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Title: The Wash-Fenland Embayment : sediment sources and supply during the Holocene.
Author: Holt, Tina.
ISNI:       0000 0001 3580 9991
Awarding Body: University of Reading
Current Institution: University of Reading
Date of Award: 1999
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For appropriate management of any stretch of coastline, it is desirable to understand (and ultimately to be able to predict) the exchange, transfer and storage of material at the landocean boundary. To this end, the multidisciplinary Land-Ocean Interaction Study (LOIS) was set up by the UK Natural Environment Research Council (NERC), focusing chiefly on eastern England as an example. Distinction between short-term fluctuations and long-term trends is particularly important when devising predictive models of coastal change. Within LOIS, the Land-Ocean Evolution Perspective Study (LOEPS) provided data on a Holocene time scale using evidence from the sediment record of east coast sinks including the Humber, the Fens and the North Norfolk coast. As part of LOEPS, the present study centred on the Wash-Fenland Embayment, the largest accumulation of Holocene tidal sediments in Britain. Since initial marine inundation of the area around 7,000 years BP, approximately 24 km' of sand and mud have been deposited by vertical and lateral accretion under varying rates of sea-level rise. However, in the last 50 years, parts of the shoreline have started to erode, raising questions over sediment supply and other conditions necessary for maintaining the position of the intertidal zone. The main aim of the work presented in this thesis was to ascertain the main sources of sediment supplied to the Fenland and adjacent Lincolnshire coast. Selected tidal sediments from early Holocene to recent age were compared with a range of potential source lithologies. The latter included sections of eroding coast between Holderness and North Norfolk and local strata exposed within the embayment and its river catchments. In the Fens, use of chemical ratios showed the majority of Holocene sediment to be well mixed and very homogeneous, variations in bulk chemical data mainly being a function of sediment grade. However, samples with anomalous chemical ratios were identified at the base of the succession close to the landward margins. Grain-size specific analyses of these samples suggest that they have a similar composition to lithologies from Fenland river catchments and the floor of the embayment. For example, clay mineralogy indicated an early Holocene fluvial input of Oxford Clay at Adventurer's Land. In a similar way, surface area, mineral magnetic analyses, optical mineralogy and SEM of anomalous sand samples show quantitatively and qualitatively the links between selected non-marine sources and these early Holocene sediments. The bulk of the Fenland sediment appears to have been well mixed in the North Sea sediment pool prior to deposition. Comparisons of the potential marine source lithologies showed the fine fraction of the glacial tills to the north and east of the embayment to be chemically very similar. On the basis of clay mineralogy, subtle differences between Devensian and Anglian Tills were identified, and Fenland sediment was found to have an intermediate composition. The sand fraction of most Devensian Till samples could be distinguished from the more quartz-rich sand fraction of the Anglian Tills, and quantitative analyses of surface area and magnetic properties of selected Fenland samples suggest till eroding from the Lincolnshire foreshore is the most likely source. Particle size analysis, summarised using Principal Components Analysis (PCA), proved successful in characterising sediments according to depositional environment. Grain-size data indicated a general fining-upwards trend in the sand fraction. In the embayment as a whole, vertical accretion was accompanied by lateral progradation indicating that sediment supply was more than sufficient to keep pace with sea-level rise. The use of particle size analysis together with PCA seems widely applicable to studies of modern and Holocene sedimentary environments, estuarine sedimentation history and consideration of long term sediment budgets. Chemical ratios appear to have potential as first indicators of changing sediment source.
Supervisor: Not available Sponsor: Not available
Qualification Name: Thesis (Ph.D.) Qualification Level: Doctoral
EThOS ID:  DOI: Not available