S.J. Livingstone
Subglacial processes on an Antarctic ice stream bed. 1: Sediment transport and bedform genesis inferred from marine geophysical data
Livingstone, S.J.; Stokes, C.R.; O Cofaigh, C.; Hillenbrand, C-D.; Vieli, A.; Jamieson, S.S.R.; Spagnolo, M.; Dowdeswell, J.
Authors
Professor Chris Stokes c.r.stokes@durham.ac.uk
Professor
Professor Colm O'Cofaigh colm.ocofaigh@durham.ac.uk
Professor
C-D. Hillenbrand
A. Vieli
Professor Stewart Jamieson stewart.jamieson@durham.ac.uk
Professor
M. Spagnolo
J. Dowdeswell
Abstract
The spatial pattern and morphometry of bedforms and their relationship to sediment thickness have been analysed in the Marguerite Bay Palaeo-ice stream Trough, western Antarctic Peninsula. Over 17 000 glacial landforms were measured from geophysical datasets, and sediment thickness maps were generated from acoustic sub-bottom profiler data. These analyses reveal a complex bedform pattern characterised by considerable spatial diversity, influenced heavily by the underlying substrate. The variability in length and density of mega-scale lineations indicates an evolving bedform signature, whereby landforms are preserved at different stages of maturity. Lineation generation and attenuation is associated with regions of thick, soft till where deformation was likely to be the greatest. The distribution of soft till and the localised extent of grounding-zone wedges (GZWs) indicate a dynamic sedimentary system characterised by considerable spatio-temporal variability in sediment erosion, transport and deposition. Formation of GZWs on the outer shelf of Marguerite Trough, within the error range of the radiocarbon dates, requires large sediment fluxes (upwards of 1000 m3 a−1 (m grounding line width)−1), and a >1 m thick mobile till layer, or rapid basal sliding velocities (upwards of 6 km a−1).
Citation
Livingstone, S., Stokes, C., O Cofaigh, C., Hillenbrand, C., Vieli, A., Jamieson, S., …Dowdeswell, J. (2016). Subglacial processes on an Antarctic ice stream bed. 1: Sediment transport and bedform genesis inferred from marine geophysical data. Journal of Glaciology, 62(232), 270-284. https://doi.org/10.1017/jog.2016.18
Journal Article Type | Article |
---|---|
Acceptance Date | Nov 5, 2015 |
Online Publication Date | Mar 17, 2016 |
Publication Date | Apr 1, 2016 |
Deposit Date | Jan 27, 2016 |
Publicly Available Date | Feb 1, 2016 |
Journal | Journal of Glaciology |
Print ISSN | 0022-1430 |
Electronic ISSN | 1727-5652 |
Publisher | International Glaciological Society |
Peer Reviewed | Peer Reviewed |
Volume | 62 |
Issue | 232 |
Pages | 270-284 |
DOI | https://doi.org/10.1017/jog.2016.18 |
Files
Accepted Journal Article
(2.8 Mb)
PDF
Copyright Statement
Copyright © The Author(s) 2016 This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Published Journal Article (Advance online version)
(2 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
Advance online version
Published Journal Article (Final published version)
(2.1 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
Copyright Statement
Final published version