Barnett, C., Scaife, R. G., Truckle, N. and Russell, J. (2008). The Upper and Middle Wentlooge Sequence and Environments at Plot 8000, The Western Approaches Distribution Park, Avonmout, South Gloucestershire. Archaeology in the Severn Estuary 19. Vol 19.
Title The title of the publication or report |
The Upper and Middle Wentlooge Sequence and Environments at Plot 8000, The Western Approaches Distribution Park, Avonmout, South Gloucestershire | ||
---|---|---|---|
Issue The name of the volume or issue |
Archaeology in the Severn Estuary 19 | ||
Series The series the publication or report is included in |
Archaeology in the Severn Estuary | ||
Volume Volume number and part |
19 | ||
Downloads Any files associated with the publication or report that can be downloaded from the ADS |
|
||
Licence Type ADS, CC-BY 4.0 or CC-BY 4.0 NC. |
ADS Terms of Use and Access
|
||
Publication Type The type of publication - report, monograph, journal article or chapter from a book |
Journal | ||
Abstract The abstract describing the content of the publication or report |
A borehole survey and archaeological investigations undertaken in advance of development at Plot 8000 of the Western Approach Distribution Park, Avonmouth, South Gloucestershire, enabled examination of the deep Wentlooge Formation (lower, middle and upper). The recovered sedimentary sequence of middle Wentlooge estuarine silts and peats and their associated palaeoenvironmental remains were analysed and dated to the middle Neolithic to middle Bronze Age using radiocarbon. It is demonstrated that following fully marine conditions at the Site in the early-middle Holocene, lower energy estuarine conditions expanded. A subsequent shift in the proximity of the Site to the estuary mouth in the middle Holocene is demonstrated by a microfaunal assemblage indicative of intertidal mudflats and low marsh environment. Stabilisation of sediments by emergent vegetation and the formation of stretches of wet marsh and terrestrial fen environments adjacent to mudflats with brackish creeks occurred from the middle Neolithic. Drier areas were well-wooded and there is evidence for the expansion in heathland and/or raised mire vegetation at this time. A reversion to dominantly estuarine and salt marsh conditions occurred, still within the middle Neolithic period, in response to positive eustatic change. Evidence for prehistoric human activity is scarce but pieces of comminuted charcoal occur in two thin layers of middle Neolithic and early Bronze Age date, the latter followed by possible evidence for expansion of pasture. Unlike the adjacent Plot 4000, the Site showed no evidence for Roman activity, with only ephemeral featuresof 18th-20th century date found, indicating this area was more marginal to settlement due to its topography and waterlogged nature. | ||
Year of Publication The year the book, article or report was published |
2008 | ||
Source Where the record has come from or which dataset it was orginally included in. |
ADS Archive
(ADS Archive)
|
||
Relations Other resources which are relevant to this publication or report |
|
||
Created Date The date the record of the pubication was first entered |
09 Oct 2017 |