Williams, Jocelyn S
Chew the Fat: An Examination of the Preservation of Fatty Acids in Archaeological Bone
Fatty acid analysis was performed on archaeological bone from various fauna from sites in the Canadian arctic to better understand the preservation of fatty acids and their potential applications to palaeoecological and palaeodietary studies. These data were complemented by analyses of modern bone and soft tissue samples from livestock and harp seals (Pagophilus groenlandicus). Results of modern analyses revealed that in terrestrial species, bone has inherently lower concentrations of most fatty acids relative to other soft tissues (adipose, marrow, and muscle). These analyses suggest that the distribution of fatty acids in bone is unique compared to other tissues, and the types and abundances of fatty acids in bone may be linked to dietary sources of lipids. Of the archaeological samples analyzed, terrestrial species (caribou [Rangifer tarandus]) generally exhibited higher concentrations of saturated fatty acids compared to marine species (ringed seals [Pusa hispida] and polar bears [Ursus maritimus]), whereas marine species had higher concentrations of monounsaturated fatty acids compared to terrestrial species. Results of analyses on both modern and archaeological samples provided insight into the degradation of fatty acids in bone, and the rapid loss of polyunsaturated fatty acids in particular. Because the abundances of fatty acids are likely altered in the burial environment, it is recommended that future analyses incorporate compound specific isotope analysis to focus on applications of fatty acids that are typically in the highest abundance and arguably have undergone the least amount of change, including palmitic (C16:0) and stearic acid (C18:0)
Author Keywords: Archaeological Science, Bone Lipids, Fatty Acid Analysis, GC-MS, Lipid Preservation, Palaeoecology
Reassessing Bioarchaeological Sex Determination and Research into Gender at the Early Anglo-Saxon Worthy Park Burial Ground Round in Hampshire, England
When bioarchaeologists investigate ancient gender identity, they typically place skeletal remains into one of six sex assessment categories: male, female, possible/probable male, possible/probable female, ambiguous, and indeterminate. However, the study samples are often reduced to male and female reproducing a male/female gender and sex binary prevalent in the "Western" cultural milieu and bioarchaeology when inferences are made about gender and sex in the past.
In order to allow for the existence of non-binary cultural genders and biological sexes, this thesis: 1) demonstrates the multitude of ethnographic, ethnohistoric, historic, and medical evidence relating to non-binary sex and gender expression; 2) tests a method inspired by Whelan (1991) that looks at gender as an identity not fully inspired by biological sex; 3) keeps all sex assessment categories used by bioarchaeologists separate in analysis and interpretation; and 4) analyses patterns relating to all available material culture and biological attributes in a mortuary sample to investigate gender identity.
This thesis used the Early Anglo-Saxon (470-600 AD) burial ground at Worthy Park in Hampshire to achieve these objectives. This thesis found that when examining all sex assessment categories among all mortuary variables, only the male sex was clearly defined by its mortuary assemblage. This suggests a one gender structure corresponding to linguistic evidence for one gender in Old English.
Author Keywords: Anglo-Saxon, Bioarchaeology, Gender identity, Mortuary archaeology, Osteoarchaeology, Sex determination
Testing the Validity of Dental Calculus as a Proxy to Bone in Paleodietary Studies Using Stable Isotope Analysis
This study investigates the use of dental calculus for paleodietary studies using stable isotope analysis of a skeletal sample from the Greek colonial site of Apollonia Pontica, Bulgaria (5th to 3rd century BC). A sample of 27 individuals was used to examine the δ13C and δ15N values of paired dental calculus and bone samples, and the dental calculus was analyzed as separate organic and inorganic components. No significant correlation was found between the δ13C values of either the bone collagen and organic dental calculus samples, or the bone apatite and inorganic dental calculus samples. A significant correlation was found between the δ15N values of the bone collagen and organic dental calculus samples; however, the reason for this correlation is unclear. A greater range of variation in the δ13C and δ15N values was found in the organic dental calculus samples compared to the respective bone collagen samples. These results suggest that dental calculus is not an appropriate proxy to bone for paleodietary studies using stable isotope analysis and that any dietary signal is clouded by other data. The oral microbiome is considerably diverse and is the most probable explanation for the great range of stable isotope values obtained from dental calculus. A significant, strong correlation was found between the C/N ratios and δ15N values of the organic dental calculus samples, suggesting that the lowest C/N ratios and δ15N values depict deposits with the least bacterial alteration.
Author Keywords: carbon, dental calculus, nitrogen, paleodietary studies, Social Sciences, stable isotopes