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首页> 外文期刊>Fisheries Research >Bomb radiocarbon analyses validate and inform age determination of longnose skate (Raja rhina) and big skate (Beringraja binoculata) in the north Pacific Ocean
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Bomb radiocarbon analyses validate and inform age determination of longnose skate (Raja rhina) and big skate (Beringraja binoculata) in the north Pacific Ocean

机译:炸弹RadioCarbon分析验证和告知北太平洋长鼻溜冰箱(Raja rhina)和大滑冰(Bingraja Binoculata)的年龄确定

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Age and growth estimates based on growth band counts of sectioned vertebrae have been produced for longnose skate (Raja rhina) and big skate (Beringraja binoculata [formerly Raja binoculata]) populations in the Gulf of Alaska, British Columbia and California. Previous growth studies involving estimates from different laboratories in the USA (Alaska Fisheries Science Center, AFSC; Pacific Shark Research Center, PSRC at Moss Landing Marine Laboratories) and Canada (Fisheries and Oceans Canada, DFO) have produced dissimilar results for either species, highlighting the need for development of a consistent age determination protocol and more importantly an age validation study. Archived large specimens of longnose skate and big skate collected in Monterey Bay, CA, in 1980 and 1981 had minimum preliminary age estimates from vertebral growth band counts old enough to suggest that radiocarbon (C-14) signals from bomb testing conducted in the late-1960s could be used to establish dates of growth band formation. To this end, we micro-milled skate vertebral thin sections, measured Delta C-14 using mass spectrometry, and estimated year of growth band formation based on the estimated age from growth band counts using both unstained and stained preparation methods Non-linear random effects modeling, implemented in a Matkov Chain Monte Carlo (MCMC) simulation, was used to compare the skate Delta C-14 data set to a marine teleost otolith reference chronology for the California Current System. Results showed Delta C-14 measurements for big skate were non-informative as none of the archived samples were old enough for comparison to the reference curve, hence validation of the age estimation approach was not possible. However, for longnose skate, Delta C-14 data were more informative to fit pulse function models and compare results to the reference chronology. Modeling results indicated longnose skate age estimates based on unstained vertebral thin sections were less biased (overestimated to a smaller degree) than estimates based on stained vertebral thin sections. The degree of bias depended on agency ageing criteria, with the least biased age estimates produced by age readers from the AFSC. The AFSC age estimates had about a 70% probability that age estimates of longnose skate was within + / 2 years of the expected age based on the radiocarbon assays. We were able to validate the age estimation methodology for longnose skate and establish criteria for growth band counts, which should now be useful to generate region-specific accurate growth and life history parameters required for more reliable stock assessment approaches.
机译:基于椎骨(Raja Rhina)和大滑冰(Beringraja Binoculata [前raja binococulata])在阿拉斯加,不列颠哥伦比亚省,不列颠哥伦比亚省的湾(Bingraja Binoculata)和加利福尼亚州的群体的年龄和成长估算。以前的成长研究涉及美国不同实验室的估计(阿拉斯加渔业科学中心,AFSC;太平洋鲨鱼研究中心,PSRC在MOSS登陆海洋实验室)和加拿大(渔业和海洋加拿大,DFO)对任一物种产生不同的结果,突出显示需要发展一致的年龄确定方案,更重要的是年龄验证研究。 1980年和1981年,在蒙特雷湾收集的Longnose滑冰和蒙特雷湾收集的大型标本,从椎体增长带算起的最低初步估计,足以建议在末期进行的炸弹测试中的辐射碳(C-14)信号。 20世纪60年代可用于建立增长乐队形成的日期。为此,我们使用质谱法测量的ΔC-14测量的δC-14,以及基于使用未染色和染色的制备方法非线性随机效应的生长带计数的估计年龄的估计年龄的生长带形成年在Matkov Chain Monte Carlo(MCMC)模拟中实施的建模用于将滑板Delta C-14数据集比较加州电流系统的海洋电讯替代电视参考年表。结果表明,大滑冰的Delta C-14测量是非信息,因为没有归档的样本足够大,以便与参考曲线比较,因此不可能验证年龄估计方法。然而,对于Longnose Skate,Delta C-14数据更有信息,适用于适合脉冲功能模型,并将结果与​​参考年表进行比较。建模结果表明,基于未染色的椎体薄切片的Longnose滑冰年龄估计比基于染色的椎体薄截面的估计,偏差较小(高估到较小程度)。偏差程度取决于代理老龄化标准,最不偏向于AFSC的年龄读者的年龄估计。 AFSC年龄估计有大约70%的概率,即长鼻冰鞋的年龄估计是基于无线碳测定的预期年龄的+ / 2年。我们能够验证Longnose Skate的年龄估计方法,并建立增长乐队计数标准,现在应该有助于为更可靠的股票评估方法产生更具体的准确增长和生命历史参数。

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