Geomorphology of a modern carbonate slope system and associated sedimentary processes: Example of the giant Great Abaco Canyon, Bahamas. Issue 1 (27th August 2020)

• Record Type: Journal Article
• Authors: Recouvreur, Audrey; Fabregas, Natacha; Mulder, Thierry; Hanquiez, Vincent; Fauquembergue, Kelly; Tournadour, Elsa; Gillet, Hervé; Borgomano, Jean; Poli, Emmanuelle; Kucharski, Jean‐Baptiste; Wilk, Stanislas
• Editors: Hendry, Jim
• Is Part Of: Sedimentology. Volume 68:Issue 1(2021)
• Page Start: 266
• Page End: 293
• Publication Date: 2020-08-27
• Subjects: Backscatter -- Bahamas -- carbonate slope -- echofacies -- giant canyon -- sea floor morphology -- sedimentary processes; Sedimentology -- Periodicals; 552.5
• DOI: 10.1111/sed.12777
• Languages: English
• ISSNs: 0037-0746

Abstract

Abstract: The large acoustic data set acquired during the Carambar cruises is composed of high resolution bathymetry, backscatter data and very‐high resolution seismic lines which allow for an overview of the morphology and sediment transfer processes from the shallow upper slope to the abyssal plain of a modern carbonate system: the north‐eastern slope of the Little Bahama Bank. Surficial distribution of the acoustic facies and echofacies reflects a wide variety of sedimentary processes along and across the slope. The western sector of the Little Bahama Bank is dominated by depositional processes whereas its eastern sector, which is incised in the lower slope by giant canyons, is affected by erosion and bypass processes. Datasets suggest that currents play an important role both in along‐slope sedimentary processes and in the abyssal plain. The Antilles Current appears to affect a large part of the middle and lower slopes. The absence of sizeable present‐day channel/levée complexes or lobes at the mouth of the canyon – revealed by the bathymetric map – indicates that the southward flowing Deep Western Boundary Current influences modern abyssal sediment deposition. Based on depositional processes and indicators of canyon maturity observed in facies distribution, the current study proposes that differential subsidence affects the eastern versus western part of the bank. The morphology of the Great Abaco Canyon and Little Abaco Canyon, which extend parallel to the platform, and the Little Bahama Bank slope appears to be related to the Great Abaco Fracture Zone.