A skeleton of a male, 50-55 years old Mammuthus meridionalis, dated to the Pleistocene and conserved at the Spanish Fort in L’Aquila (Italy), showed a broken left tusk, in association with the presence of a deep (15x20 cm) bone erosion, involving the dental alveolus and the premaxillary bone, in close proximity to the maxillary sinus and the nasal cavity. During gross examination, small samples from three representative areas of the eroded bone were obtained. Thin sections were made and the specimens were examined under plane and polarized light, using a high resolution microscope with an incorporated digital camera. Microscopical study revealed the intra vitam origin of the lesions, characterized by the presence of woven bone fibers, typical of the early phases of bone remodeling, and lamellar bone with dilated and remodeled Haversian systems. The gross and histological findings were consistent with an osteomyelitis with bone sequestration, caused by a localized blunt trauma or, more likely, resulting from an ascending, post-traumatic chronic pulpitis, due to the tusk fracture occurred during an accident or interspecies fights. The histological exam excluded the involvement of granulomatous inflammation (e.g. tuberculosis) or neoplasia. A disease process of at least several months in duration may be hypothesized, as suggested by the histologically visible bone remodeling. A long survival of the animal after tusk loss may also be supposed, since alteration of masticatory function with altered molar teeth consumption and postural changes (i.e. atlantoaxial fusion), resulting from asymmetric weight distribution, were observed. In this study, the application of (paleo)histological techniques proved to be fundamental in order to establish the nature of bone lesions detected on archeological samples, also providing a good case for studying skull trauma and shedding light on the life history of these large mammals.

Paleopathological study of Mammuthus meridionalis of Madonna della Strada (L’Aquila)

FORNACIARI, GINO
2015-01-01

Abstract

A skeleton of a male, 50-55 years old Mammuthus meridionalis, dated to the Pleistocene and conserved at the Spanish Fort in L’Aquila (Italy), showed a broken left tusk, in association with the presence of a deep (15x20 cm) bone erosion, involving the dental alveolus and the premaxillary bone, in close proximity to the maxillary sinus and the nasal cavity. During gross examination, small samples from three representative areas of the eroded bone were obtained. Thin sections were made and the specimens were examined under plane and polarized light, using a high resolution microscope with an incorporated digital camera. Microscopical study revealed the intra vitam origin of the lesions, characterized by the presence of woven bone fibers, typical of the early phases of bone remodeling, and lamellar bone with dilated and remodeled Haversian systems. The gross and histological findings were consistent with an osteomyelitis with bone sequestration, caused by a localized blunt trauma or, more likely, resulting from an ascending, post-traumatic chronic pulpitis, due to the tusk fracture occurred during an accident or interspecies fights. The histological exam excluded the involvement of granulomatous inflammation (e.g. tuberculosis) or neoplasia. A disease process of at least several months in duration may be hypothesized, as suggested by the histologically visible bone remodeling. A long survival of the animal after tusk loss may also be supposed, since alteration of masticatory function with altered molar teeth consumption and postural changes (i.e. atlantoaxial fusion), resulting from asymmetric weight distribution, were observed. In this study, the application of (paleo)histological techniques proved to be fundamental in order to establish the nature of bone lesions detected on archeological samples, also providing a good case for studying skull trauma and shedding light on the life history of these large mammals.
2015
http://www.pathologica.it/volume-107-issue-3-4-september-december-2015/
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11568/788698
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