R.C. Chiverrell
Ice margin oscillations during deglaciation of the northern Irish Sea Basin
Chiverrell, R.C.; Smedley, R.K.; Small, D.; Ballantyne, C.K.; Burke, M.J.; Callard, S.L.; Clark, C.D.; Duller, G.A.T.; Evans, D.J.A.; Fabel, D.; van Landeghem, K.; Livingstone, S.; Ó Cofaigh, C.; Thomas, G.S.P.; Roberts, D.H.; Saher, M.; Scourse, J.D.; Wilson, P.
Authors
R.K. Smedley
Dr David Small david.p.small@durham.ac.uk
Assistant Professor
C.K. Ballantyne
M.J. Burke
S.L. Callard
C.D. Clark
G.A.T. Duller
Professor David Evans d.j.a.evans@durham.ac.uk
Professor
D. Fabel
K. van Landeghem
S. Livingstone
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Head Of Department
G.S.P. Thomas
Professor Dave Roberts d.h.roberts@durham.ac.uk
Professor
M. Saher
J.D. Scourse
P. Wilson
Abstract
We present a new chronology to constrain ice‐margin retreat in the northern Irish Sea Basin. Estimates on the timing of ice thinning derived from surface exposure ages for boulders from the summits of the Isle of Man and south‐west Cumbria suggest that ice thinning was commensurate with the rapid retreat that followed the short‐lived advance of the Irish Sea Ice Stream (ISIS) to maximum limits in the Celtic Sea. This ice retreat in the northern Irish Sea Basin was fastest at 20 ka in response to a wider calving margin, but slowed as ice stabilized and oscillated against the Isle of Man. We provide the first age constraints for the Scottish Readvance (19.2–18.2 ka) and demonstrate that it was a potentially regional event across the Isle of Man and Cumbrian lowlands not linked with Heinrich Event 1. After the Scottish Readvance, the ice front retreated northwards towards the Southern Uplands of Scotland at the same time as climate north of ∼45°N warmed in response to summer insolation. This sequence demonstrates the importance of internal dynamics in controlling ice retreat rates in the Irish Sea, but also that deglaciation of the northern Irish Sea Basin was a response to climate warming.
Citation
Chiverrell, R., Smedley, R., Small, D., Ballantyne, C., Burke, M., Callard, S., …Wilson, P. (2018). Ice margin oscillations during deglaciation of the northern Irish Sea Basin. Journal of Quaternary Science, 33(7), 739-762. https://doi.org/10.1002/jqs.3057
Journal Article Type | Article |
---|---|
Acceptance Date | Jun 21, 2018 |
Online Publication Date | Jul 31, 2018 |
Publication Date | Oct 31, 2018 |
Deposit Date | Aug 14, 2018 |
Publicly Available Date | Aug 15, 2018 |
Journal | Journal of Quaternary Science |
Print ISSN | 0267-8179 |
Publisher | Wiley |
Peer Reviewed | Peer Reviewed |
Volume | 33 |
Issue | 7 |
Pages | 739-762 |
DOI | https://doi.org/10.1002/jqs.3057 |
Public URL | https://durham-repository.worktribe.com/output/1323449 |
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Copyright Statement
Advance online version © 2018 The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in anymedium, provided the original work is properly cited.
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