Reconstructing the experienced temperature during the larval oceanic migration of anguillid eels from otolith stable oxygen isotopes

Migration routes and the depth patterns of anguillid eel larvae migrating long distances from spawning grounds in the ocean remain poorly understood. We used otolith stable isotope analysis to study the oceanic migrations of anguillid eels by reconstructing experienced water temperature histories of larvae. The otolith stable oxygen isotopes (δ<sup>18</sup>O<sub>otolith</sub>) of recruited Anguilla japonica glass eels were analyzed to assess the relationship with the experienced water temperature of the early larval stage in laboratory experiments. A negative linear relationship between rearing water temperature and δ<sup>18</sup>O<sub>otolith</sub> values was observed for eel leptocephali reared at five different temperatures between 19 °C and 27 °C. Subsequently, the obtained equation between water temperature and δ<sup>18</sup>O<sub>otolith</sub> was applied to estimate the water temperature experienced by wild-caught glass eels during their larval oceanic migration according to recruitment latitude, season, and species. The δ<sup>18</sup>O<sub>otolith</sub> values of A. japonica glass eels were significantly higher at higher recruitment latitudes from Taiwan to Japan and later recruitment periods of 6 months, from November to March, indicating that the individuals were exposed to lower water temperatures along the Kuroshio flowing northward as they reached the higher latitudes in the later recruitment seasons. Furthermore, the δ<sup>18</sup>O<sub>otolith</sub> values of the temperate A. japonica were higher than those of the tropical Anguilla marmorata, recruited at the same locations in southern Japan and Taiwan. This suggests that larval migratory behavior in the ocean may differ between the two eel species, although they have sympatric spawning areas in the western North Pacific. Collectively, these results suggest that δ<sup>18</sup>O<sub>otolith</sub> provides a reasonable estimation of the experienced water temperature and may prove useful for reconstructing the early migratory history of anguillid eels in the ocean.

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Journal
Scientific Reports
Published
2025-01-10
DOI
https://doi.org/10.1038/s41598-025-85523-z
Primary Topic
Marine and fisheries research
Type
article
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article

Reconstructing the experienced temperature during the larval oceanic migration of anguillid eels from otolith stable oxygen isotopes

Mari Kuroki, Kotaro Shirai, Shunsuke Hayasaka, Toyoho Ishimura et al.
1 links
Scientific Reports
Marine and fisheries research
article

Reconstructing the experienced temperature during the larval oceanic migration of anguillid eels from otolith stable oxygen isotopes

Mari Kuroki, Kotaro Shirai, Shunsuke Hayasaka, Toyoho Ishimura, Yu‐San Han, Yoshiaki Yamada, Kozue Nishida, Akihiro Okamura
article en

Abstract

Migration routes and the depth patterns of anguillid eel larvae migrating long distances from spawning grounds in the ocean remain poorly understood. We used otolith stable isotope analysis to study the oceanic migrations of anguillid eels by reconstructing experienced water temperature histories of larvae. The otolith stable oxygen isotopes (δ<sup>18</sup>O<sub>otolith</sub>) of recruited Anguilla japonica glass eels were analyzed to assess the relationship with the experienced water temperature of the early larval stage in laboratory experiments. A negative linear relationship between rearing water temperature and δ<sup>18</sup>O<sub>otolith</sub> values was observed for eel leptocephali reared at five different temperatures between 19 °C and 27 °C. Subsequently, the obtained equation between water temperature and δ<sup>18</sup>O<sub>otolith</sub> was applied to estimate the water temperature experienced by wild-caught glass eels during their larval oceanic migration according to recruitment latitude, season, and species. The δ<sup>18</sup>O<sub>otolith</sub> values of A. japonica glass eels were significantly higher at higher recruitment latitudes from Taiwan to Japan and later recruitment periods of 6 months, from November to March, indicating that the individuals were exposed to lower water temperatures along the Kuroshio flowing northward as they reached the higher latitudes in the later recruitment seasons. Furthermore, the δ<sup>18</sup>O<sub>otolith</sub> values of the temperate A. japonica were higher than those of the tropical Anguilla marmorata, recruited at the same locations in southern Japan and Taiwan. This suggests that larval migratory behavior in the ocean may differ between the two eel species, although they have sympatric spawning areas in the western North Pacific. Collectively, these results suggest that δ<sup>18</sup>O<sub>otolith</sub> provides a reasonable estimation of the experienced water temperature and may prove useful for reconstructing the early migratory history of anguillid eels in the ocean.

Scientific ReportsVol. 15(1)
Tokyo Institute of Technology (JP), National Taiwan University (TW), Kyoto University (JP), Ibaraki National College of Technology (JP), National Institute of Technology, Kagoshima College (JP), Hitachi (Japan) (JP), The University of Tokyo (JP)
University of Tokyo, Japan Society for the Promotion of Science, Japan Science and Technology Agency
Life below water
Openalex Percentile: Top 100%
Marine and fisheries research
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