Volume 69, Issue 5 pp. 1658-1670
TECHNICAL NOTE

Disaster victim identification: Stable isotope analysis and the identification of unknown decedents

Lesley A. Chesson MS

Lesley A. Chesson MS

Defense POW/MIA Accounting Agency Laboratory, Joint Base Pearl Harbor-Hickam, Honolulu, Hawaii, USA

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Gregory E. Berg PhD

Corresponding Author

Gregory E. Berg PhD

Defense POW/MIA Accounting Agency Laboratory, Joint Base Pearl Harbor-Hickam, Honolulu, Hawaii, USA

Correspondence

Gregory E. Berg, Defense POW/MIA Accounting Agency Laboratory, Joint Base Pearl Harbor-Hickam, Honolulu, HI 96853, USA.

Email: [email protected]

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Mary Megyesi PhD

Mary Megyesi PhD

Defense POW/MIA Accounting Agency Laboratory, Joint Base Pearl Harbor-Hickam, Honolulu, Hawaii, USA

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First published: 10 June 2024
Citations: 4

Presented in part at the 74th Annual Scientific Meeting of the American Academy of Forensic Sciences, February 21–25, 2023, in Seattle WA; and at the 75th Annual Scientific Meeting of the American Academy of Forensics Sciences, February 13–18, 2023, in Orlando, FL.

Abstract

Within the complex world of disaster victim identification, or DVI, forensic science practitioners use a variety of investigative techniques to work toward a common goal: identification of the decedents, bringing closure to the affected communities. Identification is a complex undertaking; the event (disaster) also can be extraordinarily complex, as it may be an acute event, or one that spans months or years. Compounding this time issue, remains may be heavily fragmented, dispersed, commingled, or otherwise disrupted by either the perpetrators or the disaster itself. To help solve these complexities, we explore the use of stable isotope analysis (SIA) in DVI events. SIA can be used with a variety of body tissues (hair, nail, bone, and teeth), and each represents different time depths in a decedent's life. Bone collagen and tooth enamel carbonate are useful to reconstruct an individual's diet and source water intakes, respectively, leading to likely population or geographic origin determinations. Additionally, the carbon and nitrogen isotopic signatures of bone collagen have calculated intraperson ranges. These facts allow investigators to determine likely origin of remains using isotopic data and can be used to link skeletal elements (to an individual), or perhaps more importantly, show that remains are not linked. Application of SIA can thus speed remains identification by eliminating individuals from short lists for identification, linking or decoupling remains, and reducing the need for some DNA testing. These strategies and hypothesis tests should commence early in the DVI process to achieve maximum effectiveness.

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