Evaluating the role of physical mechanisms as possible triggers for turbidity currents in a deep ocean seamount

Turbidity currents on continental margins are often attributed to cyclic climate variability and sea-level change, while the causes of deep ocean turbidites are as yet to be tested. The Atlantic Iberian margin provides a unique setting to contrast deep ocean and continental environments, including depression features that further protect from resuspension and erosion by along-slope bottom currents. We present records of low-frequency, non-periodic, climate-independent turbidites from three deep cores covering up to 426,000 years in the Tore seamounts area. By evaluating a range of physical oceanographic mechanisms, the breaking of internal waves and mesoscale Mediterranean-eddies against unstable slopes in the seamounts area arises as the most likely triggers that precondition the recurrence pattern of the observed deep ocean turbidites. • Low-frequency, non-periodic, climate-independent sign in deep turbidites off Iberia. • Physical oceanographic processes evaluated as triggers for deep ocean turbidites. • Internal waves and Meddies role in less frequent turbidites away from continents. • Turbidite recurrence is cyclical near the Iberian continental margin canyons.

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Publication Details

Journal
Deep Sea Research Part I Oceanographic Research Papers
Published
2025-07-19
DOI
https://doi.org/10.1016/j.dsr.2025.104557
Primary Topic
Geology and Paleoclimatology Research
Type
article
Field-Weighted Citation Impact
0.00

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article

Evaluating the role of physical mechanisms as possible triggers for turbidity currents in a deep ocean seamount

Jordi F. López, María Isabel Reguera, Raphaël Hébert, Claire Waelbroeck et al.
Deep Sea Research Part I Oceanographic Research Papers
Geology and Paleoclimatology Research
article

Evaluating the role of physical mechanisms as possible triggers for turbidity currents in a deep ocean seamount

Jordi F. López, María Isabel Reguera, Raphaël Hébert, Claire Waelbroeck, Laura Antón, Belén Martrat, Simon J Crowhurst, Susana Lebreiro, Rocío Lozano-Luz, Silvia Osorio Nave, Álvaro Peliz, Alejandra Lopez-Rodriguez
article en

Abstract

Turbidity currents on continental margins are often attributed to cyclic climate variability and sea-level change, while the causes of deep ocean turbidites are as yet to be tested. The Atlantic Iberian margin provides a unique setting to contrast deep ocean and continental environments, including depression features that further protect from resuspension and erosion by along-slope bottom currents. We present records of low-frequency, non-periodic, climate-independent turbidites from three deep cores covering up to 426,000 years in the Tore seamounts area. By evaluating a range of physical oceanographic mechanisms, the breaking of internal waves and mesoscale Mediterranean-eddies against unstable slopes in the seamounts area arises as the most likely triggers that precondition the recurrence pattern of the observed deep ocean turbidites. • Low-frequency, non-periodic, climate-independent sign in deep turbidites off Iberia. • Physical oceanographic processes evaluated as triggers for deep ocean turbidites. • Internal waves and Meddies role in less frequent turbidites away from continents. • Turbidite recurrence is cyclical near the Iberian continental margin canyons.

Deep Sea Research Part I Oceanographic Research PapersVol. 224
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), Centre National de la Recherche Scientifique (FR), University of Lisbon (PT), Instituto Geológico y Minero de España (ES), National Laboratory of Energy and Geology (PT), Institute of Environmental Assessment and Water Research (ES), Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (FR), Department of Earth Sciences (RU), Institut de Recherche pour le Développement (FR)
Department of Earth Sciences, University of Cambridge, Ministerio de Educación, Cultura y Deporte, Ministerio de Ciencia e Innovación, Agencia Estatal de Investigación
Life below water
Openalex Percentile: Top 77%
Geology and Paleoclimatology Research
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