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Experimental support towards a metabolic proxy in fish using otolith carbon isotopes
Jasmin C Martino1, Zoë A Doubleday2, Ming-Tsung Chung3
1Southern Seas Ecology Laboratories, School of Biological Sciences, The University of Adelaide, Adelaide, SA 5005, Australia Jasmin.Martino@unisa.edu.au.
The Journal of Experimental Biology
|March 30, 2020
Summary
Stable carbon isotopes in fish otoliths can estimate metabolic rates, a crucial factor for survival and reproduction. This study validates using these isotopes as a reliable proxy for metabolic signatures in wild fish populations.
Area of Science:
- Physiological Ecology
- Isotope Geochemistry
- Fisheries Science
Background:
- Metabolic rate is fundamental to fish survival, reproduction, and ecological interactions, yet challenging to measure in wild populations.
- Stable isotopes, specifically carbon isotopes (δ13C) in otoliths, show potential as indicators of lifetime metabolic signatures.
- Experimental validation is essential to confirm the utility of otolith δ13C as a metabolic proxy.
Purpose of the Study:
- To experimentally validate the use of stable carbon isotopes (δ13C) in fish otoliths as a proxy for metabolic rate.
- To investigate the relationship between environmental temperature, metabolic rates (SMR, MMR, AAS), and otolith isotopic signatures (δ13C, δ18O).
- To establish quantitative relationships between otolith δ13C and metabolic rate components for application in wild fish.
Main Methods:
- Juvenile Australasian snapper (Chrysophrys auratus) were reared under varying temperatures.
- Standard metabolic rate (SMR) and maximum metabolic rate (MMR) were determined using intermittent-flow respirometry.
- Otoliths were analyzed for stable carbon (δ13C) and oxygen (δ18O) isotopes using isotope-ratio mass spectrometry.
Main Results:
- Increasing temperatures led to significant decreases in otolith δ13C and δ18O, alongside increases in SMR and MMR.
- Negative logarithmic relationships were observed between otolith δ13C and both SMR and MMR.
- Exponential decay curves linked the proportion of metabolically sourced carbon in otoliths (Moto) to SMR, indicating physiological thresholds regulate these relationships.
Conclusions:
- Otolith δ13C serves as a reliable proxy for metabolic rates, reflecting both basal energy for subsistence and activity metabolism.
- The quantitative relationships established support the use of otolith δ13C for reconstructing lifetime metabolic trends in wild fish.
- This validated proxy offers a powerful tool for ecological and fisheries research, overcoming limitations of direct metabolic measurements in natural environments.

