Pearl grafting: Tracking the biological origin of nuclei by straightforward immunological methods

Abstract

International audienceFrench Polynesia is renowned for the production of Tahitian black pearl. These gems are obtained by grafting a nucleus into the gonad of a receiving oyster together with a graft, i.e. a small section of mantle tissue of a donor oyster. This procedure initiates the formation of a pearl sack around the nucleus, and subsequently, the deposition of concentric layers of nacre. The nucleus plays a key-role in pearl formation and its characteristics influence markedly the quality of the final product. As it is manufactured from mollusc shells, it contains a small percentage of organics. In the present paper, we used a set of biochemical techniques to characterize and compare the organic matrices from two types of nuclei that are currently used in French Polynesia: that from the freshwater mussel Amblema sp., and that from the pearl oyster Pinctada sp. To this end, we extracted the matrices from nuclei and performed FT-IR, monodimensional electrophoresis, and enzyme-linked immuno-sorbent assay (ELISA). Our data show that the matrix associated with Amblema nuclei has a very different biochemical signature from that of Pinctada nuclei, a fact that may explain the improved tolerance of grafted oysters to nuclei of Pinctada origin. In the absence of complex physical methods of investigation, simple immunological techniques and FT-IR performed on the extracted organic matrix are extremely reliable and effective for discriminating nuclei from these two sources. We assert that such techniques can be used as a diagnostic test to track unambiguously the biological origin of nuclei to avoid fraud

The shell matrix and microstructure of the Ram’s Horn squid: Molecular and structural characterization

“…At this stage of investigations, the reason of this variance from other samples remains still undetermined. However, in recent studies on other shells of marine animals, such as Pinctada margaritifera (Schmitt et al, 2018) and Porites australiensis (Takeuchi et al, 2018), we already made the same spectroscopic observations on AIM fractions leading to comparable suppositions about the presence of PO4 3 groups.…”