Timing and pace of ice‐sheet withdrawal across the marine–terrestrial transition west of Ireland during the last glaciation

Colm Ó Cofaigh, S. Louise Callard, David H. Roberts, Richard C. Chiverrell, C. K. Ballantyne, David J. A. Evans, Margot Saher, Katrien J. J. Van Landeghem, Rachel Smedley, Sara Benetti, Matthew Burke, Chris D. Clark, Geoff A. T. Duller, Derek Fabel, Stephen J. Livingstone, Stephen Mccarron, Alicia Medialdea, Steven G. Moreton, Fabio Sacchetti

Research output: Contribution to journalArticlepeer-review

8 Citations (Scopus)
18 Downloads (Pure)

Abstract

ABSTRACT: Understanding the pace and drivers of marine‐based ice‐sheet retreat relies upon the integration of numerical ice‐sheet models with observations from contemporary polar ice sheets and well‐constrained palaeo‐glaciological reconstructions. This paper provides a reconstruction of the retreat of the last British–Irish Ice Sheet (BIIS) from the Atlantic shelf west of Ireland during and following the Last Glacial Maximum (LGM). It uses marine‐geophysical data and sediment cores dated by radiocarbon, combined with terrestrial cosmogenic nuclide and optically stimulated luminescence dating of onshore ice‐marginal landforms, to reconstruct the timing and rate of ice‐sheet retreat from the continental shelf and across the adjoining coastline of Ireland, thus including the switch from a marine‐ to a terrestrially‐based ice‐sheet margin. Seafloor bathymetric data in the form of moraines and grounding‐zone wedges on the continental shelf record an extensive ice sheet west of Ireland during the LGM which advanced to the outer shelf. This interpretation is supported by the presence of dated subglacial tills and overridden glacimarine sediments from across the Porcupine Bank, a westwards extension of the Irish continental shelf. The ice sheet was grounded on the outer shelf at ~26.8 ka cal bp with initial retreat underway by 25.9 ka cal bp. Retreat was not a continuous process but was punctuated by marginal oscillations until ~24.3 ka cal bp. The ice sheet thereafter retreated to the mid‐shelf where it formed a large grounding‐zone complex at ~23.7 ka cal bp. This retreat occurred in a glacimarine environment. The Aran Islands on the inner continental shelf were ice‐free by ~19.5 ka bp and the ice sheet had become largely terrestrially based by 17.3 ka bp. This suggests that the Aran Islands acted to stabilize and slow overall ice‐sheet retreat once the BIIS margin had reached the inner shelf. Our results constrain the timing of initial retreat of the BIIS from the outer shelf west of Ireland to the period of minimum global eustatic sea level. Initial retreat was driven, at least in part, by glacio‐isostatically induced, high relative sea level. Net rates of ice‐sheet retreat across the shelf were slow (62–19 m a−1) and reduced (8 m a−1) as the ice sheet vacated the inner shelf and moved onshore. A picture therefore emerges of an extensive BIIS on the Atlantic shelf west of Ireland, in which early, oscillatory retreat was followed by slow episodic retreat which decelerated further as the ice margin became terrestrially based. More broadly, this demonstrates the importance of localized controls, in particular bed topography, on modulating the retreat of marine‐based sectors of ice sheets.
Original languageEnglish
Pages (from-to)805-832
Number of pages28
JournalJournal of Quaternary Science
Volume36
Issue number5
Early online date7 Apr 2021
DOIs
Publication statusE-pub ahead of print - 7 Apr 2021

Bibliographical note

Funding Information:
This research was funded by the UK Natural Environment Research Council grant NE/J007196/1 ?Britice-Chrono?. The work was supported by the NERC Radiocarbon Facility (Allocation No. 1722.0613 and 1878.1014). Thanks are due to the staff at the SUERC AMS Laboratory, East Kilbride, for carbon isotope measurements, and to Sally Morgan and Elke Hanenkamp (University of Leicester) for acquisition and processing of the multi-sensor core-logger data. We gratefully acknowledge the Irish Marine Institute and the Geological Survey of Ireland for access to the INSS and INFOMAR multibeam datasets. We thank the officers and crew of the RRS James Cook for their assistance with data acquisition, as well as the British Geological Survey and UK National Oceanography Centre for vibro- and piston core collection, respectively, during cruise JC106. We are grateful to Caroline Clason and an anonymous reviewer whose helpful comments led to improvements to the manuscript.

Publisher Copyright:
© 2021 The Authors. Journal of Quaternary Science Published by John Wiley & Sons Ltd.

Keywords

  • Earth and Planetary Sciences (miscellaneous)
  • Palaeontology
  • Arts and Humanities (miscellaneous)
  • ice sheet retreat
  • British–Irish Ice Sheet
  • radiocarbon dating
  • Last Glacial Maximum
  • Special Issue Articles
  • Porcupine Bank
  • glacimarine sediments
  • Special Issue Article
  • ice sheet extent
  • subglacial till
  • western Ireland

Fingerprint

Dive into the research topics of 'Timing and pace of ice‐sheet withdrawal across the marine–terrestrial transition west of Ireland during the last glaciation'. Together they form a unique fingerprint.

Cite this