• An opportunity to investigate the distribution of pollutants in deep-marine channel systems, with potential to influence policy
• Fieldwork possibilities in Mexico, South Africa, and Spain
• Novel experiments in Environmental Fluid Dynamics Laboratory, Leeds
• Vibrant research community in the sedimentology
• Internationally leading supervisory team
Submarine slope valleys are the main conduits for the transfer of particulates from the continents to the deep oceans, including huge volumes of clastic sediment, and increasing amount of pollutants (e.g. microplastics; Kane and Clare, 2019). Slope valleys are dominated by sediment bypass for much of their lifespan. However, buried systems show that internal levee and terrace deposits are a major volumetric component of ancient slope valley-fills (Hansen et al., 2015). These confined overbank settings act as a major store for fine-grained sediment, and are thought to comprise low-density turbidites. The role of submarine slope valleys as sinks for anthropogenic pollutants, such as microplastics, pharmaceuticals, and pesticides, is poorly constrained because the sedimentary processes and grain-size distributions of internal levee and terrace deposits are barely monitored in modern systems.
Our understanding of their sedimentology and stratigraphy deposits is limited to a few exhumed systems (Kane and Hodgson, 2011), and several cores in modern systems (Babonneau et al., 2010). Therefore, fieldwork is an essential component of this PhD studentship to examine exhumed slope valley systems and to document the grain-size distributions, sedimentary facies and depositional architecture in these ancient systems. Examples of exhumed internal levee and terrace deposits include the Karoo Basin, South Africa, the Rosario Formation, Mexico, and the Ainsa Formation, NE Spain.
The sedimentary processes, and dynamic morphology, which internal levees and terraces form within the conduits has never been captured experimentally. Therefore, a series of novel physical experiments will be designed to investigate processes where flows spill into confinement. Smaller sinuous channel forms, both leveed and terraced, sitting inside a larger container represent the slope valley confinement. Initially, the ‘inset’ channel forms will be simple, in order to compare results to previous experiments run in the Sorby Environmental Fluid Dynamics Laboratory that did not have a larger scale confining surface (Keevil et al., 2006). This will form a baseline, and to identify process differences with the new experimental set-up, with scope to employ morphologies from modern systems in later experiments.
Aims and objectives:
The principal aim of the proposed PhD project is to investigate the processes sedimentology, and stratigraphic architecture, of internal levee and terrace deposits, and to assess their role as sinks for pollutants. The results from the fieldwork and experimental components will be integrated in order to address the following objectives:
- To assess where particulates (e.g. pesticides, microplastics) with different hydrodynamic properties will be concentrated within submarine canyon systems
- To investigate the process differences between internal levee and ‘depositional’ terraces
- To examine whether turbidity currents start to decouple to form a higher density thalweg confined current, and lower density weakly confined current
This PhD will commence October 2020 and run for 3.5 years. During this period, the student will be eligible for all the postgraduate training typically provided to students attending the University as part of the PANORAMA DTP. This interdisciplinary project will provide the successful PhD candidate with highly valued and sought-after skills in modelling, and a deep understanding of particulate gravity flow. The student will receive training in relevant software packages, field based description, experimental techniques and data analysis, technical/scientific writing, and presentation of research to both scientific and public audiences. There will be opportunities to present results at major, international conferences, and the student will be encouraged to publish their research during their studentship. The student will be based in the School of Earth and Environment at the University of Leeds, and will join the sedimentology group at Leeds, which is one of the largest and most vibrant in the UK, with a active group of doctoral and postdoctoral researchers, and close collaboration with researchers in the University of Manchester.
Babonneau, N., Savoye, B., Cremer, M. & Bez, M. (2010). Sedimentary architecture in meanders of a submarine channel: detailed study of the present Congo turbidite channel (Zaiango project). Journal of Sedimentary Research, 80, 852-866.
Hansen, L. A., Callow, R. H., Kane, I. A., Gamberi, F., Rovere, M., Cronin, B. T. & Kneller, B. C. (2015). Genesis and character of thin-bedded turbidites associated with submarine channels. Marine and Petroleum Geology, 67, 852-879.
Kane, I.A. & Hodgson, D.M. (2011). Sedimentological criteria to differentiate submarine channel levee subenvironments: exhumed examples from the Rosario Fm. (Upper Cretaceous) of Baja California, Mexico, and the Fort Brown Fm. (Permian), Karoo basin, S. Africa. Marine and Petroleum Geology, 28, 807-823.
Kane, I.A. & Clare, M.A. (2019). Dispersion, accumulation, and the ultimate fate of microplastics in deep-marine environments: a review and future directions. Frontiers in Earth Science, 7, 1-27.
Keevil, G.M., Peakall, J., Best, J.L. & Amos, K.J. (2006). Flow structure in sinuous submarine channels: Velocity and turbulence structure of an experimental submarine channel. Marine Geology, 229, 241-257.