Bedform evolution along a submarine canyon in the South China Sea: New insights from an autonomous underwater vehicle survey

Sun, Yue, Wang, Dawei, Canals, Miquel, Alves, Tiago M. ORCID: https://orcid.org/0000-0002-2765-3760, Wang, Weiwei, Zhu, Yousheng, Qin, Yongpeng, Zeng, Fanchang and Zheng, Yu 2024. Bedform evolution along a submarine canyon in the South China Sea: New insights from an autonomous underwater vehicle survey. Sedimentology 71 (3) , pp. 793-826. 10.1111/sed.13152 Item availability restricted.

PDF - Accepted Post-Print Version Restricted to Repository staff only until 29 October 2024 due to copyright restrictions. Download (4MB)

Abstract

Traditional mapping of bedforms in submarine canyons relied on vessel-mounted and towed sensors, but their fine-scale geomorphology and shallow structure requires higher resolution datasets. This study utilizes a high-resolution dataset obtained from an autonomous underwater vehicle, combined with seismic reflection profiles and sediment cores, to analyze bedform sets within a 25.6 km long submarine canyon (canyon C14) in the northern South China Sea. A train of crescent-shaped axial steps, indicative of cyclic steps formed by supercritical turbidity currents, is imaged along the canyon. Axial steps in the upper course show erosional truncations and sub-horizontal reflectors on the lee and stoss sides, respectively, pointing to erosional–depositional cyclic steps formed by confined flows with high erosional capacity. This is facilitated by canyon narrowness and steeper axial gradient. After a transition segment, the lower course widens, with a gentler axial gradient, resulting in increased asymmetry and wavelength of axial steps. Backset bed deposits on the stoss sides of these steps indicate depositional cyclic steps with higher aggradation. Sediment filling, almost padding each cyclic step associated scour suggests the reworking of previously formed bedforms by gravity flows fed by destabilization processes on the canyon sidewalls and upstream lee faces and, possibly, by shelf-edge and uppermost slope spillover into the canyon. At the lowermost course, cyclic steps transition to a furrow field, likely associated to flow velocity reduction facilitated by canyon floor widening and a further decrease in slope gradient. Flow braiding and re-convergence, related to the erosion of fine-grained deposits within the canyon floor, should have played a role to produce furrows under supercritical conditions. This work enhances our understanding of the detailed morphology and shallow relief configuration of bedforms in deep-water submarine canyons, providing insights into their causative processes and evolution.

Item Type:	Article
Date Type:	Publication
Status:	Published
Schools:	Earth and Environmental Sciences
Publisher:	Wiley
ISSN:	1365-3091
Date of First Compliant Deposit:	10 November 2023
Date of Acceptance:	16 October 2023
Last Modified:	18 Apr 2024 17:15
URI:	https://orca.cardiff.ac.uk/id/eprint/163798

Actions (repository staff only)

Edit Item