Final deglaciation of the Malin Sea through meltwater release and calving events.

• Published in: Scottish Journal of Geology
• Main Authors: Tarlati, S., Benetti, S., Callard, S.L., Ó Cofaigh, C., Dunlop, P., Georgiopoulou, A., Edwards, R., Van Landeghem, K., Saher, M., Chiverrell, R., Fabel, D., Moreton, S., Morgan, S., Clark, C.D.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Geological Society 2020
• Subjects: Barra; Ice Sheet; Neogloboquadrina pachyderma
• Online Access: http://dro.dur.ac.uk/30802/; http://dro.dur.ac.uk/30802/1/30802.pdf; https://doi.org/10.1144/sjg2019-010

During the last glacial maximum, the British–Irish Ice Sheet (BIIS) extended to the shelf edge in the Malin Sea between Ireland and Scotland, delivering sediments to the Donegal Barra Fan (DBF). Analysis of well-preserved, glacially derived sediment in the DBF provides new insights on the character...