Bone weathering patterns of metatarsal v. femur and the postmortem interval in Southern Ontario.
Twenty-five defleshed pig femora and 25 metatarsals were placed outdoors and observed over 291 days to establish: (1) bone weathering patterns for use in estimating time since death in Southern Ontario and (2) whether larger (femora) or smaller (metatarsals) bones provide a better indicator of time since death. Pig hind limbs were observed to determine a timeline for decomposition of soft tissues during the fall and winter. Ambient air temperature, humidity, precipitation, sunlight, soil pH, and freezing and thawing were considered as factors affecting the breakdown of bone. Weathering patterns were observed based on the extent of bleaching, amount of periosteum and soft tissues present, as well as the appearance of greasiness, cracking and flaking of cortical bone. Both entomological activity and climatic conditions affected soft tissue decomposition. Animal activity affected both the process of bone weathering and soft tissue decomposition, causing variability in sample decomposition and bone breakdown. The variation in microenvironment, partially caused by soil composition, introduced variability in bone weathering rates. Four bone weathering stages were established based on patterns observed. Femora proved to be more resilient and showed more degrees of change due to weathering, thus proving to be a better indicator of time since death than metatarsals.
Janjua
Martyna A
MA
McMaster University, Department of Anthropology, 1280 Main Street West, Hamilton, Ontario, Canada L8S 4L9.
Rogers
Tracy L
TL
D000818:Animals; D005247:Feeding Behavior; D005269:Femur / Q000473:pathology*; D018732:Forensic Anthropology; D005658:Fungi / Q000254:growth & development; D006863:Hydrogen-Ion Concentration; D008682:Metatarsal Bones / Q000473:pathology*; D009864:Ontario; D011180:Postmortem Changes; D012987:Soil; D034421:Sus scrofa; D014887:Weather
D012987:Soil