Charles K. Paull
Powerful turbidity currents driven by dense basal layers
Paull, Charles K.; Talling, Peter J.; Maier, Katherine L.; Parsons, Daniel; Xu, Jingping; Caress, David W.; Gwiazda, Roberto; Lundsten, Eve M.; Anderson, Krystle; Barry, James P.; Chaffey, Mark; O’Reilly, Tom; Rosenberger, Kurt J.; Gales, Jenny A.; Kieft, Brian; McGann, Mary; Simmons, Steve M.; McCann, Mike; Sumner, Esther J.; Clare, Michael A.; Cartigny, Matthieu J.
Authors
Professor Peter Talling peter.j.talling@durham.ac.uk
Professor
Katherine L. Maier
Daniel Parsons
Jingping Xu
David W. Caress
Roberto Gwiazda
Eve M. Lundsten
Krystle Anderson
James P. Barry
Mark Chaffey
Tom O’Reilly
Kurt J. Rosenberger
Jenny A. Gales
Brian Kieft
Mary McGann
Steve M. Simmons
Mike McCann
Esther J. Sumner
Michael A. Clare
Dr Matthieu Cartigny matthieu.j.cartigny@durham.ac.uk
Associate Professor
Abstract
Seafloor sediment flows (turbidity currents) are among the volumetrically most important yet least documented sediment transport processes on Earth. A scarcity of direct observations means that basic characteristics, such as whether flows are entirely dilute or driven by a dense basal layer, remain equivocal. Here we present the most detailed direct observations yet from oceanic turbidity currents. These powerful events in Monterey Canyon have frontal speeds of up to 7.2 m s−1, and carry heavy (800 kg) objects at speeds of ≥4 m s−1. We infer they consist of fast and dense near-bed layers, caused by remobilization of the seafloor, overlain by dilute clouds that outrun the dense layer. Seabed remobilization probably results from disturbance and liquefaction of loose-packed canyon-floor sand. Surprisingly, not all flows correlate with major perturbations such as storms, floods or earthquakes. We therefore provide a new view of sediment transport through submarine canyons into the deep-sea.
Citation
Paull, C. K., Talling, P. J., Maier, K. L., Parsons, D., Xu, J., Caress, D. W., Gwiazda, R., Lundsten, E. M., Anderson, K., Barry, J. P., Chaffey, M., O’Reilly, T., Rosenberger, K. J., Gales, J. A., Kieft, B., McGann, M., Simmons, S. M., McCann, M., Sumner, E. J., Clare, M. A., & Cartigny, M. J. (2018). Powerful turbidity currents driven by dense basal layers. Nature Communications, 9(1), Article 4114. https://doi.org/10.1038/s41467-018-06254-6
Journal Article Type | Article |
---|---|
Acceptance Date | Aug 20, 2018 |
Online Publication Date | Oct 5, 2018 |
Publication Date | Oct 5, 2018 |
Deposit Date | Oct 15, 2018 |
Publicly Available Date | Oct 16, 2018 |
Journal | Nature Communications |
Publisher | Nature Research |
Peer Reviewed | Peer Reviewed |
Volume | 9 |
Issue | 1 |
Article Number | 4114 |
DOI | https://doi.org/10.1038/s41467-018-06254-6 |
Public URL | https://durham-repository.worktribe.com/output/1316470 |
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This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
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