Temperature and depth distribution of Japanese eel eggs estimated using otolith oxygen stable isotopes

• Published in: Geochimica et cosmochimica acta 2018-09, Vol.236, p.373-383
• Main Authors: Shirai, Kotaro, Otake, Tsuguo, Amano, Yosuke, Kuroki, Mari, Ushikubo, Takayuki, Kita, Noriko T., Murayama, Masafumi, Tsukamoto, Katsumi, Valley, John W.
• Format: Article
• Language: English
• Subjects: Anguilla japonica; Glass eel; Otolith; Oxygen stable isotopes; SIMS; Spawning temperature and depth
• ISSN: 0016-7037; 1872-9533
• DOI: 10.1016/j.gca.2018.03.006

Oxygen isotope ratios of the core region of otoliths were examined in Anguilla japonica glass eels collected from two rivers in Japan to verify the possible temperature and depth layer experienced by these eels when they were at the egg stage in their spawning area. To determine the relationship between otolith δ18O values and water temperature, the otoliths of glass eels reared under four different temperatures (15, 20, 25 and 30 °C) were analyzed. The otolith δ18O values showed an inverse relationship to ambient water temperature. Linear regression of the fractionation between otolith oxygen isotopic ratio from the δ18O of seawater and water temperature produced a precisely determined relationship from 15 to 30 °C: δ18Ootolith,PDB − δ18Oseawater,SMOW = −0.153 × T (°C) + 1.418. The δ18O core,PDB values of the otolith core region of the glass eels from the two locations were −2.53 ± 0.12 and −2.59 ± 0.07 respectively, and could be converted to water temperatures of 26.3 ± 0.8 °C and 26.7 ± 0.4 °C, respectively, using the equation and assuming a seawater δ18Oseawater,SMOW = 0.06‰. The water depth corresponding to these temperatures is ∼150 m in the water column in the spawning area of Japanese eels, which corresponds to the upper-most part of the thermocline and chlorophyll maximum in the vertical hydrographic profile. These results were consistent with the field studies that egg development after the beginning of otolith formation and hatching occurs around the upper-most part of thermocline, suggesting that stable isotope micro-analysis is a powerful method to extrapolate unknown spawning ecology of fishes.