Yes / In this study, period-specific dietary trends, along with socio-economic and religious influences on foods consumed by Pictish and medieval inhabitants from Portmahomack are investigated. Bone collagen from human adults (n = 137) and fauna (n = 71) were analysed for stable carbon and nitrogen isotope ratios to enable dietary reconstructions of the whole adult skeletal assemblage. Adult mean δ13C and δ15N values from all periods (6th to 17th century) were −19.5‰ ± 1.3‰ and 13.3‰ ± 1.7‰ respectively. A diachronic change in diet between early medieval Pictish lay and monastic communities (periods 1–3) and the later medieval parish layfolk (periods 4–5) was found that suggests changing socio-economic and religious influences, along with age and gender differences in diet that reflect possible divisions in labour and status. Faunal data also reflected a diachronic change in diet, most likely related to a change in animal husbandry practices over time. This is the first large-scale study on the Portmahomack assemblage and presents new isotope data to provide a more comprehensive insight into Pictish and medieval subsistence patterns, along with evidence of how religious and social foci may influence diet over time. Such comprehensive investigations can only be adopted by analysing the whole skeletal assemblage, providing robust faunal baselines and inter- and intra-site comparisons. Most importantly, this significant new evidence fundamentally changes our knowledge of diet and subsistence in medieval Scotland and the potential influences therein. / Supported by grants from the NERC Isotope Geosciences Facility Steering Committee (IP‐1302‐0512), the Arts and Humanities Research Council (AH/I019103/1), and Historic Scotland (AMJ/4208/4).

The ability of current clinical tools to predict bone fractures is poor, likely because these tools focus on bone mass and mineral content and neglect bone quality and the collagen phase. The Mechanical Response Tissue Analyzer (MRTA) is an instrument that provides a non-invasive mechanical measurement of the whole bone. It has traditionally been used to obtain a bone stiffness constant (Kb), but can provide a bone damping constant (Bb) that has not previously been considered. The goal of this research is to determine whether the MRTA can detect three damage modes that do not alter bone mass or mineral density: γ-irradiation, collagen over-crosslinking, and fatigue. The MRTA detected a reduction in Bb due to over-crosslinking. Fatigue was found to increase Bb and decrease Kb, and these changes were confirmed through dynamic bending tests. The MRTA shows potential to diagnose increased fracture risk in scenarios where damage is currently undetectable.

The ability of current clinical tools to predict bone fractures is poor, likely because these tools focus on bone mass and mineral content and neglect bone quality and the collagen phase. The Mechanical Response Tissue Analyzer (MRTA) is an instrument that provides a non-invasive mechanical measurement of the whole bone. It has traditionally been used to obtain a bone stiffness constant (Kb), but can provide a bone damping constant (Bb) that has not previously been considered. The goal of this research is to determine whether the MRTA can detect three damage modes that do not alter bone mass or mineral density: γ-irradiation, collagen over-crosslinking, and fatigue. The MRTA detected a reduction in Bb due to over-crosslinking. Fatigue was found to increase Bb and decrease Kb, and these changes were confirmed through dynamic bending tests. The MRTA shows potential to diagnose increased fracture risk in scenarios where damage is currently undetectable.

Following the argument of cultural change between the Romano-British and Anglo-Saxon periods in Britain, the purpose of this thesis is to find evidence of change in human diet and animal husbandry in the Upper Thames Valley across this boundary. Research questions are set to find differences in human diet, animal diet, and birth seasonality of herbivores at Horcott, a site showing human activity in both periods. Stable carbon and nitrogen isotope measurements on collagen from humans and livestock animals and enamel carbonate extracted from herbivores were analysed. Results showed changes in the diets of cattle, sheep/goats, pigs, and human, and birth seasonality of cattle and sheep/goats. These changes were argued to have been caused by differences in the intensity of fertilising crop fields, the amount of animal protein fed to adult pigs, the amount of non-local food in human diet, and the significance and purpose of livestock rearing and the preference of dairy products. The outcome of this thesis enhances the understanding of: a) the strategy and the amount of human effort put into crop cultivation and livestock management; b) the availability and preference of food for humans depending on the period; and c) the site-dependent differences in the extent of change in the course of transition between the Romano-British and Anglo-Saxon periods. This thesis demonstrates the importance of animal data in order to discuss human diet, and the advantage of modelling enamel carbonate sequential data when analysing worn and shortened teeth.

No / Is it possible to identify cooked, rather than burnt, bone? Mild heating (≤100 °C,1 h) – typical of cooking – does not lead to detectable changes in any biochemical parameter of bone yet measured. If it is only possible to detect charred bone, how is it possible to detect cooking in the archaeological record? In a previous paper (Koon et al., 2003, J. Arch. Sci.), we used a Transmission Electron Microscopy (TEM) based approach to investigate changes in the organization of the bone protein, collagen, as it is heated, using bone from heating experiments and short term burials. The work revealed that mineralized collagen, despite requiring aggressive treatment to gelatinise the protein (e.g. 90 °C, 240+ h), readily accumulates minor damage. We believe that the presence of mineral matrix stabilises the collagen enabling the damage to accumulate, but preventing it from causing immediate gelatinisation. Once the mineral is removed, the damage can be observed using appropriate visualization methods. In this paper the visualization technique was tested in a blind study of bovine bone from the Anglo-Scandinavian site of Coppergate, York. The purpose of the study was to determine if the method could discriminate between bones thought likely, on the basis of zoo-archaeological and spatial evidence, to have been cooked (high meat yield bones from a domestic context) and those which were butchered but unlikely to have been cooked (low yield bones from a butchery site). The results of the TEM analysis identified two clear groups of bones, one set more damaged than the other. This finding was consistent with archaeozoological interpretation, with the exception of one bone from the domestic context, which was not identified as having been cooked.

Yes / The Early Bronze Age barrows at Irthlingborough and Gayhurst in central England are notable for the large number of cattle (Bos taurus) remains associated with their human Beaker burials. Previous work using strontium isotope analysis has indicated that most of the cattle analysed, and one aurochs (Bos primigenius), were of local origin (Towers et al. 2010). In this study, stable isotope analysis of enamel and bone was carried out to investigate whether the mature cattle had experienced similar husbandry practices, climate and environment. Bulk carbon, nitrogen and sulphur isotope analysis of collagen suggested most were consuming similar sources of plant protein from environments probably local to the sites and this was supported by high resolution intra-enamel carbon isotope profiles. Oxygen isotope profiles indicated the aurochs and most of the cattle experienced similar climatic regimes: the only exception being an animal with a non-local strontium isotope ratio. However, a comparison of seasonality profiles of the local animals using estimated tooth formation times showed that there was no consistency in season of birth: the animals appeared to have been born throughout the year. Cattle can breed throughout the year but it requires considerable human effort and intervention to successfully overwinter young stock; it is therefore unlikely to have been carried out without good reason and benefit if winters were harsh. One reason is to ensure a continuous supply of milk. Measuring oxygen isotope profiles to identify year-round calving may thus be a potential indicator of dairying economies.

Yes / The carbon (δ13C) and nitrogen (δ15N) isotope ratios of human bone collagen have been used extensively over the last 40 years to investigate the diet of past populations. It has become apparent that bone collagen can give an unreliable temporal dietary signature especially in juveniles. With higher temporal resolution sampling of collagen from tooth dentine, it is possible to identify short‐term changes in diet previously invisible in bone. This paper discusses the inherent problems of using bone collagen for dietary studies and suggests better sample choices which can make our interpretations more robust, using breastfeeding and weaning as an example. / The modern data was collected and analysed using funding from the Rank Prize Funds New Investigator Award and sponsorship from DB Orthodontics, Bradford. The Tooth Fairy team acknowledges the support of the National Institute for Health Research Clinical Research Network (NIHR CRN). / Research Development Fund Publication Prize Award winner, February 2020.

Yes / Objectives: Diffuse idiopathic skeletal hyperostosis (DISH) has recurrently been associated with a rich diet (high in protein and higher trophic level foods); however, very few studies have investigated this link using carbon and nitrogen (δ13C and δ15N) stable isotope analysis. This paper explores the relationship between DISH and diet in two Roman urban communities by analyzing individuals with and without DISH. Materials and methods: δ13C and δ15N analysis carried out on collagen from 33 rib samples (No DISH: 27; early DISH: 4; DISH: 2) selected from individuals buried at the Romano-British site of Baldock (UK), 41 rib samples (No DISH: 38; early DISH: 3) from individuals from the Catalan Roman site of Santa Caterina (Barcelona, Spain). Additionally, six faunal samples from Baldock and seven from Santa Caterina were analyzed. Results: Standardized human isotope data from Santa Caterina show high δ15N probably associated to a diet combining terrestrial resources and freshwater fish. In contrast, isotope results from Baldock suggest a terrestrial-based diet. Individuals with DISH do not show isotopic ratios indicative of rich diet and there is no correlation between stage of DISH development and δ13C and δ15N. Conclusion: The results of this study suggest that individuals with DISH followed a similar or isotopically similar diet as those individuals without DISH in Baldock and in Santa Caterina and therefore, while DISH may have been influenced by individual's dietary habits, this is not reflected in their isotopic signature. / Institute of Life Sciences Research Studentship, University of Bradford, Bradford, UK

The utilisation of 3D digitisation and visualisation has grown considerably since 2008 and is becoming an increasingly useful tool for the digital documentation and metric analysis of archaeological artefacts and skeletal remains. It provides public access to rare and fragile specimens of palaeontological and palaeopathological importance whilst reducing the physical impact on these remains. Research in engineering and computer vision provides some insight into the impact of surface properties such as colour, specularity, reflectance and shape on the quality of the recorded 3D image, but within the archaeological and palaeontological disciplines comparable work has not yet been developed. If archaeology and anthropology are to provide long term reliable data from archaeological and palaeontological specimens in a way that doesn’t require repeated re-digitisation, we need to understand the impacts that the taphonomic histories of such samples have on our ability to 3D record them. Understanding the relationship of these taphonomic histories and the surface and optical properties will promote informed choices about the suitability of recording techniques. This thesis considers the taphonomic processes that affect the preservation of bone over archaeological, forensic and palaeontological timescales and the effect this has on the quality of 3D digital models. The digital refit of fragmentary bone samples is considered in relation to the effect of taphonomic alterations to bone. Conclusions regarding the key taphonomic factors and 3D digital model quality are drawn and areas of further work are identified.

Changes in marine production play a key role in determining the trophic structure of the northeastern Pacific Ocean. This is a region of great environmental fluctuations due to modern, historical, and paleo-environmental variability recorded throughout the Holocene. These fluctuations are recorded in the bone collagen of the marine mammals that reside in these waters. Marine mammal remains from four previously excavated archaeological deposits on Unalaska Island, Alaska are used as a proxy for marine production changes throughout the Holocene (4,500 BP to 350 BP). Historic and modern samples from museum collections, subsistence harvests, and previously published data provide a distinct contrast to prehistoric marine mammals. Stable carbon and nitrogen isotope ratios (δ13C and δ15N) derived from marine mammal bone collagen correlate to changes in marine production and food web length. The 13C and 15N of prehistoric marine mammal taxa covary through the Holocene, indicating no trophic level change with fluctuations in 13C. Changes in δ13C and δ15N of marine mammals are correlated to periods of environmental fluctuations within the Holocene. Cooler climatic periods (transitional interval, beginning of the Neoglacial Interval, and Little Ice Age) show enrichedδ13C, reflecting primary production increase, compared to warmer climate periods (end of the Neoglacial Interval into the Medieval Climatic Anomaly). Unidentified cetacean bones are isotopically distinguishable into orders Mysticeti (baleen) and Odontoceti (toothed) due to different feeding ecologies. The δ13C depletion in modern pinnipeds compared to prehistoric is likely caused by the effect of increased anthropogenic atmospheric CO2 and resulting decrease in primary production.