Analysis of traces of prints and the effects of wind on bones of a modern vertebrate: contribution of taphonomy to the forensic registry

Introduction: Taphonomic analysis of bone remains could allow us to obtain information on some of thepost-depositional processes that affected them in the short, medium and long term. This work aims to expose some of the results on the formation and distribution of prints on bone remains as part of...

Full description

Autores:
Nasti, Atilio
Tipo de recurso:
Article of journal
Fecha de publicación:
2019
Institución:
Universidad Cooperativa de Colombia
Repositorio:
Repositorio UCC
Idioma:
spa
OAI Identifier:
oai:repository.ucc.edu.co:20.500.12494/44372
Acceso en línea:
https://revistas.ucc.edu.co/index.php/ml/article/view/2881
https://hdl.handle.net/20.500.12494/44372
Palabra clave:
forensic anthropology
environmental prints
taphonomic history
post mortem interval
antropología forense
huellas medioambientales
historia tafonómica
intervalo post mortem
antropologia forense
pegadas meio ambientais
história tafonômica
intervalo post mortem
Rights
openAccess
License
http://purl.org/coar/access_right/c_abf2
Description
Summary:Introduction: Taphonomic analysis of bone remains could allow us to obtain information on some of thepost-depositional processes that affected them in the short, medium and long term. This work aims to expose some of the results on the formation and distribution of prints on bone remains as part of the diagenetic processes. Methods and materials: For the print analysis, five samples of flat bones, analyzed by means of the electron scanning electron microscopy technique, were selected. To obtain topographic images of the prints, a 3D optical profilometer was used. Results and discussion: Whilst pressing the periosteum surface onto the sediment, ablations (continuity solutions due to collapse of the periosteum) occur that are frequently associated with the presence of multiple prints. With respect to the marks produced by wind erosion, these show two types of morphology: one is presented as small holes with symmetrical perimeters, generally coinciding with the morphology of sediment grains. The other type of print shows a more asymmetrical shape in the form of an elongated shape. Conclusion: The taphonomic processes can be reconstructed from a diachronic sequence of the alteration that allows modeling a timeline that reconstructs the processes that affected the organic remains since the death of an organism. The diagenetic model of Equus sp. shows that wind erosion could remain within a few weeks of deposition and would act over longer periods of time, with an interruption period at the time of burial of Equus via sedimentation processes.