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首页> 外文期刊>Zoological Studies >Otolith O and C Stable Isotope Compositions of Southern Bluefin Tuna Thunnus maccoyii (Pisces: Scombridae) as Possible Environmental and Physiological Indicators
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Otolith O and C Stable Isotope Compositions of Southern Bluefin Tuna Thunnus maccoyii (Pisces: Scombridae) as Possible Environmental and Physiological Indicators

机译:南部蓝鳍金枪鱼Thunnus maccoyii(双鱼座:Scombridae)的耳石O和C稳定同位素组成可能为环境和生理指标

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摘要

This study evaluated the use of stable isotopic signatures stored in otoliths to study the migratory life history of the southern bluefin tuna (SBT, Thunnus maccoyii). Otolith powders were sequentially collected from the edge to the core for stable oxygen (O) and carbon (C) isotopic analysis. All specimens (n = 11) analyzed showed a 3-stage profile of stable O and C isotope compositions. Values of delta ~(18)O decreased from approximately -1.5%o to -3.0%o in early life, followed by an increase to approximately -1%o at an age of 1 yr, and the values remained at thedelta ~(18)O-enriched level with moderate fluctuations for the remaining lifetime. Hatchling SBT appeared to stay in the spawning ground for approximately 1 mo and then migrate southward, experiencing a temperature decrease of 8-10°C to about 20-25°C until 1 yr old. Water temperatures varied between approximately 15 and 25°C with no evident trend over the remaining life. However, the ambient water temperature might have been overestimated during the subadult to adult stages of the SBT when their thermal conservation ability was fully developed. The otolithdelta ~(13)C profile followed broadly similar trends to those of delta ~(18)O, showing depletion from approximately -6.5%o to -10.5%in the early life stages, followed by abrupt enrichment up to -6% to -8%o at an approximately age of 1 yr. Otolith delta ~(13)C reached a plateau earlier in the 1st year than diddelta ~(18)O and showed greater variation over the remaining life. Interpretation of otolith delta ~(13)C values is complicated, but the results suggest progressive transitions of ontogeny, metabolism, and trophic levels for the SBT. Otolith stable O and C isotope analyses provide continuous information about the migratory lifehistory and contribute to our presently limited understanding of the SBT migratory cycle. http://zoolstud.sinica.edu.tw/Journals/48.1/71 .pdf
机译:这项研究评估了使用保存在耳石中的稳定同位素特征来研究南部蓝鳍金枪鱼(SBT,Thunnus maccoyii)的迁徙生活史。从边缘到核心依次收集耳石粉,以进行稳定的氧(O)和碳(C)同位素分析。分析的所有标本(n = 11)均显示出稳定的O和C同位素组成的3阶段分布图。 δ〜(18)O的值在生命的早期从大约-1.5%o降低到-3.0%o,然后在1岁时增加到大约-1%o,并且值保持在δ〜(18) )富氧水平,在剩余使用寿命内波动适中。孵化的SBT似乎在产卵场中停留了大约1个月,然后向南迁移,经历了8-10°C的温度下降到大约20-25°C,直到1岁。水温在大约15至25°C之间变化,在剩余寿命中没有明显的趋势。但是,当SBT的热保存能力得到充分发挥时,在亚成人到SBT的成年阶段,可能已经高估了周围的水温。 otolithdelta〜(13)C曲线的变化趋势与delta〜(18)O的变化趋势大致相似,在生命的早期阶段从大约-6.5%o耗尽至-10.5%,随后突然富集直至-6%至-8%o在大约1年的年龄。耳石(Otolith delta〜(13)C)在第一年比Diddelta〜(18)O达到了平稳期,并且在剩余寿命中表现出更大的变化。耳石δ〜(13)C值的解释很复杂,但结果表明SBT的个体发育,代谢和营养水平逐渐过渡。耳石稳定的O和C同位素分析可提供有关迁徙生活史的连续信息,并有助于我们目前对SBT迁徙周期的了解有限。 http://zoolstud.sinica.edu.tw/Journals/48.1/71 .pdf

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