Dr Megan Baker megan.l.baker@durham.ac.uk
Assistant Professor
Dr Megan Baker megan.l.baker@durham.ac.uk
Assistant Professor
Sophie Hage
Peter J. Talling
Sanem Acikalin
Robert G. Hilton
Negar Haghipour
Sean C. Ruffell
Ed L. Pope
Ricardo Silva Jacinto
Michael A. Clare
Sefa Sahin
Burial of organic carbon in marine sediments is a long-term sink of atmospheric CO2, and submarine turbidity currents are volumetrically the most important sediment transport process on Earth. Yet the processes, amounts, and efficiency of organic carbon transfer by turbidity currents through submarine canyons to the deep sea are poorly documented and understood. We present an organic carbon budget for the submarine Congo Canyon, offshore West Africa, constrained with time-lapse bathymetry, sediment cores, and flow monitoring, including the effects of two >1000-km-runout canyon-flushing turbidity currents. In one year, flows eroded an estimated 6.09 ± 2.70 Mt of previously buried terrestrial organic carbon in the canyon, primarily from fine-grained and vegetation-rich muddy sand facies with high organic carbon contents (as high as 11%). The age and composition of organic carbon in the Congo Canyon is comparable to those in the Congo River, indicating that transfer is efficient. Over the whole canyon-channel system, we extrapolate that 43 ± 15 Mt of organic carbon was eroded and transported to the deep (>5 km) sea, equivalent to 22% of the annual global particulate organic carbon export from rivers to oceans and 54%–108% of the predicted annual terrestrial organic carbon burial in the oceans. Canyon-flushing turbidity currents carried a globally significant mass of terrestrial organic carbon down just one submarine canyon in a single year, indicating their importance for redistribution and delivery of organic carbon to the deep sea.
Baker, M. L., Hage, S., Talling, P. J., Acikalin, S., Hilton, R. G., Haghipour, N., Ruffell, S. C., Pope, E. L., Jacinto, R. S., Clare, M. A., & Sahin, S. (2024). Globally significant mass of terrestrial organic carbon efficiently transported by canyon-flushing turbidity currents. Geology, 52(8), 631-636. https://doi.org/10.1130/g51976.1
Journal Article Type | Article |
---|---|
Acceptance Date | May 22, 2024 |
Online Publication Date | Jun 13, 2024 |
Publication Date | Aug 1, 2024 |
Deposit Date | Sep 13, 2024 |
Publicly Available Date | Sep 13, 2024 |
Journal | Geology |
Print ISSN | 0091-7613 |
Electronic ISSN | 1943-2682 |
Publisher | Geological Society of America |
Peer Reviewed | Peer Reviewed |
Volume | 52 |
Issue | 8 |
Pages | 631-636 |
DOI | https://doi.org/10.1130/g51976.1 |
Public URL | https://durham-repository.worktribe.com/output/2863414 |
Accepted Journal Article
(2.2 Mb)
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