Gemstone Windows and Dark Patches: What to Look for in a Cut Gem
Radiocarbon research adds a time-related question to pearl testing: when did the sampled pearl material form? This can help investigate historical claims, but age and natural-versus-cultured formation are different questions. A recent pearl can be either natural or cultured.
SSEF’s 2013 article describes collaboration with ETH Zurich. A small amount of pearl material was removed and measured using accelerator mass spectrometry. The method used carbon-isotope information, including the increase linked to twentieth-century atmospheric nuclear testing.
Unlike an X-ray image, this procedure consumes a sample. The article describes an early research project, so its sampling amount and service availability should not be assumed to apply to every current test.
Marine reservoir effects can influence the apparent age. Freshwater pearls may be especially difficult because older carbon from limestone can enter the growing pearl. The resulting number needs calibration and environmental context; it is not automatically an exact calendar year.
SSEF explains that pearl formation still needs assessment with radiography and microtomography. An age consistent with an old object may support its history without proving every provenance claim. Ask what part was sampled, what uncertainty applies and whether separate evidence established natural or cultured origin. A scientific age is most useful when the interpretation and its limits are clearly explained.
SSEF Swiss Gemmological Institute, Facette, issue 20, January 2013, pp. 16, “Radiocarbon Age Dating of Pearls”. Read the original SSEF PDF.
This independent educational article explains historical SSEF research in original, simple English. It is not an SSEF publication. No source photographs or illustrations are reproduced.
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