Moisture can be the dominant environmental parameter governing cadaver decomposition in soil.
Forensic taphonomy involves the use of decomposition to estimate postmortem interval (PMI) or locate clandestine graves. Yet, cadaver decomposition remains poorly understood, particularly following burial in soil. Presently, we do not know how most edaphic and environmental parameters, including soil moisture, influence the breakdown of cadavers following burial and alter the processes that are used to estimate PMI and locate clandestine graves. To address this, we buried juvenile rat (Rattus rattus) cadavers (approximately 18 g wet weight) in three contrasting soils from tropical savanna ecosystems located in Pallarenda (sand), Wambiana (medium clay), or Yabulu (loamy sand), Queensland, Australia. These soils were sieved (2mm), weighed (500 g dry weight), calibrated to a matric potential of -0.01 megapascals (MPa), -0.05 MPa, or -0.3 MPa (wettest to driest) and incubated at 22 degrees C. Measurements of cadaver decomposition included cadaver mass loss, carbon dioxide-carbon (CO(2)-C) evolution, microbial biomass carbon (MBC), protease activity, phosphodiesterase activity, ninhydrin-reactive nitrogen (NRN) and soil pH. Cadaver burial resulted in a significant increase in CO(2)-C evolution, MBC, enzyme activities, NRN and soil pH. Cadaver decomposition in loamy sand and sandy soil was greater at lower matric potentials (wetter soil). However, optimal matric potential for cadaver decomposition in medium clay was exceeded, which resulted in a slower rate of cadaver decomposition in the wettest soil. Slower cadaver decomposition was also observed at high matric potential (-0.3 MPa). Furthermore, wet sandy soil was associated with greater cadaver decomposition than wet fine-textured soil. We conclude that gravesoil moisture content can modify the relationship between temperature and cadaver decomposition and that soil microorganisms can play a significant role in cadaver breakdown. We also conclude that soil NRN is a more reliable indicator of gravesoil than soil pH.
Carter
David O
DO
School of Pharmacy and Molecular Sciences, James Cook University, Douglas, QLD 4811, Australia. dcarter2@unl.edu
Yellowlees
David
D
Tibbett
Mark
M
D000818:Animals; D002048:Burial; D002244:Carbon / Q000032:analysis; D002245:Carbon Dioxide / Q000032:analysis; D018732:Forensic Anthropology; D006863:Hydrogen-Ion Concentration; D009555:Ninhydrin / Q000032:analysis; D009584:Nitrogen / Q000032:analysis; D010447:Peptide Hydrolases / Q000032:analysis; D010727:Phosphoric Diester Hydrolases / Q000032:analysis; D011180:Postmortem Changes; D051381:Rats; D012987:Soil; D014867:Water
D012987:Soil; D014867:Water; D002245:Carbon Dioxide; D002244:Carbon; D010727:Phosphoric Diester Hydrolases; D010447:Peptide Hydrolases; D009555:Ninhydrin; D009584:Nitrogen