Sara Benetti
Exploring controls of the early and stepped deglaciation on the western margin of the British Irish Ice Sheet
Benetti, Sara; Chiverrell, Richard C.; Cofaigh, Colm Ó; Burke, Matt; Medialdea, Alicia; Small, David; Ballantyne, Colin; Bateman, Mark D.; Callard, S. Louise; Wilson, Peter; Fabel, Derek; Clark, Chris D.; Arosio, Riccardo; Bradley, Sarah; Dunlop, Paul; Ely, Jeremy C.; Gales, Jenny; Livingstone, Stephen J.; Moreton, Steven G.; Purcell, Catriona; Saher, Margot; Schiele, Kevin; Van Landeghem, Katrien; Weilbach, Kasper
Authors
Richard C. Chiverrell
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
Matt Burke
Alicia Medialdea
Dr David Small david.p.small@durham.ac.uk
Assistant Professor
Colin Ballantyne
Mark D. Bateman
S. Louise Callard
Peter Wilson
Derek Fabel
Chris D. Clark
Riccardo Arosio
Sarah Bradley
Paul Dunlop
Jeremy C. Ely
Jenny Gales
Stephen J. Livingstone
Steven G. Moreton
Catriona Purcell
Margot Saher
Kevin Schiele
Katrien Van Landeghem
Kasper Weilbach
Abstract
New optically stimulated luminescence dating and Bayesian models integrating all legacy and BRITICE-CHRONO geochronology facilitated exploration of the controls on the deglaciation of two former sectors of the British–Irish Ice Sheet, the Donegal Bay (DBIS) and Malin Sea ice-streams (MSIS). Shelf-edge glaciation occurred ~27 ka, before the global Last Glacial Maximum, and shelf-wide retreat began 26–26.5 ka at a rate of ~18.7–20.7 m a–1. MSIS grounding zone wedges and DBIS recessional moraines show episodic retreat punctuated by prolonged still-stands. By ~23–22 ka the outer shelf (~25 000 km2) was free of grounded ice. After this time, MSIS retreat was faster (~20 m a–1 vs. ~2–6 m a–1 of DBIS). Separation of Irish and Scottish ice sources occurred ~20–19.5 ka, leaving an autonomous Donegal ice dome. Inner Malin shelf deglaciation followed the submarine troughs reaching the Hebridean coast ~19 ka. DBIS retreat formed the extensive complex of moraines in outer Donegal Bay at 20.5–19 ka. DBIS retreated on land by ~17–16 ka. Isolated ice caps in Scotland and Ireland persisted until ~14.5 ka. Early retreat of this marine-terminating margin is best explained by local ice loading increasing water depths and promoting calving ice losses rather than by changes in global temperatures. Topographical controls governed the differences between the ice-stream retreat from mid-shelf to the coast.
Citation
Benetti, S., Chiverrell, R. C., Cofaigh, C. Ó., Burke, M., Medialdea, A., Small, D., Ballantyne, C., Bateman, M. D., Callard, S. L., Wilson, P., Fabel, D., Clark, C. D., Arosio, R., Bradley, S., Dunlop, P., Ely, J. C., Gales, J., Livingstone, S. J., Moreton, S. G., Purcell, C., …Weilbach, K. (2021). Exploring controls of the early and stepped deglaciation on the western margin of the British Irish Ice Sheet. Journal of Quaternary Science, 36(5), 833 - 870. https://doi.org/10.1002/jqs.3315
Journal Article Type | Article |
---|---|
Acceptance Date | Mar 18, 2021 |
Online Publication Date | Jun 2, 2021 |
Publication Date | 2021-07 |
Deposit Date | Jul 30, 2021 |
Publicly Available Date | Jul 30, 2021 |
Journal | Journal of Quaternary Science |
Print ISSN | 0267-8179 |
Electronic ISSN | 1099-1417 |
Publisher | Wiley |
Peer Reviewed | Peer Reviewed |
Volume | 36 |
Issue | 5 |
Pages | 833 - 870 |
DOI | https://doi.org/10.1002/jqs.3315 |
Public URL | https://durham-repository.worktribe.com/output/1243848 |
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http://creativecommons.org/licenses/by/4.0/
Copyright Statement
Advance online version This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
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