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Estimating blue whale skin isotopic incorporation rates and baleen growth rates: Implications for assessing diet and movement patterns in mysticetes

机译:估计蓝鲸皮肤同位素掺入率和巴利安生长率:对神秘者饮食和运动方式的评估

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摘要

Stable isotope analysis in mysticete skin and baleen plates has been repeatedly used to assess diet and movement patterns. Accurate interpretation of isotope data depends on understanding isotopic incorporation rates for metabolically active tissues and growth rates for metabolically inert tissues. The aim of this research was to estimate isotopic incorporation rates in blue whale skin and baleen growth rates by using natural gradients in baseline isotope values between oceanic regions. Nitrogen (δ15N) and carbon (δ13C) isotope values of blue whale skin and potential prey were analyzed from three foraging zones (Gulf of California, California Current System, and Costa Rica Dome) in the northeast Pacific from 1996–2015. We also measured δ15N and δ13C values along the lengths of baleen plates collected from six blue whales stranded in the 1980s and 2000s. Skin was separated into three strata: basale, externum, and sloughed skin. A mean (±SD) skin isotopic incorporation rate of 163±91 days was estimated by fitting a generalized additive model of the seasonal trend in δ15N values of skin strata collected in the Gulf of California and the California Current System. A mean (±SD) baleen growth rate of 15.5±2.2 cm y-1 was estimated by using seasonal oscillations in δ15N values from three whales. These oscillations also showed that individual whales have a high fidelity to distinct foraging zones in the northeast Pacific across years. The absence of oscillations in δ15N values of baleen sub-samples from three male whales suggests these individuals remained within a specific zone for several years prior to death. δ13C values of both whale tissues (skin and baleen) and potential prey were not distinct among foraging zones. Our results highlight the importance of considering tissue isotopic incorporation and growth rates when studying migratory mysticetes and provide new insights into the individual movement strategies of blue whales.
机译:Mysticete皮肤和baleen板中的稳定同位素分析已被反复用于评估饮食和运动方式。同位素数据的准确解释取决于对代谢活性组织的同位素掺入率和对代谢惰性组织的生长率的了解。这项研究的目的是通过使用大洋地区之间基线同位素值的自然梯度来估算蓝鲸皮肤中同位素的掺入率和巴利安的生长率。从三个觅食区(加利福尼亚湾,加利福尼亚现行系统)分析了蓝鲸皮的氮(δ 15 N)和碳(δ 13 C)同位素值和潜在猎物,以及哥斯达黎加巨蛋(Costa Rica Dome)在1996年至2015年之间。我们还从1980年代和2000年代搁浅的六只蓝鲸收集的baleen板的长度上测量了δ 15 N和δ 13 C值。皮肤分为三个层次:基础皮,外皮和皮肤脱落。通过拟合在加利福尼亚湾和加利福尼亚州收集的皮肤地层的δ 15 N值的季节性趋势的广义加和模型,估计平均(±SD)皮肤同位素掺入率为163±91天。加州现行制度。利用三只鲸鱼的δ 15 N值的季节性振荡,估计平均巴利恩生长速率为15.5±2.2 cm y -1 。这些振荡还表明,多年以来,鲸鱼对东北太平洋不同的觅食区具有很高的保真度。来自三只雄性鲸鱼的baleen子样本的δ 15 N值没有振荡,表明这些个体在死亡前仍在特定区域内停留了几年。觅食区的鲸鱼组织(皮肤和巴里)和潜在猎物的δ 13 C值均不相同。我们的结果强调了在研究迁徙神秘者时考虑组织同位素掺入和生长速率的重要性,并提供了对蓝鲸个体运动策略的新见解。

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