Edward Pope edward.pope@durham.ac.uk
Honorary Fellow
Long-term record of Barents Sea Ice Sheet advance to the shelf edge from a 140,000 year record
Pope, E.L.; Talling, P.J.; Hunt, J.E.; Dowdeswell, J.A.; Allin, J.R.; Cartigny, M.J.B.; Long, D.; Mozzato, A.; Stanford, J.D.; Tappin, D.R.; Watts, M.
Authors
Professor Peter Talling peter.j.talling@durham.ac.uk
Professor
J.E. Hunt
J.A. Dowdeswell
J.R. Allin
Dr Matthieu Cartigny matthieu.j.cartigny@durham.ac.uk
Associate Professor
D. Long
A. Mozzato
J.D. Stanford
D.R. Tappin
M. Watts
Abstract
The full-glacial extent and deglacial behaviour of marine-based ice sheets, such as the Barents Sea Ice Sheet, is well documented since the Last Glacial Maximum about 20,000 years ago. However, reworking of older sea-floor sediments and landforms during repeated Quaternary advances across the shelf typically obscures their longer-term behaviour, which hampers our understanding. Here, we provide the first detailed long-term record of Barents Sea Ice Sheet advances, using the timing of debris-flows on the Bear Island Trough-Mouth Fan. Ice advanced to the shelf edge during four distinct periods over the last 140,000 years. By far the largest sediment volumes were delivered during the oldest advance more than 128,000 years ago. Later advances occurred from 68,000 to 60,000, 39,400 to 36,000 and 26,000 to 20,900 years before present. The debris-flows indicate that the dynamics of the Saalian and the Weichselian Barents Sea Ice Sheet were very different. The repeated ice advance and retreat cycles during the Weichselian were shorter lived than those seen in the Saalian. Sediment composition shows the configuration of the ice sheet was also different between the two glacial periods, implying that the ice feeding the Bear Island Ice stream came predominantly from Scandinavia during the Saalian, whilst it drained more ice from east of Svalbard during the Weichselian.
Citation
Pope, E., Talling, P., Hunt, J., Dowdeswell, J., Allin, J., Cartigny, M., …Watts, M. (2016). Long-term record of Barents Sea Ice Sheet advance to the shelf edge from a 140,000 year record. Quaternary Science Reviews, 150, 55-66. https://doi.org/10.1016/j.quascirev.2016.08.014
Journal Article Type | Article |
---|---|
Acceptance Date | Aug 9, 2016 |
Online Publication Date | Aug 24, 2016 |
Publication Date | Oct 15, 2016 |
Deposit Date | Oct 24, 2016 |
Publicly Available Date | Dec 15, 2016 |
Journal | Quaternary Science Reviews |
Print ISSN | 0277-3791 |
Publisher | Elsevier |
Peer Reviewed | Peer Reviewed |
Volume | 150 |
Pages | 55-66 |
DOI | https://doi.org/10.1016/j.quascirev.2016.08.014 |
Public URL | https://durham-repository.worktribe.com/output/1372136 |
Related Public URLs | http://nora.nerc.ac.uk/id/eprint/514259/ |
Files
Published Journal Article
(3.6 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
© 2016 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
You might also like
Predicting turbidity current activity offshore from meltwater-fed river deltas
(2023)
Journal Article
Carbon and sediment fluxes inhibited in the submarine Congo Canyon by landslide-damming
(2022)
Journal Article
Longest sediment flows yet measured show how major rivers connect efficiently to deep sea
(2022)
Journal Article
Downloadable Citations
About Durham Research Online (DRO)
Administrator e-mail: dro.admin@durham.ac.uk
This application uses the following open-source libraries:
SheetJS Community Edition
Apache License Version 2.0 (http://www.apache.org/licenses/)
PDF.js
Apache License Version 2.0 (http://www.apache.org/licenses/)
Font Awesome
SIL OFL 1.1 (http://scripts.sil.org/OFL)
MIT License (http://opensource.org/licenses/mit-license.html)
CC BY 3.0 ( http://creativecommons.org/licenses/by/3.0/)
Powered by Worktribe © 2025
Advanced Search