Abstract

AbstractThe location of inhumations, in the absence of ferrous grave goods, often presents a considerable challenge to archaeological geophysics, given the small size of the features and the slight physical contrast between the fill of the grave and the surrounding subsoil. Even during excavation, the identification of graves may be complicated where site conditions do not favour the preservation of human skeletal remains and only a subtle soil stain is likely to survive. A recent initiative in the UK has seen the formation of the Buried Organic‐matter–Decomposition Integrated with Elemental Status (BODIES) research group, to examine the decomposition of organic artefacts in ancient graves with respect to localized changes in pH, redox potential and nutrient status. This paper presents initial results from a limited mineral magnetic study of two grave sites in an attempt to ascertain whether the decomposition of organic remains may lead to a detectable magnetic signature within the soil. Results from a series of isothermal, hysteresis and magneto‐thermal experiments will be presented together with surface magnetometer and topsoil susceptibility surveys. Copyright © Crown Copyright 2004. Recorded with the permission of Her Majesty's Stationery Office. Published by John Wiley & Sons, Ltd.

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