Elemental analysis of vertebrae discerns diadromous movements of threatened non-marine elasmobranchs.
Michael I GrantPeter M KyneJulie JamesYi HuSushmita MukherjiYolarnie AmepouLeontine BajeAndrew ChinGrant JohnsonTegan LeeBrandon MahanChristopher WursterWilliam T WhiteColin A SimpfendorferPublished in: Journal of fish biology (2023)
River sharks (Glyphis spp.) and some sawfishes (Pristidae) inhabit riverine environments, although their long-term habitat use patterns are poorly known. We investigated the diadromous movements of the northern river shark (Glyphis garricki), speartooth shark (Glyphis glyphis), narrow sawfish (Anoxypristis cuspidata), and largetooth sawfish (Pristis pristis) using in situ laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) on vertebrae to recover elemental ratios over each individual's lifetime. We also measured elemental ratios for the bull shark (Carcharhinus leucas) and a range of inshore and offshore stenohaline marine species to assist in interpretation of results. Barium (Ba) was found to be an effective indicator of freshwater use, while lithium (Li) and strontium (Sr) were effective indicators of marine water use. The relationships between Ba and Li, and Ba and Sr were negatively correlated, while the relationship between Li and Sr was positively correlated. Both river shark species had elemental signatures indicative of prolonged use of upper estuarine environments, while adults appear to mainly use lower estuarine environments rather than marine. Decreases in Li:Ba and Sr:Ba at the end of the pre-natal growth zone of P. pristis samples indicated that parturition likely occurs in freshwater. There was limited evidence of prolonged riverine habitat use for A. cuspidata. The results of this study support elemental-environment relationships observed in teleost otoliths, and indicate that in situ LA-ICP-MS elemental characterization is applicable to a wide range of elasmobranch species as a discriminator for use and movement across salinity gradients. A greater understanding of processes that lead to element incorporation in vertebrae, and relative concentrations in vertebrae with respect to the ambient environment, will improve the applicability of elemental analysis to understand movements across the life history of elasmobranchs into the future. This article is protected by copyright. All rights reserved.