Reconstruction of temperature experienced by Pacific bluefin tuna Thunnus orientalis larvae using SIMS and microvolume CF-IRMS otolith oxygen isotope analyses
英文:
Reconstruction of temperature experienced by Pacific bluefin tuna Thunnus orientalis larvae using SIMS and microvolume CF-IRMS otolith oxygen isotope analyses
<jats:p>This study aimed to reconstruct temperatures experienced during the larval period by adult Pacific bluefin tuna <jats:italic>Thunnus orientalis</jats:italic> using high-resolution otolith stable oxygen isotope (δ<jats:sup>18</jats:sup>O) analysis. A novel otolith sample preparation protocol for secondary ion mass spectrometry (SIMS) analysis developed in this study reduced the background noise of SIMS measurements, enabling analyses of >10 times higher resolution around the otolith core compared to previous studies using conventional isotope ratio mass spectrometry (IRMS). The values obtained from SIMS were compared to those obtained by microvolume δ<jats:sup>18</jats:sup>O<jats:sub>otolith</jats:sub> analysis using micromilling and conventional continuous-flow IRMS (CF-IRMS). There was a systematic offset (average 0.41‰ with SIMS resulting in lower values) most likely caused by matrix effects on SIMS δ<jats:sup>18</jats:sup>O<jats:sub>otolith</jats:sub> values that can be calibrated using a strong linear relationship between SIMS and CF-IRMS measurements (r<jats:sup>2</jats:sup> = 0.78, p < 0.001). The core-to-edge δ<jats:sup>18</jats:sup>O<jats:sub>otolith</jats:sub> of 5 Pacific bluefin tuna revealed fine-scale seasonal variations in water temperature agreeing with known migration patterns. In addition, the ambient water temperature experienced during larval stages (about 10-20 d post hatch) estimated from otolith core δ<jats:sup>18</jats:sup>O ranged from 26.7 to 30.7°C, overlapping with temperatures associated with the occurrence of larval Pacific bluefin tuna. Combining SIMS and microvolume CF-IRMS δ<jats:sup>18</jats:sup>O <jats:sub>otolith</jats:sub> analyses offers a microscale examination of fish ecology that is not possible with conventional IRMS techniques. This novel method is particularly useful for understanding the early life history of fish that may be affected by climate change and reconstructing a well-resolved migration history for fish species that have small otoliths and/or narrow growth increments.</jats:p>
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