J Archaeol Sci 33 (1)

The head capsules of chironomids (Insecta: Diptera) are well preserved in sediments and can be recognised to a high taxonomic level, usually genus and sometimes species. Work on lake sediments has shown that they can be accurate indicators of water temperature, oxygen regimes, and nutrient status (particularly total phosphorus and chlorophyll-a), as well as heavy metal pollution. No systematic chironomid analyses, however, have previously been undertaken on archaeological deposits. In order to address this the authors assessed the use of chironomids in three types of archaeological deposit; firstly, a lake core at the edge of a lake settlement (crannog), secondly, a palaeochannel infill adjacent to a multi-period settlement site and lastly, a Roman well deposit from a floodplain environment. The chironomid assemblages are shown to vary significantly both between and within the sites and reflect the immediate environment and the adjacent area. The lake sediment assemblage reflects the construction of the crannog through elevated levels of organic detritus, wood and woody debris. The palaeochannel assemblage reveals changing natural conditions and nutrient enrichment probably associated with settlement during the Saxon period. The well assemblage is taxonomically restricted and indicative of organic debris, dead plant material, animal dung and possibly human effluent deposited after abandonment of the well. Dry storage of the palaeochannel and well sediments for several years did not appear to affect the concentration or state of preservation of the head capsules. The chironomid reconstructions are shown to provide an additional indicator of human activity which has the potential to provide quantitative data on the character of aquatic environments associated with archaeological sites.

The value of testate amoebae in the reconstruction of changes in surface wetness from ombrotrophic mires is well known, but the potential value of such records in specifically archaeological investigations has not yet been investigated. This note describes the analysis of testate amoebae for a sediment sequence from the multi-period wetland archaeological site of Derryville, Co. Tipperary, Ireland. The reconstructed watertable is presented and plotted against the range of dates from excavated archaeological features in the wetland area. The data demonstrate a clear association between periods of low watertable and increased anthropogenic activity as reflected by site construction. The value of testate amoebae in future integrated archaeological investigations of wetland systems is discussed.

The authors report on stable carbon and nitrogen isotope measurements of human and faunal bone collagen from the Iron Age, Viking Age, and late medieval site of Newark Bay, Orkney. A wide range of results was found for humans in both 13C and 15N values. The enriched carbon and nitrogen values indicate the consumption of significant amounts of marine protein, which is very unusual for post-Mesolithic (e.g. 4000 cal BC) UK and European populations. Also of interest is a statistically significant difference in 13C and 15N values, and therefore diets, between adult males and females at this site, with males having, on average, a higher proportion of marine protein than females. The weaning age of the sub-adults was difficult to interpret due to the large isotopic variation in the adult females, but nearly all individuals between birth and 1.25 years have elevated 15N values indicating that they were breastfed to some extent.