Abstract
AbstractSubmarine channels deliver globally important volumes of sediments, nutrients, contaminants and organic carbon into the deep sea. Knickpoints are significant topographic features found within numerous submarine channels, which most likely play an important role in channel evolution and the behaviour of the submarine sediment‐laden flows (turbidity currents) that traverse them. Although prior research has linked supercritical turbidity currents to the formation of both knickpoints and smaller crescentic bedforms, the relationship between flows and the dynamics of these seafloor features remains poorly constrained at field‐scale. This study investigates the distribution, variation and interaction of knickpoints and crescentic bedforms along the 44 km long submarine channel system in Bute Inlet, British Columbia. Wavelet analyses on a series of repeated bathymetric surveys reveal that the floor of the submarine channel is composed of a series of knickpoints that have superimposed, higher‐frequency, crescentic bedforms. Individual knickpoints are separated by hundreds to thousands of metres, with the smaller superimposed crescentic bedforms varying in wavelengths fromca16 m toca128 m through the channel system. Knickpoint migration is driven by the passage of frequent turbidity currents, and acts to redistribute and reorganize the crescentic bedforms. Direct measurements of turbidity currents indicate the seafloor reorganization caused by knickpoint migration can modify the flow field and, in turn, control the location and morphometry of crescentic bedforms. A transect of sediment cores obtained across one of the knickpoints show sand–mud laminations of deposits with higher aggradation rates in regions just downstream of the knickpoint. The interactions between flows, knickpoints and bedforms that are documented here are important because they likely dominate the character of preserved submarine channel‐bed deposits.
Highlights
Submarine channels are conduits for turbidity currents, which are one of the most volumetrically important processes for the delivery of sediments, nutrients, organic carbon and pollutants into the deep sea (Bouma, 2000; Peakall et al, 2007; Paull et al., 2010; Azpiroz-Zabala et al, 2017)
Knickpoint migration is driven by the passage of frequent turbidity currents, and acts to redistribute and reorganize the crescentic bedforms
Prior studies have recognized the prevalence of crescentic bedforms over a range of subaqueous depositional settings, including delta slopes (Hughes Clarke et al, 2012; Turmel et al, 2015; Hage et al, 2018), the axis of shallow-water submarine channels (Smith et al, 2005; Hughes Clarke et al, 2014; Normandeau et al, 2014; 2015), the axis of deep-water channels (Babonneau et al, 2013; Heijnen et al, 2020) and across unconfined submarine fans (Normark et al, 2002; Shao et al, 2021)
Summary
Submarine channels are conduits for turbidity currents, which are one of the most volumetrically important processes for the delivery of sediments, nutrients, organic carbon and pollutants into the deep sea (Bouma, 2000; Peakall et al, 2007; Paull et al., 2010; Azpiroz-Zabala et al, 2017). Integration of sediment cores with repeat seafloor bathymetric surveys showed how frequent, supercritical turbidity currents can drive the upstream102 migration of crescentic bedforms, reworking and reorganizing previous deposits (Hage et al, 2018; Vendettuoli et al, 2019) This reworking was found to leave behind ungraded or poorly-graded units of massive sands that infill scours (Hage et al, 2018; Vendettuoli et al, 2019; Englert et al, 2020). These bedforms shed light on the transition from river flow to submarine density flows and on the resulting modifications of seafloor geomorphology, and can be linked to observations of back-stepping beds and scour fills preserved in the sedimentary record (Hage et al, 2018)
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