Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/25568
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: MMI partial extraction geochemistry for the resolution of anthropogenic activities across the archaeological Roman town of Calleva Atrebatum
Author(s): Sylvester, Graham
Mann, Alan
Cook, Samantha
Wilson, Clare
Contact Email: c.a.wilson@stir.ac.uk
Keywords: soil geochemistry
archaeological prospection
partial extraction
MMI
Roman metal extraction
Issue Date: Feb-2018
Date Deposited: 3-Jul-2017
Citation: Sylvester G, Mann A, Cook S & Wilson C (2018) MMI partial extraction geochemistry for the resolution of anthropogenic activities across the archaeological Roman town of Calleva Atrebatum. Geochemistry: Exploration, Environment, Analysis, 18 (1), pp. 58-74. https://doi.org/10.1144/geochem2017-009
Abstract: Sixty three soils samples, fourteen samples of previously excavated archaeological material, and five background soil samples taken at the Silchester Roman Town of Calleva Atrebatum in the County of Hampshire, United Kingdom were analysed by the Mobile Metal Ion (MMI) method for a total of fifty three elements. Samples from within the town walls showed considerably higher concentrations than samples outside for many elements; Au, Ag, Cu and Sn were in extremely anomalous concentrations, Bi, Cd, Hg, Mo, P and Pb were anomalous and Sb and Zn in elevated concentrations. The overall pattern of element distribution is one of an annulus of higher elemental concentrations surrounding a centre of generally lower values centred on the previously excavated Forum basilica. The elements Zr, Ti, Th, Ti, Tl, Nb, Sn, Sc, Cr, Co, Sb, Bi, Ce, Nd (and all other REEs), show similar distributions to one another, and their distribution and that of the noble and base metals, as highlighted by various additive indices, is considered to be the result of metallurgical processing on site. The low values for most elements around the Forum basilica are the result of disturbance of the soil geochemical profile in this area by previous archaeological excavation.
DOI Link: 10.1144/geochem2017-009
Rights: This item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. Publisher policy allows this work to be made available in this repository. Geochemistry: Exploration, Environment, Analysis, 18, 2018 https://doi.org/10.1144/geochem2017-009 © Geological Society of London 2017

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