Quantifying fish otolith mineralogy for trace-element chemistry studies

R. Seth Wood, Bryan C. Chakoumakos, Allison M. Fortner, Kat Gillies-Rector, Matthias D. Frontzek, Ilia N. Ivanov, Linda C. Kah, Brian Kennedy, Brenda M. Pracheil

Research output: Contribution to journalArticlepeer-review

8 Scopus citations

Abstract

Otoliths are frequently used to infer environmental conditions or fish life history events based on trace-element concentrations. However, otoliths can be comprised of any one or combination of the three most common polymorphs of calcium carbonate—aragonite, calcite, and vaterite—which can affect the ecological interpretation of otolith trace-element results. Previous studies have reported heterogeneous calcium carbonate compositions between left and right otoliths but did not provide quantitative assessments of polymorph abundances. In this study, neutron diffraction and Raman spectroscopy were used to identify and quantify mineralogical compositions of Chinook salmon Oncorhynchus tshawytscha otolith pairs. We found mineralogical compositions frequently differed between otoliths in a pair and accurate calcium carbonate polymorph identification was rarely possible by visual inspection alone. The prevalence of multiple polymorphs in otoliths is not well-understood, and future research should focus on identifying otolith compositions and investigate how variations in mineralogy affect trace-element incorporation and potentially bias environmental interpretations.

Original languageEnglish
Article number2727
JournalScientific Reports
Volume12
Issue number1
DOIs
StatePublished - Dec 2022

Funding

We thank Jim Long, Karin Limburg, and Jessica Leuders-Dumont for comments that improved this manuscript. Funding was provided by ORNL Laboratory Directed Research and Development SEED funds awarded to BMP and BCC. This research used resources at the High Flux Isotope Reactor and the Center for Nanophase Materials Sciences, U.S. Department of Energy Office of Science User Facilities operated by the Oak Ridge National Laboratory. RSW was funded by the U.S. Department of Energy Science Undergraduate Laboratory Internship program. We thank Jim Long, Karin Limburg, and Jessica Leuders-Dumont for comments that improved this manuscript. Funding was provided by ORNL Laboratory Directed Research and Development SEED funds awarded to BMP and BCC. This research used resources at the High Flux Isotope Reactor and the Center for Nanophase Materials Sciences, U.S. Department of Energy Office of Science User Facilities operated by the Oak Ridge National Laboratory. RSW was funded by the U.S. Department of Energy Science Undergraduate Laboratory Internship program.

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