onset zone at Lake Rogen, the patchy distribution of streamlined landforms suggests that sliding was restricted to slippery spots. These patterns, together with the wider spacings of ribbed moraines ridges down-ice, indicate significant basal shearing gradients and extensional ice flow towards the west (Finlayson & Bradwell, 2008;Knight & McCabe, 1997). ...

... In comparison with other Pleistocene deposits containing R. globulifera, the environment can be characterized as glaciomarine, neritic, nearshore, estuarine with reduced salinities at 0.5-2.5°C (McCabe & Clark 1998). Since this reddish-grey clay with its unique fauna is widely distributed in NE Germany we here propose the name Roundstonia clay. ...

... The first of these was from its short-lived advance into the Celtic Sea and the second from the northern most part of the North Sea losing connection with the FIS in this region (Bradwell et al., 2019;Chiverrell et al., 2013). The ice sheet rapidly retreated northward across southern Ireland, leaving much of the region deglaciated (Barth et al., 2016;Ó Cofaigh et al., 2012). The exception was the Kerry-Cork region which was covered by an isolated ice cap, the Kerry-Cork Ice Cap ( Figure 1C) until its disappearance ca. ...

... The fact that ice is now known to have completely covered Ireland in the LGC does raise doubts about the presence of surface glacial features relating to this penultimate glacial cycle. In terms of deposits, it is likely that deposits previously interpreted Munsterian are in fact Midlandian in age (Warren, 1985;Eyles and McCabe, 1991;Coxon 1993). ...

... In particular, this reconstruction showed that, after a period of ice retreat, the remaining ice masses readvanced during what Synge (1969) referred to as the Drumlin Readvance, providing the first evidence of a dynamic ice sheet that experienced substantial changes in ice flow. Subsequent work documented further evidence for large-scale changes in ice flow during the last deglaciation , and detailed stratigraphic and geochronologic investigations documented widespread fluctuations of the IIS margin that corresponded to North Atlantic abrupt climate changes (Bowen et al., 1996(Bowen et al., , 2002McCabe and Clark, 1998;McCabe et al., 2005McCabe et al., , 2007bClark et al., 2009a;Clark et al., 2009b). ...

... The occurrence of undeformed stratified sediments in 713 drumlins has long been recognised (section 3.5) and a large body of work has drawn 714 attention to their presence, specifically at the lee-side of drumlins (e.g. Dardis and 715McCabe, 1983;Dardis et al., 1984;Dardis, 1987;Dardis and McCabe, 1987; Hanvey, 716 1989 Hanvey, 716 , 1992;Dardis and Hanvey, 1994;Fisher and Spooner, 1994). 717Investigating a relatively large sample of drumlins (55 in total) compared to most 718 studies,Dardis et al. (1984) describe several lee-side stratified sequences, see 719 example in ...

... It was typically dull, with thicknesses varying from 10 to 25 cm. The peat beds suggested that the plant sedimentation occurred rapidly in humid paleoclimate (e.g., McCabe et al., 1984;McCabe, 2009). This facies might also derive from a back swamp with persistent, slow-receding, moderate drainage, and plenty of vegetation (Diessel, 1992). ...

... Nonetheless, studies indicate climatic transition and enhanced period of sediment reworking. The studies were further supported by sedimentary transformations through fluvial activity and slope processes for shorter time scale (Jackson et al. 1982;Eyles et al. 1988;Harrison 1991;Wright 1991). The relevance of such paraglacial processes in deciphering the post-glacial climatic changes is obviously the objective of geoscientists to quantify the post glacial rapid palaeoclimatic changes. ...

... cal a BP (McCabe and Clark, 1998;Ballantyne and Ó Cofaigh, 2017)] and (ii) the East Antrim Coastal Readvance of Scottish Ice [occurring either at c. 16.5k cal a BP (Finlayson et al., 2014) or c. 15.6-15.0k cal a BP (McCabe and Williams, 2012)]. The latter shaped much of the drumlinized landscape. ...