Dr Megan Baker megan.l.baker@durham.ac.uk
Assistant Professor
Seabed Seismographs Reveal Duration and Structure of Longest Runout Sediment Flows on Earth
Baker, Megan L.; Talling, Peter J.; Burnett, Richard; Pope, Ed L.; Ruffell, Sean C.; Urlaub, Morelia; Clare, Michael A.; Jenkins, Jennifer; Dietze, Michael; Neasham, Jeffrey; Silva Jacinto, Ricardo; Hage, Sophie; Hasenhündl, Martin; Simmons, Steve M.; Heerema, Catharina J.; Heijnen, Maarten S.; Kunath, Pascal; Cartigny, Matthieu J. B.; McGhee, Claire; Parsons, Daniel R.
Authors
Professor Peter Talling peter.j.talling@durham.ac.uk
Professor
Richard Burnett
Edward Pope edward.pope@durham.ac.uk
Honorary Fellow
Sean Ruffell sean.ruffell@durham.ac.uk
PGR Student Doctor of Philosophy
Morelia Urlaub
Michael A. Clare
Dr Jenny Jenkins jennifer.jenkins@durham.ac.uk
Assistant Professor
Michael Dietze
Jeffrey Neasham
Ricardo Silva Jacinto
Sophie Hage
Martin Hasenhündl
Steve M. Simmons
Catharina J. Heerema
Maarten S. Heijnen
Pascal Kunath
Dr Matthieu Cartigny matthieu.j.cartigny@durham.ac.uk
Associate Professor
Claire McGhee
Daniel R. Parsons
Abstract
Turbidity currents carve the deepest canyons on Earth, deposit its largest sediment accumulations, and break seabed telecommunication cables. Powerful canyon‐flushing turbidity currents break sensors placed in their path, making them notoriously challenging to measure, and thus poorly understood. This study provides the first remote measurements of canyon‐flushing flows, using ocean‐bottom seismographs located outside the flow's destructive path, revolutionizing flow monitoring. We recorded the internal dynamics of the longest sediment flows yet monitored on Earth, which traveled >1,000 km down the Congo Canyon‐Channel at 3.7–7.6 m s−1 and lasted >3 weeks. These observations allow us to test fundamental models for turbidity current behavior and reveal that flows contain dense and fast frontal‐zones up to ∼400 km in length. These frontal‐zones developed near‐uniform durations and speeds for hundreds of kilometres despite substantial seabed erosion, enabling flows to rapidly transport prodigious volumes of organic carbon, sediment, and warm water to the deep‐sea.
Citation
Baker, M. L., Talling, P. J., Burnett, R., Pope, E. L., Ruffell, S. C., Urlaub, M., Clare, M. A., Jenkins, J., Dietze, M., Neasham, J., Silva Jacinto, R., Hage, S., Hasenhündl, M., Simmons, S. M., Heerema, C. J., Heijnen, M. S., Kunath, P., Cartigny, M. J. B., McGhee, C., & Parsons, D. R. (2024). Seabed Seismographs Reveal Duration and Structure of Longest Runout Sediment Flows on Earth. Geophysical Research Letters, 51(23), Article e2024GL111078. https://doi.org/10.1029/2024gl111078
Journal Article Type | Letter |
---|---|
Acceptance Date | Nov 6, 2024 |
Online Publication Date | Nov 28, 2024 |
Publication Date | Dec 16, 2024 |
Deposit Date | Dec 2, 2024 |
Publicly Available Date | Dec 2, 2024 |
Journal | Geophysical Research Letters |
Print ISSN | 0094-8276 |
Electronic ISSN | 1944-8007 |
Publisher | Wiley |
Peer Reviewed | Peer Reviewed |
Volume | 51 |
Issue | 23 |
Article Number | e2024GL111078 |
DOI | https://doi.org/10.1029/2024gl111078 |
Keywords | organic carbon, ocean‐bottom seismographs, ocean fluxes, seismic monitoring, turbidity currents |
Public URL | https://durham-repository.worktribe.com/output/3115977 |
Files
Published Journal Article
(2.7 Mb)
PDF
Publisher Licence URL
http://creativecommons.org/licenses/by/4.0/
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