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Geological Society, London, Special Publications; 2000; v. 175; p. 253-279;
DOI: 10.1144/GSL.SP.2000.175.01.19
© 2000 Geological Society of London

Stratigraphic architecture, relative sea-level, and models of estuary development in southern England: new data from Southampton Water

A. J. Long1, R. G. Scaife2 & R. J. Edwards1,*

1 Environmental Research Centre, Department of Geography, University of Durham, South Road, Durham DH1 3LE, UK
2 Department of Geography, University of Southampton, Highfield, Southampton SO17 1BJ, UK
* Faculteit der Aardwetenschappen, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, Netherlands

This paper presents the results of an investigation into the Holocene depositional history of Southampton Water, southern England. A three phase history of estuary development is proposed. Between c. 7500 and 5000 BP (8200 to 5700 cal. a BP), mean sea-level rose rapidly from c. –9m to –4 m OD. During this interval thin basal peats which developed in present outer estuary locations were inundated and the area of intertidal and subtidal environments within the estuary expanded. Relative sea-level (RSL) rise began to slow between 5000 and 3000 BP (5700 and 3200 cal. a BP) and a phase of saltmarsh and freshwater peat accumulation occurred. In this interval freshwater peat-forming communities extended outwards and seawards across former saltmarsh and mudflat environments and caused a reduction in the extent of the intertidal area within the estuary. During the late Holocene there was a switch to renewed minerogenic sedimentation as most of the freshwater coastal wetlands of Southampton Water were inundated. This tripartite model is broadly applicable to the Thames and the Severn estuaries, suggesting that regional processes have controlled their macroscale evolution. RSL change and variations in sediment supply emerge as key controls during the first two phases of estuary development. The late Holocene demise of the estuary wetlands probably reflects a propensity for increased sediment reworking and unfavourable conditions for the accumulation and preservation of organogenic deposits due to reduced rates of long-term RSL and watertable rise.





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Radiocarbon-dated sediment sequences from the Belgian coastal plain: testing the hypothesis of fluctuating or smooth late-Holocene relative sea-level rise
The Holocene, 2008; 18: 1219 - 1228.
[Abstract] [PDF]