Haslett, S. K., Davies, P., Davies, C. F C., Margetts, A. J., Scotney, K. H., Thorpe, D. J. and Williams, H. O. (2000). The Changing Estuarine Environment in Relation to Holocene Sea Level and the Archaeological Implications. Archaeology in the Severn Estuary 11. Vol 11, pp. 35-53. https://doi.org/10.5284/1069476. Cite this via datacite
Title The title of the publication or report |
The Changing Estuarine Environment in Relation to Holocene Sea Level and the Archaeological Implications | |||
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Issue The name of the volume or issue |
Archaeology in the Severn Estuary 11 | |||
Series The series the publication or report is included in |
Archaeology in the Severn Estuary | |||
Volume Volume number and part |
11 | |||
Page Start/End The start and end page numbers. |
35 - 53 | |||
Downloads Any files associated with the publication or report that can be downloaded from the ADS |
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Licence Type ADS, CC-BY 4.0 or CC-BY 4.0 NC. |
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DOI The DOI (digital object identifier) for the publication or report. |
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Publication Type The type of publication - report, monograph, journal article or chapter from a book |
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Abstract The abstract describing the content of the publication or report |
Estuarine development has been previously modelled in relation to the rate of relative sea-level rise, suggesting intertidal surfaces attain different vertical positions within the tidal frame according the rate of sea-level rise. These model results are significant in the context of Holocene sea-level rise, which experienced a continuum of very rapid to low sea-level rise rates, in that the estuarine palaeoenvironment and its resource potential for prehistoric populations is suggested to have changed through time. The present study empirically investigates the palaeoenvironmental development of the Somerset Levels (UK), an extensive coastal wetland (palaeo-estuarine system) that is of international archaeological importance. A composite sequence of Holocene sediments is analysed using foraminiferal and molluscan-based palaeoenvironmental techniques, and dated through radiocarbon and chemostratigraphic methods. The results indicate that during the Early Holocene (Mesolithic) the estuary was dominated by low saltmarsh and mudflat palaeoenvironments dictated by the rapid rate of post-glacial sea-level rise. This intertidal surface, low within the contempory tidal frame, would have been characterised by soft mud and sparse vegetation due to frequent tidal indundation, and would have possessed a high hydraulic duty (cf the amount of tidal water accommodated by the surface) with associated large tidal creeks/channels. Towards the Middle Holocene (Neolithic) a transition to palaeoenvironments higher within the tidal frame is evident, so that mid and then high saltmarsh dominate the estuary. This transition was in response to a progressively decreasing sea-level rise rate, allowing the intertidal surface to elevate through the tidal frame. These intertidal surfaces are likely to have become progressively drier and more richly vegetated due to increasingly infrequent tidal inundation, with a corresponding reduction in hydraulic duty and creek/channel size, culminating in emergence and supratidal peat growth. The results also suggest that this sequence is reversed through the Late Holocene (late Neolithic, Bronze Age, Iron Age) so that Roman reclamation of the Somerset Levels took place against a rising sea-level. These data support previous theoretical models, and have significant implications for the resource potential of these changing estuarine palaeoenvironments for prehistoric populations. | |||
Year of Publication The year the book, article or report was published |
2000 | |||
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Created Date The date the record of the pubication was first entered |
09 Oct 2017 |