Evaluation of micromilling/conventional isotope ratio mass spectrometry and secondary ion mass spectrometry of δ 18 O values in fish otoliths for sclerochronology
Autor: | Reinhard Kozdon, John W. Valley, Thomas E. Helser, Ian J. Orland, Craig R. Kastelle, Jennifer L. McKay |
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Rok vydání: | 2018 |
Předmět: |
0106 biological sciences
Fish migration biology Resolution (mass spectrometry) Chemistry 010604 marine biology & hydrobiology 010401 analytical chemistry Organic Chemistry Pacific cod Mineralogy Mass spectrometry biology.organism_classification 01 natural sciences 0104 chemical sciences Analytical Chemistry Secondary ion mass spectrometry medicine.anatomical_structure Sclerochronology medicine Isotope-ratio mass spectrometry Spectroscopy Otolith |
Zdroj: | Rapid Communications in Mass Spectrometry. 32:1781-1790 |
ISSN: | 1097-0231 0951-4198 |
DOI: | 10.1002/rcm.8231 |
Popis: | Rationale Stable oxygen isotope ratios (δ18 O values) measured in fish otoliths can provide valuable detailed information on fish life history, fish age determination, and ocean thermography. Traditionally, otoliths are sampled by micromilling followed by isotope ratio mass spectrometry (IRMS), but direct analysis by secondary ion mass spectrometry (SIMS) is becoming more common. However, these two methods have not been compared to determine which, if either, is better for fish age validation studies. Hence, the goals were to: (1) determine if the δ18 O signatures from the two different methods are similar, (2) determine which method is better for fish age validation studies, and (3) examine biogeographic and migration history. Methods Both analytical techniques, micromilling/IRMS and SIMS, were used to measure δ18 O values in six Pacific cod (Gadus macrocephalus) otoliths. A series of measurements was made from the center of each otolith to its edge to develop a life-history δ18 O signature for each fish. Results The sampling resolution of SIMS analyses was 2-3 times greater than that obtained by micromilling/IRMS. We found an offset between SIMS and micromilling/IRMS δ18 O values, about 0.5‰ on average, with SIMS yielding lower values. However, the δ18 O patterns from both methods (i.e., the number of δ18 O maxima) correspond to the estimated age determined by otolith growth-zone counts, validating fish age determination methods. Conclusions Both techniques resolved δ18 O life-history signatures and showed patterns consistent with seasonal variation in temperatures and changes due to fish migration. When otoliths are large, micromilling/IRMS can provide adequate resolution for fish age validation. However, SIMS is the better option if greater sampling resolution is required, such as when otoliths are small or specimens are longer lived and have compact growth zones. |
Databáze: | OpenAIRE |
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