日本地球惑星科学連合2018年大会

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セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS09] Marine ecosystems and biogeochemical cycles: theory, observation and modeling

2018年5月23日(水) 13:45 〜 15:15 105 (幕張メッセ国際会議場 1F)

コンビーナ:伊藤 進一(東京大学大気海洋研究所)、平田 貴文(北海道大学地球環境科学研究院)、Eileen E Hofmann (共同)、Enrique N Curchitser (Rutgers University New Brunswick)、座長:伊藤 進一(東京大学)

14:15 〜 14:30

[AOS09-14] Reconstruction of experienced temperature in early stage of chub mackerels Scomber japonicas by otolith oxygen isotope measurement

*樋口 富彦1石村 豊穂2上村 泰洋3白井 厚太朗1進藤 花2西田 梢2小松 幸生1伊藤 進一1 (1.東京大学大気海洋研究所、2.茨城工業高等専門学校、3.国立研究開発法人水産研究・教育機構 中央水産研究所)

The growth of chub mackerel is influenced by marine environment such as water temperature. It has been reported that the growth rate of the juvenile has a positive correlation between the sea surface temperatures. However, the water temperature that chub mackerel juvenile actually experiences is not directly observed, and the growth and the experienced environment are not compared. In this study, oxygen stable isotope (δ18O) of chub mackerel otolith in early stage were analyzed and the experienced temperature was estimated. Larvae and juveniles of chub mackerel Scomber japonicus were collected in the western North Pacific. After measuring fork length, radius of otolith, number of daily rings and otolith daily growth rate, δ18O were analyzed with isotope ratio mass spectrometer for whole of otolith samples from 2004 to 2015 (10-20 samples per year, excluding 2006). For the juveniles, the δ18O value was positively correlated with the radius of otolith (R=0.73, n=130). It shows a high δ18O value as the otolith size increases. On the other hand, δ18O decreases with the growth of otolith during the larval stage (R=-0.54, n=31). The yearly trend was small and measured values were widely distributed. From the cluster analysis for the initial growth rate, the six clusters (CL*1 – CL*6) resulted. CL*5, 6 (showing high growth) showed higher otoliths δ18O than CL*1, 2 (showing low growth) and it was suggested that CL*5, 6 experienced the lower water temperature range. When converting the difference of otolith δ18O to the water temperature, CL*5, 6 experienced low water temperature as about 1.1 °C. Therefore, it was shown that a positive spiral, in which individuals with high initial growth proactively entered to the low water temperature area and obtained high nutritious diet.