3D visualization of bioerosion in archaeological bone
More On Article
- Reading All the Lines of Archaeological Legacy Records
- Early Gravettian genomic data from Western Europe reveal population movements before the LGM
- At the onset of the Late Gravettian: An updated chronology and stratigraphy for the multi-layered Gravettian open-air site Grub-Kranawetberg I (Austria).
- New Chronology Sheds Light on Human Occupation just before the onset of the Last Glacial Maximum
- Fire, temperature control, and silcrete heat treatment at Diepkloof and Mertenhof Rock Shelters, West Coast, South Africa
Duffett Carlson, K.S., Mandl, K., McCall, A., Brönnimann, D., Teschler-Nicola, M., Weiss-Krejci, E., Metscher, B., 2022. 3D visualization of bioerosion in archaeological bone. Journal of Archaeological Science 145, 105646.
Abstract
Palaeoradiology is increasingly being used in archaeological and forensic sciences as a minimally invasive alternative to traditional histological methods for investigating bone microanatomy and its destruction by diagenetic processes. To better understand ancient mortuary practices, taphonomic studies using microCT scanning methods are gaining an ever more important role. Recently it was demonstrated that 2D virtual sections obtained by microCT scanning of intact samples are comparable to physical sections for the rating and diagnosis of bioerosion in archaeological bone. Importantly, volume image data obtained from tomographic methods also allow the rendering and analysis of 3D models. Building on these methods we provide (1) detailed descriptions of bioerosion in 3D volume renderings, virtual sections, and traditional micrographs, and (2) accessible techniques for the visualization of bioerosion in skeletal samples. The dataset is based on twenty-eight cortical bone samples, including twenty femora (of which five are cremated), two ribs, two parietals, one mandibular ramus, one humerus, and two faunal long bones from five archaeological sites in Lower Austria dating from the Early Neolithic to the Late Iron Age. Notably, we reduce the need for time-consuming image segmentation by sequentially applying two noise-reducing, edge-preserving filters, and using an image-display transfer function that visualizes bioerosion, as well as Haversian and Volkmann canal structure and density in 3D. In doing so we are also able to visualize in 3D the invasion of canals by microbiota, which has previously only been reported in 2D sections. Unlike conventional thin sections, the 3D volume images shown here are easy to create and interpret, even for archaeologists inexperienced in histology, and readily facilitate the illustration and communication of microtaphonomic effects.