Effect of X-ray irradiation on ancient DNA in sub-fossil bones - Guidelines for safe X-ray imaging
Immel APapers in this archive, Le Cabec APapers in this archive, Bonazzi MPapers in this archive, Herbig APapers in this archive, Temming HPapers in this archive, Schuenemann VJPapers in this archive, Bos KIPapers in this archive, Langbein FPapers in this archive, Harvati KPapers in this archive, Bridault APapers in this archive, Pion GPapers in this archive, Julien MAPapers in this archive, Krotova OPapers in this archive, Conard NJPapers in this archive, Münzel SCPapers in this archive, Drucker DGPapers in this archive, Viola BPapers in this archive, Hublin JJPapers in this archive, Tafforeau PPapers in this archive, Krause JPapers in this archive
Abstract
Sub-fossilised remains may still contain highly degraded ancient DNA (aDNA) useful for palaeogenetic investigations. Whether X-ray computed [micro-] tomography ([μ]CT) imaging of these fossils may further damage aDNA remains debated. Although the effect of X-ray on DNA in living organisms is well documented, its impact on aDNA molecules is unexplored. Here we investigate the effects of synchrotron X-ray irradiation on aDNA from Pleistocene bones. A clear correlation appears between decreasing aDNA quantities and accumulating X-ray dose-levels above 2000 Gray (Gy). We further find that strong X-ray irradiation reduces the amount of nucleotide misincorporations at the aDNA molecule ends. No representative effect can be detected for doses below 200 Gy. Dosimetry shows that conventional μCT usually does not reach the risky dose level, while classical synchrotron imaging can degrade aDNA significantly. Optimised synchrotron protocols and simple rules introduced here are sufficient to ensure that fossils can be scanned without impairing future aDNA studies.
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